township: mathews report no,: 10 work performed by! … · diamond drilling 48c13ne8681 18 matthews...

DIAMOND DRILLING 48C13NE8681 18 MATTHEWS 010

TOWNSHIP: Mathews REPORT No,: 10

WORK PERFORMED BY! Lobo Gold S. Resources Inc.

CLAIM No.

SSM 773880 SSM 773886 SSM 773887 SSM 773367 SSM 773873-75 SSM 773877 SSM 773879-80

707*1;

HOLE No.E-30E-40E-52W-4W-10W-10BW-25

FOOTAGE350' 350' 288 1 300' 150' 241' 300'

1 17-7

DATEAuq/8**- Auq/8 1*- Auq/84- Auq/8^ Auq/Sf Auq/Slf

NOTE

d) d) (D ID d) m (i)

NOTES: ID #io?-65

LESRELEVES

SURVEYS INC.

•42C13NE8681 1 0 MATTHEWS 0S0

53, rue AllardVal d'Or, Qu6. J9P 2X9

T6I.: (819) 825-6263

S. S. MARIEM INI NO DIV.

JUN l 01985 HWA

SUMMARY REPORT

ON THE

DRILLING PROGRAM

MATTHEWS TOWNSHIP, ONTARIO.

LOBO GOLD RESOURCES INC.

Val d'Or, Quebec. September, 1984

C.D.I. Surveys Inc.Daniel Labadie, B.Se. GeologyExploration Geologist

4aC13NE8681 1 0 MATTHEWS 020CTABLE OF CONTENTS

Introduct ion...............................................l

Work done..................................................l

Conclusions and recommendations............................2

ANNEX Diamond drill logsHoles: W-4, W-10, W-25, E-30, E-40, E-52,

W-lOB.

Sections

Certificates of analyses

IN POCKET; Location map of the drill holes

-1-

INTRODUCTION

The present report describes the results of the drilling

program recently performed on the Matthews township property of Lobo Corporation.

Six (6) of the best conductive zones have been tested

by drilling. Seven (7) angle holes {45 O dip) have been

drilled, for a total of 1979 feet, to intersect these strongest

VLF-EM16 anomalies. Each drill hole is numbered -by its related geophysical anomaly.

Several stringers of sulphides, altered zone and veinlets

of secondary quartz have been intersected within metavolcanic

rocks. The best mineralized sections have been assayed

and give only trace amounts, in oz/ton, of gold and silver.

WORK DONE

Holes W-10, W-10B, W-25, E-30, E-40, and E-52, located

on the enclosed map, cut through a granodiorite gneiss

or a hybrid gneiss which is a granodiorite gneiss, more

or less contamined by a hornblende schist. These holes

intersected weakly mineralized shear zones or highly altered

zones that caused the electromagnetic conductors.

Hole W-4 is associated with a magnetic high and cut

metavolcanic rocks, mostly quartz-plagioclase-hornblende

schist, and intersected three (3) mineralized sections.

Trace amounts, in oz/ton, in gold and silver have been found.

CONCLUSIONS AND RECOMMENDATIONS

The drilling program done by Lobo Corporation on the

Matthews township property has intersected all the most

important VLF-EM16 anomalies and found trace amounts of

gold and silver in 02/ton. The drilling program outlined

numerous traces of chalcopyrite and lesser pyrrhotite but

not of significant importance.*

At present, no additional works are recommended to be

carriedout on the Matthews township property of Lobo Corporation.

t.Val d'Or, Quebec. Daniel Labadie, B.Se. Geology September, 1984 Exploration Geologist

LOCATION

LATITUDE ELEVATION '

MOND DRILL RECORD'ROPERTY t Matthews Township OntarioE-30 LENGTH' 350'

11+50E 21+50NDEPARTURE "

U m r- C*

' AZIMUTH: 165 DIP - 4 5\ugust 25. 1984 FINISHED :

FOOTAGE DIP AZIMUTH FOOTAGE OIR AZIMUTH

HOLE No. i E-30 SHEETNo.1

REMARKS'

"i~i. "- ~~ f ~7~~7'3tfS'C:'

CLOGGED BY s Daniel Labadie

FOOT ACE

FROM

0

52.0

TO

52.0

350.0

DESCRIPTION

OVERBURDEN

BIOTITE-HORNBLENDE-QUARTZ-FELDSPAR GNEISS

Medium-grained, greenish grey rock with somepink grains. The rock is composed of feldsparand quartz with 40% to 50% by volume of thegneiss, hornblende makes up the greater part ofthe remainder (35 to 45%), with a lesser amountof biotite. Crosscutting veinlets of calciteand/or epidote is common. Epidote is locallyimportant, especially along some planes ofweakness .

Trace amounts of disseminated pyrite andchalcopyrite. Grains range from 1/20 inch to1/10 inch in diameter.

55.6 to 57.8 PEGMATITE

Occuring as veins. The rock is cream white topink. Pegmatite grains rarely exceed 1/2 inchin diameter. Traces only of ferromagnesianminerals. The main constituents are potassiumfeldspars, quartz ranges from 10% to 30% b^volume of the rock. Hematization, causingthe reddening of the planes of weakness likefractures, is common.

Unmineralized .

SAMPLE

No. A

lUlphMliFOOTAGE

FROM TO TOT AU

A3 SAYS

V. A OX/TOM

Au

Ox /lea

'

HOLE Nat

LOCATION i

LATITUDE ' ELEVATION '

MOND DRILL RbCORD'ROPERTY J Matthews Township Oirt-m-ii-%

E-30 LENGTH" 350'11+50E 21+50N

DEPARTURE ** - O a O

" AZIMUTH' 165 DIP ' 45

August 25. 1984 FINISHED .

FOOTAOE OIK AZIMUTH FOOTAOe OIR AZIMUTH

HOLE NO. : E-30 SHEET NO.: 2

REMARKS i

LOGGED BY* n?n i9 i Labadio

FOOT A e E

FROM TODESCRIPTION

^ n5^0 fi?V5 FRACTURED ZONES 62 . 0 to 62 . 6

The rock is fractured and is entirely pebbly


Unmineralized .

110.5 to 112.0 ALTERED FRACTURE ZONES

The rock is brownish red. This reddening is dueto the hematization of the feldspar which arealso saussuritized and sericitized. All themafic minerals are weathered out. Some traces ofcalcite have been noted. The rock has anargillaceous aspect .

Unmineralized .

112.5 to 113.5

INCLUSIONS OF QUARTZ-PLAGIOCLASE-HORNBLENDESCHIST

These inclusions are more mafic with a highercontent of hornblende and biotite.

Unmineralized .

SAMPLE

No.. -A FOOTAGE "

FROM TO TOT AU

AS SAYS

A V. Ox /ton Ox /to*

HOLE No.' LOCATION ' LATITUDE " ELEVATION '

MOND DRILL RbCORD*ROPERTY t Matthews Township Ontario

E-30 LENGTH * 350*11+50E 21+50N

DEPARTURE 'o o

AZIMUTH' 165 DIP' 45August 25, 1984 FINISHED '

FOOTAGE DIP AZIMUTH FOOTAGE OIR AZIMUTH

HOLE No.' E-30 SHEET No. :_3__

REMARKS'

LOGGED BY t Daniel Labadie

P 0 0 T A G E

FROM TODESCRIPTION


Unmineralized .

119.9 to 120.5 INCLUSIONS OF QUARTZ-PLAGIOCLASE-HORNBLENDE SCHIST

Chlorite occurs as an alteration product of hornblende. In these inclusions, biotite isoften a main constituent.

Unmineralized .

134.0 to 134.75

144*0 5to0 144 3 25 PEGMATITE

149.4 to 150.3

Occur ing as veins. From 134.0 to 134.75 the rock shows parallel fractures.

Unmineralized .

171.5 ALTERED FRACTURE

Epidote is a main mineral and feldspar is hematized on this plane of fracture.

Unmineralized .

SAMPLE

Ne.Vi FOOTAGE

TO

ASSAYS

V. •t. Ox X rea

Au

Ox/to*

DIAMOND DRILL RE-CORDNAME OF PROPERTY -. Matthews Township OntarioHOLE Nai E-30 '.ENGTH i ISO*LOCATION i 11+50E 21+50Nl ATITUDE i DEPARTURE"

ELEVATION' AZIMUTH' 165 DIP i 4 S OSTARTED .A-gUSt 25, 1984 FINISHED .

FOOTAOC DIP AZIMUTH FOOTAOE OIR AZIMUTH

MOLE No. i E~ 30 SHEET No. : 4

REMARKS t

LOGGED BY'paniel T.nhartif

r o o i

F ROM

AGE

TO

f

DESCRIPTION

175.9 to 178.2 FAULT ZONE

Epidotized fractures and veinlets. Slickensidestriae are a common visible structure and occuron fault planes. Feldspars are hematized andare associated with chlorite and epidote.

Unmineralized .

202.4 to 207.7 PEGMATITE 230.0 to 230.9 AGMATITE

Approximately ^ of apatite occurs as anaccessory mineral.

1* by volume of magnetite grains. Tra:e amountsof disseminated pyrite and chalcopyrite.

237.0 to 238.0

Narrow stringers of calcite, in part weatheredout, follows the gneissosity. These veinletsmake up 5% by volume of the rock.

MMno.V.

MlpMdH

SAMP

FROM

L E

FOOTAGETO TOTAL

y^ V. O* /ten

AM

O* /to*

DIAMOND DKIIL RtCORDNAME OF PROPERTY : Matthews Township Ontario

HOLE No." E-30 LENGTH t 350'

LOCATION t 11 + 50E 21+50N

LATITUDE i DEPARTURE 'O o

ELEVATION t AZIMUTH' 165 DIP. J 45w a ** *- * J-k **l *STARTED t August 25, 1984 FINISHED '

FOOTAGE 01 P AZIMUTH rOOTAGC OIR AZIMUTH

E 30HOLE No. ' S HEET No. : 5

RFMABKSl

l "'7 1 r 'i r 'v* ' - ' \ ' l 1*

A-^^\ ^W-ixA

LOGGED BY 1 Daniel Labadie

FOOT

r ROM

r A A PM V b

TO

350.0

DESCRIPTION

279.1 to 282.4291.9 to 292.5294.1 to 294.6 GRANODIORITE300.4 to 301.2302.6 to 303.1

Occurs as veins. It is a fine-grained, lightgrey rock.

Unmineralized .

308.25 to 308.75 PEGMA^TTF 345.7 to 346.5 PEGMATITE

Unmineralized.

END OF HOLE.

