CANADIAN OCCIDENTAL PETROLEUM LTD.

MINERALS DIVISION

GEOLOGY AND GEOCHEMISTRY

OF THE

SANDY 'B' CLAIM TRENCHES

SANDY LAKE BELT

NORTHWESTERN ONTARIO

14 MINING CLAIMS

NO. KRL 561276-561289

CLAIM SHEET M3017 - KAKAPTAM LAKE

BY:

F.W. GITTINGS, HON. B.Se.

COVERING WORK COMPLETED DURING OCTOBER 1 982

010

TABLE OF CONTENTS PAGE

l. SUMMARY AND RECOMMENDATIONS

2. INTRODUCTION.. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . l2.1 Location and Access.......................... 32.2 Previous Work................................ 5

3. WORK COMPLETED 19823.1 Trenching.................................... 53.2 Sampling and Analyses........................ 53.3 Petrography.................................. 63.4 Magnetic Susceptibility Survey............... 6

4. GEOLOGY.......................................... 74.1 General Geology.............................. 74.2 Geology of the Sandy 'B' Claims.............. 84.3 Geology of the Trenchs....................... 9

4.3.1 Trench SAN-82-B-Tl.................... 94.3.2 Trench SAN-82-B-T2a and T2b........... 104.3.3 Trench SAN-82-B-T3.................... 114.3.4 Trench SAN-82-B-T4..............,..... 12

4.4 Rock Geochemistry........................... 13

5. CONCLUSIONS....................................,. 14

6. REFERENCES................... . . ..... . . . . . . . . . . . . . 15

LIST OF TABLES

Table l Analyses on Sandy 'B 1 Rocks................. 62 Table of Rock Units......................... 9

LIST OF FIGURES

Figure l Index Map..............................,.... 22 Location of Sandy Claims.................... 4

APPENDICES

Appendix I Analytical Results........................ 16II Thin Section Descriptions................. 22

III List of Personnel......................... 43

PLANS (In Back Pocket)

Plan l Geology of the Sandy 'B' Claims2 Geology, Geochemistry and Magnetic Susceptibility

Trench SAN-82-B-Tl3 Geology, Geochemistry and Magnetic Susceptibility

Trench SAN-82-B-T2a4 Geology, Geochemistry and Magnetic Susceptibility

Trench SAN-82-B-T2b5 Geology, Geochemistry and Magnetic Susceptibility

Trench SAN-82-B-T36 Geology, Geochemistry and Magnetic Susceptibility

Trench SAN-82-B-T4

- l -

l. SUMMARY AND RECOMMENDATIONS

Five trenches totalling 44.0 m in length were

blasted out across gold occurrences located during Canadian

Occidental's 1981 summer program in the Sandy Lake Belt.

The rocks exposed in the trenches include:

metasediments including iron formation, intrusives of rhyolite

and dacite composition and quartz veins. Gold occurrences

appear to be related to narrow shear zones or in quartz veins.

The trenches were chip sampled at a 0.25 m interval.

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

of the 170 samples collected contained 500 ppb Au. Generally

the results were disappointing.

Due to budgetary cutbacks and the low potential for

gold mineralization on these claims it is recommended that no

further work be done and the claims allowed to lapse.

2. INTRODUCTION

The Sandy 'B 1 Claims are one of a group of claim

blocks staked in 1981 to cover known areas of iron formation

outcrop on the Sandy Lake Greenstone Belt. All 14 claims in

the group are contiguous and are presently held by Canadian

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

Rexdale, Ontario, M9W 6A9.

Five trenches were blasted out across areas where-

high gold values were discovered during the 1981 Canadian

Occidental field mapping program in the Sand Lake Belt. The

purpose of the trenches was to investigate the areas potential

for economic gold mineralization.

o^

J Northwestern Ontorio Index Map

LOCATION OF CANAD1ANOXY PROJECTS

SANDY CLAIMS

-SMirlrj^X o^~

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

LegendPaved road

Grovel rood

Town

Indion settlement

- 3 -

This report present the results of the trenching

work and is submitted on behalf of Canadian Occidental

Petroleum Ltd., the holders of the claims.

2.1 Location and Access

The Sandy 'B 1 Claims are located on the north

shore of Sandy Lake 225 km north of Red Lake in northwestern

Ontario (N.T.S. map sheet 53/F/3). The B claims are in the

Red Lake Mining Division of the Patricia Portion of the District

of Kenora (see Figures l and 2).

The native settlement of Sandy Lake is located 12 "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 20 km east of the claims.

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) .

KEY MAPscale : l inch 1o 200 miles

x- MAP AREA

PROJECT SANDY North Western Ontario N.T.S 53 C 8 53 F

LOCATION MAPSeole: 11250,000CANADIAN OCCIDENTAL PETROLEUM lMmerol* Division Nov 82

- 5 -

2.2 Previous Work

During the late 1930's and early 1940's, the Sandy

Lake Greenstone Belt was prospected for gold, however there

are no reported gold occurrences on the Sandy 'B' Claims.

In the summer of 1981, Canadian Occidental carried

out a shoreline mapping program of their Sandy Lake claim groups

including the 'B' claims. The results of this program are

contained in an internal Canadian Occidental report entitled

"Geology and Geochemistry of the Sandy Claims, Sandy Lake Belt,

Northwestern Ontario, March 1982".

3. WORK COMPLETED

3.1 Trenching

Five trenches totalling 44.0 ra 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 5 days

during the period September 30 to October 8, 1982, drilling,

blasting, mucking, mapping and sampling the trenches.

3.2 Sampling and Analyses

A total of 170 channel chip samples were collected.

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

gold, silver and arsenic. One sample from trench B-T3 and all

samples from B-T4 were also analysed for Ni, Cu, Co and Zn.

Two samples have whole rock analyses. 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 2, 3, 4, 5

and 6, and listed by sample number in Appendix I.

- 6 -

TABLE l

Element

Au

As

Ag

Cu

Ni

Co

Zn

ANALYSES ON

Lower Detection Limit

5 ppb

2 ppm

0 . 1 ppm

1 ppm

2 ppm

1 ppm

1 ppm

SANDY 'B'

Extraction

Aqua Regia

ROCKS

Method

Fire Assay AA

Nitric Pet- Colourimetric rochloric Digestion

HN0 3 -HC1 Atomic Absorption hot extr.

d

ti

M

11

Whole Rock Analyses Q.1%

ii

H

H

H

Semi-quantitative

3.3 Petrographic Analysis

No. of Samples

170

170

170

21

21

21

21

A total of 12 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.

3.4 Magnetic Susceptibility Survey

A magnetic susceptibility survey was conducted along

each trench. Readings were taken on 0.25 m interval. The

survey was undertaken to determine the actual magnetic strength

of the various rock types. These observations will be used in

the future by 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.

- 7 -

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 General Geology

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

(Bennettand Riley, Operation Lingman Lake 1969). Data collected

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

modify Satterly's interpretation. As a result, the author has .

relied heavily on the work of Satterly.

"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.

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 90S; of the belt.

The remainder of the belt is felsic to intermediate metavolcanics,

metasediments, and metagabbro" {the above excerpt taken from

Satterly, 1938).

- 8 -

4 .2 Geology of the Sandy 'B* Claims

The Sandy 'B' Claims were mapped by Kevin Leonard

of Canadian Occidental in July 1981. The map produced is

included in this report as Plan l with the location of the

1982 trenches, which have been added.

The three main rock types are mafic metavolcanics,

dacite porphyry and iron formation. Iron formation outcrops

along the north shoreline of Sandy Lake and on the north side

of a small island in the southwestern portion of the claim

group. In the south, the country rocks are hornblende schist

and amphibolite which are part of the mafic metavolcanic sequence,

Along the north shore of Sandy Lake the main country rock is a

dacite porphyry. The dacite porphyry is a grey to green rock

containing many lapilli-sized fragments set in an aphanitic,

massive to faintly foliated matrix; the phenocrysts described

by Satterly (1938, p. 17) are crystal lapilli. The rock is

therefore a dacite tuff, although dacitic flows and sills may

also be present in minor amounts. Iron Formation exposed

generally trends east-west although no dips are shown on the

map, the regional dip appears to be vertical or steeply dipped

to the north as shown by Satterly 1938.

- 9 -

TABLE 2

TABLE OF ROCK UNITS

AGE NAME DESCRIPTION

Archean Iron Formation Alternating bands of quartz anhedraand magnetite giving a corregated appearance on weathered surface. Very fine grained, finely laminated and slightly metamorphosed. Tremolite commonly associated with magnetite rich layers.

Phyllite Green coloured, very fine-grainedfinely laminated with orientated flakes of chlorite, biotite and sericite.

Quartz-feldspar PorphyryLight grey-green colour strongly foliated to massive, with large (0.5 cm) blue quartz phenocrysts which have been elongated in the direction of foliation. K-feldspar and plagioclase phenocrysts are variable in size (up to 4 mm) and density. Rhyolitic composition.

Dacite Porphyry Light grey-green usually massivesimilar to Quartz-feldspar porphyry except it lakes K-feldspar phenocrysts.

4.3 Geology of the Trenches

4.3.1 SAN 82-B-Tl (Plan 2)

Trench B-Tl was blasted across an outcrop of iron

formation. A grab sample collected in 1981, from this outcrop

contains 350 ppb gold (see Plan 1). The trench is 12.5 m in

length with a 2 m wide break in the middle where the outcrop

was at water level and blast holes could not be drilled.

The iron formation exposed in the trench was regularly

banded with thin -^O.S cm laminae of magnetite and white sugary

textured quartzite. The iron formation is vertically dipping

and strikes consistently northwest-southeast. A thin section

(82-SAN-1014) cut from a sample of iron formation collected at

- 10 -

3.5 m was described by Dr. Boutcher as a finely laminated

tremolite-bearing quartzite, with magnetite-rich bands (refer

to Appendix II for a full description).

A quartz-feldspar porphyry intrusive occurs from

6.5 to 7.5 m in the trench. This dyke is dioritic in composition

and has blue quartz phenocrysts which are characteristic of this

felsic rock type. From 6.5 to 7.0 m the dyke has been strongly

sheared and was mapped in the field as a phyllite (see Plan 2).

A rusty quartz vein occurs along the contact between the iron

formation and the phyllite.

The highest gold values are contained in the iron

formation. None of the values approach economic levels. The

highest gold value is 310 ppb. There appears to be a depletion

halo surrounding the porphyry dyke. The significance of this

depletion halo is not known.

4.3.2 Trench SAN 82-B-T2a and T2b {Plans 3 and 4)

The purpose of these two trenches was to enable a

systematic sampling and investigation of the iron formation for

its gold potential.

The iron formation exposed in these trenches is quite

similar to the iron formation in SAN 82-B-Tl except that it does

not contain any anomalous gold values (its highest gold value is

15 ppb). The iron formation consists of regularly interbedded

magnetite and quartz laminae and is well reflected by the magnetic

susceptibility profile (see Plan 3). The magnetite rich laminae

are up to l cm thick.. Tremolite rich zones are present along

the boundary between the quartz and magnetite layers (refer to

-li

the petrographic analyses of sample 82-SAN-1068 in Appendix II

for a complete description).

The iron formation metasediments are interbedded with

chloritic phyllite. These metasediments are vertically dipping

in the southern sector of trench 2a and become northerly dipping

from 5.0 m in trench 2a and in trench 2b.

Contacts between the metasediments and the quartz-

feldspar intrusives is sharp. The dominant phenocryst in the

porphyry is K-feldspar and the rock is rhyolitic in composition.

The porphyry in trench Tl lacked K-feldspar and is dioritic in

composition. In addition, Dr. Boutcher observed remnant

spherulitic texture in sample 82-SAN-1043 from trench B-T2a (see

Appendix II).

The gold, silver and arsenic levels in the trenches is

very low indicating a very low potential for iron formation hosted

gold deposits in the area of the trenches.

4.3.3 Trench SAN 82-B-T3 (Plan 5)

Trench B-T3 was blasted in the area where, in 1981, a

grab sample collected in a gossanous shear zone ran 40 ppb gold.

The sample (67288) was reportedly collected from a shear zone in

dacite porphyry near the western boundary of the claim groups (see

Plan 1).

The stripping and trenching revealed a dacite porphyry

(quartz-feldspar porphyry) in contact with a very thinly banded

and strongly folded iron formation (see Plan 5). Massive pyrite

horizons occur at two places in the trench. The first is along

the contact between the porphyry and the iron formation; the

second is as a 2 to 10 cm wide layer within the iron formation

- 12 -

(see Plan 5) .

