Post on 24-Apr-2018
transcript
39 DONA LAKE 010
DIAMOND DRILLING
AREA: DONA LAKE REPORT NO: 39
WORK PERFORMED FOR: Power explorations Inc.
RECORDED HOLDER: Same as above [ xx ] : Other [ ]
Cla
Pa Pa
Pa
Pa
Pa
Pa
Pa
Pa
Pa
am No .
7868567 786855
786856
850854
850855
850846
786864
786869
786868
Hole No.
EL-87-1
EL-87-2
EL-87-3 EL-87-4
EL-87-5
EL-87-6
EL-87-7
EL-87-8
EL-87-9
Footage
297'
317 1
397' 477'
307'
317'
257 '
327 '
397'
Date
Nov/87
Nov/87
Nov/87 Dec/87
Dec/87
Dec/87
Dec/87
Dec/87
Dec/87
Note
(1)
(1)
(1) (1)
(1)
(1)
(1)
(1)
(1)
NOTES: (1) #W8803.111, filed in August/88
iEOCflNEH"
I
1
l
l
J
l
l
l
l
REPORT ON
GEOLOGICAL MAPPING, PROSPECTING
AND
LITHOGEOCHEMICAL SAMPLING
AND
DIAMOND DRILLING
EYE LAKE PROPERTY
DISTRICT OF KENORA, PATRICIA MINING DIVISION
NORTHWESTERN ONTARIO
FOR
POWER EXPLORATIONS INC.
NTS 52-0/8E
ONTARIO GEOLOGICAL SURVEY ASSESSMENT FILES
APR 2 2 1988
RECEIVED
February 1988 R.I. Fogal, B.Se. R.A.V. Higginson, B.Se,
l l l l l ll I l l ll i i i i i i i
TABLE OF52088NE8888 39 DONA LAKE
VV \010C
MAR 2 81988*- HOI.O SUMMARY
2.0 INTRODUCTION
3.0 PROPERTY DESCRIPTION
4.0 LOCATION, ACCESS AND SERVICES
5.0 PHYSIOGRAPHY AND VEGETATION
6.0 PREVIOUS WORK
7.0 REGIONAL GEOLOGY AND ECONOMIC MINERALIZATION
8.0 PROPERTY GEOLOGY
8.1 General Geology
8.2 Volcanics
8.3 Intrusives
8.4 Metamorphism
8.5 Structure
9.0 GEOPHYSICAL SUMMARY
10.0 DESCRIPTION OF PROGRAMS
10.1 Geological Mapping, Prospecting, and Lithogeochemical Sampling Programs
10.2 Diamond Drilling Program
II.0 DISCUSSION OF RESULTS
12.0 CONCLUSIONS
13.0 RECOMMENDATIONS
13.1 Phase I
13.2 Phase II
14.0 ESTIMATED COST OF RECOMMENDED EXPLORATION PROGRAM
15.0 REFERENCES
Page
1
2
4
6
7
8
9
11
11
12
13
13
13
13
15
15
15
16
19
19
19
19
23
24
1111111111111I111111
LIST OF APPENDICES
AA CERTIFICATES OF QUALIFICATION
B TECHNICAL DATA STATEMENT AND REPORT OF WORK
C ROCK SAMPLE DESCRIPTIONS AND ANALYSES
D ROCK SAMPLE ASSAY CERTIFICATES
E DIAMOND DRILL LOGS
F LEGEND AND DIAMOND DRILL SECTIONS
G CORE SAMPLE ASSAY CERTIFICATES
LIST OF TABLES
TABLE NO. 1 - SUMMARY OF DRILL HOLE DATA
LIST OF FIGURES
FIGURE NO. 1 - LOCATION MAP
FIGURE NO. 2 - CLAIM SKETCH
FIGURE NO. 3 - PROPERTY LOCATION ANDREGIONAL GEOLOGY
FIGURE NO. 4 - PLAN OF DRILLING
FIGURE NO. 5 - LEGEND
FIGURE NO. 6 - DIAMOND DRILL SECTION: EL-87-1,2
FIGURE NO. 7 - DIAMOND DRILL SECTION: EL-87-3,4
FIGURE NO. 8 - DIAMOND DRILL SECTION: EL-87-5,6
FIGURE NO. 9 - DIAMOND DRILL SECTION: EL-87-7
FIGURE NO. 10 - DIAMOND DRILL SECTION: EL-87-8
FIGURE NO. 11 - DIAMOND DRILL SECTION: EL-87-9
LIST OF DRAWINGS
DRAWING NO. 1 - PROPERTY GEOLOGY-EYE LAKE SECTION
DRAWING NO, 2 - PROPERTY GEOLOGY - KOMAR SECTION
Back of report
II M II
II II II
II II II
II H II
II M II
II II II
Page 20
Page 3
Page 5
Page 10
Page 17
Appendix F
F
F
F
F
F
F
In map pocket
n H n
l l l l l l l l l l l l l l l l l l l
l. O SUMMARY
The Eye Lake property, held under a joint venture agreement
between Van Horne Gold Exploration Inc. and Power
Explorations Inc., is located in the Pickle Lake greenstone
belt, one mile east of the Placer Dome - Dona Lake Mine, and
6.5 miles southeast of the town of Pickle Lake.
The stratigraphy has been subdivided into two distinct
lithologic assemblages; a thick sequence of largely mafic
volcanics which grades into intermediate pyroclastic and
andesitic flows, and a broad package of banded gneiss to the east.
Anomalous gold mineralization of subeconomic grade was
encountered during both the surface geological exploration
program and the nine hole, 3,093 foot diamond drilling
program. The mineralization is hosted in quartz-carbonate
veining and sulphide-bearing horizons spatially associated,
or coincident with a geophysically interpreted regional
fault-shear system, which transects the property in a north-south direction.
A two-phase exploration program is warranted and recommended
for the property. Phase I of the proposed program would involve ground-magnetics and induced polarization surveys
along the interpreted regional break, followed by power
stripping, mapping and sampling of specific areas with
potential to host gold mineralization. Phase II would
involve a minimum of 2,000 feet of diamond drilling as a
follow-up to both Phase I and current progam results.
l l ll I l l ll i i i i i i i i i i
- 2 -
2.0 INTRODUCTION
The following report describes the results of a comprehen
sive exploration program consisting of geological mapping,
prospecting, lithogeochemical sampling, and diamond drilling
on the Eye Lake property in the Dona Lake area. The property
is located 6.5 miles southeast of the town of Pickle Lake
(Fig. No. 1) in the Patricia Mining Division, District of
Kenora, northwestern Ontario.
The present program and concurrent geophysical surveys,
including VLF-EM, ground magnetics and induced polarization,
were carried out by Geocanex Ltd.
The property consists of 69 contiguous mining claims. All
work was done on a cut picket line grid. The grid has a
north-south baseline with perpendicular lines at 400 foot
intervals across the strike of the local stratigraphy.
Several tie lines were cut to ensure control on long picket
lines. Geological mapping and geophysical plotting were done
at a scale of l inch ^ 200 feet.
The personnel involved in the geological surface exploration
program were:
R. Higginson Project Geologist Oro Station, Ontario
J. Drew Geologist North Bay, Ontario
B. Howes Field Assistant Kingston, Ontario
Geophysical anomalies were prospected and quartz veins and
mineralized volcanics were sampled. All sample descriptions
and assays are included in this report.
l
l
l
l
l
l
l
l
i
l
l
l
I
l
l
l
l
l
l
- 3 -
^,V^v,/^-O-I^-X-v
t
C." N 'V \\OWVPIMISKANLAKE
EYE LAKE'PROPERTYPICKLE5"?*
ONTARIO
KENORA-
^ '-) f ^ -'
''"'--c;-?'**r
li* 1 —c-L-i:-^^"" s-'""\i
UNITED
STATES
HEM LO,--'-v-;::7 X WAWA
TIMMINS*
KIRKLAND
SAULT STE MARIE
SUDBURY
^1'-" Greenstone Belts
ot
lOOmilo
POWER EXPLORATIONS INC.
EYE LAKE PROPERTY Patricia M.D., Ontario
LOCATION MAP
SCALE: It lOOmiDATE: FEB. 1988 I B Y; H.H./H.T.M
FIQ.NOi. l
l l l l ll i i i i i l i i i i t i i
- 4 -
The geological work was performed between July 22, 1987 and
August 5, 1987. The time breakdown for the work performed is
as follows:
Man-Days
Mapping and Prospecting: 33 1/4 Man-Days
The personnel involved in the diamond drilling program were:
R. Fogal Geologist Windsor, Ontario
R. Higginson Geologist Oro Station, Ontario
J, Pierce Field Assistant Wasaga Beach, Ontario
A total of nine holes were drilled to investigate geophysical
and geological targets proposed subsequent to the geological
surface exploration program. All diamond drill logs and
assays are included in this report.
The drilling program was carried out between November 23,
1987 and December 18, 1987. The time breakdown for the
diamond drill program is as follows:
Man-Days
Logging and Splitting Core: 52 Man-Days
3.0 PROPERTY DESCRIPTION
The Eye Lake property consists of 69 contiguous unpatented
mining claims in the Dona Lake area, Patricia Mining
Division, northwestern Ontario (Fig. No. 2). The claim
numbers and recording dates are as follows:
l
l
l
l
l
l
l
l
l
l
l
l
l
l
l
l
R l l
l90 0 05' CONNELL TWP
l l ,l s
f -T f lI'll9B49I5 j 964914) 964913 964912 964911
9B4920 964919 964918 B649I7
964932 964931 964928 964*27
MCCULLAGHTWR
' l l l l f- — — 4- — — 4- -i—-| 964925.964924 964925 964922 j 964921' '
964933) 964930 964929:
9S4926 \— — 4- —— -f- —— -4~ ' ——J ' 850845 j 8508461,
90S528 l 850849
850850850857 850856
J ': l l 903525 1 403526 . 9035zV 850852 '850851l
-"J-^——— i--, ——— IX-
786857 j 786856 ' 786855 j 78685
786850 786851 786852 78OT53
769379 j 786848 | 786847 l 788846
S
l786642 l 786844 l 786849
l l—— I— r——786840 i 786839 786838
51 0 25' ——
778970 778972 l 786837
- — --j- — —-f- — — -
786863(786864 ' 786865 ' 786866
— _ i _ _ L | _ — .
766869 . 786868 l 786867
7868,72 , 788B73
l mile
POWER EXPLORATIONS INC.
EYE LAKE PROPERTY Patricia M.D., Ontario
CLAIM SKETCH
OEOCANEX LTD TORONTO. CANADA
BYTR.tM.DATE JAN 1988 SC ALE: l"* 2640' FlG. No' 2
MINES, PAST PRODUCER
r"1--'
GEOLOGY LEGEND
'Gc'C C' t1 Ou'1 dO'y
LOCATION MAP
GOLD PRODUCTION -OZ? '."--1 .- 52.806
MAP AREA
Onto rio
On* or-o Geo'ogico' SurveyVise pope" 199, '984S'o" G V 9 Wo"ace HVap 2 2'9 , Co' Lake - D ' eh le Lone,Sage e' a' , '9/2
RED LAKE MD PATRICIA '
Pickte-L^.
Golden Patricia DiscoveryB60,000fo fl s ct 0-58oz7toi Au
Wright Lake
Obaskaka Lake
Hasaga200,000 tons o* 0-19 oz/ton Au
LAKE ST JOSEPH
Carpenter L.
90MINES, PAST PRODUCER
A Central Patricia No lB Cenfroi PatriCic MeC Pickle Crow No lD Pickle Crow No 2
E Albanyf tfowshoreG UMEX Thierry Vine
Collishaw Lake
GOLD PRODUCTION , ,PROPERTY TONS OZS GUL'D OZ/TON
t'-it o Parr.oo l, . . .f.cue Crov. 3,r37, 57? 1,446,214
Total 4,966,820 ?,068,020
MCCULLAGH . TWP
LAKE PROPERTYKOMAR SECTION
Dona Lake Discovery1,400,000 tons at 0-24oz7ton Au
Kawinogans Lake
POWER EXPLORATIONS INC.
EYE LAKE PROPERTY
Patricia M. D., Ontario/OsnaburghHasago
'? ?00,000 tons ot 0-19 oz/fon Au PROPERTY LOCATION AND REGIONAL GEOLOGY
l.AKE ST. JOSEPH
DATE: Jan.1988SCALE: 1 r 4miGEOCANEX LTD
TORONTO, CANADA
l l l l l l l l l l l l l l l l l l l
- 6 -
Claim Numbers
Pa 786837-
Pa 786842
Pa 786844-
Pa 786850-
Pa 786863-
Pa 786871-
Pa 778970,
Pa 769379
Pa 850845,
Pa 850849-
Pa 903525-
Pa 964911-
786840 inclusive
786848 inclusive
786857 inclusive
786869 inclusive
786873 inclusive
778972
850846
850857 inclusive
903528 inclusive
964933 inclusive
Recording Dates
April 30, 1984
April 30, 1984
April 30, 1984
April 30, 1984
April 30, 1984
April 30, 1984
April 30, 1984
April 30, 1984
February 13, 1986
February 13, 1986
June 24, 1986
January 29, 1987
Total Claims 69
The claims are held under a joint venture agreement between
Van Horne Gold Exploration Inc. and Power Explorations Inc.,
both of 1003-34 King Street East, Toronto, Ontario, M5C 1E5.
4.0 LOCATION, ACCESS AND SERVICES
The property can be reached by float/ski plane or helicopter
from Pickle Lake 6.5 miles to the northwest. An all weather
gravel road from Highway 599 ends one mile west of the
property at the Placer Dome Inc. gold deposit near Dona Lake.
A winter drilling road extends from the mine to the
property.
Pickle Lake is a mining and transportation centre with a
population of approximately 350. The Dona Lake mine, slated
for production, has sparked new developments in Pickle Lake,
including housing and related service facilities. UMEX
l l l l l l l l l l l l l l l l l l l
7
Inc. (Union Miniere) operates a 4,000 TPD copper-nickel mine
and concentrator seven miles northwest of Pickle Lake. The
mine is presently closed due to depressed base metal prices.
Pickle Lake is connected by paved Highway 599 to Savant Lake
and the Canadian National transcontinental railway line, 90
miles to the south, and to Ignace and Trans Canada Highway
17, 180 miles to the south. Electricity is supplied by a
hydro line connecting Pickle Lake to the Ear Falls generating
station. Air, ground and water transportation for local use
are readily available in town. Pickle Lake is also serviced
by regular NorOntair flights from Thunder Bay.
5.0 PHYSIOGRAPHY AND VEGETATION
Most of the property is covered by flat-lying spruce and
spruce-tamarack over muskeg. Cedar-alder swamps and grassy
bogs surround several small lakes and creeks. Several
northeast-southwest trending glacial ridges occur in the
central portion of the property, with hummocky glacial mounds
prevailing to the south. Many of the ridges are bedrock
controlled with outcrop exposures flanking individual ridges.
Vegetation on the ridges consists of birch-poplar and spruce
forests.
Outcrop exposures constitute S-10% of the property, and are
generally confined to the west and central portions of the
property.
l l l l l l l l l l l l l l l l l l l
- 8 -
6.0 PREVIOUS WORK
In 1967, M. Firth had two holes drilled 1/2 mile southwest of
the property. The drilling encountered andesite, dacite and
rhyolite with minor mineralized tuff horizons. The minerali
zation consisted of pyrite, pyrrhotite and trace chalcopy
rite. Assay values up to 0.01 ounces of gold per ton and
Q.13% copper were reported.
In 1984, Van Horne Gold Exploration Inc. staked the original
block of 31 claims. Geocanex Ltd. was contracted to
undertake geological mapping and geophysical surveys,
including ground magnetics and VLF-EM (Gillick, R.E., 1984, and North, J.W., 1984). Assays of 0.093 and 0.206 ounces of
gold per ton were obtained from grab samples of sulphide and
sulphide-quartz filled shears in andesite. This showing is
located east of BLO between L79N and L78N. Several geo
physical anomalies interpreted as potential gold-bearing
sulphide mineralization zones associated with faulting were
detected in the southwestern part of the property.
In 1985, Geoterrex Ltd. flew airborne regional electro
magnetic and total intensity magnetics surveys over the
Pickle Lake area for the Ontario Geological Survey. The
surveys covered the entire Eye Lake property.
In 1986, Van Horne Gold Exploration Inc. obtained an
additional 28 claims adjoining the original property to the
north. Van Horne Gold Exploration Inc. subsequently signed a
joint venture agreement with Power Explorations Inc.
Geocanex Ltd. was then contracted to complete the current
geophysical, geological and diamond drill programs.
l l l l l l l llllllllllll
- 9 -
7.0 REGIONAL GEOLOGY AND ECONOMIC MINERALIZATION
The Pickle Lake area is located within the Uchi Subprovince,
a part of the Superior Province of the Canadian Shield. The
area is characterized be several arcuate, highly deformed and
coalescing greenstone belts, consisting of predominantly
mafic to intermediate volcanic flows, which have been
intruded by numerous granitic to ultramafic intrusive bodies.
The metamorphic grade ranges from greenschist to amphibolite
facies. The volcanics host subordinate amounts of felsic to
mafic pyroclastics, sediments and iron formation. Felsic
quartz-feldspar porphyry dykes are commonly found in all
lithologies (Fig. No. 3).
Ultramafic rocks host copper-nickel mineralization at the
Union Miniere Thierry Mine, seven miles northwest of Pickle
Lake, with mined ore and mineral reserves totalling
14,000,000 tons grading 1.6% copper and Q.2% nickel.
Historically, gold production in the Pickle Lake area has
occurred in structurally controlled vein type deposits or
sulphide replacement bodies spatially associated with, or
contained within, bands of Algoman (chert-magnetite) iron
formation.
The former producing Pickle Crow and Central Patricia mines
operated from 1935 to 1966 and 1934 to 1951, respectively,
collectively producing 2,068,020 ounces of gold from
4,966,820 tons of ore for an average grade of 0.416 ounces of
gold per ton. Gold was recovered from quartz veins, vein
networks and sulphide replacement bodies which occupied
shears, faults, fissures and fold axial plane fractures in
highly deformed mafic volcanics and iron formation. Gold-
bearing quartz veins were also mined within quartz-albite
l l l l l l l l l l l l l l l l l l l
- 11 -
porphyry sills near the contact of mafic volcanics and iron
formation.
Placer Dome Inc. and St. Joe Canada Inc. both recently
announced plans to open new mines in the Pickle Lake area.
Placer Dome's Dona Lake property, located approximately one
mile west of the Eye Lake property, has reported reserves of
1,500,000 tons grading 0.3 ounces of gold per ton. Gold
mineralization occurs as sulphide replacement bodies within a
band of highly deformed oxide facies iron formation (Northern
Miner, September 1986). The mine is expected to produce
approximately 40,000 ounces of gold per year over a ten year
period.
St. Joe Canada's Golden Patricia property is reported to have
an estimated 500,000 ounces of gold reserves with a grade of
0.58 ounces of gold per ton. The property is located
approximately 40 miles west of Pickle Lake. Gold minerali
zation occurs in a quartz vein at a contact between a
mylonitized unit and sheared mafic volcanics in close
proximity to banded iron formation (Northern Miner Magazine,
September 1986). The initial mining project has drill
indicated reserves of 283,000 tons grading 0.88 ounces per
ton, and is expected to produce 40,000 ounces of gold
annually (Northern Miner, March 23, 1987).
8.0 PROPERTY GEOLOGY
8.l General Geology
The Eye Lake property is underlain by a north-south trending
limb of the Pickle Lake greenstone belt. The local strati
graphy, as noted by North (1984) can be subdivided into two
l l l l l l l l l l l l l l l l l l l
- 12 -
broad sequences: a thick package of mafic volcanics,
including basalt, andesite and amphibolite in the western
portion of the property grading into dacitic pyroclastics and
andesitic flows in the north-east and north central portions
of the property; and a thick sequence of banded gneiss
forming the second area in the eastern part of the property.
The volcanic-gneiss contact has been interpreted as a fault
contact which trends north-northeast across the property.
Gillick (1984) and Medd (1987) indicate that this fault is a
continuous regional feature.
8.2 Volcanics
Mafic volcanics exposed west of BLO+00 are fine-grained,
green, chloritic pillowed to massive flows of basaltic to
andesitic composition. The pillows are generally deformed,
however an exposure on L28+OON at L17+OOW provided a west
facing top direction.
East of the baseline, the mafic volcanics grade into dacitic
tuffs and andesitic flows.
The tuffs are light green to buff in colour, fine-grained,
and laminated to banded.
Banded gneiss exposed in the southwestern portion of the
property is described by North (1984) as varying composi-
tonally from biotite-quartz gneiss to hornblende-quartz-
gneiss.
l l l l l l l l l l l l l l l l l l l
- 13 -
8.3 Intrusives
A felsic quartz-feldspar porphyry intrusive sill is exposed
at LSO+OONjlO+OOE. The intrusive has an orange-buff fine
grained groundmass of quartz and feldspar with euhedral
porphyritic feldspar laths.
8.4 Metamorphism
The volcanics exposed in the west and central portion of the
property are highly chloritic and indicate a metamorphic
grade of greenschist facies. The banded gneisses in the
southwest corner of the property exhibit lower amphibolite
facies metamorphism. It is suggested that the volcanics and
gneisses are separate units that are fault bounded, and do
not represent gradual changes in metamorphic grade across the
property.
8.5 Structure
Minor isoclinal and kink folding was noted in several
locations on the property and may represent parasitic
features associated with large scale folds and faults
interpeted from geophysical data.
Observed shearing and foliation directions are roughly
concordant with bedding directions obtained from pillows in
the western part of the property and trend due north to
north-northeast.
l l l l l l l l l l l l l l l l l l l
- 14 -
9.0 GEOPHYSICAL SUMMARY
Several ground magnetic, VLF-EM and regional airborne magne
tic surveys have been completed over the Eye Lake property.
Based on these surveys, two lithologic packages have been
delineated, separated by an interpreted fault contact
trending approximately north-south through to the middle of
the property. The west side is generally characterized by
relatively higher amplitude magnetics than the eastern
portion. Both units exhibit discontinuous, irregular lenti
cular magnetic expressions roughly trending in a north-south
direction, which corresponds to the regional magnetic
expression.
A large fold/fault structure has been detected in the north-
central area of the property, along the previously mentioned
contact. Several inferred faults transect both lithologic
units, manifested as magnetic discontinuities and/or abrupt
interruptions in the magnetic expression.
Several discontinuous VLF-EM conductors trending subparallel
to the property stratigraphy have been delineated. These
have been interpreted to represent weak to moderate zones of
disseminated mineralization. Of particular interest is a
north-northeast trending conductor in the southwest corner of
the property coinciding with a small creek/lake system. A
fault or shear related source is suggested for this anomalous
conductor.
Combined, these surveys proved valuable in delineating
favourable diamond drill targets.
l l l l l l l l l l l l l l l l l l l
- 15 -
10.0 DESCRIPTION OF PROGRAMS
10.1 Geological Mapping, Prospecting and Lithogeochemical
Sampling Programs
The geological mapping, prospecting and lithogeochemical
program was carried out between July 22, 1987 and August 5,
1987, by Geocanex Ltd. Maps were prepared at a scale of l
inch to 200 feet and may be found at the back of the report.
A total of 37 grab samples were collected from favourable
geologic environments. The main focus of sampling included
quartz and quartz carbonate veins and vein networks, sheared and altered volcanics, and sulphide-mineralized horizons.
Bondar-Clegg and Company Ltd., of Ottawa, Ontario analyzed
all submitted surface samples for gold using fire assay
techniques. All results and sample descriptions are included
in Appendix C. Analytical certificates are shown in Appendix D.
10.2 Diamond Drilling Program
The diamond drilling progam was contracted to Midwest
Drilling of Winnipeg, Manitoba. A total of nine B.Q. size
(1-7/16") diamond drill holes totalling 3,093 feet were
completed between November 23, 1987 and December 18, 1987,
under the supervision of Geocanex Ltd. Diamond drill hole
targets were chosen subsequent to the geological mapping/
sampling program. Favourable geophysical targets were also
considered for diamond drill hole testing.
Midwest Drilling provided room and board on site for both
geological and drill crews. The camp was supplied by heli
copter and ski-plane from Pickle Lake.
l l l l l l l l l l l l l l l l l l l
- 16 -
Detailed core logging was followed by sampling of favourable
horizons. A total of 507 samples were submitted, each
consisting of halved core, over intervals from .5 to 5.0 feet
in length. Core samples were analyzed by two separate
laboratories over the course of the program. The labora
tories involved were Bell-White Analytical Laboratories Ltd.
of Haileybury, Ontario, and Assayers (Ontario) Limited of
Toronto, Ontario.
All samples were analyzed for gold using standard fire assay
techniques; results were reported in ounces of gold per ton.
Hole locations are shown in Figure No. 4. Drill sections are
shown in Appendix F. Diamond drill logs and assay certifi
cates are enclosed in Appendices E and G respectively.