M no.V,

*!:*MM

SAMP L eFOOTAOE

• t/W

i. -

V. Oi/tos

Au

Ox /lo*

i

J-f/,501

J3.00 4*OON 8-CON II*50N 12,00 N

xv-v', -vVv v V; ,'i'^:'r\ ''' V X v.vX', x*x wx . v . x.V /. ' , .' f ' ^' t.^'S-J s /^^ N -x ^v ///' y x * s ' ' . . ' /v*"p x \ - x OVERBURDEN ^ V v " ' ^ ' ' " //V ' S ' N "* '^ -

^^^ {y^^ )^.xh ri^x^.xv:^

Pegmotite

"^Ptgmotlt*

Ptgmotit* nclusion of Ouorti- Ptagloclon-Hornbltnd* Schist

BIOTITE - HORNBLENDE- QUARTZ - FELDSPAR GNEISS

s A LTERED ZONES

^LOStf (?OL/? RESOURCES Inc.Matthews twp , Ontario

SECTION SHOWING No- E-30

21* 50 htxtcuTEo er coi SURVEYS

SUPERViSCO B* D. LA8AOIE

SCALE t" ' SO 1

AZIMUTH 1 6}*

DIP 45*

OAT C AUGUST i?b4

-•*.

Vj

M J

K

•-N

A

'-.j

^.

* rv

^4

f -

v' -

! N

^ -,

-:-'

C v^

Ci N^

. v

-^ l*

is

* -

i u

u

DIAMOND DRILL RECORD'NAME OF PROPERTY * Matthews Township Qntarin———- HOLE Na" E-40_________ LENGTH ' 350'.^^—M—- LOCATION t 44 + OOE 15+50N____________________

LATITUDE ' -————^—-^ DEPARTURE

ELEVATIONtut .~..~" _____________ AZIMUTH' 3600 STARTED i August 25, 1984 FINISHED '

Dlf? 45

FOOTAGE DIP AZIMUTH FOOTAOC OIR AZIMUTH

HOLE No. E~ 40 SHEET No. -. l

REMARKS' —^—--————.—^—-

LOGGED BY* Daniel Labadie

FOOT

F ROM

0

28.0

A e e

TO

28.0

233.4

DESCRIPTION

OVERBURDEN

BIOTITE GRANODIORITE GNEISS

Medium-grained, light grey to greenish grey rock.This gneiss has a prominent augen-type structureand sometimes a lepidoblastic structure. Theaugen have an average diameter of 1/4 inch. Thisrock grades to a biotite-hornblende-quartz-feldspar gneiss where biotite and hornblende areimportant. This gneiss seems to be a hybridbetween biotite granodiorite gneiss and quart z-plagioclase-hornblende schist . The reddening ofthe rock on planes of fracture is common.Biotite and hornblende range from 15% to 35% byvolume of the rock. Epidote and hematite areAocally important in fracture zones.

Trace amounts of disseminated pyrite.chalcopyrite and magnetite, mainly closelyassociated with the more mafic minerals-richzones .

——————————————————————— ———————————————— - ——— . ———

*•A

i A M P"

L E

FOOTAGE1 TOTAL,

•A Ox /to*

A*

Ox /leu

DIAMOND DRILL RECORDNAME OF PROPERTY s Matthews Township Ontario———HOLE No.* E-40________ LENGTH ' 350*____________ LOCATION t 44 + OOE 15+50N——^-—-^——————————LATITUDE ' _______________ DEPARTURE ' ^———^—-^^—^— ELEVATION t AZIMUTH: 360STARTED t August 25, 198^| NIS HED .

DIP, 45

FOOTAGE 01 R AZIMUTH rOOTAGC DIR AZIMUTH

P-4O HOLE No.' SHEET No. s.

REMARKS'

LOGGED BY-- Daniel Labadie

r o o i

r ROM

'AGE

TODESCRIPTION

57.0 to 71.978.7 to 79.493.25 to 94.4100.1 to 103.0 120.3 to 121.1 PEGMATITE

150.5 to 152.1175.2 to 176.9

The rock is cream white to pink and has agranitic composition. Pegmatite grains have anaverage diameter of 1/4 inch. Apatite occursas an accessory mineral. Reddening offractures by hematization of feldspars is common.

Trace amounts of disseminated hematite andmagnetite.

182.5 to 182.7186.6 to 186.8 FRACTURE ZONES216.9 to 217.2

The rock has an argillaceous aspect and iscompletely altered by hematization of thefeldspars and chloritization of mafic minerals.From 216.9' to 217.2', the rock has a talco-chloritic composition where talc makes up 75% byvolume of the rock, chlorite 15%, hematite 5* andepidote 5%.

Unmineralized .

fc*-^**9,

•A•VlpMdM

SAMP

FROM

L E

FOOT* 0 CTO TOTAL

•/. */. Ox /re*

Au

Ox/tan

HOLE No.' LOCATION t LATITUDE ' ELEVATION

feOND DRILL R t CO R D*ROPERTY i Matthews Township Ontario

E-40 LENGTH. 350'44+OOE 15+50N

DEPARTURE ' , rrioobu j, ,-u

" AZIMUT' DIP s 45

Auaust 25. 1984nmsHED *

FDOTAOC DI R AZIMUTH rooTAoe DIP AZIMUTH

HOLE No. i E-40 SHEET No. : 3

REMARKS l

LOGGED BY i Daniel Labadie

r o o T A a EFROM

233.4

249.9

TO

249.9

350.0

O E S C N 1 P- T 1 O N

QUARTZ- PLAGIOCLASE-HORNBLENDE SCHIST

Partially assimilated by biotite granodioritegneiss and grading to a biotite-hornblende-quartz-feldspar gneiss. The rock has crosscutting vein-lets of quartz. Chlorite occurs as an alterationproduct of biotite and hornblende.

2% by volume of pyrite in narrow stringersassociated with epidote and secondary quartz.


It is predominantly a granodiorite contaminedby the quartz-plagioclase-hornblende schist. Themafic minerals, like biotite and hornblende, aremore important in proportion.

Trace amounts of disseminated pyrite.


Unmineralized .

SAMPLE

Ne.

11208

•A UlpkWU

2 243,6

FOOTAGE

244,25

AS SAYS

•h V. Ol/TO*

AH

traces

Of/ten

Ag

traces

DIAMOND DKILL RbCORDNAME OF PROPERTY ' Matthews township OntarioHOLE No.' E-40 LENGTH i 350'LOCATION , 44+OOE 15+50N

LATITUDE . DEPARTURE tQ

ELEVATION t AZIMUTH' 360 DIP t

STARTED t AUQUSt 25. 1984 FINISHED t

FOOTAGE OIK AZIMUTN FOOTAOE OIR AZIMUTH

4HOLE No. i E-40 SHEET No.'

REMARKS'

l / ' " -ri * l ' l ] l \-r^^i*s-J ±^U-*VA

\ ^

LOGGED BY* Dailifil Labadie

FOOT A 8 E

FROM TO

350.0

DESCRIPTION

265.0 to 265.6291.3 to 291.9 ,.n . Mx^,.^T, T mr. 330.9 to 332.4 GRANODIORITE339.9 to 344.25

The rock has a prominent felsic composition.Feldspar makes up 75% to 80% of the rock, quartz15% to 20%, biotite being the remainder.

Unmineralized .

END OF HOLE

SAMPLE

N*.•A

••irm** FOOTA8E

AS S A T S

•A •f. Of/to*

Au

Oz/toa

J-44 *00 g

15.SON 16.0 ON 20.00N Z8.00N

BIOTITE - GRANODIORITE GNEISS

QUARTZ - PLAGIOCLASE - HORNBLENDE SCHIST

Ptgmotitt

BIOTITE - HORNBLENDE - QUARTZ - FELDSPAR GNEISS

Gronodioritt

390'

..- ALTERED ZONES

LOBO GOLD RESOURCES Inc.Motihews 'wp , Ontario

SECTION SHOWING No* E-40J-44*008 X 15*50 A

CXECJTCO It COI SURVEYS inc.

SUPERV1SCO BY O L48AOIC

SCALl l" ' SO'

AZIMUTH ' 310'

DIP 45*

DATC AUGUST 19(4

1*—

~^ J~\

t- N

rn ^ o

HOLE Nat LOCATION i LATITUDE ' ELEVATION

MOND DRILL KbCORD*ROPERTY : Matthews Township Ontario

r.-^J LENGTH ' 9Bfit56+OOE 24+OON

DEPARTURE 'Q O

' AZIMUTH' 180 DIP i 45August 25, 1984FINISHED :

FOOTAOE DIP, AZIMUTH j FOOTAOE

jII||II||||

OIR AZIMUTH

HOLE NOLI E~52 SHEET No. s ——^.

RFUARKSi

—— T - v ''

*~ *

77 TftVLOGGED BY' Daniel Labadie

POOl

FROM

0

10.0

r A B f

TO

10.0

130.5

DESCRIPTION

OVERBURDEN

BIOTITE-GRANODIORITE GNEISS

Light grey to pinkish grey. The rock is medium- grained and has a predominant augen-type structure.

Trace amounts of pyrite.

74.0 to 74.1

Greenish grey, argillaceous material filling a fracture.

74.1 to 76.1 AMYGDALOIDAL LAVA

Massive, dark green to black rock with round amygdule s of quartz and phenocrysts of plagioclase. Amygdules and phenocrysts have an average diameter of 1/8 inch. The rock is composed of 90% hornblende replaced in part by chlorite, 5% of sericitized plagioclase, quartz and a lesser amount of biotite making up the remainder.


M*.•A

WlpkWH

SAMP L E

FOOTAOCr TO ipTOT A L •h •f.

S S A Y

Ox/t.n

A*

S

Ox/fM

DIAMOND DRILL RbCORDKAME OF PROPERTY i Matthews Township Ontario

E at toot™,~. ...- ~ 5Z LENGTH t Z tJBLOCATION " Sfi + OOE 24 + OONLATITUDE t D EPARTURE t

O OELEVATION: A. 'MUTH ' 180 DIP' 45

— — T t\ O ASTARTED 'AugUSt 25, 1984 pin, S HED ,

FOOTAGE OIR AZIMUTH fOOTAttE OIR AZIMUTH

HOLE No. t E-52 SHEET No.: 2

REMARKS'

LOGGED BY' Daniel Labadie

r o o r A e E

FROM

130.5

TO

192.1

DESCRIPTION

76.1 to 76.35

The planes of fracture have slikenside striae composed of talc and chlorite, indicating a faulted zone.

Unmineralized .

87.1 to 88.0

The rock shows a brecciated texture. Epidote makes up 303; by volume of the rock with traces of calcite. The more calcite-rich zones areweathered out. Feldspars are highly nema t i zed giving a reddish colour to the rock. Epidote is frequently found in well formed crystals ranging from 1/8 inch to 1/4 inch in diameter. Epidotization is a low- temperature metasomatism and is found in veins and joints fillings.

Unmineralized .

GRANODIORITE

Massive, light grey to cream white rock. It is fine-to medium-grained. Biotite makes up approximately 5% by volume of the rock. The contact is gradational with the biotite granodiorite gneiss.

Unmineralized.

SAMPLE

H*.•A

wripkMMFOOTAGE

AS SAYS

•h •A Ox /ton

A*

Ox /ten

DIAMOND DRILL RbCORDNAME OF PROPERTY : Matthews Township Ontarxo

HOLE No.' E-52 LENGTH ' 2 88'LOCATION s 56+OOE 24 + OONLATITUDE . DEPARTURE '

o o oELEVATION ' AZIMUTH: 180 DIP ' 45

STARTED i AuqUSt 25. 1934 FINISHED :

FOOTAGE DIP AZIMUTH rooTAee OIK AZIMUTH

HOLE (to. i E-52 SHEET No.' 3

REMARKS:

LOGGED BY* | (A..i**l T.^h^^ i **

POO1

FROM

192.1

194.6

ABE

T.

