32E04SE0035 - Geology Ontario

32EMSE0035 OM91-138 ABBOTSFORD 

010 

H.T.S.:- 32 E/4 

RPT. NO. S-91-8 

Latitude: 49 04 

Longitude:79 45 

EXPLORATION REPORT 

ON THE 

LA REINE RIVER PROPERTY 

HEPBURN TOWNSHIP 

NORMETAL AREA 

LARDER LAKE MINING DIVISION 

ONTARIO 

FOR 

SEAL RIVER EXPLORATIONS LIMITED 

F.J. SHARPLBY DECEMBER 1991

32E04SE0035 OM91- 

01OC 

TABLE OF CONTENTS 

PAGE 

SUMMARY 

1.0 INTRODUCTION 7 

2.O PROPERTY 7 

2.1 Claims 7 

2.2 Location and Access 8 

2.3 Topography 9 

3.0 EXPLORATION HISTORY 10 

3.1 Regional History 10 

3.2 Property History 11 

3.3 Recent Regional Activity 12 

4.0 GEOLOGY 14 

4.1 Regional Geology 14 

4.2 Property Geology 14 

5.0 MINERALIZATION 16 

5.1 Regional Mineralization 16 

5.2 Property Mineralization 17 

6.0 MAGNETOMETER SURVEY 18 

7.0 INDUCED POLARIZATION SURVEY 20 

8.0 DISCUSSION OP RESULTS 21 

9.0 CONCLUSIONS AND RECOMMENDATIONS 23 

10.0 REFERENCES AND SELECTED BIBLIOGRAPHY 25 

11.0 CERTIFICATE OF QUALIFICATIONS: F.J. SHARPLEY 27

Appendix I: LIST OF FIGURES page 28 

Figure I: 

Figure 2: 

Figure 3: 

Figure 4: 

Location Map 

Claim Map 

Abitibi Subprovince of the Archean Superior Province 

Grid map 

Appendix II: 

Proposed Diamond Drill Holes 1992 

29 

Appendix III 

Detailed Budget Proposal 

31 

Appendix IV: 

Project Expenditures 

33 

Appendix 

Dwg. No. 

S-91-8-01 

S-91-8-02 

S-91-8-03 

S-91-8-05 

List of Maps 

Magnetic Survey: Total Field Readings 

Magnetic Survey: Total Field Profiles 

Topography 

Geophysical Compilation 

41 

Scale 

1:10,000 

1:10,000 

1:10,000 

1:10,000 

Appendix VI: Assays 42 

Appendix VII: Instrument Specifications 43 

List of Maps in Pocket 

Dwg. No, 

S-91-8-04 

S-91-8-01 

S-91-8-02 

S-91-8-03 

S-91-8-05 

Scale 

Compilation Map 1:10,000 

Magnetic Survey: Total Field Readings 1:5,000 

Magnetic Survey: Total Field Profiles 1:5,000 

Topography 1:5,000 

Geophysical Compilation 1:5,000

SUMMARY 

The La Reine River Property consists of 62 contiguous, nonpatented 

mining claims situated in Hepburn Township, Ontario 

along the Normetal-Ligneris greenstone belt which forms part of 

the Abitibi Subprovince of the Archean Superior Province of the 

Precambrian Shield. 

This greenstone belt is considered to be Hunter Mine Group 

(2708my) in age (OGS Hap 2484) consisting of an assemblage of 

mafic to felsic metavolcanics, metasediments and igneous rocks 

which are bordered by granitic batholiths. Diabase dikes are 

interpretated to cross the area in a northeast direction. 

The property was flown in March of 1988 by Aerodat Limited using 

their helicopter borne electromagnetic and magnetic system along 

lines at 100 metre intervals. During 1990 a total of 13.5 km of 

linecutting, magnetometer and induced polarization surveys, 

geological mapping, gold in humus geochemistry and one diamond 

drill hole was completed totalling 256 metres. 

During the present program in 1991 the old baseline was extended 

from 30E to 54E. A total of 12.6 km of linecutting and a 

magnetometer survey was carried out along the baseline and 

crosslines at 200 metre intervals from 36E to 54E. An induced 

polarization survey totalling 8 km was carried out on lines at 

200 metre intervals from 36E to 50E.

The Hepburn Fault zone is indicated by anomalous local magnetics 

and induced polarization zone No. 3 from line 25E to 48E which is 

a resistivity low with associated weak frequency effect and metal 

factor that may be disseminated pyrite. This zone on the Aerodat 

airborne is represented by a resistivity low. Diamond drill hole 

Mo. RR-90-1 investigated the IP anomaly No. 3 and intersected the 

shear zone on section 24B. The drill hole indicated a highly 

sheared zone over a width of 50 metres with low gold values but 

strong alteration (silicification: 7^, pyritization: 2-4% and 

garnetization: 3%) and numerous grey feldspar porphyry dikes on 

footwall and hangingwall. Grab samples from outcrop along the 

Hepburn Fault Zone on line 46E at 2+62N returned values of 96 and 

41 ppb Au. The outcrop is strongly sheared with strong 

silicification, pyritization (S-5%) and contains banded quartz. 

Induced polarization anomaly No. l south of the baseline extends 

from 15E to 50E as a resistivity low with good response on the 

frequency effect, metal factor and magnetic correlation in part. 

The cause of the anomaly is possibly disseminated sulphides and 

or magnetite in a mafic tuff. Gold in humus geochemistry from 

line 15E to 30E returned negative results. 

An exploration program of geological mapping, gold in humus 

geochemistry and three diamond drill holes totalling 450 metres 

is recommended to test the two induced polarization anomalies

6 

from 36E to 54E for gold mineralization. This Includes 

investigating the IP anomaly No. 3 and the mineralized altered 

outcrop on line 46E along the Hepburn Fault Zone; and the IP 

anomaly No. l in possible mafic tuff along the volcanosedimentary 

contact for gold mineralization. 

The expenditures for the recommended exploration program on the 

La Reine River Property are estimated at $ 46,250.

1.0 INTRODUCTION 

Geophysical ground surveys have been completed that were 

partially funded under Ontario Mineral Incentive Program (OHIP) 

and the Ontario Prospectors Assistance Program (OPAP) by Lesley 

Blain on the La Reine River Property, Hepburn Township, Province 

of Ontario. The geophysical ground program was designed to 

investigate the Hepburn shear zone with IP and magnetometer 

surveys as indicated on the Aerodat helicopter borne 

electromagnetic and magnetic system by a series of resistivity 

lows. 

The Induced Polarization survey was carried out by Remy Belanger 

from December 18 to 21, 1991 and the magnetometer survey by Fred 

Sharpley from December 17 to 30, 1991. 

2.O PROPERTY 

2.1 Claims 

The La Reine River property consists of 62 contiguous, non- 

patented mining claims located in Hepburn Township in the Larder 

Lake Mining Division of Northeastern Ontario. 

The claims appear on claim map M-500 and are shown on Figure 2 

and numbered as follows:

8 

L-954528 to L-954531 Inclusive 

L-954542 to L-954546 Inclusive 

L-954870 to L-954873 inclusive 



L-1185946 (16 units) 

The claims total 2480 acres or 1003.62 hectares and are 

registered in the name of Seal River Explorations Limited. 

Claim block L-1185946 consisting of 16 units was recorded on 

December 17,1991. 

2.2 Location and Access 

The property is located 103 kms (64 mi) east of Cochrane, Ontario 

in Hepburn Township: 24 kms (15 mi) north of Lake Abitibi and 3 

kms (2 mi) west of the Ontario-Quebec border. The Cochrane-La 

Sarre Highway (Ontario 652 or Quebec 111) is an all weather 

highway and 

provides access to the central part of the property; 

a distance of 3.5 kms (2 mi) by four wheel drive from the main 

highway at mileage 111. The turn-off from the Patten River road 

is at 7 kms where an old road extends to old Camp 24. The area is 

accessible by helicoper from La Sarre, a distance of 48 kms

(30 mi) to the southeast. By road the property is 47 kms (29 mi) 

from Normetal or 68 kms (42 mi) from La Sarre. 

9 

2.3 Topography 

The topography on the property is gently rolling with outcrop 

knolls and sand, gravel forming ridges less than 15 m (50 ft). 

The outcrop areas form less than l percent of the area. The 

swamps form the 60 percent of the property. The forest cover is 

mainly spruce. The soil cover is mainly clay with local areas of 

sand, gravel and boulders between the swamps. 

The area has been cut over by AP&P and is undergoing second 

growth. 

There are a few small intermittent streams on the claim group. 

Water for drilling purposes is probably available from the small 

lakes and ponds on the property or from the La Reine River. 

The climate is typical 

of northern Ontario with snow cover and 

cold weather from mid November until May.

10 

3.0 EXPLORATION HISTORY 

3.1 Regional History 

The first geological observations were recorded in 1901 by 

Coulthard, Tanton 1919, Hopkins 1918, Knight 1919, Mavdsley 

1930, Flaherty 1839 and Thompson 1937. Since the 1920's, 

prospectors and mining companies have shown great interest in the 

region, chiefly because of the proximity to the Normetal mine 

which is 10 miles to the east of the La Reine River property. The 

Normetal mine produced 12 million tons grading 2.20 % Cu and 5.20 

* Zn with 1.4 OPT Ag and 0.02 OPT Au (NM 1989). The mine is now 

shut down. 

The area was mapped geologically by S.B. Lumbers of the O.G.S. 

(O.D.H. Geological Report No. 14; Map 2025; South Patten River 

Area) in 1963 on a scale of 1"-1X2 mile. 

The area was mapped again in 

(Map 2453) on a scale of 1:100,000. 

1978 by G.W. Johns of the O.G.S. 

The airborne magnetic map 2366 G by the 

area. 

G.S.C.-O.D.M. covers the 

The airborne magnetic and electromagnetic survey of the Detour- 

Burntbush-Abitibi Area was carried out by the Ontario Geological 

Survey in 1989.

11 

3.2 Property History 

Canadian Superior Explorations Limited in 1966 carried out ground 

horizontal loop electromagnetic surveys over a grid on the 

northwest edge of the property and drilled nine diamond drill 

holes to test anomaly No. A-4 in Adair Township. The anomaly was 

caused by massive to disseminated pyrrhotite and pyrite in felsic 

tuffs. 

Gold Hill Resources Inc. in 1984 explored the extension of 

Anomaly No. A-4 in Adair Township with two diamond drill holes. 

Keldor Resources Inc. in 1987 drilled 27 reverse circulation 

holes east of the La Reine River property on strike in Hepburn 

Township adjacent to the Quebec border. Hole No. 42 on claim 

906492 on the boundary of the La Reine River property returned an 

assay of 14045 ppb Au in a basal till sample containing three 

grains of gold. The drill hole is located adjacent to the 

volcanic-sedimentary contact (Compilation Map: S-91-8-05). This 

sample did not have the delicate grains of gold but Hole Nos. 41 

and 59 contained two and one delicate grains in basal till 

samples respectively adjacent to the volcanic-sedimentary 

contact.

12 

In 1988 the Seal River Explorations Limited property was flown by 

Aerodat Limited using a combined helicopter borne magnetic and 

electromagnetic and VLP survey using a three frequency E.M. 

system with lines spaced at 100 metre intervals. 

The combined magnetic and electromagnetic survey of the Detour- 

Bur ntbush-Abitibi Area flown by the O.G.S. in 1989 with 200 metre 

lines covers the La Reine River property on Map 81228. 

Seal River Explorations Limited in 1990 carried out 13 line km of 

induced polarization and 13.5 line km of magnetometer surveys, 

geological mapping and limited gold in humus geochemistry. 

Seal River Explorations Limited drilled one diamond drill hole 

for a total of 256 metres in late 1990. 

3.3 Recent Regional Activity 

The Casa Berardi-Normetal greenstone belt has undergone extensive 

activity since 1984. The 

Golden Pond discoveries by Inco-Golden 

Knight in Casa Berardi Township started production in 1988 with 

reserves of 10 million tons grading 0.22 OPT Au (Canadian Mines 

Handbook - 1988-89). 

The companies currently active in the Normetal area on the

13 

Ontario side ace Cominco Limited, 

Noranda Explorations Limited 

and BPH-Utah who drilled 15 diamond drill holes in Abbotsford 

Township in late 1991. 

Cominco Limited in joint venture with Exploration Miniere 

Normetal Inc. 

is currently re-examining the Normetal property in 

Desmeloizes and Perron Townships for base metals. Geological 

Reserves are stated at 431,000 tons grading 12% Zn and l OPT Ag 

(Canadian Mines Handbook 1988-89).

14 

4.O GEOLOGY 

4.1 REGIONAL GEOLOGY 

The La Reine River property Iles along the Casa Berardi-Normetal- 

Lignerls greenstone belt which forms part of the Abitibi 

Subprovince, Superior Province of the Precambrian Shield. 

The greenstone belts north of the Destor-Porcuplne Fault are 

considered to be Hunter Mine Group, Cycle II; the Kidd Creek 

rhyolites are 2702 my. (OGS Map 2484 - 

the Abitibi Subprovince). 

Lithostratigraphic Map of 

The Casa Berardi Fault extends through the northern part of the 

area. The Abitibi Fault extends through the southern part of the 

area. The Privat-Launay Fault extends through the Normetal area. 

A swarm of northeastern trending diabase dikes extend through the 

Abitibi-Normetal area. 

4.2 Property Geology 

The La Reine River property lies near the southwestern boundary 

of the Casa Berardi-Normetal greenstone belt which forms a part 

of the Abitibi Subprovince, Superior Province of the Canadian 

Shield (Figure 3).

15 

The La Relne River portion of the greenstone belt consists of an 

assemblage of mainly mafic with minor felsic metavolcanics, 

metasediments and igneous intrusive rocks which are bordered by 

granitic batholiths. The rocks strike southeast and dip steeply 

northeast in all parts of the area. 

The La Reine River property is underlain by mafic metavolcanics 

in the central part of the property with minor felsic to 

intermediate tuffaceous rocks. The metasediments composed mainly 

of greywacke and calc-silicate rock predominate in the southern 

part of the property. The Patten River Pluton which is 

granodiorite in composition borders the northeast edge of the 

property. 

A strike fault (Hepburn Fault) crosses the central portion of the 

property. 

Metamorphism of the flow rocks has produced fine to mediumgrained, 

amphibole-rich metavolcanics ranging in color from grey 

or pale green to dark greenish black metamorphosed basaltic and 

andesitic flows. Most of the flow rocks are foliated and exhibit 

volcanic structures recognized as massive, amygdaloidal, 

pillowed, diabasic or gabbroic, and porphyritic types (Lumbers 

1963). Felsic metavolcanics consist of flow, tuff, lapilli-tuff, 

pyroclastic breccia, and tuff breccia.

16 

5.0 MINERALIZATION 

5.1 Regional Mineralization 

Base metal mineralization at the Normetal mine Is in a lenticular 

body of massive sulfldes comprising mostly pyrite, chalcopyrite 

and sphalerite. The deposit is in a shear zone striking N 65 W 

and dipping 80 NW in felsic tuffs and agglomerates. It is cut by 

the north trending diabase dike. The Normetal mine produced 12 

million tons grading 2.20 % Cu and 5.20 * Zn with 1.4 OPT Ag and 

0.02 OPT Au. The mine is now shut down (NM 1989). The present 

reserves as listed by Normetal Mining Exploration Inc. in the 

Canadian Mines Handbook - 1991-92 are 431,000 tons averaging 12 * 

Zn and l OPT Ag. 

Gold mineralization in the Casa Berardi area is stratabound 

associated with pyrite, arsenopyrite, quartz veining and 

sericite-carbonate alteration in a volcano-sedimentary 

environment (Descarreaux 1984). 

Gold mineralization in the Ligneris area is stratabound 

associated with disseminated pyrite in a felsic volcanic 

environment.

17 

5.2 Property Mineralization 

Vary little outcrop has been observed on the property. The 

airborne geophysics indicates the rocks in the central portion of 

the property have been depleted in iron probably due to the 

closeness of the granodiorite pluton. 

The Hepburn Fault Zone traverses the central part of the property 

at 40 degrees and dips northeast at 70 degrees. In hole No. RR- 

90-1 the fault is a highly altered shear zone over a width of 50 

metres. The hangingwall and footwall of the shear zone contain 

numerous narrow grey feldspar porphyry dikes. The alteration 

consists of silicification, pyritization (2-4%) and garnetization 

(3%). A whole rock analysis and an ICP analysis of one sample 

from DDH No. RR-90-1 from 171.69 to 172.39 metres (sample No. 

9770) indicated high silica (71*), alumina (12.6*) and ferrie 

iron (4.09*). High trace elements are chromium (458ppm), barium 

(869ppm), zirconium (196ppm), Y (45ppm), SR (90ppm) RB (39ppm) 

and NB (32ppm). The gold assays from the drill core were very low 

with a peak value of 12 ppb. 

Grab samples from outcrop on line 46E at 2+62N returned values of 

96 and 41 ppb Au. The outcrop is strongly sheared with strong 

silicification, pyritization (3-5*) and contains banded quartz. 

A whole rock and an ICP analysis of this sample No. 2 indicated 

high silica (75.69*) and ferrie iron (12.15*); and low in soda

18 

U.05%), potash (0.31*), magnesia (Q.85%) and lime (G.72%). High 

trace elements are chromium (1034ppm) and manganese (721ppm).

19 

6.0 MAGNETOMETER SURVEY 

The old baseline was extended from 30E to 54E with stations 

established at 25 metre intervals. Crosslines were established at 

200 metre intervals from 36E to 54E (eg. 36E, 38B, 40E, 42E, 44E, 

46E, 48E, 50E, 52E and 54E). A proton total field magnetometer 

survey was carried out over this grid. 

A Geometric G-816 

proton total field magnetometer with direct 

readout was used for the survey. Magnetic diurnal variations 

were monitored by establishing base stations at 25 metre 

intervals along the baseline. Readings were taken along grid 

lines spaced at 200 metre intervals with stations spaced at 12.5 

metres along the line. Magnetic diurnal variations were monitored 

by looping lines and checking into established baseline base 

stations (at the intersection of baseline and crosslines) at 

intervals of less than one and one half hours. Approximately 12.6 

line kilometers of data were recorded in this way. 

Corrections to the magnetic field values recorded during the 

field 

survey were made using the approximate time and diurnal 

change information. A regional value of 58,000 gammas was 

subtracted from all the corrected magnetic values. The values 

were then plotted at a scale of 1:5000 and profiled along the 

line using a base of 58,400 gammas. A separate magnetic value and 

profile map was produced and then reduced to a scale of 1:10,000

20 

(see Map S-91-8-01, 02). To correlate with the old survey a value 

of 100 gammas was added to the new readings. The baseline from 

30E to 50E and the corresponding crosslines were read on December 

17 and 18,1991. The baseline from 50E to 54E and the 

corresponding crosslines were read on December 30,1991.

21 

7.0 INDUCED POLARIZATION SURVEY 

Remy Belanger carried out a dipole-dipole induced polarization 

survey over a 200 metre grid system. A total of 8.0 kms of 100 

metre spreads n^ to n-4 was used with .25 and 4.0 hertz 

frequencies. A Phoenix I.P.V-1 receiver and a I.P.T-1 transmitter 

was used to carry out the survey with a generator of 2.0 kw. 

The data is presented in a separate report by Remy Belanger as 

pseudo-sections of the calculated apparent resistivity and 

percentages of frequency effect. Plan maps are presented as 

surface projections of the interpretated I.P. anomaly zone, 

frequency effect of n=2 / 

factor of n=2. 

apparent resistivity of n z 2 and metal 

The induced polarization survey was carried 

out during December 

1991. Lines 36E, 38E, 40E, 42B, 44E, 46E, 48E and 50E are 

presented in a separate report by Remy Belanger.

22 

8.0 DISCUSSION OF RESULTS 

The regional magnetic background across the areas surveyed is 

approximately 58,500 gammas. Investigation of a series of Aerodat 

airborne resistivity lows resulted in the following I.P. 

anomalous zones: 

Anomalous Zone f l (H-l) 

Anomalous zone fi from line 30E to 50E at 0+50S to 2+OOS 

indicates a good response on the frequency effect of up to 2.9% 

in a low resistivity zone with an average metal factor of 10. 

Magnetic correlation is mainly on the flank of the IP anomaly of 

up to 1200 gammas above background. The best response is on line 

40E from 23 to 3S and on line 48E from 0+50S to 2S. This IP 

anomaly is the continuation of the same anomaly from line 15E to 

30E on the old grid. 