11.0 DISCUSSION OF RESULTS
Several anomalous gold values were obtained during the
mapping and prospecting phases of the program. Significant
gold values up to 1,220 parts per billion were encountered in
various lithologies. A common feature to all of the anoma
lous values was the presence of quartz carbonate veining and
limonitic staining indicating a probable sulphide-gold
association.
On the basis of compiled geological, geochemical and geophy
sical data, several favourable fault-fold structures and
potentially gold-bearing sulphide horizons were defined. A
preliminary set of nine holes were thus chosen to test these
features.
l l l l l l l l l l l l l l l l l l
- 18 -
The primary drilling target of this program was a moderate to
strong VLF-EM conductor interpreted as a regional, north-
south trending fault-shear zone. Several trenches occurring
on the flank of the main conductor were grab sampled by North
(1984), and reportedly returned gold values of .206 and .093
ounces per ton.
Elevated gold values were obtained from Holes EL-87-1, 2, 3
and 4 (see Table No. 1). Hole EL-87-1 returned a 5.0 foot
intersection grading .010 ounces per ton gold in intermediate
to felsic tuff containing quartz ^ carbonate stringers with
minor sulphides. Hole EL-87-2 y-ielded a 5.0 foot interval of
.02 ounces per ton gold in quartz j^ carbonate veinlets hosted
in intermediate flows. Hole EL-87-3 returned .026 ounces per
ton gold over 3.0 feet in well-banded intermediate tuff
containing up to 31 pyrrhotite, pyrite and trace chalco
pyrite. A 21.0 foot interval in Hole EL-87-4 returned gold
values ranging from trace to .024 ounces per ton in inter
bedded felsic and intermediate tuffs containing S-5% pyrite
and pyrrhotite. Hole EL-87-5 returned a gold value of .024
ounces per ton over 1.9 feet in calcite j^ quartz veinlets
containing up to 3ti pyrite and pyrrhotite hosted in mafic to
intermediate volcanics.
The gold mineralization in these holes was intersected in
various lithologies, however, it was consistently associated
with quartz jj^ carbonate stringers and/or pyrite-pyrrhotite
mineralization.
l l l l l l l l l l l l l l l l l ll
- 19 -
12.0 CONCLUSIONS
Gold mineralization of sub-economic grade was encountered on all phases of the current program. Compilation of geological, geochemical, geophysical and diamond drilling results indicate that the gold mineralization encountered occurs in association with quartz-carbonate veining and sulphide-bearing horizons, spatially related to a geophysically indicated regional fault-shear system, which transects the property in a north-south direction.
Additional work is warranted and indicated to delineate the nature and extent of potentially economic gold minerali zation.
13.0 RECOMMENDATIONS
A two-phase exploration program is recommended and warranted for the property and would involve:
13.1 Phase I
Geophysical surveys, including detailed ground magnetics with readings at 10 to 25 foot intervals, as well as induced polarization on a 100 foot spaced picket line grid over selected portions of the regional fault-shear system. This would be followed by power stripping of selected sites to delineate potential structurally or stratigraphically controlled gold mineralization.
13.2 Phase II
A minimum of 2,000 feet of diamond drilling is estimated to test potentially gold-bearing structures and horizons defined in Phase I and as a follow-up to the current program.
TABLE I SUMMARY TABLE OF DRILL HOLE DATA
Drillhole Number
Grid Location (metric)
Length
(feet)
ASSAY RESULTSSUMMARY DESCRIPTION Intersection
(feet)Width (feet)
oz./Au/ ton
Description
EL-87-1 0+50S, 297 Mafic flows intercalated with felsic to inter- 2+15E mediate well banded tuffs, exhibiting two
distinct sulphide-bearing silicified zones, typically containing minor sericite j^ garnet.
195.5-200.5 5.0 .010 Felsic to inter mediate tuffs, well developed banding, sul phides to 5% l containing quartz HK carbo nate stringers.
EL-87-2
EL-87-3
0+50S, BL 0
11+OON, 6+35E
317 Thick intermediate flows with minor felsic 105.0-110.0 constituent as well as a banded tuff horizon, typically containing abundant barren quartz + carbonate veinlets, randomly distributed.
397 Felsic to intermediate flows, with minor 370.5-373.7 poorly banded siltstone as thin horizons, and
5.0 .020 Intermediate flows containing irregular quartz * carbonate stringers, minor chlorite, sul phides to 2% as fracture coatings .
3.2 .026 Well banded intermediate
ro o
intermediate tuffs dominating further down hole. Trace disseminated sulphides and garnet.
tuffs, abundant quartz -*- calcite stringers. Trace sulphides.
EL-87-4 11-K30N 477 Dominantly mafic to intermediate flows and 3+20E tuffs, minor narrow siltstone horizons and
quartz - feldspar porphyry.
Abundant quartz j^ carbonate, sericite, epidote.
with lesser
89.2-91.0 1.8 .016 Well banded maficto intermediate tuff, minor silt stone, quartz- carbonate stringers.
240.6-242.6 2.0 .012 Mafic to inter- 252.0-255.6 3.6 .014 mediate tuffs,
containing pyrite * pyrrhotite
TABLE I SUMMARY TABLE OF DRILL HOLE DATA
Drillhole Grid Length Number Location
(metric) (feet)
ASSAY RESULTSSUMMARY DESCRIPTION Intersection Width oz./Au/ Description
(feet) (feet) ton
fracture infill ing to 5?;. Minor associated garnet .
426.0-430.0 4.0 .012 Interbedded 433.5-437.0 3.5 .016 felsic and inter- 442.0-447.0 5.0 .024 mediate tuffs,
abundant carbonate vein- lets, minor pyrrhotite blebs; garnets to 5*.
EL-87-5 44+50N, 307 3+30W
EL-87-6 44+50N, 317 9+OOW
EL-87-7 0+00, 257 12+55W
Mafic to intermediate flows and tuffs contain- 186.8-188.7 1.9 .024 Massive mafic to ing several highly altered, silicified zones, intermediate minor sericite, tourmaline. flows, finely
disseminated sulphides to 3%.
Dominantly mafic to intermediate volcanics as flow and tuffs, moderately carbonate zed. Abundant quartz * calcite typically barren.
Mafic to intermediate tuffs, containing minor mafic flows. Highly silicified section,
l
K)
containing up to 5% sulphides, occurs with minor associated sericite + muscovite.
TABLE I SUMMARY TABLE OF DRILL HOLE DATA
Drillhole Number
Grid Location (metric)
Length
(feet)
ASSAY RESULTSSUMMARY DESCRIPTION Intersection
(feet)Width (feet)
oz./Au/ ton
Description
EL-87-8 2OOOS, 327 Mafic to intermediate volcanic flows, massive, 7-fOOW grading into well banded tuffs of similar
composition. Sporadic quartz * calcite veinlets, typically barren. ~~
24+OOS,397Mafic to intermediate tuffs, overlain by flows 1+60E of similar composition. Trace sulphides as
fine disseminations throughout.
EL-87-9
l - 23 -
l 14.0 COST OF RECOMMENDATION
14.1 Phase I
l Line cutting 25.5 miles at ?350Xlinemile, all inclusive————————————————————————5 8,925,00
l Ground magnetics at 10 to 25 footintervals, over 36 miles at ?3007linemile, all inclusive————————————————————————5 10,800.00
— Induced Polarization survey overselected VLF-EM axes 5 line miles
M at 31,2007line mile———————————————————————5 6,000.00
Power stripping/trenching, bacXhoe
I plus operator for 10 days at a rate of ^SOO/day, all inclusive———————————————————5 5,000.00
g Trenching, mapping and sampling, onel geologist plus assistant for 10 days at— a rate of SSOO/day, all inclusive—————————5 5,000.00
l Contingencies 201——-————————————-——-——-——3 7,145.00
Total Cost of Phase I ——————————————————————— S 42,870.00
l 14.2 Phase II
I Diamond Drilling: 2,000 feet at a rate of 535/foot——————————————————————————5 70,000.00
— Contingencies 20*———————————————————————S 14,000.00
" Total Cost of Phase II———————————————————? 84,000.00
l Total Cost of Phases I and II —————————————— 3126,670.00
fl Respectfully Submitted,
l R.A.V. Higgihson, B.Se.
I s/YsT^ tf "7c s f*' f f* t—*- '''f fi
R.I. Fogal, B.Se. Geocanex Ltd.
l
l l l l l l l l l l l l l l l l l l l
- 24 -
:5.0 REFERENCES
Gillick, R.E., 1984. Report on Ground Magnetic and VLF-EM Surveys on the Eye Lake property of Van Horne Gold Exploration Inc. for 591343 Ontario Ltd., Pickle Lake area, Northwestern Ontario; unpublished report of Geocanex Ltd.
Map 2218. Cat Lake - Pickle Lake area, O.G.S. Geological Compilation Series.
Medd, S.B., 1987. Report on Magnetic and VLF-EM Surveys on the Komar Property, District of Kenora, Patricia Mining Division, Northwestern Ontario for Van Horne Gold Exploration Inc.; unpublished report of Geocanex Ltd.
North, J.W., 1984. Report on Geological Mapping and Geochemical Sampling, Eye Lake property, Dona Lake area, Patricia Mining Division, Northwestern Ontario for Van Horne Gold Exploration Inc.; unpublished report of Geocanex Ltd.
O.G.S., 1980. Dona Lake area, District of Kenora (Patricia Portion); Ontario Geological Survey Preliminary Map P.2319, Sioux Lookout Data Series, Scale 1:15,840. Data compiled 1979.
O.G.S., 1986. Airborne Electromagnetic and Total Intensity Magnetic Survey, Pickle Lake area, District of Kenora (Patricia Portion), Ontario; by Geoterrex Limited for Ontario Geological Survey, Geophysical/ Geochemical Series, Map 80932, 80934. Scale 1:20,000. Survey and compilation from February to July, 1986.
O.G.S., Resident Geologist Files - Toronto and Sioux Lookout, Various unpublished assessment reports.
CERTIFICATE OF QUALIFICATIONl l l l l l l l l l l1
V"i /^A, j J /tf&f B DATED THIS 7 DAY OF /'//U^ //^*
l
l
l
l
l
THIS IS TO CERTIFY THAT:
I am a resident of Oro Township, Ontario.
I am a graduate of the University of Waterloo, Waterloo, Ontario, with a degree in Bachelor of Science, Earth Science; major (Geology).
I have worked continuously as an exploration geologist since 1984, in gold exploration in northwestern Ontario.
I supervised geological mapping and geochemical sampling programs on the Eye Lake property, from July 22, 1987 to August 5, 1987.
The statements contained in this report, and conclusions reached, are based upon the study of all relevant assessment work records of the Ontario Geological Survey, and geological reports and maps published by the Ontario Ministry of Natural Resources.
In this report, I have disclosed all relevant descriptive and interpretative material, which is, to the best of my knowledge, necessary to gain a complete understanding of the viability of the project and the recommendations.
Robert A.V. Higginson, B.Se Geologist
l l l l l l l l l l l l l l lal
EYE LAKEMinistry of Geophysical-Geologlcal-Geochemical Northern Development Technical Data Statementand Mines
Ontario
TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT
TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.
Type of Survey(s). Township or Area. Claim Holder(s)—
Geological Sampling S Mapping
Dona Lake—.^—,,—,—.,.-———.——,—— Power Explorations Inc.
Survey Company —. Author of Report — Address of Author R ' R -
Geocanex Ltd.R. Higginson
Oro Station, Ontario, LOG
Covering Dates of Survey July 22, 1987 ~ August 5.(linecutting to office)
Total Miles of Line Cut—————————.————.——————.
1987
SPECIAL PROVISIONS CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.
ENTER 20 days for each additional survey using same grid.
Geophysical
—Electromagnetic.
—Magnetometer_—Radiometric——
—Other-™—-
DAYS per claim
40
Geochemical.AIRBORNE CREDITS (Special provision credit* do not apply to airborne jurveyi)
Magnetometer. .Electromagnetic
DATE:.
(enter dayi per claim)
SIGNATURE:t or Agent
Res. Geol.. .Qualifications.Previous Surveys
File No. Type Date Claim Holder
MINING CLAIMS TRAVERSED List numerically
See Attached Sheet(prefix) (number)
i
TOTAL CLAIMS. 38
837 (857(2)
GEOPHYSICAL TECHNICAL DATA
GROUND SURVEYS — If more than one survey, specify data for each type of survey
[
INDUCED POLARIZATION
PFmSTTVTTV GRAVITY ELECTROMAGNETIC MAGNETIC
Miimher of Stations Niimher of Readings
Station interval Line spar.ina
Profile srale
Hontour interval
Instrument
Arrurary — Srale ronstant
Diurnal rorrertion method
Rase Station rherk-in interval (hours)
Rase Station loration and value
Instrument
Toil ronfipuration
Toil separation
Arrurary
Method: CD Fixed transmitter O Shoot back O In lineFrequenry
(specify V.L.F. station)
Parameters measured
Instrument
Srale ronstant
Torrertions made
Base station value and loration
Elevation accuracy
Instrument .. ..
Method d Time Domain D Frequency DomainParameters - On time Frequency
Off time Range1
' — J Via y timet | — Tnt^gratinn time
i i-
Electrode array- ————————————————————————————————————————————————
Electrode spacing — ———————————————————————————————————— - — —— — ——Type of electrode . ——————————————————————————————————————————————————
1111111
D Parallel line
1
1
1
1
1
1
1
1
1
1
GEOCHEMICAL SURVEY - PROCEDURE RECORD
Numbers of claims from which samples taken 964922, 964917, 850857, 850856, 903525, 903527, 786856, 786868, 850854
Total Number of Samples Type of Sample.
37
(Nature of Material)
Average Sample Weight——————— Method of Collection Grab Samples
2 kg
Soil Horizon Sampled. Horizon Development. Sample Depth————. Terrain.————————
Drainage Development——————————— Estimated Range of Overburden Thickness.
ANALYTICALValues expressed in: per cent
p. p. m. p. p. b.
D d S
Cu, Pb, Zn, Ni, Co, Ag, Mo, As.-(circle)
___Gold
Field Analysis (. .tests)Extraction Method.AnalyticalReagents
Field Laboratory AnalysisNo. (.——-.-^——
SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)
Mesh size of fraction used for analysis -150
Extraction Analytical Method. Reagents Used __
Commercial Laboratory 37 -tests)Name of Laboratory, Bondar-Clegg s Co. Extraction Mrthnrl Aqua Regia ______ Analytical Reagents Used
F. A. - A. A. S.
GeneraL General.
1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1
t
SELF POTENTIALInstrument
Survey Method
Corrections made
RADIOMETRIC
Instrument
Values measured
Energy windows (levels)
Heipht of instrument
Size of detector
Overburden
Range
Background Count ,
(type, depth - include outcrop map)
OTHERS (SEISMIC, DRILL WELL LOGGING ETC.)
Type of survey
Instrument
Accuracy,
Parameters measured
Additional information (for understanding results),,. ,
AIRBORNE SURVEYSType of snrvey(s) .. .
Instrument(s) — ————————————————————————————————(specify for each type of survey)
Accuracy(specify for each type of lurvey)
Aircraft used,
Sensor altitude . . ,
Navigation and flight path recovery method ,C* O l J
Aircraft altitude
Miles flown over total area
Line Snarino
Over claims only
—————————————————————— ^^^^^^m^mf
l l l l l l l l l l l l l l l l l l l
- LIST OF CLAIMS
P,-i H 5 O H 4 5 R r)OH46
Pa H50H49 M 5 OH 5 O M50H5 l H 5OB 5 2 H 5 O H 5 3 H50H54 M50H55 H50H56
Pn 90 3 r) 2 5
903527 90 3 r) 2 M
J'a 96491.1 9649 l 296491396491496491596491696491 7964910964919964920964921964922964923964924964925964926964927 96492H964929964930964931964932964933
Totnl : 38 Claims
11 '11I11111w1
1111111
^ EYE
SAMPLE # ASSAY #
KE-1 1201
KE-2 1202
KE-3 1203
KE-4 1204
JD-01 1205
JD-02 1206
JD-03 12-7
JD-04 1208
JD-05 1209
JD-06 1210
JD-07 1211
JD-08 1212
JD-09 1213
JD-10 1214
JD-11 1215
LAKE GRAB
LOCATION
63+OON,42+OOE
60+OON,20+30E
50+OON,09+30E
48+20N,06+60E
48+OON,16+50E
48+OON,16+50E
45+25N,09+50E
45+25N,09+50E
44+30N,08+40E
44+30N,08+40E
44+40N,08+35E
36+70N,07+80W
31+80N,17+OOW
31+80N,17+OOW
31+80N,17+OOW
SAMPLE DESCRIPTIONS
DESCRIPTION
grab, highly folded dacite tuff withquartz vein, quartz-carbonate-hematitestringers, i-2% arsenopyrite.
12" quartz vein in dacite tuff.
24" quartz-feldspar porphyry in ande-sitic-dacitic volcanics.
8" X 24" quartz pod in folded inter mediate volcanics.
intermediate-volcanic (dacite tuff?) withlimonite staining along fractures.
quartz vein, 6", in intermediate vol canics, limonite staining near wallrock.
silicified intermediate volcanics withheavy limonite staining.
quartz pod (2" X 6") in intermediatevolcanics.
dacitic tuff(?) with trace-0.5% pyrite,minor limonite staining.
6" quartz vein, folded, minor limonitestaining, trace-0.5% pyrite.
folded, intermediate volcanics{possibly dacitic tuff with trace-0.5%pyrite), heavy limonite staining.
3" quartz vein, cross-cutting maficvolcanics, minor limonite staining.
4' wide quartz vein network, chertnear center of veins, limonite stain ing near contact with mafic volcanic.
mafic volcanic with carbonate and minorlimonite staining.
3" wide felsic dyke, boudinages andsinistrally offset.
Au ppb
^
^
10
5
10
^
10
105
10
925
1220
90
95
10
5
11 ' 1111111111I111111
tSAMPLE #
JD-12
JD-13
JD-14
JD-15
EY-BH-1
EY-BH-2
EY-BH-3
EY-BH-4
EY-BH-5
EY-BH-8
EY-BH-6
EY-BH-7
JD-16
JD-17
EY-BH-9
ASSAY
1216
1217
1218
1219
1220
1221
1222
1223
1224
1225
1226
1227
1228
1229
1230
EYE LAKE GRAB
# LOCATION
26+OON,22+40W
26+OON,22+40W
27+70N,17+OOW
27+70N, 17+OOW
03+48E,16+OON
13+OON,03+50E
12+OON,03+85E
11+OON,03+50E
11+OON,03+50E
11+OON,03+50E
10+25N,03+40E
10+25N,03+40E
00+80S, 00+80W
00+80S,00+80W
03+80E,08+OON
SAMPLE DESCRIPTIONS
DESCRIPTION
10" wide shear in mafic volcanic(pillowed) with quartz stringers throughout.
2" X 6" quartz pod, minor limonitestaining.
12" X 18" quartz pod in pillowedmafic volcanic, minor limonite stain ing.
12" quartz cross-cutting pillows, minor limonite staining.
dacite, minor limonite staining.
mafic, fine pillowed flow minor ironweathering.
andesite, limonite staining.
quartz vein, 2" wide, traces of pyrrho-tite/pyrite and arsenopyrite.
andesite, minor limonite staining,traces of pyrite.
andesite, disseminated sulphides,S-5% pyrite, T-2% arsenopyrite.
andesite, 1-23, pyrite.
quartz pod, 3" X 12", clear.
12" wide felsic dyke in intermediate volcanics.
mafic volcanics with limonite stain ing, trace pyrrhotite.
quartz vein, 3" wide, minor ironstaining.
Au ppb
70
^
5
tf
^
^
25
630
15
100
10
G
^
5
5
11 1111111g1111iiiiii
^ EYE LAKE GRAB
SAMPLE # ASSAY # LOCATION
JD-18 1231 mOON,04+OOE
JD-19 1232 11+OON,04+OOE
JD-20 1233 09+OON,03+80E
JD-21 1234 08+OON,04+OOE
KE-5 1235 31+90N,14+50W
EY-BH-10 1236 18+50N,30+OON
KE-6 1237 20+80S,05+OOW
SAMPLE DESCRIPTIONS
DESCRIPTION Au
6" wide sheared dacite (?), 2-33Spryite, quartz-carbonate stringers.
3" wide quartz-carbonate vein with2-3# pyrite, limonite staining.
1" quartz carbonate vein, trace-0.5%pyrite, limonite staining.
medium grained mafic volcanic withtrace-0.5% pyrite, quartz-carbonatestringers present, limonite staining.
1" quartz-carbonate vein in pillowedmafic flows, limonite staining.
2" quartz vein in pillowed mafic flowswith trace of sulphides.
1" - 6" quartz-carbonate vein, irregular,minor limonite staining in bandedgneissic mafic-intermediate flows.
ppb
5
10
10
^
5
rt
G
I //'" yyfocek lid..
/A, Oninrin. /Ait,*one'
f Mnp*n) l.ld.
W ll i i i i i i i i i i i i i i i
KIJ 8xsI6QI 744.2J2n
Geochemical Lab Report
REPORT: 017-3930 ( COflPLETE
CLIENT: GEOCftNEX L1HUED PROJECT: KOftAR
REFERENCE INFO:
SUBMITTED ir. J.D, WU PRINTED: 3-SEP-87
ORDER ELEHENTmm OF LOVERANALYSES DETECTION LlfllT EXTRACTION IIETHOD
1 ftij Silver 2 Au Gold
SARPLE TYPES NURBER
ROCK 18 '
1 0.1 18 5
SIZE FRACTIONS•268
m m
' ' : ' -'* '
HC1-HN03, (1 AQUA RE6IA
NURBERST^^Wft^
IB
:3) Atoiit Absorption FA-AA 1 10 ji Height
SARPLE PREPARATIONS NURIER
*BiiiP8F*^REHARKS: (: HEANS LESS THAN
REPORT COPIES TO: H. HODGER. HI66INSON
INVOICE TOt H, HODGE
1l/
111111I111111i111
S -bf tt 4 (unpin) Lid. ' **'' '0*
/Awl M., ifflmffl/
f Art* toT's'x'i Bmnir. ,fanc: UMtW 2220 WffiBI
REPORT! 017-3930
SAHPLE EIEHENTmm UNIIS
12201221 122212231224
12251226122712261229
123012311232 1233 1234
1235 12361237
. . , ...,..,, ...
.•ftjuM m .. ^PAV.... . . . ,''^^toifciifAih^^ neochemicfll/^//^M^jjMiiaiayfciiaiiiii^^ j Lab RCPOHIB^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^HNJ^^^^^^^^^^^^^^^^^^^^^^^^H
j | PROJECT: wm PAGE iAg Au
PPft PPB :
<5 ' - -(5 25
63015
" ioo "•- ---------- - •••-•---•- - . -...-.- — - -.....--..... . . . .10 .
. ^ '^\:^M^W^.^^l^---
l
50.4 5 .
10 '' '-;' -'^iti^J ' .' .- ' . to i-^f -^:iy^ ' , ; , ..-i.;. . ; ^ '--. .
5 ; , . . "' ----— — - --- - - <5 : . . ,,,-.:- . ,(5
V
.,.-..-...-^-, __ -r - -v-, r , r TT^
' -' ' ' -
li liGeochemical
Lab Report
" REPORT: o!7-3?G9('COMPLETE")""" """""""l r, V; ^fEFERENCi INFO:. . ...—.—,...... ,-.™..——.____...J i':':";.v', :.:.'-.;::_____..._.
( "CLIhNiV'^CCANEniMiiED"* ~~~~"———~—~-——;--:————, ;! ...;, ; . ,;v;?:; SUBfllTIEU DH U HllkST- PROJECT: KOMAR ' -^ ''^v'-vi^^y.,;:f JAiE'PJiiHiEP:.24-AUG-87
. ... _......,.....-..,-..-,.___.. m.........™..™,.__.____' :'..^:;. i :::. •.'.••: ^WM'.'^:'f** '^:*j,..'^ '.'.L'-'v ' •,.... - -.,-,-. ........,, .....,.......,™... ......--,......,,.. ^.^^^ LOWER •.,:;i,.,v,v:: v ^7" ~~
l ORDER ELEHENT ftNltt.YSES'-;'':.reiECII(|l|.4i||3f;^•i ' ; - : ' '' , -'- ^''' : ..''^|v|^^' -'' -' '••••^'''• : ^':-?'; i,' ' ' '
l ftu Gold ' 19 ' ' 5 PPB^'^'A'QUA Jii8!frr s : :v " ' FA-AA B 10 gm weight
I...... . .......-Sfihi'Lt TYPES"~ """""""}|UJiiiK~~". ™"SI2E'fRfiCIII)HS—^"Tl,,
l, . ....ROCK ': ^.l.itfK;:- W^?^^ -
M... ... ..pc^,i^c;!..^asi.p.42^ i^C,.J^.fiTurD HAIIIP6. tie t tin ' . : -'r .v ,.iJ ,*. :',;.v ^ r . . ,. . , ,i
™ """ SAMPLE 12i i "HAS""IW '' MEANS LESS THAN,
lREPORT COPIES TO! K. HODGE , V ' r'' WVOICE10: HvfjODGB
D iiTppTiipnii ^ " Jl: -"'"".' H r:"' r /"r r "T""~"™~"~r.'r~."r.
l
l
t^m^^^mt^^&^y^"''
l S/f li lixnptii) Ud.