194.6

235.2

DESCRIPTION

PEGMATITE

Cream white to pink, coax se- grained rock with less than 5% biotite and traces of apatite. The rock has a granitic composition.

Unmineralized .

QUARTZ-PLAGIOCLASE-HORNBLENDE SCHIST

In some places, the rock is highly distorted showing ptygmatic folded quartz and granodiorite veins. The rock is partially chloritized and sericitized. Contacts with intrusive rocks are more biotite-rich zones.

Trace amount of disseminated pyrite.

207.5' to 208.9 211.5 to 214.25 GRANODIORITE 216.6 to 219.2

Occurs as veins cutting the quart z-plagioclase- hornblende schist. It is a fine grained, cream white, equigranular rock. Trace amounts of calcite have been noted.

Unmineralized .

H*.•A

HtptMM

SAMP

FROM

L eFOOTAOE

TO 1•A •/. Oz/ton

A*Ox /to*

;

DIAMOND DKILL RbCORDNAME OF PROPERTY . Matthews Township OntarioHOLE No.' E-52 LENGTH ' 288*LOCATION i 56+OOE 24+OONt ATITUDE : DEPARTURE t

O OELEVATION i AZIMUTH: 180 DIP i 45STARTED i Augus t 25, 1984 FIN , S HIr 0 ,

FOOTAOC DIft AZIMUTH rooTAoe OIR AZIMUTH

HOLE No. t , E-52 SHEET No.: *

REMARKS'

r if l r tX1 1 ' i' l t' ' -Alt^Ji 1^±^t Si, L*•^^^ fj — " "

LOGGED BY- Daniel Labadie

r o o T

F MOM

235.2

AGE

TO

288.0

288.0

DESCRIPTION

226.25 to 228.7 PEGMATI^Z

BIOTITE GRANODIORITE GNEISSThe rock has a more prominent lepidoblasticstructure.

Unmineralized .

240.1 to 241.4

The rock has few inclusions of dark grey to darkgreen quart z-plagioclase-hornblende schist.

264.4 to ?66.4 PEGMATITE

Trace amounts of molybdenite and magnetite.

END OF HOLE.

*•A

SAMP

FROM 1

L eFOOTAGE

TO 1 TOTA^,** •li OxX*ofi

Au

Ot /t**

16.00 N 20*00N_______ 24*00 N _______28*00 N j\y7.iy ^~Wt/ -'.VT*' •n^-NVr^*-".-/'-''''

Ift'

BIOTITE - GRANODIORITE GNEISS Amygdoloidol Lava

GRANODIORITE

PEGMATITE- Gronodioril*

QUARTZ - PLAGIOCLASE - HORNBLENDE SCHISTortz.Plogioclot*-Hornblende Schiif

-PtgmotittBIOTITE-GRANODIORITE GNEISS

ALTERED ZONES

LOBO GOLD RESOURCES Inc.Matthews twp , Ontario

SECTION SHOWING No- E-52l-56tOO S /

EXECUTED IV' C DI SURVEYS Inc.

tUPCMViSED

SC*CE

D.L*S*DIE

90'

AZIMUTH

Bif- 4 5*

DATE AUGUST it

*

iV

M -o

DIAMOND DRILL RECORD'1 NAME OF PROPERTY t Matthews Township Ontario

HOLE No.' W-A__________ LENGTH ' ' .tfl *-—-—^———24+82SLOCATION t 43-97W

LATITUDE ' _______———-— ELEVATION t ____________ MUTH s STARTED ' August 25, 1984 FINISHED i

178 Dlp 45

FOOTAOE OIK AZIMUTH II rOOTAOE

11

H

||

OIK AZIMUTH

HOLE No. i.

REMARKS'

W-4SHEET' e.:.

LOGGED BY t Paniel Labadier o o i

F ROM

0

12.3

13.3

13.75

A S E

TO

12.3

13.3

13.75

32.7

DESCRIPTION

OVERBURDEN

Mostly glaciolacustral deposit.


Light grey rock with an average grain size of1/16 inch. This gneiss has a lepido-blasticstructure, but in some places an augen-typestructure. The average composition of the rockin volume is: 25% quartz, 6(^ feldspar and15% biotite.Unmineralized .

CONTACT ZONE

40^6 biotite by volume with crosscuttingpegmatite vein of granitic composition.Minerals grain diameter is 1/8 inch and the veinis one inch thick.Unmineralized .

QUARTZ-PLAGIOCLASE (CHLORITE) HORNBLENDE SCHIST

Medium-grained, dark green rock with 5 to 15%of crosscutting veinlets of quartz, havingan average thickness of 1/4 inch. This rockis composed, in % volume, of hornblende (80 to90!*), plagioclase (10 to 15%), the remainderbeing quartz. Secondary quartz is sometimespTn^Ant- Thp" main ^r"g**fi*;nry minerals

Ha"•A

MlpMfa*

SAMP L E

FOOTAOe •J^ Ox /to*

Att

O* /fa*

HOLE Nat LOCATION ' LATITUDE ' ELEVATION t

MOND DRILL RbCOttDPROPERTY" Matthews Township Oni-ario.

W-4 LENGTH . 300'

d^ + QTW 74-I-R7S

DEPARTURE '1 TQ U A C w

t AZIMUTH: -L'O DIP ' 4 5

August 25 1984 FINISHED :

FOOTAOC OIK AZIMUTH rOOTMC OIK AZIMUTH

HOLF NO. ' W-4 SHEET NO. ^

REMARKS i


r o o i

FROM

32.7

34

M V C,

TO

34.0

55.0

are biotite, pyrite and rare epidote. Chlorite is present as the alteration product of hornblende. The rock has minor zones of morebiotite- rich composition.

5% pyrite from 13.75 to 15.0 2% pyrite from 17.6 to 19.6 In distorted veinlets as replacement of felsic minerals in planes of schistosity. Rock has generally traces of disseminated pyrite.

GRANODIORITE

Medium-grained, grey rock with some pink stain from microcline. The composition of this rock ic plagioclase, microcline, quartz with lesser biotite. The rock has no foliation.

Traces of disseminated pyrite.

QUARTZ -PLAGIOCLASE (CHLORITE) HORNBLENDE SCHIST Biotite ranges from 5to 103; (in volume) in the rock composition.

2% (in volume) of pyrity. Disseminated or as replacement of felsic minerals.

Ne.•A

wlphUM

SAMP L C

FOOTAGE •/. •/. Ox /ton

A*

Ox/ten

DIAMOND DRILL RECORD'NAME OF PROPERTY * .

HOLE No.' W-4 LOCATION . 43 + 97W

Matthews Township OntarioLENGTH

24+82SLATITUDE '

ELEVATION tSTARTED. August 25,

DEPARTURE '

AZIMUTH: 17801984 FINISHED :

DIP. t 4S0

FOOTAGE OIK AZIMUTH FOOTAGE

H

OIK AZIMUTH

HOLE No.' W~ 4 SHEET No.: 3

REMARKS:__________________

LOGGED BY' Daniel

FOOT

FROM

55.0

AGE

TO

63.9

DESCRIPTION

35.75 to 36.7548.0 to 48.6 BIOTITE-HORNBLENDE-QUARTZ-FELDSPAR

GNEISS

Medium-grained, greenish grey rock with lepido blastic texture. It occurs as layers inter-banded with quart z-plagioclase (chlorite)hornblende schist in gradational contact andwith minor bands of more biotite-rich schist.The rock is composed of biotite (15 to 30%),feldspar (45 to 55%) quartz (15 to 20%), andhornblende (15 to 30%) as replacement ofbiotite. Traces of calcire and epidote.

Traces of disseminated magnetite. Associatedwith more biotite-rich zones.

QUARTZ -PLAGIOCLASE (CHLORITE) HORNBLENDE SCHIST

With amphibolite zones. Hornblende is the mainconstituent with 80% (in volume) of the rock.the remainder being biotite and chlorite with10% and 5% respectively. The main accessoryminerals are pyrite, magnetite, sericite andrare epidote. This medium-grained amphiboliteis closely associated with quartz-plagioclase(chlorite) hornblende schist and is probably aslightly different phase.

No.

11202

•A wlpMdM

5

SAMP

.

57.6

U E

FOOTAGE TO

58.5

TOTAL'•/.

A

*h

3 S A Y

Ox /lo*

f

traces

s

Ol/lon

Ag

traces

DIAMOND DKILL RECORDNAME OF PROPERTY " Ma.t-the.ws Township Onl-a-rin

HOLE Nai W- 4 LENGTH ' 300'• orATioN, 43 + 97W 24+82SLOCATION ' n.M

1 ATITUDE i DEPARTURE i—

FI EVATION i AZIMUTH: 17^" DIP s ARO

STARTED lAuquS t 25. 1984 FINISHED :

FOOTAOC OIK AZIMUTH FOOTAOE OIR AZIMUTH

HOI F No. t W- 4 SHEET No.: 4

REMARKS'

LOGGED BY * Of* r" t* 1 T.nhaH i o

F O O T A 6 E

FROM

63.9

64.7

TO

64.7

69.0

DESCRIPTION

l% o f disseminated magnetite. Varying in sizefrom 1/20 to 1/10 inch. S t of disseminatedpyrite of in narrow stringers along the planesof schistosity. And frequently associated withsecondary veinlets of quartz.


Greenish grey and green mottled rock withlepidoblastic texture. Grains have an averagediameter of 1/10 inch. The rock is composed, byvolume, of hornblende 30%, biotite 10%, feldspar45% and quartz 15%.

Traces of very fine pyrite. Also a lesseramount of chalcopyrite .

AMPHIBOLITE

Dark green, medium-to coarse-grained rock withhornblende comprising 85% of the rock, plagio clase and biotite making up the remainder with10% and 5% respectively. Main accessorymineral is pyrite. Sericite is present as thealteration product of plagioclase. This rockhas 10% of crosscutting veinlets of quartz.

From 65.1 to 65.3, 5% pyrite as replacement offelsic minerals. And in stringer along asecondary quartz veinlet. Associated with

SAMPLE

Ne.•A

••IpMte.FOOTA6E

TO

AS SAYS

•h •t. Os/tvn

A*

O s /to*

-

DIAMOND DRILL RECORD'NAME OF PROPERTY

HOLE No. i W-4

LOCATION ' ^

LATITUDE ' ^

ELEVATION '

Matthews Townshio OntarioLENGTH ^QQ'

43+97W 24+82SDEPARTURE ' -——

AZIMUTH: 178( DIP 'STARTED : August 25, 1984 FINISHED '

FOOTAGE 01 R AZIMUTH || rOOTACE

11

||

OIK AZIMUTH

HOLE N*. ' W-4 SHEET No.:__L

REMARKS * ^^^^^—-—™——-—


r o o i

FROM

69.0

A e E

TO

70.2

DESCRIPTION

epidote. Traces of disseminated magnetite. Often associated with veinlets of quartz.