Anomalous zone 13 (Hepburn Fault Zone) 

The No. 3 zone is possible anomalous from 36E to 40E at 

H-50N to 

3N and from 46E to 48E at 3N. The frequency response varies from 

Q.3% to 1.1\. The metal factor varies from 1.1 to 1.8. The best 

metal factor 

response is on line 46E at 3N and on 36E at 2N. The 

resistivity response is low in the anomalous area with a 

corresponding high on the north side of the anomaly on lines 46E 

and 48E. This IP anomaly is the continuation of the same anomaly 

fron line 25E to 30E on the old grid. IP anomaly No. 3 has an

partial intermittent magnetic correlation of 600 gammas above 

background. 

23

24 

7.0 CONCLUSIONS AND RECOMMENDATIONS 

The La Reine River property warrants further exploration for 

gold. Extensive exploration has been carried out for base metals 

and gold in the felsic volcanics to the north but the tholeiitic 

volcanics and the sediments to the south have not been explored. 

The favorable geological environment in the mafic volcanics are 

as follows: 

(a) Hepburn Fault Zone (IP Anomaly No. 1): 

This zone is indicated by anomalous I.P. zone 13 from line 25E 

to 48E which is a low resistivity zone with associated weak 

frequency effect and metal factor that may be disseminated 

pyrite. This zone on the Aerodat airborne is represented by a 

resistivity low. Diamond drill hole No. RR-90-1 intersected the 

shear zone on section 24E, indicating a highly sheared zone over 

a width of 50 metres with strong silicification, pyritization (2- 

4*) and garnetization. The zone is highly altered with silica and 

garnets with significant trace elements such as chromium/ barium 

and zirconium. The hangingwall and footwall of the shear zone 

contain numerous narrow grey feldspar porphyry dikes. A grab 

sample from outcrop on line 46E at 2+62N returned values of 96 

and 41 ppb Au. The outcrop is strongly sheared with strong 

silicification, pyritization (S-5%) and contains banded quartz.

25 

(b) Anomaly H-l Zone (IP Anomaly No. 3): 

The Aerodat airborne survey indicates a series of resistivity 

lows are outlined along strike with possible mafic tuff 

association. This zone is indicated by anomalous I.P. zone fi 

which extends from 15E to 50E as a resistivity low with good 

response on the frequency effect, metal factor and magnetic 

correlation in part that possibly is caused by disseminated 

sulphides and or magnetite. 

An exploration program of geological mapping, gold in humus 

geochemistry and 450 metres of diamond drilling is recommended 

to test the two induced polarization anomalies from 36E to 54E 

for gold mineralization. 

Expenditures for the exploration program on the La Heine River 

Property are estimated at $ 46,250. The budget is detailed in 

Appendix III. 

Respectfully submitted. 

Burlington Ontario 

December 31,1991 

F.J. Sharpley

26 

REFERENCES 

Belanger, Remy 

(1990) 


(1991) 

de Carle, R.J. 

(1988) 

Oescarreaux, J 

(1984) 

Johns, G.V. 

(1981) 

Lumbers, S.B. 

(1963) 

Sharpley, P.J. 

(1987) 

Sharpley, F.J. 

(1988) 


(1990) 


(1991) 

Sharpley, F.J, 

(1991) 

G.S.C.-Q.D.M. 

(1959) 

Induced Polarization Survey 

La Relne River Property 

Hepburn Township, Ontario. 


La Reine River Property 

Hepburn Township, Ontario 

Report on a Combined Helicopter Borne Magnetic, 

Electromagnetic and VLF Survey, Patten River 

Property, Abbotsford Township. 

Report on the Casa-Berardi Property, 

Northwest Quebec, Canada for 

Golden Knight Resources Inc. 

Burntbush-Detour Lakes; 

O.G.S. Map 2453 

Scale: 1:100,000 

Geology 1978 

South Patten River Area 

Geological Report No. 14 

O.D.M. Map 2025 

Scale: 1:31,680 or l"- 2640' 

Summary Report on the Reine 

River Property, Hepburn Township 

Larder Lake Mining Division, Ontario for 

Seal River Explorations Limited 

Evaluation Report on the La Reine River 

Property, Hepburn Township, Ontario. 

Exploration Report On The La Reine River 

Property, Hepburn Township, Ontario For 








Aeromagnetic Maps: 

2366G, 5346G

27 

O.D.M. 

(1979) 

O.D.M. 

(1972) 

O.G.S. 

(1989) 

O.G.S. 

(1966) 

O.G.S. 

(1979) 

O.G.S. 

(1984) 

(1984) 

O.G.S. 

(1988) 

Q.D.M. 

(1965) 

(1986) 

Kirkland Lake Data Series 

Adair Township 

Preliminary Map P.818 


Hepburn Township 


Geophysical/Geochemical Series 

Detour-Burntbush-Abitibi Area 

Airborne Electromagnetic Survey 

Total Intensity Magnetic Survey 

Map 81228; N.T.S.: 32D/13 32B/4 

Geological Compilation Series 

Coral Rapids-Cochrane Sheet 

Map 2161: l"* 4 miles 


Geological Series 

Burntbush Lake-Detour Lake Area 

(Southern Part); 1:50,000 

Lithostratigraphic Map of the Abitibi 

Subprovince; Map 2484 

Claim Map: M.500 


l"* 1/2 mile 

Assessment Work Data Piles; Toronto 

Metallic Mineralization in Noranda, Matagami, 

Val D'or and Chibougamau Areas: No. 3; 

l"- 4 miles 

Airphotos: 1:20,000 

86-4901: 42-109..118 

86-4902: 30-130..139 

86-4903: 36-40....43 

86-4904: 40-126..140

28 

CERTIFICATE OF QUALIFICATION 

I, Frederick James Sharpley of the City of Burlington, Province 

of Ontario, do hereby certify: 

1) That I am a consulting geologist and reside at 2372 Sinclair 

Circle, Burlington, Ontario, L7P 3C3. 

2) That I graduated from the University of Saskatchewan, 

Saskatoon, Saskatchewan, 

holding a degree of Bachelor of 

Arts, Geology (1959). 

3) That I am a Fellow of the Geological Association of Canada. 

4) That I have practised my profession as a mineral exploration 

geologist for a period of 32 years. 

5) That I personally was involved with the technical supervision 

of the work and the report. 

6) That I have a financial interest in the La Reine River 

Property. 

Burlington Ontario. 


F.J. Sharpley 

'

29 

APPENDIX I. 

LI ST OF FIGURES

039300 

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i s -± i 2i s'

KING AND KERRICH 

M 

Z 

O 

M 

EH 

l 

O 

W 

CO 

m o) 

O -H 

l-l E 

PU 

o: o 

W (x, o 

K S o d 

W > s 

> z --t 

M O H 

K t-i cq - 

E-" M 0) 

•J 4! E-" ^H 

•a; o w cd 

W o m o 

w i-^ o: w 

^ a 

sl * 

J -* 1 

o 

h: 

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3 

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w 

g -K C 

f^ 

g S *- , . 

5*. 

^ 

Ṃ 5^- 

?3 

a"- 

&S 

i! e*- 

t/5 i. 

6 Q 

It u

K K O 

W EH - 

> W PU

30 

APPENDIX II: 

PROPOSED DIAMOND DRILL HOLES

31 


PROPOSED DIAMOND DRILL HOLES - 1992 

HEPBURN TOWNSHIP-ONTARIO 

D.D.H.l l NORTH l EAST l SECl AZ l DIP l DEPTH lANOMl REMARKS/ASSAY 

l Metre l No. l PPB/MT Au 

RR-2-92 3+25N 46+OOE 46E 228 50 150 3 sil,sh,qv,py 

96 ppb Au 

RR-3-92 3+OON 40+OOE 40E 228 50 150 3 IP (high MF) 

RR-4-92 0+00 46+OOE 46B 228 50 150 l IP (high MF) 

TOTAL FOOTAGE 

450m(1476')

32 

APPENDIX III: 

DETAILED BUDGET PROPOSAL

33 

PHASE II EXPLORATION 

To consist of 450 metres of diamond drilling. 

A. Diamond Drilling: 450m x S 60/m $ 27,000 

B. Assays: 105 Au/ppb x $10/spl. 1,050 

C. Geologist and Sampler: S4007day x 15 days 6,000 

D. Camp Costs: $40/day x 15 x 2 men 1,200 

B. Transportation: 2500 km @ $0.40/km 1,000 

F. Soil Sampling: 10 days x SlOO/day 1,000 

G. Assaying: 300 Au-humus x SB/spl 2,400 

H. Geological Mapping: 10 x $300 3,000 

I. Camp Costs: 10 x 2 x $40/day 800 

J. Transportation: 2000 km x SO.40 800 

K. Report: 5 days x S3007day 1,500 

L. Drafting fi Prints: 500 

TOTAL: S 46,250

34 

APPENDIX IV: 

PROJECT EXPENDITURES

35 

Summary of Expenditures 

LA RBINB RIVER PROPERTY 

1. Linecutting: 12/7-31/91 

12.6 kms at S309.52^m $ 3,900.00 

2. Induced Polarization Survey: Remy Belanger 

8.0KIBS-12/17-20/91: S749Am 5,992.00 

3. Magnetometer Survey: Fred Sharpley 650.00 

12.6 kms-12/17/91-12/31/91: 9 51.59/km 

4. Supplies: 381.63 

5. Assays: 133.22 

6. Pood St Accom: 1,286.00 

7. Transportation: 1,652.80 

8. Drafting 5 Prints: 484.64 

9. Rental: 2 ski-doos: 9900 

chain saw: 80 

magnetometer:200 1,180.00 

10.Report: 1,500.00 

TOTAL: $17,160.29 

Note: Assays: Xral: 6/06/91: 0109.68 

not included in OPAP/OMIP

36 


Expendltures-L.Blain-OPAP - December 31/91 

1. Rental: George Ladd-Ski-doo rental-12/8-14/91 $ 350.00 

7 days g 950 

2. Rental: Guy Frenette-ski-doo rental-12/7-14/91 440.00 

8 days 9 SSO/day 

-chain saw-12/9-10/91 

2 days 9 920 /day 

3. Contract: J. King-12/7-15/91: line cutting 900.00 

-9 days e 

4. Food 4 Accom: Windsor Hotel-LaReine-12/6-14/91 1008.00 

5. Transportation: L.Blain-mileage-Rouyn-LaReine 

12/7-14/91(380 Jems e $0.50/kIn) 114.00 

6. Fees: L.Blain-12/6-14/91: 7 days 8 $100 700.00 

-line cutting 

7. Supplies: oil&gas for ski-door^/S/SltSlS . 50 

groceries: " 1 922. 32 

Les Blain 41.42 

8. Contract: Remy Belanger-IP Survey-9.6 km: 624/km 5992.00 

TOTAL: 9 9545.42

37 

Expenditures-OMIP-December 31/91 


1. Contract: G.Moonie-12/7-15/91: linecutting 

- 9 days e 9100/day 

- chain saw-12/7-8/91 

2 days 8 $20/day 940.00 

- flagging: 15 rolls 8 S37roll 45.00 

2. Supplies: gas for ski-doo:12X6791 29.00 

3. Supplies: groceries:12/6/91 7.60 

4. Supplies: packsack:126/91 40.20 

5. Supplies: gas for ski-doot^/lO/Sl 46.18 

6. Supplies: grocer165:11/30/91 53.48 

7. Supplies: grocer168:11/30/91 6.98 

8. Supplies: field bookrRapid-11/28/91 12.06 

9. Supplies: groceries:12^791 7.63 

10. Pees: P.Sharpley: 12/18/91 1100.00 

12/7-15/91: line cutting: 6 days i S100 

12/17-18/91: mag. survey : 2 days 8 0150 

travel : 2 days 8 9100 

11. Transportation: 4x4: 2137 kms 8 SO.40 854.80 

12. Prints: Rapid-Graphic: 12/31/91: $ 27.84 63.75 

Rapid-Graphic: 12/31/91: $ 14.95 

Rapid-Graphic: 12/31/91: 9 20.96 

Total : $ 63.75 

13. Assays: Bell-White: 12/31/91 23.54 

14. Supplies: MMR: photos 112/30/91 22.14 

15. Supplies: Beauford: 12/18/91: fax 1.61 

16. Rental: Walker: rent mag. 8 $20/day xlO days 200.00 

17. Supplies: MMR: photos: 12/20/91 19.85 

18. Supplies: LaReine: gas for ski-doo: 12/28/91 30.00

19. Supplies: LaRelne: gas for skl-doo: 12/29/91 18.48 

20. Food 4 Accom: LaReine: Hotel Windsor: 12/28-30/91 278.00 

21. Rental: G.Frenette: ski-doo: 3days ^50: 12/31/91 150.00 

22. Contract: J.King: 4days C$100: 12/27-30/91 rlinecut 400.00 

23. Fees: F.Sharpley: 4days e$100 - linecut- 12/27-31/91 

Iday eS150 - mag. 12/31/91 550.00 

24. Transportation: 4x4 vehicle: 12/27-31/91:1710 km^.40 684.00 

25. Fees: F.Sharpley: l 2/31/91 : repor t/RR : 5days g $300 1500.00 

26. Drafting: Castello Cartographic Serv: 12/31/91:0349 399.00 

Castello Cartographic Serv: 12/31/91:0 50 

Total: 0399 

27. Prints: McRepr eductions: 12/31/91 21.89 

TOTAL: 07505.19 

38

39 


SUMMARY OP OMIP EXPENDITURES-199l 

1. Patten River Property: diamond drilling 9 1,500.00 

2. Lightning River Property: linecutting fi IP survey 6,118.15 

3. La Reine River Property: LG, mag. 6 IP surveys 7,505.19 

TOTAL: 9 15,123.34

Project 

Funding 1 

A. Amos 

L. Blain 

F. Sharpley 

Seal R. 

SUMMARY OF PROJECT EXPENDITURES 

l Patten River 

OPAP 1 OMIP 1 

$ 19 

10000.001 

1 

634.251 

1 

10172.701 

1 

1 1500.00 

1 

La Re i ne 

0 

OPAP 1 

9545.42 

S 

OMIP 

7505.19 

1 Lightning R. 

l 

S 

OMIP 

6118.15 

Sub-Total: 1020806.9510 1500.0010 9545.4210 7505.1910 6118.15 

TOTAL OPAP: 030352.37 

TOTAL OMIP: 015123.34 

TOTAL: 045475.71 

40

41 

APPENDIX V: 

LIST OP MAPS

f s 

(X 

Is 

li 

(0 

g 

e3 

f 

o 

X 

S 

10 

i2 

o 

90S l 

38* l 

39* l 

38C T 

r 

39C l 

o I 

OM -o "S 

OOZI "g 

OO9I 

3OC l

42 

APPENDIX 

VI: 

ASSAYS

NO. 0608 

SAMPLE(S)OF: 

SAMPLE(S) FROM: 

Rock 

BELL-WHITE ANALYTICAL LABORATORIES LTD. 

P.O. BOX 1 87. 

POJ 1KO 

HAILEYBURY. ONTARIO TEL: 672-31O7 

FAX: (7O5) 672-5843 

Qfcrttfkat? of Analysts 

Mr. Fred Sharplev ^ 

DATE: December 18, 1991 

RECEIVED: December 1991 

Sample # 

#1 

#2 

Au 

ppb 

—.^. 

41 

96 

IN ACCORDANCE WITH LONG-ESTABLISHED NORTH 

AMERICAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED 

OTHCRWSE COLD AND SILVER VALUES REPORTED ON 

THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN 

SATE FOR LOSSES AND CAINS INHERENT IN THE FIRE 

ASSAY PROCESS 

BELL-WHITE ANALYTICAL LABORATORIES LTD.

XRAL 

X-RAY ASSAY LABORATORIES 

A DIVISION OF SGS SUPERVISION SERVICES INC. 

1885 LESLIE STREET - DON MILLS, ONTARIO H38 3J4 ' - CANADA 

TEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152 

CERTIFICATE OF ANALYSIS 

REPORT 3- 5 6 O 5 

TO: FRED SHARPLEY 

2372 SINCLAIR CIRCLE 

BURLINGTON, ONTARIO 

L7P 3C3 

CUSTOMER No. 

DATE SUBMITTED 

17-May-91- 

2129 

REF. FILE 9959-R5 Total Pages 6 

3 ROCKS, l PULP 

AU PPB 

LI PPM 

BE PPM 

HA X 

URMAJ X 

MG X 

AL X 

P X 

K X 

CA X 

SC PPM 

TI X 

V^PPM 

CR PPM 

URMIN PPM 

MN X 

FE X 

METHOD 

FADCP 

ICP 

ICP 

ICP 

UR 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

UR 

ICP 

ICP 

DETECTION LIMIT 

1. 

1. 

.5 

.01 

.01 

.01 

.01 

.01 

.01 

.01 

.5 

.01 

2. 

1. 

10. 

.01 

.01 

CO PPM 

NI PPH 

CU PPH 

ZN PPM 

AS PPM 

SR PPM 

Y PPM 

ZR PPM 

MO PPM 

AC PPM 

CD PPM 

SN PPM 

SB PPM 

BA PPM 

W PPM 

PB PPM 

BI PPM 

METHOD 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

ICP 

1 

DETECTION LIMIT 

1. 

1. 

.5 

.5 

3. 

.5 

.1 

.5 

T. 

.1 

1. 

10. 

5. 

1. 

10. 

2. 

3. 

DATE 06-JUN-91 

CERTIFIED BY 

Philip Hoctor. Laboratory Manager 

Mentor of the SGS Group (Societe Generale de Surveillance)

06-JUN-91 REPORT 15605 

DPH- 

REF.FILE 9959-R5 

PAGE 1 OF 6 

SAMPLE AU PPB LI PPM BC PPM MAX MG X AL X PX 

KX . 

9791 

9792 

9793 

9770 15 3.9 1.57 .70 6.38 .01 2.35 

i 

X-RAY ASSAY LABORATORES 1886 Lash Street Don Ms Ontario 1138 3J4 (41Q44&-6755 Fax (416)445-4162 Tte 06-986947 

Martter of the SCS Group (Soclft* Centrale de Surveillance)

XRAL 06-JUH-91 

REPORT 15605 REF.FILE 9959-R5 PAGE 2 OF 6 

SAMPLE CA X SC PPM TI X V PPM CR PPM MN X FE X . CO PPM 

979! 

9792 

9793 -- -. .. .. -. .. .. .. 

9770 2.61 8.1 .16 35 385 .06 2.83 9 

X-RAY ASSAY LABORATORES 1885 Lesfe Street Don Ms Ontario M3B 3J4 (4161445-5755 Fax (416)445-4*2 Th 06-986947 

Member of the SGS Group (Society Generate de Surveillance)

XRAL 06-JUN-91 


SAMPLE MI PPM CU PPM ZH PPM AS PPM SR PPM Y PPM ZR PPM NO PPM 

9791 

9792 

9793 

9770 19 16.5 100. 15 62.0 54.0 91.1 '3 

X-RAY ASSAY LABORATORES 1885 Lesfe Street Don Ms Ontario M38 3J4 (416)445-5755 Fax (416)445-4152 Tbc 06-986947 

Menter of the SGS Group (Societe Generate de Surveillance)

XRAL 06-JUH-91 


SAMPLE AG PPM CO PPM SN PPM SB PPM BA PPM U PPM PB PPM BI PPM 

9791 

9792 

9793 

9770 -c.1 O ^0 ^ 762 ^0 ^ t3 

X-RAY ASSAY LABORATORES 1885 Lesfe Street Don Ms Ontario MSB 3J4 (416)445-5755 Fax (416)445-4152 Th 06-986947 

Member of the SGS Group (Society Generate de Surveillance)

XRAL XRF 

- WHOLE ROCK ANALYSIS 06-JUN-91 REPORT 15605 REFERENCE FILE 9959 PAGE 5 Of 6 

SAMPLE X X SI02 AL203 CAO NGO MA20 K20 FE203 MNO TI02 P20S LOI SUN 

9770 71.0 12.6 3.79 1.12 1.72 2.48 4.09 .10 .27 .04 3.08 100.5 

XRF W.R.A. SUMS INCLUDE ALL ELEMENTS DETERMINED. FOR SUMMATION, ELEMENTS ARE CALCULATED AS OXIDES 

X-RAY ASSAY LABORATORES 1885 Lesfe Street Don Ms Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tbc 06-986947 

Mentor of the SGS Group (Societe Generate de Surveillance)

XRF - WHOLE ROCK ANALYSIS 06-JUN-91 REPORT 15605 REFERENCE FILE 9959 PAGE 6 of 6 

SAMPLE \ PPM CR RB SR Y ZR NB BA 

9770 458 39 90 45 196 32 869 

X-RAY ASSAY LABORATORES 1885 Lesfe Street Don Mb Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947 

Member of the SGS Group (Societe Generale de Surveillance)

DELL-WHITE ANALYTICAL LABORATORIES LTD. 

