010 DIAMOND DRILLING WORK PERFORMED FOR: H.J ......Pa 913289 to 913310 (inclusive) 22 March 27, 1987...

520865*0084 15 NAB8MAKOSEKA LAKE010

DIAMOND DRILLING

AREA: NABEMAKOSEKA LAKE REPORT NO: 15

WORK PERFORMED FOR: H.J. Hope

RECORDED HOLDER: Same as Above [xx]: Other f j

Claim No.

Pa 913300

Pa 913289

Hole No.

NB-89-5

NB-89-6 NB-89-7

Footage

347.0'

347.0'

330.0'

Date

Feb/89

Feb/89 Feb/89

Note

(D

(D (D

NOTES: (1) W8903-107, date filed June/89

11 i11111111111111111

^^FEOtnNEH m.'"

1 Oi^;;'; f -'oT^wT^kT] f AOOL-.SSMENT RLFS l l OFFICE: f

REPORT ,: ,, f

ON J JI 'N 16 1989

DIAMOND DRILLING L. R E C E 1 V E D f"*"*"'

NABEM LAKE PROPERTY

PATRICIA MINING DIVISION, DISTRICT OF KENORA

NORTHWESTERN ONTARIO

FOR

PANTHEON MINERALS LTD.

NTS 52 0/6 ,- ^^

f 9 i .^VV O, V\l '-f C^\ *s? fs V-\H ^\^ 3?^ V\ql ^ ^ bv4Vs?^jty ^^/^^

A P ri] ' 1989 E. D. Timoshenko, B. Se.

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520665*0884 15 NABEMAKOSEKA LAKE 010C

TABLE OF CONTENTS

Page

l. O SUMMARY l

2.0 INTRODUCTION 3

3.0 PROPERTY DESCRIPTION 3

4.0 LOCATION, ACCESS AND SERVICES 6

5.0 PHYSIOGRAPHY AND VEGETATION 7

6.0 PREVIOUS WORK 7

7.0 REGIONAL GEOLOGY AND ECONOMIC MINERALIZATION 9

7.1 Regional Geology 9

7.2 Economic Mineralization 12

8.0 PROPERTY GEOLOGY 14

8.1 General Geology 14

8.2 Rock Types 16

9.0 SUMMARY OF GEOPHYSICS 19

10.0 DESCRIPTION OF PROGRAM 20

10.1 Description of Program 20

10.2 Discussion of Results 21

11.0 CONCLUSIONS 25

12.0 RECOMMENDATIONS 26

13.0 ESTIMATED COST OF RECOMMENDED PROGRAM 28

14.0 REFERENCES 29

APPENDICES

A CERTIFICATE OF QUALIFICATION Back of Report

B PLAN OF DRILLING AND DIAMOND DRILL LOGS " " "

C LEGEND AND DIAMOND DRILL SECTIONS " " "

D ASSAY CERTIFICATES " " "

l l I ll l l l l l l l l l l l l l l

LIST OF TABLES

I SUMMARY OF DIAMOND DRILLING RESULTS

LIST OF FIGURES

1 LOCATION MAP

2 CLAIM SKETCH

3 PROPERTY LOCATION AND REGIONAL GEOLOGY

4 PLAN OF DRILLING

5 LEGEND TO ACCOMPANY DRILL SECTIONS

6 DDK NB-89-1, 2 Section 32+OOW

7 DDK NB-89-3, 4 Section 60+OOW

8 DDK NB-89-5 Section 56+OOE

9 DDH NB-89-6, 7 Section 48+OOE

page

23

Page

4

5

10

APPENDIX B

APPENDIX C

APPENDIX C

APPENDIX C

APPENDIX C

APPENDIX C


l. O SUMMARY

A diamond drilling program consisting of seven holes

totalling 2,222 feet was carried out on the Nabem Lake

property for Pantheon Minerals Ltd. between January 27th

and February 14th, 1989.

The property consists of 48 contiguous mining claims located

in the Meen-Dempster Greenstone Belt, approximately 48 miles

west of pickle Lake, Ontario, and seven miles west of the

Golden patricia Mine of Bond Gold Canada Inc.

The claim group straddles the contact between granitic rocks

of the Obaskaka Lake pluton to the south and interbedded

mafic to intermediate volcanics with clastic and chemical

sediments {of the Dempster Lake Cycle?) to the north. A

small mafic to ultramafic stock intrudes volcanic rocks in

the southwest corner of the property.

Diamond drilling was concentrated in the north property area

on a sequence of mainly volcanic rocks which are on strike

with gold mineralization discovered on the adjacent Dobie

River property of the Power Explorations Inc./North American

Rare Metals joint venture. No economic gold values were

obtained during the present program, although one geo-

chemically anomalous, sheared and silicified zone approx

imately 70 feet wide was intersected in hole NB-89-2.

Future exploration work on the property is recommended,

consisting of geologic mapping and lithogeochemical

sampling, limited geophysical surveys (magnetometer, VLF-EM,

and induced polarization/resistivity), and 2,500 feet of

diamond drilling. Diamond drilling should concentrate on

three main areas:

l l *

( i) the volcanic-sedimentary sequence in the north

l property area, tested partially in the present

program

' ( ii) volcanics along the granite-greenstone contact

g the central property area, and

(iii) the mafic to ultramafic intrusive in the south-

I west corner of the property.

l The total estimated cost of the recommended exploration program

is $159,540.00.

l

l

l

l

l

l

l

l

l

l

l

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2.0 INTRODUCTION

This report describes the results of a diamond drilling

program carried out on the Nabem Lake property.

The property consists of 48 mining claims located 48 miles

west of the town of pickle Lake {Fig. No. 1) in the Patricia

Mining Division, District of Kenora, Northwestern Ontario.

The present program was supervised by Geocanex Ltd. and drilling was contracted to N. Morissette Canada Inc. of

Haileybury, Ontario.

All drill hole sites were located on a cut picket line grid

with an east-southeast trending baseline and perpendicular

lines cut at 400-foot intervals across the strike of the

local stratigraphy.

The personnel involved in the program were:

E. Timoshenko Project Geologist Brampton, OntarioM. Reitsma Core Splitter Brantford, OntarioD. Lorente Core Splitter Renfrew, Ontario

All drill logs, sections and assays are included in this

report. The program ran continuously from January 27th to

February 14th, 1989.

3.0 PROPERTY DESCRIPTION

The Nabem Lake property consists of 48 contiguous unpatented

mining claims, located in the patricia Mining Division,

District of Kenora (Fig. No. 2). The claims are shown on

the Ministry of Natural Resources claim sheets G-2135,

Nabemakoseka Lake, and G-2122, Meen Lake.

PROPERTYO N T A R

KENORA

^ ^v'o fc*t X*"""'' i? c-~-C~'" TIMMINS

UNITED

STATES

KIRKLAND fv LAKE.

~'-" Greenstone Belts

O t

lOOmilssrrd


NABEM LAKE PROPERTY Patricia M.D., Ontario

LOCATION MAP

SCALE: l"' lOOmTDATE: April.'89

BY! H.H./H.T.M FIG. NO. 1

l lili

l l l lll l ll

l ll l ljll i

-5-

9I 0 I5'

913319 l 913324 913329 913334 - — — 4- — — 4 —— ——— - — ^

913320 ' 9)3329 ' 913330 ' 913338.T--4-——4-

1 s-s^.4- 913321 ' 913326' 913331 l 91333*-——l-——4-T-4——

9 l 3 32'' MS SZrS 33 Z ^l 3 32' M u .

53S 91333* l 913298 ' 9^329?' 9132961^1329^19^94 ———L—— —^ — —.4-^—-)- -f.-— -f — —

5I 0 22'30"

. . i i -x ^9133391 913342 ! 913343 l 9I3S03 l 913302 l 913301 l 9I3300 1 9IS29ff\L9l3309-..4-... H — --t-T— f —— + --N- —— -t-u

^9l334ol 913341 9133441 913308 l 9IS30rT9l3306| 913305^913304 l 9IS3IO

l j ______ l^ ____ i _______ l—t ______ ±^\ ________ J ___ —i^^-.

NABEMAKOSEKA

LAKE

O 0-5b~~rr—rrt^^a:

c..


NABEM LAKE PROPERTYPatricia M.D., Ontario

CLAIM SKETCH

HIOEOCANEX LTD

TORONTO. CANADA

BY R.T.M. — DATE April 1989SCALEJ s2640' TIG. Norg


-6-

Claim details are listed below:

Claim Numbers Recording Date

Pa 913289 to 913310 (inclusive) 22 March 27, 1987 Pa 913319 to 913344 ( " ) 2JL " "

48 claims

The claims are held by H.J. Hodge Inc. of Toronto, Ontario

under an option agreement with pantheon Minerals Ltd.

4.0 LOCATION, ACCESS AND SERVICES

The property is located in Northwestern Ontario (latitude

51 0 21'N, longitude 91 0 17'W) approximately 48 miles west of

Pickle Lake and 170 miles north of Thunder Bay.

Access may be gained by way of ski or float-equipped

aircraft into Dorothy Lake, immediately west of the

property. A winter road running adjacent to a power line

from pickle Lake to the Golden patricia Mine of Bond Gold

Canada Inc. provides access to within seven miles of the

property.

Services, supplies, and manpower can be obtained in Pickle

Lake, a mining and transportation center of approximately

500 people.

Highway 599, a paved all-weather road, connects pickle Lake

to the Canadian National Railway line at Savant Lake, 90

miles to the south, and the Trans-Canada Highway at Ignace,

180 miles to the south.


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5.0 PHYSIOGRAPHY AND VEGETATION

The property is slightly hilly and covered mainly by black

spruce, with sparse stands of poplar and jackpine. Areas

close to lakes and along creeks are slightly boggy, with

alder and tamarack. Outcrop exposure is probably less than

2%, as suggested by O.G.S. published maps. Lakes cover

approximately 15* of the property area.

6.0 PREVIOUS WORK

In 1960, the Nabem Lake property was mapped as part of a

large scale reconnaissance program by the Geological Survey

of Canada (Emslie, 1960).

The property area was mapped again as part of a reconnais

sance survey by the Ontario Division of Mines (Sage et al.,

1975; Sage and Breaks, 1982).

In 1978, Cominco conducted a number of surveys in the area,

including the present Nabem Lake property. Exact survey

locations are not available on public file. Follow-up work

by Cominco in 1980 included a total field magnetic survey

and a horizontal loop electromagnetic survey. To test

conductive horizons, a drilling program was conducted with

two holes drilled in the south section of the adjacent Dobie

River property held by power Explorations Inc., North

American Rare Metals and Osisko Lake Mines (Power/NARM JV).

In 1982, the property area was again mapped by the Ontario

Geological Survey as part of a 1:15,840 scale reconnaissance

program (Stott and LaRocque, 1983). This program covered

only the northwesterly portion of the Nabem Lake property.


-8-

In 1986/ Geoterrex Ltd. completed an airborne magnetic and

electromagnetic survey over most of the Meen-Dempster Belt,

including the Nabem Lake property, on behalf of the Ontario

Geological Survey (Maps 80897, 80898; O.G.S., 1986).

In 1987, Geocanex Ltd. conducted a vertical field magnetom

eter survey and a VLF-EM survey over the adjacent Dobie

River property for the Power Explorations inc/North American

Rare Metals (NARM) joint venture (Gillick, 1988). This was

followed by a diamond drilling program totalling 9,645 feet (Burk 1988a) .

Further magnetometer and VLF-EM surveys, geologic mapping

and prospecting, and diamond drilling (5,145 feet) were

carried out on a detailed grid in the west-central part of

the Dobie River property during the summer of 1988 (Burk,

1988b).

Gold values on the Dobie River property were obtained from

three different zones within a small section of the metavolcanic sequence measuring approximately 2,400 feet long

by 700 feet wide. The highest value obtained was 0.219

ounces gold per ton over 5.0 feet in a drill hole which

intersected a 30 foot wide interval of sheared, brecciated

and silicified intermediate volcanics containing variable

amounts of pyrite (up to 201) and pyrrhotite (11 on

average). Subsequent drilling around this intersection

yielded negative results (Burk, 1988b). Two additional

gold-bearing zones (Zones I and li) yielded sporadic sub

economic gold values (up to 0.068 ounces per ton) from mafic to intermediate volcanics and intrusives that are locally

sheared and silicified (Burk, 1988b).

In July, 1988, Geocanex Ltd. completed a magnetometer and

VLF-EM survey over the Nabem Lake property (Hodge, 1988).

-9-

7.0 REGIONAL GEOLOGY AND ECONOMIC MINERALIZATION

7.1 Regional Geology

The property is situated on the western half of the Meen-

Dempster Greenstone Belt. The Belt consists of Archean

metavolcanic and metasedimentary rocks which form part of

the uchi Lake Subprovince in the Superior province of the

Canadian Shield. A number of pre-, syn- and post-tectonic

granitoid and gabbroic plutons intrude these supracrustal

rocks (Fig. No. 3).

The supracrustal rocks are formed from three complete vol

canic cycles, each of which comprises massive to pillowed

basalts capped by dacitic to locally rhyolitic pyroclastic

rocks. The three complete volcanic cycles (from the

youngest to oldest) are known as:

1. Bancroft Lake volcanic Cycle2. Dempster Lake Volcanic Cycle3. Meen-Jacknife Lakes volcanic Cycle

The Billet Lake Sedimentary Belt unconformably overlies the

adjacent volcanic cycles mentioned above and is located

along the southern margin of the Greenstone Belt. On a

regional scale, the rocks become younger to the south.

