DENTON010

NEWMONT EXPLORATION OP CANADA LIMITED

A GEOLOGICAL, GEOCHEMICAL ANDGEOPHYSICAL REPORT ON THE

BROWN-McDADE OPTIONDENTON TWP., ONTARIO

SUBMITTED FOR ASSESSMENT CREDIT ON CLAIM NO. P.568473

JUM -

Submitted by,

R.A. Archer Project Geologist May, 1987

42Aesseei32 2.i ei ea DENTON

CONTENTS

IntroductionProperty Location, Accessand DescriptionRecorded HolderSubmitting PartyAcknowledgementsPrevious WorkRegional GeologyLithogeochemistry and Property GeologyElectromagnetic SurveyDiscussionReferences

O10C

PAGE

1

2223468

111213

TABLES

1. List of Claims - Brown McDade Project

FIGURES

1. Property Location Map2. Topography of Claim No. P.5684733. Geological Compilation of Brown-McDade Option4. Electromagnetic Profiles for 444 Hz Frequency5. Electromagnetic Profiles for 1777 Hz Frequency

2.3.

APPENDICES

Assay Results of Hollinger-Argus Drilling Program- 1983Lithogeochemical Results of Newmont Sampling - 1986 Invoices for Assaying Expenditures, & Geotechnical Data Statement

INTRODUCTION

In October, 1986, Newmont Mines Limited entered into an

agreement with Brown-McDade Resources Ltd. to option the

latter's 12-claim property in Denton Twp ., 30 km

southwest of Timmins, Ontario.

The property is located in the western Abitibi Belt and

is underlain by mafic and felsic metavolcanics intruded

by a granodiorite body. Gold mineralization occurs at

the contact between the intrusive and the basalts and is

associated with pyrrhotite in quartz veins within zones

of intense carbonatization, sodium depletion and

potassium enrichment . Approximately 1000 tons of this

material grading O .14 oz Au/ton was mined by Brown-

McDade in 1982. Eleven of the twelve claims have 200

days assessment credit and one (P .554599) has been

brought to lease. The twelfth claim, however, (P.568473)

requires 100 days to bring it up to the 200 day maximum.

In September of 1986, Newmont conducted a program of

lithogeochemical sampling of outcrops and older diamond

drill core to aid in the interpretation of the property

geology. In addition, a horizontal loop electromagnetic

survey was carried out on claim no . P .568473 for

assessment credits . The results of these surveys and

the subsequent geological interpretation are discussed

herein, with specific reference to claim number

P.568473.

-2-

PROPERTY LOCATION, ACCESS AND DESCRIPTION

The Brown-McDade Option consists of 12 contiguous claims

located in the northwest quarter of Denton Township,

about 30 kilometres southwest of the City of Timmins

(Fig. 1, Table 1). The property straddles Highway 101

and is further accessed by several logging roads and an

all-weather gravel road. One of the claims, P.554599*

has been brought to lease and ten others have 200 days

assessment credit. Claim no. P.568473 has only 100 days

assessment credit, however, and is the subject of this

report.

There is approximately 10# outcrop on the property as-

indicated in Fig . 3 . The remainder of the area is

overlain by a thin sheet of glacial debris and surficial

vegetation . The latter consists mainly of spruce,

poplar and jackpine with alders, cedar and some tamarack

near Cripple Creek (Fig's. 2 A 3).

RECORDED HOLDER

The recorded holder of the claims is Newmont Mines

Limited, Suite 900, 808 West Hastings Street, Vancouver,

B.C.

SUBMITTING PARTY

-3-

The submitting party is Newmont Exploration of Canada

Ltd., 637 Algonquin Blvd. East, Timmins, Ont., license

number A37767 . All work described herein was done by

Newmont personnel or by companies contracted by Newmont.

The submitting author was directly involved in the

program and takes full responsibility for this report.

ACKNOWLEDGEMENTS

Guy Thibault Exploration Services of Timmins carried out

both the linecutting and the Max-Min II electromagnetic

survey on claim no. P.568473* including drafting of the

profiles. Lithogeochemical sampling was conducted by the

author and R . Norman of Shear Exploration Ltd . The

interpretation of geology and geophysics was carried out

by the author. Rock samples were analysed by Technical

Service Laboratories of Toronto.

PREVIOUS WORK

Gold was first discovered on what is now the Brown-

McDade claim group in 1910 (Harding and Berry, 1938) .

Two small shafts were sunk on the showings and, in 1935,

several diamond drill holes were completed with

apparently erratic results.

In 1945, twelve diamond drill holes, totalling 4,250

feet, were completed by Wakemac Denton Gold Mines Ltd.

to test two shear zones trending north 70 east about 200

and 400 metres south of the southwest block of the

Brown-McDade property. Weak gold mineralization (up to

0.17 oz/ton- over 2.8 feet) associated with arsenopyrite

in quartz-carbonate stringers was intersected in the

northernmost shear, however, no significant assays were

obtained from the southern structure. The last of the

twelve holes was drilled north of the shear zones on

what is now claim no. P.554601 of the Brown-McDade group

and was designed to test the continuity of a surface

showing which assayed 0.19 oz Au/ton in a grab sample,

While a few specks of visible gold were noted in a half-

inch wide quartz stringer, this section was excluded

from assaying and all other core samples assayed nil .

No further work was recorded in the area until Brown-

McDade Mines Ltd . staked the present claim group in

1979-80. Subsequent linecutting, magnetic and V .L .P.

surveys were carried out followed by power stripping and

-5-

plugger work on claim nos . P .554599 and P.567640 and

diamond drilling on claim no. P.554599- All field work

was performed by J-Dex Mining and Exploration Ltd . on

behalf of Brown-McDade. The drilling consisted of 422.5

feet in 8 holes and was designed to test a zone of gold

mineralization associated with pyrrhotite in

carbonatized basalts at the contact with a granitic

intrusion. Approximately 1000 tons of ore grading 0.14

oz Au/ton were subsequently mined from two pits at this

location in the summer of 1982.

In 1983, Hollinger Argus Limited optioned eleven of the

Brown-McDade claims and carried out geological,

magnetic, electromagnetic, and limited induced

polarization surveys . Sixteen diamond drill holes

totalling 3965 feet were drilled by Hollinger in late

1983 and early 1984 to test several targets outlined by

the ground surveys and to determine the extent of the

known gold mineralization . Several holes intersected

ore grade gold values, the best being a 17 foot section

assaying 0.146 oz Au/ton, however, an apparent lack of

continuity was sufficient reason for Hollinger to

terminate their option at this time. A complete list of

all core assays greater than 0.01 oz Au/ton is given as

Appendix 1.

