central patricia property pickle lake, ontario · 2017-01-17 · in the patricia mining district of...

52089SE0a68 52008NEee44 TARP LAKE 010

REPORTON THE

DIAMOND DRILLING, GEOLOGY,PROSPECTING, SOIL GEOCHEMISTRY AND

TRENCHINGON THE

CENTRAL PATRICIA PROPERTY

PICKLE LAKE, ONTARIO

FOR

GOLDEN SHADOW RESOURCES INC,

g?- z-?

JANUARY 18TH, 1984 G,B, BURTO

52009SE*068 52088NE0044 TARP LAKE

TABLE OF CONTENTS

010C

PAGE

1.0 SUMMARY . . . . . . . . . . . . . . . . . . . . l

2.0 INTRODUCTION . . . . . . . . . . . . . . . . . 2

3.0 LOCATION AND ACCESS . . . . . . . . . . . . . . 2

4.0 PROPERTY DESCRIPTION . . . . . . . . . . . . . 2

5.0 WORK PERFORMED . . . . . . . . . . . . . . . . 3

6.0 DISCUSSION OF RESULTS . . . . . . . . . . . . . 6

7.0 CONCLUSIONS AND RECOMMENDATIONS . . . . . . . . 12

APPENDICS

REFERENCES . . . . . . . . . . . . . . . . . . 15

LIST OF DRAWINGS . . . . . . . . . . . . . . . 16

DIAMOND DRILL HOLE LOGS GS-83-1 to GS-83-5 . (back of report)

DRAWINGS (back of report)

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1.0 SUMMARY

During the past year, a drilling, geological mapping, prospecting and trenching program in specific areas was carried out on the Central Patricia property of Golden Shadow Resources Inc. A geochemical soil sampling program was also conducted on the eastern most portion. The property^ is located in the Pickle Lake area within the Patricia Mining District of Northwestern Ontario. Access is either by road from Ignace or via scheduled aircraft from Thunder Bay.

A total of 1700 feet of diamond drilling was completed in 5 holes. Two holes investigated an iron formation in the west central portion of tne property. A third hole explored an EM^ and magnetic conductor in the central portion. Two holes examined the potential of the ore zone established on claim PA 627. Only trace amounts of gold were encountered in the first three holes. Low values were obtained in the ore zone on claim PA 627, the best being 0.18 oz Au over 5 feet.

Reconnaissance geology was conducted in 7 areas in the east end. Detailed mapping was done around the trenches, which were completed in 5 areas. Only low gold values were obtained.

"B" horizon soils were collected where ground permitted and analysed for gold. "A" horizon soils were taken where the "B" wasn't available. Certain areas were good sampling, whereas others were poor. The quartz veins at the Springer and the Hook Veips showed weak soil geochemistry anomalies just above background. Poor sampling ground prevented adequate testing of most of the remaining mineralized zones. A number of good geochemical anomalies were identified that require further investigation.

A comprehensive exploration program involving detailed geological mapping over the entire grid, detailed I.P., as well as detailed geochemical soil sampling is highly recommended for this property.

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2.0 INTRODUCTION

During the past year, the former Central Patricia proper

in the Pickle Lake area of Northern Ontario has been subjecte

tyd to

a mining exploration program, conducted by Geocanex Ltd. of

Toronto. The 110 claim property is held under option by

Golden Shadow Resources Inc., also of Toronto. The exploration

program conducted by Golden Shadow consisted of diamond drilling

in selected areas, geochemical soil sampling, prospecting,

geologizing and trenching over a specific area in the eastern

portion of the property. The diamond drilling was performed

by Tindale Drilling of Midland during January and February,

1983 while the. geochemical, geological and trenching were

carried out from September to October, 1983. Geologists,

Robert Burns, of Sault Ste. Marie and Kathy Gerrie of Orangeville

conducted the geological, trenching and soil sampling. Work j.'ar,

aided by Steven O'Brien, a student of Waterloo University.

Garth B. Burton supervised the program as well as conducting

geological reconnaissance sortees.

3.0 LOCATION AND ACCESS

The property is located in Connell and Ponsford townships,

in the Patricia Mining district of Northwestern Ontario. The

town of Pickle Lake lies to the west of the claim group while

the town of Central Patricia lies within the property. These

communities can be reached via scheduled air flights from

Thunder Bay, approximately 200 miles to the south. The claims

can also be accessed by Highway 599 from Ignace on Trans-

Canada Highway 'lo. 17. A good gravel road from which access

to the grid is available, traverses the property in an almost]

east-west direction.

4.0 PROPERTY DESCRIPTION- - '.---.-U - - '- L -'L -L- -J ———— ---..'.- J

The property consists of a total of 110 mining claims ir

Connell and Ponsford Townships of the Patricia Mining district.

The diamond drilling was carried out on claims PA2457 and PA80

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in the northwestern portion of the property, claim PA689 in the

central section and over the known mineralized area, on claim PA627. The geochemical soil sampling was conducted on the eastern part of the property comprising the following claims:

parts of

PA

PA

PA PA PA PA

PA

625-631

634-636

647-650 653-655

2005-2010 2015 and 2016

2018 and 2019

inclusive inclusive

inclusive

inclusive

inclx'sive

The prospecting and geological work was performed on specific sections of claims PA625, PA627, PA634, PA635, PA636, PA647,

PA648, PA2005 and PA2008, all in tho eastern part of the property. Trenching was confined to claims PA627, PA635, PA648, PA655 and

PA2008.m

5.0 WORK PERFORMED

Drilling- r ' -*- j

A total of 1,700 feet of diamond drilling was completed in Janaury and February of 1983. Following is the distribution of the footage:

GS-83-1

GS-83-2

GS-83-3

GS-83-4 GS-83-5

claim PA 2457

claim PA 80 claim PA 689

claim PA 627 claim PA 627

TOTAL:

299 ft.

297 ft.

298 ft.

538 ft.268 ft.

1700 ft.

The location of these 5 drill holes are shown on the composite map of the Central Patricia Property illustrated by Drawing No, GS-17. The geological logs of the drilling are

presented in Appendix I along with geological sections showingl

assays for gold. These drill sections are designated drawings No's GS-18 to GS-22.

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Geology/Prospecting and Trenching

Seven areas for exploration were selected from the magnetic expressions obtained in a previous magnetometer

survey which are considered to be areas where gold deposition could take place, and general prospecting. These

are referred to as areas l through 7 respectively in this report.

Area l is located in claim 648 and lies between line

67+60E and 69+80E at about 6+25N to 6+75M. Soil stripping exposed "islands" of iron formation and volcanics surrounded

by muskeg and water. Six trenches were blasted and sampled. Area 2 is located in claim 655, where two backhoe trenches

were dugj One on line 54E at 1+50S and the other on line 54+50E at 2+25S. In area 3 soil stripping was done at 8+50S

to 8+80S on both sides of line 68E. This area lies in claim 2008. In area 4, located in claim 635, stripping was attempted

on the east side of line 62E between 6+25S and 6+75S. This area is muskeg and is below the water table. No trenching was done in area 5. A single backhoe trench was dug in area 6, at 4-M2N approximately 2m east of line 59E. A depth of 12-14 feet (4m) was reached, but bedrock was not exposed due to water problems. This area is located in claim 627. Area 7, located in the southeast of claim 636, was not mapped in detail). due to lack of time available, though some reconnaissance

mapping was completed.

Detailed geologic mapping was completed in areas

1,2,3 and 5 and part of area 4 and 7. Area 6 showed no significant outcrops. Bedrock trenching and rock sampling (bulk and/or chip and/or grab) were carried out in areas 1,2,3 and 4 including some sampling of old trenches on area 2.

The reconnaissance geological mapping showing locations

of the trenching, is shown at a scale of 1:5,000 on the Geology Map over selected Magnetic anomalies (Drawing No. GS-23).

Detailed geological mapping and information on the

trenches are illustrated on a sequence of small maps labelled drawing No's GS-24 to GS-32.

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Geochemlstry

A geochemical soil sampling survey was conducted ov^r

the majority of the eastern portion of the claim block. A to cal

of 3,383 soil samples were collected on the grid at 25 metre

intervals along the lines spaced at 100m. The target horizon

was B and was sampled when possible.. The A horizon was sampled

when the B horizon was not attainable. Depending on the dept

of the sample, either an auger or a grub hoe was employed, th

former being used for the majority of the survey. The averag:

depth was 3 feet (1m). To insure accurate results a sufficient

amount of soil was collected for the required 10 gram sample

size. The samples were then dried and shipped to Bell-White

Analytical Laboratories in Haileybury, Ontario, and were

assayed for gold content in parts per billion, using the fire

assaying and atomic absorption methods. Some samples were

analysed for silver.

Histograms have been plotted for both the A horizon

and the B horizon shown on the geochemical soil sampling map

(Drawing No. GS-33). The median value and the standard

deviation were calculated and used to establish a background

level and an anomalous threshold value respectively. Anomolous

values were established at two standard deviations from the

median and highly anomalous values at three standard deviations

from the median. These parameters have been summarized on

Drawing No. GS-33 along side the histograms. In order to

develop a consistent range for the results, a number of values

were isolated from the statistical array when a cutoff point

of 50 ppb was utilized. These values should not be ignored as

they are indicative of an area with very high gold mineralization.

All results for the B horizon have been plotted and

contoured on the geochemical soil survey map at a scale of

1:5,000 (Drawing No. GS-33). The values for the A horizon were

also plotted but due to the scattered nature of results and t^e

low number of anomalous values the results could not be contoured,

Line 52E and Line 54E, 0+00 to 10+OON are areas of anomalous

reading and have been profiled, shown on the contoured map

(Drawing No. GS-33).

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6.0 DISCUSSION OF RESULTS

PrillingJ-l.-.J.U-.l-T --~ ..." !