Kil , (, Onlano,
l KIJ 8X5
lelev 033 J2J
Geochemical Lab Report
l l l l l l l
. jtm. ~
l l
l
l
l
l l
l l
———'PftQE lIZ1
SAWIEXLnfcEIi
1203
1205
1206 12:7 120B
1210
12111212121312141215
"ELEKEiil"
UNITS PPP
105
10
!0i 105
10925
1220" 9095
,: 10;: ; '3
259
70•;s5x'5
' ;: : ^:i^TfTTTT'l\*Xjfff\F'{':3!-"\':
^^^.V^wy^*v;,.'--v,;
l.Adv-Ora A Comprnj Li*.
5420 Cu
CiniilaPhone: (61 J) 149-1220Telci: 053-3233
Certincate of Analysis
\m
j j •i'l 1
l
l
REPORT: 417-3769 ( COHPIETE )
M
REFERENCE INFO: .
CLIENT: 6EOCANEX L1HITED PROJECT: KOHftR
SUBMITTED BY: R. HIGG1SON DATE PRINTED: U-KEP-87
ORDFR ELFHEN!
l ftu Gold -Assay
HUHBER OF LOUERWftLVSCS OEtECIION Llflll EXTRACTION
l 0.001 OPT
rirtfir-II IVCff;
OIK
NUHOER
1
SI7F f RUCTIONS
'1'ilV l Ml
^, . . . . ,... . .., , ; . . ; ; ,.
NUH9CR fiftHllf PRIffiRAHON^
1 I'lj; V|iv!,! i*Ji
V™*r.r^-*.
trrmt tR. IllGGINSON
i
l
-OrttACompuiyLld.J420 Cinottk M.,
Onllii KU
(413)149)110
Certificate of Analysis
l l l l
i l
RFPOK1: 417-3/69
NUDl.ll K
i;'i!i
FSoJECTi KOMAR PAGE l
AuUN! ir; od
i'adi^a^MlaMl^siia^aliiiiM:^^:,::,
,; viI|'; -i^llillSS*; 5:^-0::/- •'•.."^V.'O'V ^•Y^M^S^j^^W.v.-y ; .-.-- - ^•^-.••y: : --' ".
DIAMOND DRILL RECORDHOLE NO. EL-87- l SHEET NO. ' " '_
NAME OF PROPERTY EYE LAKE
HOLE NC
LOG ATIO
LATITUD
ELE VATI
STARTED
i. EL-R7-1 LENGTH 297N 00+505, 02+15E
FOOTAGE DIP AZIMUTH
.0' ———— ——0.0 45 0
29/.0 10"
3N A7IMUTH 090" DIP -45" ———————— —————— —— —————
Nov. 27/87 F.NisnFn Nov. 28/87 ———— ——— ———— -
FOOTAGE DIP AZIMUTH
REMARK S PA786856
f.
LOGGE
PA786855
UMMARY LOG
R HigginsonD BY
FOOTAGE
FROM
0.0
10.0
57.8
98.0
171.7
194.3
195.5
224.8
266.2
271.0
TO
10.0
57.8
98.0
171.7
194.3
195.5
224.8
266.2
271.0
297.0
297.0
DESCRIPTION
SUMMARY LOG
CASING
MAFIC FLOWS
SILICIFIED - SHEARED INTERMEDIATE TUFF
MAFIC FLOWS AND TUFFS, 80:20
SILICIFIED - SHEARED INTERMEDIATE TUFF
MAFIC FLOWS
FELSIC TO INTERMEDIATE TUFF
- 195.5' to 200.5' - well-banded tuff containing quartz-car bonate stringers, pyrrhotite ft pyrite as fracture infill- ings.
MAFIC TO INTERMEDIATE VOLCANICS, tuffs - flows, 40:60.
FELSIC TO INTERMEDIATE TUFF
MAFIC TO INTERMEDIATE VOLCANICS, as above.
E.O.H.
ONTARIO GEOLOGICAL SURVEY ' ASSESSMENT FILES
OFFICE
APR 2 2 1988
RECEIVED
SAM
NO.
12041
SI^PSH
3-5
P L E
FOOTAGEFROM
195.5
TO
200. 5
TOTAL
5.0
ASSAYS
OZ/TON
.010
OZ/TON
DIAMOND DRILL RECORDNAM E OF
HOLE NO.
LOC AT ION
LATITUDE
ELEVATION
STARTED
PROPERTYEL-87-1
JQ15QS.
Nov.
OP+15F
27/87
EYE LAKEL E N G T H
DEPARTURE
AZIMUTH
FINISH Fn
297
090 0
Nov.
.0'
-45 0
28/87
FOOTAGE
0.0
297.0
DIP
45 040 0
AZIMUTH FOOTAGE DIP A7IMUTHHOLE NO. EL -87- 1 SHEET NO.
REMARK s PA786856^^Pa786855
LOGGED BYR. Higginson
FOOTAGE
FROM
0.0
10.0
57.8
TO
10.0
57.8
98.0
DESCRIPTION
Casing.
Mafic Flows - dark green to black, medium grained, massive.Modal percent: Amphibole 45-5036
Plagioclase 40-4536Chlorite 3-5*Quartz 1-256Carbonate 1-256Pyrite tr-0.5*
Amphibolitic to oohit.ic texture, disseminated pyrite as fracturecoatings, 1-256 quartz-carbonate stringers, foliation at 36 0 tocore axis at 21.0', 50" at 37.0', 38" at 50.0'. Fracturing at 27 0to core axis at 12.0', 35 0 at 47.0'.
Silicified - Sheared Intermediate Tuff - light to dark grey, finegrained, banded.
Modal percent: Quartz 35-4056 Plagioclase -, 2Q -^ Sericite J ^ "*Chlorite 10-15*Amphibole 5-10*Pyrrhotite -i , r*Pyrite J J ~ S*Carbonate 2-3* Garnet tr-2*
Common sericite pseudomorphs after plagioclase, disseminated,allotriomorphic, pink, garnet porphyroblasts in some sections,2-3X carbonate as bands, pyrrhotite and pyrite as bands, stringersand blebs, minor parasitic-kink folds.
- 57.8' to 58. l 1 - quartz-carbonate, clean banded vein.
SAMPLE
NO.
12001
1 200?
Ol
1 2003
SULPH IDES
tr
tr
JTARK ASS
J
RE
tr
FOOTAGEFROM
10.0
52.8
) G6OLO ESSME
OFFI
iPR2l
CE!
TO
15.0
57.8
SIGAL S NT FIL CF.
i miVE
57.8 62.8
TOTAL
5.0
5.0
URVEY EfS
D
5.0
ASSAYS
/4IXfi?(S/j
\X
^^?v~(TjTT
n-f/yjLy^"-,vs^^^
ozAUON
.002
tr
PJpDGi^ —
oF o^ vnfffc^Hfit^
tr
07/TON
X' \j]'J
y
DIAMOND DRILL RECORD NAME OF
HOLE NO
. EYE LAKE
".MM T NO
FOO T AC- F
f ROM
57.8
98.0
TO
98.0
171.2
DESCRIPTION
Cont'd.- 58. T to 59.1' - friable with garnets.- 59.1' to 61.0' - irregular coarse grained quartz vein, 2-3*
coarse grained pyrite blebs.- 61.0' to 62.8' - 2-3* disseminated garnets, 3-5* pyrite
bands.- 62.8' to 74.3' - well banded, 1-2* pyrite as fine grained
wispy blebs, 2-3* quartz-carbonate veiningwith 2-3* coarse grained pyrite blebs,1-2* muscovite-biotite coronas aroundfeldspar (microcline?) grains.
- 74.3' to 80.7' - dark grey, finely banded, 2-3* pyrrhotite,pyrite blebs, bands and stringers, crenu-lated, kink folded.
- 80.7' to 98.0' - finely banded, 5-7* carbonate parasiticfolds with 2-3* quartz-carbonate veins upto 0.4 feet wide (possibly axial planar),2-3* pyrite as fracture coatings, zones of1-2* wispy pyrite blebs, 1-2* dissemin ated garnets.
Fracturing at 40 0 to core axis at 68.0', foliation at 64 0 -67 0 tocore axis.
Mafic Flows and Tuffs - 80:20. Flows typical, tuffs banded with2-3* quartz-carbonate-epidote stringers and 3-10* biotite as bandsand disseminated grains foliation at 61 0 to core axis at 116.0,58 0 at 126.5', banding at 64" to core axis at 154.5', 67" at141.0', fracturing at 50 0 to core axis at 155.0'.
- 98.0' to 121.8' - flows, 2-3* quartz-carbonate veins up to0.3 feet wide, trace pyrite in veins.
- 121.8' to 124.1' - crudely banded tuff, biotite - 1-2*tourmaline blebs, 2-3* quartz-carbonatestringers.
- 124.1' to 132.1' - tuff, 1-2* quartz-carbonate stringerswith trace pyrite.
- 132. T to 142.3' - flows, 2-3* quartz-carbonate stringers.
SAMPLE
' IO
120041200512006
1200712008
1200912010120111201212013
120141201512016120171201812019
1202012021120221202312024
•'.1)1 CM
lur 5
1-21-21-2
2-32-3
3-53-53-53-53-5
trtrtrtrtrtr
trtr
FOOT AGt
FROM
62.867.872.8
74.377.3
80.782.787.092.095.3
98.0102.0107.0112.0117.0121.8
124.1129.1132.1137 .1140.1
ro
67.872.874.3
77.380.7
82.787.092.095.398.0
102.0107.0112.0117.0121.8124.1
129.1132.1137.1140.1142.3
*0 Ml
5.05.01.5
3.03.4
2.04.35.03.32.7
4.05.05.05.04.82.3
5.03.05.03.02.2
A'.r.AY'j
- "l.
tr.002.002
.006tr
trtrtrtrtr
trtr.008tr
.006
.006
trtrtrtr
.008
DIAMOND DRILL RECORD NAMl Df
HOLE: NO
EYE EAKEEL-87-1 3 of 4
FOOT AGf
F ROM
98.0
171.?
194.3
195.5
TO
171.2
194.3
195.5
224.8
DE- SCRIPT ION
Cont'd.- 142.3' - 146.3' - tuff, 1-2* quartz-carbonate stringers.- 146.3' - 171.2' - flows with 2-3* quartz-carbonate-epidote
interflow and stringers, massive, traceto 1* disseminated pyrite blebs, limonitestaining.
Silicified - Sheared Intermediate Tuff - typical, foliation at 60"to core axis at 177.0', 61" at 192.0'.
- 171.2' - 177.2' - laminated to finely banded, 2-3* wispypyrrhotite, pyrite blebs, 2-3* dissemin ated fine to medium grained garnets, 1-2*quartz-carbonate stringers.
- 177.2' - 185.5' - 3-5* quartz-carbonate stringers and bandstrace-3* wispy pyrite blebs, finely lami nated with 3-5* pyrrhotite near bottom ofsection.
- 185.5' - 187.0' - coarsely banded, trace-0.5* pyrrhotiteand pyrite, 1-2* quartz-carbonate strin gers.
- 187.0' - 189.2' - crudely banded, folded, crenulated, 2-3*pyrite, 1-2* pyrrhotite.
- 189.2' - 194.3' - crudely banded, trace-0.5* pyrrhotite andpyrite.
Mafic Flows - atypical, 15-20* chlorite, fracturing at 52 0 to coreaxis at 195.0'.
Felsic to Intermediate Tuff - dark grey, fine grained, banded.Modal percent: Quartz 40-45*
Plagioclase 15-20*Chlorite 10-15*Sericite -i g ^QVMuscoviteCarbonate 3-5*Pyrrhotite i T rvPyrite J *
SAMPLF
•K,
1202512026T2027I202S120291203012031
1203212033
1203412035
12036
12037
1203812039
12040
12041120421204312044
IPFS
tr-1tr-1tr-1tr-1tr-1tr-1
2-32-3
tr-3tr-3
tr
3-5
trtr
tr
3-53-53-53-5
F O O T A G F
fBQM
142.3146.3149.5152.0157.0162.0167.0
171.2174.2
177.2182.0
185.5
187.0
189.2191.8
194.3
195.5200.5204.0207.0
rn
146.3149.5152.0157.0162.0167.0171.2
174.2177.2
182.0185.5
187.0
189.2
191.8194.3
195.5
200.5204.0207.0210.9
T'lFAI
4.03.22.55.05.05.04.2
3.03.0
4.83.5
1.5
2.2
2.62.5
1.2
5.03.53.03.9
A ', fl, A Y S
AM,,.
.002trtrtrtrtrtr
trtr
trtr
tr
tr
trtr
tr
.010trtrtr
DIAMOND DRILL RECORD NAMI: or pKOPF.fi'i'v E lE LAKE
HOLb NO ...E L -87-1 mi i no 4 Of 4
FOOT AC.F-
I ROM
195.5
224.8
266.2
271.0
TO
224.8
266.2
271.0
297.0
297.0
ntSCRIPTION
Cont 'd.Minor parasitic folding, S-5% quartz-carbonate stringers, pyrrho tite and pyrite as very fine grained blebs and stringers, bandingat 47" to core axis at 211.0'.
- 210.9' - 215.3' - 3-5X carbonate and quartz-carbonatestringers and veins up to 0.5 feet wide.
Mafic to Intermediate Volcanics - 60:40 - flows: tuff, light greyto green, fine to medium grained, banded to massive.
Modal percent: Amohibole -i Ar. Ac- vs* i i . , HVJ — *T 0 rt)Chlorite JPlagioclase 35-37%Quartz 3-5JSBiotite 2-55SCarbonate 1-355Pyrite tr-0.5%
T-3% carbonate and quartz-carbonate stringers, wispy biotite bandsminor kink folding, banding at 48" to core axis at 237.0', 78 0at 262.0'.
- 257.3' - 258.3' - light grey, sericite (5-10X), poorlydeveloped schistosity.
Felsic to Intermediate Tuff - typical mottled to coarsely banded,light grey.
Mafic to Intermediate Volcanic - as above, banding at 48 0 to coreaxis at 277.0', 68" at 297.0', fracturing at 55 0 to core axis at275.0'.
- 287.3' - 290.6' - kink folded, 2-3X quartz-carbonatestringers at fold hinge, with coarsegrained amphibole prisms as inclusions.
E.O.H.
SAMPLE
•M,
120451204612047
12048
12049
12050
12051
12052
!l*f 5
3-53-53-5
tr
FOOT AGfc
f ROM
210.9215.3220.3
224.8
257.3
266.2
287.3
294.0
TO
215.3220.3224.8
227,8
258.3
271.0
290.6
297.0
r.ctM
4.45.04.5
3.0
1.0
4.8
3.3
3.0
A V, AY S
.A v,,.
trtrtr
tr
tr
tr
tr
tr
j : T 14
DIAMOND DRILL RECORDNAME OF PROPERTY
HOLE NO. EL-87-2
EYE LAKELENGTH 317.0'
LOCATION 00+50S. BLO__.—^—--——LATITUDE ___________________ DEPARTURE
ELEVAT ION
STARTED — Nov. 28/87AZIMUTH
FINISHED ,
090 0 -46"
Nov. 30/87
FOOTAGE
0.0
307.0
DIP
-46"-43 0
AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. EL-87-2 SHEET N0.
REMARKSPA786856______
SUMMARY LOG
LOGGED BY R. Hjgginson
r o o T A G E
FROM
0.0
14.0
228.5
250.0
TO
14.0
228.5
250.0
317.0
317.0
D E S C R 1 P T 1 ON
SUMMARY LOG
CASING
INTERMEDIATE FLOWS- 105.0' - 110.0' - randomly distributed quartz-carbonate
stringers; chloritic fractures. Tracesulphides as fracture infillings.
FELSIC TUFFMAFIC TO INTERMEDIATE FLOWSE.O.H.
ONTARIO GEOLOGICAL SURVEY' ASSESSMENT FILES
OFFICE
APR 2 2 1988
RECEIVED
SAMPLE
NO.
12073
sAfeg" FOOTAGEFROM
105.0
TO
110.0
TOTAL
5.0
ASSAYS
-,; OZ^VON
.020
OZ/TON
DIAMOND DRILL RECORDNAME OF PROPERTY EYE LAKE
LOCATION
LATITUDE
ELEVATION
STARTED
EL-87-200+50S, BLO
Nov. 28/87
1- ENGTH
AZIMUTH
FINI^HFn
317.0'
090 0 DIP -46 0Nov. 30/87
FOOTAGE
0.0
307.0
DIP
-46 0-43 0
AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. EL-87-? SHEET NO. ' Of 3
REMARKS PA786856
LOGGED BYR. Higginson
FOOTAGE
FROM
0.0
14.0
TO
14.0
228.5
DESCRIPTION
Casino,.
Intermediate Flows - light grey to green, fine to medium grained,massive to poorly banded.
Modal percent: Plagioclase 35-405! Amphibole 30-355! Quartz 10-155!Biotite 5-105!Carbonate 1-25!Pyrite trace
1-25! quartz-carbonate stringers, wispy biotite bands in some sec tions few widely spaced fractures with carbonate-limonite coatingsfoliation at 41" to core axis at 32.0', 50" at 63.0', 50" at 137.057 0 at 166.0', 66 0 at 205.8', 50 0 at 228.5'.
- 14.0' - 27.6' - fine to medium grained, medium grainedamphibole prisms in fine grained groundmass.
- 26.2' - 27.6' - medium grained, felted bio-tite-amphibole, carbonate stringers with1-25! vuggy pyrite.
- 27.6' - 43.1' - fine grained, massive.- 43.1' - 55.0' - 2-35! quartz-carbonate stringers, medium
grained biotite rich bands.
- 55.0' - 121.8' - fine grained, 2-35!, irregular quartz-car bonate stringers, chloritic fractures,1-25! pyrite as fracture coatings, trace-15!pyrrhotite as fine disseminated grains.
SAMPLE
NO.
i
120531205412055
120561205712058120591206012061I20621 2063120641206512066
SJ&SM-
*NTAFAS
trtr
1-2
1-3
FOOTAGEFROM
iOOEOLSESSM
OFf
APR 2
ECE
14.019.024.0
27.632.637.640.643.147.052.055.060.065.070.0
TO
XJICALENT FI ICE
2 198
1 VE
19.024.027.6
32.637.640.643.147.052.055.060.065.070.075.0
TOTAL
ASSAYS
/#
SURVEY!^*/pq l 'J \\ r; i/ l" tL (siB IWj V0r^ l ^D 1——— 1
5.05.03.6
5.05.03.02.53.95.03.05.05.05.05.0
•;.
^"
lm' r
s.'/f, ^^•'ctic
07/TON
^x^0J/ '
IGI.,*
^/' f"-'o^/'' -s-^'
trtrtr
trtrtrtrtrtrtrtrtrtrtr
OZ/TON
S'o\
ri 1
f
73
DIAMOND DRILL RECORD NAMf OF PI.-OPF. HI ' EYE LAKE
of 3
F GO f AGT
FROM
14.0
T fi
228.5 Cont'd.
DESCRIPTION
?1.8' - 126.2' - medium grained amphibole, fine grainedbiotite bands.
?6.2' - 151.5' - fine to medium grained, 2-35S irregularquartz-carbonate stringers, minor kinkfolding.
31.5' - 164.8' - crudely banded to mottled, medium grainedamphibol itic. T-2% pyrite as fracturecoatings. Z-5% carbonate.
54.8' - 180.2' - fine grained, massive, 2-33S fine quartz-carbonate stringers, minor discontinuitieswith changes in orientation of stringersand foliation, T-2% disseminated-roundedpyrite blebs.
- 166.0' - 167.0' - *\-21l, tourmaline asaggregates of grains with pyrite matrix.
- 176.0'- 180.2' - 2-3SS pyrite as stringersblebs and disseminated grains.
30.2' - 186.9' - altered tuff?, 10-15* fine grained seri cite and biotite, 2-3* quartz-carbonatestringers with 1-3* pyrite grains.
36.9' - 205.8' - fine grained, 2-3* quartz-carbonatestringers.
- 200.0'- 205.8' - 1-2* disseminated pyriteblebs along fractures or contacts ofquartz-carbonate stringers.
35. 8' - 210.5' - massive, fine grained, dark grey, 1-2*pyrite along fractures.
10.5' - 228.5' - crudely banded to mottled, 2-55! quartz-carbonate stringers, 1-2* disseminatedpyrite blebs.
SAMPL F
;.,
I2067I20681 2069I207012071I2072I2073I20741 207 5I2076I2077I2078I20791 2030120811 20821 20831 20841 20851 2086I20871 20881 20891 2090120911 20921 20931 20941 20951 2096I2097
1 2098209921002101
•••H PH
IDFS
1-21-21-21-21-21-22-31-31-3
1-21-21-2
1-21-21-21-2
FOOTAGt
FROM
75.080.085.090.095.0100.0.105.0110.0115.0119.0121.8126.2130.0135.0140.0145.0149.0151.5156.0161.0164.8167.8172.8176.0180.2183.2186.9191.9196.9201.9205.8
210.5215.5220.5224.5
TO
80.085.090.095.0100.0105.0110.0115.0119.0121.8126.2130.0135.0140.0145.0149.0151.5156.0161.0164.8167.8172.8176.0180.2183.2186.9191.9196.9201.9205.8210.5
215.5220.5224.5228.5
T 'j7Al
5.05.05.05.05.05.05.05.04.02.84.43.85.05.05.04.02.54.55.03.83.05.03.24.23.03.95.05.05.03.94.7
5.05.04.04.0
A S A Y *o
.AU
trtrtr
.002trtr.020trtr.trtrtrtr
.002trtrtr.002trtrtrtrtrtrtrtrtrtrtrtrtr
trtrtrt r
, , ,,
DIAMOND DRILL RECORD N AMI OF P*' O F-' F- f? T V .
nni r MO t L -o f -t
EYE LAKE
r,MI i T MO 3 Of J
F DOT Ac;r
228.5
250.0
250.0
317.0
317.0
DFSCRIPT ION
Felsic Tuff - light grey, fine to medium grained, foliated tobanded.
Modal percent: Quartz -i re enyr* , . -j J D 3 ~" DU/bPlagioclase Sericite 10-15*Microcline S-10%Muscovite 5-7*Carbonate 2-5*Pyrite 1-3*
Highly fractured, minor brecciation, 2-5* quartz-carbonate frac ture fillings and stringers with disseminated pyrite blebs and grains, abundant plagioclase lapilli, waxy sericitic coatings on fractures and foliation planes, foliation at 50 0 to core axis at 239.0'; 47 0 at 248.0'.
Mafic to Intermediate Flows - dark green to grey, fine to mediumgrain"'!, massive to foliated.
Modal percent: Amphibole 40-45* Plagioclase 35-40* Sericite 3-5*Chlorite 3-5*Quartz 2-3* Carbonate 2-3*Pyrite 1-2*
Amphibolitic to schistose(sericite-chlorite sections), 2-3* quartz- carbonate stringers, few widely spaced fractures, disseminated pyrite blebs, foliation at 55 C to core axis at 276.0' and 291.0'; 50" at 316.0'.
- 250.0' - 255.6' - 2-3* quartz-carbonate stringers.
- 279.3' - 283.0' - tuff, 3-5* biotite bands, 2-3* quartz- carbonate bands.
E.O.H.
SAMPL.E
•10
12102 1210;12104 1210P 1210E
121071210f
121091211C12111
-•-ut CH
mf s
1-3 1-31-3 1-3 1-3
f OOTAGtf ROM
228.5 233.5238.5 243.5 247.0
250.0.252.8
255.6279.3312.0
m
233.5 238.5243.5 247.0 250.0
252.8255.6
260.6283.0317.0
Tlj TAl
5.0 5.05.0 3.5 3.0
2.82.8
5.03.75.0
— ---A *, 3 A Y ',
7^
.002 trtrtr tr
t rtr
trtrtr
, r.