66.0 to 69.0

More biotite-rich amphibolite, which has a more lepidoblastic aspect with biotite varying from 20* to 45* , chlorite 5*, feldspar 5* and hornblende being the remainder.


Light grey, medium-grain rock with a lepido blastic structure. The constituents of the rockare quartz 25*, feldspar 60* and biotite 15*, potassium feldspar being 20* of this average composition.

Traces of pyrite.

69.8 to 69.9 BIOTITE SCHIST

Biotite is the main constituent with 90* of therock, chlorite 5*, quartz and feldspar making up the remainder.

Traces of magnetite.

No.•A

wlpkMM

SAMP

FROM 1

L E

FOOTAGE TO 1 TOTAL

•A •h Oz/ton

Au

Ox /ton

DIAMOND DRILL RECORD'NAME OF PROPERTY '

HOLE No.' W-4 LOCATION . 43 + 97W

LATITUDE ' —^—.—--. ELEVATION '

Matthews Township OntarioLENGTH 3on

24+82SDEPARTURE :

___........ _______________ AZIMUTH:.STARTED t August 25, 1984 FIN , SH ED i

178' DIP i 4 5

FOOTAGE DI f. AZIMUTH FOOTAOC DIP AZIMUTH

HOLE No. t W-4 SHEET No. i 6

REMARKS'___________._____.

LOGGED BY-. Daniel Labadie

F O O T A 6 E

FROM

70.2

70.7

74.25

TO

70.7.

M. 25

74.75

O E S C R 1 PTION

AMPHIBOLITE

Dark green rock with hornblende (80%), biotite(15%) and plagioclase, partially altered insericite, being 5% of the average composition.The rock is coarse-grained with an averagediameter of 1/10 inch, and has crosscuttingveinlets of quartz and granitic material.

5% of magnetite. Grain diameter is 1/8 inch.


This medium-grained, greenish grey rock with amottled aspect has a lepidoblastic texture.The rock is composed of hornblende 25*, biotite15%, quartz 20t and feldspar 40%.


QUAPT7IPE

The rock is light grey to white and very coarse-grained. The grain size is 1/4 inch. The rockhas 20% of inclusion 1/4 inch thick. Theseinclusions are composed of chlorite, hornblendeand sulphides.

SAMPLE

Ne.

11201

VfcwlpkMw

17

FOOTAOE

74.25 74.75

•" *U

A3 SAYS

•h •1. Ol/t**

Att

traces

Ox /ten

Aa My

- -

traces

Oz/tonMO

.225

DIAMOND DRILL RECORDNAME OF PROPERTY i Matthews Townshio OntarioHOLE No.' W' 4 LENGTH i 300LOCATION : 43+97W 24 + 82SLATITUDE i DEPARTURE '

- ^ *J^ f OELEVATION^ AZIMUTH: 178 QIR ' 45

STARTED sAUQUS t 25. 1984 FINISHED :

FOOTAOC ote AZIMUTH FOOTAOe OIR AZIMUTH

HOLE No. : W~ 4 SHEET No. : 7

REMARKS:


F 0 0 T A C E

FROM

74.75

75.0

TO

75.0

87.8

DESCRIPTION

The rock contains approximately 15% by volume ofpyrite, 2% molybdenite and trace amounts ofchalcopyrite and magnetite. The sulphideminerals are found in narrow banded structures.

PEGMATITE

Pegmatite vein of granitic composition. Therock is cream white with pink staii *romperthite. ""'ie pegmatite grains have an averagediameter OL 1/4 inch. Pink perthite is the mainmineral making up approximately 40% of the rock.quartz and albite make up 25% and 35%respectively. Traces of biotite have beenobserved .

5% of magnetite in a 3/8 inch grain. Occuringas an accessory mineral.

QUARTZ -PLAGIOCLASE- HORNBLENDE SCHIST

The rock has the same characteristics except forbiotite, this mineral varying from 5% to 40% asreplacement of hornblende. From 83.5 to 84.6,an altered zone, with more epidote-richcomposition is carbonatized. The rock has 15%of crosscutting veinlets of quartz or graniticveins, ranging from 1/8 inch to 2 inches inthickness.

s A u F- L e

H..•A

..IpWHHFOOTAGE

A3 SAYS

•A •A Oz/t**

AM

O* /to*

-

DIAMOND DRILL RECORD'NAME OF PROPERTY HOLE No. i W-4

LOCATION t _

LATITUDE ' — ELEVATION t

Matthews township OntarioLENGTH 300'

43+97W 24+82SDEPARTURE '

AZIMUTH-178*

STARTED. August 25, 1984 FIN , S HED .DIP

45V

FOOTAGE 01 R AZIMUTH II rooTAoe^i!1-

OIR AZIMUTH

HOLE No. t W-4 SHEET No. t.

REMARKS ' ^—^—^^^————

8

LOGGED BY* Daniel LabadieFOOT

r MOM

87.8

A O C

TO

98.1

O E SCMI f T t O K

Pyrite and traces of chalcopyrite for a total of2%, occuring generally as replacement of felsicminerals in fine stringers or associated withcrosscutting veinlets of secondary quartz.Pyrite is also found disseminated as anaccessory mineral. The main mineralized zone islocated from 92.0 to 84.75' where mineralizationis composed of 5% pyrite and It chalcopyrite.


The rock is composed of hornblende ( 20*), biotite(15%), feldspar (45%) and quartz (20t). Therock has gradational contacts with quar t z-plagioclase-hornblende schist and has inclusionsof biotite schist. The gneiss is a medium-grained rock of greenish grey colour and has amottled aspect from hornblende and biotite.Bands of more quartz-feldspar-rich content arefound in contact zones.

Unmineralized .

88.5 to 89.189.3 to 89.6 BIOTITE SCHIST96.75 to 97.1

Medium-grained, dark green rock. Biotite is themain constituent varying from 70* to 90% of therock. The remainder being quartz and feldspar.Chlorite occurs as alteration product of biotite.

H*nv*•A FOOT* C C •Jt,rt*

A

0***

S S A Y

O* /f*"

A*

S

Ot/tM

1

LATITUDE '

ELEVATION i

MOND DKILL RECORD'ROPERTY i Matthews Township OntarioW- 4 LENGTH ' 300'41-4.Q7W 7A.I.R7QT *j T ^ , o At^TUA^

DEPARTURE 'O fi

' AZIMUTH' 178 DIP t 45August 25, 1984 F1NISMED ,

FOOTAGE 01 R AZIMUTH FOOTAGE OIR AZIMUTH

HOLE No. i W 4 SHEET No. i 9

REMARKS'

LOGGED BY* Daniel Labadier o o i

r MOM

98.1

- A a e

TO

125.2

DESCRIPTION

Unmineralized .

QUART2-PLAGIOCLASE-HORNBLENDE SCHIST

The rock has approximately 15S of crosscutting granitic veins or veinlets of quartz, ranging from 1/8 inch to 1 inch. Chlorite is present as alteration product of biotite and hornblende.

Traces of disseminated pyrite and magnetite. Pyrite is sometimes found with veinlets of quartz. 5% pyrite from 124.0 to 124.5' as replacement o/ felsic minerals.

106.0 to 106.4

Band of biotite-hornblende-quart z- feldspar gneiss.

Unmineralized .

At 105.5, 108.5, 111.0 and from 119.4 to 120.4 ROCK- FISSURES

Characterized by an assemblage of white to light grey calcite, epidote, actinolite and traces of siderite; all as crystals ranging from 1/20 to 1/8 inch in diameter. Calcite is the main constituent making up 80* of these zones, epidote being the second main mineral.

H*.•t,

wlpkUwFOOTAOE

V.

A

•A

S S A 1

Ox /ten

Aa

S

Oi/ra*

-

HOLE Na-

LOCATION '

LATITUDE ' ELEVATION t

STARTED t

MOND DKILL RbCORDPROPERTY' Ma t" l"h ** ws Township Ontario

W-4 LENGTH ' 300*43+97W 24+82S

DEPARTURE 'O O

t AZIMUTH' 178 DIP ' 45**^*y UO L, f. *j g JL*7Q** pi M 1 S M P Q i

FOOTAGE 01 R AZIMUTH rOOTAGE OIR AZIMUTH

HOLE Mr : W-4 SHEET No. : 1 0

REMARKS!

LOGGED BY. Daniel Labadie

r o o T A e e

FROM

125.2

130.5

TO

130.5

149.4

D E. 3 C M 1 PTION

The quart z-plagioclase-hornblende schist isgradually carbonatized and epidotized close tothese zones.

Traces of pyrite.

BIOTITE-HORNBLENDS-QUARTZ-FELDSPAR GNEISS

One-inch thick granitic vein at 126.9*.

Traces of disseminated pyrite, the averagegrain diameter is 1/20 inch.


Dark green, fine-to medium-grained rock withvariable amount of crosscutting veinlets ofquartz and granitic veins varying in size from1/10 to 1 inch. Many narrow bands of moreamphibolitic composition, averaging one inchthick, and where hornblende makes up to 90% ofthe rock have been observed. Sulfidemineralizations are closely associated withthese amphibolite zones. The felsic minerals,like quartz and feldspar , rarely exceed 30% involume of the rock.

135.5 to 135.75138.25 to 138.50 - 5% pyrite142.25 to 142.6

SAMPLE

H*.

1120(

•AwMpfcUM

5 147.0

FOOTAGE

147.7

•h •A Oi /fen '

Au

traces

Oz/to*

-

traces

9

DIAMOND DRILL RECORD'NAME OF PROPERTY t Matthews Township OntarioHOLE Nat

LOCATION :

LATITUDE '

ELEVATION ^____^_^___STARTED .August 25, 1984

W- 443+97W

LENGTH t 300'24rS2S

DEPARTURE *i AZIMUTH: 178 DIP . 450

POCTAOE DI R AZIMUTH rooTAoe Oil! AZIMUTH

HOLE No.'W-4

SHEET No. t. 11

REMARKS t.

LOGGED BY i Daniel Labadier o o i

FROM

149.4

- A o e

"O

153.4

DESCRIPTION

145.5 to 147.7

2% pyrite, traces amounts of pyrrhotite, andchalcopyrite. The main sulfide-rich zone istraced from 147.0 to 147.7', where it is foundpyrite 6 % , pyrrhotite 4%, with trace amountsof chalcopyrite. Sulfide occurs as partialreplacement of felsic minerals in narrowstringers following the foliation of the rock.These mineralization are restricted to morehornblende-rich zones in the quartz-plagioclase-hornblende schist .

PEGMATITE

Light pink to pinkish grey rock. The pegmatitegrains range in size from 1/8 inch to 3/8 inchin diameter with the average diameter being1/4 inch. Microcline with pink perthiteinclusions is the main mineral making upapproximately 45% of the rock, with quartz 30%and Albite 25%. Trace amounts of biotite andhornblende have been noted. This graniticpegmatite occurs as vein cutting the quartz-plagioclase-hornblende schist.

Unmineralized.

