010 canadian occidental petroleum ltd. geology and geochemistry · 2017-01-17 · 010 canadian...

010

CANADIAN OCCIDENTAL PETROLEUM LTD.

MINERALS DIVISION

GEOLOGY AND GEOCHEMISTRY

OF THE

SANDY 'ZAHAVY 1 CLAIM TRENCHES

SANDY LAKE BELT

NORTHWESTERN ONTARIO

6 MINING CLAIMS

NO. KRL 614679-614684

CLAIM SHEET M3016 - RAHILL LAKE

RECEIVEDJAH 101983

MINING LANDS SECTION

BY:

F.W. GITTINGS, HON. B.Sc,

COVERING WORK COMPLETED DURING OCTOBER 1982

TABLE OF CONTENTS PAGE

1. SUMMARY AND RECOMMENDATIONS...................... l

2. INTRODUCTION.................................. . . . 22.1 Location and Access.......................... 22.2 Previous Work................................ 4

3. WORK COMPLETED 19823.1 Trenching.................................... 63.2 Sampling and Analyses........................ 63.3 Petrography.................................. 63.4 Magnetic Susceptibility Survey............... 7

4. GEOLOGY.................... . ................ . . . . . 74.1 General Geology.............................. 74.2 Geology of the Sandy 'Zahavy 1 Claims......... 84.3 Geology of the Trenches...................... 9

4.3.1 Trench SAN-82-Z-T1 (Plan 1)........... 94.3.2 Trench SAN-82-Z-T2 (Plan 2) ...........11

4 .4 Rock Geochemistry........................... 11

5. CONCLUSIONS.............. . ..............,.. . . . . . . 12

6. REFERENCES.......... . . . . . . . . . . . . ......... . . . . . . . . 13

LIST OF TABLES

Table l Analyses on Zahavy Rocks.................... 62 Table of Rock Units......................... 7a

LIST OF FIGURES

Figure l Index Map................................... 32 Location of Zahavy Claims................... 53 Geology and Trench Locations................10

APPENDICES

Appendix I Analytical Results........................14II Thin Section Descriptions.................17

III List of Personnel......................... 28

PLANS (In Back Pocket)

Plan l Geology, Geochemistry and Magnetic SusceptibilityTrench SAN-82-Z-Tl

2 Geology, Geochemistry and Magnetic Susceptibility Trench SAN-82-Z-T2

- i -

- l -

1. SUMMARY AND RECOMMENDATIONS

Two trenches totalling 12.0 m in length were

blasted out across a shear zone with carbonate veins and a

small otucrop of iron formation located on the northern tip

of a small island near where, in 1946, Berens River Gold

Mines discovered gold bearing quartz veins.

Trench^ SAN-82-Z-T1 exposed a shear zone with

minor quartz-carbonate veins in a diabase dyke in contact

with a dacitic dyke or sill. In trench SAN-82-Z-T2 metasediments,

including iron formation, in contact with mafic metavolcanics

are exposed. Shearing is evident in phyllite along the contact

between the metasediments and the metavolcanics.

The trenches were chip sampled at a 0.25 m inteval.

All samples were analysed for gold, silver and arsenic. One

of the 40 samples contains 450 ppb Au. Generally the results

were diappointing.

The area surrounding the trenches has not been

sufficiently mapped for the writer to make a realistic

appraisal of the potential of the claim group as a whole,

however the iron formation and quartz veins tested do not

indicate a high potential for iron formation host gold deposits.

Further mapping is recommended.

- 2 -

2. INTRODUCTION

The Sandy 'Zahavy 1 Claims are part of an option

agreement with Zahavy Mines Ltd. All six claims in the claim

group are contiguous and are presently held by Canadian

Occidental Petroleum Ltd. of 180 Attwell Drive, 4th Floor,

Rexdale, Ontario, M9W 6A9.

The claims were staked by Zahavy Mines Ltd. to

cover the area in which a 1946 drill intersection containing

gold bearing quartz veins is reported.

Two trenches were blasted. One across a small

outcrop of iron formation and the other across the contact

between mafic volcanic and a dacitic sill to investigate the

gold potential of these rock types.

This report presents the results of the trenching

work and is submitted on behalf of Canadian Occidental Petroleum

Ltd., the holders of the claims.

2.1 LOGat ion and Acce s s

The Sandy 'Zahavy 1 Claims are located on Sandy Lake

225 km north of Red Lake in northwestern Ontario (N.T.S. map

sheet 53/F/3). The Zahavy claims are in the Red Lake Mining

District of Kenora (see Figures l and 2).

The native settlement of Sandy Lake is located 20 km

west of the claims. There are bi-weekly scheduled flights from

Winnipeg to Sandy Lake by Air-Dale as well as scheduled flights

from Thunder Bay and Pickle Lake.

Canadian Occidental chartered a float equipped Beaver

from Green Airways in Red Lake for transportation to the work

area from a base camp 10 km west of the claims.

"^f- Favourable Lake M one Site

Northwestern Ontario Index Map

LOCATION OFCANADIANOXY PROJECTS

SANDY CLAIMS

Figure lNTS. 528,52N,520,53A , 538, 53C.53F, 53G, 53H

O

Legend

- ' Poved road

—— Grovel roodTown

* Indian settlement

- 4 -

Highway 808, a new all weather road from Pickle Lake

to Windigo Lake comes within 50 miles of the properties to the

southeast. Winter haulage roads have been used in the past to

transport heavy equipment and supplies into the area.

Getty Mines Ltd. is presently undertaking development

work at the old Favourable Lake Mine 32 km southwest of the

claims. If the mine is brought into production there is a

possibility that an all weather road will be extended into the

area and provide direct road transportation to the south

(see Figure 1).

2.2 Previous Work

In 1938 Berens River Gold Mines drilled four holes

on their "Island Prospect". One hole intersected 0.98 oz/ton

Au over 0.3 feet and another intersected 0.76 oz/ton Au over

3.1 feet. Both intersections were in quartz veins. These drill

holes are believed to be located on the northern tip of the island

trenched in 1982 but no trace was found to indicate their

original collar locations.

In January 1982 ground magnetics and VLF-EM surveys

were conducted for Canadian Occidental Petroleum Ltd. over

the Zahavy Claims. The north-south survey lines are 100 m apart

with stations picketed at 20 m intervals along the lines. Results

from this survey are reported in "Report on Ground Magnetic

and VLF-EM Surveys, Grid A and Zahavy Grid; Patricia Portion,

District of Kenora, Northwestern Ontario", by F.L. Jagodits, 1982.

KEY MAP stole : 1 inch to 200 mite*

Fimire 2

PROJECT SANDY

North Western Ontario

N.T.S 53 C B 53 F

LOCATION MAPScol*: l'250,000 Figjre

CANADIAN OCCIDENTAL PETROLEUM LT!MinefoH Diyiiion Hov 82

- 6 -

3. WORK COMPLETED

3.1 Trenching

Two trenches totalling 12.0 m in length were blasted

out. The blast holes were drilled out using two pluggers,"an

Atlas Copco and a Wacker. The four-man crew spent one day,

October 10, 1982, drilling, blasting, mucking, mapping and

sampling the trenches.

3.2 Sampling and Analyses

A total of 40 channel chip samples were collected.

The sample interval was 0.25 m. All samples were analysed for

gold, silver and arsenic. Analyses were done in Ottawa by

Bondar-Clegg Ltd. The elements analysed, methods used and the

lower detection limits are listed in Table 1. Analytical

results are shown graphically on Plans l and 2, and listed by

sample number in Appendix I.

TABLE l

ANALYSES ON ZAHAVY ROCKS

Lower No. of Element Dectection Limit Extraction Method Samples

Au 5 ppb Aqua Regia Fire Assay AA 40As 2 ppm Nitric Pet- Colourimetric 40

rochloric Digestion

Ag 0.1 ppm HN0 3 -HC1 Atomic Absorption 40hot extr.

3.3 Petrographic Analysis

A total of 6 rock specimens were thin sectioned by

Geoplastech in Toronto and sent to Dr. S. Boutcher of St. Vital,

Manitoba for petrographic analyses. Her reports are in

Appendix II.

- 7 -

3.4 Magnetic Susceptibility Survey

A magnetic susceptibility survey was conducted along

each trench. Readings were taken on a 0.25 ra interval. The

survey was undertaken to determine the actual magnetic strength

of the various rock types. These observations will be used

in the future be enabling a comparison between the actual

magnetic properties of known rock types to the data received

from the ground magnetic survey. The results of this comparison

will aid in the interpretation of magnetic units not exposed and

provide a better understanding of the distribution of iron

formations underlying the claim block.

The instrument used was a Scintrex SM-5. Results of the

surveys are shown graphically on each plan of the trenches.

