I Summers Township Joint Venture Property · proposed a fore arc accretionary prism, The major...

l l l l

42E12SW8033 2.13286 BEARDMORE AREA 010

2.13286GEOPHYSICAL REPORT

on theElectromagnetic and

l Induced Polarization Surveys " on the

Summers Township Joint Venture Property

I '* of GOLDEN DRAGON RESOURCES LTD.

andGLEN AUDEN RESOURCES LIMITED

Summers TownshipDistrict of Nipigon

Thunder Bay Mining Division, Ontarioby

Richard Lachapelle, B.Sc.Ing.Jr. January, 1990

RECEIVED

* MAY O a 1990

l MINING LANDS SECTION

l l l l l l

M-347

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

42E12SWae33 2.13286 BEARDMORE AREA 010C

TABLE OF CONTENTS

PAGE

ABSTRACT . . . . . . . . . . . . . . . . . . . . . . . . , , . . . . . . . . . . . . . . . . . , . . i

INTRODUCTION . . , . . , . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . l

LOCATION AND ACCESS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . l

CLAIM GROUP . . . . . , . . . . . . . . . . . . . . . . . . , . . . . . . . . . . . . . . , . . . 2

REGIONAL GEOLOGY . . . . . . . . . . . , . . , . . . . , . . . . . , . . . . , . . . . . . . . 3

PROPERTY GEOLOGY , . . . . . . . . . . . . . . . . . . . . . . , . . . . . , . , , , , . , . , 5

PREVIOUS WORK . . . . . . . . , . . . . . . . . . . . . . . . . , . . . . . . , . . . . . . . . 5

SURVEY PROCEDURE VLF

Theory . . . , . , , , . , , . , . . . . , , . , . . , . , . , . , . . . . . , , , , 9Field Method . . . . . . . . . . . . . . . . . . . , . . . . . . . . . . . . . . . JONotes on the Fraser Filter . . . . . . . , . . . . . . . . . . . . . . . . . . Jl

INDUCED POLARIZATION/RESISTIVITYTheory , . , . , . , , , . . . . , . , , . . . . . , , , . , , , . . , . , . . , , , JjfFjeJd Method . . . . . . , . . , . , . . , . . . , . . , . . . . . . . . . . , . . J5

PERSONNEL AND EQUIPMENT . . , , . . , , . . . . . . . . , . , . . . , . . . . . , , . . . 13

SURVEY STATISTICS . . . . . . . . . , . . . . . . . . . . . . . . . , . . . . . . . . . . . . J4

INTERPRETATION . . . . . . . . . . . . . . , . . . , . . . . . . , . . . . . . . . . . . . . . . J4VLF-EM Survey . , . . . . . . . . . . . . , . . . . . . . . . . . . . . . . . . . . . . J4Induced Polarization Survey , . , , . . . . , , , . , . . . . . . . . . . . . . . . 17

CONCLUSIONS AND RECOMMENDATIONS . . . . , . , . . . . . . . . . . . . . . . . . . . 18

REFERENCES . . . . . . . . , . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19

CERTIFICATION

l l l l l l l l l l l l l l l l l l l

LIST OF FIGURES

Figure l Figure 2 Figure 3a Figure 3b Figure 3c Figure 4a Figure 4 b Figure 4c Figure 5a Figure 5b Figure 5c

APPENDIX A:

APPENDIX B:

Property Location - RegionalRegional Location Map and Claim MapVLF-EM Survey, Block AVLF-EM Survey, Block BVLF-EM Survey, Block CFrazer Filter VLF-EM, Block AFrazer Filter VLF-EM, Block BFrazer Filter VLF-EM, Block CGeological and Geophysical Compilation Map, Sheet lGeological and Geophysical Compilation Map, Sheet 2Geological and Geophysical Compilation Map, Sheet 3

Equipment Specifications

IP Pseudosections4*OOW(2), 5+OOW, 7+OOW, 9+OOW, 11+OOW, 13+OOW, 15+OOW, 17+OOVf

-y-

l l l l lm ABSTRACT

A combined electromagnetic and induced polarization survey performed,

l during the month of September, 1989, on the Summers Township Property of Golden

Dragon Resources Ltd. and Glen Auden Resources Limited of Toronto, Ontario

|X

delineated several VLF-EM and chargeability anomalies,

m A follow-up program totalling $221,900.00 is recommended in order to

investigate the known anomalies and other anomalies that could have economic

l potential for base and/or precious metals,

l

l

l

l

l

l

l

l

l

l l l -1-

1NTRODUCTION

l From September 12, 1989 to September 21, 1989, a program of geophysical

surveying was conducted on the Summers Township Property for Golden Dragon

l Resources Ltd. and Glen Auden Resources Limited of 301-121 Richmond Street West,

m Toronto, Ontario.

The survey comprised VLF electromagnetic and time-domain induced

l polarization,

The survey was conducted as a follow-up to an airborne electromagnetic

l survey done by the Ontario Government (OGS, 1989), a lithogeochemical sampling

m report (Farrow, 1989) and a geological report (Bent, 1989) all of which delineated

structures and anomalies which might be indicative or associated with possible

l economic mineral deposits.

l LOCATION AND ACCESS

m The property is located in the southwest portion of Summers Township,

Thunder Bay Mining District. The eastern most portion of the claim group borders

l the community of Beardmore, Ontario, which is located on Trans Canada Highway

No.ll approximately 80 kilometres west of Geraldton and 120 kilometres northeast

m of Thunder Bay.

m The property is afforded excellent access via two bush roads which traverse

its length in a southwesterly direction. These bush roads provide convenient

l access to all parts of the property except for the extreme western portion.

l

l

l

Golden Dragon t Glen Auden Properly

•o*

l

l

l

l

•l*

PROVINCE OF ONTARIO

ID*

Fig. l

REVISIONS ROBERT 8, MIDDLETON EXPLORATION SERVICES INC.

GOLDEN DRAGON RESOURCES INC. TliK

PROPERTY LOCATION REGIONAL

tp. it txi\t\ l •160ml. i..i.?. ,u-jo———l * jT...—. — .1; lgiii;j-*jj-jM-


-2-

CLAIM GROUP

The property consists of 93 unpatented contiguous mining claims in Summers

Township, Thunder Bay Mining Division, Ontario. The VLF-EM geophysical survey

was conducted on the following claims:

Claim i No. Recording Date

519491519782810007-810010 inc.814301-814306 incl.815573-815574 inch815613-815614 incl.939667-939669 incl.1034165-1034167 incl.103600710559671073132-1073135 incl.1073137107313910731411073150-1073153 incl.1073155-1073159 incl.107316210731641073173107317610837481087478-1087484 incl.10874901087492-1087493 incl.1087495-1087496 incl.1116271-1116273 incl.1126548-1126550 incl.11265561126560

Total

l l 4 6 223 3 l l 4 l l l45 l l l l l 71223 3 l l

65 claims

November 29, 1979 December 03, 1979 September 04, 1984 September 04, 1984 September 04, 1984 September 04, 1984 August 01, 1986 October 05, 1988 October 05, 1988 July 17, 1989 October 05, 1988 October 05, 1988 October 05, 1988 October 05, 1988 October 05, 1988 October 05, 1988 October 05, 1988 October 05, 1988 October 05, 1988 October 05, 1988 October 05, 1988 October 31, 1988 November 09, 1988 November 09, 1988 November 09, 1988 September 20, 1989 September 20, 1989 September 20, 1989 September 20, 1989

The induced polarization survey was performed on the following claims:

1111111111111111111

*— 3

Claim # No.

519782 1814301-814303 incl. 3814306 1815613-815614 incl. 21055967 11073152 11073158 11087479 11087483 11116271-1116273 incl. 31126560 1

Total 16 claims

The claims are shown on Figure 2,

REGIONAL GEOLOGY

The following is quoted from Bent, 1989:

"The Beardmore-Geraldton belt is

'

Recording Date

December 03, 1979September 04, 1984September 04, 1984September 04, 1984

October 05, 1988October 05, 1988October 31, 1988October 31, 1988September 20, 1989September 20, 1989

underlain by three units of

westerly trending metavolcanic rocks, which are separated by

metasedimentary units (Williams, 1986). The area is considered to be

part of the Wabigoon Volcanic-Sedimentary Belt (Ayers, 1969), with the

southern most volcanic sequence in fault contact with the Quetico Belt,

which consists of a sedimentary sequence of higher metamorphic

grade. The westerly trending metavolcanic and metasedimentary

assemblages extend for approximately 180 kilometres from Lake Nipigon

to east of Little Long Lac. The repetition of major metavolcanic and

metasedimentary units within the Wabigoon Subprovince was postulated

as being the result of isoclinal folding (Pye, 1952; Horwood and Pye,

1955; Pye et al 1966; Mason and Mcconnell, 1983). However, this model

has been questioned by Mackasey (1975) due to the lack of facing

directional reversals, and questioned by Williams (1986) who has

l l- t .' ' -*' i* . , '. - . - -V .1.•V.-"--! .^' - : - .-:nv. : \R'V-.'V'. : .l™ •^.•"•^7 A i ' - .-"Xr^;

f-v Tjaarj:' 4e-.et V'V"*''M

ROBERT S. MIDDLETON EXPLORATION SERVICES INC

GOLDEN DRAGON RESOURCES INC. ie

PROPERTY LOCATIONa

CLAIM MAP' Flo. 2

l l l -4-

proposed a fore arc accretionary prism, The major east-vest trending

l volcanic-sedimentary units are bounded by right hand shear zones.

The three prominent shear zones of the Wabigoon Belt are: the

l Blackwater River (Empire), Watson Lake, and Paint Lake fault zones,

fi The Paint Lake Fault forms the Wabigoon-Quetico boundary (Williams,

* 1986).

l The metavolcanics are Keewatin age and the metasediments are

considered to be Timiskaming age. This belt of Archean rocks are

l folded, faulted and intruded by units of gabbro, diorite, granodiorite,

m and diabase. The metavolcanic unite consist of basaltic to andesitic,

massive pillowed flows, tuffs, volcanic breccia, and iron formation.

l The metasediments are composed chiefly of interbedded greywacke,

arkose, siltstone, and iron formation units, The iron formation within

l the southern metasedimentary unit can be correlated across the entire

m Beard more-Gerald ton Belt,

Nearly all gold production of the Beard more-Gerald ton Belt has

l been from metasedimentary units; with the exception of the Northern

Empire Mine which is hosted in a metavolcanic sequence. Iron

l formation host approximately 30X of the ore deposits (MacDonald, 1983)

m either as auriferous sulphide replacement zones and/or within

associated quartz veins. The remaining ore deposits of the Wabigoon

l Belt are largely quartz vein hosted and to a lesser extent shear zones

hosted by greywacke and less commonly porphyry bodies."

l

l

l

l l l -5-

PROPERTY GEOLOGY

l The following is quoted from Bent, 1989:

"The geological mapping of Summers Township Property has

l been divided into three map sheets designated 1,2, and 3 which are

m presented at 1:2500 scale (see attached map folder). Outcrop exposure

throughout the property is adequate to allow for detail mapping with

l the following exceptions: (1) the area east of the Tower Showing is

covered by glacial drift, and (2) the portion of the property north of

l the Empire Fault, which is underlain by metasedimentary units, offers

m limited exposure. The entire property is generally covered by a

relatively thin veneer (l-2m) of glacial drift, consisting of sandy till

l or sandy gravel, which thickens toward the east. The areas of

sulphide mineralization with possible economic potential are hosted in

l

the metavolcanic rocks."

PREVIOUS WORK

l The following is quoted from Bent, 1989:

"In 1935, the Empire Contract Gold Syndicate held a group of 28

m claims in Summers Township. The eastern claim boundary tied onto

m the Northern Empire Mine and stretched westward to the vicinity of

present day claims 1073156 and 1073155. Exploration concentrated on

l the western section was along a schistose zone with good sulphide (?)

mineralization and minor quartz veining. The highest reported gold

m assay value was 0.1 Au oz/ton.

m In 1938, Princess Lake Mines held a group of 25 contiguous

claims that straddled the Summers and Eva Townships boundary,

l

l l l -6-

encompassing Princess Lake. A mechanical stripping program along

l the metavolcanic and metasedimentary contact revealed a series of NE

trending quartz veins, upwards to 1.8 metres wide. Samples of the

l quartz vein system returned gold assay values ranging from 0.2-2.0

m Au oz/ton.

In 1938, the Morgan Property consisted of 3 contiguous claims

l adjoining the Princess Lake Mines property to the immediate east, A

series of five blasted pits were sunk along a NE trending fault scarp

l (the Northern Empire Fault). Visible gold was reported in a 3.5 metre

•j wide quartz vein. Several excellent gold assay values were recorded:

1.0 Au oz/ton, 2.0 Au oz/ton and a high assay value of 8.0 Au oz/ton.

l In 1938, Erie Canadian Mines inspected the Princess Lake Mines

property and the Morgan property. At the time of inspection water

B filled trenches prevented proper mapping and sampling. Low gold

m assay values were returned from a few selective grab samples.

In 1936, Buffalo Beardmore Gold Mines held a 13 claim group

l straddling Summers Township and the Beardmore Area western

boundary, immediately north of the Black Water River. Surface work

l

l

consisted of 450 metres of stripping and the excavation of a "deep"

m test pit. No assay values were reported.

