42A03SE0026 - Geology Ontario

s i 2-17489
January 20, 1997
ST"" i
CAMECO CORPORATION
& TRI-ORIGIN EXPLORATION LIMITED
1996 DIAMOND DRILLING REPORT^ iV0)
ENGLISH PROPERTY, ONTARlp
English and Semple townships
N.T.S. 42 A/3
42A03SE0026 2 1 7489 ENGLISH
n0
Peter Chubb
010

SUMMARY
The southern portion of the English property consisting of 21 unpatented mining claims (336Ha) and
referred to as the "C" block was the focus of a drilling program. The property is located 50km south of
Timmins, Ontario within the English and Semple townships.
The property lies within the Abitibi greenstone belt of the Superior Province, and is underlain by Archean
mafic and felsic meta-volcanic and meta-sedimentary lithologies. The volcanic lithologies appear to be
stratigraphically equivalent to the Tisdale and Deloro Groups, respectively of the Timmins-Porcupine
Mining Camp. The property straddles the contact between the Deloro and Tisdale Groups, and includes
dacitic quartz-feldspar porphyry flows intercalated with pyroclastic quartz feldspar phyric fragmentals and
a sulphide- and oxide- rich iron formation. The felsic lithologies are overlain by spinifex and cumulate
textured ultramafics and pillowed to massive Fe- and Mg-rich tholeiites of the Tisdale Group.
Mapping and power stripping by Cameco (1995/1996) delineated the surficial extent of the various
lithologies and structure within the property area. Based on this mapping, trenching and geochemical
sampling, a diamond drill program was undertaken.
The diamond drill program completed in November of 1996 consisted of 7 drill holes totalling 1354m that
intersected favourable, highly altered and deformed geology with erratic anomalous gold values. Six of the
seven holes display moderate to strong alteration characterized by sericite, chlorite and graphite in the felsic
volcanics; dolomite, ankerite, fuchsite, serpentine and talc in the ultramafics; and, chlorite, calcite and quartz
in the mafic volcanics. Weakly anomalous gold intervals in the 100's of ppb are present in six of the seven
holes with spikes over Ig/t in holes ENG9602 and ENG9604. Anomalous gold is associated with felsic dike
intrusions (up to 1989ppb Au over 1m) and fuchsite-carbonate-?graphite altered ultramafic volcanics (up
to 1269ppb Au over 1m) in hole ENG9602.
Trace element geochemistry indicates a weak positive correlation between gold and Mo, Ag, As, Pb and
Zn for the different lithologies with the gold bearing graphitic sediments also containing weakly anomalous
Sn.
Based upon the presence of gold and consistently favourable geology and alteration, further work is
recommended. The 1997 work program should include detailed examination of the mafic-ultramafic contact
zone along strike from the diamond drill site near the fold nose of the large scale synform to the southwest,
and to the property boundary to the northeast.
English Project - 1996 Diamond Drill Program

SUMMARY
1.0 Introduction
l. l Purpose of Drill Program
2.0 Property Location and Access
3.0 Topography and Vegetation
4.0 Property Geology
4.1 Geology
4.2 Structure
5.0 1996 Diamond Drilling Program
6.0 Geochemistry
7.0 Conclusions
8.0 Recommendations
9.0 References
Statement of Qualifications
TABLE OF CONTENTS
APPENDICES
Appendix A Diamond Drill Logs
Appendix B Major Oxide, ICP and Gold Assay Data Sheets
Appendix C Maps
English Project - 1996 Diamond Drill Program
42A03SE0026 2.17489 ENGLISH
Page
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l
5
5
5
6
8
21
23
24
25
010C

LIST OF FIGURES
Page
Figure l. Location map of the English Project 2
Figure 2. Claim Map for the "C" Block 3
FigureS. Generalized Geology Map of the "C" Block 7
Figure 4. Schematic Section illustrating alteration disposition 12
LIST OF MAPS
Map l. General Geology Map of the English Property back pocket
Map 2. Vertical Section for ENG9601-04 back pocket
Map 3. Vertical Section for ENG9605-07 back pocket
LIST OF TABLES
Table l. Claim listing of the English Project 4
Table 2. English Project Drill hole Collar Location 10
Table 3. Summary of significant (Mg/t Au) Samples from Drilling 22
Table 4. Average Trace Element Abundances for the Various Lithologies 23
LIST OF PHOTOGRAPHS
Plate 1: A37 NDS Drill at ENG9602 Collar Site
Plate 2: Serpentinized and quartz-carbonate veined ultramafic 11
Plate 3: Fuchsite and quartz-carbonate altered ultramafic 14
Plate 4: Pyritized albitite dike 15
Plate 5: Fault breccia with quartz-carbonate fragments in ultramafic 16
Plate 6: Spinifex textured serpentine rich ultramafic 17
Plate 7: K-feldspar altered tuff breccia 18
Plate 8: Pyritic-graphitic argillite 20
English Project - 1996 Diamond Drill Program

ENGLISH PROJECT
1996 DIAMOND DRILLING REPORT
1.0 Introduction
This report documents the 1996 diamond drill program conducted on the English Project
situated in the English township, N.T.S. 42 A/3, located 50 kilometres south of Timmins,
Ontario (Figure 1). The program consisted of seven diamond drill holes totalling 1354m,
728 gold assay and 728 ICPmultielement analyses obtained from core specimens. A contractor
was used to conduct the diamond drilling (NDS drilling of Timmins) at all seven sites,
with prospector Dan Brunne and geological technician Gregory Pigeau assisting with the
sampling.
1.1 Purpose of Drill Program
Drilling was conducted at specific locations in order to test the spatial and temporal
relationships between the geological environment and mineralization. The test was
conducted in an attempt to establish the relative timing, spatial relationships and
importance of events with respect to gold mineralization.
2.0 Property Location and Access
The portion of the English property covered by the drill program consists of 21
unpatented claims set in the "C" block (Figure 2) situated in the English and Semple
townships. The claims are currently under option by Cameco Corp. from Tri-Origin
Exploration Ltd. The property lies within the M.N.R. administrative district of Sudbury
and the Porcupine Mining Division.
Access is provided to the property via Pine street (south of Timmins) or the Forks River
road (south of South Porcupine) that intersect the east-west Matachewan road. A
powerline road accessible from the Matachewan road provides access along the length of
the "C" block. Numerous logging roads splay off from the main gravel roads providing
good access to various parts of the property. The gravel roads are not maintained during
the winter season thereby limiting access to the property during that time period.
The portion of the property covered by this report consists of the "C" block straddling the
English/Semple townships east-west boundary. The claim group layout for the area
described in this report is illustrated in figure 2 and listed in Table l.
English Project - 1996 Diamond Drill Program

MANITOBA
Legend
A Existing Project
Cameco District Office
100 200 300 400 500km
Scale 1:8,000,000
ONTARIO
QUEBEC
Property Location Map
Compiled By Peler Chubb_____97/OI/H
Droftcd By Cloyton Durbin
Scale: 1:6.000.000
N.T.S.:
Datum:
.Dispositions):
O.o No.:ECG94007
Figure 1

CLAIM MAP
"C" Block
Compied 8* Ptttf Chubb 97/01/H

Table 1. Claim Listing for the English Property "C" Block
block
C
C
C
c c
c
c c
c ccc
c
c c
c
c cc
c c
Claim #
1 147258
1147259
1147260
1147261
1147262
1147263
1147264
1 147265
1 147266
1147267
1147268
1147269
1147270
1147271
1 147272
1155886
1155887
1155888
1155889
1155890
1155891
Work Req.
5400
S400
5400
S400
5400
S400
5400
5400
5400
5400
5400
S400
5400
S400
5400
5400
5400
5400
5400
S400
5400
Claim Units
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
Work Req.
S400
S400
S400
5400
S400
5400
S400
S400
5400
S400
5400
S400
5400
S400
5400
5400
5400
5400
5400
5400
5400
Due date
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
16/07/99
Township
Semple
Semple
Semple
Semple
Semple
Semple
Semple
Semple
Semple
English
English
English
English
English
English
English
English
English
English
English
English

3.0 Topography and Vegetation
The property lies within the Hudson Bay watershed, approximately 70km north of the
divide between the Great Lakes and Hudson Bay watersheds, with the Redstone Creek
draining north into James Bay. The property displays low relief with both lithologic and
esker controlled topographic highs. The region is covered by a thin to moderately thick
veneer of glaciofluvial and glaciolacustrine sediments topped by eolian sands and gravels.
An esker-fan complex (topographic high) in the area trends north-south and runs through
the central portion of the English Township. Rock exposure is limited to approximately
^o of the property with exposure decreasing towards the southeast.
Vegetation consists of moderately sized cedar swamps (2xlkm in size) and forests in the
topographic lows and cedar, jackpine, spruce, white and yellow birch, rock maple, poplar
and balsam in the topographic highs.
Logging activity in the area has resulted in deforestation of approximately 2007o of the
property and continued activity in the southern portion of the English Township is
providing improved access to the property. Winter clear cutting operations are slated for
this year (1996/97).
4.0 Property Geology
4.1 Geology
The property lies at the contact between the Deloro and Tisdale groups with the contact
representing an important stratigraphic marker horizon in the Timmins-Porcupine mining
camp. The Deloro Group consists mainly of felsic volcanics, while the Tisdale Group is
composed mainly of mafic volcanics and ultramafics flows. For a more detailed regional
geological overview the reader is referred to the 1996 assessment report for the English
property (Chubba, 1996).
"C" Block
A detailed geological overview of the "C" block is presented in the 1996 trenching report
(Chubbb, 1996) and mapping report (Chubbc, 1996). The "C" block mapping (Map 1)
outlined a northeasterly plunging synform consisting of a similar stratigraphic section to
that encountered in the "A" and "B" blocks (Chubba, 1996). The stratigraphy'consists of
a basal felsic package of rhyodacite flows, tuffs, crystal tuffs and tuff breccia capped by
oxide and sulphide-rich iron formation and a highly chloritized quartz-eye felsic volcanic.
The felsic package is overlain by ultramafic volcanics belonging to the Tisdale Group.
The ultramafic volcanics consist of spinifex, polysutured and cumulate textured fine to
English Project - 1996 Diamond Drill Program 5

medium grained flows that display variable grainsize and alteration assemblages.
Alteration in the "C" block is typified by pervasive carbonate (ankerite and dolomite),
with discrete zones of fuchsite alteration present and also abundant quartz-carbonate
veining. Grain size is variable and may be a result of carbonate replacement of the host
rock mineralogy.
The mafic volcanics overlying the ultramafics are poorly exposed. At the contact the two
lithologies are difficult to distinguish due to shearing. The mafic volcanics at the contact
are characterized by an intense foliation and chlorite-carbonate alteration (and may be
ultramafic). The central and upper portions of the mafic volcanics consist of fine grained
variably chloritized massive to pillowed flows reflecting cyclic changes from Fe-tholeiite
to Mg-tholeiites magmas. The mafic package is intruded by a series of gabbroic sills and
dikes.
Later felsic (albitite) and intermediate dikes, some of which are temporally associated with
nearby intrusive bodies intrude the stratigraphy. The albitite dikes have undergone
deformation and are observed to be folded, stretched and disjointed by later deformation
events (D2 8c D 3). The syenite dikes appear less deformed with the mafic dikes the least
deformed.
4.2 Structure
Recent structural studies in the Timmins region (Bleeker, 1995; Heather, 1995) have
identified pre-Timiskammg polyphase folds indicative of at least two early fold events (D0
(fe D,). These predominantly "mushroom type" fold interference patterns were faulted,
unroofed and truncated by a pre-Timiskaming unconformity which was subsequently
tightly folded around upright axial planes with shallow to moderately plunging axes (30-
40"). The youngest folding is related to strike-slip structures and is manifested by steeply
plunging asymmetric S- and Z-folds.
Map units on the OGS maps (ace. report 231; Bright, 1984) define large scale east- to
east-northeast trending fold structures (deformed hooks, synforms and antiforms). To the
east of the property area near West Nighthawk Lake and Kitchiming Lake, as well as
south of English Lake, map patterns define closed, doubly plunging structures suggesting
the presence of polyphase folding. The D, event responsible for thrust folding and the
regional penetrative foliation was subsequently folded by the north trending D 2 event.
Structural symbols shown on the OGS map suggest the dominant foliation (S,) is broadly
conformable with the primary layering of the units (S 0), although around fold closures,
two sets of foliation orientations are common. One foliation is conformable to the gross
lithologic layering and a second foliation is broadly coincident with the interpreted axial
English Project - 1996 Diamond Drill Program O

Plate 2 : Intensely altered ultramafic volcanic displaying serpentinization and abundant quartz-
carbonate veining parallel and subparallel to the foliation. Pyrite mineralization is present as fine
euhedral crystals upto 3 07o volume. Deformation can be observed by the folding of the quartz-
carbonate veins. Interval from hole ENG9601 at a depth of 195m.

l
Mafic metavolcanic Si gabbro
Ultramafic metavolcanic
Felsic metavolcanic
D 1 thrust
D 2 synform, antiform
D 3 synform, antiform
Ductile high strain zone
Cameco
250 500 750 10GO
Scale 1:25,000
ENGLISH
PROPERTY
Generalized Geological Sketch
of the Area Underlying
Blocks "B", "C" and "D"
Bf Q. Thomoa 96/12/11
By H, Q.
Scdc 1:Z5.0QO
Figure 3

surface trace of the folds.
Previous mapping by Cameco shows the development of deformed quartz veins (Q,) in
the mafic volcanics of the Janeway trench (Chubbb , 1996) that reflect an early episode of
deformation (D0) which predates the D, thrusting and S, fabric development.
A second set of quartz veins (Q 2) were emplaced prior to or during the regional
penetrative foliation (D,) event. The quartz veins (Q2) were progressively transposed into
a plane of flattening by the D 2 event that is also responsible for the development of the
regional synform.
A late set of north-northwest trending open folds (D 3) are superimposed on the northwest
limb of the synform (D2).
The feldspar phyric and aphyric felsic dikes and aphyric mafic dikes are overprinted by
a S, fabric associated with D, but later deformed by D 2 (folding and boudinage features).
5.0 1996 Diamond Drilling Program
A 1354m drill program commenced on the 22rid^Octobj;rJj)96^and was completed on the
7th November^ 1996. The drill program tested various aspects of the mafic volcanics,
ultramafics and the felsic volcanics within the "C" block of the property as outlined in
detail below and illustrated on Map 1.
Hole ENG9601 was collared in the mafic volcanics 140m south of the mafic/ultramafic
contact to test:
1) Whether gold mineralization increases with depth.
2) Whether the fuchsite alteration located within the ultramafics on surface persists at
depth and its relationship to the mafic contact, dikes and mineralization.
3) Whether the I.P. anomaly is an indication of mineralization along the contact.
Hole ENG9602 was collared within the ultramafics to test:
1) Whether gold mineralization increases with depth.
2) Whether the fuchsite alteration located within the ultramafics on surface" persists at
depth and its relationship to the felsic contact, dikes and mineralization.
3) Whether the strong I.P. anomaly is an indication of gold mineralization at depth along
the contact and its relationship to the iron formation.
English Project - 1996 Diamond Drill Program

Hole ENG9603 was collared within the ultramafics near the felsic contact to test:
1) Mineralization at the felsic/ultramafic contact at shallow depth.
2) The change in direction of the felsic-ultramafic contact near surface.
3) The strong I.P. anomaly unexposed at surface that is interpreted to be related to pyrite
mineralization within the deformed tuff breccia and sulphide and oxide iron formation.
Hole ENG9604 was collared within the felsic volcanics approximately 80m north of the
felsic/mafic contact to test:
1) Mineralization within the mafic volcanics and at the mafic/ultramafic contact at 100m
depth.
2) Mineralization within the ultramafics and felsic lithologies.
Hole ENG9605 was collared in the felsic volcanics to test:
1) The potential for gold associated with iron formation along strike from hole ENG9604:
2) The strong I.P. anomaly unexposed at surface that is believed to be related to possible
gold mineralization within the sulphide and oxide iron formation or structural feature.
3) The ultramafic/mafic volcanic package at depth for possible mineralization or trace
element changes indicating direction to more significant gold values.
Hole ENG9606 was to be collared in a cedar swamp overlying the felsic volcanics and
facing south towards the felsic/ultramafic contact but instead was collared in the mafic
volcanics facing away from the area of interest and was therefore halted. The hole was
supposed to test:
1) The ultramafic/mafic volcanic package at depth for possible mineralization or trace
element changes indicating direction to more significant gold values.
Hole ENG9607 was collared in the mafic volcanics along strike from ENG9601 to test:
1) The ultramafic/mafic volcanic package at 100m depth for possible mineralization and
trace element changes that may indicate a direction leading to more significant gold values
associated with an increase in alteration.
English Project - 1996 Diamond Drill Program

Hole#
ENG9601
ENG9602
ENG9603
ENG9604
ENG9605
ENG9606
ENG9607
TOTAL
Claim #
1155889
1155889
1155891
1155891
1155888
1147272
1 147272
Location
L6E,
L6E, 275N
L6E,
L6E,
LIE, 2+85N
LIE,
130N
535N
688N
1 + 10N
L2E , BLO
Bearing
315-,
315-,
-45"
315',
-45"
135",
110",
110',
no 0 ,
-45"
-45 '
-45"
-50'
-50"
Table 2. English Project 1996 Drill Collar Locations on the "C" Grid
Depth (m)
222
349
154
116
304
34
175
1354m
Overall results from the drill program suggest that there is continuiancy of the various
lithologies with depth. Alteration is pervasive and strong with the development of
large alteration zones temporally associated with regional and local deformation (D 3)
and the emplacement of felsic-intermediate dikes.
The two cross sections based upon drilling on L6E and a composite based on drilling
on L2E and LIE illustrate the interpretation for the development of intense fuchsite
alteration. The cross sections for LIE and L6E indicate that the fuchsite alteration is
constrained to tight isoclinal folds temporally associated with the D 3 deformation and
further intensified by the emplacement of felsic and intermediate dikes. The overall
shape of the alteration can best be described as a subvertically oriented curviplanar
(see figure 4) block that on the cross section is illustrated as a curvilinear sigmoidal
feature across the section.
Sulphide mineralization is widespread and locally enriched mineralized zones are
observed along the margins of intruding dikes and within intensely altered zones.
The following is a summary of the highlights of the individual diamond drill holes
with the sections for hole ENG9601-04 presented on Map 2 and the remaining sections
on Map 3:
DDH ENG9601 tested the mafic volcanics and ultramafic contact at 100m depth as well
as a weak IP anomaly interpreted as the contact between the mafic and ultramafic
volcanics. The mafic volcanics consist of a series of massive flows and tuffaceous units
English Project - 1996 Diamond Drill Program 10

Felsic
Volcanics
Legend
Ultramafic
Volcanics
/^~^\^,^ D 1 thrust
J/ _ to Do synform
^ z y
I -+. 0 3 antiform
Mafic Volcanics
r*
Cameco
ENGLISH
PROJECT
Schematic of the Curviplanar
Distribution of Fuchsite Alteration
within the Ultramafic Volcanics
Compiled Bf P eter Chubb 97/01/22 D.g No.:ENC9700l
Drafted B Y- Cloyton Ourbin
Scole: not to scole
N.T.S.: Ootu m:
J)i3po5ilion(s): ^ .
Figure 4.

that have undergone variable degrees of recrystallization and for the most part are very
weakly foliated. The mafic volcanics display variable alteration dominated by chlorite
and calcite with epidote and hematite restricted to the quartz veins (Q,). Quartz veining
is prevalent (up to 5 07o of the rock volume), with disrupted and highly folded (Q,) veins
and later less altered and deformed quartz veins (Q2). Mineralization in the mafics
consists of thin intervals of finely disseminated to coarse pyrite up to P/o volume.
The ultramafic volcanics are massive to spinifex textured and are pervasively carbonatized
(dolomite and ankerite), talcose and serpentinized with minor fuchsite present in the
quartz-carbonate veins (Q2). Mineralization within the ultramafics is sporadic and consists
of trace to \ 0A pyrite and minor pyrrhotite. The stratigraphy is intruded by a series of
grey to pink thin syenite dikes that display quartz veining (Q 2) and f-2% pyrite
mineralization. One assay of 139ppb over 1m was obtained within a mafic pyroclastic.
DDH ENG9602 tested the ultramafic volcanics at depth. The ultramafic volcanics consist
of massive to spinifex textured flows that display strong and pervasive carbonate alteration
with the other alteration assemblages consisting of serpentine, silica (Q2), talc and
fuchsite. Barren quartz-carbonate veining (Q2 and/or Q,?) is present as subparallel to
parallel cm wide veins.
The ultramafic volcanics are intruded by a series of albitite dikes up to 40m in width and
thin syenite (l-3m wide) and mafic dikes. The felsic and intermediate dikes are well
mineralized with up to 5*^o finely disseminated pyrite. Sporadic weakly anomalous values
in the lOOppb range were obtained from the ultramafic volcanics. Weakly anomalous
gold values in the lOOppb range, were obtained over 3-4m intervals in all of the
lithologies present with a high of 1989 ppb over 1m in a felsic dike, and 1269ppb in a
fuchsitic and ?graphitic ultramafic volcanic.
DDH ENG9603 tested the ultramafics at the felsic contact but due to folding did not
penetrate the contact. The ultramafic volcanics consist of massive to spinifex textured that
display variable degrees of alteration dominated by serpentine-talc-carbonate-silica to
fuchsite-carbonate-silica. Carbonate alteration consists of dolomite and ankerite with silica
alteration developed as thin zones of quartz flooding or discrete carbonate-quartz veins
(Q2). Sulphide mineralization is variable with pyrite and pyrrhotite present in f-2%
abundances. The ultramafic volcanics are intruded by numerous felsic to intermediate
dikes that also contain pyrite mineralization. Weakly anomalous gold assays in the 100
of ppb's are present in both the ultramafic volcanics and dikes.
English Project - 1996 Diamond Drill Program 13

ENTIMETRES
Plate 3: Fuchsite and quartz-carbonate altered ultramafic flow with J-2% finely disseminated
pyrite mineralization. This interval is located along the margin of a felsic (albitite) dike.Two
series of quartz-carbonate veining are present with the later veining subparallel to the foliation
and older quartz-carbonate veins. This interval is from hole HNG9602 at a depth of 37m.

l t- 3 4 b 6 7
CENTIMETRES
Plate 4: F ine grained felsic (albitite) dike containing 2-3 07o finely disseminated pyrite and limited
quartz-carbonate veining. The albitites are massive and appear undeformed yel on surface can
be seen to be folded and/or disjointed. This interval is from hole ENG9602 at a depth of 38m.

Plate 5 : Fault breccia set within a serpentinized and quartz-carbonate rich ultramafic flow.
Fragments consist mainly of the quartz-carbonate vein material while the host serpentinized
ultramafic forms a soft fine grained matrix. Interval from hole ENG9602 at a depth of 74m

Plate 6: Spinifex textured ultramafic flow displaying increased pyrite mineralization along the
margin ol" a syenite dike. The ultramafics are highly carbonatized with minor serpentinization.
Pyrite mineralization decreases sharply away from dike. Interval from hole ENG9602 at a depth
of 98m.

Plate 7 : K-feldspar altered tuff breccia (Deloro Group). The fragment contacts are diffuse as
a result of interaction with hydrothermal fluids passing through the porous matrix. Interval from
hole ENG9604 at a depth of 55m.

DDH ENG9604 tested the felsic-ultramafic contact at depth. The felsic volcanics consist
of intercalated tuff, lapilli tuff and tuff breccia with minor argillaceous components.
Alteration is dominated by sericite with minor chlorite, blue qtz-eyes and kfeldspar
concentrated within the matrix. Fragments are for the most part sericitized with minor
kfeldspar present. The contact with the overlying ultramafic volcanics is sharp and
unmineralized:
The ultramafics volcanics consist of massive to spinifex textured that are variably altered
to serpentine-talc-carbonate and fuchsite-carbonate with minor silica (Q,?). Alteration is
intensified towards the margins of the intruding dikes. Sulphide mineralization in the
ultramafic volcanics consists of pyrite and pyrrhotite developed as fine disseminations that
display an intensification towards the dike margins. The entire stratigraphy is intruded
by abundant felsic-intermediate dikes that are all mineralized with finely disseminated
pyrite.
Gold assays from this drill hole display weakly anomalous values in the 100's of ppbs in
the felsic-intermediate dikes, with a high of 1026ppb over 30cm from a fuchsitic
ultramafic volcanic adjacent to a syenite dike.
DDH ENG9605 tested the felsic-ultramafic contact at depth. The felsic volcanics consist
of a highly strained package of tuff, lapilli tuff and tuff breccias intercalated with thin
intervals of fine sediments capped by a massive sulphide iron formation and graphitic
argillite horizon. Alteration is dominated by sericite and quartz with minor chlorite and
thin intervals of kfeldspar and graphite (rare).
Sulphide mineralization consists of finely disseminated, coarse euhedral pyrite set within
fractures or along the margins of fragments. Framboidal and botryoidal pyrite is present
within the graphite horizon.
The ultramafics consist of massive to spinifex textured ultramafics that are dominated by
serpentine and carbonate (dolomite and ankerite) with minor silica, talc and fuchsite.
Sulphide mineralization is dominated by pyrite with minor pyrrhotite present as fine
disseminations up to 2 07o volume.
The stratigraphy is intruded by a series of albitite and syenite dikes that contain up to 207o
pyrite as fine disseminations. Gold assays over lOOppb are erratic but are present in all
of the lithologies with a high of 370ppb obtained from the graphitic sediments.
English Project - 1996 Diamond Drill Program

Plate 8: Py rite-graphitic argillite (Deloro Group) set within the Sulphide rich iron formation.
Some of the pyrite appears framboidal while other sections appear to be sulphide fragments.
Interval is from hole ENG9605 at a depth of 94m.

DDH ENG9606 was expected to test the flesic/ultramafic contact at shallow depth, but
was collared in the mafic volcanics facing away from the area of interest and therefore
terminated at a depth of 34m. The geology of the hole consisted of massive mafic
volcanics with chlorite alteration and minor quartz-calcite veining present.
DDH ENG9607 tested the mafic-ultramafic contact at 80m depth. The mafic volcanics
are dominated by chlorite and calcite alteration with variable quartz-calcite veining.
Sulphides are restricted to finely disseminated pyrite at ^"/o abundance within narrow
intervals. The contact between the ultramafics and mafic volcanics is sharp and
dominated by serpentine with trace coarse pyrite present.
The ultramafics are massive to spinifex textured with alteration dominated by serpentine,
talc, dolomite and minor ankerite and silica. Fuchsite is also spatially associated with the
abundant quartz-carbonate veins (Q 2).
Sulphides are present as finely disseminated pyrite within narrow intervals associated with
the altered and fuchsite rich margins of intruding felsic-intermediate dikes. The only gold
assay over lOOppb was obtained from a 1.2m section of syenite dike that ran 353ppb.
6.0 Geochemistry
A total of 728 gold assay and 728 ICPmultie iement analyses for drill core samples were
obtained during the 1996 diamond drill program on the English project. Samples were
analyzed by Swastika Laboratories in Swastika, Ontario using Fire Assay l AA method for
gold assay and ICPmu |tielement scan for 30 trace elements.
Gold anomalies MOOppb are present in the mafic, ultramafic and felsic volcanics
associated with highly altered lithologies or in the presence of iron formation. Gold
anomalies are also present within the felsic and intermediate dikes. Gold mineralization
is spatially associated with the felsic-intermediate dike emplacement within the ultramafic
volcanics.
English Project - 1996 Diamond Drill Program 21

Hole#
ENG9602
ENG9602
ENG9604
Rock Type Interval Width (m)
Felsic/Int. 41.8-42.8 1
Dike
Ultramafic 321.3-322.3 1
Ultramafic- 107.2-107.5 0.3
Syenite
contact
Au (g/t) Alteration
1.989 Ag, Pb, Mo, Zn,
Pe, Cu, As, Si,
Ca
1.269 Fe, Carb, ?Fsch,
Ag, As, Cu, Zn
1.029 Sil, Kfelds, Carb,
Mg, Pb,
Fsch
Table 3. Summary of Significant ^Ig/t) Gold Intersections obtained from the Drill Program
Trace element geochemistry indicates that there are a number of positive but weak
correlations (Table 3) between gold mineralization and Ag, As, Cu. Mo, Zn, Pb, Ca,
and Mg. The trace element geochemistry in conjunction with field observations and
surface major element geochemistry indicates that large scale hydrothermal activity in
the area has taken place, resulting in the formation of extensive carbonate alteration
zones (calcite in mafics, and ankerite-dolomite in ultramafic volcanics) and smaller
more distinct zones including fuchsite (ultramafic volcanics), kfeldspar (sediments),
silica (mafic, ultramafic and felsic volcanics).
Average trace element abundances are illustrated in Table 4. The presence of spot
highs that affect the overall STD for all of the rock types is indicative of massive
chemical transfer between the different rock types. This transfer of fluid through the
various lithologies deposits specific elements within micro-environments conducive to
precipitation.
English Project - 1996 Diamond Drill Program 22

Table 4. Average Trace Element Abundances for the Various Lithologies
graphitic sed.
felsic/int. dike
felsic vole.
albitite
iron formation
int. dike
mafic vole.
syenite
ultramafic
avg
std
avg
std
avg
std
avg
std
avg
std
avg
std
avg
std
avg
std
avg
std
Au ppb
178
95
538
629
16
29
94
90
209
79
41
69
9
12
47
113
31
108
Ag
1.00
0.93
0.57
1.05
0.09
0.37
0.02
0.13
3.33
0.47
0.00
0.00
0.00
0.00
0.04
0.23
0.20
1.99
Al
1.07
0.65
0.48
0.11
1.92
0.91
0.38
0.35
0.58
0.25
1.21
0.95
3.25
0.64
1.59
0.90
1.83
0.71
As
25.7
16.8
3.6
4.4
4.3
6.8
1.2
3.2
33.3
4.7
3.6
6.1
7.5
9.2
3.5
5.9
2.8
5.4
Ba
10.7
12.2
8.1
4.8
15.1
12.9
42.7
47.0
0.0
0.0
147.9
204.2
26.3
36.8
173.8
207.8
48.9
79.4
Bi
0.00
0.00
0.00
0.00
0.00
0.00
0.04
0.46
0.00
0.00
0.00
0.00
0.00
0.00
0.00
0.00
0.03
0.56
Ca
1.25
1.16
4.29
0.81
3.07
1.09
2.13
1.22
0.20
0.08
5.09
1.13
4.43
2.22
4.05
1.22
5.07
1.74
Co
37.1
16.5
39.3
5.9
17.7
6.7
14.5
6.4
52.7
4.5
36.8
25.0
40.3
16.6
* note gold in ppb with the rest of the trace elements in pprn except Al, Ca, Fe, Mg, and Na that are in "/o.
* a positive correlation exists between Au and Ag, As, Cu, Pb, and Zn
29.3
8.2
46.2
14.6
Cr
491
394
112
38
90
53
154
62
150
H
394
469
131
89
261
222
749
385
Cu
257
283
183
70
30
19
19
19
35
6
50
30
151
128
54
36
52
32
Fe
11.19
7.42
6.60
0.50
7.27
3.01
1.97
1.06
19.33
0.47
4.56
1.60
5.92
1.59
3.79
0.85
4.52
1.24
Mg
1.24
0.74
2.03
0.10
1.35
0.38
0.98
0.57
0.42
0.04
2.04
0.31
1.78
0.27
2.00
0.32
2.35
0.23
Mn
693
504
1007
63
2496
884
365
234
760
196
1141
718
1113
346
701
212
960
323
Mo
10.0
10.1
2.3
2.7
1.8
6.1
0.7
2 t
4.7
0.9
0.3
1.0
0.3
1.9
0.3
1.1
0.1
0.5
Na
0.00
0.00
0.03
0.01
0.03
0.02
0.04
0.02
0.02
0.00
0.01
0.01
0.02
0.01
0.02
0.02
0.00
0.01
Ni
251
262
76
H
28
17
30
40
80
5
137
213
125
115
146
112
438
214
P
289
230
416
332
479
219
1138
497
350
37
1261
726
256
265
1521
516
288
421
1'b
32.1
25.0
1.9
2.0
0.8
3.0
2.5
7.1
82.0
8.6
1.4
3.0
0.0
0.0
0.9
3.6
0.1
0.7
Sb
0.71
1.75
0.00
0.00
0.07
0.57
0.00
0.00
3.33
2.36
0.00
0.00
0.00
0.00
0.00
0.00
0.00
0.00
Se
4.29
3.69
15.14
3.52
4.57
2.57
1.64
2.22
0.33
0.47
9.86
5.51
15.09
7.76
9.43
6.05
14.29
3.50
Sn
12.9
24.3
0.0
0.0
0.0
00
0.0
0.0
0.0
0.0
0.0
0.0
0.0
0.0
0.0
0.0
0.0
0.0
Sr
40.9
28.1
106.9
37.2
75.8
82.4
233.3
148.7
12.7
2.5
410.0
213.5
58.7
34.0
228.5
128.7
224.1
114.7
Ti
13.9
9.6
4.0
2.0
18.8
13.6
18.8
10.2
6.0
28
25.1
12.6
874.2
745.3
112.2
247.3
54.5
130.2
V
23.7
21.3
19.9
4.2
20.9
15.0
4.6
3.4
2.7
3.8
24.6
29.4
113.8
38.1
41.3
42.7
48.2
32.8
Y
2.00
0.93
3.00
1.31
2.91
1.18
4.15
2.11
1 33
0.94
6.36
269
6.47
3.09
7.09
2.30
3.35
1.74
Zn
95.7
43.4
59.3
6.9
134.4
147.3
24.9
14.3
38.0
8.6
57.4
39.3
85.5
69.8
51.4
20.6
42.0
23.5
Zr
12.0
4.8
9.9
3.5
9.2
3.1
6.0
4,5
9.3
4.1
7.1
2.5
8.3
4.3
5.8
4.5
7.5
2.9

7.0 Conclusions
The 1996 diamond drilling program on English has shown that:
1) The stratigraphy observed at surface continues to depth but the thickness of the
various lithologies does vary due to deformation. The oxide- and sulphide-iron
formation is developed as discontinuous lenses up against the felsic ultramafic contact.
2) The felsic volcanics are pervasively sericitized with minor Kfeldspar-chlorite and
calcite present. Alteration is pervasive within the ultramafics but displays variable
mineral assemblages with either serpentine-talc-carbonate-quartz or fuchsite-carbonate-
quartz present. The fuchsite alteration appears to be spatially related to areas intruded
by numerous felsic-intermediate dikes and intense quartz-carbonate veining within
highly deformed zones. The mafic volcanics are recrystallized and chlorite-calcite rich
with quartz-epidote-chlorite and minor hematite developed within veins.
3) Elevated gold values obtained from the iron formation and graphitic argillaceous
sediments are not directly correlative to the sulphide content. Gold in the felsic-
intermediate dikes and intensely altered dike/host rock margins display a weak
association with pyrite.
4) Trace element geochemistry of samples obtained from the core display positive
correlations between Ag, Au, As, Mo, Pb, Zn, and Ca. The graphitic sediments as
well as having similar trace element anomalies like the other lithologies also have
weak Sn anomalies.
5) The timing of gold mineralization can be related to two separate events: The first
event is remobilization/redeposition of gold related to the D 2 and D 3 deformation
episodes that allowed massive fluid flow through the various rock types. The second
event represents a syn- or post gold remobilization/introduction associated temporally
with the emplacement of felsic-intermediate dikes and the formation of associated
contact aureoles.
English Project - 1996 Diamond Drill Program 24

8.0 Recommendations
The following recommendations based on drilling and previous work for this part of
the property:
1) Prospecting, detailed mapping and trenching are warranted to the southwest
(foldnose and limb area) and northeast of the drill sites to determine the local
structural complexities, alteration and mineralization.
English Project - 1996 Diamond Drill Program 25

9.0 References
Bleeker, W. 1995. Surface geology of the Porcupine Camp; in Tectonics and
metallogeny of the Archean Crust in the Abitibi-Kapuskasing-Wawa region,
ed. Heather, K.B. et al., Geological Survey of Canada Open File 3141, 148p.
Bright, E.G. 1984. Geology of the Ferrier Lake-Canoeshed Lake Area, District of
Sudbury; Ontario Geological Survey Report 231, 60p. Ace. Maps 2289, 2290,
2291
Chubba, P.C., Panagapko, D., and Thomas D. 1996. 1996 Assessment Report of the
English Property, English and Zavitz townships, N.T.S. 42 A/3; Cameco
Corp. 32p.
Chubbb, P.C., Faber, A., and Thomas D. 1996. 1 996 Trenching Report - English
Property, English and Semple townships, N.T.S. 42 A/3; Cameco Corp.
27p.
Chubbc, P.C., Panagapko, D., Turcotte, M., Faber, A., Brunne, D. 1 996 Geological
Mapping Report "C" Block - English Property, English and Semple
townships, N.T.S. 42 A/3; Cameco Corp. 25p.
Heather, K.B., Percival, J.A., Moser, D. 8z Bleeker, W. 1995. Tectonics and
metallogeny of the Archean crust in the Abitibi-Kapuskasing-Wawa
Region, ed. Heather, K.B. et al., Geological Survey of Canada Open File
3141, 148p.
Matthews, R. and Simard, J. 1996. 1 996 Assessment Report - A Technical Report
on Geophysical Work (Induced Polarization Survey) on the English
Project, English Township, Ontario. SAGAX and Cameco Corp.
Pyke, D.R. 1978. Geology of the PeterLong Lake Area, Districts of Timiskaming
and Sudbury; Ontario Geological Survey Report 171, 53p. Ace. Map 2345
Pyke, D.R. 1982. G eology of the Timmins Area, District of Cochrane; Ontario
Geological Survey Report 219, 141p. Ace. Map 2455
Smith, J.P., Spooner, E.T.C., Broughton, D.W., and Ploeger, F.R. 1993. Archean Au
-Ag-(W) Quartz Vein/Disseminated Mineralisation within the Larder Lake
-Cadillac Break, Kerr Addison -Chesterville System, North East .Ontario,
Canada, Ontario Geoscience Research Grant Program, Grant No. 364;
Ontario Geological Survey, Open File Report 5831, 31 Op.
English Project - 1996 Diamond Drill Program 26

CERTIFICATE
I, Peter Chubb, of Apt# 201, 1490 Kelly Lake Rd., Sudbury, Ontario, P3E 4L9, do hereby certify
that:
I am currently employed as a Geologist by Cameco Corporation,
1349 Kelly Lake Road, Unit #6, Sudbury, Ontario, P3E 5P5
I graduated from Carleton University in 1989 with a Bachelor
of Science degree (honours) in Geology, and Laurentian
University in 1994 with a Masters of Science degree (1st
Class) in Geology. I have been practicing my profession
continuously since graduation.
I am a member in good standing of the Geological Association
of Canada and the Sudbury Geological Discussion Group.
I am directly responsible for the work outlined in this report
and was present on the property when the work was being
carried out.
Signed at Sudbury, Ontario, this 10th day of January, 1997.
Peter T.A. Chubb
Geologist, M.Sc.

APPENDIX A
Diamond Drill Logs
for
English Property 1996 Drill Program

PROPERTY: English
HOLE No.: ENG9601
Collar Eastings:
Collar Northings:
Collar Elevation:
483399.00
5319531.00
O . 00
Contractor was NDS Drilling of Timmins, Ont.
FROM TO
0.0 15.0
LITHOLOGICAL DESCRIPTION
CASING IN OVERBURDEN (Ob)
TISDALE GROUP
Cameco Corporation
DIAMOND DRILL LOG
15.0 22.8 MAFIC VOLCANICS (lp?-c) The mafic volcanics are composed
of a series of fine grained dark green tuffaceous layers
intercalated with fine to medium grained massive flows
and pillowed mafic volcanics. Quartz-carbonate veins are
usually less than 5mm wide and barren. There are three
types of quartz veins present: type l is the oldest
quartz vein type and appears to be strongly disrupted and
contains less than 10V chlorite; type 2 are generally
less than 1mm wide, folded and weakly disrupted and are
at a high angle to the foliation; and, type 3 are white
translucent and parallel to the foliation with fracture
density up to 5%. Alteration in this section is
dominated by chlorite, lesser amounts of calcite and
minor quartz veining up to S \ volume. Alteration haloes
are preserved about some of the quartz carbonate veins
extending up to 20mm and consisting of finely
disseminated pyrite up to 104, calcite up to I0 !i,
chlorite up to 31 and sericite up to Sir. Mineralization
is characterized by fine to coarsely disseminated pyrite
within type l quartz veins and thin chlorite veinlets.
Collar Inclination: -45.00 .
Grid Bearing: 315.00
Final Depth: 222.00 metres
Hole collared in claim # 1155889
SAMPLE No. FROM
96001
96002
96003
19.20
20. 75
21. 75
Logged by: Peter Chubb
Date: 22/10/96-25/10/96
Down-hole Survey: acid
ASSAYS
TO WIDTH Au (ppb)
19. 70
21.75
22 . 75
0. 50
l . 00
1. 00
39
NIL
2
HOLE No: ENG9601

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: Engli sh
HOLE No.: ENG9601 Page 2
FROM TO LITHOLOGICAL DESCRIPTION
Patchy disseminations and clots of pyrite up to 2 \ volume
are also present along fractures and fragment boundaries.
Section is moderately soft and nonmagnetic. Magnetic
susceptibility readings are as follows: 5:0.96 at 1 5m.
22.S 5 5.5 MAFIC VOLCANICS PYROCLASTIC (lac) Similar to the above
unit but no pillowed volcanics and more homogenous
looking. Various lapilli tuff horizons are up to 3m
thick. Section is intruded by thin intermediate dikes up
to 20cm in width at 50 degrees c.a. that make up 14 of
the total volume. Alteration is similar except for
a 10cm wide quartz carbonate vein that displays spotty
fuchsite alteration at the 23.1m section. This section
appears coarser grained in general with larger tuffaceous
fragments. Alteration continues to be dominated by
chlorite and calcite with quartz veining also present.
Quartz veins appear to be discontinuous and folded or
disrupted. Sulphide mineralization is present in trace
amounts as fine disseminations of pyrite with lesser
chalcopyrite. Clots of pyrite are also developed but are
rare up to 14 volume. The core is soft and is variably
magnetic. Magnetic susceptibility readings are as
follows: 5:0.69 at 27m, 5:0.65 at 32m, 5:0.77 at
36m, 5:0.98 at 39m, 5:0.77 at 42m, 5:0.53 at 45m, 5:0.96
at 48m, 5:3.36 at 51m, 5:24.0 at 52.5m.
55.5 68.4 MAFIC VOLCANIC/INTRUSIVE (Sa/lac) Similar to the
previous section except that leucoxene is more prevalent
SAMPLE No. FROM
96004
96005
96006
96007
24.00
25.00
39.00
40.00
96008 59.30
TO
25.00
26.00
40.00
41. 00
59.80
ASSAYS
WIDTH Au (ppb)
1.00
1.00
1. 00
1.00
0.50
3
3
26
NIL
15
HOLE No: ENG9601

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9601 Page 3
FROM TO LITHOLOGICAL DESCRIPTION
and grain size is finer. This section maybe a fine
grained gabbro. Some of the quartz carbonate veins
display brecciation features with fragments of wallrock
included. Sulphides are limited to finely disseminated
pyrite along fractures and in association with quartz-
carbonate veins. Magnetic susceptibility readings are as
follows: 5:1.0 at 54m, 5:8.58 at 60m, 5:0.98 at 63m.
68.4 68.6 FAULT ZONK (f.z.) Highly chloritic blocky
zone with fragmented quartz veins but no mineralization.
Dry fault no cementing fluids.
68.6 95.6 MAFIC VOLCANIC/INTRUSIVE (Sa/lac) Similar to
the previous section except that leucoxene is more
prevalent and grain size is finer. This section maybe a
fine grained gabbro. Some of the quartz carbonate veins
display brecciation features with fragments of wallrock
included. Sulphides are present in trace amounts and
limited to finely disseminated pyrite along fractures and
within quartz-carbonate veins. Limited sections of core
less than 1m wide contain coarser pyrite up to 2%
abundance. Magnetic susceptibility readings are as
follows: 5:1.04 at 66m, 5:0.71 at 69m, 5:0.73 at 72m,
5:0.79 at 75m, 5:0.75 at 78m.
95.6 101.0 MAFIC PYROCLASTIC (lac) Tuffaceous fine grained
and dark green in colour this mafic volcanic. Sulphides
are present in trace amounts and limited to finely
SAMPLE No. FROM TO
96009
96010
96011
68 . 00
78 .60
87.00
69.00
79.60
88.00
ASSAYS
WIDTH Au (ppb)
l .00
1.00
1.00
14
2
NIL
HOLE No: ENG9601

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9601 Page 4
FROM TO LITHOLOGICAL DESCRIPTION
disseminated pyrite along fractures and within quartz-
carbonate veins. Limited sections of core less than 1m
wide contain coarser pyrite up to 2% abundance. Magnetic
susceptibility readings are as follows: 5:1.04 at 66m,
5:0.71 at 69m, 5:0.73 at 72m, 5:0.79 at 75m, 5:0.75 at
78m, 5.061 at 84m, 5:0.73 at 87m, 5:0.53 at 90m, 5:0.63
at 93m, 5:0.63 at 96m, 5:0.77 at 99m.
100.0 115.0 FAULT ZONE (f. z.) Blocky chlorite mafic
volcanics within a series of 1m wide faults consisting
of blocky fragments of strongly foliated vein and rock
material. The faults are separated by strongly foliated
chlorite tuffs and lapilli tuffs. Sulphide
mineralization is pervasive and consists of finely
disseminated pyrite along fractures and foliation planes
up to 2*. Magnetic susceptibility readings are as
follows: 5:0.77 at 102m, 5:0.75 at 105m, 5:0.55 at 108m,
5.049 at 114m.
115.0 147.0 MAFIC PYROCLASTIC (lac) Tuffaceous fine
grained and dark green in colour this mafic volcanic is
intruded by thin medium grained mafic dikes. Thin
mineralized quartz vein related albitized, feldspar
altered syenite dikes are abundant below 141m depth. M
type folds are evident within the core as displayed by
the deformed quartz veins. Quartz-carbonate vein are
folded and deformed and usually less than 4mm wide and
have irregular contacts. Chlorite veinlets are also
SAMPLE NO. FROM TO
96012
96013
96014
96015
96016
96017
96018
96019
96020
96021
96022
96023
96024
101. .00
102. 00
103. 00
104 , 00
105. .00
106. .00
107. .00
108. .00
109. . 00
110 .00
125 .00
126 .00
143 .50
102. 00
103 . 00
104. 00
105. 00
106. .00
107, .00
108. .00
109. .00
110. .00
Ill .00
126 .00
126 .50
144 .50
ASSAYS
WIDTH Au (ppb)
1 . 00
1. 00
1. 00
1. 00
1. 00
1. .00
1. 00
1. 00
1. .00
1. .00
1. .00
0 .50
1 .00
24
3
9
22
5
2
5
14
3
NIL
48
7
139
HOLE NO: ENG9601

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9601 Page 5
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO
present up to 3mm in width and are discontinuous.
Alteration continues to be dominated by chlorite and
calcite, with minor quartz and leucoxene. Sulphides are
present in trace amounts and limited to finely
disseminated pyrite and small clots less than 2mm in
diameter along fractures and within quartz-carbonate
veins. Vein at 126m is characterized by first appearance
of epidote alteration. Core appears massive, competent
and moderately hard. Magnetic susceptibility readings are
as follows: 5:0.71 at 115m and 5:0.73 at 117m, 5:0.67 at
121m, 5:0.57 at 129m, 5:0.61 at 132m, 5:0.82 at 138m,
5:0.73 at 141m, 5:0.34 at 144m, 5:0.75 at 147m.
147.0 149.5 MAFIC PYROCLASTIC (lac) Lapilli tuff to
tuffaceous fine grained and light grey to dark green in
colour. This section is the contact zone between the
mafic and ultramafic lithologies and is characterized by
intense chlorite alteration. The quartz carbonate
veining is more abundant and has an associated albite and
quartz halo that is usually mineralized. The core is
relatively hard and non-magnetic. Magnetic
susceptibility readings are as follows: 5:10.1 at 147.5m,
5:0.84 at 148m, 5:1.00 at 149m.
149.5 150.6 GREY SYENITE DIKE (9e) Fine grained medium grey
massive lithology with elongate and rounded chloritic and
felsic fragments less than lcm in diameter. The average
size is less than 2mm diameter. Sulphide banding is
96025
96026
96027
96028
147.10
148.10
149.10
149.60
148.10
149.10
149.60
150.00
ASSAYS
WIDTH Au (ppb)
1.00
1.00
0.50
0.40
22
7
5
NIL
HOLE No: ENG9601

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9601 Page 6
FROM TO LITHOLOGICAL DESCRIPTION
developed over a 5cm interval associated with disrupted
quartz bands.
150.6 151.7 ULTRAMAFIC VOLCANICS (4a) Fine grained and
dark grey highly foliated ultramafic? with 2%
disseminated 1mm euhedral and clotty pyrite. This unit
is homogenous and contains limited quartz veining less
than Ifc. Alteration is dominated by chlorite, with minor
serpentine and calcite. The core is soft and weakly
magnetic. Magnetic susceptibility readings are as
follows: 5:2.84 at 151.5m
151.7 152.2 ULTRAMAFIC VOLCANICS (4e) Weakly serpentinized
fine grained mafic or ultramafic lithology. This section
is grey to apple green in colour and is highly foliated.
Mineralization is pervasive with l-2% disseminated and
clotty pyrite throughout. Alteration is dominated by
chlorite, serpentine and minor calcite and quartz. Quartz
veining is limited to l!r abundance consisting of the
three quartz vein types. Some of the mineralization is
associated with the quartz veins as clotty pyrite along
the edges of the vein. Magnetic susceptibility readings
are as follows: 5:0.59 at 152m.
152.2 160.6 ULTRAMAFIC VOLCANICS (4b) Massive highly
foliated dark grey to black ultramafic volcanics with
spinifex and cumulate textures. This section contains
minor talc, and lots of quartz + m inor carbonate veining
SAMPLE No.
96029
96030
FROM
150.00
150.90
TO
150.90
151.40
96031 151.40 152.20
96032
96033
152.20
153.00
153.00
154.00
ASSAYS
WIDTH Au (ppb)
0.90
0.50
0.80
0.80
1.00
12
3
3
NIL
HOLE No: ENG9601

PROPERTY: English
HOLE No.: ENG9601
FROM TO LITHOLOGICAL, DESCRIPTION
Cameco Corporation
DIAMOND DRILL LOG
up to 3(H. The veins are generally parallel to the
foliation with older vein types also present. Alteration
is dominated by silica flooding with trace calcite and
fuchsite. Fuchsite is limited to trace amounts within
some of the quartz veins. Sulphide mineralization is
limited to trace amounts heterogeneously distributed core
is relatively soft and non-magnetic. Magnetic
susceptibility readings are as follows: 5:0.65 at 152.5m,
5:0.67 at 153.5m, 5:0.61 at 156m, 5:0.59 at 159m.
160.6 161.7 SYENITE DIKE (9e) Fine grained with variable
K-feldspar content and sulphide mineralization.
K-feldspar alteration is intensified about irregular
quartz veins intruding dark red syenite. Pyrite
mineralization is prominent near the margins of the
quartz veins as fine to coarse disseminated euhedral
crystals up to 2% abundance. Core is hard and strongly
magnetic with magnetic susceptibility readings as
follows: 5:15.0 at 160.7m and 5:20.0 at 161.5m.
161.7 172.1 ULTRAMAFIC VOLCANICS (4b) Similar to previous
ultramafic volcanic description. Magnetic susceptibility
readings are as follows: 5:0.61 at 162m, 5:1.55 at 165m,
5:1.47 at 167.1m, 5:7.54 at 168m, 5:10.6 at 171m.
172.1 172.6 SYENITE DIKE (9e) Fine grained moderately
foliated dark red syenite with biotite and felsic
inclusions similar to section at 149.5m. Contact at 58
SAMPLE No. FROM TO
96034
96035
159.70
160.80
160.80
161.70
ASSAYS
WIDTH Au (ppb)
1.10
0.90
2
29
Page 7
HOLE No: ENG9601

