REPORT ON GEOLOGICAL RECONNAISSANCE ......Keweenawan Rift beneath Lake Superior. The method of...

41K16NE0004 2 16289 MARNE 010

REPORT

ON

GEOLOGICAL RECONNAISSANCE, PROSPECTING,

LITHOGEOCHEMICAL SAMPLING, PETROGRAPHIC DESCRIPTIONS,

AND INTERPRETATION

OF THE

WOLFE LAKE PROPERTY

TUPPER, SHIELDS, ARCHIBALD, AND MARNE TOWNSHIPS

SAULT ST. MARIE MINING DIVISION, ONTARIO

NTS 41K/16

Wr1DtC -

aLANUb

Jon NorthWMC International Limited27 October 1995

SUMMARY

A linear, steeply-dipping quartz-chlorite-magnetite

ironstone approximately 5 m wide, trending 120 degrees, was

traced in outcrops for 4 km. In the area of the Pitch-Ore Copper

Occurrence at Wolfe Lake the ironstone contains accessory,

secondary silicate minerals in decreasing order of abundance:

quartz, chlorite, actinolite or hornblende, and epidote. The

secondary oxide and sulphide minerals are in decreasing order of

abundance: magnetite (up tc 7*), chalcopyrite (l to 2^), hematite

after magnetite, and trace native copper. The host rocks are

magnetite-rich gabbro of probable Proterozoic age in the

southwest and hematized red Archean basement gneiss in the

northeast.

Samples of mineralized ironstone at the Pitch-Ore occurrence

contain up to 12034 ppm Cu, 17 ppb Au, and 14. l 'k Fe. Elsewhere,

the ironstone contains up to 107 ppb Au and 10.1* Fe but it is

not enriched in Cu or other trace metals. The ironstone pinches

out or is very narrow northwest cf Wolfe Lake because it was not

discovered in outcrops or glacially-transported boulders. Because

of the narrow width and short strike length of the mineralized

part of the ironstone, ne further work is recommended.

11

41K16NEOOO* 2 16289 MARNE 01 OCTABLE OF C

page

SUMMARY...................................................... ii

TABLE OF CONTENTS............................................iii

LIST OF TABLES............ .. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . v

LIST OF FIGURES AND MAPS..... .. .... . .... .. . . . . . . . . . . . . . .. . . . . v

1.0 INTRODUCTION

1.1 Basis for exploration and objectives................ l

1.2 Property description................................ 4

1.3 Location and access....... . . . . . . . . . . . . . . . . . . . . . . . . . . 4

1.4 Summary of fieldwork and methods of exploration..... 6

1.5 History of mineral exploration in the area of

the Wolfe Lake Property..... . . . . . . . . . . . . . . . . . . .. . .. 8

2.0 GEOLOGY OF THE ARCHEAN, PROTEROZOIC, AND PHANEROZOIC

ROCKS IN THE EASTERN LAKE SUPERIOR AREA OF ONTARIO........... 11

2.1 Regional geology, tectonic setting, and age of

the Archean, Proterozoic, and Phanerozoic rocks..... 11

2.2 Regional magnetic and gravity anomalies............. 14

3.O GEOLOGY OF THE WOLFE LAKE PROPERTY..... . . . . . . . . . . . . . . . . . . 17

3.1 General statement................................... 17

3.2 Topography, Quaternary and Recent deposits.......... 18

3.3 Archean rocks and their distribution................ 18

3.4 Rocks of probable Proterozoic age and their

distribution........................................ 20

111

5 Folds and faults................................. . .. 21

3.5.1 General...................................... 21

3.5.2 Wolfe Lake Fault............................. 22

3.6 Metamorphism........................................ 23

3.7 Secondary hydrothermal mineral assemblages.......... 23

3.7.1 Property scale............................... 23

3.7.2 Pitch-Ore Copper Occurrence.................. 23

3.8 Abundances of copper and trace metals in rock

samples............................................. 27

3.8.1 Samples collected along reconnaissance

traverses.................................... 27

3.8.2 Pitch-Ore Copper Occurrence.................. 28

4.0 SYNOPSIS OF EVIDENCE FOR CU-AU ORE DEPOSIT MODEL......... 28

5.O CONCLUSIONS.............................................. 31

6.O RECOMMENDATIONS..... .. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 32

APPENDIX A: CERTIFICATE OF QUALIFICATIONS........ . . . . . . . . . . . . 33

APPENDIX B: ROCK SAMPLE DESCRIPTIONS..... . . . . . . . . . . . . . . . . . . . . 34

APPENDIX C: ROCK SAMPLE ANALYSES........ . .... . . .. . . . . . . . . . . . . 45

APPENDIX D: PETROGRAPHIC DESCRIPTIONS........................ 61

APPENDIX E: MISCELLANEOUS GEOCHEMICAL DATA FOR KEWEENAWAN

GRANITE........ . . . . . . . . . . ..... ........ .... . . . . . . . 64

REFERENCES.... . ... .... . .... . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 69

IV

page

LIST OF TABLES

Table 1: Cu-Au-Fe oxide deposit target ranking sheet......... 5

Table 2: Claim numbers and recording dates................... 6

Table 3: Summary of previous diamond drilling at the

Pitch-Ore Copper Occurrence......................... 9

Table 4: Comparison of Cu-Au deposits, porphyry Cu deposits,

epithermal Au deposits, and Wolfe Lake.............. 30

LIST OF FIGURES AND MAPS

Figure 1: Wolfe Lake Project location map and regional

tectonic setting................................... 2

Figure 2: Wolfe Lake Project claim map....................... 7

Figure 3: Geology of the Batchawana Bay area................. 12

Figure 4: Magnetic anomalies of the eastern Lake

Superior area.................................... . . 15

Figure 5: Gravity anomalies of the eastern Lake

Superior area...................................... 16

Figure 6: Geology of the Pitch-Ore Cu Occurrence with

drill collars from exploration in 1955............. 24

Figure 7: Rock sample plan of the Pitch-Ore Cu Occurrence.... 29

Map 1: Geology, and rock sample locations, Wolfe Lake

Property.................................(back of report)

1.0 INTRODUCTION

1.1 Basis for exploration and objectives

Area selection and targeting of the Wolfe Lake Property

(Figure 1) was done following an appraisal of i) regional geology

and tectonic setting, ii) nature and distribution of mineral

occurrences, and iii) regional metal endowment of the Lake

Superior area, viz:

i) Regional geology and tectonic setting

* east edge of the 1.1 Ga intracratonic Keweenawan Rift at

boundary with Archean basement rocks

* edge of circular positive gravity anomaly adjacent to the

long wavelength anomaly of the Keweenawan Rift

* annular magnetic anomaly with several radiating apophyses,

one of which is through the area of Wolfe Lake

* semi-circular topographic features in the area, ostensibly

remnants of Proterozoic ring faults

* near south edge of Kapuskasing structure

* lineaments parallel to the Kapuskasing structure offset

rocks of the Keweenawan Rift and form ENE-trending fault-

bounded blocks

ii) Nature and distribution of mineral occurrences

* Keweenawan (1.1 Ga) basalt-hosted Cu in chalcocite-calcite

veins, Coppercorp Mine, Mamainse Point, 849,547 tons, X.15%

Cu, .06 ppm Au, 8.33 ppm Ag.

* Keweenawan porphyry-associated Cu-Mo, Jogran Occurrence,

WMC Intern^rtto DmffedAmerica* Division — CxploraHon

WOLFE LAKE PROJECT

LOCATION MAP

O N T

3

Q.19% Cu and Q.05% Mo, no mineral inventory calculated

* Keweenawan breccia-hosted Cu-Ag-W-Mo-Au, Tribag Mine,

1,831,013 tons, 1.6^ Cu, ea. .01 ppm Au, 10.52 ppm Ag,

anomalous in W and Mo.

* Pitch-Ore Cu Occurrence at Wolfe Lake and others like it in

the eastern Lake Superior area, quartz with or without

calcite and magnetite in breccias and vein occurrences in

Archean granitoid rock and magnetite-rich gabbro of probable

Proterozoic age, Cu with minor Au

* Archean base and precious metal VMS and lode-type

occurrences, Batchawana Greenstone Belt

iii) Regional metal endowment

* Keweenawan Rift: 5 billion kg Cu in lower basaltic part of

Keweenawan Rift plus 6.6 billion kg Cu at White Pine Mine,

both at Keweenaw Penninsula, Michigan

* Keweenawan Rift: 400 million tons containing Q.2% Ni within

the Duluth Complex, Minnesota

* Lower Proterozoic Penokean orogen: Superior-Type iron

Formations in the Marquette Range Supergroup and Animikie

Group, the Negaunee Iron Formation alone in the Marquette

Range Supergroup has ea. 200 billion tons of reserved

taconite ore

* Archean Hemlo Gold Deposit, Ontario, 20 million contained

ounces

* Lower Proterozoic Sudbury basin, 1.648 billion tonnes at

X.2% Ni

4

Using information derived from the foregoing, a target

ranking sheet for the Wolfe Lake Property was completed (Table

1). Because of the high ranking of the area, it follows that it

is permissive for rift-related Cu-Au deposits, hence the

objective of this exploration is to discover a Proterozoic Cu-Au

deposit near the intracratonic Keweenawan Rift and, should the

metal concentration not be discovered in this exploration at

Wolfe Lake, understand the relationship between the Cu

concentration at Wolfe Lake and areas about Wolfe Lake vis a vis

WMC's general model for Cu-Au deposits in order to critically

assess this area for future exploration.

1.2 Property description

Thirteen claim units comprising 2 claims and 208 ha (Table

2) in Tupper and Shields Townships were optioned in November 1994

from R.H. Sutcliffe. The Pitch-Ore Copper Occurrence is exposed

in several trenches in the centre of these claims. In February

1995 WMC acquired 190 additional 16 ha claim units in 16 claims

surrounding the optioned claims in Tupper, Shields, Archibald,

and Marne Townships (Figure 2).

1.3 Location and access

The Property is at 46 : 52'N, 84" 15' W and is 40 km north of

Sault Ste. Marie, Ontario. Access to the property is by secondary

roads 7 km east of Trans Canada Highway 17, or 4 km west of the

Algoma Central Railway.

Table 2.

Claim

116346411634651163466116346711634681163469116347011634711163472116347311634741163475116347611634771163478116347911914651191466

Claim numbers and recording dates.

Units

81212168161681681616161642103

Area

128192192256128256256128256128256256256256643216048

(ha) Township Recording date

Shields 95/02/09Shields 95/02/09Shields 95/02/09Shields 95/02/09Marne 95/02/09Tupper 95/02/09Tupper 95/02/09Archibald 95/02/09Archibald 95/02/09Tupper 95/02/09Tupper 95/02/09Archibald 95/02/09Tupper 95/02/09Archibald 95/02/09Shields 95/03/06Tupper 95/03/06Tupper 93/10/07Shields 93/10/07

Total 203 3248

1.4 Summary of fieldwork and methods of exploration

Compilation of government magnetic and gravity data was done

to interpret the geophysical associated with the Cu occurrence at

Wolfe Lake. This compilation reveals that a 120 C magnetic linear

originating near Batchawana Bay of Lake Superior trends through

the Pitch-Ore Cu Occurrence and is also on the gradient of a

gravity anomaly adjacent to the long wavelength anomaly of the

Keweenawan Rift beneath Lake Superior.

The method of exploration was i) to examine and sample the rock

types and secondary minerals at the Pitch-Ore Cu Occurrence and

determine whether those rocks could explain the magnetic anomaly,

and ii) traverse across the magnetic anomaly and prospect the

rocks along the anomaly for extensions to that metal

ARCHIBALD

MARNE

UPPER SHIELDS

WMC INTERNATIONAL LIMITED

Wolfe Lake Project C.'cim MGD

8

concentration. Where there were no landmarks to establish

accurate location in the field, rock sample locations were

determined by Garmin Model 45 GPS with nominal precision of 50 m.

Sixty-one days were spent in the field by the following

personnel:

John Everest: student geologist May 9-19, and May 26 - June 5,

1995

Jon North: Project Geologist April 19-27, May 9-19, May 26 - June

5, Sept 14-21

Eighty-six rock samples were collected on reconaissance traverses

and analyzed for trace elements. Two samples were analyzed for

major oxides. Twenty-seven rock samples were collected in

trenches at the Pitch-Ore Cu Occurrence and analyzed for trace

elements. Three standard rocks were analyzed to monitor labratory

precision and accuracy.

1.5 History of mineral exploration in the area of the Wolfe Lake

Property

1955: Tupper 0012

Pitch-Ore Uranium Mines Limited report the logs of 11

diamond drill holes at Wolfe Lake, on what is now called the

Pitch-Ore Copper Occurrence (Table 3). The assessment report

includes the logs of holes l to 4, 8 to 10, and LI to L4, a total

of 665 m of AQ core drilling. The holes were drilled between July

and October 1955. Assays were not reported for LI to L4. The rock

types intersected in the holes were, arkose, quartzite, granite

breccia, granite, chloritized mafic intrusions, and amygdaloidal

basalt, all of which have variable amounts of carbonate, pyrite,

magnetite, hematite, uraninite, and chalcopyrite.

Table 3. Summary of previous diamond drilling at the Pitch-Ore Cu

Occurrence, Wolfe Lake Property. Note that holes 5, 6, 7 were

drilled on the same section.

ddh

fi

12

13

14

15

16

f7

#8

19

fioLI

to

L4

azimuth

192

192

192

148

192

12

192

192

192

no

assays

angle

-46

-46

-62

-45.5

-45

vert

-45

-45.5

-45

-46

from m

20.88

26.91

.58

0

0

0

0

15.24

67.88

7.62

to m

24.38

27.92

9.24

13.72

20.42

35.05

3.05

35.05

71.63

29.44

length

3.51

1.01

8.66

13.72

20.42

35.05

3.05

19.81

3.75

21.83

Cu \

.15

.82

.04

.08

.46

.88

.82

.23

.9

.37

other

Tr. Au

.OU Co

up to 1

g/ 1 Au

1956: Tupper 0010-El

This report, either by Pitch-Ore Uranium Mines Limited or

the Algoma Central Railway, describes the assays of the best

intersections in three drill holes at the Pitch-Ore Cu

10

Occurrence. Presumably these holes, numbered 5, 6, and 7 were

also drilled in 1955 (Table 3). There are no logs for the holes

in the Sault St. Marie MNDM files, hence the total metreage and

rock types are not known.

1955: Shields 0011-Bl.

Pitch-Ore Uranium Mines Limited reported the results of a

ground-based scintillometer and magnetometer survey and concluded

that there were no "radioactive deposits" at surface but that

uranium and minor copper is concentrated near a diorite or

diabase body approximately 60 m wide intruded by younger

granite. The uranium and copper is concentrated in areas where

the surrounding rocks are silicified, and have stringers of

magnetite and hematite.

1963: No file number

The total magnetic intensity of the area about Wolfe Lake

was measured and reported in the 1963 Geological Survey of Canada

airborne magnetic survey map for Searchmont 4Ik/l6 at a scale of

1:63,360.


The Ontario Gazette reported the cancellation of patented

claims WD 255 and WD 256 in Shields Township. There are no

reported records of exploration on these patents. It is likely

from the geology of the claims described below that they were

11

issued for iron exploration.


The geology of the property and area is illustrated in OGS

Map 2419 at 1:253,440 scale (Giblin and Leeahy 1976).

2.1 Regional geology and tectonic setting of the Archean,

Proterozoic, and Phanerozoic rocks

The main assemblages of supracrustal and related rocks and

their distribution in the eastern Lake Superior area are as

follows (Figure 3)(cf. Ontario Geological Survey 1991):

i) Archean: These rocks are widespread and include Neo- to

Mesoarchean gneissic tonalite, massive to foliated granite and

granodiorite with felsic to mafic volcanic greenstone belts,

notably the Batchawana Greenstone belt, part of the Abitibi

Subprovince of the Archean Superior Province

ii) Paleoproterozoic: layered siliciclastic rocks and minor ea.

2.2 Ga diabase intrusions of the Cobalt Group, the uppermost

subdivision of the Huronian Supergroup unconformably overly the

Archean basement rocks in a homoclinal south-facing succession

south of Batchawana Bay of Lake Superior.

iii) Mesoproterozoic: gently to steeply-dipping subareal basalt

flows and alluvial-fluvial conglomerate of the Osler Group and

unconformably overlying feldspathic sandstones of the Jacobsville

Group, all of the Keweenawan Supergroup, unconformably overly

both Archean basement rocks and rocks of the Cobalt Group. This

i r—i n i—i r—) f—n r—i r—] r—im r—i

ExplanationKcwwHWwan Ctastic S*cto

Kvwuvnuwan

Huronian Supergroup

ArctXMin Umruiuid Ruck*

Archtan

WMC Intoniahonal Limited

Geology of the BATCHAWANyVBAY AREA

13

west-facing sequence mainly crops out along the shoreline of Lake

Superior, hence the sequence is mostly covered by the lake,

iv) Cambrian to Ordovician siliciclastic and carbonate rocks of

the Michigan basin unconformably overly all of the Precambrian

rocks in a south-facing, gently dipping succession that subcrops

along the unconformity approximately at the U.S.A.-Canadian

border.

