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TARP LAKE AREA - Geology Ontario

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51 C 37' 30' 51 37'30'<br />

51 0 30 00'<br />

Pens f or<br />

la-2c,h<br />

P o, PY. gf<br />

O ov 46<br />

* la;2a,c,f;IF<br />

po. py, cp<br />

AEM<br />

AEM<br />

,la;2h<br />

t P 0 - py, g'<br />

l (X. 2fo,c,f,h;3b;4b<br />

' EM<br />

ovlOO<br />

la 2b3bd<br />

po, py, cp, Au(tr.<br />

ov 45<br />

la;2a,b:3a;6a; 7c<br />

ov<br />

la:3b,d:7c<br />

) '<br />

6v42<br />

la;2b.c,e,3b \<br />

ov40<br />

2o.b,c,f,h<br />

, py, gf<br />

V)0v27<br />

2a,b,c,f,h<br />

py,Hf<br />

O ov57<br />

2a,b,c,f,h;IF<br />

py,9f<br />

\\AEM<br />

la,f;2h:3c<br />

py,gf<br />

ov 30 -^<br />

la.f;4b;IF<br />

r PV, mag<br />

l ov 2o'<br />

'-. ia,f;4L; .<br />

^PV<br />

ov30<br />

2a.b,c,f,h<br />

po,py,Bt,gf ov!5<br />

1a,f;-4b;IF<br />

po, PV, cp<br />

ov 50 -.<br />

lb:2b<br />

py<br />

Ov25'<br />

)b:2b;iFQ<br />

py, mag/<br />

ov 45<br />

la,b;2b;IF<br />

py,mag<br />

ov31<br />

2b;lF<br />

po,py,cp,asp, magVAuttf<br />

,ov54\ v<br />

2b ^ ^<br />

po.py i<br />

ov66"<br />

PICKLE CROWQ<br />

No.2SHAFT*<br />

72l'-1518<br />

ov27<br />

2 b.; IF<br />

po, pv,cp, mag<br />

ovlO PICKLE<br />

la;2b;6a;IF No.3 SHAF<br />

po, py, mag, Au<br />

ov!2'<br />

la;2b;6o;IF<br />

po, py, mag, A<br />

ov27<br />

la;2b;6a;IF<br />

po, PY, mag, Au(tr ov50<br />

C^ Qla;2b,e;6a la;2b<br />

r.) r .j * po, py,cp,Au<br />

\ )la;2b;4b<br />

la;2b;IF j pO,py, Auftr.<br />

po,py,cp,mag, A^<br />

Qovll' ^ Ov65<br />

* la.f;2b,e,f;IF f 'la;2b,e;6a<br />

po.py, mag, tfu po,PY.cp<br />

O ? ,^<br />

? ov<br />

la,f:2b,e.f<br />

py,Au(tr.<br />

26<br />

la;2b,e<br />

'p Au(tr.<br />

OovlO<br />

J py, cp, mag<br />

ov22'<br />

la,f; IF<br />

py<br />

51 C 30' 00"<br />

INDEX MAP Scale l : 1013760<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

