rpt on ground geophysical surveys...ground geophysical survey scale : 1 : 1,600,000 survey by jvx...

fil l l l l l l l l l l l l l l l l l

. 14777010

REPORT ON GROUND GEOPHYSICAL SURVEYS ON THE LAVOIE LAKE COPPER NICKEL PROJECT LANSDOWNE HOUSE AREA, PICKLE LAKE REGION NORTHERN ONTARIO

On Behalf Of :

Kewagama Gold Mines (Quebec) Ltd. 3200, 630 Rene Levesque Blvd. W. Montreal, Quebec H3B 1S6

Contact : Norman Brewster Tel: (514) 866-6001 Fax: (514) 866-6193

By:

JVX Limited60 West Wilmot St.- Unit 122Richmond Hill, OntarioL4B 1M6 ,,--

Contact: Slaine Webster Tel.: (416) 731-0972 Pax.: (416) 731-9312

JVX Ref: 9216 May, 1992

NOV 2 - 199?

MINING LANDS bHANCH

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TABLE OP CONTENTS

1. INTRODUCTION

2. SURVEY ACCESS AND LOCATION

3. SURVEY GRID AND COVERAGE

4. PERSONNEL

5. INSTRUMENTATION

5.1 HLEM System5.2 Mag/VLF System5.3 Data Processing

6. SURVEY METHOD AND FIELD PROCEDURES

6.1 Horizontal Loop EM6.2 Total Field Magnetics6.1 Very Low Frequency (VLF) EM

7. DATA PROCESSING AND PRESENTATIONOF RESULTS

7.1 Presentation Plate Index7.2 Anomaly Classification

8. DISCUSSION OF RESULTS

9. SUMMARY AND RECOMMENDATIONS

•III Illl14777 SPRINGER LAKE

Page No.

1

1

2

5

5

555

6

668

9

910

10

16

010C

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•J VXFIGURES

Figure 1:

Figure 2:

Figure 3:

TABLES

Table 1:

Table 2:

Table 3:

APPENDICES

Appendix 1:

Appendix 2:

West Grid

Plate la:

Plate lb:

Plate 2a:

Plate 2 b:

Plate 3a:

Plate 3b:

Plate 4:

East Grid

Plate 5a:

Plate 5b:

Plate 6a:

Plate 6b:

Plate 7a:

Plate 7b:

Plate 8:

Location Map scale 1:1,600,000

Claim Map scale 1:30,000 {approx.)

Phaser Diagram

Mag 1 VLF Production Summary

HLEM Production Summary

Presentation Plate Index

Instrument Specification Sheets

Plates, scale I"r200' (1:2400)

Total Field Magnetics Contours

Total Field Magnetics Profiles

VLF-EM Profiles - Cutler 24.0kHz

Fraser Filtered VLF Cutler 24.0kHz

HLEM Profiles 888Hz, c.s.:400ft

HLEM Profiles 1777Hz, c.s^400ft

Compilation Map

Total Field Magnetics Contours

Total Field Magnetics Profiles

VLF-EM Profiles - Cutler 24.0kHz

Fraser Filtered VLF Cutler 24.0kHz

HLEM Profiles 888Hz, c.s.r200ft

HLEM Profiles 1777Hz, c.s.r200ft

Compilation Map

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

•J VX

A REPORT ON GROUND GEOPHYSICAL SURVEYS CONDUCTED ON THE LAVOIE LAKE COPPER NICKEL PROJECT

LANSDOWNE HOUSE AREA, PICKLE LAKE REGION, NORTHERN ONTARIO

On Behalf Of

KEWAGAMA GOLD MINES (QUEBEC) LTD.

1. INTRODUCTION

Between April 24th and May 17th, 1992, Horizontal Loop Electromagnetic (HLEM), Total Field Magnetics, and VLF surveys were carried out on the Lavoie Lake copper nickel Project, Lansdowne House area, by JVX Ltd. on behalf of Kawagama Gold Mines (Quebec) Ltd.