The sequence of events in the Lake Superior area is summarized as

follows:

* 2670 Ma: Abitibi Subprovince including the Batchawana

Greenstone Belt, end of orogenesis

* 2660 Ma: Kapuskasing Structure forms along transcurrent

fault

* 2450 Ma: northwest-trending Matachewan diabase dikes

* 2450-2200 Ma: deposition of the Huronian Supergoup on the

south margin of the Superior Province craton

* 2219 Ma Nipissing diabase dikes

* 2040 Ma: Kapuskasing diabase dikes

* Ring faults and 1537 Ma alkalai English Bay granite (in Lake

Nipigon)

* 1900 Ma: Dextral transpression, northwest over southeast

thrust faulting in Kapuskasing Structure

* 1885 Ma: Alkalic complexes (Cargill and Borden) in

Kapuskasing Structure, and uplift

* ea. 1220 Ma: northwest-trending Sudbury diabase dikes

14

* 1145-1015 Ma: Alkalic-carbonatite complexes into Kapuskasing

Structure

* ea. 1100 Ma: east-trending Marquette-Baraga County diabase

dikes

* 1109-1094 Ma: intrusion of Duluth and Coldwell complexes and

deposition of mainly volcanic rocks of the lower part of the

Keweenawan Supergroup into an intracratonic Rift

* *cl094 Ma: Deposition of the upper part Keweenawan

Supergroup/ fluviatile Copper Harbour Conglomerate and

Jacobsville Sandstone through erosional unroofing of

Keweenawan Rift flanks

* 1000 Ma: Grenville Orogeny

* Deposition of Paleozoic rocks of the Michigan Basin

2.2 Regional gravity and magnetic anomalies

Total magnetic intensity (Figure 4) is high relief and high

amplitude in the area of Batchewana Bay. Note that Wolfe Lake is

at UTM 711000 5194500. A short wavelength gravity anomaly

adjacent to the long wavelength anomaly of the Keweenawan Rift

(Figure 5) is surrounded by an annular magnetic anomaly. An

interpretation is that these coincident magnetic and gravity

anomalies are caused by a dense magnetic body, possibly a

Keweenawan intrusion in the area of Batchawana Bay.

17

3.0 GEOLOGY OF THE WOLFE LAKE PROPERTY

3.1 General statement

Most of the rocks exposed in the area of the property are

granitic gneiss and foliated to massive biotite-bearing granite,

and conventional wisdom (Giblin and Leahy 1976, Ontario

Geological Survey 1991) is that the area about Wolfe Lake is a

mass of felsic Archean basement rocks separating the Batchawana

greenstone belt in the north from the lower Proterozoic Cobalt

Group in the south. The pattern of topographic lineaments in the

area of Wolfe Lake is different from that in other areas where

they are northwest and northeast. At Wolfe Lake the linears are

east-trending and semi-circular concave to the west. Moreover the

area of granitic basement from Batchawana Bay for 100 km east,

including the area about Wolfe Lake, has numerous occurrences of

Cu, Ni-Cu, Mo-Cu, Pb-Zn-Ag, and minor Fe which other areas of

granitoid basement rocks in the Archean lack. Hence, either the

mapped geology of this area is subject to major revision, or

these metal concentrations have been superimposed on the Archean

basement complex by processes that are either not generally

extant in the Archean, or are Proterozoic. Given that the area is

proximal to the present edge of the lower Proterozoic Huronian

Supergroup and Upper Proterozoic Keweenawan Supergroup, and that

those kinds of metal concentrations are abundant in those rocks,

an interpretation is that they were superimposed on the basement

rocks during the Proterozoic.

18

3.2 Topography/ Quaternary and Recent deposits

The area about Batchawana Bay of Lake Superior at 184 ra ASL

is a rugged upland area with hills up to approximately 653 m ASL.

The uplands about Lake Superior are caused by residual uplift

within the "Lake Superior Swell" (Allen et al. 1991), a

manifestation of underplated juvenile crust beneath the

Keweenawan Rift which has not been completely unroofed. Wolfe

Lake, at 408 ra ASL is within the uplifted area with hills in the

area of the property up to 152 m above Wolfe Lake.

Quaternary deposits are mainly coarsely stratified to massive

sand and boulder till deposits and trough cross-bedded sand

several m thick. They are interpreted as ice-marginal Pleistocene

or Holocene deposits. Recent deposits are minor muskeg and grass

bogs. The area is thickly vegetated with mixed maple, beech,

birch, balsam, and pine forest.

3.3 Archean rocks and their distribution (Map 1)

Gneiss, Unit GUI: The most widespread rocks on the property are

cm-scale banded to massive, grey or pinkish-grey, fine to medium-

grained quartzo-feldspathic gneisses. An average modal

composition of these rocks is:

quartz: 40 to 50%

orthoclase plus plagioclase: 40 to 50%

biotite: l to 51

amphibole: trace to 5%

muscovite: trace to 2%

19

The gneissosity is defined by darker biotite layers, where

present. The composition of these rocks varies widely from

biotite and amphibole bearing to grey or white rocks with no

mafic minerals and trace disseminated fine-grained magnetite and

minor greenish muscovite.

Granite and pegmatite, Units GR and pgGR: Minor red to pink

hornblende-biotite or biotite-bearing foliated to massive granite

bodies crop out within the gneiss complex. Presumably these rocks

intruded the gneiss complex, however the margins of these

intrusions were not observed. The granite sometimes has cm- to

m-scale discordant, massive pegmatoidal to aplitic phases. The

pegmatoidal phases cut the basement gneiss and may occur without

association with granite. They are generally very coarse-grained

and sometimes have mm-scale miarolitic cavities. In one instance

(sample 103002, UTM 708526 5195675) a m-wide red pegmatite dike

intrudes the gneiss and is composed of interlocking potassic

feldspar and quartz with 5 to 7% disseminated, fine-grained

magnetite, and massive coarse-grained magnetite clots up to 5 cm

diameter.

Orthoquartzite, Unit MSq: A single outcrop (sample 103009, UTM

709043 5195755) of white, massive, poorly sorted orthoquartzite

crops out within the basement gneisses. The rock contains

amphibole-orthoclase segregations, hence it does not appear to be

part of the lower metamorphic grade Proterozoic rocks and may be

a supracrustal remnant of an Archean sedimentary sequence.

20

3.4 Rocks of probable Proterozoic age and their distribution

Diabase, Unit Md and Gabbro, Unit Mgb: Black to dark green, fine

grained, massive, m-scale dikes sometimes containing mm- to cm-

scale plagioclase phenocrysts, almost glomeroporphyritic in

places, 2 to 5% disseminated fine-grains and rare stringers of

magnetite.

Basalt, Unit MV: Basalt does not crop out on the property however

a few cm- to m-scale boulders of basalt were noted. They contain

secondary calcite, chlorite, hematite, and epidote in fractures

and hence are likely to be from the Keweenawan Supergroup.

Syenite Unit STq: A petrographic description, CIPW norm

calculation and mineralogical and geochemical discrimination of

this rock is in Appendices D and E. The rock is brick red granite

but was mapped as quartz syenite in the field. The unit crops out

in the northwest part of the property as a ea. 200 m diameter

intrusion in SSM 1163477. The rock is massive and medium-grained,

with 2 to 3% mm- to cm-scale miarolitic cavities. The texture of

the intergrown quartz and feldspar is granophyric or myrmekitic.

Because it has abundant miarolitic cavities however, the texture

is granophyric, caused by eutectic crystallization of the

feldspar and quartz. The "syenite" has a chilled margin against

the grey myrmekitic gneissic basement rocks, hence it is younger.

Because of rock type similarity between this undeforraed intrusion

and miarolitic-textured syenitic rocks in the Coldwell Alkaline

Complex, 260 km north-northwest, this unit is interpreted as a

Keweenawan-age intrusion. The approximate modal mineralogy of the

21

rock (cf. Appendix D and E) is:

K feldspar: eS-70% myrmekitic or granophyric texture with quartz

plagioclase: trace

free quartz grains: S-15%

amphibole: trace

chlorite: 5 to 7% pseudomorphous after disseminated fine- to

medium-grained amphibole

epidote: trace to 2 %, intergrown with chlorite

secondary oxides in miarolitic cavities: trace manganite,

hematite, and goethite as coatings

calcite: less than H.% disseminated irregular nun-scale masses and

fine disseminated grains.

The mean Na concentration of the rock calculated from INAA

analyses (nz !7) is 2.0(^ and the mean K concentration is S.72%

(n^7). The rocks contains <l% calcium. Sodium-rich sample 103042

with S.78% Na and Q.24% K is brecciated and hematized, evidence

that Na-metasomatisra post-dated crystallization of the syenite

and was attendant with brecciation.

3.5 Folds and Faults

3.5.1 General

Measurements of planar fabrics in dip/direction format are

as follows:

gneissosity: 70/345, 43/32080/158, 42/335, 70/333, 55/076

joints: 68/116, 84/144, 77/043, 47/1663, 80/030, 75/38, 88/78

fracture cleavage: 84/206, 75/086

22

Hence, the gneissosity of the Archean basement rocks trends

approximately 60 and dips moderately to steeply northwest.

There is no evidence from this limited dataset of cleavage and

joint measurements that a penetrative fabric is developed in the

rocks through folding.

3.5.2 Wolfe Lake Fault

The magnetic anomaly through Wolfe Lake originating near

Batchawana Bay is the most prominent geophysical linear in the

area. The rocks in the linear, including the Pitch-Ore Cu

Occurrence have abundant fractures and secondary hydrothermal

minerals (cf. description below; file Tupper 0012) with or

without preferred orientation. The fractured rock and secondary

hydrothermal mineral assemblage, including planar quartz

stockworks and banded parallel vein sets, interpreted as shear

veins were traced in outcrops and several measurements of the

attitude of the shear veins were collected. Planar fabric

measurements in dip/direction format are as follows:

85/016, 84/030, 68/026, 86/230, 82/230, 82/006, 77/043. Hence the

trend of the quartz-chlorite-magnetite rock is 106 to 140 and

dips steeply northeast or southwest. The rock usually dips to the

northeast in the northwest part of the property and dips

southwest in the southeast part of the property.

One observation of minor fold assymmetry with dextral

displacement was observed in the quartz-chlorite-magnetite rock.

23

3.6 Metamorphism

Archean basement gneiss is upper amphibolite to granulite

grade. Gabbro and diabase within the gneiss are not folded or

metamorphosed, except by retrograde metamorphism to chlorite.

3.7 Secondary hydrothermal mineral assemblages

3.7.1 Property scale

Widespread but minor cm-scale bands or veinlets of epidote,

quartz, and orthoclase are parallel or discordant to gneissosity

in basement rocks. There is minor epidote in gabbroic rocks.

A large area several 10'S of ra of myrmekitic granitic

pegmatite crops out along the south margin of the red granite in

claim 1163477. There is no penetrative planar fabric in the rock.

The myrmekitic granite (sample 103043) contains S.63% Na, nil Ca,

and Q.39% K, hence the texture of the rock could be caused by

late Na metasomatism either associated with the younger granite

or it could be caused by exsolution of albite and quartz from

anorthitic feldspar during Archean metamorphism of the rock.

Because the rock does not have a penetrative planar fabric the

former interpretation is the most logical.

3.7.2 Pitch-Ore Copper Occurrence (Figure 6)

Quartz-chlorite-magnetite rock: A petrographic description of a

sample of this rock is in Appendix D. This rock is at the contact

of red, massive to weakly foliated granite and fine-grained dark

green gabbro or diabase. The rock is a vein, vein breccia and

Wolfe Lake

SSM . SSM 1191465 i 1191466

711 711200 711300

519460C

5194500

-5194400

711400

LEGEND

A Boulder Sample x Rock Sample

^/~ Trench

—— Fault

— Shoreline

Geological Contact

Quartz-nagnetite-chlorite- chalcopyrite rock

WMC International LimitedAmerica) Dlvlilon - Exploration

Wolfe Lake P roperty Pitch—Ore Copper Occurrence

Geology

MTb M. ItM

KAUl 111400 PHI 4051

OMIl

PLUtl WtfM.Mg

25

partial replacement of the host rocks consisting primarily of:

vein quartz: 75 to 95% massive, clear, somewhat saccharoidal

chlorite: 3 to 25% dark green to emerald or blue green acicular

mm-scale clots and disseminated fine-grains, and massive nun-scale

fracture coatings

amphibole: trace to H brownish-green fine grains intergrown with

chlorite

pyrite: l to 3% fine-grains and disseminated stringers mainly

intergrown with chalcopyrite

chalcopyrite: trace to 3% disseminated fine-grains, stringers,

and mm-scale fracture-coatings, always intergrown with chlorite

magnetite: trace to 7% disseminated stringers and fine- to

medium-grains, and mm-scale fracture coatings with chlorite

hematite: trace to ea. 3% / always intergrown with and probably

pseudomorphous after magnetite and sulphide minerals

native copper: trace fine disseminated grains within quartz.

This body of rock has wide variation in the constituent minerals,

hence along the strike length the amount of Cu varies

considerably. The trend of the rock is 100" to 115 0 and the dip

is approximately 85 3 northeast. Southeast of the Pitch-Ore Cu

Occurrence this rock persists in approximately the same

stratigraphic relationship as at Wolfe Lake but with a thinner or

only intermittently intruded gabbro on the south side and massive

to weakly foliated biotite granite on the north side. In this

area the rock is more chloritic and more rich in magnetite (up to

, and contains up to l * disseminated pyrite but only trace

26

chalcopyrite.

Granitic host rock on north side of quartz-chlorite-magnetite

rock: This rock is exposed in trenches and shoreline outcrops on

the south side of Wolfe Lake where quartz-magnetite stockworks

trending 095 to 110 cut the granite. Five percent of the massive,

red granite is ram- to cm-scale massive magnetite veinlets with

mm-scale quartz selvages with or without minor chlorite. The

veinlets are spaced 10's of cm apart. Some of the veinlets are

quartz only veinlets with minor disseminated grains and clots of

magnetite. The magnetite within the stockworks sometimes has a

red streak because of intergrown pseudomorphs of hematite. Minor

massive cm-scale magnetite-granite-quartz clast cataclasite is

parallel to magnetite-quartz stockwork veins. Nearest the quartz-

chlorite-magnetite vein the rock is a medium brown, soft,

granular quartzofeldspathic, micaceous schist.

Gabbro host rock on south side of quartz-chlorite-magnetite rock:

Massive fine-grained to plagioclase-phyric with 2 to 5%

disseminated fine-grained magnetite, trace pyrite, and trace

chalcopyrite.

The quartz-chlorite-magnetite rock of the Pitch-Ore Cu

Occurrence has lower metamorphic grade than the country rock

gneiss. The attitude of the quartz-magnetite-chlorite rock is

discordant to other planar fabrics measured on the property. The

27

rocks have textural characteristics indicative of brittle failure

such as discordant vein stockworks, randomly oriented sulphide

and silicate fracture coatings, cataclasite, and quartz matrix

hydrothermal breccia. The presence of quartz shear veins is

evidence of ductile failure of the host rocks, but the lack of a

penetrative cleavage envelope about the quartz-chlorite-magnetite

rock is evidence that ductile failure of the rocks is a local

phenomenon and not part of a regional strain fabric imparted by,

for example, a compressional phase of orogenesis. Hence, the

quartz-chlorite-magnetite rock is interpreted as a secondary

hydrothermal mineral assemblage superimposed on older rocks

within a brittle fault.

3.8 Abundances of copper and trace metals in rock samples

(Appendix C) (Map 1)

3.8.1 Samples collected along reconnaissance traverses

Most of the samples anomalous in trace metals were collected from

the southeast part of the property along the Wolfe Lake fault,

within the quartz-chlorite-magnetite rock or adjacent rocks.

Sample 103056 of a quartz stockwork in diabase and granite

contains 18 ppb Au. Sample 103057 of a pseudobreccia with quartz

interclast material in basement gneiss contains 107 ppb Au, 4.4

ppm As, 24 ppm U, 134 ppm Cu, and 229 ppm Pb. The gabbroic dike

in the Wolfe Lake Fault contains up to 141 total iron within

disseminated magnetite and is the likely source rock for the

magnetite-rich veins and fracture coatings within the quartz-

28

chlorite-magnetite rock.

3.8.2 Pitch-Ore Copper Occurrence (Figure 7)

Most of the samples of quartz-chlorite-magnetite rock

collected at this mineral occurrence contained anomalous

concentrations of copper. Sample 103015 contains 1.2% copper

within chalcopyrite and native copper. All of the other samples

contain less than l * Cu and most of those contain less than Q.5%

Cu. Sample 103027 contains 17 ppb Au. The most iron-rich sample

is 103021 with 15.2 % Fe, and most of the other samples contain

less than 10% iron. Sample 103015 contains 27 ppm U and is the

most uraniferous sample from the mineral occurrence.