20<br />

21<br />

22<br />

23<br />

24<br />

si Jo on<br />

j P23is| Sioux Lookout Data Series Maps Published in this Area.<br />

P2315 Maps in Progress.<br />

SYMBOLS<br />

Drill hole (vertical; inclined; OV - over<br />

burden depth in feet downhole); Lirholo-<br />

gical units are in numerical order and do not<br />

represent abundance or stratigraphic order<br />

Airborne electromagnetic anomaly<br />

Ground electromagnetic anomaly<br />

VEM. . . . . . . . . . . . . . . Vertical loop;<br />

HEM. . . . . . . . . . . . . .Horizontal loop;<br />

VLF . . . . . . . . Very low frequency<br />

Shaft (Depth given in feet)<br />

SPARTAN SYSTEM<br />

1 A Anomaly<br />

1 B Anomaly<br />

x x i 2 A Anomaly<br />

2 B Anomaly<br />

"l 3 Anomaly<br />

~] X - type Anomaly<br />

DATA FILED WITH THE<br />

RESIDENT GEOLOGIST<br />

ONTARIO MINISTRY<br />

OF NATURAL RESOURCES<br />

SIOUX LOOKOUT<br />

Current to July 1, 19V 1 )<br />

Bankur Patricia Gold Mines Limited<br />

Canadian Nickel Company Limited<br />

Central Patricia Gold Mines Limited<br />

Conwest Exploration Company Limited<br />

Cowe Group<br />

Ciowshare Patricia Gold Mines Ltd.<br />

Gateway Patricia Gold Mines<br />

Goldsearch Limited<br />

Greatnat Corporation Limited<br />

(Rio Tinto Canadian Exploration Ltd.l<br />

James Bay Mining Corporation<br />

Kaw-Crow Patricia Gold Mine Limited<br />

New Force Crag Mines Limited<br />

(Crow River Gold Mines Inc.)<br />

Newmont Mining Corporation of Canada<br />

Limited<br />

Norpick Gold Mines Limited<br />

Pickle Crow Explorations Limited<br />

Pickle Crow Gold Mines Limited<br />

Pickwick Gold Mines Limited<br />

Pic Pat Syndicate<br />

Savoy Copper Minus Limited<br />

Success Mines Limited<br />

Transterre Explorations Limited<br />

Union Mmiere Explorations and Mining<br />

Corporation Limited<br />

Union Miniere Explorations anil Mining<br />

Corpoiation Limited and Internanonal<br />

Nickel Company of Canada Limiled<br />

(Joint Venture)<br />

Winoga Patricia Gold Mines Ltd.<br />

Surface showings are nurneious around<br />

Pickle Crow.<br />

"Assay Values<br />

"Prospectus and/or Property Report<br />

*** Pick le Crow Gold Mines Limited<br />

drilled a total of 1 02 holes for a total<br />

length of 58,755 feet. (Not all the<br />

diamond drill holes have been plotted<br />

due to lack of space, therefore only<br />

representative samples of drill holes<br />

have been chosen for plotting).<br />

' " "Winoga Patricia Gold Mines dulled R<br />

total of 50 holes for a total length of<br />

21,927 feet. (Not all the diamond<br />

drill holes have been plotted dje to<br />

lack of space, therefore only rupresen<br />

tative samples of drill holes have been<br />

chosen for plotting).<br />

T Shafts and development work<br />

#An airborne electromagnetic: and magne<br />

tic survey by Umex Corporation Limited<br />

covers the entire map sheet.<br />

Ground magnetic anornal lies a re nut plotted<br />

companies 1 .3,5,13,21 did not show signi<br />

ficant anomallies.<br />

TtDrill logs and locations not recorded.<br />

GEOLOGICAL<br />

60<br />

47<br />

60<br />

61<br />

DIAMOND DRILLING<br />

72<br />

47<br />

48<br />

36<br />

37<br />

77<br />

36<br />

tt<br />

46<br />

34-40<br />

44-46<br />

48<br />

50<br />

64<br />

36<br />

37<br />

50<br />

60<br />

61<br />

71<br />

72<br />

73<br />

73<br />

36<br />

37<br />

SAMPLES CORE<br />

METAL AND MINERAL ABBREVIATIONS<br />

Au . . . . . . . . . . . . Gold<br />

cp. . , . . . . , Chalcopyrite<br />

Cu . . . . . . . . . . .Copper<br />

gf. . . . . . . . . . .(Graphite<br />

gt. . . . . . . . . . . . Garnet<br />

QUESTOR INPUT SYSTEM<br />

[Lino Thiough anomaly normal to flight line)<br />

6 Channel Anomaly<br />

5 Channel Anomaly<br />

4 Channel Anomaly<br />

3 Channe.' Anorridly<br />

AIRBORNE<br />

71<br />

MAGNETOMETER<br />

/1#<br />

TYPE OF WORK<br />

mag . . . . . . . . Magnetite<br />

po . . . . . . . . .Pyrrhotite<br />

py . . . . . . . . . . . .Pyrite<br />

S .Sulphide Mineralization<br />

(tr) . . . . . . . . . . . . Trace<br />

y? 2 Channel Anomaly<br />

'r- 1 Channel Anomaly<br />

v TO77Dnt;ct Ma'j'iet'C Correlation<br />

MP50J<br />

"-j Flanking Magnetic Correlation<br />

il. Limits of Conductive Overburden<br />

- - Axis of Anomaly.<br />

Note:The numbers on the above list stand for the year when the work was done, e.g., 66 for 1966. On the accomp<br />