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9601 Page 8
FROM TO LITHOLOGICAL DESCRIPTION
degrees c. a. Core is hard and weakly magnetic. Magnetic
susceptibility readings are as follows: 5:2.43 at
172.3m.
172.6 178.3 ULTRAMAFIC VOLCANICS (4b) Similar to previous
section of ultramafic volcanics. Spinifex textures
observed at 177m depth. Sulphide mineralization is
limited to trace coarse euhedral pyrite associated with
the quartz carbonate vein stockwork. Magnetic
susceptibility readings are as follows: 5:1.66 at 174m,
178.3 179.3 SYENITE DIKE (9e) Similar to previous
fragment/inclusion rich syenite, dark red in colour and
medium grained. Contact at 60 degrees c .a. Sulphide
mineralization is developed as concentrations of
disseminated pyrite at the contacts and as fine
disseminations heterogeneously distributed within the
dike. The syenite is foliated and is hard and strongly
magnetic. Magnetic susceptibility readings are as
follows: 5:43.8 at 178.4m, 5:46.0 at 179.0m.
179.3 180.9 ULTRAMAFIC VOLCANICS (4b) Similar to previous
ultramafic section. Core is moderately hard and non
magnetic. Magnetic susceptibility readings are as
follows: 5:0.55 at 179.5m.
180.9 183.0 MAFIC DIKE (Ile) Fine grained mafic to
intermediate dike intruded by numerous quartz-carbonate
SAMPLE No. FROM TO
96036
96037
172.30
176.40
173.30
177.40
96038 178.30 179.20
96039
96040
180.90
181.90
181.90
182.40
ASSAYS
WIDTH Au (ppb)
1.00
1. 00
O. 3 0
1. 00
0.50
NIL
NIL
l
12
HOLE No: ENG9601

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9601 Page 9
FROM TO LITHOLOGICAL DESCRIPTION
veins with a K-feldspar or hematite component. Quartz
veining makes up ID-20% volume. Sulphides consist of
fine grained disseminated pyrite associated with the
margins of the quartz veins. Dike is weakly foliated and
has a magnetic susceptibility of 5:17.4 at 181m.
183.0 222.0 ULTRAMAFIC VOLCANICS (4b) Similar to
previous sections with spinifex textures prevalent at
200m and 220m depth. Quartz veins are typical to
previous sections and are oriented in all directions to
the core axis and make up to ID-15% of the volume. Core
is variably hard and variably magnetic. Magnetic
susceptibility readings are as follows: 5:1.16 at 186m,
5:4.44 at 192m, 5:0.77 at 195m, 5:0.69 at 19Bm, 5:10.5 at
201m, 5:0.67 at 204m, 0.71 at 207m, 1.51 at 213m, .10.7 at
: 216m, 0.67 at 219m, 32.1 at 222m.
222.0 END OF HOLE
DOWN-HOLE SURVEY DATA
DEPTH INCLINATION BEARING
100.00 -46.00 315.00
.222.00 -45.00 3^5 QO
SAMPLE No. FROM
96041 182.40 183.00
96042
96043
96044
96045
96046
96047
96048
183.00
200.60
201. 70
202.70
207.80
217.60
221.00
ASSAYS
TO WIDTH Au (ppb)
184.00
201. 70
202. 70
203. 70
208.80
218.60
222 . 00
0.60 NIL
1 . 00
1 .10
1.00
1 . 00
1. 00
1. 00
1 . 00
NIL
NIL
NIL
NIL
NIL
2
NIL
HOLE No: ENG9601

PROPERTY: English
HOLE No.: ENG9602
Collar Eastings: 483292.00
Collar Northings: 5319641.00
Collar Elevation: 0.00
Contractor was NDS Drilling of Timmins, Ont.
FROM TO LITHOLOGICAL DESCRIPTION
0.0 1.0 CASING ON BEDROCK (Ob)
TISDALE GROUP
Cameco Corporation
DIAMOND DRILL LOG
1.0 1.1 ULTRAMAFIC VOLCANICS (4d) Fuchsite rich fine to medium
grained ultramafic volcanics. This section displays
cumulate textures and recrystallization of the
ultramafics package. The ultramafics are intruded by
numerous quartz-carbonate veins. Core i s relatively hard
but competent with only minor fracturing. Magnetic
susceptibility readings are as follows: 5:0.43 at O.lm.
i 1.1 1.2 ALBITITE DIKE (lOcq) This dike is a fine grained cream
white to beige coloured massive lithology that contains
l-2% finely disseminated pyrite. Albitite has been
intruded by quartz veins that appear barren. Magnetic
susceptibility reading is 5:0.36 at 1m.
1.2 5.2 ULTRAMAFICS VOLCANICS (4d) Fuchsite rich, fine to
coarse grained ultramafic volcanics. This section
displays cumulate textures and recrystallization
of the ultramafics package. Main intense fuchsite
alteration zone is in the top 2.5m of this section. The
ultramafics are intruded by numerous quartz-carbonate
Collar Inclination: -45.00
Grid Bearing: 315.00
Final Depth: 349.00 metres
Hole was collared in claimtt 1155889
SAMPLE No. FROM
96049
96050
96051
0.60
1.30
2.00
Logged by: Peter Chubb
Date: 26/10/96-27/10/96
Down-hole Survey: acid
ASSAYS
TO WIDTH Au (ppb)
1.30
2. 00
2. 50
0.70
O. 70
0. 50
5
9
34
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 2
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM
veins. Fuchsite alteration becomes less apparent with
depth with fuchsite restricted to the quartz-carbonate
veins and associated alteration haloes at the bottom of
the section. Magnetic susceptibility readings are as
follows: 5:0.55 at 1.3m, 5:0.71 at 3.5m, 5:0.55 at 4m,
5:1.39 at 4.5m, 5:0.65 at 5m.
5.2 7.3 INTERMEDIATE DIKE (9) Medium grey medium to fine
grained with 2% specular hematite. This section has a
sharp contact with the host lithologies and is weakly
foliated. Quartz-carbonate vein at 6.5m is fuchsite
altered. Magnetic susceptibility readings are as
follows: 2.37 at 5.5m, 2.19 at 6m, 1.06 at 7m.
7.3 20.4 ULTRAMAFIC VOLCANICS (4a-d) Medium to dark grey
coarse grained recrystallized ultramafic volcanic.
This section is intruded by numerous quartz veins at
variable core angle that also possess a chlorite halo.
Fuchsite alteration is variable with a 1m section up to
St but the rest is n.% or less, but observed in quartz-
carbonate veins. Magnetic susceptibility readings are as
follows: 5:1.57 at 8.5m, 5:1.53 a t 1 0m, 5:0.59 at 12.6m,
5:0.94 at 13m, 5:0.77 at 16m, 5:0.69 at 19m.
20.4 MAFIC DIKE (11) Very fine grained, medium grey coloured
dike. Core is hard and silicified. Magnetic
susceptibility reading is 5:0.49 at 20.6m.
ASSAYS
TO WIDTH Au (ppb)
96052 5 .20 6.20 1.00
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 3
FROM TO LITHOLOGICAL DESCRIPTION
20.8 32.0 ULTRAMAFIC VOLCANICS (4a) Similar to previous
ultramafic section has both a fine and coarse grain
component and is medium grey in colour. This section has
lots of quartz-carbonate veining up to J.5% volume with
minor fuchsite and chlorite alteration. Core appears
bleached and is moderately hard. Magnetic susceptibility
readings are as follows: 5:2.48 at 22m, 5:1.18 at 25m,
5:3.32 at 28m, 5:2.33 at 31m, 5:2.31 at 34m.
32.0 34.2 ULTRAMAFIC VOLCANICS (4a) This section is very fine
grained and light grey in colour with gradational
contacts with surrounding rocks types as well as
overlapping alteration. The base of this unit is
fuchsite altered up to Sfc while the top is chlorite
altered. Quartz veins constitute only a minor portion of
this section up to 2* volume.
34.2 37.7 ULTRAMAFIC VOLCANICS (4d) Greyish, medium t o c oarse
grained ultramafic flows that are fuchsite altered up to
1(^ and intruded by up to 10% volume of quartz carbonate
veins. Trace disseminated pyrite is present associated
with quartz-carbonate veins. Core is hard and
non-magnetic. Magnetic susceptibility readings are as
follows: 5:0.86 at 35m, 5:0.57 at 37m.
37.7 45.9 ALBITITE DIKE (lOcq) Fine grained cream white
coloured albitite dike. This dike has sharp contacts
with the host lithologies at 67 degrees c.a.. This unit
SAMPLE No.
96063
FROM
96053 35. 00
96054
96055
96056
22.80 23.80
37. 80
38.80
39. 80
ASSAYS
TO WIDTH Au (ppb)
36.00
38.80
39.80
40.80
l .00 NIL
1.00 41
1.00
l .00
1.00
163
197
646
HOLE No: ENG9602

PROPERTY: English
HOLE No.: ENG9602
Cameco Corporation
DIAMOND DRILL LOG
FROM TO LITHOLOOICAL DESCRIPTION SAMPLE No. FROM
is variably mineralized with J.% finely disseminated
pyrite throughout and up to 104 in quartz veins. Unit is
massive and weakly foliated. The albitite is crosscut by
a few variably sized quartz-carbonate veins that appear
to concentrate the sulphides within a few centimetres of
their contact. Magnetic susceptibility measurements are
as follows: 5:0.86 at 38m, 5:0.49 at 40m, 5:0.63 at 43m,
5:0.86 at 45.5m.
45.9 46.1 ULTRAMAFIC CONTACT AUREOLE (4a) Fine grained, well
foliated and chlorite rich contact aureole with
fracture related pyrite and possibly chalcopyrite
mineralization. Magnetic susceptibility measurements are
as follows: 5:0.67
46.1 50.2 ULTRAMAFIC VOLCANICS (4d) Similar to previous section
of ultramafic volcanics, with fuchsite alteration
at 20% volume. Quart z-carbonate veins are abundant at 15V
volume. Fuchsite alteration declines in intensity
sharply as fault zone is approached. This section is well
foliated and the core is competent and moderately hard.
Magnetic susceptibility are as follows: 0.59 at 47.5m,
0.55 at 49m.
50.2 50.4 FAULT ZONE (f.z.) Chlorite rich ultramafic and
quartz breccia zone. Fault contact is at 45 degrees
c.a. and is sharp. The fault consists of a fault gouge
and larger quartz dominated angular fragments less than
96057
96058
96059
96060
41 . 80
42 . 80
43. 80
44 . 80
ASSAYS
TO WIDTH Au (ppb)
42.80
43.80
44 . 80
45.80
1.00
1. 00
1.00
1.00
1989
583
79
110
96061 45 . 90 46.10 0.20 17
96062 46 . 10 47.10 1.00 15
Page 4
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 5
FROM TO LITHOLOGICAL DESCRIPTION
50.4 50.6
50.6
3cm in length. Alteration is dominated by chlorite and
serpentine with minor quartz and carbonate assemblages.
This section is non-magnetic, highly friable and
extremely soft. Magnetic susceptibility readings are as
follows: 5:0.24 at 50.3m.
ULTRAMAFIC VOLCANICS (4d) Similar to previous
ultramafic section except that the fuchsite is gradually
declining in intensity with depth. Contact at base of
this section is sharp and is alteration dependant with a
sharp change from fuchsite to chlorite dominated.
Alteration is dominated by carbonate, silica and fuchsite
with minor chlorite. This section is med grey-green in
colour and contains S-10% quartz-carbonate veining
generally less than 5mm wide. Magnetic susceptibility
readings are as follows: 5:0.43 at 50.5m.
ULTRAMAFIC VOLCANICS (4a) Typical dark green to
black serpentinized and chloritic ultramafic flows.
The flows contain variable amounts of quartz carbonate
veining forming stockworks up to 154 volume. Alteration
is dominated by carbonate, talc, quartz, serpentine, with
lesser chlorite. Talc is developed throughout the core
section and within some of the veinlets. Carbonate
flooding and replacement is variable but up to 30-404
volume. ' Areas of decreased vein intensity usually
display carbonate flooding with an associated lightening
in colour. Complex M type folds and fragment rich
SAMPLE No. FROM
96064
96065
96066
96067
52.00
58.00
59. 00
60. 00
ASSAYS
TO WIDTH Au (ppb)
53 .00
59.00
60. 00
61 . 00
1.00
1.00
1.00
1. 00
NIL
NIL
14
2
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 6
FROM TO LITHOLOGICAL DESCRIPTION
veining is present throughout this section. Core is
soft, well veined and competent. Magnetic susceptibility
readings are as follows: 5:0.59 at 52mm, 5:0.59 at 55m,
5:14.1 at 58m, 5:13.3 at 61m, 5:13.0 at 64m, 5:13.0 at
64.3m, 5:23.0 at 65.6m.
66.7 SYENITE DIKE (9e) Dark reddish grey, medium to fine
grained homogenous syenite, with abundant micro veinlets
of quartz and chlorite up to 2% of rock volume. This
section is weakly foliated at 50 degrees c.a. at
65.9m. Core is moderately hard, competent and magnetic.
Magnetic susceptibility readings are as follows: 5:36.9
at 65.9m.
66.7 89.9 ULTRAMAFIC VOLCANIC FAULT BRECCIA ZONE (4a,f.z.)
Same as previous ultramafic volcanic section
except for the presence of metre to 3 metre wide
ultramafic fault breccias and fault gouges. Relict
spinifex textures present at 86m depth. Alteration is
dominated by quartz, carbonate, chlorite, serpentine and
talc with silicification more prominent than previous
sections. Silicification is intense in the last 1m of
this section. Foliation measurements are highly variable
with folds observed. Sulphides are limited with trace
pyrite occurring in small 30cm sections. Magnetic
susceptibility readings are as follows: 5:5.24 at 70m,
8.42 at 73m, 3.87 at 75m, 5:4.24 at 79m, 3.38 at 82m,
0.88 at 85m, 8.77 at 88m, 0.49 at 89.8m. High magnetic
SAMPLE No.
96068
96069
96070
96071
96072
96073
96074
96075
FROM
65.80
66 .70
73 .00
74 .00
75.00
76.00
87.00
88.00
ASSAYS
TO WIDTH Au (ppb)
66. 70 0.90 NIL
67.70
74 . 00
75.00
76.00
77.00
88.00
89.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
3
10
NIL
NIL
NIL
3
2
HOLE No: ENG9602

PROPERTY:
HOLE No.:
Cameco Corporation
DIAMOND DRILL LOG
English
ENG9602 Page 7
FROM TO LITHOLOGICAi DESCRIPTION
features are related to the fault breccias and
intensification of serpentine alteration.
89.9 90.3 GREY SYENITE (9e) Dark greyish red fine grained
syenite with 1C^ disseminated pyrite mineralization.
Mineralogy is dominated by feldspar and chlorite
and minor quartz. Massive and highly altered
more like a contact aureole than a true syenite dike.
Magnetic susceptibility reading of 5:0.28 at 90.0m.
88.9 92.8 ULTRAMAFIC VOLCANIC FAULT BRECCIA ZONE (4a,f.z.)
Similar to previous section but has undergone
intense alteration with a sharp contrasts between
chlorite and serpentine altered zones and silicified
zones. It appears that the chlorite and serpentine rich
alteration is vein related. Quartz-carbonate veins are
abundant and make up 1C^ of the rock volume. Sulphides
are abundant up to 14 as fine to coarse euhedral
disseminations of pyrite in association with quartz-
carbonate veins and massive serpentine zones. Magnetic
susceptibility readings are as follows: 5:0.47 at 91m,
5:O.34 at 92.7m.
92.8 96.5 SYENITE DIKE (9e) The syenite dike contact consists
of a fine grained grey section that is highly
mineralized with fine disseminations of pyrite up to 10%
volume. The syenite becomes more reddish in colour with
depth. The syenite is fractured with veins consisting of
SAMPLE No.
96076
96077
96078
96079
96080
96081
96082
96083
FROM
89.00
90.00
91.00
92 . 00
92.80
93 .80
94.80
95.80
ASSAYS
TO WIDTH Au (ppb)
90.00
91.00
92 . 00
92. 80
93.80
94.80
95. 80
96 . 50
. 00
1. 00
l . 00
0.80
1.00
1.00
1.00
0. 70
24
72
NIL
NIL
34
53
98
63
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 8
FROM TO LITHOLOGICAL DESCRIPTION
serpentine, talc and quartz. The down hole contact is a
fault related and is 10cm wide. Quartz veins make up
less than 2% of the rock volume. Sulphide mineralization
is homogenous with some coarser pyrite clots associated
with the veins. The core is relatively hard and
competent. Magnetic susceptibility readings are as
follows: 5:0.45 at 93m, 5:0.47 at 94.5m, 5:0.31 at 96m.
96.5 96.6 FAULT ZONE (f.z.) Ultramafic fault breccia with
relict spinifex textured and quartz vein fragments.
Quartz veins are less than 2% volume. Matrix is
serpentine rich.
96.5 98.6 ULTRAMAFIC SPINIFEX TEXTURED VOLCANIC (4c) Classic
spinifex textured ultramafic volcanics pale cream
green in colour intruded by only a few quartz-carbonate
veins less than H volume. Magnetic susceptibility
readings are as follows: 5:0.75 at 97m, 5:1.23 at 98.4m.
98.6 101.6 INTERMEDIATE DIKE/SILICIFIED MASSIVE ULTRAMAFIC (9/43)
Homogenous fine to medium grained creme green to white
lithology. This section displays a relatively sharp
contact with the overlying spinifex textured lithology.
Quartz veins are present at 2?r volume levels and appear
to brecciated the host rock. Alteration haloes about
quartz veins are not present. Magnetic susceptibility
measurements are as follows: 4.55 at 98.5m, 0.95 at
99.5m, 0.57 at 101m.
SAMPLE No. FROM
ASSAYS
TO WIDTH Au (ppb)
96084 96.50 97. 50 1.00
96085 100.50 101.50 1. 00 NIL
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 9
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No.
101.6 102.1 SYENITE DIKE (9e) Dark red fine grained syenite
with contact aureoles associated with the contact
areas. The contact aureole is within the syenite and is
darker and more mineralized than the main body of
syenite. Sulphide mineralization at the contacts is up
to 2% finely disseminated pyrite, intensified at vein
margins. Syenite contains chloritic fragments that
display alteration along the margins. Magnetic
susceptibility readings are as follows: 5:0.43 at 102m.
102.1 102.4 INTERMEDIATE DIKE/SILICIFIED MASSIVE ULTRAMAFIC (9/43)
Similar to previous intermediate/ ultramafic section.
Magnetic susceptibility reading of 5:0.43 at 102.2m.
102.4 102.9 SYENITE DIKE (9e) Similar to previous syenite
dike section at 102m. 2-3cm clot of pyrite associated
with quartz-chlorite-serpentine veins. Magnetic
susceptibility reading of 5:0.51 at 102.6m.
102.9 103.6 S ILICIFIED ULTRAMAFIC VOLCANIC ( 4a) M edium to
coarse grained massive ultramafic. Alteration is
dominated by silicification and carbonate minerals.
Magnetic susceptibility reading of 5:0.82 at 103m.
103.6 104.7 SYENITE DIKE (9e) Similar to previous syenite
dike. This section contains a 1m zone of 3% coarse
pyrite mineralization. Specular hematite is developed as
ASSAYS
FROM TO WIDTH Au (ppb)
96086 101.50 102.00 0.50 38
96087 102.00 102.30 0.30 NIL
96088 102.30 102.90 0.60 14
96089 102.90 103.80 0.90 NIL
HOLE No: ENG9602

PROPERTY: English
HOLE No.: ENG9602
Cameco Corporation
DIAMOND DRILL LOG
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM
fine dissemination throughout this section at li
abundance. Magnetic susceptibility readings as follows:
0.3 at 103.7m, 0.51 at 104m, 0.58 at 104.7m.
104.7 108.1 INTERMEDIATE DIKE/SILICTFIED MASSIVE ULTRAMAFIC (9/43)
Similar to previous sections of intermediate/ultramafic
zone. This section contains clots of chalcopyrite at
H; volume of the quart z-carbonate veins. Minor fuchsite
alteration is also developed within the larger quartz
veins but at low concentrations J.% abundance. Magnetic
susceptibility readings are as follows: 5:0.53 at 106m,
5:1.76 at 107m.
108.1 108.5 SYENITE DIKE (9e) Similar to previous syenite dike.
Finely disseminated pyrite at 14; volume. Specular
hematite is developed a s f ine dissemination throughout
this section at J.% abundance. Magnetic susceptibility
readings as follows: 5:0.71 at 108.3m.
108.5 110.1 INTERMEDIATE DIKE/SILICIFIED MASSIVE ULTRAMAFIC (9/43)
Similar to previous sections of intermediate/ultramafic
zone. This section contains clots of specular hematite
at 5% volume of the quartz-carbonate veins. Minor
fuchsite alteration is also developed within the
larger quartz veins but at low concentrations J.%
abundance. Magnetic susceptibility reading of 5:1.25 at
109m.
ASSAYS
TO WIDTH Au (ppb)
96090 103.80 104.80 1.00 81
96091 104.80 105.80 1.00 33
96092 105.80 106.80 1.00 NIL
96093 106.80 107.80 1.00 NIL
96094 107.80 108.10 0.30 5
96095 108.10
96096
96097
108.50
109.10
108.50
109.10
110.10
0.40 26
0.60
1.00
NIL
77
Page 10
HOLE No: ENG9602

PROPERTY: English
HOLE No.: ENG9602
FROM TO LITHOLOGICAL DESCRIPTION
Cameco Corporation
DIAMOND DRILL LOG
110.1 111.2 SYENITE DIKE (9e) Similar to previous syenite
dikes with up to 2% fine to coarse pyrite mineralization.
This section is crosscut by S-5% quartz serpentine-
chlorite veins. Mineralization is concentrated along
some of the veins. Magnetic susceptibility readings are
as follows: 5:055 at 111m.
111.1
118. 5
118.6 ULTRAMAFIC VOLCANICS (4a) Similar to previous
ultramafic volcanics observed higher up in the section.
This section contains abundant quartz-carbonate veins up
to 15% volume. Bottom part of this section is highly
silicified up to SO 1!; and spinifex textured. Minor
specular hematite disseminated in core at trace amounts.
Veins indicate that the ultramafics have undergone
polyphase folding. Magnetic susceptibility readings as
follows: 5:1.9 at 112m, 5:2.29 at 115.5m, 5:0.41 at 118m.
SYENITE DIKE (9e) Similar to previous syenite
dikes, highly fractured. Fractures infilled by quartz,
chlorite and serpentine. Magnetic susceptibility
readings as follows: 5:0.38 at 119m.
126.8 ULTRAMAFIC SPINIFEX TEXTURED VOLCANICS (4cd)
Fuchsite altered spinifex textured ultramafics that
contain abundant quartz-carbonate veining as in previous
ultramafic sections. Fuchsite alteration is limited to
less than il.% within the quartz veins and along foliation
planes, with local concentrations reaching 101 abundance
SAMPLE No.
96098
96099
96100
96101
96102
96103
96104
96105
96106
96107
96108
96109
FROM
110.10 111.20
111.20 112.20
112.20 113.30
116.60 117.60
117.60 118.60
118.60 119.20
119 .20
121.00
122.00
123 .00
124 .00
125.00
ASSAYS
TO WIDTH Au (ppb)
120. 10
122. 00
123.00
124. 00
125. 00
125. 90
1.10 74
1.00
1.10
1.00
1.00
0.60
0.90
1.00
1.00
1.00
1. 00
0. 90
NIL
NIL
7
NIL
26
147
NIL
2
2
3
9
Page 11
HOLE NO: ENG9602

PROPERTY: English
HOLE No.: ENG9602
FROM TO LITHOLOGICAL DESCRIPTION
130.2
over 5cm. Magnetic susceptibility readings as follows:
5:3.15 at 121m, 5:0.38 at 124m, 5:51.5 at 26m.
127.8 FAULT ZONE (f.z.) Ultramafic fault breccia with
relict spinifex textured and quartz vein fragments.
Quartz veins are less than 2% volume. Matrix is
serpentine rich. Magnetic susceptibility reading is
5:0.32 at 127.2m.
130.2
Cameco Corporation
DIAMOND DRILL LOG
ULTRAMAFIC VOLCANICS (4ad) Fuchsite altered
massive ultramafic. Fine to coarse grained with limited
fuchsite alteration along fracture planes and within
quartz-carbonate veins. Similar to previous ultramafic
volcanics except colour is medium grey. Alteration is
dominated by carbonates, quartz, fuchsite and serpentine.
Quartz-carbonate veins are abundant up to 30% volume and
are highly folded and for the most part follow the
foliation. Pyrite mineralization is limited to trace
amounts of finely disseminated and coarse euhedral pyrite
in close proximity to the quartz-carbonate veins.
Magnetic susceptibility readings are as follows: 5:0.51
at 128.2m, 5:0.65 at 130m.
SYENITE DIKE (9e) Similar to previous syenite
dikes. This syenite is pinkish red and contains I'i
coarse pyrite mineralization. Core is hard and massive.
Magnetic susceptibility reading is 5:0.57 at 130.3m.
ASSAYS
SAMPLE No. FROM TO WIDTH Au (ppb)
96110 125.90 126.80 0.90
96111 126.80 127.80 1.00
96112 127.80 128.80
96113 128.80 129.80
96114
96115
129.80
130.30
130.30
130.80
1.00
1.00
123
NIL
2
0.50 NIL
0.50 3
Page 12
HOLE No: ENG9602

PROPERTY: English
HOLE No.: ENG9602
FROM TO LITHOLOGICAL DESCRIPTION
131.4
Cameco Corporation
131.4 ULTRAMAFIC VOLCANICS (4a) Serpentine altered
massive ultramafic. Fine to coarse grained with limited
serpentine alteration along fracture planes and within
quartz-carbonate veins. Similar to previous ultramafic
volcanics. Alteration is dominated by carbonates,
quartz, serpentine. Quartz-carbonate veins are abundant
up to 3(H volume and are highly folded and for the most
part follow the foliation. Pyrite mineralization is
limited to trace amounts of finely disseminated and
coarse euhedral pyrite in close proximity to the
quartz-carbonate veins. Magnetic susceptibility reading
of 5:0.41 at 131m.
DIAMOND DRILL LOG
SYENITE DIKE (9e) Similar to previous syenite dike.
Colour i s p inkish red and contains 5% chloritic fragments
and 14 coarse and fine pyrite mineralization. Magnetic
susceptibility reading is 5:0.32 at 131.7m.
134.1 ULTRAMAFIC VOLCANICS (4a) Similar to previous
ultramafic volcanic sections. Quartz-carbonate veins are
highly folded and display M-type folds. Magnetic
susceptibility readings as follows: 5:0.79 at 133m.
134.1 135.7 INTERMEDIATE DIKE (9) Fuchsite altered mafic
dike with small lathes of muscovite and fuchsite. Dike
is fine'grained and porphyritic. Dike contains
inclusions of syenite. Minor ?arsenopyrite or pyrite at
contact with syenite up to 2%. Magnetic susceptibility
SAMPLE No. FROM
96116 130.80 131.40
96117 131.40 131.80
96118 131.80 132.40
96119 132.40 133.10
96120 133.10 134.10
96121
96122
134.10
135.10
ASSAYS
TO WIDTH Au (ppb)
135.10
135.70
0.60
0.40
0.60
0. 70
1. 00
1. 00
0.60
NIL
2
31
NIL
NIL
7
Page 13
HOLE NO: ENG9602

PROPERTY: English
HOLE No.: ENG9602
FROM TO LITHOLOGICAL DESCRIPTION
reading of 5:0.38 at 135m.
135.7 138.2 SYENITE DIKE (9e) Similar to previous syenite
dikes with chloritic fragments and silicified
fragment of ultramafic rock enclosed. Sulphides are
pervasive and up to 1 \ f inely disseminated and coarse
pyrite. Magnetic susceptibility readings as follows:
5:0.69 at 136m, 5:5.43 at 138.2m.
Cameco Corporation
DIAMOND DRILL LOG
138.2 148.4 DIORITE OR GREY SYENITE DIKE (9e) Coarse grained
intrusive mafic syenite, medium grey with a touch
of pink but variable in colour and grain size. This
section contains fragments of other syenite dikes and
ultramafic lithologies. Ultramafic fragments are
strongly serpentinized and contain abundant quartzcarbonate
veins up to 20% volume. Syenite fragments are
well mineralized and contain up to 2% disseminated
pyrite. Sulphides are present as disseminated and clotty
pyrite associated with fractures, margins of fragments
and K-feldspar rich sections. Core is hard and non
magnetic. Magnetic susceptibility readings are as
follows: 5:0.69 at 142m, 5:0.67 at 145m, 5:0.51 at 148m.
148.4 150.7 ULTRAMAFIC VOLCANIC (4a) Similar to previous
ultramafic volcanics. Quartz-carbonate veining accounts
for 35% 'Of the volume with disseminated and clotty pyrite
observed up to trace amounts. Alteration is dominated by
quartz and carbonate with serpentine and ?fuchsite
SAMPLE No.
96123
96124
96125
96126
96127
96128
96129
96130
96131
96132
96133
FROM
135. 70
136. 70
137. .70
138. 20
142. 00
143 . 00
144 . 00
145. .00
146 . .00
147 . .00
148. .00
ASSAYS
TO
136. 70
137. 70
138. 20
139. 20
143. 00
144 . 00
145. 00
146. 00
147. 00
148. . 00
148. . 40
WIDTH Au
1 . 00
1. 00
0. .50
1 . 00
1 . .00
1. .00
1. .00
1. . 00
1. .00
1 . . 00
0. .40
96134 149.70 150.70 1.00
(ppb)
101
19
NIL
NIL
NIL
NIL
NIL
7
3
NIL
43
Page 14
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 15
FROM TO LITHOLOGICAL DESCRIPTION
present. Magnetic susceptibility reading of 5:0.63.
150.7 161.8 SYENITE DIKE (9e) Fine to medium grained pinkish
to grey intrusive syenite containing chloritized
fragments of host lithologies up to 4cm in size. The
chloritized fragments also possess alteration haloes
indicating that some assimilation of the fragments took
place during transport. Sulphide mineralization is
developed as fine disseminations throughout the core and
as clots along the margins of quartz veins. Quartzcarbonate
veins constitute up to 2% of the rock volume
and are less than 10mm thick. This section shows
variable colour and grain size changes locally, and a
contact aureole with the underlying ultramafic rock that
is approximately 20cm wide. The contact aureole is dark
grey green and contains 24 fine to coarse pyrite. The
syenite is fractured with chlorite infilling and is also
weakly foliated. Lower contact is sharp and is at 59
degrees c. a. Core is hard with magnetic susceptibility
readings as follows: 5:0.41 at 151m, 5:0.38 at 154m,
5:0.53 at 157m, 5:0.41 at 160m.
161.8 166.2 ULTRAMAFIC VOLCANICS (4a) Similar to previous
section of ultramafic volcanics. Spinifex textures
occurs at 164m depth. Alteration is dominated by quartz-
carbonate, minor chlorite, serpentine and trace fuchsite.
Core is folded with M-type, S-type and Z-type folds
present. Lower contact is irregular and trends 36
SAMPLE No.
96135
96136
96137
96138
96139
96140
96141
96142
96143
96144
96145
96146
96147
96148
96149
FROM
150. .70
151. .70
152. 70
153 . 80
154 . 90
156. 00
157 . 00
158. 00
159. 00
160. 00
161. 00
161. 70
162 . 70
163. 70
164 . .70
ASSAYS
TO
151. 70
152. 70
153. 80
154. 90
156. 00
157. 00
158, 00
159. 00
160, 00
161. 00
161. 70
162. 70
163. 70
164. 70
165. .70
WIDTH Au
1 . .00
1. .00
1. .10
1. .10
1. .10
1 . 00
1 . .00
1. .00
1 . .00
1. 00
0. . 70
1 .00
1 , .00
1 .00
1. .00
(ppb)
51
209
41
93
10
21
7
26
84
21
120
7
2
9
5
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 16
FROM TO LITHOLOGICAL DESCRIPTION
degrees to c.a. Sulphides are observed as trace finely
disseminated pyrite. Magnetic susceptibility reading of
5:0.43 at 163m, 5:0.71 at 166m.
166.2 171.7 BRECCIATED INTERMEDIATE DIKE/ULTRAMAFIC VOLCANIC (9/43)
This dike is light to medium grey in colour and
may represent a highly silicified disrupted ultramafic
volcanic that contains brecciated sections of
syenite and later felsic dike components. Sulphide
mineralization up to ^ occurs along foliation planes as
disseminated euhedral pyrite. Contact with underlying
massive albitite dike is sharp and at 7 degrees c.a.
Core is moderately hard and competent with only minor
fracturing present. Magnetic susceptibility readings as
follows: 5:0.59 at 167m, 5:0.59 at 169m.
171.7 174.0 ALBITITE DIKE (lOcq) Fine grained cream peach
coloured this massive felsic dike contains 1-2*^
finely disseminated euhedral pyrite throughout. Lower
contact is irregular and at 26 degrees c.a. Dike appears
undeformed but is intruded by quartz-carbonate veins up
to 2% volume and chlorite infilled fractures. Magnetic
susceptibility reading of 5:0.33 at 172.0m.
174.0 183.4 SILICIFIED ULTRAMAFIC VOLCANIC (4a) Similar
to previous section of ultramafic volcanics. Quartz-
carbonate veining present at 351 volume with fuchsite
visible at 176m. Trace pyrite developed as fine
SAMPLE No. FROM
ASSAYS
TO WIDTH Au (ppb)
96150 166.30 167.00 0.70
96151 167.00 168.00 1.00
96152 168.00 169.00 1.00
96153 169.00 170.00 1.00
96154
96155
172.00
173.00
96156 174.00
96157 175.00
96158 178.00
96159 180.60
173.00 1.00
174.00 1.00
175.00
176.00
179.00
181.60
l . 00
1.00
1.00
1.00
108
173
9
10
5
NIL
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 17
FROM TO LITHOLOGICAL DESCRIPTION
dissemination throughout core, but picks up in the last
l-2m of this section to approximately a.% abundance.
Magnetic susceptibility readings as follows: 5:0.51 at
175m, 5:0.51 at 178m, 5:0.63 at 181m.
183.4 202.4 MAFIC DIKE/SILICIFIED ULTRAMAFIC VOLCANIC (8aX4a)
Similar to above but more massive looking and
contains approximately lQ-15% quartz-carbonate veining.
The core is relatively soft and appears to be
recrystallized with foliations difficult to distinguish.
Alteration is dominated by quartz-(-carbonate and minor
serpentine and fuchsite associated with veins and
fractures up to 2fc. Questionable spinifex textures
developed at 198m. Sulphides are developed as very fine
disseminations and coarser euhedral crystals up to 5mm in
size locally. Sulphide abundance is l-2%. Veining
displays minor brecciation of host rock as it intruded.
Magnetic susceptibility readings as follows: 5:0.53 at
184m, 5:0.59 at 187m, 5:0.53 at 190m, 5:0.43 at 193m,
5:0.53 at 196m, 5:0.61 at 199m, 5:0.47 at 202m. Contacts
between flows? is at 56 degrees c.a.
202.4 230.8 SERPENTINIZED ULTRAMAFIC VOLCANICS (4e) Dark
Green to black fine grained massive and competent
lithology with spinifex and cumulate textures developed
periodically. Alteration is dominated serpentine and
talc, with quart z-carbonate veining limited to less than
3* w ith minor fuchsite present along a few of the
SAMPLE No.
96160
96161
96162
96163
96164
96165
96166
96167
96168
96169
96170
96171
96172
96173
96174
96175
96176
96177
96178
96179
96180
FROM
181.60
182 . 60
183. 50
184. 40
185. 50
186 . 50
187. 40
189. 40
190 . 40
195. 00
197. 50
198. 50
199. 50
200. 50
201 . 50
202.40
203.40
207. 00
208.00
209. 00
210. 00
ASSAYS
TO WIDTH Au (ppb)
182.60 . 00
183. . 50
184. 40
185. 50
186. .50
187. 40
188. 40
190. 40
191. 40
196. 00
198. 50
199. 50
200. 50
201. 50
202. .40
203.40
204.40
208.00
209.00
210. 00
210. 90
0. . 90
0. . 90
1. . 10
1. 00
0. . 90
1. .00
1 . .00
1 . 00
1 . 00
1. .00
1. 00
1. 00
1. 00
0. . 90
1. 00
1. 00
1 . 00
1. 00
1.00
0. 90
7
10
9
9
7
17
10
9
14
2
3
2
. 2
NIL
5
NIL
NIL
5
NIL
3
HOLE No: ENG9602

PROPERTY: English
HOLE No.: ENG9602
FROM TO . LITHOLOGICAL DESCRIPTION
Cameco Corporation
DIAMOND DRILL LOG
margins. Sulphide development is variable with both
coarse and finely disseminated pyrite up to 2* from 207m
to 215m, and trace amounts of pyrite locally developed.
Core is soft and competent with only a few fractures.
Magnetic susceptibility readings are as follows: 5:0.61
at 2 04m, 5:0.59 at 208m, 5:0.65 at 211m, 5:1.33 at 214m,
S:1.45 at 218m, 5:1.96 at 220m, 5:3.83 at 223m, 5:2.68 at
225m, 5:0.98 at 229m.
231.1 232.5 SYENITE DIKE (9e) Dark red and fine grained this
dike is altered and contains serpentine. The upper
contact is at 90 degrees c.a. and the lower contact is at
57 degrees c.a. The core is moderately hard and
competent. Magnetic susceptibility reading of 5:0.73.
Trace specular hematite present.
231.5 236.0 SILICIFIED ULTRAMAFIC VOLCANICS (4a) Massive medium
to light grey ultramafic volcanics with 5% quartz
carbonate veining intruding at various angles subparallel
to the core axis. Fuchsite alteration is developed along
the margins of the veins and at the base contact with the
underlying syenite dike. Lower contact is at 65 degrees
c.a. Sulphides are developed within two 30cm wide zones
associated with fuchsite altered quartz veins and the
basal contact. Sulphides in the two zones consist of
2-3% coarse pyrite heterogeneously distributed within the
zones. This section is harder than the serpentinized
ultramafics due to associated silicification. Magnetic
SAMPLE No. FROM
96181 212.00 213.00
96182 213.00 214.00
96183 214.00 215.00
96184 219.00 220.00
96185 229.00 230.00
96186
96187
234.00
235.00
ASSAYS
TO WIDTH Au
235.00
236.00
1.00
1.00
l . 00
1.00
1. 00
1. 00
1.00
(ppb)
NIL
2
2
NIL
3
12
189
Page 18
HOLE No: ENG9602

PROPERTY: English
HOLE No.: ENG9602
FROM TO LITHOLOGICAL DESCRIPTION
susceptibility readings of: 1.1 at 2 32m, 0 .38 at 2 35m.
Cameco Corporation
236.0 2 38.5 SYENITE DIKE (9e) Massive pink fine to medium
grained syenite that displays a change to a g rey
coloured syenite at 237m. The syenite contains
chloritized fragments and up to 5fc 1mm sized euhedral
pyrite. Sulphide content drops off in the grey syenite.
Lower contact at 60 degrees c.a.. Magnetic
susceptibility reading of 5:0.38 at 237m.
DIAMOND DRILL LOG
238.5 241.5 SILICIFIED ULTRAMAFIC VOLCANIC (4a) Similar to
previous silicified ultramafic volcanic section. This
section is medium grey green and contains more serpentine
than the previous section. Sulphides are developed in a
thin 15cm section at the basal contact with the
underlying felsite/albitite. Sulphides consist of S-5%
disseminated and foliation plane related pyrite.
Magnetic susceptibility reading of 5:0.61 at 241m.
241.5 298.7 ALBITITE/FELSITE DIKE (lOacq) The felsite/albitite
dike forms a massive beige coloured unit with both
a coarse and fine plagioclase+quartz phyric lithology.
Sulphides are developed as fine disseminations and
as clots associated with crosscutting quartz veins.
Sulphide content average between l and 2%. Veins
consist mainly of quartz with minor carbonate in
some of them with vein abundance averaging 2% volume with
the larger veins at 15 degrees c.a. Large veinlets
SAMPLE No.
96188
96189
96190
96191
96192
96193
96194
96195
96196
96197
96198
96199
96200
FROM
236.00 237.00
237.00 238.00
238.00 238.50
238.50
240. .60
241. .60
242 . .60
243 .60
244 .50
245 .50
246 .40
247 .30
247. .80
ASSAYS
TO WIDTH AU (ppb)
239.50
241. .60
242. .60
243. .60
244. .50
245 .50
246 .40
247 .30
247 .80
248, .30
1.00
1. 00
0. 50
1.00
1. .00
1. .00
1. .00
0. . 90
1, .00
0 . 90
0 .90
0 . 50
0, .50
75
5
NIL
70
240
31
36
41
87
86
36
38
Page 19
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 20
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No.
greater than 5cm occur at 272m, 283m, 286-287m. Some of 96201
the veinlets contain blowouts of massive pyrite. An 96202
increase in the number of micro veinlets occurs at 283m, 96203
286m up to 15* volume. Upper contact is at 72 degrees 96204
c. a., with an internal contact between the two phases at 96205
30 degrees c. a. at 245m. Magnetic susceptibility are as 96206
follows: 5:0.12 at 243m. 96207
96208
96209
96210
96211
96212
96213
96214
96215
96216
96217
96218
96219
96220
96221
96222
96223
96224
96225
96226
96227
96228
FROM
248. 30
248. 80
249. 30
250. .30
251. .30
252 . .30
253. .30
254 . .30
255. .30
256. .00
257. .00
258 .00
262 . 00
263 .00
263. . 90
264. .80
265 .80
266 .80
267 .70
268 . 70
269 .70
270 .60
271 .60
272 .60
273 .60
274 .60
275 .60
276 .50
ASSAYS
TO WIDTH Au
248. 80
249. .30
250 . .30
251. .30
252. .30
253 . .30
254. .30
255 .30
256 .00
257 .00
258 . 00
259 .00
263 .00
263 . 90
264 .80
265 .80
266 .80
267 .70
268 .70
269 .70
270 .60
271 .60
272 .60
273 .60
274 .60
275 .60
276 . 50
277 .40
0. 50
0. 50
1. 00
1. 00
1. 00
1 . 00
1. 00
1. 00
0. 70
1 . 00
1. . 00
1. .00
1 . 00
0. . 90
0. . 90
1. . 00
1 . . 00
0. . 90
1 .00
10 . 00
.90
1 .00
1 .00
1 . 00
1 . 00
1 .00
0 .90
0 . 90
(ppb)
24
55
62
43
279
50
134
58
38
111
65
53
190
58
51
2
31
36
45
51
24
43
48
45
98
43
120
60
HOLE NO: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 21
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No.
96229
96230
96231
96232
96233
96234
96235
96236
96237
96238
96239
96240
96241
96242
96243
96244
96245
96246
96247
96248
96249
96250
298.7 323.0 FUSCH. -GRAPH. ? ULTRAMAFIC VOLC . +SEDS . (4dX5d) 96251
Package of fuchsite rich and fuchsite poor quartz- 96252
carbonate vein rich ultramafics. Some of the 96253
horizons appear to contain graphite. The section is 96254
intruded by a fuchsite rich felsic dike approximately 96255
FROM
277. .40
278. .30
279. .30
280. .20
281 .20
282 . 10
283 .10
284 . 10
285. . 00
286 . . 00
286. .90
287 . 90
288 . 80
289 . 80
290 . 80
291 . 70
292 .70
293 .60
294 .60
295 .60
296 . 60
297 .60
298 . 60
298 .90
299 . 90
300 . 90
301 . 90
ASSAYS
TO WIDTH Au
278. . 30
279. .30
280. .20
281 .20
282 .10
283 .10
284 .10
285 .00
286 .00
286 .90
287 . 90
288 . 80
289 .80
290 .80
291 .70
292 .70
293 .60
294 .60
295 .60
296 .60
297 .60
298 .60
298 .90
299 .90
300 .90
301 .90
302 .90
0 .90
1 .00
0 .90
1 .00
0 . 90
1 . 00
1 .00
0 .90
1 .00
0 .90
1 .00
0 .90
1 .00
1 .00
0 . 90
1 .00
0 .90
1 .00
1 .00
1 .00
1 .00
.00
1
0
1
1
1
1
.30
.00
.00
.00
.00
(ppb)
51
79
31
98
50
27
24
38
29
39
36
113
120
99
36
34
27
69
89
38
43
14
24
2
3
2
51
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 22
FROM TO LITHOLOGICAL DESCRIPTION
30cm wide with contacts at 35 degrees c. a. . The
ultramafics are massive and contain up to 25% veins by
volume. Sulphide development is variable with trace
amounts of pyrite present throughout this section. The
graphitic horizons contain up to S-10% euhedral
disseminated pyrite. The fuchsite horizons near the
graphitic horizons contain up to 2* disseminated pyrite.
Magnetic susceptibility readings as follows: 5:0.59 at
301m, 5:0.57 at 304m, 5:0.32 at 307m, 5:0.57 at 310m,
5:0.49 at 313m, 5:0.53 at 316m, 5:0.49 at 319m, 5:0.23 at
322m.
323.0 323.8 INTERMEDIATE DIKE (9) Pale grey with dark
spots. Trace pyrite locally, massive and competent.
Dike is crosscut by numerous quartz-carbonate veins up to
10% volume. Magnetic susceptibility reading of 5:0.47 at
323m.
SAMPLE No.
96256
96257
96258
96259
96260
96261
96262
96263
96264
96265
96266
96267
96268
96269
96270
96271
96272
96273
96274
96275
96276
FROM
302. 90
303. 90
304 . 90
305 . 90
306. 90
307 . 90
308. 90
310. 00
311. 00
312. 00
313 . 00
314. 00
314 . 30
315. 30
316 . 30
317. 30
318. 30
319. 30
320. 30
321. 30
322 . 30
ASSAYS
TO WIDTH Au (ppb)
303. 90
304 . 90
305. 90
306. 90
307. 90
308 . .90
309. .90
311. 00
312 . 00
313. 00
314 . 00
314. 30
315. 30
316. 30
317. 30
318. 30
319, .30
320. .30
321. .30
322 . .30
323 .30
323.8 328.3 ULTRAMAFIC VOLCANICS (4a) Serpentine and 96277 323.30 323.90 O . 60
1.
1 .
1.
1 ,
1 .
1 .
1.
1 .
1 .
1 .
1 .
0.
1
00
00
00
00
00
00
00
00
00
00
00
30
1 . 00
1. 00
1. 00
1 . 00
I. .00
1 . .00
1. .00
1 . 00
00
375
62
19
10
106
46
12
39
14
744
437
283
43
151
98
387
842
267
375
1269
63
HOLE No: ENG9602

PROPERTY: English
HOLE No.: ENG9602
Cameco Corporation
DIAMOND DRILL LOG
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM
carbonate rich ultramafic volcanics with a well
developed foliation. Sulphide development is local and
up to 5fc disseminated and fracture related pyrite.
Magnetic susceptibility readings as follows t 5:0.49 at
325m, 5:0.71 at 328m.
328.3 330.3 INTERMEDIATE DIKE (9) Similar to section at
323.0-323.8m. Magnetic susceptibility reading of 5:0.49
at 329m. Core is relatively hard and competent.
330.3 334.3 SYENITE DIKE (9e) Typical of previous pink
syenite dikes, fine grained, massive and hard. This
section contains X-5% disseminated fine and coarse
euhedral and fracture related clots of pyrite. Syenite
is fractured with infillings of chlorite and quartz.
Magnetic susceptibility reading of 0:10 at 331m.
334.3 336.0 INTERMEDIATE DIKE (9) Similar to previous
intermediate dike. Magnetic susceptibility readings of
5:0.86 at 335m. Trace disseminated pyrite locally
developed.
336.0 336.9 ULTRAMAFIC VOLCANIC (4a) Typical serpentinized
medium to dark green ultramafic volcanics
intruded by a fine grained orange coloured dyke that has
altered the surrounding ultramafics in this section. A
thin fault breccia is also developed over a 10cm
interval. Alteration is dominated by serpentine and
96278 327.50 328.50
96279 330.30 331.30
96280 331.30 332.30
96281 332.30 333.30
96282 333.30 334.30
96283 334.30 335.30
ASSAYS
TO WIDTH Au (ppb)
1. 00
1. 00
1. 00
1.00
1.00
1. 00
2
19
34
3
22
Page 23
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE NO.: ENG9602 Page 24
FROM LITHOLOGICAL DESCRIPTION
quartz t carbonate with minor fuchsite present near the
larger quartz-carbonate veins. Sulphides consist of
trace to 2% finely disseminated pyrite set homogenously
disseminated throughout this section but concentrated
near the fault breccia.
336.9 343.7 MAFIC S; INTERMEDIATE DIKE (11&9) A series
of fine grained dark green to black mafic and
intermediate dikes crosscut the ultramafic volcanics
and large fragments of ultramafics are present within
the dikes near the contact with .the ultramafics.
Contacts at 55 degrees c.a. The dikes are massive and
fine grained and have been crosscut by a series of
subparallel quartz veins some of which contain massive
pyrite within the mafic dikes. Sulphide mineralization
is limited to the more mafic looking dikes where it is
developed as fine dissemination up to Ut. Magnetic
susceptibility readings as follows: 5:1.14 at 340m, and
5:0.75 at 343m.
343.7 348.2 SERPENTINIZED ULTRAMAFIC VOLCANICS (4e) Similar
to previous serpentinized and talcose ultramafic
volcanics this section contains up to 20% quartz-
carbonate veining. Minor intervals of sulphides are
developed up to 5cm wide consisting of 2-3% coarse
euhedral pyrite associated with serpentine enriched
zones. Magnetic susceptibility reading of 5:0.43 at
346m, 5:0.61 at 348m.
SAMPLE NO. FROM
96284 336.00
96285 339.00
96286 340.00
ASSAYS
TO WIDTH Au (ppb)
337.00
340.00
341.00
1.00
1. 00
1. 00
10
NIL
5
96287 346.00 347.00 1. 00 10
HOLE No: ENG9602

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9602 Page 25
FROM TO LITHOLOGICAL DESCRIPTION
348.2 349.0 SYENITE PORPHYRY DIKE (9e) Coarse grained
blotchy dark red porphyritic syenite. Contact at 55
degrees c.a.. The porphyries are indistinct and this
section maybe a recrystallized brecciated syenite.
Magnetic susceptibility readings are as follows: 5:0.45.
Sulphides consist of trace amounts of finely disseminated
euhedral pyrite.
349.0 END OF HOLE
DOWN-HOLE SURVEY 'DATA
DEPTH INCLINATION BEARING
l . 00 -45.00
100.00 -47.00
200.00 -47.00
349.00 -49.00
315.00
315.00
315.00
315.00
ASSAYS
SAMPLE No. FROM TO WIDTH Au (ppb)
96288 348.30 349.00 0.70
HOLE No: ENG9602

PROPERTY: English
HOLE No.: ENG9603
Collar Eastings: 483126.00
Collar Northings: 5319807.00
Collar Elevation: 0.00
Contractor was NDS Drilling of Timmins, Ont.
FROM TO LITHOLOGICAL DESCRIPTION
0.0 6.0 CASING ON BEDROCK (Ob)
TISDALE GROUP
Cameco Corporation
DIAMOND DRILL LOG
6.0 16.0 ULTRAMAFIC VOLCANICS (4e-d) Serpentine rich ultramafic
volcanics with minor fuchsite alteration. This section
is well foliated and contains up to 30% volume quartz-
carbonate veins. Sulphide mineralization is erratic but
ranges from trace up to 5% volume and is concentrated
about the veins and serpentine rich zones. Sulphides are
developed as fine to coarse disseminations of euhedral
pyrite associated with veins and fractures and the
margins of minor intruding dikes. Average for this
section is UT volume pyrite. A number of thin albitite,
syenite and mafic dikes intrude the section all of which
are mineralized with up to 3% disseminated pyrite.
Contacts of the dikes are at 40 degrees c.a., 70 degrees
c.a.. Magnetic susceptibility readings as follows:
5:0.45 at 7m, 5:0.51 at lOrn, 5:0.26 at 13m.
16.0 19.0 MAFIC SYENITE DIKE (11) Fine to medium grained medium
grey massive dike. The quartz-carbonate veins are
present in l* abundance and are barren. Sulphides are
present in trace amounts as disseminated pyrite. Lower
Collar Inclination: -45.00
Grid Bearing: 315.00
Final Depth: 154.00 metres
Hole was collared in claimtt 1155891
SAMPLE No.
96289
96290
96291
96292
96293
96294
96295
96296
96297
96298
96299
FROM
. oo
6 .
7 . .00
8 .00
B. . 60
10 .00
11 .80
12 .70
13 .70
14 . 70
15. 70
16 . 10
Logged by: P. Chubb
Date: 28/10/96-28/10/96
Down-hole Survey: Acid
ASSAYS
TO WIDTH Au (ppb)
7 . 00
8. 00
8. .60
10. . 00
11 .10
12. .70
13 . 70
14 .70
15 .70
16 .10
17.10
1 . 00
1 . 00
0. .60
1 , .40
1 . 10
0 . 90
1 .00
1 .00
1 .00
0.40
1.00
58
163
65
17
NIL
38
53
151
77
46
235
HOLE No: ENG9603