4.0 SYNOPSIS OF EVIENCE FOR CU-AU ORE DEPOSIT MODEL

Table 4 is a comparison of the mineral assemblage, water

composition, and tectonic setting of several types of Cu-Au

deposits. There is no critical geochemical data about the Wolfe

Lake Property, nevertheless the comparison is instructive to put

the main characteristics of the area about Wolfe Lake in

perspective with known deposits. The mineral assemblage mostly

contrasts with the deposit types in this comparison, however, if

one assumes that the hematite in the Pitch-Ore Cu Occurrence is

late and pseudomorphous after magnetite than there is a

1Q3102XGNI-c-o-bi

•1o3i05XGNl-qv-cp

l lil-ep ̂ 103020^x A

-5194500

-5194600

LEGEND

Boulder Sample Rock Sample

Trench

0 WMC International Limited Amcrlcas Dtvttlon - Exploration

Wolfe Lake Property

Pitch-Ore Copper Occurrence Rock Sample Plan

; COUNLIPl JN

DUrriOt TU

OATll Ort. IMS

SCAU: 1:2300

UVttXX: Hut, *e***.nt

31

paragenetic similarity to both Ernest Henry and Olympic Dam with

early magnetite-rich assemblages and late hematite-rich

assemblages. Because the Wolfe Lake Fault has characteristics of

brittle failure and is a quartz-chlorite-magnetite assemblage it

is different from Ernest Henry and Olympic Dam. The rocks

remotely resemble some quartz-rich magnetite ironstones in the

Mt. Isa Inlier (Ernest Henry) but the characteristics of brittle

failure indicate that the depth of formation was probably less

than Ernest Henry but not as shallow as Olympic Dam. Moreover,

the width of the linear zone of iron metasomatism at Wolfe Lake

is minor and contains only minor Cu and Au. Whether the local

iron enrichment is related to widespread regional iron

metasomatism, as at Olympic Dam and Ernest Henry, is not known.

Future property examinations and geological reconnaissance are

planned to evaluate this.

5.0 CONCLUSIONS

1. The Wolfe Lake Property covers 4 km of a brittle fault which

contains less than 5 m thickness of quartz-magnetite-chlorite

rock.

2. Within the quartz-magnetite-chlorite rock there is a 200 m

long segment enriched in Cu, and with anomalous but minor

concentrations of Au, Fe, and U.

3. Previous diamond drilling, and this exploration, indicate that

32

this Cu concentration is narrow and with minor strike length.

4. The mineral assemblage does not compare favourably with known

Cu-Au deposits, although there is minor paragenetic similarity in

the sequence of iron oxide formation.

6.0 RECOMMENDATIONS

Given the favourable target ranking of the Wolfe Lake

Property, the area about eastern Lake Superior should be further

evaluated for Cu-Au projects, however the Wolfe Lake Property

should not be explored further by WMC.

Respectfully submitted,

Jon NorthSenior Project GeologistWMC International Limited

33

APPENDIX A

CERTIFICATE OF QUALIFICATIONS

I, Jon North, of the City of Ottawa, Province of Ontario, hereby

certify that:

1. I am a geologist residing at 875 Dundee Ave, Ottawa, ON K2B

5T2.

2. I am a graduate of the University of Western Ontario with the

degree of B.Se. awarded in 1984, a graduate of Memorial

University of Newfoundland, with the degree of M.Se. awarded in

1988, and a graduate of the University of Western Ontario with

the degree of Ph.D. awarded in 1993.

3. My principal occupation since 1984 has been as a consulting

exploration geologist and researcher.

4. I ara a member of the Prospectors and Developers Association of

Canada, the Geological Society of Zambia, a Fellow of the

Geological Association of Canada, and a member of the Northern

Ontario Prospector's Association, as well as a Licenced Turkey

Hunter #019797 in the Province of Ontario.

5. I have been employed by WMC International since 1993.

6. l supervised and performed the technical work described

herein.

Jon North

Senior Project Geologist

34

APPEHDIX B

ROCK SAMPLE DESCRIPTIOHS

1. Rock savples collected at and near the Pitch-Ore Cu Occurrence

Battle Number

105 HO

103011

10301C

103013

1030H

103C15

103016

103017

103018

Location

Wolfe Lake Trenches

Wolfe Lake Trenches

Hoi f e Lake Trenches

Wolfe Lake Trenches

Wolfe Lake Trenches




Wolfe Lake Trenches

Description

Qnz-chlorite-amphibole vein in gabbro, fly

rock, 95 t vq, 3 - 5 ft clots of accicular

dark green chlorite. It diss py, .St diss

cpy, non magnetic

Qtz-chlorite-amphibole vein in gabbro, fly

rock, 95 t vq, 3-54 clots of accicular

dark green chlorite, sin to 103010 (f res: same

-rench), slightly more cp.

Hall rock to 103010 and 103011, dk greer.

anphibole-mt-chl schist, veinlets contain

wcg acicular to mass amph (hydrothermal?), 1

to 2 t diss vcg cubic py, magnetic (2-3S diss

mag)

Quartz w/ .5 to .75 t diss fg cpy, and 1 i

py, 2* diss rat associated w/ chl-act clc.s,

sim to 103010

similar to 103012,

silicified gabbro?, qt-chl-mt rock, 2 t cpy,

13 at, trace of native Cu, possible Cu5FaS4

p.ear cpy

punky qtz-feld-chl greissen-like rock wi-h

disseminated mt veinlets, tr py and cr cpy

silicified basement rock - brown, 70 to 30 t

granular qtz to rock w/ St mm size diss at,

and few cm size qtz-mt veinlets. .5 to 1 t py

in veins

silicified rock, qtz-chi-mt-py-cp, 2-3t py,

1-2 t cpy clots, 5 t dk green random chl

clots, few mt veinlets

35

103019

103020

103021

103022

103023

103024

103025

103026

103027

103028

103029

10303C

103031

103032

Wolfe Lake Trenches

Wolfe Lake - Trench 3

Hoi f e Lake - Trench 4

Wolfe Lake Trenches

Wolfe Lake - Trench 5,

Location 3, SW. end of

trench.

Wolfe Lake Trenches

Wolfe Lake Trenches

Wolfe Lake Trenches

Wolfe Lake Trenches

Wolfe La.ce Trenches

Wolfe Lake - outcrop

area S. of trer.ches

Wolfe Lake - shoreline

Wolfe Lake - shoreline

Wolfe Lake - island

sin to 103017, traces of diss py, more chl (~

5*)

Silicified fly rc-rk - sim to Trench 5,

Location 3, cpy < ^.

Chl/Amphibclite r^ck, < i i cpy occurs

within silica veins, magnetic

Qtz-chl-mt local fly rock w/ 3 to 5\ crs amph

clots, 1 % cpy, 2 t py.

Extremely silicified rock iaainly S1O2 with

mnr accicular mafic minerals) with pinkishH

hue (hem staining;, < 1 % cpy

SiO2 amphibollte-chic-rite rock w/ minor diss

mt, probably hydrcthermally alt 'd bsmt rock

or edge of gabbro, trace py t cpy

Qtz-magnetite^5%)-=^.l!2-3%: fly rock, trace

cpy .5 to 1*, diss py clots

Gabbro - magnetic, punk, local fly rock, 2-5

t; mm size qtz veins w/ tr sulphides

Qtz-magnetite(5t)-chl(3-5*: rock w/ .St py,

.51 cpy in diss crains, either a local or

distal fly rock

Gabbro - massive, punky, weathered brown,

magnetic, 5 to 10 i qtz-mt cm size veins,

trace sulphides

Gabbro float, fresh, mass, plag, amphibole,

cpx, 2 i fr. grained m.t, and probably some

qtz, tr py, tr cp, vfg

Silicified rsck, ;-z cO*, chl r-2% clots -

diss grains, mt - 5S diss mn size grains, py

.5t, cpy 14, hem.

Qtz-mt stockwork causing cx'n of red granite,

5-10 t mt associated w/ chl.

Basement banded gneiss, gry to pinkish gry,

stockwork of mt (- hexi ~- to mm size

ve inlets , 3tz veinlets

36

103033

103034

103101

103102

103103

103104

103105

Wolfe Lake - island

Wolfe Lake - island

Wolfe Lake - Trench 6,

Location - 1





1/2 ways up trench on M.

side

gneissic basement rock, red, silicified, very

sugary, .5 % diss ait, tr py.

basement gneiss, red, massive, silicified, 1

i diss fg rat, diss fg cbl

Silicified rock (from outcrop) with mr.r

jccicular mafic minerals (chl/hbld*. . Mnr :py

and py (.5 tol i)

.-jnphibolite fly rock, amphibole/ chl - x- rut

by barren qtz veins, nmr bornite (-c.5%)

Silicified fly rock w/ accicular cr.l grains,

?C* Si02, 10 * mafic (cbl), .5 to 1 % cpy

Silicified fly rock w/ accicular cr.l grains,

*C4 Si02, 20 % mafic (chl), nnr malachite

staining, .5 to l% cpy and bornite.

Amphibolite from outcrop cut by qt: veins (30

- 401 of specimen!, cpy occurs ir. veins and

matrix (.5 to li)

2. Samples collected alone reconnaissance traverses

103001

103002

103003

103004

103005

103006

S. if road near Wolfe

Lake. Traversing across

mag anomaly.

JIM: 708526, 5195675

see nap

UTM: 701900, 5154395

ri. side of road, H. end

of small gabbro outcrop

UTM: 708644, 5196052

UTM: 708792, 5196352

Red biotite/hrnblnd granite w/ significant

hematite-epidote-quartz alteration.. . 5 10 1

* hematite clots. Myrmekitic textr. prel

fdspr grains - appear zoned from Ka ~o K rich

(Rapakivi?)

Mass fg-cg red biotite-hornblende srainite

dyke w/ 5t magnetite {clots and diss grains).

Pegmatite - 80*k-spar, 20 l quartz, trace

biotite. Mn3O4 coating. Pegnatite ur.de f c med

Gabbro - lots of nur. size hematite coated

fractures, sometimes almost to a bx, epidote

rrm size in fracture.

Granite float - red, k-spar-hbld-mr.t-chl 1 to

2 1 diss fg mt

Gabrro/basalt float - totally alt's to CaCO3

- chl - hem - cp. Resembles Coppercorp rock.

37

103007

1O300S

103009

103035

103036

10303?

103038

103039

103040

103041

103042

103043

103044

103045

UTM: 708831, 5795761

see map

UTM: 709043. 51957=5

Traverse S. W. of Wolfe

T

Traverse S. H. of Wolfe

L.

Traverse S. M. of Hoi f e

L.

no sample collected

Traverse S. H. of Wolfe

L.

Traverse in N.W. corner

of the claim.

UTM: 706150, 5196054

Traverse in N.H. corner

of the claim.

Traverse in N.H. ccrr.er

of the claim.

Traverse in H. W. corr.er

of the claim.

Traverse in N.H. corr.er

of the claim.

Traverse in S. E. corner

of property around ;lc

patented claims.

Alaskite - mass, white, qtz - 40*, alb - 401,

greenish muscovite - 20 t

Gabbro - chloritized, 3 - 5 * diss fg mn:, 3t

vcg pyrite cubes, hematite fractures. Reck

ippears to be Keweenawan diabase -

chloritized and hematized

quartzite - white to buff green, sericitic.

gabbro dike in grey gneiss, sugary texture

with 54 diss mt, 21 qtz-mt veinlets, very

xuch like the altered gabbro at Wolfe Lake Cu

occurrence

5 at thick magnetic diabase dike, red granite

he st rock somewhat brecciated, trace azurite

stain, tr py and cpy in wall rock breccia

> 5 m angular float of grey gneiss intruded

by m-scale miarolitic aplitic granite dike

with 3t diss mt in stringers and fractures

Gabbro - massive, magnetic, specularite ir.

fractures, and minor hematite, also possible

Mn3O4 coating

Red Granite - brick red K-spar (albite? )-

rhlorite-qtz rock, qtz and Mn3O4 in

miariolites, non magnetic

Red Granite - excellent red miariolitic

Brecciated Red Granite ( Float in river) w/

broken quartz grains, hematite

Granite - myrmekitic, quartz stockwork, very

coarse pegmatitic texture

cobble of red eg feldspar rock with 15*

ir.-erclast quatz-biotite, albite? breccia

Gabbro - chlorite schist w/ disseminated

magnetite (-10*). Outcrop contains qtz-

chlorite-mt-py veins.

38

103046 Traverse in S-E. corner

of property around old

pater.-ed claims.

Qtz (80*)-Magnetite (20*) vein associated

with gabbro.

103047 Traverse in S.E. corner


patented claims.

Qtz (801)-Magnetite (20*) vein associated

wich gabbro. Pyrite .5 to It fg ~o sg

d i sseminated.


of prrperty around old

patented claims.

Qtz-magnetite veins on the edge of foliated

gabbro.Stockwork is Qtz (30*) - Chi (60*; -

Magnetite (10*).



patented claims.

Qtz-magnetite veins on the edge of quartz

stockwork exposed DO ridge. Stockwork is Qtz

- Chl - Magnetite. Similar to 153047 but

niore chlorite. Trace of pyrite.

103050 Traverse -in S. E. corner


patented claims.

Qtz-Magnetite-Chlorite stockwork an E. side

cf mt gabbro. Gabbro is very punky w/ red

goethite where mn size py grains are present

and oxidized. 5-10* mt, 30-40* qz springers

md veins, .5-1* py, 50* chlorite.



patented claims.

Hagnetite-Qtz-Chl stockwork in fractured pink

granite. Trace py.



paten-ed claims.

Gabbro - very coarse grained, porphyritic,

magnetic. Trace Py in chl qtz veinlets.

Probably the tail end of the stockwork.


of prrperty around old

patented claims.

Qtz-Mt-Chl stockwork on ridge. Veir. q-jartz

"54 (sugary), magnetite grains and veinlets

(5-7*), Chlorite !IO-15*I. Trace pyrite

disseminated throughout.


of property arcund old

patented claims.

Bleached Silicified, white, intrusive rock.

Ne mafic minerals. Hematitic fractures are

common.



patented claims.

Granite and Gneiss - red/grey w/ enclaves of

fine grain dark green amphibolite and miner

magnetic diabase all with a qtz st

no magnetite noted

39

103057

103058

103059

103060

103061

103062

103063

103064

103O65

103066

103061

103068

103069

103070

103071

103072

Traverse in 3. E. -romer

of property arc-jnd old

patented claims.


of property ar-und old

patented claims.

Traverse in c. E. corner

of p-roper*y arc-rid old

patentee rlaims.



patented .claims.

Traverse from Kclfe Lake

to Prugh Lake area

Traverse from Viel f e Lake

to Prugh Lake area


to Prugh Lake area


tc Prugh Lake area

Standard

Standard

Standard

west of Kclfe lake

west of /Sol f e Lake

west of Hoi f e Lake

UTM 7103-S3 5196664

west of Molfe Lake

Pseudo Breccia - forr.ed by quartz stockwork

in basement gneiss ; 1 i , non magnetic, w/ chl-

carb. 75% vein quartz w/ trace pyrite.

Trace malachite after cpy?7

Pseudo breccia - qtz - Kspar rock. Similar

to 103057. 80* vein quartz, 20* flesh

coloured red Kspar, OS rhlorite.

Stockwork (S. W. edge; i r. hbld-biot granite of

the basement complex., - 5* fine qtz veinlets

w/ cbl salvages. Trace py, some hematite

stain.

Basement Granitic Gneiss - weak to moderately

chloritized, 54 qtz veins, reddish feldspar -

hem alt'n, no sulphides.

Biotite - Qtz - Feldspar pink gneiss.

Grey/pink gneiss along linear EN. of

linear???). Some reddining due to alt'n.

Gabbro float. Meter scale. Chloritized,

magneticw/ few qtz veins on a mm scale.

Minor diss biotite. Locks like S. side of

qtz-mt stockwork.

Gabbro - Strongly magnetic, foliated, looks a

little like fault breccia, 1* diss py, edge

of qz-mt stockwork if present.

HR - 8

HR - 8

HR - 9

basalt or fine-grained gabbro, chlorite and

hematite in late fractures

silicified granitic gneiss, 70* qtz flooding

pink mg granitic gneiss, minor amphlbolitic

segregations

massive pink mg gneiss

massive mg gabbro, minor chl

40

103073

1C3074

103075

105106

103107

103108

103103

103110

103111

103112

103113

103114

103115

SE part of property

Keweenawan syenite, NH

part of property

Keweenawan syenite, NH

part of property

no sample collected

no sample collected

Traverse across mag

anomaly, H. of Wolfe L.

See nap.

Traverse across mag

anomaly, M. of Wolfe L.

See map. *

Traverse across mag

anomaly, H. of Wolfe L.

See map.

Traverse in S. W. corner

of the claim block


of the claim block


of the claim block


of the claim block.