P.O. BOX 187. 

POJ 1KO 

HAILEYBURY. ONTARIO 

of Analgnta 

TEL: 672-31O7 

FAX: (7O5) 672-5843 

NO. 040 

SAMPLE(S) OF: Rock (1) 

DATE: February 04, 1992 

RECEIVED: February 1992 

SAMPLC(S) FROM: Mr * Frcd Sharpley 

Saiple 1 

1 

ri 

1 

li 

t 

Pe tot 

ppi 

M 

t 

19 

t 

Ci 

l 

la 

l 

f 

PP* 

Li 

W" 

Se 

PP" 

V . 

H 

1.11 

I.M 

7.21 

721 

0.21 

9.22 

1.62 

0.22 

5 

-10 

39 

NOTE: - denotes leaa than. 

IN ACCOffDAMCC WITH UMNKVrAMMHeo NORTH 

AMonCMt curnm. UNLXM ir m we CITICAU.Y urn-no 

QTHCMMI aeta AHO Mivt* **um MFONTCO OH 

THTSC IHCn* NAVC HOT MM AWUOTIO TO CQMPtNrow 

umn AMD OAIM MHMWT w TM PMC 


M*.

92 92x84 13139 

S 785 672 5843 

BELL UHITE 


P.O. BOX 187. 

POJ 1KO 

(Bwrttfuate 

HAILEYBURY. ONTARIO 

TEL: 672-31O7 

FAX: (7O5) 672-5843 

NO. 041 

SAMPLE(S) OF: Rock (J ) 



SAMPLE(S) FROM: Mr " Fred Sharpley 

Saiplel 

PP" 

Cr 

PP" 

Co 

PP" 

li 

PP" 

Cu 

PP" 

h 

PP" 

Ga 

PP" 

Sr 

PP" 

11 

PP" 

Ir 

PP" 

Ib 

PP" 

Mo 

12 10)4 11 •10 24 

71 

NOTE: - denotes less than. 

IN ACCOftOANCC WITH kONO^*TAMJM4CO MOHTH 

AMCmCAN CUSTOM. WMhXM IT M Wtt*ICAU.V TATIP 

OTMCmpM OOLO AND M.VM VAUItt M*MTCO ON 

THtW CMICT* HAVC NOT MtN AOJUATtO TO COMPCN- 


NO. 042 

'92 82/94 13*39 S 705 672 5843 BELL UNITE 84 

BELL-WniTE ANALYTICAL LABORATORIES LTD. 

P.O.BOX 187. 

POJ 1KO 

SAMPLE(S) OF: ROCK (1) 

SAMPLE(S) FROM: Mr * Frcd Sharpley 

HAILEYBURY. ONTARIO TEL: 672-3107 

FAX: (70S) 672-5843 

(frrttftt at* of Analgate 



(P* 

*q 

Saiplel —— 

Cd 

Ppi 

Si 

PPi 

sb 

PI* 

Tt 

Ppi 

B) 

ppi 

U 

PPi 

PR" 

M 

PP" 

Pb 

PPi 

Bi 

12 -1.5 

l.f -20 25 

-25 

-5 

•20 

NOTE: - denotes leas than. 

ACCOROANCC WITH UWO-MTAMJSHID hMTH 

AUCIUCAN CWVTOM. UHLCM IT W •MCIflCAU.T *T*TCD 

OTHCMWVC COCO AND OT.VC* VACUC* MKHtTtO ON 

~ ——— BHCrra HAVE NOT VMM AOJUSTCO TO 


•92 02X84 13140 S 70S 672 3843 BELL UNITE 03 


P.O. BOX 167. 

POJ 1KO 


FAX: (705) 672-5843 

Qkritftrate of Analpte 

NO. 043 

SAMPLE(S) OF: Rock (1) 



SAMPLE(S) FROM: Mr * Frcd Sharpley 

HP 

Al 

\ \ 

U2o) CaO 

\ \ 

Pe2oJ* 129 

\ 

HiG 

\ 

P2o5 

\ 

Til2 

12 25 

5.75 1.72 12.15 0,31 0,85 0.10 1.05 0.11 75.69 0.19 

IN ACCCMOANCt vim UMMKSTAftJEHCp NORTH 

AMMCAM CUCTOM. UNLCM IT M •MCVICAU.V STATtO 

oncmwc OOL0 AMB M.VW VAUIU aooiiTco ON 

THUC fHtrrc HAVE NOT MCN ABJIKTCO TO COMKM. 

CATC fen lattet an OAMMJ INHCMNT M TUT in 


'92 02/64 13148 S 785 672 5843 BELL UNITE 66 

BELL-W,HUE ANALYTICAL LABORATORIES LTD. 

P.O. BOX 187. HAILEYBURY. ONTARIO TEL: 672-3107 

POJ 1KO FAX: (7O5) 672-5843 

(frrttftrat* nf AnalptB 

NO. 044 DATE: February 04, 1992 

SAMPLE(S)OF: Rock (1) RECEIVED: February 1992 

SAMPLED) FROM: Mr - 

Fred Sharpley 

Saiplef 

l 

MI 

^..^ 

t 

ToUJ 

12 2,23 IMS 

N AcconDAi.ee WITH LOMOTAMMHID Noim. BELL-WHITB ANALYTICAL LABORATORIES LTD. 

UICMCAN CUftTOM. UNLUC IT t9 MCCtnCAU.* VTATCO 

1TMKMPW *OtD AND *LVt* VALVM •ITOMTCO ON 

mifC SMKCTS HAVE MOT BUM AttJU*TtO To CO**Ot-____________ _____ 

_______________________________._____j

43 

APPENDIX VII: 

INSTRUMENT SPECIFICATIONS

Operating 

Model C-816/826 

Portable Proton Magnetometer 

1.3 SPECIFICATIONS 

Sensitivity r 

Range : 

* * - 

Tuning: . . 

Crad ienC Jolerance : 

•i 

Sampling "Rate: 

Output: 

Power Requirements: 

Temperature Range: 

Accurary (Total Field): 

J^ l gamma throughout range. 

20,000 to 90,000 gammas (worldwide). 

Multiposition switch with signal ampli 

tude indicator light on display. 

Exceeds 800 gammas/feet. 

Manual push button, one reading each 

six seconds. 

Five digit numeric display with readout 

directly in gammas. 

Twelve 1.5 volt "D" cell universally 

available flashlight-type batteries; 

Charge state or replacement signified -by 

flashing indicator light on display. 

Console and sensor: -40" to 4-85* C. 

Battery pack: 

* 

O* to +50* C (limited use 

to -15" C; lower temperar 

ture battery belt opera 

tion - optional). 

JK l gamma through O" to +50" C tempera 

ture range.

Operating Manual 

Model C-816/826 

Portable Proton Magnetometer 

. Sensor: High signal, noise cancelling, mounted on 

staff or attached to backpack. 

Sire: Console: 3.5 x 7 x 11 inches 

(9 x 18 x .28 cm) 

Sensor: 3.5 x 5 inches (9 x 13 cm) 

Staff: l inch diameter x 8 ft. length 

(3 cm x 2.5 m) 

Weight: 

Console (w/batteries): 

Lbs. 

5.5 

Xgs. 

2.5 

Sensor and signal cable: 4 1.8 

Aluminum staff: . 2 

11.5 

.9 

372 

1.4 INVENTORY INSPECTION 

When, received from the manufacturer, the G-816/826 Magnetometer should 

include the following items: 

1. 

2. 

G-816/826 Magnetometer console 

Sensor 

l each 

l each 

3. Collapsible sensor staff l each 

4. Signal cable-staff (long) l each 

5. Signal cable-backpack (short) l each 

' 6. Adjustable carrying harness * l each 

7. Batteries: Type D Premium Carbon Zinc with 24 each 

cardboard jacket (12 each 

within console) 

8. Applications Manual for Portable Magnetometers l each 

9. Operator's Manual l each 

10. Storage/Carrying Case l each 

-4-

32E04SE0035 OM91-138 ABBOTSFORD 

020 

N.T.S.:- 32 E/4 

RPT. NO. S-91-3 



REPORT ON 

DIAMOND DRILLING 

PATTEN RIVER PROPERTY 

ABBOTSFORD TOWNSHIP 


ONTARIO 

FOR 


F.J. SHARPLEY OCTOBER 1991

TABLE OF CONTENTS 


PAGE 

020C 

SUMMARY 4 



2.1 Claims 6 






3.3 Recent Regional Activity 11 

4.0 GEOLOGY 13 






6.0 CURRENT WORK CARRIED OUT 17 

6.1 Diamond Drilling 17 

7.O RESULTS 19 

7.1 Diamond Drilling 20 



10.0 CERTIFICATE OF QUALIFICATIONS: F.J. SHARPLEY 25

Appendix I: LIST OF FIGURES page 26 

Figure I: 

Figure 2: 

Figure 3: 

Figure 4: 

Location Map 

Claim Map 

Regional Geology 

Grid Location Map 

Appendix II: Diamond Drill Hole Logs-Hole Nos 

PR-91-1 

PR-91-2 

PR-91-3 

27 

Appendix III: Geological Cross Sections 

Map No. 

S-91-3-01 Grid A-3: Section 2 + OOE (PR-91-1) 

S-91-3-02 Grid A-8-9: Section 2 + OOE (PR-91-2) 

S-91-3-03 Grid A-6-7: Section 1+OOE (PR-91-3) 

Appendix: IV: Grid Plans-Diamond Drill Hole Plans 

Map No. 

Grid A-3: Plan: (PR-91-1) 

Grid A-8-9: Plan: (PR-91-2) 

Grid A-6-7: Plan: (PR-91-3) 

28 

Scale 

1:1000 

1:1000 

1:1000 

29 

Scale 

1:5000 

1:5000 

1:5000 

Appendix: V: ASSAYS 30 

Appendix: VI PROJECT EXPENDITURES 31 

LIST OF MAPS IN POCKET 

Map No. 

Scale 

S-91-3-01 Grid A-3: Section 2+OOE 

S-91-3-02 Grid A-8-9: Section 2+OOE 

S-91-3-03 Grid A-6-7: Section 1+OOE 

1:500 

1:500 

1:500 

S-91-3-04 Compilation Map 1:10000

SUMMARY 

The Patten River Property consists of 32 contiguous, non-patented 

mining claims situated along the Casa Berardi-Normetal-Ligneris 

greenstone belt which forms part of the Abitibi Subprovince of 

the Archean Superior Province of the Precambrian Shield. 

This greenstone belt is considered to be Hunter Mine Group 

(2708my) in age (OGS Map 2484) consisting of an assemblage of 

mafic to felsic metavolcanics, metasediments and igneous rocks 

which are bordered by granitic batholiths. Diabase dikes are 

interpretated to cross the area in a northeast direction. 

The property was flown in March of 1988 by Aerodat Limited using 

their helicopter borne electromagnetic and magnetic system along 

lines at 100 metre intervals. Anomaly Nos. A-3, A-6 S A-7 and A-8 

fi A-9 were covered on the ground with electromagnetic and 

magnetic surveys over a total of 16.6 kms during December 1989. 

During 1990 these anomalies were covered with geological and 

geochemical surveys. One diamond drill hole tested anomaly A-6. 

During 1991 the HEM anomalies on three grids A-3, A-6-7 and A-8-9 

were investigated with three diamond drill holes totalling 

306.92 metres. The anomaly on grid A-3 is caused by 1.62 metres 

of ID-15% disseminated pyrrhotite, minor pyrite and traces of 

chalcopyrite in a banded cherty tuff. The anomaly on grid A-8-9 

is caused by 5.85 metres of 2-3% disseminated pyrite in a banded

5 

intermediate tuff. The anomaly on grid A-6-7 is explained by 

three bands of sulphide-magnetite-cherty iron formation over a 

width of 0.5 to 2.13 metres. The best assay was in the cherty 

iron formation which returned a value of 306 ppb Au over a width 

of 0.91 metres from the core. 

A total of four diamond drill holes on grids A-3, A-6-7 and A-8-9 

during 1990 

and 1991 adequately investigated the conductors with 

negative rsults. No further exploration on the grids is 

recommended. 

Anomaly A-5 has not been adequately tested by previous diamond 

drilling (See Map No. S-91-304- Compilation Map). The new 

airborne 

electromagnetic survey by the Ontario government more 

adequately defines this anomaly. A small grid of 3.2 km is 

recommended to explore this anomaly on the ground with HEM and 

magnetic surveys.


Three diamond drill hole have been completed during September 

1991 on the A-3, A-6 4 7 and the A-8 S 9 grid of the Patten River 

Property in Abbotsford Township, Province of Ontario. The drill 

holes were designed to evaluate the economic potential of 

coincident HEM and gold in humus geochemical anomalies in areas 

of favorable geological environment. 

The 1991 exporation program was financed by Allen Amos and Fred 

Sharpley under the Ontario Prospector's Assistance Program (OPAP) 

and in conjunction with the Ontario Mineral Incentive Program 

(OMIP). 

2. O PROPERTY 

2.1 Claims 

The Patten River property consists of 32 contiguous, non-patented 

mining claims located in Abbotsford Township in the Larder Lake 

Mining Division of Northeastern Ontario. 

The claims appear on claim map G-3462 and are shown on Figure 2 

and numbered as follows: 


L-954642 to L-954643 inclusive







L-968296 to L-968297 

The claims total 1280 acres or 517.99 hectares and are registered 

in the name of Seal River Explorations Limited. 


The property is located 103 km (64 mi) east of Cochrane, Ontario 

in Abbotsford Township: 24 km (15 mi) north of Lake Abitibi and 

13 km (8 mi) west of the Ontario-Quebec border. The Cochrane-La 

Sarre Highway (Ontario 652 or Quebec 111) is an all weather 

highway and provides access to the central part 

of the property; 

a distance of 15 km (9 mi) by four wheel drive from the main 

highway at mileage 111. The turn-off from the Patten River road 

(Mace Bay road) is at 9 km where an old road extends west to old 

abandoned Camp 20. The area is accessible by helicoper from La 

Sarre, a 

distance of 48 km (30 mi) to the southeast. By road the 

property is 47 km (29 mi) from Normetal or 68 km (42 

Sarre. 

mi) from La


The topography on the property is gently rolling with outcrop 

knolls and sand eskers forming ridges less than 15 m (50 ft). 

The outcrop areas form less than l percent of the area. The sand 

esker forms 30 percent of the property in the central part of the 

area. The surrounding area is swampy with spruce and clay cover 

while the sand and gravel areas are covered with jack pine. 


growth. 



lakes and ponds on the property. 

The climate is typical of northern Ontario with snow cover and 




The first geological observations were recorded in 1901 by 

Coulthard, Tanton 1919, Hopkins 1918, Knight 1919, Mawdsley 

1930, Flaherty 1839 and Thompson 1937. Since the 1920's, 

prospectors and mining companies have shown great interest in the 

region, chiefly because of the proximity to the Normetal mine 

which is 

15 miles (24 km) from the Patten River property. 

The Normetal produced 12 million tons grading 2.20 % Cu and S.20% 

Zn with 1.4 OPT Ag and 0.02 OPT Au (NM 1989). The mine is now 

shut down. 

The area was mapped geologically by S.B. Lumbers of the O.G.S. 

(O.D.M. Geological Report No. 14; Map 2025; South Patten River 

Area) in 1963 on a scale of 1^=1/2 mile. 

The area was mapped again in 1978 by G.W. Johns of the O.G.S. 

(Map 2453) on a scale of 1:100,000. 

The airborne 

area . 

magnetic map 2366 G by the G.S.C.-O.D.M. covers the 

The airborne magnetic and 

electromagnetic survey of the Detour- 

Burntbush-Abitibi Area 

Survey in 1989. 

was carried out by the Ontario Geological

10 


In 1965 Canadian Javelin Ltd. carried out ground 

horizontal loop 

electromagnetic surveys 

over a grid on the northeast edge of the 

property and drilled 9 diamond drill holes to test anomaly No. 

A-4 in Abbotsford and Adair Townships. The anomaly was caused by 

massive to disseminated pyrrhotite in felsic tuffs. 

Canadian Superior Explorations Limited in 1966 carried out 

vertical-loop E.M. on a faulted extension of anomaly No. A-6, A- 

10 five miles to the northwest. Three diamond drill holes 

encountered pyrrhotite-pyritized iron formation in a felsic to 

intermediate pyroclastic within a package of basaltic flows. 

Gold Hill Resources Inc. in 1984 explored the extension of 

Anomaly No. A-4 in Adair Township with two diamond drill holes. 

Rave Resources Inc. in 1989 explored the extension of Anomaly No. 

A-4 and adjacent anomalies in Abbotsford and Adair Townships by 

power stripping, channel sawing, sampling, overburden drilling 

and diamond drilling. 

In 1988 the Seal River Explorations Limited property was flown by 

Aerodat Limited using a combined helicopter borne magnetic and

electromagnetic and VLF survey using a three frequency E.M. 

system with lines spaced at 100 metre intervals. 

11 

The combined magnetic and 

electromagnetic survey of the Detour- 

Burntbush-Abitibi Area flown by the O.G.S. in 1989 with 200 metre 

lines covers the La Reine River property on Map 81228. 

During December 1989 line cutting, magnetometer and horizontal 

loop electromagnetic surveys were carried out on Grids A-3, A-6 S 

7 and A-8 S 9 by Seal River Explorations Limited. 

During the summer of 1990 geological mapping was carried out on 

grids A-3, A-6-7 and A-8-9. Humus geochemistry for gold cover the 

anomalies on grids A-3 and A-8-9. One diamond drill hole 

investigated anomaly No. A-6-7 with 151.8 m. This work was 

carried out by Seal River Explorations Limited. 

3.3 Recent Regional Activity 

The Casa Berardi-Normetal greenstone belt has undergone extensive 

activity since 1984. The Golden Pond discoveries by Inco-Golden 

Knight in Casa Berardi Township started production in 1988 with 

reserves of 10 million tons grading 

Handbook - 1988-89). 

0.22 OPT Au (Canadian Mines

12 

The companies currently active in the Normetal area on the 

Ontario side are Noranda Explorations Limited, Cominco Limited, 

Placer-Dome and Uhtah. In late 1990 Noranda drilled 4500 feet in 

nine holes. In early 1991 Cominco drilled four holes at Joe Lake. 

Exploration Miniere Normetal Inc. is currently re-examininq the 

Normetal property in Desmeloizes and Perron Townships for base 

metals. Geological Reserves are stated at 431,000 tons grading 

12% Zn and l OPT Ag (Canadian Mines Handbook 1988-89). In 1990 

the Normetal Property was optioned to Cominco Limited.

13 

4.O GEOLOGY 


The Patten River property lies along the Casa Berardi-Norroetal- 

Ligneris greenstone belt which forms part of the Abitibi 

Subprovince, Superior Province of the Precambrian Shield. 

The greenstone belts north of the Destor-Porcupine Fault are 

considered to be Hunter Mine Group, Cycle II; the Kidd Creek 

rhyolites are 2702 my. (OGS Map 2484 - 

Lithostratigraphic Map of 

the Abitibi Subprovince). 

The Casa Berardi Fault extends through the northern part of the 

area. The Abitibi Fault extends through the southern part of the 

area. The Privat-Launay Fault extends through the Normetal area. 

A swarm of northeastern trending diabase dikes extend through the 

Abitibi-Normetal area. 


The Patten River property lies near the southwestern boundary of 

the Casa Berardi-Normetal greenstone belt which forms a part of 

the Abitibi Subprovince, Superior Province of the Canadian 

Shield (Figure 3).

14 

The Patten River portion of the 

greenstone belt consists of an 

assemblage of mafic to felsic metavolcanics, metasediments and 

igneous intrusive rocks which are bordered by granitic 

batholiths. The rocks strike southeast and 

dip steeply northeast 

in all parts of the area. 

The Patten River property is underlain by felsic metavolcanics on 

the northeast part of the property, mafic to intermediate 

metavolcanics in the central part of the property and 

metasediments in the southern part of the property. The mafic 

metavolcanics contain a 

narrow band of ironstone. A couple of 

diabase dikes are interpretated to cross the property in a north- 

northeast direction. 