PROPERTY: English
HOLE No.: ENG9603
Cameco Corporation
DIAMOND DRILL LOG
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM
contact at 70 degrees c.a..
reading of 5:0.38 at 19m.
Magnetic susceptibility
19.0 23.0 ULTRAMAFIC VOLCANICS (4e-d) Similar to previous section
of ultramafic volcanics. Magnetic susceptibility reading
of 5:0.55 at 22m. Sulphides are developed along the
contacts with intruding thin dikes and along the upper
and basal contacts with larger dikes up to l-2%
disseminated pyrite. Lower contact at 65 degrees c.a.
23.0 23.7 SILICIFIED COARSE FELDSPAR PORPHYRY (lOcy) Coarse
grained and silicified feldspar porphyry, with K-feldspar
alteration and trace disseminated pyrite. Lower contact
at 39 degrees c.a. Magnetic susceptibility reading of
5:0.12 at 23.5.
23.7 27.1 SYENITE DIKE (9e) Coarse grained massive pink syenite
dike. Magnetic susceptibility of 5:0.30.
27.1 30.5 ALBITITE DIKE (lOcq) Typical albitite fine grained
massive beige lithology as observed in other holes. This
section contains J.% disseminated pyrite. Micro quartz
veinlets crosscut the dike up to 2fc abundance. Magnetic
susceptibility readings of 5:0.14 at 27.9m.
30.5 32.3 SILICIFIED COARSE FELDSPAR PORPHYRY (lOcy) Same as
previous similarity named section. Lower contact at 42
degrees. Sulphides consist of disseminated trace pyrite.
ASSAYS
TO WIDTH Au (ppb)
96300 19. 00 20.00 1.00
96301
96302
9S303
96304
96305
23.60
24.60
29. 00
30. 00
31. 00
24.60
25.60
31.00
32. 00
1. 00
1.00
1.00
1.00
1. 00
22
113
439
221
245
Page 2
HOLE No: ENG9603

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9603 Page 3
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM
Magnetic susceptibility reading of 5:0.06 at 31m.
32.3 34.0 FUCHSITIC ULTRAMAFIC VOLCANICS (4d) Typical ultramafic
volcanics with fuchsite alteration at 3^ abundance.
Quartz carbonate veins ate 30% volume. Sulphides present
in trace amounts as finely disseminated euhedral
crystals. Magnetic susceptibility reading of 5:0.63 at
33m. Lower contact at 45 degrees.
34.0 36.9 INTERMEDIATE DIKE (9) Medium to coarse grained medium
grey in colour and massive. This section contains
inclusions of fuchsite rich ultramafic fragments.
Sulphide content is up to 2 \ a s fine and coarse euhedral
crystals heterogeneously distributed in the dike.
Magnetic susceptibility readings of 5:0.41 at 36.4m.
36.9 49.0 BRECCIATED ULTRAMAFIC VOLCANICS (4d-a) Typical fuchsite
rich ultramafics that become less fuchsitic with depth.
The ultramafic appear to be more brecciated than the
previously strongly foliated volcanics. Foliations are
also at a lower angle to the core axis. This section
contains brecciated mafic to intermediate dike material
as well as competent dikes less than 1m in thickness.
Sulphide content is variable with short intersections up
to 2% coarse pyrite. Magnetic susceptibility readings
as follows: 5:0.36 at 37m, 5:0.45 at 40m, 5:0.61 at 43m.
49.0 59.0 SIL. ULTRAMAFIC VOLCANICS/INTERMEDIATE DIKE (43/9)
ASSAYS
TO WIDTH Au (ppb)
96306 33 .00 34 .00 1.00
96307
96308
96309
96310
96311
96312
34. 00
35. .00
36. . 00
37 .00
37. .50
45. .00
35. 00
36. .00
37. .00
37 .50
38. . 50
46 .00
1. 00
1 . .00
1 .00
0 .50
1 .00
1 .00
21
65
74
170
115
213
NIL
96313 54.20 55.20 . 00 NIL
HOLE No: ENG9603

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9603 Page 4
FROM TO LITHOLOGICAL DESCRIPTION
Competent and brecciated lithology similar to the
previous ultramafic sequence but medium to dark grey with
minor serpentine alteration. Quartz-carbonate veining
varies in abundance and appears to be more of a stockwork
than the previously foliation parallel veining. Magnetic
susceptibility readings of: 5:0.60
59.0 59.5 FUCHSITIC ULTRAMAFIC VOLCANICS (4d) Alteration contact
aureole to the underlying lithology. Magnetic
susceptibility reading of 5:0.59.
59.5 66.2 COARSE FELDSPAR PORPHYRY DIKE (lOcy) Similar to
previously named lithology. Massive pyrite within a 2cm
vein at 61m. Minor quartz veining up to it volume
subparallel to the core axis. Minor fracturing up to 2%
with infilling by chlorite. Sulphides consist of trace
to J.% finely disseminated euhedral pyrite throughout the
section. Contact at 53 degrees c .a. Magnetic
susceptibility reading as follows: 5:0.12 at 61m, 5:0.14
at 64m, 5:0.28 at 66.1m.
66.2 67.2 FUCHSITIC ULTRAMAFIC VOLCANICS (4d) Similar to previous
fuchsite rich sections located at the margins of albitite
dikes. Magnetic susceptibility reading of 5:0.63. Fold
axis observed at this section.
67.2 80.1 SERPENTINIZED ULTRAMAFIC VOLCANICS (4e) Similar to
previously described serpentine rich ultramafics. This
SAMPLE No.
96314
96315
96316
96317
96318
96319
96320
96321
96322
96323
96324
96325
FROM
57.60
58 . 60
59. 60
60 . 60
61. 60
62 . 60
63 . 60
64 . .50
65. 50
66.20
71. 00
72 . 00
ASSAYS
TO WIDTH Au (ppb)
58.60
59. .SO
60 .60
61 .60
62. .60
63 . .60
64. .50
65 .50
66 .20
67 .10
72 .00
72 .40
1.00
1 . 00
1 . 00
1. 00
1 . 00
1. 00
0 . 90
1 . 00
0. 70
0.90
1.00
0.40
3
177
393
57
120
298
245
101
12
NIL
NIL
HOLE No: ENG9603

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9603 Page 5
FROM TO LITHOLOGICAL DESCRIPTION
section is characterized by a 3(H quartz -carbonate vein
content by volume and sporadic sulphide mineralization up
to 3fc coarse pyrite over short intervals of 10cm.
Section is intruded by thin metre wide dark syenite dikes
at 68m. Alteration is dominated by serpentine with minor
talc and fuchsite in some of the quartz-carbonate veins.
Magnetic susceptibility readings as follows: 5:5.45 at
70m, 5:17.5 at 73m, 5:20.5 at 76m, 5:10. 2 at 79m.
80.1 82.3 SYENITE DIKE (9e) Dark red, medium grained and
variably mineralized syenite. .Sulphide content is
between trace and it finely disseminated pyrite
heterogeneously distributed along chloritized and
serpentinized fractures. Syenite is weakly foliated.
Magnetic susceptibility reading of 5:47.2 at 80.2m,
5:9.63 at 81m, 5:0.51 at 82m.
82.3 88.1 SERPENTINIZED ULTRAMAFIC VOLCANICS (4e) Typical
serpentine rich ultramafics with fault breccia zone in
the last metre of this section. Alteration dominated by
serpentine and talc, quartz and carbonate and minor
kfeldspar in some of the veins. Sulphides are developed
sporadically as mm sized euhedral pyrite crystals
associated with foliation planes over 5cm intervals.
Magnetic susceptibility readings as follows: 5:0.73 at
83m, 5:'0.49 at 85m, 5:0.59 at 88m.
88.1
ASSAYS
SAMPLE No. FROM TO WIDTH Au
96326 72.40 73.40 1.00
96327 77.10 78.10 1.00
96328 80.10 80.20 0.10
96329 80.20 81.20 1.00
96330 81.20 81.60 0.40
96331 81.60 82.60 1.00
96332 82.60 83.60 1.00
118.5 SYENITE DIKE SWARM (9e) This section contains a 96333 88 .20 89.10 0. 90
(ppb)
NIL
2
3
2
NIL
NIL
NIL
HOLE No: ENG9603

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9603 Page 6
FROM TO LITHOLOGICAL DESCRIPTION
series of syenite dikes with metre wide intervals of
serpentinized and brecciated ultramafics. The dikes vary
from bright red to greyish red in colour and from fine
grained to medium grained. Contact range from 60 degrees
to 22 degrees. Some of the dikes contain inclusions from
the other dikes. The last 2m of this section is
dominated by a fine grained highly silicified red syenite
with 2-3% pyrite intercalated with fuchsite rich
ultramafic volcanics and epidote rich massive syenite
dikes . Sulphide content of the syenite is trace to il.%
disseminated pyrite, and variable amounts of magnetite up
to 2V volume. Magnetic susceptibility readings are as
follows: 5:0.53 at 88.5m, 5:19.0 at 91m, 5:13.6 at 94m,
5:6.49 at 97m, 5:0.67 at 104m, 5:0.34 at 106m, 5:0.39 at
108m, 5:0.49 at 109m, 5:0.53 at 112m, 5:0.51 at 115m,
5:0.45 at 118m.
SAMPLE No.
96334
96335
96336
96337
96338
96339
96340
96341
96342
96343
96344
96345
96346
96347
96348
96349
96350
96351
96352
96353
96354
96355
96356
96357
96358
96359
96360
96361
FROM
89. . 10
89. .60
90. .60
91. . 50
92 . .60
93 . .60
94. .60
95. .60
96. .50
97 . 50
97. .80
98 . . 90
100 .00
101. .00
101, .90
102. .80
103 . .80
104 . .80
105. .70
106 .70
107 .80
108 .80
109 .80
110 .70
111 .70
112 .70
113 .70
114 .70
ASSAYS
TO WIDTH Au
89. .60
90. .60
91 . 50
92. .60
93. .60
94, .60
95 .60
96 .50
97 .50
97 .80
98 .90
100 . 00
101 . 00
101 . 90
102 .80
103 .80
104 .80
105 . 70
106 .70
107 . 80
108 .80
109 . 80
110 .70
111 .70
112 .70
113 .70
114 .70
115 .70
0. 50
1. 00
0. 90
1 . 10
1 . 00
1. 00
1. 00
0. 90
1. 00
0. 30
1. .10
1. 10
1 . 00
0. 90
0. 90
1. 00
1. 00
0. 90
1. 00
1 . 10
1. .00
1. .00
0. .90
1 . .00
1 . . 00
1. .00
1. 00
1. .00
(ppb)
NIL
NIL
NIL
NIL
NIL
NIL
NIL
NIL
2
NIL
NIL
NIL
NIL
NIL
2
NIL
81
96
180
259
295 .
98
33
22
2
10
9
24
HOLE No: ENG9603

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9603 Page 7
FROM TO LITHOLOGICAL DESCRIPTION
118.5 126.0 FUCHSITIC ULTRAMAFIC VOLCANICS (4d) Fuchsite
rich up to 30* volume set in massive to spinifex textured
ultramafics that are crosscut by numerous quartzcarbonate
veins up to 35* volume. Sulphides are variable
up to 2% coarse pyrite heterogeneously distributed in
core. The ultramafics are intruded by a set of
intermediate fuchsite rich dikes that intensify fuchsite
alteration in the ultramafics at the contacts. Magnetic
susceptibility readings as follows: 5:0.69 at 120m,
5:0.63 at 124m, 5:0.45 at 126m.
126.0 142.0 ALBITITE DIKE (lOcq-y) The top 3m of this
section is characterized by a 50*!: distribution of
intermediate fuchsitic dikes and coarse to fine quartzfeldspar
phyric albitite dikes. After the initial 3m the
section consists of massive competent albitite, 80% fine
and 20% coarse grained with less than 1m intersection of
the foliated fuchsite-rich intermediate dike spaced every
5m. An inclusion of highly fuchsite rich spinifex
textured ultramafics is included at 142.3m depth.
Alteration is dominated by K-feldspar observed along
fractures and more pervasively at the 139m interval in
proximity to a large zone of coarse grained albitite.
Sulphide mineralization is pervasive and consists of very
SAMPLE No.
96362
96363
96364
96365
96366
96367
96368
96369
96370
96371
96372
96373
96374
96375
96376
96377
96378
96379
96380
96381
96382
FROM
115. .70
116 . 10
117 , .00
117. .90
118 , .90
119. . 90
123 . . 90
124. . 90
125 . 90
127. .00
128 . 00
128 .60
129 .30
130 .30
131 .30
132 . 30
133 .30
134 .20
135 .20
136 .10
137 . 20
ASSAYS
TO WIDTH Au
116. .10
117. 00
117 .90
118. . 90
119. .90
120 .90
124. . 90
125 .90
126
128
128
129
130
131
132
133
134
135
136
137
137
.90
.00
.60
.30
.30
.30
.30
.30
.20
.20
.10
.20
.60
0. .40
0. .90
0 . . 90
1 . .00
1. .00
1 .00
1 . .00
1
. 00
1
1
0
0
1
1
.00
.00
.60
.70
.00
.00
1 .00
1 .00
0 . 90
1 .00
0 .90
1 .10
0 .40
(ppb)
2
7
NIL
5
7
3
19
33
79
142
62
82
94
79
235
82
178
159
357
147
214
HOLE NO: ENG9603

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9603 Page 8
FROM TO LITHOLOGICAL DESCRIPTION
fine disseminations of pyrite in trace to 2%
concentrations. Sulphides are carried by all rock types
in this section. Quartz-carbonate veins contain minor
pyrite mineralization along the margins up to UT, with
the veins developed at 2% volume and subparallel to the
c. a. at approximately 44 degrees c. a. Magnetic
susceptibility readings are as follows: 5:0.18 at 127m,
5:0.59 at 130m, 5:0.43 at 133m, 5:0.10 at 136m, 5:0.20 at
139m, 5:0.12 at 142m.
142.0 143.6 ALBITITE AND ULTRAMAFIC VOLC . (lOcqy S, 4 ed)
This section represents the transition between
143.6 154. O
the albitite dike and the ultramafic volcanics and
consists of 50% dike and 50% ultramafic material.
Alteration is variable and consists of fuchsite and
serpentine in the ultramafics and kfeldspar and fuchsite
in the intermediate and albitite dikes. Sulphide
mineralization consists of trace disseminated pyrite in
the dikes. Dike contacts at 50 degrees c.a. and 20
degrees c.a. Magnetic susceptibility reading of 5:0.67.
ULTRAMAFIC VOLCANICS ( 4cd-e) Spinifex
textured fuchsite rich ultramafic volcanics typical of
previous spinifex textured sections, with up to 3*^ coarse
euhedral pyrite for the initial 6m then changes to a more
massive'serpentine rich ultramafic volcanic. Magnetic
susceptibility readings as follows: 5:0.53 at 144m,
5:0.84 at 145m, 5:0.30 at 148m, 5:0.71 at 151m and 5:0.53
SAMPLE No.
96383
96384
96385
96386
96387
96388
96389
96390
96391
96392
96393
96394
96395
FROM
137 .60
138 .60
139 .50
140 .50
141 . 50
142 .10
143 .10
143 .60
144.60
145.60
146 .60
147 . 50
148 .40
ASSAYS
TO WIDTH Au
138. .60
139 . 50
140 . 50
141 . 50
142 .10
143 . 10
143 .60
144. 60
145. 60
146.60
147. 50
148.40
149.40
1 . 00
0. . 90
1. .00
1 . . 00
0 .60
1 .00
0 . 50
1.00
1. 00
1. 00
0 . 90
0. 90
1.00
(ppb)
233
154
312
201
79
82
81
12
5
9
3
NIL
7
HOLE NO: ENG9603

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9603 Page 9
FROM TO LITHOLOGICAL DESCRIPTION
at 154m.
154.0 END OF HOLE
DOWN-HOLE SURVEY DATA
DEPTH INCLINATION BEARING
1.00 -45.00 315.00
100.00
154.00
-44.00
-45.00
315.00
315.00
SAMPLE No.
ASSAYS
TO WIDTH Au (ppb)
HOLE No: ENG9603

PROPERTY: English
HOLE No.: ENG9604
Collar Eastings: 483016.00
Collar Northings: 5319932.00
Collar Elevation: O. 00
Contractor was NDS Drilling of Timmins, Ont.
FROM TO LITHOLOGICAL DESCRIPTION
0.0 8 .0 CASING ON BEDROCK ( Ob)
DELORO GROUP
Cameco Corporation
DIAMOND DRILL LOG
8.0 44.0 FELSIC FRAGMENTAL (3ad) Strongly foliated felsic
f ragmental/breccia . The felsics vary from a medium green
to a pale creme white colour. Alteration is variable and
swings from a chlorite dominated matrix to a sericite
dominated matrix with variable silica flooding also
present. The variety of alteration dominated matrices
play host to lapilli sized felsic to quartz elongate
fragments. The chlorite altered section is heavily
intruded by a series of parallel but displaced quartz-
carbonate veins that are yellowish and to a lesser extent
white in colour. These veins are highly folded and
disrupted and in some cases from breccia zones. The
sericite section is contains a lower abundance of veins
but is similarily deformed. Within both the sericite and
chlorite sections blue quartz is observed as irregularly
shaped disrupted quartz vein inclusions up to 2cm in
size. Faults are developed at 9m, 10m, 13m and are
approximately 20cm wide. Sulphides are developed as fine
disseminations up to il.% and sporadically as clots within
chlorite infilled fractures and along foliation planes up
Collar Inclination: -45.00
Grid Bearing: 135.00
Final Depth: 116.00 metres
Hole was collared in claimft 1155891
SAMPLE No. FROM
96396
96397
96398
96399
96400
96401
96402
96403
96404
96405
96406
10. .00
11 . .00
16 . .00
28 . 00
29 . 00
30 .00
37 .00
38 .00
39 .00
43 .00
43 .70
Logged by: P. Chubb
Date: 29/10/96-30/10/96
Down-hole Survey: Acid
ASSAYS
TO WIDTH Au (ppb)
11 . 00
12. 00
17. 00
29. 00
30. 00
31 . 00
38. 00
39. 00
40. 00
43. 70
43. 90
1 . ,00
1 . .00
1 . 00
1 .00
1 .00
1 .00
1 .00
1 .00
1 .00
0 .70
0 .20
NIL
NIL
NIL
33
NIL
3
NIL
NIL
NIL
5
NIL
HOLE No: ENG9604

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9604 Page 2
FROM TO LITHOLOGICAL DESCRIPTION
to 4% volume. Disseminated pyrite is also developed
within small quartz veins up to J.% volume. The base of
this section displays strong magnetic signatures over
short intervals that may represent a poor oxide facies
iron formation. Thin less than 25cm wide albitite and
intermediate dikes less than J.% volume of section intrude
the stratigraphy. Magnetic susceptibility readings as
follows: 5:1.96 at Bm, 5:0.34 at 10m, 5:0.32 at 13m,
5:0.55 at 16m, 5:1.08 at 22m, 5:0.73 at 25m, 5:0.30 at
28m, 5:1.18 at 31m, 5:0.63 at 34m, 5:29.5 at 37m, 5:0.43
at 40m, 5:0.61 at 43m. The more mafic looking sections
are also more magnetic.
44.0 64.0 FELSIC TUFF-BRECCIA (3ae) The upper contact of this
unit is gradational and displays with tuff and
tuff-breccia intercalated. The contact and top portion
of the tuff-breccia displays variable but strong
K-feldspar alteration of the tuff-breccia fragments. The
matrix between the fragments consists of a lapilli tuff
and is chloritized to varying degrees, and can be
strongly magnetic. The fragments are themselves composed
of a lapilli-tuff. The entire section is well foliated
and variably mineralized. This section is intruded by a
few syenite and intermediate dike types that contain
trace to li' finely disseminated pyrite. Magnetic
susceptibility readings are as follows: 5:0.73 at 45m,
5:4.65 at 49m, 5:25.2 at 52m, 5:1.31 at 55m, 5:0.82 at
58m, 5:2.35 at 61m, 5:1.90 at 64m. Sulphide
SAMPLE No.
96407
96408
96409
96410
96411
96412
96413
96414
96415
96416
96417
96418
96419
43 . 90
45 . 10
46 . 10
47 . 20
48 . 20
49. 10
55. .10
56. .10
57 . .00
58 . .00
59. .10
60. .10
61. .00
ASSAYS
TO WIDTH Au (ppb)
45. 10
46 . 10
47. .20
48 . 20
49. .10
50. .10
56. .10
57. .00
58. .00
59. .10
60. .10
61 .00
62 .00
1 . 20
1 . 00
1. 10
1. 00
0. 90
1. .00
1. .00
0. .90
1 . . 00
1. .10
1 . . 00
0 .90
1 .00
NIL
NIL
19
NIL
NIL
158
NIL
14
NIL
NIL
7
10
5
HOLE No: ENG9604

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9604 Page 3
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM
mineralization consists of coarse euhedral pyrite
associated with the darker phases of this section with
local concentrations up to 2fc. Blue quartz fragments
lapilli sized are common in some sections within the tuff
breccia. Core is competent and relatively hard.
64.0 65.6 FELSIC TUFF BRECCIA (3ae) Similar to the above section
but no kfeldspar alteration. Sulphide content consists
of trace to J.% disseminated and fragment margin related
pyrite. Magnetic susceptibility readings is 2.19 at 65m.
65.6 66.9 GABBRO (8a) Medium grained massive gabbroic dike with
sharp contacts at 60 degrees c.a. at 66m. Magnetic
susceptibility reading of 5:1.04 at 66m.
66.9 69.8 ALBITITE DIKE (lOcq) Fine grained albitite dike with
small fuchsitic to chloritic elongate lapilli sized
fragments. Sulphide mineralization consists of
disseminated pyrite throughout the section. Magnetic
susceptibility reading of 5:0.22 at 68m. upper contact
at 90 degrees c.a. and lower contact at 75 degrees c.a..
69.8 74.3 FELSIC TUFF BRECCIA (3ae) Similar to the previous tuff
breccia. Primary textures are more distinct with a well
developed foliation. Sulphides consist of trace amounts
of clotty pyrite and minor magnetite associated with the
chlorite rich matrix. Magnetic susceptibility reading of
5:9.92 at 70m, 5:3.34 at 73m, 5:1.17 at 74m.
96420 63 .80 64 .80
96421
96422
96423
96424
96425
96426
96427
96428
96429
96430
64 .80
65.80
66 . 90
67. 90
68.90
69.70
70.70
71 .70
72 .10
73 .00
ASSAYS
TO WIDTH Au (ppb)
65. 80
66. 90
67.90
68.90
69. 70
70.70
71.70
72.10
73 .00
74 .00
1. 00
1.10
1.00
1.00
0.80
1.00
1 . 00
0 .40
0.90
1.00
NIL
NIL
113
365
146
NIL
NIL
5
34
NIL
HOLE No: ENG9604

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9604 Page 4
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No.
74.3 75.1 INTERMEDIATE DIKE (9) Massive medium grey gabbroic to
leucocratic dike with trace pyrite. Magnetic
susceptibility reading of 5:1.14 at 75m. Pyrite developed
as fine disseminations. Upper contact at 39 degrees c.a.
and lower contact at 42 degrees c.a.
TISDALE GROUP
75.1 75.5 ULTRAMAFIC VOLCANICS (4a) Well foliated with abundant
quartz-carbonate veins, this competent medium grey
section appears to be weakly silicified. Magnetic
susceptibility reading of 5:3.71. Sulphides consist of
trace finely disseminated pyrite and up to 3V pyrite at
the dike margins.
75.5 85.2 ALBITITE, SYENITE AND INTERMEDIATE DIKE SWARM ( 10cqS9)
Fine grained creme white albitite dikes up to 3m wide and
intermediate dikes less than 2m wide intrude the
ultramafic volcanics in this section and make up 80% of
the rock mass. The ultramafics are typical of what is
observed in other holes and are pervasively serpentinized
and chloritized with minor fuchsite within the quartz-
carbonate veins. The ultramafic display sulphides at the
margins ,of the dikes but are otherwise barren. Sulphides
within the dikes are developed as fine disseminations
within the albitite dike but are less apparent within the
ASSAYS
FROM TO WIDTH Au ( ppb)
96431 74.00 74.80 0.80 67
96432 74. 80 75.30 O. 50
96433
96434
96435
96436
96437
96438
96439
96440
75. 30
76. 30
76. 80
77. 30
77. 80
78. 30
79. 30
80. .30
76 . 30
76. 80
77. 30
77. 80
78 . 30
79. 30
80. 30
81. .30
1. 00
0. 50
0. 50
0. 50
0. 50
1. 00
1. 00
1. .00
9
NIL
3
NIL
NIL
NIL
2
NIL
HOLE No: ENG9604

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9604 Page 5
FROM TO LITHOLOGICAL DESCRIPTION
intermediate dike. Magnetic susceptibility readings are
as follows: 5:0.20 at 76m, 5:0.51 at 79m, 5:0.71 at 82m,
5:10.0 at 85m. The highest reading is associated with a
syenite dike.
85.2 89.5 ULTRAMAFIC VOLCANICS (4a) Typical serpentinized
spinifex and massive ultramafic volcanics. This section
is dark green except for the quartz carbonate veining
that makes up lS-20% of the volume. Lower contact is at
32 degree c.a.. Magnetic susceptibility reading of
5:0.57 at 88m. Section is barren of sulphides.
89.5 91.5 SYENITE DIKE (9e) Syenite dike is similar to those
described previously and is dark red and medium grained
with small less than 2mm sized fuchsitic fragments. No
sulphides observed. Magnetic susceptibility reading of
5:0.51 at 91m.
91.5 94.4 ALBITITE DIKE (lOcq) Similar to previously described
sections of albitite dike. This section contains
inclusions of fuchsitic ultramafic volcanics less than
5cm in width. Sulphides are developed as fine
disseminations of pyrite up to H volume. Minor
intrusion by small quartz-carbonate veins. Magnetic
susceptibility readings average 5:0.41 over the entire
dike.
SAMPLE No. FROM
96441
96442
96443
96444
96445
96446
96447
84. .40
85. .40
89, .40
90 .40
91 .40
92 .40
93 .40
ASSAYS
TO WIDTH Au (ppb)
94.4 97.7 FUCHSITIC ULTRAMAFIC VOLCANICS (4d) Massive fuchsite 96448 94.40 95.40 1. 00 NIL
85. 40
86 . 40
90. .40
91. .40
92. .40
93. .40
94, .40
1. 00
1. 00
1. .00
1, . 00
1 , . 00
1 . 00
1 .00
NIL
3
NIL
NIL
9
NIL
261
HOLE No: ENG9604

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9604 Page 6
FROM TO LITHOLOGICAL DESCRIPTION
rich ultramafic volcanics similar to the previous section
with spinifex and massive textures present. Sulphides
are developed as disseminations along foliation planes in
trace amounts. Magnetic susceptibility reading of 5:0.47
at 97m.
97.7 104.2 ALBITITE DIKE (lOcq) Typical albitite dike with
a faint pink tinge due to minor kfeldspar. The albitite
is intruded by an intermediate fuchsite rich dike.
Sulphides are developed as fine disseminations of pyrite
throughout the core in both dike types. Magnetic
susceptibility readings as follows: 5:0.22 at 100m,
5:0.10 at 103m. The upper contact is at 72 degrees c. a.
and the lower contact is at 27 degrees c. a.
104.2 107.6 FUCHSITIC ULTRAMAFIC VOLCANICS (4d) Similar
to the previously described ultramafics with a lower
gradational alteration contact. Trace pyrite developed
as mm sized clots. One major quartz vein runs the length
of the core the rest are parallel to the foliation.
Magnetic susceptibility reading of 5:0.61 at 106m.
107.6 112.5 SYENITE -t- SERF. ULTRAMAFIC VOLCANICS (9e4-4e)
Coarse grained metre thick dark red syenite dikes set
within serpentinized ultramafic volcanics making up 50%
volume of the rock. Syenite has \ '-i d isseminated pyrite
mineralization. This dike gets progressively darker with
depth. Upper contact at 75 degrees. The ultramafic are
SAMPLE No.
96449
96450
96451
96452
96453
96454
96455
96456
96457
96458
96459
96460
96461
96462
96463
96464
96465
96466
FROM
95. .40
96. .40
97. .40
97. .70
98. 70
99. .70
100. 70
101. .70
102. . 70
103 . .60
104 . .20
105. .20
106. . 10
107. .20
108 .60
109 . 60
110 .20
110 . 80
ASSAYS
TO WIDTH Au (ppb)
96 .40
97 .40
97 .70
98 .70
99 .70
100 .70
101 .70
102 .70
103 .60
104 .20
105 .20
106 .10
107 .20
107 . 50
109 .60
110 .20
110 .80
112 .00
1 . 00
1. . 00
0. .30
1. . 00
1. . 00
l . 00
1. . 00
1 , . 00
0. . 90
0. .60
1
0
1 0
.00
.90
.10
. 30
1 .00
0 .60
0 .60
1 .20
NIL
NIL
NIL
106
74
15
51
27
266
17
21
55
62
1029
17
12
NIL
NIL
HOLE NO: ENG9604

PROPERTY: English
HOLE No.: ENG9604
FROM TO LITHOLOGICAL DESCRIPTION
Cameco Corporation
barren of sulphides but are well foliated. Quartz-
carbonate veining amounts to 5% of the volume. Magnetic
susceptibility reading of 5:18.6 from the syenite and
5:0.56 from the ultramafics.
112.5 116.0 SERPENTINIZED ULTRAMAFIC VOLCANICS (4e)
Massive dark green soft ultramafics as described
previously in other sections. Magnetic susceptibility
readings average 5:25.0 over this section. No sulphides
observed.
116.0 END OF HOLE
DOWN-HOLE SURVEY DATA
DEPTH INCLINATION B EARING
i.oo -45.00 135.00
116.00 -45.00 1 35 0 0
DIAMOND DRILL LOG
SAMPLE No. FROM
96467 112.00
96468 113.00
96469 114.00
96470 115.00
ASSAYS
TO WIDTH Au (ppb)
113.00
114.00
115.00
116.00
1.00
1.00
1.00
1.00
NIL
S
l
NIL
Page 7
HOLE No: ENG9604

PROPERTY: English
HOLE No.: ENG9605
Collar Eastings: 482986.00
Collar Northings: 5319240.00
Collar Elevation: 0.00
Contractor was NDS Drilling, Timmins, Ont.
FROM TO LITHOLOGICAL DESCRIPTION
0.0 8.0 CASING ON BEDROCK (Ob)
DELORO GROUP
Cameco Corporation
DIAMOND DRILL LOG
8.0 58.0 FELSIC LAPILLI TOFF (3d) The lapilli tuff is medium
grey green in colour and well foliated. Fragments are
monomictic but poorly sorted, angular to rounded and
matrix supported. This section is intruded by a number
of thin fragment rich grey syenite dikes that contain up
to It disseminated pyrite. The dikes are developed at
18m. Small intersections of fine grained sediment are
intercalated with the felsic volcanics. Within the
poorly sorted felsic fragmentals are a section of well
sorted finer grained tuff to lapilli tuff. Alteration is
dominated by sericite with small intervals less than 2m
wide sections of chlorite dominated alteration. Narrow
fault zone less than 20cm wide at 12.4m and at 41m.
Sulphide mineralization is restricted to fractures and
small intersections of the host rock where it is
developed as fine disseminations and clots of pyrite up
to 2%. Trace amounts of chalcopyrite are present within
larger pyrite clusters and clots. Pyrite mineralization
is also concentrated along the edges of the coarser sized
fragments. Questionable disrupted pyrite fragments in
Collar Inclination: -45.00
Grid Bearing: 110.00
Final Depth: 304.00 metres
Hole Collared in claimtt 1155888
SAMPLE No. FROM
96471
96472
S6473
96474
96475
96476
96477
96478
96479
96480
96481
96482
96483
96484
96485
96486
964B7
96488
96489
96490
10. 00
11 . 00
15. 10
16 . 10
17. 10
17. 50
18 . 50
25. 40
26. 40
27. .40
28. 40
29. .40
30. . 30
33 .50
34 . 50
35 .50
36 . 30
38 .00
48 . 10
49 .10
Logged by: P. Chubb
Date: 31/10/96-02/11/96
Down-hole Survey: Acid
ASSAYS
TO WIDTH Au (ppb)
11.
12.
16.
17.
17.
18.
19.
26.
27.
28.
00
00
10
10
50
50
50
40
40
40
29. 40
30. . 30
31, .30
34 . . 50
35. . 50
36 . 30
37. . 30
39 . 00
49 . 10
50 . 10
1. 00
1 . 00
1 . 00
l . 00
0 . 40
1. 00
1 . 00
1. ,00
1 . .00
1 , .00
1. .00
0 .90
i .00
i . 00
i .00
0 .80
1 .00
1 .00
11 . 00
.00
5
12
NIL
NIL
33
41
15
65
NIL
NIL
NIL
9
12
14
31
NIL
NIL
19
NIL
NIL
HOLE No: ENG9605

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9605 Page 2
FROM TO LITHOLOGICAL DESCRIPTION
core. Quartz veins are minimal and make up less than I'fe
of the core. The veins are oriented subparallel to the
foliation intersecting the core at 30 to 90 degree c. a..
Magnetic susceptibility readings as follows: 5:0.32 at
10m, 5:1.08 at 13m, 5:0.84 at 16m, 5:0.32 at 19m, 5:0.61
at 22m, 5:0.32 at 25m, 5:0.36 at 28m, 5:0.88 at 32m,
5:0.28 at 34m, 5:0.57 at 37m, 5:0.32 at 40m, 5:0.30 at
43m. Core is competent and moderately hard.
58.0 76.0 FELSIC TOFF BRKCCIA (3ae) This section is dominated by
a sericite rich lapilli-tuff to tuff breccia that has
been highly altered and is polymictic with a variety of
fragments present. Alteration is dominated by sericite
but the core has also been weakly silicified and is
relatively hard compared to the previous sections.
Section becomes more chloritic with depth up to 5% at
base. Quartz veins are limited to less than H; but occur
as 5cm wide pure bull quartz. Some of the quartz veins
appear to be disrupted and fragmented in places.
Sulphide mineralization is pervasive and at 2-3%
abundance as fine to coarse euhedral pyrite disseminated
in core and concentrated along fragment margins and vein
related. Magnetic susceptibility readings as follows:
5:0.22 at 58m, 5:0.59 at 61m, 5:0.36 at 64m, 5:0.34 at
67m, 5:1.71 at 70m, 5:1.2 at 73m, 5:0.49 at 76m.
76.0 78.9 ALBITITE DIKE (lOcq) Typical albitite dike as observed
in other holes with pervasive trace to 14 pyrite set
SAMPLE No.
96491
96492
96493
96494
96495
96496
96497
96498
96499
96500
96501
96502
96503
96504
96505
96506
96507
96508
96509
96510
96511
96512
96513
96514
FROM
50. .10
51 . .00
51. .90
52 . 90
53 .90
54. .90
60 . .00
61. .00
62 .00
63 .00
64 .00
65. .00
66 .00
67. .00
68, . 00
69. . 00
70. . 00
70 .60
71, .20
72 .20
73 .20
74 .20
75 .20
76, .20
ASSAYS
TO WIDTH Au
51. 00
51. 90
52. 90
53. 90
54. 90
55. . 90
61. .00
62 . . 00
63 . 00
64 . .00
65. 00
66. .00
67. , 00
68. .00
69. . 00
70. .00
70. .60
71, .20
72. .20
73 . .20
74 . .20
75, .20
76 .20
77 .20
0. .90
0 . .90
1 . .00
1, .00
1 .00
1 , .00
1. .00
1. .00
1 . .00
1. .00
1, .00
1. . 00
1, .00
1. .00
1 .00
1 . .00
0, .60
0 .60
1, .00
1 .00
1. . 00
1 .00
1 1
.00
.00
(ppb) '
2
103
9
3
NIL
36
2
10
9
7
7
10
146
50
36
5
2
7
7
36
10
14
33
55
HOLE No: ENG9605

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9605 Page 3
FROM TO LITHOLOGICAL DESCRIPTION
within a fine grained beige massive lithology. Upper
contact is irregular and at 43 degrees c. a. and the lower
contact is at 35 degrees c. a.. Magnetic susceptibility
reading of 5:0.32.
78.9 82.1 LAPILLI TOFF SUPPORTED SULPHIDE IRON FORMATION (3ae k 6d)
Semi-massive to massive sulphide set within a lapilli
tuff. Sulphides appear to either have replaced some of
the fragments or represent disrupted sulphide beds within
a proximal turbidite. Sulphides account for SO-60%
pyrite. Magnetic susceptibility readings average:
5:0.52.
82.1 90.7 SILICIFIED LAPILLI TUFF (3ae) Similar to previous
lapilli supported iron formation except that the sulphide
content is approximately 5fc abundance. Last metre of
this section becomes intensely silicified and cherty
looking. 20cm wide massive medium grained barren mafic
dike at the end of this section. Magnetic susceptibility
readings as follows: 5:0.38 at 85m, 5:0.36 at 88m, 5:0.22
at 90m.
90.7 94.0 GRAPHITIC SILTSTONE (5dp) Black massive to
foliated/banded very fine grained and hard graphitic
siltstone. Quartz vein/fragment content is ls-30% but
drops of within the first 50cm of this section until it
reaches less than l* volume. Sulphide content varies
with sulphides developed within thin bands/foliation
SAMPLE No.
96515
96516
96517
96518
96519
96520
96521
96522
96523
96524
96525
96526
96527
96528
96529
96530
96531
96532
FROM
77. 20
78. 20
78. .90
79. .20
80. .20
81. .15
82 . 10
83 . .10
84 . 10
85. .10
86. .10
87. .10
88 .10
89 .10
90 .10
91 .00
92 .00
93 .00
ASSAYS
TO WIDTH Au
78. 20
78. 90
79. .20
80. .20
81. . 15
82. .10
83. 10
84. 10
85. 10
86. 10
87. 10
88. 10
89. 10
90. 10
91. . 00
92. . 00
93, .00
94 .00
1. 00
0. 70
0. .30
1 . .00
0 . 95
0 .95
1 . 00
1. 00
1 . 00
1. 00
1. 00
1. 00
1. 00
1 , 00
0 . 90
1 .00
1 . . 00
1 . 00
(ppb)
69
182
14
250
99
278
57
51
5
33
29
15
14
12
81
144
370
187
HOLE No: ENG9605

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9605 Page 4
FROM TO LITHOLOGICAL DESCRIPTION
planes and as framboidal to botryoidal pyrite growths up
to 3cm in diameter. Sulphides vary in abundance from
trace to 4C^ over a 70cm interval. Intense folding is
observed within the core with M-type folds present.
94.0 97.0 LAPILLI TUFF SUPPORTED SULPHIDE IRON FORMATION (3ae k 6d)
Semi-massive to massive sulphide set within a lapilli
tuff. Sulphides appear to either have replaced some of
the fragments or represent disrupted sulphide beds.
Disrupted quartz carbonate veins are prominent with 20%
of the volume accounted for. Pyrite accounts for 20-30%
of the total volume. Magnetic susceptibility readings
average: 5:1.51.
TISDALE GROUP
97.0 137.1 ULTRAMAFIC VOLCANICS (4ad) Massive to spinifex
textured competent ultramafics. Alteration is dominated
by carbonate assemblages including dolomite and ankerite
with accessory fuchsite also present. Fuchsite is
present only for the initial 4m of this section in the
host rock but persists in the quartz carbonate veins
sporadically for an extended interval. Quartz-carbonate
veining makes up ID-15% of the total volume. The
ultramafics are initially green grey but become pale grey
with depth. Sulphide mineralization in the top 3m
consists of 1-2V coarse pyrite. Fuchsite alteration in
SAMPLE No.
96533
96534
96535
96536
96537
96538
96539
96540
96541
96542
96543
96544
96545
96546
FROM
94.00
95.00
96 .00
97. .00
98. .00
99. .00
100. .00
101 .00
115 .30
124 .00
129 .00
134 .40
135 .40
136 .40
ASSAYS
TO WIDTH Au (ppb)
95.00
96.00
97.00
98. 00
99. 00
100. 00
101. 00
102. .00
116 . .30
125. .00
130. .00
135. .40
136 .40
137. .10
1.00
1.00
1.00
1. 00
1. 00
1. 00
1 , .00
1. .00
1. .00
1. . 00
1 .00
1, .00
1 .00
0. .70
219
58
185
3
5
3
NIL
2
3
21
7
17
3
77
HOLE No: ENG9605

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9605 Page 5
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM
the quartz-carbonate veins becomes more prevalent in the
last 3m and sulphide content is up to 2%. Magnetic
susceptibility readings are as follows: 5:0.55 at 100m,
5:0.71 at 103m, 5:0.47 at 106m, 5:0.61 at 109m, 5:0.65 at
112m, 5:0.65 at 115m, 5:0.69 at 118m, 5:0.61 at 124m,
5:0.65 at 127m, 5:0.69 at 130m, 5:0.53 at 133m, 5:0.65 at
136m.
137.1 141.5 ALBITITE DIKE (lOcq) Typical beige albitite
dike with chloritized subrounded to angular fragments up
to 2cm in size. Sulphides are developed as fine to
coarse euhedral disseminations' of pyrite throughout the
core and as concentrations along the margins of some of
the fragments. Sulphide abundance is up to Ifc. Average
magnetic susceptibility reading of 5:0.51 for this
section. Upper contact at 34 degrees c.a. and the lower
contact is at 35 degrees c.a.
141.5 169.0 ULTRAMAFIC VOLCANICS (4a) Similar to the
previous ultramafic volcanics section. Metre wide
intervals of fuchsite rich quartz-carbonate and It pyrite
are scattered through this section and make up 3% of the
section volume. Magnetic susceptibility readings as
follows: 5:0.47. at 142m, 5:0.51 at 145m, 5:0.63 at 148m,
5:0.65 at 151m, 5:0.59 at 154m, 5:0.60 at 160m, 5:0.49 at
163m, -5:0.53 at 166m.
169.0 208.0 FUCHSITIC ULTRAMAFIC VOLCANICS (4d) Similar
96547
96548
96549
96550
96551
96552
96585
96553
96554
96555
137.10
138 .10
139.10
140. 10
141. 10
141.40
148. 00
156. 00
166. 00
167.10
ASSAYS
TO WIDTH Au (ppb)
138 .10
139. 10
140. 10
141 .10
141 .40
142 .40
149 .00
157 . 00
167 .10
168 . 10
1.00
1. 00
1.00
1 . 00
0. 30
1.00
1.00
1.00
1.10
1 . 00
17
38
17
12
48
24
7
15
14
24
96556 168.10 169.10 . 00 57
HOLE No: ENG9605

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9605 Page 6
FROM TO LITHOLOGICAL DESCRIPTION
to previous section except that fuchsite alteration and
minor albite/silica alteration are present within
quartz -carbonate veins and as thin haloes. This section
displays an increase in the degree of alteration. Well
mineralized section from 169 to 181m depth with up to 2%
disseminated and clotty pyrite. Fuchsite and albite
alteration become less prominent by 196m depth. Magnetic
susceptibility readings are as follows: 5:0.61 at 169m,
5:0.92 at 172m, 5:1.0 at 175m, 5:0.51 at 178m, 5:0.51 at
181m, 5:0.51 at 184m, 5:0.45 at 187m, 5:0.61 at 190m,
5:0.51 at 193m, 5:0.59 at 196m, 5:0.53 at 199m, 5:0.45 at
202m, 5:0.49 at 205m.
SAMPLE No.
96557
96558
96559
96560
96561
96562
96563
96564
96565
96566
96567
96568
96569
96570
96571
96572
96573
96574
96575
96576
96577
96578
96579
96580
96581
96582
96583
96584
FROM
170.10
171. 00
172 . 00
173 . 00
174 . 00
175. 00
176 . 00
177. 00
178. 00
179. 00
180 . 00
181. 00
182 . 00
183 . 00
184 . .00
185. .00
186 . .00
187. 00
188 . .00
189. .00
190. .00
191. .00
202 . .00
203 . . 00
204 . .00
205 . . 00
206 . .00
207 . . 00
ASSAYS
TO
171.00
172 . 00
173 . 00
174 . 00
175 . 00
176 . 00
177 . 00
178 . 00
179. 00
180. 00
181. 00
182. 00
183 . 00
184 . 00
185 . 00
186. 00
187 . 00
188. 00
189. 00
190. 00
191. 00
192 . 00
203 . 00
204 . 00
205 . 00
206 . 00
207. .00
208 . 00
WIDTH Au
0.90
1. 00
1 . 00
1. 00
1. 00
1. oo
1 . 00
1 . 00
1 . 00
1 . 00
x . 00
1. 00
1 . 00
1 . 00
1 . 00
1 . 00
1 . .00
1 , 00
1. 00
1. .00
1. .00
1 . .00
1 . .00
1 . . 00
1 , .00
1. .00
1 , .00
1. .00
(ppb)
22
27
75
134
93
149
96
22
10
3
69
10
10
14
7
130
9
21
12
3
2
46
NIL
5
9
2
5
7
HOLE No: ENG9605

PROPERTY: English
HOLE No.: ENG9605
FROM TO LITHOLOGICAL DESCRIPTION
Cameco Corporation
208.0 218.0 ULTRAMAFIC VOLCANICS ( 4s.) S imilar to the
previous ultramafic section but fuchsite is very limited
less than H abundance and restricted to some of the
quartz-carbonate veins. Mineralization is sporadic and
associated with zones of higher alteration. Pyrite
mineralization is less than l* and consists of coarse
pyrite and fine disseminations. Magnetic susceptibility
readings are as follows: 5:0.57 at 208m, 5:0.53 at 211m,
5:0.61 at 214m, 5:0.49 at 217m.
DIAMOND DRILL LOG
218.0 232.0 FUCHSITIC ULTRAMAFIC VOLCANICS (4d) Similar
to the previous fuchsitic section except the host rock
also contains up to 45% fuchsite but averages about S-10%
alteration. Sulphide mineralization consists of coarse
to finely disseminated pyrite. Magnetic susceptibility
readings of: 5:0.57 at 223m, 5:0.61 at 226m, 5:0.47 at
229m, 5:0.51 at 232m.
232.0 261.6 ULTRAMAFIC VOLCANICS (4a-d) Similar to
previous ultramafic sections with variable fuchsite
alteration up to 15% but averaging approximately 2 ^.
Massive -fine to coarse grained and generally pale green
in colour. Alteration is dominated by the
quart z- carbonate veins up to 25% volume with serpentine
SAMPLE No.
96586
96587
96588
96589
96590
96591
96592
96593
96594
96595
96596
96597
96598
96599
96600
96601
96602
96603
96604
96605
96606
96607
96608
FROM
210. 00
211. 00
212. 00
213 . 00
214. 00
215. 00
219. 00
220. 00
221 . 00
222 . 00
223 . 00
224 . 00
225. 00
226. 00
227. 00
228 . 00
229. 00
235. 00
236 . 00
237. 00
240. 00
241. 00
242 . 00
ASSAYS
TO WIDTH Au
211. .00
212 . .00
213. .00
214. .00
215. .00
216. .00
220. .00
221. .00
222 . .00
223. .00
224. .00
225 .00
226 .00
227 . 00
228 .00
229 .00
230 . 00
236 .00
237 . 00
238 . 00
241 .00
242 .00
243 . 00
1 .
1.
1 .
1 .
1 ,
1.
1 .
1 .
1.
1 .
1 .
1
1
1
1 1
1
1
1
1
1
1
1
00
00
oo
00
00
.00
.00
00
.00
00
00
00
.00
. 00
.00
.00
.00
.00
.00
. 00
.00
.00
.00
(ppb)
5
5
3
3
5
2
NIL
NIL
12
3
NIL
2
22
9
3
3
NIL
48
2
2
NIL
5
31
Page 7
HOLE No: ENG9605

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9605 Page 8
FROM TO LITHOLOGICAL DESCRIPTION
and fuchsite also present. Sulphide mineralization is
variable and consists of trace to 3% disseminated and
clotty pyrite along fractures and within the host rock.
Magnetic susceptibility readings are as follows: 5:0.65
at 235m, 5:0.59 at 238m, 5:0.59 at 241m, 5:0.61 at 244m,
5:0.61 at 247m, 5:0.57 at 250m, 5:0.34 at 253m, 5:0. 5 6 a t
256m.
261.6 265.0 ALBITITE DIKE (lOcq) Similar to previous
albitite dikes, with a contact aureole approximately 5cm
at upper contact and up to 30cm wide at the lower
contact. Upper contact at 21 degrees c. a., lower contact
is indistinct. Magnetic susceptibility readings average
5:0.27. Sulphide content is pervasive and up to 24
disseminated pyrite. Contact aureoles contain up to Sicoarse
pyrite.
265.0 266.6 FUCHSITIC ULTRAMAFIC VOLCANICS (4d) Similar
to previous fuchsitic zones associated with the margins
of the albitite dikes. Sulphide mineralization consists
of up to J.% pyrite set in a fuchsite rich matrix.
Magnetic susceptibility reading of 5:0.53.
266.6 267.7 ALBITITE DIKE (lOcq) Similar to previous
albitite dike. Upper contact at 44 degrees c. a. and
lower contact at 55 degrees c.a. Sulphide content at
SAMPLE No.
96609
96610
96611
96612
96613
96614
96615
96616
96617
96618
96619
96620
96621
96622
96623
96624
96625
FROM
243 . 00
244 . 00
245. 00
246. 00
247. 00
248 . 00
249. .00
250. 00
251. .00
261. 30
262 .30
263 . .30
264 .00
265 .00
265 .40
266 .40
266 . 70
ASSAYS
TO WIDTH Au
244 . 00
245. 00
246 . 00
247. 00
248. 00
249, .00
250. .00
251 00
252 .00
262 .30
263 .30
264 .00
265 . 00
265 .40
266 .40
266 . 70
267 .30
1 . 00
1. 00
1 . 00
1. 00
1 . 00
1. .00
1. .00
1 .00
1 .00
1 .00
1 .00
0 .70
1 .00
0 .40
.00
1
0 .30
0 .60
(ppb)
3
5
14
12
10
31
9
5
14
5
7
24
34
70
2
NIL
9
HOLE No: ENG9605

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9605 Page 9
FROM TO LITHOLOGICAL DESCRIPTION
volume of mm wide disseminated euhedral pyrite. Magnetic
susceptibility reading of 5:0.24.
267.7 292. 8 SERPENTINIZED ULTRAMAFIC VOLCANICS (4e)
Typical massive to weakly spinifex textured ultramafics
that show a gradual shift towards a serpentine rich
package over the initial 5m. The section becomes black
in colour and contains up to H.0% quartz-carbonate veins.
A few albitite at 283m, and a mafic dike crosscut the
section with contacts at 42 degrees. Magnetic
susceptibility reading as follows: 5.: 0.47 at 271m, 5:0.57
at 274m, 5:0.36 at 277m, 5:0.59 'at 280m, 5:13.1 at 283m,
5:0.55 at 286m, 5:0.47 at 28Sm, 5:0.45 at 292m.
292. S 299.5 SYENITE DIKE (9e) Medium to coarse grained
dark red to grey syenite/diorite dike. The dike contains
inclusions of chloritic and serpentinized ultramafics. No
visible sulphides present. Magnetic susceptibility
readings range from 5:22.0 to 5:0.88.
299.5 304.0 ALBITITE DIKE (lOcq) Fine grained albitite
dike similar to previous samples with n.% disseminated
pyrite intruding thin intervals of serpentinized
ultramafic volcanics. Magnetic susceptibility readings
averaging approximately 5:0.35.
SAMPLE No.
96626
96627
96628
96629
96630
96631
96632
96633
96634
96635
96S36
9S637
96638
96639
96640
96641
96642
96643
96644
96645
96646
96647
FROM
267. 30
271. .10
271. 60
280. 50
281. 50
282. 50
286. .00
288 . .80
289. .80
290. .80
291. .90
292 . .90
293. .70
294 . .60
295. .60
296 . .60
297 . .50
298 . .50
299 .50
300 .70
301 .70
302 .70
ASSAYS
TO
268. 30
271. 60
272. 60
281. 50
282. 50
283. 50
287. .00
289. .80
290. . 80
291. . 90
292. . 90
293. . 70
294. .60
295. .60
296. .60
297. .50
298. . 50
299. . 50
300 .70
301 . 70
302 .70
304 .00
WIDTH Au
1. 00
0. 50
1. 00
1. 00
1. 00
1. 00
1. 00
1. 00
1. 00
1 . 10
1 . 00
0. 80
0. 90
1 . 00
1 . .00
0. .90
1 . .00
.00
1.
1. .20
1. .00
1. .00
1. .30
(ppb)
NIL
17
5
NIL
17
2
3
2
2
3
5
3
31
22
12
39
5
3
53
7
12
9
HOLE No: ENG9605

PROPERTY: English
HOLE No.: ENG9605
Cameco Corporation
DIAMOND DRILL LOG
FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM
304 . O END OF HOLE
DOWN-HOLE SURVEY DATA
DEPTH INCLINATION BEARING
1.00 -45.00 1 10.00
100.00 -46.00 1 10.00
200.00 -46.00
304 .00 -47 . 00
110.00
110.00
ASSAYS
TO WIDTH Au (ppb)
Page 10
HOLE No: ENG960S