The surveys yielded coverage on two grids. The western grid contains the "C" and "D" mineralized zones and the eastern grid contains mineralized zone "A".

The Mag/VLF survey employed the Scintrex IGS-2/MP-4/VLF-4 system. The sample interval was 50 feet and the VLF transmitter NAA Cutler Maine (frequency 24.0kHz) was employed.

The HLEM survey utilized the Max-Min II system with a coil spacing of 200ft and 400ft and a station interval of 100ft. The 400ft coil spacing was used on lines L-114W to L-140W on the west grid and on lines L-15E and L-16E on the east grid. The west grid coverage of the 400ft coil spacing was 7.2 line-mi and the east grid coverage was .68 line-mi. The 200ft coil spacing was employed with a 50 ft. reading interval on the west grid on line L-120W and on lines on L-600SE to L-2600SE totalling 7.3 miles line-mi, on the east grid.

This report describes the survey procedures and includes an interpretation of the results. Drafted presentation of the results is in the form of contour plan maps and offset profiles with conductors indicated and labelled.

2. SURVEY ACCESS AND LOCATION

The Kewagama Gold Mines Ltd. property consists of three 16 unit claims (1133764, 1133765, and 1133766) straddling Lavoie Lake located approximately 125 miles north east of Pickle Lake, northern Ontario.

Access to the property is by air from Pickle Lake via Highway 38. The location of the property with respect to nearby towns at a scale of 1:1,600,000 may be found in Figure 1.


^SURVEY AREA l

LOCATION MAP

KWG RESOURCES INC. LAVOIE LAKE PROJECT

LANSDOWNE HOUSE AREA Northwestern Ontario

GROUND GEOPHYSICAL SURVEY

Scale : 1 : 1,600,000

Survey by JVX Ltd. Figure t

CLAIM MAP

KWG RESOURCES INC.LAVOIE LAKE PROJECT


GROUND GEOPHYSICAL SURVEY

Scale: i: 30,000 (approx.)

Survey by JVX Ltd. Figure 2


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3. SURVEY GRID AND COVERAGE

WEST GRID ( Mineralized zones C SL D ): The baseline of the grid was oriented nominally east-west. The wing lines are nominally 100ft apart.

EAST GRID ( Mineralized zones A ): The baseline of the grid was orientednominally at 135 with wing lines cut at 100 ft. intervals.A detailed listing of the survey coverage may be found in Table l A 2.

TABLE l

MAG f VLP PRODUCTION SUMMARY

West Grid

LINE

14000W13900W13800W13700W13600N13500N13400W13300W13200W13100W13000W12900W12800W12700W12600W12500W12400W12300W12200W12100W12000W11900W11800W11700W11600W11500W11400W11300W11200W11100W11000W10900W10800W

FROM

2400N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2500N2450N2450N2450N2500N2500N2500N2500N2850N3000N3050N

TO

5800N5800N5800N5800N5800N5800N5800N5800N5800N5800N5700N5500N5500N5500N5500N5550N5500N5500N5500N5500N5600N5600N5600N5600N5600N5500N5500N5500N5500N5500N5500N5500N5500N

Total :

LENGTH(feet)

340033003300330033003300330033003300330032003000300030003000305030003000300030003100310031003150315030503000300030003000265025002450

101600 feet(19.24 miles)


0J VX- 3 ~

Mag f VLF PRoduction SUMMARY cont.'dEast Grid

LINE

0200SE400SE600SE700SE800SEgoose

1000SE1050SE1100SE1150SE1200SE1250SE1300SE1350SE1400SE1500SE1600SE1700SE1800SE1900SE2000SE2100SE2200SE2300SE2400SE2500SE2600SE2700SE2800SE2900SE3000SE3100SE3200SE3300SE3400SE3500SE3600SE3700SE3800SE3900SE4000SE

FROM

2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW800SW

2000SW800SW

2050SW800SW

2050SW800SW

2000SW2050SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW2000SW

TO

1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE

01000NE

01050NE

01000NE

01000NE1000NE1000NE1000NE1000NE1000NE10 DONE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE1000NE