Metamorphic grade is greenschist facies for most of the

belt, grading to amphibolite facies near the margins of the

belt adjacent to batholiths.

The western half of the greenstone belt, between Meen Lake

and Graniteboss Lake, comprises the two oldest volcanic

cycles only. The Meen-jacknife Lake Cycle (the oldest

cycle) is dominated by tholeiitic basalts at its base with

90 0 30'

MINES, PASTPRODUCA Centre' PatriC'O Mo 'B Centra' Patricia No 2C fickle Crow No 'D Pickle Crow *^o 2*- Albanyc CrowshoreG UVEX Tlierry Mine

GOLD PRODUCTIOV1INE PROPERTY TONS OZ

Central Po'ncia ', 729,2*8 6;Pickle Crow 3,237, 572 l fl'

GEOLOGY LEGENDLOCATION MAP

Geoiogico' boundary

Diaoo

Wise poper 199, '98* 1 G (V a Wol'oce H

Wop 2218 , Co 1 Loke - Pickle Low Soge f ol , 1972

RED LAKE PATRICIA

l /-Golden Patricia Discovery\-L—.—— 860,000fons at O-SSoz/ton Au

Kawinogans LakeWright

Lake

Dempster

Hasaga200,000 tons o* O-'Soz/ton Au

LAKE ST. JOSEPHt ~—

Carpenter L.

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M1NES, PAST PRODUCERA ^en+ro' Po'riciO No '

8 Ceri'ro! PolriC'O NO 2

C Pickle Crow No '

D Pickle Crow Mo 2f AIDony River

c Crowsriore

G UVEX Tl,,erry Vine

Collishaw Lake

GOLD PRODUCTIONVINE PROPERTY TONS OZSGOLO OZ/TONCen'rol Po'ricio ' , ? 2 9, 2 4 8 621,806 0359Pickle Crow 3,237,572 1,446,214 0-44

^?

PONSFORD TWP

Dona Lake Discoveryl.4OO.OOOtons ot 0-24ozAon Au

Kawinogans Lake


NABEM LAKE PROPERTY

Patricia M.D., OntarioHasoga200,000 tons o* O-'Soz/ton Au PROPERTY LOCATION

AND REGIONAL GEOLOGYLAKE ST. JOSEPH

DATE: Aprtl 1989SCALE: l"r 4 m j

F l G. No: 3GEOCANEX LTD

TORONTO. CANADA


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stratigraphically continuous marker units of magnetite-

quartz iron formation. The top of the oldest cycle contains

intermediate to felsic pyroclastic rocks with interlayered

and overlying sulphide and oxide iron formations, graphitic

schists and clastic metasediments.

The Dempster Lake Cycle forms the overlying volcanic cycle.

Its base is marked by pillowed and massive basalts contain

ing iron carbonate amygdules. The top of the cycle contains

felsic to intermediate ash-flow tuffs. A thick sequence of

metawackes with minor interbeds of aluminous mudstone (the

Billet Lake Sedimentary Belt) unconformably overlies this

volcanic cycle.

A number of .early and late granitoid and gabbroic plutons

intrude the volcanic belt. Granitoid intrusions vary in age

from probable subvolcanic intrusions, such as a quartz

porphyry stock near Meen Lake, to syntectonic intrusions,

such as the large Dobie Lake Batholith that flanks the north

side of the belt. Late tectonic intrusions include the

Southern pluton and the Graniteboss Lake stock. Several of

the gabbroic masses intrude the volcanic rocks. Two of

these include the Kawashe Lake Gabbro and the Dempster Lake

Gabbro which discordantly intrude rocks of the Meen-jack-

nife Lake Cycle and the Dempster Lake Cycle.

Structurally, the belt forms a south-facing homocline

although there is evidence of tight isoclinal folding. Much

of the regional deformation, particularly in the western

half of the belt, is a result of the emplacement of the

Dobie Lake Batholith to the north. In the Meen lake area

only local folding occurs - a syncline on the southern part

of Meen Lake and tight folding along the southern margin of the belt. At present, regional stratigraphic correlations

of the metasedimentary and felsic to intermediate meta-


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volcanic rocks just north of the Southern pluton remain

problematical (Stott, 1984). These rocks strike southeast

ward into the Dorothy Lake area and onto the Nabem Lake

property, and were previously known as the Lower Meen Lake

Group (Stott and Larocque, 1983).

Major ductile deformation zones {shear zones) are known to

occur in places along both the north and south granite-

greenstone contact in the western half of the Meen-

Dempster Greenstone Belt. They display a dextral sense of

shear and vary in width from discrete mylonite zones to more

extensive zones up to several thousand feet wide (Stott and

Wilson, 1986) .

7.2 Economic Mineralization

Historically, gold production in the pickle Lake area has

come from stucturally controlled vein-type deposits or

sulphide replacement bodies in close proximity to, or

within, banded magnetite-chert (Algoman) 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

porphyry sills near the contact of mafic volcanics and iron

formation.

Placer Dome Inc. and Bond Gold Canada are developing new

mines in the pickle Lake area. The placer Dome Inc. Dona

Lake Mine has reported reserves of 754,000 tons of proven

l l l ll l l l l l l l l l l l ll l

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and probable ore grading 0.24 ounces gold per ton, and 1.17

million tons of possible ore grading 0.17 ounces per ton

(Northern Miner Magazine, 1989). Gold mineralization occurs

as sulphide replacement bodies within a band of highly

deformed oxide facies banded iron formation (Northern Miner,

1986). Production will commence in the second quarter of

1989 and gold output is expected to be in the 40,000 ounces

per year range.

Bond Gold Canada's Golden Patricia Mine has recently

commenced production and has proven and probable reserves of

405,000 tons grading 0.60 ounces per ton. It is expected to

produce 48,000 ounces of gold annually (First Quarter Report,

Bond International Gold, Inc., Sept. 30, 1988). The gold

mineralization 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,

1986) .

Recently, Bond Gold announced discovery of a gold zone two

miles northeast of the Nabem Lake property. This zone, the

Dobie River, is reported to have 360,000 tons grading 0.17

ounces per ton gold from preliminary drilling.

A gold discovery in the Pickle Lake area was announced by

joint venture partners Power Explorations inc. and Moss

Resources Ltd. on their Kasagimminis Lake property (Northern

Miner, April 18, 1988). The mineralized zone has geolog

ically inferred reserves of 2.9 million tons grading 0.14

ounces gold per ton.

On March 20, 1989, Goldhunter Explorations Inc., Pinetree

Explorations Ltd. and Caviar Resources Ltd. announced a new

gold discovery in the Wright Lake area, within the Meen-

Dempster Lakes Belt. The mineralized intersection assayed at

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0.66 ounces of gold per ton over 6.0 feet in a quartz vein

within a shear zone trending at a high angle to the regional

stratigraphic trend, at the contact between mafic meta-

volcanics and a quartz-feldspar porphyry (H.J. Hodge,

personal communication, March, 1989).

Ultramafic rocks host copper-nickel mineralization at the

Union Miniere (UMEX) Thierry Mine, seven miles northwest of

Pickle Lake, with mined ore and mineral reserves totalling

14,000,000 tons grading 1.6% copper and D.2% nickel.

8.0 PROPERTY GEOLOGY

8.l General Geology

The property has not been mapped or prospected in detail.

However, geophysical evidence and limited reconnaissance

scale mapping (l inch to 1/4 mile) by the Ontario Geological

Survey in 1982 (Stott and Larocque, 1983) suggests that the

property straddles the contact between mafic to intermediate

volcanics of the Dempster Lake Cycle to the north and the

Obaskaka Lake granitic pluton to the south.

A few small outcrops of pillowed mafic flows were mapped in

the northwest property area by the O.G.S. Facing directions

of the pillow tops were not obtained but tops generally face

south or southwest in the vicinity of the property.

Geological information from diamond drilling on the property

is limited almost exclusively to the northern sections where

six of seven holes in the present program were collared. Of

interest in this area is a sequence of supracrustal rocks

l l l l l l l l I l l l l l l l l l l

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striking east-southeast across the northwest and northeast

corners of the property. These are on strike with gold-

bearing units discovered on the intervening Dobie River

property of the Power/NARM joint venture (Burk, 1988 a,b).

The sequence is coincident with a broad magnetic high and

consists mainly of mafic to intermediate flows and tuffs and

minor felsic tuff, with interbedded clastic metasediments and

lean oxide facies iron formation. Intrusions of diorite,

hornblende gabbro and quartz-feldspar porphyry occur locally.

Geologic mapping along this sequence (Stott and Larocque,

1983; Burk, 1988 b) indicates that a strongly defined

foliation, F^, has overprinted primary igneous and sed

imentary features. Foliations generally trend between 100 0

and 120 0 azimuth and dip 60 to 80 0 to the north. Lineations,

LI, generally plunge about 50 0 toward the east-southeast

although locally they are highly variable, possibly due to

the effects of emplacement of the late to post-tectonic

Obaskaka Lake Pluton to the south. A secondary cleavage

locally overprints F-^ with an attitude of approximately OOO 0 ,

25 0 E. The sequence has been tested by drilling at various

points on both the Nabem and Dobie River properties over a

combined strike length of approximately 3.6 miles and a width

of roughly 2,000 feet. Several strongly foliated, silic

ified, and potassically altered zones were noted in several

holes along this trend and likely reflect shearing concordant

to lithologic trends.

Cherty tuffaceous horizons with massive to semi-massive

primary sulphide mineralization were also intersected

(eg. NB-89-07) and account for the strong VLF-EM conductors along the sequence.

The orientation and lithology of supracrustal rocks in the

vicinity of the Obaskaka Lake pluton on the Nabem Lake

property is uncertain. One hole (NB-89-05) drilled in the

vicinity of the granite/greenstone contact was cored entirely

in massive granodiorite. Magnetics suggest that there may be

l l ll l l l l l l l l l l l l l l l

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a minor reorientation of the supracrustal rocks along

east-northeasterly trends in the central property area

immediately north of the pluton.

The metamorphic grade of rocks intersected by drilling varies

from upper greenschist to lower amphibolite. Evidence for a

metamorphic aureole surrounding the Obaskaka Lake pluton has

been found on the adjacent Dobie River property(Burk, 1988 a)

and may extend across the Nabem property. Garnet content in

volcanic and sedimentary rocks appears to increase closer to

the pluton. An envelope of metasomatism extends for 50 to 60

feet from the pluton on the Dobie River property, manifested

by increased silicification and potassic alteration (Burk,

1988 a) .

8.2 Rock Types

The following is a description of rock types intersected by

drilling on the Nabem Lake property.

i) Metavolcanics.

Dark green to greyish-green mafic to intermediate flows and

tuffs were the dominant rock type intersected by drilling.

The flows are typically fine to medium grained, weakly

foliated assemblages of amphibole-plagioclase-biotite ^

quartz ± chlorite, volcanoclastic rocks, including ash-tuff,

lapilli-tuff, and rare tuff-breccia, are mostly intermediate

in composition, the typical assemblage being amphibole-plag-

ioclase-chlorite-quartz ± biotite ± alkali feldspar. Fine

grained mafic tuffs, composed mainly of amphibole and

chlorite, often contain 2-7% garnet porphyroblasts.

Tuffaceous rocks are typically strongly foliated with a

finely laminated or banded appearance. They are often grada-

tional into fine grained sedimentary rocks and typically have


-17-

a higher sulphide content than the flows. Small ovoid blebs

composed of carbonate, epidote and/or alkali feldspar occur rarely in volcanic units (eg. NB-89-07) and appear to be

amygdules, although they may be the result of deuteric

alteration (Stott and Larocque, 1983).

Ultramafic metavolcanics were only rarely intersected. They

consist of narrow intervals of actinolite-chlorite schist

with slickensided, carbonate- and serpentine-rich fracture

surfaces (eg. NB-89-02).

Felsic metavolcanics were not intersected in drill core.

However, several intersections were obtained along strike on

the adjacent Dobie River property (Burk, 1988 a) and it is

possible that thin lenses form locally on the Nabem Lake property.

ii) Clastic Metasediments.

In the north property area clastic metasediments form as

thin, discontinuous units (locally up to 40 feet wide) within

the metavolcanics. They consist mainly of greyish-brown to

greenish-brown wackes, composed mainly of quartz and feldspar

in a matrix of biotite and chlorite. These are usually fine

grained and finely laminated, and grade into finer grained sediments or tuffaceous volcanics.

Lesser amounts of dark grey mudstone, greyish-brown to

greenish cherty siltstone, and dark green pelite occur within

the metavolcanic sequence. Most of the sediments contain

small garnet porphyroblasts and minor disseminated sulphide

(pyrite and/or pyrrhotite).


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iii) Chemical Metasediments.

Chemical metasediments in the north property area form narrow

units usually less than 10 feet wide, interbedded with

clastic metasediments and mafic to intermediate tuffs. They vary in composition from cherty tuffs with disseminated

magnetite, to massive and magnetiferous chert, to well banded

oxide facies iron formation (chert-magnetite ^grunerite).

Magnetite and grunerite contents are generally quite low, in

the 2-101 range (locally up to 251). Sulphide content is

generally 1-3?;, consisting predominantly of pyrrhotite and

pyrite, and rarely chalcopyrite. There was very little evidence for folding in either the chemical or clastic

sediments in the north property area. Brittle deformation

appears to be more common as chert bands are often strongly

brecciated and carbonatized.

iv) Intrusive Rocks.