The quartz-feldspar porphyry which was mapped in the

field as a dacite porphyry when examined in thin section appears

to be a rhyolite porphyry with quartz, K-feldspar and plagioclase

phenocrysts (see 82-SAN-1119 in Appendix II).

The highest gold value of 350 ppb is contained in a

sample of iron formation. This lone high value is more a

reflection of erratic nature of gold distribution rather than any

unique characteristics of the sample. The surrounding iron

formation does not contain detectable amounts of gold.

The iron formation is described by Dr. Boutcher as a

slightly metamorphosed, magnetite-rich, banded iron formation with

well developed secondary cleavage at a moderate angle to the

bedding. The thin section also includes a band composed

predominantly of tremolite (see 82-SAN-1133 in Appendix II).

4.3.4 Trench SAN 82-B-T4 (Plan 6)

The purpose of this trench was to investigate the

potential of a pyritiferous shear zone which when sampled in 1981,

yielded a value of 1200 ppb Au and 18.0 ppm Ag.

The trench exposed a series of quartz veins in dacite

porphyry close to its contact with chlorite phyllite (see Plan 6).

Three samples 1162, 1163 and 1164 contain anomalous

concentrations of copper, silver and gold. Averaged over the

1.5 m combined width of the three samples, the quartz veins

contain: gold -0.01 oz/ton; silver -0.57 oz/ton and copper -

J.,07%.

The area around this trench should be examined for

evidence of a quartz stockwork associated with the porphyry-phyllite

contact exposed in the trench.

- 13 -

4.4 Rock Geochemistry

All five trenches were sampled continuously at a 0.25 m

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

In trench B-Tl, there appears to be a gold depletion

halo around the dacite porphyry which intrudes the iron formation.

When compared with the other iron formations sampled on the 'B 1

claims however, the iron formation in trench B-Tl appear generally

enriched except for the area immediately surrounded the sheared

intrusive. The significance of this depletion/enrichment pattern

of gold is not known. There is no direct relationship between

anomalous gold values and silver or arsenic in B-Tl or in fact in

any of the iron formation sampled.

Trenches B-T2a and B-T2b are similar in geology to B-Tl

but the gold, silver and arsenic levels are consistantly low.

Trench B-T3 contains one anomalous gold sample. This

sample contains 350 ppb gold, 1.5 ppm silver and 6 ppm As. No

reason for this single sample rock geochemical anomaly can be

found. The iron formation which hosts this sample appear uniform

throughout the trench.

Whole rock analyses were done on two samples of iron

formation from trench B-T-3. The iron content of the two samples

averaged 45.5%, expressed as Fe 2 0 3 . The Ti0 2 content was Q.05% and

the Si0 2 content averaged 52.8 s! (see Appendix I for full results).

Overall the geochemical results from the iron formation

were disappointingly low, indicating a low potential for a high

tonnage iron formation hosted gold deposit on the 'B 1 Claims.

- 14 -

5. CONCLUSIONS

The Sandy 'B 1 claims where investigated offer a low

potential for iron formation related gold deposits.

The iron formation is dominantly oxide facies and

slightly metamorphosed. It is relatively undisturbed structurally

which may account for the lack of gold concentration associated

with it. In thin section, the rock is composed of magnetite-rich

and quartz-rich laminae. Tremolite is commonly associated with

the magnetite.

Arsenic does not appear to be a good pathfinder element

for gold in this area; there was no direct correlation between

high arsenic and high gold values.

Of the five trenches only B-T4 contains significantD??ls

gold and silver values (0.01 oz/ton Au and \s#i oz/ton Ag over

1.5 m). These values however were not associated with iron formation

but were obtained from quartz veins associated with an intrusive-

metasedimentary contact.

Respectfully submitted,

Toronto, Ontario

December 1982

F.W. Gittings, Hon. - B.Se,

- 15 -

6. REFERENCES

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.

- 16 -

APPENDIX I

ANALYTICAL RESULTS

- 17 -1

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l REPORT: 112-1795 PROJECT: SANDY ROCKS 1 i

SAMPLE ELEMENTL. JMffiER....... UNITS

SAN-B-1001SAN-B-1002

i

! i

ii

i

i

SAN-B-1003SAN-B-1004

. JANrB-1005 m..

SAN-B-1006SAN-B-1007SAN-B-1008SAN-8-1009SAN-B-1010

A3...FWL-.

0.1O.lO.lO.l

O.l0,1O.lO.lO.l

AsJWL.....

tttttttt tt

22242

Au ut/Au NOTES..PPB.......... CM. ......,............

3030302060

10011030^tf

SAMPLE ELEMENTNUMBER UNITS

SAN-B-1041SAN-B-1042EAN-B-1043SAN-B-1044 SAN-B-1045

SAN-B-1046SAN-B-1047SAN-B-1048SAN-B-1049SAN-B-1050

MPPH

O,lO,lO,lO,l O.l

O.lOil0.1O.lO.l

R-ii'.'.x J

PAGE

AsPPM

354

tt

tt2

tttttt

Geochemical Lab Report

l

Au wt/Au NOTESPPB GH

305160

10

S

G^^O5

SAN-B-1011 SAN-B-1012SAN-B-1013

^ttN-B-1014 ^PtN-B-101S

SAN-B-1016SAN-B-1017SAN-B-1018SAN-B-1019SAN-B-1020

SAN-B-1021SAN-B-1022SAN-B-1023SAN-B-1024SAN-B-1025

SAN-B-10261 SAN-B-1027

SAN-B-1028SAN-B-1029SAN-B-1030

O.l

O.lS',i

0.1O.lO.l

0,10,2

0,7O.lOilO.l

0,1

0,1O.lO.lO.lOil

tttttt tt

2tt225

2tttttt

2

tt4

tt22

<5 <5<5

<5

tf<5<5

5<5

^<5<5<5<5

K5K5<5^<5

SAN-B-1051 SAN-B-1052SAN-B-10536AN-B-1054 SAN-B-1055

SAN-B-1056SAN-B-1057SAN-B-1058SAN-B-1059SAN-B-1060

SAN-B-1061SAN-B-1062SAN-B-1063SAN-B-1064SAN-B-1065

SAN-B-1066SAN-B-1067SAN-B-1068SAN-B-1069SAN-B-1070

0,10,1

0,1O.l0,1

O.lO.lO.lO.1O.l

O.l0,10,10,10,1

0,10,1O.l0,10,1

tttttt tt

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i.

2tt622

S^

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tf^^^G

tf^^^G

tf^<5^<5

SAN-B-1031SAN-B-1032SAN-B-1033SAN-B-1034SAN-B-1035

0,1O.lO.l0.1O.l

22

904tt

tf15604070

BAN-B-1071SAN-B-1072SAN-B-1073SAN-B-1074SAN-B-1075

0,10,1O.lO.l0.1

2tttt2tt

^<5<5^<5

.^^^k.

AN-B-1036SAN-B-1037SAN-B-1038SAN-B-1039SAN-B-1040

O.l0,1O.l0,10,1

22242

7595

310110253

SAN-B-1076SAN-B-1077SAN-B-107BSAN-B-1079SAN-B-10BO

0.1O.l0.10,10.1

tttttttttt

<5^<5^5

- IR -

IH.

164 Btlfut n. Onurio

: 0954455

BDNDABrJCLB3B

REPORT; 112-1795 PROJECT: SANDY ROCKS cz PAGE 2

SAMPLE ELEMENT A3 JiUHBER.- ......UNITS...,. EPH-.

SAN-B-1081 O.ISAN-B-1082 O.ISAN-B-1083 O.ISAN-B-1084 O.ISAN-B-1085 O.I

SAN-B-1086 O.ISAN-B-1087 O.ISAN-B-1088 O.ISAN-B-1089 O.ISAN-B-1090 O.I

SAN-B-1091 O.ISAN-B-1092 O.lSAN-B-1093 O.I

N-B-1094 O.IN-B-1095 O.I

SAN-B-1096 O.ISAN-B-1097 O.ISAN-B-1098 O.ISAN-B-1099 O.ISAN-B-1100 O.I

SAN-B-1101 O.lSAN-B-1102 O.lSAN-B-1103 O.lSAN-B-1104 O.lSAN-B-1105 O.l

SAN-B-1106 O.lSAN-B-1107 O.lSAN-B-1108 O.lSAN-B-1109 O.lSAN-B-UIO O.l

AsPPH

<2<2<2<2<2

<2222^

tfV<2<2<2

24454

45V22

42244

Au ut/Au NOTESPPB CM

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REPORT: ii2-ie30 PROJECT; SANHY ROCKS |

SAMPLE ELEMENT NUMBER UNITS

82-SAN-1151 82-8AN-1152 82-SAN-1153 82-SAN-1154 82-SAN-1155

Cu PPM

16 49 23 28

250

Zn PPM

28 37 31 37 36

Ni PPM

7 8 8 7 7

Co PPM

4 4 5 5 5

A3 PPM

0,1

xO.l0,7

As PPM

3 2

3

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Au wt/Au NOTES 1 PPB GM

<5 tf <5

82-SAN-1156 62-SAN-1157 82-SAN-1158 82-SAN-1159 82-SAH-1160

137 1410

491 1470

702

36 85 55 68 25

6 6

12 15

4 4 5

22 9

0,4 3,2 1,4 4,3 2.1

2<520

5

82-SAN-1161 82-SAN-1162 82-SAN-1163OO^CAU^I 1^^ j ^^^ *)Hil i ion

^ S AN- 11 65

445 9080 9970

13180 375

40 187 235 330 35

7 23 25 38 H

6 5

29 162 62

1,2 18,7 18,6 21,5 1.2

3

2

2

s'S

130 500 410

10

82-SAN-1166 82-SAN-1167 82-SAN-1168 82-SAN-1169 82-SAN-1170

82-SAN-2001 82-SAN-2002 82-SAN-2Q03 82-SAN-2004

j 82-SAN-2005

1650 490

85 500 119

65 46 85

104 93

1326 80 73 80

7 26 30 34 31

3,7 0,6 0.1 0,3 0,3

0,1 0,1 0,1 0,1

xO.l

2

6 22

8 12 11

25 <5

<5

<5

^

^

82-SAN-2006 82-SAN-2007 82-SAN-2008 82-SAN-2009 82-SAN-2010 '

0,1 s'O.l (0,1 0,3

(0,1

14 94 25 10

8

<5 <5

<5 <5

82-SAN-2011 82-SAN-2012 82-SAN-2013 82-SAN-2014 82-SAN-2015

-SAN-2016 82-SAN-2017 82-SAN-2018 82-SAN-2019 82-SAN-2020

sO.l

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10 1710 20 48

12 6 6

11 3

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SAMPLE ELEMENT1 .JilflffiER... UNITS .^

82-SAN-113782-SWH141B2-SAN-201282-SAN-205782-SAH-2058 . .

82-SAN-2059' 82-SAN-2060

82-SAN-2062j 82-SAN-2081\ 82-SAM-2105

Si02PCT .

49,5055,1056,8049,10

.48,70 .

49,8050,9049,7053,7049,60

Ti02PCT

0,080,030,020,070,77

0,730,760,790,011,13

A1203PCT

2,180,890,841,41

12,70

12,5013,3012,30

0,2414,30

/•••'••ieiiij

1Fe203l

W..