REGIONAL GEOLOGY

The property lies at the western end of the Abitibi

greenstone belt near the Timmins gold camp. The regional

geology of the Timmins area is well documented and is

described by Pyke (1982) to consist predominantly of two

major cycles of Archean volcanic rocks unconformably

overlain by a thick sequence of epiclastic sediments,

all of which are complexly folded, faulted and cut by

younger diabase dykes.

The oldest of the volcanic cycles, the Deloro Group, is

composed predominantly of calc-alkaline basalt and

andesite near the base with dacitic to rhyolitic flows

and pyroclastics in the upper part, locally capped by

iron formation . The younger Tisdale Group consists of

ultramafic flows and basaltic komatiites overlain by a

thick sequence of tholeiitic basalts. These are in turn

overlain by volcaniclastic calc-alkaline dacites.

The Porcupine Group metasediments are largely turbiditic

in nature with conglomerates common near the base of the

sequence. They are locally observed to lie unconformably

on top of the Tisdale and Deloro Group volcanics and are

proposed by Pyke to be contemporaneous with the Tisdale

Group.

A few, small felsic porphyries intrude the Tisdale Group

rocks and may be synvolcanic in origin . These are

spatially, ' and possibly temporally, related to gold

-7-

mineralization at the Hollinger, Mcintyre and Dome

Mines, the three largest gold producers in the Timmins

c amp.

All rock types are cut by north-south trending diabase

dykes of Matachewan age.

The structure of the Timmins area is complex and the

number and sequence of deformational phases is unclear.

Possibly the best known structural feature is the

Destor-Porcupine Fault, an east-northeast-trending shear

zone several hundred kilometres long with which much of

the gold mineralization in the area is associated. At

least two periods of folding are evident, the most

obvious of which is the Porcupine Syncline . The

Porcupine Group metasediments locally form the core of

this fold with the volcanic rocks of the Tisdale and

Deloro Groups wrapped around them, the synclinal axis

striking east-northeast . Younger, cross-cutting faults

are common and add to the structural complexity of the

region.

LITHOGEOCHEMISTRY AND PROPERTY GEOLOGY

All samples were analysed by ICP (emission spectrograph)

at Technical Service Laboratories in Toronto . Prior to

analysis the samples were crushed to -250 mesh, weighed

and mixed with a fusion flux, and heated to 1200 degrees

Celsius, after which the bead was dissolved in nitric

acid and diluted.

While only 45 sets of analytical results are being

submitted for assessment credit on claim no. P.568473*

more than a hundred rock samples have been taken by

Newmont from outcrops and old diamond drill core on and

around the property. Prom this database it was possible

to classify the rock types on the property and to

identify the type and intensity of alteration found in

the mineralized zones. All surface samples and previous

diamond drill holes are plotted on Pig . 3 and

geochemical results are appended.

The Denton Twp . property is underlain predominantly by

supracrustal volcanic rocks of Archean age . They are

thought to represent part of the Tisdale Group (Pyke,

1982) within the north limb of the Porcupine Syncline.

The volcanics are intruded to the north" by a

granodioritic body and all rock types are cut by

younger, north-south-trending diabase dykes . A

geological compilation of the property is illustrated in

Figure J.

Foliations in the volcanics typically strike east-

northeast and lithological contacts appear to strike

roughly east-west. All dips are sub-vertical.

The supracrustal rocks consist of tholeiitic basalts,

bordering between Pe- and Mg-rich varieties, and calc-

alkaline rhyolites, with minor interbedded iron

formation in the northeast corner of the property.

The basalts are green, fine- to medium-grained and

mainly massive, with minor pillows observed in the

central part of the property . Within the alteration

zones there is a marked decrease in Na20 content from

the norm of 2-3# to less than ^ % . This is usually

accompanied by an increase in K20 from less than 1# to

2-3# and reflects the alteration of feldspars to

sericite . In addition, these zones show an increase in

LOI, indicative of carbonatization, and a slight

enrichment in barium.

The rhyolite is a beige, fine-grained, laminated unit

and is probably a flow or ash tuff . It typically

contains in excess of 70# Si02 and about 5# combined

Na20 and K20 . It is locally sheared and, in these

areas, shows depletion of Na20 and enrichment of K20 .

The granodiorite is a white to pink and black, medium-

to coarse-grained, massive rock containing quartz,

feldspar and biotite. It has an intermediate composition

averaging 67^ Si02, 15# A1203, 4-5# Fe203 and 5-6#

combined alkalis . Locally, it exhibits the same

-10-

alteration patterns as the basalts.

The iron formation is a cherty, black, massive rock

where exposed and is highly magnetic . It has been

locally sulphidized such that pods of quartz and pyrite

are common . No samples were taken of this unit .

Diabase dykes are fine- to medium-grained and locally

magnetic . Only one sample of this rock type was

submitted for analysis (no . 9350) and it showed a

composition similar to the basalts but with lower A1203

and higher Fe203 and Ti02.

While there is about 10# outcrop on the property, claim

no. P .568473, the subject of this report, is lacking

any exposure . Based-on geological trends, however, it

is believed to be underlain by the same tholeiitic

basalts which outcrop near the western boundary of the

claim (Fig. 3).

Gold mineralization on the property appears to be

spatially related to the basalt-granodiorite contact. It

is found associated with pyrrhotite and minor

chalcopyrite within quartz veins on both sides of the

contact . Intense carbonatization, sodium depletion and

potassium enrichment accompany the mineralization.

-11-

ELECTROMAGNETIC SURVEY

A horizontal-loop electromagnetic survey was carried out

over claim number P.568473 by Guy Thibault Exploration

Services of Timmins . An APEX Max-Min II unit was used

with a coil spacing of 100 metres. One hundred and two

stations were read at 25m intervals for a total of 3-2

kilometres. Both in-phase and out-of-phase readings were

taken for each of the 444 Hz and 1777 Hz frequencies,

giving a total of 408 readings. Profiles are illustrated

in Pig's. 4 and 5* A geotechnical report is appended.

No anomalies were detected by the survey and it is

therefore concluded that no conductive bodies underly

this claim within the detection limits of the Max-Min II

unit.