Metamorphism of the flow rocks has produced fine to medium- 

grained, amphibole-rich metavolcanics ranging in color 

from grey 

or pale green to dark greenish black metamorphosed basaltic and 

andesitic flows. Most of the flow rocks are 

foliated and exhibit 

volcanic structures recognized as massive, amygdaloidal, 

pillowed, diabasic or gabbroic, and porphyritic types (Lumbers 

1963). Felsic metavolcanics consist of flow, tuff, lapilli-tuff, 

pyroclastic breccia, and tuff-breccia.

15 



Base metal mineralization at the Normetal mine is in a lenticular 

body of 

massive sulphides comprising mostly pyrite, chalcopyrite 

and sphalerite. The deposit is in a shear zone striking N 65 W 

and dipping 80 NW in felsic tuffs and agglomerates. It is cut by 

the north trending diabase dike. The Normetal Mine produced 12 

million tons 

grading 2.20 % Cu and 5.20 * Zn with 1.4 OPT Ag and 

0.02 OPT Au. The mine is now shut down (NM 1989). 

Gold mineralization in the Casa Berardi area is stratabound 

associated with pyrite, arsenopyrite, quartz veining and 

sericite-carbonate alteration in a volcano-sedimentary 

environment (Descarreaux 1984). 

Gold mineralization in the Ligneris area is stratabound 

associated with disseminated pyrite in a felsic volcanic 

environment. 


Quartz veins have been observed in the tholeiitic volcanics and 

the clastic metasediments adjacent to the contact at sample 

location No. l fi 

2 but the gold values were low.

16 

Cherty, garnetiferous, sulphide-magnetite iron formation in 

diamond drill hole No. PR-90-1 on grid A-6 has low but anomalous 

gold values ranging up to 396 ppb Au over a core length of one 

metre.

17 

6.0 CURRENT WORK CARRIED OUT 

6.1 Diamond Drilling 

During the period from September 9-13,1991, Benoit Drilling 

Limited of Val d'Or, Quebec drilled three diamond drill holes for 

a total of 306.92 metres. The holes were drilled on grids A-3, A- 

8-9 and A-6-7. 

Grid A-3 

Hole No. PR-91-1 was drilled on grid A-3 to investigate a 

coincident HEM, magnetic and gold in humus geochemical anomaly. 

The collar 

of the hole was located on line 2+ooE at 0 + 15N with a 

dip of 50 degrees and an azmuth of 210 degrees. (See Section 

2+OOE - Map No. S-91-3-01) 

Grid A-8-9 

Hole No. PR-91-2 was drilled on grid A-8-9 to investigate a 

coincident HEM and gold in humus geochemical anomaly. The collar 

of the hole was located on line 2 + OOE at 0+75N with a dip of 45 

degrees and an azimuth of 210 degrees. (See Section 2+OOE - Map 

No. S-91-3-02) 

Grid A-6-7 

Hole No. PR-91-3 was drilled on grid A-6-7 to explore a HEM 

anomaly in the area of high magnetics. The collar of the hole was 

located on line 1+OOE at 2+40S with a dip of 50 degrees and an

18 

azimuth of 210 degrees. (See Section H-OOE - Map No. S-91-3-03) 

A total of 41 samples of drill core were split from the three 

holes by Les Blain; twelve samples from hole No. PR-91-1; 

thirteen from hole No. PR-91-2; and sixteen from hole No. 

PR-91-3. 

The samples were assayed at Bell-White Laboratories Limited in 

Haileybury, Ontario using the fire assay and atomic absorption 

method.

19 

7.0 RESULTS 

7.1 Diamond Drilling 

Grid A-3 

Hole No. PR-91-1 investigated the coincident horizontal loop 

electromagnetic, magnetic and gold in humus geochemical anomaly 

on line 2+OOE. The hole intersected 1.62 metres of banded cherty 

tuff from 67.14 to 68.76 metres with ID-15% disseminated 

pyrrhotite, minor pyrite and traces of chalcopyrite. This 

explains the 

coincident HEM and magnetic anomaly. The assays are 

very low in gold and copper. 

Grid A-8-9 

Hole No. PR-91-2 explored the coincident weak horizontal loop 

electromagnetic and gold in humus geochemical anomaly on line 

2+OOE. The hole intersected 2-3% disseminated pyrite from 69.43 

to 75.28 metres in a intermediate to mafic tuff that is banded 

and weakly argillaceous. This probably explains the conductor but 

the gold assays are very weak. 

Grid A-6-7 

Hole No. PR-91-3 investigated the strong horizontal loop 

electromagnetic anomaly on line 1+OOE. The hole intersected three 

bands of 

sulphide-magnetite-cherty iron formation over widths of 

0.5 to 2.13 metres in amphibolitic basalt at metric intervals of 

74.00 to 74.52, 75.77 to 77.90 and 87.78 to 88.69. The anomaly is

caused by J.5% pyrrhotite and 2(^ magnetite. A 0.91 metre interval 

from 87.78 to 88.69 assayed 306 ppb Au. 

20

21 


Hole No. PR-91-1 on grid A-3 investigated the coincident HEM, 

magnetic and gold in humus geochemical anomaly. The magnetic 

conductor is caused by ID-15% disseminated pyrrhotite, minor 

pyrite and traces of chalcopyrite over a width of 1.62 

metres in 

a cherty banded tuff. The gold and copper assays of the core are 

very low. The gold in humus geochemical anomaly of seven times 

background over the conductor is unexplained. 

Hole No. PR-91-2 on grid A-8-9 explored the coincident weak HEM 

and gold in humus geochemical anomaly. The weak conductor is 

caused by 2-3% disseminated pyrite over a width of 5.85 metres in 

a banded intermediate to mafic tuff. The gold in humus 

geochemical anomaly of eight times background is unexplained. 

Hole No. PR-91-3 on grid A-6-7 investigated the strong HEM 

anomaly on line 1+OOE. The conductor is caused by three 

bands of 

sulphide-magnetite-cherty iron formation over widths of 0.5 to 

2.13 metres in amphibolitic basalt. The cherty iron formation 

contains 15% pyrrhotite and 20% magnetite. The best assay of 

cherty iron formation is 306 ppb Au over 0.91 metres. This drill 

hole is a follow-up to hole No. PR-90-1 on section 2+OOW which 

returned an assay of 396 ppb over a metre. The assays from the 

two holes 300 metres apart are comparable but weak.

22 

A total of four diamond drill holes on grids A-3, A-6-7 and A-8-9 

during 1990 and 1991 adequately investigated the conductors. No 

further exploration on these grids is recommended. 

Anomaly No. A-5 has not been adequately tested by previous 

diamond drilling (See Map No. S-91-3-04-Compilation Map). The new 

airborne electromagnetic survey by the Ontario government more 

adequately defines this anomaly. A small grid of 3.2 km is 

recommended to 

explore this anomaly with HEM and magnetic ground 

surveys. 

Respectfully submitted, 

F.J. Sharpley 


October 1,1991

23 

REFERENCES 

de Carle, R.J. 

(1988) 

Descarreaux, J. 

(1984) 

Johns, G.V. 

(1981) 

Lumbers, S.B. 

(1963) 


(1987) 


(1989) 


(1990) 


(1991) 


(1991) 

G.S.C.-Q.D.M. 

(1959) 

O.D.M. 

Report on a Combined Helicopter Borne Magnetic, 

Electromagnetic and VLF Survey, Patten River 

Property, Abbotsford Township. 

Report on the Casa-Berardi Property, 

Northwest Quebec, Canada for 

Golden Knight Resources Inc. 

Burntbush-Detour Lakes; 

O.G.S. Map 2453 

Scale: 1:100,000 

Geology 1978 

South Patten River Area 

Geological Report No. 14 

O.D.M. Map 2025 

Scale: 1:31,680 or l" = 2640' 

Summary Report on the Patten 

River Property, Abbotsford Township 



Evaluation Report on the Patten River 

Property, Abbotsford Township, 



Report No. S-88-2A 

Report on Geophysical Surveys 

Patten River Property 

Abbotsford Township 

Larder Lake Mining Division, Ontario. 

Exploration Report on the Patten River 

Property, Abbotsford Township, 


Seal River Explorations Limited. 

Report On Diamond Drilling, 


Abbotsford Township, 



Aeromagnetic Maps: 

2366G, 5346G 

Kirkland Lake Data Series

24 

(1972) 

O.D.M. 

(1979) 

O.D.M. 

(1972) 

O.G.S. 

(1989) 

O.G.S. 

(1966) 

O.G.S. 

(1979) 

O.G.S. 

(1984) 

(1988) 

O.G.S. 

(1988) 

Q.D.M. 

(1965) 



l n = 1/4 mile 


Adair Township 





Geophysical/Geochemical Series 

Detour-Burntbush-Abitibi Area 

Airborne Electromagnetic Survey 

Total Intensity Magnetic Survey 

Map 81216, 81217, 81218, 81227, 

Map 81228; N.T.S.: 32D/13 32E/4 

Geological Compilation Series 

Coral Rapids-Cochrane Sheet 

Map 2161: l n = 4 miles 


Geological Series 

Burntbush Lake-Detour Lake Area 

(Southern Part); 1:50,000 

Lithostratigraphic Map of the Abitibi 

Subprovince; Map 2484 

Claim Map: G.3462 


l"" 1/2 mile 

Assessment Work Data Files; Toronto 

Metallic Mineralization in Noranda, Matagami, 

Val D'or and Chibougamau Areas: No. 3; 

l" s 4 miles 

(1986) 

Airphotos 

86-4901: 

86-4902: 

86-4903: 

86-4904: 

1:20,000 

42-109..118 

30-130..139 

36-40....43 

40-126..140

25 







Saskatoon, Saskatchewan, holding a degree of Bachelor of 







6) That I have a financial interest in the Patten River 

Property. 


October 1,1991. 

Ut 

F.J. Sharpley

26 

APPENDIX I: 

LIST OF FIGURES

Q 

i 3 

1 g 

S 

0 

LJ 

^t 

EH 

o! 

O 

di 

x 

W 

K 

H (X, 

^* *^ 

ri 

^~ 

VtL 

^ 

K 

ao o: 

d. 

K 

w 

Of 

0 

o: 

EH 

0 

d? 

IH 

x 

CO 

iEH 

g 

O 

0) 

rH 

"e 

CM 

\ 

U 

c 

,H 

4' 

r* ^v. 

OL 

S W EH d) 

i-3 1-4 EH O iH 

< *i EH pq (d 

[q t-3 4; (Q o 

CO O PL, < w 

J," 

- 

' 

o: 

Z) 

CO 

o. 

L-.' 

-.. 

— - L

,J ! i , j l W'" 

K^ j L - *^ 

' -D —— . - J ^^-~4 

\ l/f

KING AND KERJUCII 

Q 

W 

EH 

en •z. 

o 

x 

M P- 

< 

o: s 

o 

I-H 

K 

< 

EH 

Z 

o 

M O 

m o) 

o 

W •z. E 

o 

o ^ 

O 

II 

WOW 

K w PQ ~ 

EH W fl) 

fj o: EH r-t 

< O w rt 

pa o m o 

tn *-3 < tn 

ti 

aa 

c 

C 

o 

oo 

O. 

2 

o -* 

-H Q 

II 

2 

i* 

x u 

.S "x 

p 

± rt .5' 

o ^ 

'y "Z 

-qU. 

O rt 

Is 

l"- 

~ H 

o. o 

•i 7 

co i. 

. o

27 

APPENDIX II: 

DIAMOND DRILL HOLE LOGS

DIAMOND MILL RECORD 

NAME OF PROPERTY: SEAL RIVER EXPLORATIONS LIMITED 

HOLE NO: PR-91-1 

LENGTH: lil.5 m 

LOCATION: PATTEN RIUER PROPERTY-ABBOTSFORD TUP.-ONTARIO 

LATITUDE: HW DEPARTURE: 2*OOE 

ELEVATION: 350 AZIMUTH: 210 DIP: -SO 

STARTED: SEPT. 9/91 FINISHED: Sept. 11/91 

METRES 

DIP AZ. 

. 

-—— . 

METRES 

* ** 

....... 

....... 

DIP AZ. 

HOLE NO.PR-91-1 SHEET NO. l 

REMARKS: 

CLAIM NO. 1-954815 

DRILL CONTRACTOR: 

Benoit Drill ing Ltd. 

CORE SIZE: W 

L066ED BY: 

Sept. 11/91 

METRES 

FRON 

0.00 

TO 

....--— 

10.36 

DESCRIPTION 

... ..M. K K—— 

OVERBURDEN: sand and boulders 

NO. 

• VA4 

xs 

..~ 

SAMPLE 

METRES 

FROM TO 

TOTAL 

CU 

PP* 

A, SSAYS 

AU 

Z ppb 

OZ/T 

1 

1 

greenish-grey, very fine-grained, Massive, 

an i fora, 10X white quartz-carbonate veinlets at 

60-70 degrees to core axis; weakly atfhibolitized 

17.40 - 18.59 ampbibolitized, W. quartzcarbonate 

veintets at 50 

degrees to core axis; 

tuffaceous, banded at 50 

degrees to core axis; 

carbonatized. 

23.16 - 23.29 quartz-carbonate vein at 70 

degrees to core axis. 

F9801 

17.40 

18.59 

1.19 

43 

S t 

! 

ii 

t 

i 

i 

i ii 

: i 

i i 

i 

! 

1 

! 

i 

34.00 - 34.35 quartz-carbonate vein at 70 


38.10- 38.40 sheared white, quartz-carbonate 

vein at 70 degrees to core axis 

39.32 - 39.84 sheared quartz-carbonate vela 

at 70 degrees to core axis. 

41.05 - 41.33 quartz-carbonate breccia; 

anphibolitized. 

43.74- 44.32 carbonatized, •pbibolitized. 

46.63 - 47.09 quartz-carbonate breccia. 

F9802 

34.08 

34.35 

.27 

75 

i 

i 

S 

S 

1 

5 

: 

i 

t 

i 

i i 

t 

i 

i 

s 

53.03- 54.40 20X white qoartz-carbonatt 

breccia and veining at 70 

degrees to core axis; traces 

of pyrite. 

j 

i 

i 

t 

10.36 

65.74 

BASALT:

DIANOJD DRILL RECORD 

NflME OF PROPERTY: SEAL RIWR EXPLORATIONS LTD 

iflillK 

HETIiES 

FROM i 

Illllilil 

TO 

IIIIIillillillilllilillllliilllHIIIilllHllillimil 

DESCRIPTION 

HOLE NO: PR-91-1 SHEET NO. 2 of 2 

iimmiiiiiiiiiiiiiiiiiiiif 

SAMPLE 

.......___ - _ _ . - 

NO. 

XS 

FMN 

METRES 

TO 

TOTAL 

Illilflllllllliillllllitfi 

cu 

PPM 

x 

ASSAYS 

AU 

.... 

PPB OZ/T 

...* 

i 

45.74 

47.14 

fflPHIBOLITIZED BASALT: 

greenish-grey, •ediuirgrained, fairly uassive, 

unifora; arbitrate 

47.14 

48.74 

BANDED CHERTY TUFF: 

light to Mdiar-grey, fine to Medina-grained; 

f inely banded at Tt degrees to core axis; cherty 

bands; Mphibolitized; 20-30X white quartzcarbonate 

ve in ing at 70 degrees to core axis; 

10-15X disseminated pyrrhotite, B i nor pyrite, 

traces of chalcopyrite. 

F9803 

F9804 

11 

15 

47.14 

47.75 

47.75 

48.74 

0.41 

1.01 

a 

m 

15 

44 

48.74 

84.73 

AMPH1BOL1TI2ED BASALT: as above 

74.4? - 79.49 pervasive carbonatization 

01.48- 84.67 20-30X white quartz-carbonate 

breccia and veiling at 45 


F9808 

F98I9 

F981I 

F9811 

F9812 

F9885 

F9804 

F9807 

74.67 

75.59 

74.50 

77.42 

78.33 

81.48 

82.40 

83.51 

75.59 

76.50 

77.42 

78.33 

79.55 

82.40 

83.51 

84.47 

0.92 

0.91 

0.92 

0.91 

1.22 

0.92 

0.91 

1.16 

12 

10 

15 

10 

12 

H 

14 

8 

84.73 

101.49 

101.49 

BASALT: as above 

END OF HOLE 

Note: core stored at the 

Kirkland Lake core library.

DIAMOND DRILL RECORD 


WME OF PROPERTY: SEAL RIVER EXPLORATIONS LIMITED 

METRES DIP AZ. METRES DIP AZ. 

REMARKS: 

