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
page
3.5 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.
1974: No file number
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.
1976: No file number
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
Hoi f e Lake Trenches
Hoi f e Lake Trenches
Hoi f e 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
Wolfe Lake - Trench 2
Wolfe Lake - Trench 2
Wolfe Lake - Trench 2
Wolfe Lake - Trench 2
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
of property around old
patented claims.
Qtz (801)-Magnetite (20*) vein associated
wich gabbro. Pyrite .5 to It fg ~o sg
d i sseminated.
103048 Traverse in S.E. corner
of prrperty around old
patented claims.
Qtz-magnetite veins on the edge of foliated
gabbro.Stockwork is Qtz (30*) - Chi (60*; -
Magnetite (10*).
103049 Traverse in S.E. corner
of property around old
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
of property around old
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.
103052 Traverse in S.E. corner
of property around old
patented claims.
Hagnetite-Qtz-Chl stockwork in fractured pink
granite. Trace py.
103053 Traverse in S.E. corner
of property around old
paten-ed claims.
Gabbro - very coarse grained, porphyritic,
magnetic. Trace Py in chl qtz veinlets.
Probably the tail end of the stockwork.
103054 Traverse in S.E. corner
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.
103055 Traverse in S.E. corner
of property arcund old
patented claims.
Bleached Silicified, white, intrusive rock.
Ne mafic minerals. Hematitic fractures are
common.
103056 Traverse in S.E. corner
of property around old
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.
Traverse in S. E. corner
of property ar-und old
patented claims.
Traverse in c. E. corner
of p-roper*y arc-rid old
patentee rlaims.
Traverse in S. E. corner
of property around old
patented .claims.
Traverse from Kclfe Lake
to Prugh Lake area
Traverse from Viel f e Lake
to Prugh Lake area
Traverse from Kclfe Lake
to Prugh Lake area
Traverse from Kclfe Lake
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
Traverse in S. W. corner
of the claim block
Traverse in S. W. corner
of the claim block
Traverse in N.W. corner
of the claim block.
UTM : 705426, 5197496
Traverse in N.W. corner
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.
Red Granite - brick red colour due to
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
Red Granite - brick red colour due to
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.
103125 Traverse on old patented
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
103127 Traverse on old patented
claims - east side of
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
claims - east side of
claim block along the
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
103129 Traverse on old patented
claims - east side of
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.
103130 Traverse on old patented
claims - east side of
claim block along the
gabbro ridge.
Gabbro - similar tc 103130. 5 to 10*
magnetite in a chloritic schist, minor
sulphides along fractures.
103131 Traverse on old patented
claias - east side of
claim block along the
gabbrc ridge.
Gabbro - chloritic schist w/ 1-2 4 pyrite
within gound mass. Magnetite is disseminated
as very fine grains throughout.
43
103132 Traverse on old patented
claims - cass side of
claim block along the
gabbro ridge.
Gabbro - chloritic schist with 2-5* pyrite,
2-5* magnetite disseminated throughout, dark
areen
103133 Traverse or. -Id
claims - east side of
claim block along the
gabbro ridge.
Gabbro - fine grained, chl/anphibole,
magnetite disseminated throughout
103134 Traverse in N.W. corner
of the claim block
UTM: 706415, 5136844
Red Granite - brick red colour due to
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
Red Granite - brick red colour due to
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
Red Granite - brick red colour due to
hematized albite(k-spar?), quartz 10*,
feldspar 80*, mafic minerals 10*.
103137 Traverse in M.H. corner
of the claim block along
north trending road.
Red Granite - brick red colour due to
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
north trending road.
UTM: 7O623O, 519601O
Red Granite - brick red colour due to
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
103140 Traverse in N.H. corner
of the claim block along
north trending road.
UTM: 706075, 5195970
White Granite - consist dominantly of a white
feldspar, no quartz.
103141 Traverse in N.H. corner
of the claim block along
north trending road.