anying DATA LOCATION MAP, only areas for which work was submitted to the Ministry are outlined, and<br />

thus a company may hold more ground than indicated here. The numbers on the DATA LOCATION MAP<br />

and any circled numbers refer to the company above.<br />

DATA LOCATION MAP<br />

AIRBORNE<br />

71<br />

ELECTROMAGNETOMETER<br />

71*<br />

AIRBORNE<br />

RADIOMETRIC<br />

GROUND<br />

46<br />

50<br />

60<br />

74<br />

77<br />

74<br />

MAGNETOMETER<br />

50<br />

61<br />

71<br />

SOURCES OF INFORMATION<br />

Compiled by A.A. Speed and G.J. Maxwell, 1979 trom data on<br />

file at the Resident Geologist's Office, <strong>Ontario</strong> Ministry of<br />

Natural Resources, Sioux Lookout. Information to July 1, 1979.<br />

Base-map derived from the Forest Resources Inventory map,<br />

Lands and Waters Group, <strong>Ontario</strong> Ministry of Natural Resources.<br />

Metric Conversion Factor: l foot = 0.3048 m<br />

E wry passible ut f art has been made (u ensure the accuracy D f the informa<br />

tion presented on (fm map; tiuwever, the <strong>Ontario</strong> Minisiry of Natural<br />

Resources does noi assume any I/ability for errors that mfiy occur. Users<br />

may wish lo verify critical information; sources include hnth f/x? references<br />

listed heret, snd information on file at the Resident or Regional Geologist's<br />

office and the Mining Recorder';, office nearest the map n'Pti.<br />

This compilation project is part of the Northern <strong>Ontario</strong> Geolo<br />

gical Survey program and is funded by the <strong>Ontario</strong> Ministry of<br />

Northern Affairs.<br />

This map is published with the permission of E.G. Pye, Director, <strong>Ontario</strong><br />