DIAMOND DRILL RECORDHOLE NO. EL-87-3 SHEET NO. ' 0 ^ \
NAME OF PROPERTY EYE LAKE
HOLE NC
L OCA T 10
L ATITUD
EL E VAT 1
STARTED
) EL-87-3 LENGTH 397N 11+OON, 06+35E
0'
3 N A7 ,MUTH 090 0 n .o -44. 5 0Nov. 30/87 FINISHED Dec
FOOTAGE
FROM
0.0
44.0
60.2
60.7
70.2
98.8
101.5
129.2
230.1
236.5
273.9
324.5
TO
44.0
60.2
60.7
70.2
98.8
101.5
129.2
230.1
236.5
273.9
324.5
397.0
397.0
D E
2/87
S C R 1 P T 1 O N
SUMMARY LOG
FOOTAGE
0.0200.0397.0
DIP
-44.5-43.0-41.0
CASING
FELSIC TO INTERMEDIATE VOLCANICS
MAFIC INTRUSIVE DYKE
FELSIC TO INTERMEDIATE VOLCANICS
SILTSTONE
FELSIC TO INTERMEDIATE VOLCANICS
MAFIC TO INTERMEDIATE FLOUS
MAFIC TO INTERMEDIATE VOLCANICS AND SILTSTONE, 45:55
INTERMEDIATE FLOWS
INTERMEDIATE TUFF
INTERMEDIATE FLOWS- 370.5' - 373.7' - well banded tuff, abundant quartz-carbon
ate eyes.
INTERMEDIATE TUFF
E.G. H.
ONTARIO GEOLOGICAL SURVEY ' ASSESSMENT FILES
OFFICE
APR 2 2 1988
RECEIVED
AZIMUTH "DOTAGE
SAM
NO.
12195
S,^PSH
DIP
RLE
AZIMUTH
REMARKS PA850854
SUW
LOGGE
FOOTAGEFROM
370.5
TO
373 7
TOTAL
3.2
1ARY LOG
R. Higginson3 BY
ASSAYS
X
Ven ^
,***— " ,**L:
'/P
^^'*CE ci""•-^
oz/HoN
:;0-^"yp,yo**/***^
.026
O 7 /T ON
1X
.J^
DIAMOND DRILL RECORDNAME OF PROPERTY EYE
HOL E NO. -
LOCATION
LATITUDE
ELEVATION
STARTED
EL-87-31HOON, 06+35E
Nov. 30/87
LAKELENGTH
DEPARTUR E
AZ IMUTH
FIN ISHFn
397.0'
090 0 DIP -44. 5 0Dec. 2/87
FOOTAGE
0.0
200.0
397.0
DIP
-44.5-43.0-41.0
AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO.
EL-87-3SHEET NO. L-.-,.l Of 5
R EM ARKS PA850854
LOGGED BY.R. Higginson
FOOTAGE
FROM
0.0
44.0
60.2
TO
44.0
60.2
60.7
DESCRIPTION
Casing,
Felsic to Intermediate Volcanic - light to dark grey, fine grainedmassive to banded.
Modal percent: Quartz j 70-75* PlagioclaseAmphibole 10-15*Biotite 3-5*Chlorite 2-3*Pyrite tr-3*Carbonate tr-1
Variable textures from fine grained massive to weakly banded,foliation at 60" to core axis at 45,5' and 60.0' fracturing at48 0 to core axis at 60.0' .
- 44.0' - 52.0' - 2-3* disseminated pyrite.- 51.2' - 52.0' - quartz vein with felsic
inclusions, 1-2* pyrite along contacts.- 52.0' - 56.8' - cherty, massive trace pyrite, epidote in
filling of minor fractures.- 56.8' - 60.2' - light greenish-grey, massive 20-25* quartz
veining, trace disseminated pink garnets.0.5-1* chalcopyrite blebs, trace-0.5*pyrite, 10-15* potash feldspar in maficinclusions, angular mafic inclusions - xeno-liths in host - possibly agglomeratic.
Mafic Intrusive Dyke - light green, fine to medium grained, por-pyritic.
Modal percent: Amphibole 65-70*Biotite 15-20*Plagioclase 5-10*
SAMPLE
NO. SULPH IDES
ONT/A
j1i F———
1211212113
12114
12115
121 1 6
2-32-3
tr
0.5-1
FOOTAGEFROM
RIO QECSSESS
O
APR
EC
44.048.0
52.0
56.8
60.2
TO TOTAL
cumupLOOICAr ^-...^ /ENT FILES TICF.
2 2 N88
E i V|E D
48.052.0
56.8
60.2
60.7
.
4.04.0
4.8
3.4
0.5
ASSAYS
OZ/TON
trtr
tr
tr
t r
OZ/TON
DIAMOND DRILL RECORD MAM! OF PCOCF-fM V
EL-87-3
EYE LAKE
HOt-E NO NO 2 Of 5
FOOT AGF
F ROM
60.2
60.7
70.2
98.8
101.5
1 O
60.7
70.2
98.8
101.5
129.2
DESCRIPTION
Cont'd.Medium grained biotite flakes in fine grained amphibole-plagio-clase groundmass, contacts at 80" to core axis.
Felsic to Intermediate Volcanic - as above gradational lower con tact with sediments.
Siltstone - dark green to brownish grey, fine grained, massive tobanded.
Modal percent: Quartz ] 4CM5XPlagioclaseBiotite 20-25*Chlorite ID-15%Carbonate 5-10*Amphibole 3-5*Pyrite tr-0.5*
Massive on top and bottom of section, increasingly well bandedtoward middle, minor kink folding, 1-2* quartz-carbonate stringers,banding at 49 0 to core axis at 92.0', 70 0 at 97.4', conjugatefractures at 40/500 to core axis.
- 87.3' - 87.8' - quartz vein, clean.- 97.4' - 98.3' - quartz veining, 2 generations, trace tour-
maline on contacts of second set of veinscross-cutting first set, clean.
Felsic to Intermediate Volcanic - as above 1-2* quartz-carbonatestringers near lower contact with 1-25! pyrite and 1-2* epidotebands, foliation at 55 0 to core axis at 101.0'.
Mafic to Intermediate Flows - dark green, fine grained, massive.Modal percent: Amphibole 45-50*
Plagioclase 40-45*Chlorite 3-5*Quartz 0.5-1*Carbonate tr-1*Pyrite trace
Massive, few widely spaced chloritic fractures, minor disseminated
SAMPLE
•m
121171211f
1211?121 2(12121
121251212-12124
1212E
1212612125121261212?1213C12131
Mil fit
.Df S
tr-3tr-3
tr-.5tr-.5tr-.5
tr-.5tr-.5tr-.5
1-2
trtrtrtrtrtr
FOCTAGt
FROM
60.765.7
70.275.280.2
85.290.295.2
98.8
101.5106.5111.5116.5121.5126.5
TO
65.770.2
75.280.285.2
90.295.298.8
101.5
106.5111.5116.5121.5126.5129.2
T' ( TAI
5.04.5
5.05.05.0
5.05.03.6
2.7
5.05.05.05.05.02.7
———— lA r, j AYS~~Au
•UN
trtr
trtrtr
trtrtr
tr
trtrtrtrtrtr
DIAMOND DRILL RICORD ,of.rmv. EYE LAKE
EL-87-3 3 of 5
F QQT Ae-f
FROM
101.5
129.2
TO
129.2
230.1
DF SCRIPT ION
Coni 'd.quartz blebs and pyrite grains, irregular fractures at 21" to coreaxis.
Mafic to Intermediate Volcanics and Siltstone - 45:55.- 129.2' - 134.8' - siltstone, atypical, 25-30* carbonate,
35-40* biotite, fractures at 30 0 and 60 0to core axis.
- 134.8' - 136.3' - intermixed tuff and siltstone gradationalzone.
- 136.3' - 139.3' - silicified tuff, massive light grey toto banded grey-green, amphibolitic tocherty, 1-2* carbonate stringers, folatiorat 61 C to core axis at 137.0'.
- 139.3' - 152.8' - tuff and flows, 20:80, 3-5* quartz-carbon ate veining, trace-1* disseminated tour maline, trace pyrite, banding at 50-56 0to core axis.
- 152.8' - 168.4' - siltsone and tuff, 90:10, amphibole bandswith carbonate stringers as cores, bandimat 52 0 to core axis, at 154.0'.
- 168.4' - 179.6' - tuff, 5-10* carbonate stringers, minorkink folding, dislocations at 25" to coreaxis, 0.8 feet apart, 1/4 inch displace ment, fracturing at 47" to core axis at169.0', foliation at 60 0 to core axis at172.0'.
- 179.6' - 189.6' - flows, typical, foliated at 52" to coreaxis.
- 181.5'-184.5' - 3-5* quartz-carbonatestringers with trace tourmaline blebs.
- 189.6' - 200.1' - siltstone, finely banded, 5-10* carbonate,crenulated kink folded.
SAMPLE
-,o
121321213:
1213'
1213!
1213f121371213?1213?1214C12141121421214:1214'1214J1214(
1214/1214?
121491215012151
mf S
trtrtrtr
FOOT AGEFROM
129.2132.2
134.8
136.3
139.3144.3147.3150.3152.8153.8158.8163.8168.4172.4177.4
179.6184.6
189.6194.6197.6
TO
132.2134.8
136.3
139.3
144.3147.3150.3152.8153.8158.8163.8168.4172.4177.4179.6
184.6189.6
194.6197.6200.1
P'.TAI
3.02.6
1.5
3.0
5.03.03.02.51.05.05.04.64.05.02.2
5.05.0
5.03.02.5
ASSAY *j
.-w.
trtr
tr
tr
trtrtrtrtrtrtrtrtrtrtr
tr.002
tr.002tr
IP.' T; (i
DIAMOND DRILL RECORD NAMI: or PROPERTY ..
not.E NO -J-L-87-3
EYC LAKF.4 of 5
TOO T A Li E
F ROM
129.2
230.1
236.5
273.9
T o
230.1
236.5
273.9
324.5
DESCRIPTION
Cont'd.- 200.1' - 205.5' - tuff, medium grained, amphibolitic, crude-
banded, sericitic alteration of plagio clase.
- 205.5' - 220.2' - mixed sediments and tuff, banding at 45 0to core axis at 206.0' .
- 220.2' - 224.2' - tuff, minor dislocation or disconformi ties2-3% quartz-carbonate stringers.
- 224.2' - 226.0' - intermixed sediments and tuff.- 226.0' - 230.1' - siltstone, folded, 10-2056 carbonate,
3-556 quartz-carbonate stringers, tracelimonite staining.
Intermediate Flows - 2-356 quartz-carbonate stringers, banding at57 0 to core axis at 235.5'.
Intermediate Tuff - atypical, sericitic with potassic alterationalong contacts of quartz-carbonate stringers (3-556), 20-2556 car bonate, banding at 45" to core axis at 245.0', 30 0 at 269.0',fractures at 40 0 to core axis at 282.0'.
- 251.9' - 253.3' - massive, no stringers.- 253.3' - 273.9' - 1-356 rounded pyrite blebs, minor discon
tinuities from faulting or erosion?
Intermediate Flows - foliation at 53" to core axis at 274.5'.
- 273.9' - 284.6' - massive, foliated, tr-256 pyrite as wispyblebs in 1-356 fine quartz-carbonatestringers.
- 284.6' - 285.8' - chloritic, schistose, 2-356 pyrite blebs.- 285.8' - 290.4' - massive, as above- 290.4' - 301.2' - massive, light grey, ampibole and chlorite
wisps, foliated at 70 0 to core axis,trace-356 pyrite blebs.
SAMPLE
' IO
12152
12153121541215512156
1215712158
1215912160
121611216212163
1216412165121661216712168
12169121701217112172
1217321741217E1217612177
sill fn
KiFS
1-31-31-31-3
1-3tr-2tr-2tr-2
2-3
tr-3tr-3tr-3
FOOTAGEFROM
200.1
205.5210.5215.5220.2
224.2226.0
230.1233.1
236.5241.5246.5
251.9253.3258.3263.3268.3
271.3273.9278.9281.9
284.6285.8290.4294.3297.8
10
205.5
210.5215.5220.2224.2
226.0230.1
233.1236.5
241.5246.5251.9
253.3258.3263.3268.3271.3
273.9278.9281.9284.6
285.8290.4294.3297.8301.2
TOTAL
5.4
5.05.04.74.0
1.84.1
3.03.4
5.05.05.4
2.45.05.05.03.0
2.65.03.02.7
1.24.63.93.53.4
ASSAYS
"1\1T
tr
trtrtrtr
trtr
trtr
trtrtr
trtrtrtrtr
trtrtrtr
trtrtrtrtr
DIAMOND DRILL RECORD NAMt or PPOPERT Y..,. EYE LAKE noi.t NO . EL-87-3 H, l r NO 5 Of
FOOT A Li F.
F ROM
273.9
324.5
T l)
324.5
397.0
397.0
Ot OCRIPTION
Coni' d.- 301.2' - 324.5' - foliated - schistose, S-7% quartz-carbon-
ate-epidote stringers, crenulation andkink folding, S-5% biotite bands, 0. 5-156pyrite grains.
Intermediate Tuff - typical, banded, abundant quartz-carbonate eyesand s'tringers banding at 40-68" to core axis (average 58").
- 353.8' - 355.2' - flow, massive, typical.- 358.8' - 359.7' - as above.- 361.7' - 362.7' - as above.- 363.5' - 364.2' - as above.- 367.0' - 373.7' - greyish-green, foliated, Z-3% quartz-car
bonate stringers.
E.O.H.
SAMPLE
.10
1217812179J2180121811218212183
121841218512166121871218812189121901219112192121931219412195121961219712198121991 2200
IDFS
.5-1
.5-1
.5-1
.5-1
.5-1
.5-1
FOOTAGLF BOM
301.2304 . 2307.5312.5317.5322.5
324.5327.0332.0337.0342.0347.0352.0355.5360.5363.5367.0370.5373.7377.0382.0387.0392.0
JO
304.230 7 .531?. 5317.5322.5324.5
327.0332.0337.0342.0347.0352.0355.5360.5363.5367.0370.5373.7377.0382.0387.0392.0397.0
F uT At
3.03.35.05.05.02.0
2.55.05.05.05.05.03.55.03.03.53.53.23.35.05.05.05.0
A 'j 'j A Y 'j
AU
trtrtrtrtrtr
trtrtrtrtrtrtrtrtrtrtr.026trtr.002trtr
,: T..V
DIAMOND DRILL RECORDEL-87-4 SHEE1 N0 . of ?
NAME OF PROPERTY EYE LAKE
HOLE NC
LOC AT IO
LATITUD
ELEVATI
STARTED
v EL-87-4 LENGTH 477.0'N 11+OON. 03+20E
3N AZIMUTH 090 0 n,P 47 0Dec. 2/87 F.N.SHFO Dec . 5/87
FOOTAGE
FROM
0.0
14.0
60.0
91.0
151.6
155.0
156.1
177.9
183.0
255.6
263.2
277.3
281.5
293.7
311.2
326.0
346.4
TO
14.0
60.0
91.0
151.6
155.0
156.1
177.9
183.0
255.6
263.2
277.3
281.5
293.7
311.2
326.0
346.4
421.0
FOOTAGE
0.0
200.0477.0
DIP
47"
46"
44.5"
DESCRIPTION
SUMMARY LOG
CASING
MAFIC TO INTERMEDIATE FLOWS
MAFIC TO INTERMEDIATE TUFF AND SILTSTONE - 80:20.
- 89.2' - 91.0' - quartz-carbonate stringers; sulphides to 23,
INTERMEDIATE FLOWS AND TUFF
QUARTZ-FELDSPAR PORPHYRY
INTERMEDIATE VOLCANICS
MAFIC TO INTERMEDIATE FLOWS
INTERMEDIATE TUFF
MAFIC TO INTERMEDIATE FLOWS AND TUFF- 240.6' - 242.6' - quartz-carbonate stringers to 3!
tite to 355. - 252.0' - 255.6' - as above.
MAFIC TO INTERMEDIATE TUFF
FELSIC VOLCANICS
MAFIC TO INTERMEDIATE TUFF
FELSIC TO INTERMEDIATE VOLCANICS
INTERMEDIATE FLOWS
MAFIC TO INTERMEDIATE FLOWS
INTERMEDIATE FLOWS
MAFIC TO INTERMEDIATE FLOWS
i; pyrrho-
ONTARIO GEOLOGICAL SUHVl-Y ' ASSESSMENT FILtS
OFFICE
APR 2 2 1988
RECEIVED
AZIMUTH FOOTAGE
SAM
NO.
12211
12246
12249
SULPH IDES
2-3
DIP
P L E
AZIMUTH
RFMARKSPA850854
SUMMARY LOG
R. HigginsonLOGGED BY 3J
FOOTAGEFROM
89.2
240.6
252.0
TO
91.
242.
255.
0
6
6
TOTAL
1.8
2.0
3.6
(i
y
ASSAYS
f. "*v'Oi
— — *,FESS/0,
m™-~--
OZ^TON
.016
.012
.014
OZ/TON
. -t -,-i
•MAmVNU VKILL KEVVKV ., , t ,, ,, ; , ,.- L , L ^HOI. E NO ..EL-87-4 SKI i ^ NO 2 of 2
F OO T AC.E
F ROM
421.0
456.2
T fi
456.2
477.0
477.0
DESCRIPTION
SUMMARY LOG CONI 'D
INTERBEDDED FELSIC AND INTERMEDIATE TUFFS -- 426.0' - 430.0' - quartz-carbonate stringers; fine-grained
wispy pyrrhotite, pyrite, S-5% garnetpoiki loblasts.
INTERMEDIATE VOLCANICS
E.O.H.
SAMPLE
NO
I22781 2280I2282
••ill Pu
l DF S
1-51-51-5
FOOT A G t
CROM
426.0433.5442.0
TO
430.0437.0447.0
T 0 T A i
4.03.55.0
A ^ ". A Y 'J.
,. AAi
.012
.016
.024
DIAMOND DRILL RECORDNAME OF PROPERTY
EL-87-4EYE LAKF
HOLE NO. LENGTH 477.0'L oc A T ION ,11+OON. 03+20E ________LATITUDE —————-———.—.^———— DEPARTURE
ELEVATION _____________________ AZIMUTH ———
STARTED O eC - 2/87______ FINISHED -—
090 0 47 C
Dec. 5/87
FOOTAGE
0.0
200.0477.0
DIP
470
46 044.5'
AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. EL-87-4 SHEET NO. ] Of 5
PFMARKC.PA850854___________________
LOGGED BYR. Higginson
FOOTAGE
FROM
0.0
14.0
60.0
TO
14.0
60.0
91.0
DESCRIPTION
Casing.
Mafic to Intermediate Flows - dark green, fine grained massive.Modal percent: Amphibole 45-50*
Plagioclase 40-45* Sericite 3-5*Quartz 1-2*Calcite 1-2*
Amphibolitic to phaneritic, minor zones of medium grained amphi bole in fine grained sericitized plagioclase groundmass, foliationat 55 0 to core axis at 19.0', 44 0 at 42.0', 60 0 at 33.0', 50" at60.0'.
- 29.5' - 30.5' - 0.3-foot clean quartz vein, crosscutting. - 39.5' - 40.5' - 0.2' carbonate vein, medium grained.
Mafic to Intermediate Tuff and Siltstone - 80:20, dark green, tobrown to white fine grained, banded.
Modal percent: Amphibole 55-60*Biotite 15-20*Quartz 15-20*Carbonate 2-3*
Well to crudely banded, 2-3* carbonate veins and stringers, 3-5 *quartz-carbonate bands and stringers, banding at 48 0 to core axisto 66.0', 55 0 at 74.2', 62 0 at 88.0'.
- 74.2' - 75.6' - biotite rich siltstone, brown, fine grainedbanded.
- 77.6' - 80.4' - as above.- 87.0' - 89.2' - as above.- 90.0' - 91.0' - carbonate vein, 1-2* finely disseminated
pyrrhotite, 0.2-foot quartz vein at lowercontact.
SAMPLE
NO.
12201
1220:
1220412205
I220612208122091221012211
SULPH IDES
~~.
3NTAI At
R
1-2
FOOTAGEFROM
14.0
;io GfioiSESSW
OF
APR l
ECE39.5
55.060.0
70.275.677.687.089.2
TO
19.0
OQICAL ENT F:)CE:
i m(VE40.5
60.065.0
75.677.680.489.291.0
TOTAL
5.0
ASSAYS
i
LERV it f'
I li1 \*
B \
D l l .1.0
5.05.0
5.42.02.82.21.8
^v.'^wj\sJ-Z f
^VV0'-/ "^^*Sfe f*"''
'"
OZ/TON
-tn"--L/r^PAs*
-^ .;w--r fiv c '
tr.008
trtr
.002tr
.004tr
.016
OZ/TON
'CySs ,o f•;''''y"7' . -s*
V,l.;
DIAMOND DRILL RECORD N AM t. OF PRO P E R T N ^ t IL LAKL
HOLE NO .EL-87-4.. .. NO 2 Of 5
F OOT AGT
TROM
91.0
151.6
TO
151.6
155.0
DESCRIPTION
Intermediate Flows and Tuffs - dark greenish-grey, fine to mediumgrained, massive to schistose (flows), banded (tuffs).
Modal percent: Plagioclase 45-5055Amphibole 40-453!Quartz 3-5*Carbonate 3-5*Pyrite tr-1%
- 91.0' - 101.8' - flows, few quartz-carbonate stringers,trace pyrite.
- 101.8' - 125.0' - flows, carbonatized, S-5% carbonatestringers, abundant irregular fractures,trace - 0.5* disseminated pyrite, minorzones of sericitized plagioclase.
- 101.8'-103.7'- highly fractured, highlycarbonatized.
- 103.7'- 125.0' - moderately to weaklycarbonatized.
- 125.0' - 147.9' - tuff and flows, 70:30, 2-3* quzrtz-car-bonate stringers.
- 146.6'-147.9'- schistose, 2-3* dissemin ated garnets.
- 147.9' - 151.6' - carbonatized, schistose, 10-20* carbonatestringers, minor breccia, minor disloca tions, trace-0.5* finely disseminatedpyrite.
Foliation averages 60 0 to core axis.
Quartz-Feldspar Porphyry - white medium grained phenocrysts in afine grained grey groundmass.
Modal percent: Quartz 45-50*Plagioclase 45-50*Carbonate 2-3*Pyrite tr-1%
SAMPLE
'1O
1221212213122141221512216122171221E1221912220
12221122221222312224122251222612227
12228
tor*;
trtrtr
tr-.5tr-.5tr-.5tr-.5tr-.5tr-.5
tr-.5
tr-1
FOOT AOLf ROM
91.094.097.0101.8103.7107.0112.0117.0122.0
125.0128.0132.0137.0142.0146.6147.9
151.6
TO
94.097.0101.8103.7107.0112.0117.0122.0125.0
128.0132.0137.0142.0146.6147.9151.6
155.0
'l)TAl
3.03.04.81.93.35.05.05.03.0
3.04.05.05.04.61.33.7
3.4
•\G"j AY cj
.ML
trtrtrtrtrt rtrtrtr
.008tr
.002
.002trtrtr
tr
DIAMOND DRILL RECORD EYC LAKE
E; NO EL-87-4 3 of 5
FOOT AOL
F- ROM
151.6
155.0
156.1
177.9
183.0
255.6
TO
155.0
156.1
177.9
183.0
255.6
263.2
OE- SCRIPT ION
Cont'd.Highly fractured, foliated at 50 C to core axis, quartz-carbonatefracture fillings, minor brecciation, plagioclase phenocrysts inqiiartz-plagioclase groundmass.
Intermediate Volcanics - carbonatized, as per 147.9' - 151.6', witt'{-2'?* disseminated and banded tourmaline, amphibole bands withquartz-carbonate cores, foliation at 51" to core axis at 155.5'.
Mafic to Intermediate Flows - typical foliation at 48 C to core axisat 160.5' , 54" at 170.0'.
- 156.1' - 168.0' - irregular quartz-carbonate-epidote strin gers, Q.5-1% disseminated pyrite, coarsegrained bleb of pyrrhotite at tip ofsection.
Intermediate Tuff - 3-536 wispy biotite bands, T-2% disseminatedpyrite foliation at 50 0 to core axis at 183.0'.
Mafic to Intermediate Flows and Tuff - 80:20, 1-3/& quartz-carbonatestringers.
- 247.6' - 255.6' - 2-336 carbonate and quartz-carbonate vein-ing and 2-356 pyrrhotite blebs.
Foliation averages 58 0 to core axis fracturing at 400 to core axisat 221.0'.
Mafic to Intermediate Tuff - atypical, 3-5X garnet, S-10% chlorite,3-536 irregualr pyrite stringers, trace-1% pyrrhotite, slightlymagnetic, foliation at 62 0 to core axis at 262.0'.
- 255.6' - 257.0' - quartz veining, clean, 1-236 pyrite, tracesubhedral garnets.