4. GEOLOGY

4.1 Gene ral Ge ology

This belt was first mapped in 1938 at a scale of

l inch to l mile (1:63,360) by Satterly (1938), and was later

included in a regional, l inch to 2 mile reconnaissance survey

(Bennett and Riley, Operation Lingman Lake 1969). Data

collected during the Bennett et al. (1969) survey was insufficient

to modify Satterly's interpretation.

"The underlying bedrock of the area is entirely

Precambrian in age. Throughout the region a heavy drift-mantle

of Pleistocene age overlies the bedrock with a maximum thickness

of 50 feet. Much of the drift is varved clay laid down in a

post-glacial lake; towards the east end of Sandy Lake the drift

consists of sand and boulders as well as clay.

- 7a -

TABLE 2

TABLE OF ROCK UNITS

Unit Description

Quartz-feldspar Porphyry Massive, light grey-green rock with sparse quartz and abundant feldspar phenocrysts set in a very fine grained groundmass.

Diabase Massive, medium grained dark green rock with an ophitic texture. Strongly altered with uralitic amphibole after pyroxene and chlorite and epidote after plagioclase laths.

Iron Formation Alternating bands rich in magnetite/ quartz and chlorite, hornblende and plagio clase.

Phyllite Light green, finely laminated with orientated flakes of chlorite biotite and sericite.

Basalt Massive, dark green, altered to tremolite and chlorite.

- 8 -

The Sandy Lake Belt is about 50 miles long and has a

maximum width of about 10 to 15 miles. Mafic to intermediate

volcanics which have undergone metamorphism to greenschist and

almandine amphibolite facies make up 80 to 90% of the belt.

The remainder of the belt is felsic to intermediate metavolcanics,

metasediments, and metagabbro" (Satterly, 1938).

4.2 Geology of the Sandy 'Zahavy* Claims

The geological information over the Zahavy Grid is

taken from Satterly 1 s map (1938). Along the shore of Sandy Lake

and the inland andesite is shown to occur together with quartz

stringers near the tip of the peninsula, which is covered by the

1982 geophysical grid. Amphibolite (part of the metavolcanic

sequence) was mapped on the small island in the southern part of

the grid. Porphyry dyke f quartz veins are shown at the southeast

tip of the island and it is noted that a rhyolite dyke is

indicated at the northern tip of this small island.

The exact location of the four holes drilled in 1946

is not known, but records would imply, that they are located on

the northern tip of the small island. Two of the holes

intersected gold bearing quartz veins associated with pyrite,

little pyrrhotite and chalcopyrite. The host rocks are

described as "fine grained greenstone andesite, coarse grained

siliceous andesite, very basic greenstone and diorite".

In his 1982 report, F. Jagodits compiled a geological

map using information from Satterly's report as well as

interpretation of the ground geophysical data. Figure 3

represents this geological interpretation. It shows three

major units underlying the claims block: 1) Unit l - Iron

- 9 .

Formation, characterized by large-amplitude magnetic anomalies;

2) Unit 2 - Mafic Volcanics, linear magnetic anomalies within

these units are believed to be more magnetic horizons within

the mafic volcanic stratigraphy; 3) Unit 3 - Felsic to

intermediate volcanics, characterized by gentle magnetic

gradients.

In Figure 3, a discontinuous magnetic horizon 2-1,

2-2 and 2-3 is shown. Jagodits stated that these magnetic

horizons probably represent a single unit disrupted by faulting.

This magnetic unit appears to lie immediately below the

contact between the mafic and felsic volcanic units. Trenching

done on the Zahavy grid shows that 1) the disruption in the

magnetic unit is due to the intrusion of dacitic and diabase

dykes and 2) there are at least minor amounts of iron formation

in the mafic volcanics which are reflected in the magnetic

anomalies.

4.3 Geology of Trenches

4.3.1 SAN-82-Z-T1 {Plan 1)

This 3.0 m trench was blasted across a sheared contact

between a quartz-feldspar porphyry and a diabase dyke.

The diabase dyke rock is medium grained, with an

ophitic texture. The rock has been extensively altered and

appears quite strongly strained in sample 82-SAN-4003 {see

petrographic reports in Appendix II). The rock is now composed

of uralitic amphibole, chlorite, epidote and remnant plagioclase.

The contact with the quartz-felspar porphyry is sharp.

The quartz-felspar porphyry contains sparse quartz

phenocrysts and very abundant plagioclase phenocrysts set in

an extremely fine grained groundmass. Quartz phenocrysts range

up to l mm in size and are often embayed when viewed in thin

- 10 -

MAJOR UNITS1 iron formation2 mafic volcanics with magnetite rich horizons3 felsic to intermediate volcanicsSYMBOLS

postulated faull magnetic anomaly

-xx—XX— edge of flat lying conductor— -——- postulated contact

xo: o

CANADIAN OCCIDENTAL PETROLEUM LTD. Minerals Division

PROJECT SANDY ZAHAVY CLAIM GROUPNorth Western Ontario N.T.S. 53 F2

1982 Trench Locations and Major Geological UnitsSCALE- 1=5000

FIGURE 3

FWG/gv/Dec.1982

- 11 -

section (see Appendix II, sample 82-SAN-4010).

Gold values are at or below the detection level of

5 ppb {see Plan l and Appendix I).

4.3.2 SAN 82-Z-T2 (Plan 2)

This 7.0 m trench was blasted to investigate the

gold potential of the iron formation located at the northern

tip of 'Zahavy Island 1 .

The iron formation exposed in the trench is

interbedded with other metasediments eg. phyllite and argillite

and appears conformable with the overlying and underlying mafic

metavolcanic rocks (see Plan 2).

The bedding strikes west-northwest and is vertical

or steeply dipping to the north. The contact with the overlying

basalt has been strongly sheared (see Plan 2 at 1.0 m). A 3 cm

wide pyrite rich bed occurs at the lower contact with the

underlying mafic metavolcanic amphibolite. Two grab samples

from this pyrite band were anlaysed and contain 60 and 15 ppb Au.

The sheared phyllite along the upper contact contains 450 ppb gold,

The irregular magnetic susceptibility profile of the

metasediment sequence reflects the interbedded nature of the

magnetic oxide facies iron formation with the non-magnetic

argillite and phyllite.

4.4 Rock Geochemistry

Forty samples were collected in the two trenches.

All samples were analysed for gold, silver and arsenic. The

results were disappointingly low.

The highest gold value is 450 ppb in a sheared phyllite

at the top of the metasedimentary sequence in trench Z-T2.

;.-J 4

l

- 12 -

Silver values were all below the 0.1 ppm detection limit.

Arsenic values ranged from below the detection limit of < 2 ppr to 235 ppm in an interbedded phyllite and iron formation. Th high arsenic value was accompanied by the second highest gold value of 100 ppb. Generally, however, there is no direct correlation between arsenic and gold content of the rock.

5. CONCLUSIONS

The Sandy 'Zahavy 1 Claims where investigated offer a low potential for iron formation hosted gold deposits. No sulphide facies iron formation was located. The small outcrop of oxide iron formation that was located and trenched does not contain economic levels of gold mineralization (the highest go value is 450 ppb).

The quartz-feldspar dyke exposed in trench Z-Tl is dacitic in composition and not the rhyolite dyke reported by Satterly (see section 4.2). The breaks in the iron formation distribution shown in Figure 3 are caused, at least in the are.- investigated, by the intrusion of diabase dykes and quartz- feldspar intrusions. Geophysics proved capable of aiding in the location of the iron formation in trench SAN 82-Z-T2.

Additional mapping should be carried out over the claim group where possible. The area along the southeast tip of the island should be investigated for iron formation

Respectfully submitted,r\Toronto, Ontario

December 1982

F.W. Gittings, Hons. B.Se

AUTHOR'S QUALIFICATIONS

FRED W. GITTINGS

Fred W. Gittings graduated from Brock University, St. Catharines, Ontario, with an Honours Bachelor of Science in geology in 1975.

Since graduation he worked as a mineral exploration geologist with Uranerz Mining and Exploration until joining Canadian Occidental Petroleum Ltd. in November, 1979.

While employed with Canadian,Occidental he has carried out and supervised mineral exploration projects in Saskatchewan, Yukon, and Ontario.

He is currently a member of the Canadian Institute of Mining and Metallurgy.

- 13 -

6. REFERENCES

jagodits, F.L., 1982: Ground Magnetic and VLF-EMSurveys, Grid A and Zahavy Grid, Patricia Portion, District of Kenora, Northwestern Ontario (53/F); unpublished report for Canadian Occidental Petroleum Ltd.

Leonard, K.W., 1982: Geology and Geochemistry of theSandy Claims, Sandy Lake Belt, Northwestern Ontario; internal report for Canadian Occidental Petroleum Ltd.

Satterly, J., 1938: Sandy Lake Area, Map No. 47F in47th Annual Report, Part 7, Ontario Deptartment of Mines.