Gvo/oyicat Stirwy. ^ .<br />

GROUND<br />

74<br />

77<br />

ELECTROMAGNETOMETER<br />

72<br />

36<br />

74<br />

61<br />

71<br />

36<br />

GROUND<br />

RADIOMETRIC<br />

INDUCED<br />

POLARIZATION<br />

POTENTIAL SELF<br />

RESISTIVITY<br />

GRAVITY<br />

GEOCHEMICAL<br />

1980<br />

TRENCHING<br />

OTHERS<br />

t<br />

t<br />

74-"<br />

76"'<br />

4G*<br />

46*'<br />

73*'<br />

3',<br />

42.<br />

55,47<br />

5152<br />

535E<br />

62,64<br />

37*<br />

36<br />

<strong>Ontario</strong><br />

Ministry of<br />

Natural<br />

Resources<br />

Hon. James A,C. Auld<br />

Minister<br />

Or J K Reynolds<br />

Deputy Minister<br />

ONTARIO GEOLOGICAL SURVEY<br />

: PRELIMINARY MAP R2318<br />

SIOUX LOOKOUT DATA SERIES<br />

Ministry of<br />

Northern<br />

Affairs<br />

Hon. Leo Bernier<br />

Minister<br />

Art Herndge<br />

Deputy Minister<br />

<strong>TARP</strong> <strong>LAKE</strong> <strong>AREA</strong><br />

Mile M CSZ^<br />

Metres 100 O<br />

OMNR-OGS 1980<br />

DISTRICT OF KENORA<br />

(PATRICIA PORTION)<br />

Scale 1:15840<br />

o y.<br />

0.2 0.4<br />

!Sl l l<br />

NTS Reference: 52 0/9F<br />

ODM-GSC Aeromagnetic Map: 924G<br />

ODM Geological Compilation Map: 2218<br />

l<br />

1 Kilometre<br />

Paris of (his publication may be quoted il credit is given and the<br />

material is ptopeily refeienced.<br />

PHANEROZOIC<br />

CENOZOIC<br />

QUATERNARY<br />

PRECAMBRIAN<br />

LEGEND 1<br />

PLEISTOCENE AND RECENT<br />

LATE PRECAMBRIAN<br />

Till, clay, sand, gravel<br />

10 Diabase dikes<br />

UNCONFORMITY<br />

INTRUSIVE CONTACT<br />

EARLY PRECAMBRIAN (ARCHEAN)<br />

MAFIC INTRUSIVE ROCKS<br />

9 Dionte, gabbro,.anorthosite gabbro 3<br />

INTRUSIVE CONTACT<br />

FELSIC INTRUSIVE ROCKS<br />

MASSIVE FELSIC INTRUSIVE ROCKS<br />

S3 Unsubdivided<br />

S a Porphyritic quart? monzonite to granodiot itc<br />

8b Biotite-hornblende monzonite to syenodiorite<br />

Se Biotite-hornblende quart? diorite to diorite<br />

8d Trondhjemite<br />

Se Pegmatite, aplite<br />

8f Trondhjemite to granodiorite<br />

FOLIATED FELSIC INTRUSIVE ROCKS<br />

7 UnsubdiVidfid<br />

7a Migmatite predominantly orthngnfiks<br />

7b Foliated to gneissic biotite and hornblende<br />

trondhjemite to granodiorite<br />

7c Diorite, quartz diorite<br />

INTRUSIVE CONTACT<br />

METAMORPHOSED hELSIC INTRUSIVE ROCKS<br />

MIGMATITE<br />

6 Unsubdivided<br />

6a Quart? and/or feldspar porphyry 13<br />

6b Trondhjemite to quart? mon7onite<br />

INTRUSIVE CONTACT<br />

5 Unsuhdivided<br />

5a Biotite-quartz-feldspar gneiss (metasedimentai y<br />

migmatite)<br />

5b Hornblende-teldspai-quart? gneiss [metavolcanic<br />

migmatite)<br />

INTRUSIVE CONTACT<br />

METAMORPHOSED MAFIC INTRUSIVE ROCKS 8<br />

4 Unsubdivided<br />

4a Gabbro<br />

4b Diorile<br />

4c Porphyritic gabbro^<br />

4d Peridotite<br />

INTRUSIVE CONTACT<br />

IV! ETA VOLCANICS AND METASEDIMENTSfi<br />

METASEDIMENTS<br />

3 Unsubdivided<br />

3a Conglomerate<br />

3b Wacke, quartzite, siltstone<br />

3c Slate, argillite<br />

3d Biotite-quarU-plagioclase schist and gneiss<br />

METAVOLCANICS<br />

Felsic to Intennediatc Mctavolcamcs<br />

2 Unsubdivided<br />

2a Rhyodacite to rhyolitic flows<br />

2b Dacittc lo andesilic flaws<br />

' ' -.<br />

2r Tuff<br />

2d Lapilli-tuff<br />

2e Tuff-breccia<br />

2f Agglomerate<br />

. " !<br />

2ri Fine to medium-grained<br />

2h Graphitic tuffs and schists<br />

potphyiiiic flows<br />

Intermediate to Mafic tVletavulcanics<br />

1 Unsubdivided<br />

1 a Fine-to medium-grained flows and derived<br />

amphibolite, chlorite schist (:<br />

1b Medium-to coarse-grained flows (diabase and<br />

amphibolite) 0<br />

le Pillowed lavas<br />

Id Pillow breccia<br />

le Porphyritic flows a ' c<br />

If Intermediate tuff, lapilli-tuff, tuff-breccia<br />

lg Intermediate agglomerate (mafic fragments!<br />

In Crystal tuff<br />

IF - IRON FORMATION<br />

a) Occurs as dikes or sills.<br />

b) Occurs as small dikes only.<br />

c.) May be intrusive in part.<br />

d) May be extrusive in part.<br />

e) Rocks in these groups arc subdivided lithologically and the order<br />

does not imply arje relationships within ur drnoriq the groups.<br />

This legend is in part deiived from R.P, Sdye's ct a!, coloured Geological<br />

Map 2218, Cat Lake-Pickle Lake.<br />

C O N M L SI 30 00<br />

Information from this publication may be quoted if credit is<br />

given. It is recommended that reference to this map be made in<br />

the following form:<br />

Speed, A.A. and Maxwell, GJ.<br />

1980: Tarp Lake Area, District of Kenora (Patricia Portion);<br />

<strong>Ontario</strong> Geological Survey Preliminary Map P.2318<br />

Sioux Lookout Data Series. Scale 1:15 840 or 1 inch to<br />

li mile. Data compiled 1979.<br />

Scale 1:63360

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