SAMPLF
MO
12229
1223012231122321225012207
12233
122341223512236122371223S12239 1224C1224112242
122431224412245122461224712248122491225112252
'-.lit PH
i or s
tr-.5
.5-1
.5-1
.5-1
1-2
2-32-32-33-53-5
r DOT A G t
FROM
155.0
156.1161.1166.1170.2174.9
177.9
183.0188.0193.0198.0203.0207.0 212.0217.0222.0
227.0232.0237.0240.6242.6247.0252.0255.6259.4
T 0
156.1
161.1166.1168.0171.6177.9
183.0
188.0193.0198.0203.0207.0212.0 217.0222.0227.0
232.0237.0240.6242.6247.0252.0255.6259.4263.2
r '.T*l
1.1
5.05.01.91.43.0
5.1
5.05.05.05.04.05.0 5.05.05.0
5.05.03.62.04.45.03.63.83.8
A 'j 'j A Y 'j
".-Ay,
ir
trtrtrtrtr
tr
trtrtrtrtrtr trtr
.002
trtrtr
.012
.002tr
.014trt r
j - r 'W
DIAMOND DRILL RECORD
263.2
277.3
281.5
293.7
311.2
277.3
281.5
293.7
311.2
326.0
HOLE NO
F c) f-'OPF:m V-
EL-87-4
EYE LAKE
Sill l T NO 4 Of 5
DESCRIPTION
Felsic Volcanics - dark grey to white, fine grained, finely toto crudely banded.
Modal percent: Quartz 40-45*Plagioclase BO-35%Sericite 30-35*Carbonate ID-15%Chlorite 5-10*Pyrite Q.5-1%
Q.5-1% finely disseminated pyrite, foliation - banding at 72 0 tocore axis at 276.0', 67 0 at 266.5'.
- ?76.3' - 277.3' - quartz veining, trace garnet, 1-2* pyrite.
Mafic to Intermediate Tuff - as per 255.6' - 263.2', finely banded,foliation at 59" to core axis at 280.5'.
Felsic to Intermediate Volcanic - dark grey to black, fine grained,banded to massive.
Modal percent: Quartz 60-65*Plagioclase eO-65%Amphibole IB-20%Chlorite ID-15%Pyrite 1-2*
Finely disseminated pyrite, foliation at 62 0 to core axis at 284.0'- 286.2' - 287.2' - quartz-carbonate veining, carbonate on
contacts, T-2% pyrite on fracture planesnear contacts.
Intermediate Flows - typical, foliation at 62 0 to core axis at304.0', 52 0 at 310.0', 1-2* quartz-carbonate stringers .
- 308.2' - 308.9' - banded quartz-carbonate veining, 1-2*disseminated pyrite and pyrrhotite.
Mafic to Intermediate Flows - foliation at 53 C to core axis at312.0'.
SAMPLE
- 10
122531225412255
12256
12257
1225812259
12260122611226212263
122641226512266
H)F*i
3-5
1-2
1-21-2
1-2
^COT AGt
f R'JM
263.2268.2273.2
277.3
281.5
286.5291.5
293.7297.0302.0307.0
311.2316.2321.2
TO
268.2273.2277.3
281.5
286.5
281.5293.7
297.0302.0307.0311.2
316.2321,2326.0
TOTM
5.05.04.1
4.2
5.0
5.02.2
3.35.05.04.2
5.05.04.8
f, 'j'. A Y 'j
•ty*
tr.002tr
tr
tr
trtr
trtrtrtr
trtrtr
DIAMOND DRILL RECORD EYE LAKE
E MO ,EL-87-4 o 5 of 5
FOOT AGt
FHOM
326.0
346.4
421.0
456.2
T O
346.4
421.0
456.2
477.0
477.0
lit SCRIPTION
Intermediate Flows - foliation at 37" to core axis.
Mafic to Intermediate Flows - atypical, medium grained, 2-35I5quartz-carbonate stringers with minor potash feldspar, amphibo-litic texture, foliation at 37-40 0 to core axis, banding at 48 0 tocore axis at 373.0', fractures at 35 0 and 50 0 to 58 0 to core axis.
- 377.0' - 392.0' - T-2% disseminated pyrite and pyrrhotiteblebs.
- 419.0' - 419. 5 1 - 0.3-foot clean quartz vein.
Interbedded Felsic and Intermediate Tuffs - 2-3X quartz-carbonatestringers with horizons of S-10% carbonate stringers, 3-5X garnetin intermediate tuff. T-3% fine grained wispy pyrrhotite blebs,spotty horizons of S-5% pyrite blebs, well to poorly banded, foli ation and banding at 45 0 to core axis.
Intermediate Volcanics - typical, fractures with quartz-carbonateor pyrite infillings (1-2X).
- 457.7' - 467.0' - fault gouge, soft, friable, foliated,highly fractured with minor compet ntclasts hosted in schistose matrix.
Foliation at 50 0 to core axis at 477.0', fracturing at 55 0 to coreaxis at 477.0' .
E.O.H.
SAMPLE
,,0
122671226812269
122701227112272
12273122741227512276
1227712278122791228012281122821228312284
12285
12286122871228812289
S'U PM
H' F S
1-21-21-2
1-51-51-51-51-51-51-51-5
1-2
1-21-2
FOOT A Gf
r B:} M
326.0331.0336.0
341.0344.0346.4
377.0382.0387.0417.0
421.0426.0430.0433.5437.0442.0447.0452.0
456.2
457.7462.0467.0472.0
TO
331.0336.0341.0
344.0346.4351.4
382.0387.0392.0421.0
426.0430.0433.5437.0442.0447.0452.0456.2
457.7
462.0467.0472.0477.0
IfilAI
5.05.05.0
3.02.45.n
5.05.05.04.0
5.04.03.53.55.05.05.04.2
1.5
4.35.05.05.0
A 'j i, A Y r, .,. .^ — .
. .' r r j M
trtrt r
trtr.002
trtrtrtr
tr.012tr
.016
.002
.024trtr
tr
.002trtrtr
1 i ,' r . K
DIAMOND DRILL RECORDEL-87-5 SHEET NO. Of l
NAME OF PROPERTY EYE LAKE FOOTAGE DIP
HOLE NC
LOG AT IO
LATITUD
ELE VAT 1
STARTED
, EL-87-5 IF NC,TH 307.0' —— —^—^N 44+50N. 03+30W —— iL-dL.
307.0 -43 0
DM AZIMUTH Grid East DIP -45" ———— — — —Dec. 5/87 FINI^HFH Dec . 10/87 ———— — —
FOOTAGE
FROM
0.0
117.0
121.9 144.8 152.6 178.2
201.6 245.7 263.3
TO
117.0
121.9
144.8
152.6
178.2
201.6
245.7
263.3
307.0
307.0
DESCRIPTION
SUMMARY LOG
CASING.
MAFIC TO INTERMEDIATE TUFF
MAFIC TO INTERMEDIATE VOLCANICS (FLOWS)
SILICIFIED MAFIC VOLCANICS (FLOWS)
SILICIFIED MAFIC TO INTERMEDIATE TUFF
MAFIC TO INTERMEDIATE VOLCANICS (FLOWS)- 186.8' - 188.7' - abundant calcite veinlets to 3mm wide;
sulphides to 31i as fins disseminations.MAFIC TO INTERMEDIATE TUFF AND FLOWS - 70:30
FELSIC TUFF
SILICIFIED MAFIC TO INTERMEDIATE TUFF
E.O.H.
i ONTARIO GEOLOGICAL SURVEY ' ASSESSMENT FILES
OFFICE
APR 2 2 1988
RECEIVED
AZIMUTH "OOTAGE
SAM
NO.
12316
S^PSH.
1-3
DIP
P L E
AZIMUTH
RFMARKSPA850855
SUMM
LOGGE
FOOTAGEFROM
186.8
TO
188 7
TOTAL
1.9
ARY LOG
R. I. FogalD BY
ASSAYS
•; OZ/^ON
.024
OZ/TON
DIAMOND DRILL RECORDNAME OF PROPERTY
EL-87-5EYE LAKE
HOLE NO. 307.0'LOCATION 44+50N. 03+30WLATITUDE
ELEVATION
STARTED —
DEPARTURE
Dec. 5/87AZIMUTH Grid East DIP
Dec. 10/87
FOOTAGE
0.0
307.0
DIP
-45"-43 0
AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. L l -O7 - 3 SHEET NO. ' U '
REMARKS PA850855
LOGGED 8YR.I. Fogal
FOOTAGE
FROM
0.0
117.0
121.9
TO
117.0
121.9
144.8
DESCRIPTI ON
Casing.
Mafic to Intermediate Tuff - medium grained, grey to medium green.massive to poorly foliated. Plagioclase-quartz lapilli to 2mmlong appear locally, showing poorly developed foliation. No evi dence of quartz and/or calcite veining. Dominantly massive, med ium green. Red feldspar as minor fracture infilling. Little/no evidence of sulphides. Minor limonitic staining.
Modal percent: Plagioclase 35-40* Quartz 35-40*Amphibole 35-40*Chlorite 5-10*Mica 3-5*
B"C
Feldspar 1-3* LLimonite 1-3*Sulphide trace
- 117.0' - 121.9' - as above
Mafic to Intermediate Volcanics (Flows) - light grey to green,massive. Fine to medium grained, dominated by 1-2mm amphiboles.Trace evidence of sulphides as fine disseminations of pyrite.Minor limonitic staining, restricted to fractures, commonly infill ed with quartz-calcite.
Modal percent: Amphibole 45-55*Plagioclase 25-35*Quartz 3-5*Calcite 3-5*Limonite 1-3*Sulphides trace
- 121.9' - 131.9' - typical, as above
SAMPLE
NO,
•~..~..
NTARAS:
R
12301
1230212303
S,^1H -
0 Gi(ifcSS
oAPR
EC
tr
trtr
FOOTAGEFROM
LOGlCAiWENT fFFICE
22 19
TO
SURVEILES
88
E IV
117.0
121.9126.9
ED
121.9
126.9131.9
TOTAL
{ rl *
1 ^
x"\
4.9
5.05.0
ASSAYS
jQ
fv*^vlf
"— ***.1 —— -v
m.,**r..-I*^
^ra****
AUOZ/TON
•y^\/s y\V'\k s•o
\0 f-5'' jT
*r
tr
trt r
O7-/TOM
\
DIAMOND DRILL RECORD N AMf OF" PPOF J F (^ I ' EYE LAKE2 of 4
FOOT AOf
f ROM
121.9
144.8
152.6
178.2
Td
144.8
152.6
178.2
201.6
DESCRIPTION
Cont'd.- 137.1' - 144.8' - as above, containing up to WU quartz-
calcite veins, typically barren ofmineralization, containing minor sericiteand epidote, both as wisps and discontinu ous lenses within quartz veins.
Silicified Mafic Volcanics (Flows) - interval similar composition- ally to 121.9' - 144.8', containing up to 40* as quartz veins(with lesser carbonate). Volcanics appear dominated by dark greenamphiboles, locally as crystals to 8mm across. Overall massiveappearance. Quartz veins containing sericite withlesser amounts of tourmaline and blebs of pyrite, pyrrhotite asfracture coatings. Veins appear highly deformed, often inter mixed with wisps, lenses of mafic country rock.
- 147.5' - 149.1' - interval dominated by quartz vein, con taining up to 3* pyrite as secondaryfracture coating within vein.
- 149.1' - 152.6' - as above.
Silicified Mafic to Intermediate Tuff - well developed banding,light to medium grey, fine to medium grained. Typical foliations;45 0 at 157.0', 3D 0 at 169.5', 38 0 at 172.0'. Abundant quartz andcalcite veins, parallel to banding, containing trace amounts ofpyrite and pyrrhotite as fine disseminations. Veins averaging1-2mm wide, hosted in an assemblage dominated by amphibole andplagioclase. Few carbonate-rich veins contain blood-red blebs oflimonite along with trace chalcopyrite. Irregularly distributed -discontinuous streaks of mica (potassic alteration?).
Modal percent: Plagioclase 40-55*Quartz 40-55*Amphibole 35-45*Carbonate 8-10*Mica 3-5*Limonite 1-3*Sulphides trace
Mafic to Intermediate Volcanics (Flows) - light to medium green,
SAMPLE
...,
I2304I2305
1 2306
I2307
1 2038
1 23091231012311123121231312314
12315
•or s
trtr
tr
1-3
tr
trtrtrtrtrtr
tr
FOOTAGtfflOM
137.1140.1
144.8
147.5
M9.1
152.6157.6162.6167.6172.6175.6
178.2
TO
140.1144.8
147.5
149.1
152.6
157.6162.6167.6172.6175.6178.2
183.2
TOTAL
3.04.7
2.7
1.6
3.5
5.05.05.05.03.02.6
5.0
iVjSAY 1,
..AM,,.
trtr
tr
tr
tr
trtrtrtrtrtr
tr
,,.- t,*
DIAMOND DRILL RECORD N AMI Of PHOf* FH1 Y.
t-1 n i r" M f i t L - o l - D
EYE LAKE
..H, l r NO 3 Of 1
Foo 1 A c, r
178.2
201.6
201.6
245.7
DESCRIPTION
Cont'ri.
massive, fine-grained. Simi lar compositionally, texturally to121.9' - 144.8' containing very few quartz veins, typically 1-2mmwide, discontinuous, randomly distributed, and barren of minerali zation. Trace evidence of finely disseminated pyrite.
- 186.8' - 188.7' - typical, containing abundant calcite(-quartz) veins averaging 2-3mm wide,sulphides as fine disseminations of py rite, pyrrhotite, with lesser chalcopy rite, overall up to 3?S. Veins trendingat 35 0 to C. A.
- 195.3' - 198.9' - similar to 186.8' - 188.7', containinglesser amounts of sulphides, commonlytr.-U. Veining at 48 0 to C, A.
Mafic to Intermediate Tuffs and Flows - 70:30. Well banded, finegrained, medium green tuffs, containing abundant quartz and cal cite veins, intercalated with lesser amounts of massive, fine grained mafic flows, light to medium green colour. The tuffs con tain abundant (up to 403S) quartz and calcite veins, averaging2-3mm in width, typically barren of mineralization, similar com positionally, texturally to 117.0' - 121.9', trending at 42" toC. A. The flows show little/no quartz or calcite veining, containingtrace pyrite as fine disseminations; less commonly as fracturecoatings. Similar to 121.9' - 144.8' .
- 201.6' - 204.4' - typical mafic-intermediate tuff. Traceevidence of finely disseminated sulphides.
- 207.3' - 211.3' - as per 201.6' - 204.4'.- 212.7' - 217.0' - as above, containing trace arsenopyrite a:
fracture infillings, typically Ornrn wide.- 218.9' - 245.7' - typical mafic to intermediate tuff, con
taining numerous streaks (averaging 8-10mm wide) of mica-rich zones. Also evi dence of orange-red limonite staining.Well developed banding at 40 0 to C. A.
SAMPLE
-H,
1231J
12316
12317
1231E
1231S1232C
1232 1123221232j123241232512326
icirs
tr
1-3
tr-1
tr
trtr
trtrtrtrtrtr
FOOT AGtCBOM
178.2
186.8
195.3
201.6
207.3212.7
218.9223.9228.9233.9238.9241.9
TO
183.2
188.7
198.9
204.4
211.3217.0
223.9228.9233.9238.9241.9245.7
TOTAl
5.0
1.9
3.6
2.8
4.04.3
5.05.05.05.03.03.8
A ', :. A Y '?
Mu,
tr
.024
tr
tr
trtr
trtrtr
.002
.002tr
DIAMOND DRILL RECORD N AMT OF PKOPF.f* I r
HOt-E NO EL-87-5
EYE LAKL
.H|-f ' NO 4 Of 4
FOOT A C. F
263.3 307.0
307.0
DESCRIPTION
Silicified Mafic to Intermediate Tuff - similar compositional ly,texturally to 152.6' - 178.2'. Well developed banding at 40 0 toC. A. Abundant quartz and calcite stringers, typically 2-3mm wide,parallel to banding; trace pyrite, as fine disseminations, re stricted to mafic-intermediate tuff. Micaceous zones as discon tinuous streaks, lenses, barren of mineralization.
- 267.0' - 282.6' - banding becomes highly irregular, contortod.
- 282.6' - 291.9' - banding is quite distinct, at 45 0 to C. A.Barren quartz vein at 282.7' - 283.3'.
- 291.9' - 293.4' - highly carbonatized section showing cavitywith well developed calcite crystals(about 1mm across) growing inwards fromcavity wall. Dusting of pyrite crystalsis also evident, up to 31t.
- 293.4' - 307.0' - typical, showing well developed banding a40 0 to C. A. Quartz vein with minor pyrr hotite and sericite-tourmaline at 305.8' -306.3'.
E . 0 . H .
SAMPLE
r IO
12331
12332I2333I2334I233512336I2337
I2338I2339I2340
'.in PHl [ ' F r.
tr
trtrtrtrtr1-3
trtrtr
FOOT AGEFROM
263.3
267.0272.0277.0282.6287.6291.9
293.4298.4303.4
TO
267.0
272.0277.0282.6287.6291.9293.4
298.4303.4307.0
' ri i A i
3.7
5.05.05.65.04.31.5
5.05.03.6
A rj r, A Y r.Au,,,
tr
trtrtrtrtrt r
trtrtr
DIAMOND DRILL RECORDNAME OF PROPERTY
EL-87-6[YE LAKE
HOLE NO.
LOCAT.ONLATITUDE
ELEVATION
STARTED
44+50N, 09+OOW
DeC. 10/87
LENGTH 317.0'
DEPARTURE ————
AZIMUTH GridFINISHED —
-45 C
Dec. 12/87
FOOTAGE
0.0307.0
DIP
45"42"
AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. t- L ~\" " SHEET NO.
REMARKS PA850R46___________
Of
SUMMARY LOG
LOGGED BY R - ?- F0 9 a1
FOOTAGE
FROM
0.0
81.8
200.3
225.0
244.5
TO
81.8
200.3
225.0
244.5
317.0
317.0
DESCRIPTION
SUMMARY LOG
CASING.
MAFIC TO INTERMEDIATE VOLCANICS (FLOWS)
MAFIC TO INTERMEDIATE TUFF
MAFIC TO INTERMEDIATE VOLCANICS (FLOWS)
MAFIC TO INTERMEDIATE TUFF
E.O.H.
i ONTARIO GEOLOGICAL SURVEY ' ASSESSMENT FILES
OFFICE
APR 2 2 1988
RECEIVED
SAMPLE
NO. ',UDLEHSH -FOOTAGE
FROM TO TOTAL
ASSAYS
07^4 ON O7/TON
DIAMOND DRILL RECORDNAME OF PROPERTY ____EYE! LAKE
HOLE NO. EL-87-6_________ LENG
LOCAT.ON 44+50N. 09-^OOW
LATITUDE
ELEVATION
STARTED
317.Q'
Dec. 10/87
DEPARTURE ^———^^^—
AZIMUTH Grid East
FINISHED .
-45 C
Oec. 12/87
FOOTAGE
0.0307.0
DIP
45"42"
AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. EL-87-6 SHEET NO. ' Of 5
REMARK s PM50846————.———-
LOGGED BY.R.I. Fogal
FOOTAGE
FROM
0.0
81.8
TO
81.8
200.3
DESCRIPTION
Casing.
Mafic to Intermediate Volcanics (Flows) - moderately carbonatized,fine-grained, dark to medium green, massive to poorly foliated.Abundant calci te-quartz stringers, averaging 2-5mm in width, typically barren of mineralization; stringers appear discontinuousoften as lensoidal pods at 50" to C. A. Blood-red limonitic stain ing occurs as fracture infillings associated with calcite string ers. Country rock containing little/no sulphides, rarely as finedisseminations of pyrite.
Modal percent: Amphibole 55-65*Plagioclase 15-20*Calcite 10-15*Quartz 3-5*Limonite tr-1%Sulphide tr-1*
- 81.8' - 91.8' - typical
- 97.0' - 102.0' - typical, containing abundant calcite stringers, few containing light-green carbonateankerite?
- 113.3' - 123.3' - typical.
- 128.8' - 133.8' - typical, containing irregular pods, lens es of calcite veins/lenses, commonly withlittle/no quartz content.
- 133.8' - 137.3' - as per 128.8' - 133.8', containing minorwisps, streaks of mica, commonly Ommwide.
- 138.9' - 142.2' - typical, containing up to 3* sulphides as
SAMPLE
NO.
f~i
123411234212343
123441234512346
12347
12348
S^PSH-
3NTA
R
trtrtr
trtrtr
tr
1-3
FOOTAGEFROM TO
HO GEOLOGICALibtSSMENT F
APR
ECf
81.886.897.0
113.3118.3128.8
133.8
138.9
5219
; i v i
86.891.8102.0
118.3123.3133.8
137.5
142.2
TOTAL
SUF1VEVILES
8 (1
". D
5.05.05.0
5.05.05.0
3.7
3.3
ASSAYS
X*"*^•o^fyi'• i -N/%^v.
-,
^,'r '-''
"T
fm,;,•C; OV--- -.i •,.
OZ/TON
ix^'•j ^""\X;
.- ..' !.'
..''•''"''S..•'^-
.002
.002
.002
.002
.003
.002
.003
.002
OZ/TON
)
\ ' \
j
DIAMOND DRILL RECORD NAME. OF Ph'OF J E.liT V
HOI.t NO JL-87-6
EYE LAKE
rocn
r ROM
81.8
r AGE.
T f)
200.3 Cont'd.
- 142.2'
- 147.0' - 152.0'
- 162.7'
- 167.0'
- 170.6' - 177.0'
- 182.8'
- 191.2'
l ) E: SC R 1 P T 1 0 N
fracture fillings associated with calciteinjection, typically in stringers Ommwide; parallel to calcite veinlets, dis continuous; sulphides as pyrite, withlesser pyrrhotite.
.2' - 147.0' - as per 138.9' - 142.2', however pyrrhotitecontent increases, as discontinuous blebs,typically Omm wide; also associated withcalcite (with lesser quartz) stringers,particularly at 144.5' .
.0' - 152.0' - typical.
.0' - 156.1' - typical, with highly carbonatized, brec ciated zone at 154.6' - 155.0', containingup to 3X sulphides, commonly pyrite asfine fracture infillings, and a light-green carbonate-ankerite.
.7' - 167.0' - typical, containing highly contorted cal cite stringers, typically barren ofmineralization.
.0' - 170.6' - as per 162.7' - 167.0'. containing 1-3*pyrrhotite as vein infilling at 168.2',approximately 8-10mm wide, associated withcalci te-quartz veining.
.6' - 175.6' - typical.
.0' - 180.0' - typical, containing pyrrhotite lens asso ciated with calcite stringers at 177.1'.
.8' - 186.6' - typical, showing well developed brecciateczone at 183.0' - 183.6', infilled withcalcite-quartz, along with T-3% sulphides,commonly pyrrhotite with lesser pyrite;associated with calcite infilling.
.2' - 195.9' - typical, containing numerous hair linefractures infilled with calcite randomlydistributed throughout interval, typicallybarren of mineralization.
SAMPLE
..o
12349
1235012351
12352
12353
1235412355
12356
12357
j U f . S
1-3
tr1-3
tr
1-3
tr1-3
1-3
tr
F O Ci T AGt
FflOM
142.2
147.0152.0
162.7
167.0
170.6177.0
182.8
191.2
TO
147.0
152.0156.1
167.0
170.6
175.6180.0
186.6
195.9
rrjlAI
4.8
5.04.1
4.3
3.6
5.03.0
3.8
4.7
,\',:,,\Y ',
mi
.003
.003
.004
.003
.003
.003
.002
.003
.002
,- ,.,
DIAMOND DRILL RECORD NAMl OF PROPERTY..
HOLE NO ..EL -87 -6
EYE EAKE
NO 3 of 5
FOOT AGE
F HOW
81.8
200.3
225.0
TO
?00.3
??5.0
?44.5
DESCRIP7 ION
Coni 'd.- 195.9' - 200.3' - typical. An increased feldspar content
is noted.
Mafic to Intermediate Tuff - medium grey to light green, fine tomedium grained. A well developed compositional banding is observerindividual discrete bands varying from 2mm to 3cm in width; cross cutting at 45-50 0 to C. A. Composition ranging from amphibole-richdark green bands to amphibole-poor, feldspar(plagioclase)-rich bands,light to medium grey in colour. Secondary carbonization is evi dent as calcite stringers, subparallel to banding, and as irregularcalci te-inf i 1 led hairline fractures, sporadically distributed,typically barren of mineralization; minor associated brecciationzones, also calcite infilled. Trace evidence of sulphides, com monly as fine disseminations of pyrite; to a lesser extent as py rite and pyrrhotite fracture infillings/coatings. Individualfeldspar lapilli rarely observed. Few intercalated bands of mas sive, dark to medium green volcanic flows.
Modal percent: Amphibole 40-555SFeldspar 20-30*Quartz TO-15%Calcite 8-10tChlorite 1-3JSSulphide trace
- 200.3' - 204.6' - typical, containing amphibole needles to8mm.
- 204.6' - 207.0' - typical with up to 30X calcite in irregu lar pods, veins to 10cm wide.
- 207.0' - 217.0' - typical.
- 218.4' - 225.0' - typical, containing trace arsenopyrite asfine disseminations.