- 14 -

APPENDIX I

ANALYTICAL RESULTS

- 15 -

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[ REPORTS 112-1830 PROJECT? SANDY ROCKS J

1 SAMPLE ELEMENT Cu Zn Hi CoL NUHBER UNITS PPM F'PM PPM PPM

-82-SAN-3036-82-SAN-400182-SAN-400282-SAN-400382-SAN-4004

82-SAN-400582-SAN-400682-SAN-4007B2-SAN-400882-SAN-4009

82-SAN-401082-SAN-401182-SAN-4012

^2-SAN-4013^-SAN-4014

82-SAN-401582-SAN-401682-SAN-401782-SAN-401882-SAN-4019




^^Bk.

WK-SAN-403582-SAH-403682-SAN-403782-SAN-403882-SAN-4039

MPPM

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O.IO.I0.1

O.IO.Io.i0.10.1

O.IO.IO.IO.IO.I

O.IO.IO.IO.IO.I

O.IO.IO.IO.IO.I

O.I0.1O.IO.IO.I

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O.IO.IO.IO.IO.I

Asm

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tfQ332

44

23235192

31731

317

33333

4442

51

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| PAGE 7

Au ut/Au NOTESm CM

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ô^tf

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5^tf^^

5^40

450^

10<5

5100

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^<5<5^60

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Ud.764 Btlfut Ra OtUwi.Onurio

K K, 0/5 :(6I))2J7-JIIO

'dn: 0)34453

BDNDABrCLEGGM Geochemical Lab Report

REPORT: 112-1930 PROJECT: SANDY ROCKS PAGE B

f SAMPLEL ,!1UM?ER

ELEHENT Cu Zn Ni Co Ad As Au wl/AuPPM ™ PPM PPM PP

82-SMH040 10 15

NOTES

- 17 -

APPENDIX II

THIN SECTION DESCRIPTIONS

- 18 -

Specimen No. - 82-SAN-4003

Rock name - strained looking ( amphibolitised and chloritised, diabase

Mineralogy - abundant - uralitic amphibolechlorite epidote

moderate amounts - remnant plagioclasesmall amounts - sericite

leucoxene carbonate pyrite - trace

Description - This rock is a medium grained diabase, with an ophitic texture f which has been extensively altered and quite strongly strained, so that it now has a confused looking texture and is largely composed of secondary minerals. However, some of the original plagioclase remains i and enough of the original texture can be distinguished for the original rock type to be clearly established.

The original texture is mainly retained by areas of uralitic amphibole which show almost simultaneous extinction. These are up to about ^ mm across t have irregular outlines i and typically enclose lath shaped crystals of plagioclase (in varying stages of alteration) in an ophitic fashion. These presumably represent the sites of original ophitic pyroxene crystals of medium grain size. These uralitic areas often have a rather cracked appearance, so that they appear to consist of a number of adjacent but slightly disoriented fragments. The amphibole is colourless, and sometimes intermingled with a little carbonate and/or chlorite.

No phenocrysts, or phenocryst pseudomorphs, were included within the area of the thin section. However, the hand specimen contains very occasional, relatively large, compact, light green patches which have the appearance of sparse phenocrysts.

The shearing stress which has affected this rock appears to have been taken up mainly by the altered plagioclase. Therefore, apart from those plagioclase laths which are enclosed by the uralitic amphibole, the altered plagioclase in this rock shows little or no trace of its original texture. It is now composed of a variable mixture of chlorite and finely granular epidote, containing jumbled remnant 'fragments' of plagioclase, which have a typically very highly cracked appearance. Patches of fairly dense, sheaf like, chlorite appear to represent areas of particular strain. The proportion

(continued overleaf)

- 19 -

82-SAN-^003 - continued

of epidote to chlorite is very variable! and a little sericite is intermingled with these minerals in some places, Small amounts of carbonate are also rather unevenly scattered through the rock. Angular masses of leucoxene, usually of the order of 0.5 mm across, are scattered through the rock probably making up about 5# of it. These probably represent original iron oxides. One irregular crystal of pyrite was also noted within the area of the thin section.

- 20 -


Rock name - strained and sericitised quartz-feldspar porphyry

Mineralogy - phenocrysts

groundmass

plagioclase quartzquartzo-feldspathic material sericite - abundant carbonate ) chlorite ) leucoxene

moderate amountsleucoxene )apatite )very small amountspyrite )

Description - This rock is a porphyry! with sparse quartz phenocrysts and very abundant plagioclase phenocrysts set in an extremely fine grained groundmass. The rock has been strained and altered, with the production of -abundant sericite accompanied by moderate amounts of carbonate and chlorite.

Quartz phenocrysts in this rock are small and sparse. They are up to about l mm in grain size, typically rounded or lobate in outline , and often embayed. They typically have a very highly strained appearance, but are not granulated. Plagioclase phenocrysts, by contrast, are extremely abundant. They range in size up to a maximum of about 3 ram, and grade down into the groundmass. They are only shadowily visible, as they are partially obscured by a finely disseminated covering of secondary sericite intermingled with a little carbonate. Some crystals have a rather cracked appearance, with quartz, sericite, or carbonate filling narrow cracks which run across the crystals. The plagioclase phenocrysts range from subhedral tabular to anhedral in outline.

The groundmass of this rock is extremely fine grained, with a rather streaky and irregular texture. It is composed predominantly of extremely fine grained quartzo-feldspathic material which is too fine grained for individual crystals to be clearly distinguished. This quartzo-feldspathic base contains abundant finely disseminated sericite which makes up around 2 0fo o f the groundmass. The sericite is rather streakily and somewhat unevenly distributed and shows a rather poorly developed preferred orientation. Intermingled rather irregularily with the sericite there is a moderate amount of tiny anhedra of carbonate. Moderate amounts of chlorite are also present, but are mainly restricted to clots and stringers of variable size and shape which are composed virtually entirely of chlorite and leucoxene. One or two of these clots have a form which is suggestive of a possible derivation from a biotite crystal, but most have very irregular outlines and tend to


- 21 -

8 2-SAN-^-010 - continued

be drawn out within the same direction as the preferred orientation of the sericite. It seems likely that the chloritic clots represent a low proportion of original ferromagnesian material. Leucoxene in this rock is mainly restricted to the chloritic clots, although a few tiny clots do occur in the main part of the groundmass. One or two tiny grains of pyrite were also noted, and there are occasional tiny euhedra and subhedra of apatite scattered through the groundmass.

The thin section is cut across by a narrow fracture zone in which the material is finely granulated. ^e^e there is a dense base of finely granulated material containing angular fragments of the host rock, finely disseminated carbonate, extremely fine grained epidote, and a little patchy chlorite. This zone is about 2 mm wide.

- 22 -

Specimen No. - 82-SAN-^013

Rock name - uralitised basalt

Mineralogy - very abundantabundant small amounts

uralitic amphibole remnant plagioclaseclinozoisitesericitemagnetitecarbonate ) mainlychloritepyriteepidote

) in fractures

Description - This rock is a fine grained i non-porphyritic, basalt which has been pervasively uralitised. The original ferromagnesian material has been completely replaced by uralitic amphibole , while the original plagioclase of the rock remains relatively unaffected by the alteration, and clearly retains the original texture of the rock.

Plagioclase appears to have made up slightly less than 50^ of the original rock. It formed randomly oriented, lath shaped, crystals of rather variable size. These average around 0.25 ram in length, with the maximum being about 0.5 mm. They are relatively fresh with respect to the associated ferromagnesian material, but are partly obscured by secondary minerals. These include marginal invasion by the surrounding uralitic amphibole, and varying proportions o f extremely fine grained clinozoisite, accompanied by some sericite. Some crystals also contain a little patchy chlorite. Some retain traces of compositional zoning, but they are too badly obscured for their composition to be determined.

The plagioclase crystal remnants are surrounded by a mass of shreddy looking uralitic amphibole which completely replaces the original ferromagnesian minerals of the rock. This amphibole is fine grained; occasional optically continuous areas are up to about 0.5 mm across, suggesting that this was probably the maximum grain size of the pre-existing pyroxene. The original rock therefore probably had a doleritic i texture. The amphibole has a pale green colour, and is probably of actinolitic composition.. It contains a moderate amount of small, scattered, inclusions of magnetite. A very little carbonate and chlorite is found scattered throughout the rock.

The thin section is criss crossed by a network of fine fractures. These are marked by a narrow zone composed mainly of a mixture of chlorite and carbonate, along with occasional scattered masses of pyrite. These fractures have rather poorly defined margins in most cases. Other fractures contain a little finely granular epidote, or fine grained feldspar.

- 23 -

Specimen^No. - 82-SAN-4020

Rock name - finely laminated iron formation, with magnetite-rich, and quartz-rich laminae. The rock is cut by numerous microscopic faults.