Drill holes GS-83-1 and GS-83-2 were designed to test

a conductive magnetic anomaly indicative of oxide iron formation at two different locations where it appeared that the zone was interrupted by east-west striking faults as determined from magnetics and VLF EM results. The first drill hole intersected

i

a 136 ft. wide band of iron formation in mafic volcanics. A 5 foot fault zone was also intersected in this hole. Only trance amounts of gold were encountered in the drilling. The second drill hole intersected two seperate sections of iron formation, 22 feet and 53 feet, in intermediate to mafic volcanics. This hole also returned trace amounts of gold.

The third drill hole, GS-83-3 was put down to test an EM conductor with magnetic association in an area favourable for gold deposition. The hole encountered several bands of iron formation along with graphite and massive sulphides in a

mixture of intermediate tuff and mafic volcanics. Several

quartz veins were also interesected. All assays returned trace values in go]d.

Drill holes GS-83-4 and GS-83-5 were put down in the

vicinity of the gold mineralization encountered in previous drilling on claim PA627. The holes were designed to substantiate and expand the known mineralized zone in the iron formation horizon. The two holes intersected the mineralized iron formation

on target. Hole No. GS-83-4 returned the following assays across the ore zone.

Depth Length Oz Au/ton139.8 to 144.8 5.0 ft. .02144.8 to 149.3 4.5 ft. .02149.3 to 154.3 5.0 ft. .18

154.3 to 158.8 4.5 ft. .06158.8 to 163.0 4.2 ft. .05

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All remaining assays gave only trace amounts of goJ.d.

Another mineralized section from 373.5 to 398.5 had the best assay of .08 02 Au/Sft. from 388.0-393.0. Other assays in the group ranged from .01 to .04 oz Au/ton.

The second hole, GS-83-5, returned the followng assays in the same mineralized horizon:

D^jpth Length O z Au 1 1 on129.5 to 134.0 4.5 ft. .02134.0 to 139.0 5.0 ft. .04139.0 to 143.5 4.5 ft. .03143.5 to 148.0 4.5 ft. .02

All other assays gave trace gold.

Geology

Area l

Basic to intermediate volcanics with pillows and

fragmental textures and a lean cherty siderite iron formation, grading towards oxide facies with variable magnetite content

with some chlorite silicate laminae, 0.1 to 50 mm wide have tpeen exposed by soil stripping (compare trenches 4-6). Folding

within the iron formation consists of both "S" and "Z" folds formed from penecontemporaneous slumping prior to consolidation. Generally the plunge is vertical. A fault contact between andesitic greenstone with fragmental pillowed structures, approximately 100-500m long and a lean cherty siderite iron

formation with some magnetite, chlorite, pyrite and pyrrhotineis observed in the eastern part of the area. The south side ofthe volcanics appear to be moze massive. The iron formation hosts quartz veinlets with pyrite and pyrrhotite trending NN in the north end of the formation. In the mid and south are^s the quartz veins are more numerous and run both NMW and NE.

In the east central part of the stripped area (trenches 7-9) a banded cherty siderite occurs with some magnetite and

scattered quartz veinlets generally trending WNW and with some

pyrite and pyrrhotite. The veinlets are 10-50 mm wide. The

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iron formation becomes more magnetic to the west, where 1-57* pyrrhotite and pyrite are found throughout, and a greater

concentration of quartz veinlets. There is an abundance of quartz veinlets to the south (trench 4) but, become scattered

and smaller in the north and show no apparent relationship to folding in the iron formation. The quartz veinlets generally

i

trend WNW and NE with some running NNW with a thickness of less than 20 mm wide.

The outcrop area in the central portion of trench lO consists of iron formation with large blocks of andesitic

greenstone, essentially in place, north of the outcrop area.

The iron formation is a cherty siderite with minor magnetite

and some chlorite laminae, possibly silicate facies IF. The iron formation lamina is 2-50 mm wide. Pyrite and Pyrrhotite are scattered throughout with a greater abundance within the quartz veinlets. The quartz veinlets trend NNW throughout

the formation with many ENE veinlets in the north and becoming scattered to the south. The veinlets carry iron carbonate, pyrite, pyrrhotite and to the north some galena in a ENE vein. They also carry some sericite, chlorite,

late calcite and late quartz. A strong "S" fold with a vertical plunge is observed. Bedding is near north-south in the south end.

In the west portion of the area there is a fault contact between the andesitic greenstone and the iron formatioii.

Faulting occurs throughout the area displacing iron formation. Two parallel faults in the east and west ends of the area

strike approximately 80.No outstanding gold values were obtained from the

trenching. The highest assay returned 0.054 over 2 feet in

trench No. 83-5.

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Area 2

The soil trench excavated by means of a backhoe at

1+50S on line 54E exposed bedrock in which a trench was blasted

(Trench 83-2). This was sampled for gold, silver and copper. Quartz veins with pyrite, pyrrhotite, chalcopyrite, chlorite

and carbonate occur in both oxide iron formation and andesite. The iron formation is well banded and consists of mixed

chert, iron silicate, magnetite, and 5 to 107. pyrite and

some pyrrhotite. There is heavy mineralization in places.

In trench 83-3 at 54+50E just south of trench83-2, there is lamenated silicate iron formation cut by ankerit^ veinlets with some pyrite. These follow the shearing which is about 120a, same as the veins. Bedding is approximately 110?

Low gold values were encountered in both trenches.

Area 3

The stripped area revealed cherty iron formation with

minor siderite, some chlorite, a trace of magnetite and l to 370 pyrite. Locally, there is up to 107. pyrite in rows (spotty) and veinlets along bedding planes. There is also some pyrrhotite. North of the stripped area a vuggy quartz vein occurs with limonite, iron, carbonate, pyrite (10-157*) and a trace of tourmaline. Some of the rock reveals a black

argillite containing 3 to 5" fine pyrite along bedding and foliation planes.

Area A

Stripping has exposed small areas of outcrop containing andesite and iron formation. The iron formation

is a cherty, sideritic unit with magnetite, quartz veins

and pyrite. The iron formation is broken in vertical plates which are deeply weathered. Quartz veins with limonite, carbonate, pyrite and chlorite occur at the north end. Shearing

is at 355*(north end). Sheared greenstone with quartz veins

and pyrite likely indicate the presence of a fault. The proposed fault matches the displacement evident between the

central and eastern parts of area 1. Poor gold values were obtained.

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Area 5

The geology encountered in area 5 consists pie- dominantly of intermediate to andesitic volcanic rocks, mostly of the massive and pillowed variety. Foliation is at 105-110** and dipping north.

Area 6

There is no outcrop in area 6.

Area 7

Limited outcrop in this area revealed massive andesite with foliation at about 1000 dipping north at 70* to 80*! Several

quartz veins are present. These appear barren.

Folding does not appear to be important. In the iron formation folding is original sedimentary slumping. Faulting has been observed in two of the areas explored during this

phase, (l and 4). In area one a series of four parallel faults exist with two larger faults to the east and west of the area striking approximately 45 0 and dipping about 80? The

four other faults strike in a different direction with small

or no displacement of the geological units. One other large fault striking approximately 3500 displaces the central and east parts of area 4.

Geochemistry

It is difficult to assess the success of the geochemical program for several reasons. The nature of the soil deposits

are not accurately known, therefore, the proper distribution of gold in the soils from known mineralized areas is difficulty

to assess. Also the distribution of the various soil types, glacial sands and gravels with minor clays intermixed with

muskeg and swamp, did not provide a consistent sampling mediuri to co-ordinate the results. Despite these drawbacks, the geo chemical sampling did show some anomalous features that are

noteworthy.

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Prime amongst these is the low value of 20 ppb obtained

in good soils just south of the Springer Vein. (It was impossible to obtain a sample over the vein itself because

I of insufficient soils.) This value is significant in that it shows that at single,low value on the wide grid spacing used, i.e. 25m stations on 100m lines, suggest the possibility of

i good gold mineralization in quartz veins such as that mined

at the Springer. In support of this observation, a weakf geochemical anomaly of only 14 ppb was obtained in the vicinity

of the Hook Vein, (approximately 20m southeast of it). This

1 anomaly occurs in an area of good sampling. In much of the other areas where gold mineralization is

known, it was difficult to collect proper samples. Consequently f it was impossible to obtain characteristic geochemical signatures

over these mineral zones.

i Despite "he difficulties in obtaining samples, there were:a number of j-.eochemically anomalous areas defined during the

i survey. Two north-northwesterly trending zones have been out-j

lined. Extremely high values were encountered on line 68E of

g one zone that extends from 600N on line 66E to the baseline on f 70E. This value reached over 1400 ppb. A possible extension

to this zone occurs at 750S on line 74E and 825S-900S on line

l 75E. The second north-northwest striking zone runs from 950Non line 52E to 325N on line 56E. There are good high values cm

^ line 52E, but the values on the remaining lines are mediocre.These zones appear to be fault controlled.

I Another area of anomalous geochemical values occurs at the south ends of lines 64E, 65E and 66E. Multiple scattered pealjs

appear in a random fashion in a poor sampling area. i Other anomalous zones are:

between 200S and 375S, lines 78E and 79E between 675S and 825S, lines 78E and 79E

between 725N and 750N, lines 62E and 63E along the boundary.

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Individual peaks are located as follows:

Line 53E - 525N

Line 55E - 725N Line 57E - 200S

Line 5AE - 700S Line 59E - 550S

59E - SOON59E - 600!'

Line 62E - 625N Line 6AE - 225N

6AE - 125N Line 63E - 050S

63E - 175S Line 65E - AOON

Line 66E - 150S66E - 250S66E - 350N-450N

Line 70E - 200N

These areas are ideal candidates for gold quartz veins sijch as the Springer and Hook Zones especially the 33 peak value at 050S on line 63E.