Mafic to Intermediate Volcanics (Flows) - similar compositional ly,texttirally to 81.8' - 200.3'. Massive, light to dark green incolour, fine-grained, moderate degree of carbonization as numerouscalcite stringers, averaging 2-3mm wide, typically barren ofmineralization. Few 2-3cm wide tuffaceous horizons are evident,
SAMPLE
NO
1235S
12359
1?360
12361123621236312364
1236512366
SIM PH
l[tf ^
tr
tr
tr
trtrtrtr
trtr
12367 tr
FOOT AGtFROM
195.9
200.3
204.6
207.0212.0218.4222.0
225.0230.0239.5
Tt
200.3
204.6
207.0
212.0217.0222.0225.0
230.0235.0244.5
if)TAi
4.4
4.3
2.4
5.05.03.63.0
5.05.05.0
A:.:, A Y;.'In*
.003
.004
.003
.001
.00?
.002
.004
.00?
.003
.001
1 1 .' l in
DIAMOND DRILL RECORD NAMF of PROFJ EF; T Y... EYE LAKE HOI.c NO .EL-87-6.. . NO 4 of 5
225.0
244.5
244.5
317.0
DESCRIPTION
Cont'd.exhibiting well preserved lapilli to 1mm. Sulphides restricted tofine disseminations of pyrite; pyrrhotite to a lesser extent.
Mafic to Intermediate Tuff - similar compositionally, texturallyto 200.3' - 225.0'. Well developed compositional banding is alsoobserved, trending at 50 0 to C. A. Sulphides as finely dissemin ated pyrite, trace amount.
- 244.5' - 254.5' - typical, containing abundant barren cal cite stringers, veinlets, averaging 3-5mmwide, parallel to subparallel to banding.
- 257.9' - 266.8' - typical, appearing well brecciated withcalcite infilling. Individual lapillialso observed. Trace evidence of sul phides, as fine disseminations of pyritethroughout.
- 271.3' - 285.6' - typical.
- 285.6' - 292.3' - typical, containing an increase in feld spar content to WZ, brown-red in colour,forming discrete beds, averaging 8mm widebarren of mineralization. Sub td anhedraquartz grains to 2mm wide occur in a dis tinct band at 291.6' - 292.3'. Ground mass appears fine grained, light grey,well banded, dominantly feldspar. Traceevidence of pyrite and pyrrhotite as dis continuous pods/lenses within this unit.Probably of sedimentary origin. Barrenquartz vein at 287.1' - 287.4'.
- 292.3' - 309.8' - typical, exhibiting an increased silicacontent, along with decrease in feldsparcontent. Well developed banding at 50"to C. A.
SAMPLE
,,,.
1236?1236?
1237C1237112372
1237;123741237E1237C12377
123781237?1238C12381
f,\n PH :nrs
trtr
trtrtr
trtrtrtrtr
trtrtrtr
POOT AGt
* ROM
244.5249.5
257.9261.2264.1
271.3276.3281.3285.6288.5
292.3297.3302.3305.3
'O
249.5254.5
261.2264.1266.8
276.3281.3285.6288.5292.3
297.3302.3305.3309.8
"i 1 Al
5.05.0
3.32.92.7
5.05.04.32.93.8
5.05.03.04.5
A 'S, AY',
,-AH.
.002
.004
.004
.003
.003
.002
.002
.001
.002
.002
.002
.002
.002
.002
i.; [MN
DIAMOND DRILL RECORDFOOT A C. C
244.5 317.0
317.0
Cont'd.
E.O.H.
NAMt. Of PRO!J tF-iTV
HOLE NO EL-87-6
EYE LAKE
NO 5 of 5
HF. SCRIPT ION
09.8' - 311.2' - well laminated, light grey, fine to med ium grained. Anhedral quartz grains to2mm enveloped by feldspar and quartz-richmatrix. Probably of sedimentary origin,as at 291.6' - 292.3'. Mica laminations(Omm wide) define the bedding, which islocally contorted, but typically at 50 0to C. A. Pyrrhotite and pyrite as discon tinuous pods, to 35S,
!11.2' - 317.0' - as per 292.3' - 309.8'.
SAMPLE
M,.
12382
1238:1238^
MM Pu
lUf S
1-3
trtr
FOOT AGtFROM
309.8
311.2314.2
ro
311.2
314.2317.0
Tl 1AI
1.4
3.02.8
'••j'.. A y o
,'^
.001
.002
.002
DIAMOND DRILL RECORD
00+00, I2+55W
NAME OF PROPERTY
HOLE NO. FI -87- 7
LOCATION
LATITUDE
ELEVATION
STARTED
EYE LAKE
Dec. 13/87
DEPARTURE —————^———
AZIMUTH Grid EastFINISHED Dec. 14/87
-45 0
FOOTAGE
0.0
247.0
DIP
45"44.5
AZIMUTH FOOTAGE DIP AZIMUTHSHEET NO. Of
REMARKS PA786864
SUMMARY LOG
P.I. FogalLOGGED BY
FOOTAGE
FROM
0.0
21.4
111.4
203.8
238.5
TO
21.4
111.4
203.8
238.5
257.0
257.0
DESCRIPTION
SUMMARY LOG
CASING.
MAFIC VOLCANICS.
MAFIC TO INTERMEDIATE TUFF.
FELSIC TO INTERMEDIATE TUFF.
MAFIC TO INTERMEDIATE TUFF - silicified.E.O.H.
^.mm^ t i ii H i" 1 "' —— *
ONTARIO OEOtOOICAt SURVEY. ASSESSMENT FILtS
OFFICE
APR 2 2 1988
SAMPLE
NO. S ut PH - ICES
FOOTAGEFROM TO TOTAL
f
\\
A S S A V S
s '
fi''" /'
f^t'
\^',-
-- -.
,ui i- ; - ;
^
" \ .
AUOZ/TON
: .^r;f: -'-.iy*-
OZ/TON
1
; \
DIAMOND DRILL RECORDNAME OF PROPERTY
EL-87-7EYE LAKE
HOLE NO.
LOCATION
LATITUDE
ELEVATION
STARTED —
257.0'00+00. 12+55U —
Dec. 13/87
DEPARTURE
AZIMUTH
FINISHED .
Grid East Dec. 14/87
-45 C
FOOTAGE
0.0
247.0
DIP
45"44.5
AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. EL-87-7 SHEET MO.
R.MARKS PA786864
Of 3
LOGGED BY.R.I. Fogal
FOOTAGE
FROM
0.0
21.4
- ^.- ARICi ASSss
l
R l^D
D
|
/)
S iJ!
j
TO
21.4
111.4
GEOLOISSMEOFFI
.PR2
C tr c
DESCRIPTION
Casing.
Mafic Volcanics - dark qreen, massive, fine grained. Few sporadiccalcite-quartz veinlets, 2-5mm in width, typically barren ofmineralization. Sulphides limited to fracture coatings and infillings of pyrite, in trace amounts.
Modal percent: Amphibole 55-7055Feldspar 15-20*Calcite 3-55!Quartz 1-355Sulphide trace
- 33.1' - 36.6' - typical, containing lenses/clots of pyrite,with lesser pyrrhotite, 1-2mm across.
iiCAL suRv^'P' - 46.2' - typical with numerous calcite stringers, !IT tin 0 averaging 1-3mm in width, associated pyrite VL '~ ILUO and pyrrhotite to 35! as fracture infilling*2f. coatings.
- 54. ' - 59.3' - typical.J 1988' 69 - ; ' " 72 - 8 ' - typical, containing numerous quartz and cal
cite stringers, barren of mineralization.- 76. '' - 78.9' - as per 69.8' - 72.8', containing orange-red
w C n feldspars as accessory minerals associated1 v u with quart7-ralritP vpirx:
- 87.0' - 90.4' - typical, containing light to medium bluemineral as fracture infilling, associatedwith quartz-calcite. Possibly sodalite (?)
- 90.4' - 92.3' - typical, containing quartz vein, continuousfrom 90.8' - 91.8'. Minor orange-red feld spar and chlorite; small flecks (Ornmacross) of pyrite.
SAMPLE
NO.
123851238^
12385
1238J 1238S
1239C12391
12392
12393
12394
sti^-
trtr
tr
1-31-3
trtr
tr
tr
tr
FOOTAGEFROM
21.426.4
33.1
39.0 42.2
54.369.8
76.0
87.0
90.4
TO
26.431.4
36.6
42.2 46.2
53.372.8
78.9
90.4
92.3
TOTAL
5.05.0
3.5
3.2 4.0
5.03.0
2.9
3.4
1.9
ASSAYS
AU OZ/TOH
.001
.001
.003
.003
.001
.002
.002
.002
.002
.001
OZ/TON
DIAMOND DRILL RECORD OF PROPF-KlY ..EYE LAKE
HOLE. NO
FOOTAGF
21.4
111.4
111.4
203.8
DESCRIPTION
Cont'd.106.4' - 111.4' - typical.
Mafic to Intermediate Tuff - moderate to well developed banding,at 48" to C. A. Fine to medium grained, light grey to medium greenIndividual lapilli observed to 2mm. Quartz grains, sub to anhedraalso locally observed, enveloped by feldspar and amphibole matrix.Trace sulphides as fine disseminations of pyrite. Few sporadiccalcite stringers, barren.
Modal percent: Amphibole 40-55XPlagioclase 15-25*Quartz S-10%Chlorite 1-351!Calcite 1-3*Sulphide trace
- 118.4' - 120.2' - typical, with quartz-feldspar vein at118.8' - 119.5'. Feldspar appears purplein colour, crystals to 1cm across. Minorassociated chlorite. Barren of minerali zation.
- 126.2' - 137.0' - typical, containing an increase in feld spar content, to 40*. Trace evidence ofdisseminated pyrite. Well Banded at 40 0to C. A. Barren quartz veins at 126.5' -126.7' and 136.1' - 136.4'.
- 146.2' - 153.4' - typical, well banded at 380 to C. A.
- 153.4' - 166.0' - typical, highly deformed and contorted inappearance. Numerous quartz-calciteveins; barren.
- 166.0" - 176.0 - typical, displaying well developed bandintat 400 to C. A.
- 179.1' - 194.8' - typical, containing numerous quartzstringers, averaging 5.8mm wide, withtrace amounts of pyrite and pyrrhotite asclots/pods, ^mm wide.
- 197.0' - 203. 8 1 - typical.
SAMPLC
no
1239E
12396
12397
1239E1239912400
124011240212403124041240S12406124071240f124091241C12411124121241:
IDE 5
tr
tr
tr
trtrtr
trtrtrtrtrtrtrtrtrtrtrtrtr
F O O T A G tF RUM
106.4
111.4
118.4
126.2129.2132.5
146.2150.4153.4157.0161.8166.0171.0179.1182.1187.0191.6197.0199.8
TO
111.4
116.4
120.2
129.2132.5137.0
150.4153.4157.0161.8166.0171.0176.0182.1187.0191.6194.8199.8203.8
"i 1 *1
5.0
5.0
1.8
3.03.34.5
4.23.03.64.84.25.05.03.04.94.63.22.84.0
A V. A Y S
.,/to,
.002
.003
.001
.002
.001
.001
.002
.002
.002
.003
.001
.002
.002
.001
.001
.001
.002
.001
.001
...' T'.,
DIAMOND DRILL RECORD NAMf OF PKOPEFi I V. .
HOLE NO EL-87-7
EYE LAKE
HI i i MO 3 of 3
FOOT AUf
203.8
238.5
238.5
257.0
257.0
DESCRIPTION
Felsic to Intermediate Tuff - medium to light grey, well banded,fine to medium grained. No mafic component is observed. Micaceousstreaks (sericite L muscovite) define the banding, often contortedand intercalated with quartz and calcite stringers, commonly Ownwide, subparallel to banding at 45" to C. A. Trace to 35! associatecpyrite and pyrrhotite, also occuring in blebs/clots.
Modal percent: Plagioclase -, rr 7m;Quartz J 3D-/U*Mica 20-25*Calcite 8-103!Sulphide tr-3%
- 203.8' - 209.3' - typical with pyrite and pyrrhotite bearincquartz-calcite veins at 204.3' - 205.7'and 207.7' - 209.0'.
- 209.3' - 214.3' - typical, containing contorted beds. Foldclosure at 209.9' .
- 214.3' - 238.5' - typical, containing 1-33! pyrrhotite (withlesser pyrite) as fracture infillings,commonly Omm wide. Well banded at 480to C. A.
Mafic to Intermediate Tuff - highly silicified. Similar compo-sitionally to 111.4' - 203.8', however abundant quartz veins occur,making up to 405! of interval. Quartz veins contain pyrrhotite andpyrite, locally to 53!, as fracture infillings. Minor carbonatiza tion. Little evidence of chloritization. Sericite-muscovite alsoassociated with quartz veining, infilling fractures.
- 238.5' - 240.1' - typical, containing pyrrhotite as fractureinfillings. Few quartz veins.
- 240.1' - 245.6' - continuous quartz vein, containing 1-32!pyrrhotite, with minor amphibole andchlorite and sericite as fracture infill ing.
- 245.6' - 248.2' - as per 238.5' - 240.1'.- 248.2' - 251.3' - as per 240.1' - 245.6'.- 251.3' - 257.0' - typical.
E.O.H.
SAMPLF
l IO
1241412415
12416
1241712418124191242012421
12422
1242312424
1242512426124271242E
•".in PH
I0f S
1-31-3
1-3
1-31-31-31-31-3
1-3
1-31-3
tr1-31-31-3
FOOT AGEFROM
.
203.8207.0
209.3
214.3219.3224.3229.3234.3
238.5
240.1243.1
245.6248.2251.3254.1
10
207.0209.3
214.3
219.3224.3229.3234.3238.5
240.1
243.1245.6
248.2251.3254.1257.0
T 0 I A 1
3.22.3
5.0
5.05.05.05.04.2
1.6
3.02.5
2.63.12.82.9
A'jGAVS
.001
.003
.004
.001
.004
.001
.007
.002
.001
.001
.001
.001
.001
.001
.002
DIAMOND DRILL RECORDHOLE NO. El-87-8 SHEE1 N0. l Of
NAME OF PROPERTY EYE LAKE
HOU E NC
LOG AT IO
L ATITUD
EL E VAT 1
STARTED
, EL-87-8 , .r*,,-.™ 3?7.n'N 20-H)OS. 07+OOW
ON A7IMLITH Gfld EdSt46"
Dec. 15/87 F , N ,SHF D Dec. 16/87
FOOTAGE
FROM
0.0
14.1
49.4
231.2
TO
14.1
49.4
231.2
327.0
327.0
D E S C R 1
SUMMARY
CASING.
P T 1 O N
LOG
FOOTAGE
0.31/.
00
DIP
46 043 0
MAFIC TO INTERMEDIATE VOLCANICS (FLOWS).
INTERMEDIATE TUrF.
MAFIC TO INTERMEDIATE TUFF.
E.O.H.
ONTARIO GEOLOGICAL SURVEY ' ASSESSMENT FILES
OFFICE
APR 2 2 1988
RECEIVED
AZIMUTH FOOTAGE
SAM
NO. siS^
DIP
P L E
AZIMUTH
RFMARKS PA786869
SUMM
LOGGE
FOOTAGEFROM TO TOTAL
ARY LOG
D BY K.I- Fogal
ASSAYS
OZ/TON OZ/TON
DIAMOND DRILL RECORDNAME OF PROPERTY
HOLE NO. EL-87-8LOCAT ION
LATITUDE
EL EVATION
STARTED
EYE LAKE
20+OOS, 07+OOW
Dec. 15/87
327.0'
DEPARTURE
AZIMUTH .
FINISHED
Grid East Dec. 16/87
46 C
FOOTAGE
0.0
317.0
DIP
46 043"
AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. EL-87-8 SHEET NO.
REMARKS PA786869_____
LOGGED BYR.I. Fogal
FOOTAGE
FROM
0.014.1
49.4
TO
14.149.4
231.2
DESCRIPTION
Casing.Mafic to Intermediate Volcanics (Flows) - medium green to lightgrey, massive, fine to medium grained. A poorly developed bandingis locally observed; overall massive appearance. Sporadic quartz-calcite stringers, averaging 2-5mm wide, typically barrenof mineralization. Sulphides restricted to finely disseminated pyrite, less commonly as fracture infillings. Isolated brecciated zones appear secondarily infilled with quartz-calcite.
Modal percent: Amphibole 45-5556Plagioclase -, ,n , n5(.Quartz ^Calcite 3-5XChlorite 1-356Sulphide trace
- 29.9' - 39.9' - typical.
Intermediate Tuff - well developed banding at 70 0 to C. A. Lightto medium grey with isolated amphibole-rich dark green bands.Sulphides as fine disseminations of pyrite. Micaceous laminations,averaging Omm wide, define the banding. Minor calcite and quartzveinlets, discontinuous, typically barren of mineraliation.
Modal percent: Plagioclase -, ,,. 7t.~.Quartz J bt) -' b *Sericite , , Muscovite J '"-'^Amphibole S-5%Calcite 3-556Sulphide trace
- 49.4' - 54.4' - typical, isolated brecciated zone, barren,
SAMPLE
NO.
1242912430
194111 C *T -J \
12432
12433
S^PSH-
trtr
tr tr
tr
FOOTAGEFROM
14.119.1
TO
19.124.1
| ~*N i AF H f\L
29.9*34.9
49.4
R39.9
54.4
TOTAL
5.0
5.0
(0 GEOl SESSN
OF
APR J
ECE5.0
5.0
A S S A V S
5GICAI ENT FICE
2 19
IV l
r
l\
-,;
SUFiVEILES
38
: D
.^^^f fi j
s h*J M/,^4C -r-S/^o,^v'''"^'
OZ/TON
.001
C001
y
001 001
ofr-^ff*^0-"1 -
"t T" ' '
7?^. .
'Ci OV (
^jla^-rfS
.002
07/TON
"l-s,
'''f
'.S^
"f . 4/
i f/
Jr. - o
**** jj^\ v jf^
7
i
\
DIAMOND DRILL RECORD NAMI" Of PKOPKRTY
HOLE NO --- EL-87-8.
EYC LAKC
2 of 3
FOOT A O f
f ROM
49.4
T O
231.2 Cont'd.
54.4'
67.0'
81.3'
98.2'
104.4' 112.5'
123.8' 131.0'
183.2'
194.5'
198.1 208.0'
- 143.8' -
DESCRIPTION
at 50.6' - 50.9' infilled with calcite (withlesser quartz ).
1 - 63.0' - typical.
1 - 77.0' - typical, appearing poorly banded to locallymassive.
1 - 91 .3' -as per 67.0' - 77.0' .
' - 102.5' - typical, containing finely disseminatedpyrite and pyrrhotite to 3/6, as fractureinfilling in poorly banded intermediatetuff.
4' - 109.2' - as per 98.2' - 102.5'.5' - 122.5' - poorly banded to massive, possibly an
intermediate flow.8' - 125.1' - as per 98.2' - 102.5' .0' - 141.0' - massive intermediate, containing streaks/
clots of pyrite and pyrrhotite to 35S asfracture infillings. Quartz vein, barrencontaining orange feldspar, at 131.3' -131.5'.
8' - 183.2' - highly altered sulphidized zone containincdiscontinuous streaks of pyrite, withlesser pyrrhotite up to 1cm wide, sporadi cally distributed throughout poorly tomoderately banded intermediate volcanic(flow or tuff).
2' - 188.2' - typical, well banded intermediate tuff,crosscutting at 65" to C. A. Trace evid ence of finely disseminated pyrite.
5' - 196.4' - typical, containing distorted bands with1-3^ pyrite, with lesser pyrrhotite asfracture infillings to 1mm wide.
1' - 202.0' - as per 194.5' - 196.4'.D' - 219.8' - as per 183.2' - 188.2', containing pyrite-
SAMPLF
MO
I2434I2435I2436I2437I243824392440
12441124421244;1244'1244512446
124471244812449124501245112452124531245412455
12456
1245712458
'.III PH
HIT'.
trtrtrtrtrtr1-3
1-3trtr1-31-31-3
8-108-108-108-108-108-108-108-10tr
1-3
1-33-5
FOOT AGt
FROM
54.458.567.072.081.386.398.2
104.4112.5117.5123.0131.0136.0
143.8148.8153.8158.8163.8168.8173.8178.8183.2
194.5
198.1208.0
TO
58.553.072.077.086.391.3102.5
109.2117.5122.5125.1136.0141.0
148.8153.8158.8163.8168.8173.8178.8183.2188.2
196.4
202.0212.5
*') Mi
4.14.55.05.05.05.04.3
4.85.05.01.35.05.0
5.05.05.05.05.05.05.04.45.0
1.9
3.94.5
A S 0 A V 'j
Ay-. ; H DN
.001
.001
.001
.001
.002
.002
.002
.003
.003
.003
.001
.001
.001
.001^001.002.001.001
^001.001.001
<.001
.002
.002
.002
i j ; r . K
DIAMOND DRILL RECORD NAMF. OF" PHOPEH1 r ..
HOLE: NO ...EL-87-8
EYE LAKE
'.MI I ^ NO 3 of 3
FOOT A L; r
FROM
49.4
231.2
7 O
231.2
327.0
327.0
INSCRIPTION
Cont'd.pyrrhotite to 5X as fracture infilling* tc1mm wide, scattered randomly, parallel tosubparallel to banding.
Mafic to Intermediate Tuff - well developed compositional banding,crosscutting at 55 0 to C. A. Alternating 2-5mm bands of dark greenamphibole-rich mafics and medium to light grey feldspar-rich assem blage. Sulphides typically as fine disseminations of pyrite, andpyrrhotite to a lesser extent.
Modal percent: Amphibole 45-5536Plagioclase -, , g , Q^Quartz ^Chlorite 1-336Calcite 1-336Sulphide trace
- 244.5' - 254.5' - highly contorted bands, exhibiting foldclosures. Sulphides as trace pyrite -finely disseminated.
- 262.0' - 279.6' - well banded, containing light green feld spar, possibly as an alteration product.No associated sulphides.
- 287.3' - 295.8' - poorly banded, containing light-greenfeldspar, as per 262.0' - 279.6'. Tracepyrite.
- 302.0' - 327.0' - poorly banded to massive, containing tractevidence of finely disseminated pyrite.Light green feldspar as secondary infill ing making up to 205! of interval. Minorcarbonatization as calcite stringers. Veinmaterial consisting of feldspar and quartzcalcite; typically barren of minerali zation.
E.O.H.
SAMPLE
'40
1245912460
1246112462
1246312464
124651246612467124681246912470
1247112472124731247412475
Mil (Ml
Htf r*
3-53-5
trtr
trtr
trtrtrtrtrtr
trtrtrtrtr
FOOTAGE:FROM
212.5215.6
231.2236.2
244.5249.5
262.0267.0272.0275.0287.3291.3
302.0307.0312.0317.0322.0
TO
215.6219.8
236.2241.2
249.5254.5
267.0272.0275.0279.6291.3295.8
307.0312.0317.0322.0327.0
TOTAL
3.14.2
5.05.0
5.05.0
5.05.03.04.64.04.5
5.05.05.05.05.0
ftV.AY'j
.,'w.
.001
.001
.002
.001
.001
.001
.002
.002
.001
.001
.001
.002
.002
.001
.001
.001^001
DIAMOND DRILL RECORDNAME OF PROPERTY
EL-87-9EYE LAKE
24+OOS, 01+60EHOU E NO.
LOCATION
LATITUDE ———————————
ELEVATION ——————————
STARTED Dec. 16/87
397.0'
DEPARTURE
7IMUTH Grid East DIP Dec. 17/87
-45. 5 C
FOOTAGE
0.0
200.0
397.0
DIP
45. 5 043. 0 040. 0 0
AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. FL-87-9 SHEET NO.
REMARKS PA786868 ————————
SUMMARY LOG
P.I. FogalLOGGED BY
FOOTAGE
FROM
0.0
36.6
150.5
TO
36.6
150.5
397.0
397.0
D E S C R 1 P T 1 ON
SUMMARY LOG
CASING.
MAFIC TO INTERMEDIATE VOLCANICS (FLOWS).
MAFIC TO INTERMEDIATE TUFF.
E.G. H.
SAMPLE
NO. bMH ' FOOTAGEFROM TO TOTAL
ASSAYS
ON TARIO C ASSE5
AF
..,
O//HON
EOLOG iSMEN OFF1C
R22..,
OZ/TON
CAL B H T i-ll^
1988
V E t
" : !'.'tV
0
)
DIAMOND DRILL RECORDNAME OF PROPERTY FYF
HOLE NO. .
LOCATION
LATITUDE
EL E VAT ION
STARTED
EL-87-924+OOS, 01+60E
Dec. 16/R7
l AKFLENGTH 397.0'
DEPARTIIB F
AZIMUTH Grid East OIP -45. 5 0F.NISHFH Dec. 17/87
FOOTAGE
0.0200.0397.0
DIP
45.543.040.0
AZIMUTH
'
1
FOOTAGE DIP AZIMUTHHOLE NO. EL-87-9 SHEET NO. ] Of 3
.PA786868REMARKS.
LOGGED BYR.I. Fogal
y- u*ST- jVi
z
vB*7"7
* i•••ZO a O
1•J)UJ
1<
FOOTAGE
FROM
0.0
36.6
p j C- C"- C* oh ci 5 i*, *ir
-•-•^,-r.