Much of the south property area is interpreted to be

underlain by the Obaskaka Lake pluton (Hodge, 1988). One

hole in the southwest property area (NB-89-05) intersected

the pluton and yielded medium to coarse grained, equigranular

granodiorite. The granodiorite contains up to 11 anhedral

magnetite grains which could account for the several isolated

magnetic highs (up to 600 gammas) in the south-central

property area. The magnetic highs could also possibly be due

to large xenoliths or rafted-off portions of the bordering

metavolcanic package. Numerous small mafic volcanic

xenoliths up to 4" wide were found in the drillcore.

Small pegmatite dykes up to 4" wide composed of glassy

quartz, white alkali feldspar and minor plagioclase with

accessory magnetite, tourmaline and pyrite occur within the

granodiorite. The pluton has a composition grading towards

quartz-monzonite on the adjacent Dobie River property (Burk,

1988 a).

lI t ll l l l l l l l l l l l l l l l

-19-

In the extreme northeast corner of the property, a drill hole (NB-89-06) intersected considerable amounts of

quartz-feldspar porphyry. The fine-grained felsic groundmass

has a medium grey colour and contains abundant small epidote

grains and up to 11 magnetite. There are typically S-15%

phenocrysts, consisting predominantly of buff white, pink and

yellowish alkali feldspar and minor clear to milky quartz.

On the southeast shore of Dorothy Lake, the O.G.S. examined

an outcrop of massive coarse-grained gabbroic anorthosite

which cuts mafic metavolcanics. These are in turn brecci

ated and cut by pink to red medium grained equigranular

granitic rock. From aeromagnetic data, a small mafic stock

of approximately l square mile in surface area is interpreted

to be present on the southeast corner of Dorothy Lake (Sage,

1982). Part of this magnetic anomaly covers the southwest

corner of the Nabem Lake property.

9.0 SUMMARY OF GEOPHYSICS

A vertical field magnetometer and VLF-EM survey was completed

on the property during June, 1988, and is described in detail

by Hodge (1988) .

The dominant east-southeasterly to southeast trends of the

supracrustal rocks in the north half of the property is

evident from the contoured magnetometer data. in the extreme northwest there are at least three subparallel bands of

higher magnetics which are caused by multiple horizons of

lean iron formation and/or magnetic sulphides within the

volcanic rocks. Two of these zones can be projected along

strike to the extreme northeast property area where readings

as high as 27,000 gammas reflect the presence of oxide facies iron formation. Strong VLF-EM conductors coincident with the


-20-

magnetic trends are likely caused by massive to semi-massive

sulphide horizons similar to those intersected on the

intervening Dobie River property (Burk, 1988 a). East-west

trending VLF-EM conductors in the northwest property area may

reflect sulphidized shear zones crosscutting the supracrustal

units at a low angle.

The presence of the granitic Obaskaka Lake pluton is reflected

by a broad area of relatively low magnetic relief in the

south-central property area. A discontinuous, weak to

moderate magnetic high and VLF-EM anomaly may outline the

location of the granite-greenstone contact. These anomalies

could possibly indicate a significant shear/mylonite zone with

associated sulphide mineralization similar to the Golden

Patricia gold deposit located 7 miles to the east, where

supracrustal rocks lie in sheared contact with the Dobie Lake

Batholith (Stott, 1986).

Previous regional magnetometer surveys suggest the presence

of a mafic to ultramafic intrusive stock on the southeast

corner of Dorothy Lake (Sage and Breaks, 1982). This feature

extends into the southwest corner of the property and is

reflected by a moderate increase in the magnetometer readings.

10.0 DIAMOND DRILLING PROGRAM

10.1 Description of Program

The diamond drilling program was designed to test geophysical features potentially related to the emplacement of gold min

eralization. The targets were located (a) along strike from

gold-bearing zones discovered on the adjacent Dobie River

property of Power/NARM, and (b) in the vicinity of the granite/greenstone contact in the east-central part of the

property.

l l l l l ll l l l l l ll l l l l l

-21-

Diamond drilling was contracted to N. Morissette Canada Inc.

of Haileybury, Ontario. Seven B.Q. size drill holes totalling 2,222 feet were completed between January 27th and

February 14th, 1989, under the supervision of Geocanex Ltd.

Drill core was logged, split, and stored at the campsite on

the southeast shore of Dorothy Lake. All features of

potential economic interest were sampled in sections ranging

from l to 5 feet in length.

Samples were shipped to Accurassay Laboratories Ltd. in

Pickle Lake, Ontario, where they were crushed, split and

pulverized to -150 mesh, prior to shipment to Accurassay in

Red Lake, Ontario, for fire assay with AA finish (5 ppb gold

detection limit) .

Drill hole collar locations and azimuths are shown on the

Plan of Drilling (Fig. No. 4, Appendix B). Complete drill

logs are also included in Appendix B. The legend (Fig. No.

5) and drill sections (Fig. Nos. 6 to 9) are shown in Appendix C. All analytical certificates are compiled in

Appendix D.

10.2 Discussion of Results

Table No. l summarizes the results of the diamond drilling

program and lists the assays over 50 ppb gold.

Four boreholes (NB-89-01, 02, 03, and 04) were drilled to the

northwest along strike from the gold occurrences on the Dobie

River property and two holes (NB-89-06 and 07) were drilled

along strike to the southeast. No economic gold values were

returned from these holes although several yielded geo-

chemically anomalous results.

The best results were obtained from hole NB-89-02 in the

northwest property area. A 70 foot wide section of mafic to

TABLE I SUMMARY OF DIAMOND DRILLING RESULTS

Drill Hole Number

GridLocation (feet)

S SLength (feet)

Summary Descriptionl) L T S

Intersection (feet)

Width Au.oz Au. (feet) /ton ppb

Sample Description

NB-89-01

NB-89-02

32+OOW, 18+96N

32+OOW, 22+97N

297.0

297.0

Almost entirely mafic to inter- 31.0-36.0 mediate metavolcanics, mostly flows with minor tuffs; minor wacke near bottom of hole.

predominantly mafic meta volcanics (mostly flows, minor tuff) with minor intermediate tuffs and flows; minor wacke.

141.7-146.0 146.0-149.5 149.5-152.5

160.5-162.5 162.5-166.5

181.2-186.2 201.0-204.0 204.0-207.0 207.0-211.0 211.0-214.5

240.4-244.4

5.0

109.5-113.0 3.5

4.3 3.5 3.0

2.0 4.0

175.0-178.8 3.8

3.0 4.0 3.5

4.0

0.010

54

110

9662

181

18463

117

347256112156116

54

Mafic to intermediate flows and minor tuff; 2-51 quartz veinlets, trace pyrite.

Mafic flow, trace dissemi nated pyrite and pyrrhotite.

Mafic tufff?), possible sheared ultramafic flow; weakly brecciated, strongly carbonatized, x-2% pyrite.

Sheared mafic to ultra mafic flows; reddish hematite common in vein lets, trace disseminated pyrite.

Mafic flow; 2-5% quartz- carbonate veinlets, often containing hematite, pyrite.

Mafic flow, hematite blebs common in quartz-carbonate veinlets, trace pyrite.

lN)t-o

l

Mafic to intermediate flow; trace disseminated pyrite, minor hemotite in veinlets.

TABLE I SUMMARY OF DIAMOND DRILLING RESULTS

Drill Hole Number

NB-89-03

NB-89-04

NB-89-05

NB-89-06

NB-89-07

Grid Location (feet)

60+OOW,6 + 90N

60+OOW,10+83N

56+OOE3 + 49N

48+OOE,30+96N

48+OOE,34+98N

ALength Summary Description Intersection (feet) (feet)

327.0 Predominantly intermediate tuff, 265.1-267.1often interbedded with wacke;minor mafic flows and tuff.

277.0 Predominantly clastic metasedi- 122.5-127.0ments (wacke, siltstone, andmudstone); several narrow bedsof lean garnetiferous iron for mation; minor intermediate tuffand flows, minor mafic flows.

347.0 Granodiorite, minor granitepegmatite dykes.

347.0 predominantly porphyritic felsic 54.0-59.0to intermediate (subvolcanic?)intrusives; minor intermediateflows, oxide facies iron for- 158.0-161.0mation, mafic tuff and wacke.

242.0-245.5

330.0 Upper 3/4 of the hole consists 323.8-327.4mostly of intermediate to mafic

S S A YWidth Au.oz (feet) /ton

2.0

4.5

5.0

3.0

3.5

3.6

R EAu. ppb

51

84

66

124

112

59

S U L T SSample Description

Quartz pods and veinlets inintermediate tuff, 14pyrite blebs.

Interbedded wacke and mud stone with S-5% quartz *carbonate veinlets, tracepyrite .

Quartz-feldspar porphry,trace disseminated pyrite.

As per above.

As per above, abundantepidote .

Chloritic mafic tuffenclosing brecciated chert

ltoLO

l

tuff; remainder composed of oxide facies iron formation and clastic metasediments; several strongly mineralized intervals (pyrrhotite and pyrite).

trace - 21, pyrrhotite,

l ll l l l l l l l l l l l l l l l l

-24-

ultramafic flows and minor tuffs returned numerous values

over 100 ppb gold. The upper 30 feet is strongly sheared and

carbonatized, while the lower sections are massive to weakly

foliated, with minor carbonatization. Sulphide minerali

zation (pyrite and pyrrhotite) generally occurs in trace

amounts but increases to 2\ in thin tuffaceous bands.

Quartz-carbonate veinlets containing earthy, red hematite are

common (locally up to 51) throughout the interval. The

highest gold value from the program, 347 ppb (0.010 ounces per ton), was obtained near the bottom of this interval.

Geophysically, the anomalous zone is associated with a

magnetic abatement and lies on the eastern extremity of a

moderate to strong VLF-EM conductor. The conductor trends

east-west, oblique to the dominant east-southeast trending

stratigraphy, for approximately 2,300 feet. This may

indicate further shearing and sulphide mineralization west of

NB-89-02.

No other geochemically anomalous zones of significant width

were found in the remaining five holes drilled on this

sequence, although sporadic values over 50 ppb gold were

found in every hole. None of the iron formation or massive

sulphide horizons yielded any anomalous gold values. Most of

the values are found in mafic to intermediate volcanics with

moderate to strong quartz-carbonate veining (often with

accessory hematite, pyrite, and pyrrhotite) and weak, dissem

inated sulphide mineralization (trace -2%). Three anomalous

values were also obtained from a quartz-feldspar porphyry in

the northeast property area (NB-89-06) .

A single drill hole (NB-89-05) was targeted on a coincident

magnetic high and strong VLF-EM anomaly in the east-central

property area. This was considered to possibly indicate

shearing along the contact bedtween granitic rocks of the

Obaskaka Lake Pluton and supracrustal rocks of the Dempster

Lake Cycle. Major deformation zones are known to occur along


-25-

granite-greenstone contacts in other areas of the greenstone

belt. However, the drill hole was cored entirely in medium

equigranular grandoiortie and it appears that the VLF-EM

anomaly is topographically induced. Disseminated magnetite

(up to l?;) in the granodiorite may explain the magnetic high,

On the adjacent Dobie River property the contact was inter

sected by one hole but no significant shearing or mylo

nitization was observed. However, potassic alteration and

silicification were found to increase toward the pluton

(Burk, 1988 a).

11.0 CONCLUSIONS

No economic gold values were obtained in the present diamond

drilling program on the Nabem Lake property. A sequence of

rocks was tested along strike from known gold mineralization

on the adjacent Dobie River property of the Power Explor

ations Inc/North American Rare Metals Ltd. joint venture,

with generally negative results. However, drilling was

restricted to favourable geophysical targets and did not include a complete cross-section of the stratigraphic

sequence.

A 70 foot wide, geochemically anomalous, sheared and silicified zone found in hole NB-89-02 yielded numerous

values in the 50-350 ppb range. VLF-EM survey results

suggest that this zone may represent the eastern extremity of

a 2,300 foot long, east-west trending shear zone crosscutting the stratigraphy at a low angle. The east-west orientation

is similar to that of Zone I on the adjacent Dobie River

property, approximately 4,000 feet along strike to the

southeast (Burk, 1988 b).


-26-

Sporadic anomalous gold values over 50 ppb were found in all

but one hole in the program, mainly in mafic to intermediate

volcanics and quartz-feldspar porphyry. None of the iron

formation or massive sulphide intersections yielded any

anomalous gold values.

Volcanics along the contact with the Obaskaka Lake pluton

have yet to be tested for possible shear ing/mylonitization

which occurs along similar contacts in other areas of the

Meen-Dempster Greenstone Belt.

The mafic to ultramafic stock located in the southwest property area appears to have a similar structural setting to

copper-nickel showings on Kapkichi Lake and parts of the UMEX

Thierry deposit, both near Pickle Lake. In these cases mafic

to ultramafic rocks hosting the mineralization have intruded

the metavolcanic package in close proximity to a large

granitic pluton (Sage and Breaks, 1982) . In addition,

supracrustal rocks in the southwest corner of the property

may have undergone polyphase deformation (shearing) related

to the emplacement of the stock and the Obaskaka Lake pluton;

sheared ultramafic volcanics host the bulk of the economic

mineralization in the Thierry deposit.

12.0 RECOMMENDATIONS

Further exploration work on the Nabem Lake property is

warranted and should be concentrated on the following areas:

i) the volcanic-sedimentary package along strike from

the Dobie River gold occurrences, patially explored in

the present program;


-27-

ii) the granite-greenstone contact in the central property

area; and

iii) the mafic-ultramafic stock in the southwest property

area.