PROPERTY: English
HOLE No.: ENG9606
Collar Eastings: 483056.00
Collar Northings: 5319160.00
Collar Elevation: O .00
Contractor was NDS Drilling of Timmins, Out.
FROM TO
0.0 22 .0
CASING ON BEDROCK (Ob)
TISDALE GROOP
LITHOLOGICAL DESCRIPTION
Cameco Corporation
DIAMOND DRILL LOG
22.0 34.0 MASSIVE MAFIC VOLCANICS (lam) Medium-dark green fine
grained and calcite rich mafic volcanics. This section is
crosscut by a number of mm wide quartz and epidote rich
veins. The veins possess alteration haloes up to 2cm
from the vein and consist of epidote and hematite and
quartz. The quartz veins are almost perpendicular to the
core axis and form a fine network up to 2% volume of the
section. Core appears undeformed but displacement and
folding of veins indicates that this section was
recrystallized. Magnetic susceptibility readings are as
follows: 5:1.06 at 24m, 5:0.73 at 27m, 5:0.77 at 30m. No
sulphides were observed. Core is competent and
moderately hard with chlorite the main alteration
mineral.
34.0 END OF HOLE
Collar Inclination: -50.00
Grid Bearing: 110.00
Final Depth: 34.00 metres
Hole was collared in claimtt 1147272
SAMPLE No. FROM
96648
96649
26.00
27. 00
Logged by: P. Chubb
Date: 03/11/96-03/11/96
Down-hole Survey: Acid
ASSAYS
TO WIDTH Au (ppb)
27.00
28 . 00
1. 00
1. 00
HOLE No: ENG9606

DOWN-HOLE SURVEY DATA
DEPTH INCLINATION BEARING
1.00 -50.00 HO . 00
34.00 -50.00 110.00

PROPERTY: English
HOLE No.: ENG9607
Collar Eastings: 483197.00
Collar Northings: 5319155.00
Collar Elevation: 0.00
Contractor was NDS Drilling of Timmins, Ont.
FROM TO LITHOLOGICAL DESCRIPTION
0.0 5.5 CASING ON BEDROCK (Ob)
TISDALE GROUP
Cameco Corporation
DIAMOND DRILL LOG
5.5 79.0 MASSIVE MAFIC VOLCANICS/GABBRO (lam/Sa) Medium to dark
green fine to medium grained massive and calcite rich
mafic volcanics. This section is crosscut by a number of
mm and cm wide quartz and epidote rich veins. The quartz
veins are almost perpendicular to the core axis and form
a fine network up to 2 \ volume of the section. Section
is intruded by a number of thin metre wide and less
syenite and mafic. Quartz-calcite-hematite veins are up
to 3% total volume of section. Core appears undeformed
but displacement and folding of veins indicates that this
section was recrystallized and folded. Magnetic
susceptibility readings are as follows: 5:58.2 at 6m,
5:0.63 at 7m, 5:1.16 at 10m, 5:1.13 at 13m, 5:0.79 at
16m, 5:0.63 at 19m, 5:0.75 at 25m, 5:0.71 at 28m, 5:0.61
at 31m, 5:0.59 at 34m, 5:0.67 at 37m, 5:0.67 at 40m,
5:0.75 at 43m, 5:0.63 at 46m, 5:0.49 at 49m, 5:0.61 at
52m, 5:0.53 at 55m, 5:0.38 at 58m, 5:0.58 at 61m, 5:0.65
at 64m., 5:0.77 at 67m, 5:0.73 at 70m, 5:0.77 at 73m,
5:0.73 at 76m, 5:0.76 at 78m. Trace amounts of fine to
mm sized euhedral disseminated pyrite are observed over
Collar Inclination: -50.00
Grid Bearing: 290.00
Final Depth: 175.00 metres
Hole was collared in claimft 1147272
SAMPLE No. FROM
96650
96651
96652
96653
96654
96655
96656
96657
96658
96659
96660
96661
96662
96663
96664
96665
96666
96667
96668
96669
6 . 00
8 . 00
9 . 00
10. 00
19. 00
20. 00
20. 80
21. 20
25. 00
27. 00
28. .00
36. 60
37. 60
41, . 00
42. .00
46. .00
49 . 00
50, .00
51, . 00
52 .00
Logged by: P. Chubb
Date: 04/11/96-05/11/96
Down-hole Survey: Acid
ASSAYS
TO WIDTH AU (ppb)
7 . 00
9. 00
10 . 00
11 . 00
20. 00
20 . 80
21 . .20
22 . 10
26 . 00
28 . 00
29. .00
37. .60
38 . 60
42 , . 00
43 . . 00
47 . . 00
50 . 00
51 . 00
52 .00
53 .00
1 ,
1 .
1 .
1 ,
1 ,
.00
00
.00
. 00
. 00
0. . 80
0, .40
0, .90
1 , . 00
l. .00
1 .00
11 .00
.00
1 .00
1 .00
1 . 00
1 .00
1 . 00
11 .00
. 00
NIL
NIL
2
NIL
NIL
5
5
12
7
9
5
9
NIL
5
NIL
12
3
NIL
5
7
HOLE No: ENG9607

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9607 Page 2
FROM TO LITHOLOGICAL DESCRIPTION
metre intervals, with clots of pyrite up to 5% in the
larger quartz-carbonate-hematite veins. Core is
competent and moderately hard with chlorite, calcite and
amphibole the main alteration minerals with epidote and
hematite minor phases .
79.0 108.9 MAFIC/ALTERED ULTRAMAFIC VOLCANICS? (la j 7/43 j)
Highly foliated very fine to medium grained dark green
mafic volcanics. Alteration is dominated by chlorite and
calcite, with quartz-calcite veins ranging up to 15%
abundance over short intervals. Sulphides are variable
in content with short intervals up to H over 10cm
consisting of coarse euhedral pyrite. Magnetic
susceptibility readings as follows: 5:0.77 at 80m, 5:0.69
at 82m, 5:0.79 at 85m, 5:0.67 at 88m, 5:0.67 at 91m,
5:1.23 at 94m, 5:0.90 at 97m, 5:0.75 at 100m, 5:1.16 at
103m, 5:0.69 at 106m.
108.9 135.2 MASSIVE .S SPINIFEX ULTRAMAFIC VOLC . (4eca)
Pale green highly foliated and quartz-carbonate rich
ultramafic volcanics. Quartz-carbonate veining up -to 20t
SAMPLE No.
96670
96671
96672
96673
96674
96675
96676
96677
96678
96679
96680
96681
96682
96683
96684
96685
96686
96687
96688
96689
96690
96691
96692
96693
96694
96695
FROM
53. 00
53. 40
57. .00
61. . oo
62. .00
67. 00
69. 00
70. 00
72. 00
73. .00
79. 00
80. 00
85. 00
91. 00
101. 00
102 . 00
103. 00
104. 00
105. 00
106. .00
107. 00
108. 00
108. 50
108. 80
112. . 80
113 . . 80
ASSAYS
TO WIDTH Au
53 .40
54 .40
58 . 00
62. . 00
63 . . 00
68. .00
70. .00
71. .00
73 . 00
74 . .00
80 . . 00
81 .00
86 .00
92 . 00
102. .00
103 . .00
104 .00
105 .00
106 .00
107. . 00
108. .00
108. .50
108 . 80
109 .80
113 .80
114 .60
0 .40
1 .00
1 . 00
1. . 00
1 . . 00
1 , .00
1. . 00
1. .00
1. . 00
1 . .00
1 . . 00
1 . . 00
1. . 00
1
. 00
1. .00
1. . 00
1. .00
1 .00
1, .00
1. .00
1. .00
0. .50
0. . 30
1 .00
1 . .00
0. . 80
(ppb) ;
10
3
NIL,
12
51
NIL
10
29
5
7
NIL
2
NIL
12
NIL
2
3
7
3
NIL
5
41
9
7
5
NIL
HOLE No: ENG9607

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9607 Page 3
FROM TO LITHOLOGICAL DESCRIPTION
volume. Minor fuchsite alteration associated with the
quartz-carbonate veins near the syenite dikes. Sulphide
mineralization is limited and consists of coarse euhedral
pyrite. Minor fault over 10cm at 112m. This section
becomes strongly serpentinized within a metre of the
contact . The contact area is intruded by metre wide grey
and red syenites that contain exotic fragments. Minor
fault zone at 132m depth. The red syenite is well
mineralized and contains up to a.% mm sized euhedral
pyrite. Magnetic susceptibility readings as follows:
5:1.04 at 118m, 5:28.9 at 124m, 5:86.5 at 127m, 5:116 at
130m, 5:7.50 at 133m.
135.2 142.0 SYENITE DIKE (9e) Typical dark red fine to
medium grained syenite with Ifc disseminated euhedral
pyrite. The red syenite intruded an earlier grey
syenite. Upper contact at 57 degrees c. a. and lower
contact at 40 degrees c. a. Contacts with the syenite
dike are marked by intensification of fuchsite alteration
up to St volume. Magnetic susceptibility readings as
follows: 5:0.65 at 136m, 5:8.53 at 139m.
142.0 165.0 SERPENTINIZED SPINIFEX ULTRAMAFIC VOLC . (4ec)
Dark grey to black tine grained massive and spinifex
textured ultramafic volcanic. Section is intruded by a
series of thin 10cm wide syenite dikes that make up less
than 1 1s o f the volume for this section. The section is
highly foliated and contains up to 35^ quartz -carbonate
SAMPLE No.
96696
96697
96698
96699
96700
96701
96702
96703
96704
96705
96706
96707
96708
96709
. 96710
96711
96712
96713
96714
96715
96716
96717
FROM
114 . 60
115. .00
116, .00
117. .00
119. .00
127. .00
128 . . 00
129. 00
134 . 20
135. 20
136. 10
137. 10
138. 10
139. 10
139. 40
140. 40
141. 40
142. 20
143. .40
144. .30
145 .40
148. . 80
ASSAYS
TO WIDTH Au
115. .00
116. . 00
117 . . 00
118. .00
120. . 00
128. . 00
129. . 00
130. .00
135. . 20
136. .10
137. 10
138. 10
139. 10
139. .40
140. .40
141. .40
142. 20
143. .40
144. .30
145. .10
146. .40
149. .80
0. .40
1 . 00
1. .00
1. .00
1 . .00
1. .00
1 . 00
1. .00
1. .00
0. 90
1 , 00
1. 00
1 . 00
0. 30
1. 00
1. 00
0. 80
- 1. 20
0. 90
- 0. .80
1 .00
1 .00
(ppb)
3
NIL
3
2
2
15
NIL
NIL
NIL
3
NIL
3
NIL
NIL
NIL
3
NIL
NIL
2
NIL
NIL
57
HOLE No: ENG9607

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9607 Page 4
FROM
165 . 0
TO LITHOLOGICAL DESCRIPTION
veining. Minor breccia zones within this section span
10-20cm and make up 5% of the volume . Spinifex textures
present in small zones . Sulphides consist of finely
disseminated pyrite along foliation planes in proximity
to the syenite dike contact. Magnetic susceptibility
readings as follows: 5:0.65 at 142m, 5:0.67 at 145m,
5:0.36 at 148m, 5:3.79 at 151m, 5:61.1 at 157m, 5:0.67 at
160m, 5:0.63 at 163m.
168.0 FUCHSITE ULTRAMAFIC VOLCANICS (4dc) Similar
to previous ultramafic volcanic section except for the
gradual increase in fuchsite alteration initially
developed within veins but located more within the host
rock with depth. Magnetic susceptibility readings as
follows: 5:0.65 at 166m.
168.0 168.6 ALBITITE DIKE (lOcq) Similar to previously
described albitite dikes. Sulphide content is at l*
finely disseminated pyrite. Upper contact at 80 degrees
c.a. and lower contact at 80 degrees c.a. Magnetic
susceptibility reading of 5:0.22.
168.6 171.6 SILICIFIED ULTRAMAFIC VOLCANICS (4a) Similar
to previous sections except pale grey in colour due to
silicification and carbonate alteration. Magnetic
susceptibility readings of 5:0.49 at 169m. Sulphides
consist of trace amounts of finely disseminated euhedral
pyrite.
SAMPLE No .
96718
96719
96720
96721
96722
FROM
152. 80
157. 00
163. 00
166.00
167.00
ASSAYS
TO
153.80
158 . 00
164 .00
167.00
168.00
WIDTH Au
1.00
1.00
1. 00
1.00
1.00
96723 168.00 168.60 0.60
96724
96725
168.60
170.60
169.60
171.60
1. 00
1. 00
(ppb)
NIL
NIL
7
5
34
10
HOLE No: ENG9607

Cameco Corporation
DIAMOND DRILL LOG
PROPERTY: English
HOLE No.: ENG9607 Page 5
FROM TO LITHOLOGICAL DESCRIPTION
1.71.6 172.8 SYENITE DIKE (9e) Similar to previously
described syenite dikes. The quartz veins contain up to
5* clotty pyrite with finely disseminated pyrite
disseminated throughout this section. Upper contact at
50 degrees c.a. and lower contact at 85 degrees c. a.
Magnetic susceptibility reading o f 5 :0.98 at 172m.
175.0 SILICIFIED ULTRAMAFIC VOLCANICS (4ad)
Similar to previously described ultramafic section except
that minor fuchsite along some of the quartz-carbonate
veins. Sulphides are limited'to trace amounts of finely
disseminated euhedral pyrite. Magnetic susceptibility
reading of 5:0.65.
175.O END OF HOLE
DOWN-HOLE SURVEY DATA
DEPTH INCLINATION BEARING
1.00 -50.00 290.00
100.00 -50.00 290.00
i75.oo -50.00 290.00
ASSAYS
SAMPLE No. FROM TO WIDTH Au (ppb)
96726 171.60 172.80 1.20 353
96727
96728
172.80
174.00
174.00
175.00
1.20
1.00
3
NIL
HOLE No: ENG9607

APPENDIX B
Assay and ICP multielement Analyses
for
English Property 1996 Drill Program

Swastika Laboratories
A Division o f TSL/Assayers Inc.
Established 1928 Assaying - Consulting - Representation
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: ENG 96-D
Attn: P. Chubb
We hereby certify the following Geochemical Analysis of 75 Core samples
submitted OCT-29-96 by .
Sample
Number
ENG96D-001
ENG96D-002
ENG96D-003
ENG96D-004
EN396D-005
ENG96D-006
EN396D-007
ENG96D-008
ENG96D-009
ENG96D-010
ENG96D-011
ENG96D-012
EN396D-013
ENG96D-014
ENS96D-015
ENG96D-016
ENG96D-017
ENG96D-018
EN396D-019
ENG96D-020
ENG96D-021
ENG96D-022
EN396D-023
ENG96D-024
EN396D-025
ENG96D-026
ENG96D-027
ENG96D-028
E^G96D-029
EM396D-030
One assay ton portion used.
Au Au Check
PPB PPB
39
Nil
2
3
3
7 26
Nil
15
14
2
Nil
24
3
9
22
5
2
5
14
3
Nil
48
7
139 137
22
Nil 7
5
Nil
12
3
Certified by_
Au 2nd Mil t i
PPB Element
Results
to
f o 1 1 ow
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705) 642-3244 FAX (705) 642-3300
-
-
-
-
-
Page l of 3
6W-4572-RG1
Date: NOV-06-96

Swastika Laboratories
A Division o f TSL/Assayers Inc.
E stabHshedi928 Assaying - Consulting - Representation
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: ENG 96-D
Attn: P. Chubb
We hereby certify the following Geochemical Analysis of 75 Core samples
submitted OCT-29-96 by .
Sampl e
Number
ENG96D-031
ENG96D-032
ENG96D-033
ENG96D-034
BNG96D-035
EN396D-036
ENG96D-037
ENG96D-038
EN396D-039
EN396D-040
ENG96D-041
ENG96D-042
EN396D-043
ENG96D-044
ENG96D-045
ENG96D-046
ENG96D-047
EN396D-048
ENG96D-049
ENG96D-050
ENG96D-051
EN396D-052
EN396D-053
ENG96D-054
EN396D-055
EN396D-056
ENG96D-057
ENG96D-058
BNG96D-059
EN396D-060
One assay ton portion used.
Au Au Check Au 2nd Mil t i
PPB PPB PPB Element
9
3
Nil
2
29 21
Nil
Nil ' ~
2 3
7
12 - -
Nil
Nil
Nil
Nil
Nil
Ni 1
2
Nil
5
9
34
3 -' ~
41
163
197
646 621
1920 1637 1989
583 583
79
110
Certified by
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705) 642-3244 FAX (705) 642-3300
/]
Page 2 of 3
6W-4572-RG1
Date: NOV-06-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: ENG 96-D
Attn: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers I nc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 75 Core samples
submitted OCT-29-96 by .
Sample
Number
EN396D-061
ENG96D-062
ENG96D-063
EN396D-064
EN396D-065
EN396D-066
ENG96D-067
ENG96D-068
ENG96D-069
ENG96D-070
ENG96D-071
ENG96D-072
EN396D-073
ENC96D-074
EN396D-075
One assay ton portion used.
Au
PPB
17
15
Nil
Nil
Nil
14
2
Nil
3
10
Nil
Nil
Nil
3
2
Au Check Au 2nd Mil t i
PPB PPB Element
12
-
Nil
Certified by_
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705) 642-3244 FAX (705) 642-3300
Page 3 of 3
6W-4572-RG1
Date: NOV-06-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: ENG 96-D
Attn: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers I nc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 58 Core samples
submitted OCT-29-96 by .
Sampl e
Number
ENG96D-076
EN396D-077
EN396D-078
ENG96D-079
ENG96D-080
EN396D-081
EN396D-082
ENG96D-083
ENG96D-084
EN396D-085
ESG96D-086
ENG96D-087
ESG96D-088
EN396D-089
ENG96D-090
HNG96D-091
ENG96D-092
ENG96D-093
EN396D-094
EN396D-095
EN396D-096
EN396D-097
EN396D-098
ENG96D-099
EN396D-100
ENG96D-101
BG96D-102
EN396D-103
EN396D-104
ENG96D-105
One assay ton portion used.
Au Au Check
PPB PPB
24
72 69
Nil
Nil
34
53
98
63
9
Nil
38
Nil
14
Nil
81
33 10
Nil
Nil
5
26
Nil
77
74 77
Nil
Nil
7
Nil
26
147
Nil
Certified by
Mil t i
Element
Resul ts
to
f o 1 1 ow
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705) 642-3244 FAX (705) 642-3300
Page l of 2
6W-4573-RG1
Date: NOV-05-96

Swastika Laboratories
A Division of TSL/Assayers Inc.
Estab.ished 1928 Assaying - Consulting - Representation
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: ENG 96-D -
Attn: P. Chubb
We hereby certify the following Geochemical Analysis of 58 Core samples
submitted OCT-29-96 by .
Sampl e
Number
EN396D-106
EN396D-107
EN396D-108
EN396D-109
ENG96D-110
EN396D- 1 1 1
EN396D-112
EN396D-113
ENG96D-114
ENG96D-115
ENG96D-116
ENG96D-117
EN396D-118
ENG96D-119
ENG96D-120
ENG96D-121
ENG96D-122
EN396D-123
ENG96D-124
ENG96D-125
ENG96D-126
EN396D-127
EN396D-128
ENG96D-129
ENG96D-130
ENG96D-131
ENG96D-132
EN396D-133
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
2
2
3
9
123 93
2
Nil
2
Nil
3
Nil
3
2
21
Nil
Nil
7
101
19
Nil
Nil
Nil Nil
Nil
Nil
7
3
Nil
43
Certified by-
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705) 642-3244 FAX (705) 642-3300
Page 2 of 2
6W-4573-RG1
Date: NOV-05-96
l

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Attn: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 88 Core samples
submitted OCT-31-96 by .
Sample
Number
ENG96D-134
EN396D-135
ENG96D-136
ENG96D-137
ENG96D-138
ENG96D-139
ENG96D-140
ENG96D-141
ENG96D-142
EN396D-143
EN596D-144
EN396D-145
ENG96D-146
ENG96D-147
E1SG96D-148
EN396D-149
ENG96D-150
ENG96D-151
EN396D-152
EN396D-153
ENG96D-154
EN396D-155
EN396D-156
EN396D-157
EN396D-158
EN396D-159
ETNG96D-160
EN396D-161
EN396D-162
E^G96D-163
One assay ton portion used.
Au Au Check
PPB PPB
3
51
209
41
93 87
10
21 7
26
84
21
120 110
7
2
9
5
3
2 3
9
108
173 159
9
10 5
Nil
217
10 9
Certified by
Mil t i
El ement
Resul ts
to
f o 1 1 ow
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705) 642-3244 FAX (705) 642-3300
Page l of 3
6W-4574-RG1
Date: NOV-14-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Attn: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 88 Core samples
submitted OCT-31-96 by .
Sample
Number
EN396D-164
EN396D-165
ENG96D-166
EN396D-167
ENG96D-168
EN396D-169
EN396D-170
ENG96D-171
ENG96D-172
EN396D-173
ENG96D-174
ENG96D-175
EN396D-176
ENG96D-177
EN396D-178
EN396D-179
EN396D-180
ENG96D-181
ENG96D-182
ENG96D-183
ENG96D-184
ENG96D-185
ENG96D-186
EIsG96D-187
EN396D-188
EN396D-189
EN396D-190
EN396D-191
E^G96D-192
ENG96D-193
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
9
7
17
10 10
9
14
2
3
2
2
Nil
5
Nil
Nil
5
Nil
3
Nil
2
2
Nil
3
12
189 166
75
Nil 2
70
240
5 2
Certified by
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone ( 705)642-3244 FAX (705)642-3300
Page 2 of 3
6W-4574-RG1
Date: NOV-14-96
^~ ^

Swastika Laboratories
A Division of TSL/Assayers Inc.
Established 1928 Assaying - Consulting - Representation
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Ann: P. Chubb
We hereby certify the following Geochemical Analysis of 88 Core samples
submitted OCT-31-96 by .
Sampl e
Number
EN396D-194
ENG96D-195
ENG96D-196
EN396D-197
EN396D-198
ENG96D-199
ENG96D-200
ENG96D-201
EN396D-202
ENG96D-203
ENG96D-204
EN396D-205
ENG96D-206
EN396D-207
ENG96D-208
ENG96D-209
EN396D-210
EN396D-2H
EN396D-212
EN396D-213
ENG96D-214
E^G96D-215
E^G96D-216
E^G96D-217
EN396D-218
E^G96D-219
E^G96D-220
EN396D-221
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
31
36
41
87
86
36
38 36
24
55
62
43
279
50
134
58
38
111
65
53
190 182
58
51
2
31
36
45
51
24
Certified by_
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705) 642-3244 FAX (705) 642-3300
Page 3 of 3
6W-4574-RG1
Date: NOV-14-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Attn: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers I nc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 47 Core samples
submitted OCT-31-96 by .
Sample
Number
EN396D-222
EN396D-223
ENG96D-224
ENG96D-225
ENG96D-226
ENG96D-227
ENG96D-228
ENG96D-229
ENG96D-230
EN396D-231
ENG96D-232
ENG96D-233
EN396D-234
ENG96D-235
ENG96D-236
ENG96D-237
ENG96D-238
EN396D-239
ENG96D-240
ENG96D-241
EN396D-242
EN396D-243
ENG96D-244
EN396D-245
EN396D-246
ENG96D-247
ENG96D-248
ENG96D-249
E^G96D-250
ENG96D-251
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
43 - Results
48 - to
45 - f o 1 1 ow
98
43
120
60
51
79
31
98
50
27 24
24
38
29
39
36
113 115
120
99
36
34
27
69 65
89
38
43
14
24
Certified by
P.O. Box 10, Swastika, Ontario POK1TO
Telephone (705)642-3244 FAX (705)642-3300
Page l of 2
6W-4575-RG1
Date: NOV-14-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Aim: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 47 Core samples
submitted OCT-31 -96 by .
Sample Au Au Check Mil t i
Number PPB PPB Element
ENG96D-252 2
EN396D-253 3
EN396D-254 2
EN396D-255 51
EN396D-256 375
EN396D-257 62 "" -
EN396D-258 19
ENG96D-259 10
ENG96D-260 106
ENG96D-261 46
EN396D-262'''''''''''' - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - ~
EN396D-263 39
ENG96D-264 14
ENG96D-265 744 737
E^G96D-266 437
EN396D-267 283 285
EN396D-268 43
One assay ton portion used.
Certified by
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone ( 705) 642-3244 FAX ( 705)642-3300
Page 2 of 2
6W-4575-RG1
Date: NOV-14-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Attn: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 81 Rock samples
submitted NOV-04-96 by .
Sampl e
Number
Eng96D-269
Eng96D-270
Eng96D-271
Eng96D-272
Eng96D-273
Eng96D-274
Eng96D-275
Eng96D-276
Eng96D-277
Eng96D-278
Eng96D-279
Eng96D-280
Eng96D-281
Eng96D-282
Eng96D-283
Eng96D-284
Eng96D-285
Eng96D-286
Eng96D-287
Eng96D-288
Eng96D-289
Eng96D-290
Eng96D-291
Eng96D-292
Eng96D-293
Eng96D-294
Eng96D-295
Eng96D-296
Eng96D-297
Eng96D-298
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
151
98
387
816 842
267
375
1269
63
2
5
2
19
34 15
3
22
10
Nil
5
10
2
58
163
65
17
Nil
38
53
72 151
77
46
Certified by
P.O. Box 10, Swastika, Ontario POK1TO
Telephone (705)642-3244 FAX (705)642-3300
Page l of 3
6W-4691-RG1
Date: NOV-15-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Atm: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 81 Rock samples
submitted NOV-04-96 by .
Sampl e
Number
Eng96D-299
Eng96D-300
Eng96D-301
Eng96D-302
Eng96D-303
Eng96D-304
Eng96D-305
Eng96D-306
Eng96D-307
Eng96D-308
Eng96D-309
Eng96D-310
Eng96D-311
Eng96D-312
Eng96D-313
Eng96D-314
Eng96D-315
Eng96D-316
Eng96D-317
Eng96D-318
Eng96D-319
Eng96D-320
Eng96D-321
Eng96D-322
Eng96D-323
Eng96D-324
Eng96D-325
Eng96D-326
Eng96D-327
Eng96D-328
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
235
3
22
113
439
221
245 189
21
65
74
170
115
213
Nil
Nil
3
3
175 177
393
57
120
298
245 228
101
12
Nil
Nil
Nil
2
3 3
Certified by_
P.O. Box 10, Swastika, Ontario POK1TO
Telephone (705) 642-3244 FAX (705) 642-3300
Page 2 of 3
6W-4691-RG1
Date: NOV-15-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Attn: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 81 Rock samples
submitted NOV-04-96 by .
Sample Au Au Check Mil t i
Number PPB PPB Element
Eng96D-329 2
Eng96D-330 Nil Nil
Eng96D-331 Nil
Eng96D-332 Nil
Eng96D-333 3
Eng96D-334 Nil
Eng96D-335 Nil Nil
Eng96D-336 Nil
Eng96D-337 Nil
Eng96D-338 Nil
Eng96D-339 Nil
Eng96D-340 Nil
Eng96D-341 Nil
Eng96D-342 2
Eng96D-343 Nil Nil
Eng96D-344 Nil
Eng96D-345 Nil
Eng96D-346 Nil
Eng96D-347 Nil
Eng96D-348 2
Ena96D-349 Nil
One assay ton portion used.
Certified by
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705)642-3244 FAX (705)642-3300
Page 3 of 3
6W-4691-RG1
Date: NOV-15-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Attn: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 82 core samples
submitted NOV-04-96 by .
Sampl e
Number
Eng96D-350
Eng96D-351
Eng96D-352
Eng96D-353
Eng96D-354
Eng96D-355
Eng96D-356
Eng96D-357
Eng96D-358
Eng96D-359
Eng96D-360
Eng96D-361
Eng96D-362
Eng96D-363
Eng96D-364
Eng96D-365
Eng96D-366
Eng96D-367
Eng96D-368
Eng96D-369
Eng96D-370
Eng96D-371
Eng96D-372
Eng96D-373
Eng96D-374
Eng96D-375
Eng96D-376
Eng96D-377
Eng96D-378
Eng96D-379
One assay ton portion used.
Au Au Check
PPB PPB
81
96
180
259 254
295
98
33
22
2
10
9
24
2
7
Ni 1 Ni 1
5
7
3
19
33
79
101 142
62
82
94
79
235
82
178
159
Certified by
Mil t i
Element
Results
to
f o 1 1 ow
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone ( 705)642-3244 FAX (705)642-3300
^
Page l of 3
6W-4692-RG1
Date: NOV-18-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Arm: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 82 core samples
submitted NOV-04-96 by .
Sample
Number
Eng96D-380
Eng96D-381
Eng96D-382
Eng96D-383
Eng96D-384
Eng96D-385
Eng96D-386
Eng96D-387
Eng96D-388
Eng96D-389
Eng96D-390
Eng96D-391
Eng96D-392
Eng96D-393
Eng96D-394
Eng96D-395
Eng96D-396
Eng96D-397
Eng96D-398
Eng96D-399
Eng96D-400
Eng96D-401
Eng96D-402
Eng96D-403
Eng96D-404
Eng96D-405
Eng96D-406
Eng96D-407
Eng96D-408
Eng96D-409
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
357
147
214
233
154
312
201 156
79
82
81
12
5
9
3
Nil
7
Nil
Nil
Nil
27 33
Nil
3
Nil
Nil
Nil
5
Nil
Nil
Nil
19 17
Certified by
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705 ) 642-3244 FAX (705) 642-3300
/l
Page 2 of 3
6W-4692-RG1
Date: NOV-18-96

Swastika Laboratories
A Division of TSL/Assayers Inc.
Established 1928 Assaying - Consulting - Representation
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Ann: P. Chubb
We hereby certify the following Geochemical Analysis of 82 core samples
submitted NOV-04-96 by .
Sample Au Au Check Mil t i
Number PPB PPB Element
Eng96D-410 Nil
Eng96D-411 Nil
Eng96D-412 158
Eng96D-413 Nil Nil
Eng96D-414 14
Eng96D-415 Nil
Eng96D-416 Nil
Eng96D-417 7
Eng96D-418 10
Eng96D-419 5 2
Eng96D-420 2
Eng96D-421 Nil
Eng96D-422 Ni l
Eng96D-423 113
Eng96D-424 365
Eng96D-425 146
Eng96D-426 Nil
Eng96D-427 Ni l
Eng96D-428 5
Eng96D-429 34
Eng96D-430 Nil Nil
Eng96D-431 67
One assay ton portion used.
Certified by
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone ( 705) 642-3244 FAX (705) 642-3300
Page 3 of 3
6W-4692-RG1
Date: NOV-18-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Ann: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 59 Rock samples
submitted NOV-05-96 by .
Sample
Number
Eng96D-432
Eng96D-433
Eng96D-434
Eng96D-435
Eng96D-436
Eng96D-437
Eng96D-438
Eng96D-439
Eng96D-440
Eng96D-441
Eng96D-442
Eng96D-443
Eng96D-444
Eng96D-445
Eng96D-446
Eng96D-447
Eng96D-448
Eng96D-449
Eng96D-450
Eng96D-451
Eng96D-452
Eng96D-453
Eng96D-454
Eng96D-455
Eng96D-456
Eng96D-457
Eng96D-458
Eng96D-459
Eng96D-460
Eng96D-461
One assay ton portion used.
Au Au Check
PPB PPB
7
9
Nil
3
Nil
Nil
Nil
2
Nil
Nil
3
Nil
Nil
9
Nil
237 261
Nil
Nil
Nil
Nil
106 96
74
15
51
27
262 266
17
21
55
62
Certified by
Mil t i
El ement
Results
to
Fo 1 1 ow
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705)642-3244 FAX ( 705)642-3300
/"l 1 XI
Page l of 2
6W-4689-RG1
Date: NOV-20-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Mm: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 5 9 Rock samples
submitted NOV-05-96 by .
Sampl e
Number
Eng96D-462
Eng96D-463
Eng96D-464
Eng96D-465
Eng96D-466
Eng96D-467
Eng96D-468
Eng96D-469
Eng96D-470
Eng96D-471
Eng96D-472
Eng96D-473
Eng96D-474
Eng96D-475
Eng96D-476
Eng96D-477
Eng96D-478
Eng96D-479
Eng96D-480
Eng96D-481 '
Eng96D-482
Eng96D-483
Eng96D-484
Eng96D-485
Eng96D-486
Eng96D-487
Eng96D-488
Eng96D-489
Eng96D-490
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
994 1029
17
12
Nil
Ni 1
Ni 1 Ni 1
5
7
Nil
5
12
Nil
Ni 1
33
41
15
65 57
Nil
Nil
Nil
9
12
14
31
Nil
Nil
19
Nil
Ni 1 Ni 1
Certified by
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705)642-3244 FAX (705)642-3300
Page 2 of 2
6W-4689-RG1
Date: NOV-20-96

Swastika Laboratories
A Division of TSL/Assayers Inc.
Established 1928 Assaying - Consulting - Representation
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Ann: P. Chubb
We hereby certify the following Geochemical Analysis of 59 Rock samples
submitted NOV-05-96 by .
Sample
Number
Eng96D-491
Eng96D-492
Eng96D-493
Eng96D-494
Eng96D-495
Eng96D-496
Eng96D-497
Eng96D-498
Eng96D-499
Eng96D-500
Eng96D-501
Eng96D-502
Eng96D-503
Eng96D-504
Eng96D-505
Eng96D-506
Eng96D-507
Eng96D-508
Eng96D-509
Eng96D-510
Eng96D-511
Eng96D-512
Eng96D-513
Eng96D-514
Eng96D-515
Eng96D-516
Eng96D-517
Eng96D-518
Eng96D-519
Eng96D-520
One assay ton portion used.
Au Au Check
PPB PPB
2
91 103
9
3
Nil
36
2
10
9
7
7
10
142 146
50 43
36
5
2
7
7
36
10
14
33
55
69
182
14
250
99 89
278 158
Certified by
Mil t i
El ement
Resul ts
to
f o 1 1 ow
P.O. Box 10, Swastika, Ontario POK1TO
Telephone (705) 642-3244 FAX (705) 642-3300
Page l of 2
6W-4690-RG1
Date: NOV-21-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Attn: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation Page 2 of 2
We hereby certify the following Geochemical Analysis of 59 Rock samples
submitted NOV-05-96 by .
Sampl e
Number
Eng96D-521
Eng96D-522
Eng96D-523
Eng96D-524
Eng96D-525
Eng96D-526
Eng96D-527
Eng96D-528
Eng96D-529
Eng96D-530
Eng96D-531
Eng96D-532
Eng96D-533
Eng96D-534
Eng96D-535
Eng96D-536
Eng96D-537
Eng96D-538
Eng96D-539
Eng96D-540
Eng96D-541
Eng96D-542
Eng96D-543
Eng96D-544
Eng96D-545
Eng96D-546
Eng96D-547
Eng96D-548
Eng96D-549
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
57
51
5 5
33
29
15
14
12
81
144
370 312
187
219
58
182 185
3
5
3
Nil
2
3
21
7
17
3
77 74
17
38
17
Certified by
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705) 642-3244 FAX (705) 642-3300
6W-4690-RG1
Date: NOV-21-96

Established 1928
Geochemical Analysis Certificate
Company:
Project:
Ann:
CAMECO GOLD INC
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting . Representation
We hereby certify the following Geochemical Analysis of 100 Core samples
submitted NOV-04-96 by .
Sampl e
Number
ENG96D-550
ENG96D-551
EN396D-552
ENG96D-553
EISG96D-554
ENG96D-555
EN396D-556
EN396D-557
e*396D-558
ENG96D-559
EN396D-560
EN396D-561
EN396D-562
EN396D-563
ENG96D-564
EN396D-565
ENG96D-566
EN396D-567
ENG96D-568
EN396D-569
ENG96D-570
BSG96D-571
EN396D-572
ENG96D-573
EN396D-574
EN396D-575
E^G96D-576
EN396D-577
EM396D-578
ENG96D-579
One assay ton portion used.
Au Au Check
PPB PPB
12
26 48
24
15
14
24
57
22
27
75
134
93
149
96
22
10
3
69 60
10
10
14
7
130
9
21
12 32 7
46
Nil
Certified by
Mil t i
Element
Resul t s
to
Fo 1 1 ow
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705) 642-3244 FAX (705) 642-3300
Page l of 4
6W-4806-RG1
Date: NOV-20-96

Established 1928
Geochemical Analysis Certificate
Company:
Project:
Ann:
CAMECO GOLD INC
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 100 Core samples
submitted' NOV-04-96 by .
Sampl e
Number
ENG96D-580
ENG96D-581
ENG96D-582
ENG96D-583
ENG96D-584
ENG96D-585
EN396D-586
ENG96D-587
EN396D-588
EN396D-589
ENG96D-590
EN396D-591
ENG96D-592
BNG96D-593
EN396D-594
EN396D-595
EN396D-596
ENG96D-597
ENG96D-598
ENG96D-599
ENG96D-600
EN396D-601
B*G96D-602
ENG96D-603
ENG96D-604
ENG96D-605
EN396D-606
ENG96D-607
ESG96D-608
E1NG96D-609
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
5
9 2
5 5
7
7
5
5 33
5
2
Ni 1 Ni 1
Nil
12
3
Nil 2
22 9
3
3
Nil
48
2
2
Nil
5 5
31 3
Certified by
P.O. Box 10, Swastika, Ontario POK1TO
Telephone (705) 642-3244 F AX (705) 642-3300
Page 2 of 4
6W-4806-RG1
Date: NOV-20-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project:
Attn:
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 100 Core samples
submitted NOV-04-96 by .
Sampl e
Number
ENG96D-610
ENG96D-611
ENG96D-612
EN396D-613
ENG96D-614
EN396D-615
ENG96D-616
EN396D-617
ENG96D-618
EN396D-619
EN396D-620
EN396D-621
EN396D-622
ENG96D-623
ENG96D-624
ENG96D-625
EN396D-626
EN396D-627
EN396D-628
EN396D-629
EN396D-630
EN396D-631
EN396D-632
ENG96D-633
EN396D-634
ENG96D-635
E^G96D-636
ENG96D-637
ENG96D-638
EN396D-639
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
5
14
12
10
31
9
5
14
5
7
24
34 27
69 70
2
Nil
9 5
Nil
17
5
Nil
17
2 Nil
3
2
2
3
5
3 3
31
22
Certified by
P.O. Box 10, Swastika, Ontario POK1TO
Telephone (705) 642-3244 FAX (705) 642-3300
/o
Page 3 of 4
6W-4806-RG1
Date: NOV-20-96

Established 1928
Geochemical Analysis Certificate
Company:
Project:
Ann:
CAMECO GOLD INC
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 100 Core samples
submitted NOV-04-96 by .
S amp l e
Number
EN396D-640
EN396D-641
EN396D-642
ESG96D-643
EN396D-644
ENG96D-645
ENG96D-646
EN396D-647
ENG96D-648
EN396D-649
One assay ton portion used.
Au
PPB
"\2
39 53
53
7
12
9
7
2
Au Check
PPB
10
Certified by
Mil t i
Element
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705) 642-3244 FAX (705) 642-3300
Page 4 of 4
6W-4806-RG1
Date: NOV-20-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Ann: P. Chubb
Swastika Laboratories
A Division of TSL/Axsayers Inc.
Assaying - Consulting - Representation Page l of 3
We hereby certify the following Geochemical Analysis of 79 Core samples
submitted NOV-07-96 by .
Sampl e
Number
Eng96D-650
Eng96D-651
Eng96D-652
Eng96D-653
Eng96D-654
Eng96D-655
Eng96D-656
Eng96D-657
Eng96D-658
Eng96D-659
Eng96D-660
Eng96D-661
Eng96D-662
Eng96D-663
Eng96D-664
Eng96D-665
Eng96D-666
Eng96D-667
Eng96D-668
Eng96D-669
Eng96D-670
Eng96D-671
Eng96D-672
Eng96D-673
Eng96D-674
Eng96D-675
Eng96D-676
Eng96D-677
Eng96D-678
Eng96D-679
One assay ton portion used.
Au Au Check
PPB PPB
Nil
Nil
2
Nil
Ni 1 Ni 1
5
5
12
7
9
5
9
Nil
5
Nil
12
3 2
Nil
5
7
10
3
Nil
12
51 45
Nil
10
29
5
7
Certified by
Mil t i
Element
Resul ts
to
f o 1 1 ow
P.O. Box 10, Swastika, Ontario POK 1TO
Telephone (705) 642-3244 FAX ( 705) 642-3300
x)
6W-4736-RG1
Date: NOV-21-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Aim: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers I nc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 79 Core samples
submitted NOV-07-96 by .
Sampl e
Number
Eng96D-680
Eng96D-681
Eng96D-682
Eng96D-683
Eng96D-684
Eng96D-685
Eng96D-686
Eng96D-687
Eng96D-688
Eng96D-689
Eng96D-690
Eng96D-691
Eng96D-692
Eng96D-693
Eng96D-694
Eng96D-695
Eng96D-696
Eng96D-697
Eng96D-698
Eng96D-699
Eng96D-700
Eng96D-701
Eng96D-702
Eng96D-703
Eng96D-704
Eng96D-705
Eng96D-706
Eng96D-707
Eng96D-708
Eng96D-709
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
Nil
2
Nil
12 12
Nil
2
3
7
3
Nil
5
41 46
9 7
5
Nil
3
Nil
3
2
2
15
Nil
Nil
Nil
3 Nil
Nil
3
Nil
Nil
Certified by
P.O. Box 10, Swastika, Ontario POK1TO
Telephone (705) 642-3244 FAX (705) 642-3300
/l
Page 2 of 3
6W-4736-RG1
Dace: NOV-21-96

Established 1928
Geochemical Analysis Certificate
Company: CAMECO GOLD INC
Project: English
Attn: P. Chubb
Swastika Laboratories
A Division of TSL/Assayers Inc.
Assaying - Consulting - Representation
We hereby certify the following Geochemical Analysis of 79 Core samples
submitted NOV-07-96 by .
Sampl e
Number
Eng96D-710
Eng96D-711
Eng96D-712
Eng96D-713
Eng96D-714
Eng96D-715
Eng96D-716
Eng96D-717
Eng96D-718
Eng96D-719
Eng96D-720
Eng96D-721
Eng96D-722
Eng96D-723
Eng96D-724
Eng96D-725
Eng96D-726
Eng96D-727
Eng96D-728
One assay ton portion used.
Au Au Check Mil t i
PPB PPB Element
Nil
3
Nil
Nil
2
Nil
Ni 1 Ni 1
57
Nil
Nil
7
5
34
10
5
3
353 285
O
Nil -
Certified by
P.O. Box 10, Swastika, Ontario POK1TO
Telephone (705) 642-3244 FAX (705) 642-3300
Page 3 of 3
6W-4736-RG1
Date: NOV-21-96

CAMECO CORPORATION
ATTN: P . CHUBB
PROJ: ENG 96-D
6W-4572-RG1
SAMPLE #
ENG96D-001
ENG96D-002
ENG96D-003
ENG96D-004
ENG96D-005
ENG96D-006
ENG96D-007
ENG96D-008
ENG96D-009
ENG96D-010
ENG96D-011
ENG96D-012
ENO96D-013
ENG96D-014
ENG96D-015
ENG96D-016
ENG96D-017
ENG96D-018
ENG96D-O19
ENG96D-O20
ENG96D-021
ENG96D-022
ENG96D-023
ENG96D-024
EN096D-025
ENG96D-026
ENG96D-027
ENG96D-028
ENG96D-029
ENG96D-030
ENG96D-031
ENG96D-032
ENG96D-033
ENG96D-034
ENG96D-035
2 Ag::l Al
:S;fci 3 . 4
22W1 3.0
s-:'x2-i 3.0; S'x'Sl 3. 5 ;
i|ifi| 3.5;
SfXSl 3.8;
2SX2i 4.3
W 3- 5i
:;Sxii 3 . 2';.;
"S Si 3.4-
lil* 2.4':
|2-:,B;l. 3.12
^:C S''"' :''Sv iS
"v-V'.V'.'-l -a T...
" .7. - V. J. O.I"
rSxifi 3.i7
* ' :' : '1" 1 R ' ' "
11 : 1.': 1* *- - O-/
M'cSl 2.4
4 - 4S
: v'.::'::y:?-,;.v''^ v ;S
PW/^rr 2 fi'"'-
Sill 3.33i
IP; 3- 2?
22X251 l . i;.;
Sixll 2. 2 i -*i 5 - <
•.•f..-'-:.:':?--?"-'------ • . --..- i
./..-. : ...-a.-":?-:'-,
: y . -' ."v v.'.y - *
SRI! 3.32.
;f2;X;il 3.22:
SixSl 2.5
2.322
0.9522
AS
/Ppra
ix''5 : <
Si-5 <
3:20 <
It* '
Sib <
ip? <
V/s
;20 <
I;M *
B i
ppm :
ppm
;'x is < ioi :2-"5
'.-.. /lo < 107
S'29"
S 20
Sfes < 107:
lOf
107
ibi
loS
103
102
ioS
IOS
loi:
1 n'--'
f 20
iol
ioS
io;S
72=7 ! 3.42 1072;
fei* 1-^l 2720 <
12*21 2.52:;
jjffg 1 2 . 9.;? SIP <
i:::^--^ :!:F:^: :^:; 1 '••!*t •f
fi;xSi 2.7.7 ^ -S < 1O|7
xfs < 10727
lofi W
101I
loSj
:^::^ : :i: W
10*
:i,'2't
Si i
2:X-xSl 3 . 6; 102
pt:;! 3.4; iS'5' < S 19
S'lO < 7-25
.;*;'i
i-S'2.
2 7X71' 3 . 0: fx;5 { 102 :t:33
S* .'5 < 10 2228
ixSs ( 10
l" 10::2 2253
lyH'V -. v
'"''K
'•••34
:;iis
X7;l
-iilO
P
SS* rj
'^5
pi;
fs
A .5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 min and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
Be 2|Bi.;/ ea iS :cd/
ppra ; i ppm Sf 7 ,ppm
( i2-x:.-5 4.2.;2xii
( lii;X.i5 4.4; r:x'i i ;
< riixSs 3.6SX21-
< i|ai:;5 4.922ix.;-l.
< 122X.25; 4.lIWii
< i77x;;;f 3.9S;;;xii
< i;i7xi.5' 3.8777x;;i
< i.22:f;5 5.i2;;xi::.i
( 17;. :;U25 4.62^71-
< li: 2^75. 4 . 3,; 2:: x '1
< i'2;V-; :5 4.5;;s'x::i
( lii'*:;;! -l - 52.;:-x2 :i
< l2-;-:^2.:5; 2.6;Sx2:i
< 1;77 :X25 3.i77;c7;l
< iS'piS 2.17i^7l
( 17:i.X:75 4 ..322x71-
< i:-;:x'i5' i7J:r^i;i
< lS;X:-5 7.9iW|cV;i
< llpi 7.4H1I
( ^i!*;^ lopp;
< 1::;2X25 5.5-22x11
< i;-;ixS5 i.9.;.l|.;::i
^ l 1 " "'''C"-' 5 1 2?"""'"^ f •••'••ip
< iWcis 2.4^|l;j :
< iSSiS 5.i-aflf2f
( i||?;t 2.o:S|ii;
< i;-;'iV:.'5 3.o;iv;;:i:
< liScfis; 4.9:pi::r
y l"1" ' ' "V " S 7 O"-"" /- : l"1 "
*. . v. ^ -. V ' . 7,.'....,.-V,y-.^..
< l72ixSB 8.3S'28i :
' e.oiScEi
TSL/ASSAYE .aboratories
1270 FEWSTER DRIVE, UNIT 3 MISSISSAUGA.ONTARIO L4W-1A4
PHONE it: ( 905)602-8236 FAX #: (905)206-0513
co -;-;scr :;
ppm ppm
35.22299
42;:S7i5'?
I.C.A.P. PLASMA SCAN
- S ;:"::'Si:?. 1;;:
;;'. 1.';,".;::.:.:.:/-. . /.
36 "' . (55
4 6 -i;::. 59
35 ::.i::S'6;5'
34; i 130
45vs;iib
140221:60
6122-160
592l'50
4 2 -; 2130
26i;7i :8fb
^lli
^•\:^:^-
•'•'- " ii - '" '"'
i3o::ii6bb
91 1800
36;;.i :23b
Cu 2,
ppm
120.:
130;
140-:
120i
120 1
97 i
Aqua-Regia Digestion
170S fei 1' 73 i-^0 * 2^070.1
62i
1302
1002
;Fei: Mg i. Mn : Mo :;2,.Ha '-;
* : * L ppra ppm:-* ; ::
7.7 1.5 1400 < 2, 0.03
X7.1 1.0:1600 < 2'0.06
22oi 2?i2 1.1:1400 < 2-ip;'02
1307 ml, 1 .671200 ( 27blo2
JKf)'- -'4 ''tt - ' : x ''' :':::".::.::...: ; ..
*- 3 U
;:: : . T : :,:. - .::::.TI ..V;^ ' . Y* v4
22' :2; 2;.2--22..: - ::-727:7::
i?:. 3 1.571300 < 2

CAMECO Cv,
ATTN: P. CHUBB
PROJ: ENG 96-D
6W-4572-RG1
SAMPLE #
ENQ96D-036
ENG96D-037
EN096D-038
ENG96D-039
ENG96D-040
ENO96D-041
ENG96D-042
ENQ96D-043
ENG96D-044
ENG96D-045
ENG96D-046
EN096D-047
ENG96D-048
ENG96D-049
ENG96D-050
ENG96D-051
ENG96D-052
ENG96D-O53
ENG960-054
ENG96D-055
ENG96D-056
ENG96D-OS7
ENG96D-058
ENG96D-059
ENG96D-060
ENG96D-061
ENG96D-062
ENG96D-063
ENG96D-064
EN096D-065
ENG96D-066
ENG96D-067
ENG96D-068
ENG96D-069
ENG96D-070
RATION
Ag Al As B : Ba Be
ppra fc PPra PPmi viPpra ppra.
O 1.75.^5 < 10:5100 < liv;
ci 1.6 ./V'S < 10*5120 * 1-i
(l 0.78 5.5. x 10;5l60 < 15
< l 1.3X5 ( 10:5380 ( l5
Ci 1.4- :10 < 1051525 < 15
< i 1.6:;. ( 5 , iq: ;;32o < iii
* l 1.6i; "IO < 10 ;;;.94 < 15
X ;1 2.6: .,-C;,5 < 10555 ; 8 < IV
xi i.3r55'5': ( i o;;:;,;^;.i < i;:;
•"(••i i .7::5.x5 5 ( i q5',x5i < i;.
1.5;
0.8 e;;;;;:: lo
0.9355*55
.5x:;l < 15
10
ii:v;;;2.5 < i5
lo;
s5i4 < iii
:.X-'l 0.45 : 5X;;5 < 10-
X l 1.2'55xl;5 < 10; 5150 < l
:"xvi o.38;5x:i5 < 10: :;5v30 < li
5:;:5 < i5
;x5i o.3i55x :55 < 10;
;vv:i 0.47;;;
3 0.565
:.?1 0.355
: l 0.675;
:; l 0.53S
! 5l 2. Si
;iil l.lf; :
vi;5 < 10
x;:;5 < i o"
bio < 10
C;5 < 10
l . 6ViiX;;:5 < IP' 1 .' 1
2.415:^5 < lOt
2.311155 < i o :;;
vX ;;1 l. 9VVWX
;vc.i;l 1.6i : i;x
Sftl 2.3l5"x
ii{':S 2. o!55i
10
10
380
iiati
ppm
< lisJSS
( l
( Ifi
A .5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 rain and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
TSL/96
*;' 5
TSL/ASSAYE'
1270 FEWSTER DRIVE, UNIT 3
PHONE #: (905)602-8236
:Cd
ppm
4.1;v
5.9;v ;x: i
4 .9 j .x: i i
6.8
5 .8
7.0
4 .0
5. i:
3.9,,
4.55
5. 3 2;, C Vi
5.6;:
3 . 3;;
4.8-V
3 . 25
4 . 9;;
4. eS
4. gf
5.l5
4 . li
3.0;;
4. i:::
4.75
4. is
s. o;;
4.35
7. 8|
"''*'i l
'?M:t
5;;:x5i:
-"boratories
JISSAUGA, ONTARIO L4W-1A4
FAX #: (905)206-0513
I.C.ft.P. PLASMA SCAN
co ;v crv. cu :;;
ppmvvppra ppm.
4751200 62 i:
48",;9fiq 57ii
32.;5 124q 82
98/1400 43
68:;;i3pb 55:
4q; : ibbb
33:i : i2ioq
35;ibqb
s&islbb
40 : V :
Aqua-Regia Digestion
Fe
5.2
4 f 8
V4. 6
4.9
tiiiz
74V5V3.4
33:;:
34V:
61^; ;;38q 30V
485.1550 6v;
46;:;::38b 29
sriSioiq 270"
4055':65 240i
;4 ;.;3.
43S;vl9q ISO;:: :;5iV7
375iii:14q 1305
vie i 7
3iv5;;|qq: 725
32ii;5i;4;i 260'i: vfcl
40 ; :96q 58 v
'4 ei
Mg Mn
'l ^ ppra
2.4 850
2. 5;flOOp'
2. 2:5 810
2.4 960
2.4 1000
2.4 :i;iiqq
2.4;i5;97.p
2.:
2.3^:930
2. 4g 9 60
4.2 2.5 ;900
2.755.740
2.55;i :68b
2.2 920
i8o;5;:6io 2.i5iibo
ssfb
v:3:7
;5:;3
30;;,
29;i;;.i'7.i6Q 345
44;5,;94;b 545 :5.;o
4i5iiqq 49i
43i: :iiiqq 46 ":
2.0 f;970
l. 95 :,9i8b
2 . 21,5,1680
2 .5";;t990
2.5
2.6;i;5i82b
REPORT No.
Page N o.
File No.
Date
M8268
2 of 3
NV07MA
NOV-12-1996
Mo V '.Ka ' Ni :;;5.p\... Pb 5;.i; :Sbi : se :;;;Sri; Sr . 'vvTi,, V VvW,.; Y ,5'Zn-'.. Zr :
ppm' v ife v ppmVvvvVppra ppmvrppni ppm;:,ppro ppm ;ppm ppmVbppm: ppm ppm ppm.
< 2^0.01
2xb.Pl
< 2 ip v 03
580'5|420
8701260
720;
720:v
36
.'.'.50
72^5250
72a:v47q
65i5vv2?q
2.4:i5 :890 < 2 (0101 3 505;i,56
2. 5; 1200
t li
ix-vS
S'p?
?Sr5
1SS*?:S
i,;;iS;55.
5;:i|i;5
5*l:x:|5;
< liivllifs
< iv'lvpg
210W::v220 < i;tgx
76o:jjf62 < li'iW
eebBivM < I'iiSX
4205i5i?'4 < 45:1
< l-
< l:i:
< IV
55
is; xviq
i 7 xvio;
20 x ib
15 ..t iq 670 ;,
17ix5io 2 00; v
2zi^;lQ i 6q:vv;
l45ixV;tb 1505;
15i'l;iO 140'5
15
16: X 10
15i x5io
li: x;
I35x;.;iq
2i;v
13i;
iiviq
vib
21f,fclO
2o5fclib
340;
230
530;
210
99V.!
100:5
i5o;5 ,:35
150V, ilb
iio'iv
1705 51
915 vi 37
1505
87;:
120;:
i7o5;
1305
120'
695
52;i:
87.55:v::l2
iob|p;5li8
16o|:i:532
7855537
1405:553'
270; :
2iq;v
14 o5 ;120
110;i iibb
290i: i, 32
;v:.24 51i;x,lP
220 i2q;x ib
'134 535x';iq
,5;36, 55;v;xi;ilO
iioSxiivib
596;;1P
514 VlP
17Sx,
vib
i75x : 'vi'ib
87:; : X;*ib
475X;V,1P
10
2v 22 8
2 18 6
11 .55 9i
2'i"'v;i"3'b 8"
i43
.;.iq
vilfi
5; 20
528
5-ib
;..'i;3
"' 22
5'6b
535
38
;:76
vvlS.
5i5
8.
9.5
I0i,4
8 5;
9.,v:;v
8.5,
a 5?
s',;,;'
4 ;';i
6'5
5;5
8.i.v' :
li;.i;-
i65:i
9.;;.
7 V
10
11'
7;'
10:
12;V
8