1937 A 24.5 metre shaft was sunk and continued

m stripping and sampling revealed a series of

auriferous quartz veins. The area was designated

No.4 Zone, or "Hill" vein and later became known as

the Long Beard Showing.

l l l -7-

1938 Continued surface exploration and a 3048 metre

l diamond drill program was conducted with

encouraging results.

l 1939 A scheelite discovery propelled continued

m exploration along four mineralized zones, in

particular the No.4 Zone.

l 1940 A limited surface program and diamond drill

program. No assay values were reported.

l 1942 Surface work continued and a limited diamond drill

m program.

1943 Continued scheelite exploration with a limited

l stripping and diamond drill program,

1949 Very little exploration was conducted from 1943

m onward, and in 1949 the company's Ontario Charter

m was cancelled.

In 1949, Broadview Gold Mines Limited acquired 21 contiguous

l claims in Summers Township, seven of which covered the No.4 Zone of

the former Buffalo Beardmore Gold Mines property. Later that year a

l magnetometer survey by J.H. Low, consulting geophysicist, outlined

M nine separate magnetic high features in the vicinity of the No.4 Zone.

A proposed follow-up program of diamond drilling and surface work

l was never performed due to financing difficulties,

The Long Beard property was relatively dormant during the

l

l

next forty years. The property changed ownership several times with

little exploration achieved.

l l l -8-

In 1959, E.B. Rentz drilled 4 shallow holes immediately south of

l the Morgan Showing, totalling 210 metres. Minor pyrite and

arsenopyrite mineralization was reported,

l In 1960, G. Petrie drilled 6 shallow holes on the present day

m claim 1073176. Sheared and altered greywackes were intersected with

no mineralization reported.

l In 1981, Gold Fields Resources Canada Ltd. held a 65 contiguous

claim group coinciding with the northern half of the present claim

l group, and extending westward into Eva township. A cut grid at 100

m metre spacing and picketed at 25 metre intervals blanketed the entire

property. A magnetometer survey, VLF-EM survey and a humus

l geochemistry survey of the property were conducted, A follow-up

mechanical stripping program and a 6 diamond drill hole program

m intersected minor sulphide mineralization. No assay values were

m reported.

In 1983, A, Hopkins held a 51 claim group encompassing the

l Morgan Showing and Long Beard Showing. Stripping at the Morgan

Showing was the only reported work.

l In 1984, Thorco Gold Finders held 11 contiguous claims

m straddling the SW Summers Township boundary, and east of the Long

Beard Showing. A surface program of mechanical stripping, sampling,

l geological mapping and a magnetometer survey was implemented. An

8.2 metre wide oxide facies iron formation was located. One diamond

l

l

l

drill hole intersected the oxide zone at depth with low gold assay

values,

SURVEY PROCEDURE

l l l

In 1986, Legion Resources acquired 48 contiguous claims in the

l S W portion of Summers Township. The claim group encompassed the

Long Beard Showing. An airborne magnetometer and EM survey was

m conducted by Terraquest Ltd. The airborne survey revealed strong

m EM conductors associated with magnetic high features in the Long

Beard vicinity."

l

lm Theory

The VLF (Very Low Frequency) electromagnetic system is a frequency domain

l system which uses military transmitters designed to communicate with submarines

as a source. The system measures the response of conductors to these time

m varying electromagnetic fields.

m The transmitted, or primary EM field is a sinusoidally varying field in the

range of 15.0 to 30.0 KHz, dependant on the source station used. This field induces

l an electromotive force (emf), or voltage in any conductor through which the field

passes, This is defined by

l Jk.dl = el/31 (The Faraday Induction Principle)

where E is the electric field strength in volts/metre (and sojtE.dlis the emf around

l a closed loop) and j6 is the magnetic flux through the conductor loop. This emf

causes a "secondary" current to flow in the conductor in turn creating a secondary

m electromagnetic field, which is measured by the receiver.

m The VLF transmitting antennae are vertically oriented, thus the primary field

is horizontal perpendicular to the transmission direction.

l

l l l -10-

The secondary field from a conductor is different in amplitude from the

l primary, and shifted in phase. Because both fields are sinusoidal, the resultant

electromagnetic vector traces an ellipse. The receiver measures two of the

l following properties of the ellipse: orientation of the minor axis (tilt), ratio of

m minor to major axis (elipticity), or amplitude of the minor axis (field strength).

The receiver has two receiving coils built in, one coil with a normally vertical

l axis and the other horizontal. The signal from the vertical axis coil is first

minimized by tilting the instrument. The remaining signal in this coil is finally

l balanced out by a measured percentage of a signal from the horizontal coil, after

m being shifted in phase by 90 degrees.

Assuming the secondary signal is small compared to the primary field, the

l mechanical tilt angle is an accurate measure of the vertical real (in phase)

component of the secondary, and the 90 degree compensation signal from the

M horizontal coil is a measure of the quadrature vertical signal.

m Field Method

A transmitter station is selected which gives a strong field as close as

l possible to right angles to the suspected strike of the geology.

The reference (horizontal) coil is oriented parallel to the primary field, and

l then the instrument is tilted until the minimum is heard. The quadrature

m component (compensator) is then adjusted until a further minimum is reached, and

the tilt angle and compensation field recorded as in-phase and quadrature field in

l percent.

Readings are normally taken at 25m intervals. Shorter spaced readings may

m be taken unless the data is to be Fraser Filtered for plotting.

l

l

l l l

Notes on the Fraser Filter

l This is a system for presenting VLF tilt angle data devised by D.C. Fraser

(Contouring of VLF-EM Data, Geophysics, Vol.34, No.6, December, 1969). It is

l basically a combination of a low pass (noise removal) filter and a gradient filter

m which smooths the data and converts high gradients (cross-overs) to peaks. These

results are then plotted on a map and contoured to show high values in regions of

l high conductivity.

The filter operator is [M3 f M4 - Ml - M2] where Ml, M2, M3, M4 are four

l consecutive data points.

™ INDUCED POLARIZATION/RESISTIVITY

l Theory

The induced polarization (IP) and resistivity exploration methods are

l electrical methods based on measuring the response of the earth to an applied

m direct current.

The principle is to apply a known electric current to the earth, and measure

l the electric potential created by it at the survey location. The resistivity, a bulk

property of the rock itself, is calculated from the difference between the applied

l current and the measured potential, corrected for the geometry of the current and

M potential electrode configuration.

The induced polarization measurement is based on the "over-voltage" effect.

l Most of the electric current carried by the earth is conducted by the flow of ions

in the solutions filling the pore spaces in the rock. At the surface of any metallic

l particle in the path of current low, the ionic flow in the solution is changed to an

M electronic flow in the metal. In the process of the change, an electric charge of

trapped ions is built up at the surface of the metal, storing a small voltage. If the

l

l l l -12-

voltage increases, the apparent resistance of the rock also increases. If the

l applied current flow is decreased or stopped, the voltage will create a potential in

the opposite direction to the original applied current, and start a current flowing

l in the opposite direction.

m In time domain induced polarization the applied current is abruptly stopped,

and the reverse potential created by the over-voltage effect is measured over time

l as it quickly decays. The definition of chargeability is:

M = V (t =CO) - V (t = 0) l V(t

•j where V(t r 0) is the voltage at turnoff, and V(t z&y) is the late-time voltage. This

is usually measured over a certain time period after turn-off as an integral of

l voltage over time, corrected for the length of the time period, and normalised to

the voltage at time O. It is usually expressed in millivolts per volt (mV/V),

m The over-voltage charge taken time to build-up or decay, so that if the

m applied current is caused to oscillate more and more frequently, the apparent

resistance will decrease, as the over-voltage does not have time to build at higher

l frequencies. This effect is used to measure the IP effect in frequency domain IP

surveys, wherein the current is applied at two or more frequencies, and the

m "percent frequency effect" (PFE) is calculated from the change in resistivities (P)

m between the different frequencies.

PFE r P (low freq) - P (high freq) x 100X— P (high freq)

Although not identical, for most purposes the PFE is approximately equal to

l the chargeability.

m Because the IP effect responds to effects on small metallic particles, it is

particularly useful for detecting disseminated metallic minerals. Also because of

l

l l l

this, it will respond strongly to the "membrane polarization" created by the electric

l charges resident on clay particles or layered or fibrous minerals,

Field Method

l The survey was conducted using a pole-dipole array with a dipole length of

m 25m and array spacings of n - 1,2,3,4 dipole. This array configuration involves

having a dipole for the receiver measuring Vp, the potential and a single current

l transmitter electrode on the grid, separated from the receiver dipole by each 'n'

interval in turn. The other current electrode, 'the infinity' is situated 2 kilometers

l or more from the grid.

•j For this survey the measurements were taken in the time domain, so the

transmitted current was a bipolar on-off square wave with each on or off lasting

l two seconds, Measurements of resistivity and chargeability were taken,

l PERSONNEL AND EQUIPMENT

m The following personnel from Robert S, Middleton Exploration Services Inc.

conducted the surveys:

I Brad Malpage, Technician Darryl Ball, Technician Melvin Booth, Labourer

U Rodney Booth, Labourer

The equipment used were a Geonics EM-16 Electromagnetometer, a Scintrex

l IPR-11 Time-domain induced polarization receiver, a Scintrex TSQ-3, 3 KW

m Transmitter and a Huntec 7.5 KW Transmitter. Specifications for these instruments

™ are included in Appendix A,

l

l

l

l l l

SURVEY STATISTICS

l The survey comprised 67,075 line km of VLF electromagnetics and 4.85 line

km of time-domain induced polarization,

m The survey required 10 days to complete, of which two days were used for

m mobilize tion/demobiliza tion.

l

l

INTERPRETA TION

The combined results of the geophysical surveys and previous geological

I'*

mapping program (Bent, 1989) are illustrated on Figures 5a, 5b and 6c. The results

of the VLF-EM survey are illustrated on Figures 3a, 3b, 3c, 4a, 4b and 4c,

VLF-EM Survey

l The VLF-EM survey delineated 18 anomaly axis denoted VI to V18 inclusively.

These anomaly axis are denoted in order of importance and extent, the stronger

m and longer in extent an axis is, the smaller its' index; i.e. VI is stronger than V18.

m The anomaly axes are enhanced in some areas by topographic features, each

anomaly is hereafter described and interpreted.

l Anomaly axis VI is a weak to strong conductivity axis extending from station

1+50N on line 7+OOW to station 1+50N on line 29+OOE. This anomaly axis is sub-

| parallel to an airborne EM conductor axis delineated by OGS, 1989, It is also sub-

m parallel in some areas (see Figs. 5b and 5c) to the trace of the Empire Fault

delineated by Bent, 1989. This anomaly axis is interpreted to represent shearing

l of the metavolcanic rocks accompanied with sulfide mineralization. This

interpretation is supported by ground evidence by Bent, 1989.

m Anomaly axis V2 is a strong conductivity axis extending from station 12+50S

M on line 17+OOW to station 12+OOS on line 4+OOW. This anomaly axis is located 100

meters south and sub-parallel to the projected trace of the Swamp Lake Fault. Axis

l

l l l -16-

V2 is therefore interpreted to possibly represent shearing and associated sulfide

l mineralization within the metavolcanic rocks caused by the Swamp Lake Fault,

Anomaly axis V3 is a weak to strong conductivity axis extending from station

l 6+OOS on line 22+OOW to station 6+OOS on line 3+OOE. This anomaly axis is sub-

M parallel to a weak to strong conductor axis delineated by OGS, 1989, Axis V3 is

therefore interpreted to possibly represent sulfide horizons within the metavolcanic

l rocks,

Anomaly axis V4 is a moderate to strong conductivity axis extending from

g station 1+25N on line 21+OOW to station 0+50N on line 10+OOW. Anomaly axis V6 is a

B weak to strong conductivity axis extending from station 2+50N on line 20+OOW to

station 1+50N on line 3+00 W. These anomaly axes are interpreted to represent

l splays of axis VI and are therefore interpreted to be of the same nature,


l station 16+25S on line 11+OOW to station 16+OOS on line 1+OOW. This anomaly axis is

m 250 meters south and sub-parallel to the Long Beard Showing, and is therefore

interpreted to possibly represent shearing and associated sulfide mineralization

l within the metavolcanic rocks,


l station 15+75S on line 11+OOW to station 15+25S on line 3+OOVf, This anomaly axis is

M 150 meters south and sub-parallel to the Long Beard Showing, and is therefore

interpreted to possibly represent shearing and associated sulfide mineralization

l within the metavolcanic rocks.