Mineralogy - very abundant - quartzabundant - magnetitemoderate amounts - chlorite (in magnetite rich laminae)

small amounts - goetheitecarbonate

Description - This rock is a very finely laminated, and slightly metamorphosed, banded iron formation. It is composed of laminae of quartzite, intercalated with laminae rich in magnetite. The magnetite-rich laminae also contain a moderate amount of quartz and chlorite. Within the area of the thin section the rock is cut by a number of microscopic faults. These are subparallel to each other, and oriented approximately at right angles to the bedding planes of the rock. These faults result in some minor crumpling of the laminae. They typically have offsets of the order of about l mm.

The thin section contains two fairly well defined quartzitic bands 4-5 mm wide, with magnetite rich bands both between and on either side of them. The quartzitic bands are composed essentially df a very fine grained, sutured, mosaic of quartz anhedra of rather variable size, averaging around 0.05 mm. Scattered through this quartzose base there are very occasional tiny patches and crystals of carbonate and, in some places, a few tiny granules of magnetite and flakes of chlorite.

The magnetite rich bands are extremely finely laminated. The laminae are as narrow as 0.02 mm wide, and are distinguished by the varying proportions of magnetite present. All gradations from virtually monomineralic magnetite laminae to the virtually magnetite-free quartzite are present. The magnetite occurs in masses of very tiny compact crystals, usually of the order of 0,01 mm or less in grain size. It is set in a base composed of fine grained quartz, similar to that described from the quartzite band, intermingled with varying amounts of very tiny chlorite flakes. The proportion of chlorite is very variable, from virtually none to laminae in which it is abundant as the associated quartz. The chlorite is a fairly deep green penninitic variety, and forms minute flakes which show a very poorly developed preferred orientation parallel to the bedding of the rock. Where the minor faults cut the magnetite rich bands, segregations of quartz, or chlorite, tend to infill


- 24 -

82-SAN-4020 - continued

some of the faults, while the magnetite-rich bands also contain a number of irregular quartzose and chloritic segregations. Occasional carbonate-rich stringers which run across the quartzite bands, parallel the microscopic faults and probably indicate planes of weakness parallel to them. A little goetheitic material is present in some of the fault planes, and within some of the magnetite-rich bands.

- 25 -


Rock name - finely laminated banded iron formation, with chlorite and hornblende-rich bands

Mineralogy - abundant - chloritehornblendemagnetiteplagioclase

moderate amounts - carbonatetraces - pyrrhotite

chalcopyrite epidote

Description - This rock is a banded, magnetite-bearingt iron formation. Within the main bands, which are of the order of 0.5 - l cm thick i the bands:.are themselves very finely laminated. Within the area of the thin section there is one magnetite-rich band, a band composed predominantly of chlorite, and a relatively wide band composed of a mixture of chlorite, hornblende, and plagioclase. The latter band is characterised by a number of cross-cutting cracks and irregular segregations, usually filled by carbonate.

The magnetite-rich band is composed of very fine, rather streaky looking, laminae of magnetite, intermingled with streaks and lenses of fine grained carbonate, and with abase of extremely fine grained chlorite intermingled with some hornblende. A little extremely fine grained feldspathic material is also intermingled with the chlorite and hornblende in some parts of this band. Overall, magnetite probably makes up close to 50^ of this band, with the proportions of other minerals being rather variable.

The predominantly chloritic band makes up the other side of the thin section from the magnetite-rieh.band. It consists predominantly of extremely fine grained, pale green, chlorite which shows a very well developed preferred orientation paralleling the lamination of the rock. Intermingled with the chlorite there is a low proportion of very tiny feldspathic anhedra, and a low proportion of scattered magnetite anhedra, (about 5?0 * Occasional somewhat larger anhedra of deep blue-green hornblende are scattered through the chlorite. These tend to be elongated within the plane of schistosity established by the chlorite. The average grain size in this band, and in the magnetite-rich band, is typically less than 0.02 mm. The chlorite-rich band also contains a low proportion of tiny, scattered, epidote granules.

(continued overleaf).

- 26 -

82-SAN-4033 - continued

The central portion of the thin section is composed of a rather variable, and less clearly laminated, mixture of plagioclase, chlorite and hornblende. The plagioclase occurs in angular 'chips' which are up to about 0.3 mm in grain size and have the appearance of sand-sized detrital grains. These are usually 'pitted 1 by tiny scattered inclusions of chlorite. These grade in size down into the surrounding rock t and are intermingled with abundant irregular anhedra of deep blu-green hornblende of similar size which appear to be randomly oriented. Both minerals are embedded in a base composed of extremely fine grained chlorite and feldspathic debris. This band is characterised by the presence of numerous cracks, most of which are oriented approximately at right angles to the bedding, which are filled by a fine grained carbonate mosaic. In addition, there are a number of irregular, carbonate-filled, segregations within this band as well as spme irregularily disseminated carbonate. Magnetite is almost absent within this band.

PYRITIC METASILTSTONE*

82 SAN - 4040

Offcut :

Crudely banded grey-green to black rock with crystalline aggregates and veins of pyrite. Hard and siliceous gangue. One darker band is quite strongly magnetic.

Mineralogy :

Quite variable, depending upon position in slide.

Quartz 70 0A Av. 0.05 mm (50 micron).Opaques 15&, pyrite; includes disseminated magnetite.Carbonate 103*,Epidote 5#, granular, yellow-green.Chlorite 2 1, Fe/Mg ** 0,5, pale-green.

A carbonate - quartz breccia vein occurs at one end of the slide.

Texture, Structure, Fabric

The rock consists of weakly crenulated bands of chlorite - epidote, sulphide-carbonate and sulphide (pyrite), interbanded with fine grained mosaic quartz. In contrast to SAN 1137, the sulphide is crystalline, and rarely spongy. The nature of the quartz suggests the rock has under gone cataclasis, and this is confirmed by the appearance of the 0.5 cm wide quartz-carbonate vein. This vein is composed of broken fragments of composite quartz with undulose extinction set in a matrix of carbonate. Chlorite (blue-green-purple under X-polars) forms a selvage to the quartz carbonate breccia vein, suggesting a genetic relationship between the two.

* Meta-argillite is also applicable.

- 27 -

Specimen No. - 8 2-SAN-40 38

Rock name - tremolite amphibolite of indeterminate origin

Mineralogy - very abundant - tremolitic amphibole moderate amounts - chloritesmall amounts - plagioclase

leucoxene sericite

Description - This rock is a tremolite amphibolite! with a very confused looking texture and no trace of the original texture to indicate the original nature of the rock t It is composed of a mass of shreddy looking anhedra of tremolite* through which there i s scattered a moderate amount of very irregularily distributed fine grained chlorite. A low proportion of plagioclase is present* in small irregularily shaped anhedra , and there is also a little scattered leucoxene and sericite.

There is no regularity of texture in this rock, or traces of pseudomorphic textures. Tremolite makes up about Q Ofo of the rock. It is a virtually colourless, very fresh looking* mineral which forms irregularily shaped, shreddy looking, masses which are almost optically continuous over areas of around 0.5 mm diameter in many cases. These are intermingled with, and cut across by, patches in which the tremolite is composed of very finely matted, fibrous, crystals. Chlorite occurs, intermingled with the tremolite in a very irregular fashion. In some cases the chlorite is intimately intermingled with the tremolite; in other cases it forms irregular patches of varying size and shape, scattered through the tremolitic material. The chlorite is also virtually colourless, and is almost isotropic.

The plagioclase which is present in this rock is sparse (10-15^), occurs in small roughly equidimensional anhedra, and gives no textural indication of the original rock. The crystals are only sparsely twinned, generally very fresh looking, and are probably of metamorphic origin. They tend to be marginally invaded by needle-like fibres from the 'frayed 1 margins of the adjacent tremolite crystals.

The only other minerals identified in this rock were sericite and leucoxene. Sericite occurs extremely sparsely, in tiny flakes which are irregularily scattered through the tremolite. Leucoxene is somewhat more abundant, forming small compact masses, usually of the order of 0.1 mm across, which are rather irregularily scattered through the tremolite. They often tend to occur in loose aggregates of several masses.

Late stage carbonate veinlets are also present, which are generally oriented perpendicular to the banding.

Alteration :

The crudely banded nature of the euhedral sulphide suggests this sediment contained a primary sulphide component. There is an intimate association of pyrite with carbonate, however, which could imply that the pyrite has formed through re-actions involving ferroan-dolomite and/or siderite during a sulphidation event. Some of the larger non-banded segregations of pyrite certainly suggest this possibility.

Opaques :

White to creamy pyrite is the dominant sulphide present. Some of the sulphide grains are embayed, suggesting the original sulphide was euhedral. At high power magnification numerous small (5-10 micron) inclusions of pale yellow-white chalcopyrite are resolved. Minor grey magnetite is disseminated throughout the slide. No visible arsenopyrite. The Cu assay should be moderate ^100 ppm). One large (l mm) grain of pyrite is observed in a non-pyrite-bearing portion of the slide.

Assay :

15 ppb Au, 10 ppm As.