-02-

DISCUSSION

It is concluded from the work described herein that

claim number P.568473, in Denton Twp., is underlain by a

unit of tholeiitic basalt, possibly belonging to the

Tisdale Group described by Pyke (1982) for the Timmins

area . There are no conductive bodies present and the

contact with the granodiorite is believed to pass to the

north of the claim. There are, therefore, no obvious

targets of economic interest on this ground at the

present time.

-13-

REPERENCES

Harding, W.D. and Berry, L.G.

1938: Geology of the Keefer-Eldorado Area; Forty-

Seventh Annual Report of the Ontario

Department of Mines, VOL. XLVII, PART IV,

26p. Accompanied by Map No. 47d, Scale 1

mile to the inch.

Pyke, D.R.

1982: Geology of the Timmins Area, District of

Cochrane; Ontario Geological Survey

Report 219, 141 p . Accompanied by Map

2455, Scale 1:50000, 3 Charts, and 1

Sheet Microfiche.

TABLE 1 - CLAIM LIST - BROWN McDADE OPTION

f

CLAIM NO.

P.539619 539622554597554598554599554600554601554602554603567640567641568473

RECORDING DATE

October 17,December 5,FebruaryFebruaryFebruaryFebruaryFebruaryFebruaryFebruaryMay 16,May 16, 1980May 21, 1980

19791979

28, 198028,28,28,28,28,28,

1980

198019801980198019801980

Now lease no. 103583

CARSCALLEN TWR

DANA a JOWSEY PROV. PAUK RESERVE

NEWMONT EXPLORATION OF CANADA LIMITED

FIG. l PROPERTY

LOCATION MAP

BROWN-McDADE OPTION

42 A/5

APPENDIX I

ASSAY RESULTS OP HOLLINGER-ARGUS DIAMOND DRILLING - 1985

APPENDIX

Results of drilling on claims in Denton Township optioned by Hollinger Argus Limited and Esso Resources Limited from Brown-McDade Resources Ltd.

Hole No. D4-1-83 - Location: Length of Hole: Azimuth:

Depth

554.1 meters West/114.4 meters North30.7'3300 Dip: -50O

Core Length Assay

Hole No.

8' - 10' 10' - 12'

D4-2-83 - Location:

2' 2'

562.2 meters

0.136 0.207

West/114Length of Hole; Azimuth:

Depth25' - 27'32' - 33.5'47' - 50'

60.7'1500 Dip: -650

s Length2 1

1.5' 3'

Assay0.012 0.024 0.030

Hole No. D4-3-83 - Location: 133+42^/106+20^ (Main Grid)Length of Hole: 25'Azimuth: 30O Dip: -60O

No significant assay values.

Hole No. D4-4-83 - Location: Length of Hole: Azimuth:

Depth2' -5' -

5' 7'

133+57^/106+18^ (Main Grid)15'1200 Dip: -700

Core Length3' 2'

Assay

0.4850.020

Hole No. D4-5-83 - Location: Length of Hole: Azimuth:

Depth34' 45' 47' 60' 62' 67' 70' 75'

35' 47' 50' 62' 65' 70' 75' 80'

148+28^/118+78^ (Main Grid)86'ISO0 Dip: -56.50

Core Lengthl' 2' 3' 2' 3' 3' 5* 5'

Assay0.0420.0340.0320.0120.0120.0100.0180.020

Note: Assays less than 0.01 ounces of gold per ton are not included

- 2 -

Hole No. D4-6-83; Location : XL O @ 75' SE of S.L. 'A'Length of Azimuth

Depth 44'- 45'

95 - 97 97 - 100

100 - 102

105 - 107

112 - 115

127 - 130

Hole No. D4-7-83: LocationLength of Azimuth

58'- 61' 61 - 62

76.5- 78

195 - 197

226 - 227

240 - 242

272 - 275 275 - 277

Hole No. D4-8-83: LocationLength of Azimuth

10'- 15'

123 - 125 125 - 130 130 - 135 135 - 140 140 - 142160 - 165 165 - 170 170 - 175 175 - 180190 - 192 192 - 195 195 - 196213 - 216235 - 239 239 - 240 240 - 245 245 - 248 248 - 250

Hole: 153' : 3000

Core Lengthl 1

2 3 2

23

3

: XL 0 Hole: 298'

: 3000*

3'1

1.52

1

2

3 2

: XL 0 Hole: 318'

: 34005'

2 5 5 5 25 5 5 52 3134 1 5 3 2

Dip: -500

Assay

.018

.016

.020

.014

.070

.024

.080

6 175' SE of B. L. 'A'

Dip: -500

.042

.014

.064

.016

.056

.016

.010

.010

@ 20.5' S of B. L, 'B'

Dip: -450

.063

.026

.048

.015

.153

.010

.052

.191

.002

.018

.036

.014

.010

.246

.092

.106

.198

.687

.006

- 3 -

Hole No. D4-9-B3 Location: XL O @ 100'N of S.L. 'C'Length of Hole: 602'Azimuth: 135' Dip: -55O

This hole was drilled to test geophysical anomaly. No significant assays were obtained.

Hole No. D4-10-83 Location: XL 400'W @ 100'N of B.L. 'C 1Length of Hole: 405'Azimuth: 158O Dip: -45O

This hole encountered no significant assay values.

Hole No. D4-11-83 Location: XL O @ 100'S of B.L. 'B'Length of Hole: 379^ Azimuth:

Footage118' - 121'

121' - 122'

130' - 131.5'135' - 140'

195' - 198'

198' - 200'

203.5 - 206.5'245' - 247'

247' - 250'

293' - 295'

297' - 298.5'329' - 330'

330' - 332'

341.5 - 342.5'

Hole No. D4-12-83 Location: XL 300'E @ 100'S of B.L. 'B 1Length of Hole: 263.6'Azimuth: 310O Dip: -45O

This hole was drilled to test a geophysical (magnetic) anomaly. No significant assays were obtained.