Anomaly axis V8 is a weak to strong conductivity axis extending from station

l 4+50N on line 11+OOW to station 2+50N on line 27+OOE. This anomaly axis is sub-

M parallel to the interpreted trace of the Empire Fault and is therefore interpreted

to possibly represent shearing and associated sulfide mineralization within the

l

l l l

l

l

-16-

metavolcanic rocks. Bent, 1989 has also postulated that this axis represents the

l contact between the metavolcanic and metasedimentary units.


l station 11+50S on line 11+OOW to station 11+50S on line 1+OOW, This anomaly axis is

interpreted to represent a splay of axis V2 and is therefore interpreted to be of

the same nature,

l Anomaly axis V10 is a moderate to strong conductivity axis extending from

station 10+50S on line 17+OOW to station 10+50S on line 5+OOW. This anomaly axis is

l sub-parallel and to the north of the Swamp Lake Fault and is therefore interpreted

to possibly represent areas of shearing and associated sulfide mineralization within

the metavolcanic rocks,

l Anomaly axis Vll is a weak to strong conductivity axis extending from station

5+SOS on line 22+OOW to station 4+75S on line 11+OOW. This anomaly axis is

m interpreted to represent a splay of axis V3 and is therefore interpreted to be of

m the same nature.


l station 3+25N on line 12+OOW to station 3+50N on Line 5+OOW. This anomaly axis is

interpreted to represent a splay of axis V8 and is therefore interpreted to be of

l the same nature,

m Anomaly axis V13 is a moderate to strong conductivity axis extending from

station 4+25S on line 22+OOW to station 4+50S on line 16+OOW. Anomaly axis V14 is

l a weak to strong conductivity axis extending from station 5+25S on line 2+OOW to

station 5+25S on line 5+OOE. Anomaly axis V15 is a weak to strong conductivity axis

l extending from station 7+OOS on line 3+OOW to station 6+75S on line 3+OOE. These

m anomaly axes are interpreted to represent splays of axis V3 and are therefore

interpreted to be of the same nature.

l

l l l


l station 13+50S on line 11+OOW to station 13+50S on line 8+OOW, Anomaly axis V18 is

a moderate conductivity axis extending from station 12+50S on line 11+OOW to station

l 12+76S on line 9+OOW, These anomaly axis are interpreted to represent splays of

m axis V2 and are therefore interpreted to be of the same nature.

Anomaly axis V17 is a moderate conductivity axis extending from station

l 17+OOS on line 11+OOW to station 17+25S on line 7+OOW. This anomaly axis is

interpreted to represent a splay of axes V6 and V7 and is therefore Interpreted to

l be of the same nature,

m Induced Polarization Survey

The limited induced polarization survey delineated several features of

l interest, namely:

- the chargeability signature of VLF-EM axes V9 (at line 11+OOW), V2 (at line l 7+OOW and 11+OOW) and V10 (at line 15+OOW);

- the shears associated with VLF-EM axis V10 (all along the axis);

l - alteration borders of VLF-EM axes V12 (at station 3+25N on line 4+OOW) and V3 (at station 6+25S on line 4+OOW);

l - chargeability anomalies at station 8+OOS on line 17+OOW.

l

l

l

l

l

l

lll CONCLUSIONS AND RECOMMENDATIONS

l The combined VLF-EM and IP surveys delineated several conductors and

chargeability anomalies interpreted to represent sulfide mineralization within the

l metavolcanic rocks. The IP survey also delineated alteration borders of VLF-EM

m conductors worthy of further work.

The recommendations for further work are the same as those outlined in Bent,

I 1989, i.e. a first phase of induced polarization totalling $44, 300.00, a second phase

of geological sampling totalling $17,250.00 and a third phase of diamond drilling

l totalling $160,350.00. The combined phases total $221,900.00.

Respectfully submitted

lRichard Lachapelle, B.Sc.Ing.Jr.

-

m

l

l

l

l

l

l

l


-19-

REFERENCES

BENT, H. 1989

FARROW, D.G. 1989

GEOLOGICAL REPORT on the Summers Township Property for Golden Dragon Resources Ltd. and Glen Auden Resources Limited, November, 1989

A Brief Summary of Lithogeochemical Sampling and Assays Results from the Beardmore Area Property of Legion Resources Inc., January 25

ONTARIO GEOLOGICAL SURVEY1989 Airborne Electromagnetic and Total Intensity Magnetic Survey,

Tashota-Geraldton-Longlac Area, District of Thunder Bay by Aerodat Limited for the Ontario Geological Survey, Geophysical/Geochemical Series, Map 81337 Scale 1:20,000 Survey and Compilation, June to December 1988.

l l l l l l l l l l l l l

l l l l

CERTIFICATION

I, Richard Lachapelle, of 136 Cedar Street South, in the City of Timmins, Province of Ontario, certify as follows concerning my report on the Golden Dragon Resources Ltd. and Glen Auden Resources Limited property in Summers Township, Province of Ontario and dated January 15, 1990:

1. I am a junior member in good standing of 1'Ordre des Ingenieurs du Quebec.

2. I am a graduate of 1'Universite de Sherbrooke, Sherbrooke, Quebec with a B.Se. degree in Physics, obtained in 1984.

3. I am a graduate of 1'Ecole Polytechnique de Montreal, Montreal, Quebec with a B.Ing degree in Geological Engineering obtained in 1987.

4. I have been practising in Canada since 1987.

5. I have no direct interest in the properties, leases, or securities of Golden Dragon Resources Ltd, or Glen Auden Resources Limited, nor do I expect to receive any.

6. The attached report is a product of:a) Examination of data included in the report which was collected

on the property concerned.

Dated this 15th day of January, 1990 TIMMINS, Ontario

Richard Lachapelle, B.Sc.Ing.Jr. Geophysicist

l* Ontario

l•"ype of Survey(s)

township or Area

laim Holder(s)

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

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

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

C.

lurvey ftDT)/ ^T6

Author Of Rt-pnrt

ddress of Authort"Co

lvering Dates of Survey,

fotal Miles of Line Cut_(linecuttlng 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—————

DAYS per claim.

Geological.Geochemical.

AIRBORNE CREDITS (Special provlilon credit! do not apply to airborne lurveyi)

Magnetometer Electromagnetic(enter dayi per clai

SIGNATUR

lRes. Geol.. .Qualifications.

lIreyious Surveys File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

(prefix) (number)

TOTAL CLAIMS.

I

Jc.®" Ontario

1*pe of Survey(sc t unship or Area

im Holder (s) x70 /fat

Mr ve y Company Author of Report f dress of Autho

vering Dates oi

Vtal Miles of Lit

Fi1 Ministry of Natural Resources" GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL , TECHNICAL DATA STATEMENT

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


/f^PoCtrp pOLs^/î^fiTfft^L ..SOMÊf^S T/Or.)DLl)fi\l T)Â6'ONi P^soo/fcES 1-T&.i/UDJLETo^ P^P^L5P^/ /MC 'T?rtrtitJ5

jft'c/JA^ f AcMP^-Ufr /^^ C^D//^ 3f~AfcfLT~ ^dt^P/J '//n'f'^5o ^pPfyJD /QP9 -m V/^/T-O/ /Q&QSurvey v^C \ l /(jJk f/tf f I^J ^-"—f f cxi/ l /Q 7

(linecutljng to offjce) e Cut 7^f?l /^ /VT)

fcpEClAL PROVISIONS DAYSCREDITS REQUESTED n.™,..,..,.! i™*"--

(ENTER 40 dayline cutting) foi

Burvcy.T;NTER 20 day

(dditional sum ame grid.

r '

-Electromagnetic.. , s (includes . r- t -Magnetometer ———————

* 11 0 l

—Radiometric..—,...s for each -OtherT "sing Ctrolngiral

npnr}|P?Tlif?'l

MRBORNE CREDITS (Special provltlon credlti do not apply to airborne lurveyi)

hHgnetometer

'

1

Is. Geol.

vious Surveys

,,, F-|prtr"m?pn*'Hf. . ^^^lorn^tr(enter dayi per claimLr li * rt

f Author of Report o/ Agent

Qualifications

File No. Type Date Claim Holder

f....................f...................f.....................

If

MINING CLAIMS TRAVERSED Lilt numerically

f&SlWffi -f&fs'teo/7T5 Î^BOZZ,

(number)^.cj/y^^........f8^j06 78 V#bftIZfr/fyy Tb((#p?6f73/^/5^ Tfi/oW&tirS/^f/79 TB/^7^77? ////T^ 1 T& ////"~).7~2 ID ///ctXT 1 , ' C* f ' r(\ **- T ^-

^ W&73 "t9ffet*66

TOTAL CLAIMSf r*"**

i;

M

sa

GEOPHYSICAL TECHNICAL DATA

W more than one survey, specify data for each type of survey

f umber of Stations. ation interval__

Profile scale ——~——.jutour interval.

l

l

l

ll

l

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

InstrumentCoil configuration Coil separation —— Accuracy .-———— Method: Frequency____

.Number of Readings

.Line spacing ——-———

Q Fixed transmitter D Shoot back D In line D Parallel line

Parameters measured.(ipedfy V.L.F. nation)

GRAVITY

m

1 1m

Sr^lf rnnpfanf .

Crirrrrtinii* tiiarlc... ,

Base station value and

Elevation accuracy —

location . . , . . ...... —

Instrument —Method 03 Time DomainParameters — On time ———

- Off time ——— Delay time ___— Integration time.

CJ Frequency Domain _ Frequency______ Range ^^——^——,

Power 7. 5Electrode array — Electrode spacing

flumber of Stations.

Jptation interval Profile am le.

mtour interval.


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

.Number of Readings JLine spacing_~~ rt)

HA?

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

Instrument g ri-/Coil configuration —— Coil separation -———± /y,Accuracy ———J- ( ft?

Method:Frequency.

l. Parameters

D Fixed transmitter

W

D Shoot back D In line

(ipedfy V.L.F. ititlonj

D Parallel line

Or 3/Tc^/s/^/TX

. Instrument.Scale constantCorrections made.

Base station value and location ,

Elevation accuracy.

"i

InstrumentMethod CD Time Domain Parameters - On time .

-Off time .— Delay time— Integration time.

PowerElectrode array — Electrode spacing,

D Frequency Domain- Frequency —————— Range ———————

Ontario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

13286l l

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


ype of Survey(s) Township or Area Jaim Holder(s)

C.

9orvey rorJ

Author of Report — ddrcss of Author-ZJLk.lCovering Dates of Survey S?PT /2 ff&r

(linecutting to office)

tal Miles of Line Cut

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———^.

DAYS per claim.

Geological.Geochemical.

f•aRDORNE CREDITS (Special provlilon ctediu do not apply to airborne tump) .gnetometer____Electromagnetic ————.R^diome^ri c

(enter dayi per claim

SIGNATURE:

lRes. Geol.Bc

jF

.Qualifications.cvious Surveys ile No. Type Date Claim Holder

l

I I


....:,,...... .. ...(prefix)

~.T;.fTT7v*l.i-.VW(.7(number)

'.f

7/3 7/l UTAL CLAIMS

1

i

1

1r

\t

\ 1

1

]

,

1 -

1 Ontario

1 TECHNIC

lype of Survey(s) /'

Kwnship or Area ^ l"

lim Holder(s)(ÔLl)f i\l

Jo /ftrt/DDLE-T

t )^C .t -v rvey Company K - /I/I

\nrhorofReport OO

E dress of Author /o k-

vering Dates of Surveyo

I)tal Miles of Line Cut

SPECIAL PROVISIONSCREDITS REQUESTED

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

Fi Ministry of Natural ResourcesGEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL

TECHNICAL DATA STATEMENT

O BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORT FACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT AL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

OpQClrp pOL-^'7iATf()tJ^HEf^3 T/0^7)ÔN\ tf^SOO/fc^S LT&.

i f) AO.^ ^6K fC3 7CM p^ft-^Pw/rtC fiHrtit-JS)T)irfT7ZyJ eXf*CAi(A?lONJ 5CC^C^5 /RJA^D /AcArtP^-UfceD^/Jr^^^T- ^d6ryj -y/^^Js^fV^yS^TOvSH/^/ ^j^

(Unecutting to offjce)

DAYS ~ , . , per claim.Geophysical—Electromagnetic. . , -

s— Magnct^mrtfr., , , ,, ,,,—Radiometric. - .-Olhi-r

Ornlngiral

OpnrhTnir?!

MRBORNE CREDITS (Special proviilon credit) do not apply to drborne lurveyi)— /l gnptnmpter, , F-lTtrnm?pnriir , /'"xfeariinWpt.rir

(enter dayi per clairrtjf^ II

^TP.fRNi ft/JD RinNATHRR^^McJ^Wfik

1Res. Geol.

•cvious Surveys

7 Author 6( Report or AgWt

Oiialifiraf ions

Vile No. Type Date Claim Holder

1:::: ::::: i:i:::::::::::.l.....................................

...,,,.., ,.,.,, ..., ———— ... ——————— . ———— .-....^...M....^.,,.,.,.....,.^

1"


fB5/??^ 78 2/^30 f(prefix) ' (number)

7ft (5Vy*^3T^f/v^ Xy3 ?i5(?ftT&it/Pty/ ,TS ^p?^fTft/^ffl^*** T& /o-? 3/5 fi

Ifa^fiJ!

?fi ///6tf3 -

5/^7^?

.. .

TOTAL CLAIMS /k

If space insufficient, attach lift


P rM'MM^ t PVrY'i If more than one survey, specify data for each type of survey

^lumber of Stations-Station interval ———

Profile scale^-—-—jntour interval.

.Number of Readings

.Line spacing.————

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

instrumentCoil configuration - Coil separation —— Accuracy ————— Method: Frequency-—————

Parameters measured.