Ho.•fm

mlpkMMFOOTAGE - •A ••/m Oz/to*

Au

Oz/IM

-

DIAMOND DRILL RECORD'NAME OF PROPERTY' Matthews Township OntarioHOLE No. i

LOCATION '

LATITUDE 'ELEVATION

W-4

43+97W

.

\uqust 25,

LENGTH '24+82S

DEPARTURE

AZIMUTH :

1984 FINISHED i

300'

:

17R0 DIP ' 4SO

FOOTAGE OIK AZIMUTH FOOTMC OIR AZIMUTH

HOLE No. t W-4 SHEET No.:.

REMARKS'______________.

LOGGED BY' Daniel Labadie

F O O 1

FROM

153.4

'ACE

TO

269.6

DESCRIPTION

QUARTZ -PLAGIOCLASE- HORNBLENDE SCHIST

Dark green to black, medium-grained rock withcrosscutting veinlets of quartz and graniticveins .

Trace amounts of disseminated pyrite andmagnetite. Pyrite is rarely found in stringersexcept from 163.25 to 163.4', where the rock isfound to contain l % of pyrite and pyrrhotitewith trace amounts of chalcopyrite. From 202.25to 202.35', the rock contains 5% of pyrite andtrace of pyrrhotite. In these zones.mineralization is found in narrow stringers aspartial replacement of felsic minerals in/oralong the crosscutting veinlets or quartz.

159.25 to 159.4 inn o t-* i fti f PEGMATITEloU . y to lol . Z

This light grey rock occurs as veins cuttingthe quartz-plagioclase-hornblende schist.Pegmatite grains range from 1/8 inch to 1/2inch. The average composition of the rock is:Quartz 35%, Albite 40t and plagioclase 25%.Hornblende occurs as an accessory mineral.Veins are 3.5 inches in thickness. This rockis unmineralized.

Ho.V.

MtBMdM

SAMP L E

FOOT* 0 E •h •h O* /to*

Au

O* /to*

-

DIAMOND DRILL RECORD'NAME OF PROPERTY i

HOLE No. i ____W-4

LOCATION ' -

LATITUDE ' — ELEVATION '

Matthews Township OntarioLENGTH '300!

43+97W 24+82SDEPARTURE

AZIMUTH: DIPSTARTED .August 25, 1984 FIN1SHEO ,

FOOTAoe DIP AZIMUTH II FOOTAGE

N" 11

l

H

DIP AZIMUTH

HOLE No.! W-4 _ SHEET No.:

REMARKS' ———^^-—-—---—

13

LOGGED BY'Daniel Labadie

f 0 O 1

F ROM

' A a t

TODESCRIPTION

185.0 to 185.6 BIOTITE GRANODIORITE GNEISS

This intrusive is unmineralized.

188.4 to 188.8192.0 to 193.6 BIOTITE-HORNBLENDE-QUARTZ-FELDSPAR 202.5 to 206.7 GNEISS

Here biotite rarely exceede 5% by volume of the rock.



Medium-grained, dark green to black rock with round amygdules of quartz and phenocryst s of plagioclase. It is predominantly a quartz- plagioclase-hornblende schist. The rock is composed mainly of hornblende replaced in part by chlorite.


207.8 to 235.5

The quartz-plagioclase-hornblende schist becomes gradually lighter in colour as quartz and feldspar increase the felsic proportion of the rock. Hornblende is the main constituent with

IhkWQ.

•ASAMP L C

FOOT* 0 E 'h

A

*/.

3 S A Y

Ox /tan

A*

S

Ox /tom

DIAMOND DRILL RbCORDNAME OF PROPERTY J Mr* f t" h*1 1-7 *5 Tnwnch-ip nn*-pt--i n

HOLE NO.I W-4 LENGTH t 300"LOCATION . 43+97W 24+82SLATITUDE i DEPARTURE i

O r*ELEVATION' AZIMUTH: 178 DIP i 45STARTED . August 2 5 , 1 984 FINISHED -.

FOOTAOC OIK AZIMUTH FOOTAGE OIK AZIMUTH

W-4 14 HOLE NdL t SHEET No. 8

REMARKS)

LOGGED BY'-J2anieTi J.^hrirti**

r o o i

F ROM

r A e r* w t

TODESCRIPTION

701 by vola 3 of the rock instead of 80%, whichwas the usual proportion of hornblende.

227.4 to 235.5

The rock shows a relative segregation ofminerals and is partly gneissic.

234.75 to 235.2

Altered zone. Epidote is the main constituentwith 50% by volume of the rock, quartz, calciteand hornblende make-up the remainder with 25t ,10% and 15t respectively.

^ of disseminated, wee-formed pyrite as anaccessory mineral.

235 5 to 237.25 BIOTITE-HORNBLENDE-QUARTZ-FELDSPARGNEISS

Biotite rarely exceeds 2 % by volume of the rock.

Unmineralized .

237.25 to 238.25

Here the quartz-plagioclase-hornblende schisthas approximately 5% of epidote and partlychloritized.

H*"•A

SAMP

.

L E

FOOTA6E *i •/. Ox/Ten

Au

Ox/ten

DIAMOND DRILL RECORD'NAME OF PROPERTY ' HOLE No. i _ W-4 LOCATION ' — LATITUDE ' — ELEVATION ' ,

Mat-th^ws Townshi OntarioLENGTH * 300'

43+97W 24+82SDEPARTURE AZIMUTH' DIP.

45V

STARTED t August 25,

FOOTAGE DI R AZIMUTH II rooTAoe

H

OIK AZIMUTH

HOLE No. t W-4__ SHEET No. tJ.5

REMARKS'

LOGGED Labadie

root

FROM

269.6

r A a E

TO

274.0

DESCRIPTION

J.% of disseminated pyrite. Often associated with epidote.

238.25 to 240.25 HORNBLENDE-QUARTZ-FELDSPAR GNEISS

Biotite is not present. The rock is medium- grained rock of greenish grey color with some pink feldspar grains. Epidote occurs as an accessory mineral.

1* of disseminated pyrite


Trace amounts of pyrite as an accessory mineral.

266.7 to 267.4 GRANODIORITE

Fine-to-medium-grained, light grey rock. Occurs as vein in the quartz-plagioclase-hornblende schist .

Trace amounts of very fine pyrite.


Medium-grained, lj.ght grey rock with narrow inclusions of quartz-plagioclase-hornblende s' 'list . The rock has sometimes an augen-type structure but more commonly a lepidoblastic

L . ei^r-nril-jLLCfi —————————————————————————

" HanOv

•ASAMP

FROM

L C

FOOT* e eTO TOT AU

•f. •^ Ot/tow

Aa

Ol/te*

DIAMOND DRILL RbCORDNAME OF PROPERTY i Matthews Township OntarioMOLE NO.I W-4 LENGTH t 3 00*LOCATION . 43+97W 24+82SLATITUDE i DEPARTURE :

O OELEVATION: AZIMUTH' 178 DIP' 45

STARTED * AuqUSt 25, 1984 FINISHED t

FOOTAGE OH! AZIMUTH rOOTAOC

—DIP AZIMUTH

HOLE No. t W-4 SHEET No. * 1 6

REMARKS'

s-^P fi PI 1 -^J U'Ut

lLOGGED BY-- Daniel T.flhadies

r o o T A o E

FROM

274.0

281.7!

TO

281.7!

300. (

300.0

DESCRIPTION

Unmineralized.


The rock is highly intruded by distorted granodioritic material. Biotite makes up from 25 to 40% of the rock and is formed instead ofhornblende. Chlorite occurs as an alterationproduct of biotite. The rock has a mottled effect by the granodioritic material.



The rock has approximately 20% of inclusions which consist to the quartz-plagioclase- hornblende schist. Both lepidoblastic and augen-type structure have been noted. This rock is a gneissic equivalent of the granodiorite .


END OF HOLE

SAMPLE

No.•A FOOTA6C

A 2 SAYS

•t. •A Ox /to*

Au

Of/ton

-

2-43*90

32*005 2StOOS 24.82S 24*005

SOO

BIOTITE-GRANODIORITE GNEISSGronodiorite

QUARTZ-PLAGIOCLASE (CHLORITE) HORNBLENDE SCHISTBIOTITE-HORN BLENDE-QUARTZ-FELDSPAR GNEISS

. AMPHIBOLITE\XBK)TITE-GRANODIORITE GNEISS

*~~T-~BIOTITE-HORNBLENDE-QUARTZ- FELDSPAR GNEISS QUARTZ- PLAGIOCLASE- HORNBLENDE SCHIST

BIOTITE - HORNBLENDE-QUARTZ- FELDSPAR GNEISS

- Biotite- Hornblende- Quartz - Feldspar GneissQUARTZ-PLAGIOCLASE-HORNBLENDE SCHIST

-Biotite-Hornblende-Quartz-Feldspar Gneiss ~ tz-PlogiC'dast-Hornblenu'e Gneiss

i blende-Quart z-Feldspar Gneiss

BIOTITE-GRANODIORITE GNEISS QUARTZ- PLAGIOCLASE- HORNBLENDE

BIOTITE - GRANODIORITE GNEISSSCHIST

ALTERED ZONES


SECTION SHOWING No* W-42-43*91 W

EXECUTED ST COl SURVEYS inc.

SUPERVISED f o. L*BAD'E

SCALt "" * 50'

AZIMUTH : US'

DIP 43*

DATE AUGUST

DIAMOND DRILL RECORD'NAME OF PROPERTY '

HOLE No.. W-10LOCATION . 16 + 72W

LATITUDE .

ELEVATION tSTARTED . August 25

Mat-f-hftWS TnwnfifHn Onl-^-r i rt

LENGTH i0 + 78S

DEPARTURE '

AZIMUTH', 1984p| NIS HED .

150'

500 DIP , 450

rooTAOE OIK AZIMUTH i POOTAOe

H

OIK AZIMUTH

HOLE No. t W- 10 SHEET No. t

REMARKSt -——————.^——70'


r o o i

FROM

0

50.0

' M fl e

TO

50.0

134.0

OeSCMIPTION

OVERBURDEN

GRANITE

Massive medium-grained pink to pinkish grey rock.Granite grains range in size from 1/10 inch to3/8 inch with the average diameter being 1/8 inchPink to red potassium, feldspar is the mainmineral making up approximately 40 to 50% of therock, quartz and plagioclase making up 25% and15% respectively. Epidote, chlorite andhornblende becotr locally important, varyingfrom 10% to 20% by volume o f the rock.Reddening of the granite is common along thefracture planes. The red colour is due to thehematization of the feldspars.

Trace amounts of pyrite and magnetite asaccessory minerals.

59.0 to 60.0

Altered zone where the rock has an earthy aspect .All ferromagnesian mineral tend to weather out.leaving pale-green coloured cavities on thesurface. In some places, feldspar has beensaussuritized and sericitized. Minor amountsof calcite have been noted. This assemblage ofchlorite, saussurite, sericite, hematite andcalcite gives an argillaceous aspect to the rock.

H*.•A

MlpkMM

SAMP

FROM

L eFOOT A a efo "" 1 TOTAL

•h •h Ol/t**

A*

Ox /le*

DIAMOND DRILL RECORDNAME OF PROPERTY i

HOLE No.'