3400

Width3'

1'1.5'

5'

3'2'

1'

2'

3'

2'

1.5'

1'2'1'

Dip: -450

Au (ozs/ton)

0.060

0.121

0.050

0.032

0.0160.020

0.012

0.010

0.0360.014

0.0260.018

0.026

0.431

- 4 -

Hole No. D4-13-83 Location:Length of Hole: Azimuth:

Footage

32' - 33'33' - 35'

112' - 113'

113' - 114'

115' - 117'

117' - 119'

119' - 120'

120' - 121'

125' - 127'

127' - 130'

130' - 132'

132' - 135'

143' - 144'

- 160'

- 163'

- 165'

- 167'

- 171'

- 173'

- 175'

158'

162'

163'

165'

170'

171'

173'

Width

XL O @ 54.5'N of B.L.218'3400 Dip: -450

'B'

175' - 177'

210' - 215'

1'2'

1'

1'

2'

2'

l 1

1'

2'

3'

2V3'

1'

2'

1'

2'

2'

1'

2'

2'

2'

5'

0.179

0.026

0.018

0.205

0.090

0.038

0.030

0.108

0.309

0.135

0.034

0.024

0.054

0.012

0.290

0.088

0.028

0.110

0.010

0.159

0.232

0.010

Autozs/ton) Ag(ozsXton)

4.86

9.13

- 5 -

Hole No. D4-14-84 Location: XL IOO'E/O+50'N of BL "B" Length of Hole: 372'Azimuth

Intersection

110' -111 1113' - 114'

125' - 127'

127' -128*

128' -130'

130' -132'132' - 134'

134' - 135'

135' -140'

140' - 142'151' - 152'

237' -239'241' - 243'

255' -257'

260' -265'

34 Oo Dip: -45O

Core Length

l 1 of .101 Au (ozs per ton)

l 1 of .046 Au

2' of .026 Au "

l 1 of .845 Au "

2' of .109 Au "

2' of .062 Au - "2' of .020 Au "

of 1.40 Au "

of .002 Au "

098 Au "010 Au w

016 Au "118 Au "

026 Au "

028 Au "

l 1

5 1

2' of

l' of

2' of

2' of

2' of

5' of

(125* - 142') - 17' of .169 ozs per ton Au (uncut)

Hole D4-15-84 Location: Length of Hole: Azimuth:

Intersection

182' -185'

187' - 189'

189' - 190'

XL 100 'W @ 50 'N of BL "B"242'340O Dip: -45O

Core Length

3' of .022 Au (ozs per ton)

2' of .020 Au "

l' of .105 Au "

- 6 -

Hole D4-16-84 Location: 100' South of D4-14 on Line 100'E of BL "B"Length of Hole: 497' Azimuth: 34Oo Dip: -50O

Intersection Core Length

22' - 23' l' of . 018 Au (ozs per ton)

310' -311' l 1 of .012 Au "

o

APPENDIX II

LITHOGEOCHEMICAL RESULTS OP NEWMONT SAMPLING - 1 986

TECHNICAL SERVICE LABORATORIES1301 FEUSTER DRIVE* MISSISSAUGA* ONTARIO

TELEPHONE J (416) 625 ~ 1544L4U 1A2

CERTIFICATE OF ANALYSIS

NEWMONT EXPLORATION

P.O. BOX 1130 TIMMINS ONTARIO P4N 7N2 "

YOUR REFERENCE SAMPLE *

93129313931493159316

93179318931993209321

93229323932493259326

93279328932993309331

93329333933493359336

93379338933993409341

HATE ! 30-OCT-B6

^^ n ^ T, S. L. REPORT * 5 Cf-v'M 6v c , Z^ OOVN. D rft,S T. 8. L. File

1 T. S. L. Invoice

ICE : ATTN:Si02 A1203

54.29 13.2364.37 15.9249.67 16.5151.20 16.3751.36 15.35

52.61 13.6450.24 17.0150.16 17,5249.56 15.7878.96 11.53

50.09 15,5750.38 15.8875.37 13.5150.46 16.2248.66 15.56

50.35 16.2849.31 16.0669.20 14,7349,61 12.9350.22 15.59

48.43 16,4148.74 15.7149.50 15.4749,56 14,8678.81 13.37

76,10 12,8274.39 12.9269.29 14.7981.67 11.1366.86 13.67

86

No. : No. tNO. ;

T - 1526 240CT

M. UhiteFe203

13.386.2612.6311.5311.13

17.6111 .6711.9613.291.51

12.2312.902.0311.7013.25

11.2711.82B. 0417.6512.22

12.2412,1812.3512.842.93

3.514.875.762.317.27

CsO

9,445,478,56

10.0210.72

9.6710.5315.4712.031.88

10.819.881.81

11.0212.79

10.0311.264.828.939.41

11.8911.2310.5011.091.35

1.362.113.051.456,59

Mao

5,062.108.236.067.68

2.175.762.935.74.26

7.166.89.58

7.456.13

7.968.751.144.667.54

7.908.318.758.74.46

.32

.42

.821.60.63

Na20

2.744.172.383.262.25

2.613.07.29

2.214.11

1.912.294.941.721.95

2.941.68.62

2.633.23

1.832.442.291.68.90

4.483.915.01.36

3.95

K20

.44

.69

.76

.21

.34

.38

.26< . 10

.241,57

1.10.60

1.35.29.49

.20< .10

.61

.69

.72

.18

.29< .10< .102.02

1.191.01.60

1.18.11

T102

1.10.72

1.001.10.90

.591.161.29.85.10

.84

.90

.32

.89

.88

.72

.76

.522,33.80

.83

.80

.80

.84

.09

.11

.24

.42

.19

.52f* ^ *

MnO

.21

.09

.16

.15

.17

.47

.16

.18

.22

.02

.19

.20

.03

.18

.21

.17

.19

.13

.26

.19

.20

.20

.19

.21

.04

.05

.07

.11

.04

.17) .

P205

.10

.20

.10

.09

.08

.25 -

.13

.14

.09

.04

.09

.09

.06

.07

.07

.08

.08

.19

.30

.00

.09

.09

.08

.08

.04

.05

.07

.15

.06

.21

Bs

612921204673

100864739

313

8070

46848

101

4552

432348315

28401727

537

333301130116107

Sr

120461171212144

19024728512490

11292

134126156

156180354154138

137246112108162

8871

11164162

Zr

61193645560

23570735390

4244

1075856

4449

20516950

49464344

133

191403355253242

LOI

1.261.662.611.722.24

1.051.953.231.511.13

15.3612.921.762.521.78

2.583.281.881.781.71

2.181.992.302,652,05

1.410.981.181.570.66

TOTAL

99,92100,57100.8699.84100.44

100.66100.23100,4699.31100.12

100.07100.0099.87100.78100.47

98.6097.5899.64100.7199.52

98.1698.8897.9798.2497.79

99.1599.7198.7298.22100.13

SIGNED ! _______ ^t^^^Zr^?:- .... Adrian H. Debnam Ph.D.