. Instrument.Scale constant,Corrections made.

CD Fixed transmitter D Shoot back CD In line D Parallel line

(tpedfy V.L.F. lUtlon)

Base station value and location

Elevation accuracy.

Instrument —Method t0 Time DomainParameters — On time .

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

Power

CD Frequency Domain _ Frequency______ Range _______

7.5Electrode array —

Electrode spacing.

l l l

Number of Stations Station interval ^Profile scale ———,


- If more than one survey, specify data for each type of survey

.Number of Readings JLine spacing _

Contour int^l &P tffafg F/tfGC.

M

l

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

Instrument ,Coil configuration __ Coil separation ——-. Accuracy ± l /c*

Method: D Fixed transmitter8 77/jE W. g

D Shoot back D In line D Parallel line

Parameters

Instrument.Scale constant.Corrections made.

(ipedfy V.L.F.iUtlon)Of

Base station value and location.

l

l

l

Elevation accuracy.

Instrument ™—-————. Method D Time Domain Parameters — On time ___

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

PowerElectrode array — Electrode spacing , Type of electrode ,

D Frequency Domain Frequency ————— Range ————————

l

l

l

l

APPENDIX A

•EM16 VLF Electromagnetic Unit

lPioneered and patented exclusively by Geonlcs Limited, the

•VLF method of electromagnetic surveying has been proven to•be a major advance In exploration geophysical Instrumentation.

Since the beginning of 1965 a large number of mining ompanles have found the EM16 system to meet the need for simple, light and effective exploration tool for mining eophyslcs.

EThe VLF method uses the military and time standard VLF ansmlsslons as primary field. Only a receiver Is then used to easure the secondary fields radiating from the local con

ductive targets. This allows a very light, one-man Instrument ô do the job. Because of the almost uniform primary field, Bjood response from deeper targets Is obtained.

The EM16 system provides the In-phase and quadrature omponents of the secondary field with the polarities Indicated.tnterpretation technique has been highly developed particularly

to differentiate deeper targets from the many surface Indications.

vrlnclple of Operation^he VLF transmitters have vertical antennas. The magnetic

signal component Is then horizontal and concentric around •he transmitter location.

JSpeclfications

tource of primary field

ransmlltlng stations used

rfi

il

perallng frequency range arameter* measured

Method of reading

cale range eadablllty

VLF transmitting stations.

Any desired station frequency can be supplied with the Instrument In the form of plug-In tuning units. Two tuning units can be plugged In at one time. A switch selects either station.

About 15-25 kHz.

(1) The vertical In-phase component (tangent of the tilt angle of the polarization ellipsoid).(2) The vertical out-of-phase (quadra ture) component (the short axis of the polarization ellipsoid compared to the long axis).

In-phase from a mechanical Inclino meter and quadrature from a calibrated dial. Nulling by audio tone.

Reading time

Operating temperature range

Operating controls

Power Supply

DimensionsWeightInstrument supplied with

In-phase ± ISO'/o; quadrature ± AQVt. Shipping weight

10-40 seconds depending on signal strength.

-40 to 50* C.ON-OFF switch, battery testing push button, station selector, switch, volume control, quadrature, dial ± 40 0/., Inclinometer dial ± 150Vo.

6 size AA (penllght) alkaline cells. Life about 200 hours.

42 x 14 x 9 cm (16 x 5.5 x 3.5 In.)

1.6 kg (3.5 IDS.)

Monotonlc speaker, carrying case, manual of operation, 3 sfallon selector plug-In tuning units (additional fre quencies are optional), set of batteries.

4.5kg(10lbs.)

l

GEONICS LIMITED Designers A manufacturers of geophysical Instruments

subsidiary of Deorlng Milliken (no,

2 Thorncllffe Park Drive, Toronlo/Onlarlo/Canada M4H1H2 Tel: 425-1824 Coblei; Qoonioi

tesy ol Newfoundland A Labrador Corp. Lid,

J

Areas ol VLF SignalsCoverage shown only lor well-known stations. Other reliable, tully operational stations exist. For lull Information regarding VLF signals In your area consult Oeonlcs Limited. Extensive field experience has proved that the circles of coverage shown ere very conservative end are actually much larger In extent.

EM 18 Profile over Lockport Mine Property, Newfoundland AdcBonal case histories on request.

vertical coll

horizontal . coil

W T 'i""r10-0 4 10

Station Selectorunits can be plugged

n amne time. A switch selects Mhtistetlon.

inuonvojfm amne thWst

l

Receiving Colls Vertical receiving coll circuit In Instrument picks up any vertical signal present. Horizontal receiv ing coil circuit, after automatic 00' signal phase shift, leeds signal Into quadrature dial In series with the receiving coll.

In-Phese Dial shows the tilt-angle of the mont for minimum signal. This angle Is the measure of the vertical In-phase signal expressed In percentage when compared to the horizontal field.

Quadrature Dlatfs calibrated In percentage mark- Ings and nulls the vertical quad rature signal In the vertical coll circuit.

By •looting a suitable transmitter station as a source, the EMw user can survey with the most suitable primary field azimuth.

TheVM 16 has two receiving colls, one for the pick-up of the horfcntal (primary) field and the other for detecting any anomalous vertical secondary field. The coils are thus ortho gonal, and are mounted inside the instrument "handle".

Th^clual measurement Is done by first tilting the coll assembly to minimize the signal In the vertical (signal) coll and [hen further sharpening the null by using the reference signal to nek out the remaining signal. This is done by a calibrated "qfldrature" dial.

The tangent of the tilt angle is the measure of the vertical in-phase component and the quadrature reading Is the signal at right angles to the total field. All readings are obtained in per cenlages and do not depend on the absolute amplitude of the primary signals present.

The "null" condition of the measurement Is detected by the drop In the audio signal emitted from the patented resonance loudspeaker. A jack Is provided (orthose preferring the use of an earphone Instead.

The power lor the Instrument Is from 6 penllght cells. A battery tester Is provided.

Or.f/73

Time Domain IP Receiver

• Technical Description-of tte IPR-11 Broadband'^H ^W^ S BAA. —— J^\ — ••.jk ——^ ! ——— l ^^ J^^ -^ __ __ ? - -. __ -

l l l

Input Potential Dipoles

input impedance

Input Voltage (Vpj Range

M Automatic SP Bucking Range

Chargeability (M) Range

l l l l i i

Absolute Accuracy of Vp, SP and M

IP Transient Program

VP Integration Time

Transmitier timing

Header Capacity

B Data Memory Capacity

li

liExternal Circuit Check

l

l

l

Filtering

Internal Calibrator

1 to 6 simultaneously.

4 megohms.

100 microvolts to 6 volts lor measurement. Zener diode protection up to 50V.

± 1.5V.O to 300 mV/V (mils or 0/00)

Vp; ± y/o of reading (or Vp > 100 mic rovolts. SP; ± 30Xo of SP bucking range. M; ± y/o of reading or minimum ±0.5mVW. ,

Ten transient windows per input dipole. After a delay from current off of t, first four windows each have a width of t, next three windows each have a width of 6t and last three windows each have a width of 12t. The total measuring time Is therefore 58t. t can be set at 3.15,30 or 60 milliseconds for nominal total receive times of 0.2,1,2 and 4 seconds.

In 0.2 and 1 second receive time modes;0.51 sec.In 2 second mode; 1.02sec.In 4 second mode; 2.04 sec.

Equal on and off times with polarity change each half cycle. On/off times of 1, 2,4 or 8 seconds with ± Z.5% accuracy are required.

Up to 17 four digit headers can be stored with each observation.

Depends on how many dipoles are re corded with each header. If four header items are used with 6 dipoles of SP, Vp and 10 M windows each, then about 200 dipole measurements can be stored. Up to three Optional Data Memory Expansion Blocks are available, each with a capacity of about 200 dipoles.

Checks up to six dipoles simuiianeousfy using a 31 Hz square wave and readout on front panel meters, In range of O to 200k ohms.

RF filter, spheric spike removal; switchable 50 or 60Hz notch filters, low pass filters which are automatically removed from the circuit in the 0.2 sec receive lime.

1000 mV of SP, 200 mV of Vp and 2.43 mV/V of M provided In 2 sec pulses.

{Technical DescriptionofthfilPR-11 Broadband

|TimTOomain IP Receiver

l l Digital Display

l

Standard Rechargeable Power Supply

Disposable Battery Power Supply

Dimensions

Weight

l Analog Meters

l Digital Data Output

l

l

l

l

l

l

l

l

ll

l

l

Two, 4 digit LCD displays. One presents data, either measured or manually entered by the operator. The second display: 1) indicates codes Identifying the data shown on the first display, and 2) shows alarm codes indicating errors.

Six meters for: 1 j checking external circuit resistance, and 2) monitoring input signals.

RS-232C compatible, 7 bit ASCli, no parity, serial data output for communication with a computer, digital printer, digital storage device or modern.

Eight rechargeable NiCad D cells provide approximately 15 hours of continuous operation at 250C. Supplied with a battery charger, suitable for 110/230V, 50 to 400 Hz, 10W.

At 250C, about 40 hours of continuous operation are obtained from 8 Eveready E95 or equivalent alkaline D cells.

At 25"C, about 16 hours of continuous operation are obtained from 8 Eveready 1150 or equivalent carbon-zinc D cells.

Operating Temperature Range

Storage temperature Range

345 mm x 250 mm x 300 mm, Including lid.

io.5 kg, including batteries.

"-20 to * 55"C, iimiied by display.

-40 to 4600C.

Standard Items

Optional Items

Shipping Weight

Console with lid and set of rechargeable batteries, RS-232C cable and adapter, 2 copies of manual, battery charger.

Muitidipole Potential Cables. Data Mem ory Expansion Blocks, Crystal Clock, SOFT II Programs, Printer, Cassette Tape Recorder, Disk Drive or Modern.

25 kg includes reusable wooden shipping case.

At Scinlrex we are continually working Improve our line of products and beneTi innovations may result in changes to our specifications without prior notice.

222 Snldercrott Road Concord Ontario Canada L4K 1B5

Telephone: (416) 669-2280 Fax: (416) 660-6138

loiclal

Geophysical and Geochemical Instrumentation and Services

l i

TechnicalDescription ofTSQ-MOOWTime ana Frequency DomainIP and Resistivity Transmitter

l

l

l

l

l

l

TSQ-3 transmitter with portable motor generator unit

222 Snidercroft Road Concord Ontario Canada L4K 1B5

Telephone: (416) 669-2280 Telex: 06-964570 FAX: (416)669-5132 Cable: Geoscint Toronto

Geophysical and Geochemical Instrumentation and Services

Transmitter Console

Output Power

Output Voltages

Output Current

Output Current Stability

Digital Display"

Absolute Accuracy

Current Reading Resolution

Frequency Domain Waveform

Frequency Domain Frequencies

Time Domain Cycle Timing

Time Domain Polarity Change

Time Domain Pulse Durations

Period Time Stability

Efficiency

Operating Temperature Range

Overload Projection

Underload Protection

Thermal Protection

Dimensions

Weight

Power Source

Type

Motor

Alternator

Output Power

Dimensions

Weight

To tat System

Shipping Weight

3000 VA maximum

300,400, 500, 600, 750, 900, 1050,1200. 1350 and 1500 volti, switch selectable

10 amperes maximum

Automatically controlled to within ±0.1 "/o for up to SO'/o external load variation or up to ilOVo Input voltage variation

Light emitting diodes permit display up to 1999 with variable decimal point; switch selectable to read input voltage, output current, external circuit resistance. Dual current range, switch selectable

± 3Vo of full range

10 m A on coarse range (0-10A) 1 mA on fine range (0-2A)

Square wave, continuous with approximately BVc off time at polarity change

Standard: 0.033,0.1,0.3,1.0 and 3.0 Hz, switch selectableOptional: any number of frequencies in range O to 5 Hz.

l:l:t:t,on:oll:on:ofl;automallc

each 21; automatic

Standard: t - 1, 2,4, 8, 16 or 32 seconds Optional: any other timings

Crystai controlled to better than .or/o. An optional high stability clock provides stabiliza tion to better than 1 ppm over -20/ * 50" C.

.76

-30" C to 4 500 C

~Aulomaiic shuT-off at 3300 VA~

Automatic shut-off at current below 100 m A

Automatic shut-off at Internal temperature of t 85" C

350 mm x 530 mm x 320 mm

25.0 kg.

Motor flexibly coupled to alternator and Installed on a frame with carrying handles.

Briggs and Stratton, four stroke, 8 H.P.

Permanent magnet type, 800 Hz, three phase 230 V AC.

3500 VA maximum

520 mm x 715 mm x 560 mm

72.5 kg.

150 kg includes transmitter console, motor generator, connecting cables and re-usable wooden crates.

1111111

1 1l111111111

s ra)

b)

c)

d)

e)

f)

g)

h)

i)

j)

k)

D

m)

m 7.5

ECiriCATlONS

Power:

Output:

C u r r e n t regulator:

Output frequency(selectable onfront panel):

Frequency accuracy:

Output duty cycle- defined ast . /(t -f- t ) :ON ON OFF

Output currentme ter:

Ground resistancemeter:

Input voltagemeter:

Dummy load:

Temperature range:

Size:f

Weight :

,

'

HUUTEC

96-144 V line to neutral, 3 phase, 400 Hz (from liuntec generator set), 7500W

Voltage: 100-3200V de in 10 steps Current: 16A maximum on low ranges

<.l% current change for 10X changein load resistanceSettling time to IX approx. 15 msec.