UTM : 705426, 5197496


of the claim block.

60* qtz, 30% kspar, 10* biotite in weakly

foliated Archean granite

syenite, for whole rock analysis and thin

se-rtion

syenite, for whole rock analysis and thin

section

7rey gneiss w/ pink hue (hem staining)

Gabbro - fn grained, magnetic in sections

Alaskite - white, 50 % qtz, 50 * albite

Silica - white, cloudy, massive, barren.

Minor chl in fractures.

Grey Gneiss? Amphibole and chlorite "^.

feldspar 30i.

Grey Gneiss, fine grain, granitic, pink

cculour, hematite staining along fractures.

Feldspar-quartz-biotite, weak foliation

Red Granite - brick red colour due to

recurrence of k-spar (hematizec albite?)

3=4, quartz 5t, raafics 5t, miarolitic

cavities

Se- Granite - brick red colour due to

occurrence of k-spar (hematized albite?)

?C*, 10 t mafic minerals - amphibole?, non

magnetic, meti grain

41

103116 Traverse in X.K. romer

of the claim tiers.


occurrence of k-spar (hecatizec albite?)

50*, quartz 5*, mafics 5*. encrusting of Mn

on surface due to occurrence at sod-bedrock

interface.

10311-; Traverse in N.N. romer

of the claim clcr:-:. At

intersection :f ::. claim

line and nor'h -rending

road.

Red Granite - brick red colour cue to

occurrence of k-spar (herr.atizec albite?)

30*, quart; 101, mafic minerals 10 %

103118 Traverse in N.W. romer

of the claim i:'----: along

north trending rr ad.

UTM: 7059(00, 513-196

Red Granite - brick red colour cue to

occurrence of k-spar (hecatized albite?)

60*, quartz 5%, mafic minerals 5*. Mafic

minerals are greenish in colour, possibly

chlorite. Miarolitic cavi.ies.

103119 Traverse in H.W. romer

of the claim tl^r:-: along

north trending read.

UTM: 706035, 5196=2-

Red Granite - brick red cciour due to

occurrence of k-spar {hecatizec albite?).

Rock is somewhat rotted; difficult to

determine mineral proportions.

103120 Traverse in H. 3*. romer

of the claim tlcCfC along

north trending r:ad.

UTM: 706000, clSe'SO


occurrence of k-spar (heeatized albite?)

95t, quartz S-7%, mafic minerals 5-7*,

somewhat rotted.

103121 Traverse ir. K.S. romer

of the claim t ice/: along

north trending r:3d.

UTM: -06085, 51r656~

Red Granite - brick red cclcur cue to

occurrence of k-spar (hematizec albite?)

-35*, quartz St, mafic minerals 10*.

103122 Traverse in S.S. romer

of the claim clcc.-c.

From sane cutcrrc 35

103112, bu^ 30 T. - c, -he

south.

Grey Gneiss? Greenish colour due to

occurrence of greenish feldpar - 90 *, quart:

10 *.

103123 North/south traverse in

N.E. corner of nr.e claim

block

Grey Gneiss - reddish colour (hematized),

non-magnetic

42

103124 Traverse on old patented

claiir-5 - east side of

claim blocic.

Gabbro - 70*amphibole, 30 % feldspar, dark

green colour, slightly magnetic very coreact,

no sulfides.


claims - east side of

claim clock.

Gneissic rock - strongly silicified and

henatized, some magnetite,. Hematite occurs

as disseminated grains (1-2*1 and within }tz

veins. No sulfides

103126 Traverse on i-ld patented

clairvs - east side of

claim clock.

Gabbro - chloritic, schistose, dark greer., 2

- 3* pyrite, 5-10 * quart:, 904

chiorite/amphibole, magnetic



claim block along the

Gabbro ridge.

Gabbro - fine grained, chlorite/amphibole

95*,

jaec green, magnetite - finely disseminated

throughout and as coatings along foliation

planes (5*), pyritel-2% w/ some euhedral

grains up to l cm in size.

103128 Traverse en old patented



gabbro ridge. Lower on

ridge -han 103127.

Gabbro - silicified, 704 silica, 30t

chloritic schist, the chloritic schist part

of the sample contains 2C - 30* silica and 1-

2* pyrite, magnetite is extremely sparse.

Silicate portion of rock contains chlorite

filled fractures containing pyri.e. Silica

is devoid of pyrite



claim t ice le along the

gabbrc ridge. Higher on

ridge tS-.an 103128.

Gabbro - Chloritic schist containing - 1C%

euhedral to subhedral magnetite i. 5 to 2 rtn).

Minor pyrite wichir. fractures.




gabbro ridge.

Gabbro - similar tc 103130. 5 to 10*

magnetite in a chloritic schist, minor

sulphides along fractures.


claias - east side of


gabbrc ridge.

Gabbro - chloritic schist w/ 1-2 4 pyrite

within gound mass. Magnetite is disseminated

as very fine grains throughout.

43


claims - cass side of


gabbro ridge.

Gabbro - chloritic schist with 2-5* pyrite,

2-5* magnetite disseminated throughout, dark

areen

103133 Traverse or. -Id



gabbro ridge.

Gabbro - fine grained, chl/anphibole,

magnetite disseminated throughout

103134 Traverse in N.W. corner

of the claim block

UTM: 706415, 5136844


nematized albite(k-spar?), miarolitic quartz

and feldspar lined cavities, quartz 10%,

feldspar 804, mafic minerals 10*.

103135 Traverse in M.W. corner

of the claim block.

UTM: 706170, 5196956


hematized aibite(k-spar?), miarolitic quartz

and feldspar lined cavities, quartz 10*,

feldspar 9C*, mafic minerals 10*.

103136 Traverse in M. W. corner

of the claim block alrr.g

north trending road.

UTM: 706080, 5196490


hematized albite(k-spar?), quartz 10*,

feldspar 80*, mafic minerals 10*.

103137 Traverse in M.H. corner

of the claim block along



hematized albite(k-spar?), quartz St,

feldspar 30*, mafic minerals including

epidote 15%.

103138 Traverse in N.H. corner

of the claim block alrr.-g


UTM: 7O623O, 519601O


hematized albitelk-spar?), quartz 2-5*,

feldspar 85*, mafic minerals 12*.

103139 Traverse in I.'.W. corner

of the claix block alrr.a

north trendir.g road.

Red Grar.ize - brick red colour due to

hematized albite(k-spar?), quartz 2-5*,

feldspar 35*, mafic minerals 12*, fine

grained, along contact with white granitic

rock.

44




UTM: 706075, 5195970

White Granite - consist dominantly of a white

feldspar, no quartz.




White Granite - quartz and feldspar w/ some

pink colouration (hematite) along fractures

and minor hematite in matrix.




Gabbro - medium grain size, dark green, 6C3

amphibole, 40* feldspar, slightly magnetic.




Pegmatite - minor myrmekitic textures, red

colouration due to multiple fine hematite

fractures, cuts through grey gneiss.

103144 Traverse -in N.W. corner



Granitic rock (pegmatite) - coarse grained,

quartz looks shocked. Quartz 35%, K-spar -

55*, mafics 10*.

45

APPENDIX C

ROCK SAMPLE ANALYSES

Activation Laboratories Ltd. Work Order: 8286 Report: 8167

Sanpln description

103001103002103003103004103005

103006103007103006103009

AUPPB

3c2rtrt3

3rtrtrt

AC

PPH

cScSc5cSCS

cb<5<5cS

ASPPH

cO.5CO. 5cO.50.9

CO. 5

cO.5cO.bcO.SCO. 5

BAPPH

270250280c50

4400

100CSO70

170

BRPPH

cO.5

CO. 5i.e

CO.!)CO. 5

cO.5cO.SCO. 51.3

CAt

1cici62

2ci11

COPPH

33

ci243

2ci382

CRPPH

10

12ci100cS

11114613

CSPPH

2cicici1

1ci3

ci

FE1

1.235.8b0.527.292.43

0.960.2418.80.89

HFPPH

23323

2ci72

IIGPPM

cicicicici

cicicici

IRPPB

cbcSc5cbcS

cbcScSc5

HOPPH

ci22

ci1

cici7

ci

NAt

3.774.873.491.212.36

3.944.761.404.07

HIPPM

c20c21c20C20c20

c20C20C20C20

RBPPM

445693

CISISO

elbCIS33

CIS

SBPPM

cO.lcO.lcO.lcO.lCO.l

0.2cO.lcO.lCO.l

sePPH

1.63.81.3

311.6

1.72.8

382.5

SEPPH

c3c3c3c3c3

c3c3c3c3

SN

PPH

clOOclOOclOOclOOClOO

clOOclOOclOOClOO

SRPPH

cbOOCSOOcSOOCSOO1800

cbOOcSOOCSOOcSOO

TAPPH

1.2CO. S2.9cO.SCO. S

1.2CO.S1.2

CO.S

THPPH

4.23.88.21.08.0

S.O0.94.23.0


Sample description

103001 103002103003103004103005

103006103007103008103009

U PPH

9.45.81.62.2

2.740.52.61.7

H ZN PPH PPH

41 c50ci 4504 1 450ci 119ci 450

ci cSOci 4502 4bO

ci c50

1A PPM

8.6 3.12.19.6

73

8.840.55.0

11

CB PPM

18 76

21180

1301917

ND PPM

6

c51090

* 5c59B

SH

PPH

0.8 0.30.71.9

16

0.9cO.l3.01.1

EU PPH

0.3 ^0.2cO.21.04.8

0.3 CO. 21.10.3

TD PPH

cO.5 40.540.540.51.1

40.540.540.540.5

YB PPH

0.3 0.91.22.21.0

0.540.26.40.7

LU PPM

0.06 0.100.190.370.18

0.08cO.051.310.10

HlBl

9

30.23 26.8229.4034.1230.24

27.5928.1035.1032.26

Activation Laboratories Ltd. Work Order: 8286 Report: 8167B

Sanpl* description CUDDU

103001103002103003103004103005

103006103007103008103009

4.10.e.

110.4.

9.2.

180.3.

PB PPM

11.13.21.11.27.

10.13.5.

18.

ZN AC HI PPM PPM PPM

17. -cO.20. -CO.3. *:0.

62. 4:0.37. *0.

11. -CO.2. *0.

26. <0.9. 4:0.

3.10.4.

41.3.

7.IS.45.9.

MN PPM

113.140.52.

1029.568.

175.110.268.75.

SRPPMrrn

278.119.41.

315.1604.

127.36.78.

430.

CD PPM

4:0.5 CO. S :0.5^jQ f J

*iO * S

40.540.540.5<0.5

DI V PPM PPM

<S. 17.45. 35.45. 2.45. 222.<5. 59.

45. 11.45. 2.<5. 253.<5. 20.

CA

1

0.920.380.216.241.65

2.740.110.951.47

P

0.0260.0350.0020.0380.072

0.0140.0050.1610.039

MG

0.440.450.032.790.50

0.531.875.280.40

TI

0.120.120.010.520.41

0.050.010.880.15

XL

6.697.366.627.668.71

6.236.459.356.93

K

1.330.774.060.317.18

0.510.040.230.45

YPPM

2.6.7.

22.28.

5.2.

43.7.

BE PPM

rt.rt.2.

rt.rt.

rt.rt.rt.2.


bvmpl* description

103036 103037103039103040103041

103042 103043103044103043103046

103047103048103049103050103051

1030S2103053103054103055103056

103057103058103059J03060103061

1030621030631030641030f5~110306. l ^

103067 J103fiT~103112103113103114

103115103116103117103118103119

103120103121103122103123103124

AU PPB

42

42424242

4 ri42

rt42

rtrtrtrt25

42

42

42

42

18

10742

4242

42

422

422399

14502

42

42

42

42

42

4242

42

42

4242

42

s

AC

PPM

45

45

45

45

45

45

45

45

45

45

45

45

4b4545

45

45454545

45

45

45

4545

45

45

645

45

45

45

45

4545

45

45

45

4545

45

454b4545

ASPPM

1.2 40.51.71.40.7

40.5 40.540.540.540.5

40.540.540.52.1

40.5

40.540.50.8

40.52.2

4.440.540.540.540.5

40.540.540.55555

38040.540.540.540.5

40.540.540.540.540.5

1.20.80.91.3

40.5

BA PPH

340 1500510

1200880

82

190450450

450160450450450

24045045080

270

150ISO95

390260

350190190490540

450450530580970

8701100620910810

880850180670370

BR PPH

40.5 2.440.540.51.5

40.5

1.40.6

40.5

0.940.540.540.540.5

40.540.540.540.540.5

40.540.540.50.7

40.5

40.540.540.540.540.5

40.540.540.540.540.5

1.82.11.2

40.51.1

40.540.50.6

40.540.5

CA t

3 23

41

41

41

41

41

41

41

41

4l

41

41

41

41

41

41

2

41

41

4l

441

41

41

41

41

41

41

41

41

2

41

41

41

41

41

41

41

41

41

41

6

CO PPH

13 2

4212

11

71317

e38324337

829616

1146

1641

1

234411

41

41

441

12

411

41

113

41

43

CR PPH

21 101976

13

181538

2050828234

7853225

17

318

22509

740

1305

45

45

17131245

66

45

45

7

109

157

30

CS PPH

3 2S22

4l

41

41

4l

41

41

4l

41

41

4l

1

41

41

1

241

41

1

1

241

41

1

41

441

1

22

2311

41

21

41

341

FS t

2.59 1.12

11.62.311.94

3.750.70 3.192.694.29

2.438.409.81

10.17.22

2.029.903.340.331.21

2.351.651.254.720.75

0.715.40

12.60.510.49

0.950.241.441.602.01

2.061.771.871.842.51

2.062.071.020.9710.0

HP PPH

4 349

10

61 7

41

41

41

1

2

22

24

41

44

41

241

23

32344

154l

429

HG PPH

41

4l

41

4l

41

41

41

41

41

41

41

41

41

41

4l

41

41

41

41

41

41

41

41

41

41

41

41

41

41

41

9

4l

41

41

41

41

41

4141

41

41

41

41

41

41

IR

PPB

45

45

45

45

45

45

45

454545

4545

45

4545

454545

4545

45

4545

4545

4545

454545

45

45

4545

45

4545

4545

45

45

45

454545

MO PPM

41

41

41

41

41

41

341

41

4

21

41

41

41

41

41

341

41

41

341

4141

41

41

41

241

4l

1

4l

41

41

41

41

41

41

41

41

41

41

41

41

NA t

2.86 4.862.161.801.34

3.78 3.633.010.070.50

0.370.810.951.180.61

3.492.420.075.393.27

0.033.990.560.712.01

2.170.802.810.510.52

0.020.052.982.951.89

1.971.652.061.841.69

1.301.943.992.071.81

NI PPH

426 430431

421

420

426 424425420420

420420420421420

42211043

425421

420422420420420

420420424420420

42042068

420420

420420420420420

420420420420420

RB PPH

87 SI75

150140

27 38se

415415

415415415

31415

415415

415 US100

34415

34140190

17042386654

304155564140

110150110110140

15014041516062

SB PPM

40.1

40.1

0.240.1

0.2

40.1

40.1

40.1

0.10.1

0.140.1

40.1

0.140.1

40.1

0.340.1

40.1

0.2

0.340.1

40.1

0.20.1

40.1

40.1

40.1

1616

7340.1

40.1

40.140.1

40.1

0.240.10.240.1

0.10.2

40.140.140.1

sePPM

5.5 1.5

343.53.5

5.7 0.93.83.17.1

4.516

22196.7

8.8295.32.93.4

6.31.01.7

162.0

2.117351.11.0

3.10.41.91.83.0

3.42.92.93.03.2

3.03.14.71.6

34

SE PPM

43

43

rtrtrt

rt43

433

43

43

43

4343

43

4343

43

43

43

43

43

43

43

43

43

43

43

343

1643

43

4343

43

43

34343

43

43

4343

43

SN PPH

4100 41004100

41004100

41004100

410041004100

41004100

410041004100

4100

4100

4100

41004100

41004100

41004100

4100

4100

4100

4100

4100

4100

41004100

4100

41004100

4100

4100

41004100

4100

41004100

4100

41004100

SR PPM

4500 4500450045004500

4500 4500450045004500

45004500450045004500

45004500450045004500

45004500450045004500

45004500450045004500

45004500450045004500

45004500450045004500

45004500450045004500

TA PPM

2.440.540.52.62.0

40.5 40.52.4

40.540.5

40.540.540.540.51.1

40.540.540.53.6

40.5

40.540.540.540.540.5

4.140.540.51.11.1

3.040.540.540.51.7

1.81.92.21.92.6

2.72.21.31.7

40.5

TB PPM

4.0 2.23.9

2322

204.6

280.60.5

0.31.01.41.31.1

3.54.40.69.99.8

0.81.51.12.0

24

201.82.29.29.3

301.25.91.6

20

2319191920

19214.4

333.0


Sample description

10312* 103126103127103128103129

103130103131103132103133103134

10313510313610313710313810313*

103140103141103142103143103144

AU PPB

rt 3

e2rtrt

rtrt3

rtrt

rtrtrtrtrt

2rt3

rt3

AC PPN

cb

00CbeS

ebebOeSeS

<Se5eb<5<5

C5

ebeb<5eb

ASPPM

0.9 eO.SCO. b<0.50.8

eO.S<0.5<0.5<0.5eO.S

<0.5CO.S

CO. 51.60.8

CO. b1.7

CO.5

0.9<0.5

BA

PPM

<!>0 <SOeso<SO<50

<50<50CSO

<SO1100

9601200960

1200610

290260400200250

BR PPM

1.2 CO. 5 cd. 50.62.0

eO.bCO. b<0.5<0.5<0.5

1.9 CO. 5cO.S<O.S1.0

3.2.

