sewell-reeves proj assay results re west blk drilling ...€¦ · tic u-.u reeves twp.,~u-r -...

42B01NE0085 2 .13263 PENHORWOOD

SEWELL-REEVES PROJECT

ASSAY RESULTS

RE:

WEST BLOCK DRILLING

PENHORWOOD TOWNSHIP

010

RECEIVEDAPR 30 1990

MINING LANDS SECTION

CONTENTS:

- copy of Report of Work

- claim sketch showing where assays were taken

- summary of assay sheets

- representative invoices

- breakdown of assays in drillholes by claim

- Technical Data Statement

- logs of drillholes with assays entered

plus: photo-reduced claim maplocation sketch at 1:5000

- assay sheets in chronological order.

2.13263

Dale R. Alexander Senior Exploration Geologist

//f

NORTH GF THE t mi. l e. POS.T

l*

Tic u-.u

REEVES TWP.

,~u

-r - —i— - -f-T

Head

S*' trai

ffff^ - Kartea

p]U( ^. co c, o o loo o o o10* V J C" 9 -

8888888IH -J'-o

t too MM

RODERT S. MIDDLETON EXPLORATION SERVICES INC.

GOLOROCK RESOURCES INC.

Cloim Mop Penhorwood Township

SEWELL-REEVES PROJECT

SUMMARY OF ASSAY SHEETS

WEST BLOCK DRILLING 1989

November 9

12

14

15

17

30

December 3

3

5

8

11

11

13 samples

36

31

58

38

48

58

64

28

78

75

80

607 samples

x $7.50 cost per assay

$4552.50 / $15 - 303.5 days credit.

All assaying was completed at the Holt-McDermott assay lab at a charge of $7.50 per sample a representative invoice signed by the Regional Exploration Manager is attached. The charge is all-inclusive of sample preparation and assaying. Since the assay rate is considerably less than a commercial lab, check samples and assays of additional elements are charged at the same $7.50 rate. All samples are assayed for gold in grams (or ppm).


American Barrick Resources CorporationHOLT-MCDERMOTT MINE

P.O. Box 278 * Kirkland Lake, Ontario * P2N 3H7 Telephone: l (705) 567-9251 * Fax: l (705) 567-6867

December 15, 1989

American Barrick Resources Corporation Exploration Division P. O. Box 1203 Kirkland Lake, Ont P2N 3H7

INVOICE #89-13

Assays November 1989

1630 at 7.50

Advertisement at 501

Less: U.P.S. collect charge

$12,225.00

125.00

512,350.00

(172.88)

INVOICE TOTAL ,177.12

Please make cheque payable to:

American Barrick Resources CorporationHolt-McDermott MineP. O. Box 278Kirkland Lake, Ont -tP2N 3H7 P- l *77f 6 u' *

D. Mitchell Chief Accountant

DM:rb

• t l' C. (•••II il II (k* ' t•l II t* * i *i . 'i ii tri i -• 1--LJ.J.I J-J-l.*-..l..k.

American Barrick Resources Corporation HOLT-MCDERMOTT MINE

P.O. Box 278 * Kirkland Lake, Ontario * P2N 3H7 Telephone: l (705) 567-9251 * Fax: l (705) 567-6867

January 16, 1990

American Barrick Resources Corporation Exploration Division P. O. BOX 1203 Kirkland Lake, Ont P2N 3H7

r,i JANlil ' B 1990

INVOICE 90-02

Assays December 1989

1648 at 7.50

Advertisement at 501

Invoice Total

$12,360.00

195.30

$12,555.30

Please make cheque payable to:

American Barrick Resources Corporation Holt-McDermott Mine P. O. Box 278 Kirkland Lake, Ont E2N 3H7

D. Mitchell Chief Accountant

DM:rb

P- Ho -

00

tt f.

Claim 950022

Claim 950021

Claim 950025

Claim 950027

Claim 950031

Claim 639978

Claim 924167

Claim 92416B

Breakdown of Assays in drillholes, by claim

DDH 12 upper part DDH 14 lower part

DDH 12 lower part DDH 13

DDH 14 upper part

DDH 15 upper part

DDH 15 lower part DDH 16

DDH 17

DDH 18

DDH 19

49 assays 41 assays

90 assays 45.0 days

95 assays 67 assays

162 assays 81.0 days

5 assays 2.5 days

18 assays 9.0 days

15 assays 84 assays

99 assays 49.5 days


88 assays 44.0 days

45 assays 22.5 days



Ministry ofNorthern Developmentand Mines

Ontario

Geophyslcal-Geologlcal-Geochemical Technical Data Statement

File..

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey(s) - Assaying Drill Core 77-19Township or Area - Penhorwood Township ,Claim Holder(s) American Barrick Resources Corporation l——

Optionee of Record ^—————-—————.———.Survey Company\merican Barrick —————^-————————————-—.—Author of Report - Dale !R. A1 pYH.nflm'' —-^^^^^-^—^.^———.———

Address of Author c /o Amen' nan 'Rn.vT'-i^'k K"i T*k-1 anrl j fnfcQ Ont-

Covering Dates of Survey Nov. Q, IQBO tn DPQ, 11 t IQftQ(linecutting to office)

Total Miles of Line Cut N/A ——....^.^^—^^————

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical—Electromagnetic.—Magnetometer^—Radiometric——

DAYSper claim

Geological.Geochemical.

AIRBORNE CREDITS (Special provision credits do not apply to airborne lurveyi)

Magnetometer. .Electromagnetic . Radiometric

DATE:

(enter days per claim)

SIGNATUR"Author of Report or Agent

Res. Geol.. .Qualifications.Previous Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSEDList numerically

***j*it************(prefix) (number)

.ssjaasa.....

l

TOTAL CLAIMS.

B37 (85/12)

INDUCED POLARIZATION

PFSTSTTVTTY GRAVITY ELECTROMAGNETIC MAGNETIC

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS — If more than one survey, specify data for each type of survey

Number of Stations Niimher nf Readingso Station interval Line spacing

Profile srale

Contour interval

Instrument

Arrurary — Srale rnnstant

Diurnal rorrertion method

Base Station rherk-in interval (hours)

Rase Station location and value

Instrument

Coj] rnnfignratinn

fVijl separation

Arrurary

Method: O Fixed transmitter d Shoot back D In line

Frequency(specify V.L.F. ttation)

Parameters measured

InstrumentScale constant

Torrertions made

Base station value and location . . ,,

Flevat-"

InstrumentMethod D Time Domain di Frequency DomainParameters On time ......, Frequency

Off time Range

Delay time— Integration time

Power ——— ——————————————————————————————————————————— — —— —Electrode array. ————————————— — — ———————————————————————— - —Electrode spacing . ———————— - ——————————————————————————————— — — — —

Type of electrode —————————— - ——————————————————————————— — — —

* I

1

1

1H

1

1D Parallel line

1

1

1

1

1

1

1

1

SELF POTENTIAL Instrument————— Range.Survey Method.

Corrections made.

RADIOMETRIC

Instrument.Values measured.Energy windows (levels). Height of instrument ——. Size of detector————. Overburden —-—-———-

.Background Count.

(type, depth — include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.)

Type of survey————————————————^^-——Instrument ——————-—————.—^^^^^^—^—Accuracy——————————————————————————Parameters measured.

Additional information (for understanding results).

AIRBORNE SURVEYS

Type of survey(s) ———— Instrument(s) —————

Accuracy—-——————-(specify for each type of survey)

Aircraft used.Sensor altitude.

(specify for each type of lurvey)

Navigation and flight path recovery method.

Aircraft altitude.Miles flown over total area.

.Line Spacing——

.Over claims only.

GEOCHEMICAL SURVEY - PROCEDURE RECORDl

Numbers of claims from which samples takpn Drillholes950031. 6^QQ78 r 921*167 r Qpln ffi

Tntal Niimhpr nf Samplps 607

TyppnfSamplp Split drill core(Nature of Material)

Avpragp Samplp Wpight .1 . ^ Irgc

Method of 001Iertion--d.iprr""vn ':' ^T* -5 1 1 -in r*— — J 1 o

Sni] Hnriznn SamplpH n/a

Hnri'/nn Dpvplnpmpnt n/a

Samplp Dppth variableTrrrain

Drainagp Dfvplnnrnpnt.Estimate Rangpnf Ovprhnrdpn Thirknpss 0 to 70m

SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)

Vfpsh sizp nf frarrinn nspH fnr analysis. -200 mesh

ppnfral The sample IR dvifidj nnishftfl (jivcrusher and cone crusher) and ispulverized (disc pulverizer) to-200 mesh.

on claims P.Q50022 r Q50021 T QSOOpq, 0.50027,,

ANALYTICAL METHODSValues expressed in: per cent D

p.p. m. Q p. p. b. D

Cu, Pb, Zn, Ni, Co, Ag, Mo, As.-(circle)

Othprs Au

FiplH Analysis (. , t^Kt?)

Extraction MpfhnH,

Analytiral MpthnH

Reagpnts IJspH

Field Laboratory AnalysisNo. ( .., tests)Kxtractinn Method.

Analytiral MpthnH

Reagpnts UspH

flommprrial I.ahoratory (. 607 tp^t?)

Namp nf I.ahnratnry, ,HnT t.-MfT)ormott

F.vtrartinn MpthnH Aqua reeiaAnalytiral MPthnH fire and AARpagPntsTWH flUX, AfWO^ WO^, HC1

General The sample is fluxed nnd fuspflto produce a gold bead whi nhis subsequently dissolved inAqua regi a ft.nd rfiRfl wit. ViAtomic Absorption.

1 1 1

1 1 1

1

1 1 1 1 1

1 1 1

1

'M

B.

^H

- W

KEIT

H

TOW

NS

HIP

PEN

HO

RW

OO

D

TOW

NS

HIP

^o

92.0ir, NORtH OF t* mite. P OS.T

o C *^K W Ul t^i! WU) ut til uj*tfi 8?888888 fS gf c * *. - ?

uiur. oo o oloo o o oROBERT S. MIDDLETON

EXPLORATION SERVICES I MC

GOLDROCK RESOURCES INC

CloJm Mop Penhorwood Township

AMERICAN BARRICK RESOURCES CORPORATION

ft..0 .0

180.0

-50.0

.0

230.4

ftziiuth:

Dip:

Elevation;

Length:

Measurement: Metric

Couents: Casing Pulled

Depth Aziiuth Dip

45.7291.44

DIAMOND DRILL RECORD

Section:

Core Size: BD

HOLE NO.t SR.89-12

Property: SEWELL - REEVES

Location: L2*OOE 17+50S

Date Started: October 31, 1989Date Completed! Noveiber 2, 1989Logged by: H. Bergeron

Depth Aziiuth Dip

-43.0-38.0

-Log Susaary-

137.16182.88

-34.0-32.0

Depth Aziiuth Dip

230.43 -31.0

.00 6.35 OVERBURDEN. 6.35 8.80 BASALT. 8.80 13.20 ULTRAMAFIC. 13.20 38.40 BASALT.

33.50 - 35.0 felsic intrusive. 38.40 42.25 BASALT, flow breccia. 42.25 56.75 ULTRAMAFIC.

50.10 - 52.45 BASALT. 56.75 84.30 BASALT.

56.75 - 57.55 BASALT weakly foliated. 57.55 - 58.05 tafic intrusive. 58.05 - 60.65 BASALT foliated. 60.65 - 61.55 felsic intrusive. 61.55 - 71.73 BASALT foliated intercalated ULTRAMAFIC.71.73 - 84.30 BASALT lassive.

84.30 103.65 ULTRAMAFIC.85.50 - 85.70 BASALT. 91.45 - 92.05 BASALT. 96.45 - 99.15 BASALT.

103.65 110.30 Felsic intrusive. 110.30 142.65 ARGILLITE ; 6REYHACKE.

114.70 - 115.30 graphitic ARGILLITE. 116.35 - 116.95 felsic intrusive. 124.60 - 130.85 foliated. 130.85 - 135.85 felsic intrusive. 135.85 - 138.85 graphitic ARGILLITE. 141.40 - 142.65 graphitic ARGILLITE.

142.65 145.95 Felsic intrusive. 145.95 185.35 ULTRAMAFIC.

fjt^*^*-^ VMERiQANIBARWCK

RESOURCES CORPORATION

AMERICAN BARRICK RESOURCES CORPORATION...................................... Hole n0i , 8R,8H2

Page No,i 2

f^v To ———————————Description———————————— Bnple Froi To Length Z Sul 6H Au g/t

145.95 - 148.0 silicified zone.148.0 - 153.5 chlorite talc carbonate schist.153.5 - 165.4 sheared ULTRAMAFIC.160.10 - 161.65 felsic intrusive.165.40 - 185.35 talc chlorite carbonateschist.170.90 - 171.28 LAHPRDPHYRE,175.70 - 176.0 LAMPROPHYRE.176.48 - 176.65 FAULT ZONE.

1B5.35 230.43 ULTRAMAFIC.190.7 - 200.3 BASALT.224.20 - 226.40 silicified brecciated zone.

230.43 END OF HOLE.

.00 6.35 OVERBURDEN

6.35 6.BO BASALT97433 7.BO 8.80 i.00 NIL .020 .02

Moderately hard, fine grained grey-green, noniagnetic •afic volcanic. Strongly chloritic, loderately ankeritic. Poorly veined. Barren of eineralization. There is a weak to loderate foliation at 35 to 45 degrees to the core axis.Lower contact is sharp at 40 degrees to the core axis. Froi B.3 to B.8, there are l to 3J ankerite - quartz veins, l to 3 M Nide, elongated along foliation.

8.80 13.20 ULTRAMAFIC97434 8.80 9.80 1.00 NIL .040 .0497435 12,20 13.20 1,00 NIL .070 .07

Moderately soft to soft, fine grained, tediui grey blue, noniagnetic, lassive ultramafic flow. Strongly chloritic, loderately talcose, noderately ankeritic. There are 2 to 42 ankerite veins as fracture filling at randoB angles.Barren of Mineralization. Locally there is a tteak foliation averaging 45 degrees to the core axis. Lower contact is sharp at 45 degrees to the core axis,

FTW

AMERICAN BftRRICK RESOURCES CORPORATION..................................... Hol e N0i , SR.89-12

Page No.t 3

j0 ———————————Description——————————— Saiple Froi To Length Z Sul 6H Au g/t

13.20 38.40 BASALT97436 13.20 14,20 1,00 NIL-TR .110 .1197437 14.20 15.20 1.00 NIL-TR .090 .09

Moderately hard, fine grained, lediui grey-green, weakly 97438 17,07 17.80 .73 NIL-TR .051 .07•agnetic froi 29.45 to 38.4, lassive to weakly foliated 97439 17.80 18.80 1.00 NIL-TR .080 .08•afic volcanic. 97440 29,00 30.00 1,00 NIL-TR .080 .08Moderately to strongly chloritic, weakly ankeritic 97441 32,50 33,50 1,00 NIL-TR .060 .06pervasively. There is a weak patchy biotitic alteration 97442 33.50 35.00 1.50 NIL-TR .060 .04fro* 14 to 17 *. There are trace, l to 2 M wide, white 97443 35.00 36.50 1.50 NIL-TR .090 .06ankerite veins. Fracture fillings. 97444 37.40 38.40 1.00 NIL-TR .050 .05There is nil to rare trace of very fine pyritedisseminated.The weakly developed foliation averages 45 degrees tothe core axis. Foliation is strongly contorted froi18.10 to 18.50. Lower contact is sharp at 60 degrees tothe core axis.14.02 17.07 : there are 0.85 i lost core. Mafic

volcanics are toderately fractured at 80 to85 degrees to the core axis,

17.07 17.80 : tafic volcanic are intercalated by a•oderately foliated talc - chlorite -carbonate schist. Foliation and contacts are45 degrees to the core axis, There are 51,2 to 5 li wide ankerite quartz veins pinchedalong foliation. Barren of lineralization.

32.50 32.70 : strongly fractured core at 85 degrees tothe core axis intercalated ilnor talc alongfractures.

33.50 35,00 Felsic intrusive. Hard, fine grained, lediuigrey, noniagnetic feldspar porphyry dyke.There are 52, white - beige hypidioiorphicfeldspars, 2 to 5 n wide. Unveined. Barrenof lineraliiation. Contacts are 45 to 70degrees to the core axis.