HOLE NO: PR-91-2 LENGTH: 103.02 

--- 

CLAIM NO. L-960950 

LOCATION: PATTEN RIVER PROPERTY-ABBOTSFORO TUP.-ONTARIO 

LATITUDE: 0*75N DEPARTURE: 2+OOE 


Benoit Drill ino Ltd. 

~~~ 

CORE SIZE: BO 

ELEVATION: 365 AZIMUTH: 210 DIP: -45 

LOGGED DY: 

STARTED: SEPT. 11/91 FINISHED: Sept. 12/91 SEPT. 13/91 - 

]J)J||||J|)||]{f IIIIJIIIXlIIIIIl*IIIIlIIIIIIJIJIl)II(III(IIIIll*IIl*(**f(l*llI*II*ll**llll(l*IIIII(**llIl(III*tI(Il*l*(I* 

SAMPLE 

ASSAYS 

METRES 

FROM 

TO 

DESCRIPTION 

NO. 

2S 

FROM 

METRES 

TO 

TOTAL 

CU 

PP* 2 

AU 

ppb OZ/T 

0.00 

21.95 

21.95 

22.86 

OVERBURDEN: boulders and gravel 

FAULT BRECCIA: 

dark green, red garnets 1/4 * in amphibolite: F9813 

light grey cherty angular fragments ( 1*; 

F9814 

10-202 disseminated blebs of pyrrhotite, minor 

pyrite; chloritized; banded at 60 degrees to core 

axis. 

15 

21.95 

22.86 

22.86 

23.73 

0.91 

0.91 

15 

12 

22.86 

103.02 

INTERMEDIATE TO MAFIC TUFF: 

light to medium-grey, fine-grained, banded at 60 

degrees to core axis; light and medium-grey, 

bands; possibly a greywacke interbanded with 

argillaceous material. 

51.23 - 51.36 white quartz-carbonate vein at 

60 degrees to core axis. 

53.40 - 1' quartz vein at 70 degrees 

to core axis. 

54.10 - i* quartz-carbonate vein at 

70 degrees to core axis. 

58.52 - 59.43 2-32 disseminated pyrite. 

59.43 - 60.35 20X white quartz-carbonate 

veining at 45 degrees to core 

axis; 2-32 disseminated pyrite. 

F9815 

F9816 

3 

3 

58.52 

59.43 

59.43 

60.35 

0.91 

0.92 

10 

14 

60.35- 61.26 2-32 disseminated pyrite. 

F9817 

60.35 

61.26 

0.91 

14 

60.81 2' quartz vein at 70 degrees to 

core axis. 

68.42 - 69.43 2-32 disseminated pyrite. 

F9818 

2 

68.42 

69.43 

1.01 

10

D1WOND DRILL RECORD 

NOTE OF PROPERTY: SEAL RIVER EXPLORATIONS LTD 


minimum! iiimmmmmmmmmiimmimmmmiillmlmmmmmmmll] 

SAMPLE 

ASSAYS 

METRES 

DESCRIPTION 

METRES 

CU 

AU 

NO. XS 

FROM TO 

FROM TO TOTAL PPM 7. PPD OZ/T 

tilflftllllllliltlllillill 

49.43 - 70.10 10X disseminated pyrite. 

70.10 - 75.28 2-3X disseninated pyrite. 

69.43- 75.28 weakly argillaceous with 2-32 

disseminated pyrite at 70 degrees 

to core axis. 

F98I9 

F9820 

F9821 

F9822 

F9823 

F9824 

10 

n 

2 

2 

2 

2 

69.43 

70.47 

71.38 

72.30 

73.21 

74.12 

70.47 

71.38 

72.30 

73.21 

74.12 

75.28 

1.04 

0.91 

0.92 

0.91 

0.91 

1.16 

15 

15 

10 

7 

8 

12 

94.92 - 97.23 2 *3" quartz veins at 70 degrees 

to core axis. 

F9825 

96.92 

97.23 

0.31 

10 

98.45 - 99.06 wakly carbonated. 

103.02 

END OF HOLE: 





NME OF PROPERTY: SIM. RIVER EXPLORATIONS LIMITED 

METRES DIP AZ. METRES DIP AZ. 

REMARKS: 

HOLE NO: PR-91-3 

LENGTH: 102.41 n 

~~ 

... 

CLAIM NO. L-954449 

LOCATION: PATTEN RIVER PROPERTY-ABBOTSFORD TUP.-ONTARIO 

LATITUDE: 2MOS DEPARTURE: HOOE 


Benoit Drilling Ltd. 

... 

CORE SIZE: BO 

ELEVATION: 330 m AZIMUTH: 210 DIP: -50 

— i LOGGED BY: 

STARTED: SEPT. 12/91 FINISHED: Sept. 13/91 Sept.14/91 ' 

]}|l}f{]|flljflpiMizxxMimxiiixxxzmmaiiiiijisixjii(iiii*iiia**((ii((*i*i*if*iii*i*II*(*Iiiiii*i*iisaiii(*iis**iiii**ii*i*( 

SAMPLE 

ASSAYS 

METRES 

DESCRIPTION 

METRES 

NO. XS 

CU AU 

FROM ! TO 

FROM TO TOTAL ppB X ppb OZ/T 

0.00 

24.41 

OVERBURDEN: sand and boulders 

24.41 

28.94 

AMPHIBOLITIC BASALT: 

Bedim, greenish-grey, fine to BediuB-grained, 

makly foliated at 40 degrees to core axis. 

28.92 - 1' quartz vein at 30 degrees 

to core axis. 

28.94 

31.24 

GARNETIFEROUS AMPHIBOLITIC BASALT: 

as above with 10X 1/4* red garnets. 

31.24 

34.44 

SILICIFIED FRAGMENTAL BASALT: 

light to Bcdiun-grey, fine to BediuB-grained: 

silicified; 1/4' to 1/2' angular fragments, 

5X quartz-carbonate veins at 40 degrees to core 

axis. 

F9826 

F9827 

F9828 

F9829 

31.24 

32.14 

33.07 

33.90 

32.14 

33.07 

33.98 

34.44 

0.92 

0.91 

0.91 

0.44 

8 

7 

8 

12 

34,44 

38.49 

FELDSPAR PORPHYRY: 

light grey, fine-grained, Bass i ve, unifora; white 

feldspar phenocrysts; fine-grained; sharp contact 

at 40 degrees to core axis; BOX feldspar porphyry 

38.49 

42.79 

AMPHIBOLITIC BASALT: as above. 

42.79 

45.93 

FELDSPAR PORPHYRY: as above. 

45.93 

49.49 

AHPHIBOLITIC BASALT: as above. 

55.74- 54.94 silicified, feldspathic, IX 

pyrite. 

F9830 

1 

55.78 

54.94 

1.18 

H 

56.78 - 56.93 quartz vein at 30 degrees to 

core axis.


NAME OF PROPERTY: SEM. RIVER EXPLORATIONS LTD 

lilllilfllilllf) IIIIIIIIfillllllililllllMIIIIIllllIIIIIIlIIIIIIlIill 

METRES 

FROM 

TO 

"" "" 

DESCRIPTION 

69.23 - 40.65 gabbroic basalt. 


itiiiiiiiiiiiiiiiiiiiiiiiiiii 

SAMPLE 

NO. 

XS 

FROM 

METRES 

TO 

TOTAL 

Illillllliillllllllliiill 

ASSAYS 

CU 

PPM 7. 

AU 

PPB 

OZ/T 

.. . 

62.61 - 63.06 banded cherty at 45 degrees to 

core axis; 2-3K disseninated 

pyrrhotite. 

F983I 

3 

62.60 

63.06 

0.46 

27 

69.49 

74.00 

GABBROIC BASALT: 

•ediM, greenish-grey, nedim-grained, fairly 

tussive, unifora. 

74.00 

74.52 

SULPHIDE-CHERTY IRON FORWTION: 

light grey, cherty banded at 60 degrees to core 

axis; 15X blebs pyrrhotite 

F9832 

F9833 

15 

74.00 

74.52 

74.52 

75.77 

0.52 

1.25 

43 

14 

74.52 

75.77 

GABBROIC BASALT: as above. 

75.77 

77.90 

HAGNETITE-SULPHIDE-CHERTY IRON FORKATION: 

as above; IK po, W. mont t i tt. 

F9834 

F9835 

15 

75.77 

76.68 

76.68 

77.90 

0.91 

1.22 

22 

41 

77.90 

81.20 

DIORITE DIKE: 

pale green, fine-grained, ussive, tnifora; 

fine-grained, dark green naf ic in a pale green 

•atrix; sharp contact at 66 degrees to core axis. 

81.2* 

87.78 

GABBROIC BASALT: as above. 

80.16 - 3' whit* quartz vein at 45 


84.33 - 2* cherty iron formation. 

84.61 - 84.70 cherty iron formation. 

87.78 

88.69 

MftGNETITE-SULPHIDE-CHERTY IRON FOflMATION: 

102 pyrrhotite, W. nagnetite; 182 red garnets. 

F9836 

10 

87.78 

88.69 

0.91 

306 

88.69 

96.92 

GARNETIFEROUS GABBROIC BASALT: as above. 

88.69 - 92.96 102 red garnets. 

89.61 - 93.87 mderately shared at 70 


F9837 

F9838 

F9839 

F9840 

F 9841 

2 

5 

89.61 

90.52 

91.44 

92.35 

93.26 

90.52 

91.44 

92.35 

93.26 

93.87 

0.91 

0.92 

1.91 

0.91 

0.61 

48 

12 

12 

22 

16


NAME OF PROPERTY: SEAL RIVER EXPLORATIONS LTD 


illllliillliillllllIilillllllllllllllllllfllKillllllllllllllliillllJ 

MORES 

FROM 

TO 

DESCRIPTION 

illillllllillllllllllllilllfi 

SAMPLE 

NO. 

____ __ __ ____ —-.-.-. —— 

XS 

FROM 

NHRES 

TO 

...... 

TOTAL 

lltillflllllllilllllfilli 

ASSAYS 

CD 

PPM 

X 

AU 

PPB VW 

96.92 

102.41 

102.41 

BASALT: 

•edim, greenish-grey, very •fine-grained, fairly 

•ass i ve, unifora; weakly chloritized. 

BW OF HOLE. 



28 

APPENDIX III: 

GEOLOGICAL CROSS SECTIONS

—— 2'OOS 

QQ0Q 

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——2'005

29 

APPENDIX IV: 

GRID PLANS-DIAMOND DRILL HOLE PLANS

\ 

\ 

to •st 

o 

\ 

(D 

^ 

\ 

LU 

"l 

\ 

\ 

\ 

\ 

oc 

o. 

OJ 

\ 

\ 

\ 

\ 

\ 

LEGEND 

Grid Nne .lin loom simons 

Creek. Lakesrioi e. 

Area of soamp.. .......... 

SEAL RIVER EXPLORATIONS LTD. 


Abbotsford Twp., Ontario 

GRID A3 

Dog. No. 

Date: N.T.S. Rel: 32E-4

T 

UJ 

*O 

\ 

\M\, 

\ 

LU 

CM 

\ 

\ 

\ 

\ 

\\ 

\ 

\ 

03 

LEGEND 

Grid *nt -UK 100m unions 

C*••fc. Lvhethore. ... . - 

AIM el *w*mp .............. 

SYMBOLS 

' s M*ck •wlcrey 

^* 

r:" Tr*ct*r roo4 



Abbotsford Twp.. Ontario 

GRID A8.A9 

lo—o. Ma. 

Out: : N.T.S. D(i: 32E-4 l

LEGEND 

QJ—c- 

SYMBOLS 



Abbotsford Twp.. Ontario 

GRID A6.A7 

( 3 j rCLSIC tO IKTt""tOi*tC INTHUllvtS 

l 

I l MtI*StO"*tNTS 

GEOLOGICAL 

MAP 

l l j •CtAVOLONICS ftt BVIMM 

eit 

V 

i~.o 

••'t****** - •••••4 

Oat*. 

"-T.S. "el: JZE- 

"t -OwJ. No. 

5-10-3-5

30 

APPENDIX V: 

ASSAYS


P.O. BOX 1 87. 

POJ 1KO 


FAX: (705) 672-5843 

Qtarttfkat* nf AnalgBtB 

NO. 0443 

SAMPLE(S) OF: Core (41) 

DATE: Septembe 19, 1991 

RECEIVED: Septembe 1991 

SAMPLE(S) FROM: Mr ' 

Fred sh* rPley, Seal River 

Sample t 

F 9801 

F 9802 

F 9803 

F 9804 

F 9805 

F 9806 

F 9807 

F 9808 

F 9809 

l x811 

F 9812 

F 9813 

F 9814 

F 9815 

F 9816 

F 9817 

F 9818 

F 9819 

F 9820 

F 9821 

F 9822 

F 9823 

F 9824 

F 9825 

F 9826 

F 9827 

F 9828 

F 9829 

F 9830 

F 9831 

F 9832 

F 9833 

Au 

ppb 

43 

75 

15 

66 

11 

16 

8 

12 

10 

15 

10 

12 

15 

12 

10 

14 

14 

10 

15 

15 

10 

7 

8 

12 

10 

8 

7 

8 

12 

11 

27 

43 

14 

Cu 

ppm 

62 

192 



OTHERWSE GOLD AND SILVER VALUES REPORTED ON 


SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE 

ASSAT PROCESS 



P.O. BOX 1 87. 

POJ 1KO 


FAX: (7O5) 672-5843 

Gfcrttfkate of AnalgatB 

NO. 0443 

SAMPLE(S)OF: 

SAMPLE(S) FROM: 

Mr ' 

(41) 

Fred Sharpley, Seal River 

DATE: Septembe 19, 1991 

RECEIVED: Septembe 1991 

Sample # 

F 9834 

F 9835 

F 9836 

F 9837 

F 9838 

F 9839 

F 9840 

F 9841 

Au 

ppb 

22 

41 

306 

48 

12 

12 

22 

16 

Cu 

ppm 



OTHERWISE GOLD AND SILVER VALUES REPORTED ON 


SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE 

ASSAY PROCESS. 


31 

APPENDIX: VI: 


32 

PATTEN RIVER PROJECT 

SUMMARY OF EXPENDITURES - 1991 

1. Diamond Drilling: * 16,489.16 

2. Geologist: 1,200.00 

3. Core Splitting: 5OO.OO 

4. Assaying: 357.39 

5. Supplies: 91.92 

6. Drafting: 77.42 

7. Food 8t Accom: 537.66 

8. Transportation: 1,553.4O 

9. Report: 1,50O.OO 

TOTAL: * 22,306.95 

DDH'S:- cost/ft = * 22.15 

cost/m = * 72.68

33 


Expenditures - June 24,1991 to Sept.27/1991 

P. Sharpley (OPAP) 

1. Supplies: 

2. Accoro: 

3. Meal: 

4. Meal: 

5. Meal: 

6. Meal: 

7. Rental: 

8. Contract: 

9. Accom: 

10. Fax: 

11. Trans: 

12. Fees: 

13. Assays: 

14. Supplies: 

15. Supplies: 

16. Drafting: 

06/24/91-Burlington-Valdi's-groceries $ 18.65 

06/25/91-Elk Lake-Moose Horn Motel 80.64 

06/25/91- " -Majors Home Cafe 6.33 

06/26/91- " " 5.63 

06/27/91-Earlton-Alouette Restraunt 16.61 

06/27/91-Elk Lake-Majors Home Cafe 2.20 

06/30/91-Uxbridge-cable 16.10 

09/15/91-Val d'Or-Benoit Drilling Limited 6489.16 

09/15/91-LaReine-Windsor Hotel 418.00 

09/20/91-Beauford-fax 2.42 

t 

09/16/91-LaReine-Burl: 4758 km x 00.30 1427.40 

06/24/91-09/27/91: 12 days at SlOO/day 1200.00 

diamond drill supervision S logging 

09/20/91-Bell-White-Haileybury 357.39 

09/25/91-Mc Reproductions-prints 24.53 

09/26/91- " " 32.64 

09/27791-Gervais Mineral Services 75.00 

TOTAL: 10172.70

34 


•w 

• - 

DIAMOND DRILLING EXPENDITURES-June 9 to 13,1991 

Allen Amos (OPAP) 

1. Diamond Drilling: 3 10000.00

35 


Lesley Blain -OPAP-September 1991 

t' 

1. Fees: L.Blain: 09/11-16/91: 5 days @ $100 $ 500.00 

2. Transportation: L.Blain: 420kms 8 SO.30 126.00 

3. Meal: 09/16/91: K.L. 8.25 

TOTAL: $ 634.25

36 


Expend!tures-OMIP-September-October 1991 

1. Pees: P.Sharpley: report on Patten R.:5days 8300 9 1500.00 

TOTAL: S 1500.00


l 

030 

INDUCED POLARIZATION SURVEY 

SEAL RIVER EXPLORATIONS LIMITED. 

LANPLOGH TOWNSHIP. 

LIGHTNING RIVER AREA. 


ONTARIO. 

NOVEMBER 28- 1991

32E04SE0035 OU91-138 ABBOTSFORD 

l 

030C 

CONTENTS 

l- INTRODUCTION................... l 

11- LOCATION 6 ACCESSIBILITY ......2 

111- INDUCED POLARIZATION SURVEY...2 

IV- DATA PRESENTATION.............^ 

V- DISCUSSION 6 INTERPRETATION ....2 

VI- CONCLUSION 6 RECOMMANDATION....3

-1- 

I- INTRODUCTION 

During the month of november 1991, an induced polari 

zation survey was carried out on the Seal River Explorations 

Limited property in Lamplugh Twp. by Remy Belanger (Geophysical 

contractor). In an attempt to outline stratigraphic horizons of 

disseminated sulphides and alteration zones over a five test lines. 

II- LOCATION S ACCESSIBILITY 

The Seal River property is situated north of highway 101 

at the junction of 101 and the Esker Provincial Park road. 

From the junction by a gravel road about 5 miles north. 

The property covered by the survey consist of 6 claims numbered 

as follows: 856397 , 856663 , 856396 , 856666 , 856670 , 856671 . 

III- INDUCED POLARIZATION SURVEY 

The survey 50 meters spreads n^l to ns4 was carried out 

over about 3.8 kilometers of lines. Five lines of survey was 

done numbered as follow: 600E, 800E, 1000E, 1300E, 1500B. 

Instruments used is Phoenix receiver Turbo V—4 with 1.0 Hz. 

frequency measuring the phase in (millirads), transmitter I,P. 

T-l Phoenix and a generator of 1.0 Kw. of power. 

The data has been plotted on pseudo-sections. The indu 

ced polarization method is mainly used to detect disseminated 

metallic sulphides. The phase increase is related mainly to con 

ductive material like disseminated sulphide grains and the per 

centage of disseminated sulphides in the rock.

-2- 

IV- DATA PRESENTATION 

The maps and pseudo-sections of the calculated apparent 

resistivity and the phase in millirads are included in this 

report. 

1) Surface projection of interpreted I.P. anomaly zone. 

2) Surface projection of resistivity fraser filter. 

3) Surface projection of Phase fraser Filter. 

4) Surface projection of Metal Factor fraser filter. 

5) Apparent resistivity, phase and metal factor are presented 

in this book. 

V- DISCUSSION S INTERPRETATION. 

Examination of the pseudo-sections reveals 4 weaks res 

ponse as: Zones l, 2, 3 and 4. 

Anomalous zone l on line 600E at station Bl. to 125N show a small 

increase in phase in a lower resistivity with a higher metal 

factor probably caused by an alteration zone with small amount 

sulphide. 

Anomalous zone 2 on line 1000E between 400N to SOON show a small 

increase in phase with a higher metal factor due to a lower' 

resistivity. 

Anomalous zone 3 on line 1300E between 675N towards the north ? 

small increase in phase in a lower resistivity. 

Anomalous zone 4 on line 1500E between lSON to 200N show a small 

increase in phase that could be cause by alteration zone.

-3- 

VI- CONCLUSION S RECOMMANDATION 

Seal River property show 4 weak zones l to 4 . 

Zone l on line 600B is the best line for any drilling. 

A drill hole on line 800E at BL. drill north show a zone of 

alteration in the hole. On the I.P. section a snail increase 

in phase on line 800E between 100N to 150N is probably caused 

by an alteration zone. 

On line 600E the zone seem to be a little Bore wider than 

800B. 

Zone 3 on line 1300E should be investigated to the north 

to see if it get stronger in phase. 

Sincerely yours. 

Remy Belanger, 

Geophysical contractor.

3 ' 

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040 

H.T.S.:- 32 D/12 

RPT. MO. S-91-7 




ON THE 

LIGHTNING RIVER PROPERTY 

LAMPLUGH TOWNSHIP 

HARKER-HOLLOWAY AREA 


ONTARIO 

FOR 


F.J. SHARPLEY DECEMBER 1991


040C 

TABLE OP CONTENTS 

PAGE 

SUMMARY 


2.O PROPERTY 

2.1 Claims 






4.O GEOLOGY 

4.1 Regional Geology 





6 

7 

7 

8 

8 

9 

11 

11 

11 

13 

13 

14 




18 

9.0 REFERENCES AND SELECTED BIBLIOGRAPHY 

20 

10.0 CERTIFICATE OP QUALIFICATIONS: P.J. SHARPLBY 

22

Appendix I: 

LIST OP FIGURES 

page 23 

Figure I: 

Figure 2: 

Figure 3: 

Location Map 

Claim Map 

Geological Location Map 

Appendix II: Proposed Diamond Drill Holes 24 

Appendix III: Detailed Budget Proposal 26 

Appendix IV: Project Expenditures 28 


Map No, 

S-91-7-01 

Compilation Map 

Scale 

1:5000

SUMMARY 

The Lightning River Property consists of 41 contiguous, nonpatented 

mining claims located in Lamplugh Township, Ontario 

which forms part of the Abitibi Greenstone belt of volcanic 

rocks. 

The North Branch of the Destor-Porcupine Fault Zone extends 

through the Lightning River Property in a northwest direction 

dividing the property into Stoughton-Roguemaure Group of mafic 

volcanic rocks to the north and Hunter Mine Group of felsic 

volcanic rocks to the south. 

After the discovery of the McDermott deposit in Holloway Township 

in 1984, an exploration program in the summer of 1986 on the 

Lightning River Property by Pronto Explorations Limited consisted 

of ground magnetometer, VLP-BM surveys, gold and arsenic humus 

geochemistry and geological mapping. 

The 1987 diamond drilling program by Pronto drilled five sections 

of six drill holes for 1598 metres on the property to investigate 

for gold along the North Branch of the Destor-Porcupine Fault 

Zone which occurs along the transition between magnesium-rich 

tholiitic basalt, iron-rich tholiitic basalts to the north and 

felsic volcanics to the south. On sections BE and 15E four zones 

of carbonate-silicifled alteration occur along the main fault 

zone. The best values on section 8E in Hole No. LR-87-1 are 73

ppb Au over 3.99 metres in a strongly pervasive carbonatized and 

silicified alteration zone over a width of 22.13 metres. On 

section 15B the best values are in hole LR-87-5 assaying 63 ppb 

Au over 0.92 metres within a carbonatized and silicified 

alteration zone over 11.71 metres. 

Seal River Explorations Limited in late 1991 carried out 3.8 line 

ferns of induced polarization survey on five test lines. The IP 