47,8043,2037,8043,4018,20

14,2015,3019,20 '39,8014,00

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MnOPCT

0,520,460,440,480,26

0,230,250,280,600,22

H30PCT

2,971,934.323,718,52

9,148,649,451,798,08

Cat)PCT

0,481,490,730,788,44

8,809,758,040,378,10

1Ka20

PCT

{0,010,010,030,022.65

1,781,250,94

{0,012,31

K20PCT

0,16{0,010,030,150,69

1,131,210,69

{0,011,78

PAGE

P205PCT

{0,010,180,060,480,09

0.050,100,100,500,17

1

SPCT

0,100,310,070,53

{0,01

0,01{0,01{0,01{0,01{0,01

LOI NOTESPCT

0,050,050,100,903,00

3,301,602,650,100,40

82-SAN-2115B2-SAN-2118

1 82-SAN-3Q01j 82-SAN-3002j 82-SAN-3003

W-SAN-3004 '82-SAN-300582-SAN-3008

t 82-SAN-301382-SAN-3014

45,3045,5044,6046,7042,10

46,8077,8073,9062,1063,60

0,820,990,530,380,41

0,680,040,270,171,75

12,5014,005,724,554,65

7,5213,4014,802,03

14,30

18,0017,2014,5013,1012,40

15,500,792,87

23,8011,20

0,230,220,260,180,17

0,23{0,010,070,530,45

9,109,19

22,6022,7024,30

16,000,461,000,931,59

8,679,66

10,608,545.49

12,300,040,470,562,35

1,642,450,710,080,04

3,100,150,170,141,04

0,190,24

{0,01{0,01

0,05

0,114,294,400,553,59

0,110,100,090,410,25

0,08{0,01{0,01

0,260,52

{0,01{0,01{0,01{0,01{0,01

{0,01{0,01{0,017,950,56

5,351,750,404,207,05

1,851,952,454,252,05

82-SAN-3026 47,90 1,20 13,60 14,80 0,25 8,13 10,80 1,06 0,86 0,22 0,01 0,95

- 22 -

APPENDIX II

THIN SECTION DESCRIPTIONS

- 23 -

Specimen No - 82-SAN-1014

Rock name - finely laminated tremolite-bearing quartzite, with magnetite-rich bands

Mineralogy - very abundant - quartzmoderate amounts - magnetite

tremolitesmall amount - carbonate

Description - This rock is a fine grained quartzite, withmoderate amounts of scattered tremolite crystals, andnumerous fine laminae containing varying proportions of magnetite.Within the thin section overall the proportion of magnetiteis relatively small. However, in the hand specimen there aretwo bands which are very rich in magnetite, on either side of thequartzite portion which is visible in the thin section.

The quartzite is composed of a fine grained mosaic of smooth sided quartz anhedra, with an average grain size of around 0.05 mm. Scattered throughout the quartzose base there is a low proportion of tiny magnetite granules. These are typically compact and less than 0.01 mm in grain size. The lamination of the rock results from the presence of very narrow laminae which contain varying proportions of magnetite, occasional laminae being composed virtually entirely of magnetite. The quartzite also contains a moderate amounts of fairly evenly scattered tremolite, which makes up around 15# of the rock. This tremolite occurs in very long, fine, needle-shaped crystals which are typically oriented at a high angle to the laminae. In addition, a very little carbonate is rather unevenly scattered through the rock in very tiny anhedra.

The thin section includes two minor fractures, oriented at a high angle to the laminae, which offset the laminae slightly. There tends to be a relatively high concentration of tremolite along these fractures. In addition, the thin section contains one narrow, quartz-filled, veinlet which is oriented at right angles to the laminae, but which shows no offsetting of the laminae whatever.

- 24 -

Specimen No. - 82-SAN-1022

Rock name - strongly sheared quartz-feldspar porphyry i now approaching a sericite-chlorite phyllite

Mineralogy - phenocrysts

groundmassabundant

quartz plagioclasequartz )sericite )chlorite )plagioclase )biotite - small amountsmagnetite )apatite ) very small amountszircon )

Description - This rock is a very strongly sheared quartz- feldspar porphyry. Scattered, relatively large, quartz phenocryst remnants and smaller plagioclase phenocryst remnants are set in a very fine grained groundmass with a typically metamorphic texture. This is composed predominantly of a fine mosaic of quartz, with some plagioclase, and abundant streakily distributed sericite and chlorite.

The quartz phenocrysts are the most prominent feature of the rock. They are up to about 6 mm across. The smaller ones are usually strongly strained looking, but retain their identity as a single crystal. The larger ones show varying amounts of breakdown of the original crystal. Some of the larger ones have a clearly embayed character, confirming their original porphyritic nature. The schistosity of the rock flows around these phenocryst remnants. In this particular rock the plagioclase phenocrysts have been relatively strongly affected by the shear. They were probably originally relatively small and moderately abundant. They are now present as shadowy remnants of the original phenocrysts, partly obliterated by abundant inclusions of chlorite and sericite, often with very patchy extinction {probably largely as a result of strain) and often broken up into a number of closely adjacent irregular fragments which have been slightly disoriented with respect to each other. The maximum size was probably around 2 mm. No K-feldspar phenocryst remnants were identified in this rock. The schistosity also flows around the more coherent plagioclase phenocryst remnants s the fragmented ones tend to be drawn out within the plane of the schistosity.

As stated above, the groundmass has a metamorphic looking texture. It is composed of an extremely fine grained mosaic of tiny quartz anhedra, intermingled with some plagioclase,

(continued overleaf)

- 25 -

82-SAN-1Q22 - continued

and containing abundant, very fine grained, sericite and chlorite. The grain size is of the order of 0,02 mm or less, so that it is difficult to determine the relative proportion of quartz to plagioclase, especially as the latter is untwinned. Plagioclase is probably relatively sparse, apart from the recognisable phenocryst remnants. Sericite and chlorite are present in approximately equal proportions, and make up around 1/3 of the groundmass between them. They are rather irregularily and streakily distributed, with sericite predominant in some parts and chlorite in others. Both minerals show a well developed preferred orientation indicating the direction of shear. There are also occasional streaks of relatively dense sericite or chlorite which are sometimes virtually monomineralic. The chloritic streaks sometimes contain scattered, relatively large (up to 0.3 mm) flakes of very fresh looking reddish biotite. This is randomly oriented, and appears to be of very late stage, post-stress, origin. The thin section also contains a very small amount of tiny magnetite grains, usually associated with chlorite. Occasional euhedra of apatite are also present, and reach up to about 0.25 ram across. One small anhedral crystal of zircon was also noted.

- 26 -

Specimen No. - 82-SAN-1024

Rock name - sheared and sericitised quartz-feldspar porphyry

Mineralogy - phenocrysts

groundmass

plagioclase quartzquartz ) plagioclase) abundantsericite

carbonate magnetite biotite apatite

)raoderate amounts

)) very small amounts )

Description - This rock is a fairly strongly sheared quartz- feldspar porphyry. The original rock contained sparse, relatively large, quartz phenocrysts and abundant, somewhat smaller, plagioclase phenocrysts. These were set in a very fine grained, probably predominantly quartzo-feldspathic, groundmass. There may possibly have been very occasional ferromagnesian phenocrysts, now represented by compact lenses of ferromagnesian minerals. The groundmass has now been extensively sericitised, with moderate amounts of scattered carbonate and chlorite. -

The quartz phenocrysts reach up to about 7 mm across, but are quite sparse, only about 5 occurring within the area of the thin section. They are roughly oval to rounded in outline, strongly strained looking, and frequently strongly embayed. No K-feldspar phenocrysts were identified. Plagioclase phenocrysts are, however, very abundant. They reach up to about 3 ram across, range from tabular subhedra to anhedra, and are rather shadowily visible as they are heavily impregnated by finely disseminated secondary minerals. These consist of a mixture of varying proportions of sericite, carbonate and subsidiary chlorite, and generally impregnate the plagioclase crystals quite evenly. The plagioclase base around the secondary minerals often shows rather blotchy extinction patterns, probably at least partly as a result of strain. The thin section contains several compact lenses composed predominantly of relatively coarse grained chlorite, intermingled with occasional flakes of very fresh looking, reddish brown, biotite which are randomly orientated (and were probably of post-stress formation). Tiny granules of magnetite are scattered through these chloritic lenses, along with a low proportion of quartz. The largest clot is about 6 mm long by 1.5 mm wide. It seems likely that these clots may represent a low proportion of relatively small ferromagnesian phenocrysts in the original rock.

The groundmass is very fine grained, and has a streaky and rather indeterminate looking texture. It is composed

(continued overleaf)

- 27 -

82-SAN-1024- - continued

of a rather patchily variable mixture of quartz, sericite and plagioclase with subsidiary amounts of chlorite and carbonate. Owing to the very confused and fine grained nature of the groundmass (less than 0.02 mm grain size) it is difficult to determine relative proportions of quartz and plagioclase. However, quartz appears to be greatly in excess of plagioclase. Sericite is abundant throughout, but somewhat streakily distributed. It probably makes up around 20-25^ of the rock and shows a well developed preferred orientation, curving around the phenocryst remnants. Carbonate is rather unevenly disseminated through the groundmass in irregular anhedra of variable size; patches of relatively coarse carbonate tend to occur adjacent to phenocrysts. Chlorite occurs rather irregularily throughout the groundmass, in moderate amounts, forming compact flakes which are somewhat larger than the associated sericite. A low proportion of very tiny, randomly oriented, very fresh looking, biotite flakes tends to be associated with the chlorite. A low proportion of tiny magnetite grains also tends to be associated with chlorite. Apatite is a noticeable accessory mineral in this rock, forming euhedra and subhedra which are slightly coarser than the associated groundmass minerals.

- 28 -

. - 82 -SAN -l 04-3

Rock name - sheared quartz-feldspar porphyry, with remnants of spherulitic texture

Mineralogy - phenocrysts

groundmass

secondary

K-feldsparquartzspherulitesquartzofeldspathic material biotite - very sparse

pyrite carbonatechlorite garnetsphenezeolitic material

)mainly in fracture

filling fe

Description - This is a quartz-feldspar porphyry, of rhyolitic composition, which has been quite strongly sheared. The rock contains abundant phenocrysts of quartz and K-feldspar , and scattered phenocryst-sized spherulites, surrounded by an extremely fine grained quartzo-feldspathic groundmass. The thin section is cut across by a fracture which contains a variety of different minerals including pyrite, garnet, and zeolitic material.

The original rock was quite abundantly porphyritic. The phenocrysts most probably tended to occur in crystal clusters, as many of them now occur in streaks of sheared looking crystals. The most abundant phenocryst type was K-feldspar, which ranged in size up to about 3 mm and were often euhedral to subhedral in form. The K-feldpar phenocrysts are usually finely perthitic, some show microcline twinning. They have a slightly turbid appearance, and are often speckled by a little carbonate, but are otherwise unaltered. They are now usually quite strongly strained looking and some have been partially fragmented. Quartz phenocrysts are also quite common, of similar size, and sometimes show crystal form. They have been more strongly affected by the strain, and are very strongly strained looking and often broken down into a lensoid patch of highly sutured quartz mosaic. Some crystals show remnants of an embayed structure. This rock also contains numerous remnants of spherulitic structures. These appear to have been relatively large (up to about 2 mm across) and to have occurred both as isolated spherulites and formed around a core which was usually a quartz phenocryst . In some instances the core was also a K-feldspar phenocryst. These spherulites are also quite strongly strained looking in most cases but their basic structure is still clearly visible.

(continued overleaf)

- 29 -

82-SAN-10^-3 - continued

The groundmass in this rock has a somewhat streaky appearance and tends to curve around the phenocrysts and phenocryst clusters. It is composed essentially of an extremely fine grained, rather featureless ( mosaic of quartz and acid feldspar with a finely granulated looking texture. Scattered in very low proportions through this base there are tiny flakes and stringers of biotite and chlorite. A few small clots of chlorite and irregular stringers of carbonate also tend to be scattered through the phenocrysts crystal clots. One or two relatively large anhedra of pyrite are also scattered through the rock.

An irregular fracture i with variable width andvery irregular margins, cuts across the centre of the thin section. This is bordered on each side by a marginal zone of relatively coarse grained, randomly oriented, masses of chlorite. This zone is of very variable width. The centre of the fracture contains a variety of different minerals, which are also relatively coarse grained (up to about 2.5.mm). These include patches of carbonate mosaic, occasional anhedra of sphene and garnet, and masses of zeolitic minerals. The latter tend to be intermingled with the chlorite. The chlorite in this fracture zone is a very bright green variety with a relatively high birefringence.

- 30 -

Specimen^No. - 82-SAN-1054

Rock name - slightly metamorphosed banded iron formation, with tremolite-magnetite and quartzite bands, and some distortion of the laminae by numerous minor fractures

Mineralogy - abundant - tremolitemagnetite quartz

moderate amounts - carbonate small amounts - chlorite

Description - This rock is a banded, magnetite-rich, iron formation. Within the area of the thin section there are two types of bands. One is a fine grained quartzite containing relatively little magnetites the other is relatively rich in magnetite, intermingled with a mixture of tremolite and carbonate and completely lacking quartz. The rock is crossed by a series of minor fractures which are oriented at a fairly low angle to the bedding, and which tend to distort the laminae. In other cases the laminae are merely crenulated.