1/16 Hz to l Hz (time domain andcomplex resistivity)1/16 liz to 4 Hz (frequency domain)

so ppm, -30 0 C to 60 DC

'i to 15/16 in Increments of 1/16 (time domain)15/16 (complex resistivity) 3/4 (frequency domain)

Two ranges - O-IOA, 0-20A

Two ranges - 0-10K ohms, 0-100K ohms

O-15.0V

Two levels: 2000W, 6000K

-34 0 C to 50 D C

53 x 1*3 x 43cm (21 x 17 x 17 ins)

50 kg (110 IBs.) -

lIP Transmitter 7500 Section l June 1980

DOCUMENT No.

,//.y//^ /.Report of Work

Mining Act (Geophysical, Geological and Geochemical S li'aEissweMa'a.'i'asee BEARDMORE AREA 900Mining l...

Address

Suvey Cc."*[-,;iny

t'jame and Address of Author (of Geo-Technical Report)

l IUI.IUIKI}' vt mva

. . . ^Mftt.^ .^^ Prospector's Licence No.

O .lophono No.

Date ot Survey (from 4 to)

Credits Requested per Each C'aim in Columns at right Mining Claims Traversed (List in numerical sequence)ay l Mo l Vr O.i? | Mo |

Special Provisions

For first si ve (

Fnter 4C d 3-, s (This includes line cull. r g)

Fo r each ;:i]'V onai survey: JSiriO. the : irr:t: rpci

Enter ?C 2ays (!ot eacfi)

Man Days

Complete uêrso side and enter totali-:) here

Airborne Oedits

Note: S[ '.oa' provisions f -.nits oo not ar; I-, to Airborne

Geophysical

- E-ieclrontacnetic

- Magnetometer

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magne'ometer

- Other ; , P.

Geological

Geochemical

Electromaonelic

Magnetometer

Other

Total miles flown over claim(s).

Days per Claim

Days per Claim

to! *JQ .

Days per Claim

)ato [ Recorded Holder or Agent (Signature)

M^^kG/^D l.^J/.^^/J'ertificaticn Ventying ReprjrJ^)f)Work

Mining Claim

Prefix

T6

— --....

..........

Number

5/97S5L

Mining Claim

Piefix

-S^Strr- 1^

5^1Cj \ii**i s* f ~ ' ^^f

f-JBlÔiV- -4*

./O.73/J5S -~- /c^9?V?9 '/Oo?no3-'-

1 1 t * *^* ^ *\ nr

III/ ^ "1 9

-f/JH T^/Vl l(S-\^ *S.±^*S~7-

Nunibcr

0"

:-

~--

t

Mining Claim

Prefix

i -J

3 j

^3 C/^

H^ ••'

ro

Total nunibcr of mining claims covered by this report of work.

Number

pi--.:CP O-5------

l

^trety •c*'-";*, thai i have a personal find intimate knowlodcjo of the Jacls set forth m Ihis Report of Work, having pcrlormod the work or witnessed sanio during and/or .tic: its cot' p'L'f'OM and annexed report is foe

d '•dJ'-.'fjS ot Person Certifying

-:K

Assessment Work Breakdown

1.1,in Days an: based on eight (8) hour Technical 01 Line-cutting days. Technical days include work performed by i••jnsultants, diattsmen, etc..

Technical Days Linn -cutting Credits Days

m7cchnic.il Days Une-cuUinQ

Credits Days

| 7 | ^ | | 4 —

No. of Total Credits Claims

-f- 1 ^

Days per Claim

To-'tiriciit O.'iys Lint? cutliny No. of [};iys porC.rodits Days lota! OeJits Claims Ooirn

X 7 -LJZJ* s -f- ^

DOCUMENT No.

O.'ltiJMO

InMruclion

X// AMining Act

Report of Work /7/AV /v *- Â *''' *(Geophysical, Geological and Geochemical Surveys)

PCX l oO ; ',

t MMTfinE fc&e.^ ;- Refer lo Section 77. the Mining Act for ;i:,so"..smont work requirement;

and maximum credits allowed per survey type- if number ot mining claims traversed exceeds spare on this lorm,

attach a list.- Technical Reports and maps in duplicate should be submitted lo

Mining Lands Section. Mineral Development and Lands Branch:

Mining Division Township or Area

Aricfrev.

P-O- Box JL3?Survey C (•'•iruiny

Name a*.:) Address of Author {of Geo-Technica! Repori)

-.k-L/a

2. 13286•. ^ iJI^tM Ct 5,.... J ALG...

t/? iPfospeclor's L icence No

T --5/6-9Telephone No.

Dale ol Survey (Irom S to)A? 09 fe9 \ n O9 89Day l Mo j Yr. D.iy j Mo l Yr

Credits riequested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)

l hi-Trtiy ' ?rtity iha! i h:nje a personal and intimate knowledge of the (acls se! forth in ihis Report o) Work, having po'formcd tho v;ork or witnessed same durtruj and/or1 f its t fiiîotion tind annexed report is true.:.v

(l

; tin : AfJdrivss of Person Certifying

A ' /-f DA vt o

For Office Use Only

c.

a i. MOCutUC'd

Oee

Mining RecorderderR [; C 1-; ; V L L/

..\:-i- O:- 1990

MINING IANOS SECTION

Instructions- f'loa&o lypo or print

i* 3 o

Mining ActReport of Work(Geophysical, Geological and Geochemical Surveys)

and n- K niirt

a ttac f- lechr

o S(vl on 77, the M'Miruj Acl for .'isscs'.inont work roijurromonl .credits allowed per survey lypo.

b(-r ol mining claims traversed exceeds space on Ihis form, a l.sl, Gill Reports and maps in duplicate should lw submitted lo

Mining Lands Section, Mineral Development and Lands Branch:

Mining Division Township or Area

Prospector's Licence No.

Addres

..Survey Conipany

.. .- ......-Name .i-id Address of Author (ol Goo-Technical Report)

Telephone No.

Date ol Survey (from * to)

__ . .. ———Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions

For l:r? : survey:

Ento- '10 d.'4/s ("fnis includes lino Jtting)

For ea :-i addd.onal survey: using re iiame grid.

Ente- 20 days (for each)

Man O.1 y s

Compii-T rrvorbO side and entef !- ml(s) hero

Airborne Credits

Note: Special provisions credits do not apply t-"i Airborne

Geophysical

- Electromagnetic

- Magnetometer

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Other

Geological

Geochemical

Electromagnelic

f/agnctomeier

Other

Total miles flown over claim(s).

Days per Claim

--

Days perClaim

—- -— .

Days per Claim

--—-

D ile f Recorded Holder or Agent (Signature)

Conduction Verifying Report o! Work

Mining Cla m

Prefix

...ra..

,. — -

— -...,.

.--.---

------

Number

./.C67..VBO.

.j&f&y&Liti&^&aloBJjoQ-^B^.' .teB&QQ.-'/(96"-?v^2- ..jD&i-yQ^.

i i i S *^"^ J

,f^l^tt \z/ *Ô^C^ ^

li Aki -3 J Ci

Mining Claim

Pielix

-.-— -

~""\

4

Number

^

.---— --- ---.. -

X..—?-,*/ * x i

Tolamini by tt

Mining ClaimPfCllX

-

12

number of ng claims covered iis reporl ol work.

Number

- -- ------"

8*

^^

1 htwl'y certify that 1 have a persona! and intimate knowledge ol Ihe (acts set lorth in this Report ol Work, having performed the work or Viit/HJSsed same during and/or alu-r it co;'tf.'V'!ior anil annexed repor: is true. V* ;

Nan. t ;T! Ad-.irey; ot Person Certifying — ,

. . . . i::"} -

For Office Use Only

TOM: Jays , Dale RoLC/rded C; no--.ri1.-n i

: fxvo Approved as Recorded

Tetophone No.

Min.ng Recorder

I'rovincia M.uiagor, Mining l ands

Date

Fleceivod Stamp

Certified By (Signature)

13 (n w o

rv i-*

ntario

Ministry ofNorthern Developmentand Mines

Ministere duDeveloppement du Nord et des Mines

July 12, 1990

Mining Lands Section 880 Bay Street, 3rd Floor Toronto, Ontario MSS 1Z8

Tel: (416) 965-4888

Your File: W9004.141 Our File: 2.13286

Mining RecorderMinistry of Northern Development b Mines435 James Street SouthP. O. Box 5000P7C 5G6

Dear Sir/Madam:

Re: Notice of Intent dated June 6, 1990 for Geophysical (Electromagnetic) Survey submitted on Mining Claims : TB 519491 et al in Simmers, Beardmore and Mary Jane Lake Area.

The assessment work credits, as listed with the above mentioned Notice of Intent, 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,

W. R. CowanProvincial Manager, Mining LandsMines S Minerals DivisionK)S:zm

Encl:

cc: Mr. W. D. TiernanMining St Lands Coirmissioner Toronto, Ontario

Golden Dragon Resources Ltd, Timmins, Ontario

Resident Geologist Thunder Bay, Ontario

isvy o( hCi'n D Mines

"Tcclinicnl Assessment

Work CreditsOntario June 6.

'"2.13286

GOLDEN DRAGON RESOURCES LTDTownihlp

SUMMERS, BEARDMORE AND MARY JANE LAKE

Assessment days credit p*rGeophysical 15.9

nlofl Ctlimi Art*n*d

Magnetometer.

Radiorrveiric._

Induced polarization.

Other.————————-

-days

-day*

-cSays

. days

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

Geological .———-—.——.————--—.——— days

————————-——djyj

Airborne Q

Ground (y

f.laa days Q

Spceia( proviiiori fTV

(3 Credit! have be*n reduced because of partial coverage ol c'aimj.

FI Credits have been reduced because o( correction! to work dates and (ioures of applicant.

TB 519491 519782

* 810007 to 010 incl.* 814301 to 306 incl,* 815573 - 74* 815613 - 14

939667 to 669 incl. .1034165 to 167 incl.10360071073132 to 135 incl.-1073137, 1073139, 10731411073150 to 153 incl.1073155 to 159 incl.1073162, 107317610837481087478, 1087483, 10874901087492-931087495-96

* 1116271 to 273 incl.* 1126548 to 550 incl.* 1126556, 1126560

SpecJal credits under section 77 (16) for the followin} mining claims

* Credits of 15.9 days electromagnetic approved through this survey but

the maximum credits for geophysics have been reached (See original worksheet)

have been ailowid for tiie following mining damn

JAlullicitnl Kc''n.C4l dlK fi'fd

TB 107316^, 1073173 1087480 to 482 incl,

1087484

Ifxc l^',i\inf ntcolOf mf y ccducr tht a&Ovt C<<<Jll1 if nrciiu'v in O(dc( H.il If,, loi.l nun^(xr of •dP'Ottf inoirtxnt d"V1 IfCOfdrd 00 C4*:fi Claim <^0<l

r net t a l li f mj.imum •Ho'vrd tl toiio*vi: Ctoo'-viicii -00; GfOiojooi. 40; CroctKiKiul - *0; Stciion JHtSI - CO.

Ontario


Ministere duDeVeloppement du Nord et des Mines

August 01, 1990

Mining Lands Section 880 Bay Street, 3rd Floor Toronto, Ontario MSS 1Z8

Tel: (416) 965-4888

Your File: Our File:

W9004.141 2.13286

Mining RecorderMinistry of Northern Development St Mines435 James Street SouthP. O. Box 5000THUNDER BAY, OntarioP7C 5G6

Dear Sir/Madam:

Re: Notice of Intent dated June 6, 1990 for Geophysical (Electromagnetic) Survey submitted on Mining Claims: TB 519491 et al in Summers, Beardmore and Mary Jane Lake Area.

The assessment work credits, as listed with the above mentioned Notice of Intent, have been approved as of July 12, 1990. On the original data statement, claim TB 1087479 was inadvertently left off. This data statement has now been amended.

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

Yours sincerely,

W. R. CowanProvincial Manager, Mining LandsMines St Minerals DivisionnsLuS:zm Encl:

cc: Mr. W. D. TiernanMining S Lands Commissioner Toronto, Ontario

Golden Dragon Resources Ltd. TIMMINS, Ontario

Resident Geologist THUNDER BAY, Ontario

AMENDE D

Northern Development Mines

Technical Assessment Work Credits

Ontario June 6, 1990' ' ' "

2.13286'CflH'l IffitorTol'

W9004.141

Recorded Holder

GOLDEN DRAGON RESOURCES LTDTownship or

SUMMERS, BEARDMORE AND MARY JANE LAKE

Type of tufvey *nd number of Assessment days credit par claim Mining Claims

Geophysical

Electromagnetic . 15.9

Magnetometer.

Radiometric __

Induced polarization.

Other-———-————

-days

-days

-days

-days

- days

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

Geological ____________________days

Geochemical.————————-—-————^—days

Man days | |

Special provision g]

Airborne |~]

Ground fv)

Credits have been reduced because of partial coverage of claims.