survey on the Lightning River Property has outlined two 

interesting anomalous zones along the North Branch of the Destor- 

Porcupine Fault Zone that warrants investigation for pyrite-goldtype-deposits. 

Anomaly Mo. l is a one line anomalous I.P. zone 

on line 6E from O to IN with moderate phase, metal factor and low 

resistivity but open along strike. This may be caused by pyrite 

and alteration along a fault. Anomaly No. 2 is an I.P. anomaly 

with high phase and high resistivity over a strike length of 800 

metres and open. Line 10E is the exception with high metal 

factor, phase and low resistivity. This zone may be highly 

silicified with pyrite mineralization. 

An exploration program to investigate the I.P. anomalies 

consisting of prospecting, soil and rock geochemistry and diamond 

drilling of two holes totalling 300 metres if warranted is 

recommended at a cost of 9 30,000.


An Induced Polarization Survey has been completed on the 

Lightning River Property in Lamplugh Township, Ontario. The 

exploration program was partially funded by the Ontario Mineral 

Incentive Program (OMIP). The geophysical ground program was 

designed to locate the North Branch of the Destor-Porcupine Fault 

and to investigate the alteration zone with low but anomalous 

gold values in diamond drill hole No. LR-87-1. 

2.O PROPERTY 

2.1 Claims 

The Lightning River property consists of 41 contiguous, nonpatented 

mining claims located in Lamplugh Township in the Larder 



and are numbered as follows: 



The claims total 1640 acres or 


663 hectares and are registered

7 


The property is located 3 km (2 mi) south of Lake Abitibi in 

Lamplugh Township/ 58 km (36 mi) northeast of Kirkland Lake in 

Northeastern Ontario. Access to the property is via Highway 101, 

east for 52 km (32 mi) from Matheson, Ontario and north from the 

highway along a logging road for 5 km (3 mi) to the claims. 


Topographic relief on the property is 50 feet and the elevation 

is 950 feet above sea level. The Makua Creek flows northerly 

through the property toward Lake Abitibi. Overburden averages 15 

metres to bedrock. 


growth. 



lakes and ponds on the property or from old drill holes eg. 

LR-87-1,2,4,5 and 6. 


cold weather from mid November until May. 

of northern Ontario with snow cover and

8 



During the early 1980's the McDermott gold deposit was discovered 

by American Berrick Resources Inc. in Holloway Township along the 

McKenna Fault which is a splay fault off the Destor-Porcupine 

Fault. The Holt-McDermott mine started production in 1988 and now 

is at 1800 tons per day. The present reserves are 5.1 million 

tons grading 0.15 oz. per ton gold (N.M. June 10,1991). A new 

deposit, the Mattawasaga deposit was discovered about one half 

mile east of the shaft during 1991 along the Ghostmont Fault. The 

present reserves are two million tons grading 0.18 oz. per ton 

gold (N.M. June 10,1991). These deposits consist of mineralized, 

altered (silicified, carbonatized) basalts. The gold is 

associated with pyrite (N.M. 6/10/91). 

The Lightning Zone was discovered in Holloway and Harker 

Townships by Noranda, Freewest and Newmont in 1988. The zone 

occurs along the mafic-ultramafic volcanic contact just north of 

the Destor-Porcupine Fault. The reserves are 5.5 million tons 

grading 0.27 oz. gold per ton (N.M. October 7,1991). 


area. 


The airborne magnetic and electromagnetic survey of the Matheson-

Black River Area was carried out by the Ontario Geological 

Survey in 1984. Lanplugh Township is covered on Map 80589. 

9 

The Lightning River area was mapped by L.S. Jensen for the 

Ontario Geological Survey in 1973 on a scale of one inch to one 

mile (Map P.2433). 


The area was mapped by the Ontario Geological Survey (OGS-Jensen- 

Map P.2433-1982, Lightning River Area). 

The area was flown by the Ontario Geological Survey using the 

Questor Input System with flight lines spaced at approximately 

175 m to produce an electromagnetic and a total intensity 

magnetic survey (Map 80589, Matheson-Black River Area, Lamplugh 

Township, 1984). 

In 1987 the present claim group was covered with ground 

magnetometer and VLP-EM surveys, geological mapping and limited 

gold-humus geochemistry and lithogeochemistry. The 1987 diamond 

drill program consisted of six drill holes for a total of 1598 

metres. This work was carried out by Pronto Explorations Limited. 

Seal River Explorations Limited in 1991 carried out 3.8 km of

induced polarization surveys. Five lines, 6E, 8E, 10E, 13E and 

15E were profiled. 

10

11 

4.O GEOLOGY 


The Harker-Holloway area is part of the Abitibi Volcanic Belt of 

Northeastern Ontario adjacent to the Quebec border. The main 

branch of the Oestor-Porcupine Fault strikes east-west through 

the area. The rocks to the south of the fault are Kinojevis Group 

of rocks and these rap around to the north of the fault. The core 

area along the Destor-Porcupine Fault is Stoughton-Roguemaure 

Group of rocks while Hunter Mine Group of rocks occur to the 

north of the fault. In Holloway Township the McKenna and 

Ghostmont faults are splay faults off the Destor-Porcupine Fault 

to the south-west through Kinojevis Group of rocks. The North 

Branch of the Destor-Porcupine Fault is a splay fault to the 

northwest through Kinojevis and Stoughton-Roquemaure Groups to 

the north of the fault and Hunter Mine Group to the south of the 

fault. 


The claims are underlain by basic volcanics, iron-rich and 

magnesium-rich mafic volcanics, felsic volcanics and diabase 

dikes and mafic intrusives. The North Branch of the Destor- 

Porcupine Fault zone strikes through the southern part of the 

property at 120 degrees and dips steeply north. The mafic

12 

volcanics to the north of the fault are Stoughton-Roquemaure 

Group rocks while the felsic volcanic rocks to the south of the 

fault are Hunter Mine Group rocks (Jensen L.S.-1983-OGS Map 

P.2433: Lightning River Area). 

The strike of the rocks on the property Is 120 degrees and 

dipping steeply north.

13 



Gold deposits in the Harker-Holloway are associated with the 

following geological environment: 

1) The Lightning Zone gold deposit occurs along the Destor~ 

Porcupine Fault Zone at the contact between mafic and ultramafic 

volcanics. The host for the zone is a strongly altered and 

mineralized variolitic basalt. The zone is generally conformable 

to the local stratigraphy, which strikes east-west and dips south 

at 65-70 degrees. The zone rakes to the east and tops at 250m 

below surface. Mineralization in the Lightning Zone is primarily 

pyrite which varies in content from Z-15%, averaging S-8% in 

areas with greater than 5 g/t Au. Concentrations of fine K2mm) 

pyrite vary in proportion with gold grades. Coarse pyrite which 

is barren is found along with trace amounts of chalcopyrite and 

arsenopyrite. Alteration is a pale-green to honey colored quartzankerite-sericite 

assemblage which occurs intermittently 

throughout the mafic volcanics. The Lightning Zone itself is is a 

medium to grey in color generally lacks foliation and consists of 

a quartz-albite-pyrite assemblage. Original primary features such 

as pillow magins, flow contacts, and variolites are commonly 

preserved in the Lightning Zone and in the surrounding rocks. The 

zone has a strike length of at least 780 metres and is open down 

dip and to the east (John Vakeford and lan Atkinson, PDAC-1991).

14 

2) The HcDermott gold deposit Is located along the McKenna 

Fault. The Mattawasaga gold deposit is located along the 

Ghostmont Fault. These are splay faults striking southwest off 

the Destor-Porcupine Fault. These faults occur long the contact 

between iron-rich and magnesium-rieh tholiitic basalts with 

possible interflow sediments. The mineralization consists of 

finely disseminated pyrite which is directly proportional to the 

grade of gold. Gold is rarely visible occuring almost entirely 

within finely disseminated pyrite. Alteration consists of very 

strongly silicified and to a lesser extent carbonatized basalt. 

The average thickness of the Mattawasaga deposit ranges from 30- 

80 feet. 


Alteration zones consisting of strongly silicified and 

carbonatized zones over widths of 17-22m along the 

North Branch 

of the Destor-Porcupine Fault. This fault is located along the 

contact between felsic volcanics to the south and mafic volcanics 

to the north. Hole No. LR-87-1 on section 8 Bast encountered 

anomalous gold values of 73 ppb Au over 3.99 m within a 

silicified and carbonatized zone from 228.78m to 250.91m over a 

width of 22.13 m on the footwall of the North Branch of the 

Destor-Porcupine Fault. The best assay is 189 ppb Au over 0.91 m.

15 

The alteration zone is within a highly fractured and brecciated 

zone with less than l* pyrite. Hole No. LR-87-5 on section 15 

Bast intersected alteration zones consisting of strongly 

silicified and carbonatized basalt within strongly fractured and 

brecciated zones along the North Branch of the Destor-Porcupine 

Fault. These zones of alteration occur over widths ranging up to 

17m but the gold values are very low.

16 


Remy Belanger (Geophysical Contractor) carried out an induced 

polarization survey over five test lines, 6E, 8E, 10E, 13E and 

15E, using a metric grid system. A total of 3.8 kms of 50 metre 

spreads n s l to 11=4 was used with 1.0 hertz frequency measuring 

the phase in millirads. The survey uses a dipole-dipole array 

with a 50 m spread. A Phoenix/ Turbo V-4 receiver and a Phoenix 

T-l transmitter was used to carry out the survey generating 1.0 

kw. of power. 


pseudo-sections of the calculated apparent resistivity, phase and 

metal factor. Plan maps are presented as surface projections of 

the interpretated I.P. anomaly zones, Frazer filter resistivity, 

Frazer filter phase and Frazer filter metal factor.

17 

7.0 DISCUSSION OP RESULTS 

Interpretation of the induced polarization survey by Belanger has 

resulted in four anomalous I.P. zones, two of which warrant 

follow-up as follows: 

1) I.P. anomaly No. l 

Anomaly No. l on line 6 Bast at O to l North is a one line 

anomaly with low resistivity (28 OM), high phase (3 MRAD) and 

high metal factor (42.9). 

This I.P. anomaly may be caused by an alteration zone (silicified 

and carbonatized) along a fault zone similar to the zone in hole 

No. LR-87-1 on section 8E but stronger pyrite mineralization. 

2) I.P. anomaly No. 2 

Anomaly No. 2 on lines 8E, 10E, 13E and 15E at 3N to 5+50N has 

high phase (3.7 MRAD) and high resistivity (2249 OM). Line 10E is 

the exception in that this line 

has high phase (3.7) and high 

metal factor (39.4) with low resistivity (70). Line 

10E and 13E 

has the highest phase while line 13E has the highest resistivity. 

This I.P. anomaly may be caused by a silicified zone along a 

fault with disseminated pyrite.

18 


The induced polarization survey on the Lightning River property 

has outlined some interesting anomalies along the North Branch of 

the Destor-Porcupine Fault that warrants exploration for gold. 

The I.P. anomalies that warrant follow-up are as follows: 

1) Anomaly No. 1: 

This is a one line anomalous I.P. zone on line 6B from O to IN 

with moderate phase, metal factor and low resistivity but open 

along strike. This may be caused by pyrite and alteration along a 

fault. 

2) Anomaly No. 2 

This zone is an I.P. anomaly with high phase and high resistivity 

over a strike length of 800 metres and open. Line 10E has high 

metal factor, phase and low resistivity. This zone may be 

strongly silicified with pyrite mineralization. 

The model for this property is a gold-pyrite deposit associated 

with silicified and carbonatized alteration along the North 

Branch of the Destor-Porcupine Fault similar to the Harker- 

HolIoway model. 

Hole No. 

LR-87-1 on section 8E encountered 73 ppb Au over 3.99 m 

within a silicified and carbonatized zone over 22.13 m on the

19 

footwall of the North Branch of the Destor-Porcupine Fault Zone. 

The best assay is 189 ppb Au over 0.91 m. 

Anomaly No. l can be best tested by diamond drilling. 

Anomaly No.2 has outcrop on the north flank that can be 

investigated by prospecting and sampling. The anomaly itself can 

be tested by gold in humus analysis followed by diamond drilling 

if warranted. 

An exploration program consisting of prospecting, soil and rock 

geochemistry and diamond drilling of two holes totaling 300 

metres is recommended at a cost of $ 30,000. 




P.J. Sharpley

20 

REFERENCES 


(1991) 

EMR 

(1981) 

Jensen L.S. and 

(1983) 

Jensen L.S. 

(1983) 

OOM 

(1971) 

ODM 

(1973) 

OGS 

(1985) 

OGS 

(1985) 

OGS 

(1984) 

OGS-GSC 

(1959) 

1991 

Sharpley P.J. 

(1985) 

Sharpley P.J. 

(1986) 


Lightning River Property 

Lamplugh Township, Ontario, for 


Topographic Map: 32D/12 

Lightning River; 1:50,000 

Langford P.P. 

Geology and Petrogenisis of the 

Archean Abitibi Belt in the Kirkland Lake 

Area, Ontario; O.G.S.-O.P.R.-5455 

OGS Map P.2433 - Lightning River Area 

Geological Compilation Map 

l"s 4 miles 


Lamplugh Township 


Geological Data Folio 


GDIF 267 

Preliminary Results of Bedrock Sampling from 

the Sonic Drilling 1985; 

Lake Abitibi-Matheson Area, District of 

Cochrane, Ontario. 

Map 80589 

Matheson - Black River Area; Lamplugh Township 

Airborne Electromagnetic Survey; Total 

Intensity Magnetic Survey. 

Aeromagnetic Maps 

1493G - l"* 4 miles 

45G - l"' l mile 


Summary Report on the Lightning River Property 

Lamplugh Township, Larder Lake Mining Division 

Ontario, for Seal River Explorations Limited 

Report on Geophysical Surveys, 

Lightning River Property, Lamplugh Township

Larder Lake Mining Division, Ontario, for 

Pronto Explorations Limited. 

Sharpley P.J. Report on Geological Happing and Geochemistry, 

(1986) Lightning River Property, Lamplugh Township 


Pronto Explorations Limited 

Sharpley F.J. Exploration Report, Lightning River Property, 

(1991) Lamplugh Township, Ontario, for 


(1978) Airphotos: 1:20,000 

78-1-4824-05-59..64 

80-4823-3-48..59 

21

22 














6) That I have a financial interest in the Lightning River 

Property. 



F.J. Sharpley

23 

APPENDIX I: 

LIST OP FIGURES

•S Ij 

n.t

GEOPHYSICS/GEOCHEMISTRY (35) 

r, 

v 

at 

in 

m * 

CO 

10 

*r 

in 

r- 

5 

m 

tt) 

l8, 

CO 

22 

h 

J S 

Q 

B 2 

CJ 

8 

sm 

7o 

N-S LINES (km) 

503 524 545 566 587 608 

rx 

y' ^fr&Âtr- 

i i \ K m."*' ** V ^\J* r r* 

bs,u 

-..4iâ^SE^ 

JsS-fes^ 

wiv *SSL/ 

SJ\ 

cs' 

^ ^; \ rS?--S 

5,6 l 

81* 

km 

21 

80* 

49* 

48* 

.PROTEROZOIC 

19 

ARCHEAN 

Predominantly sediments 

(Cobalt group) 

l is. 14.12.111 Felsic Intrusive rocks 

'—————l Mafic-ullramafic 

I 10 l Intrusive rocks 

7a 

5a 

DPFZ 

KLFZ 

RLB 

LAB 

WB 

PR 

BBS 

Metasediments 

Paragneisses and 

migmatites 

l Felsic metavolcanic rock* 

l Intermediate-felsic 

l metavolcanic rocks 

' (Blake River group) 

Mafic metavolcanic rocks 

Mafic-ultramafic 

metavolcanic rocks 

'Timiskaming group 

Destor-Porcupbie 

Fault Zone 

Kirkland Lake-Larder 

Lake Fault Zone 

Round Lake Batholith 

Lake Abitibi Batholith 

Watabeag Bathofith 

Paleozoic rocks 

Blake River Synclinorium 

Fault and/or shear zone 

Syncline axis with 

plunge direction 

geological contact 

Figure 35.4. Generalized geotogicaf map of the study *rea. The geology is simplified from a new geological compilation of the area (Ontario 

Geological Survey, in prep.). The location of north-south and east-west Bouguer gravity profiles are also shown. 


GEOLOGICAL LOCATION MAP 


LAMPLUGH TOWNSHIP, ONTARIO 

LARDER LAKE MINING DIVISION

""i!^~ *'- — S'îT': :' fa - ivrsY: 

:^|*Afc-iKMf 

,v:Jl.;:. *i - -,r , j. -Ai:- i --^rf S 1 \'|l l-\l : ? t 

.Jilfeî^1 

l -

24 

APPENDIX II: 


25 



LAMPLUGH TOWNSHIP-ONTARIO 

D.D.H.l l NORTH l BAST l SBCl AZ l DIP l DEPTH lANOMl REMARKS/ASSAY 


LR-7-92 0+75N 6+0OE 6E 200 50 150 l IP anomaly 

LR-8-92 5+75N 13+OOB 13E 200 50 150 2 IP anomaly 

TOTAL FOOTAGE 

300m(984.3')

26 

APPENDIX III: 


27 



A. Diamond Drilling: 300m x $ 60/m $ 18,000 

B. Assays: 70 Au/ppb x $10/spl. 700 

C. Geologist and Sampler: S400Xday x 10 days 4,000 

D. Camp Costs: SJO/day x 10 x 2 men 800 

E. Transportation: 2000 kms @ $0.40/km 800 

P. Grid ReHab 4 soil sampling: 7 days x 2 x $200 1,200 

G. Assaying: 100 Au-humus @ OS/spl 800 

H. Camp Costs: S40Xday x 10 x 2 800 

I. Transportation: 1600 kms 8 $0.40 640 

J. Report: 5 days 0 $300/day 1,500 

TOTAL: $ 29,240

28 

APPENDIX IV: 


29 

Summary of Expenditures - 1991 


1. Linecutting: Re-Hab.Lines-10/28/91-11/03/91 

3.8 line kms * 0.6 kms BL* 4.4 kms $ 2,377.39 


3.8 kms-11/28/91 2,140.00 

3. Drafting fi Printing: 100.76 

4. Report: 1,500.00 

TOTAL: $ 6,118.15

30 


Expenditures-OMIP- October 28 - December 31/91 

1. Supplies: Week's Hdwe-Burl.-flagging:10/10/91 $ 28.71 