The quartzite makes up approximately half of the thin section, and is bordered on either side by magnetite-rich bands, The quartzite is composed of a fine grained mosaic of somewhat strained looking sutured quartz anhedra of rather variable grain size. Scattered throughout the quartzose mosaic there is a moderate, but variable, amount of very tiny magnetite granules which are arranged in narrow 'trains' across the thin section, giving a very fine lamination to the quartzite. A low proportion of very long, needle-like, crystals of tremolite is rather unevenly scattered through the quartzite. These often form roughly radiating clots of crystals, and are randomly oriented. The fractures which cut across this portion of the thin section tend to^filled by a mixture of carbonate and quartz, or by a tremolite-quartz mixture. They are often discontinuous and sometimes have rather diffuse margins.

There is a sharp contact between the quartzitic and the magnetite-rich bands. The latter are characterised by very abundant magnetite and tremolite, and a lack of quartz. The magnetite makes up a high proportion of much of this band, but clearly defined laminae are not present. The magnetite rich material is rather streaky or lensoid in distribution, and partly distorted by the presence of numerous narrow fractures which are oriented at a low angle to the banding. The most magnetite-rich material contains over 50# magnetite, intermingled with irregular streaks of fine grained tremolite intermingled with some carbonate. The relatively magnetite poor portion of these bands is composed predominantlyof finely massed tremolite anhedra, intermingled with

(continued overleaf)

- 31 -

82-SAN-1054 - continued

some patchily distributed carbonate and magnetite! and a little chlorite in some places. The tremolite forms masses of somewhat elongate, randomly oriented, anhedra of very variable size. It is always considerably in excess of the carbonate ( The minor fractures which cut this portion of the thin section are filled by a fine grained mixture of carbonate and tremolite.

- 32 -

Specimen No. - 82-SAN-1068

Rock name - slightly metamorphosed banded iron formation,with magnetitet tremolite i and quartz rich bands

Mineralogy abundant - quartzmagnetite tremolite

small amounts - chloritecarbonatepyrite ) traop pyrrhotite ) trace

Description - This is a finely laminated banded iron formation. It contains very magnetite-rich bands up to about l cm wide, intercalated with less magnetite rich material which is characterised by varying proportions of quartz and tremolite. Other minerals are present only in very small amounts. The rock is cut across by a series of narrow cracks, at approximately right angles to the bedding. The tremolite-rich material has tended to be squeezed 1 down some of these cracks so that it now forms projections which may extend for several millimetres from the main part of the tremolite rich band.

The thin section contains one magnetite-rich band, which is bordered by a tremolite-rich zone. This grades into quartzitic material. The quartzitic material makes up the centre of the thin section, and is itself then bordered by another tremolitic zone, which is then bordered by a second magnetite-rich zone, very little of which is included within the thin section. Both the tremolitic and quartzitic material are themselves finely laminated, as a result of narrow bands containing differing proportions of magnetite.

The magnetite-rich band is composed virtually entirely of magnetite. Scattered through the magnetite there are very occasional tiny crystals and patches of tremolite, sometimes accompanied by a little quartz. The adjacent tremolitic band is about 5 nun wide. Immediately adjacent to the magnetite-rich band it contains very little quartz and is composed mainly of a matted mass of randomly oriented, shreddy looking, very fine grained, tremolite anhedra. The proportion of quartz increases until, across about 5 rom, tremolite is virtually absent and the rock has become a quartzite. Here the quartz forms a very fine grained, sutured, rather strained looking mosaic of rather variable grain size. A very low proportion of tiny tremolite needles, and minute anhedra of carbonate are scattered rather unevenly through the quartz. Although the tremolitic and quartzitic bands contain fine magnetite-rich laminae, and a low proportion of disseminated magnetite, this mineral is not very abundantin these laminae overall.

(continued overleaf)

- 33 -

82-SAN-l 068 - continued

Where the cracks cut across the magnetite richband they tend to contain carbonate, accompanied by some chlorite. Where they cut across the tremolitic material they contain a mixture of tremolite and quartz, but lack magnetite. Where they cross the quartzite, the tremolitic material tends to be 'squeezed' down into the quartzite, sometimes for several millimetres. one or two irregular masses pyrite were, noted within the cracks, and one mass of pyrrhotite with abundant inclusions of quartz was noted within the quartzite.

- 34 -

Specimen No. - 82-SAN-1093

Rock name - sheared quartz-feldspar porphyry

Mineralogy - phenocrysts - K-feldsparquartzplagioclase

groundmass - acid feldspar ) yery abundantquartzsericitebiotitecarbonatechloritepyriteapatite

- moderate amounts

small amounts

Description - This rock is a fairly strongly sheared quartz- feldspar porphyry. It is very similar in texture , and composition, to 82-SAN-1119, but is somewhat more strongly sheared. This rock contains abundant medium grained phenocrysts, mainly of K-feldspar, with subsidiary quartz and plagioclase. The groundmass has a highly streaky appearance, and is composed essentially of fine quartzo-feldspathic material scattered through by moderate amounts of sericite.

K-feldspar is the predominant phenocryst mineral, It forms tabular subhedra to euhedra up to about b mm long. These often occur in clusters of several crystals which are typically very finely perthitic but untwinned. The feldspar appears to have been relatively resistant to the shearing stress. Many crystals show slightly strained extinction patterns, and a few are slightly cracked looking. The K-feldspar is slightly turbid, and contains a low proportion of very tiny flakes of sericite and/or patches of carbonate. It is other wise untered. Where crystals are cracked, the cracks are usually filled by fine grained carbonate and/or quartz. By contrast, plagioclase phenocrysts tend to be relatively small and sparse, usually anhedral, and are flecked by a relatively high proportion of tiny sericite flakes. Quartz phenocrysts are fairly abundant. They have been relatively strongly affected by the shearing, and seldom retain their original form. Most of them now consist of very highly strained looking oval 'eyes 1 of quartz which show varying stages of granulation. A few retain outlines suggestive of an original embayed habit. The quartz 'eyes' are up to about 2 mm across.

The groundmass is very fine grained, with a streaky appearance. It has a rather irregular texture, and is composed predominantly of acid feldspar with subsidiary quartz. The two are very finely intermingled with scattered, roughly elongate to tabular, crystals of plagioclase and K-feldspar forming

(continued overleaf)

- 35 -

82^3AN-l O93 - continued

crystals up to about 0,1 mm in grain size i surrounded by finer grained material. The grain size and texture of the groundmass is very irregular in this rock. Small flakes of sericitic mica are scattered through the groundmass. They are rather unevenly distributed. Over most of the thin section they are of moderate abundance, but at one end of the thin section the sericite becomes extremely abundant and makes up over 5 Q?o of the groundmass. The sericite shows a moderately well developed preferred orientation parallel to the direction of shear. Other minerals are present only in small amounts. Occasional small clots and streaks of tiny flakes of deep brown biotite are present in some parts of the rock, as well as a very little biotite being disseminated throughout. Occasional tiny anhedra of carbonate are also rather irregularily scattered through the groundmass, as well as rare tiny masses of pyrite and occasional crystals of apatite. Occasional relatively coarse clots of carbonate and/or biotite and/or sericite tend to occur adjacent to, and often between, feldspar phenocrysts. A fine film of deep green chlorite with a relatively high birefringence occurs in a couple of narrow fractures which cut across the rock at a high angle to the shearing direction.

- 36 -

Specimen No. - 82-SAN-1097

Roc:k name - biotite-chlorite phyllite i with secondary crinkling of the primary cleavage planet

Mineralogy - abundant - chloritequartz biotite

small amounts - pyritegoetheite

Description - This rock is a fine grained biotite-chlorite phyllite. The rock is more or less homogeneous throughout, and shows no indication of the original bedding plane direction. It is composed of a mixture of quartz, chlorite and biotite in which the chlorite and biotite show a very well developed preferred orientation. The schistosity produced by this preferred orientation is crinkled by the very regular development of a secondary cleavage plane at approximately right angles to the first, so that the rock has a finely 'puckered' appearance. This puckering gives a lineation which is clearly visible in the hand specimen.

Quartz, chlorite and biotite are all abundant in this rock, with chlorite being slightly more predominant than quartz, and biotite slightly less still. The chlorite and biotite are intimately intermingled, with the quartz being scattered fairly evenly through them. The quartz forms irregularily shaped anhedra which are usually less than 0.04- mm in grain size. However there are scattered, angular, grains of quartz up to about 0,5 mm, which probably represent a low proportion of relatively large detrital grains in the original sediment. Chlorite and biotite form small, compact, matted, flakes of similar size and habit which are evenly intermingled and both very fresh. The chlorite is a deep green variety, whereas the biotite is a deep brown. The secondary cleavage produces a regular flexing of the chlorite and biotite orientation, so that the flakes curve up and then flatten off again into the primary schistosity.

Very occasional small masses of pyrite are scattered through the rock, usually showing some marginal limonitisation. There is also a little streaky goetheitisation of the biotite and chlorite towards one side of the section. The thin section is cut across by several criss crossing fractures of variable width (up to 0.5 mm). These are composed mainly of a quartz mosaic. This contains a low proportion of scattered chlorite flakes, and occasional small masses of pyrite.

- 37 -

Specimen No. - 82-SAN-1119

Rock name - sheared quartz-feldspar porphyry

Mineralogy - phenocrysts - quartzK-feldspar plagioclase

groundmass - aeid^feldspar ) yery abundant

sericite - moderate amountscarbonate )chlorite )magnetite ) very small amountspyrite )epidote )apatite )

Description - This rock is a sheared quartz porphyry. Abundant medium grained phenocrysts, predominantly of quartz with some K-feldspar and plagioclase i are set in an extremely fine grained groundmass which is also of predominanlty quartzo-feldspathic composition. The phenocrysts, particularly the quartz f have a strongly strained to partly broken up appearances the groundmass has a distinctly streaky appearance, as a result of the shearing stress.

Quartz forms the most abundant phenocryst type, in crystals which are up to about 2 mm across. Despite the strain, these often retain indications of euhedral to subhedral crystal form, and are sometimes embayed. The majority of the crystals are merely very strongly strained looking, but some crystals show some marginal granulation, or are cut across by narrow granulated zones. K-feldspar phenocrysts are also quite common f whilst plagioclase is relatively sparse. The feldspar phenocrysts tend to occur in clusters of several crystals. They are often slightly strained looking, but have been less affected by the strain than the quartz. K-feldspar phenocrysts are up to about 3 mm long, often show a tabular subhedral form, and are typically very finely perthitic. They are very slightly turbid looking, and contain a very low proportion of tiny flecks of sericite and/or patches of carbonate, but are otherwise unaltered. By contrast, plagioclase phenocrysts are relatively small, generally anhedral, and are typically moderately altered with a fairly abundant flecking of sericite. They have a composition of sodic oligoclase.

The groundmass is extremely fine grained, with an indeterminate, streaky looking, texture. The streakiness tends to curve around the phenocrysts. The groundmass is

(continued overleaf)

- 38 -

82-SAN-1119 - continued

composed predominantly of an extremely fine grained, irregular, mosaic of tiny quartz and acid feldspar anhedra in which it is difficult to clearly distinguish individual crystals. Feldspar is somewhat in excess of quartz in the groundmass. Scattered through the quartzo-feldspathic base there is a moderate amount of tiny flakes of sericite which show a rather poorly developed preferred orientation parallel to the streakiness of the rock. There is also a low proportion of tiny clots of chlorite, often with a few tiny anhedra of .epidote associated with them. Clots of sericite and/or carbonate, tend to be adjacent to phenocrysts clusters. A few tiny grains of magnetite and pyrite are scattered through the rock, and occasional small euhedra of apatite are also present.

- 39 -

Spec imenJJo. - 82-SAN-1133

Rock name - slightly metamorphosed, magnetite-rich, banded iron formation with well developed secondary cleavage at a moderate angle to the bedding

Mineralogy - abundant - magnetitetremolite quartz chlorite

small amounts - carbonatepyrite - trace

Description - This is a banded, and finely laminated, magnetite- ricETron formation which has been slightly metamorphosed. It contains bands rich in magnetite, others rich in tremolite, and others rich in a chlorite-quartz mixture. Still other bands are predominantly composed of quartz. The rock is crossed by a secondary cleavage, at approximately 35 to the bedding, which has produced a fine crenulation of the laminae.