CO.

<0.<0.

CA1

el ci<lel<l

<lcici2

ci

cicicicici

elci6

cici

CO PPH

428309

38

243339372

Sci2

cici

cici38cici

CR PPH

14 879018

100

12086

10095e

c*8

c55

10

eb9

441010

CS PPH

ci cicicici

2cicicici

22

ci31

22

rt22

FE t

4.11 11.314.02.19

12.1

4.7313.613.910.82.57

2.072.332.462.221.54

0.350.5112.30.480.48

HP PPH

1 23

ci2

3333

10

1011101112

335

ci3

HG PPM

ciCi

cicici

cicicicici

cicicicici

cicicicici

IR PPB

c5 c5c5c5c5

cSc5c5cSCS

c5eb^CSC5

cSc5c5C5ci

MO PPH

ci cici1

ci

ci2

elcici

cicicicici

cicicicici

HAt

1.31 1.872.500.394.04

3.861.522.293.102.01

1.012.351.361.632.69

7.383.081.671.732.41

NI PPH

C20c21100C20C24

C23c22C24C24C20

c20C25c22140C24

c36C24c35c20C21

Rfl PPM

elb 25

elbCISCIS

elbCISCISCIS150

190200180ISO110

CIS17048

250250

SB PPH

0.2 cO.lcO.lcO.lcO.l

cO.lcO.lcO.lCO.lcO.l

cO.lcO.lcO.lcO.lcO.l

cO.lcO.lcO.lcO.lcO.l

SG PPH

1.1 29352.9

32

233735383.6

3.53.73.63.43.0

1.50.3

391.11.7

SE PPH

c3 c3c3Oc3

c3C3c3c3c3

c3C3c3C33

c3c3C3C3c3

SN PPH

clOO clOOclOOclOOclOO

clOOClOOClOOClOOClOO

clOOclOOClOOclOOclOO

clOOclOOClOOclOOclOO

SR PPH

cbOO cSOOcbOOcSOOcSOO

cbOOcSOOcSOOcSOOcSOO

cSOOcSOOcSOOeSOOcSOO

cbOOcbOOcSOOcSOO510

TA PPH

4.0 0.5

CO. SeO.S1.3

CO. 51.0

cO.SCO. 52.9

3.12.53.22.42.8

cO.6CO. 5cO.ScO.53.9

TB PPM

14 1.42.7

CO. 21.8

1.62.42.12.5

23

2426242428

35192.85.7

13


Sanpl* description

103036103037103039103040103041

103042103043103044103045103046

103047103048103049103050103051

103052103053103054103055103056

103057103058103059103060103061

103062103063103064103065103066

103067103111103112103113103114

103115103116103117103118103119

103120103121103122103123103124

U PPM

1.6CO. 53.38.69.4

4.81.0

13CO. 5 CO. 5

cO.51.6

CO. 54.12.1

3.24:0.5CO. 57.52.6

24CO. S0.81.27.6

6.21.1

CO. 52.12.4

12CO. 51.7

CO. 58.0

9.67.08.28.47.0

7.18.00.75.5

CO. 5

W PPM

cicicici ci

Ci

Ci

<l<l<l

<l el<l<l<l

<lCi

<l

Ci

Ci

<l

Ci

<l

<l

<l

<l

Ocici2

7 ci ci<l<l

<l2

<lCi

2

2<lcici<l

ZN PPM

c5060

46879

c50

96<SO64

<50<50

<SO101<50<5096

0093

C50<5072

12000c5013700

c5086

<50<50<50

<50<50<50c50C50

686163

cSO<50

56<SOCSO<SO130

LA PPM

188.9

173452

142.1

192.81.7

0.61.71.42.2

14

265.61.22.02.2

2.1118.07.27.8

9.38.6S. 6

1717

562.7

287.8

37

5920402536

1024122011

CE PPM

381747110110

354

3845

C3657

32

54193e

11

e22171720

2325183235

806

481378

110728274120

6574293926

NO PPM

166

152137

8O11O0

c5O0O14

185OO9

O6796

5a6

1111

IBO14O22

3914312021

717108

11

SH PPM

2.21.04.34.56.5

1.70.32.30.40.4

0.20.70.60.62.4

3.42.20.30.62.1

0.61.41.01.41.1

1.21.31.72.32.3

2.70.31.90.54.8

7.12.95.13.04.0

2.23.43.51.92.8

ED PPM

0.70.41.61.01.2

0.6cO.20.9

(0.2CO. 2

CO. 20.30.3

CO. 20.8

1.10.8

CO. 20.30.4

cO.2CO. 20.40.40.3

0.60.40.60.50.5

0.6CO.20.60.41.3

1.40.91.20.90.9

0.70.80.50.41.0

TB PPM

cO.5cO.51.2

cO.51.4

cO.5cO.5CO. 5 CO. ScO.5

cO.5cO. 5 CO. 5cO.54:0.5

cO.5CO. 5CO. 5cO.5CO. 5

CO. 5CO. 5CO. 5CO. 5cO.5

cO.5CO. 50.7

CO. 5CO. 5

0.9cO.5CO. 5cO.5CO. 5

1.1CO. 5CO. S1.00.6

1.0CO. 5cO.5CO. 50.8

YD LU PPM PPM

1.0 0.130.5 0.054.6 0.745.4 0.875.4 0.78

0.7 0.150.2 CO. 051.8 0.38

cO.2 CO. 050.5 0.08

0.4 0.071.6 0.261.3 0.231.0 0.140.8 0.14

0.7 0.124.0 0.630.4 0.071.0 0.171.0 0.10

0.4 cO.OS0.3 CO. 050.2 cO.051.2 0.211.2 0.19

1.5 0.221.7 0.283.1 0.512.5 0.432.5 0.41

8.9 1.39cO. 2 CO.050.3 cO.05

CO. 2 CO. 053.7 0.59

5.4 0.864.4 0.714.3 0.684.3 0.674.8 0.76

5.2 0.794.7 0.751.4 0.220.8 0.123.0 0.46

Mna9

27.5327.6629.9528.6933.25

34.2532.8928.8133.9532.81

33.8631.6131.9631.3234.11

32.0029.6434.0930.8727.95

31.0529.5129.2233.5728.95

28.7532.5933.8832.2129.92

20.2741.4031.0034.3931.89

31.9432.0234.7336.9932.57

34.1635.1127.9531.0436.27


Sunpl* dmcription

103125 103126103127103126103129

103130103131 103132103133103134

103135103136103137103138103139

103140103141103142103143103144

U PPM

5.7 1.01.1

CO. 50.9

0.91.9 3.31.6

11

109.88.59.0

15

415.91.11.5

18

H PPM

1 ciCicici

ciO ci aci

<l ci

5cici

cicicicici

ZN PPH

c50 117C50cSOC50

95CSO (6

C50109

6011790

c50CSO

c50c50239cSOCSO

LA PPN

4.2 5.2

101.21.0

13 8.46.01056

3142603619

3.63.7

161.34.2

CE PPH

10 142536

25204

25120

10012012012095

158

433

24

HO PPH

c5 cS6

c5C5

S10 7

1237

2533412310

9cS20c5c5

SH PPH

0.4 1.32.90.31.6

3.0

1.82.87.1

4.16.06.95.13.7

1.90.94.80.21.8

EU PPM

0.5 0.50.9

CO. 20.8

1.2

0.71.1.

1.1.1.1.21.0

cO.2CO. 21.8

CO. 20.5

TD PPM

CO. S 0.60.5

CO. 50.7

CO. 5

CO. 5cO.51.2

cO.S1.21.41.71.3

CO. 5CO. 51.2

CO.ScO.5

YB PPM

0.3 2.13.50.43.0

3.0

3.03.35.7

4.76.05.85.66.2

0.90.55.20.32.8

LU PPH

CO. 05 0.350.550.050.46

0.510.49 0.470.510.90

0.760.960.890.910.92

0.120.080.840.050.52

Mill

1

34.92 31.6131.8737.6333.09

26.9531.64 29.2633.0830.66

32.4732.0731.8330.9632.03

29.7930.0633.5532.1634.53


Swvpl* description cuPPH

PB PPM

ZN PPH

KGPPH

HI PPH

MN PPH

SR PPH

CO PPH

BI PPH

V PPH

CA HG Tl AL Y PPH

DE PPH

103036103037103039103040103041

103042103043103044103045103046

10304710304B103049103050103051

103052103053103054103055103056

103057103058103059103060103061

103062103063103064103065'103066 ;Q

'V103067.103111103112103113103114

103115103116103117103118103119

103120103121103122103123103124

295.3.

92.10.9.

4.8.7.

52.58.

8.10.10.63.

4816.

13.20.33.4.

29.

134.38.6.4.3.

4.4.

85.7.B.

e.2.7.2.7.

10.a.7.e.4.

12.4.

11.2.

185.

25.12.17.14.14.

8.8.

13.5.5.

5.7.5.5.

10.

13.7.5.6.

22.

229.5.5.

21.54.

40.8.a.

36.34.

76.5.

14.13.28.

25.19.22.16.14.

19.20.5.

30.5.

CO.

11.372.47.70.

39.16.20.10.9.

7.21.43.ie.67.

19.54.16.6.

40.

120.19.25.93.12.

IB.84.28.7.

10.

5.4.

19.43.66.

69.65.50.49.38.

S3.52.11.31.95.

<O .440.440.440.440.4

40.440.440.440.440.4

40.440.440.40.70.6

0.540.440.440.440.4

40.440.440.40.6

40.4

40.440.440.40.91.0

0.940.440.40.440.4

0.440.40.4

40.40.4

40.40.4O. 440.40.4

20.2.

30.3.2.

21.5.9.

12.23.

9.24.35.47.56.

32.27.11.8.9.

21.e.

17.(8.5.

5.28.50.2.4.

2.9.i.6.4.

(.3.2.3.2.

6.5.9.S.

SO.

438.214.

2156.136.279.

344.119.195.190.212.

90.367.399.311.619.

218.1441.145.36.

152.

137.195.219.777.143.

152.700.423.80.BS.

26.31.

213.239.880.

283.571.284.249.109.

174.203.80.

175.1415.

320.153.200.54.39.

81.91.64.3.6.

7.14.8.

22.22.

204.67.3.

66.76.

11.190.39.67.78.

74.175.71.

106.103.

69.8.

336.429.62.

78.33.63.46.34.

31.39.

144.94.

244.

0.540.50.9

40.540.5

40.540.540.540.540.5

40.540.540.

40.

0.

40.

0.40.

40.540.5

40.540.540.540.540.5

40.540.540.540.540.5

0.540.540.540.540.5

40.540.540.540.540.5

40.540.540.540.540.5

45.

45.

45.

6.6.

45.

6.45.

45.

45.

45.

45.

45.45.

13.

45.

45.

45.7.

45.

7.45.

45.

45.

45.

45.

45.45.

45.

45.

45.

7.45.

45.45.

45.45.

45.

45.45.

45.45.45.45.

45.

41.18.

295.6.2.

43.7.

35.30.56.

33.150.148.116.61.

51.224.42.4.

27.

76.21.25.146.

2.

3.119.251.

4.5.

10.3.

19.17.2.

2.2.2.3.4.

7.2.

30.4.

247.

2.080.582.810.050.20

0.500.150.200.020.13

0.060.120.110.120.32

1.061.350.040.130.48

0.140.530.273.510.65

0.451.000.910.170.17

0.140.051.162.040.40

0.440.090.350.120.07

0.050.060.440.565.34

0.0480.0190.0930.0050.010

0.1040.0120.0300.0050.007

0.0060.0270.0250.0220.093

0.0630.0b70.0060.0020.039

0.0150.0160.0170.0420.007

0.0130.0370.0440.0120.012

0.0170.0100.0320.0270.011

0.0110.0130.0090.0100.007

0.0030.0080.0430.0170.061

0.970.202.540.060.21

1.350.262.110.871.37

0.552.463.162.743.44

1.583.190.840.410.43

0.620.370.563.740.07

0.123.394.180.040.04

0.040.170.540.390.07

0.140.090.090.130.08

0.080.061.400.192.91

0.230.060.810.110.14

0.320.030.100.020.05

0.030.230.170.250.25

0.210.750.060.010.12

0.140.040.030.280.02

0.020.130.500.040.04

0.130.010.140.140.16

0.180.140.160.150.11

0.120.120.110.040.63

7.b97.726.856.066.11

6.825.665.990.831.99

0.993.514.944.964.30

6.796.191.116.696.39

1.905.682.053.856.63

6.566.067.694.194.08

12.200.327.207.746.16

6.245.945.946.275.99

6.125.957.567.076.86

1.013.150.914.113.55

0.240.390.400.030.02

0.020.100.040.570.01

0.570.160.070.091.77

0.560.290.482.764.10

3.740.730.252.372.33

0.410.041.161.344.25

4.014.053.604.073.77

4.223.840.354.100.83

8.2.41.46.50.

6.2.

17.2.4.

2.8.

11.7.e.

e.34.2.S.5.

2.2.2.

10.7.

10.11.30.12.12.

40.2.4.2.

34.

54.34.40.32.38.

42.31.10.8.

28.

42.

42.

42.

2.2.

42.2.

42.42.

42.

42.

42.

42.

42.42.

2.3.

42.

2.42.

42.2.

42.

3.2.

4.2.

42.42.42.

42.

42.

42.

42.2.

3.2.2.2.2.

2.2.2.3.

42.


Svnplo description

103125103126103127103128103129

103130103131103132103133103134

103135103136103137103138103139

103140103141103142103143103144

CUPPH

4.22.51.9.3.

2.31.62.15.9.

35.3.7.9.3.

5.4.

130.10.3.

PBPPH

5.5.5.5.5.

5.5.5.5.

12.

15.14.15.13.11.

16.14.5.9.9.

ZNPPH

4.38.27.a.

11.

18.41.46.28.71.

66.83.74.64.44.

9.28.

144.5.5.

ACPPH

*:0.4cO.4CO. 4 :0.4 cO. 4

cO.4 cO. 4*:0.44:0.40.6

0.60.4

4:0.40.70.4

4:0.4CO. 44:0.40.40.4

NIPPH

4.47.44.11.43.

31.47.

46.51.3.

9.4.S.5.3.

4.3.

32.2.3.

MNDVHrrn

183.706.537.48.

152.

149.715.847.457.207.

328.327.255.109.127.

89.61.

1701.43.

143.

SR PPM

10.32.46.5.

47.

42.26.41.

146.49.

25.38.40.57.41.

133.77.

155.39.68.

CD PPH

cO.510.54:0.54:0.54:0.5

4:0.5cO.5 CO. 54:0.54:0.5

4:0.50.5

:0.5CO. S cO. 5

4:0.5cO. 5cO. 5cO.ScO. 5

BI PPH

c5.c5.c5.c5.cS.

cS.c5.<5.c5.c5.

c5.c5.cS.C5.cS.

c5.cS.<5.7.

c5.

V PPH

15.179.375.31.

184.

145.252.225.248.

4.

14.2.4.8.2.

10.3.

325.2.4.

CA t

0.040.170.630.070.48

0.260.190.381.820.06

0.080.100.460.050.05

0.220.185.050.130.22

P

0.0100.0270.0480.0050.035

0.0390.0470.0450.0480.011

0.0090.0100.0090.0090.006

0.0020.0020.0970.0020.002

MG

0.203.624.000.442.68

5.574.564.463.290.13

0.200.080.200.070.19

0.490.112.520.120.06

TI

0.010.300.610.030.42

0.490.410.500.360.13

0.130.120.110.110.09

0.010.010.740.010.01

AL

2.316.957. 481.057.45

6.787.147.727.396.31

6.175.976.136.38s. ea

7.396.516.496.997.02

K

0.290.250.180.050.10

0.250.140.640.583.96

.33

.86

.11

.56

.00

0.173.120.716.295.11

YPPH

2.11.31.2.

26.

12.14.26.17.48.

37.38.49.46.38.

5.4.

46.2.

17.

BEPPH

^.

rt.

2.C2.c2.

C2.4:2.2.

C2.

2.

2.2.2.2.2.

C2.2.

C2.C2.2.