A geological mapping and prospecting program should be

completed over the entire property. This would also involve

lithogeochemical sampling for gold and base metals.

The prsent geophysical survey on the property (magnetometer

and VLF-EM) should be extended to cover all of the lakes. In

addition, a limited induced polarization (I.P.) and resis

tivity survey should be performed over areas where mapping

fails to define contacts between various rock units. Along

the granite-greenstone contact, for example, a resis

tivity contrast would likely be well defined, and I.P. would

determine if there is any disseminated sulphide mineral

ization related to possible shear ing/mylonitization along the

contact. Lines should also be run across the mafic-

ultramafic intrusive in the southwest property area to define

the contact and possibly indicate disseminated base metal

sulphide mineralization.

A further 2,500 feet of diamond drilling is also recommended.

Approximately 1,200 feet (four to five holes) should be

drilled in the north property area in order to: i) test for

possible gold mineralization beneath a VLF-EM conductor west

of hole NB-88-02, and ii) extend the stratigraphic coverage

cross the supracrustal sequence. The remaining footage should

be drilled to test additional geophysical and geological

targets. In particular, the granite-greenstone contact in the

central property area and the mafic to ultramafic stock in the

southwest property area should be examined by drilling,

placement of these holes will be contingent on the results of

the mapping and geophysical programs.

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

-28-

13.0 ESTIMATED COST OF RECOMMENDATIONS

phase I Geologic mapping, prospecting and

lithogeochemical sampling, two

geologists, one field assistant,

two week program . . . . . . . . . . . . . . . . . . . . . . . . . . $12,000.00

Contingencies (2(^) . . . . . . . . . . . . . . . . . . . . . . . $ 2,400.00

Total ...... $14,400.00

phase 2 Geophysical Program

7 line miles of magnetometer

and VLF-EM readings at

$350/line mile . . . . . . . . . . . . . . . . . . . .. . . . . . . . $ 2,450.00

4 line miles of Induced Polarization

and Resistivity readings

at $l,500/line mile . . . . . . . . . . . . . . . . . . . . . . . $ 6,000.00

Contingencies (201) . . . . . . . . . . . . . . . . . . . . . . . $ l,690.00

Total ........ $10,140.00

phase 3 Diamond Drilling

2,500 feet of B.Q. coring at

$45/foot, all inclusive . . . . . . . . . . . . . . . . . . . $112.500.00

Contingencies (201) . . . . . . . . . . . . . . . . . . . . . .. $ 22,500.00

Total ........ $135,000.00

Total cost of exploration programs

(Phases I, 2, and 3) ....................................^159,540.00

Respectfully Submitted,

E.D. Timoshenko, B.Se.

Geologist.


-29-

14.0 REFERENCES

Burk, C.P., 1988a. Report on Diamond Drilling, Dobie River

property - Private report for power/N.A.R.M. Joint

Venture.

Burk, C.P., 1988b. Report on Geological Mapping, Prospecting,

Lithogeochemical Sampling and Diamond Drilling, Dobie

River Property - Private report for Power/N.A.R.M.

joint venture.

Emslie, R.F., 1960. Geology of the Lake St. joseph, Kenora,

and Thunder Bay Districts, Ontario; Geological Survey

of Canada, Map 51-1960, Scale l inch to 4 miles.

Gillick, R.E., 1988. Report on Magnetic and VLF-EM Surveys,

Dobie River property - Private report for Power/

N.A.R.M. Joint venture.

Hodge, H.J., 1988. Report on Magnetometer and VLF-EM Surveys,

Nabem Lake Property - Private Geocanex Ltd. Report.

Ontario Geological Survey, 1986. Airborne Electromagnetic and

Total Intensity Magnetic Survey, Pickle Lake Area,

District of Kenora (Patricia Portion), Ontario: By

Geoterrex Ltd., for the O.G.S, Geophysical/

Geochemical Series; Maps 80897, 80898.

Sage, R.P., Breaks, F.W., and Troup, W; 1975. Cat Lake-pickle

Lake, Kenora and Thunder Bay Districts; Ontario

Division of Mines, Map 2218, Geological Compilation Series, Scale l inch to 4 miles.

Sage, R.P., and Breaks, F.W., 1982. Geology of the Cat Lake-

Pickle Lake Area, District of Kenora and Thunder Bay,

Ontario. Ontario Geological Survey, Report 207,

238 p.


-30-

Stott, G.M., and Larocque, C., 1983. Precambrian Geology of

the Meen Lake Area, Western part, Kenora District

(Patricia portion), Ontario Geological Survey,

Map p.2619 Geological Series.

Stott, G.M., and Larocque, C., 1983. Precambrian Geology of the Meen Lake Area, Eastern Part, Kenora District

(Patricia Portion), Ontario Geological Survey,

Map P.2620 Geological Series.

Stott, G.M., 1984. Regional Stratigraphy and Structure of the

Central uchi Subprovince: Meen Lake-Kasagiminnis Lake

and pashkokagan Lake Sections, p.7-14 in Summary of

Field Work, 1984, Ontario Geological Survey.

Stott, G.M., 1986. Regional Geology and Structure of the

pickle Lake Metavolcanic Belt, District of Kenora,

Patricia portion; p.9-14 in Summary of Field Work and

Other Activities 1986, by the Ontario Geological

Survey, edited by p.C. Thurston, Owen L. White, R.B.

Barlow, M.E. Cherry and A.C. Colvine, Ontario

Geological Survey, Miscellaneous Paper 132, 435 p.

Stott, G.M., and Brown, G.H., 1986. Economic Geology of the

Pickle Lake Metavolcanic Belt, District of Kenora,

Patricia Portion; p.15-19 in Summary of Field Work and Other Activities 1986, by the Ontario Geological

Survey, edited by p.C. Thurston, Owen L. White, R.B. Barlow, M.E. Cherry and A.C. Colvine, Ontario Geo

logical Survey, Miscellaneous Paper 132, 445 p.

Stott, G.M., and Wilson, A.C., 1986. Precambrian Geology of

the Muskegsagagen-Bancroft Lakes Area, District of

Kenora (Patricia Portion). Ontario Geological Survey

Map p.3049, Geological Series - Preliminary Map,

Scale 1:50,000.

APPENDIX A

CERTIFICATE OF QUALIFICATION


CERTIFICATE OF QUALIFICATION

THIS IS TO CERTIFY THAT:

I am a resident of Brampton, Ontario.

I am a graduate of the University of Waterloo, Waterloo, Ontario, with a Bachelor of Science degree (Geology).

I have worked continuously as an exploration geologist since 1985 in gold exploration in northwestern Ontario and the Yukon.

I supervised the drilling program on the Nabem Lake property between January 21, 1989 and February 14, 1989.

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 interpretative material which is, to the best of my know ledge, necessary to gain a complete understanding of the viability of the project and the recommendations.

and

DATED THIS DAY Of 1989.

E. D. Timoshenko, Geolog ist .

B. Se



PLAN OF DRILLING

BV ; E.DI/R.TM.DA-E. Feb 1989

GEOCANEX L'D"OPON'C. CANADA

SCALE I -ICOOFIG. No: 4

3(NV

1989 D.D.H.'s 1 to 7 prefixed

V---7-

'A/ - * 7—rf—— —— .^- — •X — *-r- —— -T — * ——; —— —— ——

.3 X

' 7 x l ,- ,

—^ _ _^ _ —_ ._ _ - ^_ ^_. .


Ve''. Mo Q15* C c e : d

/

//

l N 2N 3N NB-89-05

— -50

IO f

-HOC

•-I50

— -25O EO.H.347.0'

lOo dikes traces tl,chl,py

2175'o ^

For legend see Figure No. 5

-SecTion bearing grid south 50' lOO'

C- SCALE T;480

t r Qg a r - *prP(^

VL^-EV -V;;^^; 150-

125

100-

4N

|j ONTAR:O osQ:.oc:cAi. SURVSY j i - ASSESSMENT FILES jtl OFFICE H

s JUN IS ;383

R E C E l V E C


-75-

50-

5N


DDH SECTION L 56 + OOE(Looking grid west)

DDH No. NB -89-05BY. E.DJ./R.TM

GEOCANEX LT3'ORONTO, CANADA

DATE. Feb.1989SCALE l'-40ftFIG. No: 8


Vfe'V Wo O 19*'

- O C

- l

- -500

28 NO ——— - J——

— -50

— -100

•-I50

NB-89-0629 N 30N 31 N

o /b

8o,py,cor 80, Bx ,cor, py 5b

\ 2 * \ ^ h \ \ \

5b, ep

E.O.H. 347.0'-250' l

For legend see Figure No. 5

32 N

X"

33N

l

1-10 3d,7a,6f,(

E.O.H. 330.0'

217-5 - Section50'at:

SCALE l :48(

F rose r Filtered VLF-EM 4nDhose( 07o)

75

50-

-o-

3ON

NB-89-0631 N

NB-89-0732 N

^ No. 5

33N 34 N 35N

3d,2k (b) gnt, ep,po.py

\

E.O.H. 330.0'

I-IO'/ po.py 3d,7a,6t,cor ,s

8a,6f,gnt,po,bx

Section tearing grid south 50' lOO'

j ONTARIO G7.0'.OC:CAl. SURVEY ri ' ASSESSMENT FILES IS OFFICEf[;

S*' ..lit -* i-t ^ ^- f\^i i M 'C ; ^^^-iUsN -O :---

REG EI VB



DDH SECTION L 48 + OOE(Looking grid west)

DDH NOS.NB -89-06 8 07

SCALE l:480GEOCANEX LTD

T 0 0 ON T C. CANADA

. EDI/ R.T MDATE. Feb.1989SCALE l = 40ftFIG. No: 9

QUATERNARY

Stream, lake , bog deposits Glocia!, glacio'luvia! lacustrine sediments

LATE PRECAMBRIAN (Keeweenawan?)

Ile Diabase

EARLY PRECAMBRIAN

Intermediate and Felsic Intrusives!0o Granite pegmatite!0b Aplite!0c GranitelOd SyenitelOe Quartz monzonitelOf GranodioritelOg TrondjemitelOh Quartz diorite10] DioriteI0k Unsubdivided gneiss'O l Granite gneiss

Mafic Intrusives9a Unsubdivided9b Gabbro9c Leucogabbro9d Plagioclase-phyric gabbro9e Peridotite9f Pyroxenite

Iron Formation80 Oxide facies8b Carbono-te facies8c Silicate facies8d Sulphide facies

Geological Legend

Chemical Metasediments 7o Chert 7b Calcitic mo rble 7c Dolomitic marble

Clastic Metosediments6a Clast supported conglomerate6 b Matrix supported conglomerate6c Oligomictic conglomerate6d Polymictic conglomerate6e Sandstone, unsubdivided6 f Wacke6g Arenite6h Mudstone, argillite6j Feldspathic wacke6k Feldspathic arenite61 Quartz arenite6m Schistose rock ± omphibole,± biotite,

± garnet, ± chlorite of probablesedimentary origin

Felsic and Intermediate Subvolcanic Rocks5a Unsubdivided5 b Quartz-feldspar porphyry5c Quartz porphyry5d Feldspar porphyry

Felsic Metovolcomcs

4o Massive fine-medium grained flow4b Pyroclastic breccia, tuff breccia4c Tuff, lapilli *uff

Intermediate Metovolcanics3a Vass've f me-medium grained flow3b ri ow breccia3c Pyroclastic breccia, tuff breccia3d Tu *f , lapilli tuff

Mafic Metavolcanics2a Massive fine-medium groined flow2b Amygdaloidal flow2c Variolitic flow2d Pillowed f low, pillow breccia2e How breccia2f Medium-coarse groined flow centres2g Plagioclase- phyric flow2h Amphibolite2i Co-magmotic sills, dikes2j Pyroclastic breccia, tuff breccia2k Tuff, lapilli tuff21 Choree ± amphibole schist

Ultramafic Metovolcanicsla Massive fine-medium groined flow Ib Spinifex textured flow le Talc-carbonate ± magnetite ± amphibole

± serpentine ± chlorite schist

XJiCAL SURVEY ^bcS:--.:5"-J7 FILES""OFFICE

JUN161389 j

Symbols

Geological contact

Bedding..................

Foliation ................

Fault, shear zone..

Sample interval (feet) with gold assay in ounces per ''ton

Lost core.......................... LC.

0-Z53-0

strong weakSilicification....Sericitization .... Carbonatization Chloritization .... Brecciation Shearing ...

.SIL-SER CAR-CHL

BX SH

sil se fCO'

chl bx sh

Visible gold ................ VGSulphides................... sPyrite ........................ pyPyrrhotite .................. poChalcopyrite . cp Arsenopyrite. .... .........ospSphalerite . ............ sphGalena ..... ......... ....gaGraphite ...................,. grMagnetite .. .............. mtLimonite ........ ...........MmHematite............,....,. hemMolybdenite................mo

Abbreviations

Grunerite..................grunSiderite. .................. sidDolomite .................. dolAnkerite .................. ankGarnet ...................... antEpidote ...................,. ,.epTourmaline .............. tlXenolith ......................xnMylonite ...... ,. ........ .....mylScheelite ................. ..schCarbonate .................. ccQuartz /Carbonateveins...................... .qv/cvQuartz/ Carbonate stringers............. ...qs/ cs



LEGENDTO ACCOMPANY DRILL SECTIONS

GEOCANEX LTD TORONTO, CANADA

BY R.T.M.DATE: Feb. 1989"SCALE; n/o

FIG. No. 5

^ —-^ f tsts**t*i~*ir—t

DIAMOND DRILL RECORDNAME OF PROPERTY

HOLE NO. NB-89-5

LOCATION

LATITUDE

ELEVATION

STARTED —

NABEM

LENGTH 147.0

L56+OOE. 3+49N

Feb. 8. 1989

DEPARTURE ———————^—^———

AZIMUTH Grid South DIP FINISHED Feb. 10. 1989

-46.5'

FOOTAGE

0

347

DIP

•46. 5 0•44.5"

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. MR-flQ-S SHEET NO. l of l

REMARKS Pa 913300——————.