Interpretation :

A siliceous metasiltstone which has been affected by a dynamic event and flooded by pyrite and carbonate. It is difficult to tell if the pyrite is entirely introduced or has formed through sulphidation of a pre-existing iron-bearing phase.

- 28 -

APPENDIX III

LIST OF PERSONNEL

- 29 -

APPENDIX III

FIELD WORK

Name Title

LIST OF PERSONNEL

Address Dates

Mike Henrick Project Supervisor

Fred Gittings Project Geologist

Art Murdy Project Geologist

John Allard Prospector

FFICE WORK

Sue Allen

S. Annett

F. Gittings

Draftsperson

Typist

Project Geologist

Canadian Occidental Petroleum Ltd. 180 Attwell Drive 4th Floor Rexdale, Ontario M9W 6A9

Same as above

530 John Street Espanola, Ontario POP ICO

Canadian Occidental Petroleum Ltd. 180 Attwell Drive 4th Floor Rexdale, Ontario M9W 6A9

Oct. 10, 1982 (l day)

Same as above

Dec. 9 , 101982(1.5 days)

Dec. 22, 1982 (1.0 day)

Dec. 15, 161982(2 days)

900

100

1983 10 19 2.5336

Mr. Albert Scott RivettMining RecorderMinistry of Natural ResourcesOntario Government BuildingBox 324Red Lake, OntarioPOV 2MO

Dear Sir:

RE: Geological Survey and Assaying Survey on mining claims KRL 614681 it the Area of Rahill Lake

The Geological Survey and Assaying Survey assessment work credits as listed with my Notice of Intent dated September 14, 1983 have been approved as of the above date.

Please Inform the recorded holder of these mining claims and so 1nd1date on your records.

Yours very truly,

E.F. AndersonDirectorLand Management Branch

Whitney Block, Room 6643 Queen's Park Toronto, Ontario Phone:(416)965-1380

D. K1nv1g:mc

End.

cc: Canadian Occidental Petroleum Limited 180 Attwell Drive 4th Floor Rexdale, Ontario M9H 6A9

cc: Resident Geologist Red Lake, Ontario

© Ministry of Technical Assessi Natural .

Resources Work CreditsOntario ^p

men! w*2,5336

Biite Winino Recorder'1 Report of1983 09 14 WQrk ^0' 100

Recorded HolderCANADIAN OCCIDENTAL PETROLEUM LIMITED

Township or AreaRAHILL LAKE AREA

Type of survey and number of Assessment days credit per claim

Geophysical

Ei*ctromeonftic day*

|nrt"C"d pollination ,, , days

nther flays

Section 77 (19) See "Mining Claims Aliened" column

ttpnlngirpl days

fienrhpnrvral days

Man days CI Airborne D

Special provision d Ground CD

G Credits have been reduced because of partial coverage of claims.

O Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Clilmt Atsewed

S736.00 spent on petrographic studies and on assaying samples taken from mining claims KRL 614680, KRL 614683

49 days credit allowed which may be grouped in accordance with Section 76(6) of The Mining Act.

For Mining Recorder use: The work assignment

for each of the above listed two claims is 24.5 days per claim.

Special credits under section 77 (16) for the following mining claims

No credits have been allowed for the following mining claims

l — j not sufficiently covered by the survey l — l Insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary In order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 77(19)—60:

828 (83/6)

/^z\ Ministry ot Technical Assess iVr 1 Natural t i , , ^ . u \Vj Resources Work Credit*Ontario ^B

ment f*'* 2.5336

Dete Mining Recorder'! Report of

1983 09 14 work W 100

Recorded HolderCANADIAN OCCIDENTAL PETROLEUM LIMITED

Township or AreaRAHILL LAKE AREA

'Type of survey and number of

Assessment days credit per claim

Geophysical

Dthor .days

Section 77 (19) Sac "Mining Claims Assessed" column

14Geological . dayi

Geochemical f*ayi

Man days S Airborne tU

Special provision D Ground G)

j~l Credits have been reduced because of partial coverage of claims.

(~1 Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Clelms Attested

KRL 614680 614683

k

Special credits under section 77 (16) for the following mining claims

No credits have been allowed for the following mining claims

I^J not sufficiently covered by the survey l — l Insufficient technical data filed

KRL 614681-82

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on

each claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 77(19)—60:

826 {83/6)

Ministry of NaturalResources

ftario

Yourfile:#100

1983 09 14 Our file: 2.5336

Mr. Albert Scott RivettMining RecorderMinistry of Natural ResourcesOntario Government BuildingBox 324Red Lake, OntarioPOV 2MODear Sir:

Enclosed are two copies of a Notice of Intent with statements listing a reduced rate of assessment work credits to be allowed for a technical survey. Please forward one copy to the recorded holder of the claims and retain the other. In approximately fifteen days from the above date, a final letter of approval of these credits will be sent to you. On receipt of the approval letter, y^u may then change the work entries on the claim record sheets.

For further information, if required, please contact Mr. F.W. Matthews at 416/965-1380.

Yours very truly,

**\ XXXAnderson Director Land Management Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1316

^. D. Kinvig:mc

Ends:cc: Canadian Occidental Petroleum Limited

180 Attwell Drive, 4th Floor Rexdale, Ontario M9W 6A9

cc: Mr. G.H. FergusonMining S Lands.Commissioner

845 Toronto, Ontario

Ministryof Notice of Intent NaturalResources for Technical Reports

Ontario

1983 09 14

2.5336/100

An examination of your survey report indicates that the requirements of The Ontario Mining Act have not been fully met to warrant maximum assessment work credits. This notice is merely a warning that you will not be allowed the number of assessment work days credits that you expected and also that in approximately 15 days from the above date, the mining recorder will be authorized to change the entries on his record sheets to agree with the enclosed statement. Please note that until such time as the recorder actually changes the entry on the record sheet, the status of the claim remains unchanged.

If you are of the opinion that these changes by the mining recorder will jeopardize your claims, you may during the next fifteen days apply to the Mining and Lands Commissioner for an extension of time. Abstracts should be sent with your application.

If the reduced rate of credits does not jeopardize the status of the claims then you need not seek relief from the Mining and Lands Commissioner and this Notice of Intent may be disregarded.

If your survey was submitted and assessed under the "Special Provision-Performance and Coverage" method and you are of the opinion that a re-appraisal under the "Man-days" method would result in the approval of a greater number of days credit per claim, you may, within the said fifteen day period, submit assessment work breakdowns listing the employees names, addresses and the dates and hours they worked. The new work breakdowns should be submitted direct to the Lands Management Branch, Toronto. The report will be re-assessed and a new statement of credits based on actual days worked will be issued.

846 (82/5)

•Mimstryof Report of WorkNatural ,~ , . , r- , . ,R.. SO , ,r s (Geophysical, Geological,

Geochemicel arid Expenditures)

The Mining

Instructions: Please type or print.— If number of mining claims travers

exceeds space on this form, attach a.li Note: — Only days credits calculated in t

i " Expenditures" section may be enter \tif i n the "Expend. Days Cr." colum

{O — Do not use shaded areas below.Township or Area

, pf o* Sur veyis)

Geological and Chemical Report. . , ...,.Ci?-: m Holder's)

.Canadian. Occidental Petroleum Ltd.. ,. .. , . . . .Address

180 Attwell Drdve, 4th Floor, Rexdale, Ontario M9W 6A9Survey Company 'Date of Survey (~from ^ to)

Day J Mo.J Yr. Day J Mo. ± Y r.

- . .Prospector's Licence No.

T644

Total Miles of line Cut

Ni!r-,t arid Address of Author (of Geo Technical re-port)

-Er.e.d .Gl.t.^ing^,-JL8JI..At.tMaU ..Driv.e^.,JLth Floor, Rexdale,, Ontario M9.W 6A9Credits Requested per^ Each Claim in Columns at r ight M ining^Claims Traversed (List in numerical sequence)Special Provisions

For first survey:

E nter A O d ays. (This includes line cutting)

For e:och additional survey: using the same grid:

Enter ?0 days (for each)

Geophysical

- E lecjromaonetic

- Magrieiometer

- Rediomelric

- Other

Geological

Geochemicel

Days per Claim

a^ Days

Cornpirie reverse side fins' tntet totBl(s) here

Days per Cltim

- r.'c or,f tO'r.t U'

- Radiometric

- Other

Geological

Geocherriicaf

14

Airborne Credits

K'ole: Spt'Cta! precisions Elecirorrt&oneticcredits do not apply ito Ai'borne Surveys, i Magnetometer

Rodiornetric

Days per Claimr —-- —~

Expenditures (excludes power stripping)Type of work Performed Analyses of rock

Eetrographijc _ studies. ^^^ ___ ... ....Performed On Clairn(s)

KRI, 614683 and KRL 614680

iCulalion o~f Expenditure D&ys Credits

l oial T xpt'fto'hures7o;a!