7.0 CONCLUSIONS AND RECOMMENDATIONS

The 1983 drilling program was helpful in defining some of the geophysical and geological features that make up the

complexity of the Central Patricia gold property. Although low gold values were encountered, further understanding of the geology was obtained. The two holes drilled in the ore zone on claim 627 confirmed the gold mineralization occurring there. Certainly much more drilling is required on the property to properly evaluate its potential.

The reconnaissance geological and prospecting program carried out on the extreme eastern portion of the property

also provided further insight into the potential for gold

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mineralization there. Although a more comprehenisve geologica mapping program is required to satisfactorily understand the full picture, the detailed geology gathered from the trenching has provided an insight into the localization of gold mineralization. Ore controls, according to, R. Burns, geologist who did the majority of the mapping on the property, are:

1. Post porphyry mineralization and potentially favourable structures cutting the porphyries.

2. Although folding does not appear to be a con trolling factor, ore zones appear to follow the strong regional foliation, that is about 1200, where it cuts the porphyry and older rocks.

3. Faulting is important in ore control. Ore veins trend from about WNW (120 0 ) to east- west to northwest.

4. Significant iron formation types associated with ore zones include oxide, carbonate (the most abundant), and silicate facies. Sulphide facies iron formation was not particularly recognized in the present program.

The sulphides, whether in veins or in iron formations and most of that in other rocks, appears to be conventional introduced hydrothermal mineralization.

The flat topography and poor drainage make stripping difficult in this area.

The following recommendations are proposed to further

explore the Central Patricia property:

1. Detailed geological mapping over the entire property, paying close attention to quartz porphyry intrusive distribution; iron formation facies variations as well as structures and mineralization. Faulting and fracturing patterns should also be mapped closely.

2. Detailed I.P. should be conducted over specific areas such as iron formations in low magnetic areas, under swamps where possible sulphide con centrations could exist, faults and slips which could be related to veins, particularly the north-northwest striking geochemistry anomalies.

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3. Closer spaced geochemical soil sampling in areas where lengthy anomalies appear, particularly the north-northwest striking zones and around other high values.

4. Further sampling of old surface trenched areas along with trenching in new areas where feasible should be done concentrating on geochem. and I. P. anomalies.

Following careful analysis of the geology, I. P. and

geochemistry data, a comprehensive drill program should be devised.

Respectfully submitted,

GEOCANEX LTD./ ~~)

Garth B. Burton Geophysicist

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REFERENCES

Ferguson, Stewart A., 1966, Geology of Pickle Crow Gold Mines Limited and Central Patricia Gold Mines Limited, No. 2 Operation, ODM, Mis. Paper MP-4.

Tilsley, James E., 1983, Exploration of the Central PatriciaProperty, Pickle Lake Area, Northwestern Ontario for Golden Shadow Resources Inc. - company files.

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1

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1

1

1

1

1

1

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1

1

1

1

1

R11

V

LIST

GS-17

GS-18

GS-19

GS-20

GS-21

GS-22

GS-23

GS-24

GS-25

GS-26

GS-27

GS-28

GS-29

GS-30

GS-31

GS-32

GS-33

OF DRAWINGS - CENTRAL PATRICIA PROPERTY

Central Patricia Property

Vertical Section - D. D. H. GS-83-1

Vertical Section - D. D. H. GS-83-2

" - D. D. H. GS-83-3

11 - D. D. H. GS-83-4

" - D. D. H. GS-83-5

Geology Map over Selected MagneticAnomalies

Geological Mapping and SamplingArea 1 Overview

M M M

Area 1 East EndII M M

Area 1 Trenches 83-7,8,9M it ti

Area 1 Trench 83-10M tt II

Area 2 North Sectionn n MArea 2 Trench 83-2

n M MArea 2 Trench 83-3

n tt ti

Area 3n tt tt

Area 4 Stripped Section

Geochemical Soil Sampling

1:12, Of(back poc

1 ln-5C

0ket)

ft.

1 in-5CJ ft.

1 in-5q ft.

1 in-5C

1 in-ST

ft.

ft.

1:5,000(back poc :ket)

1:80C)

1:100

1:10C

l:10d

1:1,OC)0

1:50Q

1:501r

l:50Cl

l:10(j

1:5,000 (back pocket)

l

DIAMOND DRILL RECORDNAME OF PROPERTY GOLDEN SHADOW- CENTRAL PATRICIA PROP.M mr Mft GS - 83-1 , rnoTH 299 feetLOCATION Claim 2457LATITUDE 15 + 25 East nep*. ., 13 4- 25 NorthELEVATION " A7IMUTH 130* Dlp -50

STARTED January 23, 1983- 1M1 , UPn January 30th, 1983

FOOTAGE

FROM

0

125.0

130.0

|

,M|

TO

125.0

130.0

236.0

DESCRIPTION

CASING, sand, sandy clay and boulders.

FOOTAGE

299

DIP

42

MAFIC VOLCANICS, BASALT?, fine to medium grained, darkgreen, chloritic, numerous brown (limonitic)oxidized stringers, slighty porphyritic,leucoxene, strongly shepred at 40^ to C. A

minor

125.5-1^0.0 - FAULT ZONE, broken core. 2 feet of lostcore in this section.

IRON FORMATION - finely laminated to coarsely beddedwhite to grey chert and magnetite. Individualbeds up to 2 thick. Much of the magnetite ispartly oxidized to ochrous to chocolate brownlimonite. Occasional narrow (1-2 m. m) bands ofminor pyrite. Bedding at 45" to C. A. Scatteredvuggy sections suggesting leaching of ironcarbonate? Sulphides?

143.6-146.6 - heavy magnetite (and limonite), 5-87.pyrite.

146.6-159.0 - mainly light grey, well bedded chertwith fine magnetite throughout in thin (1bands and disseminations. Minor pyrite.

mm)Bedding

35 to C. A., slightly crenulated in sections.Occasional wisps of pale green chlorit . Minorreddish brown mineral in thin laminae, probablyspecularite, possibly sphalerite?

159.0-191.0 - as above with increasing chlorite,occasional sections of chert-chloritic brecciawith chert fragments in a chloritic matrixscattered sections of heavy brown, partly oxidizedmagnetite, probably representing water-bearing fracture zones, partly vugp.y with minor pyrite

AZIMUTH

-

"OOTAGE

SAM

NO,

910

911

S.fc

0

P L

FO"FROM

143.

168.

6

0

1

1

p AZIMUTHHOLE f

o GS -83- \H EET MO. -L

REM ARKS

LOGGED BV H. J. HodgC

e)TAGCTO

46

71

.C

.C

TOTAL

3.

3.

0

0

ASSAYS

t i, AUOZ/TON

T r

Tr

OZ/TON

DIAMOND DRILL RECORDM o i. r NO ....Q.S;.

rOOTAGC

f BOM

236.0

237.6

10

237.6

266.6

DESCRIPTION

from 168.0-171.0, 188.6-191.0. At 174.0 bedding30 e to C. A. Occasional cross-cutting quartz-carbonate veinlets up to 1/2" wide.

191.0-224.2 - over 502, magnetite in 2"-3" bands withinterbedded chert and occasional green chloritebands. Minor pyrite, occasional cross-cuttingstringers and veinlets of quartz 203.7-204.3 -quartz vein milky white, cataclastic texture.Bedding at 206.0 - 30'to C. A.

224.2-224.6 - Andesite, dark green (tuff)224.6-233.3 - mainly cream colored chert, finely

laminated to coarsely bedded with minor blackmagnetite bands and occasional narrow palegreen chlorite bands.PROBABLY SILICIFIED ZONE

223.0-236.0 - CHERT BRECCIA SILICIFIED, cream colouredsilicified, highly fractured and brecciated,with network of narrow bluish-white quartz vein lets, and pyrite stringers. Minor magnetitethroughout occasional chloritic stringers,generally with pyrite. Short sections showremnant fine bedding laminations. Some shortsections up to 30-40^ pyrite, probably 57,overall.

QUARTZ VEIN - bluish-white, irregular contacts, minorwispy chlorite, pyrite, 40-50* chert breccia,

IRON FORMATION, CHERT BRECCIA, as above.At 238.0-1" irregular matic dyke.

238.6-244.0, mainly laminated chert (non-brecciated) .Light grey to cream coloured beds, minorchloritic bands (beds?) with pyrite occasionalthin bands of magnetite bedding 60' to C. A.

244.0-246.0 - Silicified, cream colored, welllaminated, minor pyrite in fine bands parallelto bedding (57. overall) minor crenulations.

SAMPl

NO

912

913

914915916

917

* *UIFM

!RM r*oM

189.6

203.7

223.0228.0223.0

236.0

1TV.GQ.1.

5.3dL-.J)J5tLSHAPPW-j5MTRAl.eAmiCl/...... ___ SHE t T NO,- _ 2

eOOI*Of

TO

191.1

04.3

228.0233.0236.0

237.6

'O'Al

1.6

0.6

5.05.03.0

1.6

S, m.

ASSAYSAll

'\ *, 01 TO*

Tr

Tr

TrTrTr

T r

Of TO*

DIAMOND DRILL RECORD NAMC or

HOI. C NO. .-M?.^ SHEET NO.__i.__.

rooTAoe

f HOM

266.6

299.0

l

to

299.0

DESCRIPTION

246.0-247.4 - Magnetite plus 507. well bedded.247.4-248.4 - Grey intermediate dyke. Slightly

porphyritic iwth white feldspar phenocrysts.Minor pale green chlorite.

248.4-252.0 - as above (246.0-247.4)252.0-253.3 - Rhyolite?, pale yellowish white, highly

sericitized for first 4". Massive, minordisseminated pyrite. (Dyke?)