SUMMARY LOG

LOGGED BY E. Tlmoshenko_____

FOOTAGE

FROM

0.0

59.2

TO

59.2

347.0

347.0

DESCRIPTION

SUMMARY LOG

CASING

INTERMEDIATE INTRUSIVE - Granodiorite.

END OF HOLE

SAMPLE

NO. S&PH. FOOTAGEFROM TO TOTAL

y

ASSAYS

*

y/'

\

i

s .fi o *''*-*l'-f ^

'c*j;

,/^*

\

OZ/TON

X•^^:^-* *'•t-

V'

OZ/TON

N;y-^,'^

/

^^/' f"/"


HOLE NO. NB-89-5

LOCATION

LATITUDE

ELEVATION

STARTED —

NABEM

LENGTH 347.0 feetL56+OOE. 3+49N

Feb. 8. 1989

DEPARTURE ———-.————-

.AZIMUTH Grid SouthFeb. 10, 1989

-46.5 C

FOOTAGE

0

347

DIP

•46.5"•44.5"

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. NB-89-5 SHEET NO. l of 2

REMARKS Pa 913300________

LOOSED BY E. Timoshenko

FOOTAGE

FROM

0.0

59.2

TO

59.2

347.0

DESCRIPTION

CASING

INTERMEDIATE INTRUSIVE - overall greenish-white to grey colour,medium to coarse grained, massive with local very weakly foliatedsections.

Average Modes

Plagioclase 40 - 507.Quartz 30 - 407.Alkali Feldspar 3 - 57.Amphibole 5 - 127.Biotite 5 - 107.Magnetite trace - 17.Pyrite traceCarbonate trace

- granodiorite; predominantly medium equigranular felsic mineralswith sporadic, anhedral clots of hornblende up to 1/2" wide,fine grained biotite locally defines a weak foliation (usuallyat 0-20 0 to the core axis, up to 45" locally).

small anhedral magnetite grains usually associated with amphibole

- about 17. xenoliths of mafic volcanic flows up to 3/4" wide, 4"long, most ^1/2".

rare disseminated pyrite, minor carbonate on fracture surfaces.

- 124.4' to 124.8' - pegmatitic felsic dikecomposed of glassy quartz and white alkali feldspar, 2-37. tourmaline as anhedral grains upto 1/2" wide, 2-57. greenish plagioclase(?) ,trace magnetite, no visible sulphides; contacts at 50" to the core axis.

SAMPLE

NO.

23205

23206

23207

23208

23209

23210

23211

23212

23213

ye

tr

tr

tr

tr

tr

tr

tr

tr

tr

FOOTAGEFROM

62.0

77.5

92.0

107.0

117.0

124.0

130.0

142.0

152.0

TO

67.0

82.5

97.0

112.0

122.0

125.5

135.0

147.0

157.0

TOTAL

5.0

5.0

5.0

5.0

5.0

l;

1Si

•:

• i

'i,,,..1.5 ""

5.0

5.0

5.0

A S, S A Y SAu

'o

•''••- -'.r.**--2 1

Vi

K (::'" - .......

Z

, l -' i

'- ^-C: ;,'i

{J '"''

/.//y 7"\ r .,

'•'-'-•••••J

OZ/TON

CO. 002

CO. 002

CO. 002

CO. 002

CO. 002

""' -.. -..,.'-'f (\" t' '\v r i/Ci;

1 ' 'i --i -toc^

co.do2l^.002"

<0.002

^.002

OZ/TON

c.-i',.".~l'.''~*- ^•'•'il;'i:]

t - ,-t:O

it

!1 1 -j

y

1

j

DIAMOND DRILL RECORD NAME OF PROPERTY

HOLE NO. NR-R9-5 SHEET NO 2 Of 2

FOOTAGE

, ROM TO

347.0

DESCRIPTION

- 198.0' to 199.8' - two 3" wide pegmatiticfelsic dikes occur in this section, descriptionas per 124.4' to 124.8', except no tourmaline,reddish alkali feldspar more abundant (57.);contacts at 60-70" to the core axis.

- 208.7' to 209.6' - pegmatitic felsic dike, asper 198.0' to 199.8'; 2-57. chlorite; contacts at 70-80" to the core axis.

- 256.2' - 2" wide pegmatitic felsic dike, as per124.4' to 124.8'; 27. tourmaline, trace pyrite; contacts at 70" to the core axis.

- 309.1' to 309.5' - series of three 1/4 - 1/2"wide quartz veins at 50" to the core axis, minor alkali feldspar, trace tourmaline.

- 343.5' - 1" wide pegmatitic felsic dike, as per124.4' to 124.8', at 50" to the core axis,trace-17. tourmaline.

END OF HOLE

^-^^^

SAMPLE

'JO.

23214

23215

23216

23217

23218

23219

23220

23221

23222

23223

23224

23225

2322623227

23228

23229

23230

- SULPH

IDES

tr

tr

tr

tr

tr

tr

tr

tr

tr

tr

tr

tr

trtr

tr

tr

tr

FOOTAGE

FROM

163.0

175.0

186.0

198.0

208.0

217.0

228.0

242.0

255.0

267.5

277.0

290.0

303.0308.0

315.0

326.0

339.0

TO

168.0

180.0

191.0

201.0

210.5

222.0

233.0

247.0

257.0

272.5

282.0

295.0

308.0310.0

320.0

331.0

344.0

TOTAL

5.0

5.0

5.0

3.0

2.5

5.0

5.0

5.0

2.0

5.0

5.0

5.0

5.02.0

5.0

5.0

5.0

ASSAYSAu An01 TON

CO. 002

CO. 002

CO. 002

CO. 002

^.002

^.002

^.002

^.002

^.002

^.002

^.002

^.002

^.002^.002

^.002

CO. 002

^.002

01 TON Check

CO. 002

CO. 002

CO. 002

DIAMOND DRILL RECORDHOLE NO. NB-89-6 SHEET NO. * Of

NAME OF PROPERTY NABEM

HOLE N(

LOCATIO

LATITUD

ELEVATI

STARTEC

-v NB-89-6 LENGTH 347.0 feetM L48+OOE. 30+96N

ON AZIMUTH Grid South DIP -44"Feb. 11. 1989 FINISHFH Feb. 12 r 1989

FOOTAGE

FROM

0.0

54.0

161.0

163.3

164.0

165.3

167.6

178.2

180.2

183.5

188.4

189.7

191.1

195.3

TO

54.0

161.0

163.3

164.0

165.3

167.6

178.2

180.2

183.5

188.4

189.7

191.1

195.3

254.6

FOOTAGE

0347.0

DIP

•44"•39.5"

DESCRIPTION

SUMMARY LOG

CASING

FELSIC TO INTERMEDIATE INTRUSIVE

OXIDE FACIES IRON FORMATION - 1-27. pyrite.


MAFIC TUFF


OXIDE FACIES IRON FORMATION - sheared and brecciated, trace-27.pyrite.


INTERMEDIATE FLOW


INTERMEDIATE FLOW


INTERMEDIATE FLOW


- 236.0' to 242.3' - epidote-rich; abundant quartz veins with trace pyrite.

AZIMUTH FOOTAGE

SAM

NO. S,MH -

DIP

P L E

AZIMUTHREMARKS Pa 913JRQ

LOGGED BY . E .

FOOTAGEFROM TO TOTAL

SUMMARY LOG

TImoshenko

ASSAYS

*

V

"o

i i/.f

OZ/TON

^

OZ/TON

'•^

"* V,''

oiJ

NABEM•^•JVm*WM^^ m'm^r ^rm^mmmmm B^HII •v^r- *mi^HOLE N

FOOTAGE

PROM

254.6

267.0

300,1

303. A

338.9

TO

267.0

300.1

303.4

338.9

347.0

347.0

DESCRIPTION

SUMMARY LOG

INTERMEDIATE FLOW


INTERMEDIATE FLOW - 1-27. pyrite.


WACKE

END OF HOLE

D NB-89-6 SHEET NO

SAMPLE

'to. - SULPM IDES

FOOTAGEFROM TO -OIAL

2 of 2

ASSAYS

l 02 TON OZ TON


HOLE NO. NB-89-6

LOCATION L48+OOE

LATITUDE —————.^-——

ELEVATION -^—^.^^^—

STARTED

NABEH

LENGTH 347.0 feet30+96R

Feb. 11. 19B9

DEPARTURE ——^———-—.———.——.

AZIMUTH Grid South DIP FINISHED ____Veh. 17, 1Q8Q

-44'

FOOTAGE

0

"547

DIP

-44 0

-•^9.5'

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. NB-69-6 SHEET NO. l of 7

REMARKS Pa 913289—————————

LOGGED BY E. Titnoshenko

FOOTAGE

FROM

0.0

54,0

TO

54.0

161.0

DESCRIPTI ON

CASING

FELSIC TO INTERMEDIATE INTRUSIVE - medium to dark grey colour, por phyritic with a fine to medium grained groundmass, moderately wellfoliated at 25-35" to the core axis.

Average Modes

Quartz 40 - 507.Plagioclase 20 - 307.Alkali Feldspar 10 - 157.Biotite 5 - 157.Epidote 3 - 77.Muscovite 1 - 27.Magnetite trace - 17,Carbonate 1 - 27.Pyrite trace

10-157. phenocrysts, mostly of buff-white, pinkish and yellowishalkali feldspar with minor clear to milky quartz phenocrysts; groundmass composed predominantly of quartz, plagioclase, finegrained biotite and minor alkali feldspar.

- phenocrysts generally small ({1/16"), locally up to 1/4" wide,anhedral to subhedral; many are stretched and shattered, suggest ing shearing.

pale green epidote occurs as an alteration product of alkalifeldspars, mainly as fine grains in the groundmass, and lesscommonly within alkali feldspar phenocrysts and quartz veins.

- magnetite occurs as very fine grains within the groundmass,locally up to 17..

SAMPLE

NO.

23231

23232

23233

;5

IDES

tr

tr

tr

FOOTAGEFROM

54.0

64.5

76.0

TO

59.0

69.5

81.0

TOTAL

i/f1

5.0

5.0

5.0

ASSAYSAu Au

T-,

f r

f1f/

f "f /.^"^ ^^v,

1

"'"•••,

'"':'i/-':"--^A"''' {"

"~'O^ (-^

ct///; -

•i

'-l-, ^ 1"x"^*-.

OZ/TON

. 1 ',v*1**VVi:-'.~''-O'\

V"i''y~. "' ',,''C/;,',.

' ^ilV"C

/''- ' x.y/;.

lf' j~~ r' -.^' 'J

*"*'-.

0.002

^.002

<0.002

ppb

'" .^.^ : . i-~ ^

' k'; '.-..'^''L. ' - !*-: o'

)1

lt!,''/'

66

'-., '4*7x

fi

DIAMOND DRILL RECORD NAME OF PROPERTY. NABEM

HOLE NO. ___NB^a^f SHEET NO. J. of 7

FOOTAGE

FROM TO

DESCRIPTION

- weakly carbonatized, with very fine grained calcite within thegroundmass and rarely as small blebs within quartz veinlets.

1-27. quartz veinlets, most concordant, il/8" wide, usually withminor alkali feldspar, epidote and biotite; concordant toirregular pods and lenses composed of a very fine grained,sugary assemblage of quartz, alkali feldspar and epidote alsooccur, often zoned with alkali feldspar cores and a border zoneof mainly epidote, up to 3" wide, rarely contain pyrite.

disseminated pyrite generally rare, local blebs and euhedralcrystals up to 1/16" wide.

- 82.6' - small blebs and euhedral crystals ofpyrite up to 1/16" wide.

- 84.6' - ptygmatically folded quartz veinlet upto 1/16" wide.

- 93.1' to 95.3' - several 1-3" wide, concordantto irregular pods and lenses composed of quartzalkali feldspar, epidote and rare carbonate.

- 109.3' to 110.8' - several 1/4 - 1/2" widequartz veinlets and pods, most at 40" to thecore axis.

- 133.5' - small grains of chalcopyrite occuralong a fracture surface.

- 126.1' to 126.8' - altered section containing20-257. brick red alkali feldspar as fine grainsand stringers, minor quartz veinlets andbiotite; xenolith •of mafic flow at uppercontact.

- 135.3' to 135.6' - crosscutting quartz-alkalifeldspar vein at 30" to the core axis; tracepyrite.

SAMPLE

JO.