The main banding in this rock is of variable width , from several centimetres down to as little as 3 mm. Most of the main bands are also themselves finely laminated. The widest band included within the thin section is magnetite-rich and very finely laminated, the laminae being marked by varying proportions of magnetite. In this portion of the rock magnetite makes up around 50^ of the rock overall, in tiny compact grains which are intermingled with lesser amounts of chlorite and tremolite. The chlorite and tremolite are present in approximately equal proportions, and a very little quartz also occurs in some place's. Quartz is however mainly restricted to minor fractures which parallel the cleavage, and which are filled by a fine grained mixture of quartz, tremolite and chlorite. The grain size in this band is typically less .than 0.02 mm. Chlorite throughout the rock is a fairly deep green, penninitic, variety, whereas tremolite is colourless, shreddy looking, and usually elongate. Both chlorite and tremolite throughout the thin section show a well developed preferred orientation parallel to the secondary cleavage direction.

The thin section also includes a band composed predominantly of tremolite. This contains magnetite rich laminae, but some laminae of this band are completely lacking magnetite. They are composed of very fine grained, elongate, anhedra of tremolite which are intermingled with a relatively low proportion of fine grained chlorite and some quartz. The tremolitic material shows a- particularly strong tendency to be crenulated so that the margin of the band is drawn out into 'peaks' which penetrate the adjacent quartzose band. This adjacent band is composed

(continued overleaf)

- 40 -

82-SAN-1133 - continued

of a fine grained, highly strained and finely sutured lookingi mosaic of quartz anhedra. Magnetite is only very sparsely present in this band, in occasional tiny scattered granules. Stringers of tremolite! paralleling the cleavage direction, tend to cut across this band, which is only about 4 mm wide i and it also contsins a very little scattered carbonate.

The thin section also contains a narrow band, about 3 ra wide, which is of similar quartzose composition, and is also bordered by tremolitic material. In addition there is a band, of similar width, composed of a very high proportion of relatively coarse grained chlorite, rather streakily intermingled with a fine grained quartz mosaic. This band is also relatively free from magnetite.

A trace of pyrite was noted in this rock, scattered along one margin of the wider quartzose band.

- 41 -

Specimen No. - 82-SAN-1162

Rock name - strained and moderately altered quartz-feldspar porphyry

Mineralogy - phenocrysts

groundmass

plagioclasequartzferromagnesian mineral (pseudomorphecj

)) abundantacid feldspar

quartzsericite ) moderate amountsapatite )chalcopyrite ) small amountspyrrhotite )

Description - This rock is a quartz-feldspar porphyry with abundant plagioclase phenocrystsi and sparse quartz phenocrystSi set in a very fine grained, largely quartzo-feldspathic groundmass. The rock is moderately altered, and has been strained, with the development of some discontinuous fractures. A vein of extremely strained looking quartz runs across one end of the thin section.

Quartz phenocrysts in this rock are relatively sparse, but usually quite large, reaching up to about 5 ram in grain size. They range from subhedral to anhedral, are sometimes embayed, and are typically very strongly strained looking. A few crystals are cut across by narrow zones of granulation. Plagioclase phenocrysts are extremely abundant and of very variable size, grading down from a maximum of about 3 mm to some which are only fractionally coarser than the groundmass. The plagioclase phenocrysts are usually in the form of tabular subhedra. They are moderately altered, being covered by a finely disseminated flecking of tiny sericite crystals, which are fairly evenly distributed. Many of the plagioclase crystals have a cracked appearance, with granulated feldspar, or sericite, infilling the cracks in most instances. The plagioclase appears to have been unzoned, with an original composition of around sodic oligoclase. The thin section contains several compact clots which are now composed entirely of a mass of very fresh, bright reddish brown, secondary looking, biotite flakes. These are randomly oriented. These clots are up to about 3 mm across, and have a fairly regular form, They most probably represent the sites of pre-existing ferromagnesian phenocrysts, although their outlines are not sufficiently well defined for an indication of the composition of the original mineral to be obtained.

(continued overleaf)

- 42 -

82-SAN-1162 - continued

The groundmass of the rock is composed of a base of extremely fine grained quartz and acid feldspar with an indeterminate texture. The grain size is so fine that it is difficult to clearly distinguish individual crystals, and to determine relative proportions of quartz and feldspar. However feldspar appears to be considerably in excess of quartz. Small flakes, and clots, of a secondary looking biotite similar to that described from the phenocryst pseudomorphs are scattered rather unevenly through the groundmass. A little sericite is also disseminated, but sericite is mainly restricted to irregular streaks and stringers which cut across the rock. These range from rather diffuse streaks to fairly well defined infillings of minor cracks in the rock. In the most well defined cracks the sericite is accompanied by some quartz and, in some instances, by scattered masses of chalcopyrite and pyrrhotite. These two sulphide minerals are often intimately intergrown. Relatively large euhedra of apatite are also present in accessory amounts, in the groundmass.

The quartz veinlet which cuts across the end of the thin section can be seen in hand specimen to be at least 2 cm wide. It is composed of a monomineralic mosaic of extremely strained looking quartz anhedra of rather variable grain size. In the vicinity of the quartz vein the groundmass of the porphyry tends to be relatively rich in diffuse quartz stringers. In addition, the pseudomorphed ferromagnesian phenocrysts are composed of a mixture of sericite and biotite, rather than only biotite.

SULPHIDIZED AND METAMORPHOSED CARBONATE - (SILICATE) IRON FORMATION

82 SAN - 1137

Offcut:

Sulphide-rich pale buff-yellow rock with clots of a soft green mineral (chlorite?). Sulphide has a sieve texture, pervading the gangue. One thin band of sulphide is oxidized, the remainder is fresh and slightly magnetic.

Mineralogy;

Carbonate : 40 0Opaques : 300/ of total.

Occupy 70/S of one half of the slide. Cuimiingtonite-Grunerite : 20 - 255L Some twinning, acicular to

prismatic, B C+), high 2VChlorite: 3 - 43L Dark green - blue green (high Fe). Quartz : 2 - 3%. Fine grained mossaic.

Mineralogy is variable depending upon position in slide.

Texture, Structure, Fabric :

Half the slide consists of felted masses of carbonate, epidote and lesser chlorite. A subtle compositional banding is evident suggestive of relict bedding, although, the chlorite component imparts a schistose texture to some of the microbands. The remaining half of the slide consists pre dominantly of spongy sulphide which has invaded and replaced the carbonate -ciinoamphibole-quartz matrix. A large vein consisting of chlorite sheafs cross-cuts the pyrite, indicating that chlorite is last in the paragenesis.

What little quartz that is preserved in the section shows evidence for deformation, which is consistent with the swirling sheaf-like nature of the chlorite.

Alteration :

The intimate intergrowth of carbonate and amphibole suggests the carbonate is a primary constituent rather than resulting from a superimposed alteration event. The sulphidation is pervasive and cross-cutting and represents massive introduction (or remobilization?) of Fe and S .

Opaques :

The opaques consist entirely of cream pyrite, which is ragged and invasive creating a spongy texture. Minor oxidation occurs at one end of the slide. Although, the sulphide resembles pyrrhotite it is not magnetic and does not dissolve in concentrated hydrochloric acid.

Assay

Cu 10 ppm, Zn 55 ppm, Ni 6 ppm, Co 2 ppm, Ag 0.1 ppm, As 7 ppm. No Au detected (detection limit?).

Interpretation :

The rock was originally carbonate-rich and may well represent a mixed carbonate-silicate facies iron formation, which has been metamorphosed. The presence of cummingtonite (Biaxial *) suggests the original sediment was high in Fe and Si. Sulphide component has been introduced. There is a significant amount (-*55S of the opaques) of grey magnetite intergrown with the pyrite, which would explain the magnetic character of the rock.

- 43 -

APPENDIX III

LIST OF PERSONNEL

- 44 -

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

^OFFICE WORK

Sue Allen Draftsperson

Cord Vandevalk Chief Draftsman

S. Annett

F. Gittings

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

Same as above

Sept.30- Oct. 8 1982 (4.0 days)

Same as above

Dec. 6-8, 1982 3.0 days

Dec. 17, 1982 (0.5 days)

Dec. 29, 30,1982(1.0 day)

Dec. 9-14,1982(4 days)

SANDY 'B 1 CLAIMS

STATEMENT OF EXPENDITURES

Petrology: Dr. Boutcher $ 240.00Geoplastech 50.00 (invoice 204)

Thin sectioning: Geoplastech 154.44

Analyses: Bondar-Clegg Ltd.

170 Ag, As, Au $ 2,363.0021 Ni, Co, Cu 63.002 whole rock 90.00 2,516.00

TOTAL EXPENDITURES $ 2,960.44

St. Germain Street, Winnipeg,

Mani toba R2M

204--255-17M 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 4-9 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, and $980.00 for the Sandy reports, from Canadian Occidental Petroleum Ltd.

ftSheila M.A. Boutcher Ph.D.

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

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

Winnipeg, ManitobaR2M 4N3

COPY

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

INVOICENO.Terms:Payable upon receipt

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

M D ate: Jan 3/ 83 Shipped Via: Your Order No.: Gittings fef|fep*

Quan. ; Ordered

~1r^~1

i•:'i

fy;Sj

1

1

'•*

^ ————————— 1 ———————————————————————————————————————————————————————————————————— ——————

Description

polished thin section interpretations

Extn. Ckd. By

Rec'g. Ckd. ByDATT" rjt"i~'i-i

JAN -5 1983 -PfiEts 1 Terms Gkd, r/^ ^^^

itti^'-s to p^. Ajjp'd, ..-"' i*.

S Total

•I oaid to fiennla^tprh Inr. rprpivpri with thankc. s~\ ————

Quan. Shipped

2

2

Unit Price

50.00

Amount f V : .- - .''' 'v.: :"' -' -1 -''' : "l.''--'' " -1 . \ v'- -'-.' . '-1 -

fe^'- :: V^::^i: K,-.- •i.;.'...--:-,^ j. i r -..*. t*:-..-,'1 ' ' :~K-'V" rfV1 ' '.^ ' '.•'••'

100.00rh •••.•.'.^,- ; ' •vW; 1 .v":''s''i i;.o. •^••.•;v;--..;-j'J'i -.;--fI'^^ifi^V^.'

ft,,;;-;;.,^^;^"^-' 1

. ., ., .... i^'^^H^'';\^:*?r^-'I'if^^a^^vK-'.•.•,-MNi'.r';.''it5^;*''vV-'fc/s^s^fc:^?^?tis^m^||IHP^!: s^^^llii?Iv^l^fei !l?^f^.^|||;'.

—————————— ^ fSSfi^i^"

S loo. oo

COPY

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

INVOICENo. 1 72Terms:Payable upon receipt

SERVICES RENDERED TO:

;^;:v:-' ;:-v^^:

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

*-. : ^ ',. O / "'*s?-*'\.'"' '''' ':vft'-'--'--''^^\v-i' v.'Sk-?--!'^-:^.^-^*

'' - ±l?;'f ''-" r;"

l^y Date: Nov 19/82Quan.

, rf- OrderedV^ - - .' ,, '

"*V^ - ''•J' f'1*

--•''V"1 ^ ''*

-- '.""ji . O '^ - - - .-. ' X*,~ '- i-;.* \ **

46

PSSssfx* 1"!'**^ i

lil

Shipped Via: Your Order No.: Sittings iS

Description

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

polished thin sections

minimum charge cuts

-

shipping tp^pr,.JS.,uJBjcai|

Mm paid to |^S Geoplastech Inc.

frtn f" 1"1 RV

n ...- TH n..

tcher. St. Vital Man.

JAM -5 19ft*

received with

^•.^--•-' . -. ..,. . —Ithanks . ^)r \

Total

duan. Shipped

52

2

54

Unit Price

7.75

18.00

2.00

Amount /' •'•.vv. i '

.I;..,;;.:,,--.'-'' J::\f'.:: ••';.'^.-- . •.:-:.

403.00 fetlpS:

36.00 ^.Sjo?

96.00 ;^||^

^{^te

12.85 gS3^:

Pill

'i'^^'&ii-'

S547.85 ^SilS'BaS*^ft5i.b'-.