Sunpl* description

103010 103011103012103013103014

103015103016103017103018103019

103020103021103022103023103024

103021.10302610302710302B103029

103030103031103032103033103034

103035103101103102103103103104

103105103108103109103110103201

103202

AU PPB

42 2

4263

10rtrt4

rt

4rtrtrtrt

4rt17rtrt

2rtrtrtrt

rtrt3

rtrt

t5

rtrt19

9

AC PPM

*5 45O4545

4545454545

4545

45

45

45

45

45

45

45

45

*.i45

45

45

45

45

45

4545

45

45

45

45

45

45

45

ASPPM

2.0 4.7

40.55.0

40.5

1.11.41.67.1o.e

1.040.54.41.4

40.5

o.a40.5

0.81.2

40.5

2.41.0

40.540.540.5

40.50.8

40.50.91.0

0.71.0

40.540.5180

47

BA PPH

60 450450450450

450450120450450

450450450450450

45076

45096

480

ibU450450310450

45045011045052

57. 800450450450

450

BR PPH

40.5 40.540.540.540.5

40.540.540.540.540.5

40.540.540.540.540.5

40.540.50.6

40.540.5

40.5

40.51.51.22.0

40.540.540.540.50.6

40.540.540.540.540.5

0.7

CA t

<l41

1

41

41

41

41

41

4l

41

41

41

41

41

41

4l

41

41

4l

5

41

41

41

41

41

2

41

4l

4l

41

41

1

341

3

41

CO PPH

39 92

10015061

331611

1206

42887S

42

4125e

2534

6231247

253

1677

102

1741

570

430

CR PPH

19 31442639

2224371817

1933171640

2636182244

1423201510

5612101410

179

12045

130

SO

csPPH

41

41

41

41

41

4l

41

41

41

41

41

41

41

41

41

41

41

41

41

2

41

4l

41

1

41

41

41

4l

41

41

41

1

41

41

41

41

FE t

2.25 4.40

13.68.4612.9

4.465.91

12.38.783.11

1.9715.24.290.74

14.1

6.4611.82.256.84

11.7

1.664.206.131.641.75

7.701.414.381.311.24

3.920.935.400.1718.4

28.4

HP PPH

4l

41

441

5

41

22

41

41

41

541

41

3

13

41

41

7

4l

1

223

341

41

41

4l

41

331

41

41

HC PPH

4l

41

41

41

41

4l

41

41

41

41

41

41

41

41

41

41

4l

41

41

41

4l

41

4l

41

41

4l

41

41

41

41

41

41

41

4l

41

41

IR

PPB

45

45454545

45

45

45

45

45

4545

45

4545

45

45

45

45

45

45

45

45

45

45

45

45

45

45

45

45

45

45

45

45

45

HO PPH

14

41

341

45242

44l

324

41

322

41

341

241

4l

4l

3

41

3

3

4l

41

41

41

16

10

NAt

0.04 0.012.440.372.78

0.060.452.120.020.03

0.041.100.030.020.36

0.031.810.020.062.66

0.011.783.523.965.64

2.610.030.070.530.68

0.033.313.634.32

40.01

40.01

MI PPH

420 420426420426

42068110420420

420422420420420

420420420420425

420420420420420

421

420420420420

420420424420420

420

RB PPH

415

415

41541532

415

415

415

415

415

415415

415415

415

415

3V415

2157

415

415

41525

415

415

415

415

415

415

415

74415

415

415

415

SB PPH

0.1 0.1

40.1

40.1

40.1

0.20.2

40.1

0.240.1

0.140.1

0.20.1

40.1

0.140.1

0.10.1

40.1

40.1

40.1

40.1

40.1

40.1

40.1

0.1

40.1

40.1

40.1

40.1

40.1

0.1

0.21.2

0.4

sePPH

0.7 1.0

358.3

28

2.79.3

131.21.2

1.4323.10.3

31

8.5200.75.2

35

1.02.32.02.50.9

290.54.50.60.5

3.50.7

380.44.2

5.1

SE PPH

43

43

43

643

43

43

435

43

43

4343

4343

43

43

43

43

43

43

43

43

43

43

43

43

43

43

43

543

43

43

5

3

SN PPH

4100

4100

41004100

4130

4100

4100

410041004100

4100

4100410041004100

4100

4100410041004100

4100

4100

4100

4100

4100

4100

41004100

4100

4100

4100

41004100

41004100

4100

SR PPH

4bOO 4500450045004500

45004500450045004500

45004500450045004500

45004500450045004500

45004500450045004500

45004500450045004500

4500910

450045004500

4500

TA PPH

40.5 40.540.540.540.5

40.540.540.540.540.5

40.540.540.540.540.5

40.540.540.540.540.5

40.540.540.54.5

40.5

40.540.540.540.540.5

40.540.540.540.540.5

40.5

TH PPH

1.1 40.22.80.53.5

0.21.11.3

40.240.2

40.24.10.3

40.22.0

1.11.5

40.20.64.4

40.2112.82.33.4

2.040.21.41.41.7

0.46.52.3

191.0

0.7


Sanpl* description

103010103011103012103013103014

10301510301610301710301810301}

103020103021103022103023103024

103025103026103027103028103029

103030103031103032103033103034

103035103101103102103103103104

103105103108103109103110103201

U PPM

co.scO. 51.81.22. J

0.8cO.50.9

cO. bcO.S

0.63.40.7

CO.S

1.8

0.61.4

cO. 50.8

cO.S

*0.b5.81.02.2l.S

cO.50.6

144.25.6

271.9

cO.57.0

16

H PPM

.ci<l<l<l<l

<lcici02

O c]

<l<l<l

<lcici ci

<l

ci<l<l<l<l

<l ci

cicici

2ciciciS

ZN PPM

cbOc5073

cSOc50

cbOC50cbOcSOC50

cbOc50CbOcSOcSO

cbOcSOc50c5075

cSOCbOcSOcbOC50

c50c50cbOc50cbO

cbOcSOc50CSOc50

IA PPM

1.43.7

182.8

16

1.82.0

cO.51.3

CO. 5

cO. 53.15.5

cO.S10

11CO.S0.62.0

22

cO. b3.0

cO. 52.6

cO.5

CO. 50.92.6S. 52.8

1.88.17.0

cO.S11

CE PPM

c37

438

44

S774

c3

c31310O 21

2310 O

561

c37

c36O

15c3696

52123O23

NO PPM

C5c521ci15

c5c5c5cSC5

c5c5c5cS

8c5CSc527

c5cbc5c5c5

cbcSc5c5cb

c56

10c58

SM PPM

0.10.35.20.04. R

0.40.61.10.1

cO.l

1.0.11.50.6

cO.l

1.61.00.10.36.5

n.i0.50.20.40.3

1.4cO.l0.40.30.2

cO.l1.22.80.61.2

EU PPM

cO. 2CO. 21.60.41.5

0.20.20.6

cO. 2CO. 2

cO. 20.70.3

CO. 2

0.50.5

CO. 2CO. 22.2

cO.20.2

cO.2cO.2cO. 2

0.7CO. 2cO. 2cO. 2cO.2

cO.20.51.8

CO. 20.4

TB PPM

cO.ScO.51.3

CO. 51.3

cO.ScO.5cO.ScO.ScO.5

CO. 5cO.bcO.SCO. 5

CO.5CO.ScO.ScO.S1.6

cO. 5CO. 5cO. 5CO. bcO.S

cO.ScO.SCO.ScO.SCO.S

cO.SCO. 50.6

cO.5CO. 5

YB LU PPM PPM

cO. 2 cO. OScO.2 cO. 055.6 0.841.2 0.205.2 0.83

0.4 0.081.2 0.232.9 0.50

cO. 2 cO.05cO.2 CO. OS

cO.2 CO. OS4.4 0.750.4 0.07

cO. 2 cO. OS

1.4 0.233.3 0.52

cO. 2 CO. 050.5 0.107.3 1.09

cO. 2 tO.050.4 0.080.3 0.060.3 cO.Ob0.3 0.10

2.6 0.46cO. 2 cO.OS0.5 0.09

cO. 2 cO. OScO.2 CO. 05

0.2 CO. OScO. 2 cO. OS3.5 0.590.4 0.070.3 cO. OS

Mat*

g

36.8332.6831.9933.1230.90

34.0932.1137.1132.6636.58

35.7332. 2b32.7133.9834.66

35.6838.1140.3235.6130.76

33.8629.8630.2129.7229.51

31.6233.3331.9932.8332.40

32.3730.9230.0630.1140.78

103202 7.0 11 cSO 9.6 20 0.9 0.5 cO.5 cO.2 CO.05 47.89


Sample description

1030)0103011103012103013103014

103015103016103017103016103019

103020103021103022103023103024

103025103026103027103028103029

103030103031103032103033103034

103035103101103102103103103104

103105103108103109103110103201

CUDBUrfn

3075.2703.

37.6747.136.

12034.393.436.

33(0.BOS.

3900.1144.1450.(02.260.

366.74.

4456.114.69.

2748.44.9.5.7.

2.298.

4558.2791.2459.

8343.20.36.6.

182.

PBPPH

b.7.

17.12.5.

6.11.5.5.5.

7.6.7.6.5.

6.S.b.

12.12.

8.6.6.5.5.

10.5.

19.28.10.

14.29.23.5.

31.

ZNPPM

2.3.3.

11.5.

24.3.2.2.2.

5.10.3.5.

29.

4.11.11.2.

41.

8.11.3.3.2.

9.2.

21.11.12.

25.34.32.3.

25.

ACPI'H

cO.4CO. 4cO.4CO. 4cO.4

CO. 4CO. 4cO.4cO.4CO. 4

0.6CO.4cO.4 CO. 4cO.4

cO.4*0.4*0.4cO.4cO.4

<0.4cO.4<0.4cO.4<0.4

<0.40.4

cO.4<0.4<0.4

0.6 CO. 4<0.4<0.40.5

NIPPH

9.22.35.26.23.

13.9.5.

30.6.

7.17.13.8.

23.

17.10.4.8.

21.

8.6.8.5.6.

34.9.9.6.9.

10.5.

51.5.

62.

MNPPH

18.28.

234.80.

196.

49.112.109.31.24.

36.345.44.21.

2B8.

7b.210.27.66.

839.

29.71.35.59.33.

280.28.

107.42.40.

81.138.589.19.

571.

SRPPMrrn

2.2.

60.7.

73.

2.8.

32.2.2.

2.13.2.2.

11.

2.48.2.e.

169.

2.27.35.

143.38.

138.2.2.5.5.

2.603.230.87.31.

COPPMFFn

CO. 5

cO. 5cO.5cO. 5CO. 5

0.9cO.50.6

CO. SCO. S

cO. 50.8

cO.5CO. ScO.5

0.50.70.6

cO.51.0

CO. 5cO.5CO. 50.5

cO.5

cO.5cO.50.50.60.5

1.0cO.5CO. 5cO.SCO. 5

BIPPH

c5.cS.c5.cS.cS.

9.c5.cS.6.

cS.

c5.c5.cS.c5.c5.

c5. eb.

c5.cS.c5.

7.cS.C5.c5.cS.

cS.cS.8.

c5.cS.

9.cS.cS.c5.c5.

VPPH

s.6.

209.46.

204.

28.83.

156.9.

33.

16.209.29.3.

225.

77.170.

6.108.179.

14.24.41.16.11.

208.18.56.8.7.

64.9.

243.2.

154.

CAt

0.010.011.090.211.09

0.050.250.270.010.01

0.010.480.030.010.72

0.060.620.010.033.35

0.010.100.150.430.15

1.830.010.040.040.04

0.021.003.410.223.04

P

0.0030.0020.0840.0200.087

0.0120.0250.0470.0020.004

0.0030.1010.0040.0020.057

0.0190.0440.0030.0140.130

0.0030.0040.0240.0200.009

0.0490.0020.0160.0060.006

0.0140.0180.0730.0020.023

HG

0.310.312.831.022.17

0.601.660.600.290.18

0.292.660;530.094.47

1.251.690.140.721.80

0.160.540.150.470.30

3.190.112.020.370.23

0.670.204.160.071.28

XI

0.010.010.850.160.75

0.050.240.440.010.01

0.010.560.030.010.60

0.120.670.010.130.81

0.010.010.040.080.04

0.420.010.100.010.01

0.060.080.730.010.04

AL

0.290.315.071.325.31

0.681.913.440.330.25

0.475.780.480.154.02

1.473.540.190.926.14

0.203.274.565.906.92

6.910.142.151.241.39

1.066.977.275.631.35

K

0.010.010.010.010.01

0.010.060.030.010.01

0.030.010.010.010.01

0.010.100.010.030.46

0.010.190.110.640.11

0.050.010.040.050.04

0.032.800.380.060.01

YPPH

2.2.

44.10.37.

4.8.

16.2.2.

2.28.2.2.

30.

8.23.2.2.

54.

2.4.2.2.2.

24.2.4.2.2.

2.4.

32.4.6.

BEPPH

c2.c2.c2.c2.C2.

c2.c2.c2.c2.c2.

c2.c2.C2.c2.C2.

c2.*2.c2.c2.c2.

c2.C2.c2.C2.c2.

c2.c2.c2.c2.c2.

c2.2.3.2.11.

103202 171. 13. 14. 0.4 51. 149. CO.5 C5. 194. 0.37 0.008 0.60 0.04 0.65 0.01 16.

o o

Activation Laboratories Ltd. Work Order: 9049 Report t 8944

Sup].* description AU PPB

1010(1I030C9103010101071103072

101071103074 "S10107S/ ,

c2c2c2

2C2

c2c2C2

M JPN

c5ciciciO

cicSrt

US

cO.ScO.ScO.ScO. S

1.5

0.70.*

cO.S

M PH C* CD PPM PPM \ PPH

leo co.C90 c-0.260 *0.1*0 CO.cSO cO.

440 CO.51* 1.9*4 CO.

ci 45ci cici 15

2 S4 II

ci tci lci 1

CMnn

(4CSci12

200

9t

t

CB PHPPM i

1 10.1ci 0.2(ci 0.43i Kit

ci J. 98

3 O.H2 1.473 a. 01

V Ci'K

)ci

444

41011

uc

dCi

CI

ci0

cicici

IR PPB

•r Scici^ci

cScic*

MO PPK

ciciCi

cic2

4Ci

9

m

1.143.7k4.121.41x.ett

2.151.02Lil

HI PPM

*24C2.2c 18CISclt

7*c20cJO

MFTO

OSelbCIS

13ci}

110170140

•B PPH

cD.lCO. 1co.iCO.l

cO.l

CO.l

a. 2cO.l

BCPPH

l*2.70.32.0

10

2.23.1).i

BS TPH

cic?cicic)

c3Ci

c)

BM

ClOOClOOC103ClOOClOO

ClOOcIC'OClOO

SR

cSOOcSOOciOOCSOOc&OO

cSOOciOOc&OO

PPM

CO. i4.1

cO. tcO.ScO. i

1.71.73.1

raTPM

2. i2.1

121.51.0

313423

ot

6CMi-*

CJ

•rtA

O V

uto

Activation Laboratories Ltd. Work. Order: 9049 Report: 8944B

Bupl* U**ciiption

10)04110106*103470J03071103012

103073103074103015

HO PPH

2.2.2.2.2.

2.2.2.

OUOTH

24.4.2.

IS.26.

2.3.S.

PBmi

b.s.S.7.S.

28.IS.IS.

inPPM

78.2.2.

14.eg.

sn.77.61.

M PPM

O.C CO. 40.4CO. 4^.4

CO. 40.70.8

Ne PPM

49.t.S.0.

104.

6.S.4.

mP7M

Hll.If.10.

278.tot*.

174.27*.ice.

aitPPM

m.70.47.

34B.206.

7*.10.SI.

CD PPH

CO. ScO.5tO. S(Q. S*0.3

cO.tCO. SCD. 5

RI PPH

*3.cS.ci.C&.

ti.

45.cS.0.

VPPH

191.7.2.

21.200.

S.S.c.

Cfc

1

1.170.140.181.234.44

o.se0.410.06

F1

0.4*00.0020.001Q. 0310.0)7

0.0100.04*6.007

MG t

5. n0.140.080.704.41

0.1S0.350.07

TT t

0.500.070.010.170.51

0.040.110.10

M. 1

7.605.127.148.367.51

7.0]5.866.08

R 1

0.1)0.220.071.640.61

4.254.344.21

IPPM

13.4.2.2.

2).

1.4).40.

88 PPH

a.c2.O.C2. e J.