LOCATION "

LATITUDE '

ELEVATION

Matthews Township OntarioW-1016+72W

LENGTH i0+78S

150'

DEPARTURE ',

Auaust 25,AZIMUTH'

. 1984?INISHED '

SO0DIP ' 45

FOOTAGE OIK AZIMUTH rooTAoe OIK AZIMUTH

HOLE No., W-10 S HEET No ; 2

REMARKS'^—-——-—^™..——-


r o o T A o e

r rtoM

f1

TODESCRIPTION

Unmineralized .

71.25 to 72.2575.0 to 80.0

The rock has approximately 40% by volume ofquart z-plagioclase-hornblende schist partlyassimilated by granite. This hornblende schistis partially feldspathized. The rock has alight pinkish grey colour. The composition of thegranite is more mafic. Chlorite occurs as analteration product of hornblende in some places.The remnant of the schist are recognizable onlyby a more hornblende-rich zone in the granite.

Unmineralized .

95.1 to 97.1 MYLONITIZED FAULT PLANE

Highly altered zone with an argillaceous aspectand where granite and quart z-plagioclase-hornblende schist are intimaly admixed. Fron.95.0 to 95.5 ' the rock is crumbly and givesway to a mylonite, which is a reddish brown rock.with black and reddish white angular fragmentscemented by argillaceous material. Thesefragments are severely crushed and distorted.This mylonite is a fault gouge. It is formedonly en the fault plane.

IJnminer^l i z^d .

3 A M P L C

M*.V. . rooTAse

AS SAYS

V. •A O* /f**

Aa

Ox /ton

DIAMOND DRILL RbCORDNAME or PROPERTY t Matthews Township OntarioHOLE No.' W-10 LENGTH i 150*LOCATION t 16+72W 0+78Si ATITUDE i DEPARTURE -'

O rtFLEVATION t AZIMUTH i 50 DIP i 45•STARTED . August 25, 1984 RNISHED .

FOOTAOE 01 R AZIMUTH rOOTAOE DIP AZIMUTH

W— 1 O i HOLE NO. : " SHEET No. :^^^

REMARKS:


FROM

134.0

142.9

~ —— - —

TO

142.9

150.0

DESCRIPTION

100.3 to 105.25 GRANITE

With partially assimilated quartz-plagioclase- hornblende schist, in which the foliation iss ome t ime s appar e n t .

Unmineralized .

109.0 to 134.0

The granite has numerous fracture zones in which the rock is gravelly.

MYLONITIZED FAULT ZONE

This zone is altered and the rock is severely crushed. Only the coarse black fragments could be recognizable as hornblende schist or amphibolite. The fragments are cemented by an argillaceous material which is the main constituent of this mylonite.

Unmineralized .

AMPHIBOLITE

The rock was originally an amphibolite. Hornblende is completely replaced by chlorite, and plagioclase by sericite, making up 85% and 15% of the rock respectively. It is a fine-to

Ho.•A

wlpMdH

SAMP L E

FOOTAGE1 ™ 1 TPTAU

•h •/.

a s A t

OX /(OH

A*

s

O i /ten

DIAMOND DRILL RLCORDNAME OF PROPERTY j Matthews Townshio OntarioHOLE Na* W- 10 LENGTH ' 1 50 '

LOCATION' 16+77W O + 7RS

l ATITUDE ' DEPARTURE 'g- f* W Vi C

FLEVATION t AZIMUTH: 3 U DIP t 4 D

STARTED ' August 25. 1984 FINISHED :

FOOTAGE 01 f. AZIMUTH 11 FOOTAGEIIIIII||—r-

DIP AZIMUTH

win 4HOLE No. . ™ X U SHEET No. t

REMARKS'

s-.f it I I'T * 1 li ' *•A-^v— f ^b-UJvA

LOGGED BY' Daniel LabadieF 0 O 1'ACE

TO

150. (

medium- grained, dark green rock with manyfractures.


END OF HOLE

•h •A ' FOOTAGE •A

A

•f^

S S A Y

O* /to*

Aa

S

Ox /(o*

2-f6* 72

Quartz- Plagioclase- Hornblende- Schist-Granite

A

r^s*'ALTERED ZONES


SECTION SHOWING No* W-10

EXECUTED BY COI SURVEYS inc.

SUCEHViSCD 8* O. lABADIC

SCftct i" -- SO'

AZIMUTH OSO*

OiP 45*

ftATr JK.CIAf

DIAMOND DRILL RLCORDNAME OF PROPERTY s Maf t-h*Mi7R Township Ontario

MOLE No.' W-10B LENGTH t 241*LOCATION . 4*OOW 16+20S

LATITUDE i DEPARTURE :o f r\® M c

ELEVATION - AZIMUTH: -* 60 DIP s 45

STARTED f Aiiqvictl- 9R IQRd FINISHED:

FOOTAGC DIP. AZIMUTH FOOTAGE OIR AZIMUTH

HOLE No.. W-10B SHEET NO.:

REMARKS:

— j. "7*7^^777 f j f t r

LOGGED BY s J2aH.i **1 T.ahart i ft

r o o i

FROM

0

85.0

231.2!

'ACE

TO

85.0

231.21)

241.0

DESCRIPTION

OVERBURDEN


The rock is light grey to pinkish grey. It has alepidoblastic structure, rarely an augen-typestructure. The rock has nun-arous inclusions ofquart z-plagioclase-hornblende schist withgradational contacts. In these inclusionsbiotite is important. This gneiss has numerouszones of fracture with epidote, talc, chloriteand traces of calcite, mainly from 97.25 to115.75' .


149.5 to 152.0 r 189.25 to 192.0 PEGMATITE

I% of pyrite and magnetite in a small inclusion.1/2 inch thick, of quartz-plagioclase-hornblendeschist .

FAULT ZONE

With argillaceous material a^d crossr Lngveinlets of calcite. The roc., is compl^ -elyaltered and has a reddish brown colour.

——————————————————— — ——— -^E— —————————— — ——————————

Ibkno.•A

MlpMtfn

SAMP

rf JM

L E

FOOTAGETO TOTAL

•UPJ** •j^ Ox /Ten

Au

Ox/ran

DIAMOND DRILL RECORD'NAME OF PROPERTY t Matthews Township Ontario___HOLE Nat W-10B________ LENGTH ' 241'^_____^_^_LOCATION i 4 + OOW 16+20S

LATITUDE _______________ ELEVATION ' ______________ AZIMUTH ' 360

DEPARTURE

STARTED : August 25. 1984 FINISHED tDIP : 45

FOOTAGE DIP. AZIMUTH FOOTAQC DIP AZIMUTH

HOLE Ho. t W-1 OB SHEET No. *.

REMARKS:______________

LOGGED BY' Daniel LabadieF 0 0 1

r ROM

' * c e

TO

241.0

DESCRIPTION.

Feldspars are hematized and sericitized. All thezone is highly crumbly. The rock gives way to aclaystone.

Unnt-. neralized .

END OF HOLE.

H..•A

nlpMttMroOTABt •A •A Ox /to*

A*

3

Os /t**

1*4+00 W

6*208 6.00 S 12*003 8^)05 -A-* s * ^* ^.//^Y'//x . ^ . \

X.^ ' x . \

y K/.^ -^ \x * s~ ~ ~/"^•:/-s ^^'s -y

-OVERBURDEN' V^ v--'•/.

* \\ e

\ . S 't ,—

f-'Pegmatite

BIOTITE-GRANODIORITE GNEISS

r^r-^'

, A LTERED ZONES


SECTION SHOWING No-W-10 B

S 16+20 3EXECUTED Br C 01 SURVEYS lit

SuPfviseo 8 " D. UABAtXE

SCfitt i" ' 50'

49*

•* s.,

V

. i Vr1

-o

(M

l

.NJ

NJ

Vi

US4

NJ

U

C,

OD

(JN

si

U

tsj

,o -.

03 O

DIAMOND DRILL RECORDHOLE No. :

W~25SHEET No. s.

NAME OF PROPERTY s Matthews Township OntarioHOLE No." W-7S__________ LENGTH ' 3 00*-——M—— LOCATION s

LATITUDE '

8+50E 14+50 N

ELEVATION -

DEPARTURE - ———^

AZIMUTH: 1 65 DIP.STARTED .August 25, 1984 FINISHED

FOOTAOC DI R AZIMUTH II FOOTAGE

H

DIP. AZIMUTHREMARKS'.


r o o T A o E

FROM

0

20.0

39.25

TO

20.0

39.25

58.0

DESCRIPTION

OVERBURDEN


Medium- grained, dark green rock containingapproximately 5% of crosscutting veinlets ofquartz. The rock is composed mainly ofhornblende making up 80 to 90% by volume of therock, plagioclase being the remainder and rarelyexceeds 15% of the rock. Chlorite is present asan alteration product of hornblende.



Fine-to medium-grained rock of greenish greycolour. The average grain diameter is 1/10 inch.The rock contains hornblende ranging from 15%to 25% by volume, biotite 5 % t o 10%, quartz 25%,and feldspar 55%. This gneiss has a gradationalcontact with the hornblende schist.

Unmineralized .

SAMPLE

to.•A

••IpMtfuFOOTAGE

FROM TO TOTAL

AS SAYS

•A •t. Ox/ton

Aa

Ox /fen

DIAMOND DRILL RECORD'NAME OF PROPERTY t Matthews Township Ontario HOLE NO.' W-25__________ LENGTH ' 300*—————- LOCATION t 8+5QK 14 + 50 N——————-———————.—.LATITUDE i _______________ DEPARTURE -- _ --M.——

ELEVATION t ______________ AZIMUTH : .165 V

DIP45 V

STARTED 'August 25. 1984 FINISHED i

rooTAoe DIP AZIMUTH 1 FOOTAGE

^k

DIP AZIMUTH

—— ..... —— .J

HOLE No. t W-25 SHEET No.:.

REMARKS: ————^———^^—

LOGGED BY -- TV* n i T.ah^rl -i

r o o 1

F ROM

58.0

82.0

' A e E

TO

82.0

86.2

DESCRIPTION

39.5 to 39.7541.1 to 42.045.75 to 46.5

Presence of inclusions, with gradational contactsof amphibolite and quartz-plegioclase-hornblendeschist in the biotite-hornblende-quartz-feldspargneiss .

Unmineralized .

BIOLITE GRANODIORITE GNEISS

With partly assimilated inclusions of hornblendeschist. Hornblende is locally replaced bybiotite. The granodiorite is a medium-grained,light grey rock with a lepidoblastic structure,rarely with an augen-type structure. The mainconstituents of the rock are quartz, feldsparwith a lesser amount of biotite and hornblende.


HORNBLENDE SCHIST

Fine-grained, dark green rock with some pinkstains. The rock becomes cherty from 83.0',with some dark green angular fragments of chert.ranging from 1/4 inch to 1 inch in diameter.