23234

23235

2323623237

23238

23239

23240232412324223243

23244

23245

23246

23247

23248

- SULPH

!DES

tr

tr

trtr

tr

tr

trtrtrtr

tr

tr

tr

tr

tr

FOOTAGE

FROM

81.0

83.0

87.092.0

95.5

109.0

111.0116.0121.0126.0

133.0

143.0

149.3

154.0

158.0

ra

83.0

87.0

92.095.5

100.5

111.0

116.0121.0126.0128.0

138.0

148.0

154.0

158.0

161.0

TOTAL

2.0

4.0

5.03.5

5.0

2.0

5.05.05.02.0

5.0

5.0

4.7

4.0

3.0

ASSAYS AU All All

0! TON

:0.002

:0.002

:0.002:0.002

:0.002

:0.002

:0.002:0.002:0.002:0.002

:0.002

:0.002

:0.002

'0.002

0.004

ppb

124

Check

^.002

DIAMOND DKILL KfcWUKIf NAME oHOLE N

FOOTAGE

FROM

161.0

163.3

164.0

TO

163.3

164.0

165.3

DESCRIPTION

OXIDE FACIES IRON FORMATION - finely banded chert-magneti te-amphi-bole with thin interbeds of chloritic mafic tuff.

Average Modes

Chert 20 - 257. Magnetite 20 - 257. Amphibole 30 - 407. Chlorite 10 - 157. Biotite 2 - 37. Carbonate 1 - 27. Pyrite 1 - 27. Garnet trace

banding moderately well developed at 35-40 0 to the core axis; most bands 41/8" wide, chert bands often brecciated.

several narrow bands of chlorite ± amphibole ± biotite schist (1/4 - 1" wide), likely mafic tuff; often contains small garnets.

weakly carbonatized, veinlets rare, mostly fine disseminated grains of calcite.

pyrite occurs mainly in disseminated grains, less common are blebs and euhedral crystals -^1/16" wide.

discordant lower contact with intrusive, oriented at 30" to the core axis.

FELSIC TO INTERMEDIATE INTRUSIVE - as per 54.0' to 161.0', excepthighly biotitic (up to 307.); contains small xenoliths of chlorite ± amphibole ± garnet schist up to 1" wide (mafic tuff).

MAFIC TUFF - dark green, fine grained, well foliated at 20-30" tothe core axis.

Average Modes

Chlorite 55 - 607. Biotite 20 - 257.

f PROPE

n NB

RTY NABEM

-85-6 SHEET NO.

SAMPLE

NO

23249

- SULPH

IOES

1-2

FOOTAGEFROM

161.0

TO

163.3

TOTAL

2.3

3 of 7

ASSAYS Au Au0? TON

•CO. 002

02 TON Check

CO. 002

DIAMOND DRILL RECORD NAME OF PROPFRTY

HOLE NO. ____NB-69-6

JIABEM.SHEET NO. 4 Of 7

FOOTAGE

PROM

165.3

167.6

178.2

180.2

TO

167.6

178.2

180.2

183.5

DESCRIPTION

Garnet 5 - 107.Quartz 3 - 77. Amphibole 2 - 57.

essentially a chlorite biotite garnet schist (possibly pelitic sediment).

irregular contacts with intrusive, possibly a large xenolith.

FELSIC TO INTERMEDIATE INTRUSIVE - as per 163.3' to 164.0'.

OXIDE FACIES IRON FORMATION - strongly sheared and brecciated chert-magnetite-amphibole and thin bands of garnetiferous mafic tuff (similar composition to 161.0" to 163.3').

Most of the banding has been obliterated, fragments displaying fine banding occur locally (oriented at 10-20" to the core axis); irregular, sheared pods and patches of garnetiferous mafic tuff and porphyritic felsic intrusives compose about 107. of the section.

Weakly carbonatized; 2-37. quartz pods containing minor epidote and alkali feldspar

Trace-27, disseminated pyrite, rarely in thin stringers up to 1/16" wide.

Banded sections display small fold closures locally.

FELSIC TO INTERMEDIATE INTRUSIVE - as per 54.0' to 161.0', biotitecontent up to 207., 57. alkali feldspar phenocrysts; irregular masses of chlorite material are likely mafic volcanic xenoliths (57.); weakly sheared and carbonatized, trace disseminated pyrite; foliation at 45-50" to the core axis.

INTERMEDIATE FLOW(?) - overall greyish-green colour, coarse grained,massive.

Average Modes

Plagioclase 40 - 507. Amphibole 15 - 257. Biotite 10 - 157.

SAMPLE

NO.

23250

23251 23252 23253

23254

' SULPM

IDES

tr

tr-2 tr-2 tr-2

tr

FOOTAGE

FROM

163.3

167.6 171.0 174.5

178.2

TO

167.6

171.0 174.5 178.2

180.2

'OTAL

4.3

3.4 3.5 3.7

2.0

ASSAYSAu

~- 02 TON

:0.002

:0.002 :0.002 :0.002

:0.002

G J! TON


MOLE NO. NB-89-6

-HABE1LSHEET ND 5 Of 7

FOOTAGE

^ROM

183.5

188.4

189.7

191.1

TO

188. A

189.7

191.1

195.3

DESCRIPTION

Quartz 2 - 57.Chlorite 2 - 57.Alkali Feldspar 2 - 37.Carbonate 1 - 27,Pyrite trace

possibly a coarse grained intermediate flow centre or a differ ent phase of the intermediate intrusive (diorite?); contacts at45" to the core axis (concordant with surrounding foliation).

weakly carbonatized, quartz-carbonate veinlets absent.

local irregular masses of chlorite up to 2" wide.

trace disseminated pyrite.

FELSIC TO INTERMEDIATE INTRUSIVE - as per 54.0' to 161.0'; 3-57.alkali feldspar phenocrysts, rare quartz phenocrysts; weaklysheared at 45" to the core axis.

- 183.5' to 184.5" - phenocrysts are highly fracturedand granulated (possible cataclastic deformation);weak compositional banding.

INTERMEDIATE FLOW - as per 180.2' to 183.5', possibly an intrusive;carbonatized.

- 189.1' to 189.7' - several discontinuous quartz carbonate alkali feldspar veins up to 1/2" wide;no visible sulphides.

FELSIC TO INTERMEDIATE INTRUSIVE - as per 54.0' to 161.0'; 57.alkali feldspar phenocrysts; weakly foliated at 40-45" to the coreaxis; silicified lower contact (at 45" to the core axis).

INTERMEDIATE FLOW - massive, coarse grained flow (possible intrus ive) as per 180.2' to 183.5'.

- 193.1' to 193.3' - composite vein with walls ofalkali feldspar and quartz and a core of grey,coarse grained calcite; 1-27. disseminated biotite,trace tourmaline.

SAMPLE

no.

23255

23256

23257

23258

- SULPH

IDES

tr

tr

tr

tr

fOOTAGE

fROM

180.2

183.5

188.4

191.1

ro

183.5

188.4

191.1

195.3

TOTAL

3.3

4.9

2.7

4.2

ASSAYS Au Au

-. 01 TON

:o.oo2

:0.002

:0.002

co. 002

ill TON Check

^.002


HOLE NO. ____SB-89-6 SHEET NO 6 of 7

FOOTAGE

CROM

195.3

254.6

267.0

TO

254.6

267.0

300.1

DESCRIPTION

FELSIC TO INTERMEDIATE INTRUSIVE - as per 54.0' to 161.0'; upper10' is highly biotitic (10-157.), becoming gradually less biotitic and compos! tionally banded downhole; locally sheared and silicified;weakly carbonatized , 17. magnetite.

- 225.4' to 225.9' - quartz vein or pod, containssmall grains of white alkali feldspar, rare carbon ate and pyrrhotite.

- 231.5' to 232.5' - foliated at 0-10 0 to the coreaxis.

- 232.5' to 236.0' - foliated at 30" to the coreaxis.

- 236.0' to 242.3' - section contains 5-107. epidote,mainly as fine disseminated grains, less commonlyas thin stringers and blebs adjacent to quartzveins; 3-47. crosscutting clear to smoky quartzveins, usually at 10-30" to the core axis, mostabout 1/2" wide; trace disseminated pyrite andpyrrhotite, minor small blebs adjacent to veins.

- 249.2' to 254.6' - irregular pods and bands up to8" wide enriched in quartz, trace-17. disseminatedpyrite; most sections foliated at very low anglesto the core axis (0-20 0 ).

INTERMEDIATE FLOW - similar to 180.2' to 183.5', except mediumgrained and greater amphibole content (25-307.).

Narrow silicified zones up to 8" wide containing abundant quartzand pink alkali feldspar, trace pyrite.

- 262.9' to 264.2' - 5-107. ovoid quartz epidoteblebs up to 1/8" wide, possible amygdules.

FELSIC TO INTERMEDIATE INTRUSIVE - as per 54.0' to 161.0'; mostsections foliated at 45-50" to the core axis, 30" near upper con tact; magnetite rare.

SAMPLE

NO.

23259

23260

23261

23262

23263

23264

2326523266232672326823269

2327023271

23272

23273

2327423275232762327723278

" SULPH

IDES

tr

tr

tr

tr

tr

tr

trtrtrtrtr

trtr

tr

tr

trtrtrtrtr

FOOTAGE

FROM

198.0

206.0

215.5

225.0

226.0

231.0

236.0237.9240.1242.0245.5

249.1252.0

254.6

263.0

267.0272.0282.0287.0296.0

TO

203.0

210.0

220.5

226.0

231.0

236.0

237.9240.1242.0245.5249.1

252.0254.6

259.6

267.0

272.0277.0287.0292.0300.1

TOTAL

5.0

4.0

5.0

1.0

5.0

5.0

1.92.21.93.53.6

2.92.6

5.0

4.0

5.05.05.05.04.1

ASSAYS Au Au Au

-. 01 TON

CO. 002

CO. 002

CO. 002

CO. 002

CO. 002

CO. 002

CO. 002CO. 002CO. 0020.003

CO. 002

CO. 002CO. 002

CO. 002

CO. 002

CO. 002CO. 002CO. 002CO. 002CO. 002

ppb

112

Check

CO. 002

CO. 002


HOLE NO. ————NB-89-6

NABEM

SHEET NO 7 Of 7

FOOTAGE

f ROM

300.1

303.4

338.9

TO

303.4

338.9

347.0

347.0

DESCRIPTION

INTERMEDIATE FLOW - dark green, medium grained, massive flow, asper 254.6' to 267.0'.

1-27. quartz carbonate pods and lenses up to 1/2" wide, minorthin stringers at 30-40" to the core axis.

1-27, disseminated pyrite.

FELSIC TO INTERMEDIATE INTRUSIVE - as per 54.0' to 161.0'; foliatedat 45-50" to the core axis; trace-27. disseminated garnet, tracedisseminated pyrite and magnetite.

- 333.4' to 338.9' - sheared with abundant maficxenoliths, phenocrysts highly fractured, locallychloritic (up to 57.).

WACKE - greenish-brown, fine grained, moderately well foliated at25-30" to the core axis.

Average Modes

Quartz 55 - 607.Feldspar 3 - 57.Biotite 15 - 207.Chlorite 10 - 157.Garnet 2 - 47.Carbonate trace - 17.Pyrite trace

weak compositional banding; quartz-carbonate veinlets rare.

garnets up to 1/8" wide, mostly 0/16", generally scattered butoften in clumps of anhedral crystals.

trace disseminated pyrite.

END OF HOLE

i "

SAMPLE

NO

23279

2328023281232822328323284

23285

~, SULPH

IDES

1-2

trtrtrtrtr

tr

FOOTAGE

FROM

300.1

303. A314.0323.0329.5333.4

338.9

TO

303.4

308.0319.0327.0333.4338.9

344.0

TOTAL

3.3

4.65.04.03.95.5

5.1

ASSAYSAu Au02 TON

(0.002

CO. 002CO. 002CO. 002CO. 002CO. 002

CO. 002

01 TON Check

CO. 002

DIAMOND DRILL RECORDHOLE NO. NB-89-7 SHEET Na l of l

NAME OF PROPERTY NABEM

HOLE N(

LOCATIO

LATITUD

ELEVATI

STARTED

1 NB-89-7 LENGTH 330.0 feetw L48+OOE, 34+98N

Feb. 13, 1989 nwicuFn Feb. 14. 1989

FOOTAGE

FROM

0.0

56.5

234.1

258.0

284.0

294.9

310.0

323.8

327.4

TO

56.5

234.1

258.0

284.0

294.9

310.0

323.8

327.4

330.0

330.0

FOOTAGE

0330

DIP

-46"-42"

DESCRIPTI ONSUMMARY LOG

CASING

INTERMEDIATE TO MAFIC TUFF

- 218.0' to 234.1' - 2" to 2' bands of massive to semi-massive pyrite and pyrrhotite; strongly brecciated and carbonatlzed.

INTERBEDDED INTERMEDIATE TUFF, CHERT AND WACKE

INTERBEDDED OXIDE FACIES IRON FORMATION AND WACKE

MAFIC TUFF AND CHERT

LEAN OXIDE FACIES IRON FORMATION

WACKE

MAFIC TUFF AND CHERT

WACKE

END OF HOLE

AZIMUTH FOOTAGE

SAM

NO.'o

DIP

P L E

AZIMUTHREMARKS Pa 913289

SUMMARY LOG

LOGGED BY E. Tlmoshenko

FOOTAGEFROM TO

,9

TOTAL

,f'f'

ASSAYS

^

"' i '^-[

i

\,

1

'' •; :.V'.*X

''"^'W

ty

\;O

OZ/TON

Sx

'"i

y

OZ/TON

1


HOLE NO. NB-89-7

LOCATION

LATITUDE .

ELEVATION

NABEM

330.0 feetL48+OOE. 34+98N

STARTED Feb. 13. 1989

DEPARTURE ————-—————-—————

AZIMUTH Grid South DIP Feb. 14. 1989

-46"

FOOTAGE

0

327

DIP

-46"-42'

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. NB-89-7 SHEET NO. l of fi

REMARKS Pa 913289——————

LOGGED BY E. Timoshenko

FOOTAGE

FROM

0.0

56.5

TO

56.5

234.1

DESCRIPTI ON

CASING

INTERMEDIATE TO MAFIC TUFF

- 56.5' to 177.7' - dark green to greyish-green, fine grained, wellfoliated.