2.53.3-258.0 - Magnetite rich, as above with creamcolored silicified section 254.0-256.0,This section shows remant of partly silicifiedmagnetite with laminations crossing the re placement "front".

258.0-266.6 - bleached, silicified to cream color asbefore. Well laminated at 40" to C. A. Occasionscross-cutting bluish white quartz veinlets up to1". Minor pyrite.1" to 2" quartz veinlets at low angles to C, A.from 264.0-265.0

ANDESITE - medium grey green, fine to medium grained.Massive, occasional quartz-carbonate stringersto 1/2".

END OF HOLE

SAMPL

MD

918919

1 tut PH tors

rf ROM

258.0262,3

OtAO'.to

262.266.

rut*l

4.34.3

ASSAYS

^ ^AU or 'f**

TrTr

b r TOM

DIAMOND DRILL RECORDGS-

NAME OF PROPERTY cni.nRN RHA^nu- CENTRAL PATRICIAnmr NB. GS-83-2 LrN 0 T H 297 feetLOCATION Claim No. 80LATITUDE 13 * 70 East DrPA*Ti..r 11 * QQ NorthELEVATION " ' A'/IMUTM 130 Dlf -50*

STARTED Jan. 31st. 198JiMi*um Feb. ?nrf, 1981

FOOTAGE

FROM

0

24.0'

55.5

60.3

61.8

l

TO

24.0

55.5'

60.3

61.8

69 0

DESCRIPTION

FOOTAGE

297

DIP

45"

CASINO, sand, sandy clay, boulders near bedrock.

INTERMEDIATE VOLCANIC, (ANDESITE, SILICIFIED?)medium to light grey color, fine grained,massive to slightly banded (sheared?) at 50"to C. A.

QUARTZ VEIN. Approximately 507. bluish white and 507. cream colored(in part laminated) quartz(silicified chert?). Fractured. Minorin narrow veinlets up to 1 mm.

pyrite

55.5-56.0 - 257. pyrite and minor chlorite in irregularreinlets .

58.5-59 0 - several bands of chloritic mafic rocks.tuff?), with 15 to 207. pyrite.

59.0-60.3 - bluish white quartz, massive.

MASSIVE SULPHIDES. 607. banded pyrite, 407. chloritictiff? Banding 40" to C. A. Out contacti -regular at 20" to C. A.

CHERT (ir part TUFF?) LEAN IRON FORMATION

banded

Silicified cream to light grey, well laminated.Minor pale greenish chloritic bands withpytite "seams up to 3 mm. Bedding 50" to C. AMinor MAGNETITE in fine laminae probably 5-87.ovt-rall. Occasional fine bluish white quartzveinlet .

AZIMUTH OOTAOE DI* AZIMUTHHOLE MO. ~" "-'.. ~*HEfT MO, . * , , ,

RFMARK3 , ,.

LOPGED BY " - J - Hodge

S * M P 1 E

NO.

920

921

922

923

SULPH' Juts

FFROM

55.5

60.3

61.8

66.8

OOTAOETO

60. 3

61. f

66.

69.

ft

0

TOTAL

4.8

1 . 7

5.0

2.2

ASSAYS

* Vnu

OZ/TON

.02

T r

Tr

Tr

O7/TON

DIAMOND DRILL RECORD NAMt OF PROPER

GS-33HOLt NO. -.--....

T GOLDEN SHADOW-CENTRAL PATRICIA---- -- -- -

NO.____. .

FOOTAGE

rnoM

69.0

82.0

244.6

297.0

.

TO

82.0

244.6

297.0

DESCRIPTION

IRON FORMATION, transitional from above. Fine blackmagnetite bands with interbedded light greychert and occasional green chlorite. Occasionalnarrow bands of pyrite up to 1/8" with minorbrown limonite? or specularite?Bedding at 35 0 -40" to C. A.

MAFIC VOLCANIC, BASALT? Transitional from above.blackish grey, fine grained, well banded (tuff?)for one footfrom contact, then lighter greenishgrey and finally deep green at 85.6

85.6-106.0, mottled texture (porphyritic?) with darkgreenish black chlorite 'spots', Massivenumerous fine quartz-carbonate veinlets to 1/8",slightly magnetic.4" quartz-carbonate vein at 97.0.

106.0-110.0 - Bruken, highly chloritic (FAULT?)110.0-165.0, - as above (85.6-106.0) becomes slightly

lighter greenish grey color with bleachedsilicified section at 153.0-154,6.

165.0-244.6, darker green and mottled as before.More quartz-carbonate veinlets. Becomesfine grained at out contact.

IRON FORMATION, transitional from above. Wellbedded black variable magnetite bands andcream colored and light grey chert withoccasional green chlorite bands with minorpyrites and brown jigularite , Magnetite 257..Chert appears silicifiedT bleached.Bedding consistent at 30"-35" to C. A.

END OF HOLE

SAMPLE

HO t f III PH

1DC}

nMOM

otAoeTO 101*1

Asyyrs

-. * 0' tOM tit TOM

MUM fifi**l ta^tl^Eg^^

DIAMOND DRILL RECORDNAME or PROPERTY pOLDEh} SHADOV-r.F.NTRAl. PATRICIA PROPMOLE NO GS-83-3 LENGTH 298.0

, OCAT.ON Claim 689LATITUDE L28 4 50 E DrPA.Tn.r 4 4- 08 S

START Feb. 7. 1983 r,*,. Hm Feb. 19R1

r o o T A c E

FROM

0.0

50.0

72.0

110.0

111.3

i*

TO

50.0

72.0

110.0

111.3

167. S

OVERBURDEN

INTERMEDIATE TUFF

rOOTACr DIP AZIMUTH t

298.0 43*

OOTACe

Light to dark grey fine grained moderately to well bedded rock. Light grey chert beds noted,Sections of broken fractured core (fault zones?)at 52.5-53.0, 57.0-59.5, and 67.5-68.0.Core angles: Bedding 60-65* to C. A.

IRON FORMATION72.0-87.0 A lean Iron formation, in part oxidized.

Mainly chert and intermediate tuffs, minormagnetite oxidized to hemotite.Fault zone (?) at 76,5-78.0, with quartzstringers.

87.0-110.0 As above, with occasional graphitesections with 5*4 pyrite, increasing tolower In section.

QUARTZ VEIN

101

A greyish white quartz with 1574 tuff (wall-rock) and a 51 pyrite content.

INTERMEDIATE TUFF BRECCIAA bluish grey rock with fragmental and brecciatezones. Occasional secondary quartz(?) or chert(?) throughout the zone.Moderately bedded 141.0 is 60* to C. A.sulphide content increases down hole, averaging10-25X.

SAM

NO.

942943944945946947

924

948949950

s.fe"

DIP

PL!

FOOFROM

85.090.095.0100.104.108.

Cc0

110.0

111.3116.0120.5

T

9095

AZIMUTHHOLE MOVjS-oj-j snrrr MO. ^J. .- -

REMARKS

LOGGED BV R. T. Chstaway

AGEO

00

.06 .104.108,110.

li

IK120.12 i.

0

0

00

3

050

TOTAL

5.0

5.05.04.04.02.0

1.3'

4. 74.54.5

A SS A v S

V V O7/1OH

TrTrTrT rTrTr

Tr

TrT rTr

OI/TON

si

1C

l

i

PI AMOND DRILL RICORDHOI. E NO jLJJ?.^i?..

FOOTAGE

rHOM

111.3

167.5

171.5

178.0

.

to

167.5

171.5

178.0

180.2

DESCRIPTION

122.0-144.5 Narrow pyrite lenses (1 tnm-5 mm) thatare partly weathered (vuggy). Pyrite to 107. Quartz-magnetite bands (i74"-W2 r') with chert(?)(quartz?) bands (1") from 122.0-128.0Minor pyrrhotite associated with occasionalchloritic sections. Minor creamy-buff quartz

CONI 'D INTERMEDIATE TUFF BRECCIA144.5-150.3

Pyrrhotite averages 15-207. with only minorpyrite and occasional chalcopyrite on thincross fractures.

150.3-162.0Pyrite-f illed fractures, creamy-buff quartzfractures 'vuggy) .

162.0-167.5Sections of heavy chlorite with pyrrhotite. Afew thin fractures with chalcopyrite, i.e.(162.2').

IRON FORMATIONInterbedded grey chert (tuff?) and magnetite(25H) Occasional massive chloritic sectionswith S-8% pyrrhotite.

INTERMEDIATE TUFF BRECCIAAs before (111.3-167.5). with sections of heavychlorite (5-107. pyrrhotite) and grey chert.

QUARTZ VEIN ZONEA milky white to greyish-white quartz vein withwallrock (tuff). Minor sulphides-pyrl te andpyrrhotite.

SAMPL

NO

951952 953954

955

956957958

959

960

961962

925

, SULP*

rOCS

L J

5-3 _

;OLDEN SHADOW- CENTRAL PATRICRo

__ ,- . __ SHCET NO. __ ~ - . .

E

fOOTAOe

f MOM

125.0129.0 134.0139.0

144.0

149.0154.0158.0

163.0

167.5

171.5176.5

178.0

TO

129.1134.1 139.1144.1

149.'

154.'158.'163.

167,

171.

176.178.

180.?.

10UI

4.05.0 5.03.0

5.0

5.04.05.0

4.5

4.0

. 5. 0 1l 1.5

. 2.25

ASSAYS ill

;7TU

or TOD

TrTr TrTr

Tr

TrTrTr

Tr

Tr

TrT r

Tr

01 TO*

fcv-;-

DIAMOND DRILL RECORD GOLDEN SHADOW-CENTRAL PATRICIA

MOLE NO -:l.., SHEET NO.—--

FOOTAGE

r BOM

180.2'

225.0

231.5

233.5

242.7

l.