CAMECO CORPORATION
ATTN: P. CHUBB
PROJ: ENQ 96-D
6W-4572-RG1
SAMPLE tt
EN096D-071
EN096D-072
ENG96D-073
ENG96D-074
EN096D-075
Al EAss B s
;fp;ptti p pm}:.
2.321x55, < loiSEis
2.3igx;;f < io}}|xS|
2.o}I;p| < lOiSiat
i. slfJxSs < loifi-fl
Be
ppm
A .5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 c for 90 min and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
TSL/96
C a
:. :m0 5 .3}
||0| 4.4;
7Si5 3. 7l
r^./.v.y.-v.v.v.-. 'v
}K*f5: 8.7.}
}};X?'5: 6.9
TSL/ASSAYi. ^ aboratories
1270 FEWSTER DRIVE, UNIT 3 MISSISSAUGA,ONTARIO L4W-1A4
PHONE (f: (905)602-8236 FAX #: (905)206-0513
I.C.A.P. PLASMA SCAN
Co CU : :
ppm}
Aqua-Regia Digestion
Mg Mn
46:1000 38;:: 4/3 2.5^.910
4i}.:: 4 :;f 2.5KS7Q
47i'}3:i;7 2.4p7|cf
44Sf840 44}I3liB 2.5:}i300
59}::140i) 62lllJ7 2.5-'
Ni :;:
ppn
63&
.54
96;
Pb ;.,: :3l
ppm::;; : ppm ppm 'pm
X; 5
i c :.
REPORT
Page
No.
No.
File No.
Date
. 3n}; Sr } }Ti;.:
ppm ppm ;; ppm
16 V"lb 220}}: 35
17:;
15}" c: 10 160} '32
*Clp 120}} 53
13} X 10 460}} y44
18};: jt-'lO 290}} 39
V
, PP"
64
72
58
46
80
: M8268
: 3 of 3
: NV07MA
: NOV-12-1996
W Y Zn
:ppm ppm ;, ppm
0 10 2 18
i 10 1 }-17
:X:}10 2. J; 16
X'10 3 P12
X} 10 3 30
Zr
ppm
7
9
8
6
.10;

CAMECO
ATTN: P. CHUBB
PROJ: ENG 96-D
6W-4573-RG1
SAMPLE H
EN096D-076
EN096D-077
ENG96D-078
ENG96D-079
ENG96D-080
ENG96D-081
ENG96D-082
ENG96D-083
EN096D-084
ENG96D-085
ENG960-086
ENG96D-087
EN096D-OB8
EHG96D-089
ENG96D-090
ENO96D-091
ENG96D-092
ENG96D-O93
ENO96D-O94
ENC96D-095
ENG96D-096
ENG96D-097
ENG96D-098
ENG96D-099
ENG96D-100
ENG96D-101
ENG96D-102
EN096D-103
ENG96D-104
ENG96D-105
ENG96D-106
ENG96D-107
ENG96D-108
ENG96D-109
ENG96D-110
..IjAgl Al y:: :;.Aa' :
li ;ll 3///':///-
l-c/it l.S'l'VTS (
//.fil S.IIH^ (
1;:;:^! 2.8F;:i55 (
aSf'il 1.7;:lx:: :l5 (
|5||| 2.611//S t
^ -: ; '::i:-:;:-H ^'-:S
:S^^li-' -j 7V.'-;v'::/
ll/i 0.77 i IP (
VVPS 0.84?lf(
ill i: Si
i *Mli
<
1KB List*; /; :5 (
ilia 1.7/11
1IB 2.0/lx/
II *
lllii i.o/igj
lifsi l.si:*! /S (
Illl 1.5'llx/ ;s (
i-.5 (
::lMi 2.2,:l :'(i
I^XKl: 2. 5- x/
HIS 1.7.1111'5
(
2- ill'5
(
15" ( - -x
PUP ^^ii 5 (
5 (
?lfi:
a:i;)|ii:| 2 . i/.i/Vil5
4
PiXfl 3.2/llxl
Ivx/i i . syl] P (
liSll .. v:-..-.';.':.-"""- 1- 1' 1 . 5/lx/
'-.:."";:v i" ..m^l
i.tfmfr ;5 (
l^;w^ ?sfc
'/-e
1/5 (
'^^ir*: T - :/-'^'^/;''C'
- :.'-'w :'V'-"X 2 3- - '-'''' ;"-t ••
/.-vx^,;v::l-V *- ' -* --.v.v.-A...
ilw s.o/iH/
.vv .y-v.iv.-K. .' ' - ' - . . -.y ^ .v. . .
ia*:;yt 2.4/3;*::- is (
;i;::;m;;1 : , nv-ap
;virf;A 2.Q., :. ^~ '.y <
1/xil/l 2.5/llf/ 5 (
B 1.1 Ba/: Be //IBI/
ppra ppra ppm 'ppm
io/li/4 ( il:l;iv 5
lPs:;V-:13 : ( l'V':(l.:5
lOjl/es" ( li/lxls
loiifll ( i/lxlf
vv...^*4 //.s/Kf-/
c/"//;;.-*- zspis?
10;;; ;-10 4 l'.//:;*;:. 5
10:1/11117 ( rlS/f
IQ;.:;.;',: 8 ( I'/'/^x/S
10V".::;.40' ( l"vx;;5
lOi/llb ( I'l'xllS
lo/E/iib { il/Pf
iv:.v.-V""'-.*."-1 . '..".:,.-S.?!.-".''**.
io.;s:r|p: ( mm
lojiiio ( iSl(il
1O:;;;!::;13 ( 1/S/^ftg
iof;l;;'93: ( lilxls
log/eel ( i/:!!!
loi/i-ss' ( i/lx/is
lii-"iv /'//sis
10/^:^.70 - ( iv .'.' :'':x" :;s
:;s;r;;--;v :.---.-v-y.,5:
iP*l| ) p!8
ioll'i40 ( I'lliSs
s!"!'// /"1//1
IPS/lfiO ( i;:'a ;X::i:5
v::v- ' v:--'-' - ' ..-, " --v-v..."
10;; 190 ( iV-Vs
101/38 ( 1-.1X/5
lCf'f...f--:ftA. t r.*.:"//'!;
,"ifial*. * 1:v;rf./;/5
lOisllB ( i.;;.:;.(v;5
Sil
10?S :;S5 ( iS3Sit
i;;.;-::*'*' J-,,~.vA.v,S.
ioi?i30 ( ii;i:t:?:5
101/190 ( ll/lxls
10lS;;66 ( ll/S/5
10;;.1' :;.:16 ( IL/V'/S
v0 ':'.: ::;:."l::'';.-:. 1 . ...v v .
A .5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 rain and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
Ca VVCd'/
* .11 PPm
2.3l::(;::j :
4.2/1x11
8.7pi3i
2. 91 /Y /l
2.9'V..'(V:ii
5. 8// X lil
5. Si, Ky'jt
3 . alg'/i
9.lii\-X :|l
8.21/xll
3. o//:: (li
2.Dli:'|l|
aiitl
7.11/X/li
2. Si.//:/ /l
8
^ v - .- .-r j • v:
. l.A,; :.,yC;;;.l
7.61111
3 . liflMi
8 . 80lX; ; J,
q a illy- /W
^ * '../.vi 1 -\- t.
4 . sl'idi;
3.8l;.lxli
2 . ol/x'll
2 . 6;l;lii
9.5f lip
3.3||f'lf
2 . ifi/X-^i'
3.8llxli
7.2:llxli
4 - 4; I.: (/l
TSL/ASSAY laboratories
1270 FEWSTER DRIVE. UNIT 3 MISSISSAUGA.ONTARIO L4U-1A4
PHONE #: (905)602-8236 FAX #: (905)206-0513
Co 1: : Cr
ppm /ppm
32
37".I/MO
i;iiii-i :k;.
Zl'i.ly.i/1:
28ll'9p
28 .y;i40
49 /12PP
41 1:'67P
32 /jipip
36
35i
38;
37l
45"
33
46:
40 1730
38; 1540
54/
sol
I.C.A.P. PLASMA SCAN
l;7po
iipb
l/IP/a
I'fpO
.'.V6"5b
1/600
I/is
/MO
;;.^;.//;;;
/ /j-B-S
MtP
1200
Aqua-Regia Digestion
Cu v/Fe
ppm,: ;*
25-1/2:9
sil*;;?
171/410
35|C3i;i
.ll/;:*/'^:
7 si/Mi:
41-V/4V1/
17:1.3/7
45/V4V6
41 3,5
441/112
r:./::::;*., :--.-.--.
I9;:e;2 c;5
22P3/V
45ll 4^.3;
220^:1*3/9
si/i'fi-a
26/3,0
37.1:^:4... S
.- v-'-'V -.'"' "v
42l";3v:5
381/31.9
14P :1|4:..;2
38/1.316
a it"--..'.'-"^' - f
34::i;,.;3v.6
36l|3l|
VIST's
' :. ..:...* . P
36i3|f
SOJf '6*6
UOl'/sle
Mg Mn
* ../ppm
2.2 590
2. 4-1; 4 10
2 . 4/1/300
^ ' 2;;;;;:280
2 . 1:1/410
1 . 8: . 5*00
1.91/540
2.4/ 930
2.5 850
2 . 21/420
2 . 2/1.14:0
2.4/920
1.9/1480:
2.0/1390
2 . 4/ VS6p"
2.4/195Q
2 . 41/900
2 . 2/1//350
2 . 4/1100
2.4/ibbb
2.1/1510
2.4/1100
2 . 411.1000
- " '- 1 '. -' --:- ;
2.4V 720
2 . Ol : 360
2 . 4/liob
2.2/1580
2 . illesb
2 . 2l:;82p
2.3iiibib
Mo yVNa ;- Ni
ppm !fc ;;: ppm 1 PPm
2X0.^01 520
,V;',"4'0
( 2xb;01 530 /1200
( 2(p;pl 630 11:670
( 2XO:s01 870I'lsio
< 2Xp*pl; 140 : 2000
;:;;;;;;;;;;;:// i;::;
; ;v.':.. ; . ;
( 2Xplbl 100 :i8po
2/0; Of 52 2000
10:0.02 79: 1600
( 2X0.01 520
si
1140
( 2X0.01 720; :lll58
; 1;; 1-- li;. 1;.;"1;; v
( 2x6^01 680
'v::. v.:..": : ;:-.v
( 2,;,pip2 170. i:pbo
< 2'Xplpi 590" //24P
( 2;;;b b3 741/18pp
( 2X6Vbi: 770
( 2xbrpl 680; .;1'1.4.8
( ^(b/plll 810 240
( 2;.bvbl 150; :-j7bp
. ,.;' i'.'; 1:-': '.:" '
:;;;';;',V:/// :/
( 2XO;:01: 680-
;::-'V;-'.''.".'.--' ;;
( 2(0/01 720^
l/iso
?
:*||Q
;;;;;;;;;vv '--' ;; :;::;7 Z
s;*.:;;':/ ;;
( 2Xp:.pl 3 80l 1/300
2X0.01 300 :-:i:'86'o
( Sill 6? ^300
i:il|q
( Zi&i'QJ; 900/
ti::;;;:;;;,'/; ^
< 2XOlpl 3 ID/ WSp
( Zlofpll 320/ 128'p
( Zi&j'QZ 7 60/1 ';liil2
( 2(0lbi[r999|i
TSL/96 SIGNED
Pb ; Sb
ppm ppm
< 1/1x15
( iv/X/S
( l/lx/ls
( il'/ixls.
( ll/X/.S
. . - .- .. ,. .. .
( 1 "-..//X/ 5
( l ix 5
( li li "S
( i..l,ix:i:5
( lllWsl
( l/ix/'S
^. .-- - 1 ' 1 : " - 1 "
< i;;;;:x-;.5
( il::ix"l':"5
;.;:;:;::;/::: '/:
( l?lx?;5
( i/;' x/s'
( i:ll(l;.5
( il/V/i's'
:-..o .. li..:,-.. 1 . .-..-
( ilii^/s:
< i-i/V/s'
* 1i'-S./^'
^ J-1./.-..X.1 5
S 1 ' '- " C !?
( ll/x'ls
( 1/11/5.
< I'/lfpS
( 1;;;;,;!'(:?; 5
(
( iliix/s
< i/lil
Se
ppm
3 (
4 (
4'. (
16 (
10 X
REPORT No.
Page No.
File No.
Date
10 120
12 (. 10 210/.
12 ( 10 350 1 /-l-u:
13; (1
5l 'C'
10 3301
10 100
14/X
15/X/
6'(1
Sn Sr
ppm ppm
8 ( 10 160 1/12
7/X .10 130: ::-:-;17:
8li( ib 180
11 X 10 38oi
4:": x:
10 98- l/-':*'*
10 93
10 100
10 100
10 250
10 310
5 : X 10 110 'li. 35
11 ( 10 3BOl 1.1/6
5'lV :1P 14 O/
12 ( : Ip 590;
5 ( 10 1401 ii 1.41
v '.-/v/
10 330
1 ppm
: 18
28
111-15
/lib
V/25
11/62
10 360'
10 13O' i- .42
12 ( ilO 490, /V26
16 X 10 340 : 40
:.":'i,.:; :::
-y l ' '-:
13/X;: Ip leo/;
14";;(: lo i9p:/ ;128
4l.(l 10 no// 1/26
3''i-(i : : 10 HO/:
12-/X;'
10 480/ /l?4'
11;X/ lib 93/1
9:.(/. 10 Sil: /146
9ll(/ Ip 1301 1/2S
13 /X 10 260l 1;'72
14l'.( i 10 1701
V
ppm.: .
42 x
52; V
34il(
14/X
14'1'x
11 i(
iol (
69 1(
23l (
25l;,(
26 (
24 X
14/X; 10
20/x
39l(
34": <
48;': X.
16 X
10
K
2lV*l ;10
43 : XlIio
52.1x1
62:ix;
69/X
121(1
M8267
l of 2
NV07MA
NOV-12-1996
W
ppm
10
10
10
10
iio
10
10
10
10
:io
10
ip 10
10
10
10
10
:ilo
IP
Iio
IIP
lib
lop/x/: :io
"i o
58" ( io
70/V ib
Y
PPm
2
5
4
5 :
7
7
8
7
3
3
5 43
3; 1/20
6 : ,l38
4
7 : : .24
7
3
4
4
7
5
;1: 35
4.'lvl
2' 2
5:1 .115
51 1;:59
7/1 v/32.
8li! i;|27
41:
lvl;.- vi
4
3..'-'
3/
Zn
ppm
21
50
/:40
122
- . .^ -
28
19
21
43
115
/31
22
12
35
'l/ 42
1/25
"- 34
l;5p
/;72
'" --'55:
37
53
Zr
ppm
4
10
11
4
f 1 ;
2
2
4
6
2 "
3
3V
2
6
3
( 1
5
3/
9
2
V,
3
4 :
5
6
10
1 1
4:
6/1
8 V
4 ,

CAMECO
ATTN: P. CHUBB
PROJ: ENQ 96-D
6W-4573-RG1
a/m^LE H
ENG96D-111
ENG96D-112
ENG96D-113
ENG96D-114
ENG96D-115
ENG96D-116
EMG96D-117
ENG96D-118
ENG96D-119
ENG96D-120
ENG96D-121
ENG96D-122
ENG96D-123
EN096D-124
ENG96D-125
ENG96D-126
ENG96D-127
ENG96D-128
ENG96D-129
ENG96D-130
ENG96D-131
ENG96D-132
ENG96D-133
JRATION
- ' :*9v; Ai ;.;AS
;; .ijjgj- * , ;; .
:.;;;v^;; * :,;;^v : .
';;' . :;;^ ; : ..:..: - '
;r . C,l 2.9 V J5
' " ' ^ "'1 1 9 ' -'. v -e
:^1 lisfx'i
;;,*t Lake's
i..:?;* i - il;l.* -S
.-..v.- - ' .' '" " ' ": ' : ' . - 1.".. "'
s**-;! 2 . 2;;;v;:5
- /*. . f ". ."-v/'-.v:-.-:^ 1
4 1 1 . 6 :: g
i 2- if! 5
tlfl J'p1*
-..vv:. .:' : : ;;.JL 1 - *'61;^ ; 5
!:.' -.V4."i ? Q/H^^-et'
...- v..?.-.-:.'-.*. * * *:..-,-.v.. S.-v.'.fl
r-xll i.2li!x:?:s
;,;;xajt o.56#;*ft:i5 :
ISii o.4oiifii|.5
BHffiii 1 . 4"..;*xS5
Si;:,;;;;; t;*sS;
;;..w^-::^ o ji';.'.;'r''''e
sijiiVil Z. 4.5.4*4.5
SCI 1.4i;'';fl;i5
;;""x"--'-ili 2 a'";-:;i
. V~* *- O V.:, 5
;:;-:x*i 1.9.:.^;. 5
i;;*;;! 2.ol;iix::;,5
*lll vlRisi
lall 3.4;i;^lQ
IWffl; i.apei
ai|;i| i . o;iss,:5
:p:;;i:;^ ;;;S;:;:;
B S-BBL;:
ppm ip'pra
< lp'Ai-23
< loillcli
< l Pi ::'li :i'27
< Ib;:lll30
t io;;2lo
( io;i:i3b
< io;;i27P
K 1011113P
< lomm
< i Ol;l;l2'6
< loli^gp
< loisliio
< io:i:;;si6
< loglop
< io||Ji7o;
l lolSp
< 10 44o
< 10 270
( 10il
< 1014710:.
< 10 ::iii230
< idlips
Be ;.;Jil :
ppm ijipm
t i-lxlls
< I; .:.^l5
< 1';'1S
< iilj^ls
( I'S^Bj
< i;::l;i'l;:5
( i.?.;-*'*
< lisiWg
* 1S;^1^
< liiil-x;!'!!'
* i|ii
< iSPf
< ll-;x:l"is
< 1 : X.; S
< l'. : -.te5
( iliiiss
* ifiil
* iiii.ffi?.
i'Lifigg
A .5 gm sample ia digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 min and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
TSL/96
3. 9.1;; ^iji
v . i;:f x';il :
S.Bflixiiil
s.gal'lil
s.oiiiii
TSL/ASSAYF " ^aboratories
1270 FEWSTER DRIVE. UN,, i .SSISSAUGA,ONTARIO L4W-1A4
PHONE #: (905)602-8236 FAX # : (905)206-0513
I.C.A.P. PLASMA SCAN
Aqua-Regia Digestion
4is 2wo a-^.* * 2i;^ ^ti < W* "U;-.S 290^
37::ti|ol BZ^lj 2.3^50 4^'^ ISollloo t i^f's 1 0^ :SO , J
-ill SI;! -SI * i|| -il ' fi 3,,io ..i
REPORT No.
Page No.
File No.
c a i;i;call colfrl cugre;, Mg ;i,;Mn'; Mol :i'lNil N1 ill P. .1.1 Pb '^-i S c :ll'.Sn ' S r ; , Ti ;
ppm:::;pPm ppnTVi;-?' * -tin nnm^v'?; "'t^i . :;*,;.:^ a c - '-*'n ' ! S r v; Ti :
ti;::i: ii! ;;E;;;;::: "~ ';.';;.;.: "- ;:--S:* : ~ rr "'.:,;;:J; :.;: t't"";s^R? ppm....;:ppm ppm;/.. ppm ppm ppm
s.eSi'li 58;. 1200 9;:4.:4; 2.4,1000 ( 2x6ipl) ''99
s ;86 < i; ^ 5 16 :-t-'-lP 230
10l:lx-l
44 S;fM 12;;; ::.4:;0 2.4 iiOO < 2*0701) !
i '29
9 -"f;^:'i
'99 SMO < i:;;x ;-l5 13(^10 7 nn
45:;:ifi0 235,:3.4, 2.4;ilOO < 2Xfc6i 780^^140 * 1" :x''5 : 11 -/"in iqo
7.9S:;x.;;l
11148
^1|*| 2 3^1^V* 2- 4ll ::970 < *9m 7 60.5f50 * llli^5 13':: (.;: : 10 3401
2.7;"**'!!
li; i3 6
S
l'j;sl'3Q
1
24 : ;.,; ::2.'7,
i*
1.9.: : : 450
i
<
ilisi
2:p;p5 -TR-iJ'nA
i
,
ii
,:;;;: '.v
m
-;V;::^
i
' "v'.vsjyy v J-;.:::;.s ;::p J':X...-1P 150 \ 70
5.3?';*iiii
2.8i.pr''i:
1:69
5.5;i;x;i
.":42
7.5-"xi'i
l. 26
60t|POO 44,N"i,fi 2.4: : ; 8 60 ( 2i'6;0i Tio^Vp ( rl^ 5 14 !n ?^
e.iHUli
16
10
19^:IP: 32|ilZ,'fl 1. 6111650 2ilo;:oi 28:l90P z^J 3! ^ ^Qo^
."1:38
28;:i:S10 441*3 v9f 2.1^:790 , sfa'i^r , , , f:-^-! !,, V^? 1 90: ^
SSKf rjssm '-'ittit:;:?;: i;;;.;*::;;; 1 ' ~:.:":." ""w't"" s ' sss- 3 //..xtiio 25o-v-;?i
5.5?!
3. 9:li x'; 1
5.b'.llx' :':I
5.1;;i: : {t'i
5 - 1i:l; 1i
5 - 2l.il
6 , 0 ': X : : 1 :
-iv:: 11.:-' ;--/*.
*-mm
37S5i3P 57 :;lfti3 2.3i:ii800 < 2xP;o! ISo'Slod < 1E3K , ,;*"C ;?
25^2'(ffi 110K3VS 2. if 1680 ( Z^VOZ llO^iTda < ^ S 1 3 ^o 28o'
38 .:l'*?0i 59V4V8 2.31920 < 2;6vOl 340 Il3 00 < l/Vs 12 10 27O
3i:i:;;23o 55;:;4 :: 4 2. 2; 920 * 2,0:01 zooJSo' ( i it 5 'o lo
35,;::a7(? 93;:j;4J7 2.2rv92P { 2;OvP2 l^nSiivv , 7S- .-M? 2 6^
:v??^" L .,;;:^v :' l u v.io 220
45Hi l^Iii 2.4p'81p < 2il'oi 3
;;^ ...;.;::: ; : . i^;;^f;;;5. 15;x^lo 280
30*JM 87;;f3:,.9 2.2ai-9bO * V®M 2
20 ;;9io 7..::::::^;:^ R ::.v^iA o-art-
25;M;;;.6i5 55'si3i;i 2.0l;;600 < 2?6ri'0f 1
igiffig illiSyii S;.!';!;;' IfEffi;
Date
; 29
1:18
30
'l' : ' ;45
140
176
95
i 130
y;;59
1: 31
isle! -rfsi s;.;x-;.10 2 30i. l;2 .5'
SIGNED :
v ppm
76 "t 10
51 ^10
30 ix .10
35
18
43
26
58
46
35
15 t 10
5 * 10
5 X 10
6 -vi.iP
18 •A. 10
45
74
58
46
43
62
11;
4i
1 "'W
, ppi
M826V
2 of 2
Mb
* 10
'X 10
"t ;'lp
CllO
.X 10
* 10
< 1 0
< 10
x lo
< 10
. -," . ".
1,;.liP
:.Mo
i'- -ip
NV07MA
NOV-12-1996
V
ppm
4
4
3;
4
7
4
4
3
3
3
7
9
9
9
11
5
7
8
7
10
7...
8;;
7;1
Zn 1
ppm
47
17
"' :i7
',:i. 12
2.5
61
40
36
29
29
93
41
30
29
:.;53
55
51
87
79
66
93
53
40
Z r
ppm
6
5
6
51
1
8
3
5 i
4
' 6 "'
6
3
2
< 1
3
12
7
7
5 1
4
9 ::- ;
3'1;
3

CAMECO
ATTN: PETER CHUBB
PROJ: ENGLISH
6W-4574-RG1
SAMPLE
ENG96D-134
EN096D-135
ENG96D-136
ENG96D-137
EN096D-138
ENO96D-139
ENQ96D-140
ENG96D-141
ENG96D-142
ENC96D-143
ENG96D-144
ENG96D-145
ENG96D-146
ENG96D-147
ENG96D-148
ENG96D-149
ENG96D-150
ENG96D-151
ENG96D-152
EN096D-153
ENG96D-154
BNG96D-155
ENG96D-156
ENG96D-157
EN096D-158
ENG96D-159
ENG96D-160
ENG96D-161
ENG96D-162
ENG96D-163
ENG96D-164
ENG96D-165
ENG96D-166
ENG96D-167
ENG96D-168
INC.
Ag Al Aa
ppiQ fy ppn
;(?i 1.6? * 5
;X 1 0.94 s; 10
SIM 0.74|IX?5
JX?i 0.79???;";5"
gel 0.57?:;:??5
Hi l.B;?l(?5
|cii 1.8^'x 5
*..X?1 0.78??X -5
?Y-i 1.2 a :ris
;:x'?i : o.52 ? s
iYSi; 0.56:;3Xv;5:
S*?* 0.89?;;Y;;5"
|f || 2 . Q?5*:;;;5
f*;i 1.8??*;,*
pis* 2.Z??:;lp
i-xli 2. 5.:??*? 5
S*?i 2. li- x? 5
W?i i.5;;,M5
?(" :i 2.i-?x;;5
|xli: 2.3|fftS
??Si 1.3'???? 5.
?*3l O.eoisYlS
?x?;i i.9l?;Y:5'
?Y:Sl l . ss&io
?x|t 1.9;!?;.. s
Myt i .&u'irs
?Y?i 1 . 7?;:;:* ' 5
WM 2.4?(;x'5
Rp 2.5Px';:5'
lal 2.4|?;x,; 5
111 2.25?x;;5
?;di 2.2?;.: 10
2.4??X?5
lil! 2.4??(?5
ilYtf 2.5??X;;5
B ,: :; Ba
ppm :ppm
( 10 ?98
* 10;; :i :i9
( io?; ;Il3
< 10;; :|65
' 1 0Jlil?
( io?; ?230
( 10? ;; 90
( 10u: ;130 '?56
( 10
( 16; "?21
< 10?
< io;; l?l 6
< io?; ;i:28
< iol|;;27
' 101
< 10? lip
< i o?; Siio
( iol?;;86'
< 10y;:3Bb
* 1 0I?ttP
* 10; Se'
::::.v
??17
( 10? ??29
< 10? ?;: 17;
( 10? |?41
t 1 (jl;-
; 2
( 10 vX:;;l
* 10; ?x. 1
( Ip? "Yi
* 10?
I?!;1
( 10!
?';? '";x?l 4
< 10?
< 1 0? ;?? ; ' : 5
?,*?i
< ip;;
< i o;;
??'53
li?.
?5".4
Be
ppm
< 1
( 1
< 1
< 1
< l
< 1
< 1
t 1
* 1
< 1
< 1
< 1
< 1
* 1
< 1
< 1
< 1
< l
< l
< 1
< 1
< 1
< 1
< 1
< 1
< 1
* 1
< 1
* 1
< 1
* 1
* 1
< 1
* 1
< 1
f, . 5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 min and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
TSL/96
Bi
ppm
X ?5
v (?:5
';( :5
:,;x" 5
' :*' : '5
X 5
< 5
( 5
( 5
X 5
'x; : -5
" fcs
:X.":5
.' X:" 5
•*7*.
?X;5
(5
.. ^-"5
(5
- x. '..S
(5
(5
(5
( 5
< 5
x" 5
X 5
vf 5
X--:5
'?X,?5
'7;'s
* 5
( 5
X; 5
( 5
Ca
*
4.7
3.8
4.4
4 . 1?
3.6
5.9
5.4
3.7
5.0
3.9
3.5
3.8
7.3'
8.3;
7.5
5 . 3
5.6
5 . 9 :
5.3
4.8
2.9
3.4
7.5:
7.9
7.3 :
4.8 ;-x 1
5.9 XI
7.1 ;;V:'l
"' (' -. I
4.9
x":!
3 . 8
3.8 * 1
4.9 ( 1
4.2 ( 1
3.9 i x.'i
4.4 x 1
TSL/ASSAY: aboratories
1270 FEWSTER DRIVE. UNIT j .-iISSISSAUGA,ONTARIO L4W-1A4
PHONE tt: ( 905)602-8236 FAX tt: ( 905)206-0513
Cd
ppm
'Vi
< i
;x 1
V;l
:*"1
(i
x i
( i
x i
. * i
.ix:i
":X .1
x '.'1
x?l
:^;1
;l;i
-x ";l
^ l
XI
X 1
i'V-i
x 1
X 1
(l
?* ;1
Co ?
ppm
46 y
28
28
is;
18
30
25
19
23
20
16
21
42
41:
44
36
33;
26
31
34
28
22
41
43
41
47
51
49
49
52
46
47:
51; 1200
53; iiioo
48: ? 830
I.C.A.P. PLASMA SCAN
Cr.
PP"
?930
?170
??85
65
86
240
110
140
86
90
.'.'."..' 95
V..74
:800
1000
:J9;^
;i50
:;i40
iio
210
;i5o
75
88
850
1100
840
990
980
1200
1200
1100
iioo
iioo
Aqua-Regia Digestion
Cu Fe
ppm ,, K : .
45 4^3
78'?-3l5
47:-':;3?8
347;^;;^
32;yi2;'(S
32 3?4
26 3^8
is; 2^5:
13 :3;5
15^ ,2i7
100 ; 2y4
14;.;,4vl;
22",;4j3
10 :;?3;i4
48;?;4i;p
85-?4v9
26:?4;i4
35 3,; 8
39 3?8
56 4,3
19;;;3?9
13''-: 3^.4
33 4,0
41 .3^9
29,,' :'3X7:
33- ?4?0
40 4ii
47; 4:?3
44?4M
56.. :.i4J:4;
45 : :' 4v3
45 4.5
4 1;. 4? 5
53 ?4;i;7
51 ;4.5
Mg Mn
* ;, Ppni
2.5 920
1 . 9 ^620
1 . 9??690
1.8? V 720
1.7:; 570
2 . 3 ; 830
2.2 : 890
1.8?? 6 00
2 . 1 770
1-7 : 580
1 . 7;,?' 580
1.9?" 640
2 . 4; 3,200
2 . 5;;i200
2 . 5: ;:iibo
2 . 3 ?900
2.3 "980
2.2: 1POO
2.3 950
2.3; 870
1 . 9l i 550
1.7?; 600
2 . 5?i300
2 . 5?i3bo
2.5?1100
f.;.,;;?-
2 . 61" 870
2.5; ;990
2 . 5|?:970
2 . 6?;: 900
2 . 655BQP
2.6?: 820
2.5? 920
2 . 6?::840
2 . 6??820
2 . 5 ; : :820
Mo ??Na? Ni P
ppm;;: X: ppm -ppra
< 2 *0? 01 640 90
* 2?0,:p2 80; 1800
* 2?Pvbi 56 1700
< 2 ;;;bv02 16 2200
< 2?priP2 49 1600
< 2 X0,01 180 1800
< 2 XP?Pi 120 1500
< 2?bibl 78 :1500
< 2 ::p;bl 120 1700
< 2?0.;02 60 1700
< 2?pl02 43 1500
< 2 Oi02 45 2400
< 2xP;01 440 420
* 2XJS|01 670 72
* 2*P|Pl 520 410
< 2XO?Pl 140 2100
< 2Xb ::}bi iso 1600
< 2*0?bi 110 2000
< 2XpVbl 210 1400
* 2; bjbl 170 1700
( 2i;ffi02 64 1600
< 2?btP2 54 1400
( 2Xptbi 620 310
* 2X0:01 640 74
* 2*p;0i 650 210
< 2 *0ifll 630 58
< 2 *0vpi 690 .; 58
* 2*p;pl 580 94
* 2XP,ipi 550?: 110
( 2XK01 550 , 100
< 2XpvOi 520 78
* 2xPs;pl; 570 180
< 2 X(g:bi 620 86
< 2^otbi 560 82
< 2 (0;bi 390 82
Pb
ppm
31
2
2
( 1
1
< 1
< 1
i 1
< 1
< 1
( 1 * 5
2 * 5
< iJ 'X j 5
< i ; X. 5
i 1; ; * 5
< 1 * 5
< 1 :?V5
< 1 : * 5
< 1 ( 5
t i ( 5
< 1 ( 5
1 * 5
< 1 * 5
< 1 (5
< 1 - * 5
i 1
< 1
* 1
< 1
< 1
( !
< 1
< 1
( 1
( 1
SIGNED :
3b
ppm
* 5
X 5
;X: - 5
X: 5
* 5
* 5
< 5
* 5
* 5
* 5
* 5
* 5
* 5
< 5
(5
X 5
* 5
X 5
< 5
X 5
Se Sn
ppm ppm
13 ( 10
3 * 10
4 * 10
3 C'10
3 * 10
8 ( 1 0
5 ( 10
3 * 10
4 < 10
3 ( 1 0
2 * 10
3 * 10
12 t 10
12 < 10
13 < 10
9 X 10
7 C-'lO
7 x 10
7 * 10
6 * 10
3 * 10
3 * 10
12 * 10
13 * 10
12 * 10
13 * 10
13 < 10
14 ( 10
15."* 10
16 X 10
14 * 10
14 * 10
15 (10
15 (.-10
14 * 10
Sr
ppm
260
180
240
220
200
450
350
200
290
210
17O
170
350
400
420
300
300
270
280
210
150
160
290
300
280
75
120
130
70
100
REPORT No.
Page No.
File No.
Date
Ti .
ppm
13
25
725'
29
: ; 23
18
23
14
11
21
12
9
15
18
19
37,
19
28
26
22
19
25
17
.15
17
220 19
230 33
230 25
140 ?V - 31
120 :. : . 34:
'V'-4i
36
;;" .-.47
?5'4'
; 37
V
ppm
395" j : ( 10
*;10
5? ( 10
8 X 10
7 * 10
8
5
3 ;
4
6
2
2
37
49;
43
9
10
9
20
13
10
6
35,
40
40
55 :;X :; 10
54 "x; 10
63 ;,X,10
61 : Y 10
45 (10
M8310
l of 3
NV18MA
NOV-19-1996
W
p,pm
X 1 0
< l o
( 10
( 10
( 10
* 10
* 10
,* 10
X 10
(10
( 10
( ;io
Y 10
( 10
( 10
x 10
( 10
Y 10
(10
( 10
37: * 10
38 (10
62; X iO vx''.io
56
63: ?X\:10
Y
ppm
2
9
8
9
7
8
9
6
7
7
6
7
4
3
4
11
8
10
7
7
8
9
5
39
5... "i?32
;". '.22
3
2
3
3;
4
2
3
3
2
2
2
Zn
PP"
37
33
30
'v'22
'?26
57
:57
38
72
26
25
::33
47
25
:' ?34
?62
62
50
68
i.; 67
'':: 3 6
? 722
28
i, -30
:?';38
.f" :; 4l
'?"3^'
;?35
'36
;3'8
: '. 3 8
40
Zr
ppm
8
2
2
( 1
( 1
1
< 1
< 1
( 1
( 1
< l
1
9
4
8
4
4
3
4
4
2
3
10
4
6
5
4
7
4
7
5
10
7
9
5

CAMECO
ATTN: PETER CHUBB
PROJ : ENGLISH
6U-4574-RG1
ENG96D-169
ENG96D-170
EN096D-171
EN096D-172
EN096D-173
ENG96D-174
EN096D-175
ENG96D-176
ENG96D-177
ENG96D-178
ENG96D-179
ENG96D-1SO
ENG96D-181
ENG96D-182
ENG96D-183
ENG96D-184
ENG96D-185
ENG96D-186
EN096D-187
ENG96D-1B8
ENG96D-189
ENG96D-190
ENC96D-191
ENG96D-192
ENG96D-193
ENG96D-194
ENG96D-195
ENG96D-196
ENG96D-197
ENG96D-198
ENG96D-199
ENG96D-20O
ENG96D-201
ENG96D-202
ENG96D-203
INC.
Ag
:PPW
i i
* *
'x il
i' K --
1 1
* i
* i
: * :: 1
:ili
?;-fe;X
tfii'j
II1-
iY'f
fill
Wfi
i'Je'.l
^ ?ilii
Yt
Yii
i?!?!
ii|:l
'Yl
i. i'. 1
Y i
i, lil
i:-!1
i lil
: * il
* ?l
11
* 1
Al ,.
*
2 . 0 :
2.1
2.2
2.1
2.2
2.6
2.8
2.9
2.5
2.6
3.3
3.0
3.1
1 . 7'
1.1
2.3
2.4
1.9
0.71
0.32
0.25
0.62
0.45
0.47
0.29
0.43
0.36
0.26
0.24
As B
ppm ppm
* 5 * 10
* 5 * 10
5 * 10
* 5 * 10
* 5 * 10
* 5 * 10
* 5 * 10
* 5 * 10
X 5 * 10
* 5 * 10
10 * 10
* 5 * 10
:. 20 * 10
20 * 10
1 . 0 : i*: 5 * 10;
1.3? X -5 * 10
1 . 5 5 * 10
0.63 * 5 * 10
0.98 Ji5 * 10:
'Y; 5 * 10
* 5 * 10
10 * 10
x; 5 * 10
:- ;;i5 * 10:
x 5 * 10
1.5. * 10
* 5 * 10
15 * 10
* 5 * 10
* 5 * 10
* 5 * 10
* 5 * 10
* 5 * 10:
* 5 * 10
Ba
ppm
2
* 1
* 1
V 1
7
* 1
* 1
250
16
15
9
11
X 1
i* 1
: .-'18
68
94
12
50
130
47
47
41
51
43
36
40
23
22
49
31
75
50
31
Be Ei
ppm ppro
* l, ,x;5
( 1 i; :^i5
* lii-x'is
* li i* iS
* 1 < 5
< 1 15
* 1 -'.- V:.. 5
* i i*i5
* i?; ,, .i ;5
* i; :; i S
* IVY; 5
* r? ;Y5
* liiiYls
* 1S|S
* l?i'?i;' : -5
* 1 .'1:5
* i .Y: 5
' ^iii'ii!
* i?????Y;5
* i?5?Yi5;
* I'i?:*.;;;;
* i^iift
* l:;:;il?75:
( i;;;?Y5
( i':?iiv:.?5
* l???Y-5
* li?;Y?5:
A .5 gm sample is digested with 2 ml of 3:1 HCL/HN03
at 95 C for 90 rain and diluted to 1O ml with DI H20
This method is partial for many oxide materials
TSL/96
C a ;;:-
*. - '
4.0:
5.7
4.7:
4.0
4.3
TSL/ASSAYI laboratories
1270 FEWSTER DRIVE. UNIT J rlISSIS3AUGA. ONTARIO L4U-1A4
PHONE tt: ( 905)602-8236 FAX #: (905)206-0513
2 . 3 :
1. 8 : : ?::Y;1 33;;
4 . V? ?Y'i 38:
4.1"
?:i?i 23?i
3 . 9 i; J?l;;i 2 li;
3 . 7 igf!
ia|
3.8;? i-l;l 49? 1300
3 . 7 *Y;i 5 li 1400
: .''' /' ':vI1 ^i'-
5.0? iiigb
'i' 1 ' 1 i'.' 1'."::'.':^ 1 - . '--.
1.6:;
1 . 5':
Cd? Co S" : .:Cr
ppm ppm ; ;PP
4 . 8 :.? * 1 44i; 970
5 . Ofi?*.:i
47''. '::Wb
4.2
4 . 0 ?!:-l 46?':
4.0
libo
.'i?1 4 7ii; SI:"
: ' lil 49;i isoo
11 56'i
li 5 1
:Vl 54:
:-'Yi 53;
4.6i lil 55 1400
5.0
:--Yl 52, 1300
4.4 . .: : *?:i? 53?: .'jSoo
3.3?
^Yi 3 5l(1^?
i Y i 25?;
:??5bO
"ieeo
; 100
; ioo
i ::'*il' io;i
i'iiso
?ixi'4 li; 2i(J
1.2:
1 . 4 i'*--5'! 7i::::llp
1.1 iYl 8 ; ?ii2b
1.0
;iiM0
. .. - ./..v.v.A -\
* Iri-'Y's 0.85 -,,* :;i 9? lio(3
* lii :xii5 1-1- i..*:i 9? ^130
( l??'i*?.;5: 0.97i;?
:x : i lo? iiiisb
* liiiiis 1.2" i :i'.:l 10'; :iii :7b
( 1 * 5 1.2.;
??150
x ?i 9;
I.C.A.P. PLASMA SCAN
1300
1300
1300
1400
15| 0'
ff'ei
i;il50.
Cu
ppro
37
47
48
36
54
47
50
46
44
Aqua-Regia Digestion
40 5,5
70 4.8
51 :4.9
61 3.0
58 :?.3'v4 :
32 i? 2'; 4
6 ;:3v3
20 3 .8
19 3.4
14 3.2
84
31
25
21:;
68
is;
5
11
4
4
3
3
11
28
4
Fe
:*i
4,-4
4.0
4.2
4.4
4.7
4,7
4.6
4.6
4.7
2.9
4.9
5 . i
4.4
i';l,r3
1.1
:i;l
1.1
.1.1
;-:?l-3 :
0.83
1.1
0.82
0.91
1-1
Mg
*
2.5
2 . 5
2.5
2.6
2.6
2.6
2.5
2.6
2.6
2.6
2.6 880
2.6 940
2 . 6 1000
2.4? 770
2 . 4 950
2 . 5 i. 620
2.7 840
2.6 900
1.9 610
1.9: 610
0 . 67 i
0.56
0.61
0.46
0.42
0.36
0.41
0.37
0.46
0.47
Mn
ppm
850
920
810
840
820
780
910
850
820
910
1 - 9 iii560
2.6 :;980
2.6 1000
2 . 3 810
0.78 300
280
240
240
200
170
160
200
,: 180
210
220
Mo i;Na
ppm i*
* 2*0,01
* 2*0:01
* 2*0.01
* 2*0.01
* 2*0.01
* 2*0,01
* 2*0.01
* 2*0.01
* 2*0.01
* 2*0.01
* 2*0.01
* 2*0.01
* 2*0,01
* 2*0.01
* 2*0^dl
* 2*0.01
* 2*0:01
* 2*0.01
* 2 0,02
* 2 0,03
* 2 0.03
* 2*0.01
* 2*0.01
* 2*0:01
* 2 0. 06
* 2 0,05
* 2 0,04
* 2 0.06
* 20? 04
* 2 0.04
* 2io.03
* 2 0,05
* 2 0.04
* 2-0.03
* 2 0.04
Ni
ppm
520
460;i
600
590
570:
630
640
610
670
670
430
460
480;
320
320.
370 i.i:46
450 ???:50
630 '-•62
78 2Oob
38 2000
44 2000
470i'-:.:;40b
490 :'?260
180 ;iip p
23
7
10
7
7
11
8 ,i|20
8:
8
e
1
p :
ppm
i.78
i 70
: ?84
;:.i (H
:82
: 86
:? 90
i- 78
:i;74.
'i:.84
i 70
:i;82
• '••"•f- -n
: OO
.
: ibbo
800
920
; ?910
iiiSiBO
iibbo
i??680
: iboo
:950
Pb
ppm
* 1
* i
* i
* i
* i
* i
* i
* i
* i
* i?
* 1 :
* 1
* 1*
* 1'
* lj :
* r Ts
: -:* "s
* 1;':
* 1
6
2'i
* li? :3x'-i5
* i?iiiyii's
* l"; ??i*:i:.5 :
* 1;? axis'
4iIP.
2 iliis
3;; ;:i*i:i5'
'i'l'S
3;:
2; -i 1 5
3iiiifi'
5i
3?
4?; ili.is
liiixV'5'
3" ?i*': 5
2
SIGNED :
Sb
ppm
* 5
* 5
* 5
< 5
* 5
* 5
* 5
*is
'li5
i'*- '5
i* 5
:; t?; 5
' i li 5
x 5
X 5
ilM
-?:-i''::':5
^ 5
Se i Sn
ppm ppm
14 *i;10
14 * 10
13 x 10
14 * 10
16 * 10
15 * 10
17 * 10
18 * 10
17 * 10
17 * 10
22 * 10
20 X 10
21;;* ilO
13;*? 10
10 -Yip
iii"*'??io
12 ; : * 10
4 X 1O
3 x 10
3.X 10
15 i * 10
16 YlO
9'ix-io
2"lii;ip
i * ?io
* li* ?10
* i x io
* 1 li'iO
* 1?:X 10
* i ;-?*?;io
* li x lo
* liAilO
* i :iiio
* 1 x 10
Sr
ppm
77
120
100
76
87
90
120
100
220
93
REPORT No.
Page No.
File No.
Date
88
100
81
91 :
Q A
C34
86
170
240
230
210
200
220
210
260
190
200
230
330
190
110
170
180
190
170
300
Ti
ppm
30
33
33
30
40
55
60
56
37
54
47
39
41
27
35
52
61
18
31
53
46
34
48
24
42
26
38
^47
29
24
20
43
31
24
22
V W
ppm ppm
47 * 10
47 * 10
52 * 10
47 * 10
61 * 10
75 * 10
74 * 10
86 * 10
67 * 10
67 * 10
95 * 10
83 ( 10
89 * 10
48 1 10
53 YlO
20 * 10
17 * 10
37 * 10
6 * 10
7 *10
6 * 10
42 * 10
42 * 10
11 * 10
7 * 10
4 * 10
5 * 10
6 * 10
6 * 10
5 * 10
6 * 10
5 * 10
7 * 10
4 * 10
4 * 10
M8310
2 of 3
NV18MA
NOV-19-1996
V
ppm
2
3
3
2
1
2
3
2
2
2
2
2
2
2
2
* 1
2
3
9
11
11
3
2
8
4
3
3
3
3
3
2
3
3
3
3
Zn
ppm
34
38
35
35
41
46
44
43
40
42
59
62
47
65
140
6
7
25
34
41
45
59
62
88
29
19
15
15
12
13
14
16
15
15
13
Zr
PPI"
9
7
2
5
11
7
6
10
7
9
10
11
10
6
3
4
5
5
2
* 1
* 1
6
7
5
2
4
3
* 1
2
2
3
l
2
2
5

CAMECO
ATTN: PETER CHUBB
PROJ: ENGLISH
6W-4574-R01
SAMPLE tt
ENG96D-204
ENG96D-205
ENG96D-206
ENG96D-207
ENG96D-208
ENQ96D-209
ENG96D-210
EN096D-211
EN096D-212
ENG96D-213
ENG96D-214
ENG96D-215
EN096D-216
ENG96D-217
ENG96D-218
ENG96D-219
ENG96D-220
ENG96D-221
INC.
'' ;Ag:y Al ' :'lM.}
. :ppm , * ppm
VVM 0.49 cV5 .
V'-f'vJ. 0.27 X 5 . c 10;
v'M 0.42. -^.3 . ( 10
til 0.36 ( 5 . t 10:
;,VM : 0.23 y/ o: 's" ' c 10
v?'xi.I O.l6yv.yc:; :3 'c
10.
VjgJ 0.25VVV?5 ' c 10;
'VViVi 0.36VX 5 . t lOV:
V,M:l 0.28 ;V:5 . [ 10
V'S::! 0.35;;. *";.s ':
10:;
: ID;
V'rxvi 0.22^^-5 -
vgri o.ssVVvys .
B v
PPm
Ba
ppm
c 10 : 34
.t'yy^l 0.25 ';*. 5 . ( 10V : 21
;VxV;i 0.23 xVS ' t 10:: 49
rVC;i 0.30V;VV5 . ( 10:: :: 22
T'x&i 0 .28 X5 '(
10 T 23
32
32
23
33
9
24
25
49
38
"31
: 10;:: : ..54
; '"'X;;* 0.20Vt;5 . : lOV' i 40
.VJXi;! 0.26 Vx; 5 ':
10 y 4 O
Be
ppm
< 1
( 1;
< 1:
( 1
< 1
* 1.' : X "5
( 1
( 1
< 1
( 1
< 1
< 1
< 1
< 1
* i;
< i
< i
< i
A .5 gin sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 min and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
TSL/96
Bi
PP!"
y*:: 5'
vt:5
VCs
:x;',.5
:'X "'5
< 5
*.;5
r -.{s
(5
r^:?5
V* . s
-x- 5
VVy-S'
:'*~:?
:x 5
X 5
X 5
Ca
* ::
1-1 ^ 1
1.4 < 1
1 - 5; x 1
l . 3 ;
1.3" X i
XI
1.5
1.2
1.2
0.98
0.65
1.1
1.3
1.5
1.5
:^:';i
1-5; : < "l
1.3-
1 . 3
1^4
TSL/ASSAY ".aboratories
1270 FEWSTER DRIVE, UNIT j MISSISSAUGA,ONTARIO L4W-1A4
PHONE #: (905)602-8236 FAX #: (905)206-0513
; Cd':
ppm
••'*. l
< i
\ . 1
^ 'l
ci
' x Vi
< i
( i
x.; 1
< 1
< 1
Co
ppm
6
12
10
11
9
9
9
9
12
9
11
9
9
9
10
8
9
9
I.C.A.P. PLASMA SCAN
Civppm
70
110
190
170
150
140
140
160
220
110
180
140
160
140
190
160
180
160
Aqua-Regia Digestion
Cu ;
ppm ,. *:.;;:
4? .43 210
19; ~yui o .55V :' 240
25; Oi93 0 .58V 260
6:
5;'
;::.:'i?2 0 .47 240
:: :' :.1.1 0 .56 240
5;: ,.';.i: :.i o
15
7
8
5
3; V,;i:;'3 o
12 ;.; : l':i : 0
4 :;
0.93 0
3; ;;l,P 0
4
:.;'Fe ::
;o.95 o
;;;:l;:l 0
v.M.-,^: ....:y.'..-
Mg :
* l -
5; :6i89 0 .49
4!i
0-92 0 .48
4 1.0 0 . 50
Mn
ppm
.62 260
1.2 0 .44 210
Ir 2 0 .46 240
:l-2 0 .38: 190
0,92. 0 25: .140
- 39; ;;2oo
.56 230
.60V 260
. 61';. 240
.60 270
240
230
250
V'Na'.:
Mo
PPm
? ii*:i " :
< 2 : :0.05
4 Mi03
< 2 V6v03
2 Vo.03
< 2Vo
:,04
< 2 :;0;03
< 2 :0.05
< 2 6.04
< 2 0.03
< 2 VP?03
;;"pvo3
< 2
< 2 ;:6;b4
< 2 :;oVo3
< 2 SP r 04
< 2VO.03
< 2 6,04
< 2 6.02
< 2 'P. 03
Ni
ppm
6 iooo
8 1000
8 910
9 1000
8 V570
8
7
6
6
7
6
6
6
.'"P
ppm
6 -910
11 i 930
7. ;iOOO
9 iioo
7 990
950
940
1000
iooo
900
930
940
990
Pb
ppm
4
6V
2
3
4
3
2
1
5
3
< 1
1
2
3
2
2
Sb
ppm
( 5
X 5
X 5
< 5
:

CAMECO bo^-j
ATTN: PETER CHUBB
PROJ: ENGLISH
6U-4575-RG1
SAMPLE
EN096D-222
ENG96D-223
EN096D-224
ENG96D-225
ENG96D-226
ENG96D-227
ENG96D-228
ENG96D-229
EN096D-230
EN096D-231
ENG96D-232
ENG96D-233
ENG96D-234
ENG96D-235
ENG96D-236
ENG96D-237
ENG96D-238
ENG96D-239
ENG96D-240
ENG96D-241
ENG96D-242
ENG96D-243
ENG96D-244
ENG96D-245
ENG96D-246
EN096D-247
EN096D-248
ENG96D-249
ENG96D-250
EN096D-251
ENG96D-252
EHG96D-253
ENG96D-254
ENG96D-255
ENG96D-256
INC.
Ag Al As
^ppm * ppm
X 1 0.21 X; 5
XI 0.39 X 5
;.Vii 0.19 Xv5
,V-i 0.23 ..X:;5
Vi 0.18 if ,5
X: l 0.23 X 5
:X 1 0.16 X 5
. X 1 0.18 X.--5
;;V:1 0.30 x 5
,\V;;M 0.20.;: X;, 5
; x ;i: 0.26, x 5
VX;:! 0.13 ;:s.x-;5
v/X//* 0.18 i 't :5
irVi'i O.lSvViS
':;Vi;i o.i7.:i:;xi;5
PS f i o.io xi 5
sV:i 0.23" V s
-S'X'il 0.35::-:.xv.5
-, X*l 0.28? X 5
: x;il o.i8.::ft.i;:";5
Sic;!- 0.2i;;v.xi.5
/IVI/l 0.17l|X.f5
SX'*1: 0.27lix!-5
J-Xfl 0.19|lV5
:i;V;::i o.2i.:i;V;;5
,:'ix:|l o.isi x 5
iiXil 0.24' ; .::X'. 5
X:-l 0.21 X 5
isVsl 0.28; ;x 5
sfStll o.25l|x;i8
S/Vii o.86i;vX-5
Ixll 0.97 -S :5
.Si;/ i -o.83fi|5io
BS-Sli o.27-;;i;Vi5
B ;: ;
ppm
< 10
< 1 0
( 10-:
< 10
< 10
( 10;
< 10
< 1 0
X 10 ?' 60
< 1 0 i :::i 52
< 10 i- 21
< io/ ;,--.. 24
X 10 iS4'8
x 10 ii-
-i 3 5
< 10, 3-3.4
X IO":
< 1 0
x 10
X 10
' 'i.34
( 10,
X IO"
< 10
x 10
x 10
x 10;: S2!
x 10
< 10
( 10
X 10
( 10:
x 10;
if5;3
( 10
x 10
x 10
Ea
ppm
47
: 38
i; 55
25
64
i 48
:v. 7i
i .77
if' 5 9
; 44
49
""'. '37
-' -'S*
:':: :. 35
t 3 9
i:ii,38
i 27
35
40
-,-.i8o
i-* *
iixiii
ill'6
Be : iABi -
ppm -,Ipm
< 1 X 5
t 1 ,..':V.'..5
X i;":ixi;.5
< l :-:- V;Vi5
x li " : i X 5
( i.?-^\ 5
x l*;i;:x"5
x 1 :;V 5
* i: ; .;ix. 5
x i-i-v.5
x i^ViS
t i/l/x 5
( liif/x.i-s
< i'::'; 'Vis
* rlP?
< l ii/V.'S
x V.JxTiS
( i':.'.. /X' .5
* i : :ix-'5
< ii.pi.,5
< l.ifx!.5
( i;,4;V*5
< i/'&Vls
x i;*xi'5
( i;i!f;:5
( 1 " V c-i5
< I X 5
< 1 :.X :5
( lSjV'.5'
y.-.'v:-:':-:":v'vX.-^
< li-SXlCB
< lLiV:5
* i:.S:;;5
A .5 gra sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 rain and diluted to 10 ml with DI H20
This method is partial for many oxide materials
TSL/96
Ca
*
1.4
1.2
1.6
1.5
1.7
1.7
1.5
1.5
1.7
1.7
1.5.
1.1
0.57
1.0
1.1
o.eili-
0.97
0.82
1.2
1.2
1.5
1 . 6
1 . 4
3 . 3::: 'x. i
4 - 0 ; /; ; ' ( 1
8.2 ^x'l
6 . 9.:
7.4
TSL/ASSAYE laboratories
1270 FEWSTER DRIVE, UNIT - ..ISSISSAUGA,ONTARIO L4W-1A4
PHONE #: (905)602-8236 FAX #: (905)206-0513
Cd
ppm
< 1
( 1
x 1
X 1
< 1
x'-l
4 i
x 1
X 1
x 1
X 1
< 1
( 1
.i- -x. 1
-;': 1
"i-X..:!
j;x'v' :l
< i
rx i
X l
;x ; -i
1.3
i . 4 ; . yc i
;i-V-';l
: -.:; : x-: i
.'-.x 'l
1.5; *x 1
1.4 V i
1.5 x 1
l . 6 ; -,x i
1.8. :;^'' :
;X l
co ;
ppm ;
9 150
11 : 180
9 .1.40:
11 180
9; 150
11
9
11
11
11.
11 : 150
13 240
16:: 450
12; 220
li,; 210
12
9
11 9
13
11 160
11: ':.Jl70
9 -140
- :; i-7Q
11
10 :.i50
12 190
9 ISO
12 190
9 150
13 ,x;18|
58
54
; -'730
50 ,;i?'60
51
55
I.C.A.P. PLASMA SCAN
Cr ::i
ppm
190
140
200
190
200
260
190
^240
;i4o
;240
iiii
;:.i?P
Aqua-Regia Digestion
Cu : ,rFe Mg :
pp ra; :;*r * ,"
4 0,94 0.60
6j;i,l 0.48,
3;::0.93 0.66:
a; li, 3 o.67 :: :
12 ;;i,o 0.68
21.41,1 0.67
10J: ;i. 0 0.63
21 ,!i;0 0.62
2li l.l 0.67
8; "l. 1 0.59;
6^4:1.4 0.63;
5i3l ;:'4 o.48-'.-i
3 -. - ......- Ol . 88 ". 0 . 25 ,:-'.,; 120
6 0. 97 0 . 40 : 170
5:OJ94 0.3S; 170
6:1.1 O.SO;: 220
6. "l, 3 0.50V; : 230
7;Siv4 0.663I?50
10:SlV:54 0.634V
- :-.' ' ' . -
5:B2;:2 0.65S'
8::: :fi:;: :2 0.66'-i;,250
7:,4i;3 0.62'i;'; ::;::23:0
15-11,3 0.66;;';.
i2 :.. ; i'-i:.-i o.63; :
8";ilM 0- 851
,",'.-v'-.?.s."V'X ':'.''
:.--.:v.-:-x:-v.-."-^;'- x v ;
Mn
ppra
230
190
230
250
250
260
240
260
250
250
250
210
7iift;;90 0.2 S;: 1 ,130
SjSlri 0.42 : :'- .190
4''I:Il;.:,2 0.46:: 200
240
i 230
10 s 1.2 0.63 :230
10vO:s?93 0.63;: ; : :-230
.260
:'V50
29-34:3 2 . 7k
920
37?;lfc| 2 . 6l:
58t;;;4i?7 2 . fr:: S930
54;- : i.;j;i :'9 2.6f .1900
Mo Ha
ppm , *
( 2 0.03
< 2 0>04
( 2 Q.Q3
6 0.03
' 2 - 0?
< 2 0.04
< 20; 02
< 2 0.03
< 2 0.05
< 2 di 03
6 0.04
< 2 0.03
< 2 0:04
< 2/0-03
* 2 P-?3
, ' , ,-'...y. ".'' '
< 20. 0 2
( 2 0,04
< 2 0,06
< 2 0.03
< 2 0.03
.. . . ...- . .- .-"i''
< 2 0,02
< 2/0.04
< 2 0.03
* 2 -"?
< 2 0 . 03
< 2 0.03
( 2 0.03
( 2/6 i O*
* zs^ii
t 2^'Jof
< 2X0.01
< 2X0 i 01
< 2x0.01
< 2X0.1.61-
Ni -"p;' :-,:
ppm ppm
8 1000
9 960
7'-;-i Opo
10 i 880
9 1000
9 980
7 1000
10 960
9 1000
i o;- 1060
1 0^:1000
is' .;:93o
18 ii 500
1 2 ^990
16'^; s 9 6
11 i910
12 -is lo;
9: 980
ii : ; J90
9'iso
8'S;9JO
8;S:9;90
8 :'.:;|l^b
10 looo
7-,.:--;:950
9 i :lpOO
7J1100
i-^is
81oSI.72
650 '' V.-.78
650-^48
ssoiiifSo
560::,i:70
Pb :Sb
ppm ppm
< 1 . "x- 5
( 1 :;X : 5
< l'X;5
< 1 X 5
< IX 5
< 1 x 5
1X5
1 X 5
1 * 5
2 X 5
< 1.-.-. :X'-.5
< l/'/lx 5
( 1 < S
< 1-../X-5
2:f;:x 5
( i:.,-;::f:s
2 X 5
l-'-'./X' 5
3 X 5
4;,;x.-5
3;'s-r'x is
5"-.'i.ix.."5
3iii;ix :i5
6:'-ixi.5
3 X 5
2 ( 5
2. < 5
2::;: ::i;x;:5
2';g;.xl5
' ^M-?5 -
< l?- :?ix'i5
f 1 '••': :'-' f ' K
\ i .v.-.; "\ ; J
< iiiS'i.5.;
< li.;iX;i5"
< liS'-Vs;
SIGNED
se
ppm
( 1 < 10
< 1 ; xi 10
< 1 < 10
< 1 x' 10
< 1 < 10
< 1
< 1
< 1
( 1
< 1
< 1
< 1
< 1
< 1:
< 1
< 1
< 1
< 1
< 1
< 1
1
< 1
< 1
< 1
< l
< 1
< 1
< 1
< 1
1
14
14
16
14
16
Sn
ppra
< 1 0
< 10
x 10
< 10
< 10
x io
^10
x 10
< 10
x 10
X 10
t 1 0
< 10
X 10
X 10
X 10
X 10
'X- 10
x 10
x;io
X 10
x 10
< :10
xi/10
i 10
x io
x 10
i x ;io
;V 10
REPORT No.
Page No.
File No.
Date
S r H. jTi"; v w
ppm: PP . ppm ppm
320 ;
8o;;i:
i:.29
160- ; ; 15
160: .17
280 :
340,,
650
470
220
270
170 :. ,: : 17
190 i i: 10
63 ;.'.?ii9
120i-
-i. i*
230
260:
220
190
420
520
; 17
;i 12:
.17.
9
10
i 21
13
•f is
i: .i /:9
:. .'17
22
17
13
510 i'iiilS
370 :^1S
230; ...S; 24
190 // : i:if6
110 ::;.i5
120 . 13
98 18
83 . :y.-i:14:
89; . - .: -".--2:6
380 ;::.ii"13
320 '.-.^
130
: :j.ii^
520
230iiliii
410 :'i :x.ii
4 < 10
6VX-10
3 X 10
4ix 10
3 X 10
4 X 10
3 < 10
5 < 1 0
4 ^ 10
3 X 10
4 X 10
4 X 10
10 X 10
5 X 10
5 "x 10
6" : X' 10
5" X 10
7 X 10
4 X 10
5 X 10
3 X 10
six 10
4;:x; 10
4.ixi 10
4 x 10
4 X 10
3 X 10
3 X 10
4ix .10
f'.T/.lP
18 X ilO
16 X 10
33 X 10
nix 10
( ix 10
M829D
l of 2
NV14MA
NOV-15-1996
y PPm
3
3
3
3
3
3
3
3
4
4
3
2
2
3
3
2
3
2
3
3
3
3,
4
4
4
4 42
4 23
4 i. 17
4 20
4 16
2
2
4:
4
4
Zn
ppm
20
16
16
12
14
13
10
17
20
21
16
16
12
12
-14
9
14
12
17
17
'..'16
i 15
19
22
27
28
30
"i ..;44
44
52
Zr
ppm
5
7
7
9
6
6
6
7
3
6
4
11
15
8
9
17
5
14
7
10
10
9
5,
5
7
6
5
5
3
5
7
6
5
4
6

CAMECO GO^J INC.
ATTN: PETER CHUBB
PROJ: ENGLISH
6W-4575-RG1
SAMPLE H
ENG96D-257
EN096D-258
ENG96D-259
ENG96D-260
ENG96D-261
ENG96D-262
ENG96D-263
ENG96D-264
ENG96D-265
ENG96D-266
EN096D-267
ENQ96D-268
;-Ag' Al ; Aa : B :0;B^; Be ; ;Bi
JPPB. * , : . " ppi" PP""0;PP'" . ppm :ppm
X 1 0.21 OxfS' ( 10-,0"0f7
;X 1 0.86: 0;:ip ( lo; ;ii
:X;i 0.93 . C.;5 ( 10/OOS4
;X;l 0.69 ::;.; : ,';5 ( l600fl7
•it'jt 0 .42 10 ( 10 , 35
--' '.-.•'•.•'-. .
ixfl 0.97 < S < 1 Of Of 19
^ :rl 1.9 0 ' s < i o.0-xf;i
XI 1.7, ;X ; 5(10: O.;0?'
3 0.85 20 ( 10 x-5
0; 3 1.4'. ; : 20 ( 10 f; Vi
1 :. ..' ' . .. V' .y 111 ; v 1 :.":'.
0-2 2.40
< i 0.66
::X. 5 ( 10000"3
K 5 ( 10.00(';;1
;. - . . i;::/.: 1 :." 1';;;;:
.... .' : v;:-,.; ; ,/'..
( i -x- 5
( 1 -X,: 5
( i'OxO.5
( 1 :0x ;: 5
( 1 ; ;X -. 5
( lOfftOs
( iOc:;5
( l': :.'";X ; ' : 5
( i-f'VOs
( I"; ; x05
* i:: '5xfs
* 1..;:i*:: 5
A .5 gn sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 min and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
T3L/96
TSL/ASSAYi aboratories
1270 FEWSTER DRIVE. UNIT 3 rtlSSISSAUGA, ONTARIO L4W-1A4
PHONE #:: (905)602-8236 FAX H : ( 905)206-0513
Ca ; :;;Cd : Co f :CrO
* , - .jppra ppm VOPPJ
,
!^,;.,v
.- . - - -: ,;
;;
5.2 (1 67 0250
4.7 0( 1 57 0530
4.7; OV;1. 6oi ?640
4.9 ! ?K:.I 54;'
;' ;:4;90
5.9 . ^fl 50:' :.3tO
5.3: ^'*fl 52; ; :057p
5.9 X?l 61 3 850
4.8 : ;x;i 41;; 550
4.6 V*-l 39";". y&o
4.9 X;:l 40;i 0073
;,;;y; ,-'
3.6
;l5p"
Xil 46:;: ;
8.8!
440
'x; :yi 67,0
,;;:\.;J ;y
I. C. A. P.
Cu '...
ppm
51 ;
52
46
43
73
44
44
75
98
72
140
58
PLASMA SCAN
Aqua-Regia Digestion
life
*
4.9
4,8
, :"4 :;8
4*7
4,8
:4,8
fS?2
5.7
8.5
7 - 5
6.8
' "4.; 4
Mg Mn
* PPm
2.7 910
2.6 870
2.6 890
2.6 820
2.6 990
2.6 930
2 . 5 940
2.3 1100
2.1 1200
2.2 950
2.3 740
2.5 1300
Mo ;. Na. 0 Ni .
PPm ;:0*00 ppm;
: P Pb Sb;
,ppm ppm :ppm
.'00 "O " -- . —"'•::''-'.'\
( 2*0. '01 700 0:92 ( i-;:.x05
( 2(QVOi 660 ; 380 ( r. :x::,5
( 2X0061 6 5 o; );.'i3b ( i:: 0x : :s
( 2'VOtOi 620; Of 68 ( lfO( 5.
( 2(oVpl 510
vlloo ( i;.;;0 .x 5
^"O'.O'.'O'.':''' -
( 2(6.01 610 -.:r;i86 ( li. ;(:5
( 2XPJ01 510: iv ; : 56 ( lOO(': '"5
( 2(OTpl 240; :;2io ( 1 (5
( 2(0.01 120 0,140 ( 1- (5
( 2(POpl 130; S:. C 76 ( I;v. ; (..:'5'
( 2(0;Pl 220/ '130 < l ; x Os
( 2X(3Voi 80o"' ; 030 ( 1 -' ; ( ; 5
vV'O r'.;:;;.: :
SIGNED :
Se
ppm
16
16
16
14
14
15
19
18
13
12
14
14
Sn
ppm
( 10
( 10
( 10
(10
( 10
( 10
(10
(10
("10
( 10
x .: 10
(;10
S r
PPin
250
190
130
200
180
170
230
130
200
230
190
470
REPORT NO.
Page No.
File No.
Date
Ti ;
ppm
( 'l
8
14
5
27
6
0.15
11
7
9
11
X 1
V
PPm
( 1
10
12
11
( 1
a
47
44
17
13
26
10
: M8296
: 2 of 2
: NV14MA
: NOV-15-1996
w ppm
( 10
( 10
( 10
( 10
( 10
( 10
( 10
( 10
( 10
( 10
( 10
( 10
Y
PPm
3
4
3
3
7
3
2
4
2
2
3
4
Zn
ppm
47
55
46
42
49
48
53
64
50
52
77
29
Zr
ppm
7
11
6
8
.10
6
10
9
12
11
9
7

CAMECO o—i
INC,
ATTN: P. CHUBB
PROJ: ENGLISH
6W-4691-RG1
SAMPLE #
ENG96D-269
ENG96D-270
ENG96D-271
ENG96D-272
EN096D-273
ENG96D-274
ENG96D-275
ENG96D-276
ENG96D-277
ENG96D-278
ENG96D-279
ENG96D-280
ENG96D-281
ENG96D-282
ENG96D-283
ENG96D-284
ENG96D-285
ENG96D-286
ENG96D-287
ENG96D-288
EN096D-289
ENG96D-290
ENG96D-291
ENG96D-292
ENG96D-293
ENG96D-294
ENG96D-295
ENG96D-296
ENG96D-297
ENG96D-298
ENG96D-299
ENG96D-300
ENG96D-301
ENG96D-302
ENG96D-303
"i*3 :
llfff"*
IP;" 1
iJr.i
555:2
5553
5l :X;fl
llxSl
mm IS;::r;l
liilrii
lliri
lil
mm
5*1
HIP
Isr'i
yslll
;5x5l
5ix5i
lilll
llll
3lx5tl
ii|ji
Ifflli
v'riVlv/i^ 1'.-;;.-"
Kitol
1111
rfS-l.
5;3!i
15x5i
llli*
SIP
liS'li
|:sX|,l;
Al l
* 5
i.i;; 5x,-5
2 . 4; 5K..L 5
l- 4! 1155
1.&; llx's
2.0 5x'l5
1 . 7 "k
0.37?
0.2ll
0.29?
0.71S:
1 . 7' l
2 - 5 1
2.0
0.93
1.5;
iiAsi
;. PP mi
flils
igts
llr'5
-r 5x1.5 5"
5lrl5"
51:1.5
i.iiMSs
i - 6; Ifcfs
Us
55ib
B Ea
ppm; i PP
< 10
< 10
< 10
< 10
< 10
* ip'; ;5i22
llrf'5
lilib < lolyi.22
55=5 < 10; 1135
flxl's * 10: 15:36
< lol:-;K
; 37
< ib;
< 1 0
< 10
< 1 0
< 10
5i l- 3f
i;*l:l
fix"; i
5'x"!
5ri
51 31
IS.: 24
f;5.11
' lisp
ibo
1.3; 5l:io < l O:
1.6;;
-ills' 55.12
< 10;; 55,12
1 . 55 5*55 < 10'5:16
1 . 4 1; 5x55 < lofli:
:-i
2 . 0; iris < 10; 5533.
< lof 51:34
< IP; 5522
1.5]: ;S1;5 < lo! s-528
1.6? Sri? ( 10; 153(5
0.73; lfr;5 : < 10;
11; 19
1.8?.
< lol
i'l'ie'p
1-65
< 1011;;.
4 5
i . si; 1x55 < iol; 552;*
0.76 liis < 10;; .l;il4.b
0.48; Hlf5 < ip
;:5 :5'2
x;
Be i-'.iBp ea ;5cdf;
ppm .ppm *
;5p;iW
< 1:5LX55' 5 75;c;il
< i'"';;^ll' 2 .85;x'5i
< illx-is 3 3:5;c"l"i
< ifiyif 2 .8;;;: c 1 -; 1
* 15lri5 3 - 6;'i;.^l: :l
1 - 6;
< 10 ;Sx5i < l5::W5* 3 . 4;5^ :i
1-Sf5:X5'5
< 10 ;5"5i < ifSrlS 4
o.8ov;
. mm
5x55 < 10 liri < 15:^5.5 io;:;;xSl
1 . 0; 5xl;5 < 1015
ri ( il,lC:5 9 - i"-il'll
2 . 4;;
* 101
|p llf 6 < 151x55 6 - 05'X^i
A .5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 rain and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
TSL/96
< 1-5x1*5 5 .5:1' x 5i
< 151X35 2 4l:;xl;;l
< 151x51 i . 8-15453;
< lV.;.:xf5; 2 . o:.5x;:;i
< l;f;;:|;l5. 2 4:iilM
< i;l5X;"5; 5 .7:;fx;'.l-
< i:.;;:X5,5 3 .9.;5r:i
< 1 5 X Is 4 :o5' :;ri
< l;:;;x:::S 4 .955x5i
< 151*1:5 2
o;siiP
< i i;r;.5 7 .5 :l:;;'x;-l
< 1:1^1:5 3 . 3:5:1x1;!
< IvVlifS 1 8'5;x'Ii
( ll;;:x55 7 . 951 ('li
< il5 :M| 4 . 75;;x;;;|
v;;:;;;;;;; :;;
< i;5'*i: 5 3 .4:1; tMC
< i' :: l'rl5 4 . 4|!x Ei
< i;ilSl 4 . 4552;i
< 15 :W;I 5 . 3i;l?f i
< l;5 :(;M 8 . 3;;;5x5i
< i5.;;x5'5 4 4;5^;l|
< l55t;l5' 4 . 3;;:5x53:
. sfixii;
< ilffiSs a
< i;;-i v;:5; 2 . iSax'ii;
< ll^;:? 1 .i5;;( li
TSL/ASSAY' f ".aboratories
1270 FEUSTER DRIVE, UN^i' . .USSISSAUGA,ONTARIO L4W-1A4
PHONE #: (905)602-8236 FAX tt: ( 905)206-0513
Co 5; ilfer l'
PPm: ;PP?
35;.:;
33:1
35i;;; 5184
42.5 ..Us
4 IS
351 il9i6
365:
54:5 ;;5bo
565Mb
42;;; ;68P
31;:':; 1260
155 :J4p;
155 i:io
14g
lisb
i?i;
36;-: 5-190
4 2 :: ; WSi
34:;;' :.1'69
27.5: :4;3o
19.5 ;2?Q
37;.:; 1420
3l5i 122P
22:5 flip
325 abb
4 OS
24:5'
SO;;;; liSb
35;5; flip
322; ip
49;5;36P
31;5
48'i
lib
44;5IM
17;; :lbb
13;"? :;i7b
I.C.A.P. PLASMA SCAN
l?io
; :5:9i
lliS
;;;i53 :
iM
ilb
fib
Hi
Aqua-Regia Digestion
Cu 5:: :.pel'
ppmi;;..i(5i
7351:359
lOOi; 5/4
73;;;56lB
951,57,6
110;:l5'. :7
96l;l55 :i:
90l;5:;::2
Iib5:i3'5i
29l;-2 :,9
285:3.9
31:;-:14:;3
6:;;52,.i
8;Sliil
si'lizlb
10552J6;
ll;;S4l;4
ai'Sja
89;; ::f657
32;;;;;2.;5
i8;:l;.;2'.5
51;5;4y2
17K.3;i;9 :
14:;;;3S : 3
49;5;353
58153.3
;-:-:-v.v.vXvx .. . -.-.v..
w..v^v.-:.:.v-.v.V ;:
32?l;ia
12051356
4851358
4i:S; ::p
3155353
72i|4.;b
41113;^
38g|PS
1553213
frllivS
Mg
*
2.0 iopo
2.0 : 680
i . 9: - 177P
1.9 :;i;7po
1.9 IOPO
2.0: ;i600
l.l'' 670
0.79; S470
O.B6; ;5450
1-3; IIP0'
2.0; 1600
1 - 7; ;i3bb
1.7 1200
2.1 780
1.9; ;530
2.0: 1200
1.9'j ll670
1.7; 5370
2. li i20P
2 . li
1 - 7;;
2 . o"
Mn
,,ppm
i . a: ;;laso
i . 9 : 1200
2. r ;;3lPO
2.2
".14'PP
1300
2 . 2
116'b
;;l54P
- esp
2.0; UBIQ
2.ol 5960
2.0l11300
2.0 ;;790
2.3; 5:920
2.2 ^I2b"b
1.5* 53150
0.61;
;5i9"o
MO ; :;iNa
ppml. l S
< 2^0.01
< 2X0 ; oi
< 2xO;Oi
< 2^0.bi
2 0,01
4^bvbi
< 2lbiPi
< 2*P"."p'i
< 2X0; O!
2 *0ibl:
< 2xp;bl
< 2 0.04
< 2:0.03
< 2 b. P 4
< 2;;0,b7
( 2 p. pi
< 2 !;bl01
* 2^0;pl
< 2*0.01
< 2:0,04
< 2 PVOl
4lb:;bl
< 2:; p. 03
< 2Xp:01
< 2*0; 01
< 2lblbi
< 2|pvbi
< 2xb;;;bi
< 2Vb:M
< 2xo's;bi
< 2xP;pi
< 2XP:;P1
< 2;i;'p5oi :
< 2;ip;jb6
< 2;; b; os
Ni
ppm
420 ;
66:
76
110
150l ::59'ab
22bl 1980
580; 5:82
730 ;1 :30
5910
440;
290; i860
36 ;iiob
2 li ;i2bb
227 1300
sol
440
85
63
200
100
P';;.;
PPH
200
250
100
i IIP
- '"140
.400
libb
.1100
'";35b
250
76
.540
490; 86
220 5450
160;: 12 3 0
600.: :.l:li6
360
Hi?
iSbbi
641;
100; Isbb
320;; ;1I6P
310l ;.ll3b
510:
ffSp
fflpp
600" 83;
;5i2b
560; llZib
82; ilseb
18: 1:550
Pb Ijlsi
ppml: pj
* J-ll*
< 15^'
4;'^:
< ii;, t:
< mix
< i5l;x;
< ill'r 5
< il'"^l ::5
,. j};;:.^'
' 1li^;
< li-lxl
< lilxl
6'SH:
;'5
;5
i!:i- 5r i:.s:
< l;.;::xl
< i. :l"-:l
< i";5.x':
{ il.lv
< i;;.;;x.
< ill*
3;;
?m
5
5
5
5
5
.;"S"
is 5
J
;5
5
5
5
5
S
< l;fSrl5
< iii;^.sfs
< i5;;x; 5
< l5;;x;, :5
< ifSl
fi
( i;;:;;;x;;: ;;5f
< lll'^: is
< if!';^. , rl
< Il5;*lil
5fli; ;5
'S
< iK'r
< llfx; II
( i;i:;X; :S;
( ii.;ii ;;s
< i:-lr-5
se
ppm
13..
18
12
12
16
8 ;x:ip
^ i ip
11 ;x iO
9 < 10
15 ^19
8
2
i
2
2
B X IP
12 ( 1 0
11 < 10
9 rip
8 y lo
8 f
^10
5 X: 10
3; '*' 10
13f X:; IP
12;
7
13
14
3
< 1
Sn l
PP m
.X;lb
^10
rio
< 10
^..Ip
rio
* ip
,X 10
x ip
< : lo
ixiio
3 ri 10
7: ;rllp
9.; :xl;ip
9 * 10
9 ^ilP
:X;:ip
rib
xf;io
x: lo
rio
REPORT No.
Page No.
File No.
Date
Sr :.
ppmi;
44b5 5 :12
no 1 fflfr
180 ;llp
160 ;l 5ib
130 122
2105
2 4 oil : : ::l"9
410 1 Wl: 1
440 :,12
310; 16
240
96
85 ? ;
11 oil
120;
220 .;:
69 ; '
62
280
110
Ti
ppm
lib
8
;.;;8
1;":7
10
: 22
22
40
30
;11
82
170 10
1405; .516'
91;l: 51 9
4 7 O:;;; lio
350:5
fi/2
180 18
2805 529
320.5 1: i?
320 ; f 11
410: :;2
' 18
180.
220:;; ;:22
5 IP;;;; :l:.l :5
110 B
48 ; 11
V
ppm
M83ly
l of 3
NV19HA
27'f x, 10
38 < 10
16 "\ 1 0
21 5 10
17 f l o
10; Ir lo
4; rio
12 Ir 10
29 < 10
47 x 10
10
4; t 1 0
3 -x ''vib
3 .x lib
4 ;-'r ib
9
76
71
25
45
20 ^;10
8 : xfi'io
6 t 10
37 X 1 10
37 cub
4.
12i
14
11
9
5:
38
321
7:
6
NOV-20-1996
w ; Y
ppra
rip
X 10
rio
< 10
X. IO
x 10
:^llO
Klib
;xiib
< ip
^10
K. ib
"rib
x lib
i; 10
X 10
ppm
4
3
2
3
3
5. l
6""
5 l
3
6
6
4
4
5
4
6
4
2
2
4
4
4
2
3
3 l
8;
l : 34
3'"'f
8 1; 1:1:45.
ffi 51'
5"
52
5 ; 33
7 .
2;
5.
3
2
Zn
PPm
37
71
48
45
51
41
37
20
12
45
43
18
14
18
28
41
82
69
10
53
38
43
38
29
47
-: 51
f-24
";45
32
19
Zr
ppm
8
B
10
5
13
16
13
4
2
. 8
9
4
4
4
3
4
6
2
4
7
4
15
12
5
6
2
5
9
12
6
3
6
9
16
11

CAMECO
ATTN: P. CHUBB
PROJ: ENGLISH
6W-4691-RG1
SAMPLE #
ENG96D-304
ENG96D-305
ENG96D-306
ENG96D-307
ENG96D-308
ENG96D-309
ENG96D-310
ENG96D-311
ENG96D-312
ENG96D-313
ENG96D-314
ENG96D-315
ENG96D-316
ENG96D-317
ENG96D-318
ENG96D-319
ENG96D-320
ENG96D-321
EN096D-322
ENG96D-323
ENG96D-324
ENG96D-325
ENG96D-326
ENG96D-327
ENG96D-328
ENG960-329
ENG96D-330
ENG96D-331
ENG96D-332
ENG96D-333
ENG96D-334
ENG96D-335
ENG96D-336
ENG96D-337
ENG96D-338
INC.
x?Agi
i-PPff
i-X- 1
?-'Vl
In*
;?:;?.?:;:2
??Jil
3?iil
?:i?33
?:?il2
l'*:?!
;'?;xil
i?*:?!
?ixfi:
iixil
sai
iSii
?:?;?|f
iMl
?ix.if
il
*.;';:X#?^;v.#K
Hill
iSPsl
ilffiS
1111
Hit
IMS
mm
lijli
Btail
IS?1
,.Y ,v. ;,,i,.^;
SiXrt
fSil
A1 riM i
* ??pp'm
0.51? X ?5
0.64 . ....4 ±5
0.62??X?5
o.77iiiis
1.8??? 20
1 - 6:;:::X? "5
0.95i?;x?5
2.1?'?'^ is
1.9?i^5
2 . 8?f x,?5
- ii v. . ;
1.9;ik5
1 - 4 ?? 0.5
0.18i?i?5
0.17?;?tis
0.26?i:x?i5
0.12??;^?5
0.13.iW'5
o.i4?;-ixi5
0.22??ft?5
1 . lillJs
i . 5lil?5
2. Sim
1 . 9.i;Kf5'
2.0ili;5
2.l|gi;f
2. 4lll?t
3 . o';ip;b
2 . 8;i??!ib
1.5iaiS5
-,v.-,v^v.v;:.^
Z . V.^.MfeS
^^.-Xv^o-vXvv
KvWj*"-:^^: 1
2.6|lio
1.6?2l?5
1 . 9?,?:M?5
1 . 6i??l2b
1 . 4 ? :;i "?S
B ;.?Bai
ppm;;;pfim
< 10 i? 38
< 10? '. ,;.'28.
< ib'i'izz
< nmo®
< 10. t2
( 10? il3
< lo-;??!!
( 10?-?"i8
< ioi 2ib
< 10 : 170
< 10: : ?;:9Q
( ibiiis'o
< louis
< 10??i?15 :
< I0|f?;34
< 10?i;;;16
< ib??i '"12
< I0ffi?i,9"
< io????ii
< ib|li?4
t iQfSfW;
< io?iSb
< lOiiSb
< loJfpS
< io?flip?
< 1 0?|?230
< loiilsp
< 10?|?29b
< ibillb
< lotsifia
< ibi??4i
< 10???230
< io?i?24p
< 10i?2 :6P
< 10;;il4b
A .5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 Bin and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
TSL/96
Be :?Bi; : ea :icd?
PPm:??P|? * ?;,::^pm;
( i:??i;5 0.86? -x. 1
< 1;,; ::X?'5' l.P'i-X";!
( l??x"? :5 5.3i?X :??l
( i :;??:-c?;s 4 . 6i.;?c?l
< i??,;xi;5 4.5?,;.'x?i
< l?-.f ::?5v 3
<
(
<
l?i.G5 8 .8';;;:x; ::l
i?-?c?5 5 .0;;:?.X.?l:
l''" x; 5 8 .5?ix?l
( 1??;C;5 3 .8??x?i
: '
:
< l':??::xi5 4 5.;?.;Xi ;i
< l??;xi ::5 4 2i :x.;i
<
(
<
l'?--;;X!i5 1 .7?;:;x.?l
l?:?-(i:5 2 . 2i.;"xil
1??;;X?: :5 1 .lS?'..:'?l:
.3?:',:i'"l:
( l;i:Xi?S l,
( li:Yi?5 1, .4i.Ki:l
( i;:i.:xiS 1. . 2?;;;X?1
< iSEs i-.6?;x?l
< I?:??*' 5.
0I?S-
< liiis s. , 2??ipl
( lillis 3, . 2?S?xIl
< I?;|*i5" 3. . 9?]i??I
< liSES 4. 2ii*;|
< l^??||f 3. ' 41?;*??!
< li'llis 3. .7??*'?!
< ISPS 3, .9?;iYil
< 1? :M?.5 3. .9i;':.t;'?l
( li;Sfi :5 3, 3???Ml
.OgijH
( liisi 4.
. 9? ix '?i :
. 6iil?i
i
<
(
iSafSS" 3.
^.-fUl 3 .6?:;?^'"!
(
<
l:i'i;:S 3. 2???*il
ii;p:5 4. . 2'i:?x';;l
< li?O 4, .2?ix?l
TSL/ASSAY laboratories
1270 FEWSTER DRIVE. UNIT J MISSISSAUGA.ONTARIO L4U-1A4
PHONE tt: ( 905)602-8236 FAX #: (905)206-0513
Co ?:..'Cr?;
ppm :;ppm
15 :; ;250
19??,25b
42::::Tl8b
32i;..22p
37i?: :l3"P
32:il20
42;??570
42 i"l30
56;?;940
39?;?39P
53:1100
5i?i;6sb
15 ???2'10
18;??12P
13i :,;,i8p
11???17P
12:?' 18P
14 :;:? :2PP
13.:?i;18b
52;?;;:7"2b
j?i;S*l
33:|?660
4l|fMb
3l|lbpjp
34|l|b b
35:?;?4bb
34??l2b
38;B?|bb
38i:?:6lb
27???53P?
36|p7P
40;i40P
34 :- ! ?5bb
3"SlS
34?:?4'?p
32??-?46P
I.C.A.P. PLASMA SCAN
Aqua-Regia Digestion
Cu ,.'?Fe ' -'
ppm ;J{ a
9 1 . 8
11?:? :2,2
34;: :?-4'.-2'
19ii3i3
46;;'4;3
55i:4?2
63?;3;7?
32??:4::9
72i :?4 :?'l
37 4.4
59i;?4:";4:
56.-*'4'i3
13??2,:3
13?i;2;:i:?
8Sli7
9 ::.':?:'l.8
8? 2,0
9?i2;b
20; 2.0
48???4?i'2
38-?13?:0
87?l4l|
47i?|354
52?|3i;3
78|?;4ib
48?i3|9
36'?i4'ib
4li?'3?B
84i?2S5
130'?|3||
16:i :3;8
78-i?3?6
98 ??3V8
73-;i3?e:
64?;?3?6
"g v,
* i
0 . 60
0.84
Mn;
?PP
170
;;220
2 . 1 ? ^820
1-9?; ?61b
2. P; ?:68P
2 . 0? 670
2 . 1" 1300
2 . i?; iB50
2 . 2~ lobP
2 . 2? 560
2 . 3 ?; :?790
2 . 3? ?770
i . if ?.29P
1.3- ?,3'5P
0.55? i 170
;?2ip
0.64
o.7oi ?23b
0.65'? iaio
O.B9i 290
2 . 3 f
1IM
2.1?: i93b
2.2l ifi
2. lii83b
i'8'3"b
2.2;?
2. lii||b?p
?:p3p
2 . 2?:
2 . 3?; ;?74"0
2 . 3'i ?85'b
2. li l :?Ib
2.3?;
|l4b
2.2?: i :87.b
2. IP ies'o
2.1? io'SO
;-:;74'0
2 . li
2 . o?; i-7io
Mo ? ?Nai:
Ppm v*i
< 2 0.07
< 2 :0,11
< 2?P.P1
< 2^P?'b:t
{ 2ib?01
< 2:0? 02
< 2VO,bl
< 2?:p;:oi
< 27o?'0l
< 2:'b.p2
< 2^o;oi
< 2x0,01
8?0;09
efibi'bs
( 2?b-07
4 0.08
6:b?i2
< 2 P"b9
< 2?o;o7
< 2XP?01
< 2xp?i';bi
< 2;?b?fp?i
( 2xb??bl
< 2Vb?il
< 2?;p?, :M
< 2ib|p3?
< 2iP;ipl
< 2^0?bl
( 2;jt(feii
< 2 :|p??pl
( 2W,;P1
< 2??QibS
( 2|o,:b?2
< 2?:blb3
< 2ib;"p3
Ni ? .IP;?:: Pb i?Sb.;
ppm: :;,ppm ppn :?fipm
24 ? 520 ( 1; ^5
42; i 5 10 ( l "ix-;5
370: iTjo ( i;.; :3;?5
200;; S'57.0 < liix:: ': :'"5
24 Q;;
i:74b < i?i^.?s;
160; lioo < i??;xis
630; 5130 3??:x?5?
280, i;:3.2b < l?;;:?V- ; 5
790 ?;::98' < l :?' :'i'.?5'
300? 1200 < 1 :X?5
?'i?'-i
740? ;?i20
580? ;i430
<
<
iiii?
i-iJxl'a
1--XV5
52? ??140 2;:?X?;5
46S{ ;i'12b
14: ??570 <
4?ix;;5
l:--?K:;i5
13? - " 450
is; ?:;;"8'6
l??:x-:'s
2"?:' :X'?5
22 ??390
4 2? ??390
3??;X:?5
3' ?X?^5
650;; li?84 < I';??* is
li?? < liifs:
380?
210? 159P <
360? :?:;::96 < liixiS
320? ?|?94 < ii?;xlB
130? ;|lpb < i5,f|;;5:
?2pb < i|i;(ls:
:
170?
260; :i?soo < r?.?l|s
300? :'2'20b <
3 OP? ll?b <
200J.
l';i :x?;;5'
lills
pibp < il?l5
lib < iiii
430;
150: ?1000 < l^HiS
140? Slop < iliEs
150? ;i|pb < liiSs;
120"
-lobo < i??;'x?5
SIGNED :
Se
ppm
1 < 10
2 < 10
10 X?1P
6 X
6 '*
10
10
B
13
11
14
16
16
14
3.
4
1; X?10
2
2
2 :
2
13
14? ;X?lb
18? Si-IP
16 ; ^?10
16? ??.?ib
18 ;iip
16 x ip
19? x 10
17? x 10
14? ::*.:10
19? ^:?10
18?
19
18
19
18
Sn
ppm
: *. 10
X 10
X? 10
< 10
i 10
i 10
< 1 0
',i,;10
••*. 1 0
X 10
x 10
S 10
< 1 0
1: ip
^ ib
X 10
;x ;io
^ ' .io
x 10
Sr
ppm
44
52
250
290
320
240
540
270
250
130
REPORT No.
Page No.
File No.
Date
180 ;
190
iioi
140
57?
76?
78
75
83
230;-
190?
110?
130?; i:36
17oi 1*36
120 ?32P
190
180
170
IIP?
ri ?
ppm.
9
' 11
i",?
?' :'7
11
i b
- i?
16
19
67
30
22
;.ilb
' i?7
10
7
12
44
.11
i IP
'?3b
: 7b
490
570
440
.i'^
200;; .; :47b
140. 210
150 850
150;. ;360
190: 480
230 820
V ? W
ppm . ppm
6 (
7ic
< 1?'X
3?x"
2 :?4
4 <
28?X
6?X
44 X
91 X
50 <
21?X
6"^
2?X.
6? X
M8319
2 of 3
NV19MA
3 < 10
4 X 10
5?V 10
7 < 10
22 C 10
52?':; :10
93?{': 10
63?;X'-.'"10
59?X .10
10
i2o?x:
89i|;
siixi
120?X?
NOV-20-1996
10
10
10
10
10
10
?lb
.10
10
10
10
10
.10
10
10
110?X 10
120 s x 10
110 X lo
48?;.XS?1P
ip
-10
10
110?; 'f. IP
120 -X 10
110 :"X. 10
Y
ppm
2
2
5
5
5
5?
5:
4 :
3
5
2
4
2"
2
2
2
2
2
2
3
2?. 17
;?" : 53
4:
2 Vii?6
3 i':16
5 ?46
8^
10
10
2
10
Zn
PP"
16
20
41
37
:..52
55
??'43
?;66
43
70
38
: 49
:." '21
29
14
29
19
.16
14
i 53
56
' 65
.....44
i? 15
:?:.45:
3 47
6 i 4?
6; ;?:46
7. 45
1 . 59
Zr
ppm
13
14
11
16
14
12
9
15
6
1 12
8
10
15"
14
13
15
15.
15
18
7;
6 : -
9-
8
6
11
8
12
9
6
10
8
14
12
12
14

CAMECO oO ^iJ INC.
ATTN: P. CHUBB
PROJ: ENGLISH
6W-4691-RG1
SflMPLE #
EN096D-339
ENG96D-340
ENG96D-341
ENG96D-342
ENG96D-343
ENG96D-344
ENG96D-345
ENG96D-346
ENG96D-347
ENG96D-348
ENG96D-349
VvA{j , Al
!!!:".M; I: i.4.,:
~.\;Yv;i 1.2!;
;v.::pv5 < 10 i": IW
-i.; :- :J''..V :- i i •y'-'--
~?"''i..4 :'? 1 1 . 6
?;?S 2.2!
; -!*pi 2.7V
: ::Bl 1 . 5
''.'Y;l 1.6"'.'
vY-1 l - ft
As : B
ppra ppm
jvY'5 < 10
. -...' - .'..
vlv'S < lo:
v5a'5 < lo:
;|* : (S < 10
;V 5 ( 10
15 K 10
X 5 ( 10
•••Ba:j
;i;'lio'
Sil
:K250!
68
190
I?SP
320
f'S'! , -* :
,,^.;.\A^.3, 1 . D-./';;'*.,S
t 1 ns! !v;idrt
A 5 gm sample i. digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 min and diluted to 10 ml with DI H2o
This method is partial for many oxide materials
TSL/96
TSL/ASSAV laboratories
.
1270 FEWSTER DRIVE. UNIT o rtlSSISSAUGA. ONTARIO L4W-1A4
PHONE #: (905)602-8236 FAX #: (905)206-0513
I. C. R. P. PLASMA SCAN
Aqua-Regla Digestion
REPORT No.
Page No.
File No.
Date
M8319
3 of 3
NV19MA
NOV-20-1996
Be t!B;i.,: ca llcdl. Co Cu vpe Mg :. Mn Mo . Na :
ppm :ppm * !i;ppin
.... , ,, ,.,.' ppm"li
Ni C;V,P'V: Pb l Sb Se
ppm ( ! *
V Sn Sr : Ti V
ppm ppm SK", 1'
W Y Zn
ppm".".. pptn ppm Ppra ppm ppm ppm
::: : . ' : V V : i:
ppm ppm
" ,' : .V : -'
ppm ppm ppm
fVVv :V
.01':'. X 11 33 : Sob 71 V3.9 2.0 7.10
< i;v*;V: 5 4
< 2 0.04
"•'•.x'"' 5
. 0"" \ ^ ' : 1
130"llob
30
19
-- ' J ':'' :'' a 1-'
75vi3.,7
< 10 320
2.0
930 120 < 10
< 2!!0,p*4
6 66
< 1SS&5 4
120:1000
1
< 1
SVXS'I: 3 li
18
7ivl!lj'v.:7 2 . 0V
470 840 120 * 10 6
< 2:0.05
< iv&as 3 .Svivxiil 30^
70!v!!:'3v;6 "'680
110,1100
58
18, 490V
2 . 0
730 120
* "Si 4
33; 62v"'3'.7
isoKiiob
Y.i 10 7 57
< lv 17.
: ;:":: ' : i111': /' '••:: lip
x 10 350
2 . 1 ;. 710 * 2!!,PM
530 110
7
200|i6pO
58
V'VVi.::.?.:
..v ' •••-.'
.SI 16 :x 10 240 280 100
< l :'!5!x!} 5 5
•Y. 10 8
^VVV'V
53
40 57*3!:!?'
2 . 2 850 < 2*0.01
< li < 5 4 .2 < 1
4 60 530 < 1
45 1400
^ 5 14 (. 1 0
55 4.2 2.3
390
820
79 68 X 10
< i.;:x,:5 4
< 2