2.2.

tt.

l

(D A00

tf)O A

g

IOA s.•H O X

Activation Laboratories Ltd. Work Order: 9049 Report: 8944C

O .SAMPLL1 0 Si02 A 1201 KCJ03 fe() HftO KyO CaO NnUO K2O Ti02 MOS II2O. H2O- 101 TOTAL

,Gr103074 72. IJ 11. Si 2.66 0.86 0.04 0.41 0.51 1.59 S. SI 0.11 0.03 .0.01 .0.01 l. 92 91.41103075 74. (8 ll.lta 3.01 0.21 0.02 0.11 0.07 2.65 S. 09 0.28 0.0.1 .0.01 cO.Ol 1.14 9*. 04

SAMPLE K

103074 I0107S

BaPH4

10931 104

Sifm

3254

VFM

41ft

St;PPM

44

ItPPM

325343

tno^^

0

OftN.MO •v

61

APPENDIX D: PETROGRAPHIC DESCRIPTIONS

Sample 103074 ( l of 2): Keweenawan Granite

UTM: 706130 5196160

Hand Sample: medium-grained, red granite with mm- to cm-scale

miarolitic cavities

Quartz: 3 5 to 40 ii fine intergrowwths with K feldspar

K feldspar: 6 0% mostly complex granophyric intergrowth with clear

igneous quartz, minor very cloudy mm-scale subhedral phyric

feldspar grains are early phenocrysts overgrown by granophyric

quartz and feldspar. Note that 90*^ of all feldspar grains are

actually ultrafine sericite pseudomorphous after K feldspar. The

sericite causes patchy extinction of the erstwhile feldspar

grains.

Albite: Although the rock is albite normative, there were no

albite grains in the slide, hence the Na is contained in the K

feldspar, or plagioclase grains are too clouded by sericite to

distinguish.

Chlorite: 2 to 3% fine-grained aggregates within miarolitic

cavities, olive green in ppi, probably chamosite

Hematite: Trace as coatings on chlorite in miarolitic cavities

Manganite o r manganese oxide/hydroxide: Minor opaque coating with

bluish grain boundaries in transmitted light

Sample 103074 ( 2 of 2): Keweenawan Granite

This slide has essentially the same texture and mode as the

62

previous slide, with minor differences viz:

-phyric K feldspar grains are intensely chloritized

-some of the hematite is pseudomorphous after disseminated

primary fine-grained magnetite in the groundmass of the rock, and

minor magnetite is remnant in the cores of the larger grains

Interpretation: undeformed granite with excellent preservation of

textures indicative of rapid crystallization and degassing at

shallow depth

Sample 103075: Keweenawan Granite

UTM: 706130 5196100

Same as per 103074

Sample 103116: Keweenawan Granite

UTM: 705740 5197100

Same as 103074

Sample 103030: Pitch Ore Cu Occurrence

UTM: 711800 5194430

Hand Sample: quartz-chlorite-cpy-magnetite rock

Quartz: 9 5-98*4 fine-grained vein quartz, incipient

recrystallization

Chalcopyrite: trace to .5** fine-grained, evenly disseminated

throughout quartz

Hematite: minor hematite pseudomorphs after chalcopyrite, the

largest grain of hematite is within a chlorite aggregate where it

63

is replacing chalcopyrite

Magnetite: trace fine-grained, disseminated

Chlorite: olive green, l to 21 disseminated fine, euhedral grains

and irregular aggregates

Sample 103044: cm-scale boulder of K feldspar-dark matrix breccia

UTM: 706725 5196730

Hand Sample: unusual bright red rock of angular, coarse-grained

brecciated K feldspar fragments with dark, fine-grained, silicate

matrix

K feldspar: 8 0% medium to coarse angular fragments and grains,

very cloudy in ppi because of sericite pseudomorphs throughout

the grains, minor quartz and chlorite inclusions. Remnant

polysynthetic twinning suggests it is microcline. The edges of

the grains are broken and intergrown with fine chlorite and

quartz. Rare granophyric texture with quartz.

Albite: trace disseminated fine grains

Interclast material: 4 01 quartz and 601 chlorite very finely

intergrown.

Biotite: trace within interclast material

Hematite: 0 .5 to 11 disseminated fine grains and fracture

coatings throughout interclast material

Interpretation: Probably a brecciated pegmatoidal phase of the

Keweenawan granite

64

APPENDIX E: MISCELLANEOUS GEOCHEMICAL DATA FOR KEWEENAWAN GRANITE

SAMPLES 103074 AND 103075

CIPW Norm from file: C:\NEWPET\WOLFE.ROC sample: 103074

Oxide WT

SiO2Ti02.12O3'e2O3FeOMnOMgOCaO

Na20K2O

P205Cr203

720

11200001500

.83

.31

.56

.86

.85

.04

.43

.51

.59

.51

.03

.00

82.800.277.751.220.810.040.730.621.754.000.010.00

0CZOrAbAnLeNeKpHIThNeAcNsKsDiWoHyOlCsMtCmHm11TnPfRuApHyFIPrCcMaSiSpH2H2OtSiTo

Greenpa am % param \ 31 0.59 Qtz 75.73 3tz 82.33 01 0.59 Jd 6.60 Di 0.00

Mineral WT 3,

Quartz 40.84Corundum 2.13

Zircon 0.00Orthoclase 32.57

Albite 13.45Anorthite 2.33

Leucite 0.00Nepheline 0.00

Kaliophilite 0.00Halite 0.00

Thenardite 0.00Na Carbonate 0.00

Acmite 0.00NaMetasilica 0.00K Metasilica 0.00

Diopside 0.00Wollastonite 0.00Hypersthene 1.07

Olivine 0.00DiCaSilicate 0.00

Magnetite 1.97Chromite 0.00Hematite 1.50Ilmenite 0.59Sphene 0.00

Perovskovite 0.00Rutile 0.00

Apatite 0.07Hydraphane O.00

Fluorite 0.00Pyrite 0.00

Calcite 0.00Magnesite 0.00Siderite 0.00

Spodumene O . 00H20+ 0.00H2O- 0.00

Others 0.00Si Def 0.00Total 96.52

Formula Mole%

SiO2A1203ZrSi04

(K,Na)AlSi308(K,Na)AlSi308(Na,K)AlSi208

KAl(SiO3)2(Na,K)(Al,Si)204

AlSi04NaCl

Na2SO4Na2CO3

NaFe(Si02)3Na2Si03K2Si03

Ca(Mg,Fe)(SiO2)3CaSi03

(Mg,Fe)Si03(Mg,Fe)2SiO4

Ca2Si04FeIIFeIH2O4

Cr204Fe2O3

FeTi03CaTiSiOS

CaTi03Ti02

Ca5(PO4)3FSi02(H20)x

CaF2FeS2

CaC03MgC03FeC03

LiAl(Si03)2 H20+ H2O-

75.142.300.0012.945.670.930.000.000.000.000.000.000.000.000.000.000.000.590.000.000.940.001.040.430.000.000.000.020.000.000.000.000.000.000.000.000.000.000.00

100.00

Projection Data Walker

param % param \ Di -3.02 PI 91.06 01 5.93 01 18.21 Sil 97.40 Di -9.28

Groves Elthonparam \ param l param iQtz 100.02 Qtz 86.94 Cpx -3.8401 2.60 01 2.26 01 2.89Cpx -3.01 PI 10.46 Sil 100.68

CIPW Norm from file: C:\NEWPET\WOLFE.ROC sample: 103075

ix i de WT Mole%

Si02TiO2.12O3Fe2O3

FeOMnOMgOCaO

Na20K2O

P205:r2O3

740

11300002500

.68

.28

.78

.01

.23

.02

.11

.07

.65

.09

.03

.00

83.0.7.1.0.0.0.0.2.3.0.0.

682478272202180888640100

0CZOrAbAnLeNeKpHIThNeAcNsKsDiWoHyOlCsMtCmHm11TnPfRuApHyFIPrCcMaSiSpH2H2OtSiTo

Greenpc.-am ^ pa r am % 01 0.15 Qtz 73.74 Ot 83.36 01 0.15 Jc 9.62 Di 0.00

Mineral WT \

Quartz 39.55Corundum 1.86

Zircon 0.00Orthoclase 30.08

Albite 22.42Anorthite 0.15

Leucite 0.00Nepheline 0.00

Kaliophilite 0.00Halite 0.00

Thenardite 0.00Na Carbonate 0.00

Acmite 0.00NaMetasilica 0.00K Metasilica 0.00

Diopside 0.00Wollastonite 0.00Hypersthene 0.27

Olivine 0.00DiCaSilicate 0.00

Magnetite 0.00Chromite 0.00Hematite 3.01Ilmenite 0.53

Sphene O.00Perovskovite 0.00

Rutile 0.00Apatite 0.07

Hydraphane O.00Fluorite 0.00

Pyrite 0.00Calcite 0.00

Magnesite 0.00Siderite 0.00

Spodumene O.00H20+ 0.00H2O- 0.00

Others 0.00Si Def 0.00Total 97.95

Formula Mole%

SiO2A12O3ZrSiO4

(K,Na)AlSi3O8(K,Na)AlSi3O8(Na,K)AlSi2O8

KAl(Si03)2(Na,K)(Al,Si)204

AlSi04NaCl

Na2S04Na2C03

NaFe(Si02)3Na2Si03K2Si03

Ca(Mg,Fe)(Si02)3CaSiO3

(Mg,Fe)SiO3(Mg,Fe)2Si04

Ca2SiO4FeIIFeIII2O4

Cr2O4Fe2O3

FeTiO3CaTiSiOS

CaTi03Ti02

Ca5(PO4)3FSiO2(H2O)x

CaF2FeS2

CaCO3MgCO3FeC03

LiAl(Si03)2 H20+ H20-

73.592.040.0012.089.560.060.000.000.000.000.000.000.000.000.000.000.000.150.000.000.000.002.110.390.000.000.000.020.000.000.000.000.000.000.000.000.000.000.00

100.00

Projection Data Walker

param % param "k Di -2.73 PI 94.06 01 4.79 01 13.60 Sil 98.09 Di -7.75

Groves Elthonparam % param ^ param %Qtz 101.46 Qtz 85.56 Cpx -3.60Ol 1.28 Ol 1.08 Ol 1.93Cpx -2.73 PI 13.73 Sil 101.68

C:\NEUPETSUOLFE.ROC

15

Middlemost 1985 (fig 3.3.6)

x-p

o(S3K

O CVJ1C

10

O

1 1 1 1 | 1 1 1 1 1 1

1 1 1 1 1 1 1 1 1 1 1 1

50 60 Si02 (ut x)

70 8C

CiSNEUPETSUOLFE.ROC

AnorthiteA A: Tonalite

B: GranodioriteC: AdamelliteD: TrondhjemiteE: Granite

Albite Orthod a

69

REFERENCES

Allen, D.J., Hinze, W.J., and Cannon, W.F., 1991. The

relationship of topography and gravity over the Lake

Superior Swell: evidence for a Keweenaw hot spot?. In

Proceedings of the 37th Institute on Lake Superior

Geology, p. 4-6.

Geological Survey of Canada, 1963. Aeromagnetic Series Map 2201G,

Sheet 41k716, Searchmont, 1:63,360.

Leahy, E.J., and Giblin, P.E., 1976. Map 2419 Sault Ste. Marie-

Elliot Lake Geological Compilation Series, 1:253,440.

Middlemost, E.A.K., 1985. Magmas and Magmatic Rocks. Longman

Group, Essex.

Ministry of Northern Development and Mines, assessment files

office, Sault Ste. Marie, ON.

Ontario Geological Survey 1991. Bedrock Geology of Ontario, east-

central sheet; Ontario Geological Survey, Map 2542,

1:1,000,000.

17:49 FAI 61J T27 SB7011/30/95MinUlry ofNorthern Development and Mines

Ontario

WIC IKT'L LTD(2)002/004

Report of Work Conducted After Recording Claim

Mining Act

W9550 000

Pwtonel Information coftecled on IhU toon to oMetaed under to author ty tt eh* MWng Act. TMl Momiaflon ^ be ueed tor correspondence. OucMton* eta Idle coWecoon ihouM b* dkected to ItM Provincial Maneper. MMng Lend*. MMevy ol Maftwrn Development end Mn**. Fourth Sudbury. Ontario. P06 BAS. Utopian* (708) 870-72*4.

Instructions: - Please type or print and submit In- Refer lo the Mining Act and Ragu

Recorder.- A separate copy ol this form must- Technical reports and mapa must- A sketch, showing the dalma the

2.

41K16NEOOO4 2 16289 MARNE 900WC International Mallei -,

Addreei : 22 Gurduara Roarl Hcpcen. Ontario 'K2E flA2

kMngOhMon Sault St. Marie *T^jSMe\tol MQ r ne /Ar-J\ , Lv/e*

dent NO. 293367

telephone No (613) 727-3937MotOPhnNo. i i

C-3059 C-3U73 MS3tGfcJt'

Dele* Worfc^^ From; 95.04.19 To: 93-06-03

Work Performed (Check One Work Group Only)WorkGroup

Qeolechnlcal Survey

Physical Work. Including OrMrtg

RehabMaUon

Other Authorized Work

Assays

Assignment from Reserve

Typa ^

Heilmck Mepplig ami sampling, prospecting

ri tC *r^lv "" i

——————————————————————————————— npf* ^ q 1^0^ — —— — UC.O J? .iibr

"-*e"p MINING UNDS bRMr-:-

Total Assessment Work Claimed on the Attached Statement ol Costs \Note: The Minister may reject lor assessment work credit aft or part of the assessment work submitted II the recorded

holder cannot verify expenditures claimed hi the stalemeni ol costs within 30 days of a request for verification.

Persona and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name

.luti North

Jota everest

AddressWC Intarrwl tonal l.til 22 Ctinhan Howl; Nojwni, Ontario

Student caployerl by ttC

(attach a schedule It neceeaary)

Certification of Beneficial Interest * See Note No. 1 on reverse side

FlcerM) l i opal i l toy tt*

l certify Diel at tin Hma the wort WM perfomied. the claimi coveted In M* work i opal were recorded hi the curienl hoUar** mvrw or toU uvJer e banaacW Inlotut by Ilw current recorded holder _____________

IrSioordbdlkldcr ei Ageni~jf

•'L",

Certification of Work Reportl ceiMy Ihml l have a panonal knowtodg* of Ihe (act* Ml kwth In IMt Work report, havkig peifcwmod Ut* vork or vribieeMd t Hi completion and enn***d report li irm. _ _ _ _____ ___ ________

N*m* ind AddrMt at P*xan CMVrVCe' .—-.— ——

i during indter tftt

Jon North 87S tmnilee Avenue] Ottawa, Ontario IffiB STl

•41)0*1)

11/30/95 17:50 PAI 813 717 3970 WIC INT'L LTO 12)003/004

f

g zo-1 t:

it:o u

0-co t: t:

CT* CT-

\ \ s I

ir B

i* ?VsJ

-WJ.

liftIF

R ECB1

DEfj - R

s'tiz il?19SE

riiS

MINING UNiJS h/o

\ ^ 1- T 1-f

^V ^

iif

*rp'

Credits you ara claiming in this report may be cut back. In order lo minimize (he advene effects ol such deletions, please Indicate from which claims you wish lo priorize the deletion ol credits. Pteasa mark (r] one of Iha totowtog:1. 1*1 Credits ara lo be cul back Harling with ihe claim Kstad last, working backwards.2. I .I Crodlta w* to b* cul back equaMy over all claim* contained In llils report of work.3. G CradHs ara to be cm back aa prtorlzed on Iha attectied appendhi.

m the event that you have not specified your choica of priority, option one wfJ be Implemented.

Note t: Examples of banefldal Interest ara unracordad transfers, option agreements, memorandum of agreement*, etc.. with r**p*ci to the mining claim*.

Nol* 2: II work ha* been performed on patented or (eased land, pleat* complete Iha following:

l comfy ihal Iho recorded hoktor Marl a bontDcUI Merest hi m* pt tented (ir tooKXt (arid (l Ilw lime Ilw oak wu i i

Signature N/A

Ode l

OntarioandMbiaa

MrMaradu Oevetappement du NordM o

Statement of Costs for Assessment Creditttat des coOts aux flns du credit devaluationMining Act/Lol *ur tea mines

W955Q 00071-

2. 16289Person*! Inlormallon cotected on Into term l* obtilned under (ha muhoilry o) Hie MMng Act. Thai Information oil b* used lo maintain e record tnd ongoing *t*lu* ol In* mMng clalm(*). Oueettone mbom iNi ooleellon *hoo*d b* dk-acted lo the Provincial Manager. Mining* Land*. Mlritfry of Northern Development *nd Une*. 4lh Ftoor. 1M Cadet Street. Sudbury. OnUrlo P3E 6AS. Wephone (706) 67O-7M4.

les ronseigiiotnui** norsonnelt contemn dan* le pitsanio lornHri* *on recuoiB(envertud*l*Lol*iirteimlneee1 Mnrkom s lenir 4 |otv un region de* conc***lone mMeret. Adretter tome que*hon ev l* colleco d* c*- reruelgnemenl* au chef provlnclel de* leneln* mtrO*rt. mMM*r* di D*vetappemerK du Nord el de* Mine*, 1S0. rue Cedar. 4* Mage. Sodbun (Onurto) ne. 8AS, tsiaptiona (706) (70-7204.