Credits have been reduced because of corrections to work dates and figure* of applicant.

TB 519491 519782

* 810007 to 010 incl.* 814301 to 306 incl.* 815573 - 74* 815613 -r 14

939667 to 669 incl. .1034165 to 167 incl.10360071073132 to 135 incl.-1073137, 1073139, 10731411073150 to 153 incl.1073155 to 159 incl.1073162, 107317610837481087478, 1087483, 10874901087492-931087495-96

* 1116271 to 273 incl.* 1126548 to 550 incl.* 1126556, 1126560

1087479

Special credits under section 77 (1C) for the following^nining daims

* Credits of 15.9 days electromagnetic approved through this survey but

the maximum credits for geophysics have been reached (See original worksheet)

No credits have been allowed for the following mining claimsi————————————————————————————————————————not sufficiently covered by the iurvcy

TB 1073164, 10731731087480 to 482 incl. 1087484

injuflicitni technical dm filed

Tl.c Mining ncco.dc'f mj v (fducc U'c AOow c.ctliu H nttVHUv in O'dei Hul H.c lol.il nuo,t,c ( o( sop.o^-cO jiici.mrot Oay. rrco.dcc] on tKh claim docs ..o, C'Cccxl Hie minimum .mowed as 'ollo.vi: Gcoo'u-1't.ii - 00: Grologoc.'l - 10; Gcoclicni.col -10; Srci/on 77(191 .CO


AssessmentWorkBreakdown

1. Type of Survey ..t

2. Township or Area ....

3. Numbers of Mining Claims Traversed by

4. Number of Miles of Line Cut ...

5. Number of Stations Established

C 6. Make and type of Instrument Used .

7. Scale Constant or Sensitivity ....

8. Frequency Used and Power Output ,.

Flown

EH

d 1 .4 - - . \fi. . j.m. . - - . .

9. Summary of Assessment Credits (details on reverse side)

Total 8 hour Technical Days (Include Consultants, Draughting etc.)

Total 8 hour Line-Cutting Days ...................

Calculation

^'i CW-- v 7 ^ 14'^T S"fV- 4- --f-J 7 , i l x ' J l , ) - O \^s ~

l "

Technical Line-cutting Number of claims

Assessment credits per claim

The dates listed on this form represent working time spent entirely within the limitsof the above listed claims [y^ CheckIf otherwise, please explain .......................................................,.

Dated: ... Signed:

Note: (A) * Complete only if applicable.(B) Complete list of names, addresses and dates on reverse side.(C) Submit separate breakdown for each type of survey.(D) Submit in duplicate.

827 (85/12)


AssessmentWorkBreakdown

Ontari

1. Type of Survey ...

2. Township or Area ..

3. Numbers of Mining Claims Traversed by Survey .

v .r .ra2 II

4. Number of Miles of Line Cut ...

*5. Number of Stations Established

*6. Make and type bf Instrument Used ..

*7. Scale Constant or Sensitivity .

*8. Frequency Used and Power Output

Flown

- -l

9. Summary of Assessment Credits (details on reverse side)

Total 8 hour Technical Days (Include Consultants, Draughting etc.)

Total 8 hour Line-Cutting Days ...................

Calculation

.Q4 x 7Technical Line-'cutting

I45-& -rNumber of claims

Assessment credits per claim

The dates listed on this form represent working time spent entirely within the limitsof the above listed claims j \X CheckIf otherwise, please explain .........................................................

Dated: Signed: ..'f-

Note: (A) * Complete only if applicable.(B) Complete list of names, addresses and dates on reverse side.(C) Submit separate breakdown for each type of survey.(D) Submit in duplicate.

827 (85/12)

Details of Assessment Work Breakdown

FIELD WORK

Type of Work Name ft Address Dates WorkedNumber of 8 hour days

.4..

.L'

CONSULTANTS

Name S Address Dates Worked (specify in field or office)Number of 8 hour days

Name 6 Address Type of Work

DRAUGHTSMAN, TYPING, OTHERS (specify)

Dates WorkedNumber of 8 hour days

LINE-CUTTING

Name Address

TOTAL 8 HOUR TECHNICAL DAYS *9 V

Dates WorkedNumber of 8 hour days

TOTAL 8 HOUR LINE-CUTTING DAYS

ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

136 Cedar St. So.P.O. Box 1637Timmins, OntarioP4N 7W8Telephone (705) 264-4246Fax:705-267-6110

f]''

,A - O, c c j

RECEIVED

MINING IANDS SECTION

f /YO

Suite 301121 Richmond St. W.Toronto, OntarioM5H2K1Telephone: (416) 861-9316Fax:416-861-1367

F!* A/IEXPLORATION

services ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

136 Cedar St. So.P.O. Box 1637Timmins, OntarioP4N 7W8Telephone (705) 264-4246Fax:705-267-6110

May l, 1990

Suite 301121 Richmond St. W.Toronto, OntarioM5H2K1Telephone: (416) 861-9316Fax:416-861-1367

RECEIVEDMAYO, 1990

MftlNG LANDS SECTIONMinistry of Northern Development and Mil,Mining Lands SectionMines and Minerals Division880 Hay Street3rd FloorToronto, OntarioM5S m

Dear Sir/Madarn:

Please find enclosed Reports, Maps, and a copy of the Report of Work for ground

geophysics (E.M, k I.P) performed on claims in Summers Twp. (Thunder Bay

Mining Division).

Kindly acknowledge the accompanying copies of the Reports of Work "Received"

and return at your earliest convenience.

Thank you for your time and consideration.

Sincerely,

Cliff David

RECEIVEDMAY

MINING SECTION

D)

G

G

rn ru TO O t CD

(A?)

(^

)

^

CTH

^

O

i-

;n 1-

< n f ' -i M ci ^

-n p- rr- -J m -j

o

~O

0

li U

fO

S "

L?0

^

o

^ -

c-.-— ^,

"

"O

i

o :o

" L-

Y^

Z*1

•C

C-

"*

P '

2 !Tl "J Q.

i.

O.

O PO

O

-T) o" O i'l U

] T! H J -i tri

t J ~ —J o o o ID Q.

OT

O O .1 tt) r' Q O)

r" p O) u? •J to y r" o j. re r:) o CD CO o •o -.J Q' a' i * • fi

•n m ~ u"1

O f\i t- O ~— f~ ri •T)

l ""

C

r? c ^ 01 o -A l" -* TJ

U -T J^* o o r -j t--

O

O

"D O O O

lvl (.J

ISl

T)

LI

TJ

li

o o,

o

o rv

:) r ,i

It r1

MA

RY

JA

NE

LA

KE

G

-80

LEO

PA

RD

LA

KE

G

-68

d -•H --1

CD

™

o

in -

m

C) "•

w

—l

cj.i

0 Z O o t") x

(/i ~l m

m

3 i

z

w.

.l

AJ

Q

r r-

H

0

f

y-

rn

a

z rn

1-

^

,-"

^

^

^

CI

m

: :

?-

H

TJ^

'-'

. "i

,-

\"

'

™

Im

^

";

-

-- l3

m

-

-- v

"

0'

--

v

— -*

i

1 i

T

* l/)

*"

- T

r"

^^0

5-C

s^v,

^v,

-) -

D

-i .

^ ^

- - -

c n

•" j

'-1

^

Tl

-y,

7"

;j

j-,

J^

- r

U

,-,

^

t-

-

-

n O

. -

'"

';

n

'-'

o

o

^

i- ^

101 V

^

[ o

Q

^

m

rn L1

o

o

.Ci

—

^-(

7iJ

:(?;3

3rn

rn

^

1 ^

^

T

r"

^

o

^

P0

;m^

' ;

i ,,\

J

-; i-

o

r:

^1 *

!

' u

ui

' '

',

--

;a i

; ; i ?

: '-^-

^w

- '

' .

L)

'" f

J;,

-v '1

''

T

! ^

Of

- :

i .

H -

' z

TI i

! '-'J

,

' ^•^

j

' r

' !

m

7- u

' i

'

Jo,

',

^ 1

1 ^-

i (r

, .

l :

' ,

' , 3

;j?

'

' '

^^

15 ®

^ ri

^ c

j LI m

c o

* .

^

o rr* 7JT

"O*J

O O ^ o -Tl

o •33 o rSj" I?

f*

•p?* r*^

00

T:

o

-A l/

1 0 ' --,

1 "!

! ai

;-i. | ^ 1

rni |

Z

* ! r

i i•r

; T

ill.

f*V ff'eUrvV^LOODiNG fciGHTS o :n take" Nipigon "W r - contour elcv. 855* to H.E.P.C. "-- O.C.doted 25Jh April (930. File'12198.

"" Also reserve SS'frorftesS'coMour lo H.E.PC.

K*y Me? Fcf V*ai*r Ctorra Wi'teft* i'-cr* K F fer MC

•p—-^*1 '

.^ ' - j^_î- j.*- -

*—i --;.- f ~—-

42EI2SWM33 2.13286 BEARDMORE AREA210 i:

Aiii-ar-.-rsKt^-.-.-^tteiHiiiîiiî'-- si Tqsaa^^M

POPLAR POINT G-II 8

r7 k e

1,3134^ 173401 '075116 , 107341**

'O447O7 . KH4706 IO44706 IOM7OT

'071387 0733*4 '

83=15'

PIJITAWABIK BAY B KILKENNY TWR G-II lB 6 l

-; INFORMATION THAT ÂPPEARS. ON THIS MAP 'HAS-BEEN, "COMPILED

; FPOM.VARIOUS SOURCES,-' AND;. ACCURACY is: NOTy GUARANTEED. THOSE

- WISHING TO STAKE MIN ING CLAIMS SHOULD CON-

' SULT WITH THE MINING RECORDER, -MJNISTRY Or

"" NORTHEinN DF.VEIOP MCN7 ANOMINCS. TOMAD DJTtONAL iN ON T Mf: ITIATUS Of LANDS SHOWN

-:orl' i.ocolioi?. tNUl C! i-nn K"

LEGE N O

HIGHWAY AND ROUTE No.

OThUH ROADS .

T R A! LS

SLJRVTYEO LINES!TOV^JSM.PS, BASE LINES, ETC UOTS,MINING CtAiMS, PARCELS,ETC

UNSURVEYEO LIMES:LOT LtNfS PARCEL BOUNDARY M'N'.MG CLAIMS ETC.

ft/VLV.AY AND RIGHT OF WAY

UTILITY LiNES

KON-FEKENN1AL STREAM

FLOODING OR FLOODING RIGHTS

S'JSDIVtSJOW

OR:Gi*jat. SHORELINE

MARSH OR.MUSKEG ^ -

MINES

DISPOSITION OF CROWN LAN

TYPE OF DOCUMENT

s .PATENT, SpRfACE 6 MINING RIGHTS

•; - . ' SURFACEJRIGHTS

RIGHTS

' . LEASE. ÛRFCe 'ft WiNING RIGHTS.

" ,. SURFACE RIGHTS " MINING RIGHTS ONLY...,..,.,. .

LICENCEO'F OCCUPATION,.. M. .....^,..CROWN 'LAND SALE-- -i— .u....:.^ __

SCALE 1 l INCH "40

AFEA

M.W.R. Ai)RSIKiSTRATIVE DISTRICT

NIPIGONRISING DIVISiD

THUNDER BAYLAfiD TiTUS/ REGISTRV DIVISION

THUNDER BAY

'-

*,. Ministry of Land--Natural " Management

Resources BranchOntario f

Cite 7/FEB /I96I

d

l It

LU

LO

( 1

D

ODCO

LO Z

D

v

O

5

aOCi/)

l - -s f 2 5X

O

h-

irt -5LO

O.

LO ^

UJ CO

O?

LO

Z-1

5: Z

C I

5

^ l

LOLU

S

(~>

C

C

>cc.LOzD

Cz::: ? 2 i

ot- itrD

Z

tr

Lt

^t

'"l i/"

'

^

g

Q 5

DC D

-, -

^

CS— '

—l

Z

LJ,

CC LO

3

LULO

O.'

ttSO

D

Z

Gt/1 a:

— Q:

00

O5oocCJ

O)

oCL

c/)

i) o H u a

LOh-I-J

y

O

^

-J tt

-J

o z

"; z

O

L)

DC

Q;-

DLU

CSL U

,-

O

W M

CJZQ

O?

Ou

^

D

KLOUJo:

Q

Z(j

z o

~ 7 wo'

Oy

,

Z

Q

1 = 5a.

oQ.

XOh-o: Q

Me C

OM

BE

R

TO

WN

SH

IP66

OUJ

LJ

a: o

5ocr<LU CD

Q

W

W

IOT313Z-

'. 44.0 1-22.Q

HUf'

-5.

0

-28.

0 4z

4.0

y\

-31.0416.0

^ l

-25.0

4 17.C

\ -3

1.0-

lOjO

-27.

0 j-6.O

l '

\ -25.b4-6.0

^-.

i '

/iWff

Wfc

** a

gj^

* i ii

i ^ L

.2if^p

Mlilii

III!