"BOiMDAR'-CLEGG fi COMPANY LTD,BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX; 053-4455

CANADIAN OCCIDENTAL PETROLEUM LIMITEDF* W, 81TTIN8B180 ATTUELL DR.4TH FLOORRtXDALKf ONTARIO,H9W 6A9

(rwoicet 101378

Datet October 29* 1982

Report No} 112-1795

Project: SANDY ROCKS

B C L H i /M -

110 Analyse* of Silver Subtotal

110

110

of A Subtotal

of CRUSHfPULVERIZE -200 st Subtotal

Subtotal

l.VO

3,25

2 , 75

209 209

357

302 302

yo vo

.00

.00

.50

.30

.50

.09

.09

20V

337

302

90

,00

50

.50

Invoice Total

THIS IS A PROFESSIONAL SERVICE ACCOUNTS DUE WHEN RENDERED

BCDNDAR-CLEGG fi COMPANY LTD.BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455

CANADIAN OCCIDENTAL. PETROLEUM Ulil lF,W, CJITTIWGS180 ATTWELL DR,'UN FLOORREXDALEr ONTARIO,MVM 6A9

101429

Dsty? November 05j 1982

Report Nut 112-179'J

; SANDY ROCKS

110 of Gold - Fire A 6 1-*; y &1 6.00 660.00 Subiuial 660.00

Invoice Total

660,00

THIS IS A PROFESSIONAL SERVICEACCOUNTS PI IF WHPM RFNHFRPP

BONDAR-CLEGG SL COMPANY LTD,

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

CANADIAN OCCIDENTAL PETROLEUM LIMITEDp,w,.SITTINGS180 ATTWELL DR.4TH FLOORREXDALEi- ONTARIO,H9H 6A9

Invoice} 10HA4

Dstei November 10? 1982

Report Not 112-1830

Project! SANDY ROCKS

•A C

281 AriBlwses. of Gold - f ir* A s&aw at 6*00 1686^00 Subtotal U86.00

281 Anal**** of Arsenic SubtotiBl

si 3*25

Invoice Total

913*25

1684.00

913.23

*2S99*25

THIS IS A PROFESSIONAL SERVICE ACCOUNTS DUE WHEN RENDERED

BONDAR-CLEGG fi COMPANY LTD.

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

CANADIAN OCCIDENTAL PETROLEUM LIMITED

F,W. OITTINOB180 ATTUELL DK,4TH FLOORKEXDALEf ONTARIO tK9U AA9

Invoice t 101430

D*tftt November OSr 1982

Kwort No? 112-1830

Project: SANUY ROCKS

281 Anttlwtias gf Silver 32 Anslutttft of Cobalt 36 Anwlw6t*ft of Cooper 36 Analwfces of Nickel 23 ftnalwsws of Zinc

Subtotal

281 Samples of CRUBH*PULUERI2E -200 at Subtotal

Total

wtditt l3tif t

oft

1.900,900*900,900,90

2*75

S3 3. 9028.8032,4032,4020 , 70

64fc,20

772,75772.7S

648,20

7 72 1 70

11420*95

TH1S IS A PROFESSIONAL SERVICE ACCOUNTS DUE WHEN RENDERED

BQNDARHCLEGG S COMPANY LTD

|4 BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455

Invoices 1 01605CANADIAN QCC1UENTAL PETROLEUM LIMITEDF*W, OITTIN08 Ptftet December 02* 1982 180 ATTWELL UK,4TH FLOOR Report No J 212-1830 REXDALEr ONTARJOiMVW 6A9

Project t BANDY ROCKS

^J^^Jt

21 t'Ki^lufet'fc of Lust, on liJiili ion di 5.00 10Q.OOSubtotal 10B.OO 10S.OO

21 AnalwBefe of Whole Rock totoi-uuuii a i 4 0.00 840.00Subtotal 840.00 (340.00

Invoice ToUl *945. 00

THIS IS A PROFESSIONAL SERVICE ACCOUNTS DUE WHEN RENDERED

(J0\

\

006

-Mm.Mryo! - Report Of Work

Resources (Geophysical, Geological,Geochemicel and Expenditures)

T\ tie e' Suwey(s)

Geological and Geochemical Report.laim Holder fs)

The Mining A ct

Instructions: —' Please type or print. : -"— If number of mining claims traverse

exceeds space on this form, attach B lis Note: — Only days credits calculated in th

"Expenditures" section may iie cntere in the "Expend. Days C'." column;

— Do not use shaded areas below. i or Area

M-3017TProspector7* Licence NoT

CanadianAddress

180 Attwell Drive, 4thSurvey Connpany

P ;e t r pi e urn .L td

?j Ont.ari.o...M9W. 6A9.. .....-...-.Date of Survey (from Si to) iTota! Miles of line Cut

Day J Mo. j Yr. j pay_j Mo^j^Yr. j _ _arnearid Aociressof Author (of Geo Technical report)Fred Gittings, 180 Attwell Drive, 4th Floor, Rexdale, Ontario M9W 6A9

Cifcdits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:

Enter 40 days. (This includes line cutting)

Fof Each additional survey: using the same arid:

Enter 20 days (for each)

Man Days

Complete reverse side anri enter tol6l!s) here

Airborne Credits

Note: Special provisionscredits do not apply to Airborne Surveys.

Geophysical

- E lectrorri&gnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- E iectromapnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

E lectr omagnetic

Magnetometer

Radiometric

Days per Claim

-- - ——

Days per Claim

3.5~

Days per Claim

Experiditures (excludes power stripping)Type of work performed chemi ea l analyses and_ petrographic studies. —-——-

Pe:rfofmE-d on Claim(s)

1 2 8 2,^56 1285,

KRL 561286Calculation of Expenditure Days Credits

Toiel Expenditures

2,760if tr uct ions

Total Days Credits may be apportioned at the claim holder's choice Enter number of days credits per claim selected ir, columns Et right.

Ib'etfT"nt (Signature)

Mining Claims Traversed (List in numerical sequence!

Total number of mining claims covt-ed by this report o* work.

14

...-.for-Offi'CrOseOnly

Recorded

2 -.P*t*'Approved es-Recorded jBranch Director

Ce r tjfi c at i on Verifying Report of Workl heieby certify that l have i personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or xviu essed same during and/or after its completion and the annexed report is true. t fPL ' ^) (0 l

, a-.d Postal Acidtess of Person Certifyirig

Fred Gittings, 180. Attwell Drive, 4th Flnnr, Pexdale, Oataf'jo M9W 6A9TDa'.f Certified"" "TCenfied^y C^ignavjre) * t f-Nov. 4/82 l M.-^, J'/x ) AtTT

Report of Work(Geophysical, Geolopical, Geochtm'ical and Expenditures!

Instruction!: — Please type or print.- H number of mining claims truvertl

exreeos space on this 1orm, ettsrl-. e hi Note: — Only days credits celtulaicd in li

"Expenditures" st-cuon ma^ LIP t-nitrrJ in the "Expend. Days C' " rolunirj

— Do not use shaded areas belcmi \ f* c Su' veyU) w^^^^^^^^

Geological and Geochemical Report.Clum holderltl

Canadian Occidental Petroleum Lid.Addrrts

Survey Company

1 BWfthip o

xdaJLfi^ .On1t.ario..M9JW.-fiA9Date of Survey (from Si l o

Day j Mo. j Vr. Day

r Area

i Pi ospectO''* Licenct No

T644

) jTote! Miles of line Cut

1 Mo. 1 Yr.Nerrie and Aodiess of Author (of Geo-Technicel report)

Fred Gittings, 180 Attwell Drive, 4th Floor, Rexdale, Ontario M9W 6A9Ci edits Requested per Each Claim in Columns at rightSpecial Provisions

Fo- first survey:

E mer 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side

and enter tolal(s) here

Airborne Credits

Note: Special provisions credits do not apply to Airborne Surveys.

Geophyticel

- E ectromfcgnetic

- Magnetometer

- Radiometric

- Other

Geolopical

Geochemical

Geophysical

- Electromagnetic

- Radiometric

- Other

Geological

Geochemicel

ElectromBBnetic

Magnetometer

Radiometric

Days per Claim

. ——————

Days per Claim

3.5

Days per Claim

Expenditures {excludes power stripping)Type of work performed chemical analyses and petrographic studies.

Performed on C'sim(s)

KRL 561282, 561285,

KRL 561286Calculation of Expenditure Days Credits

TotalTotal Expenditures " — ~- ~- Dp y s CICP it*

P2,760 ' -J- 15 ^ 184nstr uct ions

Total Days C'ediis may be epponioned at the claim holder's choice Enter number of cays credits per claim selectedin columns st right.

yj Date ^rfc

j Nov. 4/82 -\-Sfded.Holde/ or /^pent (SiQn&tule) \ t f \ yr li V

^t^J( (A l^^sTJtKA \Certification Verifying Report of Work ^ ^-— —

Mining Claims Traversed (List in numerical sequence)Mining Claim

Prefix Number

KRL 561276

561277

561279r~561280

! 561281

; 561283

561284

\ 5 61285

[j 561286

561287

561288

[j561289

jf flSSr'

\

ft E.D !- 1 '

•pi~ECEI VL PtQ - P 10U-U . - i^

A.M| ^

i

Expend. De y t Cr.

1&

1-61 ..

1-6-

1-7-

r?'1-7"

1*

131'7

T7k'li50\?

aV-

12

2

2-

3.•3.

/3

A7

i

.^..-.^-or-OlficTOIe Only

Mining ClaimPrefix Number

c,

Ss Q

i ** ' ^ *s 2j co c

^ ^- g-

S | ^f--t^r -:

555 . _ .,-—

^ t C t s

^ i 'Q? 1( 1 198?M.

- ),-y). — —L^..—: —— . -

j .

j t j xJ /^L/v^^^—

Expenc Days Cr

—— ——

— ———

~1

11

^r-

— —

Total number of mining claims covt'td by this 3.4 report of work.

~^ - —— ~~^-, ———— Total Days Cr. Date Recorded s ' Minina/fi^corder , ,/s ^- — Recorded t, / . /^-, S' V^1 'JSr / ^ s

/l//'^ /6/^.Z {^^-"T^^f/l jf^-^t^^^^.^S\^}sJ /^f ' .i^C^*6^*A —— K- —— r^SSjvSL-i-^l... - .^'^l jf^^J Date Approved as Recorded

CNX-V^Sfr^

Branch Director

1 hereby certify thai 1 have i personal and intimate knowledge.of the facts set forth in the Report of Work annexed hereto, having performed the work or ivitr essed same during a^d/or after its completion and the annexed report is true. }^f?L , ^ (o l *L. *7 '^

NJan-it end Fos'el Aodiess of Person Certifying

Fred Gittings, 180 Attwell DriveUr- 4th Floor, Ro vela le Ol? ^ 3 * ^ MOM CT\ODele Certified '

NOV. 4/82 ^r^JXifcr

Assessment Work Breakdown

Man Days, are .based on eight (8) hour Technical or Line-cutting days. Technical days include work performed by consultants, draftsmen, etc..

1 y i' e 0 1 Su'vty 1

Geoloqical and Geochemical Report jT echnica!

Days

L 7 X

Technical Days Line-cutting No. of Days per Credits Days Total Credits Claims Claim

7 * 1 49 4 "49 ^ 14 s 3.5

Type o? Survey

Technical DaysL7~~ x Technical Days Line-cutting No. Of Days per Credits Days Tote! CTediis Cleims Claim

7.|* ' *

Type di Survey

T echnical Days

LTechnical Days Line-cutting No. of Days per Credits Days Total Credits Claims Claim

L -L J* - , *T ye f o* SLK v-ey

Technical Daysf- —— J x

Technical Days Line-cutting No. of Days per C'edits Days Total Credits Claims . Claim

7|-| H - *| -|

Ministry of Natural of Work'

On

Instructions — Supply required date on B separate -form f or -each -- type of work to be recorded (see table belowl.

— For Geo-iechnical war* uss form no. !3G? "Report of Work (Geologies 1 , G! or-'^ysical, Gfroohemitsl end

The Mining A ct E xpenditures)".*odre?j of Recorded Holder

Canadian Occidental Petroleum Ltd.380 Attwell Drive, 4th Floor, Rexdale, Ontario M9W 6A9

Prospector's Licence No.

T644

of Work Performance and Distribution of Credits" c la' IV or k Days C', claimed

48J ;j' re r "f r- f-.ance of the following.-.•or*. i. C" tck one only)

[JJ r/anubl Work

[ jSha't Sirikirrg Drilling orolhef L Bteral Work.

yJ*Comp r ei.sed Air, olher* 1 7 ^ i c*we T driven or

riif-c hs nice 1 fquip.

[J^ov.e- STrippinp

QJ Die mond or other Coredr i 1 tinp

Mininc ClaimPrefix j Number

KRL 561276— - - - - - - - --- -: 561277

561278

5612791! 561280

561281

1 561282l

' 561283

WorkDays Cr.