38.40 42.25 BASALT97445 38,40 39.40 1.00 NIL-TR .030 .0397446 39,40 40.40 1.00 NIL-TR .010 .01

Moderately hard, fine grained, grey brown, noniagnetic, 97447 41.25 42,25 1,00 NIL-TR .020 .02 •afic flow breccia. There are 10 to 252, 5 H to 2 ci wide angular to subangular fragients. Moderately chloritic, weakly biotitic. There are 12, l to 2 H, white calcite fracture fillings. There is nil to rare trace very fine pyrite disseminated. Contacts are 60 and 50 degrees to the core axis.


fm To -Description-

42. 25 54.75 ULTRAMAFIC

Moderately soft to soft, fine grained, lediui grey-blue,nonmagnetic, lassive ultraiafic floH. Stronglychloritic, loderately talcose, very weakly ankeritic.There are 2 to 41 ankerite veins as fracture fillings,There is nil to rare trace of pyrite disselinated. Lovercontact is veined at 45 degrees to the core axis,50.10 52.45 BASALT. Moderately hard, lediui

greenish-grey, noniagnetic tassive laficvolcanic. Strongly chloritic, very weaklyankeritic. There are IX ankerite veinsfracture fillings. There is nil to tracepyrite. Contacts are 45 to 60 degrees to thecore axis.

Hole No.! BR.89-I2 Page No.i 4

Sup l e Froi To Length l Sul 6H Au g/t

974489744997450974519745297453'

42.2549.1050,1051,1052.4555.75

43.2550.1051.1052.4553.4556.75

.00

.00

.00

.35

.00

.00

NIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TR

.040

.020

.010

.081

.070

.010

.04

.02

.01

.06

.07

.01

56.75 84.30 BASALT

56.75 57.55 BASALT weakly foliated. Moderately hard, very fine grained, noniagnetic, weakly foliated at 50 degrees to the core axis •afic volcanic, noniagnetic. Strongly chloritic, weakly ankeritic. Poorly veined. Barren of Mineral ization. Lower contact is 50 degrees to the core axis.

57.55 58.05 Mafic intrusive. Moderately hard, fine grained, noniagnetic, lassive tafic intrusive, Moderately chloritic, weakly biotitic, strongly calcitic. Unveined, barren of lineralization. Lower contact is foliated at 50 degrees to the core axis,

58.05 60.65 BASALT foliated. Moderately soft, fine grained, loderately foliated, lediui greenish-grey, noniagnetic lafic volcanic. Strongly chloritic, weakly ankeritic. There are lit, l to 2 H ankerite veins pinched along the foliation averaging 50 degrees to the core axis - they are frequently contorted. There are a few odd deciietric talc - chlorite - carbonate - schist sections. Barren of lineralization. Lower contact is 65 degrees to the core axis.

60.65 61.55 Felsic intrusive. Feldspar porphyry dyke. Sate as 33.50 to 35.0. Lower contact is irregular at 70 to 80 degrees to the core axis.

9745497455974569745797458974599746097461974629746397464

57.5559.6560.6561.5562.5563.5564.5569.7370.7371.7383.30

58.26 .7160.65 1.0061.55 .9062.5563.5564.5565.5570.7371.7372.9384.30

.00

.00

.00

.00

.00

.00

.20

.00

NIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-Tft

TR-1NIL-TR

.142

.070

.081

.020

.030

.050

.050

.130

.130

.132

.080

.20

.07

.09

.02

.03

.05

.05

.13

.1?

.11

.08


y0 ———————————Descripti on———————————

41.55 71.73 BASALT foliated. Intercalated ULTRAMAFIC. Moderately soft, aediui greenish-grey, fine grained, accurately foliated nonmagnetic•afic volcanic. Strongly chloritic, weakly ankeritic and calcitic. There are 2 to 51, ankerite - calcite veins pinched along foliation averaging 70 degrees to the core axis - frequently contorted. There is nil to trace pyrite.Foliated lafic volcanics are intercalated by 302 deciietric talc chlorite - carbonate schist sections. Lower contact is veined at 70 degrees to the core axis.

71.73 B4.30 BASALT tassive. Hediui green to greenish-grey, fine grained, nonmagnetic•afic volcanic. Strongly chloritic weakly carbonatized as ankeritic alteration with•inor patchy calcitic alteration. Poorly veined. There is nil to trace pyrite. Lower contact is veined at 40 degrees to the core axis. Froi 71.73 to 72.93 lafic volcanics are weakly foliated at 70 degrees to the core axis. There is trace to locally 1Z pyrite. Froi 74.20 to 77.70, aafic volcanics ire very weakly foliated at 70 degrees to the core axis with rare •icro-folding.

Hole No, t SR.89-12 Page No.t, 5

Saiple Froi To Length l Sul 6H Au j/t

84.30 103.65 ULTRAMAFIC

Moderately soft to soft, fine grained, tediui grey-blue, locally weakly Magnetic ultraiafic flow. Strongly chloritic, toderately talcose, weakly ankeritic. There are l!, l to 3 H ankerite veins filling fractures. There are nil to trace very fine pyrite blebs disseiinated. Lower contact is sharp at 75 degrees to the core axis. Locally ultraiafics are intercalated by a loderately soft, fine grained, noniagnetic, greenish-grey, lassive lafic volcanic. Poorly veined, barren of mineralization. 85.50 85.70 BflSftLT. 91.45 92.05 BASALT. 96.45 99.15 BASALT.99.70 103.65 : ULTRAMAFIC intercalated ii nor deciietric

weakly bleached and sericitic tafic volcanic bands. Lower contact is weakly biotitic froi 103.55 to 103.65.

97465 84.30 85.3097466 90.00 91.0097467 95.00 96.0097468 101,65 102.6597469 102.65 103.65

1.00 NIL-TR 1.00 NIL-TR 1.00 NIL-TR 1.00 NIL-TR 1.00 NIL-TR

.140

.150

.090

.050

.160

.14

.15

.09

.05

.16


To -Oescriptioo-

-—— Holeflo.J 6R.89-12Page No. i 6

Siiple Froi To Length Z Sal 6H Au g/t

103.65 110.30 FELSIC INTRUSIVE

Hard, ledius grey beige, noniagnetic feldspar porphry. Unveined. There is trace pyrite as fine euhedral grains disseiinated. Lexer contact is sharp at 30 degrees to the core axis.

110.30 142.45 AR6ILLITE

GREYWACKE.

Moderately hard to hard, thinly bedded alternating light grey and iediui grey to grey-green argillite intercalated linor greywacke. There is a neak to •oderate patchy lagnetisi. Weakly silicified and ankeritic. There are l!, l to 3 M graphitic beds along foliation. There is a weak sericitic alteration. Foliation subparallels the bedding at 60 to 70 degrees to the core axis.There are l i, l to 3 H xide carbonate-quartz veins filling fractures.There is trace to 31 pyrite and pyrrhotite as fine blebs or stringers disseminated along foliation. 110.30 114.70 : AR61LLITE l BREYHACKE are intercalated

by 3 to 52, 0.5 to 5 ci Hide graphitic argillite. Those graphitic beds contain 3 to 42 pyrrhotite, trace to 12 pyrite.

114.70 115.30 Graphitic ARGILLITE dark grey black,•oderately lagnetic. There is 2 to 52 pyrrhotite, 12 pyrite. Contacts are 66 and 70 degrees to the core axis.

116.35 116.95 Felsic intrusive. Hard, grey to grey brown coloured, feldspar porphyry. Neakly silicified and sericitic. There are 12 quartz-carbonate fracture fillings and trace very fine pyrite blebs disseiinated. Contacts are 85 and 80 degrees to the core axis,

121.85 124.60 : ARGILLITE l GREYWACKE are very thickly bedded. There are no graphitic beds. There is nil to trace disseiinated pyrite.

124.60 130.85 Foliated. Foliation is contorted and•icro-folded. Foliation varies froi 70 to 5 degrees to the core axis. There is trace to 12 pyrite and pyrrhotite disseiinated.

97470974719747297473974749747597476

974779747897479974809748197482974839748497485974869748797488974899749097491974929749397494974959749697497974989749997500975329753397534975359753697537975389753997540

103.65104.65105.65106.65107.65108.65109.65

110.30111.30112.30113.30114.70115.30116.35116.95117.95118.95119.95120.95121.65122.85123.85124.60125.60126.60127.60128.60129.60130.85131.85132.85133.85134.85135.85136.85137.85138.85139.85140.85141.40

104.65 .00105.65 .00106.65 .00107.65 .00108.65 .00109.65 .00110.30 .65

111.30 1.00112.30 1.00113.30 1.00114.70 1.40115.30 .60116.35 1.05116.95 .60117.95 1.00118.95119.95120.95121.85122.85123.85124.60125.60126.60127.60128.60129.60130.85131.85132.85133.85134.85135.85136.85137.85138.85139.85140.85

.00

.00

.00

.90

.00

.00

.75

.00

.00

.00

.00

.00

.25

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00141.40 .55142.65 1.25

TRTRTRTRTRTRTR

1-21-41-41-42-5

TR-1NIL-TR

TR-TR-TR-TR-TR-

NIL-TRNIL-TRNIL-TR

TR-TR-TR-TR-TR-TR-

TRTRTR

TR-1TR

5-255-252-3

TR-1TR-1TR-11-3

.030

.020

.020

.040

.040

.020

.026

.020

.060

.040

.084

.042

.063

.030

.070

.140

.040

.040

.054

.030

.040

.030

.050

.050

.040

.040

.060

.075

.060

.070

.060

.040

.050

.070

.060

.060

.070

.030

.033

.050

.03

.02

.02

.04

.04

.02

.04

.02

.06

.04

.06

.07

.06

.05

.07

.14

.04

.04

.06

.03

.04

.04

.05

.05

.04

.04

.06

.06

.06

.07

.06

.04

.05

.07

.06

.06

.07

.03

.06

.04


——————————Description———————————

This section is locally weakly lagnetic. There are a few odd deciietric sections brecciated along foliation planes.

130.85 135.85 Felsic intrusive. Hard, fine grained, noniagnetic, lediui grey to grey brow, feldspar porphyry. Weakly silicified. There are trace carbonate - quartz filled fractures. There is trace pyrite as fine euhedral grains disseiinated or coating fractures. Froi 133.85 to 133.93 there is an angular silicified, thinly bedded argillite/wacke fragment. Upper contact i t irregular. Lower contact is veined at 50 degrees to the core axis.

135.85 138.85 Graphitic ARGILLITE. Hard, very fine grained, dark grey black, loderately •agnetic graphitic argillite. Contacts are 45 and 60 degrees to the core am. There are trace carbonate filled fracture,

135.85 137.85 : there is 5 to 251 pyrrhotite, l to 31 pyrite, rare trace of chalcopyrite as recrystallized nodules or blebs. There are l to 31, l to 5 ci Hide dull grey cherty layers intercalated with the graphitic argillite. Foliation averages 70 degrees to the core axis but is locally contorted.

137.85 138.85 : silicified cherty argillite intercalated with 507,, i to 10 ci wide graphitic argillite beds. There is 2 to 31 pyrrhotite, l to 2Z pyrite. Foliation is 70 degrees to the core axis.

141.40 142.65 Graphitic ARGILLITE. Hard, dark grey black, very weakly to loderately lagnetic, graphitic argillite. Foliation subparallels the bedding at 65 to 70 degrees to the core axis. There are l to 3X, l ii to l ci wide carbonate - quartz veins disseeinated along foliation. There is i to 3! fine recrystallized pyrite disseiinated along foliation and associated with veining, and trace pyrrhotite.Contacts are sharp at 50 and 60 degrees to the core axis.

—-— Hole Ho. i SR.BH2Page No.i 7

Saiple Froa To Length l Sal BM Au g/t

142.65 145.95 FELSIC INTRUSIVE97541 142.65 143.65 1.00 TR .020 .0297542 143.65 144.65 1.00 TR .020 .02

^n To

AHERICAN BARRICK RESOURCES CORPORATION

-Description-

Hard, fine grained, aediui grey to grey brown, nomoagnetic feldspar porphyry. Neakly silicified. There are trace carbonate filled fractures. There is trace of very fine pyrite disseminated. Loner contact is sheared and is larked by a I D ci carbonate - quartz vein zone intercalated with si nor graphitic beds at 45 degrees to the core axis.

Hole No.i SR.B9-12 Page No.t . B

Suple Froi To Length l Sul 6H Au g/t

97543 M4.65 145.95 1.30 TR .039 .03


145.95 14B.OO Silicified zone. Hediui grey to grey bronn, hard, fine grained, noniagnetic, weakly foliated at 55 degrees to the core axis silicified zone. There is a weak talc alteration along foliation and a loderate pervasive calcitic alteration. Unveined. There is 1Z fine pyrite disseiinated. Lower contact is sheared at 60 degrees to the core axis.

148.00 153.50 ULTRAMAFIC. Moderately soft, dark grey blue to greenish grey, fine grained, weakly lagnetic, strongly foliated chloritic - talc - carbonate schist. Strongly chloritic, weakly talcose, noderately ankeritic. There are 6 to lOX, 2 to 10 H wide, grey white, ankerite quartz veins elongated along the foliation at 50 degrees to the core axis. There are a few odd centiietric barren quartz veins at randoi angles. There is trace pyrite as fine euhedral grains disseiinated. Froi 151.0 to 153.50 ULTRAMAFIC is intercalated by Bi nor deciietric silicified chlorite - carbonate - schist sections with li disseiinated pyrite.

153.50 165.40 Sheared ULTRAMAFIC. Hoderately soft, dark grey blue to greenish grey, fine grained, locally weakly lagnetic, sheared talc - chlorite - carbonate schist. Strongly chloritic and talcose, icderately ankeritic. There are 10 to 31, l to 4 H wide, grey white ankerite quartz veins foriing truncated laiellae pinched along the contorted foliation averaging 60 degrees to the core axis. There are i to 2X, white grey to white, 5 H to 1.5 ci wide quartz - ankerite veins pinched along

975449754597546975479754B9754997550975519755297553975549755597556975579755B9755997560975619756265493975639756497565975669756797568975699757097571975729757397574975759757697577

145.95146.95148.00149.00150.00151.00152.00153.50154.50155.50156.50157.50158.50159.50160.10160.85161.65162.65163.65163.71164.65165.40166.40167.40168.40169.40170.04170.90171.90172.90175.48176.48177.48183.35184.35

146.95148.00149.00150.00151.00152.00153.50154.50155.50156.50157.50158.50159.50160.10160.85161.65162.65163.65163.71164.65165.40166.40 i167.40168.40169.40170.04170.90171.90172.90173.90176.48177.48178.48184.35185.35

.00

.05

.00

.00

.00

.00

.50

.00

.00

.00

.00

.00

.00

.60

.75

.801.001.00.06.94.75.00.001.00.00.64.B6.00.00.00.00.00.00.00.00

11

TRTRTR

TR-1TR-I

TRTRTRTRTRTRTRTRTRTRTRTRTRTR

NIL-TRNIL-TRNIL-TR

TR-1NIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TR

.020

.021

.020

.030

.050

.050

.090

.060

.050

.070

.040

.030

.070

.030

.068

.040

.050

.040

.004

.047

.060

.080

.100

.150

.100

.051

.060

.190

.050

.050

.150

.050

.140

.140

.130

.02

.02

.02

.03

.05

.05

.06

.06

.05

.07

.04

.03

.07

.05

.09

.05

.05

.04

.06

.05

.08

.08

.10

.15

.10

.08

.07

.19

.05

.05

.15

.05

.14

.14

.13

AMERICAN 6ARRICK RESOURCES CORPORATION...................................... Hole No,! BR.89-12

Page No,i 9

j0 ..———..—.——Description-——-——————— Baiplc Froi To Length l Sul BM Au g/t

foliation. -Veining decreases downhole.There is trace pyrite as fine blebsdisseiinated. Lower contact is gradational.

160.10 161.65 Felsic intrusive. Hard, light grey whiteto grey, fine grained, nonmagneticfeldspar porphyry. Nonmagnetic. Moderatelysilicified, very weakly calcitic alongfractures. There is trace very finepyrite disseminated. There are a few oddcentimetric angular fragments noted.Contacts are irregular at 80 to 85 degreesto the core axis.

165.40 185.35 ULTRANAF1C. Moderately soft, dark greyblue to greenish grey, fine grained,nonmagnetic talc - chlorite - carbonateschist. Strongly chloritic and talcose,moderately to strongly carbonatized mostlyas ankeritic alteration except from 183.65to 385.35 where ULTRAMAFIC is stronglycalcitic, These are 2 to 51 carbonate -quartz veins pinched along the foliationaveraging 50 degrees to the core axis,There are li, white grey, barren, 0,5 to 2cm wide quartz - carbonate veins at randomangles. There is nil to trace pyrite asfine blebs disseminated. Lower contact isweakly sheared at 55 degrees to the coreaxis.

168.50 168.72 : quartz - carbonate vein, white grey togrey brown coloured, weakly brecciated.There is 11 pyrite as fine blebsdisseminated. Contacts are 50 and 80degrees to the core axis.