CAMECO ^OLD INC.
ATTN: P . CHUBB
PROJ: ENGLISH
6W-4692-RG1
SAMPLE tt
ENG96D-350
ENG96D-351
ENG96D-352
ENG96D-353
ENG96D-354
ENG96D-355
EN096D-356
EN096D-357
ENG96D-358
ENG96D-359
ENG96D-360
ENG96D-361
EN096D-362
EN096D-363
ENG960-364
ENG96D-365
ENG96D-366
ENG96D-367
ENG96D-368
ENG96D-369
ENG96D-370
ENG96D-371
ENG96D-372
ENG96D-373
ENG96D-374
ENG96D-375
ENG96D-376
ENG96D-377
ENG96D-378
ENG96D-379
ENG96D-380
ENG96D-3B1
ENG96D-382
ENG96D-383
ENG96D-384
;;lAg,; Al ,l,:A:sl
!;;:pj?m * 1,/pjpm
slXl.l 0.54ll^:-5
fei o-8il;ii5
i/XMl 0.49:;!!!5
issii; o.2ol :lti5
ill Mill
"lilf i . iiOlls
mm 2 .111x15
llftil 2 . 3.111s:
ISii 2.4!lx'ls
!ffif?i 2.7lllib
ffiii 2.811*5
sf Hi 2 . eS'iVss
lil 2. eiiis
ESxSl 2.1,l;;lib"
SfiJI i . 4jll?b
HI 0.9l|l|l
i'rfffif 0.77.::lx35
pjjiftflt 1 . 2l;xl;5
slrti 1 o.68;;;.:,:iib
Will 0.21;':Ml5
":--':::-:;;:-;:;::.s •./w/-:.::-.^-:-'
Sy::-'?23ziZ '••:^W'j.:^i
lilt o.islils
.v.^.^v.v/j.v.-.v.v.v :;AV.: .-. - ..-V..;..,.;....
lift* 0.14fcS*ii5
liipO o.06;a;:x.:m
IS*! 0.2lisxi5'
III 0- 141S
o. 27l'x;I
0.22l:;llS.
Exit 0. 22!::x!'5
o.2psii :
|g|| 0.23|H1S
l-:-::". ^.vXv.^.-:: Ivli'.vlf/.^.v.'v.
ffi;;*|;t o.i slips;
IfSM 0.14f!il5
llxfjj 0.1411XW
glfll 0.26ipl5
ilVll o.25:!;ip
B :;;,f Ba;:
ppm ; ppm
( lb;l :l38
( 10,;;:l-6p
( 10!l-!3B
( 10!:1'12
( 10l!:32
( loliiSo
( lO—iiO
( 10!;2iO
( 101,190
( 10:1/210
( 10;:ll49
( lO'lllSP
( lOjfipO
( l o'Sji'go
( lofffbp
( 10M900
( ibll776'
( lPJS/79
( I0l;l52
( lojsiiz
( ioi!!3~6'
( loStl
( lo:Jif37
( ibfSif
( logic's
( lolllsS
( lblll.29
( 10;;l,;-23
( 10!!l;22
( lo:ll;;18
( 10111:22:
( iolil29
( 10i;l:;1.2f
( 1 0/513 3
( i oil: 130
Be '-'iBi!
ppm : ppm
< i ;l:S'l5
( l:.llC:5
( l;:l(!5
( llW;5 ;
* 1;!'1!5
( I'/JVlS
( iLlVls
( i,':l :xl'5
( il!x";-5
( l" 15: 5
( ll'St'5
( i:l:x!5
( l;SI?!'5
( i:llx:.5
( ll;xl5
( l ;'l'xl"5
( l,l,::cls
( l-':Xr5
( 1- 111.5'
( 1-1^/5
( 1/iai's
( lit ilj
( I'SfcS
( ill/xls
< 1;S;.*1.5
( H;i;:*fej
< 1:11^15;
( illX;';?:
( i:i;;X:;:S
( i-lv-lis
( i:ll(:l5
( I'llx-?
( ll:":( ..'5
( i::;;:(;:5;
( i:' :;:X;;5
A .5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 min and diluted to 10 ml with DI H2O
Thia method is partial for many oxide materials
TSL/96
Ca l;cdl
*
.rlppni
5;: :X.'::'l
4.
7. 6:::;xll
5. .6;;K;"1
2. . 5:l;x li
4. .O.'l:f: : l
.2!; : W'i
7. . 6:;;X.;'i
4.
2. •4'1-X;'1
5. • 4,l''x:ii
4. • oi".:*''!-
5;' ;:x'-;;i
4.
4. 4l':: ^li
5. i;-;X';i
5. 6:-; Vi
5. ll;^.:!
5. 5";;'^!
,5. 6';;l'(-li
t. 5: ; :'(:;1
2":l'Vli
3.
4.
5.1;: f||
6::l,x;'lL
4.
3. 0-1 :*;i:'l
1. . 4l-;:x;;i
5. .9:;::(;:1
2. ,7;:.:;Xl:l
4. .i;!'X.::i
4. . 2:i;X:;l
3. ,5'lx5ii
2. .s'llxlf
1.
, 8; ::l;;cll
, il:x';;;l
2.
1. . 91;X:::;1
3. • i;;;.^;:i
5. .9l;:'V;'i
3. .9:l'(;i
TSL/ASSAY r laboratories
1270 FEWSTER DRIVE. UNJ.T J MISSISSAUGA.ONTARIO L4W-1A4
PHONE #: (905)602-8236 FAX tt: (905)206-0513
co ::
ppm! .ppm
28;
19; !:19P
191lizb
I7 : i: .;:150
331
22J
25^
3 li:'1;94
33: ;l37P
38; :?;4'iO
38;:
46:
4 Si
36^
371
341•W320
37': ;:370
45*;
46p:::470
581
221KBjJO
161flip
14;; va|p
27: /Ifpp
16 !;|lP
iii?.?'
17;:
20l :p82
17l;libp
131
ill?
iii
iollibTp
•.••.•.•..••.•.••••.••y-."
12! isigo
15! ::;Sb'b '.ll'ee
22:
19! •*fiB|
I.C.A.P. PLASMA SCAN
I'C r -:
liop
11;?*
lisp
;liib
3S3P
i loo
.'woo
;:1S7P
; J5ip
sift
Si?b
Aqua-Regia Digestion
Cu Fe
ppm;.* !
5 3. ;;.3l 6
4B;;1.2;,9.
32 V!::2.8
25;.:!2:.3
39 :-l:4l ::2
94!|3!b
2 5-13! 4
9lli.3V4
110l:4 ; ; : 5
110/1J4.5
5:1 4, .3
44ll4.'6
2 3114; 4
94;!;4,b
5411:3^9
5o;l;:l!7:
77,:r'4 t ;0
221/4,3
32;'?'4,.2
17l!:4v,4,
8 2 1:13:0
isSlila
2 3.1/133;
4911:315
68l;;;2l :4;
47;:!is3:
44::!l2l6
28,!l2;V6
ll^Mit
6;!;fiiv5
6':'ife9
i7lii:"8
28,11215
48;:;l3'.i6
37ll3:;b
Mg ~
*
2 . 0
2.0
1 . 9
2.1"
2-1,;
!Mn- :; .
ppm
1 . 9 , 620
2 . P 880
1 . 9 :, ,:740
1 - P^1340
1 . 9 ; 570
1:870
600
480
780
.710
: 83P
2 . 2,
2 . 3 .870
2 - 3; ;iboo
2.2! : BOO
2 . 1! :;75P
2.2; : y710
2 . 2 ; 79P
2.3 !83P
2 . 3 ; 'i :640
2 . 3." '1860
1 . 9 i1560
1 - 2;; 1:4 Pb'
0 . 65! 1:290
2.1: 17.50
1.5!
;!3?p
1 . 5; 1:460
1 . 7; :;:5ob
1 . 6; E*20
0 . 84; ;l3"io
0 . 7 o: !;:270
!;3lb:
0.78
0 . 80; !;360
1 - 5; :';S8p
1 . 9! ;iioo
1 . 6; :l70b
Mo Ilka!
PP mll*l!
( 2 0!P3
( 2;,p:i-p2
2;PlPi
( 2^0;p5
( 2,;p,.b2
( 2(0.01
( 2;(otpi
( 2, 0,02
< 2/^O.Oi
( 2 0,01
( 2xb;bi
( 2(p;bi
( 2X0 1 01
( 2(6;bl
( 2xp;, :bi
( 2(bi01
( 2xb::oi
( 2xbl :bl
( 2(P!01
( 2xp|bi
( 2:(b'bi
( 2ipirb5'
6;plb4
( 2'(0501
< 2i:b!'pl
( 2:!b:|p2 :
( 2,!bvpi
( 2! :blb2
< 2lplp2
( 2:1103
( zloliz"
2!p|ps
< 2lp|;p2
6.*6|(St
( 2;b!b2
Ni IIP!:ppm
ppm
100, 1400
iiolzibo
70!2000
18 1600
78;i7bo
100!2boO
79: 1600
60/1500
110:2200
isoi'eoo
330;! 910
570!:260
610;; 110
300:1200
270:1100
210 1600
330; 1400
520 ; 170
580'1 194
610l;: 76
eslispp
28V29QO
2ll;!570
12011800
25:;54;PP
3211800
54;;i8bb
40;;Mpb
12:1000
12;:3Mpb
ibiwpp
1511700
32::i::;970
66:1400
28 1700
Pb :::Sb:
ppm ppm
( 1 : : :: (:5
6'"-' X 5
li ,: ;"(!5
17; X 5
2:;.'X;15 :
( ii.yis
( 1 ( 5
( 1 ( 5
( 1 (5
( 1 ;x;5
( 1 (;5
( 1 (5
( 1 (5
( i , (Os
( i;.:!x!'5'
< l/ (;: : 5
( 1 ('5
( 1 (5
( l':":(:;:5
8l,;:(:5
2:;;:(l5
6:'l.xlS'
illxls
6l'l(':::5
i;-;;x';5
3:1 ;X!:5
5';--: x is
3!! :(!5.
9l.-;p"5
6? :1*!5
61 :1(1'5
2l:"(;:5
2.;Xl5
( 1 IX .5
Se ;
ppm
8 '( 10
8 X 10
6 (10
2 (10
5 (10
9
5
4
17
10
10
15
17.
14
13
14
14
13
12
12
6 X 10
3! dip
2 ^llp
8 ::X1 10
3 s;.(:;10
3
3
3
1
1
; Sn
: ppm
x 10
( 10
( ..io
(10
X;10
( 10
( 10
( 10
.Cio
X 10
(10
( 10
(10
( 10
(10
X .10
x 10
(IP
•X'1'10
(;;lp
1 x!,10
l: (;lb
3. (10
7;. (^ 10
3 ( 10
S r
ppm:
REPORT No.
Page No.
File No.
Date
510
290
110
260,
170
210
290
320
670
67o;;
630
670
340
360/,
420;
' :'- ' 1 -Tt 660 **
4 IP!, :119"
180 1,1
: ; :8
630-1 lilJ
67 O:/ 1;14
350:; '-;!|4
,,;,-., 9:
400 1
isol
2701
230
li:
PP
-•..34
360^
.'.' :'4.1
560:
410 1 : 18
130 17
250 18
124
, : -.25
; 32
81
47
;30
33
36
27
30
16
10
15
,, 6
;(.:i
600; , 1 24
680. 1:16
5 sol; ' :-";16
660! :::- ;45
190 1'1,19
•**i
12
13
V
ppm
9
3
10
56
38
8
3
13
7
( 1
l of 3
NV19MA
2
3: -X'llO
4
( 1;
3
2 (!10
( 1 ;X 10
:( '-'ip
2
3 ;(!10
4
'I'fyiO
3 (;;1P
4. xlio
2 ;( 10
4: X 10
2 ( 10
NOV-20-1996
W
ppm
17
li'
X 10
( 10
4 X 10
4 :
(10
3
x 10
X 10
< 10
( 10
X 10
..^ 10
34 ( 10
62 ( 10
66 (10
32 ( 10
29, x 10
( 10
( 10
( 10
( 10
(10
;x 10
:( 10
X 10
X; IP
Y
ppm
12
7
5
10
7
5
3
4
8
6'
a
7
3
1
2
8
6
2.
10 : :::;57.
6"
:1;3|
9
8
6"
!;'!2.4: '
4.,
"!1'26
4 :!
4.
3;
4;'.
Zn
PPm:
7 :56
10: ;:.:42
9 ;, 40
5
7': :
123
:'::;::81
-1' 51
69
72
188
,:90
91
59
57
60
! 47
1 43
: 35
1 34
1147
88
1:45
'.136
:: i Q
:36
l41
:1;'33 '
- •"•••-"'•j tt
.•'•'••'"'"T,
- 1';27
:: : 26
8 31
6/ -:,.32
Zr
ppm
5 :
4"
3
4
3
( 1
4
2
6
. 7;
13
11
10
7
6
5
6
6
7
6
4
3
11
4
4.
2
2
2
3' : :
2
3
13
11
7
4

CAMECO oO ^iJ I NC.
ATTN: P. CHUBB
PROJ: ENGLISH
6W-4692-RG1
SAMPLE #
ENG96D-385
ENG96D-386
EM096D-387
ENG96D-388
ENG96D-389
ENG96D-390
EN096D-391
ENG96D-392
ENG96D-393
ENG96D-394
ENG96D-395
ENG96D-396
ENQ96D-397
ENG96D-398
ENG96D-399
ENG96D-400
ENG96D-4O1
EN096D-402
ENG96D-403
ENG96D-4O4
ENG96D-405
ENG96D-406
ENG96D-407
ENG96D-408
ENG96D-409
ENG96D-410
ENG96D-411
ENO96D-412
ENG96D-413
ENG96D-414
ENG96D-415
ENG96D-416
EN096D-417
ENG96D-418
ENG96D-419
2,;.*3- 5 Al l:;;;:AS;
::
1 . ;,;ppm * B•app'n.
2 '22:12 f
22(2i 0.38";
;,;-x2l 0.22 ; ;;:2;S
fiSlt P. 14? 2;.(25
SE11I 0.82; 2:;:(25
1113; P. 2 8; •2^'-:?
•,-v.. : .V.:V;O::::-.Y/ :"
lil 2-^
ill 2.3;
ISO: i.6 : .;
feeai 1-82
2'2"5
B 2
ppm
;-Ba;;
ppi?
( 10: .2,44
( 10;: :2;35;
•;;.i .'- 1:(j
( io2-;;;:;1?
( io2 f -S3
( IP" 2:913
;; :-(' :;i 2
17
11
22xl| 1 . 1; 2:^25 ( ip;
;;2;2'l 1.4- 2 15 ( 10
•':2'(2i 1 .9- 2 .'5 ( 10
.;2xSi; 1.1 . ( 5 ( 10
;||iiS 0.68; 22*2.5 * 1 0 2;x;l
Pi! 1.2; 2:*-:,5 ( io22("2i:
SWIl 2.4; ;;x.;,5' ( 10.2 Cis
fixjS i.?;; 22l'b ( IP; '2;16
iSftl 1 . 6; 2' -lo < 10;:-:2
-24
22222 i . 9; 2;; 20 ( 10 2
;:',18
224::;:i 1.5; :":x25 ( 10 ;; 25
222x'.;l 1.8'- ;2io ( 10 : 17
12x21 2 .2 22 .'-'5 ( 10 ; 16
isv:-:! 2. 3 j2*.
: s" < i o,; •'2'26
C ip ( 10 2221;
:;;:";'i:6 -
;;;:,20 ( io2
llfeli 2.4- •2*25 ( 102: Sf:l
ifSi ;v.-:-:o.- ; -.. ::..'.- 2. o; -;;x ;5- ( 102; ;'^41
SiXil 1.9 2x;:5 ( 102: 2^28
llfcii 0.31.: 2:-'^ S ( 10 ;12P
21222; ;;
fsfw* 1.9 ;2(2S < 10; ;2.2o
22S2i 2 . iS ;;2lO ( io2 :;:;'i2
52 (21 1.92 2(25 < io; ':;':48
t^'5
Sit* i-'S;2*25
< 1 Q;2
11*3- 1 - 9* 2210 ( 102; 22i4:
gffiW-i -';x2'5
Mm 2 .4';
:2:zp
X 5
( 1O:;;
;;;43'
( 10;
222.;5
1.62iszb
||'( 3 2 . 7; ;2( -:|5
( 10,2: lit
< 102; ;2:6i: 22"5
< 102
A .5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 rain and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
TSL/96
Be :2;Bi':;; Ca ^uCd;
ppin.;;ppm % ; ;,:ppm
( i;;;2x,'5 3.i2-;2(.,,i
( i;;:':;;.;(;5 2 .a^K :i
< iSHsS; i.9::'"2x'2i:
( i;i;12.5 3.62";x|l
4 i:22a25 3.6;;;:x|i
( i;2:(.;.5 : 4.2"-Y"f
< i2::2^: - ; 5 3.2 ci
( l; : .-;c;5 4.0 .,X;1
< i;22i{25 4.7":"x;;;3.:
< I :22".fe5 5.02::^'l
< 1 :22x2:5 4.32.2*2,1
( l2.:;te5' 3.0:'2;f;;r
< i;;;S(-25 2.8;:2; :;(2i
< infills 2.522x21
( i::'22'x:J5; 3.2-;;.:x'::;i
< 12,2(25 2.6;2 (-i
( l';:' ::;x'-"'5' 3.o'-2x22l
( l-';2;(:.;5 3.3:-*X;:i
< i;2x--5' 3.32.2(;;:.l
( i-;:;2x;:5 2.9;.;2x v.;i
( l'-;lB-5 2.o;;;x,.i:
( i2;21'5 5.42-32.1
( 122x15 2.822S21
( i; : 2^j5 2.9::2::;(2i
( 1:2.;^.::? 3.l5 :.;;x::;i
( 1'. -':x.::,5 4.0 :; :;:2(.;:;1
< i ; 2*25 3 . 7- T; (2i
( l : .:-;'(.;-5 2.8;.;;;(2:i
( i.V';-.xj:5 2.722x2;i;
( l..;;;:;S:5 5.3;^S
( i:' :::'(25 1.82^21
( i-2' :'('25' 2. 52,; (2:1
( l:;;.;Xi;5: 2 . s:;.;;';/;;!
( Ipljl 4.8';2-;;(2l
( l-2;;(2"5 2.9:;|;:(Si
TSL/ASSAY laboratories
1270 FEVSTER DRIVE. UNIT j MISSISSAUGA.ONTARIO L4W-1R4
PHONE fh (905)602-8236 FAX H : ( 905)206-0513
Co ; •'i;':or;;:
ppmfppw
13
i?; 2;;14P
'""'"'•i"'of\
15? .:::::lOv
43i imo
23;
46; ::2..6io
39; ;:;:690
44; fllPb
48; ;|6lP
44; ;2:45P
47i
17;
14;
17*
18;
9;
14; ;;,;,|',5
i?;; iUl;
12; ::;.;;^5
13;: *:34'
18; ;::2257
22; 1120 p':'56
14;:
2ll 1M
12; '2272
16;;
IS2
13; ::.;2;8'6
15; -S;2S9
12! "1162
26;
23;
14; :
2267
16:; 2f*7
26;; fils
22,, ;;;:;;85
I.C.A.P. PLASMA SCAN
;2;:-.84.
ilw
PIS
;2ibP
;2±; :78
2:262"
2;P2
;2l68
"/^•..••'.•'•••"•'•'•"
2^fq
'-S90
Agua-Regia Digestion
cu ;vC;i?e.;
ppm- ::;:;;^.. -
54 , 2". 0
35222;4;
142::2 :,i
6952-525
59;.;.;.,.3v4;
45 4.9
46 4.3
46;; ;4.6
31 4.5
19;;,;.4;..p
45f';;4V:4
20^1^8
15=2626'
18 :;:5;8
32;,'::?;;;?:
13';':.;5'.i
25':. 6.5
19;--;-2,ll;
15 !2'';7--;: B
2o:2:7;;3
I5:2;;6v8
1522K8
1 622.528
i522:9.-:7
28;2.:2";[-Jf
f:.:]:1.. 1 . 1 ..,/1/ ".:.v
4 22,;;?-:,. 7
i22;27,9
17?" 7:1.5
23:;2;7.'lb
•41;;:,.5;;-1
31 ;7.4
12:;25^4
1522|::7
27:223'.y'9;
22;; ;.-'..7.-;.9
Mg ; Mn
* 2;PPn'
1.1; 410
1 . 4,2 510
i.i;2:43P
2.1 22870
1 . 8 ::; 690
; . ,. .:..-".v.' '
2.4 1000
2.2 680
2.3 920
2.3 1100
2.3 1000
2 . 322910
1 . 323400
0.83:;2500
0.66: 2000
0 . 88-3500
0.69 2400
0.84;;2700
1.0,4400
0.87; 3200
0.8322700
1.0 2100
1.9:3lpO
i . 2;;2iob
1 . l23700
i . o2;: sab
1 . 5-3300
i . i23lob
1.123000
0 . 9o2;290b
1 . 92l700
1.3: 1700
1.0 2200
1 . i::;2100
1 . 9-1100
1 . 422500
Mo ' :;Na; :'
ppm ,* ;
( 2 0:02
< 2 P; 05
6;;.P|b6
( 2:PvPl
< 2 .:.S;P3
( 2(0.01
< 2 0 ,02
( 2(0.01
( 2(0.01
( 2(0;bl
( 2(0,01
( 226202
( 22bW
( 2 O; 05
( 2;:0ib3
( 2 0 .05
( 2 b;05
( 2 0 ,03
( 2 fi : 04
( 2; 0,05
( 2 o;; 03
42o1;p2
( 2-0^03
22o,Q2
( 2:0202
( 2;P.03
( 2(b2oi
( 2-bib2
22&3J2
( 22b2p'2
( 2 'Pi:p2
( 2;:b;;b3
( 22pJ;p2,
( 2'2b :i'b;3
420.02
Ni i;
;.::"P:2; Pb ;:.2sb"2
ppm ppm ppm ppm
12
32':
2000 ( 1(5
50;
160:
50;
2:!i30 2--:-' -(.;' 5
;2'560 ( i;:2:;:x25
fCOo 2':"'2:(5S
:" :8'sq ( i;' :;2.f;5
400 86 (1(5
370 72 (1 ( .5
42O ,: 88
550 ';'2ioO
420'-
( 1 (5
( i!i;x2g
:;"2:;.74 ( i.22(-,5
SB":
24; .-.;3: 6'b ( i.22f'- :;:5
28-;;4'oo
( i22"c;;:5
17; 2310 ( i2^:;5
480 i;;7'b ( 12-:'(2S
;235'b ( li*.S
10 ';380 ( l; x;;5
14 ; 390 ( I'V.CB
28; 2340 ( 1 -;-(;"5
26 ;24'oo ( i2;..(;.5
4 1;, ;;:390 ( l'2x;5
84;- "2400
IIP;
( l2;,:;(";:5
:i;i'bP ( ijSy^S'
59;; 2.440 ( i;;2x25
47; 2;;3PP ( It.-^VS
is; iSpb ( i22.X:; 5;
:
63;; •;: :37b ( l2.;:^25
2524330
so; ;,';46b
32; 2'-4lb
66J;l'4pq
(
(
(
If 2x2 5
i2; :,;x:;.: 5.
l2:;'S-25
i:;.;2;;;(;-:.5
";48o ( i22x :::.5
38;
1722.-530
( l;2;;(;-;5
132 2'3.9b
130;; 1206
( l22;('25
( i;:2x25
19; '360 ( 1:2;(;;:5
Se . ; sn ;
ppm ; , ppm
15 ( 10
12 ( 10
15 x 10
12;
12
14 j:.(;;.1.0
5; ;( 10
3 ,'( 10
3 5 10
4 X 10
3
4
6:
4 : ; :x: lo
4 (;10
4 (:iO
14; x2io
5 :: ;^-;10
5 : X; 10
2l ;(; 10
5 X; 10
3 ;( 10
4; x 10
4!
x : ;lO
19:
5
3;
3
XvlO
X 10
x : 10
x 10
V 10
:x:io
( 10
(;10
( '•'.IP
12 X 10
5; X 10
Sr
ppm
REPORT No.
Page No.
File No.
Date
.
:
2 ( 10 230 21
3 x 10
3' ;( 10
12 x io
6 ( lo
170 V.-12
1902 ; ;6
2102 :
'"214
;30
190
:
290 ; 20
210 570
280; ; 40
260 ;;2o
280 20
270,;
80-
68-;
56
79
61
67
80
79:
67
39;,;
2402
53;;
572;
150
52
472
532
3io2
82
Ti ; V - w
ppm ppm l?pm
;. :2:17
29
;":-2b:
: is
23
17
17
25
28
20
22
2:46
:i9
•."".'•"23
.21
80 32
76 43
73;;: :-;28
64"
29
2702 45
26
16
23
-30
31
3 X
4 ,(
3 X
15 (
5 (
17 (
55 (
44 (
13 X
3 (
16 (
20 (
23 (
14; (
23 (
16 (
26 (
22 ;x
24 ; X
27'' '-X,
29J.X.-'
78.;x :
24;x,
22 (;
3 :.;.('
25:x
17 (
20 (
23 x
120; (
36. (
14 (
13 (
7 5" x
23 (
M8322
2 of 3
NV19MA
NOV-20-1996
10
10
IP
IP
IP
10
10
10
10
10
10
10
10
10
10
10
10
10
10
10
10
10
:io
IP
10
10
10
10
IP
10
10
10
10
10
10
y
ppm
5
4
2
7
5
2
< 1
2
4
3
2
3
3
3
2
2
2
3
3
2
3
8
3
2
5 :
4 :
3
3
3
3
6
4
Zn
ppm
27
21
220
50
33
40
29
.2:23
••••' .-14
37
2:16
251
40
48
72
:; 55
68
79
\"75
-82
200
180
160
19P
•" : ;'4P
190
140
4.;
2"
; :;;':"63"' IPP
' :"27?
7
98
: '53
57
264
72
Zr
ppm
2
B
16
12
10
7
7
9
6
7.:
6
7;
s;
11
le:
8
9
B
8;
11
10
12 :
11
172
1
12
9
g; :
10
15
11
11 8
10:
12

CAMECO GO^D INC.
ATTN: P. CHUBB
PROJ: ENGLISH
6W-4692-RG1
SAMPLE #
EN096D-420
EN096D-421
ENG96D-422
ENO96D-423
ENG96D-424
EN096D-425
ENG96D-426
ENQ96D-427
ENG96D-428
ENG96D-429
ENG96D-430
ENG96D-431
•K.:;;l
mi
Al :: AB ' B : Ba;i Be ":
* ; PP10 PPm ppm ppm;
2.5:i
2. 6r!
Wfyt 3 . ii
HIP 2.8)!!
zd
o.a
;;;Z5 < 10;
2.
;lb < 101;
2. 2;::.; :;*S5 <
2.oSa.i!'5; (
i. 7S!tf;!S < 103:
?
10 :yi:6 ( l
lo. : 16; < i
10 V;.;?i < l;
10;v.'!!4i < l :
45 < l
;i"8 < l ';
.'•7 < l
f :12
'•1-23
< r;
A 5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 ra in and diluted to 10 ml with DI H20
This method is partial for many oxide materials
T3L/96
Ca ;.,:'cdi
3.o''"! :: c;:i
1.6:. ;;x';;:l
4.8:;'iiil
2.8;;;!X;?i;
5 . 2; ;:!,H f!
2.2.".?.;;;'!
2.1 ' :!.ri
l-9'..;:*;;f
1.9, "x;?!
o.84"..;!x;;!i
4 - 2 !";SS
TSL/ASSA'. i - Laboratories
1270 FEWSTER DRIVE, UNIT
- -. — . — , ,. M U *.***jf\wn. , \jn J./VH J.U Jj^ W — i A ^
PHONE#: (905)602-8236 FAX * : (905)206-0513
I. C. A. P. PLASMA SCAN
Aqua-Regia Digestion
Co yibr- cu ;!;.;; ;Fa ; Mg ijfMn:; Mo -;:Na ; Ni : .'...•p;'5;'.; pb ,; ( ;,
Sb Se ;.Sn ,
PP"i±:;p:pm ppm;,i;
;-;:.;ft,;:S;i *"
PP m,-.:jf ';; ppm ppm ppm ; .ppm ppm ppra
;;';:'!:'s S? V:\S
21-5-45' 33; 7:8 1.3:3300 < 2;; 0. 01 15 400 ( i,:;
205i;66' 25':,,;,
X;! 5 4!(,!lb
7il 1.5."; 14 ijp' 2XPspl 23 ; 500 ( i; ;.; :
13i;;:':.;;22 4^-V
X 5 3".;V IP
l:l. 1- 9±lPO < 2^0,01 43 ;1500 < i;!
141375- 3 :!i:." 4;2 1.6; ;960 < 2;;:;p|pi 26;
v.s 1 4 * :..io
f:KJ*' * 1A"' i'
I6j;l;fp 2;S
"X: s; 2 ;:x';i6
( 2 6 i 01 29
S;;:,'Hi;'; ;.v;.? 5is ;|;;;:;;; ;;;K ,;;.5ft ";
16'~"' :"68 12"'*" ^•/; :v; ^;;; :;. ; : "
...... ,....',. .:v;.:v.. .- - -
.;. :' : ';. : ;. :'. ' "
3,8 1.7;;1300 < 2; di02 4O; 2QOQ < 1 !
isllsz? 29?;;
X 5 4 ( 1 0
14 1 . 6;3606 4XdibJt 20 ? :::5lP < l. : !' ;
*; 5' 4 ( 10
IftMSg. 27'!::,!!" 7.9 1.6i;29dO Z&Ji 32;
I3ft;;;;;"4| is'??:
:;590 < 1
T!!, 9 1.6s,35o'b 2Xpvi):l 19-
.........,.".,.,.— . .. :;.;!5.10 < i :;
15*578 12.::::.;!
X 5 3;,/ 10
si? 1.6;:..450b 4XO".01 25 !,:.470 < i;.;!;'
;: :;;;t; s;;;;-;;;;";.
;.;.. .:i; . .;;.-;...
SSSfJ S:
ie!s'l75 3i;:!!!;!l"ft
i.8.;;37oO 210V.Q.1 66.
'f',5! 6 x! 10
29i!;|5| ISS7,S
2.0V;16p6
11500 < l2- : x ;5 6 'x id
-.-.'.'.'-.i .-.•..-••. ' . •••••• 1
SIGNED
Sr
ppm
56
41
160.
REPORT No. : M8322
Page No. : 3 of 3
File No. : NV19MA
Date
no;; "•.•"14?
••.!22
99
280
58 !.
28 "-.-'vi
44 ; 24
26
210
;!;'ppm
; 26
, .26
20
: 31
27
40
27
V W
: NOV-20-1996
; r ' '. .'' - 1
I7;;x 10
19 V 10
< l':.V.!lP
< i:x:io
2 X 10
5.x 10
21 X 10
16^ 10
15 ;X 10
19 X 10
34';'-*: IP
11 -x 10
Y
ppm
3 56
3 65
a 94
5" : !,-:"6'4'
5
12
4
4
4:
3
4 ;
8
Zn
ppm
67
64
46
50
50
100
87
Zr
ppm
9
11
6
6
6
3
12
11
10
M:
4;
9

CAMECO vC
ATTN: P. CHUBB
PROJ: ENGLISH
6W-4689-R01
J I NC,
SAMPLE tt Al
*
ENG96D-432
ENG96D-433
ENG96D-434
ENG96D-435
ENG96D-436
ENG96D-437
ENG96D-438
ENG96D-439
ENG96D-440
ENG96D-441
ENG96D-442
EN096D-443
EN096D-444
ENG96D-445
ENG96D-446
ENG96D-447
ENG96D-448
ENG96D-449
ENG96D-450
ENG96D-451
ENG96D-452
ENG96D-453
ENG96D-454
ENG96D-455
ENQ96D-456
ENG96D-457
ENG96D-45B
ENG96D-459
ENG96D-460
EN096D-461
ENG96D-462
ENG96D-463
ENG96D-464
ENG960-465
ENG96D-466
;;. •...^•••s'f-;- v.,-:lil
1.2!
^"5 B 5::;::Ba;
Sppm ppm;5 ppra
5^55 <
51*5 i 2.i5; 10;
5i5*i.| 0.67VJ55
ip < io5 . V ;82 :
fiffil 0.765
'.-"•••fi"T
1*1*1 < io5w;::6?
5l!i fi' 2 . oS ;-x5*5 < io5
555'f'f 0.765; 5; ip < 10
ills' < 10; t28o
55:'*r|i i . 45: Si -j ( 1055iSp
M& 2 . 3 5. :;51P < 105 5200
555x51 2.0'55^55
< 1055.;
' ';2
5:5*5i i . 65; 'i* i* < 1055'i5P
llxll 2 . o555?:;I
* iof:
ill* 2.4s 5555 < io|
KKp'l i . 4:5
.yv,,/,:.. ;-: ..v./ 5*55 < ip|
18*5* 0.61s:: mt* 10!
1111 0-28i:jf-j5r
< 105;
1;1S 0.2 li; 5(5 5' < 1055536
15x5:1 0.315* 51*5 < 105"; 1574:
r^TO 0.57S;; 5:.;' 5 < io,, 55;7'8
lliX'll 0.55:4 ;5io < 10:;: ;;|5B
111 0.141;x;,5
< 10 ;;
'5'tS'o
1:5*51; ff :
i5*si 0.2955 5*55 < io:5. 55'i5 .
0.22! gls < 'lip 10" i
It'Wl o.24lf W'5 < lot Step
Sirtji o.2iS5:x5'5
< 105 5^0
P'M 0.3255;*5*5
< 105Up
^.Is <
1-5;;; 2
•5511
ftfli
9#
11*1
i:;!, 81
5490
lisa 5*4*40
|2|*5 :1 0.22*5
:-"'"i"i:
105:;;::.16
IM51 0.28i5 •*t5 < 10'5 ;10S
I'iO 0.295-x
5s c 105SP?
5.5^1 0.2955 :feS < 105 : :*iPO
54*51 0.45.5; 555 < 105 •120
55X51; 1.0,.:: :x|5 < 10 5 55.14
515x51 i . 85a Sio < 103; S;7 :7
55'x5i 1.555 :*|5 < 10*5: ;i4p
555*551 i. 755510
( 10 3*20
i.55*li; 2.6;".." |.i'5 < 10 180
Be
ppm
A .5 gm sample is digested with 2 ml of 3:1 HCL/HN03
at 95 C for 90 rain and diluted to 10 ml with DI H20
This method is partial for many oxide materials
< i:,;^,55 e
. sS'SSiJ
x 155x55 3 .9.; 381
< i ; 5*5*3 3 . 555x5,1
< l5:.;5*55 7 .355:X51
* i|.,:;i(-li5 s
< 15:5115 5
x l' :;**l;5 5
c 1.55^55 4
•2;; 5X;5l
•'llxll
.2'55B-:i:
.755;*::;;!
TSL/ASSAV f T,aboratories
1270 FEWSTER DRIVE, UNIT - .IISSISSAUCA.ONTARIO L4W-1A4
PHONE #: (905)602-8236 FAX #: (905)206-0513
I.C.A.P. PLASMA SCAN
Co ;;5:;Cr5 Cu :•v-.'Pe;;'
PpraXppni ppm:;;;*:,:
40:5940
i7.55;|;ip
16;:;r.;47 :
40 r 970
32;5i'5|
: ' '-:'':: ': 'l :''0
285517^
77 V^V'jiri
* ':;:.:..:;.;;py
3o'S;a;9o
* I'fc'^iS; 6. i.;;; ;...vs.j; *UJ;;;(55y
< l;5 :i55 4.65:i:x5l 3l5.:.v;330
;:'555I iflBS '5:555:::
:
< 1*5x55 5 . i :5'.5:i *5j;
<
<
<
iSx;55 4.5a!x55i
iSiSiS 4. ^;i:iH":i
-1-..: i;;;;:x;;;5 ^v^:-:^ 4*
- . 2*;BiiL
< Ift^if 4.
< i :;;;vi55 5 .
* i^'ilSs 4. 3:;" ::;xl':i
< li5X;5| 3. .7.;tf^'.i;i
< i55xlS 4 . 25l:x-5l
' ^'ili 3- 2.:|||1
< l|:l|i 2. 45{;5iili
< IvStjl 2.
0*5i'Sl
< i'55i*55 3 .
< i :;";;(5l 3. 45|f5ji
* l;:i;X55 5 .
. 4MSsi
v;;:; 1;;;^,:
:-^:.;-:.. ^..-.:
6l5:fel
5|;|;i
( i5".::;x5W 2 . 5:::^;:^:;';^
* 155155 5. 4S55^5;l
< i. :55l;''5: 2. evrni
( l'-;x55 3. fism
' r 1'^ 7. 255^5:1
( i5'x.;i-s 5. 8:5i;xJ;l
< i:5::;*5:5 5 . sliifc
< i5.:.:i:f5 4.
<
3;;5Sf|
l..*iS 3. 9-iS
* 15 i 5 4. 3.55:^11
485l?7.p
535'l300
36f|3p
9O ::^'-''Hvnri
*":-:^v.-.J.OU
soiifll*:
5"555i
345;'5i6'6
4855246
465;;:400
4655150.
5i::;S:;'i:5p
13555:11
"SIMP
13k -MS
isalfii
225i.iy
165|i4 :0
27S5i;;|8
52*5:5240
5iil95o
4055*50
35555100
3745620
36|s;;37p
3355430
41?! 1200
Aqua-Regia Digestion
v 1..;.;;;-.-;' -5,
4:5 :5'4. : 7
oy.;:. 2 :. 8
7555.2.9
32*5i"4vl
98|54, : 6
495Q.450
51i''3vl
74iS4v8
2 25 53 .8
50 ;';#- 0
4i-55 :4;52 :
62SIL4
58;;;{;4y;2;
^1-'-*'^- "t±
62;;;;-;;3;.;6
6155=358
48'5545'2
50'5!'4f7
425,:, 4V9
4255:4:v*2'
20.55'3li-5
4055 2'53
aiiMa
6356119
22\SMQ
5 155:3. 52'
I6;5|2l4 :
902S3V5
3955:455
4i;v;;'3;*3
29;:;i';3 .;7
53V..4V1
3355357.
10055450
8355:4ll
43;5;4.5l
REPORT No.
Page No.
File No.
Date
M8337
l of 2
NV21MA
NOV-22-1996
Mg Vjs.Mn:,'; Mo pvJfaR Ni lipvrj Pb *5..;Sb5: Se :; Sn5 Sr -,.,;:T'i ;i V ;V;W . Y '52145 Zr
~""" - ppm ppm ppm; ppB ppm;.ppm ppm ppn ppm
2.352300
1.8*55780
i. 85:5590
2 . 45iiop
2. i;: iioo
vv/55.55 1 '','J.
2 . 154000
2.0;;1000
2.2;: : ; I960
2.4 1100
2-2 5780
2. 4;; 5 840
2.555810
2.355:700
2.215650
2.255740
2.2ii;*7io
2.6 890
2.555870
2.6v.;:800
2.7;5570
1 . 355.290
0.88J534P
0 . 8955;350
1 . 5 5;; 460
2.1; 5 660
1 . 25:;:5320
2.351*690
2.6555580
2 . 6i 5:650
2 . 5 ; ; 5 670
2 . 3 5 v 620
2.555890
2 . 355*720
2 . 35:5700
2 . 4555870
< 2*o;-*;pi: 54055140
< 2|p :v'C*.*'i 635'I*4PO
< 25p.:.;p2 6i:; : 1500
< 2;x0501 51055250
< 2x6.pi 86;;;i3pp
5555:5; 3s.-;;;!5 :;
< 2*p5pi i2o5?pp6
< 2VP.pi 8151766
< 2xp5pi I2a5i4oo
< 2*6iPl 44o55l50
< 2 6503 130 51400
•'•••"-55:-:\',v , •\.-..-;..::-.:--"^"
'•^'•'^'-^ *-/--:;-" ".v?. .' -':-
< 2lp;i6i 550:555741
< 2Kp|qj 5905555??
< 25^16? 23o55l360
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10

CAMECO ,,0 ~J INC.
ATTN: P. CHUBB
PROJ: ENGLISH
6W-4689-RG1
SAMPLE #
EN096D-467
ENG96D-468
ENG96D-469
ENG96D-470
ENG96D-471
ENG96D-472
EN096D-473
ENG96D-474
ENG96D-475
ENG96D-476
ENG96D-477
EN096D-478
EN096D-479
ENG96D-480
ENG96D-481
ENG96D-4B2
ENG96D-4B3
ENG96D-484
ENG96D-485
ENG96D-486
ENG96D-487
ENC96D-488
ENG96D-489
ENG96D-490
;5;ASrI;
51'llS
nil
i'S'si
S5Wl!
35x5'!!
IIII
llll
IStlii
tlSS
Silt
IIHwi
pill
•v^.sf* :;;:."v;
mm
113.1
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Hil
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till
v,v,-...-,v^"v.Vj|'':
fe."--X-^:l:
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* BSppjm
2.2Jlf;5
1 . ?S 1(35
2.ol?I;;5 ;
1. 833515
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l.3f3il;|;
2 . iSKIIS
1 . 3JKS*j
o. soilfll*
o.sbllBIs
1 - 5111
2.7ifx;.;.5:
2.8li2p;
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0.73lll|f
1.335*35
1.2lll;fl :
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0 - 28lili
I.ll3:li
2.4lf:g;!5
l . 9i::;;x3
2.4|5g|
B 5 1 B'a:;; Be I:5Bi :| Ga ;I.:Cd'!
PPm :5 PPW Ppm:;|;p|m * 5 ppm
;-.:;5 335* S^R
( io;5300
< 135x55" 4 . 2'5 ;x3i
( 10.-5I1^0
< i3li:5 3 - 6:!:dm
( io':32ld
< Il5xl;5 2 .8i.5i3i
( lOlII 570 * mn * . i!3;xSt
( 10:5 13 7 < l~:yE3 2 - 9SWS
( lo;3: ••••52
( 10 55 ;;:11
( io3l : .117:
-42'
( io33
( 10 I: "*6
( lb;3l 1 21
( 1053113
( io35; m
( ioi3
:19: '
( io3?| •I:26
( 103-
( lo5:I. ;:i5
( lOlli; 124
( 1033 ?37
( io33: 141*
( id;I3
Il2
li? 1
^ 10 -i-v^-. 1
'•flS
( loin
( 10:53
. . - ...- :-".::": - ,. . - ' -' : :
\3l'
A .5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 min and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
i-i
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< 1:;:!© 2 .9i5:xi";i
< 153H8 3 •83I,x.3i
x lllffif 3 - 4l;:::;(3l
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< i|5j(i5': 2
< iII'IO 2
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.7ii5iia
' q;:H';:.ti: '^'^./"A
TSL/ASSAY ' laboratories
1270 FEWSTER DRIVE, UNIT -, MISSISSAUGA,ONTARIO L4W-1A4
PHONE #: (905)602-8236 FAX tt: ( 905)206-0513
Co ;:I|Ct:I
ppm ppm
363:570
28;588l
3o:;J9;do
29;-iiob
193,1150
26iiS
26;55;6.2 :
203:II72
is'iSid;
18-,.:,v;68
2o31:I|6
2153552
17:35 Is'8
a5IIl43'
1133359
93I3M
243557S :
I9:.'::3lf8
15;r:;.a|
16llil52 :
14 : ;3l54
23:55190
i7l|:ipO
3951165
I.C.A.P. PLASMA SCAN
Aqua-Regia Digestion
:-....' ' "'
cu II •pe;.;
ppm,':;*;;:;:
9l5 :!4.3;
59p3v5
6253334
455l3v.7:
66fll4;9;
eoIlSS
57337 ;: :4 ;
3135459;
9i5 :33:7
39.5 3.6
4i5:!: :55 :'6:
42: (59'l5
28;;3;'83;1
6:I33'a4
83:^5;
s: j -3^ B
4l5:I'5 :S6
74 :;. ::4lv7;
26 3; 2
125.1'33 :;i
'-^•.••/•••.•••^•.''•"•-\
6'3;4v5;
4155556
18;5;4;5:
59iS8J2
Mg IJrtl:; Ho 5; :'Na5
* ;:: ::;pp"o ppra;5l'^'I'i;
2.45.^740 ( 25o;02
2.355640 ( 2W :;di
2 - 4.sWo: < 21*1
2.4:;:7SO ( 2XO.:01
1.6;;2:40d ( W:m
.-::.'-~ •••- ••••' ;;:. :.: : '. .15,.' 5."
1.552600 ( 256.03
i.elljopp; ( 25oI;P4
1.452260 ( 2s'0l03
1.7il60b ( 2l;"6.vd"3i
1.851200 ( 23o.sQ3
i.5i2.4op ( 25d,:oj
1 . 53:3500 256502
i.eSspo ( 2lpjoi
0.7832000 ( 23o303
1.2326010 25o3pl|
0.80 2300 ( 2l:bi05
i.s'Iieob ( 2;b3b4
1.4;: 230Q ( 2i;d;;: o7
1.655870. ( 2? :fl?Q*
1.5.5-78(1 ( 2l;;d;3b|'
1.6:7400 ( 2lb3 :05
1.731860 ( 23bl654;
i.6ll8do; ( 25p;;:o7
1.732300 ( 2:ipi,;p3 :
Ni ;
5;.P ;:5
ppm ;Ippm
i7o;
260'
3 3 o;
280
39;
33; 5:290
so;; •3430
27;; 3:526
41; 12000
6 li; ;220p
25J3:700
19; ;5.57p.
195ii?o
9;: iisib
13S
111: :3650
23; 5:54:0
24;;: 5710
3 li woo
34:;
isl
22?:
I'l5^?p.
•••440
TSL/96 SIGNED :
36l
;19.0P
5:170
K:i8te
5.1:90
;;l3oo
'• X :3:V ' ' 3'
536lib
;2polo;
3^710
3:Mo:
Pb 5; Sb ;
ppm5Jipii(
( I5;x55
( 135® 5
< 153x3*
( 1/5^5;
* *'jM?
r;;,:::,..:.^
( 155(:I'5
( 153x55
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( 1:5; *35
( 113(55
se ;
ppm
19;
16
16
17
4
3
4:
3
2
3
2:
4
3:
2.:
3
3
55
5 1
5 J
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X 10
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x 10
(10
;(ii6
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10 (510
11
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XtlO
3'"*iio
: (IlO
K; io
(lio
(,io
*3io
x3io
xlio
(lid
•iifio
dp
REPORT No.
Page No.
File No.
Date
S r •:;:-: Ti5
ppm PP
260'3llpQ
2io3 :;:72
1705- •;3'i
I :23
190 5
49; ; 55-9
48 :: 5;;6
5835iis;
55-1 : ;:,";7
33'
210
310.
514
88 -li
53 ;::I: 127
57ll;; I36l
455.1 315
120 5 ••'1 5
:'3
5 O
57
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87;;5 6
180; I ';I3
170 I 5-3
'"I2
7o3:;
43;I
4lI5;
::I8
5. :6
33l; :I5.9
v ;..;i"3;
ppm:; jPpm
;10
eil.i: lio
675X. 10
69 ; ; ( 10
17 y 10
126/X:
12: x:
235x
lOlx
( 1 (
( 1;(
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I4:;x: 10
8 X io
( ii'iv; 10
( ii x: 10
9 ( 10
323x1 id
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3i5x, 10
M8337
2 of 2
NV21MA
NOV-22-1996
10
10
10
10
10
10: < 10
34::.(' 10
2B5x'I;io
4:'I(Ilid
4 1' (I;vib
Y
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8 31:47
3: •13-12
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3
3
3
2
3
8
9
3
3
3; ;;.I2id
3l : 35*59
2 1 3 55
3
2
3.
6
8
4
3
2
2l
;zn'
ppm
:3' i?
940
iddo
Ilsoo
Il50
51
•I;'. 73
5130
i9d
I.I' 63
lib
:; : 100
;;i39
'•:- ::J*
83
116
100
ISO
Z r
ppm
16 7--
10;
9
; 7
6;
9
Si
4
* ;iJ
8;5
10
9 :
3l
8
4 :
6:
4
4'J
35
5; ;
7
7
7!

CAMECO GOUD INC,
ATTN: P. CHUBB
PROJ: ENGLISH
6W-4690-R01
SAMPLE *
ENG96D-491
ENG96D-492
ENG96D-493
ENG96D-494
ENG96D-495
ENG96D-496
ENG96D-497
ENG96D-498
ENG96D-499
ENG96D-5OO
ENG96D-501
ENG96D-502
ENG96D-503
ENG96D-504
ENG96D-505
ENG96D-5O6
ENG96D-507
ENG96D-508
ENG96D-509
ENG96D-510
ENG96D-511
EN096D-512
ENG96D-513
ENG96D-514
ENG96D-515
ENG96D-516
ENG96D-517
ENG96D-51B
ENG96D-519
ENG96D-520
ENG96D-521
ENG96D-522
ENG96D-523
ENG96D-524
ENG96D-525
3*1*31
IMl?
IIP
iiKSi
flllf
Ezfel
fiSS
lili
35*31
J//3K1
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35fe*r
HP
11133
*;s;*il
11*5*
z:-.-Z:.---.-;-"--~
iflx;/:!
Ifmi
IIIS'i
iSa
W&ii
lltti
siii
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53*11
5-l;yli
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5/7*551
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117;i
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Il-Xfl
13*14
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11*11
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K
3;*; As", B :.;7Ba*;
JiPPl PP :PP.m
l;*35 *
3.1
3.3 lap <
4.0 13x7.5 *
2.45/1*15
*
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0.76 73575 <
0.83 3:5/10 (
0.42vSipg
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0.92.11.5
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0.88 71*3.5 *
2.1 sil "s" *
1.3 .1*555 *
0.72 111/5. <
1.1
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lllsb *
2.7
4.3
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3.5
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0.93;
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1.3lllib *
1.311135 *
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io7'; *7i
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lo/slii
io;.rtc;'tj
10;57l4
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1017111
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10.5?;;,;4
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lo/l*'".*!
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io*5i5'8
10353-23
lo5s*;23'
iO;35;2i
A .5 gm sample i a d igested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 mln and diluted to 10 ml with DI H2O
This method i a partial for many oxide materials
TSL/96
Be 3.*ii * Ca 77cd 7
": " ...':. , ". ,. ,- .. ..:.
PPm;/; ppm * ///ppm
< l;.77t;;*.5 3.975*5];
* 1*75*75 5.03 : ^7**3f
< l;5 :*f.5 3.457*3f
< i75:x7s 3.95.':'*5i
< i*3: :x.75 3.7.*:-5x5i:
73 :Sfe; 3;i:33;':':
< i !S5x7'5 : 3.85:;:*ai
* 17 X/5* 3 . B// x 1
( I*3'"i75 5.4-;-5x;-*l
* l5;i*".5 4.5'vxs't
< 1;:,;:*,;5. 3 . S.*/,;*^!
< 15175 3. si/Mi
( i;;S*45 3.975*;;-!'
* l5;3x;;f 4 . 2'}:v;*7;l
* 155x35 4.o'*:3;*7*i
* i77x:75 3.7 :;;j.'.'x*;! :
* i:5.: : (35; 3.27l*5 :l
< i-; : - :-x':*5 2.0:57**;*!
< l .,-:,;*75: 2.7-. ::5x;:'i
* i5..*.*";5 2.977-*7i
* i-i-'/ijs; 1.774X71
* i3;5*;s| 2.8*-'5K7i*
* i*3j*ll5 1.735x3.];
* 1;7*:**:5 1.6*l||:'i
* 135(35' 4.i3:;;:*7i;
* i; 7:i*.;5 4 . i;-5.X;;*i*
< lj.,;;ife5 4.4pl.j:
* l3iE5 2.4313-t
< i7*;-*75 0.30'-:;:;;;*;.;;];
* 1;'5S.':::5 0.17/1x51;
* ^S?:'? 0.127:*|*p;
* l!!/*;! 0.32*5131;
* iK7:*;;5" o.30*5;*:Pl
< 1/53**! o.38;||;l
* i;:;;;.;*;:4 2.4^*75*7/1-
< i|5x:,;5 4.5:7||3i
TSL/ASSAY. Jaboratories
1270 FEUSTER DRIVE, UNIT 3 MISSISSAUOA.ONTARIO L4U-1A4
PHONE #: (905)602-8236 FAX It: ( 905)206-0513
Co 5*;Cr;"
ppm i; ppm
1557750
iiS7;'3^
13.vwSSi
i67';;54*9;
1057548
//a/s/B
7 "* 93
17 100
Il5;;396
165:150
11;:;.;:56;4'
I655i7(5
13 :53;:55
18775152
165*1 jib
15.77120
.;...- ;' :.v..v.y;...'.'
1157558
15 :;;S51
12;::,.: i' 33
14; 45.33
215/S54-
WS33
2427ibb
2237:713
187/180
17^4^:
16/55*89
;;./;/;;.,./:;
2l|sffi88
15*7|||b
49/5160
5o7;';l :3b
59,77160
363|l9'i
47.11170
16;1|60
28|:|ifil
29l;:*24Q
I.C.A.P. PLASMA SCAN
Aqua-Regia Digestion
Cu :;5Fe'*
ppm';; * ; ;
23;78.i
18;,53l2
21*5;;ii2
495:77"**;j
21;775.vi;
26 3.9
16 .4.3
35; ]45S
24;;;4.,.l
3071/455
2177*735*
571174 2
35*3:41?
327:.''4*.;6
14;59..i2
i53Wi4
23*..;-*.i7
24:;;::l7i7
35/1710
40117., 7
58:.17l2
461./8;?
85/po
10*53/6
17:1'/:;
83.73*4;.-8
69W9C2
431/1.19
2911:19
3375.:20
221 :'1 ::I
19l;*;S7b
39/1-/4C/6'
44ll5V4
84:5/35^.7:
Mg : : ;;Mh
* l-jppm
1 . 873000
1.8/3900
1.773600
1 . 772600
1 . 6/2200
1 . 2 '1800
1.3 1700
1.5 2100
1 . 5 1900
1.2: 1600
i . 37;i6pb
1 . 552500
1 . 352200
1 - 1 * 1900
0.90/1700
1.5:12600
1 . 6 :2700
1.7:13800
i . 7i4ibb
1.5l;26bp
1 . 81/1600
1.67;2900
0.9012200
1.5 111 00
1.5;;., 850
1.65l2pb
1 . 6x4000
o.463iooo
0.365/760
0.4511:520
0.657778P
0.2 5113 30
0.69*590
1.8-1.570
2 . 13:1100
Mo v'vi
ppm./ |
2:0^ 03
4lb*ibs
270*. 02
4**,O.
06
< 2;:oj•'•05
* 20, 07
< 2 0. 06
* 20: 05
c 2lo. 08
'04
* 2**b;
< 2.10':; os:
03'
* 2lo;
216'. 03
{ 2l'pl 04
( 2 **0. 07
< 2 /0;
* 20. 02
4X0 s 01
6;*bV
e5 o5 o?
* 2.1b.. 03
4lO :, 02
2***o: bi
* 27 03 03
< 2;.pv03
< 23b!
.04:
Blplpi
47-Pl'02
47bi: 02
6iOl03
2±® PJ
4iyb302
2|b3
PI
< SiK
ia;;
'bs
oi
bi
< 2'M 02
Ni 1
ppm;
20 ; ;
14;: I'eSb
151 1430
17;*
1480
13/ •:54'ip
9
22
111
20;
13':'
1/pl ;-
7*PP"!
;543p
440
520
5.570
;l40b i;:4*S6'
Sob
191
14;; 1/250
2 li Mo
1?7:3380
18l//•430
137 -;2'9b
19 :*400
isl,;1;27.0
14? li'sb
25;
/liso
iissb
47;*
227 .5*330
237 :?250
197 1900
20/ lipq
labb
227
223 1180
765 Piio
775 llH'O
88E
llpb
46p: Slo
5 3l 5:700
275 liib
6911.1.90
91/15960
Pb :;:5sb5
ppmllppni
* l:;l;fc:5 :
* 1/77*35
< ^IfiS
* li'sxi/'s;
* 11.7f::S
< 1 :*,*;-5
< i. : :5:S1.5
2;.:'-x;-:i5'
* iil;.-5ll-**-xl
: 5
( li::/:*/:'?
< il;31 : 5
* ll/X/sS
< i-ll*7;s
l/lxl'S
( l/vPs
( iS---^7 s
< i|5;*:l;5
< iS4x;cs
< llSl'5
t. i.55**5^
< iKixM
< 17;3;3;5"
* il;:;:**55
2llx5'5
< illPs
331175*
92*11*5
83 *lS A;i
7lllxl|
19l7xl|'
16;!*!l5'
4l,*x55:
677x55'
45.7*7:5
//;/;, ././x/
REPORT No.
Page No.
File No.
Date
:
Se ,.7Sn 7 s r ;; .-Tl:
ppm ppm ppm./ ppm
--*; ."/;7 ;;-.'
e:;*; 10
67*1/10
44;; ..US
ae!;: 120
87*' ip 40*3 5*37
55*; 10 45l /li
4;*llO 407 J 7 7
3: * :10 5O
3; * *io 46*;;
3 -*; 10 761
* 1
3 X 10 56*1 • : *;;4
512'
3** lip 35 1
...... ,. ,. ^
4 X 10 39 '3.53
4i:,x;;io 433* /Ii3
3'..*lio 56*3557
33fcib 647;;
sl/s'
35* 10 467: l/".^
4* X 10 36.;
5 X 10 31 ;/
6:::*,:iO 38*1"..
631/10 405;
;/ ;2'.
l/ .1
*;-2i
48
••58
1.63
4:i;:*5:io 335; 1; 3 2
6;* ?10
5'3*!lO
140 1 1*:'28
425* 7;4b
Six-'lO
3 X 10
44!.i ;5:25
3205 .3,;;8
3 X 10 330/ 510
1 1
*
45.*;l3i;b
6lx;710
i:0 *./ 10
32ol11*7
7837 ;*'io
16;1 *7*4
* l/l/lp
il.x5lo
... "-.:-.;: v .:',:: :.
107 :7, ::4.
127* Jo
;./--.
;Vfl
* i;;**3io 15'*;.
41x110
25*510
12l,
*".5'4
isl713
6':*x3lO 290;*; ; * 14
135****ib 51ol
; li
V ;: W
ppm . ppm
30 : * 10
20.7*1 10
35 **10
24 X 10
10 x 10
6l* 10
9 * 10
4 ;* ip
8 i* 10
8 * 10
12 X 10
13 X 10
12 X 10
7; * 10
11 5* 10
23 X 10
29 * 10
36 * 10
38 * 10
26 t* 10
48 *7lO
25; X 710
19 * 10
3 * 10
2 * 10
45* 10
i6**;*ip
* li*/ 10
* i';*.io
83* 10
16V*..;*:10
4*.;* ;*io
24 7* IO
27l*;*iO
45 *;;io
M8338
l of 2
NV21MA
NOV-22-1996
Y
ppm
2
3
2
3
2
3
3
4,.
3
3
2
S'"
s:/:
3
3
2
2
1
l'-';':
2
3
1
2
6
7
7l 1/55
2 1/84" .
2*
7/39
2 *:5;27
* 1: 3;;;4.8
2;.
1
i;
3
6
Zn
Ppm
200
210
190
180
130
60
110
100
88
110
100
130
160
lib
170
150
170
170
180
160
110
•130
96
48
48
: ;*:,;6i
18
; 78
•577
140
Zr
ppm;
83
12;;
91
9
; 8
8
B
9
10
1 7;*
8
5;
9
g
9
8
6
6
15
11
13
8
B:;
3 *
3
6?
97
4/;
10
14,7
67
117
10*
15:;
20