SAMPLEz::::::::::::::::)

b^-io^l 734735736737738739740741

tx,-(*-?3 764765786787788739

ba-io-83 7"879179279379479579679775879?EC2

SI02rrrrrr)

76.0875.7775.7363.1576.2875.5374.6075.6167.2367.7877.0168.9668.7268.3079.3079.8874.6576.9976.1976.6276.976S.Q775.2675.8675.41

AL203rrrrss)

13.2612.6813.1510.4312.8713.1413.0113.3715.0015.1611.5314.7114.6514.9411.8712.4313.0613.1313.2113.0813.4612.6,113.3813.2213.04

FE203srrzrs)

2.422.832.624.992.622.693.412.034.914.742.744.114.464.135.553.903.662.292.912.661.795.1B3.052.893.29

CAOrrrrsr)

2.623.072.2011.992.493.112.785.593.913.602.883.823.813.970.920.713.732.162.001.581.275.271.821.832.63

MBOssssss)

0.250.240.204.780.470.310.51.01.80.67.44.51.50.47

0.890.900.950.290.210.!50.203.220.250.200.21

NA20rsrsrs)

4.194.354.792.564.363.904.75B. 46-4.353.440.104.204.065.EJ0.930.703.b34.404.734.965.544.054.895.034.44

K20ssr:::)

1.000.860.998.490.651.110,671.641.332.653.571.861.981.380.241.260.130.580.550.770.630.901.160.7d0.70

TI02srsssr)

0.09

0.100.111.170.130.110.150.120.680.680.470.590.580.570.160.190.160.090.110.100.070.350.100.100.11

MOs::s::}

0.04B.050.030.110.050.050.86B.060.060.070.06e. 070.070.060.050.040.060.030.04e.040.030.030.050.040.06

P205S:E:::)

0.050.050.180.330.070.060.070.050.220.210.160.170.160.160.100.060.070.040.040.040.050.270.050.050.06

GAs:::;:)

. 261214200325186270170

2209414513395452412443140233251373187216234380586283186

SR

836578360957284US275184763S027329814211511195966173

29312610199

2fisszsrs)

190213222217200203

. 2311432642061491941721931743192961762242E6143173193211229

LOIrczrl:,)

1.642.251.118.261.172.591.7B3.073.673.843.613.633.923.393.051.621.120.831.081.152.924.571.371.831.45

APPENDIX III

INVOICES FOR ASSAYING EXPENDITURES, AND GEOTECHNICAL DATA STATEMENT

Telephone (604) 682-6291 Fax (604) 682-5330

NEWMONT EXPLORATION OF CANADA LIMITEDA Subsidiary of Newmont Mining Corporation

900 - 808 West Hastings Street Vancouver, B.C. V6C 3A4

May 26, 1987

Mr. Arthur BarrMining Lands SectionMineral Development and Lands BranchMines and Minerals DivisionMinistry of Northern Development and MinesWhitney Block - Room 6610Queens ParkToronto, OntarioM7A 1V3

Dear Sir:

Re; Brown-McDade Project No. 271

Thus letter will confirm that assay fees amounting to $1,102.50 were paid to Technical Service Laboratories for assays done in September and October 1986.

Yours very truly,

'W. R. Somerville Accountant

WRS/saj

bcc: R.A. Archer

TECHNICAL SERVICE LABORATORIESO'VitlQHOf • UAOCNfA TfCMNiCAL C*V|N*llif|f ll*HTtO1301 FEWSTER DR., MISSISSAUGA, ONTARIO L4W 1A?TELEPHONE: (416) 625-1544

INVOICE NO.

35434

CHARGE TO

Newmont Exploration P.O. Box 1430 Timmins, Ontario P4N 7N2

DATE

Oct. 31/86

REFERENCE NO.

M-1526SHIPTO

R. A. Archer

YOUR ORDER NO.

101

S: NKT 1* OAVICODE

DESCRIPTION

UNIT PRICE TOTAL

i|:'.

l

30 defeerminationo of Au by PA/AA 30 whole rock without Cu, Zn S As HN'

24.50B17.SO

TOTAL

735.00

$952.50

t f'rYHA\*~^S ( "LO )(,

INVOICE - PLEASE ENCLOSE COPY OF INVOICE WITH PAYMENT

D'

li'V '

TECHNICAL SERVICE LABORATORIESDlVKiOM O' SUdOCNIM T ICHN t CAL fNTf ft'fUtf f llMITID

1301 FEWSTER DR., MISSISSAUGA, ONTARIO L4W 1A2TELEPHONE: (416) 625-1544

INVOICE NO.

.34569

li CHARGE TO

Newmont Exploration P.O. Box 1430 Timmins, Ontario P4N 7N2

DATE

Sept.11/86REFERENCE NO.

T-6966YOUR ORDER NO.

SHIP TO

M. Whitenmr M o*vi

CODE DESCRIPTION UNIT PRICE TOTAU

30 whole rock det. for major oxides

TOTAL

C^C(C*VrKVt4r f;

INVOICE - PLEASE ENCLOSE COPY OF INVOICE WITH PAYMENT

24.50 735.00

S735.00

lJprti

r

Ontario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

FUc.

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

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey(s) Township or Area Claim Hnlder(s) A

i c,eJ . fit, tt-Jl

M i^v/ ~^., j~jd

Survey Company Author of Report Address of Anthnr P. (4-10 "T, L

Covering Dates of Survey S~*p-f- '

Total Miles of Line rut 3.2.(linecutting to office)

SPECIAL PROVISIONS CREDITS REQUESTED

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

Geophysical—Electromagnetic.—Magnetometer—.—Radiometric———Other———-——,

DAYSper claim.

Geological.Geochemical.

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

Magnetometer. .Electromagnetic, .Radiometric

DATE:.

(enter days per claim)

STP.NATITRF-Author of Report or Agent

Res. Geol.. .Qualifications.Previous Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

(number)

TOTAL CLAIMS.

837 (5/79)

GEOPHYSICAL TECHNICAL DATA

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

Number of Stations. Station interval—— Profile scale ____iContour interval.

101. .Number of Readings JLine spacing ___L

c

Instrument.Accuracy — Scale constant. Diurnal correction method.Base Station check-in interval (hours). Base Station location and value '

gz0

1e1

Coil configuration /^(**~ ^ f~^~*y (-i*-t*proil separation t &Q ~,

Acairary — 27? . .Method: CD Fixed transmitter CD Shoot back US In lineFrequency 4^^ fi t^ .../JZ-H.2" i ff- ,,..,. . , , ....... .. .,

{ipecify V.L.F. lUtion)

CD Parallel line

Parameters measured. ~-f-

s51

Instrument.Scale constantCorrections made

Base station value and location.