168.72 169.20 : moderately silicified, 'talc - chlorite -carbonate schist.

170.90 171.28 LAMPROPHYRE. Mottled dark grey brown,medium to coarse grained, lamprophyredyke. Very weakly magnetic, stronglycalcitic, moderately biotitic, Poorlyveined. Barren of mineralization. Contactsare 40 and 45 degrees to the core axis andare marked by 5 mm calcite veins.

175.70 176.00 LAMPROPHYRE. Same as 170.90 to 171.28except moderately magnetic. Contacts are30 and 45 degrees to the core axis,

176.40 176.46 : LAMPROPHYRE, same as above, very weaklymagnetic, contacts are irregular at 80 to85 degrees to the core axis.

176.48 176.65 FAULT 20NE. Strongly sheared talc -chlorite - carbonate schist intercalated 5cm of gouge. Contacts are 65 and 60degrees to the core axis.


To -Description-

Role No, f; SR.6H2 Page No./ 10

Saipli Froi To Length X Sul 6H Au g/t

IBS.35 230.45 ULTRAMAFIC

Moderately soft, dark grey to lediui grey-green, fine to •ediui grained, nonmagnetic, granular textured ultramafic floNs.Strongly chloritic, weakly talcose, loderately carbonatized as patchy calcitic and ankeritic alteration, There are i to 31, l to S ut Hide ankerite - carbonate veins pinched along a very weakly developed foliation at 60 to 70 degrees to the core axis. There are a few odd millimetric to centiietric quartz - carbonate veins disseminated at random angles. There is nil to trace very fine pyrite disseminated. 186,94 1B7.01 : LAHFROPHYRE dyke, contacts are SO and SS

degrees to the core axis.190.70 200.30 BASALT. Moderately hard, dark

greenish-grey, fine grained, nonmagnetic, massive mafic volcanic, Strongly chloritic, very weakly ankeritic, There are trace carbonate - quartz filled fractures. There is trace pyrite as fine euhedral grains disseminated. Contacts are diffuse.

202.40 203.00 : foliation is subparallel to core axis. 224.20 226.40 Silicified brecciated zone. Hard to

moderately soft, dull beige - grey to dark grey black, brecciated quartz - carbonate vein and l or felsic intrusive intercalated minor ULTRAMAFIC. Contacts of the zone are irregular and weakly sheared at 50 degrees to the core axis. There is trace to 12 pyrite disseminated along fractures, There are 40 to 70Z angular to subangular silicified fragments disseminated.

227.35 230.43 : ULTRAMAFIC coarse grained, light grey beige coloured, moderately to strongly talcose. There are 101, l to 2 mm chlorite clasts disseminated.

97578 185,35 186,3597579 186,35 187.3597580 189.70 190.7097581 190.70 191.7097582 199.30 200.3097583 200.30 201,3097584 209,00 210.0097585 211,00212.0097586 218,00 219,0097587 223,20 224.2097588 224.20 225.2097589 225.20 226.4097590 226,40 227.4097591 227.40 228.4097592 228.40 229.4097593 229,40 230,43

.00 NIL-TR

.00 NIL-TR

.00 TR-NIL

.00 TR

.00 TR

.00 TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 TR-l

.20 TR-l

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.03 NIL-TR

.050

.040

.040

.050

.060

.160

.120

.120

.040

.060

.140

.228

.110

.140

.140

.051

.05

.04

.04

.05

.06

.16

.12

.12

.04

.06

.14

.19

.11

.14

.14

.05

230.43 END OF HOLE.

-ffff

KEIT

H

TOW

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HIP

PEN

HO

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REEVES TWP. l

s II !KfRODERT S. MIDDLETON

EXPLORATION SERVICES INC.GOLDROCK RESOURCES INC



Aziiuth:

Dip:

Elevation:

Length:

.0 .0

180.0

-50.0

.0

184.7

Measurement: Metric

Coisents: Casing Pulled

Depth Ariiuth Dip

45.72 -50.0


Section: L2+OOE

Core Size: 6D

HOLE NO.l SR.89-13

Property: SEWELL REEVES

Location! L2+OOE W25S

Date Started! October 25, 198? Date Colpieted: October 31, 1989 Logged by: H. Bergeron

Depth Alieuth Dip

91,44 -48.0

Depth Aziiuth Dip

137.16 -4.6.0

-Log Suuary-

.00 2.65 CASING. 2.65 17.50 HIGH HAB BASALT. 17.50 34.30 BASALT. 34.30 73.10 HIBH NAB BASALT.

68.0 - 68.79 FAULT ZONE. 72.35 - 72.70 LAHPROPHYRE. 72.70 - 72.95 brecciated. 72.95 - 73.10 FAULT ZONE.

73.10 87.17 BASALT. 87.17 170.45 HIGH HAB BASALT.

122.75 - 125.5 CONGLOMERATE. 125.50 - 126.60 LAMPROPHYRE. 127.20 - 127.50 brecciated. 127.50 - 128.10LAHPROPHYRE. 135.10 - 137.95 LAMPROPHYRE. 137.95 - 138.61 brecciated. 142.95- 144.45 LAMPROPHYRE.

170.45 184.71 BASALT.170.45 - 174.10 aafic intrusive. 171.95 - 172.0 FAULT ZONE. 173.85 - 174.10 FAULT ZONE. 180.25 - 180.75 aafic intrusive.

184.71 END OF HOLE.


AMERICAN 8ARRICK RESOURCES CORPORATION

To -Description-

Hole No,i SR.69-13 Page No,t 2

Saiple Froi To Length l M 6H Au g/t

.00 2.65 CASING

2,65 17,50 HIGH HAG BASALT

Moderately hard, fine grained, tediui grey to grey-green, loderately to strongly lagnetic tassive lafic volcanic. Hoderately chloritic, weakly calcitic as patchy alteration, There are trace, i to 2 M carbonate - quartz filled fractures, Barren of nineralization. Lower contact is veined at 40 degrees to the core axis,

97372 10,00 11.00 1,00 NIL .070 .0797373 16.50 17.50 i.00 NIL .040 .04

17,50 34.30 BASALT

Hoderately hard, fine grained, light to aediui greenish-grey, noniagnetic lassive lafic volcanic, Hoderately to strongly chloritic, weakly ankeritic pervasively. There are trace, l to 2 11 carbonate - quartz filled fractures. Barren of lineralization, Lower contact is sharp at 45 degrees to the core axis.

97374 17,5097375 31,0097376 33,30

18.5032,0034,30

1,001.001,00

NIL NIL NIL

.090

.040

.140

.09

.04

.14

34.30 73.10 HIGH HAG BASALT

Hoderately hard, dark to tediui grey, fine grained, •oderately to strongly tagnetit, aassive tafic volcanic. Hoderately chloritic, weakly ankeritic. There are trace, l to 5 m carbonate - quartz filled fractures.

973779737B97379973BO9738197382

34.303B.OO39,0042,0053,0068,00

35.3039.0040.5043.0054.0069.00

.00

.00

.50

.00

.00

.00

NIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TR

.340

.040

.060

.090

.090

.030

.34

.04

.04

.09

.09

.03

ft,

AMERICAN BARRICK RESOURCES CORPORATION...................................... Hole No.i SR.89-13

Pige No.! 3

j0 ——————————Description——————————— Saiple Froi To Length I Bul 8U Au g/t

There is nil to trace pyrite as fine grained 973B3 69.00 70.00 1.00 N1L-TR .040 .04 disseminations or coating fractures. There is locally a 97384 71.35 72.35 1.00 NIL-TR .050 .05 very weak foliation at 45 to SO degrees to the core 97385 72.35 73.10 .75 NIL-TR .045 .05 axis. Loner contact is faulted. 3B.OO 38.40 : icderately fractured core at 50 to 60

degrees to the core axis. Moderate talcalteration along fracture planes.

39.80 40.30 \ strongly fractured and ground coreintercalated Minor calcitic gouge alongfracture planes. There is a loderate talcalteration.

42.10 42.60 : strongly fractured and ground core. Thereis a weak talc alteration.

68.00 68.79 FAULT ZONE. Strongly fractured coreintercalated ground sections. Heak talcalteration.

69.36 69.38 : fracture plane filled with gouge andgravel at 40 degrees to the core axis.

72^35 72.70 LAHPROPHYRE. Moderately hard, nottled darkgrey brown, lediui grained, icderately•agnetic, lassive laiprophye dyke. Stronglycalcitic, ioderately biotitic. There are IXcarbonate filled fractures, barren ofnineralization. Upper and lower contacts aresheared at 60 and 40 degrees to the core axis

72.70 72.95 Brecciated. Dark grey, very fine grained,noniagnetic, brecciated in-situ aaficvolcanic.

72.95 73.10 FAULT ZONE. Hud and gouge intercalated iinorgravel.

73.10 87.17 BASALT97386 73.10 74.10 1.00 NIL .040 .0497387 76.00 79.00 1.00 NIL .030 .03

Moderately hard, fine grained, light to lediui grey, 97388 86.17 87.17 1.00 NIL .110 .11 nonmagnetic lassive lafic volcanic. Moderately chloritic weakly ankeritic pervasively, unveined, barren of•ineralization.Nuterous decinetric strongly fractured and ground sections intercalated with iinor calcitic gouge noted at 73.80 - 74.30, 75.70 - 75.90, 77.07 - 77.35 and 77.6- 76.0. Fron 76.0 to 83.25 nafic volcanics are weakly to Moderately fractured.Loner contact is weakly fractured at 45 degrees to the core axis, lower contact is sharp and narked by a l m carbonate filled fracture at 35 degrees to the core axis.

AHERICAN BARRICK RESOURCES CORPORATIONHole No.! SR.89-13 Page No,i 4

POM To -Description-

87.17 170.45 HI6H HAS BASALT

Moderately hard, dark to lediui grey, fine grained,Massive, toderately Magnetic Mafic volcanic.Moderately chloritic weakly ankeritic. There are trace,l to 2 in carbonate - quartz filled fractures. There isnil to trace very fine pyrite disseminated.Lower contact is sharp at 40 degrees to the core axis.HagnetisM decreases froi Moderate to weak froi 166.0 to170.45.117.75 11B.40 ; weakly foliated at SO degrees to the

core axis, strongly calcitic.120.90 121.65 : light grey, weakly bleached noniagnetic

Mafic volcanic.121.65 122.75 : light grey to tediun grey , weakly

bleached lediui grained, calcitic, nontagnetic Mafic volcanic intercalated with a few odd lilliietric to centicetric, dark brown biotitic lafic dykes. Lower contact is sharp at 45 degrees to the core axis.

122.75 125.50 CONGLOMERATE. Moderately hard to hard, •ottled dark grey brown to beige, weakly to Moderately Magnetic, polyiictic congloMerate. There are 2 to 101, 0.5 CM to 7 CM wide, subrounded fragMents. Host of the fragMents are ultraiafic with trace olivine, there are a few Mafic, and finally there are trace feldspathic fragments at lower contact. Natrix is very fine to fine grained, strongly biotitic, Moderately calcitic. CONGLOMERATE is poorly veined and there is trace pyrite as very fine grains disseMinated. Lower contact is irregular at a high angle with core axis.

125.50 126.60 LAMPROPHYRE. Sane as 72.35 to 72.70. Lower contact is subparallel to core axis froM 126.10 to 126.60.

126.60 127.20 : Mafic volcanic, Magnetic, weakly calcitic along fractures. Lower contact is 60 degrees to the core axis.

127.20 127.50 Brecciated. Mafic volcanic, Magnetic, weakly brecciated in situ. Lower contact is 40 degrees to the core axis.

127.50 12B.10 LAMPROPHYRE. Sale as 72.35 to 72.70. Lower contact is subparallel to core axis froM 127.90 to 128.10.

132.B9 133.30 : brecciated calcite veins with intercalated subangular LAKPROPHYRE and

SaMple FroM To Length Z Sul GH Au g/t

973899739097391973929739397394973959739697397973989739997400974019740297403974049740597406974079740B974099741097411974129741397414974159741697417

87.96,

108.117.118.

1700007540

119.40120.40121.122.123.124.

65757575

125.50126.127.128.132.133.134.135.136.137.137.141.142.143.144.154.166.169.

6050101030101010109595959545000045

88.1797.00109.00118.40119.40120.40121.65122.75123.75124.75125.50126.60 !127.50128.10129.10133.30134.10135.10136.10137.10137.95138.95142.95143.95144.45145.45155.00167.00170.45

.00

.00

.00

.65

.00

.00

.25

.10

.00

.00

.75

.10

.90

.60

.00i. 20.801.001.001.00.851.001.001.00.501.001.001.001.00

NIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TR

TRTRTR

NILNIL-TR

NILNIL-TR

NILNILNILNILNILNIL

NIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TRNIL-TR

.050

.090

.070

.026

.040

.060

.162

.231

.150

.130

.082

.154

.081

.072

.100

.084

.032

.050

.140

.100

.042

.110

.110

.070

.025

.040

.040

.120

.040

.05

.09

.07

.04

.04

.06

.13

.21

.15

.13

.11

.14

.09

.12

.10

.07

.04

.05

.14

.10

.05

.11

.11

.07

.05

.04

.04

.12

.04


To -Description-

fragients. Contacts are 70 l 1 0 degrees to the core axis,

133.75 134.38 : there are l to 3X, D.S to 2 c* wide, brecciated carbonate veins with intercalated angular lafic fragients.

135.10 137.95 LAMPROPHYRE. Sate as 72.35 to 72.70. Upper contact is 5 degrees to the core axis, lover contact is 65 degrees to the core axis larked by a 26 ci wide brecciated carbonate - quartz vein intercalated Kith li angular LAHPROPHYRE fragients and with ninor lafic fragments.

137.95 13B.il Brecciated. Heakly brecciated in situ •afic volcanic tagnetic.

142.95 144.45 LAHPROPHYRE. Saie as 72.35 to 72.70. Contacts are 45 and 40 degrees to the core axis.

166,10 167.20 : dark green, loderately foliated at 45 degrees to the core axis, strongly chloritic HIGH HAG BASALT.

Hole No.t SR.89-13 Page No.i 5

Saiple Froi To Length l Sul 6H Au g/t

170.45 184.71 BASALT

Hoderately soft, very fine grained, lediuigreenish-grey, nonmagnetic lassive lafic volcanic.Strongly chloritic, loderately to strongly calcitic.There are trace to 21 carbonate filled fractures. Thereis nil to trace pyrite as fine euhedral grainsdisseminated.170.45 174.10 Mafic intrusive. Hoderately hard, lediu*

grained, dark to lediui grey-green to grey brown, nonmagnetic itafic intrusive. Strongly chloritic and calcitic, locally weakly biotitic. Poorly veined. There is trace disseiinated pyrite. Loner contact is faulted at 30 degrees to the core axis.

171.95 172.00 FAULT ZONE. Hud gouge at 45 degrees to the core axis.

173.00 174.10 : lafic intrusive is intercalated by a few odd deciietric talc - chlorite - carbonate schist sections.

173.85 174.10 FAULT ZONE. Lower contact is larked by a strongly sheared talc - chlorite - carbonate schist. Hinor gouge.

175.05 176.00 : weakly fractured lafic volcanic. Intercalated ei nor talcose alteration along fractures.

180.25 180.75 Hafic intrusive. Sane as 170.45 to 174.10.

97418 170.45 171.4597419 171.45 172.4597420 172.45 173.4597421 173.45 174.1097422 174.10 175.1097423 175.10 174.1097424 176.10 177.1097425 177.10 178.1097426 178.10 179.1097427 179.10 180.1097428 180.10 181.1097429 181.10 182.1097430 182.10 183.1097431 183.10 184.1097432 184,10 184.71

.00 TR

.00 TR

.00 TR

.65 TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 TR-1

.00 TR-1

.61 TR-1

.040

.030

.030

.020

.010

.010

.020

.040

.070

.060

.030

.040

.050

.030

.012

.04

.03

.03

.03

.01

.01

.02

.04

.07

.06

.03

.04

.05

.03

.02

AHER1CAN BARRICK RESOURCES CORPORATION

To -Description-

Hole No', l SR.89-13 Page No.! 6

Saiple Froi To Length X Sul 6H Au g/t

Contacts are 40 and 3D degrees to the core axis.

182.00 184.71 : there are trace to 1Z, l to 3 u wide, carbonate - quartz veins, white grey coloured. These veins contain li pyrite, trace chalcopyrite. Locally lafic volcanic is weakly folded and biotitic. Foliation is 45 to 50 degrees to the core axis.

184.71 END OF HOLE.

KEIT

H TO

WN

SHIP

PENH

ORW

OO

D TO

WN

SHIP

9HO *sb mUe.