4

4

4

4

4

4

3

3

N' r n i n g C ictrriPrefix

-. . . .

Number

561284

( 561285

561286

i 561287

'561288

561289

WorkDays Cr.

3

3

3

3

3

3

Mining ClaimPrefix | Number

raMir—T"-'""

pj

A.M.,

-,-^r ,-, . -. —— ™ —— -^-

, . . . , . f r "\l

~~ ~

i,: r, \j j o^(—l — ,-V -^ -LJ- -— -

|7i8^ilOillil:2fl!ti~ l

WorkDa yi Cr.

— —— —-^-i^

: F,. w*r —

t?*—"P.M.

MiM

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

y. A.Work Performed on Claims: 561282 ~"

561285 — ^561286 — 2L

Dates: 9 hours on October l, 2, 3, 1982 — x 6 hours on Septesriber 30, 1982 - v^ u 3 hours on October 8, 1982 — KR.L

RECEIVEDDEC 161982

MINING LANDS SECTION

Equipment: l Atlas Copco Plugger l Wacker Plugger

Men: P'red Gittings ) Mike Henrick ) Art Murdy ) Rexdale, Ont. M9W 6A9John Allard - John St., Espanola,

Ontario

p r- c F i v P FJ v^ L. Vs. U l * i-* (a

Canadian Occidental Petroleum LtdP - ft-i O ft? 180 Attwell Drive, 4th FlocL M ^ a. w

RED LAKE/'.INING D!V.

Ccitification Vtrifyiiig Report of Work

Date of Report

Nov. 4/82

l hereby certify that or vvitnesifcd s-s^:ie du

Nanie and Postal A ridref

..Fred Git t. i r

Table of in'o;motion

7 i, ft of Work

-A /

R&F&rded Hplderlor Acent (Signature)

.-.Lhaving performed the w e

ftypes)

Sr.B*! Sinking, Drif;ir,p o', h e- LuerEl Work

ed er

//, !

ip O- other CO't

t core, number end e ngie? 01 nores. i

We-rr.-t' arid ttadresf- o f O ntario l&nd s uricyer. J

An&chrnents

Work Sketch: these ere required to show the location end extent of work in relation to the nearest claim post.

k Sketch (as ve) in duplicate

TRENCH DI MENS3 ON S

Tr e^

SAK-82-A-T1

EAN-82-A-T2

SAN-82-A-T3

SAN-82-A-T4

SAN-82-B-T1

SAN-82-B-T2

SAN-82-B-T3

SAN-82-B-T4

SAN-82-C-T1

SAN-82-C-T2

SAN-82-C-T3

SAN-82-C-T4

8 m x 3.5 x 0.8 deep

8 ni x 3.5 x 0.8 deep

13.5 m x 1.5 x 0.8 deep

13.5 m x 1.5 x 3.0 deep

10 m x 2.5 x 0.8 deep

19 m x 3.5 x 0.6 deep

10 m x 1.5 x 0.6 deep

5 x 1.2 x 0.8 deep

7.5 m x 1.8 x 0.8 deep

7.5 re x 1.3 x 1.0 deep

31.5 ir, x 3.2 x 0.6 deep

30.0 m x 0.8 x 0.7 deep

PAN-82-Z-T1

SAN-82-Z-T2

4 m x 1.0 x 0.4 deep

8 m x 1.8 x 0.6 deep

RED LAKE/.MKING DIV.

RECEIVEDDEC -S 1982

A.M. P. M i

KRL 561287

Sandy Lake

KRL 561283 KRL 561288

MOV 101982A.W

CANADIAN OCCIDENTAL PETROLEUM LTD. Minerols Division

PROJECT SANDY 'B 1 CLAIM GROUPNorth Western Ontario N.T.S. 53 F 3

1982 TRENCH LOCATIONSSCALE- V5OOO

FWG/gv/Nov. 1982

T

KRL56I278 l KRL 561279KRL56I285 7KRL56I286

",wp

SAN-B-T4-82

Sandy Lake

Q. O

CANADIAN OCCIDENTAL PETROLEUM LTD. Minerals Division

PROJECT SANDY 'B'CLAIM GROUPNorth Western Ontario N.T.S. 53 F 3

1982 TRENCH LOCATIONSSCALE- 1'5000

FWG/gv/Nov. 1982

r - f 3

1983 10 20

#102

2.5340

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

Dear Sir:

RE: Geological Survey and Assaying submitted under Section of the Mining Act RSO 1980 on mining claims KRL 561276 the Kakapitam Lake Area

The Geological Survey and Assaying Expenditures assessment work credits as listed with my Notice of Intent dated September 26, 1983 have been approved as of the above date.

Please Inform the recorded holder of these mining claims and so Indicate on your records.Yours very truly,

E.F. AndersonDirectorLand Management Branch

Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1W3 Phone:(416)965-1380

D. K1nv1g:mc

End.

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

cc: Resident Geologist Red Lake, Ontario

© Ministry of Technical Assess Nature) Resources Work Credits

Ontario ^fc

mont f"* 2.5340

Date Minina Recorder'1 Report of1983 09 26 Wqrk!jo- #102

Recorded Holder CANADIAN OCCIDENTAL PETROLEUM LTD

Township or Area

KAKAPITAM LAKE AREA

Typ* of survty and number ol Atstssment days credit per claim

GeophysicalFl*rirnrn*gn*t!e dayi

Rprtinmetrir . dayt

Othar dsyt

Section 77 (19) S** "Mining Claims Aliened" column

Geological . dayi

Geochprninfll , rlayt

Man days [D Airborne d

Special provision LJ Ground ly]

CD 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 Claim* Attested

$2,760.00 spent on petrographic studies and on assaying samples taken from mining claims KRL 561282, KRL 561285-86.

184 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 three claims is 61 days per claim

-T

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

No credits have been allowed for the following mining claimi

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

j

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)—GO:

eze

© Ministry of Technical Assess Nature) ... , ^ . ., Resources Work Credits

Ontario ^fe

ment *i*2.5340

Bite Minlrvo Rtcorder'i Report of1983 09 26 Workfj0' #102

Recorded HolderCANADIAN OCCIDENTAL PETROLEUM LTD

Township or AreaKAKAPITAM LAKE AREA

Type of survey and numbar of AMtisment day* credit per claim

Geophysical

EltC'romtgnetJC d*V

Other rljiyt

Section 77 (19) S** "Mining Claims Aliened" column

Geological . days

Gfinchfirnicfil dayt

Man days 03 Airborne LJ

Special provision LJ Ground S3

fi 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 Claims AtMwd

i

KRL 561282 561285-86

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

No credits have been allowed for the following mining claims

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

KRL 561276 to 81 inclusive 561283 -84 561287 to 89 inclusive

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)—60:858 I93S6)

Ministry ofNaturalResources

ario

Your file:

Our file: 2.53401983 09 26

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

Dear 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, you 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,

xvu^x Anderson j?\ Director

Land Management Branch

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

ffi D . Kinv1g:mc

Encls:Petroleum Ltdcc: Canadian Occidental

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

cc: Mr. G.H. FergusonMining S Lands Commissioner Toronto, Ontario

Ministry ofNaturalResources

Ontario

Notice of Intent

for Technical Reports

1983 09 26 2.5340/102

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)

CANADIAN

Canadian Occidental Petroleum Ltd.

August 8, 1983

RECEIVEDW i; i 19E-1

MINING LANDS SECTION

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

Dear Mr. Anderson:

Re: Your File 2.5340Mining Claims KRL 561276

____in the Kakapitam Lake Area

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

(1) Geological maps, in duplicate, entitled "Project Sandy 'B' Claim Group" 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.

Yours truly,

CANADIAN OCCIDENTAL PETROLEUM LTD.

RJE/sa

Enclosure

R.J. Evans Administration Manager

Minerals Division — 1BO Attwell Drive, 4th Floor, Rexdale, Ontario M9W BAB [416) 675-2312 Telex O6-9B94S3

BONDAR-CLEGG S. COMPANY LTD,764 BELFAST ROAD, ONTARIO. K1G OZ5 PHONE: 237-311O

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

WHITEHDRSE VANCOUVER OTTAWA CAMPBEL.LTON

S. G.CJNC^ANV LTD.J* —————————————————————————————————————————————————————————————————————————————

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

mktii.kim LJHITE.Mbl

11H FI. O UKl' t X M rtUfc r OH l i'*K l U . H y W

r nw i c i.* t

Uattff OctuUvr 2Vr

Hut 112-179U

SANDY kOCKB

J J V inin'Jvvev uf

11 0 Hh*'lvvi.H of f'i

^ P rt-)' iff r w l i*'H 110 yir^>^•ly>, i,' T CKUSHrKULVEKlZE

Hi s-1'.'u J l

tt

-200 a l

, 2 li

20V eo

,4'.j 7, t) o \ i*j/.\

302 . 'Jf

y o (

TH(S IS A PROFESSIONAL SERVICEmie U/UCM

/li \iOAK~CLL- .J G' "6i C LTD.

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

Ol.l JOfcNliU P fcTKOtfeUh I.J.Iimifr ,n, un utm*!J HO H* iMb'-LL UK, •HH KLUUfc

fnvoiful

r-t H uJ 1 12-1830

P ro. J &tr U B AMU V KOCKii

.'•2U1 Miir.'Jvstn ul b 11 Vi'.i ~' An y i v si v t- u i C i

,1ft Ml In) J y SI t.'IS U i'

VfcU'V uf i'i i

a l

-^00 *l

Tolt l

l , VOo ^ voo, yo o i v oV * 'J '.'

2H t BO

6-ltf ,20

7 72, 7 *J

H20, v'.t

TH/S fS A PROFESSIONAL SERVICE HUP IA/MPM

BDNDAH^CLEGG S CDlVgpANY LTD.ELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455

t?1 101464OCUPKMlVtt PETROLEUM L1M1TEU

F.M, (ttn'JHOS I**let Novtfmboi' 10? 1V82 180 An HELL fiR, •VI H KLOOR RwpQi't Mot 112-1830

Project? 3AHDY ROCKS

ol (H'ld - f'it'V A***'V fct 6100SuL'lyl*! IA8A.OO

ft /H 1StjbtoUJ y 13,25 913,2'j

THIS IS A PROFESSIONAL SERVICE

^'J3Ui\iOAf-:-GLbGG Ci UufeHANY LTD.M^^ - - ———— -—— . —————— —— ——— . M—————- -—————— :———:

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

ftH Out; lUt H l At mfcOUUH L J lil Tt Or.w, (irmwjy leo A* i wu UK. lin rLOOK

Halo J

Mot

12*

7 An,nlv 15u* of Silvu t td lul'til * uf (i

el H Sub lo1

•11*•t2 An*

t -r.' 7 An st J w i' Mi-*t.Miic

i i

SubluUl

TO t

11. l, VOt-1 C1 1 V C'

at. OiVO11 0,90

3 . 'J!

o . ',**i*^ t * wl

279.30 3X, 80 37,80 37,80

3?2*?0

•7*;

116,2V 118* 29

A W . /'J

THIS IS A PROFESSIONAL SERVICE mie U/UCM

BOND Alf; r C LEG G ST'C D fNf^PA NY LTD.

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

CAHA1DAH QCClIiEHT*l PETROLEUM 11 MITE I-,H, OITTIHOS ISO ATTWEUL UP. '1TH FU30F

r OHTARIO.MtM AA*'

J 902

Hot 11?-

An j l^*t."* of Ou.l*:I ~ Fire , 00

ule** Total

THIS IS A PROFESSIONAL SERVICE

Si COMPANY LTD,

|64 BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455

f .H, uiil HO M! r HILL'M H M.UUR

H;"IKUUUM L l fi J 1 1: l'wt 1 01 -12V

iialut Nuvwubtfr 05*

HtM'tM t Not 112-1/90

j lv of tiuJ'J - f i if At' y uli l. u l tt l

*t 6,00 660-00660 i 00 6 {S O

THfS IS A PROFESSIONAL SERVICErn ic \AJUCM

August 4, 1983 2.5340

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

Attention: Fred Sittings.

Dear Sirs:

RE: Data submitted for Assaying and Sampling credits on Mining Claims KRL 561276 1n the Kakapitam Lake Area

Returned are six Geological plans (1n duplicate) for the above mentioned survey. Please sign all copies of the maps.