Elevation accuracy.

f*

InstrumentMethod CD Time Domain Parameters — On time ———

- Off time __— Delay time -——— Integration time.

Power.Electrode array — Electrode spacing . Type of electrode

CD Frequency Domain ^ Frequency ——-,—— —. Range———————

MAXMIIM IIEM

Five frequencies: 222, 444, BBS, 1777 and 3555 Hz,Maximum coupled C horizontal-loop 3 operation with reference cable.Minimum coupled operation with reference cable. Vertical-loop operation without reference cable.Coil separations: SS, 5Q,1OO,15O, SOO and BSD m C with cable 3 or 100,500,300,400, SOO and BOO ft.Reliable data from depths of up to IBOm CBOOftl. Built-in voice communication circuitry with cable. Tilt meters to control coil orientation.

SPECIFICATIONS l

Frequencies i 222, 444, BBB, 1777 and 3555Hz. Repeatability s

Modes of Operation: MAX: Transmitter coil plane and re ceiver coil plane horizontal CMax-coupled; Horizontal-loop mode). Used with refer, cable.

MIN: Transmitter coil plane horizon tal and receiver coil plane ver tical CMin-coupled mode). Used with reference cable.

V. L. : Transmitter coil plane verti cal and receiver coil plane hori zontal CVertical-loop mode). Used without reference cable , in parallel lines.

25,SO, 1OO,15O,2OO S25Om CMMH) or 1OO, 2OO, 3OO, 4OO,BOOand BOO ft. tMMEF). Coil separations in VL.mode not re stricted to fixed values .

- In-Phase and Quadrature compo nents of the secondary field 1 n MAX snd MIN modes.

- Tilt-angle of the total field in VL. mode .

- Automatic, direct readout on SO mm C3.5") edgewise meters in MAX and MIN modes. No null ing or compensation necessary.

- Tilt angle and null in 9Omm edge wise meters in VL.mode.

In-Phase: 2OV., 1OO*/. by push button switch .

Quadrature: 2O V., TOOV. by push button switch.

Tilt: 175V,, slope .NullCVL.): Sensitivity adjustable

by separation switch.

Coll Separations;

Parameters Read:

Readouts;

Scale Ranges :

eadability: In-Phase and Quadrature : O.25 *t, to 0.5V. ; Tilt: 1V. .

iO.25Voto 1Vo normally, depending on conditions, frequencies and coil separation used.

Transmitter Output i. 222Hz : 22OAtme- 444Hz :2OOAtme- BBB Hz : 12OAtmS- 1777 Hz : 6OAtme-3555 Hz i 3OAtme

Receiver Batteries : SV trans, radio type batteries (4). Life: approx. 35hrs. continuous du ty (alkaline , O.5 Ah), less in cold weather.

Transmitter Batte rie s :

Reference Cable :

Voice Link:

12V B Ah Bel-type rechargeable battery. (Charger supplied).

Light weight 2-conductor teflon ceble for minimum friction. Unshield ed. All reference cables optional at extra cost. Please specify.

Built-in intercom system for voice communication between re ceiver and transmitter operators in MAX end MIN modes, vie re ference cable .

Indicator Lights: Built-in signal and reference warn ing lights to indicate erroneous readings .

Temperature Range: -4O"C to *BO 0C C-4OeFto*14Q0F).

Receiver Weight: B kg (13lbs.)

Transmitter Weight: 13kg C 28 IDS.)

Shipping Weight: Typically BOkg C135lbs.), depend ing on quantities of reference cable and batteries included. Shipped in two field/shipping cases.

Specifications subject to change without notification.

APEX PARAMETRICS LIMITED2OO STEELCASE RD. E., MARKHAM. DNT, CANADA, L3R 1B2

Phone: C41B) 4S5-1B12 Cables: APEXPARA TORONTO Telex KWB9flJW3JBIO)RtHtaBJCraiBlMBER: D6-966775 APEXPARA MKHM

THEORY

The moving source or "horizontal-loop electromagnetic method

is one of the most common in use as a follow-up geophysical tool

to further discriminate conductors delineated by airborne or VLF

methods.

The system is essentially a transmitter connected to a

receiver by a reference cable. The distance between the trans

mitter and receiver varies between 25 and 250 meters depending

upon the desired depth of penetration. Transmitter power is

low and several frequencies are used (four with the Max Min II

system; 222, 444, 888, 1777 and 3555 Hz). For this survey only

444, 888 and 3555 Hz were used.

Oscillator

Transmitter Reference Cable

25 - 250 meters

Compensator

Receiver

Simplified horizontal-loop diagram.

The transmitter emitts a primary field. The transmitter and

receiver move in line perpendicular to the geological strike and

any conductive bodies will emit a secondary field. This field

is referenced as a percent of the primary field by a compensating

network in the receiver. This receiver voltage is split into

two components, one in phase and one 90 or one-quarter wave out

of phase (quadrature). Where no conductors are present the in

phase and quadrature components are typically zero. As a conduc

tive body is approached both the in phase and quadrature components

increase above background or zero then decrease to a minimum as

the conductor is passed over then increase above zero and decrease

back to near zero or background as the system traverses away

from the conductor. Symmetry or assemetry of the anomaly curve

may indicate the dip of the conductor. The ratio between the

in phase and quadrature values indicates the quality of the

conductor, the larger the ratio the better the conductor. Many

vector diagrams for estimating depth and resistivity/thickness

for the various shapes and dips of conductors have been calculated

and are available to assist in the interpretation of anomalies

obtained by this method.

-— l

TxJ f——""-x __________________________ _________________________ X"———--V J^ ^

. v^______ l stn____^^^ .______ surface- :J. : /V- - .: i] ' .'. .'••'•'•X^.-" .'..'.' '-' L j

conductor

OP

background level

Tx Rx

r, =

O, 02 z = IP OP

= Tran sm itter= R eceive rCoil separationTx - conduc to r distanceRx-conducto r distanceTx- con d ucto r angleRx-conductor angleDepth to bedrock In phase or real component

:z Out of phase or imaginary componentconductor width

Survey layout, curves and measurable parameters of a typical horizontal-loop layout.