TO
36.6
150.5
* .'.'-i'-'^
D f3 L3O "m
* Lf C^ U
Q
DESCRIPT ION
Casing.
Mafic to Intermediate Volcanics - dark grey to dark green, massive,medium grained. Very few quartz veins, typically barren of minera lization. Sulphides limited to fine disseminations of pyrite, intrace amounts.
Modal percent: Amphibole 50-65*Plagioclase -i ?(; ^vQuartz J "- 1"*Mica 3-5*Calcite 1-3*Sulphide trace
11"
1)1
- 50.0' - 52.5' - typical, containing barren quartz vein at51.4' - 51. 7'.
- 57.5' - 59.5' - typical, containing small quartz vein at58.5' - 58.7', barren of mineralization.
- 64.9' - 68.3' - typical, containing irregular zones with alight green feldspar associated with lesserquartz, no apparent sulphides, discontinu ous.
- 69.9' - 73.7' - as per 64.9' - 68.3'.- 77.0' - 87.0' - typical.
- 93.7' - 96.0' - typical, containing barren quartz and feld spar vein at 94.4' - 94.8'.
- 107.3' - 112.2' - typical, with quartz and feldspar (lightgreen) vein, barren of mineralization at109.7' -110.0'.
- 114.7' - 117.7' - typical intermediate volcanic containinga quartz-feldspar vein at 115.1' - 116.2';minor chlorite, barren of mineralization.
SAMPLE
NO.
1247612477
1247?
1247?
1248C
12481124821248:12484
12185
12486
SULPH IDES
trtr
tr
tr
tr
trtrtrtr
tr
tr
FOOTAGEFROM
36.641.6
50.0
57.5
64.9
69.977.082.093.7
107.3
114.7
TO
41.646.6
52.5
59.5
68.3
73.782.087.096.0
112.2
117.7
TOTAL
5.05.0
2.5
2.0
3.4
3.85.05.02.3
4.9
3.0
ASSAYS
r* 1
f, A
f 3
l"
l 5 L1 W k l 06 "
',
V^Y'"'/^~i*y^
OzVVoN
.001
.002
:.001
.001
.001
:.001c. 001.001.001
,., f , i
.66X
^'/24k..f^..~~
OZ/TON
VX/fX7 \- jjl.
DIAMOND DRILL RECORD CYC LAKL
Fi P7 QL L - u f - 7 of 3
FOOT A GT
F ROM
36.6
150.5
TO
150.5
397.0
DESCRIPTION
Cont'd.- 117.7' - 128.3' - interval contains few intercalated tuf
faceous beds up to 5cm wide, typicallybarren, individual lath-like crystals upto 2mm long.
- 133.4' - 148.9' - typical, containing abundant tuffaceoushorizons. This marks a transition zonebetween intermediate to mafic volcanicflows and tuffs. A broad gradational con tact is observed, over a width of approxi mately 30 feet. Trace sulphides as finedisseminations of pyrite.
Mafic to Intermediate Tuff - similar compositionally to 36.6' -150.5', however crystals (laths) of feldspar are visible. Noapparent banding, rather massive. Few quartz veins, up to 5cmwide, discontinuous in nature, containing no visible sulphides.Trace pyrite overall.
- 157.0' - 159.8' - typical, containing barren quartz vein at157.9' - 158.2'.
- 168.7' - 170.9' - typical, increasing feldspar content, to50X, imparting a light grey colour.Quartz S, feldspar vein at 169.1' - 169.4'
- 184.4' - 188.9' - typical, containing quartz and feldsparvein at 187.8' - 188.1', barren of mine ral ization.
- 191.8' - 195.5' - numerous quartz and feldspar-calciteveins, averaging 1cm wide, typically bar ren of mineralization.
- 200.0' - 205.0' - typical.- 210.2' - 220.2' - typical, with numerous quartz and feldspar
veins, averaging 2-5cm in width, barrenof mineral ization.
- 227.8' - 237.8' - typical, lapilli to 2mm long evident.
- 245.0' - 247.6' - typical, quartz and feldspar vein, barrenof mineralization of 245.4' - 245.7'.
- 259.6' - 269.6' - typical, containing irregular blebs/clots
SAMPLE
•10
1248/1248f1248?
1249C1249'1249;
1249;
1249'
12495
1249e
12497
1249E1249?1250C
125011250212502
12504
-.III PH
tot S
irtrtr
trtrtr
tr
tr
tr
tr
tr
trtrtr
trtrtr
tr
FOOTAGt
FROM
117.7121.9124.9
133.9138.9143.9
150.5
157.0
168.7
184.4
191.8
200.0210.2215.2
227.8232.8245.0
259.6
ro
121.9124.9128.3
138.9143.9148.9
155.5
159.8
170.9
188.9
195.5
205.0215.2220.2
232.8237.8247.6
264.6
'i.lAl
4.23.03.4
5.05.05.0
5.0
2.8
2.2
4.5
3.7
5.05.05.0
5.05.02.6
5.0
ASS A Y 'o
,4w,
.001
.001
.001
^ 001.001.001
.001
^001
.002
.001
.002
.001
.001
.002
.001
.001
.001
^001
i ; T .*
DIAMOND DRILL RECORD NAME OF PROPERTY.
HOLE: NO ...E,L-.87-9
EYE LAKt
NO 3 of 3
rooi
F ROM
150.5
ACT
TO
397.0
397.0
Cont'd.
- 272.0'
- 283.2'
- 290.2'
- 301.8'- 310.5'- 329.1'
- 344.8'
- 363.0'
- 377.0'
- 388.9'
E.O.H.
O C SC R 1 P 7 1 0 N
of orange-red feldspar, sporadically dis tributed, averaging 1-3cm across; barrenof mineralization. Slight increase inamphibole content.
272.0' - 277.0' - containing numerous light green feldspar-quartz veins, 2-5cm wide, typicallybarren of mineralization.
283.2' - 286.0' - typical with abundant quartz veins at283.4' - 283.5' and at 284.0' - 285.1'.Minor chlorite, no evidence of sulphides.
290.2' - 295.2' - typical, containing hairline fracturesinfilled with feldspar and lesser quartz.Epidote vein, 2mm wide, at 294.8'.
301.8' - 304.5' - as per 290.2' - 295.2'.310.5' - 313.9' - as per 290.2' - 295.2'.329.1' - 339.1' - typical.
344.8' - 349.2' - typical, containing barren quartz vein at348.1' - 349.0'.
363.0' - 366.4' - containing quartz veins, weakly chlori-tized, barren of mineralization at 363.2'to 364.3' and 365.4' - 365.7'.
377.0' - 387.0' - typical, containing trace sulphides asfine disseminations of pyrite.
388.9' - 397.0' - containing abundant quartz veins, typically Ocm wide, barren of mineralization.
SAMPLE
'!O
12505
12506
12507
12508
1250912510125111251212513
12514
12515125161251712518
f,\n PH iurs
tr
tr
tr
tr
trtrtrtrtr
tr
trtrtrtr
FOOTAGE.
f ROM
264.6
272.0
283.2
290.2
301.8310.5329.1334.1344.8
363.0
377.0382.0388.8393.7
ro
269.6
277.0
286.0
295.2
304.5313.9334.1339.1349.2
366.4
382.0387.0393.7397.0
IN TAi
5.0
5.0
2.8
5.0
2.73.45.05.04.4
3.4
5.05.04.93.3
M. G AYS
W,.
.002
'.001
.001
.001
.002
.001
.001•c. 001.002
.001
•c. 001.001
^001.001
l l l l l l l l l l l l l l l l l l l
LEGEND FOR THE DIAMOND DRILL HOLE SECTIONS
FOR THEEYE LAKE (INC. KOMAR) PROPERTY
Patricia M.D., Ontario
q.v.,c.v. Quartz/carbonate veins
8 Intermediate and felsic intrusives 8a Granite 8b Diorite 8c Granite gneiss 8d Porphyry, quartz/feldspar
Mafic to ultramafic intrusives 7a Gabbro, diabase 7b Peridotite
Iron formation6a Oxide facies6b Carbonate faciesGc Silicate facies6d Sulphide facies
Clastic sediments5a Wacke5b Mudstone, argillite5c Siltstone
Felsic volcanics4a Flows4b Tuff, lapilli tuff4c Breccia, agglomerate
Intermediate volcanics3a Flows3b Tuff, lapilli tuff3c Breccia, agglomerate
Mafic volcanics2a Flows2b Tuff, lapilli tuff2c Breccia, agglomerate2d Amphibolite
Ultramafic volcanics
SYMBOLS Overburden...................^JGeological contact........77—
Bedding............................"^
Foliation...........................r-
Fault, shear zone........
Sample interval (feet) with gold assay in ounces per ton .............wt
Lost core...........................
o/b
(5 — 4
LG
Alterationsi - silicification
se - sericitization eh - chloritization ea - carbonatization
Mineralizations - sulphides
po - pyrrhotite py - pyrite cp - chalcopyrite As - arsenopyrite sp - sphalerite
Ga - galena Mo - Molybdenite
gf - Graphite tour - tourmaline
Fig. 5
VLF EM Fraser Filtered Inphase Profile (%)Vertical Field Magnetic Profile
(x 1000 gammas)
EL-87-lEL-87-2&L. 00
' E.O.H. 297-0'
E.O.H. 3I7-0
POWER EXPLORATIONS INC.
EYE LAKE PROPERTY Pickle Lake Area Patricia MD., Ontario
D.D.H. SECTION 0+50 SLOOKING NORTH
Scale r - 40 feet
For legend see Figure No. 5DDJH.Nos.EL-87-142
GEOCANEX LTDTORONTO CANADA
Vertical Fold Magnetic ProfB* (x 1000 gammas)
- 1.5
- 10
EL-87-4—— — — — Surface — -
VLF EM Fraser Filtered Inprtase Profile (S)
75 -
- 0.5- MAG
50 -*
25 -EL-87-3
4E L--0——-I- 5E 6Ei
~-!00
--20O
SEi
9E -J——O -J
•-100'-
-200-
POWER EXPLORATIONS INC.
EYE LAKE PROPERTY Pickle Lake Area, Patricia M.D., Ontario
D.D.H. SECTION 11+00 NLOOKING NORTH
KOMAR GRID SECTION
DD.H. No*. EL-87-3 ft 4
m^x GEOCANEX LTD TORONTO. CANADA
BY: RF. /R.TJI.DATE: Nov. 1987SCALE: 1:480
SO1 TOO-
Scale r - 40 feet
For legend see Rgure No. 5
E.O.H. 397-0'
•-300-
3o E.O.H. 477-0'
Vertical Field Magnetic Profile (x 1000 gammas)
- 1.5
- 1.0
- 0.5
- - O
EL-87-68W
l
20O-
7W i
EL-87-56W 5W
i
E.O.H. 317-0'
MAG
VLF EM Fraser Filtered Inphase Profile (y0)
75 -i
50 -
25 -EL-87-5
4W l o -
E.O.H. 307-0
50' 100'
Scale 1" - 40 feet
For legend see Figure No. 5
-~-—————-IOO -
POWER EXPLORATIONS INC.
--200
EYE LAKE PROPERTYPickle Lake Area Patricia M.D., Ontario
D.D.H. SECTION 44+50 NLOOKING NORTH
KOMAR GRID SECTION
D.D.H. Nos. EL-87-5 X 6
GEOCANEX LTD.TORONTO. CANADA
BY: R.F. l R.T.M.DATE: Nov. 1987SCALE: 1: 480FIGURE No. 8
l
l
l
l
l
l
l
l
l
l
l
l
l
l
l
l
l
l
l
Venice! Field Magnetic Profile (x 1000 gammas)
l- 1.5
VLF EM Fr*ser Filtered InphtM Profit* f.%)
75 -
MAG50 -
For legend see Figure No. 5
--30O——
POWER EXPLORATIONS INC.
EYE LAKE PROPERTY Pickle Lake Area, Patricia M .D., Ontario
D.D.H. SECTION 0+00LOOKING NORTH
KOMAR GRID SECTION
D.D.H. No. EL-87-7
QEOCANEX LTDTORONTO CANADA
BY: RF. /R.T.M.Nov. 19*7SCALE: 1:480FIQURE No. t
• rVertlceJ Field Magnetic Profile (x 1000 gammas) VLF EM Fraser Filtered
Inphuft Profile
i i i i i i i i i i i i i i i i l i
1.5
-•300-
POWER EXPLORATIONS INC.
EYE LAKE PROPERTY Pickle Lake Area, Patricia M.D., Ontario
D.D.H. SECTION 20400 SLOOKING NORTH
D.D.H. No. EL-87-8
GEOCANEX LTDTOnONTO. CANADA
BY:R.F.DATE: Nov. W8TSCALE: 1:480FIOURE No. W
O 50' l i , i . l
E.O.H. 327-0
100'
Scale r - 40 feet
For legend see Figure No. 5
Vertical Field Magnetic Profito (x 1000 gammas)1-15
VLF EM Fraser Filtered Inphase Profto (%)
5E
--iOO -
-300-
--IOO -
50* 100-
Scato r - 40 feet
For legend see Figure No. 5
-200-
E.O.H. 397-0
POWER EXPLORATIONS INC.
EYE LAKE PROPERTY Pickle Lake Area. Patricia MD., Ontario
D.D.H. SECTION 24+00 SLOOKING NORTH
DDK No. EL-87-9
BDBC&MIEJL GEOCANEX LTD.TORONTO. CANADA
BY: RF. t R.T.M.DATE: Nov. 1987SCALE: 1:460FIGURE No. H
ijgi\5i
NO.
•SAMPLE
•SAMPLE
^^ BELL- WHITE ANALYTICAL LABORATORIES LTD.\^r^ P.O.
4061
BOX 187,
/TT .\t*4-f -
(S) OF: Core (136)
(S) FROM: Mr
l Sample No. 0
1
1
1
1
1
1
1
1
1
1
1
H BfccORDANCt
121123456789
12120123456 789
12130123d56 789
1214012345
* Estimated
WITH LONO. ESTABLISHED
. R. Higgi
z. Gold
TraceTraceTraceTraceTraceTraceTraceTrace TraceTraceTraceTraceTraceTraceTrace TraceTrace1 raceTrace1 raceTraceTrace TraceTraceTrace TraceTraceTraceTraceTraceTraceTraceTraceTrace
NORTH
HAILEYBURY. ONTARIO TEL
firat? of AnnlptfiPage 1 of 2
DATE:
RECEIVED:
nson, Geocanex Ltd.
PROJECT:
Sample No
12146789
12150123456789
12160 1234567 S9
12170 123456789
672-3107
December 17, 1987
December 1987
Lye Lake
Oz. Gold
TraceTrace0.002*Trace0.002*TraceTraceTrace TraceTraceTraceTraceTraceTraceTrace TraceTraceTraceTraceTraceTraceTrace TraceTraceTrace TraceTraceTraceTraceTraceTraceTraceTraceTrace
BELL-WHITE ANALYTICAL LABORATORIES LTD.
.MCRICAN CUSTOM. UNLtOG IT IS i P C C II It ALL * STATED ^^J*~\ ^^^F
HEU| SHEETS HAVE NOT BEfN ADJUSTED TOKAT^VOR LOSSES AND CAINS INHERENT IN 1 H ASSAY PROCESS
COMHEN.THE FIRE f J4g^^
DELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-31O7
lf
LNO. 4061
SAMPLE (S) OF:
Qlerttfirat? of AnalplaPage 2 of 2
DATE:
Core (136)
JAMPLE(S) FROM: Mr. R. Higginson, Geocanex Ltd
December 17, 1987
RECEIVED: December 1987
PROJECT: Eye Lake
1Sample Mo. Oz. Gold
1
1
1
1
1
1
1
1
1
1
1
1 ^CORDINCCMEHICAN CUSTOMTHERWISE COLD(ES^SHEETS HAV
JAltMoR LOSSES
12180123456 789
12190123456 789
12200 123 456 789
12210 123
* Estimated
WITH LONG-ESTABLISHEDUNLESS IT IS SPECiriCAlL
TraceTraceTraceTrace TraceTraceTraceTraceTraceTraceTraceTraceTraceTrace Trace0.026Trace Trace0.002*TraceTraceT r s c eTrace0.008 TraceTrace0.002* TraceTrace0.004Trace 0.016TraceTrace
NORTHY STATED
Sample No.
12214567 89
122201234567 89
12230 1234567 89
12240 1234 567
BELL-WHITE ANALYTICAL
^ __ ^^
Oz. Gold
TraceTraceTraceTrace TraceTraceTrace 0.008Trace0.002*0.002*TraceTraceTrace TraceTraceTrace TraceTraceTraceTrace T r d c eTraceTrace TraceTraceTrace Trace0.002*TraceTrace Trace0.0120.002*
LABORATORIES LTD.
AND SILVER VALUES RI PORTED ON .^^ J^^^i NOT BEEN ADJUSTED TOAND CAINS INHlHlNt IN ASSAY PHOCCSS
COMPEN.THE r IRE /J^^r
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187. HAILEYBURY. ONTARIO TEL: 672-3IO7
111
"
1111111111111
Qkrttf irafe of AuaUjBtaNO. 0140
SAMPLE(S) OF:
SAMPLE(S) FROM:
S amp le No .
12301231 56789
123101 234 56189
12320
* Estimated
IN ACCORDANCF WITH l ONG -f STAHL ID
Core (40)
Mr . Rob Fogal ,
Oz. Gold
TraceTraceTraceTrace Trace1 raceTraceTraceTraceTraceTrace TraceTraceT r ace Trace0.024TraceT raceTraceTrace
HfO NORTH
DATE:
RECEIVED:
Geocanex Ltd.
PROJECT: E
Sample No.
1232123
b6789
123301 234 56789
12340
BELL-WHITE ANALYTICAL. __ ---7
January 6, T988
December 1987
ye Lake
Oz . Gold
TraceTraceT r o c en . o o 2 *0.002*TraceTraceTraceTraceTraceTrace TraceTraceT r o c e TraceTrace1 r a c eTraceTraceTrace
LABORATORIES LTD.
OTHrPWI'.f GOLD AND 5.ILVIM VAillf;; Mff'OMTrD ON s^SJS ^^~***^ IHIsr MltlTS IIAV1 NOT litIN AOnlMI.D lo COMPIN. /S^^ .^P^*^^ SA1E rOH LOSSES AND GAINS INIILHINT IN THE FIHt S-jK——^l'^^^
AbbAV PKOCrsi. ^-^^S^C*^^
1 JB1 Vi
^ BEU.VVHITE ANALYTICAL LABORATORIES LTD.••^ ——————— .1. .11.1 K l' ————————————————————————————————————————————————————————————————————————————
^^^ P.O. BOX 187. HAILEYBURY. ONTARIO TEL
(Crrtiffrat? of AnalgaiBNO. 4008
| SAMPLE (S) OF: Core (67)
. SAMPLEBB
1
1
11
1
1
11
1
1
1
1III ACCORDANCIAffTHICAN CUtTOMOTHtftWKI GOLD
(S) FROM: Mr. James
Sample No .
120456789
12050123456789
12060123456789
120701234567e
* Estimated
WITH LONO'tfTA*LliH(D NORTH. UNLII* IT II irtCiriCALLY (TATCOAND *H.VIN VAlUtt KtrOXItO OH
Pierce,; ,, '
Pt Cold
TraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTrace TraceTraceTraceTraceTraceTraceTraceTraceTraceTrace0.002*TraceTrace0.020TraceTraceTraceTraceTrace
i 672-3107
DATE: December 11, 1987
RECEIVED:
Geocanex Ltd.PROJECT:
Sample No.
1207912080
123456789
12090123 A56789
12100123 456789
121102
'
,
•CLL-WHITt ANALYTIC^-**o yy.^^r JS^
December 1987
Eye Lake
Oz Gold
Trace0.002*TraceTraceTrace0.002*TraceTraceTraceTraceTraceTraceTraceTraceTrace TraceTraceTraceTraceTraceTraceTraceTrace0.002*Trace TraceTraceTraceTraceTraceTraceTraceTrace
AL LABORATORIES LTD.
THIK (NlfTI HAV1 NOT IICN ADJUIUD TO COMFIN- ^'^5f ^.^^'•flk f on koittt
1
AMP OAINf INMININT IN TMt r mlAIIAT PNOCtll. ffj^^^&rfi*"*^^
1 4^^
i JgPE
•m BELL -WHITE ANALYTICAL LABORATORIES LTD.V^y P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-3IO7
Qfcriifiratr of AnalpteNO. 4007
1 SAMPLE(S) OF: Core (44)
I SAMPLE(S) FROM: R. nigginson, Geocanex
1
1
1
1
1
1
1
,
1
1
1 re^
IN HcCORDANCrAM^CAN CUSTOMbrnEBWISE COLD
Sample No.
120012345 6789
12010123456789
1202012
* Estimated
oSt/ecd ' .
WITH LONrt ESTABLISHED NORTHUNLESS 11 IS S.PECIMCAI.LY STATtD
AND SILVEf* VALUES REPORTED ON
Oz Gold
0.002TraceTraceTrace0.002* 0.002*0.006TraceTraceTraceTraceTraceTraceTraceTraceO.OORTrace0.0060.006TraceTraceTrace
DATE: December 11,1987
RECEIVED:
Ltd.
PROJECT: Eye
-
Sample No.
120234567 89
12030123456789
120401234
December 1987
Lake
Oz Gold
Trace0.0080.002*TraceTrace TraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTrace0.010TraceTraceTrace
BELL-WHITE ANALYTICAL LABORATORIES LTD.
^-tSlIHISf SHEETS HAVC NOT BEEN ADJU&TCO TO COMPCM. ^^^ ^^^^^^BATE.tOB LOSSES
1
AND CAINS INHERENT IN THE TIREASSAY PROCESS /^r^j^L^U&^E^^
Pv* ^^^^^^^^^^^fisr . . . , . . . .
I^SJHL BELL- WHITE ANALYTICAL LABORATORIES LTD.iiSSSr P.O. BOX 187. HAILEYBURY. ONTARIO TEL: 672-31O7
QJrritfiratr of AttalgataNO. 0114
JsAMPLE(S) OF:
— SAMPLE(S) FROM:
1
1
1
1
1
1
1
1
1
1
1
1
l,/
Core (28)
Mr. James
Sample No.
122489
122501234567 B9
1226012
1227789
122801 2345678 9
* E st i m a t
DATE: January 5, 1988
RECEIVED: December 1987
Pierce, Geocanex Ltd.
PROJECT: Eye Lake'
Oz. Gold
Trace -0.014-TraceTrace -Trace-Trace *0.002*Trace*Trace -Trace- Trace-Trace-Trace-Trace-Trace-Trace .0.012-Trace-0.016v0.002* 0.024'Trace-Trace*Trace'0.002*Trace'Trace ' Trace *
ed
IN ^•tCCOnDAMCf WITH I.ONG-tSTARLISHrD NORTH*M||ICAN CUSTOM. UNLES? (T IS iPfCIMCALLY STATEDOTHtfiVVISE GOLD AND btLVfft VAL Utb REMOftftD ONT Mf SE t M f C T S HA^L' NOT li LIN APJUSH.D TO COMf't N-
ATE f OR LOSSES AND OAiNb INMtNtNT IN T H t FINE•j AS&Ar PNOCC&S.
BELL-WHITE ANALY LABORATORIES LTD.
1 111l11111111111111
t
OU.h;,;..
Receive-:
Submituv i. 1,
Pro j ect :
Sample No.
12450
12451
12452
12453
12454
12455
12456
12457
12458
12459
12460
12461
12462
12463
12464
12465
12466
12467
12468
12469
l/
GEO-77/
Geocane
EYE LAKE
Auoz/ton
.001-
.001'
^001.
.001 .
.001 -<.001 .
.002 '
.002 '
.002 '
.001 '
.001-
.002,
.001'
.001'
.001-
.002-
.002-
.001-
.001-
.oor
7262
x Ltd.
Sample No.
12470
12471
12472
12473
12474
12475
12476
12477
12478
12479
12480
12481
12482
12483
12484
12485
12486
12487
12488
12489
69
Auoz/ton
.002 -
.002'
.001'
.001'
.001 ,
^001 t
.001 '
.002'
^001 .
.001,
.001 .
^001-<.001 .
.001 '
.001'
.001'
.001'
.001'
.oor
.001'
Sample No.
12490
12491
12492
12493
12494
12495
12496
12497
12498
12499
12500
12501
12502
12503
12504
12505
12506
12507
12508
12509
j
J . va,n
,,,,,,3^,
December 31, 1987
Drill Core
Att'n: Mr. H. J. Hoclgec. c. Mr. J. Adams
Au Auoz/ton Sample No. oz/ton
^001, 12510 .001-
.001' 12511 .001-
.001' 12512 ^001-
.001' 12513 .002'
^001' 12514 .001-
.002' 12515 ^OOr
.001- 12516 .oor
.002' 12517 *:.001-
.001- 12518 .001'
.001-
.002-
.001',
.001-
.001.<.001''
.002'
<.001 '
..001")
\QQ1'.002-•1
I^-Jt t <^f^.^f^'^J} L- JKii 1 f. l i
s'
' ' l !