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ANERICAN BARRICK RESOURCES CORPORATION

lords: .0 .0

Aziiuth: 180.0

Dip: -50.0

Elevation: .0

Length; 154.2

Measurement: Metric

Conents: Casing left in hole

Depth Aziiuth Dip

45.72 -51.0


Section: L2+OOE

Core Sizei BD

HOLE NO.! SR.89-14

Property! SEWELL REEVES

Location! L2+OOE 12*758

Date Started! Noveiber 3, 198? Date Coipletedi Noveiber 4, 1989 Logged byi H. Bergeron

Depth Aziiuth Dip

91.44 -51.0

Depth Aziiuth Dip

154.23 -52.0

-Log Sunary-

.0027.13 CAS1N6.

27.13 134.45 TUFF.

134.45 138.25 FOLIATED BASALT.

138.25 154.23 BASALT.

154.23 END OF HOLE.


Foi To -Description-

——— Hole No,! BR.89-14Page No,t 2


.00 27.13 CASING

Casing driven to 28.4 i.

27.13 134.45 TUFF

Moderately hard, light grey beige to beige tan, fine grained, poorly bedded to locally thinly laiinated not•agnetic aafic to intermediate tuff.The tuff is Heakly to toderately sericitic, loderatelyankeritic, weakly chloritic.There are trace carbonate - quartz filled fractures.There is trace pyrite as fine euhedral grains or blebsdisseiinated.Foliation subparallels the bedding it 40 to 5 degrees tothe core axis, averaging l OK angle Kith core axis.There are trace to 2X, lapilli-size fragients,subrounded, 2 H to 2 c* wide. Fragients and iatrixhave saie coiposition but fragients are stronglysericitic.5oie sections contain up to 20Z lapilli-size fragients,•atrix supported. In those sections, fragients vary froil to 6 ci.Lower contact is veined and contorted at 30 degrees tothe core axis.27.13 47.90 j foliation varies froi 40 to 10 degrees to

the core axis, soie sections arenicro-folded froa 16.8 to 47.9.

47.90 54.50 : foliation averages low angle with core axis 56.50 62.70 : there are 5 to 201 l apilli-size fragients.

Foliation averages 5 to 10 degrees to thecore axis.

62.70 101.20 : foliation averages low angle with core axis. Fro* BS to 88.7 there is a l ci quartz - ankerite sericitized vein pinched

97594 35.60 36.8097595 38.00 39.0097596 39.00 40.0097597 40,00 41.0097598 41,00 42.0097599 56.00 57.0097600 57.00 58.009760i 58,00 59.0097602 59,00 60.0097603 60.00 i 1.0097604 61,00 62.0097605 62,00 63.0097606 88,00 89.0097607 94,00 95.0097608 101,00 102,0097609 111,00 112.0097610 117,00 118,0097611 125.00 126.0097612 131,45 132,4597613 132,45 133.4597614 133,45 134.45

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

TRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTR

.060

.030

.060

.060

.080

.060

.060

.050

.050

.050

.070

.060

.110

.100

.130

.100

.120

.090

.090

.050

.110

.06

.03

.06

.06

.08

.06

.06

.05

.05

.05

.07

.06

.11

.10

.13

.10

.12

.09

.09

.05

.11


roi To -Description-

along foliation, barren of lineralization. Froi 94 to 94.35 quartz - ankerite sericitized veins, weakly brecciated, barren of lineralization.

101.20 101.80 ! there are 10X, lapilli-size fragments.Foliation averages 30 degrees to the coreaxis.

101.80 134.45 i foliation averages 30 degrees to thecore axis. There are l to 101,lapilli-size fragients, 2 M to l ci Hide.

Hole Ho.i SU9-14 Page No,i 3

Sup l e Froi To Length l Sal 6H Au g/t

134.45 138.25 FOLIATED BASALT

Moderately hard, very fine grained, light to lediui green, strongly foliated *afic volcanic. Not lagnetic. Moderately chloritic and ankeritic, Neakly sericitic. There are 2 to 5X, 0.5 to 2 ci Hide quartz ankerite sericitic veins weakly brecciated, subparallel to the contorted foliation. Foliation varies froi 30 to 5 degrees to the core axis. There is trace pyrite as fine blebs disseminated. Lower contact is gradational.

97615 134.45 135.45 1.0097616 135.45 136.45 1.0097617 136.45,137.45 1.0097618 137.45 138.25 .80

TR .160 .16TR .120 .12TR .070 .07TR .040 .05

138.25 154.23 BASALT

Moderately hard, very fine grained, light to lediuigreen, lassive to weakly foliated safic volcanic notlagnetic.Moderately chloritic, weakly calcitic and sericitic.There are trace, 0.2 to l ci wide quartz carbonate veinsas fracture filling. There are trace pyrite as fineblebs disseminated.138.25 147.85 : lafic volcanics are weakly foliated at

30 to 30 degrees to the core axis, There are few odd deciietric pale buff yellow sericitic sections, There are trace to IX, 0.5 to l c*, brecciated quartz veins noted.

147,85 150.85 : lassive BASALT.150.85 153.45 s altered BASALT, buff yellow colour,

strongly sericitic, weakly ankeritic.153.45 154.23 i lassive BASALT.

9761997620976219762297623976249762597626976279762897629976309763197632976339763497635

138.25139.25140.25141.25142,25143.25144.25145.25146.25147,25148,25149,25150,00150.85151,85152,85153,45

139.25140.25141.25142,25143.25144,25145.25146.25147.25148.25149.25

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00150.00 .75150.85 .85151.85 1,00152.85 1.00153.45 .60154.23 .78

TRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTR

.070

.050

.030

.080

.080

.040

.010

.010

.020

.050

.030

.030

.034

.150

.090

.006

.023

.07

.05

.03

.08

.08

.04

.01

.01

.02

.05

.03

.04

.04

.15

.09

.01

.03

154.23 END DF HOLE.

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ROBERT S. MIDDLETON EXPlOnATION SERVICES INC.J J J J J -l J


Claim Mop Penhorwood Township


.0 .0

180,0

-50.0

.0

154.2

Aziiuth:

Dip:

Elevation:

Length:

Heasureient! Metric

Coiients: Casing Pulled

Depth Aziiuth Dip

45.72 -51.0


Section: L6+OOE

Core Size: BQ

HOLE NO.t SR.B9-15B


Location: L6+OOE 4+OON

Date Started: Koveiber 6, 1989 Date Coipletedi Noveiber 15, 1989 Logged by: H. Bergeron

Depth Aziiuth Dip

91.44 -52.0

Depth Aziiuth Dip

154.23 -54.0

-Log Suiiary-

.00 69.49 OVERBURDEN.

69.49 154.23 ULTRAMAFIC.

86.0 - 92.10 BASALT.

154.23 END OF HOLE.

AMERlCAtfBARRICK RESOURCES CORPORATION


FrW To -Description-

Hole. No, i SR.89-I5B Page No. i 2

Saiple Froi To Length l Sul 6H Au j/t

.00 69.49 OVERBURDEN

69,49 154.23 ULTRAMAFIC

Moderately soft, fine grained, dark green to black,variably lagnetic, ultraiafic HON.There is trace to 51, 2 ci to 25 ci long ellipsoidalfracturing l polysuturing 1. Soie deciietric spinifex -textured flows are noted.Ultraiafics are strongly chloritic, weakly to loderatelytalcose and weakly carbonatized.There is 12, 0,2 to i ci wide, unite barren carbonate -quartz filled fractures.There is trace to nil very fine pyrite blebs disselinatedMagnetise is very weak froi 69.49 to 97,20. Froi 97.20to END OF HOLE lagnetisl is weak to toderate.71.40 72.05 : spinifex textured flows. Blebs are 0.5 to

l ti thick, l ci in length, There is i weak biotitic alteration,

77.55 77.85 : loderately fractured zone intercalated linor lilliietric gouge and gravel planes it 45 to 55 degrees to the core am.

79.00 79.30 : trace pyrite noted in carbonate - quartz filled fracture.

60.10 BO.30 : sane as 77.55 to 77.65,B3.50 83.90 : aoderately fractured zone. Intercalated

iinor lilliietric gouge and gravel planes at 75 to 85 degrees to the core axis.

85.77 85.90 : DIABASE. Fine grained, tediui grey brown, very weakly lagnetic. Trace very fine pyrite disseninated. Unveined. Contacts are sharp at 45 degrees to the core axis.

86.00 92.10 BASALT. Moderately hard, fine grained, dark grey-green, not lagnetic lassive tafic volcanic. Strongly chloritic, weakly to •oderately calcitic. There are 2 to 51, 2 u

97636 69.49 70,49 1.00 TR97637 70,49 71.40 .91 TR97638 71,40 72.05 .65 TR97639 72.05 73,0597640 77,00 78.0097641 78,96 79.9697642 79,96 60,9697643 83,00 64,0097644 85,00 86.0097645 66,00 67.0097646 87,00 88.0097647 68.00 69.0097648 89,00 90,0097649 90.00 91.0097650 91.00 92.1097651 92.10 93.1097652 96,00 97.0097653 98,00 99.0097654 104.00 105.0097655 109,00 110.0097656 115.00 116,0097657 lie, 00 119.0097658 120.00 121.0097659 126.00 127.0097660 132.00 133.0097661 138.00 139.0097662 140.00 141.0097663 143.00 144.0097664 151.00 152.0097665 152.00 153.00

.00 TR

.00 TR

.00 TR

.00 TR

.00 TR

.00 TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.10 NIL-TR

.00 NIL-TR

.00 TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.020

.055

.052

.030

.020

.250

.100

.120

.130

.110

.100

.100

.110

.160

.132

.120

.160

.110

.120

.120

.160

.120

.190

.260

.130

.120

.120

.190

.290

.190

.02

.06

.08

.03

.02

.25

.10

.12

.13

.11

.10

.10

.11

.14

.12

.12

.16

.11

.12

.12

.16

.12

.19

.26

.13

.12

.12

.19

.29

.19

AMERICAN BARRICK RESOURCES CORPORATION...................................... Hoi e HO ,, BR.B7-15B

Page No. i 3

Description ——————————— Saiple Froi To length X Sul BM Au g/t

to 5 ii Hide, Nhite barren, carbonate - quartz filled fractures. There i t n il to trace very fine pyrite disseminated, Contacts are weakly sheared at 60 to 70 degrees to the core axis.

86.75 87.00 88.20 88.60, 88.80 89.0 : strongly fracturedcore.

92.10 98.00 : fine to lediui grained ultramafic f ION, intercalated few odd, l to 10 ea Hide spinifex textured sections.

120.40 120.50 : icderately fractured core. Intercalated ei nor gouge and gravel at 65 degrees to the core axis.

126.33 126.50 : strongly fractured core intercalated 40Z gouge and gravel at 70 to 75 degrees to the core axis,

140.15 141.40 i spinifex textured f Ion.

154.23 END OF HOLE.

KEIT

H

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NSH

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PEN

HO

RW

OO

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PENHORWOOD TWP.

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92.0ift NOffH 6F THE b mi.le.

i Bromley

l Shiwini

nODERT S. MIODLETOH EXPLORATION SERVICES INC.

GOLOROCK RESOURCES INC

Claim Mop Penhorwood Township


rds:

Aziiuth:

Dip:

Elevation:

Length:

.0 .0

180.0

-50.0

.0

154.2

Heasureient: Metric

Contents: All casing lost in hole

Depth Aziiuth Dip

45.72 -50.0


Section: L6+OOE

Core Size: SO

Depth Aziiuth Dip

91.44 -47.0

HOLE NO.i SR.89-14

Propertyi SEKLL REEVES

Location: L6+OOE H25N

Date .Started! Noveiber 15, 1989 Date Completed! Noveiber 18, 1989 Logged byi H, Bergeron

Depth Aziiuth Dip

140.21 -45.0

-Log Sunary-

i

.00 18.29 CAS1N6 l OVERBURDEN. 18.29 54.10 BASALT.

28.45 - 3B.J5ULTRAHAFIC. 54.10 154.23 UNDIFFERENTIATED IRON FORMATION.

54.10 - 54.90 brecciated chert I silicifiedARGILLITE.54.90 - 58.50 graphitic ARGILLITE, brecciated,•ineralized.58.50 - 60.70 brecciated chert, lineralized.60.70 - 62.45 graphitic ARGILLITE brecciated,lineralized.62.45 - 65.7 brecciated chert l carbonateintercalated CONGLOMERATE.65.7 - 66.5 silicified SREYHACKE.66.5 - 152.B .chert / carbonate intercalatedninor tagnetite.152.8 - 154.23 graphitic ARGILLITE l chert.

154.23 END OF HOLE.



To -Description-

-—— Hole No.i BR.B9-16Page No.! 2

Saiple Froi To Length l Sul BH . Au g/t

.00 18.29 CAS1NB

OVERBURDEN.

16.29 54.10 BASALT

Hoderately hard, line grained, tediui grey togrey-green, noniagnetic, lassive lafic volcanic.Strongly chloritic, weakly calcitic as patchyalteration, weakly bleached, locally weakly talcosealong fractures planes.There are 3 to 31, 2 to 4 H Hide carbonate - quartzfilled fractures. There is trace very fine pyrite,disseiinated or coating fractures. Loner contact isveined at 45 degrees to the core axis.18.29 21.05 : cafic volcanic is intercalated fay a fen

odd centiietric brecciated sericitic layers. 21.05 22.25 : dark green, very fine grained, aassive

section, strongly calcitic. 28.65 38.15 ULTRAMAFIC. Moderately hard, black with

•ediuB grey Battling, locally very weakly•agnetSc, ultraiafic. There are 50)1, 2 to 5•t in size, tediui grey polygonal grains of antigorite. Strongly chloritic, weakly talcose along fractures. There are trace, l to 2 M ankerite vein fracture fillings. There are traces very fine pyrite and pyrrhotite blebs disseiinated or coating fractures. Contacts are 45 and SO degrees

97666976679766897669976709767197672976739767497675976769767797678976799768097681976829768397684976859768697687976889768997690

18.2919.2920.2925.6526.6527.6528.6529.6530.6531.6532.6533.6534,6535.6536.6537.6538.1539.1540.1541.1542.1543.1550.2051.2052.20

19.2920.2921.0526.6527.6528.6529.6530.6531.6532.6533.6534.6535.6536.6537.6538.1539.1540.1541.1542.1543.1544.1551.2052.2053.20

.00

.00

.76

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.50

.00

.00

.00

.00

.00

.00

.00

.00

.00

IRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTR

.170

.120

.084

.660

.110

.150

.060

.060

.060

.060

.040

.100

.090

.150

.040

.020

.100

.090

.160

.090

.140

.080

.090

.100

.080

.17

.12

.11

.66

.11

.15

.06

.06

.06

.06

.04

.10

.09

.15

.04

.04

.10

.09

.16

.09

.14

.08

.09

.10

.08



to the core axis.42.00 42.15 : sheared and brecciated section, strongly

chloritic and talcose. Contacts are SO degrees to the core axis.

42.80 44.15 : Moderately fractured zone intercalated •inor talc gouge and gravel. Fracture planes are 5 to 10 degrees to the core axis and 45 to 50 degrees to the core axis.

44.15 51.20 : rafic volcanic are weakly foliated at 45 to 50 degrees to the core axis.

51.20 54.10 : strongly bleached, weakly to toderately sericitic. Weakly foliated at 50 degrees to the core axis. There are a few odd yellow brown alteration stainings along fractures,

—-—- Hole No,i SR.B9-16Page No,i 3

Saiple Froi To Length X Sul 6N Au g/t

97691 53.20 S4.10 .90 TR .081 .09

54.10 154.23 ^DIFFERENTIATED IRON FORMATION

54.1054.90 Brecciated ARGILLITE to brecciated chert. Hard, very fine grained to aphanitic, lediui grey to dark grey, nonmagnetic. There are 401, 0.5 to 1.5 ci in size, subangular chert and quartz fragients in a silicified and cherty tatrix. There is 2 to 5Z pyrite as fine euhedral grains disseninated. Lower contact is 45 degrees to the core axis, narked by a 15 ci wide silicified wacke.

54.90 5S.50 Brecciated graphitic ARGILLITE, lineralized. Hard, very fine grained to aphanitic, dirk grey to black, nonmagnetic, brecciated graphitic ARGILLITE. There are 5 to 7Z, 0.5 to 3 ci in size angular chert fragients. Bedding is poorly developed at 50 degrees to the core axis. There is 5 to lOX pyrite as aggregated pyrite nodules elongated at 40 to 50 degrees to the core axis. Froi 56.85 to 5B.5 there is 50 to BOX pyrite, also as aggregated nodules.