TO

225. (

231.5

233.5

242.7

247.5

DESCRIPTION

INTERMEDIATE TUFF BRECCIA180.25-200.0

As before, with increasing sulphide content.Strong chloritic sections, with pyrrhotite, pyrite and minor chalcopyrite. Overall average sulphide content is 201.. Numerous chert (1) orquartz(?) zones.

200.0-225.0Tuff breccia with sulphides.Sulphides occur as stringers, lenses and amatrix to the breccia. Secondary pyrite inlater fractures. Average pyrite content is 257..only minor pyrrhotite.

MASSIVE SULPHIDESPyrite to 60Z or more from 225.0-228.0Bedded 9 60" to C. A. with some vuggy andsecondary pyrite in fractures, Chert (?) orquartz(?) zones in section. Minor graphiticargillite. Minor chalcopyrite in quartz veins.

GRAPHITIC TUFFAn argillaceous tuff with 10-12* pyrite.Bedding planes 9 50" to C. A.

INTERMEDIATE TUFFAs before, with 5-8* sulphides (pyrite).Sharp contacts at 50* to C. A.

235.0-242.7Pyrite (25-40X) in narrow massive sections.

GRAPHITIC TUFFA graphitic tuff with some short breccia zones.Pyrite to 15-20*

SAMPU

WO

926927 928 929

930931932933934

935936

937

938939

940

941

. tlUfH

totsf

r*ou

80.25185.0 190.0 195.0

200.0205,0210.0215.0220.0

225.0228.0

.31,5

233.5235,5

240.3

*1 y *1 **24? . 7

ioTActTO

185.1190.i 195.i 200.

205.210.215.220.225.

!28.0!31.5

?33. 5

235.5240.3* t f\ *i242 . r

r i -j r247 . 5

TOTM

4.7'5.0 5.0 5.0

5.05.05.05.05.0

3.03.5

2.0

2.0'4.8'

f\ it- . 4

j Q l4 . 8

ASSAYS All

-, -. Ton

TrTr Tr Tr

TrTrTrTrTr

TrTr

Tr

TrTr

Tr

Tr

01 Ton

h**M0

ta'i

DIAMOND DRILL RECORDHOLE Nf

FOOTAGE

r MOM

2*7.5

298.0

i*

'O

298.0

DESCRIPTION

ANDESITEA grey-green fine to medium grained rock with minor pyrrhotite. Many c'osfl-cutting quartz- carbonate stringers (l-5mnO schistosity P 55* to C. A.

275.0-280.0A cherty sedimentary section with banded pyrrhotite and minor chalcopyrite.

END OF HOLEN. B. CASING PULLED.

" PnOl'EHTT.

j GS-S3-5

SAMPLE

NO1 *Ul'X

I0t J

toof *OM

G.QLDE.N..5.HADQW;

-. , ., SHE

Ant101*1

JCEliGC.ilCT NO

AL.1AIRICIA 4

ASSAYSAll

\ ^ 01 '(K 61 'On

!f-f '

DIAMOND DRILL RECORDNAMI or mott

GS-um r un. "" ,, . M. -- .--..WTV GOLDEN SHADOW- CENTRAL PATRICIA83-4 , . UKVU 538 Feet

~- 4T , nN Claim No. 627LATituor 4 + 13 North ^....,,... 54 4- 60 EastlUCVATIC

T ANTED , .-..~-,- u

)N .. ^.MUTM ,,'J V.-'^lo'ln.P -50'Feb. 11, 1983 , 101 . _ Feb. 1!, 1983

r o o T / o t

r*OM TO

0.0

12.0

13.0

17,5

22.5

25.5

P

12.0

13.0

17.5

22.5

25.5

36,5

ocacftiprioN

CASING

INTERMEDIATE VOLCANIC (ANDESITE?)Fine grained, dark green, massive, minorveinlets

TUFF (BRECCIA?)

roorwi300'538'

DIP

44*41*

quartz

Felsic to intermediate, white to ligth grey(bleached?) Well bedded ( lamina r.* -1) withlocally fragmental sections. Highly oxidized.3-57. pyrite principally as crosscutting veinlets.Bedding at out contact 50* to C. A.

16.0-16.4 -intermediate volcanic, ae above (12.0-13

INTERMEDIATE VOLCANIC

0)

Fine to medium grained, medium green-grey color,massive to slightly banded. Finely porphyritic?with bluish-grey feldspar? phenocrysts in a "tan"colored sericitic? ground mass.

TUFF (CHERT?)White to light grey, finely laminated nt 30 s toC. A. Minor cross-cutting quartz veinlets * idpyrite stringers.

29.0-29.8 - white to light grey (bleached?) cherty,3" irregular quartz vein at upper contact.

IRON FORMATIONPoorly to well banded, Heavy magnetite withinterbedded grey chert. Occasional chloriticintermediate tuff. Minor pyrite and quartzveinlets.

34.5-35.5 - 307.-40Z pyrite, minor pyrrhotite

A7MUTM 1 ooTAoe

SAM

NO.

963

964

965

966

siPtsV

on

f L 1

fOOrnoM

13.0

22.5

27,5

52.0

1

2

3

3

AZIMUTH

ktf^ t MO UO**DJ ̂4 ^tifff ttf\ 1

LOOOED .y H. J. Hodge

rAoe0

r

J

1

3.

5

5

0

5

TOTAL

4.5

5.0

4.5

4.5

ASSAYS

* ir.

1

nvO7/TON

Tr

Tr

Tr

Tr

07/TON

DIAMOND DRILL RECORD MAMF or PROPER'Y. yGOLDEN SHADOW-CENTRAL PATRICIA

MOLE NO GS-^3-4.._ &HEFT NO __....

FOOTAGE

rnoM

36.5

102.0

103.0

106.3

'

TO

102.0

103.0

106.3

163.0

DESCRIPTION

INTERMEDIATE VOLCANIC (ANDESITE)Medium greenish-grey, fine grained, slip,hr.lybanded at 45" to C. A.5" quartz vein - milky white at 92.5-93.0 withquartz veinlets in walls.

INTERMEDIATE TUFFWell banded 40* to C. A,, meJium green, finegrained, minor pyrrhotite (57.)

INTERMEDIATE VOLCANIC (ANDESITE)Medium green, fine grained, massive to slightlybanded.2-1" to 2" irregular quartz veins at 105.5

IRON FORMATIONCoarsely bedded, light grey chert with subordinatemagnetite, minor chloritic tuff bands. Occasionalblue-grey quartz veinlet, minor sulphides- pyrrhotite less pyrite, both as bands parallel to bedding and in cross-cutting fractures.(probably 57, overall).

113.0-163.0 - finely bedded chert and magnetite withminor chloritic tuff. Minor pyrite and pyrrhotiteNumerous interlacing blue-grey quartz filledfractures with rusty brown iron oxide.Bedding 65* to C. A.Sulphides increase down the hole to 10-127, withsections up to 257, to 307..At 134.0, A to 5" of quartz-chert breccia-fragmentof laminated chert in white quartz matrix withrusty red iron oxide.At approximately 150.0, banding becomes indistinct and changes to 35* to C. A. more irregular quartzveinlets. Sulphides increase to 457. to 507. insections, 15-207. overall .

SAMP

*IO

967

993

968969970 971 972973

974975976977 978979

^ V't PH

rpM rnou

92.5

IDS.:

106.:in.:115. f 120. f 125.6130.]

134. f"139. f144. {149.: 154.:158. i

E

rooi*ot'0

93.5

106.:

in.:115. f120.? 125Jno.:134.1

139,1144.149.154. 158.163.

lOfM

1.0

1.0

5.04. S5.0 5.0 4.54.5

5.05.04.55.0 4.5

l 4.2

ASSAYSAll ........

'. -. 01 ra*

Tr

Tr

TrTrTr Tr TrTr

Tr.02.02, 18 .06.06

fjj TOK

DIAMOND DRILL RECORD NAME Of GOl'-EN SHADOW-CENTRAL PATRICIA

SHEET NO..

FOOTAGE

mot*

163.0

165.6

199.5

'ti

i

to

165.6

199.5

368.5

DESCRIPTION

INTERMEDIATE TO MAFIC VOLCANICDark green, fine grained, highly chloritic, minorlight grey chert fragments?.

IRON FORMATIONAs above, poorly bedded chert and magnetite withminor chloritic tuff. More chert, less magnetiteBedding at 55' to C. A.Sections brecciated. Less sulphides, probably2-3* with narrow sections to 107.-15H. (pyrrhotite,minor pyrite) .

176.5-183.5 - 15-201 pyrrhotite, minor pyrite, 151Irregular quartz veins, numerous quartz and sulphide filled fractures with minor displacement

183.5-190.5 - as above but 3-51 pyrrhotite, minorpyrite occasional laminated section with bedding45* to C. A,

190.5-199.5 - becomes more banded, still with quartzstringers, minor pyrite, pyrrhotite (1-21 overall)

INTERMEDIATE TUFF? (BRECCIATED?)Dark green, chloritic, fine grained, moderately towell banded at 40* to C. A. Numerous quartzstringers up to 1". Minor pyrite, pyrrhotite(1-21)

199.5-201.3 - 501 Irregular quartz vein 223.0-233.0 - graded change to medium grey, massively

banded (bedded?) at 45* to C. A. Occasional quartzstringer to 1 to 2 mm. No sulphides

233.0-248.0 - Dark green, heavily chloritized, shearedand broken (FAULT ZONE)

248.0-318.6 - medium green as above (223.0-233.0)with interbanded section of blackish greenchloritic material. Occasional oxidized section(water bearing fault zones?) Hazy fragmentssuggest brecla.