Dt ys Cfediis

. J ^ Q5] ^ f l?-!]Insfuctions

Total Dtys C'triits rriay t-e apjportioned at the claim holder's choice Enter number of (leys credits per claim selected in coljr-iris n \ r ight.

Mining Claim "Pr efix"T Nu mber

.61.4 fi a 2..

Expend. Days Cr.

X-^S

/^NINCjiANDSSEGl

.orDfc..Ho'-ei O' Acem (S'onstu'c) j f'^JyJjydC. J v

ia! number o* rriining ci&ims cc^'Cfed by this

•For'tmice U se Only ] __J'__"

Mining Claim Prefix | Number

RfiCEJVEPOtClB1982

•xpend Days Cr

ON

Nov. ^4/82^ CtJ-tificaticM"! ^''j; | i"'yinQ^Report^c)f Work

l he:eby Certify that l h?v? i personal and intim:-.:e J.noivledge of the f^cts set forth in the Report of VVoik annexed hereto, having performed the work or v . i trif-f.sed sane djririr, ar-.d/or tfler its completion and the annexed report is true.Vsfn.:- and Festal A:ioreT.s of Pt'&on Ce'ti*yirip

Fred Gittings, 180 Attwell Drive, 4th ̂ F

3 se? (si '9)

pete CertNov.

Canadian Occidental Petroleum Ltd.

August 4, 1983

Mr. E.F. AndersonDirector, Land Management BranchMinistry of Natural ResourcesWhitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3

Dear Mr. Anderson:

RECEIVEDAU8 3 i tgf-j

M1N.NG LANDS SECT.ow

Re: Your File 2.5336Mining Claims KRL 614681

____in the Area of Rahill Lake

I enclose the following as requested in your letter of August 4, 1983:

(1) Geological maps, in duplicate, entitled "Project Sandy Zahavy Option" signed and dated by F.W. Gittings*

(2) Resume of F.W. Gittings, (3) Verification of Expenditures.

I trust the above is satisfactory.

Thank you.

i Yours truly,;' \ ' ' ( '


RJE/sa

Enclosure

R.J. Evans Administration Manager

Minerals Division — 1BO Attwell Drive, 4th Floor, Rexdale, Ontario M9W BA9 [416] B75-S31S Telex O6-9B9493

BDNDAR-CLEGG S. COMPANY LTD,

764 BELFAST ROAD. O^TTA,Yy.A1 ONTARiO, K1G OZ5

/y:'~ Fr-fH";..*-.!^fa -^".J/^D -

PHONE: S37-311O

August 16, 1983

Canadian Occidental Petroleum Limited 180 Attwell Drive 4th Floor Rexdale, Ontario M9W 6A9

Attention: Mr. R. Evans

Dear Mr. Evans

In a recent telephone discussion with Mr. Art Murdy of your firm, he had requested that we provide written confirmation that the invoices submitted with the Bondar-Clegg reports 112-1795, 112-1830 and 112-1872 had been paid.

We are confirming that full payment has been received for the following invoices, which correspond to the reports mentioned above

Invoice No.

101378

101429

101430

101464

101474

101536

Copies of these invoices are attached.

Report No.

112-1795

112-1795

112-1830

112-1830

112-1872

112-1872

Amount

959.09

660.00

1,420.95

2,599.25

1,392.99

882.00

Yours truly

WHITEHORSE VANCOUVER OTTAWA CAMPBELLTON

. ff , , u - -Jf*

i M D AFt .- C L b Gi G SL C CD NC *-V\ NY LTD .

BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455

U*HHl)lttHl .H. 01l H') M! IWKl.l MR,1IH H.OUKkhXMMt.br

UHITK.I)

Hw t 112-

SnHOY KOCKS

l 3 'j

li'.1 i

110

u(

t.*t-bub 1 1." 1. 1.1 1

fct

tfl

wf C KUBHrPULVtKnE -200 Hublolfal

Hi VCfc* J l eJllt'UUi t'lltf Ci']

IflYUJlCl'

u'.? * w* \

vo.ov vo f ov

. hit

y o.o y

f y y v, o 9

THIS IS A PROFESSIONAL SERVICE

y. CLEGG "&L UUfV^HANY LTD.BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455

PKTKUU.UMr , H, on mm*1 HO H! M4bU lib., H H KLMOR

.r UHIAK10J1VU

l O H 30

U-1 Huv(-*liibttf O'j?

Hoi 312-1830

KOCKii

tin t.* j v* vi ul fei l'/orM11 e* i V li v le O l t. u L* tt l t

. V l . l .mil/'Jl yv-'-.'i w| t ui'f*-'r HI i tit l y s t? is o|' Hit'f.ul

frU'V uf 3! i l H: ir'lblul ail

u P ffi -* r* t ion ii*iHrlt,'fe wf C

s* J,

fivt

J ,VO

o, yo o, ^o

.'it? i BC1

321'10

6-1 y, 20

*t 2. 7li 772.73

TH/S IS A PROFESSIONAL SERVICEFM 1C U/LJCM DB

BDNDAT^CLEGG S. CDf\PANY LTD.ROAD, OTTAWA, ONTARIO, K1G 025 PHONE: 237-3110 TELEX: 053-4455

H OlTIDEMIVit PETROLEUM DMITEJJF. w, aimJ80 AnNELL liH FLOUR

P* Iff t Hov^wbcT JO r

Rtipoi'l Mot 112-1830

ProJvcl* SAHDY ROCKS

ut

Ahflwt't

l. o*, w l

Atf**v

)iivoice*

00

THIS IS A PROFESSIONAL SERVICE

^ J3Lji\lDAt:'-LJLbGG fc* CJUTCHANY LID.


PETKOUUH L J II] Tt:. J)F. w, nrm now160 MllMfLt OK, 41 H r LO UK

Tuvoic^J 101

UatoJ MovofcUer 12r

t Hot 112-1072

J J) 7 A n a l ve w* of Si lv'12 I'll l tf Jl V ft V* t til l .'ut'di t

•J '^ An 41 y* w tt o f' Oui'py rl'2 fiMfrlufci'fc el HlcKi*!

• t. l, VOvi O * VO*l OtVOtt 0,90

27V*30 3X, BO 37 )8037,80

I-?'1 *iiij*Jvwei wl' Ai-itMii' •J* 23477.7 1/.

117 Swl i UMut CKUSHrPUU'EKIZC

Sub lo l s? l*l 2175

Total

118 ( 2f 118,29 11B i 29

H3V2.VV

THfS (S A PROFESSIONAL SERVICEniiP u/uPM

BDNOA1( /CLEGG Su LJLJh("PANY LID.

ELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455

InvoKtft

CAHAU1AH OCCII'E.HTAl f'ETROLEUli 11 MI IE f*

l ,W, CUTTINGS ISO ATIHEU TiRi '1TH FLOOF'

3f J 902

Wot

1 'T'' of Ool'J - Fire A .00 PR.** .00

Total

THIS IS A PROFESSIONAL SERVICEtlJLJCh.1

CDIX3RAN "Y LTD ,H- Ja


101 -12ViiH ULTJDkMlHt

f.H, UMTlfUfb ' 1*0 ill l DI tt UK,

11 H H.UMK

OS* 19fe?;2

HtM'tM l Mo l 112

PruJwtfit fcftlllJV

J!'.1 td Uul'J ~ M rf At-'., v l. u l w t

*i 6.00660 . 00 6^.0 ,

lift 4 l

THfS IS A PROFESSIONAL SERVICE Af!f;nnMT.Q mie VA/UCKJ

Ministryof GeotechnicalSees Report

Ontario Approval

File

Mining Lands Comments

MC ((.f t (i -"'.r'

To: Geophysics

Comments

l | Approved | | Wish to see again with correctionsDate Signature

To: Geology - Expenditures A'ff,Comments

Dj Approved [ | Wish to see again with corrections

one t

Tim W ?I ' 3Signature

To: Geochemistry

Comments

[^Approved Q Wish to see again with correctionsDate Signature

To: Mining Lands Section, Room 6462, Whitney Block. (Tel: 5-1380)

1593 (81/10)

August 4, 1803 2.5336

Canadian Occidental Petroleum United 180 Attwell Drive, 4th Floor Rexdale, Ontario H9U 6A9Attention: Fred GUtlngs

Dear Sirs:RE: Data submitted for Assaying and Sampling credits

on Mining Claims KRL 614681 1n the Area of Rahill Lake.

Returned herein are two geological plans (1n duplicate) lor the above mentioned survey. Please sign all copies of the maps.

Also, please submit signed receipts or cancelled cheques (1n duplicate) as verification of expenditures claimed.

When submitting this Information, please quote File No.2.5336.

For further Information please contact Mr. F.W. Matthews at 416/965-1380.

