geol gchem & geoph rpt on the brown mcdade opt€¦ · in 1983, hollinger argus limited...
TRANSCRIPT
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
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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
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0.890.900.950.290.210.!50.203.220.250.200.21
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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
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. 261214200325186270170
2209414513395452412443140233251373187216234380586283186
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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