HAI*O.V. .

talpMtf'l FROMFOOTABE

TO TOTAL V. •A Oz/ton

Au

Of /le*

DIAMOND DRILL R LCD R DNAUE OF PROPERTY t Matthews Township OntarioMOLE Na. W~ 25 LENGTH. 300'

LOCATION . 8+50E 14+50 N1 ATITlinE i DEPARTURE'

O OELEVATION* AZIMUTH' 165 DIP' 45STARTED ' Augus t 25, 1984 nNISHEDl

FOOTAOC OIK AZIMUTH rooTAoe DIP AZIMUTH

HOLE No. ' W-25 SHEET No. : 3

REMARKS'

.LOGGED B** - Daniel Labadie

r o o i

F MOM

86.2

' A A C

TO

277.0

DESCRIPTION

This silicified zone is related to a fault.Here the rock is hard and has a conchoidalfracture. Chlorite replaces hornblende in largeproportion.

5% of pyrite and trace amounts of chalcopyriteoccuring as narrow stringers, 1/10 inch thick.these stringers are intermittent.


The augen-type structure is more prominent. Therock has some crosscutting veins of pegmatite andaplite.

Trace amounts of disseminated pyrite as anaccessory mineral.

98.4 tO 98.5 T*T^U *mTH,^103.0 to 103.25 AGMATITE

Occurs as veins cutting the biotite granodioritegneiss. The pegmatite grains have an averagediameter of 1/4 inch. The rock is pink to creamwhite. Potassium feldspar is the mainconst ituant making up 45% of the rock withquartz and plagioclase making up 30% and 25%.

Unmineralized .

H*.

11207

•AMlpMdM

5

r ROM

83.0

FOOTAOCTO

84.5'

• t/*

A

V.

3 3 A *

Ox /to*

Au

traces

s

OS/IM

An "9

traces

DIAMOND DRILL RbCORDNAME OF PROPERTY * Matthews Township OntarioHOLE NO-IW-?^ LENGTH i 300'LOCATION. 8+50E 14 * SONi ATITUOE i DEPARTURE '

O OFI FVATION i AZIMUTH' 165 DIE i 45

. ** f 4 f\ f* j|STARTED t August 25, 1984 FINISHED .

FOOTAOC DIP. AZIMUTH FOOTAOC OIR AZIMUTH

W-25 4HOLE No. ' SHEET No.' ————

REMARKS'

LOGGED BY. Daniel Labadie

r o o i

FNOM

277.0

' A a e

TO

300.0

DESCRIPTION

152.7 to 155.5 APLITE

Aplite is a fine-grained, pink coloured rock.Its composition is that of a granite. Biotitemakes up lO% of the rock. Aplite has a "sugar"texture.

Unmineralized .

221.1 to 221.7 PEGMATITE 244.7 to 245.3 rt.wiAij.it,

Unmineralized .


The rock has a more mafic composition,containing 60% by volume of hornblende andbiotite, replaced in part by chlorite. The rockhas some crosscutting veinlets of calcite,partially weathered out.


294.1 to 294.7 APLITE

Occurs as vein. It is a fine-grained, pinkcoloured rock. Its composition is predominantlygranitic. Biotite makes up 10% of the rock.Quartz rarely exceeds 20%.

H*.•A-

wlpkUu

SAMP

FROM

L er DOT* e e1 ™ 1 TOT* l

•h

A

•A

* S A Tf

Ox /t**

An

S

Oi/to*

DIAMOND DRILL RECORD'NAME OF PROPERTY i Matthews Township OntarioHOLE No.W-25LOCATION LATITUDE ELEVATIC STARTED

LENGTH ' inn't 8+50E 14+50 N

. i rtPARTURE 'IN' AZIMUTH' 1650 DIP,' 4 ^O.August 25, 1984 FINISHED .

FOOT A 0 E

FROM TO

300.0

DESCRIPTION

FOOTAOC 01 R AZIMUTH FOCTAOC OIR AZIMUTHREMARKS'

LI y . jQf

fi r t

J-A^j-*\A

LOGGED BY' Daniel r.aharH**

Unmineralized .

END OF HOLE;

k A M P L C

N*.•A FOOT* 6 E

FROM TO TOTAL

AS SAYS

•h •A Ox /to*

Au

O* /M*

2-1*5014jOON 12 .DON W.50N 16*00 N

300'

f

QUARTZ- PLAGIOCLASE- HORNBLENDE SCHIST"Amphibolitt- Biotttt- Quortz - Ploglodost- Hornbtondt-Ftldspor Schist 6n*iu

BIOTITE - HORNBLENDE-QUARTZ- FELDSPAR GNEISS

BIOTITE- GRANODIORITE GNEISS ORNBLENDE SCHIST

BIOTITE - GRANODIORITE GNEISS

iplil*

Pegmotiti

BIOTITE - HORNBLENDE - QUARTZ - FELDSPARGNEISS

: SO

LOBO GOLD RESOURCES Inc.Motthews twp , Ontario

SECTION SHOWING No* W-25J-MO t /

CXCCUTCD C 01 SuRVtvS

1 a i.*t*DitSCALt

AZIMUTH 165-

OiP- 43*

O AT t AUGUST

s?-lv-is r-

N K

' '

' v

— tsi n V

D'ANALYSE BOURLAMAQUE LTtE

BOURLAMAQUE ASSAY LABORATORIES LTD.

C.D.I. Surveys Inc.

CCHANTILLONS SAMPLES ........

RECU DE RECEIVED FROM

CERTIFICAT D'ANALYSES CERTIFICATE OF ANALYSIS

41595 J

.core.................................................. VAI D-OR. ou*., ......™?.ll™...___~~ w 84ANALYSES ASSAYS .

Echantillon Au Oz/ton Atf oz/ton Mo

11201 Trace Trace

11202 Trace Trace0.225

L .ANUYSTC l ASSAYCR

i i*io, MVCMOC

LABORATOIRE ^'ANALYSE BOURLAMAQUE


C.D.I. Surveys Inc.

CCHANTILLONS SAMPLES ...... rock

RECEIVED FROM .......White...JRiver....

CERHHCAT D'ANALYSES CERTIFICATE OF ANALYSIS

41612 JVAL D-OR, QUt. ___.SSEtlJi-——

2 Au. 2 Ag.ANALYSES ASSAYS

Echantillon Au oy/tow Ag oz/ton

11206 Trace Trace

11207 Trace Trace

ANAIYSTE X ASSAYCR

t j -A

*.r. f T .w*

LABORATOIRE D'ANALYSE BOURLAMAQUE LT(E


C.D.I. Surveys Inc.CERTIFICAT D'ANALYSES

CERTIFICATE OF ANALYSIS

L 41641ECHANTILLONS core , Sept. 14SAMPLES ......••••••••••.....•***i..**.........*..*........*.......-.*...*......,...*...,,,.,.., VAL iXORf QUE** t*************************************

bus collect ANALYSES i An i Ani.......................................................................... ASSAYS ,,.............M...T:..,;^™!,...r'....'?:.a.?..,RECU DE RECEIVED FROM

Echantillon Au oz/ton Ag pz/ton

11208 Trace Trace

AHALYS/t l ASSAYfft

m..tES RELEVES

SURVEYS INC.53, rue AltardVald'Or, Que. J9P 2X9

T6I.: (819) 825-6263*

September 17, 1984 Val d'Or, Quebec.

Lobo Geld Resources Inc. Suite/402, 27,yQueen St. East. .Toronto, Ontario. I5C 2M6

INVOICE

Re: Diamond Drill Project in Matthews Township.

As per letter contract dated August 9, 1984.

Hole: E-30E-40E-52W-10-BW-4 4W-10W-25

Total:

Advance Received:

Balance due:

350 ft. 350 ft. 288 ft. 241 ft. 300 ft. 150 ft. 300 ft.

^1979 ft. a" 3350.00 = 36,926.50

-33,000.00

S3,926.50

Invoice ft 00161

E. Ingham

•fatnoil ~L*iamona atJrillinq

borage a rJjiamant y^tnoit ~J,tt1701 RUE DE L'HYDRO PARC INDUSTRIEL VAL QJWU-OuEBEC J9P4P4 TK/1819 82A9107

Lobo Gold /'Resources Inc, Suitex402,_ xOueen Street East, Toronto, Ontario.

INVOICE FACTURE N2 '2551

Date . Septembre 18th, 193

DRILLING SITEEMPLACEMENT lbLE NoDE f OR AGE White River propegtyjNo f ROM

DUTO A 196

August 22: August 23:

Cost: Cost:

Hole No. W-4: Hole No. W-10: Hole No. W-25: Hole No. W-32: Hole No. E-40: Hole No. E-52: Hole No. W-10-B:

APPROVED BV APPROUVE PAP

5,850.003,105.805,850.006,825.006,825.005,616.004,699.50

77/20

. ^ ^3Z-ji* * t - * ^^ ^ ^

. "V:"- -.'•^ ;,r-^ -w ^

Annexe l, Invoice: 2551,

August 22. 1984: ^ 20 hours at 519.10: 382.00tractor rental: 6 hours at 528.00: 168.00

r ^ -' August 23, 1984: - v "' '' "'

labour.: 26 hours at 519.10: ^496.60 tractor rental: 4 hours at 528.00-^112.00

\ 5 1,158.60 \

Hole No. W-4, from Aug/25 to Aug/30, 1984.

Drilling in overburden:from O' to 12': 12 feet at 519.50: 234.00

Drilling in bedrock:from 12' to 300': 288 feet at 519.50: 5.616.00

5 5,850.00 '

Annexe 2,Hole No. W- 10, from Aug/30 to Sept/1, 1984.Invoice: 2551.

Drilling in overburden:from O 1 to 26': 26 feet at $19.50: 507. CO

Drilling in bedrock:from 26' to 150': 124 feet at 519.50: 2,418.00

Recovery of casing:labour costs: 6 hours at 519. 10: 114.60

labour costs: 2 hours at 519.10: 38.20 tractor rental: l hour at 528.00: 28.00

3,105.80

Hole No. W-25, from Sept/1 to Sept/4 1984:

Drilling in overburden:from O' to 12': 12 feet at 519.50: 234.00

drilling in bedrock:from 12' to 300': 288 feet a t 519.50: 5,616.00

5 5,850.00

Annexe 3,Hole No. W-32, from Sept/5 to Sept/8, 1984,Invoice: 2551.

Drilling in overburden:from O* to 20': 20 feet at 519.50: 390.00


6.825.00 "

Hole No. E-40, from sept/8 to sept/10, 1984:

Drilling in overburden:from O 1 to 28': 28 feet at 519.50: 546.00


5 6,825.00

Hole No. E-52, from Sept/11 tc Sept/13, 1984: Drilling in overburden:

from O 1 to 10': 10 feet at 519.50: 195.00

Drilling in bedrock:from 10- to 288': 278 feet at 519.50: 5,421.00

5 5,616.00-

Hole No. W-10-B, from Sept/14 to Sept/16, 1984:

Drilling in o"*rburden:from O' to 85': 85 feet at 519.50: 1,657.50


5 4,699.50

— — —l- ——ll SSM SSU l

4aC13NE8681 18 MATTHEWS-4--V~T ———'

l • ei* ij SSM f SSM

i—i—n—

~"~ ~ ~7/4304) 774288 774287 | f7 74286

L" —— 4 ——— .- ——— i-' — -SSM SSM SSM J| SSM

7743OS l 77430S 774307 (774308 j, __ __ - . _ .J- — 4

-- ,,-.,... 774311 1/774310! 774309

L —— -j —— --i —— H ———

774313 (774314/1/774315 l 774316 |

J-i__ -

HAMBLETON TWP. G-2

Ministry ofNaturalResource".