Average Modes

Amphibole 35 - 457.Plagioclase 30 - 407.Biotite 5 - 157.Chlorite 5 - 107.Quartz 2 - 57,Alkali Feldspar 1 - 37.Carbonate 1 - 27.Epidote trace - 27.Sulphides trace - 37.Garnet trace - 17.

- varies from fine grained ash tuff to lapillituff; lapilli fragments usually ^1/2" wide, upto 2" wide, irregular to lens-shaped; predomin antly intermediate in composition.

- weak compositional banding locally (biotite and chlori te-rich bands); anastomosing, discontin uous streaky bands of biotite, chlorite andamphibole, and small grains of plagioclase andquartz occur in lapilli tuff.

- 1-27. quartz-carbonate, mainly as thin, discon tinuous veinlets and lenses between 1/8 - 1/4"wide, often highly irregular and anastomosing;

SAMPLE

NO.

2328623287232882328923290 23291

TV

1-21-21-21-2

tr-1 tr-1

FOOTAGEFROM

58.5

63.568.073.078.0 87.0

TO

63.568.073.078.082.5 92.0

TOTAL

y

.f

^^~~~

5.04.55.05.04.5 5.0

ASSAYS All

'i

/^,

U

'' f"

\C

'i

V ' -" J ~? f -

GA-

UN li

1 \^'•~^ '''

OZ/TON

"' ..^

v.''-, ; :.

-K r f-^

##7A* A^' * "*~

^"^,

<0.002:0.002CO. 002CO. 002CO. 002 CO. 002

OZ/TON

:"^. '^ '^c^i?

1liis1

7"'"

.

DIAMOND DRILL RECORD NAME OF PRDPFRTY

HOLE NO NB-89-7

JIABEtL

SHEET NO. . 2 of 8

FOOTAGE

f ROM TO

DESCRIPTION

frequently contain accessory epidote, alkalifeldspar and sulphides.

- pyrrhotite and pyrite occur as finely dissemin ated grains and as sporadic stringers and blebsup to 1/4" wide.

- small ovoid or lens-shaped blebs composed ofcarbonate and/or quartz with rims of reddishalkali feldspar (?) and/or epidote are likelyamygdules; occur sporadically over the unit butlocally compose up to 57. of the rock, most^1/8" wide, some are highly irregular or dis torted, up to 1/2" long.

- most sections foliated at 25-35" to the coreaxis (increasing downhole).

- 93.2' to 102.0' - 2-57. carbonate and quartzamygdules; may contain alkali feldspar, epidote,and pyrrhotite.

- 112.5' to 120.1' - 3-57. sulphide, mostly pyrrho tite with lesser pyrite, as fine disseminationsand concordant stringers up to 1/2" wide, minorvery thin crosscutting stringers.

- 131.0' - foliated at 45" to the core axis.

- 161.0' to 162.3' - blocky core, minor core loss;1-27. disseminated pyrrhotite.

- 173.0' to 176.8' - several irregular, 1/2 - 1"wide quartz-carbonate veins, trace pyrrhotite;section foliated at 55" to the core axis.

- 177,0' to 202.0' - predominantly garnetiferous mafic tuff j darkgreen, fine to medium grained, weakly foliated,weak compositional banding.

Average Modes

Amphibole 45 - 557.Plagioclase 15 - 207.

SAMPLE

NO

232922329323294

2329523296

23297

23298232992330C23301

2330223303

- SULPM

IOCS

1-21-21-2

3-53-5

tr-1

trtrtr1-2

trtr

FOOTAGErHOM

92.097.0

107.0

112.0116.0

120.0

131.0142.0154.0159.0

167.0173.0

ro

97.0101.5112.0

116.0120.0

125.0

136.0147.0159.0165.0

171.0177.0

TOTAL

5.04.55.0

4.04.0

5.0

5.05.05.06.0

4.04.0

ASSAYS Au An

o? TON

:0.002CO. 002CO. 002

CO. 002CO. 002

:0.002

:0.002:0.002:0.002co. 002

CO. 002CO. 002

o; TOX Check

^.002

DIAMOND DRILL RECORD NAME OF PROPERTY——

HOLE NO. - NB-89-7

NABEM

SHEET NO 3 Of 8

FOOTAGE

TROM

*

234.1

TO

258.0

DESCRIPTION

Biotite 15 - 207.Chlorite 2 - 57.Garnet 3 - 57.Quartz 1 - 27.Carbonate 2 - 47.Sulphide 1 - 27.

- mostly amphibole and plagioclase with irregula:patches and lenses of biotite and garnet-richmaterial; minor carbonate and quartz amygdules(1-27.).

- 2-47. quartz-carbonate veinlets, most highlyirregular, 1/8 - 1/4" wide, locally up to 1"wide.

- pyrrhotite and rare pyrite occur as fine dis seminations and minor thin stringers.

- gradational contacts; foliated at 60" to thecore axis.

- 202.0' to 234.1' - fine grained intermediate ash tuff and lapillituff as per 56.5' to 177.7'; section containsnumerous strongly mineralized bands up to 2.0'wide composed of pyrite and pyrrhotite; smallsulphide blebs and stringers are common througlout the unit; weakly foliated at 70" to thecore axis.

- 218.0' to 234.1' - strongly mineralized hori zon; bands between 2" and 2.0' wide composedof a massive to semi-massive assemblage ofpyrite and pyrrhotite; mineralized zones areusually strongly brecciated and carbonatized,fragments typically {.1/2" wide; large anhedralgrains of garnet are common in the tuffaceoussections, up to 1/2" wide.

INTERBEDDED INTERMEDIATE TUFF, CHERT AND WACKE - predominantly darkgrey to greyish-brown intermediate tuff (607.), gradational intowacke; interbeds up to 3.0' wide composed of light grey chert andchloritic mafic tuff (207.).

SAMPLE

NO

23304233052330fl23307

233082330923310

-

23311233122331323314

" SULPH

ion

1-21-21-21-2

1-22-33-10

10-2010-2030-4020-30

FOOTAGE

FROM

177.0182.0187.0192.0

202.0207.0212.0

217.0221.0225.0229.0

TO

182.0187.0192.0197.0

207.0212.0217.0

221.0225.0229.0234.0

'OTAL

5.05.05.05.0

5.05.05.0

4.04.04.05.0

ASSAYSAu Au

; 01 TON

:0.002 CO. 002:0.002F:0.002

:0.002:0.002:0.002

:0.002:0.002:0.002:0.002

(li TON Check

CO. 002

^.002

DIAMOND DRILL RECORD NAME OF PPOPFRTV

HOLE NO. NB-89-7

NABEM

SHEET NO.. 4 of 8

FOOTAGE

FROM TO

DESCRIPTION

- 234.1' to 235.6' - finely banded chert and garnetiferous mafictuff.

Average Modes

Chlorite 55 - 657.Chert 10 - 157.Amphibole 10 - 157.Epidote 3 - 57.Garnet 2 - 37.Carbonate 3 - 57.Biotite 2 - 37.Sulphides 2 - 37.

- thin, poorly developed bands of chloritictuff and minor chert, with minor bands com posed of fine grained biotite and quartz(wacke?); garnetiferous bands contain abundantepidote, chert bands are strongly carbonatizedunit is weakly brecciated, shear fracturescommon.

- pyrrhotite and pyrite occur as small blebsand concordant stringers up to 1/8" wide.

- banding at 55-60" to the core axis.

- 235.6' to 237.5' - dark grey, fine grained, well foliated inter mediate tuff; abundant chlorite and felsiclapilli, trace pyrrhotite.

- foliated at 60 C to the core axis.

- 237.5' to 238. 7 1 - interbedded chloritic tuff and chert; highlybrecciated chert fragments (207.) surrounded byanastomosing bands of very fine grainedchlorite ( amphibole) schist; 1-27. pyrrhotiteblebs, weakly carbonatized.

- 238.7' to 244.2' - intermediate tuff, as per 202.0' to 237.5',with strong sulphide mineralization; band ofmassive to semi-massive pyrrhotite between240.5' to 241.3', elsewhere 2-57. pyrrhotite pyrite blebs and stringers.

SAMPLE

NO

23315

2331623317

", SUIPH

IDES

tr-2

1-25-10

FOOTAGE'SOW

234.0

237.5240.2

TO

237.5

240.2244.2

TOTAL

3.5

2.74.0

ASSAYS AU

-. oz TDK

^.002

^.002^.002

fi l TON


HOLE NO. NR-S9-7

-NA&EH-SHEET NO.. 5 of

FOOTAGE

c ROM TO

DESCRIPTION

- 244.2' to 245.7' - as per 237.5' to 238.7', interbedded chloritic tuff and chert, strongly brecciated; 1-27. carbonate veinlets, 2-37. pyrrhotite, trace chalcopyrite.

- 245.7' to 247.3' - dark grey, fine grained wacke, finely lamin ated at 70" to the core axis.

Average Modes

2U" tZ 3- 60 - 707. FeldsparBiotite 20 - 307.Chlorite 3-77.Carbonate 1 - 27.Garnet 1 - 27.Sulphides trace - 17.

- garnets occur mainly near contacts; dissemin ated pyrrhotite, rare pyrite.

- 1-27, quartz-carbonate, mostly as irregular pods, minor concordant veinlets.

- 247.3' to 249.1' - as per 237.5' to 238.7', interbedded chloritic tuff and chert, weakly brecciated; 1-27. pyrr hotite (mostly small blebs, minor crosscutting stringers), trace chalcopyrite.

- 249.1' to 249.7' - dark brown, fine grained wacke, foliated at 55" to the core axis; no visible sulphides or veinlets; contacts highly garnetiferous.

- 249.7' to 250.5' - interbedded chloritic tuff and chert, as per 237.5' to 238.7'; 1-27. pyrrhotite.

- 250.5' to 252.8' - dark brown, fine grained wacke, no visible sulphides, minor quartz-carbonate blebs.

- 252.8' to 255.6* - as per 234.1' to 235.6'; poorly developed bands of garnetiferous mafic tuff and chert, weakly brecciated and carbonatized, trace-27. pyrrhotite; banding at 60-65" to the core axis.

SAMPLE

NO

'3318

23319

". SULPH

IDES

1-2

tr-1

FOOTAGE

rflOM

244.2

252.8

10

249.1

255.6

'OTAL

4.9

2.8

ASSAYSAu

".

(0.002

CO. 002

NAME OF PROPERTY..^^ jr-mMWB 1 ^ B-vii^ m^m^mmmmm rnnmm-^-^ m**^~HOLE N

FOOTAGE

FROM

258.0

TO

284.0

DESCRIPTION

- 255.6' to 258.0' - dark brown, fine grained wacke, minor garnet and carbonate, trace pyrrhotite.

INTERBEDDED OXIDE FACIES IRON FORMATION AND WACKE - Iron formationis very similar to the interbedded chert and mafic tuff unit above (i.e. 234.1' to 235.6") except for fine laminations of magnetite which increase in abundance downhole; interbedded with highly garnetiferous, dark brown, fine grained wacke.

- 258.0' to 262.0' - as per 234.1' to 235.6', with local fine laminations of magnetite (total 2-47.); garnet locally forms semi-massive bands up to 3" wide; trace-27. pyrrhotite.

- 262.0' to 263.4' - dark brown, fine grained wacke, up to 107. garnet, foliated at 60" to the core axis.

- 263.4' to 264.5' - predominantly mafic tuff (chlorite amphibole containing large garnets up to 1/2" wide, garnet locally forms massive bands; minor chert bands up to 3" wide contain fine lamin ations of magnetite, trace-17. pyrrhotite.

- 264.5' to 265.6' - wacke, as per 262.0' to 263.4'.

- 265.6' to 270.8' - oxide iron formation; most sections strongly brecciated.

Average Modes

Chert 20 - 307. Chlorite 40 - 507. Amphibole 2 - 57. Magnetite trace - 107, Garnet 2 - 37. Grunerite trace - 27. Carbonate 1 - 27. Sulphides trace - 27.

- predominantly chloritic tuff enclosing brec ciated fragments of chert; irregular anasto mosing bands of magnetite up to 1/2" wide locally enclose chert fragments, minor

1 NB-89-7 SHEET NO

SAMPLE

NO.

23320

23321

-. SULPH

IOCS

tr-1

tr-1

FOOTAGE

FROM

258.0

262.0

TO

262.0

265.6

TOTAL

4.0

3.6

6 of 8

ASSAYSAu

01 TON

:0.002

^.002

'Jl TON


HOLE NO. NB-89-7

NABEM

SHEET NO. 7 Of

FOOTAGE

FROM

284.0

294.9

TO

294.9

310.0

DESCRIPTION

grunerite occurs along borders of magnetitebands.

- chert bands are often strongly carbonatized.

- garnet locally forms massive bands up to 1/2"wide; usually disseminated in tuff bands.

- pyrrhotite occurs as irregular blebs andstringers adjacent to magnetite bands, andas fine disseminations in tuff bands.

- 270.8' to 275.1' - dark brown, fine grained wacke, minor bandsup to 2" wide composed of chert and mafictuff; entire unit is highly garnetiferous,locally brecciated and carbonatized, weaklyfoliated at 45 0 to the core axis.