I Ln

M M

s^s^rA

s;^

^s

î

VLF

PROFILES

— IN

PHAS

E

— — — — QU

ADRA

TURE

Profile

Scale:

Irm

^ 207.

fi.O -11.0

y9.o

|-13

.0-\3.c|-2l.O

\

f -5

.^-2

3.0

TRUE C

ROSS

-OVE

R:IP

Q\

17.0t-29.0\

TX S

TATION:

SEATTLE, 2

4.8

kHz

INSTRUMENT

: Geonlcs EM-16

\ -33.0 M6.0

v j

\ -2

4.04

14.0

-

VLF

CONDUCTORS

STRONG

Q

MODE

RATE

O

WEAK

*^*

SIGN

IFIC

ANT

ANOM

ALY

AXIS OF CO

NDUC

TOR

SCAL

E l

: 2

500

2,1

32

86 RO

BERT S. MIDDLETON

EXPLORATION

SERV

ICES

IN

C.a 15613

DENI

SON

MINE

S LTD.

BEARDMORE

PROJECT

VLF-

EM SU

RVEY

Sum

mer

s T

wp

.,

On

t.

Dat

e*

Sep1

em

ber

8942E12SWW33 3.13286 BEARDMORE AREA

Operators' Ba

ll/H

a l pag

e

} 17.0-11.0

VLF PROFILES

- - — — - QUADRATURE

Profile Scile: lcm ^ 107.-44.0+1.0

l-16.0-J.O TRUE CROSS-OVER:

30 - 15 \

l -30---15

Tx STATION: SEATTLE, 24.8 kHzINSTRUMENT : GeonJcs EM-16

VLF CONDUCTORS

STRONG

MODERATE

O WEAK

SIGNIFICANT ANOMALY

AXIS OF CONDUCTOR

SCALE l : 2 500

7Jw**dx*—-~


DENISON MINES LTD.

BEARDMORE PROJECT VLF-EM SURVEYSummers Twp., Qnt, Fig.oc42E12SW8833 2.13286 BEARDMORE AREA

BLOCK INDEX Date: September 89

Operator: Ball/Malpage Job *: H-347

r-o

OD

C

D

CD

1200

N

1100

N

^.^

1000

N

. ^.

900

N

CD

C

D

-16

T-M

!-Ill -1

3*

-20

l

-25

{-2

54-2

2 j

-1/4

-10

l

OT -O -l -

-s T

-M -9-1

-17

-27

4-1

9 +

74

27 j

30 i

23 l

13 t O -M -61

-Z t i

6t

n t

10 1

.120

0 N

— 1

100

N

__

10

00

N

..900

N

800

N

700

GOO

N.

50C

400

300

200

N_

_.

100

C ..

en CD

CO

C

D

CD

C

D

CD

CD

en CJ

CD

CD

C

D

CD

CD

CD m

LO

C

D

CD

rn

CD

C

D

CD

C J

CD

" J

r-o

CD

C

D

ro

OJ

C

J

CD

CD

r r-o

en CJ

CD

rn

CD CD

r-O

CD CD CD

......

800

—^7

00

H

.600

__

50

0

N

.400

N

..300

.200

V 1

.G

CONI

OUR

INTE

RVAL

: i o

/:

TX S

TATIO

N:

SEAT

TLF.

24.8

VH

INST

RUME

NT

: Geooics

EM-16

VLF

COND

UCTO

RS

STR

ON

G

O

V1

- S

IGN

IFIC

AN

T

ANO

MAL

Y

—

AX

IS

JF

CO

ND

UC

TOR

AR

EA250

-BL

OCK

IND

EX

SCAL

E l

: 2

500

50

|*Û

aii^

lOO

150

200

2.1

3286

T;t!

ROBE

RT

S.

MID

DLE

TON

EX

PLO

RAT

ION

SE

RVI

CES

IN

C.

DEN

ISO

N

MIN

ES

LTD

.

BEAR

DMO

RE

PRO

JECT

ER

ASER

FI

LTE

R

VLF-

EMS

um

me

rs

Tw

p.,

Q

r\t.

Fjg.

4a

Da

te:

Sep

tem

ber

89

Opera

tors

: B

aJJ

/Malp

age

.T.S

.:

Job

*:

M-3

47

700

N __

600

N

500

N...

..

400

N

300

N

200

100 N^.

100

200

S

300

S

un CD

CD

f J

400

S

500

S

600

S

700

S

800

S

r-o

r-o

CDCD

CD

CD

CD

CD

CD

CDCD

CO

CD

CD

CD

CD

en

CD CDen CD

CD

CD

CD

UJ

CD

CD

IXJ

CD

CD

CD

CD

CD

CD

CD

CO

CD

CD

CD

CD

CD

CD

CD

CO

CD

CD

en CD

CD

CD

CD

CO

CD

CD

CJ

CD

CD

CD

BLOC

K IN

DEX

t,t;

,

M Vlh

IN St'

r .

.'4.3

on .

, .

f M

2- 1

328

x

* *

:s\

^ ' K

4 *

* ^

\

fc*

.f\^

**.

: \

2.,3286 BEARDMORE AREA

270

- .

^ w Fi

g.4b

j .'

A ,'.'

^ *

," i

? ?

. ,-

J j

- M

*

J --

; ^ -'

800 S.—

900 S.

1000 5

a loo

1200 S. .

1300 S.....

MOO S.

1500 S.

1700

J 800 S

1900 5.

CDCD

enCDCD

CO CD O

CDCD

CD CD

CD CD CD

CO CD CO

r J

OD CD CD

CD CD

CD CD CD

r~

en CD CD

CD CD

CD CD

CJ CD

rUJ CD CD

.800 S

.900 S

.1000 S

.1100 S

.1200 S

..1300 S

-1400 S

— 1500 S

.1600 5

—.-1700 S

-.1800 5

.1900 S

CONTOUR INTERVAL;

TX STATION: SEATTLE. 24.8 kHzINSTRUMENT : G.onlcs EM-16

VLF CONDUCTORS

9 STRONG

O MODERATE

O WEAK

Vi - SIGNIFICANT ANOMALY

CD CD

— AXIS OF CONDUCTOR

42E12SW0033 2.13286 BEARDMORE AREA S80

' *-* ' "*-

^ :Q *~ ^', ^

Wd^5^ r -^ BLOCK INDEX

SCALE l : 2 5001IJO

2. 132S6ROBERT S. MIDDLETON

EXPLORATION SERVICES INC.For DENISON MINES LTD.Till

BEARDMORE PROJECT FRASER FILTER VLF-EM

Summers Twp., Ont. Fig. 4c

Dale: SepteiLer 69

Operators' BUl/Malpage

.T.S,:Job i: H-347.

LE

GE

ND

6a

gabb

ro

6b

pyro

xene

-por

phyr

y

6c

dior

ite

6d

feld

spar

po

rphy

ry

Abb

revi

atio

ns

scr

seric

ite

qtz

quar

tz

a.v

quar

tz

vein

si

fic

silic

ified

ca

rb

carb

onat

e cc

ca

lcite

an

k an

kerit

e ch

i ct

rtor

fte

feld

fe

ldsp

ar

mag

m

agnetit

e"

py

pyrit

epo

p

yrrh

otit

e

cpy

chalc

opyr

ite

Fe

iron

ws

wea

ther

ed

surf

ace

fs

fres

h su

rfac

e m

ag

mag

netic

vnlts

ve

inle

ts

lam

la

min

ated

In

lin

eatio

n cl

ev

ctey

gge

sen

schi

stos

ity

amy

amyd

oita

i

*olla

tion

with

di

p

bedd

ing

with

di

p

shea

ring

TX S

TATION:

SEATTLE, 2

4.8

INST

RUM

ENT

: G

eonl

c*

EM

-16

SE

DIM

EN

TAR

Y

RO

CK

S

4a

arg

illite

wac

ke

(silt

ston

e,

sand

ston

e)

4c

cong

lom

erat

e

VLF

COND

UCTO

RS

TRON

G

4e

iron

form

atio

n

grap

hitic

ro

ck

- S

IGN

IFIC

AN

T AN

OM

ALY

— A

XIS

OF C

ONDU

CTOR

VOLC

ANIC

ROC

KS

.a

-nas

sive

flo

w

or

undi

ffere

ntia

ted

3b

now

tor

etcr

a

3c

porp

hyrit

ic

flow

*u

ff,cr

ysta

l tu

ff

3e

lapi

lli

tuff

swam

p

bush

ro

ad

strip

ped

area

NTE

RM

ED

IATE

V

OLC

AN

IC

RO

CK

Sdi

amon

d dr

ill

hole

sam

ple

roca

lTbn

~Tna

r"nu

mbe

r2a

m

assi

ve

flow

or

jp

diff

ere

nt-

ate

d

t pi

llow

flo

w

2c

pillo

w

or f

m*

brec

cia

20

amyg

dalo

idal

2e

porp

hyrit

icZ

f *u

ff,

crys

tal

tuff

2g

'api

lii

tuff

foun

d cl

aim

pos

t an

d ttn

es

assu

med

MA

DC

V

OLC

AN

IC

RO

CK

S

la

mas

sive

pill

ow

or

undi

ffere

ntia

ted

"4 b

pUJe

w*d

pillo

w or

flo

w

brec

cia

Id

amyg

dalo

idal

e va

riolit

icIf

aorp

hyntic

g oy

rocl

astic

4b."-

..,.;'*

tu

n -tr

co

rfc.

i—i

str

.'o,

A ^

-'t

od

carb

s*

' ch

lor

oy

-nod

ro

t

, 'n

od

chlo

r si

ljc O

'a st

r m

od c

arb,

silic

'dv-

i 7.

py

:Vw g^

Gr'e\

MO

KO

AN

S

HO

WIN

G

D.

eh:

Qtz

ca

rb

STS

- -

y^—

D

ri; o

ws

sire

cnd

t- st

retc

hD

lllO

WS

•*"

spc,

t)ch

,ppi

ND

EX

O

F M

AP

S

'-fcE

TS

2.13

28K

fcVI

SIO

NS

RO

BE

RT

S. M

IDD

LET

ON

E

XP

LOR

ATI

ON

SE

RV

ICE

S

INC

GOLDEN DRAGON RESOURCES LTD

GLEN AUDEN RESOURCES L

TD.

50 me

tres

SJM

ME

RS

TO

WN

SH

IP

PR

OP

ER

TY

Fig.

5a

Sea

e:

25,

Xpn

rove

d:

H

C'ME

ET

ON

E

D

spc

42E

iaS

W00

33 3

.13

88

6

BEAR

DM

OR

E A

RE

A

*',

- '

q * z

st

3

3 c

mod

ch

l O

\

'a st

r *o

i .

: *ik

iy

rnod

ch

l *oi

mod

ca

rt

~hlo

r

LE

GE

ND

^ - a

-ri

oss

d* j

-a

îas

s o

V r-n

i at

z ca

rbTI

QSS

ea

carb

sr

rs

oy

P.

AN

OM

ALI

ES

RE

SIS

TIV

ITY

CO

NT

RA

ST

MO

DE

RA

TE

CO

ND

UC

TOR

) S

HE

AR

a 'T

r fo

l T

ied

carb

, :h

lor

*——

y" ~

fl or

- ca

rt)

mas

s

O st

r fo

l~

"nod

ca

rb,

chlo

r st

ain

-fb

sihc

d

Der

v ca

rb

!*.

p y

Sym

bols

folia

tion

with

dip

bedd

ing

with

dip

shea

ring

D sh

aft

cree

k

swam

p

— —

bu

sh r

oad

strip

ped

area

REV

ISrO

NS

ePO

)a

^

s?(X

^

Abb

revi

atio

ns

scr

seric

ite

Sili

c si

licifi

ed

carb

ca

rbon

ate

cc

calc

ite

anK

anK

ente

ch

l ch

lorit

e fe

id f

elds

par

moQ

in

aQne

îte

py

pynf

eDO

py

rrho

tite

coy

:noi

copy

nte

Fe

ron

ws

wea

ther

ed

surf

ace

*s *

resn

sur

face

mag

Ti

oQne

tlcvn

tts

-/ein

lets

lam

la

min

ated

In

'.nea

tion

ctev

cl

evO

Q*

scr

schi

stos

ityar

ry

amyd

oita

lve

s ve

sicu

lar

pil

pillo

ws

rx STATION: S

EATT

LE,

24.8 k

HzIN

STRU

MENT

t Geonlcs

EH-1

6

VLF

CONDUCTORS

0

STRONG

O

MODE

RATE

O

WEAK

- SI

GNIF

ICAN

T ANOMALY

. — AXI

S OF

CONDUCTOR

OF

MA

P

SH

EE

TS

2.1

32

86

faul

t

diam

ond

drill

hole

A

sam

ple

loca

tion

and

num

ber

l ^—

fo

und

daim

pos

t an

d lin

es

Q—

as

sum

ed c

laim

pos

t

l

RO

BE

RT

S. M

IDD

LETO

N

EX

PLO

RA

TIO

N S

ER

VIC

ES

IN

C.

GO

tDE

N"D

RA

GO

N R

ES

OU

RC

ES

"L T

O:'

GLE

N

AU

DE

N R

ES

OU

RC

ES

LT

D.

SU

MM

ER

S

TO

WN

SH

IP

PR

OP

ER

TY

Fig.

5b

Dat

e:

OCT.

ises

30

0D

raw

n:

A.M.