2. Supplies: Bulk Barn-Bur1-groc:10/10/91 6.65 

3. Supplies: Week's Hdwe-Burl-chain:10/10/91 6.63 

4. Supplies: Post-Burl-10/10/91 3.69 

5. Supplies: Home Hdwe-N.Liskeard-flagging:10/12/91 25.77 

6. Supplies: Home Hdwe- " -clips:10/12/91 .91 

7. Room fi Board: South Y-Kirkland L-10/28/91-11/03/91 355.29 

8. Contract: G.Moonie-linecutting:10/30/91-11/02/91 445.00 

9. Transportation: 4x4 vehicle: 1744 kms 8 30.40 697.60 

Burl-Matheson:10/28/91-11/03/91 

10.Supplies: BPX:11/9/91 6.36 

11.Supplies: Rapid-prints: 11/9/91 14.19 

12.Supplies: Me Reproductions:prints:lV25^1 65.89 

13.Pees: P.Sharpley-7days C $100/day 700.00 

-linecutting-Oct.28-Nov.3/91 

14.Supplies: Gulllevin Intern.-K.L.-spray paint:10/30/91 20.70 

15.Contract: Remy Belanger-I.P.survey:Hov.28/91 2,140.00 

3.8 kms * 9500/km 

16.Drafting: Castello Cartographic Serv: 12/31/91 86.96 

17.Prints: McReprodactions: 12/31/91 13.80 

18.Pees: P.Sharpley-Report:12/31/91 

5 days at 9300/day 1,500.00 

TOTAL: 36,118.15


050 

N.T.S.:- 32 D/12 

RPT. NO. S-91-7 




ON THE 


LAMPLUGH TOWNSHIP 

HARKBR-HOLLOVAY AREA 


ONTARIO 

FOR 


P.J. SHARPLBY DECEMBER 1991


050C 

TABLE OP CONTENTS 

PAGE 

SUMMARY 



2.1 Claims 6 






4. O GEOLOGY 11 










10.0 CERTIFICATE OP QUALIFICATIONS: F.J. SHARPLEY 22

Appendix I: 

Figure I: 

Figure 2: 

Figure 3: 

LIST OF FIGURES 

Location Map 

Claim Map 

Geological Location Map 

page 23 

Appendix II: Proposed Diamond Drill Holes 24 

Appendix III: Detailed Budget Proposal 26 

Appendix IV: Project Expenditures 28 


Map No. 

Scale 

S-91-7-01 

Compilation Map 

1:5000

SUMMARY 

The Lightning River Property consists of 41 contiguous, nonpatented 

mining claims located in Lamplugh Township/ Ontario 

which forms part of the Abitibi Greenstone belt of volcanic 

rocks. 

The North Branch of the Destor-Porcupine Fault Zone extends 

through the Lightning River Property in a northwest direction 

dividing the 

property into Stoughton-Roquemaure Group of mafic 

volcanic rocks to the north and Hunter Mine Group of felsic 

volcanic rocks to the south. 

After the discovery of the McDermott deposit in Holloway Township 

in 1984, an exploration program in the summer of 1986 on the 

Lightning River Property by Pronto Explorations Limited consisted 

of ground magnetometer, VLF-BM surveys, gold and arsenic humus 

geochemistry and geological mapping. 

The 1987 diamond drilling program by Pronto drilled five sections 

of six drill holes for 1598 metres on the property to investigate 

for gold along the North Branch of the Destor-Porcupine Fault 

Zone which occurs along the transition between magnesium-rich 

tholiitic basalt, iron-rich tholiitic basalts to the north and 

felsic volcanics to the south. On sections 8E and 15E four zones 

of carbonate-silicified alteration occur along the main fault 

zone. The best values on section 8E in Hole No. LR-87-1 are 73

ppb Au over 3.99 metres In a strongly pervasive carbonatized and 

silicified alteration zone over a width of 22.13 metres. On 

section 15E the best values are in hole LR-87-5 assaying 63 ppb 

Au over 0.92 metres within a carbonatized and silicified 

alteration zone over 11.71 metres. 

Seal River Explorations Limited in late 1991 carried out 3.8 line 

kms of induced polarization survey on five test lines. The IP 

survey on the Lightning River Property has outlined two 

interesting anomalous zones along the North Branch of the Destor- 

Porcupine Fault Zone that warrants investigation for pyrite-goIdtype 

-deposits. Anomaly No. l is a one line anomalous I.P. zone 

on line 6E from O to IN with moderate phase, metal factor and low 

resistivity but open along strike. This may be caused by pyrite 

and alteration along a fault. Anomaly No. 2 is an I.P. anomaly 

with high phase and high resistivity over a strike length of 800 

metres and open. Line IDE is the exception with high metal 

factor, phase and low resistivity. This zone may be highly 

silicified with pyrite mineralization. 

An exploration program to investigate the I.P. anomalies 

consisting of prospecting, soil and rock geochemistry and diamond 

drilling of two holes totalling 300 metres if warranted is 

recommended at a cost of S 30,000.


An Induced Polarization Survey has been completed on the 

Lightning River Property in Lamplugh Township, Ontario. The 

exploration program was partially funded by the Ontario Mineral 

Incentive Program (OMIP). The geophysical ground program was 

designed to locate the North Branch of the Destor-Porcupine Fault 

and to investigate the alteration zone with low but anomalous 

gold values in diamond drill hole No. LR-87-1. 

2.O PROPERTY 

2.1 Claims 

The Lightning River property consists of 41 contiguous, nonpatented 

mining claims located in Lamplugh Township in the Larder 



and are numbered as follows: 



The claims total 1640 acres or 


663 hectares and are registered

7 


The property Is located 3 km (2 mi) south of Lake Abitibi in 

Lamplugh Township, 58 km (36 mi) northeast of Kirkland Lake in 

Northeastern Ontario. Access to the property is via Highway 101, 

east for 52 km (32 mi) from Matheson, Ontario and north from the 

highway along a logging road for 5 km (3 mi) to the claims. 


Topographic relief on the property is 50 feet and the elevation 

is 950 feet above sea level. The Makua Creek flows northerly 

through the property toward Lake Abitibi. Overburden averages 15 

metres to bedrock. 


growth. 

There are a few small intermittent streams on 

the claim group. 

Water for 

drilling purposes is probably available from the small 

lakes and ponds on the property or from old drill holes eg. 

LR-87-1,2,4,5 and 6. 


of northern Ontario with snow cover and 


8 



During the early 1980's the McOermott gold deposit was discovered 

by American Berrick Resources Inc. in Holloway Township along the 

McKenna Fault which is a splay fault off the Destor-Porcupine 

Fault. The Holt-McDermott mine started production in 1988 and now 

is at 1800 tons per day. The present reserves are 5.1 million 

tons grading 0.15 oz. per ton gold (N.M. June 10,1991). A new 

deposit, the Mattawasaga deposit was discovered about one half 

mile east of the shaft during 1991 along the Ghostmont Fault. The 

present reserves are two million tons grading 0.18 oz. per ton 

gold (N.M. June 10,1991). These deposits consist of mineralized, 

altered (silicified, carbonatized) basalts. The gold is 

associated with pyrite (N.M. 6/10/91). 

The Lightning Zone was discovered in Holloway and Harker 

Townships by Noranda, Freewest and Newmont in 1988. The zone 

occurs along the mafic-ultramafic volcanic contact just north of 

the Destor-Porcupine Fault. The reserves are 5.5 million tons 

grading 0.27 oz. gold per ton (N.M. October 7,1991). 


area. 


The airborne magnetic and electromagnetic survey of the Matheson-

Black River Area was carried out by the Ontario Geological 

Survey In 1984. Lamplugh Township Is covered on Map 80589. 

9 

The Lightning River area was mapped by L.S. Jensen for the 

Ontario Geological Survey In 1973 on a scale of one Inch to one 

mile (Map P.2433). 


The area was mapped by the Ontario Geological Survey (OGS-Jensen- 

Map P.2433-1982, Lightning River Area). 

The area was flown by the Ontario Geological Survey using the 

Questor Input System with flight lines spaced at approximately 

175 m to produce an electromagnetic and a total intensity 

magnetic survey (Map 80589, Matheson-Black River Area, Lamplugh 

Township, 1984). 

In 1987 the present claim group was covered with ground 

magnetometer and VLP-BM surveys, geological mapping and limited 

gold-humus geochemistry and lithogeochemistry. The 1987 diamond 

drill program consisted of six drill holes for a total of 1598 

metres. This work was carried out by Pronto Explorations Limited. 

Seal River Explorations Limited in 1991 carried out 3.8 km of

induced polarization surveys. Five lines, 6E, SE, 10E, 13E and 

15E were profiled. 

10

11 

4.O GEOLOGY 


The Harker-Holloway area is part of the Abitibi Volcanic Belt of 

Northeastern Ontario adjacent to the Quebec border. The main 

branch of the Destor-Porcupine Fault strikes east-west through 

the area. The rocks to the south of the fault are Kinojevis Group 

of rocks and these rap around to the north of the fault. The core 

area along the Destor-Porcupine Fault is Stoughton-Roguemaure 

Group of rocks while Hunter Mine Group of rocks occur to the 

north of the fault. In Holloway Township the McKenna and 

Ghostmont faults are splay faults off the Destor-Porcupine Fault 

to the south-west through Kinojevis Group of rocks. The North 

Branch of the Destor-Porcupine Fault is a splay fault to the 

northwest through Kinojevis and Stoughton-Roguemaure Groups to 

the north of the fault and Hunter Mine Group to the south of the 

fault. 


The claims are underlain by basic volcanics, iron-rich and 

magnesium-rich mafic volcanics, felsic volcanics and diabase 

dikes and mafic intrusives. The North Branch of the Destor- 

Porcupine Fault zone strikes through the southern part of the 

property at 120 degrees and dips steeply north. The mafic

12 

volcanics to the north of the fault are Stoughton-Roquemaure 

Group rocks while the felsic volcanic rocks to the south of the 

fault are Hunter Hine Group rocks (Jensen L.S.-1983-OGS Map 

P.2433: Lightning River Area). 

The strike of the rocks on the property is 120 degrees and 

dipping steeply north.

13 



Gold deposits in the Harker-Holloway are associated with the 

following geological environment: 

1) The Lightning Zone gold deposit occurs along the Destor- 

Porcupine Fault Zone at the contact between mafic and ultramafic 

volcanics. The host for the zone is a strongly altered and 

mineralized variolitic basalt. The zone is generally conformable 

to the local stratigraphy/ which strikes east-west and dips south 

at 65-70 degrees. The zone rakes to the east and tops at 250m 

below surface. Mineralization in the Lightning Zone is primarily 

pyrite which varies in content from 2-15% / averaging 5-8* in 

areas with greater than 5 g/t Au. Concentrations of fine K2mm) 

pyrite vary in proportion with gold grades. Coarse pyrite which 

is barren is found along with trace amounts of chalcopyrite and 

arsenopyrite. Alteration is a pale-green to honey colored quartzanker 

ite-sericite assemblage which occurs intermittently 

throughout the mafic volcanics. The Lightning Zone itself is is a 

medium to grey in color generally lacks foliation and consists of 

a guartz-albite-pyrite assemblage. Original primary features such 

as pillow magins, flow contacts, and variolites are commonly 

preserved in the Lightning Zone and in the surrounding rocks. The 

zone has a strike length of at least 780 metres and is open down 

dip and to the east (John Wakeford and lan Atkinson, PDAC-1991).

14 

2) The MeDermott gold deposit Is located along the McKenna 

Fault. The Mattawasaga gold deposit is located along the 

Ghostmont Fault. These are splay faults striking southwest off 

the Destor-Porcupine Fault. These faults occur long the contact 

between iron-rich and magnesium-rich tholiitic basalts with 

possible interflow sediments. The mineralization consists of 

finely disseminated pyrite which is directly proportional to the 

grade of gold. Gold is rarely visible occuring almost entirely 

within finely disseminated pyrite. Alteration consists of very 

strongly silicified and to a lesser extent carbonatized basalt. 

The average thickness of the Mattawasaga deposit ranges from 30- 

80 feet. 


Alteration zones consisting of strongly silicified and 

carbonatized zones over widths of 17-22m along the North Branch 

of the Destor-Porcupine Fault. This fault is located along the 

contact between felsic volcanics to the south and mafic volcanics 

to the north. Hole No. LR-87-1 on section 8 East encountered 

anomalous gold values of 73 ppb Au over 3.99 m within a 

silicified and carbonatized zone from 228.78m to 250.91m over a 

width of 22.13 m on the footwall of the North Branch of the 

Destor-Porcupine Fault. The best assay is 189 ppb Au over 0.91 m.

15 

The alteration zone Is within a highly fractured and brecciated 

zone with less than l* pyrite. Hole No. LR-87-5 on section 15 

East intersected alteration zones consisting of strongly 

silicified and carbonatized basalt within strongly fractured and 

brecciated zones along the North Branch of the Destor-Porcupine 

Fault. These zones of alteration occur over widths ranging up to 

17m but the gold values are very low.

16 


Reroy Belanger (Geophysical Contractor) carried out an induced 

polarization survey over five test lines, 6E, 8E, 10E, 13E and 

15E, using a metric grid system. A total of 3.8 kms of 50 metre 

spreads 11=1 to nM was used with 1.0 hertz frequency measuring 

the phase in millirads. The survey uses a dipole-dipole array 

with a 

50 m spread. A Phoenix, Turbo V-4 receiver and a Phoenix 

T-l transmitter was used to carry out the survey generating 1.0 

kw. of power. 


pseudo-sections of the calculated apparent resistivity, phase and 

metal factor. 

Plan maps are presented as surface projections of 

the interpretated I.P. anomaly zones, Frazer 

Frazer filter phase and Frazer filter metal factor. 

filter resistivity.

17 

7.0 DISCUSSION OF RESULTS 

Interpretation of the induced polarization survey by Belanger has 

resulted in four anomalous I.P. zones, two of which warrant 

follow-up as follows: 

1) I.P. anomaly No. l 

Anomaly No. l on line 6 East at O to l North is a one line 

anomaly with low resistivity (28 OM), high phase (3 MRAD) and 

high metal factor (42.9). 

This I.P. anomaly may be caused by an alteration zone (silicified 

and carbonatized) along a fault zone similar to the zone in hole 

No. LR-87-1 on section 8E but stronger pyrite mineralization. 

2) I.P. anomaly No. 2 

Anomaly No. 2 on lines 8E, 10E, 13E and 15E at 3N to 5+50N has 

high phase (3.7 MRAD) and high resistivity (2249 OM). Line 10E is 

the exception in that this line has high phase (3.7) and high 

metal factor (39.4) with low resistivity (70). Line 10E and 13E 

has the highest phase while line 13E has the highest resistivity. 

This I.P. anomaly may be caused by a silicified zone along a 

fault with disseminated pyrite.

18 


The induced polarization survey on the Lightning River property 

has outlined some interesting anomalies along the North Branch of 

the Destor-Porcupine Fault that warrants exploration for gold. 

The I.P. anomalies that warrant follow-up are as follows: 

1) Anomaly No. 1: 

This is a one line anomalous I.P. zone on line 6E from O to IN 

with moderate phase, metal factor and low resistivity but open 

along strike. This may be caused by pyrite and alteration along a 

fault. 

2) Anomaly No. 2 

This zone is an I.P. anomaly with high phase and high resistivity 

over a strike length of 800 metres and open. Line 10E has high 

metal factor, phase and low resistivity. This zone may be 

strongly silicified with pyrite mineralization. 

The model for this property is a gold-pyrite deposit associated 

with silicified and carbonatized alteration along the North 

Branch of the Destor-Porcupine Fault similar to the Harker- 

HolIoway model. 

Hole No. 

LR-87-1 on section 8E encountered 73 ppb Au over 3.99 m 

within a silicified and carbonatized zone over 22.13 m on the

19 

footwall of the North Branch of the Destor-Porcupine Fault Zone. 

The best assay Is 189 ppb Au over 0.91 m. 

Anomaly No. l can be best tested by diamond drilling. 

Anomaly No.2 has outcrop on the north flank that can be 

investigated by prospecting and sampling. The anomaly itself can 

be tested by gold in humus analysis followed by diamond drilling 

if warranted. 

An exploration program consisting of prospecting, soil and rock 

geochemistry and diamond drilling of two holes totaling 300 

metres is recommended at a cost of $ 30,000. 




F. J. Sharpley

20 

REFERENCES 


(1991) 

EMR 

(1981) 

Jensen L.S. and 

(1983) 

Jensen L.S. 

(1983) 

ODM 

(1971) 

ODM 

(1973) 

OGS 

(1985) 

OGS 

(1985) 

OGS 

(1984) 

OGS-GSC 

(1959) 

1991 

Sharpley F.J. 

(1985) 

Sharpley F.J. 

(1986) 



Lamplugh Township, Ontario, for 


Topographic Map: 32D/12 

Lightning River; 1:50,000 

Langford P.P. 

Geology and Petrogenisis of the 

Archean Abitibi Belt in the Kirkland Lake 

Area, Ontario; O.G.S.-O.F.R.-5455 

OGS Map P.2433 - Lightning River Area 

Geological Compilation Map 

l"- 4 miles 




Geological Data Folio 


GDIF 267 

Preliminary Results of Bedrock Sampling from 

the Sonic Drilling 1985; 

Lake Abitibi-Matheson Area, District of 

Cochrane, Ontario. 

Map 80589 

Matheson - Black River Area; Lamplugh Township 

Airborne Electromagnetic Survey; Total 

Intensity Magnetic Survey. 

Aeromagnetic Maps 

1493G - l"* 4 miles 

45G - l"* l mile 


Summary Report on the Lightning River Property 