White Granite - quartz and feldspar w/ some
pink colouration (hematite) along fractures
and minor hematite in matrix.
103142 Traverse in N.W. corner
of the claim block along
north trending road.
Gabbro - medium grain size, dark green, 6C3
amphibole, 40* feldspar, slightly magnetic.
103143 Traverse in N.W. corner
of the claim block along
north trending road.
Pegmatite - minor myrmekitic textures, red
colouration due to multiple fine hematite
fractures, cuts through grey gneiss.
103144 Traverse -in N.W. corner
of the claim block along
north trending road.
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
Activation Laboratories Ltd. Work Order: 8286 Report: 8167
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.
Activation Laboratories Ltd. Work Order: 8349 Report: 8208
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
Activation Laboratories Ltd. Work Order: 8349 Report: 8208
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
Activation Laboratories Ltd. Work Order: 8349 Report: 8208
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
Activation Laboratories Ltd. Work Order: 8349 Report: 8208
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
Activation Laboratories Ltd. Work Order: 8349 Report: 8208B
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.
Activation Laboratories Ltd. Work Order: 8349 Report: 8208B
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.
Activation Laboratories Ltd. Work Order: 8269 Report: 8160
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
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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
Activation Laboratories Ltd. Work Order: 8269 Report: 8160
Sanpl* description
103010103011103012103013103014
10301510301610301710301810301}
103020103021103022103023103024
103025103026103027103028103029
103030103031103032103033103034
103035103101103102103103103104
103105103108103109103110103201
U PPM
co.scO. 51.81.22. J
0.8cO.50.9
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0.63.40.7
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1.8
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cO.50.6
144.25.6
271.9
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IA PPM
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0.10.35.20.04. R
0.40.61.10.1
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1.4cO.l0.40.30.2
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cO. 2CO. 21.60.41.5
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cO.ScO.51.3
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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
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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
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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
Activation Laboratories Ltd. Work Order: 8269 Report: 8160B
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.
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b.7.
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6.11.5.5.5.
7.6.7.6.5.
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8.6.6.5.5.
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19.28.10.
14.29.23.5.
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9.2.
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34.9.9.6.9.
10.5.
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18.28.
234.80.
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49.112.109.31.24.
36.345.44.21.
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CO. 5
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9.c5.cS.6.
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7.cS.C5.c5.cS.
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9.cS.cS.c5.c5.
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s.6.
209.46.
204.
28.83.
156.9.
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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.
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2.4.
32.4.6.
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c2.c2.c2.c2.C2.
c2.c2.c2.c2.c2.
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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
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ClOOClOOC103ClOOClOO
ClOOcIC'OClOO
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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.
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24.4.2.
IS.26.
2.3.S.
PBmi
b.s.S.7.S.
28.IS.IS.
inPPM
78.2.2.
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sn.77.61.
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278.tot*.
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5. n0.140.080.704.41
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0.500.070.010.170.51
0.040.110.10
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7.0]5.866.08
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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^^
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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
Ci^utpfn*nrt Rental Location de materiel
OeacrlpUon ' ;
Labour MalrHfoauvre , 'FVeW Supervision :: ;" SupervWon sur to Istfefc
^{.t
Tff*Aaaaya
Twa
AmountUonlent
11700.00
3850.00
^^^^^^^f^^i^iaiaiiLslen-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______~tRa^ardad 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
inferred geologic contct
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
Mineral Abbreviations
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
inferred geologic contct
fault
—— —— inferred geologic contct
magnetic anomaly boundary
1163470
1191465
1191466
1163469
1163464
41K1BNE0004 2 1 6289 MARNE 250
\ Mgb \
1163477
1163475
\ Mgb \ \ Mgb v
1163476
1163474
LEGEND
1163473Rock Type
Orthoquorzite
Mineral Abbreviations
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
inferred geologic contct
fault
—— inferred geologic contct
magnetic anomaly boundary
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 \