58.50 60.70 Brecciated, chert, lineralized. Hard, aphanitic, light beige grey brecciated chert. Mineralized. Noniagnetic. There are 90 to 95J, 0.5 to 5 ci in size, subangular chert fragients. There is 5 to 101 very fine euhedral pyrite filling the interstices. 2 to 4X, l to 5 DI vugs are noted,

60.70 62.45 Brecciated graphitic ARGILLITE. Sale as 54.9 to 58.5. There is 2 to 51 pyrite as fine euhedral grains disseiinated or aggregated in fine stringers.

976929769397694976959769697697976989769997700977019770297703977049770597706977079770B97709977109771197712977139771497715977169771797718977199772097721977229772397724

54.1054,9035,9056,8557,8558,5059.5060,7061,7062,4563,4564,4565,7066,5067,5068.5069,5073,0078,0082,0086,0091,0092,0097.0098.0099.00100,00101,00102,00103.00106,00107,00108,00

54.90 .8055.90 1.0056.85 .9557.85 1.0058.50 .6559.5060.7061,7062,4563,4564.4565,7066.5067.5068.5069.5070,5074,0079.0083,0087.0092,0093.0098.0099.00100.00101.00102,00103,00104.00107.00108.00109,00

.00

.20

.00

.75

.00

.00

.25

.80

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

2-55-105-10

50-8070-805-105-102-52-52-82-61-41-2

TR-1TR-l1-31-2

TR-2TR-1

TRTR-1TR-3TR-3TR-1TR-11-3

TR-1TR-80TR-80

TRTR-1

TR-80TR

.160

.100

.076

.160

.104

.050

.072

.090

.045

.050

.070

.037

.056

.020

.040

.050

.030

.050

.030

.020

.280

.220

.120

.110

.100

.100

.060

.100

.120

.070

.120

.080

.090

.20

.10

.08

.16

.16

.05

.06

.09

.06

.05

.07

.03

.07

.02

.04

.05

.03

.05

.03

.02

.28

.22

.12

.11

.10

.10

.06

.10

.12

.07

.12

.08

.09

AHERICAN SARRICK RESOURCES CORPORATIONHole Ho,t 8R.89-16 Page No.: 4

rot To

62.45

65.70

66.50

. ————————— inscription —————————————

65.70 Intercalated CONGLOMERATE. Hard, aphaniticto fine grained, light beige grey to grey,poorly bedded at 45 degrees to the coreaxis, interbedded brecciated chert andcarbonate, intercalated Minor deciietric

^{ongloierate sections. There is 2 to 82pyrite as fine euhedral grains disseiinatedalong bedding or fragments. '

66.50 Silicified GREYWACKE. Hard, fine grained to•ediuf grained, noniagnetic, gediui greybrown coloured, thickly bedded at 45 degreesto the core axis strongly silicified wacke.

Lower contact intercalated Kith tinorcherty fragments. There is i to 21 pyrite asfine euhedral grains disseminated.

152.80 Chert 1 carbonate, local lagnetite. Hard,very fine grained, to aphanitic, banded

a*ipie

9772597726977279772B97729977309773197732977339773497735977369773797738977399774097741

rroi

109.00'111.00117.75119.00120.00124.00128.00131.00135.00141.00145.00149.00150.00151.00152.00I52.BO153.80

ID L

110.00112.00119.00120.00121,00125.00129.00132.00136.00142.00146.00150.00

sngin

.00

.00

.25

.00

.00

.00

.00

.00

.00

.00

.00

.00151.00 1.00152.00 1.00152.80 .80153.80 1.00154.23 .43

A aui

TRTR-60TR-3

TR-40TR-40

TRTRTRTR

TR-3TRTR

TR-1TR-1TR-12-52-5

DR

.070

.110

.262

.100

.100

.130

.030

.040

.020

.080

.070

.070

.080

.030

.096

.060

.047

HU

.07

.11

.21

.10

.10

.13

.03

.04

.02

.08

.07

.07

.08

.03

.12

.06

.11chert and carbonate, light grey to dark grey colour, variably lagnetic. Bedding is Nell developed at 45 degrees to the core axis. Interbedded layers of chert and siderite are froi 0.5 to 5 ci Hide. There are overall IX, 0.5 to l t* w ide lagnetite beds. There are a few odd centiMetric layers of silicified ARKOSE noted. Fragnentation of cherty layers is comon. This unit is strongly silicified ( cherty ) and carbonated. There are a fen odd quartz carbonate fracture fillings. There is trace to 3Z very fine pyrite aggregated along bedding with a fen odd decinetric seni-nassive nodular pyrite sections. There is nil to trace pyrrhotite associated with Magnetite beds.

101.40 101.70 : seii-Massive pyrite102.43 102.69 : seni-iassive pyrite107.91 107.99 J seii-iassive pyrite111.07 111.35 : seMi-nassive pyrite119.20 119.35 i seii-Massive pyrite119.90 120.95 : brecciated carbonate

nodular ). nodular ), nodular ). nodular ). nodular ).

intercalated seiiMassive pyrite and 5Z Magnetite.

152.80 154.23 Graphitic ARGILLITE with intercalated chert. Hard, dark grey black, very fine grained to aphanitic, nonitagnetic, graphitic argillite intercalated with Minor cherty layers. Thinly bedded at 45 degrees to the core axis. Strongly silicified, weakly calcitic. There is 2 to 51 pyrite as fine euhedral grains disseminated or aggregated along foliation. Foliation subparallels the bedding at 45 degrees to the core axis.


To -Description-

—~— Hole No, l SR.89-14Page No.: 5

Saiple Froi To Length Z Sul EH Au g/t

154.23 END OF HOLE.

**

I'-'iT'Tl. l f -r H —i- i -f"TT T—r—T,;

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nooEnr s. MIOOLETOHEXPlOnATIOH SERVICES IHC.

' GOLDROCK RESOURCES INC.


lun: AM M~|s'Hh;


.0

186.0

-50.0

.0

184.7

.0

Az i tilths

Dip:

Elevation:

Length:

Heasurenent: Metric

Coiients: Casing Pulled

Depth Azimith Dip

45.7291.44


Section: L48+OOE

Core Size: BQ

HOLE NO.: SR.S9-I7


Location: L48+OOE 6+25N

Date Started: Noveiber 20 ,1989 Date Coipleted: November 22, 1989 Logged byi H. Bergeron

Depth Aziiuth Dip Depth Aziiuth Dip

-50.0-49.0

-Lo; Sunary-

154.23184.71

-48.0-48.0

.00 3.00 OVERBURDEN. 3.00 57.40 GREYWACKE.

17.90 - 19.40 : ARGILLITE. 20.95 - 21.90 : ARGILLITE. 35.15 - 38.40 : CONBLOHERATE. 3B.40 - 47.00 : quartzose wacke. 47.00 - 57.40 : ARGILLITE intercalated linor 6REYHACKE.

57.40 64.70 Felsic intrusive. 64.70 68.88 CONGLOMERATE. 68.88 72.90 FAULT ZONE. 72.90 111.56 Mafic to intenediate volcanics.

72.90 - 77.60 foliated, weakly brecciated. 111.56 123.86 TUFF. 323.86 132.55 ULTRAMAFIC. 132.55 162.60 BASALT. 162.60 167.30 HIGH MAG BASALT. 167.30 173.90 BASALT.

168.40 - 169.02 felsic intrusive. 171.70 - 172.40 brecciated quartz - carbonate vein. 372.40 - 173.90 TUFF.

173.90 178.20 HIGH HAG BASALT.176.75 - 177.65 TUFF.

178.20 184.71 AMPHIBOLITE. 184.71 END OF HOLE.

AMERICANBARRICK RESOURCES CORPORATION


To -Description-

———- Hole H6.i SR.89-17Page No.i 2

Saiple Froi To Length l Sul 6N Au j/t

.00 3.00 OVERBURDEN

Casing reaned to 3.66 i,

3.00 57.40 GREYNACKE

Intercalated Ji nor CONGLOMERATE and ARGILLITE.A sequence of ioderately to strongly fracturedsediments. Greywackes are doiinant and containintercalated argillite and congloierate sections.Breywackes are loderately hard, greenish-grey colour,and are noniagnetic.Breywackes are poorly bedded at 50 to 55 degrees to thecore axis. They are granular textured with visiblerounded quartz and feldspar grains.There is a weak to noderate chloritic alteration and aweak carbonate alteration.There are a i e tt odd nillitetric carbonate veins andquartz carbonate veins as fracture filling.Foliation is weakly developed subparallel to the beddingat 50 to 55 degrees to the core axis.There is trace pyrite coating fractures.17.90 19.40 ARGILLITE. Moderately hard, dark grey black

to grey, very fine grained, nonmagnetic, argillite. Very weakly chloritic and carbonatized, poorly bedded at 55 degrees to the core axis. Unveined, weakly foliated at 55 degrees to the core axis. There is trace pyrite coating fractures.

20.95 21.90 ARGILLITE. Saie as 17.90 to 19.40.25.4035.15: GREYWACKE is weakly sericitic as

lillinetric bands disseiinated along

9774297743977449774597746977479774B977499775097751977529775397754977559775697757

11.0017.9032.1533.1534.1535.1536.1537.1538.4040.6043.0047.0048,0049.0055.4056.40

12.0016.9033.1534.1535.1536.1537.1538.4039.4041.6044.004B.OO49.0050.0056.4057.40

.00

.00

.00

.00

.00

.00

.00

.25

.00

.00

.00

.00

.00

.00

.00

.00

TRTRTftTRTR

TR-lTR-1TR-1TR-1TR-1TR-1

NIL-TRNIL-TRNIL-TRNIL-TRNIL-TR

.170

.110

.130

.240

.090

.130

.060

.550

.070

.070

.040

.060

.070

.240

.090

.050

.17

.11

.13

.24

.09

.13

.08

.44

.07

.07

.04

.06

.07

.24

.09

.05

^™l

AMERICAN BARRICK RESOURCES CORPORATION...-................................. Hole No.i SR.B9-17

Page No,: 3

,JD ———————.———Description——————-———— Snple Froi To Length l Sul 8N Au g/t

foliation. Sons dedietric sections arelediuR to light grey coloured and are weaklycalcitic and sericitic.

35.15 38.40 CONGLOMERATE. Moderately hard,greenish-grey, noniagnetic congloierate.Fragients are polyiictic and latrixsupported. They are composed Mainly of 2 to4 m sub-rounded quartz and lafic clasts.Matrix is loderately chloritic and veryweakly calcitic. Foliation subparallels thebedding at 55 to 60 degrees to the coreaxis. There are trace quartz carbonateveins, 2 to 5 M wide, at randoi angles.There is trace to IX pyrite coatingfractures or as fine grains disseiinated.

38.40 47.00 : quartzose wacke. Moderately hard, lightgrey to grey-green, noniagnetic, poorlybedded at 60 degrees to the core axisquartzose wacke. There is a weak sericiticalteration along foliation. Sediments ireunveined. There is trace to H pyrite asfine blebs disseiinated. Foliationsubparallels the bedding at 60 degrees tothe core axis.

41.60 47.00 : quartzose wacke intercalated Kith a IBModd deciietric wacke/argillite sections,

47.00 57.40 ARGILLITE intercalated linor 6REYMACKE.Moderately hard to loderately soft, lightgrey to dark grey argillite, noniagnetic.There is a weak patchy silicification andsericitic alteration. Froi 49.0 to 50.20 theargillite is strongly sericitic. Argilliteis intercalated by a few odd deciietricwacke sections. There are nil to tracequartz carbonate veins as fracture filling.There is nil to trace pyrite as very fineblebs disseiinated.

57.40 64.70 FELSIC INTRUSIVE97758 57.40 58.40 1,00 NIL-TR .050 .0597759 60.00 61.00 1.00 NIL-TR .020 .02

Hard, very fine grained to aphanitic, light grey to 97760 63.00 64.00 1.00 NIL-TR .100 .10 greenish grey, noniagnetic felsic intrusive. There are 97761 64.00 64.70 .70 NIL-TR .070 .10 trace to 21, l to 4 ci quartz phenocryst*. There is a weak calcitic alteration along fractures. There are trace quartz - carbonate filled fractures and nil to trace very fine pyrite disseiinated. There is locally a weak foliation developed at 55 degrees to the core axis. This unit is weakly fractured but is intercalated with

AMERICAN BARRICK RESOURCES CORPORATION...................................... HolB H|j t , 8Ri8H7

Page No. t 4

Poi To ———————————Description——————————— Snple Froi To Length I Sul 6H Au g/t

5*, 10 c* to 20 ci) (tide zones of ground core.Lower contact is sharp and weakly graphitic at 70degrees to the core axis.

64.70 68.88 CONGLOMERATE97762 64,70 65.70 i.00 TR .120 .1297763 65.70 66.70 1.00 TR .120 .12

Moderately hard, greenish-grey to light grey, 97764 66.70 67.70 1.00 TR .210 .21 noniagnetic congloierate. Fragients are polyiictic and 97765 67.70 68.88 i.IB TR .106 .09 latrix supported. They are composed lainly of 5 u to 2 ci subangular fragments of felsic, quartz, and lafic volcanic composition.Matrix is loderately chloritic, there is a weak pervasive calcitic alteration. Conglonerate is unveined. There is trace very fine pyrite disseiinated. Foliation and bedding are poorly developed at 60 degrees to the core axis. Lower and upper contacts are irregular and brecciated. Congloaerate is intercalated by a few odd, 5 to 10 ci wide felsic intrusive dykes.

68.88 72.90 FAULT ZONE97766 66.88 69.86 1.00 NIL-TR .040 .0497767 69.88 70.88 1.00 NIL-TR .060 .06

Soft, iediim greenish-grey, nonmagnetic, sheared and 97768 70.88 71.88 1.00 NIL-TR .050 .05 faulted zone. There are 75 to 85* polyiictic fragients 97769 71.86 72.90 1.02 NIL-TR .061 .06 latrix supported. Fragients are coiposed of 2 H to 8 m rounded quartz and felsic laterial with linor 5 n to 1.5 ci subangular lafic caterial and rare quartz carbonate clasts. Matrix is a calcitic gouge. Foliation is 60 to 70 degrees to the core axis. There are rare traces of fine pyrite disseiinated. Contacts are sharp at 70 degrees to the core axis.

72.90 111.56 MAFIC VOLCANICS97770 72.90 73.90 1.00 TR-1 .160 .1697771 73.90 74.90 1.00 TR-I .060 .06

Moderately hard, lediui grey-green to greenish grey, 97772 74.90 75.90 1.00 TR-1 .110 .11fine grained, noniagnetic, nassive lafic to intermediate 97773 75.90 76.90 1.00 TR-1 .050 ,05volcanics. 97774 76.90 77.60 .70 TR-1 .056 .08Weakly to loderately chloritic, noderately ankeritic 97775 77.60 78.60 1.00 TR .080 .08pervasively. There is a weak patchy sericitic 97776 82.00 83.00 1.00 TR .080 .08alteration. There are trace to H, 2 to 5 n wide, white 97777 85.00 86.00 1.00 TR .080 .08quartz carbonate fracture fillings. There are traces of 97778 90.00 91.00 1.00 TR .050 .05



very fine pyrite blebs disseiiinaled. Lower contact it sharp at 70 degrees to the core axis. 72.90 77.60 Foliated and weakly brecciated. Breenish

grey volcanics, toderately foliated it S to 70 degrees to the core axis. There is a weak brecciation, with a toderate light green chlorite - sericite alteration along the S in to 2 ci subangular fragients. There are IX, grey white, S li to l c* wide quartz reins, pinched along foliation. There are trace to 1Z very fine pyrite blebs dissednated.

77.60 94.18 : greenish grey sections. There are 2 to 4Z, 2 ci to 15 ci wide, sericitic bands, dull beige grey in colour. These sericitic bands are cononly weakly brecciated in situ.

94.18 96.80 : iediui grey section. There are 5 to lOX, 0.5 to 1.5 us carbonate specks disseiinited. There are trace to l i lediu* grained pyrite blebs disseiinated.

96.80 97.70 : dark green lafic volcanic, very fine grained, noniagnetic, lassive. Strongly chloritic, very weakly calcitic. There are IX, quartz - carbonate filled fractures. There is trace to 1Z pyrite as iediui grains disseminated.

97.70 105.00 : iediui grey-green section, Upper contact is icderately to strongly calcitic until 99 i. There are a few odd, 2 i* to I ci wide sericitic bands at 70 to 80 degrees to the core axis. Froi 101.0 to 102.0 and 103,0 to 104.0 volcanics are very weakly brecciated, with sericitic alteration along the subangular fragnents.