Yours very truly,



S. Hurst:sc

Ends:cc: Mining Recorder

Red Lake, Ontario

10019830204 2.5336

Mining RecorderMinistry of Natural ResourcesOntario Government BuildingBox 324Red Lake, OntarioPOV 2MO

Dear Sir:

We have received data for Assaying and Sampling Credits submitted under Section 77(19) of the Mining Act R.S.O. 1980 for Mining Claims KRL 614681 et al 1n the Area of Rahill Lake.

This material will be examined and assessed and a statement of assessment work credits will be Issued.Yours very truly,



DU: se

cc: Canadian Occidental Petroleum Limited Rexdale, Ontario

Assessment Work Breakdown

f/irri Days arc based on eight (8) hour Techmcal or Line-cutting days. Technical days include work performed by consultants, draftsmen, etc..

Geological and Geocjiemical ReportL

r ••~"""""| f-'—i - f—————i r- L...4..__l X LZJ ~ L .28__l * L

1 (.cS-.ic Days

Ttc^r^Crt' Days Line- cutting C'td.ts D?yi Tote 1 Credits

No. o) Cis irm

Days per- r 14

^"ic-al D?ys C.-ec-i is

Line-cuttingDpys Totalcivil x IID * E

r::::Da yshnical Days Credits

Line-cutlinp Days

x CUD

No. ofClaims

_

Days per C'eim

No. of DP.vs per Claims C'aim

Techr.lcal t.-^.'rcsl Deys

IV I'D x H^ i:;;::;]Line-culting

Days Total CreditsNo. of Claims

Days per C.a'm

- czi

t^J J'—— -ri'-———'

S3NIW

O3)isnwsawn y

l^r ^^^ca^L^^0^of Work ~*--v*-*^^j ,-'- '.-''J"- C S.

Instructions — Supply required date on a separate form for each type o' work u be recorded (see table below).Fei- GecMsthr.ir.;. 1 nn-r us* 'o-m no. "36? "Report of Work (Geolop.c* 1 Gf c .physics', Geoci-.emicBl and Expenditures)".

Canadian Occidental Petroleum Ltd,180 Attvell Drive, 4th Floor, Rexdale, Ontario M9VJ 6A9 i-~ —— ..-.....--- . —-_..--___ ,,- __ --... -_ _._,___._ ..,™.--—._________Sumniary di IVo'k F'erio: rr.ance fcnd Distr iS.iution of Credits

; Prosriecio' s Licence No.

. -T6 4 4 . . . ...

Requited Infoirnation eg: type of equipment, Names, Addresses, etc. (See Table below)

Tele 1 Work Days C '. r :s rned

12

*-.c -K. :C'.f-:k or. f only)

Q f.'aruEi Work

other L felt ' s \\'C*r k

[^Ccm.f.r fir.;-:: Air, o 1 , herF'cnvf cinttT or r 1 -t : Li- rncf f ::L' ip-

L J DioriiDrio c.' ether Core drilling

M:nir.p ClaimF'l f f i > i K' j rnt .fr

i

KRL ' 614681

614682i

Work DE ys. C'.

6

. 6 . ..

-- — --

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Work Performed on Claims: KRL 614683 -^.G.^. c

KRL 614680 — ̂,. SKr . -̂ C, .rquipment: l Atlas Copco Plugger

l hocker Plugcer

Men: Fred Gittings ) Canadian Occidental Petroleum Ltd.Mike Henrick ) 180 Attv.'ell Drive, 4th FloorArt Murdy ) Rexdale, Ontario M9W 6A9

^ RECElVtU

1 6 IQfi?

MINING LANDS SECTION

John Allard, John Street, Espanola, Ontario

Date: 9 hours on October 10/82

1A-^ x A ^ul"b"iT\T"" l

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Certification Verifying Rt-|.)Oit of Workl htreby ct-rtif^ tritl i h;; ve c f e -t. c-rife! end intiniaU Kno-.vlt'Cipe of the "f 6 cis s e-1 forth in the Rtpyrt o"f \Vork a nnexed hereto, h aving p e'"f orrned thf- wor or vv i t n e:-. E. e. d sa-Tit1 ouririp s^sd/or t f K" ilb conip'eiior, and the annexed report i s true.

't-."iE fcrid PC-RI&! AddrpE.t of Person CeMtlytripFred Gittj--- "i sn Rtt- Drive, 4th Floor, Rexdale, Ontario M9W 6A9id b y ( Sipr,

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Attachments

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KRL 614679 j KRL6J4680

SAN-Z-T1

SAN-Z-T2-8

RED L A K ':f;.!NIS'o DiV.El K CP P ~ '

FOV 101382A.M.

K O Z

CANADIAN OCCIDENTAL PETROLEUM LTD. Minerols Division

PROJECT SANDY ZAHAVY CLAIM GROUPNorth Western Ontario N.T.S. 53 F2

I982 TRENCH LOCATIONSSCALE- );5000

FWG/gv/Nov. I982

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Canadian Occidental Petroleum Ltd.

January 7, 1983

Mr . Fred Matthews Mining Administrator Ministry of Natural Resources Mining Land Section Whitney Block, Room 6452 Queen's Park Toronto , Ontario M7A 1A2

1 f) ^983

,^ r INNING LANDS

Dear Mr. Matthews:

Please find enclosed duplicate copies of geology and geochemical reports for five separate claim groups in the Sandy Lake area (Sandy A, B, C West, C East and Zahavy).

Attached to each set of reports is a copy of the report of work forms sent to Scott Rivett, Mining Recorder in Red Lake, Along with report of work forms I have included a breakdown of costs for each claim block and proof of payment for the lapidary and petrographic work. Repeated requests to Bondar-Clegg for a statement of payment has failed to generate one, although they have promised a statement in the mail. In lieu of this statement I have used a copy of the original invoices.

I hope this will suffice. If there are any problems please call me immediately.

Yours truly,


RJErer

Enclosures

Via McLean Courier

R. J. Evans Administration Manager

Minerals Division — 1BO Attwell Drive, 4th Floor, Rexdale, Ontario M9W 6A9 [41 B] 675-2312 Telex O6-9B9493

SANDY 'ZAHAVY' CLAIMS

STATEMENT OF EXPENDITURES

Petrology: Dr. Boutcher $ 120.00Geoplastech 50.00 (invoice 204)

Thin sectioning: Geoplastech 86.22

Analyses: Bondar-Clegg Ltd.40 Ag, As, Au 556.00

TOTAL EXPENDITURES S 8 12.22

Natural Resources

f W,' k,^r -31-f O f Instructions Supply itiqunt-ci detff on a separate form for t ncti

type of work to be recorded (see table below). 1 ' For Geo-iechnita' work use form no. 13G?"Rfpon

of Work (Geological. Geophysical, Geochtrrrncai ond Expenditures)".

180 Attwell Drive, 4th Floor, Rexdale, Ontario M9W 6A9Summary of Work Performance and Distribution of Qea'itsTotal Work Days C', claimed

121or Performance of the following

[ J Manual Work

QShaft Sinking Drifting orother Lateral Work.

[2 Compressed Air, otherPower driven or mechanical equip.

[ _ |PoAer Stripping

J _ | Diamond or other Core drilling

[ _ J Land Survey

NPrefix

LKBL...

lining ClaimNumber

6146816.14682

WorkDays Cr.

6-6.. .

r.Prefix

ining ClaimNumber

WorkDays Cr,

r.Prefix

lining ClaimNumber

,

W or rDays Cr.

Required Information eg: type of equipment, Names, Addiesses, etc. (See Table below)

Work Performed on Claims: KRL 614683

KRL 614680 Equipment: l Atlas Copco Plugger

-q . G G CW/.S

Men: Fred Gittings ) Canadian Occidental Petroleum Ltd.Mike Henrick ) 180 Attwell Drive,Art Murdy ) Rexdale

John Allard, John Street

Date: 9 hours on October 10/82a fi v A i^ ,i^fVct** A Hr k^vAvN i -^ . 1 ^ ^......—— - f^) Jflti—— r,. ————— ,..., —— \ d. CT.C**1

•^ i

4th Floor, Ontario M9W 6A9

, Espanola,ifFrT'T*

;.'.ijj!NG r.r|"x r. r it ( i [v L: (u L M

Ontario l

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A.M. l"" ^^ . 1?|8i9'lOiJl.!9. j.

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j6ete "oT'Rep'brt

Nov. 4/82R-

__ . __ _ . . ———— —'jT^Tr^ t A K Ev "'i*' c ;V; f r*-'..^..V,-'^ J

1 - ^ L * 1 1

' - i - i ' -' ' O ',0 10-11 i- - ' "

A

Ê corde6 Ho!rier*6r Âpeni jE ^niu.ft)

-vuf UJ Jbt/Jox"l tiereby certify that l have t personal and intimate knowledge of the facts set forth in me Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.

Name end Postal Address of Person CertifyingFred Gittings, 180 Attwell Drive, 4th Floor, Rexdale, Ontario M9W 6A9

Date Certified

Nov. 4/82(Signature)

Table of Information/Attachments Required by the Mining Recorder

Type of Work Specific information per type Other information (Common to 2 or more Types) Attachments

l.'onua! Work

Stiaft Sinking, Drifting or O'.r.fcr Lbttral Vôrk

NilNames and addresses of men who performed manual work/opereied equipment, together with cates and hours of employment.