Report of Work

OntarioMining Act

Instruction* - Supply required data on a separate form for eachtype of work to be recorded (tee table below).

- For Geo-technical work ute form no. 1362 "Reportof Work (Geological, Geophysical, Geochemical andExpenditures)".

Nettie aiiJJv.tel Addret* of Recorded 1 'older ————————————————————————————

LOBO GOLD fi, RESOURCES INC.Pioioector'i Licence No.

T-1669

SUITE 500-67 RICHMOND STREET WEST, TORONTO, ONTARIO, M5H 1Z5Summary of Work Performance and Distribution of Credits 'Total Work Day* O. claimed

L979 "r.lot Performance of the following S S

O Manual Work

Q Shaft Sinking Drifting orother Lateral Work. ' '

Qcompresied Air, otherPower driven ormechanical equip.

Q Power Stripping

drilling jv j-LjLand Survey S. -tt;.

All the work wet performed on Mining

Required Information eg: type of

Benoit Diamond Dri1701 rue De L'HydrPare Induatriel,Val d 'Or, Quebec. J9P 4P4

C.D.I. Surveys Inc53 rue Allard,Val d 'Or, Quebec.J9P 2X9

,

Mining Claimfix | Number

M 7738667*73867

77J868

773869

773870

773871

^,, 773872

&1 773873

Workn.y. r.,.

85

85

70

70

80

85

80

70

Mining ClaimPrefix

SSM

-.. . i-

•'.- - .*V ^'sfc' !-' '

3u^4*i5'^'!^ 3&A4;*jBj ^1.•J*** •W "i*vi-.

Number

773874

773875

773876

773877

773878

773879

773880

773881CM): S SM 7 7^!^ 8 75 ' 8 77 ' ™ '

BO/" ——equiprBeTTr^-^^Vglvjyjewaii.cStlRW*

ARESfcAHC*rt CiFlCEllin j Ltd.o j m

REG— -— —— -

m

0*1985

E IV E D—— —— — —

WorkDay* O.

70

70

70

70

70

70

70

70

Mining Clelm vVor -Prefix Number Day* w

773882 70773883 70

5^73884 70..,- 773885 70

773886 70'.^-L 773887 70. -^jj, j ,

giJSL 773888 70jmjBPS ———————— ———— *m. 7 73889 - M

88(5- 881, 882, 884, 886"*

'able Below) Af/fTT^f^^ ~f~M/?,

-~??U4-t6t0L' tQ&TJL /^/35.

.y

rDaTfrof Report

\7 j? /i

B^TTcn"UN 2^"ttr?*T ^^ ^

i u ^^ * **^U^J j^^Jf^^ J fll tifi^i^

^^^ ^^ 1 *^/ aW \ gf MeLf J*V Zff

*l' Recocded Holder qfAoent^Slgneture)fo S/ sZ*~ — f - , y^n 1

Certification Verifying Report of Work1 hereby certify that 1 have a personal and intimate knowledge of the fact* let forth in the Report of Work annexed hereto, having performed the work or wltneued lame during and/or after It* completion and the annexed report i* true.

Neme end Pottal Addre** of Perton Certifying

Z. I ngham, 53 rue Allard, yDate Certified J s* Certlfivpyf'ISignatuMiJf- S'

Val d 'Or, Quebec. J9P 2X9 / v/f/ft (. jZ*f^~~Table of Information/Attachments Required by the Mining Recorder f/ ' s

Type of Work

Manual Work

Shaft Sinking, Drifting or Other Lateral Work

Comp'etied eli, ithe' power driven or mechanical equip.

Power Stripping

Diamond or other core drilling

tend Svrvey

Specific Information per type

Nil

Type of equipment

Type of equipment and imount txpended. Note: P'oof of actual cost mutt be *ubmitt*d within 30 day* o' ne O' d ing.

Signed cor* log *howing. footage, diameter of cote, number end angle* of hole*.

Name ano addreu of Ontario land lurveyer.

Other Information (Common to 3 or more type*)

Name* and eddre**e* of men who performed manual work /opereted equipment, together with detet end hour* of employment.

Name* and add'e**e* of owner or operator together with date* when drilling/itripplng dona.

Nil

Attachment*

Work Sketch: thete are required to ihow the location end extent of work In relation to the neaiett claim poet.

Work Sketch (M above) In duplicate

Nil

6*"1'J1 ///f t * SSA? 773*^7

DRILL HOLE NO. CLAIM NO. LENGTH

-W-25 773880' 160'773S79/ 140'

-W-4 773867, 300'

W-10B 773877' 241'

W-10 773S73/ 70'773874' 60'773875. 20'

-E-30 773880' 350'

v.E-40 773886' 350'

E-52 773887 J 288'

LOBO GOLD 5, RESOURCES INC,

Report of work-continued

SSM 773890773891773892

70 days70 days70 days

SEE MA? (5)

Off AM M EL SEQUENCE C x)

l/v TfeTHE

AM P a REGIONAL GEOLOGY

LEGEND

ARCHEANGRANITIC ROCKS

l 4 Gronilic r ocks, Undiftefe nlioied ! 4c Feldspor porphyry

-J 4d Bioin granite gneiss 4e Pegmatite

M ETASEDIMENTS and METAVOLCANICS

Uj Uj

'l Geological buundory , pcs'Von mter- I preied

5 miles

28-fOO N

24400 N

20+00

16 400 N

12 400 N

8 +00 N

4 400 N

B. L.0400

4 400 S

8 400 S

12 400 S

16 400 S

MATTHEWS TWP

LO C AT ON MAP

LEGENDPROPERTY^

Profiles-40 07o O ut of Phase40 Vo In Phase

^•^f M T

W^WCONDUCTOR AXES

42C13NE8681 10 MATTHEWS 200

LjJPROPERTY

U.J i h

,M.4

HI..*) f i) D

4

36400 S

l l

-A

-6

-Si-

-M

-I2't2

INDEX MAP a REGIONAL GEOLOGY

38 6

240

21

LEGEND

SYMBOLS

mi

-16! 2

-20-0i i1

-23!i

-25

-29

-33

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-33

-42

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tri

ti

^28.l

, -39.39

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~\ -'-22 \ !

LOCATION MAP

LEGEND

YL.F Profiles1440 0Xo In Phase -40 0Xo Out of Phase

xx.

ROAD

LAKE

RIVER

SWAMP

—— CONDUCTOR AXES



•l .' l l. L. l f.l f : l T. .1, (t EI. '.t I Itf J

l i-M-.pji pi"!",r i 4'! H I 'ltit gi i.nle•tt F

PROPERTY

MATTHEWS TWP

LOCATION MAP

(w-2o)

(\fr-19j LEGEND

VL.F Profiles* 40 Vo In Phase -40V. Out of P hase

VLF SUF

COMPILED R DF

APPROVE

CONDUCTOR AXES

42C13N6868I 10 MATTHEWS

Val D'Or , Quebec, July 1 983,

INDEX MAP s REGIONAL GEOLOGY

, i - (9 \,-* ' (f - " ~i ' T - 1. \ i \

" c PROPERTY

MATTHEWS TWP

i.OCX! r/O/V

PRO&ERT

-40V. Out of Phase440Vo In Phase

V.L.F SURV

CONDUCTOR AXES

COMPILED a DRAW

APPROVED BY ;

Val D'Or . t Quebec . July 1 983.

Lowlands

Lowlands


LEGEND


4 GfoniVc rocks, lindtdere nt loted 4c Feldspor porptiyr/

—— - J 4d Biotit gruniie gneiss 46 Pegmoiite

METASEDIMENTS and METAVOLCANICS

Uj

8

T.L.10- ' l

T * j G :i e is-;os i rv, f i ne i 1 ri ed, ve r t'col)

5 miles

MATTHEWS TWP

LO CAT ON MAP

(w-19 ) LEGEND

Profiles-40 07o Out of Phase+ 40 7o In Phase

I M 7V^^

CONDUCTOR AXES

48400 N

44+00 N

40+00 N

36+00 N

32+00 N

28+00 N

B.L. 25+OU N

24+00 N

20+00 N

16 +00 N

12 -tOO N

LOBO GOLD RESOURCES Inc.

MATTHEWS TWP

ONTARIO

PART EAST

VLF SURVEY "PROFILES"Inst, EM-16 Station CUTLER (NAA) Freq- 17.8 kHz

EXECUTED BY ' CD l surveys inc.

COMPILED a DRAWN BY : 5. RHEAUME

APPROVED

Val D'Or , Quebec, July 1 983.

i L

4 d,o

0L3 SM3H11VW 01 t99B3Nei3St7


LEGEND

oo

SYMBOLS-J -J -J

10

-5*

-61

-8

-II-' l

.124!

-I9.V

1 -23!

-25

-29

-33

iii

-33'

-42

-43i

i

iii-28

, -3S^9

f \ -25t-l1 V1 i

1 j i

0 ' -32'

j' y a! 0 . -2& 1\ '\ '

l l '' l i1-1 . -27

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l il i

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6

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-4

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38

30.

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TWPMATT

LOCATION MAP

LEGEND

Profiles-40Vo Out of Phase

CONDUCTOR AXES

N

4 -.J t' N

B L

4 o

-t .

4 V S

G f V M - h

b

24KA- S

28*1.


MATTHEWS TWP

ONTARIO

PART WEST

YL.F SURVEY "PROFILES"Station; CUTLER (NAA) Freq'17.8 kHz

GDI surveys inc.

COMPILED a DRAWN BY-- 5 . RHEAUME

APPROVED BY'

Vat D'Or . Quebec, July 1983.-—- --— *—— —— * - r i —--- .



-7.' (E-53 )L \^y

B.L. 25*00 N

MATTHEWS TWP

LOCATION MAP

MATTHEWS TWP

LEGEND

V.L.F Profiles

ONTARIO

PART EAST-40 0Xo Out of Phasel. *40 V* In Phase

VL.F SURVEY "PROFILES"Station CUTLER INAA

EXECUTED BY CD l surveysCOMPILED ft DRAWN PY -- S . RHEAUME

— CONDUCTOR AXES

ValDOr . Quebec. July 1983

INDEX MAP a REGIONAL GEOLOGY -

: V,

V.

MATTHEWS TWP

LO C A T ION MAP


MATTHEWS TWP

LEGENDPART W EST

-40 8/. Out o f P hase440 0Xo I n Phase

V.L.F SURVEY PROFILESStation- CUTLER ( NAA)

C D l surveysCOMPILED d DRAWN RY ' 5 . R HEAUME

CONDUCTOR AXES

008 Val D Or, Quebec. July 1983.

^

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