Total :

LENGTH(feet)30003000300030003000300030003000800

3000800

3100800

3050800

300030503000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000

117450 feet(22.24 miles)


•J VX- 4 -

West Grid

LINE

13700W13600N13400W13200W13000W12800W12600W12400W12300W12200W12100W12000W11800W11600W11400W

East Grid

LINE

600SE700SE800SE900SE1000SE1100SE1200SE1300SE1400SE1500SE1600SE1700SE1800SE1900SE2000SE2100SE2200SE2300SE2400SE2500SE2600SE

TABLE 2

HLEM PRODUCTION

FROM

2700N2700N2700N2700N2700N2700N2700N2700N2700N2700N2700N2700N2700N2700N3650N

FROM

1700SW1900SW1900SW1750SW1700SW1600SW1600SW1450SW1450SW1500SW1500SW1400SW1450SW1000SW1000SW900SW900SW900SW900SW900SW850SW

SUMMARY

TO

4100N5600N5600N5500N5500N5300N5300N5300N5300N5300N5400N5300N5300N5400N5300N

Total :

TO

300NE300NE300NE300NE300NE300NE350NE350NE400NE400NE400NE400NE450NE700NE800NE900NE800NE850NE800NE800NE100NE

Total :

LENGTH(feet)140029002900280028002600260026002600260027002600260027001650

38050 feet(7.20 miles)

LENGTH(feet)20002200220020502000190019501800185019001900180019001700180018001700175017001700950

38550 feet(7.30 miles)


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0J VX

4. PERSONNEL

Mr. Fred Moher, Geophysical Technician, operated the Max-Min and IGS system, acted as party chief and was responsible for data quality and the day to day operation and direction of the survey.

Mr. Bogdan Kasprzak, Geophysicist, operated the IGS-2 system and assisted in data compilation.

Mr. Blaine Webster - Consulting Geophysicist, JVX Ltd. Mr. Webster provided overall supervision of the reporting from the Richmond Hill office.

5. INSTRUMENTATION

5.1 HLEM

The Apex Parametrics Max-Min II EM system was used for the HLEM survey.

5.2 Magnetics/VLF

The Scintrex IGS-2/MP-4 proton precession magnetometer was used to read the Total Field component of the magnetic field along the survey lines.

Changes in the ambient magnetic field with time were monitored and recorded by a second fixed Scintrex MP-3. The base station took measurements at 10 second intervals. The base station magnetic data was used to automatically correct the survey magnetic data for diurnal variations.

The Scintrex IGS-2 with the VLF-4 option was employed to measure the VLF field components. The IGS-2 is an integrated microprocessor based instrument allowing measurement of both the magnetic and VLF fields, one after the other, while the operator is occupying the same station. The IGS-2 stores the results in an internal solid-state memory.

5.3 Data Processing

The HLEM data was manually digitized and then archived on floppy disk. The Magnetic and VLF data were archived, processed and plotted by an Corona PC-400 microcomputer using an Epson FX-80 dot matrix printer. At the conclusion of each day's data collection, data resident in the IGS memory was transferred, via serial communication link, to the computer - thereby facilitating editing, processing and presentation operations. All data was archived on floppy disk. In the Toronto office the data was ink-plotted in plan contour or offset profile format on a Nicolet Zeta drum plotter interfaced to an IBM PC/386 microcomputer.

The instrumentation is described in greater detail in the specification sheets appended to this report.


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•J VX

6. SURVEY METHOD AND FIELD PROCEDURES

6.1 Max-Min II Horizontal Loop

Max-Min II is a moving-source, frequency-domain, ground electromagnetic method, which uses a receiver and transmitter connected by cable. The transmitter supplies a reference signal against which the electromagnetically induced signal is compared at the receiver. The receiver measures the two components (in-phase and quadrature) of the secondary field, in per cent of the primary field. Depth of penetration is, nominally, one half of the distance between the transmitter and receiver.