Engelen Mgr.
•^ ^EHRfcSENFATION
f1i:
S*
ItiflCiili: i .
O(;K- :.
M GubmiMu-i i ,
Pro i e c t :
Sa
1
1
1
1
1
1
1
1
1
1
1
11
mp le No
12401
12402
12403
12404
124051240612407
1240812409
1241012411
12412
12413
12414
12415
1241612417
12418
1241912420
ASS; ; ,:nc;n/.
GEO-76/02
Geoc ane x
EYE LAKE
Au oz 1 1 on
.002-
.002-
.002.
.003.
.001 *
.002-
.002-
.001-
.001'
.001 '
.002 '
.001 ,
.001-
.001 '
.003 -
.004 '
.001 -
.004 '
.001 '
.007'
X7262
109
Ltd.
Sample No.
12421
12422
12423
12424
124251242612427
12428
12429
12430
12431
12432
12433
12434
12435
1243612437
12438 12439
12440
;. , u;j:M9-35?/
December 31, 1987
Drill Core . ... . ...... _ ..., _ ....
Att 'n: Mr. H....J. Hodgec . c . Mr . J . Adams
Au oz/ton Sample No. Au oz/ton
.002 - 12441 .003 -
.001- 12442 .003-
.001- 12443 .003'
.001- 12444 .001'
.001- 12445 .001*
.001 - 12446 .001 -
.001 - 12447 .001 "
.002 ' 12448 <.001 '
.001 ' 12449 .002 '<.001 /
•C. 001 '
.001'.
.002-
.001'
.001'
.001-
.001-
.002- ^^
.002- --^ f
.002 .
1 7 S yi^.M^y^lTED S
t'— 1 i
J . va'n Erfge len Mgr .: v HfPMtSENTATION
1 1 11111111111111111
Certificate No
Received
Submition ir,-
Project :
Sample No
12341
12342
12343
12344
12345
1234612347
12348
12349
12350
12351
12352
12353
12354
12355
1235612357
12358
12359
12360
x/
GEO-76/01 77262
Geocanex Ltd.
EYE LAKE
Au oz/ton
.002.
.002 -
.002-
. .002-
.003 -
.002-
.003 '
.002'
.003-
.003-
.004 -
.003-
.003-
.003-
.002-
.003-
.002 .
.003-
.004 .
.003'
109
Sample No .
12361
12362
12363
12364
12365
123661236712368
12369
12370
12371
12372
12373
12374
12375
1237612377
12378
12379
12380
- '!
Au oz/ton
.001 v
.002,
.002'
.004-
.002-
.003.
.001 -
.002 .
.004-
.004 '
.003-
.003.
.002- ;
.002-
.001-
.002'
.002.
.002-
.002-
.002'
J . van
•it (116)239-3527
Decembe
Drill Core
Att 'n: Mr. c .c . Mr.
Sample No
12381
12382
12383
12384
12385
123861238712388
123891239012391
12392
12393
1239412395
1239612397jU*98"~~
^'"""' 1239?
12400x-;/' s'•^7*
s
Enge l en Mgr
r 31, 1987
H. J. HodgeJ . Adams
Au oz/ton
.002-
.001 '
.002 *
.002*
.001.
.001-
.003-
.003'
.001'
.002'
.002 '
.002 .
.002'
iOOL
^002-
.003'
.001 -~) .002'
.001'
.001-
s
m
i Hi ^HfSFNIATION
EYE LAKE - LIST OF CLAIMS
Pa 769379 778970 778972786837786838786839786840786842786844786845786846786847786848786850786851786852786853786854786855786856786857786863786864786865786866786867786868786869786871786872786873
Credi
MP
^
ts Requested
60 Pa606060606060606090906060606060
100120606060606060606060606060
115
,^^^5/yX^\^- ^-V0\ f*As*. \^^*\ N j\flSfk^i1 fiV- 1 ' '~N ^* Mi Vk' o;-' vK f- A \"n^7 tf/vx ^-Vvv Vv-, ^" v -7
964911964912964913964914964915964916964917964918964919964920964921964922964923964924964925964926964927964928964929964930964931964932964933
(l*
Totalw
Credits Requested
202020 ,2020202020202020202020202020202020202020
x^EB*\f g? x^/^N/ \^i i j^ ^' \|^^.E 5/vv^— v/x^r^x
Total: 54 Claims
,--.KTp- Credits: 2,^35 :i:Jj^X -••"" -
/. ,'71:' .
i -
P ol 726BC8 l
Pol 7?C - 067ll - i ;-'"'-'.
•n/'.. lykarr. j^, l ^ O j ^0 7;,,r, l
P"
S
l""V""tpT-
J\
l \ i l
. Pa ,: Pa '76'9435 769446 ' Po ' j p 0 l i' 1*18/6707 '48C
] l/ l
v (466709 1486710 PO ? , i
(Pa 406719
©i-i .-" |Po -^~J...™- - T-Vt.i,O9?,OiCbO9a-* i Pa'•••lt: 'iO(.Mtt loogire e:.09J?
e -f] [ ,^,rt j**};**' j /".l*. l;
4---v---1..-^. j.;__i--.-..J'-^ .j /' ^ i\*W '83059? '^ ^30590 , 7 :61 43G | 7a69445 'lP?^f^;.f6 |pr--
I 'j . l l' l V769/447! t. I 1 486720
M ei l
|Po Po9" .'80? BO ?96I 1802960 l','
962
•T,::-.~-
Pq-
.'802959,
•X ',830529 1771440 1-771/1,0 'Po\ l pa l Po \)pa l Pa - ' Pa\1 'j 1771439 1 77\437 j 769437 l 769444 ) | 7 g9 ,,,, 8 . 769^455 J 76945 7; v^xj- - -\ ~ — — - . l i i i /i ; i
c l Po Xri l Po? 1830534^(1^77144
Po
.p.—t—-'—i--J1 830576] f
M N B;L4. L- (J ^\\(P rO v[4 r-)C
*Vi G } f" fy w
--l; ..J--." J77I44I \77l438lpa |(7aX l pa
\ j l 769438/1" 7 ''f'69443 ]7C9449 176 9454 1769458
L|77I443 77 |444 \ 77i^ Po ,| p a ,pa | ./pa |
. , l 7694 -1769442 7694501 769453 iPol \ l -3V l ' j |t69
.p~o ~lfa""""~-rP7n—Li----I---u-—.j/^1830587 ,830r,86 l 7 7i4|Pa ' l Po P Q l P" '' l Po l ^ ^^]769440| 7G944I | 769451 769,'452
^ S /'
•-recttfo '
iPo830^- 589
'-H^"^-!-- •r1
— l—Pa
ftSOete l 86O6+0 l 6&O6+4 l 8-5661-3 | 86
~~l Pa
-:'.' Po \
l2l 8650'64 ^
Lf'ff 0 'i —^-"iL jj^0^ —— —— —— — —— --—— —c —— —— —— —, - . ., .
__V-— V-^l"' 4,3.1 i L,.^ l^^l^ee^^-^we-l^ l , .^ l—— H-— -- — —l— — —l— —— — —-i.—j-—|Po
" ; ft 4,so) f( Mzy ^(^^^^^11^1^1.1 l±-L*4 If -J J
8508 .-49 l ' '
* 4650...-: l l.
r^jjrt70 IT^JI.' ^^j r^^iwy | 850857 l
850853 1/850850 |
---^1 __ ____ l Po \ (Po j 850852 '^ j B5085I *~'903^ X 19.-T53526|90352 ;.7
y"525 j \ * \
786857^1786856 . j 766655;
--X----^--J-^-----t---'""V0 7 '^4V47I
pa .7/86852 l 786
i CB rio;; \ ^—— :-K——T^."" "" TP"? ~~.S~ — ~ 769379 786848 |786847 | 78684'6
787357/78734.^B Jc
U--J—-____^'Po |Po i pa if '776219 , 785840 J 786839 X
f7G?\7!\ (765069 I78f,860
i ^.. ~. ^., ~.. .., ^., ^.j . \ ,, _ ^, -L- ^ , t i, ,: . [ . ... ....,. ... .,. ...^' ..-rk""" |Pf' IPO " " i \"F; O~" "" TP'C "' "" ]po"y i pa IPO j
r ..--V.|y-\ y ly-,4 -5V j 7874.10 | 78YiV-8 l \7Ht87l l 78611/2 /j/tiStt/Ti 769?0-l | W.iSf'l. j
: i'-". ; .i (N {K'-'"^ r'" ' i"-- .....! ! N ! /'""''^./' l ! .'i
Onlatio
Minist.yol RcportS'BoCUMENT No.Natural f iMn JLnesources T V'v'880^' III
Name and Postal Address of Recorded Holder
Explorations Inc.BsoasNEeeae 39 DONA LAKE
.__________S l1003-34 King Street East, Toronto, Ontario, M5C 1E5
Summary of Work Performance and Distribution of CreditsTotal Work Days Cr. claimed
3,093nlng Claim
Number
for Performance of the following work. (Chock one only)
Q) Manual Work
[]^]shalt Sinking Drifting or other Lateral Work.
| | Compressed Air, other Powor driven or mechanical equip.
Q Power Stripping
r~) Diamond or other Core drilling
| |Land Survey
ttached She(
HIO OEOtOGlCAl SSE5SMENT--T
E-G-E-4-V
Work Days Cr.
SURVEY IttS
P D
Mining ClaimPrefix Number Days Cr.
Mining ClelmPrefix Number
Work Days Cr.
All the work was performed on Mining Clai U 786856, 786855, 8508.4, 8508"55, 850846, 786864, 786869, M -786868_____:___________________'___'
Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below)^ "* \ t '~ - ~~"
Drilling Contractor: Midwest Drilling, Winnipeg, Manitoba -"'-.'O- -' 7
Core Size: BQ 1-7/16" ^ , 7Ci -jp*^ 't*~- V l ^Zrr
Number of Holes: Nine (9)
Footage: 3,093 *ttf*~ \tf/
Geologist in Chfarge: Robert I. Fogal, 1543 Marentette AvenueXFlrtdspr;, On
Dates: November 23, 1987 tj/^et^i^er/^fi,, 1987
Certification Verifying Report of Work \j\'.
89o*-t" ~ 263^
4E4
^Sx.Date of Report Recorded Holder or/\gent (Signeture)
4——————————————x: 1 i ' -ii \uy^————————————————1|-;——vi——l hereby certify that l have a personal and IntlmateicoQy'*^'8 Ojf^H'^'acti let forth In the Report of Work annexed hereto, having performed-*he work or witnessed same during and/or after It* completion and the annexed report l* true.
Nnrne and Postal Addiesf o( Person Certifying
II.J. Hodge, 1003-3A King Street East, Toronto, Ontario, M5C 1E5Date Certified
Table of Information/Attachments Required by the Mining Recorder
Typo of Work
Manual Work
Shaft Sinking, Drifting or other Lateral Work
Compressed air, other powor driven or mechanical equip.
Power Stripping
Diamond or other coredrilling
Lnrirl Survey
Specific Information per type
Nil
Type of equipment
Type of equipment and amount expended. Note: Proof of actual cost must be submitted within 30 days of recording.
Siflned core log showing; foolngo, diameter of core, number and angles of holes.
Namo and address of Ontario land surveyor.
Other Information (Common to 2 or more types)
Names and addresses of men who performed manual work/operated equipment, together with dates and houri of employment.
Names and addresses of owner or operator together with dates when drilling/strippingdone.
Nil
—— — VjAttachments
Work Sketch: those ere required to show the location and extent of work In relation to the nearest claim post.
Work Sketch (as above) in duplicate
Nil
7GH (HI '31
LEGEND
Surface projection of d lomond drill ho'e ..
Go'd in OZ/ ton —...
In *ervo ! in feet ——O 053-0
8, f- ig No. o' Section dr
DRILL HOLES ! TO 9 PRE^'XED EL-87-
O IOOO li ill-
20OO 3000
LOO
L 20S
L32S
UJ
-iUJCO
OD
LU t\J CM
POWER EXPLORATIONS INC.
EYE LAKE PROPERTY Patricia M.D., Ontario
PLAN OF DRILLING 1987
GEOCANEX LTD TORONTO. CANADA
DATE: JAN. 88 SCALE: I/I2000FIG. No: 4
AFRI PROJECT
HOLD QAFO#:
AFRI #:
ITEM:
uufc {PT
///r/
Y L o( l- (f c /C(2 c
Date: JrT. c Indexer: { ),., ( Supervisor: /'
RESOLVE
Date: Authorized by:
90 0 lb 40' OO
r w
Mccullagh Twp i
_ _ — J
Komar Property
Dona Lake Discovery
PROPERTY LOCATION
LU UJ UJ
Alders,
cedars ,
* T
Black spruce,
muskeg\\\
Open spruce, muskeg
- X
96491 5
Black spruce,
muskeg
\
X"
V
muskeg t ' X l boulders on )
y | sand S\ Spruce on Y. -l ysand boulder'
7
^X ^
) ^^^
Spruce, muskeg,
f boulders on
sand
7
x
"JMU UVAJIUCI i
Xridge l 1
}X 96 49l9x-
xx
l:\ J ^*
Spruce, muskeg
\
l
/ Open spruce, ,
l muskeg
jfc-
7l Spruce i birch '
, on sand \
Spruce,
muskegs
X/
X l A
x/
Open spruce,
muskeg
l
l \964932\
/ Spruce,muskeg r7 on sand and j" S
7 hnnlHpi-c ' \/
Spruce - cedarf' j a|ders,swamP
Spruce,muskeg on sand and boulders
96 4927
/\ Cedars* spruce
Open spruce, - muskeg -
64925
Spruce,! cedar, t alder swamp
•it
\
Spruce, poplar,
l-f
Open spruce
muskeg
\ cedarsl/
X\- 7
\ Spruce, muskeg and boulders
\ on sand
\ }
\ 4^r t ~ ^r \ *9 64924 c^ \ Spruce, muskeg,
X
Spruce, muskeg
\ Spruce, muskeg
Open spruce, ;
muskeg ; 9 6 4 9 l 2
-7-Spruce, muskeg
Mature spruce, poplar
on sand-gravel
77
y ^j Boulder - L 'sanj '"—' X
v sand ridge'
X"" W/ l ^ ~ Spruce - alder
Open spruce, muskeg
964918
7Xedar-alderX
tamarack \swamp \
X ja Spruce, \ .it \ muskeg. f. ^x
\- X* -~^ \ ^\ .,,
9649IIy Open spruce,tamarack,
/' swamp
Spruce,
muskeg
4917
l Cedar
/-tfe-
.SMomp \_i^, •~^^*\
\
Spruce, muskeg
Cedar-alder-spruce ^ swamp
\Boulder , \ sand \
\ \ hl"
X. x^
\
\ *A
. 964916 J^ :vh /\. Ooen grassy boaV. J ^V?*- "'.Q\
-^*-.^-^7l\*fX \
^ fe /: —-—"—-^ j i jt ,y~b ^
Spruce, muskeg
\
V *. x
7
l xcedars l
———f
//
96 4^933 Vi
muskeg 7-9-6 4930 /
s *- Open spruce,tamarack, /muskeg *
/
y Itf-
Spruce and birchover sand a boulders
/9 6 4 9 2 6
//
Spruce, muskeg on sand
//
850846
Spruce,muskeg on sand
Open spruce, lmuskeg
A
z.
Sandhill
~-Cedar-alder- -^
.32 spruce swamp i-
1203-
y
/
96492/2l /Cedar-spruce, j s tamarack
9649211 Sand-boulder
^ ridge
3d,4c
Spruce, muskeg
-———^^-^^--^-I204-5 /,-.^a ^
•J Sand hill
/3a^l207-IO
V * "-^ jt 7 Kx Spruce-tamarack, ^-^/^ X
, ^\ swamp _^^^U1 ^x Y ~^-u—^ -^ .. v - - -v * -
Cedar-alder \ X^ \ X
jfct
Spruce, muskeg
/
\
1209-10 s X
\ - spruce^ \ ^ ^i\ swamp )
\
JU- X
y it \
Spruce, muskeg
LEGEND
QUATERNARY
Stream, lake , bog deposits Glacial, glaciofluvial lacustrine sediments
LATE PRECAMBRIAN (Keeweenawan?)
Ma Diabase
EARLY PRECAMBRIAN
Intermediate and Felsic IntrusivesI0a Granite pegmatitelOb AplitelOc Granite
kgMMM
10* Ouorti monmite(Of GranodioritelOg TrondjemitelOh Quartz dioriteIOJ Diorite10k Unsubdivided gneiss10 l Granite gneiss
Mafic Intrusives9a Unsubdivided9b Gabbro9c Leucogabbro9d Plagioclase-phyric gabbro9e Peridotite9f Pyroxenite
Iron Formation8a Oxide facies8b Carbonate facies8c Silicate facies8d Sulphide facies
POWER EXPLORATIONS INC.
KOMAR PROPERTY Dona Lake Area
Patricia M.D., Ontario
GEOLOGY
GEOCANEX LTD
BY- RTMDATE: July 1987SCALE-
WG. No: 2
Chemical Metosediments7a Chert7b Calcitic marble7c Dolomitic marble
Clastic Metasediments6a Clast supported conglomerate6 b Matrix supported conglomerate6c Oligomictic conglomerate6d Polymictic conglomerate6e Sandstone, unsubdivided6f Wacke6g Arenite6h Mudstone, argillite6] P*W***t*ic wacke6k Feldspathic arenite61 Quartz arenite6m Schistose rock ± amphibole,! biotite,
± garnet, ± chlorite of probablesedimentary origin
Felsic and Intermediate Subvolcanic Rocks5a Unsubdivided5 b Quartz-feldspar porphyry5c Quartz porphyry5d Feldspar porphyry
Felsic Metavolcanics '
4a Massive f me-medium grained flow4b Pyroclastic breccia, tuff breccia4c Tuff, lapilli tuff
Intermediate Metavolcanics3a Massive f me-medium grained flow3b Flow breccia3c Pyroclastic breccia, tuff breccia3d Tuff , lapilli tuff
Mafic Metavolcanics2a Massive fine-medium grained flow2b Amygdaloidal flow2c Variolitic flow2d Pillowed f low, pillow breccia2e Flow breccia2f Medium-coarse groined flow centres2g Plagioclase- phyric flow2h Amphibolite2i Co-magmatic sills, dikes2j Pyroclastic breccia, tuff breccia2k Tuff, lapilli tuff21 Chorite ± amphibole schist
Ultramafic Metavolcanicsla Massive fine-medium grained flowIb Spinifex textured flowle Talc-carbonate
± magnetite ± amphibole ± serpentine i chlorite schist
SYMBOLS
ShorelineCreek, showing flow
Swamp
Beaver Dam
Break in slope
Claim post, line,witness post
Township line
Trench, pit
Diamond drill hole
Highway, bush road
Power transmission line
Outcrop, outcrop area .Geological boundary , observed,
y 2a..... \.--2a' ^r'""r'^ r...
x x x
IT ^50857Open spruce,
tamarack
\ x y '" 2ax
Jqv -.2d' -1212-90 "' :(l
x field y850856
\ ^\ Spruce,
2d y tamarack,- O
2a,
y
yyy X ^
\ Cedar - spruce j ^ \ tamarack ' Spruce, \ s*amp j muskeg \ ^ ^ ;
\/- - . \ ^±
'3a-
\
xX
X
Mature spruce foresti ^
.y y
x :y
y Spruce, muskeg
Spruce forest
\ XX"
50855\
Sand hill7 y
X xa
Open spruce, muskeg
-/-^^ X^ ^ Cedar, alder, ^
* s P ruce . s^mP 903528J&L JL M.
X x— . . . . n. , . . . i . . .Vjt \ X
K — T"
Spruce, muskeg n~ — - -^ ' hill )
X X
xX
-r-4L
1213-95.1214-IO-1215- 5'
V..2a
I236-5-2d^-^2d \ Boulders
x^o1*,*,.*- z'qv
y -f-' 2d
Inferred, inferred from geophysics.^- ———G—G
Surficial feature boundary..... ..--———----'
Rock sample location S number . . •I750IAssay for Au(ppb), Ag(ppm) -I3-0-6
Pillow;tops known, unknown ... -du -Q- Bedding ; inclined, vertical Hj— .4-.Foliation, cleavage;
60 vX .x XInclined, vertical, unknown r r r
Gneissosity, incl , vert, unknown. f ( t
Lineation , plunge ———^ 7060^ ^
Fracture, inclined , vertical . . ..
Shear zone , dip .. ~^
Shear fracture; inclined,vertical. c
Fault zone, dextral, sinistral ^ Anticline , syncline, plunge . -i- — -L.
Drag folds with plunge /7 6
Dyke ; width , dip 2
Vein, width,dip, quartz, carbonate Glacial striae
ABBREVIATIONS
t^-1216-TD" -I2l7-t5
2dWf*
2d
XX
x
-J—^
x^
x
x x x Spruce,poplar on boulders
X
50 4CaX
x
^
7
-/.
X
\Sand ^, h,ll f \
jskL
850849
Cedar,alder swamp ^ /
Spruce , muskeg, /
Open spruce,tamarack J*--Jfc. 4.
x tamarack7. I di. A
bpruce l ,forest '
muskeg/\ Spruce, t
i muskeg
^y
^
t
77
XX N
xmuskeg
, ^ jt/Open spruce/j S Cedar 7 muskeg \/* *' * i
X*x' Open spruce, '*~ swamp y | -j
^
60
i9a qv.cv
Spruce, poplar, i birch X
Silicification SIL, silSericitization..... SER.serCarbonatization CAR,carChloritization . CHL, chl
X l strong weak
Pyrite pyPyrrhotite poChalcopyrite cpArsenopyrite aspSphalerite. sphGalena gaBornite brMalachite malGraphite grChrysocolla chry
MagnetiteLimoniteHematiteMolybdeniteGruneriteSideriteDolomiteAnkeriteGarnetEpidoteTourmalineXenolithMyloniteShearingCarbonatized
\ \
,4\Alder \ swamp'
l ' l ^ /'
903526± S
/
MX S yy
. 7
.felder y7V *i '
S tr* Zy /
xy7
x x
x x x x
Cedar * ^
jTTAAOpen spruce,
muskeg |7
' 2a,ia
^2a .-it 2d
l228-<5s .1229-5:
2d /.- \2a.v ^. 3Qy.::: M
muskeg on 0 - ^sandhill t SprUC6 ' \
^50 8 5 4)- tamarack. ^/t muskeg ,
. . r . . !
7 Open spruce, i ^^ -^ . , ra.-A"^ tamarack, y
.muskeg X
xx 8 508|53X Spruce,muskeg L
X on sandhill
^
Xx x
^Open spruce,
tamarack
/"
-A
\
l
Spruce, muskeg Marsh
X J
850850
1220^5
Open spruce, tamarack y
7d*- /Spruce,
y muskeg
\Spruce, tamarack,
\\
1231-5-0 41232-10
\
Spruce , muskeg
— ' —— r -——
\
\
Open spruce, tamarack,muskeg
^^^i
7j _ A.
/
/' 4fc— -A- — —— ~x
———————————— —— . —— ——
—— y ~^^k7 '^^^Ceddr
/
Spruce, 3a muskeg
1222-25'——'1223-6301224-15
2 1225-100
1230-5 I234-K5
i/ , . 7. i
y 77 Spruce,
muskeg
77 75
XX ^
^A S
x 7
X7 muskeg \ /Mature f
f y spruce 7
850851 yX
7
7
Spruce, muskeg
x -^jL.X
A- / Xy
/./
~^ ^. y
cc :'-;. 2a,po
Grassy tamarack, ^~ marsh ^
00
2d,
1000
FEET
Floating l bog l
39 DONA LAKE 20(3
80 N
76 N
72 N
68 N
64 N
60 N
56 N
52 N
48 N
44 N
40 N
36 N
32 N
28 N
24 N
20 N
16 N
12 N
8N
4N
Ul
L. 8 S
L 12 S
L 16 S
L 20S
——— i--. — Tl
L 79 N
L 76 N
L 72 N
L 68 N
L64N ] r ~~-~J
L 60 N
L 56 N
L 52 N
L 48 N
L 44 N
— —-l — — -— —.f _ _ _ ***M , \ _ _ _ _ -ami*
. . ^ __ __ Tina l ~/ 7
——— ——— ——— ——. ___. 7M*U /
i__ t ^ i \~ '— —— — —— ivwn ——a— J—— —— —— —— ;__ __ __ __ nun J
LEGEND
O O
O O
Lafct thor* iff— — -*- _.Cruk — — —
Swamp t' ,
Claim lint -———"~ ——"
Claim post B
B* (ascumtd)
UJ Oo
39 DONA LAKE 210
VAN HOfWE QOLO EXPLORATION MG.
EYE LAKE GRID
GEOLOGY
OiOCAJCX LTD