Conductor

Typical curves over a single vertical to near-vertical conductor

Typical curves over a horizontal conductor

-Conductor

Typical curves over two vertical to near-vertical conductors

Conductorq C Conductor

Idealized profiles over commonly occurring conductive bodies.

Ontario

Ministry ofNorthern Developmentand Mines

July 6, 1987

42A85SE0132 2.let06 DENTON 900

Your File: 62/87 Our File: 2.10108

Mining RecorderMinistry of Northern Development and Mines60 Wilson AvenueTimmins, OntarioP4N 2S7

Dear Sir:

RE: Data for Assaying and Geophysical (Electromagnetic) Survey submitted on Mining Claims P 539619, et al, in Denton Township

The enclosed statements of assessment work credits for Assaying and Geophysical (Electromagnetic) Survey have been approved as of the above date.

Please inform the recorded holder of these mining claims and so indicate on your records.

Yours sincerely,

'Gary L. Weatherson, Manager Mining Lands Section Mineral Development and Lands Branch Mines and Minerals Division

Whitney Block, Room 6610 Queen's Park Toronto, Ontario M7A 1W3

Telephone: (416) 965-4888

DK/mccc: Newmont Mines Ltd

Suite 900808 West Hastings StreetVancouver, B.C.V6C 3A4

End .

R.A. Archer P.O. Box 1430 Timmins, Ontario P4N 7N2

Resident Geologist Timmins, Ontario

Onta

Ministry ofNorthern Development

nd MinesTechnical Assessment Work Credits

Date

July 6. 1987

PH*2

Mining Recorder'* Work No. ,

D

.10108Report of2/87

f-

Recorded Holder

NEWMONT MINES LTDTownship or Area

DENTON TOWNSHIPType of survey and number of

Assessment days credit per claimGeophysical

Electromagnetic , day?

InriiirAri polarization days

Section 77 (19) See "Mining Claims Assessed" column

Geological dayi

Geochemical - , days

Man days Q Airborne D

Special provision | j Ground U)

[~1 Credits have been reduced because of partial coverage of claims.Q Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

1900.00 SPENT ON ANALYSES OF SAMPLES TAKEN FROM MINING CLAIMS:

P 539619 554597 to 600 Inclusive 554622 567640-41 568500

60 ASSESSMENT WORK DAYS ARE ALLOWED WHICH MAY BE GROUPED IN ACCORDANCE WITH SECTION 76(6) OF THE MINING ACT.

Special credits under section 77 (16) for the following mining claims

No credits have been allowed for the following mining claimsf] not sufficiently covered by the survey [~~j insufficient technical data filed

f The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical - 80; Geologocal - 40; Geochemical - 40; Section 77(19) - 60.)28 (85/12)

Ministry ofNorthern Development

nd MinesOntario l

Technical Assessment Work Credits

Dm

July 6,1987

File

2.10108Mining Recorder*! Report of Work No.

62/87

Recorded HolderNEWMONT MINES LTD

Township or AreaDENTON TOWNSHIP

Type of survey and number of Assessment days credit per claim

Geophysical ?flElectromagnetic tV rtayt

Magnetometer riayj

Radiometric , .. . , , , , . ..rlays

Induce^ polarization , ., .., rlays

Other . rtayt

Section 77 (19) See "Mining Claims Assessed" column

Geological 20 rlays

Geofihemiral riays

Man days Q Airborne Q

Special provision 0 Ground E

Q Credits have been reduced because of partial coverage of claims,

[J Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

P 568473

Special credits under section 77 (16) for the following mining claims

No credits have been allowed for the following mining claimsf~j not sufficiently covered by the survey f~] insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not xcead the maximum allowed as follows: Geophysical - 80; Geologocal - 40; Geochemical - 40; Section 77(19) - 60.28(85/12)

^WITHDRAWN FROM DISPOSITION

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t E G E N D'

.^ - t . - l ' ' i -' * ' ," "' ^r' '|"*1" V.'' -'1 .f -SURVEYED UNES^.V,^ -V v^^^ V ;i,';-,'r"-'\.i '''--'l--/^ '^

:^TOWr4SH|PS,BASEi.l^K';ETC.^:*f'-i ' ' 'n \"-r UOT5.MINING CLAIMS, PARCELS/ETC.,. '.. . ^ ; ^v;- :.

'XiNESiv^l^-'l^VU;'^''-'';^^^^^v'x- : v^'j;*^^^—. •..,;. v? -..^

' 1- -LINES

;Vv PARCEL BOUNDARY-'-^MINING CLAIMS ETC, *

V RAILWAY AND RKjHT.OF WAY

\ NON-PERENNIAL STREAM * :

vFLOODING OR FLOODING flGHTS ] ?'S,\SUBDIVISION OR, COMPOSITE PLAN /,

^RESERVATIC3NSV''V; \ -.- t, :' f ^\^l^;ORiGiNACSHORELINE.'v*"^^\V; " ~) MARSH OR MUSKEG ; * fr:'.*\* *V^; ; -V.-V^yis -MINES TRAVERSE

i '.,. ' ^. 7 " t'-WM i H ; (. . . . . -,

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'^^'^•^fetyp,; ;,n/^^, E MONUMENTr^.^'V;^ .'^{^ ^^^•'--'•' ' -.''.^ '^-•'•••/ t , :*.-''-"'*"^^' ; ?'li i ; :w'T ; :.

rf . -*. , ..f . I.. -"- v ,

DISPOSITION OF CROWN LANDS

f TYPE OF DOCUMEN•* . - - ;y\ •^ PATENT,SURFACE A MINING1 :. '/, V SURFACE RIGHTS ONLY™,..,._^^^^G?: . V H'.K;' .MINJNG RlGHTSONLYiL.il. ' ''-*'"* --f*'-t? Q*f ' - t . - *'~ . ' . 1 . ^"""""'""SWTV. '* '""ft* ^

LEASE, SURFACE ft MINING fllGHT^,^.^;,;^ B 'f

; ,,r * 'SURFACE RIGHTS.ONLYJ-^^^^i^B? *v' V * .MINING RIGHTS ON! Vi*"'' "^''^ -' ' * !?"'".';. M INING RIGHTSONJ.^^^..^^

LICENCE OF OCCUPATION li*Utr ' "" V 'vB

TORDE^IN-COUNCIL.L...RESERVATION t.;tX--___ ,__^

icAlteELtfb.\'^^^^;SAND 8, C5RA^^^J4.^^-:S^^^^ ;,, -^ *- -.v - ; :Hfcy;- c;.-VvV: ^^-;*.i*-,--^;--.^i NOTf ;~MININQ MIGHTS IN PJtKCEUI PATiNTEO PRtOI1! TO MAY ft.