The results are usually plotted as a stacked series of profiles with in-phase and quadrature superimposed on the survey line. The plotting point is midway between the transmitter and receiver.

A conductor is normally marked by a deep negative trough in the profile with "shoulders" of moderately high positive values on either side. Shape and magnitude of the anomaly varies with the separation distance of the coils and frequency of the signal, and with morphology and conductivity of the conductor. The higher of the two "shoulders" is usually on the side to which the conductor is dipping. The "width" of the anomaly is conventionally defined as the distance between the points at which the in-phase measurement is zero, minus the distance between the coils.

The survey used a frequency of 888Hz, and 1777Hz with a coil separation of 200 and 400ft. Stations were spaced 100ft apart for the 400 ft data with 50 ft stations over the anomaly center.

6.2 Survey Method and Procedures (Magnetic)

The magnetic method consists of measuring the magnetic field of the earth as influenced by rock formations having different magnetic properties and configurations. The measured field is the vector sum of induced and remanent magnetic effects. Thus, there are three factors, excluding geometric factors, which determine the magnetic field. These are the strength of the earth's magnetic field, the magnetic susceptibilities of the rocks present and their remanent magnetism.

The earth's magnetic field is similar in form to that of a bar magnet. The flux lines of the geomagnetic field are vertical at the north and south magnetic poles where the strength is approximately 60,000 nanoTesla (nT). In the equatorial region, the field is horizontal and its strength is approximately 30,OOOnT.


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VX

The primary geomagnetic field is, for the purposes of normal mineral exploration surveys, constant in space and time. Magnetic field measurements may, however, vary considerably due to short term external magnetic influences. The magnitude of these variations is unpredictable. In the case of sudden magnetic storms, it may reach several hundred nT over a few minutes. It may be necessary, therefore, to take continuous readings of the geomagnetic field with a base station magnetometer while the magnetic survey is being done. An alternative field procedure is to make periodic repeat measurements at convenient traverse points.

The intensity of magnetization induced in rocks by the geomagnetic field P is given by:

I r kF

where:

I is the induced magnetizationk is the volume magnetic susceptibilityF is the strength of the geomagnetic field

For most materials, k is very much less than 1. If k is negative the body is said to be diamagnetic. Examples are quartz, marble, graphite and rock salt. If k is a small positive value, the body is said to be paramagnetic, examples of which are gneiss (k?.002), pegmatite, dolomite and syenite. If k is a large positive value, the body is strongly magnetic and it is said to be ferromagnetic, for example, magnetite (ksO.3), ilmenite and pyrrhotite.

The susceptibilities of rocks are determined primarily by their magnetite content since this mineral is so strongly magnetic and so widely distributed in the various rock types (of considerable importance, as well, is the pyrrhotite content).

The remanent magnetization of rocks depends both on their composition and their previous history. Whereas the induced magnetization is nearly always parallel to the direction of the geomagnetic field, the natural remanent magnetization may bear no relation to the present direction and intensity of the earth's field. The remanent magnetization is related to the direction of the earth's field at the time the rocks were last magnetized. Movement of the body through folding etc. and the chemical history since the previous magnetization are additional factors which affect the magnitude and direction of the remanent magnetic vector.


•JVX

Thus, the resultant magnetization M of a rock is given by:

M : Mn -f kF

where Mn is the natural remanent magnetization, and F is a vector which can be completely specified by its horizontal (H) and vertical (Z) components and by the declination (D) from true north. Similarly, Mn is specified when its magnitude and dirction are known. Thus, considerable simplification results if Mn ~ O, whereupon M merely reduces to kP. In the early days of magnetic prospecting, it was usually assumed that there was no remanent magnetization. However, it has now been established that both igneous and sedimentary rocks possess remanent magnetization, and that the phenomenon is a widespread one.

Since the distribution of magnetic minerals (magnetite, pyrrhotite) will, in general, vary with different rock types, the magnetic method is often used to aid in geologic mapping. In gold exploration, the magnetic survey is of particular importance because it will locate areas of structural complexity, carbonization, and silicification.