105.00 106.80 : lediuii grey to grey-green section. There are 5 to 10Z, 0.5 to 1.5 n carbonate specks disseainated.

106.80 109.35 : brecciated. Hediui grey to grey-green weakly brecciated in situ volcanics. There are trace to locally 2Z, 0.5 to 3 c* subangular volcanic fragients within a strongly chloritic and loderately sericitic satrix.

109.35 111.56 : tediui grey-green section, very fine grained, weakly sericitic pervasively.

Hole No.t SUH7 Page No.i 5

Sup l s Froi To Length l S ul 6M Au g/t

9777997780977819778297783977B497785977B697787977889778997790

93,1894.1895.8096.8097.70101.00103,00106.80107.80108.80109.35110.35

94.18 195,1896,8097.7098,70102,00104,00107.80108.80109,35110,35111,56

.00

.00

.00

.90

.00

.00

.00

.00

.00

.55

.00

.21

TRTR-1TR-1

1TRTRTRTRTRTRTRTR

.060

.100

.090

.117

.050

.050

.050

.110

.070

.022

.040

.097

.06

.10

.09

.13

.05

.05

.05

.11

.07

.04

.04

.08

111.56 123,86 TUFF97791 111.56 112,56 1.00 TR .120 .1297792 112.56 113.56 1.00 TR .060 .06

lVi

AMERICAN BARRICK RESOURCES CORPORATIONHole No.: SR.BH7 Pige No.i i

tot To

i i ii i

———————————— Description ————————————

Moderately hard, light grey beige to greenish grey,mafic to intenediate tuff-breccia.There are 10 to 252 subrounded fragients, 2 li to 2 ciwide, conposed of intemediate volcanics, quartz andni nor chert. The catrix is fine grained.There is a soderate chloritic and sericitic alterationNithin the aatrix. There is a weak calcitic alterationpervasively.There are trace, white grey coloured, 2 M to 1 ci Hidequartz carbonate vein fracture fillings.There is trace pyrite as fine blebs disseiinated.Sericitic alteration decreases downhole. Lower contactis sheared and veined at 70 degrees to the core axis.

saipie rroi 10 LI

97793 113.56 114.5697794 114.56 115.5697795 115.56 116,5697796 116.56 117.5697797 117,56 118.5697798 118.56 119.5697799 119.56 120.5697800 120.56 121.5697801 121.56 122,5697802 122.56 123.86

ingin

.00

.00

.00

.00

.00

.00

.00

.00

.00

.30

1 SUI

TRTRTRTRTRTRTRTRTR

TR-3

b*

.090

.120

.080

.070

.060

.110

.150

.170

.050

.793

RU

.09

.12

.08

.07

.06

.11

.15

.17

.05

.61


Moderately soft, fine grained, lediui grey black, noniagnetic, lassive ultraiafic fl OK. Strongly chloritic, weakly talcose, loderately ankeritic pervasively. There are 5X, 0.5 to 2 M wide, ankerite veins filling fractures or pinched along the weakly developed foliation at 65 to 70 degrees to the core axis. There are a few odd 0.5 to l ci wide, white, quartz ankerite veins at rando* angles. There are nil to rare traces of pyrite as fine blebs disseninated. Fro* 127.40 to 127.45 and 127.80 to 127.83, ultrasafics are intercalated with gouge and gravel planes at 60 to 75 degrees to the core axis. Lower contact is sheared and veined at 65 degrees to the core axis.

97803 123.86 124.8697804 127.00 128,0097805 131,55 132.55

1,00 NIL-TR 1.00 NIL-TR 1.00 NIL-TR

.050

.070

.030

.05

.07

.03

132.55 162.60 BASALT

Moderately hard, fine grained, dark green to green,noniagnetic tassive eafic volcanic. Strongly chloriticand calcitic pervasively,There are 2 to 5! carbonate - quartz filled fractures.Fro* 132.55 to 133.80 and 144.30 to 149.30 there are 10to 15X carbonate - quartz filled fractures.There is trace pyrite as fine euhedral grainsdisseminated. Fro* 149.10 to 149.20 and 151.60 to 151.80there is 31 pyrite as fine blebs or euhedral grainsassociated with carbonate - quartz veins.Lower contact is fractured at 65 degrees to the core axis

97806 132.55 133,5597807 138,00 139.0097808 145.00 146.0097809 148.00 149.0097810 149.00 150.0097811 151.00 152.0097812 155.00 156.0097813 159.00 160.0097814 161.60 162.60

1,00.00.00.00.00.00.00.00.00

TRTRTRTR

TR-3TR-3

TRTRTR

.060

.040

.060

.090

.060

.OSO

.080

.100

.OSO

.06

.04

.06

.09

.06

.05

.08

.10

.05

l ili ii

AHERICAN 8ARRICK RESOURCES CORPORATION...................................... Hole NO.J SR.89-17

Page No.i 7

Proi To ———————————Description——————————— Saiple FroM To Length l Sul 6H flu j/t

162.60 167.30 HIGH HAS BASALT97B15 162,60 163.60 i.00 NIL-Tft .060 .06 97816 U6.30 167.30 1.00 NIL-TR .060 .06

Moderately hard, fine grained Massive flow, weakly tostrongly Magnetic. There are trace to 52, l n to l ciwide, very fine Magnetite beds filling fractures. Thereis a strong chloritic and calcitic alteration pervasivelyThere are 2 to 5Z carbonate - quartz filled fractures.There is nil to trace pyrite as fine euhedral grainsdisseeinated. Lower contact is diffuse.

167.30 173.90 BASALT97B17 167.30 168.40 1.10 NIL .055 .05 97818 168.40 169.02 .62 TR .043 .07

Moderately hard, dark green to rediui grey, noniagnetic 97819 169,02 170,02 1.00 NIL .040 .04 itafic volcanic. Strongly chloritic, Moderately calcitic 97820171,70172,40 .70 1-2 .035 .05 pervasively. There are l to 31 carbonate - quartz filled 97821172,40173.90 1.50 NIL .060 .04 fractures.There are 5 to 202, l to 2 MR in size, carbonate specks disseminated.Barren of Mineralization. Pros 167.30 to 167.70, BASALT is weakly brecciated. 168.40 169.02 Felsic intrusive. Hard, very fine grained

to aphanitic, orange grey colour,noniagnetic. There is a weak sericiticalteration along fractures. There are 2X,i to 6 ci wide ankeritic - quartz veins at40 degrees to the core axis. There istrace pyrite as fine euhedral grainsdisseninated. Contacts are veined at 50 y40 degrees to the core axis.

371.70 172.40 Brecciated quartz - carbonate vein. Hard,very fine grained to aphanitic, weaklyMagnetic. There are 60 to 70Z, 5 MM to 2CM in size, subangular grey blue colour,quartz - carbonate vein fragients in achloritic - sericitic - calcitic Matrixwith intercalated Minor Magnetite, Thereis l to 21 f ine euhedral pyritedisseninated. Contacts are sharp at 25and 55 degrees to the core axis.

172.40 173.90 TUFF. Hard, fine grained, light grey greento pinkish grey colour, nonmagneticintemediate tuff. Poorly bedded at 50degrees to the core axis. There is a weak


rot To -Description-

silicification and heiatisation pervasively. There are l to 2X, 0.5 to 5.0 ci Hide, pinkish white coloured, quartz ankerite veins at SO to 60 degrees to the core axis. TUFF is barren of •ineralization. Lower contact is sharp at 50 degrees to the core axis.

•—— Hole No, i SUM?Page No,: B

Saiple Froi To Length X Sul GH Au g/t

173.90 178.20 HIGH HAS BASALT

Saie as 162.6 to 167.3. Lower contact is veined at 70degrees to the core axis.176.75 177.65 TUFF. Sane as 172.4 to 173.9 except there

are l!, 0.5 to 0.2 ci wide, quartz ankeritic veins. Contacts are 55 degrees to the core axis.

97B22 173.90 174.9097823 175.75 176,7597824 176.75 177.6597825 177.65 178.20

1.00 NIL-TR1.00 NIL-TR.90 NIL.55 NIL-TR

.050 .05

.040 .04

.036 .04

.050 .09

178.20 184.71 AMPHIBOLITE

Hard, fine grained to cediui grained, dark brownishgreen, loderately to strongly lagnetic hornblendicanphibolite.There is a toderately to weakly calcitic alterationdecreasing downhole. There is a weak patchy heiatitealteration, and a noderate chlorite alterationpervasively. There is a weak sericitic alteration alongfractures.There are 3 to 52, l to 5 u wide, carbonate - quartzfilled fractures and a few odd, l to 5 H wide quartz -hematite veins at randoi angles.There is trace to 51 p yrite as very fine points or blebsdisseninated.Upper contact is weakly foliated at 50 degrees to thecore axis.

97826 178.20 179.2097827 179.20 180.2097828 180.20 181.2097829 1B1.20 182.2097830 182.20 183.2097831 183.20 184.2097832 184.20 184.71

1.00.00.00.00.00.00.51

TRTR

TR-11-51-3

iTR

.040

.040

.080

.360

.040

.060

.005

.04

.04

.08

.36

.04

.06

.01

384.71 END OF HOLE.

*^Q

PENHORWOOD TWP.'- -i '- L —L -J

AU IH t*t VH iot jjj

K\ NOtTH fcF THE mi. \ e, PQS.T

ROBERT S. MIDDLETON EXPLORATION SERVICES INC.




Nsi

Aziiuth:

Dip:

Elevation:

Length:

.0 .0

186.0

-50.0

.0

154.2

Measurement: Metric

Coments: Soie casing lost in hole

Depth ftiiiuth Dip

45.72 -49.0


Section: L60+OOE

Core Size: BQ

HOLE NO.i SR.89-18

Property SEWELL REEVES

Location: L60+OOE 5*25N

Date Started: Deceiber l, 1989 Date Coipleted: Deceiber 5, 1989 Logged by: H, Bergeron

Depth AziMth Dip

91.44 -49.0

Depth AzUuth Dip

154.23 -48.O

-Log SuMary-

.00 31.39 OVERBURDEN.31.39 42.65 Mafic to intertediate volcanic. 42.85 66.28 BASALT. 66.28 70.00 Graphitic FAULT ZONE. 70.00 74.85 6REYHACKE l ARGILLITE. 74.85 81.50 Graphite intercalated graphitic ARGILLITE -

FAULT 20NE.81.50 86.05 Volcanic breccia. 86.05 88.70 Altered BASALT. 88.70 91.75 Quartz - feldspar porphyry.

89.10 - 89.12 fault plane. 91.75 104.00 ULTRAMAFIC. 104.00 115.50 CONGLOMERATE. 115.50 127.06 CARBONATE ZONE.

125.75 - 127.06 CONTACT ZONE. 127.06 154.23 SYENITE. 154.23 END OF HOLE.

AMERICAN-BARRICK RESOURCES CORPORATION

AMERICAN BfiRRICK RESOURCES CORPORATION

Froi To -Description—

Hole llo.i BR.8H8 Page No.i 2

Saiple Froi To Length Z Sul 6H Au g/t


31.39 42.85 MAFIC VOLCANICS

Moderately hard, fine grained, lediui greenish grey, noniagnetic. Volcanics are tassive, intercalated by a few odd, 5 to 10 c* Hide, brecciated zones. In those zones volcanic fragients are 0.5 to 2 c* wide, angular, and are supported by a dark green black chloritic latrix. Volcanics are strongly chloritic and noderately calcitic pervasively. There are 2 to SI, l to 5 H quart; - carbonate filled fractures. There is nil to trace pyrite as fine blebs disseninated, and rare pyrrhotite traces within brecciated zones. Lower contact is sharp and veined at 45 degrees to the core axis,

97833 34.0097834 37.5097835 41.85

35.0038.5042.85

1.00 NIL-TR i.OO NIL-TR i.00 NIL-TR

.040

.020

.010

.04

.02

.01

42.85 64.2B BASALT

Hoderately hard, fine grained, dark grey to lediui grey nonnagnetic lassive BASALT. Hoderately to strongly chloritic, loderately carbonatized as calcitic alteration froi 42.85 to 53.6 and downhole as ankeritic alteration.There are trace to IX, quartz carbonate filled fractures. There are IX, 0.5 to 2 ci, quartz - carbonate reins at 50 degrees to the core axis. There is trace pyrite as fine blebs disseminated. 63.80 66.28 : BASALT toderately foliated at 45 degrees

to the core axis with intercalated linor graphitic alteration along foliation planes.

Lower contact is larked by a 30 ea

9783697837978389783997840978419784297843

42.8547.5051.0054.0059.0062.8063.8064.80

43.8548.5052.0055.0060.0063.8064.8066.28

.00

.00

.00

.00

.00

.00

.00

.48

TRTRTRTRTRTRTRTR

.020

.230

.080

.140

.120

.110

.080

.104

.02

.23

.08

.14

.12

.11

.08

.07

Froi

AMERICAN BARRICK RESOURCES CORPORATION...................................... HoleNd.i SR.89-18

Page No,t 3

roi To ———————————Description——————————— Saiple Froi To Length l Sal 6H Au g/t

brecciated QUARTZ VEIN ZONE, There are 60Z white grey to pink, angular quartz carbonate veins. Matrix is aoderately graphitic.

46,2B 70.00 FAULT ZONE97844 68,28 69,28 1,00 TR-3 .O&O .0697845 69.28 70.00 .72 TR-3 .036 .05

Graphitic,Intercalation of ground graphite and lediui grey strongly fractured intermediate volcanic. Intenediate volcanics are very fine grained, weakly silicified, barren of lineralization and contain 101, 0.2 to 0.5 ci quartz filled fractures. Graphite appears as gouge ceienting 0.2 to 0.5 ci Hide quartz vein fragments or as strongly fractured and brecciated centiietric pieces intercalated Kith 10Z fragmented quartz veins.There is trace to 32 pyrite as fine blebs disseminated along quartz veins. There are 2 i lost core.

70.00 74.85 GREYWACKE97846 70.00 71,00 1.00 TR .090 .0997847 71,00 72,00 1,00 TR .080 .08

Intercalated ARGILLITE. 97848 72,00 73.00 1.00 TR .060 .06 Moderately hard, very fine grained to fine grained, 97849 73,00 74,00 1,00 TR .270 .27 •ediui grey to dark grey, poorly bedded wacke 97850 74.00 74.85 .85 TR .059 .07 intercalated Kith linor graphitic argillite. Ueakly chloritic, weakly calcitic as patchy alteration. There are trace to 3X, l to 3 in carbonate specks disseminated.There is a weak graphitic alteration along fractures. Sediients are poorly veined. Foliation subparallels the bedding at 45 degrees to the core axis. There is trace pyrite as fine blebs or nodules disseiinated. Lower contact is fractured.

74.85 81.50 FAULT ZONE97851 74.85 75.85 1.00 TR .070 .0797852 75,85 76,85 1.00 TR .050 .05

Graphitic with intercalated graphitic ARGILLITE. 97853 76,85 77.85 1.00 TR-4 .060 .06 Mediui grey to black colour. Graphite with intercalated 97854 77,85 78,85 1,00 TR-4 .060 .06 graphitic ARGILLITE. Graphitic ARGILLITE is thinly 97855 78.85 79.85 1.00 TR .040 .04

^w

AHERICAN BARRICK RESOURCES CORPORATION-— — — — "—— -— •—••— •"••- Hols KOil sRtBvlB

P*ge No. i 4

Description ——————————— Saiple Froi To Length l Sul 6H ;' Au g/t

bedded at 50 degrees to the core axis and weakly 97656 79,85 BO. 85 1,00 IR .050 .05fractured along foliation planes. 97857 80,85 81,50 .65 TR .072 .11There are l to 42, l to 3 DU Hide, quartz veins alongfoliation. There is trace pyrite as fine euhedral grainsdissetinated.Graphite is strongly fractured, unveined, barren offtineralization,Froa 74.85 to 78.5 graphitic ARBILLITE is intercalatedwith 30 to 407., 10 to 30 c* wide sections of graphite.Frog 77.55 to 78.03, there is l to 4! pyrite as fineblebs associated Kith quartz veining.Fro* 78.50 to 81.50 graphitic ARBILLITE.Loner contact is veined and graphitic at 5 degrees tothe core axis.

Bl.50 86.05 VOLCANIC BRECCIA97858 81,50 82,50 1.00 TR .040 .0497859 82.50 83,50 1,00 TR .060 .06

Moderately hard, aottled tediui green and dark grey 97860 83,50 84.50 1,00 TR .090 .09 green, noniagnetic volcanic breccia. 97861 84,50 85,50 1,00 TR .120 .12 There are 60 to 70Z, 0.5 to 5 c* in size, dull beige 97862 85,50 86,05 .55 TR .017 .03 green coloured, subangular, unstratified and unsorted fragments of intermediate volcanic. Weakly sericitic. Matrix is coiposed of subrounded fragments i to 5 H in size.Those fragments are cainly quartz, tafic to intenediate volcanic and feldspar, Accessory graphitic ARGILLITE subangular fragients are noted. Matrix is strongly chloritic and very weakly graphitic, The volcanic breccia is unveined. There is trace pyrite as fine blebs disseainated within the latrix. Lower contact i s ground.