L 1*ia. VESTED IN ORIGINAL'PATfNTEEV'*^ --v - LANO* ACT,.R*.Q.,1B70, CAP, MO, SCO. 03, tUMflC''

M.N.R. ADMINISTRATIVE DSTRICT

MINING DIVISION

LAND TITLES/REGISTRY DJVISION

COCHRANE 4^:

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100-S

B-L 166-S

200-S

300-S

400-S

500-S

600-S

in i roi

O OOl

LOCATION MAP

TOPOGRAPHIC

Trail portage

H H IT ~ Bush road

Good drivng road, Highway

Rail road

Claim post located

Claim post assumed location

Witness post

Creek, River

Lake shore

Swamp, Bog - Property boundry line

MAX-MIN II H.E.M. SURVEY

Profile:

In Phase

. In Phase

x. - -x- - - x- - - x- - -xOut Phase

Coil Separation: Meters

'j

:, 2 o

-w

-23CONDUCTOR

-20

-3

^•' \

*2 1

Out Phase

\.-18

-16•j

42Aa5SE(8132 2 .18108 DENTON 220

NEWMONT EXPLORATION

DENTON TWP PROPERTY

survey by: Guy Thibault Exploration ServicesOperators : Quy Jmo^ ^ T jm Be||

Instrument:Apex Parametrics Max-Min

Drafted by : G. Thibault

DATE: February 198?

i Vertical; Icm* !OV, , Horizontal: 1:2500

CEKERAL LtGENO i COMPUTER CODE

ID DIABASE JQ

t HAFIC IWTRUSIVES Ci

rtLSIC IKTRUS1VESI.I/a* Gcanit* B-2/Bb Grinodiorit* I.J/ic feldspar

Forphyrita 1.4/Bd Syenite

CHEMICAL SEDIHENTS 7T.I/la Oxide Iron Formation 7.3/lb Sulphide lion

ForMtion 1 .2111 C han, Checxy 7u(fs 7.4/Td

Car bo na 11 7.5/74 tuanv* Sir! p h id*

SEDIMENTS (0*.1;6* Tuffacioui Sedimtnti (volccn

l. i/fib Argillaceous SedlmanEs 4.3/tc Conglomerate

FELSIC VOLCANICS 5"S.l/!* Hhyoiits Flaws 5,2/Sb Rhyolit* Tuffs

S.3/5C pyroclastics (Ash Flows l 5.4/Sd Quartz

Feldspar Porphyry 5.5/5* Agglomerate, breccia

conglomerate

INTERMEDIATE - FELSIC VOLCANICS ^T

4.1/4* DaCiti. Rhyodacite flows 4.3/41S D*cit*

TuiCs 4.3/tc Pyroclastics *.4 Md Feldspar

Porpnyty or Quartz Feldspar Porphyry

( .5/Ae Agclonifltat" , breccia, eon g lorne r ax*

- INTERMEDIATE VOLCAfi ICS 3.1/Ja Ancesite-Elow* 3.2/Jb -AntK*ite-tuff*,

• chisls [ash flows to bedd*a) 3.3/3C Ar.deait*~

tragnentals 3.4/Jd Feldspar Pctphyry

KAF1C VOLCANICS . . Z.1/28 Basalt (massive] Z-2/Zb Eaaalt I.3/2C Basalt fragmental 2.4/13 Tu(i, i cms t 2.5/2* voicular basalt

l.t/la Ultransfic flows and/cr intruuve ^^

1.2/lb Koreatiitie flows and/or Intrusive

DIAMOND DRILL HOLE

CLAIM POST

GEOLOGICAL CONTACT

500

SCALE

IOOO 1 500

NEWMONT EXPLORATION OF CANADA LIMITED

.3

42A35SE0I32 2.1*1*8 DENTON 230

2000 feet i ——-——-—

~* ^ AUG ? I9B6

_______ SCALE. ^ , 67f7

GEOLOGICAL

COMPILATION

_______ PROV|S)CE: ONTARIO

J______ PROJECT: DENTON TWP.

LOCAT4QN MAP

100-N

B/L 0+00 . o

IOO-S

B-L 166-S

200-S

300-S

400-S

500-S

600-S

in i

/r

O O

roi Ml

TOPOGRAPHIC

Trail portage

H Z! ~ ~ Bush road

Good drivng road, Highway

Rait road

Claim post located

Claim post assumed location

Witness post

Creek, River

Lake shore

Swamp, Bog - Property boundry line

MAX-MIN II H.E.M. SURVEY

Profile:In Phase

In Phase

x. - - x- - - x- - - x- - -x Out Phase

Coil Separation: 100 Meters k

Frequency 444 H 2

-14

-23UMKICTOR

-2O

*2

*2 l

OutPhase*i

7' 7

*3

NEWMONT EXPLORATION

DENTON TWP PROPERTY

survey by: Guy Thibault Exploration ServicesOperators: 6uy Th|bau|t L Tjm Bel,

Instrument:Apex Parametncs Max-Mm H

Drafted by : G. Thibault

42A05SECM32 2.10108 DENTON

DATE: February 198?

CPAI C*Vertical: lcm- IO*/. O VMUC* Horizontal: I:250O

100-N

B/L 0*00 , D

100-S

B-L 166-S

200-S

300-S

400-S

500-S

600-S

42AB5SECI132 2.10108 DENTON 250

N

fOl

CMl

OO*Ol

i

LOCATION MAP

TOPOGRAPHIC

Trail portage

~ H IT ~ Bush rood

4-"

Good drivng road, Highway

Rail road

Claim post located

Claim post assumed location

Witness post

Creek, River

Lake shore

Swamp, Bog — Property boundry line

MAX-MIN II H.E.M. SURVEY

Profile:. In Phase

in Phase.3

x, - -x- - - x- - - x- - -xOut Phase

Coil Separation: 100 Meters

,/ .A

Frequency (777

n

-M

-23COWUCTM

-2O

-i

*T

*2

A

Ou*Phase *i

(l-tG ,7

*3

NEWMONT EXPLORATION

DENTON TWP PROPERTY

survey by: Guy Thibault Exploration ServicesOperators : Quy

Instrument:Apex Parametrics Max-Min II

Drafted by : G. Thibault

DATE: February 198?

Qp A j p,Vertical: Icm* 10V.Horizontal: 1:2500