1. Direct Coeta/CoOU directs 2. Indirect Cotti/CoOts endrract*

Type

Wages Satatrea

Contractor's and Consullanl'a FeaaDroM* d* rentraoranear at de I'aipert- conaaJI

•uppae* Ueed Foumtluras uMleaea

Ciûtpfn*nrt Rental Location de materiel

OeacrlpUon ' ;

Labour MalrHfoauvre , 'FVeW Supervision :: ;" SupervWon sur to Istfefc

^{.t

Tff*Aaaaya

Twa

AmountUonlent

11700.00

3850.00

^^^^^^^f^îîaiaiiLslen-ot

Total Direct Coals Total daa coOta dkocta

Total* Total giobsl

11700.00

3850.00

^r

ayynJft7S 00

U*,.w -^'...1 L

MWfr9e /^2f5-0,

yir

)

" Note: Whan ota atowabta Pour la n coM* tnd tfevciual

Type

TranaportaOofi Tnrupotl

Food end Lodging MwrttHreel

MobmnMon end OcfnoontntvOfi MobHMtlonel *Um*t,miMan

Mng ReftaMUtton woi* IrKfrecl coet* ire not

Mnbaunamanl de* travein da r4nabHteiion. le* recla ria eont pat tdmUaMa* en tent qua iravam ton. '.y.',.

Deacrlpoon

Tf5el

Cabin rental Orocaclaa

FVMl

Amount Uonttnt

350.00

UdU.uu 3660.00

200.00

Sub Total ol lixflract Coiu Total partial data coats Indlrecta

Aeraunt ABowabto (not greater than MM ol Direct Cons) •lantern *deiU*lbl* |N'*ic*dwrl pee M H de* coot* dtoct*)

Total Vahj* ol AMeaemtnt CradK Vdegr loUto du credk a*MI *l Dtracl end Uemittt f Mutton IndbMt eeeM ft*M **i coOH eVMti

Total* ToUI global

?5^t)o5*40.00

200.00

5990.00

if ft f e ajmjj i iv

7fJfC-orJ2U11.06 XXIilirX

d h

Mole: The recorded hoider wal b* requited K) vertty expendkures claimed In IM* ciatemeni ol cod* wfenln M day* of a requetl lor veriMcjtlon It verfficition l* not made, the MMeler m*y rejict lor ueetamenl wont el or part ol the emiimenl work lubniload.

Hot*:UnuWraiW pr**ent etaf det^ktr&nvle* 30 )oun *uNan) une demand* 4 eel enel. St la verfteuion n'eel pet etlectuee. le mMetni PMM (efeler kim ou une partle da* lieipy.d'evejuellon pt*

Filing tXecounta

1. Work ffled wrlWn two years ol comptelloo to dalrned at 100*Ao( th* above Tolat Vahto ol Atiasamoni OodH.

Ratnlaaa pour dapelMINING

1. La* Uavaux rMpo*a* dan* tot deux in* turvant tour achavemem tont

2. Worfc tiled ttvea. lour or frve years after completion Is cfalmad at SOMi or the above Total Value ol Aaae*ament Credit Se* catculailorts below:

otaTVirue oTAiienmenl Credl Total A****fm*fK OcJmedx 0.50 -

t. Leatravaux daposas Irols, qualrs oudnq ara aprastour schavemam som rsmboursas k 60 H de la valaur totala du credit d'evaluaikm susmanUonne. Votr las calculi d-de*toua.

Valeur Mela du credk d'evekiallon ErekMOon Mate demande* x 0.50 -

CerUflcetkMi Vedtyrng Statement of Costa

l hereby certify:thai the amounts shown are aa accurate as poaabla and lhaaa costa ware kicuned wNte conducting assessment work on the landa ertown on (he accompajrrytng Report ol Work form.

that aa Senior Project Geologist______~tRaârdad HcMer. Aeanl. Portion m Company)

. l am authorlMd

Attestation de l'4tat dea coflte

J'alleste par la prtoenie :qua lee montants Indlques sonl le plus exact possible el qua ces defenses ont at* engageas pour elfactuer lea Iravaux d'avahiallon sur las terrains bxHques dans la formuto de rapporl da irnvnll r.l-)rJiii

Et qu'4 Ulre ds' .povto oooupv okws) IB

la aula auiorlsa

lo make this cartiflcatton a falra oatta aitaataUon.

OeteNovanber 27/95

NoU : Den* c*(te tonnul*. lonqu'l deilgn* d** per tonne*, l* meeculn M) utBM *u MM rwutt*

OntarioMinistry ofNorthern Developmentand Mines

Ministere duDeveloppement du Nord et des Mines

April 11, 1996

Geoscience Approvals Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: (705) 670-5853 Fax: (705) 670-5863

Our File: 2.16289 Transaction #: W9550.00076

Mining RecorderMinistry of Northern Development S Mines60 Church StreetSault Ste. Marie, OntarioP6A 3H3

Dear Ms. Lessard:

Subject: APPROVAL OF ASSESSMENT WORK CREDITS ON MINING CLAIMS 1191465 et al. IN TUPPER, SHIELDS, MARNE S, ARCHIBALD TOWNSHIPS

All deficiencies associated with this submission have been corrected. Accordingly, assessment credits have been approved as outlined on the report of work form. The credits have been approved under Section 12 (Geology) of the Mining Act Regulations.

The approval date is April 05, 1 996.

If you have any questions regarding this correspondence, please contact Steven Beneteau at (705) 670-5855.

Yours sincerely, ORIGINAL SIGNED BY:

Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division

SBB/jl Enclosure:

cc: Resident GeologistSault Ste. Marie, Ontario

/Assessment Files Library ^Sudbury, Ontario

o oCM

DOCUMENT rto. W9550.

THE TOWNSHIP OF

TWP 25-R.I2THE MApON THAT APPEARS OW THIS MAP HAS BEeN>IQM^*ILED FROM VARIOUS SOURCES, ANDQUARANTEEO. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER. MINISTRY OF NORTHER** DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON.

ARNEOF

ALGOMASAULTMINING DIVISION

SCALE ••htt^*40'CHAIN5

LEGENDPATENTED L/mD CROWN LAltf* SALE LOCATED LANDuciNse or OCCUPATIONLIASESROADSIMPROVED ROADS RAILWAYS POWER LINES

NOTESTHIS TWP. WAS FORMERLY

PARCEL NOS - 7 55, 1 T79, UC V 2*20,BY A C. ft H. 9. RLY. PRIOR TO CROWN CO W T HW.

TO LEAfiE (UMATCHED A*EA

(TIIIBEP, RIGHTS, RY.hAV, E TCJ

SNS, rO ALGOMA CPNTRi-L

C ta S FILE

EC - P 1995-

LANDSBFWR E O E l V B

MlDATE OF ISSUE

10V SO 1995

PLAN NO- M* 1305s s /L s s s A/ j j f s s s

MINISTRY OF NATURAL Rf SOUR. -ANC 'SHIELDS TWR

DATE OF ISSUE

\

A .^g^^^^^to^^^^lg* f l

r"

*. ^

. THOSE ttXE WIN-

ING CLAIMS SHOULD CON-

Sand&GravW. . .

Contrrt point (nor utontal) ...... . ...,.^;.,..

Flooded tend

..,.,::,A ON THELANDS SHOWN HEHEON^Aca** 1:2*8*0 .

aPipeline (above around)

Gotitlaf Interval it* Wetiett

Map base UN) land dispoeKtonaVatttno by.furVBys and Mapping Branch. Ministry of Natural Resources.

The cB&posfflOR of land, location of tot fabric and parcel boundanea on this index was compiled for administrative purposes only

dOubtetracK abandoned.

Road;highway,county,township . .... access trail, bush.

Shorettne (original)

Transmission line .

Wooded area.

-•yAOft w—-*\ nr J -^"•.^jfl/U

E W , " ' r' Tff *iVit - af . j'ifri-r V

if4 ' ^Sw^-TfWRST ^ *-^i^^fefer

41K16NE0004 2 16289 MARNE

iaMMiguMiaiia&Mii

Ministry ofDevelopment

and

Ministry ofNaturalResources

INDEX TO LAND DtfTOSITION

RECEIVEP162 •

G LANDS ci

M.N.R. AONHNISTfWnVE DISTRICT

SAULT STE. MARIEMINING DIVISION

SAULT STE. MARIELAND TTTLES/rafflSTRY DIVISION

ALGOMAARCHIBALDDOCUMENT No. W9550.0607J!;

MM 7MO MM MM

Contour Interval 10 Metre*

AREAS WITHDRAWN FBOUMOPOSmONHKO- , 8RO- Surface RtgM*Of#yM+S-MWngand Surf ab* WfjTitt

* "L 4li *W ' l *

7 V . ~ "J ' ?

Lot/Concesston; surveyed . .....j ,,,,.. .unsurveyad ,... , M| ,.,.,, ,

Parcel; surveyed unsurveyed

Right-of-way, roadrailway - utility

Reservation

Cliff, PR, Pile

Contour Interpolated Approximate Depression

Control ppint (horizontal) ... . , . .-t,..*i

Flooded land. .

Mine head frame . . M

Pipeline (above ground); ,. . jfl.vtj't'*" 1 ,,

Railway, aingtetrack. . . * t-double track abandoned . .

Road, highway, county, township access . . . ., trail, bush .

Shoreline (original) . .

Transmission line

Wooded area

(A) SURFACE e'MfHINS RIOHT8 CONTROLLED *r THl CHOWN (CMMM)

tGSJttOLOa StLVER ONLY CONTROLLED SY THC CHOW* i CAITAOA I .

(M) ALUMINUM MIGHTS CONTROLLED kV TMI CJMMtt, JCMIABA J ' ,

B MUCH, DEFT.,0^CWEP. RE3CRVE9 ft TRUSTS, INPIMI CITIZENSHIP ft IMMIGRATION, OTTAWA

LAND VNDtR LAKE SUMRIW WJTHWlAWN FBC* ItWtlN* BY 0*0*R IN COUNCIL DATED APRIL 30, HHB.

IHCICATIS EAif- **A '' ~

dM^^u^^u^MtoA|^~^^^Mk j^^^^^l^^^l^^^Mb

"^•^^^•"^^^W^^"^L. ^pWNlpRiNlBN]DSNNF*

msposmoNOPft*~ ***\Patent

Surface A Mining Rights .. Surface Rights OnlyMining Rights Only .. . .

LeaseSurface A Mining Rights Surface Rights Only Mining Rights Only

Licence of Occupation

OrdeHn-Council .

Cancelled . . .

Reservation

Sand A Gravel

SOURCES.ACCURACY IS NOT GUARANTEED. THOSEVWflNG TO STAKE MH4-

fMf WININO OR

NORTHERN QfVELOP-

^- l^-UU" -.

4O9 ( N S S

S . -- K ' J * *,* ?,, i,' *? i '*y-i

The disposition OM*ndtMap base and land disposition drafting to Surveys and Mapping Branch, Ministry of Natural Resources. this index was compiled m KfinNMrUNt purpews

84"! 4'

l 7 l IOOO* E

O II63T70

l [#465 4M

3\ /9

Ministry of Ministry ofNatural Northern DevelopmentResources and Mines

Ontario

INDEX TO LAND DISPOSITIONM S . 1 62 89,

w

G-3059TOWNSHIP

TUPPEDEC - P

|NMQ LANDS BHAHGH

M.N.R. ADMINISTRATIVE DISTRICT

SAULT STE. MARIEMINING DIVISION

SAULT STE. MARIELAND TITLES/REGISTRY DIVISION

ALGOMA

Scale 1.20 000

1000 1000Mctrm

2000IMras

1000Faat i-i i-t

1000 anoo 3000 4000 5000 6000 7000 •OOP 9000 10000rm FMI

Contour Interval 10 Metre*

AREAS WITHDRAWN FROM DISPOSITIONMRO - Mining Rights OnlySRO- Surface Rights OnlyH + S- M ining and Surface Rights

SYMBOLS Description OntorMo. Date DtofKMMon Flto

.BoundaryTownship, Meridian, Baseline

Road allowance, surveyed shoreline

Lot/Concession, surveyedunsurveyed

Parcel, surveyedunsurveyed t

Right-of-way, roadrailway . utility.

Reservation

Cliff, Pit, Pile

Contour ,. Interpolated Approximate Dephession

Control point (horizontal)

Flooded land

Mine head frame

Pipeline (above ground)

Railway, single track double track abandoned

Road, highway, county, township access trail, bush

Shoreline (original)

Transmission line

Wooded area

A

NOTES

(A) SURFACE AND MINING RIGHTS CONTROLLED BY THECROWN , (CANADA)

(G S) O O LO AND SILVER ONLY CONTROLLED BY THE CROWN(CANADA)

(M) ALL MINING RIGHTS CONTROLLED BY THE CROWN

(CANADA)

ENQUIRIES REGARDING (A), (G S l AND(M) SHOULD BEDIRECTED TO THE CHIEF, RESERVES AND TRUSTS,

INDIAN AFFAIRS BRANCH , DEPT OF CITIZENSHIP ANDIMMIGRATION, OTTAWA

•S-iSSS EASTERN BOUNDARY OF INDIAN LANDS

DISPOSITION OF CROWN LANDS/f r/-

PatentSurface ft Mining Righs Surface Rights OnlyMining Rights Only ,

i Lease

Surface ft Mining Rights Surface Rights Only . Mining Rights Onty

Licence of Occupationi

Order-in-Council - *

Cancelled

Reservation .

Sand a Gravel

e o

H B

T

oc

©

THE INFORMATION THAT APPEARS OH THIS MAP HAS BEEN OOMPILED FROM VARIOUS SOURCES. AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD Ow"*l- SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON

The i t - *ov mm

JAN -5

fl

Map base and land disposition drafting by Surveys and Mapping Branch, Ministry of Natural Resources

The disposition of land, location of lot fabric and parcel boundaries on this index was compiled for administrative purposes only

l01oOl CD

HCJ"D

m

H

T)

OJ O(Ji CD

RECEIVE D

WMC International Li miteAmericas Division — Exploration

WOLFE LAKE Cu-Au PROJECT

Geology, Sample Locations Magnetic Anoma ies

DATE: 07 MAR 96 DATE:

.1628

LEGEND

Rock Type

Orthoquartzite

Mineral Abbreviations

albite

orthoclase

hornblend

biotite

actinolite

sericite

muscovite

epidote

chlorite

hematite

quartz vein

quartz

magnetite

silicification

pyrite

chalcopyrite

outcrop

small outcrop

rock sample, number prefixed by CRT 03

bedding

cleavage

gneissosity

joint

shear zone

claim post

claim line

road

trail

inferred geologic contct

fault


magnetic anomaly boundary

163468

163478

1163465

116346763466

41K16NE0004 2 162B9 MARNE 240

MAR l 3 1996

WMC International LimiAmericas Division — Exploration

Cu-Au PROJECT

Geology, Sample Locations Magnetic Anomalies

DATE: 07 MAR 96 DATE:

.16280

LEGEND

Rock Type

11634711163472

Orthoquartzite


albite

orthoclase

hornblend

biotite

actinolite

sericitemuscoviteepidote

eh l onto

hematite

quartz vein

quartz

magnetite

silicification

pyrite

chalcopyrite

outcrop

small outcrop

rock sample; number prefixed by CRT 03

bedding

cleavage

gneissosity

joint

shear zone

claim post

claim line

road

trail


fault

—— —— inferred geologic contct


1163470

1191465

1191466

1163469

1163464

41K1BNE0004 2 1 6289 MARNE 250

\ Mgb \

1163477

1163475

\ Mgb \ \ Mgb v

1163476

1163474

LEGEND

1163473Rock Type

Orthoquorzite


abite

orthoclase

horn b Ion d

chlorite hematite quart? vejnj'lMfff, ' mhi.-'--1

~ quartz magnetite silicification pyrite chalcopyrite

actinolite

airicite

muscovite

epidote

outcrop

small outcrop

rock sample, number prefixed by CR103

bedding

cleavage

gneissosity

joint

shear zone

claim post

ctatm line

road

trail


fault

—— inferred geologic contct


RECEIVED

1996

2.16289 i

41K16NEOD04 2 16289 MARNE 260

163471 '

.NOTE. All rock samples numbers prefixed by CR103.

250 500 750

METRES

WMC International Liml+ecAmerlcas Division — Exploratlor

WOLFE LAKE Cu-Au P ROJECT

Geology, Sample Locations Magnetic Anomalies

NOTE. All rock samples numbers prefixed by CR103.

M

250 500

METRES

750 1000

WMC International LimitedAmericas Division — Exploration

WOLFE LAKE Cu-Au PROJECT

Geology, Sample Locations Magnetic Anoma ies

1 10000

ISION:

DATE:

PN: 4051

PLAN. 10KGLG

MAP No.

41K16NE0004 2 162BB MARNE 280

1163475 1163472

1163477

1163476

1163470

\ Mgb J

1163473

1163469

v Mgb \

REPORT ON GEOLOGICAL RECONNAISSANCE ......Keweenawan Rift beneath Lake Superior. The method of...

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Transcript of REPORT ON GEOLOGICAL RECONNAISSANCE ......Keweenawan Rift beneath Lake Superior. The method of...