Also* please submit signed receipts or cancelled cheques (In duplicate) as verification of expenditure claimed,

When submitting this Information, please quote File #2.5340.

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

Yours very truly,

E.F. AndersonDirectorLand Management Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 41G/965-1380

S. Hurst:sc

cc: Mining Recorder Red Lake, Ontario

Encls:

Ministry ofNaturalResources

Ontario

GeotechnicalReportApproval

File

Mining Lands Comments

l^ALJOi^

To: Geophysics

Comments

L) Approved Q Wish to tee again with correctionsDate Signature

To: Geology - ExpendituresComments

[^[Approved | | Wish to see again with correctionsDate Signature

To: Geochemistry

Comments

( l Approved [ j Wish to see agai n with correctionsDate Signature

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

1593 (81/10)

1983 01 14

102

2.5340

Mining RecorderMinistry of Natural ResourcesOntario Government BuildingBox 324RBd 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 561276 et al 1n the Area of Kakapitam Lake.This material will be examined and assessed and a statement of assessment work credits will be Issued.Yours very truly,

E.F. AndersonDirectorLand Management BranchWhitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1380

DU: se

cc: Canadian Occidental Petroleum Limited Rexdale, Ontario Attn: Fred Sittings.

KRL

) 561161 'i '

KRL

KRL "j KRt

56II6Z56II6S. * .. . .. ..'

KRL j KRL

I1.5611 6 556H 66 i 561 l

KRL ! KRL i KRL

561169 (56II70 IsBII 7 l

O5 d? n d y

o

^

l O

)I

~

. w 05

V at (M

\

0^

iJ

\. \ s\ "\ ^ ^ 5 \ •^ ^ o

01

. :

fei

x:

^~

31

- —

~

r":

Sx :

3)

-

••-•

'A\*

'-

'

X V. •^

y

V

Stain River Area G-189293915

930 00'

53 0 07'30 —

00N-

O

O)

O-l

"OC Oen

o QQ

c ov-o

KRl

561

KRL

561

KRL

561

KRL

614

KRL

614

53 0 00'-

KRL l KRL l KRL l KRL

561160 l "561161 (561162 ' 561163561278 l 561279 l 56I2BO - — -L----l-- —

KRL ""^ KR

561164 l 561165 | 561166 l 56)17?

561170 56IITII——— -J.——————

614692 614689

M 695 '614694 , Safidy L ok l

Sandy

Lake

— 53 007'3O"

07

06

05

04' l

D Q)

O)j*o

oo:03'

02

01'

53 0 00'

14 1209' OB- 07' 06 05 04' 03

02' 01'

93 0 I5'930 00'

West of Niska Lake Area G-I9I3

b.k531931

REFERENCES

AREAS WITHDRAWN FROM DISPOSITION

M.R.O. - MINING R IGHTS ONLY

S.R.O. - SURFACE RIGHTS ONLY

M.+ S. - MINING AND SURFACE RIGHTS '

Uatcription Order No. Date Ditposition Fil*

DATE OF ISSUE

SEP ...6 J

Ministry of Natural Resources TORONTO

LEGEND

HIGHWAY AND ROUTE No.

OTHER ROADS

TRAILS

SURVEYED LINES:TOWNSHIPS, BASE LINES, ETC.LOTS, MINING CLAIMS, PARCELS, ETC

UNSURVEYED LINES: LOT L INES- PARCEL BOUNDARY MINING CLAIMS ETC.

RAILWAY AND RIGHT OF WAY

UTILITY L INES

NON-PERENNIAL STREAM

FLOODING OR FLOODING R IGHTS

SUBDIVISION OR COMPOSITE PLANRESERVATIONSORIGINAL SHORELINEMARSH OR MUSKEGMINESTRAVERSE MONUMENT

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOL

PATENT. SURFACE ft M INING RIGHTS .._..........™. 0

.SURFACE RIGHTS ONLY.-__—._.........- ©

.MINING RIGHTS ONLY___.......,.......... ®

LEASE, SURFACE ft MINING RIGHTS.— ..--——..-— B

" .SURFACE RIGHTS ONLY......................™. H

" .MINING RIGHTS ONLY...,—-...-..........,._. BLICENCE OF OCCUPATION .........,.,................™ TOROER-IN-COUNCIL ........M........................™. OCRESERVATION .................................^.....^. ©CANCELLED _........................................ ®

a. ft

SCALE: 1 INCH * 40 CHAINS

FEETO 1OOO 2OOO 4OOO 6OOO

200

MOO

O 2OOMETRES

1OOO11 KM)

2OOO? KM)

AREA

KAKAPITAM LAKEM.N.R. ADMINISTRATIVE DISTRICT

RED LAKEMINING DIVISION

RED LAKELAND TITLES/ REGISTRY DIVISION

KENORA/PATRICIA

Ministryof LandNatural, MIResources Branch

Or\tario

O it*FEBRUARY 16, 1983

G-1800

*1 1-p 4N 56IZ95 56)266

NDQJ67308Post 2 561285 PostB 561286

2.,*-dU,.SAN-B-T4

*3 56U6S 56U6H SAN-B-T1-82

•~ flBU. I^U VA-

NDUJ67294

0.4L-U67261 CANADIAN OCCIDENTAL PETROLEUM LTD

minerals division

PROJECT SANDY B" CLAIMS v

North Western Ontario District of Kenora(Patricia Portion)

Red Lake Mining DivisionN.I.S. 53 F/3

GEOLOGY and ROCK GEOCHEMISTRY

with 1982 TRENCHES

Quartz-feldspar porphyryPegmatite, apliteBiotite granodiorite, porptutritic biotit*granodiorite, biotite hornblende granodiorpink 'granite'Dacite PorphyryIron FormationVolcanic Groupla Andesite

Pillowed LavaBasaltAmphibolite zed DiabaseAmphiboliteHornblende SchistBiotite HornfelsTuff AgglomerateAcid Flow

brecciated

small she*r ; zone o f clove set fracture!

gossan

f*,PI mineral occurrence (Pyrrhotite, Pyrite)

direction of glacial striae

direction of tops of flows or strata

vein/stringer (Qtz-CaCO-j material)

Rock Geochemistry

rock sample location

area of outcrop

rock islets

postulated claim boundary

unlocated claim post

located claim post

unlocated witness claim post

located witness claim post

inferred fault SCALE 1=5 WO

schistosity, gneissosity,cleavage, foliation(hori sontal, inclined, vertical, dip unknown) Probably Anomalous

M 5-?OrniO-U BJ

attitudes of joints or fractures (vertical, inclined) KWL/ah/Dec.1981 revised: FWG/Dec. 82

tndicajes plunge)

ROCK GEOCHEMISTRY PROFILES

Ag As Auppm PPm.. Lio -i looo -| SOD i

900

800 -

700 -

600 -

500 -

400 -

300 -

200 -

100 -

o -

400 H

300 -\

200

loo H

MAGNETIC 'S? SUSCEPTIBILITY TO

60PROFILE K

202010

10 cgs units98765432l

Q9 0.80.7 0.6 0.50.40.30.2O.IO l T

-i———i———i———r T l T -\ l T

SAMPLE NUMBERS

i—^r

LEGEND

IF Iron Formationpo pyrrhotitepy pyritecp chalcopyriteqv quartz vein

CUD Outline of outcrop in trench

Fold with plunge direction f l Anticlinal, Synclinal axis *r "r with plunge direction

Bedding (vertical, inclined showing dip)

Schistosity (vertical, inclined showing dip)

Shear Zone

l Geological Contact l (defined, assumed)

/yf y

ROCK GEOCHEMISTRY PROFILES

Ag

10 -j

9 -

8 -

7 -

6

5

4 -

3 -

2

l

As-PEEL

1000

900

800

700

600

500

400

300 -

200 -

100 -

O

AuJ?El? '500

400 -

300 -

200 -J

100 -

MAGNETIC SUSCEPTIBILITY PROFILE

'-3 10 cgs units

10090807060504030 20 10 9 8 7 6 5 4 3 2

1.0 0.9 0.8 0.7 0.6 0.5 0.4 0.3 0.2 O.I O

X ———— X

LEGEND

IF Iron Formationpo pyrrhotitePV pyritecp chalcopyriteqv quartz vein

CUD Outline of outcrop in trench

A "r

X?

/

Fold with plunge direction Anticlinal, Synclinal axis with plunge direction

Bedding (vertical, inclined showing dip)

Schistosity (vertical, inclined showing dip)

*\AX**\AP Shear Zone

/ l Geological Contact l (defined, assumed)

Note-. Trench T2a ends 2m West of the 14 m mark of T2b

ROCK GEOCHEMISTRY PROFILES

Ag As Au ppm ppm ppb

10 -i 1000 i 500 -i

9 -

8 -

7 -

6 -

5 -

4 -

3 -

2 -

900 -

800 -

700 -

600 -

500 -

400 -

300 -

200 -

100

400 -

300 -

200 -

100 -

o J o

MAGNETIC SUSCEPTIBILITY PROFILE1009080706050403020109

10 cgs units

765432

1.00.90.80.70.60.50.40.30.2O.IO

SAMPLE NUMBERS^^tlO^ 1^ 00 ^^ CJ

CMfO CO CO

inCVI CM

N CJ

CO CO

enOJ

O - to ro

CMro ro

to roinro

to ro N

rooo ro ro O - oj ro in co o O in

PLAN SILICIFIEDCONTACT

Sandy

Lake

E O

PHYLLITE

QUARTZ - FELDSPARPORPHYRY

tr. py

— ' —

1

- — - —

IF* IF

VERVERY THINLY BEDDED, STRONGLY FOLDED IRON FORMATION

MASSIVE cp, W

E EO IT)

E O ID-U

IF popycpqv or QV

CZZ)

LEGEND

Iron Formation pyrrhotite pyritechalcopyrite quartz vein

Outline of outcrop in trench

Fold with plunge direction A i Anticlinal, Synclinal axis " "T" with plunge direction

Bedding {vertical, inclined showing dip)

Schistosity (vertical, inclined showing dip)

shear Zone

7 Geological Contact X (defined, assumed)

240

CANADIAN OCCIDENTAL PETROLEUM LTD. minerals division

PROJECT SANDY 'B' Claim Group

North Western Ontario N.T.S. 53 F/3

SAN 82-B-T3

50Scale 1:25

O 50 IOO ISO m

PLAN 5 FWG/sa/Nov. 1982

MOCK GEOCHEMISTRY PROFILECu Co Ni ppm ppm Ppm~" ' ~ 1000 T2000 -

1800 -

1600 -

1400 -

1200 -

1000 -

800 -

eoo -

400 -

200 -

o -

Ag ppm10

9

B

7

6

5

4

3

2

100 -

90 -

80 -

70 -

60 -

50 -

40 -

30 -

20 -

10 -

* O -

As"iooo"-

900 -

800 -

700 -

600 -

500 -

400 -

300 -

200 -

100 -

O -

900 -

800 -

700 -

600

500

400

300

200

100

O

Au "560""

Eo. o.

8

O O

a a

01 O)

l E 0,l S E '1 a Q.Il O Q-i

fO (O l

0 0

r—i

0 0 r

._j.-J ""i

F— i

400 -

300 -

200 -

100 -

lm o

—— —l 9 '

O. ' 4

^ i ^o. a.o- ! m

(O l —06 !-.*iL.

-. — .J

MAGNETIC SUSCEPTIBILITY PROFILE

10 cgs units

10090807060504030201098765432

1.0 0.9 Ofl 0.7 0.6 0.5 0.4 0.3

SAMPLE NUMBERS

in ro in in in intOin in

OD in01 m O - OJ

(Dro to to in to

tO ID *O

CO (O

O tO

PLAN

DACITE PORPHYRY

LEGEND

If Iron Formationpo pyrrhotitepy pyritecp chalcopyriteqv quartz vein

CUD Outline of outcrop in trench

Fold with plunge direction 4* i Anticlinal, Synclinal axis

/y- with plunge direction

•o* . ' Bedding (vertical, inclined

showing dip)

/ "91 Schistosity (vertical, r inclined showing dip)

shear Zone

/ f Geological Contact / (defined, assumed)

250

CANADIAN OCCIDENTAL PETROLEUM LTD. minerals division

PROJECT SANDY 'B' Claim Group

North Western Ontario N.T.S. 53 F/3

SAN 82-B-T4

Scale 1:253

50 50 IOO 150 m

PLAN 6 FWG/sa/Nov. 1982