Sca

le:

i: 25

00A

pr) r

oved

: H.

B.N.

T.S.

:F

ilC

v

M-3

47

spc.ppl ( tjch

\ ,\. o437 : a, carb\\. . - t \ 5436 'a,carb,î

Qtz,' carb' a.corb/

r\/ fa "ôd sire carb, '

str f- e carb, '' sai \>

Q st" sine, - e ro'C t V ^

OWN- OF BEARDMORE

i '046 4^ a graph, 4Q7. cy

a, i!OV. p y

U49- 51 Qtz /n, 1

*gd, ^k IQC magv

blebs of oy, po mask

mod chl l small qt^ bleb's/stg

j r o K e r ^. L'gc, s otey 'ex, mod

jt; carO vnits•nod f e staining•nod chl m

LEGEND

Go gabbro:

6b pyroxene -porphyry

6 c dtort'te6d feldspar porphyry

Abbreviotions

scr sericite qtz quartz qv quartz vein silic silicified carb carbonate cc calcite ank ankerite chl chlorite fftld feldspar mag magnetitepy ;pynte po pyrrhotitecoy chalcopyriteF e ironws weathered surfacefs fresh surface mag magnetic vnits. veinlets .am laminated In lineation clev clevage sch iscnlsTosity amy amydoitai ves vesicular pi! pillows

'ollation with dip

bedding with dip

shearing

TX STATION: SEATTLE, 24.e kHzINSTRUMENT J Btonic* EM-16

VLF CONDUCTORSSEDIMENTARY ROCKS

4o argillite

4b wacke (siltstone, sandstone)

4c conglomerate

STRONG

O MODERATE

O WEAK

SIGNIFICANT ANOMALY

4d chert4e iron formation

i 4f graphitic rock

VOLCANIC ROCKS

. 3o massive tlow or undifferentiated

3b flow breccia3c oorphyTitic flow

AXIS OF CONDUCTOR

stripped area3o *uff, crystal fuff 3e lapilli tuff fault

diamond drill hoi*

sample location and number

found claim post and Pnes

NTERMEDIATE .VOLCANIC ROCKS

2a rnasstVe flow or undiff erentiatcd

2b pillow flow2c pillow or flow breccia2d amygdaloidal2e porphyritic2 f ruff, .crystal tuff2g lapilli tuff

MAFIC VOLCANIC ROCKS

INtJtX O MAP SHEE IS

2.13286assumed claim post

REVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC

lo massive pillow or undifferentiatedlole pillow or flow brecciaId amygdaloidal

,e varioliticif porphyriticg pyroclastic

GOLDEN DRAGON RESOURCES LTD. GLEN AUDEN RESOURCES LTD

SUMMERS TOWNSHIP! PROPERTY

: Fig.5c

Approved: MB2.13286 BEARDMORE AREA

i t

-•3tf ' --" '- -f,' '' ' i - . . ' X-*M "' ll "" ' '"

-4™

V 'li

jjf:

4H- -E3B

h-—-- iO-00 S 9OD 5. ———î-.,-. S+50 V

L ut.

70

-1"

.C't r .a :*——-f --

42E12SW8833 2.13286 BEARDMORE AREA 320

--*-

V; : ',H*;'-,.•'' y Hjf/L-t .1. i .erl

f liter

8.13286

-0 i pole Ar-

^w*^'?1*...^'.J,.*....-.,..;/ fr.l l .

' v - a * --ô m

: IB'

F i J terec Prof iles

f ji t 'v : t giab i l T 1Fartor

Uodar . l -u Coours - L ] -- 2- 3. 5 - 7 - 5 - "l.....

Ins tr . jineot : J -f. -l l

\ .P,

-4-

or


GOLDEN DRAGONTime Don*In . PeLARIZftTIOM SURVEY

itn.) Soflw^re to t h* Eirth Srtencss,' 't...\'

r i i -. e r aid r r o l i les

'5 ? ^ c - 7 c l 'l* i , J. ' , ~ t --, /N.. IJlt.l

ROBERT S, MIDDLETON EXPLORATION'SERVICES INE.

GOLDEN DRAGON[j* 1 * . -, .t:*e;

INDUCED. l*OLNRÂtIQN SUftVEY* ' ' 5âf-^®r *' •-.;*'"--" ;-

42E125*8*33 2.13266 BEARDMORE AREA

17 + OO.w

F i .te-ed Pr of tles

fees i s t i v ; ty —— (. t-, a' 9 e 'Tit i I i t y*,V. f ,"--

l- i' 5 ' ;? - ^ -' -5

. Tr a -v,ff, t TCr I TSQ-.3

Operator: B. M^lps

tv.^. '' 9^3 v -iirrA 1±±r:-'--.i-2*'C]

ROBERT 5. MlOOilTOR '. E K? W R ft T J O N S ERV1M M.M? . I2. 182,8*

, GOLDEN

S'"iC l *T.^.V-:J-l

PtPKfSll^tt

r -v 7 .- / J J:// ' : Riljtered PrpHles

-: Hun t

Op*r a o : B. M a 1 p

j*

2^50 SL . .. _____ —i— UVGO, j

IVITV

™ 4 M (3

im 5pit*arft 10" tht- earth Tor^tp, U

2.13286

42E12S*e*33 2.1328B BEARDMORE AREA 350

.f

a

EIVONu

ROBERT S. MIDDLETON EXPLORftTION SERVICES INC.

i trGdLDEN DR'AGON

Titl(! ' TSfte DomainIND'UCEJD 'POLARIZATIOM SURVEY

f Beardmoreu ir. ir e' s;

Sept..Jot " K -M O

-

•t,' is*--''.-* -s ^.rp'-tjt* *' n ft'- --, :-.v,^*-r tf;- ; '^ vr ^-"'v

n^^Slfe^1;P^^-v^^K;li ' i" :,.- - . j; " - ' *'-.\ - '" ' If r - - V ' f . , ' f i " -.' - " il*J ' ' . •'" ' ' ''l:! -

t-O2îm;_41!^" 5

;' i * ' * i .. T

S-; '^'li^TfeW^TAji^

ra+oo s -*- 1-(M~*—'/MOO 5 -

-4^—*-*— -r-*———-tf+SG .5••"*--f J——-

f , i; l ter

J .T

i-*;. n-3

ir, - 4

-f-

, t? ^ J l-K-- -t-

-uiin :- -H-- --- - 4 - - -f --- -i

f M t'. ! ; t le r

•••j e

:HrtRGB'mUTT

W5ETP

Pt"-1ST IVI TV' ^î^ j;. J

2.1328^

4aE12SW8033 2.13286 BEARDMORE AREA 3GO

**f '..iV^v;*'-.., j lK . 1t-';.-;vi:';^.';^

^j:'-.^:;tv ::|N •^: 0qt!^D*pp^*^*& r^V'-' ^:"-' jj ;.'-' ' ,'-: "',-- .';*-.fc ; --^^.^n.'|J,.^v-'V,; t.-.^fi-

v..- - if; -;y.^^,v ffi—^ -^"- ^ '-s -1;••;ji

x a -*. 25 m- v w x ^' a 1.2,3.4

.. plot paiit . -

l

FM te^-ed Try f E.

I s t- TV 11 j- — —-' rge fib"' l l iy ——*~

! ogar l ihru '.cC on i our s l- 1-5; 2- 3. 5. 7/5. 10,...

ament: Iff?-! l

'Ir ^r i;, rt i er l Hur, t-ac 7 .

I'ptH- 3 1 ^r - 6. Ms l psp

j. P. ANOHHUS

HDDFIiC.TF

il S


fotGOLDEN DRAGON

Time DomainINDUCED POLARIZATION SURVEY

Beardmorer s T^p. ON

14,Job t.H-310

^-L

r--4

r, . 4

2+00 5

(2 ,..~-

l.'K

42E125W0033 2.13286 BEARDMORE AREA

i'.'

s, _____ J ^ .______L—— ^ . . J s, -^^- ^.-. - ^. ^, (* ..-.^-,^——f

t--

370

, UOG S ; G110 Li'SfJ ^^^. . .^^^^ ..J _ ~,..., ,-

16

- -- -*-t. -—, ~

v/-^

Ib,

*-/

fille

(MSfcf.]

2. 13286

•4 + OOw

O-i r-(VV-i ^J——.__..J——.i-..

F f I t p r f* d P r of E l es

P *i ir. t U : 1y C' 1.5- cjeab : l it y Mstal F sr.icr

i i ..u

f;; /, t -,{- : [,. Half 3 O t''

l P BMPHfc. i! j

WEnl!kt .1 i i* . 1

OHU' r K fr

.SF

ROBERT S. MIDDLETON EXPLORATION SERVICES INC

ft:GOLDEN DRAGON

. T l me Do.Ntatri INDUCED PCLARI2AT ION SURVEY

r s, Twp. UN

i1 e: Sept.' W. 5-0*1 e--l tf

li- *li

•H- -f- — -^ l,.. -—(

; -too" ? - f3*-so s 6*00 4.SO S . 4"*-; l'if -- ~,

f I I 1er

-i)

...1C1U '•f r J HI' 1W

;?iiu

•fiiS ,

/..,, 194?

4AM

42EI2SW0033 2.13286 BEARDMORE AREA 380

,^*-. ..^-,. ^.^.^^ , r.^ , t^^ L,.,. . *- ^-^..r.. ,—^..^ _*-- - - -- ^

i:}

ri * ,1

fi *A

-f-

..J

IT fI MSL i. l

hJPOL.PCiP-11

2.13286

Pala~ i-li pc l e Ar ray

*-——-JLHi ' [•"

P i b* pi- nl

l I t f? r fc H P o i i l e s

t?e!;' Ifi i i V I ij

CharpeaK I I i y

l, t'fit OUI" S

!pei a t or T B, H,,; f-sre

LF UUNf-i.r :i;

Hfrif!

l

'lH

PL 'r, [ '-if

f.OMDJC '(if

ROBERT;s. MIDDLETONEXPLORATION SERVICES INC.

f r, OGOLOEN DRAGON

•' Time DomainINDUCED POLARIZATION SURVEY

Beardmorer J3umft".er,s Twp. ON

- Sept. J6. 1969;lerj.

iob

fo- the E-ar.tb 5c ?

"l h *-

T—~T~^ C. . -J1"""™' iK t - 1 -.-'. - ;'": JM'-';-

. •••

•t

.'*

t^-

H-03 5

————l——r—.~~-4——-^.—.^î—- -*-'-——— --j———--- -i- — ~ -f.—. ..—4-. - ,-( -———.4 ........^.*-

382

42E 1 25* W33 2.13286 BEARDMORE AREA330

.M'-

h-41*-

(use:;

-f

.138G

S'*0-0w ;.

Pole'-Dipole

- 1-

n -2. 3. 4pic t pTJ

: P?. M -Of ^ i--

H-L

1

H* t

C

.ROBERT S..UIODLETON EXPLORATION SERVICES INC

GOLDEN DRAGONT;wc OomaZn

INDUCED POLARIZATION SURVEY' Bear dmore'r s T* p. l)N

r.Urp J n b 1 M-

l

•--f--

13-03 S

f r J ter

.s ;i

'

-i.4aE12SWM33 2. 1 3286 BEARDMORE AREA 400

'' '

2.13286

7 + QDw

PUe-lôlH ; r

r- .i .' s" t '. v I i y \~'n: Qt*-l .' i i I t'j

r H ; ir ' f t. '. ' - t

.B

qH 1 i

ijfe

H rt

ROBERT :S. MIDDLETON EXPLORATION SERVICES I

GOLPEN DRAGONl;n T;*e Domain

INDUCED POLARIZATION SURVEY Bear dmore

r a f v*p .

Sept. IX J9fiy. by; R .'l.

5cjieJob ' M 310

(tip| Software

ie t-" 1

0344^

-7? t-4-

U.O

-2

4\

\0

giooot

'^ s

. i

?', *....--'.177.--:^

^ 7,

/ A

"7"

BLO

CK I

NDEX

42E12SWea33 2.

]328

6 BEARDMORE

VLF

PROFILES

INPH

ASE

— — — — QU

ADRA

TURE

Prof

ile

Scaled

lcm

TRUE CR

OSS-

iXtR

: IP

STAT

ION:

SEATTLE. 24.8

INSTRUMENT

: Ge

onic

s EM

-16

VLF

CONDUCTORS

STRO

NG

O

MODERATE

O

WEAK

SIGNIFICANT

ANOM

ALY

— AX

IS OF

CONDUCTOR

13 2

86

200

ROBE

RT

S.

MID

DLE

TON

EX

PLO

RAT

ION

SE

RVI

CES

IN

C.

DEN

ISO

N

MIN

ES

LTD

.

BEAR

DMO

RE

PRO

JEC

T V

LF-E

M

SURV

EYS

umm

ers

Tw

p.,

Qn

t.

Fig.

3a

Dat

e*

Sep

tenb

er

89

Op

era

tors

* B

all/

Ha

lpag

e

N.T

.S.:

Job

*:

M-3

47

Date post:	20-Aug-2020
Category:	Documents
Upload:	others
View:	1 times
Download:	0 times

I Summers Township Joint Venture Property · proposed a fore arc accretionary prism, The major...

Documents