Lamplugh Township, Larder Lake Mining Division 

Ontario, for Seal River Explorations Limited 

Report on Geophysical Surveys, 

Lightning River Property, Lamplugh Township

21 


Pronto Explorations Limited. 

Sharpley F.J. Report on Geological Mapping and Geochemistry, 

(1986) Lightning River Property, Lamplugh Township 


Pronto Explorations Limited 

Sharpley F.J. Exploration Report, Lightning River Property, 

(1991) Lamplugh Township, Ontario, for 


(1978) Airphotos: 1:20,000 

78-1-4824-05-59..64 

80-4823-3-48..59

22 














6) That I have a financial interest in the Lightning River 

Property. 



F.J. Sharpley

23 

APPENDIX I: 

LIST OF FIGURES

^ |T \ r- 1 v

CEOPHYSICSICEOCHEMISTRY (35) 

N-S LINES (km) 

524__545 566___587 608 

1 y ' *O^ 

^^S^^lT^r^^^^' J is" 48* 19 

PROTEROZOIC 

ARCHEAN 

Predominantly sediments 

(Cobalt group) 

11S. 14.12.111 Felsic intrusive rocks 

10 

Mafic-ultramafic 

intrusive rocks 

Metasediments 

"j Paragneisses and 

migmatites 

J Felsic metavolcanic rocks 

-i Intermedlate-felslc 

l metavolcanic rocks 

-l (Blake River group) 

j 5 j Mafic metavolcanic rocks 

^ l Mafic-ultramafic 

I" 

^——.—l metavolcanic rocks 

'Timiskaming group 

--—— Destor-Porcuplne 

DPFZ Fault Zone 

KLFZ 

RLB 

LAB 

WB 

PR 

BRS 

Kirkland Lake-Larder 

Lake Fault Zone 

Round Lake Batholith 

Lake Abitibi Balholith 

Watabeag Batholith 

Paleozoic rocks 

Blake River Synclinorium 

Fault and/or shear zone 

km 

Syncline axis with 

plunge direction 

- - ~ ~ — geological contact 

Fljore 35.4. Gcneratizcd geolopcaf map of the study area. The geology is simplified from a new geological compilation of ihe area (Ontario 

Geological Survey, in prep.). The location of north-south and east-west Oouguer gravity profile! are also shown. 


GEOLOGICAL LOCATION MAP 


LAMPLUGH TOWNSHIP, ONTARIO 

LARDER LAKE MINING DIVISION

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24 

APPENDIX II: 


25 



LAMPLUGH TOWNSHIP-ONTARIO 

D.D.H.l l NORTH l EAST l SBC l AZ l DIP l DEPTH lANOMl REMARKS/ASSAY 


LR-7-92 0+75N 6-l-GOE 6E 200 50 150 l IP anomaly 

LR-8-92 5+75N 13+OOB 13E 200 50 150 2 IP anomaly 

TOTAL FOOTAGE 

300m(984.3')

26 

APPENDIX III: 


27 



A. Diamond Drilling: 300m x $ 60/m $ 18,000 

B. Assays: 70 Au/ppb x SlO/spl. 700 

C. Geologist and Sampler: $400/day x 10 days 4,000 

D. Camp Costs: $40/day x 10 x 2 men 800 

E. Transportation: 2000 kms 9 $0.40/km 800 

P. Grid ReHab 6 soil sampling: 7 days x 2 x 9200 1,200 

G. Assaying: 100 Au-humus 8 $8/spl 800 

H. Camp Costs: 940/day x 10 x 2 800 

I. Transportation: 1600 kms 8 SO.40 640 

J. Report: 5 days @ S3007day 1,500 

TOTAL: 9 29,240

28 

APPENDIX IV: 


29 

Summary of Expenditures - 1991 


1. Linecutting: Re-Hab.Lines-10/28/91-11/03/91 

3.8 line kms * 0.6 kms BL* 4.4 kms S 2,377.39 


3.8 kms-11/28/91 2,140.00 

3. Drafting 4 Printing: 100.76 

4. Report: 1,500.00 

TOTAL: 9 6,118.15


30 

Expenditures-OMIP- October 28 - December 31/91 

1. Supplies: Week's Hd we-Burl, -f lagging -.10/10/91 9 28.71 

2. Supplies: Bulk Barn-Bur1-groc:10/10/91 6.65 

3. Supplies: Week's H d we -Bur l -chain .-10/10/91 6.63 

4. Supplies: Post-Burl-10/10/91 3.69 

5. Supplies: Home Hdwe-N.Liskeard-flagging:10/12/91 25.77 

6. Supplies: Home Hdwe- " -clips:10/12/91 .91 

7. Room fi Board: South Y-Kirkland L-10/28/91-11/03/91 355.29 

8. Contract: G.Moonie-linecutting:10/30/91-11/02/91 445.00 

9. Transportation: 4x4 vehicle: 1744 kms @ SO.40 697.60 

Burl-Matheson:10/28/91-11/03/91 

10.Supplies: BPX:11/9/91 6.36 

11.Supplies: Rapid-prints: 11/9/91 14.19 

12.Supplies: Me Reproductions:prints.-11/25/91 65.89 

13.Pees: F.Sharpley-7days G SlOO/day 700.00 

-linecutting-Oct.28-Nov.3^1 

14.Supplies: Guillevin Intern.-K.L.-spray paint^0/30/91 20.70 

15.Contract: Remy Belanger-I.P.surveyrNov.28/91 2,140.00 

3.8 kms t $500/km 

16.Drafting: Castello Cartographic Serv: 12/31/91 86.96 

17.Prints: McRepreductions: 12/31/91 13.80 

18.Pees: P.Sharpley-Report:12/31/91 

5 days at $300/aay 1,500.00 

TOTAL: 

S6,118.15

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t^2 

4f* 6t^ 

4S8 

- ffi 

41 i 4(10 

3^7 

4fi 

i S6 46* 

4SS ft 4 

*ro 

fi/ 

4t9 

j-,1 

49? 41, 

44? ' S06 

45* 591 

•Hi? 

Sil 

t Ji 

t, f S 

f, 2 f 7?3 

)li* 7} -f 

tat, 

ri f 

^yv 

'ft 

5 f ^ — ^ 7 J 

)î t/5 

sai rg 3 

S7J 

5S4 

l*^S^SS^;^5i i If j^3S^S:i 23*55 

- , 

itz s*7 

•)0S 6*4 

}O4 S2* 

499 f, 4J 

fit 

f 23 

f 3o 

))S 

" bZd 

i)' 

644 1,40 

6(7 7ff 

gf 

aft 

la 74 Si 3 

98 ZL 827 

/* -t - TJ.S 

f9g f 74 

fft- 6*S 

ill 

6Si 

St*) 640 

ffi 

b*-* 

f * 43 "J 64.3 ~ 

414. -t'J -t 

^JO 

en 

1 '19 

s*-'*' -J 66 d -1 55" 

ie 4 y 

J^t'3 

Ilt1* 

14'.'' 

H i'fo r 

\i345 

n 35 

9*7 

\W 

543 

540 

f if 

6t)Z 

84* 

"b 7 

tllol 

9tok 

It 4 

3 /V 

rh 

791 

fi i 

1)20 

)j/ 

413 

4 95 

4)4 

•fH 

421 

442 

too 

iil 

b-tS 

an 

812 

MS 

1010 

1022 

y ft, 

#9* 

841 

got 

f 4 4 

6.11 

6)4 

661 

664 

5S'qk* s^v*^*Si"ft* ^ 

i, J "l" 1 V| t( ^0 ^ 

' ,' 

.}^5 ———— 

SJ7 

fit 

523 

6V}- 

i*/ 

623 

roi 

0/3 

7 H J 

T d t 

6 &I 

iff- 

(46 

*4* 

.t* 

f J S 

/Ml 

7'0 

Oil i 

661 

(.'/O 

601 

6ft 

7/2 

4*1 

as* 

; b e 

65* 

fat 

SIS 

tic 

S*-* 

65t 

t 

- 4 tt -| 4f4 -, ttfj -, 471 

•J fi' 

•)H3 

- 

- 

- 

- 

i/i 

f." 

-tet 

•i** 

J&7 

45' 

-tt t 

934 

at 

49Z 

494 

SOt 

f!l 

t'o2 

S42 

5* j 

6/y 

c J& 

tit,* 

iti 

83? 

at j 

^ O y 

itii y 

y/ 

Ait 

7. v 

fS7 

\A 

s '83 îw^ u^nj^^î^* vdviii S 

S66 

}fl —————— —————————— 

sri 

ffo tOS 

6*8 

7*3 

•f 60 

mid 

tt ST 

f/ j * t^ 

6 f lo 

646 , * 

6*7 

781 

lib* 

14/1 

ft 34 

us 

6** 

.f) 

144 

iot 

j * 

'04 . 

(tl * 

61. 

311 

3** 

S/-' 

5" ' 

f u 4 

6 7 7 

"S4lj 

Si 7 

5 14 

540 

fit 

6etl 

89? 

'•l 

Hit* 

Hi) 

lyof 

j's 

83 ~ 

it, i 

la on 

9J5 

944 

904 

tit, 

76 J 

'49 

tiff 

6S7 

* 3^ 

b'/ 

614 r. 

7 "* 

9)4 

t6U 

t ri 

101 

t 'S 

t,Sl 

en- 

699 

Hi 

gat 

7*1 

li Z 

b7f ~ 

(38 

*48 

*Sn 

to76 

619 

t/*- 

786 

831 

' . 

Ka 7 

798 

-86 

tt t 

608 

S96 

K i* a 

* )4 

49't 

4:1? 

•It* 

S n 3 

4*1 

fid 

S2* 

S 73 

6/t 

7 S3 

746 

1 20 

(VI 

7ft 

a 9 5 

n 1 Z 

"131 

9 + Z 

lot* 

it ni 

16) b 

890 

77S 

le, d 

t'7 

634 

tt 23 

6^5 -~ 

641 

641 

tS 1 

b 5* 

4J1 '* 1*'* \n tt ^ 

, f ' 

-53/ ———— 

645 

6V/ 

'/J 

j 93 

513 

}4g 

5 SO 

fit 

f 4! 

345 

S 40 

546 

Sf 

iSf 

5'' 

Jio 

I9H 

11,14 

958 

tii 

US 

Itt 

610 

5 2/? 

i^y 

4- y 3 

67 y 

5±5 

5*3 

Sg4 

St' 

S 83 

it.* 

f 67 

S27 

S* •f 

S7S 

J"7 

Sil 

fzi 

f f* 

4 it / - i 6f -1 jj^ -1 S'9 -J 5/3 O5 

S43 

ft 2 

f 84 

961 

i'9t 

ft* 

1 84 

7/2 

7S 8 

787 

829 

969 

946 

8Z^ 

7f9 

70S 

625 

S -f t 

577 

it5 

57* 

s^^ 

ft( 

S 61 

572 

S 73 

974 

513 

567 

672 

S69 

364 

f66 

SS9 

568 ^^ \r.^ 

54 Q 

549 

536 

S' 7 

fi3 

921 

S 46 

549 

5 81 

63y 

697 

Sio 

"82 

17 + 9 

23o9 

Zi 78 

167 1 

12 3 t 

1009 

8f4 

114 

70* 

6,19 

646 

(.03 

fit 

S6* 

•i H 

Sf 

f 94 

- S7S 5 N -1*4? 

59a 

- 

iiSSsU?? 

- 

- 

- 

tt} 

696 

lit 

111 

6*6 

*62i 

S3 2 

f. t 

tS4 

5 27 

Se/ 

St6 

Sti 

4tf 

Si' 

410 

41Z 

4*1 

497 

499 

sai 

491 

496 

492 

496 

fat 

f IS 

fif 

SI6 

St6 

499 

j;/*" s K ft * s 5 

szo —— -4- 

494 1 

for 

f 49 

SI 4 

fti 

648 

618 

746 

9f7 

1016 

I3f9 

170 •f 

H64 

iSSt 

1293 

1074 

9t^ 

Ttl 

74* 

1t9 

689 

678 

6*6 

it' 

f 19 

S6S 

fS4 

S3 3 

fzz 

S'4 

tm 

SI6 

SI 6 

Stl 

S3S** 

- 

- 

- 

- 

T44 

i 't 

f'6 

St 4 

fit 

441 

SH 

(16 

Sit 

521 

iti 

tin 

489 

4tt 

474 

46t 

4ff 

4fo 

437 

4(0 

4&Z 

4(Z 

46* 

411 

•192 

SOS 

SIS 

SI4 

Sil 

St r 

SiS 

f (3 

894 "\f- ^ ^ci^ *Vi uiîoiNjf 

44 1 ^y^ltiof ^*MP^*O*OD 

' •\^lâ'fl\ir*3\(J\"r\0\AO\00 

111 

T 'f t 

tan 

10 t* 

ltS4 

it Sil 

98' 

tit 

aa 

784 

lil 

ir* 

6(1 

646 

932 

(33 

641 

119 

r/6 

668 

f8i 

547 

S3* 

ill 

f 00 

fa f 

so^ 

in 

5/J 

^ 

. 

^ 

- 

584 

til 

S94 

S09 

Mf 

431 

466 

401 

460 

49) 

f 19 

Slo 

fto 

fs) 

5ti 

61" 

nt 

74 ^ 

7*7 

ri r 

6(4 

Itt 

i 90 

ft? 

39? 

S99 

601 

(tt 

6?) 

1/4 

169 

819 

846 Base line 

67107 Bearing I38 0 

7** 

1S6 

li* 

7 09 

69s- 

(89 

it f 

6.10 

Stt 

S At 

S3* 

J" 

f03 

f'6 

319 

St 6 

fi* 

Si 7 

514 

So 4 

4t9 

4 IS 

413 

476 

476 

479 

4H(, 

/vo 

7 7* 

T34 

LEGEND 

V 

( arid line with lOOm stations —'—— i — 

i 

nstrument.......... ....Geometrics G 816 

F leading m gammas above bate level of 

f18,000 gammas ......... ...... . ...-f 9 * 6 

HDHIt —— " 

SHEET INDEX 

0 S \ 

s 

s 

\ 

s 

SEAL 

RIVER EXPLORATIONS LTD. 


LA RHINE RIVER PROPERTY 

yt) 

Magnetometer Survey 

TOTAL FIELD READINGS 

0 100 200 300 400 

1 i i i 1 - ' ' ' ~" 

METRES 

Date: December 1991 | N.T. S. Ret: 32E-4 

Dwq 

No. 

S-QI-R 91 u -01 \-/ 1 

Illllllllll 

•IlllillJJll""" 32E048E003SOMBM38 ABBOTSFORD 

200 *-w~ 

""""" ' ' 

'

LJ 

O 

rO 

UJ 

O) 

ro 

UJ 

00 

ro 

UJ 

O 

UJ 

OJ 

UJ 

UJ 

10 

UJ 

CD 

UJ 

O 

in 

UJ 

CVJ 

in 

ui 

in 

5 N 

Base line 

Bearing I38 0 

LEGEND 

Grid line witn 100m stations 

—'——i— 

Instrument . Geometrics G8I6 

Profiles plotted thus - t— --t— -~ 

o 

o o 

Gammas ^ 

CD 

o 

o 

Grid line -* 

58,400qammos 




SHEET INDEX 

Magnetometer Survey 

TOTAL FIELD PROFILES 

O 100 

Li r t l 

200 

.l 

MFIRES 

300 

t 

400 

Date December I99I NTS. Ret- 32E-4 

Dwg 

No 

S-9I-8-02 

32E046FQ036 OMB1-138 ABBOtSFOR 210

954880 

954873 954879 

954544 

954545 

954872 

1185946 

1015854 X 

Base line 

954542 

954546 

954871 

Bearing 138 

954870 

954530 

954531 

Claim 1185946 

X 1600m 

954526 

954532 

954527 

LEGEND 

Grid line witn lOOm stations 

Claim post, located, unlocoted 

Claim lines . ......... . ,^. 

Drill road - - 




SHEET INDEX 

TOPOGRAPHY 

O 100 

t l I l t 

L'OO 

t 

MFTUFR 

300 400 

d 

Date 1991 NTS Ret- 32L-4 

Dwg 

No 

S-91-8-03

LEGEND 

i P ANOMALIES 

Definite 

2! Probable 

' ~i Possible 

•••iMM Totol Field Mag Trend 

•••MUM ^radiant Mag T-end 

•"II".*.'-* Major ResiS'ivtty Lew 

E M 

Ano-"-clv 

C 

'\~Ro5vES 

-E-S'C "C NTERVED'ATE NT 

VE T ASEDIVENTS 

MEV AVOLCANICS 

a) Felsic to intermediate 

* b) Mafic to intermediate 

C ~~T?I* OC3''Or 

•*—O 3 arror-c Ir. * Hole 

^v X " ..'C'Ot , 3 r eQ 0^ 3utC'0; 

—6- jiacici S' r ae 

Se!" s'osi'y iclined, \i5'' "o 

q 'op .ndica'ec: '^ -' 

Keldor Resources (ne. (198^) 

.O 

^——Sample above Bedrock 

) —— Grams Au m sample 

•Reverse Circulation Drill Hole S Number 

•Overburden depth (metres) 

4^10 \^ 

r 

l 

500 IOOO 

METRES 



HEPBURN TOWNSHIP 

COMPILATION MAP 

*" * 

ONTARIO 

32ED4SE0035 OM91-1M ABBOTSFORD 

Dcte : December 1991 

hs f. J. Sharpley 

Dwe.NaS-91-9-04 

I'Mm 

*.'- 32 E/4

LU 

O 

fO 

Ul 

ro 

* 

-l 

UJ 

CD 

ro 

UJ 

O 

UJ 

CVJ 

UJ 

Ul 

(O 

UJ 

CD 

UJ 

o 

in 

UJ 

(VJ 

in 

UJ 

^ 

in 

5N 

Base line 

Bearing 138' 

5S 

5s 

LEGEND 

Grid line with 100m stations -4- 

Inttrumtnt ........ .........Geomttrici G 816 

4- 

Profiles plotted thus :- —i——t——i— 

X v '•J i 

o DO 

Gammas !2 {^ OD ' 

IP ANOMALIES 

Definite 

CZ3QZZ39 

Probable 

Grid line -* 

68,400 gammas 

SHEET INDEX 



LA HEINE RIVER PROPERTY 

GEOPHYSICAL COMPILATION 

HPH 

j Possible 

240 

O 

t 

100 200 

- -t— 

METRES 

300 400 

Date: December 1991 N.T.S. Re f: 33E-4 

Dwg 

No. 

S-91-8-05

i 

y- 

o 

CO 

O 

o 

t/) 

LEGEND 

MAFIC INTRUSIVES 

FELSIC TO INTERMEDIATE INTRUSIVES 

METASEDIMENTS 

M'ETAVOLCANICS 

A) Felsic-to,Intermediate 

B) Mafic to Intermediate 

cjiRON FORMATION 

li 

lol-S 

l 

K 

9 

Ih 

Mm 

mug 

PIT 

Po 

eh 

ep 

lehliion 

iiiiciriid 

brieclgltd 

corbonollnd 

nrleltliid 

• mphibol i l lz*d 

gar n* ft 

f rogmtnlol 

dloritlc.gabbroic 

t uf t acicui 

alteration 

ihtortd 

himatltt 

magniilit 

tom 

quarlt vtln 

py r r ho 1 1 t* 

c her t 

chai o opy r i t * 

NOTE- 

Fault 

Zone 

ppbAu/cor* l*ngth 

Aiiayt ^0 ppb Au not 

ihown 




GRID A3 

SECTION 

LOOKING 

EAST 

2E 

METRES 

Date; Sepf 199 1 N.T.S. Ref; 32E-4 

Dwg. No. 

S-9/-3-OI 

250

o 

Ci PR-11- 3 

U) 

S 2 

O —— 

-h 

•ô 

LEGEND 



METASEDIMENTS 

METAVOLCANICS 

A) Felsic-lo,Intermediate 

B) Mafic lo Intermediate 

CjIRON FORMATION 

IChlttOM 

f 

l 

l 

K 

fl 

H 

d 

t 

tlllciritd 

brtcclaltd 

carbonailttd 

• irlcliltfd 

•mphjbol i 11 i*d 

g a r n 111 

f ragmentol 

dlorilic-ga bb ro| c 

tuffocaout 

altaration 

bondtd 

tom 

• h 

htm 

PIT 

q.V. 

PO 

eh 

cp 

ihiortd 

htmalll* 

magnilllt 

pyrlli 

quorlt vtln 

py r r ho t i te 

c her t 

chai copy r i t a 

F Z Fault Zone 

73XS99m 

p pb Au X core l englh 

NOTE. Aitayt ^0 ppb Au no) shown 




GRID A6.A7 

SECTION 

LOOKING 

EAST 

1E 

METRES 

40 

Date:l Seph 1991 N.T.S. Ref: 32E-4 

Dwg. No.

o PR- firt 

JL. 

Q 

O 

O 

O 

CO 

LEGEND 



METASEDIMENTS 

METAVOLCANICS 

A) Felsic-to,Intermediate 

B) Malic to Intermediate 

CJIRON FORMATION 

(03. O* 

a 

t 

f 

l 

J 

K 

o 

ichltloti 

illlclflid 

br*cclaled 

••rbenollttd 

iirlclllxid 

• mphibol i 11 

fragmental 

dlorific-ga bb ro l c 

tuffaceous Son.Jed 

alttration i on t 

ft) a (j 

Pf 

q.v 

po 

eh 

cp 

magnillit 

pyrll. 

quarlt 

py r rhot l le 

c bar t 

cha l c opy r i t e 

Foull 

Zona 

ppbAu/cora length 

NOTE 

Assays

LEGEND 

••• Total Field Mag Trend 

••MUM Gradiant Mag Trend 

•.' 

.-' Majo' Resisttvtty Low 

G E M Anomaly 

MAFIC tN T RUSIVES 

FELSIC TO INTERMEDIATE NTRUSIVES 

METASEDIMEMTS 

A O 

•*—O 

•1^ x 

—e- 

METAVOLCANICS 

a) Felsic to Intermediate 

b) Mafic to Intermediate 

Fault 

Sarrole location 

Diamonc Drill Hole 

C'otcrop, arec of outcrop 

Glacial Str ae 

fe-4-*- < t > Schistosity , 

—p- —i— 

inclined, vertical 

8eddmg. too rdicated, *oq unkown 

Geochemical Humus Amomaly 

V 

••••••••••IIIIMMMM 

j } Canadian Javelm Limited (1965) 

2 ) Canadian Superior Explorations Limited (1966) 

\ \ X ^ 

Gold Hill Resources Inc (1984) 

J^'*" \ i^-' 

\ 

i f ^ ' 

l ! l ' x.,'——"~^ A 

500 lOOO 

METRES 


BATHOLITH 

PATTEN RIVER PROPERTY 

ABBOTSFORD TOWNSHIP 


ONTARIO 

32E04SE003S OW91-138 ABBOTSFORD 

REVISED SEPT. , 1991 

Dwg. No. 

Date' Aug., 1988 By- F. J. Sharpley N.T.S.: 32 E/4 

S-91 -3-04J 

•** - *.

tON 

S N 

i Y i ~'..'.-' 

i \ ^ '" 

' \ \... -'I.PHtflh 

u - pnosa 

..-- --\--J 

\ i. 

• — ' * 

"'"ifitfjiiiiii. ' 

* i * 

^ 

l 

BASE LINE -O - 

41 \.\ i t ' * ' *- 

l \ . * ! 

J \ . -l - 7 i 

OU-O 

5S 

LEGEND 

Feldspar porphyry 

Diabase 

Tholeiitic basalt (iron rich) 

Tholeiitic basalt (magnesium rich) -, Andesite 

a 

b 

c 

d 

e 

f 

9 

h 

i 

j 

k 

l 

m 

n 

Felsic tuff .dacite . rhyolite 

Schistose 

Pillowed 

Variolitic 

Fragmental 

Silicified 

Brecciated 

Oioritlc 

Chloritic 

Tuffaceous - banded 

Dacite flow 

Rhyolite flow 

Carbonatized 

Pyrite 

Magnetite 

SYMBOLS 

'~) Rock outcrop 

j-*- Schistosity 

"*\ Topographic high 

rr Truck road 

zr Tractov road 

Claim post-assumed, observed 

Sample number 

Swamp 

D.D. Hole - horizontal projection 

O.B. Overburden -vertical depth (metres) 

+ Assumed claim oost (new claims) 

32E04SBD03S OM91-138 ABBOTSFORD 290 

l. P ANOMALIES 

Y//S//A Probable 

Possible 

E M-16 conductor axis from 

profiles (NAA Cutler Maine) 


LAMPLUGH TOWNSHIP,LAROER LAKE MINING DIVISION 

LIGHTNING RIVER AREA, ONTARIO 


DATE: DEC. 1991 J BY: F.J SHARPLEY OWG NO. s-si-7-oi

ION 

•;V-r? 

:- '"^'"iiiiiiitjrviiiirtMJuiiiiiiMij 

: -X:. 

/6o *.TI 

•j;"- 1 "\ 

^^H : v 

" 

5 H 

^..v'^r111"/""1 

# i-- -.w-i-rii e \ 7 

'7 ^ ' ^ " 7 ~ 

lliit 

N 

BASE LINE -O - 

^/-r - 

J \ t 

5 5 

LEG E 

N 

Feldspcr porphyry 

Diabase 

Tholftiitic basalt (iron rich) 

Tholeiitic basalt (magnesium rich) -, Andesite 

a 

b 

c 

d 

e 

f 

9 

h 

i 

i 

k 

l 

m 

n 

Felsic tuff .dacite, rhyolite 

Schistose 

Pillowed 

Variolitic 

Fragmental 

Silicified 

Brecciated 

Dioritic 

Chloritic 

Tuffaceous - banded 

Dacite flow 

Rhyolite flow 

Carbonatized 

Pyrite 

Magnetite 

f 

i 

SYMBOLS 

) Rock outcrop 

*-^ Schistosity 

; Topographic high 

x*f 

rr Truck rood 

^— Tractor rood 

Claim post-assumed^ observed 

Sample number 

Swamp 

D.D. Hole -horizontal projection 

O.B. Overburden —vertical depth (metres) 

4- Assumed claim post (new claim- x 

t. P ANOMALIES 

Definite 

V//////1 Probable 

l 

~[ Possible 

32BD4SB003S OV91-138 ABBOTSFORD 

300 

E M -16 co nducter ax i s from 

profiles (NAA Cutter Maine) 

METRES 


LAMPLUGH TOWNSHIP,LARDER LAKE MINING DIVISION 

LIGHTNING RIVER AREA, ONTARIO 


DATE: DEC. 1991 B Y: F. J SHARPLEY DWG. Mo. S-9I-7-OI

32E04SE0035 - Geology Ontario

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