318.6-319.0 - FAULT ZONE327.5-328.0 - "

aAMPL

NO

980

931982

983984 985 986

987

988989

990 991992

\4lllfM

lOt!

r' DU |

163.0

165.6170.0

175.0180.0 185.0 189.5

194.5

199.0199.5

201.3 206.3211.3

OOf A6E10

165. (

170.1175.1

180.'185.1 189. 194,:

199.

199.201.

206. 211.216.

rotAi

2.6

4.65.0

5.05.0 4.5 5.0

5.0

0.51.8

l 5.0 5.0

l 5.0

mrs i V 01 tot

Tr

.03Tr

Tr.01 Tr Tr

Tr

Tr.02

Tr T rTr

01 TON

DIAMOND DRILL RECORD NAME Of

HOLE NO 5.5.iiyL~A-.FOOT AGE

rao*

368.5

398.5

478.2

.

TO

398.5

478.2

484.5

DESCRIPTION

IRON FORMATION BRECCIATEDMainly cream colored laminated chert with minor(3-5*) magnetite, minor chlorite chaotic mixtureof well-bedded sections with variable beddingdirections (generally out 55" to 60* to C. A.)and brecciated sections. Numerous roultidirectional minute fractures with displacementalong.Numerous veins, veinlets and stringers of blue-grey quart*.. Variable sulphides-pyrite andpyrrhotite, probably 5-87. overall with sectionsup to 30*.

371.6-372.6 - irregular quartz, minor pyrite380.5-381.0 - "4" quartz (blue) at 385.03" blue quartz veins at 379.5, 392.0 and 398,0

INTERMEDIATE VOLCANIC (ANDESITE)Dark green, fine grained, moderately chloritic,possibly fragmental near 'in' contact with palebrown fragments, Numerous fine quartz-carbonatefilled fractures, Moderately banded at 50* to C. A.near in contact, becomes massive

433.5-435.5 - interbedded magnetite (20*) in severalbands to 1" at 70* to C. A.

475.0-475,6 - CHERTY IRON FORMATION

IRON FORMATIONPale brownish grey chert with occasional narrowbands of magnetite. Chaotically brecciated. Minorquartz veining. Mino:' pyrite, pyrrhotite mainlyin cross-cutting stringers

480.5-481.5 - INTERMEDIATE VOLCANIC, as above

SAMPL

HO

994

995996997998900100C

701702

'Ot I MOM

368.5

373.5378.5383.5388.0393.0397.5

478.0483.0

E

r OOTAOtto

373.!

378.:383.:388.'393. f397.!398.:

483. f485.

101*1

5.0

5.05.04.55.04.51.0

5.02.2

ASSAYSAll

; o; 'o*

.01

.04

.03Tr.08.02.01

TrTr

01 100

DIAMOND DRILL RECORDnot r NC

root ABC

f MOM

ASA. 5

525.3

538.0

.

TO

525.3

538.0

DESCRIPTION

INTERMEDIATE TUFF (ANDESITIC?)as above (398.5-478.2)3" quartz vein at 485.0

487.0-487.7 - CHERT BRECCIA - fine fragmental textureminor pyrrhotite, pyrite.

494.7-496 0, quartz- sulphide zone. Tuffaceous.Crudely banded at 50', Dark greenish grey,chloritic. 257.-307, pyrrhotite, minor pyrite.2" white quartz at in contact.

496.0-530.3, as above (484.5-487.0)

IRON FORMATION, CHERT hINOR MAGNETITEPartly brecciated as beforePale brownish grey. Humorous fine fractures withdisplacement along. Numerous fine quartz veinletn. Minor pyrrhotite, pyrite, probably 3-57, overall.

533.0-535.0 - ANDESITE TUFF, as above

END OF HOLE

j GS-8

SAMPL

MO

703

'04'05'06

till *N

r*ou

A94.7

525.3530.3535.3

(Tv GOLDEN SHADOW- CENTRAL PATRICIA3-4

root'or

TO

i96.0

530.3535.3538.0

tot/

1.3

5.05.02.7

suet T NO. .-. . .?

ASSAYSAU

-.

Tr

TrTrTr

IKmggl n^ I^^^JM^^^^^^

DIAMOND DRILL RECORDNAMI or pnopciirv GOLDEN SHADOW- CENTRAL PATRICIAHOLt NOLOC ATIOI.

GS-83-5 LiNfltn 268 feetclaim 627

L.T.Tunr 3 -r 91 N nr-A.Tn.r 54 4 60 EELEVATION . AZIMUTH "^O DIP 45"

Feb. 16, 1983 Feb. 17 1983• T A D ———————————————————— r IN IBM EO ——————————————————————————————————

r o o T A o e

r* 0 M

0

14.0

125.0

W^

TO

15.0

125.0

211.0

DESCRIPTION

CASING

INTERMEDIATE VOLCANIC

r OOTAOt

268OIP

43"

Medium grey, massive to slightly banded finegrained. Numerous quartz veins to 1". Bandingand veins at variable angles to C. A. generallyapproximately 20*. Numerous water bearingfractures with iron oxide. At 53.0 2" quartzvein.

40.0-109.0, gradual change to darker green, mediumgrained with mottled texture probably representingpartial chloritic alteration (dark green clots)3"-4" quartz veins at 89.6 and 98.0

109.0-125.0, - TUFF? fine grained, grey green. slightlybanded at 10* to C. A. Heavly cnloritized nearlower contact.

IRON FORMATION, mainly cream colored chert withmagnetite. Alternating sections of well

minor

laminated beds at 55'-60" to core and chaotic brecciated sections with chert fragments interlacedby blue grey quartz and sulphides veinlets andstringers. Probably 107. pyrrhotite and pyriteoverall with sections to 3Q7.

152.0-170.0 - well laminated, more magnetite(probably 257.) S-8% pyrrhotite and pyriteshort sections to 307.

with

170.0-178.6, CHERT BRECCIA, as before, less sulphides3-57. overall.

A/IMUTM OOTAOt DIP

NO.

'07

'08'09'10'11'12'13'14'15'16'17'18'19

W' FOOT/FROM

122.0

125.0129.5134.0139.0143.5148.0153.0158,0163.0168.0172.5177.0

fd

125

f — — — — Mn r MO. "-; "T ' -'tnttt no, ... *A JIM UTM

*rM AUKS

T .onoeo BY K. J. Hodge

Gt

.0

129.5134.0139.0143.5148.0153.0158.0163.0168172177181

.0

.5

.0

.5

TOTAL

3.0

4.54.55.04.54.55.05.05.05.04.54.54.5

Au\ t or/ TON

Tr

T r.02.04.03.02T rT rTrT rT rTrT r

07/TON

mmmmmmwmmmmmmmmu

DIAMOND DRILL RECORD NAME Or PWO^EPTY GOLDEN SHADOW-CENTRAL PATRICIA

HOI- f NO ..GS-TJ

FOOTAGE

f ROM

211.0

268.0

)

*,

i-

to

268.0

DESCRIPTION

178.6-211.0 - Well bedded in thin chert-magnetitelaminae, at 60" to C. A. Dragfold at 189.0Scattered sections of heavy chlorite withheavy pyrite and pyrrhotite, up to 3" to 4" in core length.

183.0-184.0 - Quartz rubble, FAULT ZONE in quartzvein.

200.4-200.8 - heavy chlorite with 507. pyrite.

INTERMEDIATE VOLCANIC (ANDESITE)Medium green fine grained, numerous quartz-carbonate veinlets up to 1", generally at lowC. A. (approximately 20')

260-268.0 - Highly sheared and chloritized shearing20" to C. A. Mottled texture due to greenchlorite clots in grey matrix.

END OF HOLE

SAMPL

'JO

720721722723 724725726

Ipf S

f

r*0u

181.5186.0191.0196.0 200.0201.0206.0

h.-5..^

OO . AGE'D

.86.091.096.0100. 0 101.0!06.0111.0

TO f* l

4.55.05.04.0 1.05.05.0

SHEET NO .......r. .

A K\t vst o, ra.

Tr.02T rT r Tr.03T r

[i J TO*

5J Sedimentory Rocks o-Argillite, b-Greywocke

4 J iron Formation o-Magnetite, b-Chert

T"j Mafic Vblcanlcs a- Flows, b- Fragmented

Intermediate Volcanics

o-Flows, b- Frogmentals

l J Felsic Volcanics a-Flows, b-Fragmenfals

Sulphides

Pyrite. . . . . . . . . .Pyrrhotite . Magnetite . . Sphalerite. . . .Chalcopyrite .

Quartz Vein. . . .

Fault . . Intersecting Drill Hole. .

PyPoMagSpCp

Ov

GOLDEN SHADOW RESOURCES INC.

CENTRAL PATRICIA PROPERTY VERTICAL SECTION

D.D.H. GS-83-1Looking Northeast

GEOCANEX LTDTORONTO. CANADA

BY:DATE: NOV. 1963SCALE: L-COODWG. No: GS-18

W *S|

-iivxl

Z

8

GS-83-2

-100*

-200

297'

-300'

-400'

.. 'fe LEGEND- -^ r

f~j Sedimentary Rocks o-Argillite, b-Greywacke

Iron Formationa-Magnetite, b-Chert

T] Mafic \toteanlcs a-Rows, b-Fragmentals

2 j Intermediate Volcanics

o-Flows, b-Fragmentals

T~] Felsic Volcanics o-Flows, b-Fragmentals

Sulphides

Pyrite. . . Pyrrhotite . Magnetite Sphalerite. Chalcopyrite

PyPoMag

SpCp

OvQuartz Vein. . Fault . . . . -V/V Infersecting Drill Hole. . -0-

Au (0Xo) a ijFeet "*

5O IOO fe*t




GEOCANEX LTD TORONTO. CANADA

BY:DATE: NOV. 1903SCALE: I'SOO

No: G S-19

if

I

-- --05-7^:^5fe I

V) OD O

GS-83-3

Overburden

Py-5-10% Ov

-100'

-200

L28+5OC

2b-10-25 0Xo

4o-250XoMog ' 2b-l00Xo Po

Ov

2 b -Py 25- 4007o C-50

-300'

-400'

'•AV^Mr. :

^:^y^^^^^W^^^

LEGEND

5 l Sedimentary Rocks o-Argillite , b-Grevwacke

4 j Iron Formation o-Magnetite, b-Chert

3 ) Mafic volcanics a-Flows, b- Fragmenrols

2 [ Intermediate Volcanics

o-Flows, b-Frogmentals

Felsic Volcanics o-Flows, b-Fragmentals

Sulphides

Pyrite Pyrrhotite Magnetite . Sphalerite . . . Chalcopyrite

Quartz Vein

FaultIntersecting Drill Hole. .