CAMECO
ATTN: P. CHUBB
PROJ: ENGLISH
6W-4690-RG1
SAMPLE tt
ENG96D-526
ENG96D-527
ENG96D-528
ENG96D-529
ENG96D-530
ENG96D-531
ENG96D-532
ENG96D-533
EN096D-534
EN096D-535
ENG96D-536
ENG96D-537
EN096D-538
ENG96D-539
ENG96D-540
EN096D-541
ENO96D-542
ENO96D-543
ENG96D-544
EM096D-545
ENG96D-546
ENQ96D-547
ENG96D-548
ENG96D-549
INC.
5*5* l - 4j
sfl| 1 - ^
S&lf 0.50;..
1.6;
5;?X.:ji; 0 .62
mm
0.35;,
L I?
KSmSZ 2 . 33
ISpf 1.5?;
iSSI 1.5-;
illl 2.7:?
jllll! 3.9/; •;X:?S < 101
fvifl 2.4! I--5 < 10!
gflfcri; l. Si ;fc ;S < 10;;
IIJ2I 2.4-a
Illl i- 9i
HIS 1.9!
Bpl 0.43/2
SBpi 0.31;S
,AS.)j B i.
.ppi ppm!;
;.;S.5 < 10?
5C5 < loj
?5:i| < log
5::l6 < lofc
536 < lo":
Iso < 10!
id < ios
l OS
161
:;73
?37
:22
'il
!??5
Szo iolite!
JCs < lot
igs < lo
S5 ( 10
s < IP
iiza-
laz
Be
ppm
< l;
A 5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 c for 90 min and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
T3L/96
* i :? 5Xx5 4.9: ;
< i;j;
fgS 0.96u
':;::f"'5 0.18;';
fXj;!. 0 .40 :(
5x55 o.ie;;
IfeX';:? 3.75;: :
3Xjs| 5.2 :;;:
als 9.71
||fi| 7. 3 S
;ill5 5 . 2;t
7X;|S 4 .7!
*'*Xs 5.4 : ;. :';'
4 .
^1 3 . 9'I
Sfl 4 . 0 if
i^S: 3. si;
".aboratories
1270 PEWSTER DRIVE, UNIT o CUSSISSAUCA.ONTARIO L4W-1R4
PHONE S: (905)602-8236 FAX K: (905)206-0513
30:^:320
I.C.A.P. PLASMA SCAN
Aqua-Regia Digestion
Mg
2.1J2100
2.0,1800
0.90^1300
.
37 ;:;:::450 49^^.0.57^.320
23JS"9 "oil; 18 1.5;;; 876
44,^600 1701=19 2.1:. 17.66
86; 896
79* 856
84^1766
6651366
Mo : Ni
71 5:;^-8 2.4;,:2400 < 2x6.61) 999
57:;S4;;4 2.451466
150V8 2.4,,;lZOO
55,1300 55v :,:SV6 2.5 1100
66 tj4.6
^| 24 5;5l45o soilage i.aSloOO
420
54:
*74
4351700
Pb .
ppm
SIGNED :
-Sb'...;
Se Sn
Ppm , : ppm
8;
6
3
6
1
2
l:
V
9
10
19 :: .*'. '10
.'•'CIO
14 ;
12 •C 10
19;
17 :"C;10
24
17
15
19
5X;:'1P
-f:: 1^
5^ ;;1(?
5X.;1Q
::x;io
x 10
x 10
; 70
X 10
20
V.id
< 10
x 10
: K.'lO
17;'
X; 10
16; CIO
4 cio
3 x 5 10
3 i' < 10
S r ;;.
ppm
REPORT No. :
Page No. :
File No. :
Date :
370; 5,13
380:: ;'5:.;:'.;9
loo:; f'.. .'5
36T 15;'5516.
25
11
44
loo.;
555
230 !;
I3o5;
27o ;
420
tl ;
,PPm
;;r5'?
? : '.?v7.
'?"12
•5. ;6
16
5; 35
390 1^49
390 21
330? ;.;''27
230S?;46
5.-30
51
29
19
2 60 5t
27
190y :?31'
290;? : ;;;28
250?;; '510.
280?' 5 14
260? .':?59
V
ppm
lo5<
li; x
< i?x
28 ;"X
64 :^
1005X 10
50: x 10
39^, x; ::10
785;V 10
53?X^ lo
1205-c
64 (
48; X
62 X
5o5^
,16
3;'X : '10
;10
3: ;x? 10
47?X
6?' C
M8338
2 of 2
NV21MA
NOV-22-1996
W
ppm
15?x 10
75.X 16
10;; x ?1P
4 4? X 10
9,5X :10
10
10
10
10
10
10
10
10
10
10
V
ppm
7
7 5
2
1
1?
3'
3;
6 :
140
6 210
3 :. : 99 3 : ;,
IIP
2" :' : 59
3 ,". 69
3.5 ;: 61
5 •;:;41
4 V ," 552
2;.'; ;36
S":;
Zn
PP"
94
110
3? ?166
3"
170
1' '•••-'34.
60
88
120
68
130
'•553
'553
9??
95; :':?54
7 ."'-'
: ;42
Zr
ppm
11
6
12
21?
.13
10
125
4
14
10 -
13
6
4:
10;;
7
13
14
7
10
9
9.
3: : ;
3
4.' 5

CAMECO GL
ATTN: P. CHUBB
PROJ: ENGLISH
6W-4806-RG1
SAMPLE #
ENG 96D550
ENG 96D551
ENG 96D552
ENG 96D553
ENG 96D554
ENG 96D555
ENG 96D556
ENG 96D557
ENG 96D558
ENG 96D559
ENG 96D560
ENO 96D561
ENO 96D562
ENG 96D563
ENO 96D564
ENO 96D565
ENG 96D566
ENG 96D567
ENG 96D568
ENG 96D569
ENO 96D570
ENG 96D571
ENG 96D572
ENG 96D573
ENG 96D574
ENG 96D575
ENG 96D576
ENG 96D577
ENO 96D578
ENG 96D579
ENG 96D580
ENG 96D581
ENG 96D582
ENG 96D583
ENG 96D5B4
-NC.
Ag Al As : B ;Ba; Be
ppra fc v.Vppm ppm ppra ppm
•xl
< 1
< : l
x l
: K ; 1
< i
' ? -'i
IX.1
:fX|i
1:^ . 1
i

CAMECC JO -.D INC,
ATTN: P. CHUBB
PROJ: ENGLISH
6W-4806-RG1
SAMPLE #
ENG 96D585
ENO 96D586
ENQ 96D587
ENO 96D588
ENG 96D589
ENO 96D590
ENO 96D591
ENG 96D592
ENG 96D593
ENG 96D594
ENG 96D595
ENO 96D596
ENO 96D597
ENG 96D598
ENG 96D599
ENG 96D600
ENG 96D601
ENO 96D602
ENG 96D603
ENG 96D604
ENG 96D605
ENG 96D606
ENG 96D607
ENG 960608
ENG 96D609
ENG 96D610
ENG 96D611
ENG 96D612
ENO 96D613
ENG 96D614
ENG 96D615
ENG 96D616
ENG 96D617
ENG 96D618
ENG 96D619
)?))Ag:? Al i;::' A* "j B Pia'i
i.:;;^":s:-' -, t:. 1 - 1 :^ i;:;:::,. "~
•?:?S|P? * K::.:PP"i PpmXFfepm
111 )i?. : i 'Si'1 lil!
;;?,X*1 1.8^5 ( 1 0?S;*";L
|? : C;1 1.6??:?*?;5 < 10');?;;;??'
l:-!))! 1.6?C*r?5 ( 10???,x??i;
?I?fet l.SBxSs ( lolll*
)i|M:l 1.4gi*|3 ( lolll4
SKfti l.6it:;*i:5 <
mm i -3)ixc5" (
10ili;;i:9':
ioim;
;;;;:X'.;1 1.5?;;:.*.;-.5 < 10:;?:*;,;!:
S);X:?1 1.4??:;*:? 5 < 10*:"? 2ft
IfSA 1- 2l?x)i5 < 10?f?:?;22"
;?)?X:?:J 1.4|lXi5 < lo)ll;4 :
I);*;?! 1.6):;:;*;;5 < lP;)l:).25
;;:?iX?:;* 1.9;?iX;;?5 < lOV&ff
11*31 i.6:):|*f)5 * loillis
Hill 1.7;?))f;|5 < I0i)lx|l
t);)xl:i i.r^x'is * io:i;S?-22
)1?*;;?1 1-41*15 < io!?V"5
P;X;1 1.8?:,;X::5 * I0)i:i *i il
)?;.??*Il 1.8 ?"!0 * 10?;-?;-- :'3'
lllS 2-1-1*15. * iol?*)?l:
IH 1.9lj*2 5) * lo|?|)i.
l?1?a 1.8S;N";5 * lOfic&S
8t*fl 1.6?:?i:x;i"5 * 101.353
;.-,..::-.y--.:: - : .....::..-:.:-."^.:-. , .-.' '.Y^Y.-.".
:;;?;*S1 1.8^5 * lOiSM
?li5 2- 0??iif5 * io;i|ie
llX-p l.??!*?)'? * loHi'o
?S;P i.6"?;*";?'s" * iQ?y;;:*.yi
s?;*?! i.2.,:;?*:?:5 * io.s;??;:i
fill; 1.4)?;;l5 * I0l!?2
•Sim l .iy?*i)5 * 10B:?3"4
sill? W-W Iffiifs
llfel 0.89 /X 5 * I0l?;:25
SBS* i.iSip * io?S;li
;)Sei 1.0 i, 5: Si * 10?!iy 9
i;::f;x.;;i; 0.98;;'-*:;-? ( 1 0SA;'29
);;S?)i 1.0:;:i)-ife:5 * 1 011"69
ssi;::;;,;;; ±:S;.: : ;, ::;:;;;,:;;;.-:-
Be ;-iir.)
pp"".::v : :.pp:w
* i);?:::xi;i5
< iMI?
< 1;?;:;.*?:5
* i" ;l*i;;s:
* 1)11?:
< il)|?5
< l;)i;X?.;5
* llxl'i.5
< ilD's
* l??;Si)5'
* i::;;?.*S5i
* rlfcS
< i!!l)? :
* i;;;;*5;5i
* lltfi?
< i?);;!"?"
< iii?-''*:?:5?
< l .;??*);?
< l-'?jf5
' 1S'iS
< i*?;;;ft:5
( i:llS
< i;;??X??5?
* i;ll?5
* ^'Sll
< lUS
< i :'"i)S :?
* 1 -i;i:5
< li..:;fl:?
* i';::;x)?.5i
( i^S^?'
< l"'-?iSi?i.5
< l?.'-.-^?:5
* I;?';'fi5
< li:i?i)i:S
A .5 gm sample Is digested with 2 ml of 3: l HCL./HNO3
at 95 C for 90 rain and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
TSL/96
Ca ;)?Cd.:?
* ;;;'ppm
4.5??3;?:"i)
5.7: ;;li-i
5.4?)?X- ;?. :f
5 . di)* ')?i
5 . i)'.ii;f))l
3 . 5)))5'"ii :l
5 . 0?lfli :
3.i:)???(i??i
3.4S)ixi;).ii
7.i)?.i)ili
3.s);;;pi'i
3. si i??*??: i;
3.5)1*1)1
^.'.-vv.-^irriv
S * * : • -••z*'-;;v*~-
5.iSi)ia
5 . ell??!
.8.9;;i-x?:;-!
4.3l?i*ii
6-9??:?*))l
4.4E?Xl?:l
5 . in*):)!
4.4l)*)?;i
3.sll:i)3)
4.0;1*?:1'
4.3f? ;X;ll
5 . 6?) •?*-:f
c 7";.;;v::"T
0 - ';;; .5 ; *
7.5;?;;:-?*?!-
4.6l-:X??l
4.d);?|)l
3-9)-:lIl:
3. 2;.;;- ft!
4.91-ili
3 . o?-i;x?:'i
5 . 4:?;? K!
TSL/ASSA1 Laboratories
1270 FEWSTER DRIVE, UNIT J MISSISSAUCA.ONTARIO L4V-1A4
PHONE #: (905)602-8236 FAX #: (905)206-0513
Co ;??Cr?;;
ppm? ppm
4 4?; "860
4 3):)::7?p
43')i:)78p)
42 ITOO
43ili58'8
;'.::.:: :;:,.:,.-.,,
;:;:::;-. : ;: ;.-:-,
42)i: ;w|2d
39 :??-;:6;id
43)i?i)7)-9p
4i-:li7iid
41??V)i56p
4i:l73P
44?? 83B
48:l:9iS
46?;;:if8?d?
4 Sif 836
52?)):^ld
57?i:;;;53d
46;1'9PO
44K850 4Bi :il
45II1
53W89tt
44HSd
44*;;;69d
47||8|p
50l)0 ;l.d)
Aa..:'-', -jinn
^y;::: :; OUO
49?)?I57.0
45:11(50
40l)S7p)
yssK
43S;:?40
44l7dd
38:1:680
43)?:;6.6?0)
36:1:630
I.C.A.P. PLASMA SCAN
Aqua-Regia Digestion
Cu ; : -)!'Fe:;
ppm?; .Sp:;;;
41:?,?)4V7
47:? ::?4V4
45 :?54^5
33l::4i^:i
47 :;');;4j3)
45 :;):) :4?i:5
43')?;;:3v8
46???;4.3
46);?: : 4: : 3 :
49"? 3.7
5 5?)??i4;"5?
32,;;?4;6
43WCJ9
32)S?S.4?,:4?
44);;:4),:5
35;??4;6
35 '4-55
54? ?4.7
45?-?)4;;V2.
59;S)ilJ'5
33i)?i)4)y7
54S,?4f9
37154:;"?
65)??;:4.5
56?l|i:8
::;-::.:..;;:;-,. :v::::v.v
7o?: ??)4lf
33: :4.i6
54? : ?4i; :3"
34a?4';S
Sl:?::;^:^
55ii?))4-V3
34;i.i:?4'';4
46");)*;^
27,;??4"i?3
i2ii!B)
Mg ? :.Mn
* : : ; ppm
2.5? 990
2.5); 940
2.5;?; 920
2. 5 -:"; 840
2.5? ;90P
2.5;) 810
2-4 ? 850
2.5?i 760
2.5 800
2 . 4 990
2.5)V;790
2 . 5 i 800
2. 5): ? 820
2 - 5? "890
2 . 5)?: 920
2.4; 950
2 . 4 1200
2.5?;; 850
2 . 5 )? 960
2 - slf3d
2.6" ?910
2 . 5)1890
2 . 4?i);)780
2.4)1790
2.5);i)f20
^'."••^'-"•'••'••.•:
2.5?ipOO
2 . 4):???95'0
2. 4)?! 100
2 . 5?* 900
2 . 4;?) ?790
2 . 5;i ?;730
2 . 6:S;i730
2.4l)85)d
2 . 6?)g720
2 . 4)SlpOd
: :
Mo ?;?)?Na- :?; Ni t? :fP?:-S
Ppm;5:Si,5
::::;:;;;:-;;;
ppm?
;??f"?
;,
*
*
*
<
2*0; 01 430? yil'OO
2*0. PI 450;) ;?:i?p
2*d,di: 430?; 1^6
2Xd;:pi 42d) 1:?82)
< 2XpJPl 370);
iili^o
Iffil: ?i"
*
<
<
<
2*p?jpi 440? ;)iid
2*0 KOi 360?; -1 :?78
2*0; 01 440 : "iidd
2xovpi 4oo:; ?100
< 2*0. "01 350")
* 2*d,di 44o; iio
< 2*0itit 490;? .;'l74
*
<
2*p);pi
2X0?. 01
520--?l98
510??: ::..:;.:go
* 2*0^01) 4 90 i?
l'i:9 :4'
< 21 di PI 4 4 o??:
< 2*0 ,0i Siol
iiii'4.0
< 2Xdjpi 54o;?; ;;il:|o
< 2?Cp)vP! 530:))
< 2 *di;;di? 5 IOS
* 2::plp)l 410)J
?:^d
:"3od
< 2:*did! 420?); lilid
* 2xdi|di 5oo|) |?lo)
* 2"*d;'p! 4 solifod
< 2*pfdl 510|- ife
( 2"*p|d"! 490??? iiioo
< 2?*plPi; 45oll:©
* 2*pid)l 39ols
)):i:,84'
<
*
2*0)01
2Xofdi
ilfp
sad? 1)86
550;:, idd
pgV
)?;9)d
< 2Xpldi) 49ol sM
* 2:*dfd! 4 6CS im
< 2 *:Ppf 500)??? fit
< 2 :*dipi 50P)?)i•iia'p
< 2x:djpi 36ol 11:70
pb list-?:
ppm ppm
( i;;\^" : 5
* il^;:?
* l. :;:-|X, :-5?
* i;;i-;;^--?5"
< 1??;;)^:;?
* il?l?S
< l)i?i"?{))if
* lli.sii?
< l??::?X';:-5
< l5i:?x);?5'
* li)?:!!
* i;;;:;;x;:;5
< I'liXSS
< l :""))*)?5?
< iji?;)x? : "5?
< i":i.?*;::;5
* r; ,^-"5
< l?):?iX"ii'5
< li-llisi
< i;;;--x?)5 :
E S;
< iKi*?;?5'
< iliiai
* IS-P-S
* ^iil
* 15;;vi(;.|g
< l ) :il(ill
* l ;?"i:*):;5
< ilsSs
* igsgi
* lff?;;*Ss
< 115K5
( iSlfl
* i;)?))xp
< 1?1?1)5 :
< lf))ii*l5
Se )))sn'-;
ppm ) PP
16
13
14
13
13
13;
11
15
14
18?
* 10
x Ip
)x"lp
i)* 10
* io
14 xiio
16 * id
!6 ;;*"ho
14 i'f/iio
14: :X.?IP
x 10
* id
*- 10
Iio
"*?;10
15:; )*::??io
is?; il)io
13? x?io
12;; :ii?10
H; :
i^id
:'??.-:::??.'' : . : " ,.
x id
13.
12 * io
10/i x 10
13f ^io
13?-;-X?i'ilQ
13?) i*);:10
15i) V;lio
12;': lid
15?? l-io
15?: *.;lo
REPORT No.
Page No.
File No.
Date
Sr ': : ';
ppm
i
:
230 20
180 27
160 i i?35
150
150
14? )X;flO
12 *"io
15 ^ iio
97?; 13S
isoii i ?;26
75?: i,? ; 33
14 * 10 89 i) 32
12? i*; 10 200 ; il9
110
130?
100); :
i9p?::
?:. 18
16oi;? 29
160 ?:
';Ti; ;
ppm
;):; 33
28
' 28
30
-41
180? 27
250
: 18
120 : 39
220 : 28
l 50 1 ? 47
;;4P
1401i)-3li
130;; 30
140?1 -;ii28
170,? :-'26
230 i?25"
220 27
240? :: .•16
190?;; ?:1S
210); ?13
200):? ::;.J
170;?) 111
250; ) :?:,,?7?
180?:; ; id
330); : ?
ii;;3
v
ppm
37,*
25 *
33*
26?"*
19 *
21 *
29 *
33 *
31:*
27 *
31 Y
12 *
38 *
37 X
54 *
48;i*. 10
30?*? ?io
3l) X; id
31? *
29 X
30 * 10
26 * 10
14 *; 10
19 X 10
18?;'* . 10
8?;,1 :
16? *?
18??*?'
17?)*"
9 :;x?)
M8336
2 of 3
NV21MA
NOV-22-1996
w :
PPm
i
39 * 10
32 * 10
30?* 10
28 * 10
20 X 10
id
10
10
10
10
id
10
10
io
10
10
10
10
: 10
10
iio
10
?id "id
io
10
10
Y
ppm
2 ?
2
2
2
3
2
2
2' ;
3
2 "" ::
2 34
3 , .?27
2
: 39
4 -"34
2 40
2 40
2i i i? :44
2 :, :) : 48
2 )
2
4
2
3
2
2.i;?
2;::i)
2')1
2 ;?,
i-?',
3 i
zn
PP"
3 35
3 33
2.) 1.32
1- :
30
3 ,i 2'?
40
27
29
30
27
32
38
: ?:41
-?' 41
?)4)l
44
)))47'
41
39
:)'29
;;38
36
?:"27
26
24
19
38
Zr ?
ppm
5
5,i
8
8
: si;
7);'
7
8
7;
' ^6' ;
e:
7
6
5?
7?i
8
5
9i"
5;
7 i
10
9?;
8
6?;
7?: :
6
5 ;
6' :
5?,.
5):?
8?
6?
7,:
8?\

CAMECO G
ATTN: P. CHUBB
PROJ: ENGLISH
6W-4806-RG1
SAMPLE tt
ENG 96D620
ENO 96D621
ENG 96D622
ENO 96D623
ENG 96D624
ENG 96D625
ENG 96D626
ENG 96D627
ENG 96D628
ENG 96D629
ENG 96D630
ENG 96D631
ENG 96D632
ENO 96D633
ENG 96D634
ENO 96D635
ENG 96D636
ENG 96D637
ENG 96D638
ENG 96D639
ENO 96D640
ENG 96D641
ENG 96D642
ENG 96D643
ENG 96D644
ENG 96D645
ENG 96D646
ENG 96D647
ENG 96D648
ENG 96D649
INC.
Ag Al
; PP" * :.;;
Vhl 0.50
:'Aa. :
•l 1.7;-X.
;1 2.233^
;1 0.85; ;x
•i i.o3x
•c:,!
1.3
0.84:
2 . 5V
2. 6
2. 4r
3.03
2.l3
l-9;' :
l. 9 3,3
i. 633i
B ;; ; Ba Be :
PPm :; ppm ppm;.
10 ;;ii < r
S < 103- 13 ( i
5 < io'3 i3 ( i
s < io33x 'i ( i ;
S. < 103": 17 ( l
X 5 f
10 <
X 5 <
:-(!"-5 <
3; 10 <
x ;;5
ip
10
i o:
10
10*
10 :
10
10
103
10
5
, 15
381
190
200
26
39
l. 23;;x;: 5 < 10 72
l. 6'3:iX;: 5 < 10 .110
2.23;.^- 5 < 10: i2b
1.8J3V;] P < 10
2-53*235 < 10;;;;;120
< l
< 1:
< 1
< 1
K 1
< 1
< 1
Vx ' 5
Ca
* t.
2 . 5 .
2. l
2.4
5.33
3.6 :
2.3
3.5';
2.3
4. 6v
6.8:
.' Cd;
.5 5.6:;vC:
:;5 4.13*0
;5 3.7;3;x
::5 2.73V'
3s" 4.i..- ;vx'?
•5 5.83.3'';;
':s 4-5:::3x;
"5 4. 233x;;
; 5 3.4.3;;;x"
1-433^45; < 1033200 < l5'x35 4.1 : X:
i-sgi'lb < io;3y;6b \ l v;x":S 4.iS^3
20 10;;
4.5
1.6 103
4 . 4'
i.O'gsg's- < 10-3333
;X'V1 2.313x3.5
;x3i; Lapses
-;x; :;'l 0.7333335
;; *; : l 3.5;I;;3;Il
( 10 ; 90 < i
< 1 0 "26 < l
< 103337 < i;
< 10.3*: i < i3
< 10 3x i ( i
A .5 gm sample is digested with 2 ml of 3:l HCL/HN03
at 95 C for 90 min and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
5 3.2
;,5 2.1;
••'.5 3. l3
:: S 3.6:
X :; l
;x. 'i
x
XI
TSL/ASSAYEF T -boratories
1270 FEWSTER DRIVE. UNI1
PHONE It: ( 905)602-8236
Co ;;
ppm3
22;
30
4 li i;336
3l3
35V
31;
42"- 530
353;;l;iq
36':i::890
4831166
JISSAUOA.ONTARIO L4W-1A4
FAX tt: ( 905)206-0513
I.C.A.P. PLASMA SCAN
Aqua-Regia Digestion
44V3i' 37vy '4.. 0 2.6 930
504920 72: 2.5;ilbO
37.;;M390 92'-; 2.3 3:810
32-'3'34p 93
2 . 2 '3820
40 '.3:430 82' 2.338600
31'::-
3 1| lsi
430
29;- ;";4"OQ
25};
2033266
32||SfB
34:3:166
Cu
ppm
62
27
10
18.
30
24
28V
75
4 O'33 130; V7.;3 2 . 2;3-
45:13230 100 i ]'.ii-.p 2 .43
5731000 55; •4; 5 2.53V88P
58:;iip6 53V 4.2 2.633830
54;;V956 40 ;4;2 2.63:736
833
100:- •122
753
67-V
273
34'5
36:'
393
M "5;:6
100 :;3
2.5
.'.3;. 3
-73; 9
: ; ::.3V8
:;- 8
Mg
l. 7 ;
2 .0
2. 2;
2.4
2. 43
320
: : 280
s:.38p
;-95d
:710
2.0 .350
2. 5:33756
2.23:;:336
2 .43';:;750
2.431300
-:;;750
-720s
2.2
2 . 3 S'820
2.2 ::;3776 < 236;P2
2.4;
2.1*1 Mb:
2.p33;7gO
2. lHP'o
Mo ssNa';; Ni jvvP;-:;" pb
ppm ; *: v ppm;;;;;ppm ppm
2/0.03
2;.;fc.04'
2X0301
2x'6|oi
2 ::;0fpi
2XOiOl
45J1200
230;liPp
340' : ;.;:t'i|6
4iO;,;;;ft'48
49o5;il56
140ll700
340"l20b
5301:140
62o;;
630;
< l
< 1V:
< l;:
< l
< i3
< 1;:
( lv
ijpp < i !
86 < 1;;
72 ( l
< 2x6.01 < l"3 :iS;5
< l'V'VX.v'5
93;;i7'6p < i : 3.:c;5
16051700 < l;: :.:;|35
11 0'i 16^00
12b;;li36b
631000
--
6915200 < l*.
TSL/96 SIGNED
Se VSh:
ppm ; ppm ^
3 X 10
23 * 'i6
5 X IP
H3:x3:.lo
12 ^ 10
3 { 10
11 X 1Q
4'3! i-X-'.'.lp
io3*jlo
18:XVlp
263x3:ao
18;,X4'i0
16vi .lo
16 s;
143 10
12; C.ilO
14V.X.-.10
20 t 10
19; xi iq
i7.:;'yvio
is'lviq
i6;3p;l6
is'Svip
I33x"3io
;;X; :.1P
104
REPORT No.
Page No.
File No.
Date
s r o-.
ppm
130V
100;
140 :
32o :
200 V
120 3
220
140;';
3803
380 3
M8336
3 of 3
NV21MA
NOV-22-1996
v ;iv,w:3 Y 3
ppm ppn ppm;
13; < ip
3iVV 10
8jx :';10
713XV10
22o33|66 I9o3x3: :io
58o3.. ::87.6 i8olx3io
3;;
L80fx310 19;
43O3;5'fitp SfiSplo'
290V33;
1803:.:.;:::
286;33;li
40o3:::;';32
27o.,v;360
230:3-334
190;c'3!40
22a3ll33
230-:3i|^
270;'33s52
2 5 O; 311? 3
1803";';®
50;;;X.;:io i'.
36:3^ vio < i\;
38;;x3lp 3;"
130^310 r -
iooW; ;ip el
57.!xilp
6:;
Tp
s'i
5V
63
388
' 56
30
-33
4'2
; .'31
fft:
24o3v;322: 47fp|p 5^:72"
I40|ili7 293|p'i6 433;360
100p3;23 20;lp;K 4SBv37;
39V38M iiomp 53|| :57^
38;;;iqp:6 150iS:3iO 6'-;V;63
Z r
10.
4 30 11.
2 :'3.3:18 6V
53;,: 45 3;
4";:v3,6i i 4V
2":R; :;:64 B-'.
22
17.;.;

CAMECO G^ -,1. INC.
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENO
ENG
ENO
ENG
ENO
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ENG
ATTN: P. CHUBB
PROJ: ENOLISH
6W-4736-RG1
SAMPLE # Al
96D-650
96D-651
96D-652
96D-653
96D-654
96D-655
96D-656
96D-657
96D-658
96D-659
96D-660
96D-661
96D-662
96D-663
96D-664
96D-665
96D-666
96D-667
96D-668
96D-669
96D-670
96D-671
96D-672
96D-673
96D-674
96D-675
96D-676
96D-677
96D-678
96D-679
96D-680
96D-681
96D-682
96D-683
96D-6B4
ppm
:; x'/ 1 3.1
V :'X. 1' 3.5V -';
?:/^:/
SK- i
./;; ( : i
V/X/1
//x'l
vMi
//.x/i
v/U/x
v'8'x;;l
i/l';.:*
.//c-; i
vvx; i
/i*; 1
//x-i :
Ei
iS/1
•//Ci
SM:II
s//^!
S'i'f*
;As B ,..-;B* ' Be
ppm ppm; ppm ppm
15 < io;;v : i5 < i; ; :'-x/ 5
30 < 16;: 2 * i-lxv 5
;, : v.i 3 .7:-: /20 < io|/ ..7 < i?.; :;^ ; 5
v'/x/i 3.0 ;2b < loss. 3 < I///?; 5
JV'-tSl 3.5;/' 16 < io; :// 26 < i ';'/^': 5
-t;/'"^/'" :-./-- ^ -
/;-^i 4 ,3/y-x..
's < ioff;,2'6 < i v.:x;: 5
^•..'•Ti 3. s 20 < 10 62 < 1 < 5
I'/;*:' 1 2.4.T:-.', vlO < 10^/58 * 1 V, 5
- "i ; 4 t t:; ' - j/ 1 y
; X 1 2 . 6; < 5 < lbjs.;28 < i.'';' :x.- : 5
v':'-i:,i 3 . l/;';'^5 < lOv/'/Bo < 1,;..;,. ^';.
•;;:;*;x;l 2 . 8?: :^vS < 10v :;:'-;4.7. < l/vft^5
v':V;l 3 . 3.;/. Vi 5 ( lO/ffa's i il/'^' 5
//x "-i 3-D/? "*"i.:5 < 10.V/.170 i l . V : x 5
H "i'.\ 1 3 .2.V•X.::5
< lo'/ioo < i' c 5
;/ K.l 3.0^:: V20 ( io : v::;..;..7 < i//;* 5
3 .8;rH:
-S < 10/8/32 < i ;;.;-X--:5
3 .S/; ;x 5 < I0".';;i!5;48 < 1///X} ;5
. 2'"/
3 v/5 < io.fj':-62 ( i : /:/*; .5
3 • 3V x; 5 < 10.'-; Y/8 < l;;;::';x; -5
3 .5;V 30 < 10 x;l < l/ -x; 5
4 . 2 i;,.
4 .O';;;
4 .25-3
4 .88
3 .4"':
;;|; 5 (
H5 '
loA/so ( i//:-;'*'
lo;/^,;.! ( 1-J/-/X;'
2 .2'-;. ;x;'5 <
5
3 - 5ii/i:2b
<
;5
3 . 1;" ;-;.;36 < lO'/x/iZi < 1 ;::' ; 'x -,:5
3 . 3B/lo
< loliiso < i':;- v x" /5
4 .4* j/IP
< log/.';? ( l;V::--X;:
3 - 3 '::. :. loS/;;';^ < l//;'.^'
4 . 2':v'ixss
< 10v-3:';l < l'.V-.x' 'fs 5
4 . oif"20
< lo ;|x : ;i < ivivx; -'•5
3 .s'/: ;iSb < ip/R:.! < i;.;v : x.:
3 •'l-:
;":s
il? ' 10l!Vv ' IK-;X -
'.s
i'lo < io)v:(--"i < i./:.^
ifio < lO/:.;^ 1 < it:/ x' : "s" 5
*ib < 10 :; ;:;X 1 < 1 ,;;;;:.^
".5
SS& < lO'S^-'l < IVj/X
loK.*16 < l ::";:;';;x: ;5
A . 5 gm sample is digested with 2 ml of 3:1 HCL/HNO3
at 95 C for 90 min and diluted to 10 ml with DI H2O
This method is partial for many oxide materials
TSL/96
TSL/ASSAYEP T ^boratories
1270 FEWSTER DRIVE. UNIT
PHONE tt: ( 905)602-8236
Bi Co ; /Cr/: Cu
ppm ppm ppm
5
:5
::s :
3. s:; iSV'. I
V'k"!
7. 1! ;
3. i. : - /*:.:1
2. r; '-'x 71
5. 2 v;S*
4. 2 ; ;/^!
5. 0 X 1
7. .0 ( 1
3 . ,3 < "1
4. . 6; V,!:;!
fifi
3, .5;
3, .9; }: ::'*-'l
4. .9; Sx/l
2 . 1. ,;; '^ :;:; ]--
1 .9
xI*:S
vx'.:,:i
4 .3
3 . 1: //V .7" ""''i:: '1 -l
2
3 •6 /^;-l
5 .6
-;,' V/'V-: 1 . .v
3 •2;
4 .2
4 .8; 111
4 .9; iSiSt
4
i//1-
.4;
.B"
ill
3
5 •5j^fffial
5 • B; isSti
2 .4 s//.Xc-i
2 .3: llll
"•'..'^..•"•"••'•".-^
4 . 4: /•:-'.,x.:;i.
3 .7 :v:x":l
5 .4 ;v!*':;l
5 •liS-'/^./i
3 .6
/i;i
35.:-;:v;.|6
SS'S/l'fi
35:*v::' :32
39;
33
28
JISSAUGA.ONTARIO L4W-1A4
FAX tt: (905)206-0513
I.C.A.P. PLASMA SCAN
//.30
58
98
27 MOO
130,:
120/
Agua-Regia Digestion
62 7.6
100 b. t.
53 4.1
120: :;l;:7
88 /4.4
2B//1.SO ea.::-
i 3-8
323:17.0 110.;,
30-':;;;23;b 84;.;; "' 4 - 6
32:::;;iso 170;
37V*-lfl6 120;'.
28-196 57V
28 160 200
26V 240 52
33//18P 93 ;
29;'Sf4'p 48'5 3-5
31;V:17p 130V: ;4-T4
3lSii27.6 89v
36;' ::f;;140
43/ripO
24 o
93
;Fe Mg Mo
5-7
4,9
'"f-"3
s; o
4-9
1.9/1100
1.8/12PO
i. 9:;;iipo
1.8:v;830
1.9/1006
2.6li60
,! .9 1100
1.7. 910
1.8 920
1.9';-
l - 9;
1.9
/890
'S.7'20
/680
l.SvllOO
1.9. 1000
1.9; ilOO
1.9:3JMP
2.0/jfM
2.0/lppp
1.9:pfI(J
2.o;l2,6;6
2. i/liob
i. 3/1266
'--Ha;: Ni V/p"../ Pb :;v:::Sb.;: Se //Sri:;
:^;:/;; ppm; ppin ppm ppm ppm//ppm
< 2:0^05 53/186 <
2|p;o?
< 2/0^02
2;0i03
2 6;02
58
s iS
2 Di01 60
2 0.02 60
2 0.02 46
200
lab
180
280
70:4160
88/1966
120;V40
< 1
< l :
2/0*02 74-/120 ( X
170 < l
2/0.02 81- 320 < 1 ; -
120 < l
2x6;bi
2x'.6'fpi, :
140 1300 < l
i20 ;-;;'5pb:
//x/s
Ii:S::s
iiJI
/x 5.
IP's
'X/5
< i;;:S;X.g5
< I'/SIs
< i-lJls
94;v.lSO < 1:;;;I*|;5
iio/Sisp < iv*i;5
120:i|s'p < ll/ipl
130|i:1.6.P < 1:S1':|
26o;;pio < i;5|i;5
leoSs'o < i:ifflfc|
72';S2'ob < l'-1x5-5
2710/10
41;X 10
33; t 10
24VX..10
io|p;ip
12W 10
is;
IB!
19/
fcio
x;' ^'lo 16
^ 10
REPORT No.
Page No.
File No.
Date
6531400
69/1660
70/2200
71/22,66
68;14PP
51 1266
81 9lb
90 ;740
833:2100
48 2300
M8354
l of 3
NV25MA
NOV-26-1996
V V/W'V: Y
ppm;*:: ppm pp
i* gio
130;
180; ;x";lb
isjx/lp eoijaop 130/xfip
l3;;U*lb ISOilSOp I20'7x.lp
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ATTN: P. CHUBB
PROJ: ENGLISH
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ENG 96D-686
ENG 96D-687
ENG 96D-688
ENG 96D-689
ENO 96D-690
ENG 96D-691
ENG 96D-692
ENG 96D-693
ENG 96D-694
ENG 96D-695
ENO 96D-696
ENO 96D-697
END 96D-698
ENG 96D-699
ENO 96D-700
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ENG 96D-702
ENG 96D-703
ENG 96D-704
ENG 96D-7O5
ENO 96D-706
ENG 96D-707
ENO 96D-70B
ENG 96D-709
ENO 96D-710
ENG 96D-711
ENG 96D-712
ENG 96D-713
ENG 96D-714
ENG 96D-715
ENG 96D-716
ENG 96D-717
ENG 96D-718
ENG 96D-719
i, INC.
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PROJ: ENGLISH
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PHONE #: (905)602-8236
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Ministry of
Northern Development
and Mines
Personal information collected on this form i * ^'--
Mining Act, the inform ............,,,,..m
Questions about this
933 Ramsey Lake Roi
Instructions: - F
-P
e 2 17439 ENGLISH
- -- K"" 1 "' inK -
1. Recorded holder(s) (Attach a list if necessary)
Name
Address
L3R SV4-
Name
Address
Declaration of Assessment Work
Performed on Mining Land
Mining Act, Subsoctlon 65(2) and 66(3), R.S.O. 1990
900
Client Number
Transaction Number (office use)
Assessment Files Research Imaging
l 66(3) of the Mining Act. Under section 8 of the
vork and correspond with the mining land holder.
Northern Development and Mines, 6th Boor,
, use form 0240.
Telephone Number
C*)* S) t-77-WS
Fax Number
OeO If 77- 99S;
Client Number.
Telephone Number
Fax Number
2. Type of work performed: Check ( ^ ) and report on only ONE of the following groups for this declaration.
Work Type
Geotechnical: prospecting, surveys,
assays and work under section 18 (regs)
Dales Work t ft Q X -r n Q/
Performed From IO , ^ To l " l
Day Month | Year Day [ Month | Year
Global Positioning System Data (if available) Township/Area
M or G-Plan Number
Physical: drilling, stripping,
trenching and associated assays
Commodity
Office Use
Total $ Value of ,, ^
Work Claimed 7 73 "H- ^
NTS Reference
Q] Rehabilitation
Mining Division "*~ y '' '''- ^ t'lk r^.
Resident Geologist
District ""/"/M*.*/!,":,
Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;
- provide proper notice to surface rights holders before starting work; " : - ;'"'
- complete and attach a Statement of Costs, form 0212;
- provide a map showing contiguous mining lands that are linked for assigning'work;
- include two copies of your technical report. , . .. , ;- ;-;.:,,,,
3. Person or companies who prepared the technical report (Attach a list if necessary)
Name
Pefre^ C \**\*\* L Ca^er* Corf-}
Address
Name
Address
Name
Address
4. Certification by Recorded Holder or Agent
Telephone Number
C"7*s) 57.J- t^-syj - u
Fax Number ; c ;
Telephone Number '
r ' i
Fax Number
' " ' - ' .-:'. ! ..i
Telephone Number , : . i
Fax Number
AUf3 " " ^
l. rewev C-nubb do hereby certify tl L4, havejfifsorial ^nbwiedge of the facts set
IPrlnl Name)
forth in this Declaration of Assessment Work, having caused the work to be performed or witnessed the same during
or after its completion ancHto the best of /r/ knowledge, the annexed report is true.
Signature of Recorded Date
Agent's Address
keU^ltt.
Telephone Number
- U.CCC
Fax Number

Ontario
Ministry ol
Northern Development
and Mines
Mlnlstere du
Developpement du Nord
et des mines
Statement of Costs
for Assessment Credit
Etat des couts aux fins
du credit devaluation
Mining Act/Lol sur les mines
Personal information collected on this form is obtained under the authority
of the Mining Act. This Information will be used lo maintain a record and
ongoing status of the mining clalm(s). Questions about this collection should
be directed (o the Provincial Manager, Minings Lands, Ministry of Northern
Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Onlario
P3E 6A5, telephone (705) 670-7264.
1. Direct Costs/CoQts directs
Type
Wages
Salalres
Contractor's
and Consultant's
Fees
Drolls de
('entrepreneur
et de I'expert-
consell
Supplies Used
Fournltures
utlllsles
i
Equipment
Rental
Location de
materiel
Description
Labour
Main-d'oeuvre
Field Supervision
Supervision sur le terrain
Type
D,, U G~W^
Type
Type
Amount
Montan)
So8 5
So^
O 031
68^07
Total Direct Costs
Total des coQts directs
Totals
Total global
nmr
S 14-3??
11^07 i
Note: The recorded holder will be required to verify expenditures claimed in
this statement of costs within 30 days of a request for verification. If
verification is not made, the Minister may reject for assessment work
all or part of the assessment work submitted.
,
Transaction No./N" de transaction
Les renseignomenls personnels contenus dans la presente formula sont
recuoillis en vertu de la Lot sur lea mines et servlront a lenlr a jour un reglslre
des concessions mlnieres. Adresser (oule queslton sur la collece de ces
ronseignements au chef provincial des terrains mlnlers, ministers du
Developpement du Nord et des Mines, 159, rue Cedar, 4e etage. Sudbury
(Ontario) P3E 6A5. telephone (705) 670-7264.
2. Indirect Costs/Couts indlrects
Note: When claiming Rehabilitation work Indirect costs are not
allowable as assessment work.
Pour le remboursement des travaux de rehabilitation, les
couts indirects ne sont pas admissibles en tant que travaux
devaluation.
Type
Transportation
Transport
Food and
Lodging
Nourrilure et
hebergemcnt
Mobilization and
Demobilization
Mobilisation et
demobilisation
Filing Discounts Remises pour depdt
1. Work filed within two years of completion is claimed at 100 07o of
the above Total Value of Assessment Credit.
2. Work filed three, four or five years after completion is claimed at
500A) of the above Total Value of Assessment Credit. See
calculations below:
Total Value of Assessment Credit Total Assessment Claimed
x 0.50
Certification Verifying Statement of Costs
l hereby certify:
that the amounts shown are as accurate as possible and these costs
were incurred while conducting assessment work on the lands shown
on the accompanying Report of Work form.
that as P-
(Recorded Holder, Agent, Position in Company)
to make this certi DECEIVED
AUG O 5 1997
. , - -,
t ! " , ~ ~ '".
GEOSCIENCE ASSESSMENT
Type
Description
50n^v*ii(A.
Amount
Montant
|7o *
"r-oo
Sub Total of Indirect Costs
Total partlel des couts Indlrects
Amount Allowable (not greater than 20H of Direct Costs)
Monlant admissible (n'excedant pas 20 H des couls directs)
Total Value of Assessment Credit Valeur totale du credit
(Total of Direct and Allowable devaluation
InrilrAcl eofttnl (Total dal codta dlraela
t Indirect! admissible!
Totals
Total global
r-'. "'
- * i, .1 ~. , .
!HN#*-;V
^i'pJ-S
•tit^^i'
•fZ\.o, f '
^370??
Note : Le litulaire enregistrd sera tenu de verifier les depenses demandees dans
le present etat des couts dans les 30 jours suivant une demands a cet
effet. Si la verification n'est pas effectuee, le ministre peut rejeter tout
ou une partie des Iravaux devaluation presentes.
1. Les travaux deposes dans les deux ans suivant leur achevement sont
rembourses a 100 "ft de la valeur totale susmenlionnee du credit d'evaluatton.
2. Les Iravaux deposes trois, quatre ou cinq ans apres leur achevement
sont rembourses a 50 "ft de la valeur totale du credit devaluation
susmentionne. Voir les calculs ci-dessous.
Valeur totale du credit devaluation
X 0,50 ~
Attestation de l'6tat des coQts
Evaluation totale demandee
J'atteste par la presente :
que les montants indiques sont le plus exact possible et que ces
defenses ont ete engagees pour effectuer les travaux d'evaluatlon
sur les terrains indiques dans la formule de rapport de travail ci-joint.
l am authorized Et qu'a litre de je suis autorise
(titulaire enregistre, representant, poste occupe dans la compagnle)
a faire cette attestation
Signature Date
/T7

5.' Work to be recorded and distributed.
the mining land where work was performed,
must accompany this form.
Mining Claim Number. Or if
work was done on other eligible
mining land, show In this
column .the location number
indicated on the claim map.
eg
eg
eg
1
2
3
4
5
6
7
8
9
10
11
,12
13
14
15
TB 7827
1234567
1234568
HH-7Z-72.
ussSSff
IISSS9I
HSS88^
JI5S210
Number of Claim
Units. For other
mining land, list
hectares.
16 ha
12
2
1
1
1
1
.1
Column Totals
Work can only be assigned to claims that are contiguous (adjoining) to
at the time work was performed. A map showing the contlguousjlnk; 'i
' ' ' ' "' '
Value of work
performed on this
claim or other
mining land.
-
S26, 825
0
$ 8, 892
"M-if 6*,
"2-1 O H 0
V730M-
II ^ T-O
*\ Wo
Value of work
applied to this
claim.
N/A
S24,000
S 4 ,000 -
O
o
o
0
- 0
o
Value of work
assigned to other
mining claims.
S24,000
0
0
' "" O "
. ( "
o
o
o
0
o
Bank. Value of work
to be distributed
at a future dale.
.-r..' ' - "- '
$2,825
' '.O T '
$4,892
f .1.4-^65^
^2.1 O H-O S
-i7^otfX
nq^o/
^8o~
J - ' ( * .. ,
. ' -i..; ' i":-;- ' J !
~f ' 'i" rv .-.* '
. ' . .'..'.- - ",, -'. -'
13.7^
l, , do hereby certify that the above work credits are eligible under
(Print Full Name)
subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to
the claim where the work was don
Signature of Recorded Hoi in Writing Date
6. Instructions for cutting back credits that are not approved.
Some of the credits claimed in this declaration may be cut back. Please check ( v ) i n the boxes below to show how
you wish to prioritize the deletion of credits: . "'
D 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated. '.'.'-Y.n
D 2. Credits are to be cut back starting with the claims listed last, working backwards; or.
D 3. Credits are to be cut back equally over all claims listed in this declaration; or .
D 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe); lV" "
Note: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first,
followed by option number 2 if necessary.
For
Rece
Office Use Only ' r,, o ,.,., ri. .
Deemed Approved Date ' : Dale. Notification Sent 'i .
"RECEIVED
AUG 0 5 1997
/" ; fi- 1 '
GFDRPIFMre ACCCCCHTMT
/' ;
Date Approved
Appioved lor Recording by Mininq Recorder (Signature)
.' - ' t
Total Value of Credit Approved
;-;; . . -', f - i;; .

Ministry of
Northern Development
and Mines
August 6, 1997
TRI ORIGIN EXPLORATION LTD.
8901 WOODBINE AVE.
SUITE 114
MARKHAM, Ontario
L3R-9Y4
Dear Sir or Madam:
Subject: Transaction Number(s):
Ministere du
Ontario
Developpement du Nord
et des Mines
Geoscience Assessment Office
933 Ramsey Lake Road
Status
W9760.00180 Approval After Notice
6th Floor
Sudbury, Ontario
P3E 6B5
Telephone: (888)415-9846
Fax: (705) 670-5863
Submission Number: 2.17489
We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The
attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS
SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.
If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any
steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the
Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day
Notice.
Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the
response date on the summary.
If you have any questions regarding this correspondence, please contact Lucille Jerome by e-mail at
jeromej@torv05.ndm.gov.on.ca or by telephone at (705) 670-5858.
Yours sincerely,
ORIGINAL SIGNED BY
Blair Kite
Supervisor, Geoscience Assessment Office
Mining Lands Section
Correspondence ID: 11160
Copy for: Assessment Library

Submission Number: 2 .17489
Work Report Assessment Results
Date Correspondence Sent: August 06, 1997_____________________AssessorLucille Jerome^^^^^^^^^^^^^^^^^^^
Transaction First Claim
Number Number Township(s) l Area(s) Status Approval Date
W9760.00180 1147272 ENGLISH Approval After Notice August 06, 1997
Section:
10 Physical PDRILL
The revisions outlined in the Notice dated July 25,1997, have been corrected. Accordingly, assessment work credit has been approved as outlined on the
attached Assessment Work Credit Form.
Correspondence to: Recorded Holder(s) and/or Agent(s):
Resident Geologist Peter Chubb
South Porcupine, ON SUDBURY, ONTARIO
Assessment Files Library TRI ORIGIN EXPLORATION LTD.
Sudbury, ON MARKHAM, Ontario
Page: 1
Correspondence ID: 11160

Distribution of Assessment Work Credit
The following credit distribution reflects the value of assessment work performed on the mining land(s).
Date: August 06, 1997
Submission Number: 2.17489
Transaction Number: W9760.00180
Claim Number Value Of Work Performed
1155888 21,040.00
1155889 11,420.00
1155890 9,480.00
1155891 37,304.00
1147272 14,465.00
Total: S 93,709.00
Page: l
Correspondence ID: 11160

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G-3938 ENGLISH TWP G-3938

DATUM Om
-50
-100
-150
-200
-250
Line 6+OOE
o
DDH ENG9604
-45' , 135'
DEL.ORO GROUP
FeisJc Volcanics
DELORO GROUP
Felsic Volcanics
* Trench Maps (Chubb, 1996)
Shallow but strong I.P.
\\ \ \
\ \
\\ ENG9603
" '"
Chakotay Trench
' "~~ —' ~2^1i ZS
^•tt^Kii^fe^
DDH ENG9603
, 315'
o
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P L A
1155891 Tl
Ultr
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,' — .vj .- , \ •••.j-1' ^V5 -. t'ra*^

N VIEW
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tramafic Volcanics
z:
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^v^^ig^^''. "'
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Chubb, P.O., Faber, A., and Thomas, D., 1996. 1996 Trenching Report - English
Property, Ontario. English and Semple Toumships. Cameco Corp., P.27.
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1
TISDALE GROUP
Mafic Volcanics 1155889
o
^-4
ffSDALE GROUP
Mafic Volcanics
Qtz-feldspar Phyric Felsic Dike (10cq)
Syenite Dike (9e)
Sulphide-oxide Iron Formation (6d,6b)
Graphitic Argillite (5dp)
-e
ENG9601
DDH ENG9601
-45' . 315'
Tisdale Ulramafics - Fuschite altered (4ad,4a,4d)
Deloro Felsic Volcanics (3ae,3d)
Tisdale Mafic Volcanics (1aj\1)
Unknown
Overburden
Claim Line
Foliation
Fuchsite Alteration
Camgco
O
O
SE
DATUM Om
-50
-100
-150
-200
4JA03SEOQ262 17489 ENGLISH 220
-250
ENGLISH
PROJECT
ry ft ^ Q
^ 4i w v
1996 DIAMOND DRILL SECTION
Compiled By. Peter Chubb 97/01/28 Dwg No.:ENG96Q18
Drafted By: CAD Deportment
Scale: 1:500
Map 2
N.T.S.: Datum:
Dispositions): 1155891.1155890.1155889