86.05 88.70 BASALT97863 86.05 87.40 1.35 TR .067 .0597864 87,40 88.05 .65 NIL .039 .06

86.05 87.40 : loderately hard, very fine grained, dark 97865 88,05 88.70 .65 NIL .026 .04grey to brownish grey weakly sericitic taficvolcanic, noniagnetic, Moderatelychloritic, weakly carbonatized. Unveined,weakly foliated at 60 degrees to the coreaxis. There is trace pyrite as fine blebsdisseainated. Upper contact is weaklybrecciated.

87.40 88.05 ; hard, very fine grained, light to lediuigrey, weakly sericitic and silicified *afic


To -Description-

volcanic, nonmagnetic. Poorly veined, barren of lineralization, weakly foliated at 60 degrees to the core axis.

3.05 88.70 : loderately hard, dark grey to greenish grey, loderately chloritic, weakly carbonatized lafic volcanic. Nonmagnetic, lassive. There are 3 to 52, 5 H to l ci Hide QUARTZ-CARBONATE VEINs at randoi angles. Barren of lineralization.

——- Hole No.i SR.B9-18Page No.i S


88.70 91.75 QUARTZ - FELDSPAR PORPHYRY

Moderately hard, fine grained, light to lediui grey, nonmagnetic. There are 52, l to 2 M quartz phenocryst^ in a feldspathic groundtass.There are l to 21, 2 M to i ci Hide, QUARTZ-CARBONATE VEINs disseiinated along foliation. There is nil to trace pyrite as fine blebs disseiinated. Felsic intrusive is weakly sheared and foliated at 50 to 60 degrees to the core axis.Locally weakly brecciated with lilliietric chloritic veinlets filling fractures.89.10 89.12 Fault plane. Intercalated gouge and gravel.

Contacts are 40 l 70 degrees to the core axis Lower contact is sheared at 60 degrees to the core axis.

97866 B8.7097867 89.7097868 90.70

89.7090.7091.75

1.00 NIL-TR i.00 NIL-TR (.05 NIL-TR

.050

.040

.063

.05

.04

.06


Moderately soft, dark blue grey, fine grained, weaklylagnetic talc - chlorite - carbonate - schist.Strongly chloritic and carbonatized, weakly talcose.There are 5 to iOX, l to 2 H wide carbonate veins lankeritic ) pinched along foliation or as fine specksdisseiinated along foliation.There are a few odd 2 it to i ci wide QUARTZ-CARBONATEVEINs crosscutting the foliation at 70 to 50 degrees tothe core axis.Foliation is strongly developed at 65 degrees to thecore axis. There is nil to trace pyrite as fine blebsdisseiinated. ULTRAMAFIC is intercalated with a few odddecinetric light beige green talc - carbonate schistsections.Froi 100 i to 104 i : talc - carbonate - schist.Lower contact is larked by a 22 ci, dull white - beige,

97869 91.75 92.7597870 92.75 73.7597871 93.75 94.7597872 94.75 95.7597873 95.75 96.7597874 96.75 97.7597875 97.75 98.7597876 98.75 99.7597877 99.75 100.7597B78 100.75 101.7597879 101.75 102.7597880 102.75 104.00

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.00 NIL-TR

.25 NIL-TR

.030

.040

.040

.040

.060

.070

.060

.010

.020

.050

.130

.050

.03

.04

.04

.04

.06

.07

.06

.01

.02

.05

.13

.04


————————————Description——-

sugary textured, quartz ankerite vein.

Hole No.i SR.B9-18 Page No.i 6

Sample From To Length Z Sul GH Au g/t

104.00 115.50 CONGLOMERATE

Moderately hard to hard, lottled grey-green, greenishyelloM and beige grey, polymictic congloierate, fragmentsupported.CONGLOMERATE is poorly sorted and poorly bedded at 45 to50 degrees to the core axis.There are two average sizes of fragments. One iscomposed of i to 5 ci, subrounded to subangular, maficto intermediate sericitic volcanics, and rare quartz.Those represent 20 to 252 of the conglomerate.The second is coiposed of 2 mm to 2 c*, subrounded,quartz, cafic to intermediate sericitic volcanics, andlithic fragments.There is a strong sericitic alteration and a moderateankeritic alteration with rare fuchsite alteration.There are nil to trace quartz carbonate filled fracture.There are rare traces of fine to medium grained euhedralpyrite disseminated.104.00 l05.OB : medium grey to dark grey conglomerate.

The fragments are 2 M to 5 M in size. 115.35 115.50 : loner contact is marked by a graphitic

ARGILLITE thinly bedded at 60 degrees tothe core axis.

97881 104.00 105.0697882 105.08 106.0897883 108.00 109.0097884 112.00 113.0097885 114.50 115.50

,OB NIL-TR.00 NIL-TR.00 NIL-TR.00 NIL-TR.00 NIL-TR

.054

.050

.050

.070

.060

.05

.05

.05

.07

.06

115.50 127.06 CARBONATE ZONE

Moderately hard, mottled light green to medium green andgreenish beige. Strongly carbonatized zone of possiblyultramafic conposition. Noniagnetic.There is a strong ankeritic and sericitic alterationpervasively. There is a weak patchy fuchsite alteration.There are 52 ankeritic quartz vein stringers.There is trace pyrite as very fine points or euhedralgrains disseminated.125.75 127.06 CONTACT ZONE. Moderately hard, very fine

grained, nonmagnetic, dark green black coloured ultramafic. Strongly ankeritic, Heakly sericitic pervasively. There are trace ankerite quartz vein fracture fillings. There is nil to trace pyrite as fine blebs disseminated.

9788697887978889788997890978919789297893978949789597B9697897

115.50116.50117.50118.50119.50120.50121.50122.05123.05124.05125.05125.75

116.50117.50118.50119.50120.50121.50122.05123.05124.05125.05

.00

.00

.00

.00

.00

.00

.55

.00

.00

.00125.75 .70127.06 1.31

TRTRTRTRTRTRTRTRTRTRTRTR

.060

.100

.050

.090

.120

.100

.039

.050

.060

.140

.105

.157

.06

.10

.05

.09

.12

.10

.07

.05

.06

.14

.15

.12

AHERICAN BARRIE RESOURCES CORPORATION

To -Description-

—-™ Hole No,: SR.89-18Page No.i 7

Saiple Froi To Length Z Sul GH Au g/t

127.06 154.23 SYENITE

Hard, line grained, *ediui pinkish tan to greenish pinktan colour, noniagnetic syenite.There is a strong and pervasive ankeritic alteration anda ioderate patchy sericitic alteration.There are l to 3X, white grey coloured, 2 to 5 li wide,ankerite quartz veins elongated along foliation qrfilling fractures.There is trace pyrite as very fine euhedral grainsdisseminated.There is a weak foliation developed at 50 to 55 degreesto the core axis.150.70 154.23 : SYENITE is

Interstices betweenNith chloritic•agnetic aaterial.

weakly brecciated.fragients are filled

- heiatitic, weakly

97896 127.06 128.06 1.0097699 128,06 129.06 1.0097900 129.06 130.0697901 132,00 133.0097902 135.00 136.0097903 139.00 140.0097904 141,00 142,0097905 144,00 145.0097906 147.00 148.0097907 148.70 149.7097908 149.70 150.7097909 150.70 151.7097910 151,70 152.7097911 152,70 153.70

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.00

.0097912 153.70 154.23 .53

TRTRTRTRTRTRTRTRTRTRTRTRTR

TR-2TR

.070

.140

.150

.060

.110

.090

.120

.050

.080

.090

.060

.060

.100

.060

.026

.07

.14

.15

.06

.11

.09

.12

.05

.08

.09

.06

.06

.10

.06

.05

154.23 END DF HOLE.

li

ar\

*o

*4

REEVES TWP. l

"T "Hi™ .W.

ROOEnT S. MIDDLETON EXPLOnATIOH SERVICES INC." J -*^-JJJJJ i-




ords; .0 .0

Aziiuth: 166.0

Dips -50.0

Elevation: .0

Length: 154.2

Measurement; Metric

Conents: Casing lost in hole

Depth Aziiuth Dip

45.72 -49.0


Section: L60+OOE

Core Size: BD

HOLE NO.! SR.89-19

Property! SEWELL REEVES

Location: L60+OOE 2+50S

Date Started: Deceiber 5, 1989 Date Coipleted: Deceiber 7, 19B9 Logged by: H. Bergeron

Depth Aziiuth Dip

91.44 -49,0

Depth Aziiuth Dip

152.40 -48,0

-Log Sunary-

.00 20.42 OVERBURDEN.

20.42 354.23 BASALT.20.42 - 125.50 fine to lediui grained lassiveflON,

92.13- 93.17 felsic intrusive.104.5 - 105.73 very fine grained tassive HDM,105.73 - 109.76 felsic intrusive.125.50 - 154.23 very fine grained toaphanitic lassive fION.

154.23 END OF HOLE.


AMERICAN CARRICK RESOURCES CORPORATION

To -Description-

-—— Hole No.i SR.8H9Page No.; 2



CASING reaned to 21.95.

20.42 154.23 BASALT

20.42 125.50 Fine to lediui grained tassive fION. A sequence of loderately hard, fine grained to lediui grained ( dark greenish-grey to green coloured aassive lafic volcanic. The sequence is in general nonmagnetic. Froi 37 to 44.5 there are a few odd weakly to•oderateiy lagnetic centiietric sections containing trace very fine lagnetite stringers or grains di sseni ruled. Mafic volcanics are strongly chloritic, noderately to strongly calcitic, and there are trace to 5X fine leucoxene grains disseiinated. There are i to 51, unite to white grey coloured, 2 M to i ci Hide quartz - carbonate vein fracture fillings. There are a few odd, white to unite grey coloured, I H to 5 a wide sugar textured quartz - carbonate veins at 45 to 80 degrees to the core axis. There is trace pyrite as•fine blebs or euhedral grains disseminated.

23.03 23.10 i ground core. There is a yellON brown alteration staining.

71.BO 72.23 : dull grey to beige grey sericitic section,73.15 75.60 : dark green to beige grey section. There is

a federate patchy sericitic alteration along veining and fractures.

92.13 93.17 Felsic intrusive. Hard, Bottled lediui beige grey and green, noniagnetic. There are 10 to 152, 2 ci to 5 M in size, chlorite porphyroblast* in a fine grained quartz feldspar groundmass. There is a strong

979139791497915979149791797918979199792097921979229792397924979259792697927979289792997930979319793297933979349793597936979379793897939979409794197942979439794497945

23,5030.5040.5043.1048.0052.0061.0066.5071.5072.5073.5074.5075.5081.0088.0091.1392.1393.1794.1797.00101.00104.50105.73106.73107.73108.73109.76110.76111.76115.00120.00,124.50125.50

24.5031.5041.5044.1049.0053.0062.0067.5072.5073.5074.5075.5076.5082.0089.0092.1393.1794.1795.1798.00102.00105.73106.73107.73108.73109.76110.76111.76112.76116.00121.00125.50126.50

.00

.00

.00

.00

.00

.00

.00

.00

.00f.OO.00.00.00.00.00.00.04.00.00.00.00.23.00.00.00.03.00.00.00.00.00.00.00

TRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTRTR

NIL-TRNIL-TRNIL-TRNIL-TR

TRTRTRTRTRTRTR

.070

.070

.090

.050

.050

.140

.080

.050

.200

.130

.110

.120

.280

.250

.170

.150

.697

.210

.110

.100

.130

.381

.150

.110

.090

.175

.130

.160

.430

.100

.100

.040

.080

.07

.07

.09

.05

.05

.14

.08

.05

.20

.13

.11

.12

.28

.25

.17

.15

.17

.21

.11

.10

.13

.31

.15

.11

.09

.17

.13

.16

.43

.10

.10

.04

.08

AMERICAN BARRICK RESOURCES CORPORATION .............................,........

Pace No.t 3

j0 ———————————Description——————————— Sap]e From To Length l Su) BU Au g/t

calcitic alteration. There is trace pyrite 97946 126.50 127.50 1.00 TR .080 .OBas fine euhedral grains disseminated. This 97947128.50129.50 1.00 TR .110 .11section is unveined and there is a weak 97948 134.00 135.00 1.00 TR .070 .07foliation developed at 50 degrees to the 97949 136.00 137.00 1.00 TR-2 .070 .07core axis. Contacts are sharp at 55 degrees 97950140.00141.00 1.00 TR .060 .06to the core axis. 97951 142.50 143.50 1.00 TR-2 .060 .06

104.50 105.73 Very fine grained lassive flow. Moderately 97952 147.00 148.00 1.00 TR-2 .060 .06hard, medium green, very fine grained 97953 151.50 152.50 t.00 TR-2 .100 .10•assive flow. Strongly chloritic andcalcitic pervasively. Unveined except forthe upper contact tarked by 10Z, 5 M to lci wide, white coloured quart! - carbonateveins at 45 degrees to the core axis.There is trace pyrite as fine blebsdisseminated. Lower contact is sharp at 85degrees to the core axis.

105.73 109.76 Felsic intrusive. Hard, lottled beige-pinkand green at the contacts and tottiedbeige grey and green toward the center ofthe intrusion. This section isnon*agnetic. There are 5 to lOX, 2 H to5 M in size chlorite porphyroblasts in afine grained quartz feldspar groundmass.There is no reaction with HO. There aretrace, 5 u to 2 ci wide, sugary texturedquartz - carbonate - chlorite veins atrandoi angles. There is nil to tracepyrite as fine blebs disseminated. Lowercontact is sharp at 60 degrees to the coreaxis.

125.50 154.23 Very fine grained to aphanitic. Massiveflow. A sequence of loderately hard,•ediui greenish grey coloured, nonmagnetic, massive mafic volcanic. Hafic volcanics are strongly chloritic and moderately to strongly calcitic pervasively. There are trace to 2t, 2 to 5 mm quartz - carbonate filled fractures and a few odd, white grey coloured, 5 mm to 2 cm in size quartz veins at random angles. Those veinlets locally contain trace to 21 p yrite and magnetite as fine euhedral grains. In this section, there is trace pyrite as fine blebs, or euhedral grains disseminated. The sequence is uniform and massive. From 146 m to end of hole mafic volcanic intercalated with rare 5 cm to 10 cm wide, brecciated sections.