Coi-.prcivtrf t'.r, o'her power C'uen or n i; '.tnicd! equip.

Type of equipment

Fo.'.er SlippingTyf'e of equipment ancf amount expencêcf. Note: Pioof of actual COM mutt be submitted

Work Sketch: tKtse are required 10 ^^.c>^^ the locetior, a r. o txttnl of work in relation to the neatest clfc'iro pt)S\.

CANADIAN OCCIDENTAL PETROLEUM LTD. Minerals DivisionPROJECT SANDY ZAHAVY CLAIM GROUPNorth Western Ontario N.T.S. 53 F2

1982 TRENCH LOCATIONSSCALE- 1'5000

Sw rf!

^ St. Germain Street, Winnipeg,

Mani toba R2M 4N3

20^-255-17^1 December 30th 1982

To Whom It May Concern -

This is to certify that, during the fall of 1982, I produced petrographic descriptions of 16 rock samples from the Horseshoe claim property and ^-9 rock samples from the Sandy claim property. These were delivered to Canadian Occidental Petroleum Ltd., Minerals Division. I received payment of $320,00 for the Horseshoe reports i and $980.00 for the Sandy reports, from Canadian Occidental Petroleum Ltd.

Sheila M.A. Boutcher Ph.D.

SHEILA M.A. BOUTCHER, Ph.D. Petrologist

Phone:(204)255-174134 St. Germain Street,

Winnipeg, ManitobaR2M 4N3

ins.

COPY

212 King St. West Suite 100 Toronto, Ontario M5H 1K6 596-0381/82

INVOICENo. 1 72Terms:Payable upon receipt

SERVICES RENDERED TO:Canadian Occidental Petroleum Limited 4th Floor 180 Attwell Drive Rexdale, Ontario

.'tsr.v-r^i ,','i.-r i -.i--:--'tv^'^^.-.4--^.-^: .•v-: ;; :.:.- ;,'v-vi;^i;::':;v/

'^'^tft^VJf --55^-:*?,--••V 'iiXli'^V''-'-''-.'-'':-.';

f^ Date: Nov 19/82- ,.' : Quan.

;tfr; Ordered

fi "

p 2

H 46Ipi

^

H|lg] ————

Shipped Via:Description

Your Order No.: Gittings J

thin sections (could not section 82-SAN-2086)

polished thin sections

minimum charge cuts

shipping to Dr.

8MM paid to ^ Geoplastech Inc.

^jJJjoujtcher . St. Vital Man.

fvtn, Ckd. By ____ . ————— 1

p. ,'- rM. r-- - _ 1

1.-'.

receivfr -' 0 V S t i r' ' A' 1 '^' J

' ———— . (^\J^\ red with thanks. KJv \———— \

Total

Quan. Shipped

52

2

54

Unit Price

7.75

18.00

2.00

tAmount (

iftP

403.00 f L

36.00 Ii

96.00 i

112.85 t

1

S547.85

1

COPY

212 King St. West Suite 100 Toronto, Ontario M5H 1K5 596-0381/82

INVOICENo. 204Terms:Payable upon receipt

'^•^•,:'',-''^'':'^^SERVICES RENDERED TO

Canadian Occidental Petroleum Limited 4th floor - 180 Attwell Drive Rexdale, Ontario

•-f.' 1-.-'

-/•v^:- ;s-;-^.i-. - f. i'.'^Vi ̂ ,i ^•^••^•'^3

• r -^-^;s^Â:;^#:^'' -' .1. V-'' '̂ - v *-,-r*4h'.- *.',- s .- "-v: i rT** , -^*î-- ,^

i's;-.": 'SJ/r Jî^î-.w.--*

^ D ate: Jan 3/ 83Ouan.

;. Ordered

3

J 24i

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Shipped Via:Description

Your Order No.: Sittings ^

polished thin section interpretations

im nairl to Rpnnlastprh Inr.

—

Exfn. Ckd. By

Rec'g. Ckd. D-—— D AT r: — Rr;c'D. ——

JAN -5 1983* -

PfiEEi ft Terms Ghd. ryj ..^^^ -

W* to P-.&. AWM.

rprp-iupri with thanlcc /îTotal

Ouan. Shipped

2

2

Unit Price

50.00

Amount'f'. '.' '

100.00

Sioo.oo——————————

K T"'•;C"'.,

V- '': '

lifi-?vV;

1:'?'l *v, ^l

Vf??

BONDAR-CLEGG S. COMPANY LTD.


CANADIAN OCCIDENTAL PETROLEUM LIMITEDF.w, SITTINGS180 'ATTWELL DR.4TH FLOORREXDALEf ONTARIO,H9W 6A9

Invoice:

Patei Moveu.ber lOr 1982

Report Not 112-1630

Pi-oJectJ SANDY ROCKSi ^ c ^,-^Uc.

281 Analyses of Gold - Fire Astaw &1 Subtotal

281 An*lwtt6fc of Arfc&nic m i

Invoice? Total.

of Subtotal

6.00 1686.00 1A86.00 1686.00

913,23

THIS IS A PROFESSIONAL SERVICE ACCOUNTS DUE WHEN RENDERED

BQNDAR-CLEGG S COMPANY LTD.BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: Q53-4455

CANADIAN OCCIDENTAL PETROLEUM LIMITEDP.W* CUTTINGS180 ATTUELL DR,4TH FLUORRfc'XDALEi ONTARIO iM9W AA?

Invoice} 101430

Date} November 05* 1982

Report No J U2-1830

P coJoe t J SANDY ROCKS)

28132363623

281

Art*? 1 wiitffcAnalysesAn* lute*Analv&esAna? lyses

Le PreporSamples

of Silverof Cobaltof Copperof Nickelof Zinc -iBut' total

, iat ionof CRUSHfPULVERIZE -200Subtotal

Invoice Total

atatatsteft

oft

10000

2

,vo.90t 90.90,90

,75

S3328323220

A4t*

772772

,90.80*40,40.70.20

.73,7S

648,20

772*73

11420,95

THIS IS A PROFESSIONAL SERVICE ACCOUNTS DUE WHEN RENDERED

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rROCK GEOCHEMISTRY PROFILES

i Ag As Au . ppm ppm ppb

i ; "JO -i "lOOO -, 500-1

7 -

4 -

3 -

900 -

600 -

700 -

600 -

500 -

400 -

300 ~

EOO-

100 -

O O J

400-

300-

200-

100 -

MAGNETIC SUSCEPTIBILITY PROFILE;

"310 cgs units

SAMPLE NUMBERSCO Nl l

QUARTZ FELDSPAR PORPHYRY

SAN 82-Z-T1

FWO/sa/Nov. 1082

eio

i L12GENDl , ' l r l . : - -

It* i Iron formationpo ; pyrrhotitePY ; pyrite \cp i chalcopyriteqv : quartz vein

Outline of outcrop in trench

Told with plunge direction 4* -t- Anticlinal* Synclinal axis " i^ with plunge direction

Bedding (vertical, inclined showing dip)

S ̂ Schistosity (vertical, r Y inclined showing dip)

*w Shear Zone

Geological Contact f i (defined, assumed)

CANADIAN OCCIDENTAL PETROLEUM LTD minerals division

l PROJECT SANDYZahavy Option

! North Western Ontario N.T.S. 53 F/2

ROCK GEOCHEMISTRY PROFILES

Ag As ppm

10 i 1000 -i 500 -

MAGNETIC SUSCEPTIBILITY PROFILE

•PH*3

10 cgs units

SAMPLE NUMBERS s 8 eo o o o o

(RONFORMATION

SANQY

LAKE:Quartz-calcite

veinlels in PHYLLITE with minor Iron Formation

AMPHIBOLITE

Grab Sample 4039 Au - 60 ppb Ag-O.lppm As - 51 ppm

3cm wide py rich bedfractured Iron Format ion

Grab Sample 4040 Au-15ppb Ag-O.I ppm As- 10 ppm

IFpopy cp qv

i

S*9 X/

y?r /

'j LEGEND

Iron Formationpyrrhotitepyritechalcopyritequartz vein

Outline of outcrop in trench

Fold with plunge direction Anticlinal, Synclinal axis with plunge direction

Bedding (vertical, inclined showing dip)

Schistosity (vertical , inclined showing dip)

shear Zone

l Geological Contact j (defined, assumed)


{minerals division PROJECT SANDYi Zahavy Option

North Western OntarioN.T.S. 53 F/2i

SAN 82-Z-T2

cale 1:

50 100 15pm

PLAN 2 FWG/sa/Nov. 1 982

010 canadian occidental petroleum ltd. geology and geochemistry · 2017-01-17 · 010 canadian...

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