- 275.1' to 284.0' - oxide facies iron formation, similar to265.6' to 270.8', except this section has amuch higher magnetite content (15-257.); mostof the unit is strongly brecciated, localfine banding at 35-40" to the core axis;weak carbonatization locally, garnet gener ally rare; trace-37. pyrrhotite, usually asnarrow irregular stringers.

MAFIC TUFF AND CHERT - dark green, garnetiferous mafic tuff (mostlyfine grained chlorite, minor amphibole and biotite) enclosesbrecciated fragments of light grey chert (107.); garnet contentusually between 2-47., locally up to 107.; most sections weaklyfoliated at 50-60" to the core axis, locally highly contorted.

- 293.6' to 294.0' - 3-57. pyrrhotite, 17. chal copyrite as fine disseminations and concor dant stringers up to 1/4" wide.

LEAN OXIDE FACIES IRON FORMATION - predominantly chloritic mafictuff, as per 284.0' to 294.9', with thin Irregular bands of magne tite locally occurring within chert bands, also finely disseminatedand infilling thin, crosscutting fractures in several tuffaceousbands (1-57. overall).

SAMPLE

NO.

!3322

23323

!332423325

23326

23327

23328233292333023331

". SULPH

IDES

tr-2

tr

tr-3tr-3

tr-1

tr-2

tr-1tr-11-21-3

FOOTAGEFROM

265.6

270.8

275.1280.0

284.0

291.5

294.9299.0304.0307.0

10

270.8

275.1

280.0284.0

288.5

294.9

299.0304.0307.0310.0

TOTAL

5.2

4.3

4.94.0

4.5

3.4

4.15.03.03.0

ASSAYSAu Au

'. 01 TON

CO. 002

CO. 002

CO. 002CO. 002

CO. 002

CO. 002

CO. 002CO. 002CO. 002CO. 002

m row Check

CO. 002

CO. 002

DIAMOND DRILL RECORD NAME OF PPOPFRTY

HOLE NO flBjL&a

JJARE1LSHEET ND 8 of 8

FOOTAGE

FROM

310.0

323.8

327.4

TO

323.8

327.4

330.0

330.0

DESCRIPTION

Chert is usually strongly brecciated and weakly carbonatized;biotite locally forms bands up to 2" wide; garnet generally rare(locally up to 37.).

Trace-27, disseminated pyrrhotite blebs.

WACKE - dark brown, fine grained, moderately well foliated wacke,similar to 245.7' to 247.3'; essentially a quartz feldspar-biotite sediment, very minor chlorite and chert bands.

Foliated at 10-20" to the core axis, minor small fold closures.

MAFIC TUFF AND CHERT - as per 284.0' to 294.9'; chloritic tuffenclosing brecciated chert fragments, garnet locally up to 57.,trace-27. pyrrhotite blebs.

WACKE - as per 310,0' to 323.8', abundant garnet along uppercontact, trace pyrrhotite.

END OF HOLE

SAMPLE

NO.

2333223333

23334

SUIPM

'DES

trtr

tr-2

FOOTAGEFROM

310.0319.0

323.8

TO

315.0323.8

327.4

TOTAL

5.04.8

3.6

ASSAYS AU All All

~

02 TON

^.002^.002

0.002

ppb

59

Check

:0.002

•1 ^^^

OKI1 ifPv

.^L\ \^.^K. l -A.

ACCURASSAY LABORATORIES LTD.KIRKLAND LAKE,

P.O. BOX 604ONTARIO, CANADA P2N 3J5

TEL.: (705) 567-6343

1 x^L. President: Dr. GEORGE DUNCAN, M.SC.

1

1

1 25924

lSAMPLE

— Ac cur assay1" 444271

444272

1 444273444274444275

1 444276444277444278444279

1 444280444280444281

1 444282444283444284444285

M 444286" 444287

444288

1 444289444289444290444291

l 444292" 444293

444294

1 444295444296444296

1

1LF-30

1

, Ph. D., C. Chem (Ont.l, C. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of AnalysisMr. H. J. Hodge

Geocanex Ltd. 1003-34 King Street E;Toronto, OntarioM5C-1E5

NUMBERSCustomer

23205232062320723208232092321023211232122321323214232 1 4232152321623217 Resul232182321923220232212322223223232232322423225232262322723228232292323023230

Page: 1

natfi . February 20 19 89ast

Work Order tt : 090028Project : Nabem

Gold Goldppb Oz/T

S.5 *; 0.002o *; 0.002O *:: 0.002•i 5 t. 0.002o 4:0.002o *:. 0.002^ < 0.00211 *: 0.002t.5 ^:: 0.002<5 -x 0.002O *:: 0.002 Check*;s -^ 0.002

5 't. 0 . 002t to be forwarded

5 4; 0.00217 < 0.002<5 '.•i 0.00211 ^; 0.002<5 *: 0.00210 'C 0.002

6 K 0.002 Check6 s, 0.002

24 4:0.0028 -^ 0 . 0027 4:0.0027 -^ 0.0026 4:0.0026 s^ 0.0026 4:0.002 Check

Per: \^X,-. ___ . \ .'' , J^ V

ORIGINAL

l l l l l l l l l l l l l l l l l l l LF-30

ACCURASSAY LABORATORIES LTD.P.O. BOX 604

KIRKLAND LAKE, ONTARIO, CANADA P2N 3J5 TEL.: (705) 567-6343

President: Dr. GEORGE DUNCAN, M.SC., PH. o., c. Chem (om.i, c. Chem (U.K.), M.C.I.c., M.R.S.C., A.R.C.S.T.

Certificate of Analysis" D r n r." .

Mr. H.J. HodgeGeccanex Ltd.!Q03-34 King Street EastToronto, OntarioM5C 1W5

SAMPLE NUMBERS

Accurassay 444283

Customer 23217

**result to be forwarded

Date:

Pacje: l

February 21

REASSAY Work Order # Prcj ect

090028Nab era

OriginalAssay

ppb Oz/Ti; i; * *

Reassay Result

ppb Os/T

Per:

19.89.

ORIGINAL

1111111111111111111

^ N

J^v^Ihk. Presii

25952 ci t

SAMPLEAc c ur assay

4444824444B3444484 444485444486444487444488 444489444490444491 444491444492444493 444494444495444496444497 444498444499444500 444500444501444502444503 444504444505444506 444507444508444509 444509

LF-30



President: Dr. GEORGE DUNCAN, M.SC., Ph. D., c. chem (Ont.i, c. chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of AnalysisMr. H.J. Hodge

Geocanex Ltd. 1003-34 King Street East Toronto, Ontario M5C-1E5

NUMBERS

Page: l

Date:February 21 19 89

Work Order Project

tt 090033 Nabem

omer

23231232322323323234232352323623237232382323923240232402324123242232432324423245232462324723248232492324923250232512325223253232542325523256232572325823258

Goldppb

66612^^55^8^1.316585665

124119

148

1411^^^O10^

GoldOz/T

0.002 (0.002x: 0.002'C 0.002*; 0.002 c: 0.0020x002*C 0.002^.002^.002^.002t. 0.002*: 0.002K 0.002*; 0.002*; 0.002x: 0.002^.0.0020.004

x: 0.002s.. 0.002< 0.002^.002< 0.002s, 0.002*; 0.002( 0.002< 0.002^.002< 0.002*; 0.002

Check

Chec k

Chec k

Per:

ORIGINAL

1111111111111111111

fi ^

25

< \ Ac c ur a*

444510444511444512 444513444514444515 444516444517444518444518 444519444520444521 444522444523444524 444525444526444527444527 444528444529444530 444531444532444533444534 444535444536444536

LF-30



President: Dr. GEORGE DUNCAN, M.SC., PH. D., c. chem (Ont.i, c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of flnalysisMr. H.J. Hodge


SAMPLE NUMBERS

Page: 2

Date: February 21______ 19 89

Work Order tt s O90033 Project J Nabem

omer

232592326023261232622326323264232652326623267232672326823269232702327123272232732327423275232762327623277232782327923280232812328223283232842328523285

Goldppb

6O^8O5O266

171122057^2014^5

106

1710216

23O^56

GoldOz/T

<0.0024:0.002^.002^.002^.002^.002*; 0.002*; 0.002^.002*; 0.0020.003

'.-: 0.002^'0.002'.i 0.002< 0.002< 0.002^.002< 0.002< 0.002< 0.002K 0.002*; 0.002^C 0.002< 0.002< 0.002*: 0.002x: 0.002<0.002< 0.002*: 0.002

Check

Chec k

Chec k

Per:

ORIGINAL

1111111111111111111

ks

y&v^hk. Pres

26030 'i

SAMPLEAc cur assay

445037445038 44503944504044504 1445042 445043445044445045 445046445046445047445048 445049445050445051 445052445053445054 445055 445055445056445057 44505B445059445060 44506 1445062445063445064 445064

LF-30



President: Dr. GEORGE DUNCAN, M.SC., PH, D., c. Chem (Om.i, c. chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of RnolysisMr. H.J. Hodge


NUMBERSCustomer

23286232872328823289232902329123292232932329423295232952329623297232982329923300233012330223303233042330423305233062330723308233092331023311233122331323313

Page: l

Date: February 28 19 89

Work Order Project

090034 Dorothy Lake

Goldppb

137975

1,5'.-:s*;s5796

'C 57

*;s897898

1785567

11152113

GoldOz/T

-x 0.002*; 0.002*; 0.002*C 0.002*; 0.002< 0.002t. 0 , 002^1.002*: 0.002'' 0.002*:: 0.002*: 0.002*; 0.002•t 0.002K 0.002S. 0.002^:: 0.002^.002*; o . 002^.002-; o . 002*; 0.002K 0 . 002*: 0.002*; 0.002^.002^: 0.002'C 0.002^. 0.002^.002*'. 0 . 002

Chec k

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ORIGINAL

l111111111111111111

CA *\

26

Ac cur as

445065445066445067 445068445069445070 445071445072445073 445073 445074445075445076 445077445078445079 445080445081445082445082 445083445084445085 445085

LF-30



President: Dr. GEORGE DUNCAN, M.SC., Ph, o., c. chem (om.i, c. cham (U.K.i, M.C.I.C., M.R.s.c., A.R.C.S.T.

Certificate of AnalysisMr. H.J. Hodge

Geocanex Ltd. 1003-34 King Toronto, Ontario M5C-1E5

SAMPLE NUMBERSy Customer

233142331523316233172331823319233202332123322233222332323324233252332623327233282332923330233312333123332233332333423334

,st

Goldppb

18191223

81216121220141521IB2419

9171514

7175927

Page: 2

Date: February 28 19 89

Work Order tt : 090034Project : Dorothy Lake

GoldQz/T

^.002*: 0.002'O:i.002'C 0.002'i 0.002'.- 0.002•0X002^r. 0.002•OD. 002*; 0.002 Check•O:i.002*: 0.002^.0. OO2'.'0.002< 0.002-: 0.002t. 0.002*: 0.002O:i.002t. 0.002 Check*; 0.002-:: 0.002

0.002*; 0.002 Check

Per: un.

ORIGINAL

Ministry ofsNorthern Development and Mines

Report of Work

OntarioMining A

Name and ^^al Address of Recorded Holder

pf^se see attached52oa6sweee* is NABEMAKOSEKA LAKE 300

_____________l Please see attached

c/'o- 1003 - 34 King Street East Toronto, Ontario M5C 1E5Summary of Work Performance and Distribution of CreditsTotal Work Days Cr. claimed

for Performance of the following work. (Check one only)

Q Manual Work

DD

Shaft Sinking Drifting or other Lateral Work.Compressed Air, other Power driven or mechanical equip.

Power Stripping

] Diamond or other Core drilling Land Survey

All the work was performed on Mining Claim(s):Pa 913334, 913289, 913300, ?A33**y

Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below) f tfal3eiXAk*sejc

Contractors: Morrisette Diamond Drilling Ltd. Haileybury, Ontario

Core Size: BQ l 1/17"

Geologist in Charge: Eric Timoshenko, R.R. # 9 Brampton, On

Number of Holes: 7

Total Footage: 2,222 feet iXsiVa fas KfiOft S'i

Dates: January 27th, to

l?ja day qUsing Pa 913334

510 days

Certification Verifying Report of Work

ResprdM "Horder or Agent (Signature)

June 5th, 1989

l hereby certify that l have a personal and intimate knowledge of the facts set forth In the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report Is true. ^^~

Name and Postal Address of Person Certifying

H.J. Hodge 1003 - 34 King Street East Toronto, Ontario M5C 1E5Date Certified

June 5th, 1989Table of Information l Attachments Required by the Mining Recorder

Type of Work

Manual Work

Shaft Sinking, Drifting or other Lateral Work

Compressed air, other power driven or mechanical equip.

Power Stripping

Diamond or other core drilling

Land 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.

Signed core log showing; footage, diameter of core, number and angles of holes.

Name 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 hours of employment,

Names and addresses of owner or operator together with dates when drilling/stripping done.

Nil

Attachments

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

Work Sketch (as above) in duplicate

Nil

768 (85/12)

CLAIM NUMBER

P e^ ; 13290 13291 913304

913326913327913339

OWNER

J. Robert

NO.

R. Darveau

E 29771n

S 6095n

QREDITS^REOUESTED

858585

858585

Total 510 credits

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010 DIAMOND DRILLING WORK PERFORMED FOR: H.J ......Pa 913289 to 913310 (inclusive) 22 March 27, 1987...

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Transcript of 010 DIAMOND DRILLING WORK PERFORMED FOR: H.J ......Pa 913289 to 913310 (inclusive) 22 March 27, 1987...