Au (07o) Feet

PyPoMag

SpCp

Ov

50 IOO



D.D.H. GS-83-3Looking East


Bf:DATE: NOV. i*9JSCALE: l'COOOWO. No: 65^20

i.**- ',- ir.-v^-.-

-100

-200'

GS-83-4

S-I35O 33 S. of sect.

4b

-300

4b 3-507oPy,Po

2o

4bPo-25-30%

2b

538 O

-400

LEGEND

Sedimentory Rocks o-Argillite , b-Greywocke

Iron Formationo-Magnetite, b-Chert

j j Mafic \tolconfcs a-Flows, b- Fragmentats

2 [ Intermediate Volcanics

o-Flows, b-Frogmentals

l Felsic Volcanics o-Flows, b-Fragmentals

Sulphides

Pyrite. Pyrrhotite . Magnetite Sphalerite. Chalcopyrite .

Py

Po

Mog

Sp

Cp

OvQuartz Vem

Fault .

Intersecting Drill Hole. . - -

Au (0Xo) c *, Feet

5O



D.D.H. GS-83-4Looking North


BY:

DATE: NOV. 11*63SCALE i'6OCOWQ. No. GS^Zl

5j Sedimentary Rocks o-Argillire , b-Greywacke

^ Iron Formation o - Magne tile, b - Cher t

Mafic \tolcanics a-Flows, b- Frogmenfals

[ 2 j Intermediate Volcanics

o-Flows, b-Fragmentals

TJ Felsic Volcanics o-Flows, b-Fragmentals

Sulphides

Pyrite. . F/rrhotite Magnetite . Sphalerite . Chalcopyrite .

PyPoMag

SpCp

OvQuartz VeinKOUlt . . . . -v/v

Intersectmg Drill Hole. . -0-

Au (70) ** Feet

50 IOO

GOUJMM SHAUOV: RESOURCES INC.



GEOCANEX LTD TORONTO, CANADA

BY:DATE: MOV 1985SCALE: i 600iDwo. NO: GS-22

li

^

-too

-200

-300

-400'

^-::::r"vv

. u r- u

6. SON

6. DON

C

A c

: '-- -y :- '. ,-'-; - -. .'-.---r .'-- "' - - : . - - ' -. . - ' ' - - -

J u

5 st f

T*

1

ss

~- ^ ^

r*,-- -" —r-

r-* r* f

i~- i—

^^- f^****^ r-*

-"-"""^ r* r-'

LEGEND Sutpnidp5

-4j Quortz Porphyry pyr|fe

3 j Volcanics - mafic to intermed- Pyrrhotite . . . .'ate Chalcopyrite . . . .

pi2 Argillite ( in port silicate Iron VJUICMU . . ..

—— l - ,. v Carbonate . . . . . . . .Formation ;

Chlorite . . . . . .1 Iron Formation- oxide and car

- bonote facies and some silicate facies

)uortz Vein . . . . . . . . . . . . . . Qv

-

———— .- , ..-...--••e.^^.sl^gi...... ....,, ,... .îMii^^^^^HBrtaa^^^^^-^î^^^V' '--- ;V^--. -.^, ,;.,,- -.--•.••:,,.

S : ^-fS^-;- •v;: ^r^P^;.- : - -. -••^; . : j3 - - ,Vv- - - - - -- -.- ;"' "10. . . : rJ '\ - ,-.. : .':: - ' - ,' : "r -t- /' -

. - - f-"r*

t-"

' rX'

\ S " ^~"-^ cr^"^\ ' -' \ '^^ T'^'

r Tr 83-9^4 — V^ît- -^^.oposed jj^^ f ̂ ^ ..^^\ ̂ S3-e

L 4*r \ .- - .....y jL^vi^r-^ ^-^T ^Wr' ^r\':' - ^--~~~7 ^^-83-4

Proposed -^^j pfe /JflK \"^ ^ 7 ^- :^..l^' /--7 r Tr83-8 ^

^-/" " ** ^-Tr83-7 ^. ^^^^ T* ^ *- ^ "t ' ^ ~k\V v^, , . :, \^, ^ '^ ' lt^^

^^^^ ^ 'i^-V^^Î^X ^ L-Tr 83-10 Y^-\\^v^ ^ lt

\l l

4

,i li— — -

/'/^3^y/"1 ; v/

J~~^~) 10* | —————— —--———- ———— —— ———————————————— ——Trench . . . . . . . . . . . . . f^~s Foliation (inclined, vertical) y^*' .j^ ,~-r^t nPN qwAnow RF^niiRPFc: IMP

Dy ^™* — *-^^ ' ^^ ' VJ V^ L. Lx i- 1 V Ori/^L/V-/ VH (l LO V/ wli V^CO UNO.

. . Po Swamo . . . . . . . . -i- AssuTiec Contact . — ? — OPMTRAI PATRICIA PPOPPDTVJ " r - . - . - - - - - - - - . - - — " V^LN 1 rirtU rM 1 Mlîr\ r Mvjrt-li 1 Y

Cp pillows ^ AU- AO Geological Mappingriuows. . . . . . . . . . . . . . ô.. AU Mg ^ ]f. Nn a ,., -, ,, * r f am *. "" and Sampling

C Fault Direction --^ r 0

Cl Fracturing ............XX AREA 1C^vorx/ioxA/Bedding (inclined , tops \y v ̂ i v ITS W

unknown) X X ——————— ————————————

IT i, f i ^r M ? IO 20 30 40 50 crfjSfi DATE NOV. IMS'Fuull (turned, defined) . . ^ " - "KWu GEQCANEX LTD SCALE ,-eoo

^•^ mwl... - - TORONTO, CANADA DWG. No: GS-24

••-•••'•'-•'.•' . i .

'"-ff't-- tt -j-'~^- -f..*•••••••i

3h.

J

*v^

.-;v-

;- ,^-:. V V^*|

LU

8•*-

o to

tu oCO

'K

Z928

293O

t

Trench 83-6—-" -- Proposed Trench

S"

-T -Trench 83-5

y l- 6. 5O N

Trench 83-4•' T- ' -a~ 3

: 3

LEGENDQuartz Porphyry

Volcanics - mafic Jo intermed iate

Argillite (in port silicate Iron Formation )

Iron Formation- oxide and car - boiiofe facies and some silicate facies

Quartz Vein . . . . . . . . . . . . . . Qv

Sulphides

PynTe .Pyrrhotite .ChalcopyriteGalenaCarbonateChlorite

Py PO Cp Gn C

CI

Trench . . . . .

Swamp. . . . . .

Pillows. . . . . .

Fault Direction

Fracturing . . .

so*Foliation (inclined, vertical)

Assumed Contact . . .—7

Au ' Ag Sample No.. "** ' '"

Bedding (inclined, tops unknown). . .

S

s 8 O

metres

Faulf (assumed, defined)


CENTRAL PATRICIA PROPERTYGeological Mapping

and Sampling

AREA 1 East End

GEOCANEX LTD TORONTO, CANADA

QV

DATE NOV. iSCALE iDWG. NO. G ry-2"5

•.V- - .'y —— .-..-^-^ '^m^^^\

00 ID

2925

Trench 83-8

/;M

LEGEND

Quortz Porphyry

Volconics - mofic to intermed iate

Argillite (in part silicate Iron Formation )

Iron Formation- oxide and cor -Donate facies and some silicate facies

. Quartz Vein . . . . . . . . . . . . . . Qv

Sulphides

Pyrite . . . . Pyrrhotite . . Chalcopyrite Galena . Carbonate . Chlorite .

PyPo Cp Gn.C C!

Trench. . . . . .

Swamp. . . . . .

Pillows.

Fault Direction

Fracturing . . .

80*

Foliation (inclined, vertical).

Assumed Contact . . . . . —?

mSample No.

S

Bedding (inclined, tops unknown). . .

O l

metre*

Fault (assumed, defined)



and Sampling

AREA 1 Trenches 83-7 -8 -9

GEOCANEX LTD .TORONTO. CANADA

DATE NOV. 1983SCALE:owa No GS-26

|f,:,-

-:^:/

;ii i i i i i i i i i ii i i iiliS-v,:,:.. '-•i^w,1 - -•

••KR?•- •••3'*-^', -,/ ui -;^;--"--... - -.-vaf-.V;

9 ? '1^' s1 ' — — 6. SON

.-••••""" - ^"""^ li"" ~

~~"~ ~~?l '\/''''?'- ^ s ' S - '

^^ py ^ /' ^ j"^. —^ -^ ^- /x , -. o x x- ^ /" -X x X ~/ ' S s . -^ S \ ' s ' i 's' X - ^X / ,—— -. - 7 /OD^ V4^'//saV// 7 M^^

/^ :^-TPO //( U77^/; ) /x -y•-•--.-.........//////^ •- ••....... ..../././^

LEGEND CiilphiH..

3 Volcanics - mafic to intermed- Pyrrhotite . . . . . . . . . Po Swamp. . . . . . . . . . .ia ' e Chalcopyrite . . . . . . . . . . . Cp7 Pillows. . . . . . . . , . .