154.23 END OF HOLE.

AMERICAN BARRICK RESOURCES CORPORATIONHolt-McDermott Mine

P.O. Box 278. Kirkland Lake, Ont, P2N 3H7

Asa ay Certificate

No. of Determinations: 37 Lab ID: 89N09-2x

SflMPLE o/t Au SflMPLE g/t Au

Data: Nov. 09, 1989 ftcct. No.: Exploration

SflMPLE o/t Au

9737297393

949596

973979899

010203

0.07 0.04 0.06 0.13 0.21 0.15 0.13 0.11

0.14/0.13 0.09 0.12 0.10

Signed

AMERICAN EARRICK RESOURCES CORPORATIONHdt-McDermott Mine

P.O. Box 278, Kirkland Lake, Ont., P2N 3H7

Assay Certificate


SAMPLE g/t Au SflMPLE Q/t Au

Date: Nov. 12, 1989 Acct. No.: Exploration

SflMPLE g/t Au

9737374757677787980818283848586878889909192

0.040.090.040.140.340.040.04

0.08/0.100.090.030.040.050.060.040.030.110.05

0.08/0.100.070.04

97404050607080910111213141516

0.070.040.050.140.100.05

0.09/0.130.110.070.050.040.040.12

Signed

W-


P.O. Box 278, Kirkland Lake. Ont. P2N 3H7

Aasay Certificate

No. of Deterninations: 69 Lab IDs 89N14-IX

SflMPLE Au SflHPLE Q/t Au

Date: Nov. 14, 1989 fleet. No.: Exploration

SflHPLE Q/t Au

97433

2/i(hi/i"0j^V)

343536373839404142434445464748495051525354555657585960

0.020.040.070.110.090.070.08

0.09/0.070.060.040.060.050.030.010.020.040.02

0.01/0.010.060.070.010.200.070.090.020.030.05

0.05/0.05

Signed



Assay Certificate


SftMPLE g/t Au


SftHPLE o/t Au

97461626364656667686970717273747576

Oroo*-*- 77~)SOO 2- f 78

7980818283848586878889909192

0.130.130.110.080.140.150.090.050.16

0.03/0.030.020.020.040.040.020.040.020.060.04

0.06/0.060.070.060.050.070.140.040.040.060.03

0.04/0.040.040.05

97493949596979899

9750097532

333435363738394041424344

cip•JK

0.050.040.040.060.060.060.07

0.05/0.060.040.050.070.060.060.070.030.06

0.04/0.030.020.020.030.02

- 8"*9'l W"

Q/t Au

Signed

AMERICAN BARRICK RESOURCES CORPORATIONHdt-McDermott Mine

P.O. Box 278, Kirkland Lake. Ont., P2N 3H7

Assay Certificate

No. of Daterninations: 79 Lab ID: 89N17-lx

SflHPLE o/t Au SflHPLE o/t Au


SAMPLE g/t Au

974171819202122232425

2 26; 27

97561 0.04 *, 2862 0.06 ' 29

o*5 3031

1 . 32l 97545

46J 4?d 48fr 49So 50* 5 1w 52

5354555657585960

0.040.040.03

0.02/0.040.030.010.010.020.040.070.060.030.04

0.04/0.060.030.020.020.020.030.050.05

0.05/0.060.060.050.070.040.030.070.050.090.05

0.05/0.05

Signed

AMERICAN BARRICK RESOURCES CORPORATIONHolt-McDarmott Mine

P.O. Box 278. Kirkland Lake. Ont.. P2N 3H7

Aa3ay Certificate

No. of Determinations s Lab ID: 89N30-1x

SAMPLE o/t Au

50

SAMPLE g/t Au

Date: Nov. 30, 1989 Acct. No.: Exploration

SMELE O/t Au

97563 64 65 6667686970717273747576777879

^ 80T 81fc 82t 83X 8 4

8586878889909192

1 93

0.08 97595 0.03 0.08 96 0.06 0.10 97 0.06 0.15 98 0.08 y,. , ?0.10 99 0.06 "^ o*0.08 7 97600 0.07/0.050.07 ** 0 1 0.05

0.22/0.15 - 02 0.050.05 ft 03 0.050.05 04 0.070.15 05 0.060.05 65493 0.05 — Sft-*9-0.140.140.130.050.04

0.05/0.030.050.060.160.120.120.040.060.140.19

0.10/0.110.140.140.05

94 0.06 -

Signed


P.O. Box 278, KlrWand Lake, Ont, P2N 3H7

Assay CertificateNo. of Determinations! 84 Lab ID: 89D03-2x

SAMPLE g/t Au SAMPLE g/t Au

Oatet Dec. 03, 1989 Acct. No.! Exploration

SAMPLE Q/t Au

9760607080910111213141516171819202122

^ 237 24fi 2 S

, 2604 27ft 2 8

293031323334

1 351 36

37

0.110.100.130.10

0.10/0.140.090.090.050.110.160.120.070.050.07

0.04/0.050.030.080.080.040.010.010.020.050.03

0.05/0.030.040.150.090.010.030.02 SR0.06

976383940414243444546

Vi 477 48* c4.'

' 50ffi 5 1

52535455565758

- 13

0.080.03

0.01/0.030.250.100.120.130.110.100.100.110.16

0.11/0.120 17 * /** fi **. *0 1 e *-*LtW *1i . 1 D0.110.120.120.160.120.19

Signed

•M!'.

AMERICAN BARRICK RESOURCES CORPORATIONHo!t-McDermott Mine


Aa8ay CertificateNo. of Determinations: Lab ID: 89D03-1x

SftHPLE g/t Au

64

97659 ^ 60 7 61 (h 62 ? 63 # 64

, 651 66

676869707172

0 737 74GN 75to yei 77fr 78

798081828384858687888990

0.26 0.14/0.12

0.12 0.12 0.19 0.29 0.190.170.120.1 10.66

0.10/0.120.150.060.060.060.060.040.100.090.15

0.04/0.030.040.100.090.160.090.140.080.090.10

0.08/0.08

SftHPLE g/t Au

Date: Dec. 03, 1989 Acct. No.: Exploration

SftHPLE g/t Au

Op

V)

976919293949596979899

9770001020304050607080910111213141516

0.090.200.100.060.160.160.050.050.09

0.04/0.080.050.070.030.070.020.040.050.030.05

0.02/0.040.020.280.220.120.110.10

Signed


P.O. Box 278, Kirkland Lake. Ont., P2N 3H7

Asa ay Certificate

No. of Determinations: 96 Lab ID: B9D05-1*

SAMPLE g/t Au SAMPLE g/t Au

Date: Dec, 05, 1989 Aoct. No.i Exploration

SAMPLE g/t Au

97714

i?jfei01

151617181920212223242526272829303132333435363738394041

no sampleno sampleno sample

0.100.060.10

0.12/0.110.070.120.080.090.070.110.210.100.10

0.12/0.140.030.040.020.080.070.070.080.030.12

0.08/0.040.11

Jt?

Signed


P.O. Box 278. Kirkland Lake, Ont., P2N 3H7

Aa 8 ay Certificate

No. of Determinations: 81 Lab ID: B9D08-2x

SAMPLE g/t Au

a

9774243444546474849505152535455565758596061626364656667686970

0.17 0.11 0.13 0.24 0.09 0.13 0.08 0.44

0.08/0.06 0.07 0.04 0.06 0.07 0.24 0.09 0.05 0.05 0.02

0.12/0.08 0.10 0, 0. 0.21 0.09 0.04 0.06 C.05 0.06

0.13/0.19

1212

Datet Dec. 08, 1989 Acct. No.i Exploration

SflMELE

977717273747576

D 771 78S 79

801 811 97882

8384858B87

fc 88' HPtfft 90

919293949596979899

979000102

g/t Au

0.060.110.050.080.080.080.08 .0.050.06

0.08/0.120.090.050.050.070.060.060.100.050.09

0.10/0.140.100.070.050.060.140.150.120.070.14

0.13/0.160.060.11

SAMPLE

97X030405060708

2 09(V 10 0.1/1 11

12

b*L

g/t Au

0.090.120.050.080.090.060.06

12/0.080.060.05

Signed


P.O. Box 278, KlrMand Lake. Ont., P2N 3H7

Assay Certificate

No. of Determinations: 88 Lab 10: B9D11-2x

SftHPLE o/t Au SAMPLE Q/t Au

Datet Dec. 11, 1989 Acct. No.i Exploration

SftHPLE o/t Au

9791314151617IB1920212223242526272829

^ 30i * 31 W 3 2

333435363738394041424344

0.07 97945 0.080.07 46 0.080.09 47 0.110.05 48 0.070.05 ^ 49 0.070.14 Q/ 50 0.05/0.060.08 W 51 0.06

0.05/0.05 . 52 0.060.20 f. 53 0.100.130.110.120.280.250.170.150.67

0.24/0.18 ^- 0.11 (9.100.130.310.150.110.090.170.13

0.15/0.170.430.100.100.04

9778283848586878889909192939495

^^^™" Q t*

J 97i/J 98

9997800

01020304050607080910H1213

0.130.050.050.050.110.070.040.04

0.06/0.090.120.060.090.120.080.070.060.110.15

0.22/0.12 0.050.610.050.070.030.060.040.060.09

0.05/0.060.050.08e. 10

Signed



Assay Certificate

No. of Determinations: 75 Lab 10: 89D11-lx

SAMPLE g/t Au SAMPLE o/t Au

Data: Dec. 11, 1989 Acct. No.: Exploration

SAMPLE g/t Au

97814

r~~T

V)

iV

Oo

Si

15161718192021222324252627282930313233343536373839404142434445

0.050.060.060.050.070.04

0.05/0.050.040.050.040.040.090.040.040.080.36

0.02/0.050.060.010.040.020.010.020.230.080.14

0.11/0.120.110.080.070.060.05

9784647484950515253545556575859

^ 60T 61Qi e?w BZ

636465666768697071727374757677

0.09 97878 0.050.08 79 0.130.06 * 80 0.04/0.030.27 ' 81 0.05

0.07/0.07 W0.070.050.060.060.040.050.110.040.06

0.07/0.100.120.030.050.060.040.050.040.060.03

0.05/0.030.040.040.060.070.060.010.02

Signed

, b .//c

s—OFT:

—iZc\ \^s~-~! •,--"

~T v* osooeyj; 'di etU99'di "l

l VZE8*6'd|^CZC8fr6'dj^

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90C880II S0t880l|

^^ jJijjpOOQTvl ^M8Befd

^^————————1--^--

HS'iWQt

Ontario^.

Ministry ofNorthern Development

Mines

DOCUMENT No 9006-00

Mining ActReport of Work(Expenditures, Subsection 77(19))

42B01NE0e85 2 .13263 PENHORWOOD 900

Type of Work Performed77-19 Assaying Drill Core

Recorded Holder American Barrick Resources Corporation,

Address P.O. Box 1203, Kirkland Lake, Ontario

Mining DivisionPorcupine

Township or AreaPenhorwood Township

Exploration Division

P2N 3M7 Optionee of Record

Work Performed By American Barrick Resources, Assay Lab Holt-McDerraott Mine ^

Name and Address of Author (of Submission)

Dale R. Alexander, c/o American Barrick , Kirkland

All the work was performed on Mining Claim(s): Indicate no. of days performed on each claim. *See Note No. 1 on reverse side

Mining Claim

P. 950031Mining Claim

No. ol Days

1*9.5No. ol Days

Mining Claim

P. 639978

Mining Claim

No. ol Days

50No. of Days

Instructions Total days credits may be distributed at claim holder's choice. Enter number of days credits per claim in the expenditure days credit column

Mining Claim


P. 92*4167

Mining Claim

Cal

No. ol Days 1*5

No. ol Days

Ul*No ol Days

Lakei

Mining Claim


P. 921*168Mining Claim

No. ol Days

81No ol Days

22.5No. ol Days

culation of Expenditure Days Credits Total Expenditures

S 1*552. 50 5 .

c * J

Prospector's licence No.T-831*

Telephone No, (705)567-1*91*1

^J1 Q O fez*ba^wfiS

93 , li , 9? hMining Claim

P. 950025

Mining Claim

Mining Claim

Total Days Credits

303.5

No. o( Days Mining Claim

2.5 P. 95002No ol Days Mining Claim

No ol Days Mining Claim

iMVrrned

ihli, 9?No. ol Days

7 9No ol Da^s

No ol D.iys

Total Number of Mining Claims Covered by Ihis Report o( Work

12

Mining Claims (List in numerical sequence). If space is insufficient, attach schedules with required informationMining Claim

Prefix

P.

Number

92l4l65

921*166

921*167

921*168

921*169

921*170

921*171921*172

Expend. Days Cr.

!*0

UO

20

20

20

20

20

20

Mining ClaimPrefix

P.

Total Number ol Days Performed

303.5

Number

921*173921*171*

921*175

921*176

Expend. Days Cr.

1*0

1*0

20

3.5

Mining ClaimPrefix Number

Expend. Days Cr.

td

ftpR a

Mining ClaimPrefix

tVffi m

MINING LAIRDS SB

Total Number of Days Claimed

303.5

Number

D ———

T10N

Expend Days Cr.

Total Number ol Days lo be Claimed al a Future Date |

____ j

Certification of Beneficial Interest 'See Note No. 2 on reverse sidel hereby certify thai, a! the lime the work was performed, the claims covered in this report ol work were recorded in the current recorded holder's name or held under a beneficial interest by the current recorded holder. ~ ~~

Dai Holder ignature)

Certification Verifying Report of Work

l hereby certify thai l have a personal and intimate knowledge of Iho facts set forth in the Report ol Work annexed hereto, having poiformod Iho work or witnessed during nnd/or alter ils completion and the annexed report is true.

"Name a nd Address ol Person Certifying .

Dale R. Alexande 53 Resources, Exploration Division

Kirkland Lake, Oified By (Signaturf)).

For Office Use OnlyReceived Stamp l l

r ARECORDED ,

REFERENCEAREAS WITHDRAWN FROM DISPOSITION

M.R.O. - MINING RIGHTS ONLY

S.R.O. - SURFACE RIGHTS ONLY

M.+ S. - MINING AND SURFACE RIGHTS

Description Ordw No. D rt* Dopcwrtkwi F iU

400 RESERVE

SEC 45/70

SEC. 16/80

27/12^72

tl'7/SI

S. R. O.

S. R. O.

S. R. O.

135.537

I6SOO6 V2

135537

OWJ6R OF ThE MASTER *33/B7 DATED MARCH iOtB7

WITHDRAWS MT4I4G AND SURFACE RIGHTS L*CER SECTIOH

36 OF THE MINING ACT RSO 1980

SAND AND GRAVEL

GRAVEL FLE 38729

GRAVEL PfT FI.E 13555 V.6

GRAVEL FLE IOG274

OUARRY PERMT *228O5 ISSUED FOR THE REMOVAL OF THE

QUARTZ JULY l . 1987.

QUARRY PERMFT t Z280B ISSUED f OR THE REMOVAL OF

QUARTZ SEPT, ID. 1387

CANCELLED PATENT AfO LEASED CLfMS

43BaiNE0C85 2.13263 PENHORWOOD 200

REEVES TWP.6.0 M 4.5M 3.0M l .5 W

7.5 M--

osetoe Ipjoasias l /

—L.-J P.944907 [P.944B04 f.944896 l P .94485U P.944S*a P.9448B3"30(546 I D.9O1343 JP.9449I6PJ06834B~| *J/———

tP.901342 ET9449I5

P.9446at (P-944885;.'P.9OC348 |P.90(34J

PJOZ79I |PJO27910 y PJO27909

|P.947t50 ^947149

l _ \TC_ -r 1^— -^— — —

__________J_____ ™-J p73M07 (P.7558(3X

X

I079S7 l 1079*8 f 107969 l i OTSTX)! 699885 /P.699886 H 9OI26 f !

^——^---oa? * T

*cww~e] 90TfM, 9044a .

IO9V5\ 108414s111588 P.996855 l C Li: ij05 - "l "596*83'P-996aaS

5j11(725 l l M 726 l III72B

lp.9H880( |P.948B02lei lo l ' fi

V ^^^ ,, j^.__i__ ' "^ T " IP

I";O75O40| :07*01, i IO75O42

** ' il ' '^ /S \l

S J ^ JT— — —J

^.99^.4633.994632 P.9946SE

IP.994635 |P.994]'e36 IP.99463J' '

Jl J—-- J/964379 , ~ l'

l I029&06 l IO29505 i

Horwood Lake

7.5 M 6.0 M 1.5M

HARDIMAN TWP.

LEGENDHIGHWAY AND ROUTE No.

OTHER ROADS

TRAILS SURVEYED L INES:

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

UNSURVEYED LIMES:LOT LINESPARCEL BOUNDARYMINING CLAIMS ETC.

RAILWAY AND RIGHT OF WAY

UTILITY LINES

NON-PERENNIAL STREAM

FLOODING OR FLOODING RIGHTS

SUBDIVISION OR COMPOSITE PLAN

RESERVATIONS

ORIGINAL SHORELINE

MARSH OR M USKEG MINES

TRAVERSE MONUMENT

oisposrnoN OF CROWN LANDSTYPE OF DOCUMENT

PATENT. SURFACE ft MINING RIGHTS

.SURFACE RIGHTS ONLY^^^

.MINING RIGHTS ONLY ^^^

SYMBOL

LEASE,SURFACE ft M INING RIGHTS,

" .SURFACE RIGHTS ONLY—-—.

" . MINING RIGHTS ONLY————

LICENCE OF OCCUPATION '

ORDER-IN-COONCIL _________:—

RESERVATION ___________'...'

CANCELLED _______________

SAND s- GRAVEL ^_____

B B T

oc

LAND USE PERIffT - - - - . . . . ~ *tOTE: MINING PJIGHTS IN P ARCELS PATENTED PWIOH TO MAY 6.

1913. VESTED IN ORIGINAL P ATENTEE *V THE PUBLIC LANDS ACT. R.S.O. 1870. CHAP. 3*0, *EC. *3. ftUBSEC 1.

SCALE: l INCH * 40 CHAINS

1OOO TOGO *OOO 6000 eooo

O 2OOMETRES

1OOO fi K M)

20OO [J KM)

ACTIVATED JANLUVRY 3O, 199O.,~\

TOWKSHIP

PENHORWOODM.R.R. ADMINISTRATIVE DISTRICT

CHAPLEAUMINING D1V1SIOM

PORCUPINELAHD TITLES/ REGISTRY DIVISION

SUDBURY

Ministryof L andNatural Management

. Resources BranchOntario

Dtti !SB5• ••ktr

-

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