2 Argillite ( in port silicate Iron a ^n r- c -. n- ,- y . Carbonate . . . .C Fault Direction . . . . .Formation J

Chlorite . . . . . . . . CI Froeturmg . . . . . . . .[ 1 j Iron Formation - oxide and cor

-bonote facies and Bedding (inclined, tops some silicate facies unknown). . .

^ Quart/ Vein . . . . . . . . . Qv Fault (assumed, defmec

, - : : ^;-;^' r ^ •....-•. -:/-- . :- - .- :.' - - . - - ---.v--: .••-:-..'..- -•;'-:-;v:"^^^'

•' - " . ' ' --.

^•^LL— "29^--......_ ̂ '9 * * - - - . . . ^

1- V--..^-a- 3932 PO |^— ".j".

x ~~ U---T j,--...X ' -*- " X , W- ?Q^ f --~ 1 i?X /r *^ , 1-04-' l

t- x \i^S"\^ -'

X *- 2934 f 1-7,' ^"-'"— " PV ^ I| -^ .••\ i..- i.--'N ) r* " 2935 t ' -J/ r?^ C.-33J . - - - - . ,.. - - - . . .....\.. . -

/

~Ti — .-' 2936 1

•"•-"" '-'V, If- / if! W)-A-(//ytî '1J

. . . C-^s Foliotion {inclined, verticol) *** ^ GOLDEN SHADOW RESOURCES INC.

. .. ^ Assumed Contoct .— ? — CENTRAL PATRICIA PROPERTY

AU AQ Geological Mapping. . . ^ Ay Ag sompte No * *. - . ,, ** r' 1"m *. and Sampling

' ' J^ AREA 1o , , , . . Trench 83-1O

^ x . ————————————————— -' ' ' ' ' m*trt* ~?)Xr~ BV:

n eifriû DATE NOV "MU . . -v.-w W"^ GEOCANEX LTD SCALE i- IOO

'vv" *" " TORONTO. CANADA DWG. NO; 9S-27

: " - ^. - .-^-.

i:\*-*-'SyJ-

"•' V ---i-*^..:-^ ,-jjf, ^ ^

*^..^^,,-y.,,, . -,.,- .,.,. r v..;.-,-:,--:--,:-- , :-^:—— -.v----^--: ? , î^.^^-vS-^^ --.*-v: ••^^••-.^^;•^*.^r^^-W,?Â^^r^^^.^^^^

aSgHiM'IB^VK?* -~ ' ''gs^Bifejs-vV'.'-

Pli-:.

II

fi

1

I

1

1

1

1

1t '

P

6'Urn---

ijv'./

K

i^^^jS^^^S^^v*:^' : ;-"-7:^*'^f^jt^^'^%— ': ': ' ; ; - : "' . "\-T'-' ^D-^~^- -- " ' ; .. . - •."•':"

- . ^ ^ - ' ~- - . .

- : .: ''."

LEGENDf~4 | Quartz Porphyry

|3 | Volcanics - mafic to iniate

2 Argillite ( in part silicotFormation )

| 1 Iron Formation - oxide- bonate facsome silicate

• Quartz Vein- - ; v ; " ; :-.'" '- - - 'l'- ' -'•' .-••-'-, ,- -' --••-•" .\ . ,1*'- ' -

" ' . ' ' -' ' - ' " " " ' -^ * - . * -' V " . - ' ^ k ' -- - '-. ' ~ v -- - . -

•iui

Z955

/*: 2956

2954 - .Ol oz/too Au

Bose Line 00

Sulphides

Pyrite . . . . . . . . . . . . . . . . PyPyrrhotite . . . . . . . . . . . . . . . . PoCholcopyrite . . . . . . . . . . . . . CpGolena . . . . . . . . . . . . . . . GnCarbonate. . . . . . . . . . . . . . .CChlorite . . . . . , . . . . . . CI

Trench. . . . . . . . . ^ . . . . .

Swamp. . . .. . .;;:i:.

Pillows. ........ .. .

Fault Direction . ®i. . . . .

Fracturing . . ^.^'^-. . . .' ',!tt---~-' ."- "

Bedding (inclinedôps


Assumed Contact . . . . — 7 —

Au " Ag Sample No.. . " -* '' " ,...

f

Fault {assume^?cjeiRned)^vv -V.W, ,.......... -p^,^. ;; - ::vv.

sfeH^'Sls; :..-^pfeiîl^SSi!Zl''-'--'

m

o 10 20 3 s



and Sampling

AREA 2 North Section

61GEOCANEXLTO

TORONTO. CANADA

BY;DATE: NOV. 19*3SCALE- I'lOOO

•i&N?l-'-'OVt^Vi ^ . v\* iÊ, V.-

fî^^x^^&î^

^^'^'^^-•'^•.•••'''••^''•^''^^•'Â'^.^'^^-f^^

^Sia^d&^t^^^SêEifÛ^îHKSiJMiî'fiW'i^^^

DWG. No: 6 S -28

mm-^3&Zm

-S&asfiiss-

i if*.

i is l l l

2941

2942

2943

Qv,C,CI,Py, Po

^//

-l.50 S

Excovoted oreo

l m:-*t:l

l

l

l

i lssr

^

ste?^;v\-|g^^

LEGEND

4 l Quartz Porphyry

Volcanics - mafic to intermed iate


Sulphides

Pyrite . . . . . . . . . . . . . . . PyPyrrhotite . . . . . . . . . . . . . . . . PoChalcopyrite . . . . . . . . . . . CpGalena . . . . . . . . . . . . . GnCarbonate . . . . . . . . . . . . . . .CChlorite . . . . . . . . . . . . CI

l l iron Formation- oxide and car -bonate facies and some silicate facies

Quartz Vein . . . . . . . . . . . . . . Qv

Trench. . . . . . . . . . . . . .

Swamp. . . . . . . .. .. .. . . j^.

Pillows. . . . . .. . . . . . .. . ^

Fault Direction . . . . . . . . . ±z^

Fracturing . . . . . . , . .. . . /^ S


Assumed Contact . . . . . . — \

Au " A9 Sample No.. . f-** - '-y

Bedding (inclined, tops unknown). .. XX

m

O 5 IO 15 2O 25

Fault (assumedt defined) ;.; -;- :.-.^ri^W;c:; v


CiJJTRAL PATRICIA PROPERTYGeological Mapping

and Sampling

AREA 2 Trench 83-2

GEOCANEXLTD TORONTO. CANADA

BY:DATE: MOV.SCALE: K500DWQ. 6S-29

- , j-"*^rv ';" ."""VtV

®tf^*^@)t^^

MAGNETIC READINGS'I 1

7O69

5984

6O7O

2951

295O 25^-

2949 ^-,

2948 *-

Z42I

1164

957

Bockhoe trench

.2947

LEGENDQuortz Porphyry

Volconics - mafic to intermed iate


Iron Formation- oxide and car - bonate facies and some silicate facies

Quortz Vein . . . . . . . . . . . . . . Qv

Sulphides

Pyrite . . . . . . . . . . . . . . PyPyrrhotite . . . . . . . . . . . . . . . PoChalcopyrite . . . . . . . . . . . CpGalena . . . . . . . . . . . . . . GnCarbonate . . . . . . .. . . . . . .CChlorite . . . . . . . . . . . . . CI

Trench. . . . . . . . . . . . .

Swamp. . . . . . . . . .. . .

Pillows. . . . . . . . . . . . .

Fault Direction . .. . . . .

Fracturing . . . . . . . . . .

(C?SO*


Assumed Contact . . . — 7

Au-im

Sample No. .

Bedding (inclined,tops unknown):..;.

S

s O 5 10 15 2O 25 m*tr**.•"..v-'-.;'

Fault (assumed, defined) .


CENTRAL PATRICIA PROPERTY Geological Mapping

and Sampling i

AREA 2 Trench 83-3

DATE NOV. 1989

GEOCANEX LTD TORONTO. CANADA Dwa No: GS-3O

•C^g&g^^;^^^

l l l l

fiV'V, -

ElfIK

LEGENDQuartz Porphyry

Volcanics - mafic to intermed iate


Iron Formation- oxide and cor - bonote facies and some silicate facies

Quartz Vein . . . . . . . . . . . . . . Qv

Sulphides

Pyrite . . . . . . . . . . . . . . . . . . PyPyrrhotite . . . . . . . . . . . . . . . . FoChalcopyrite . . . . . . . . . . . . CpGalena . . . . . . . . . . . . . GnCarbonate . . . . . . . . . . . . .CChlorite . . . . . . . . . . . . . . CI

Trench. . . . . .

Swamp. . . . . .

Pillows.

Fault Direction

Froc luring . . .

Foliotion (inclined, vertical).

Assumed Contact . . . . . . .

Au " Ag Sample No.. . L

—?—

m

S

Bedding (inclined,tops unknown)...

O 5 10 15 2O 25

Fault (assumed, defined) ..



and Sampling

AREA 3


___

DATE: MOV. I98J SCALE: I-5OO

teB^>k^^

lfyfe

lft

Kr

l"mm

l

l

l

l

l

l

Tllli

Ov,CI,Py

Ov,Py

4

T

LEGEND

Quartz Porphyry

Volconics - mofic to intermed iate


Sulphides

Pyrite . Pyrrhotite Chalcopyrite Galena . , Carbonate. . Chlorite . .

PyPoCpGn-CCI

• li Iron Formation- oxide and cor -bonate f&cies and some silicate facies

Quartz Vein . . . . . . . . . . . - . - Qv

Trench.

Swamp.

Pillows.

Fault Direction

Fracturing . . .


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central patricia property pickle lake, ontario · 2017-01-17 · in the patricia mining district of...

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