On the Lavoie Lake copper - nickel project magnetic measurements were taken at 50 foot intervals.

6.3 Survey Method and Field Procedures (VLF)

The Very Low Frequency (VLP) Electromagnetic Method measures variations in the components of the electromagnetic fields, set up by communication stations operating in the 15 to 25 kHz frequency range. These stations, located around the world, generate signals for the purposes of navigation and communication with submarines.

In far field, above uniform earth, the groundwave of the vertically polarized VLF radiowave has three field components:

1) a radial, horizontal electrical field,2) a vertical electrical field, and3) a tangential, horizontal magnetic field.

When these three fields meet conductive bodies in the ground, eddy currents are induced causing secondary fields to radiate outwards from these conductors.

The primary field from a VLF station can vary considerably. For the most part, the field fluctuates moderately during the course of the day due to changes in atmospheric conditions. There are, however, more dramatic changes indicated in the recording. Towards evening there is a large upward swing in the field strength, and at several points during the day, both partial and total drops in the field amplitude can be observed. In the light of these irregularities, the horizontal field data should always be considered with reservation as it is difficult to know whether changes are caused by conductors or by variations in the station's signal.


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•JVX _____________________If the primary field strength is constant, changes in the amplitude of the horizontal magnetic field mainly reflect variations in the conductivity of the earth. Normally there will be no vertical magnetic field. However, near a conductor, a vertical field will be observed. The relative amplitudes of the in-phase and quadrature components may be used to interpret the conductivity-thickness characteristics of the conductor.

The survey employed the transmitted primary signal from, Cutler Maine, USA (24.0kHz). Measurements of three VLF components were taken along line at 50 foot intervals.

7. DATA PROCESSING AND PRESENTATION

To allow for the computer processing of the Mag/VLP data, the raw data stored internally in the IGS-2 system was transferred at the end of a survey day to floppy diskette by the in-field microcomputer and appropriate communications software. The raw data was filed on diskette in ASCII character format using an IBM compatible (MSDOS) microcomputer. The Max-Min data was digitized manually.

After correction of the total field magnetic data by linking the mobile and base station units and employing the built in diurnal correction software, the corrected data was dumped to the microcomputer and stored on floppy diskette.

After the completion of the survey, contoured plan maps and profiles with posted values of the total field magnetic data and profile plots of the VLP and HLEM data were computer generated and fine-drafted on mylar at the Richmond Hill office at a scale of I"s200'. VLF-EM Fraser Filter maps were also plotted at the same scale.

A listing of the final presentation product follows:

7.1 Plan Maps Plate Index (Table 3)

West Grid

Plate la: Total Field Magnetics Contours

Plate lb: Total Field Magnetics Profiles

Plate 2a: VLF-EM Profiles - Cutler 24.0kHz

Plate 2b: Fraser Filtered VLF Cutler 24.0kHz

Plate 3a: HLEM Profiles 888Hz, c.s.s400ft

Plate 3b: HLEM Profiles 1777Hz, c.s.s400ft

Plate 4: Compilation Map

PHASOR DIAGRAMFOR A VERTICAL (DIP*90 0 ) THIN (t**O.OI95x s) HALF-SHEET

IN RESISTIVE HALF-SPACE

Figure 3

OUT OF PHASE(PEAK TO PEAK)

30 "/c

o". C ONDUCTIVITY ( S/m ) t ''THICKNESS s i COIL SEPARATION(m) f i FREQUENCY (Hertz)

IN PHASE(PEAK TO PEAK)

Mq d


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•J VX ________________________

Plan Maps Plate Index (Table 3) cont.d East Grid

Plate 5a: Total Field Magnetics Contours

Plate 5b: Total Field Magnetics Profiles


Plate 6b: Fraser Filtered VLF Cutler 24.0kHz

Plate 7a: HLEM Profiles 888Hz, c.s.:200ft

Plate 7b: HLEM Profiles 1777Hz, c.s.r200ft

Plate 8 : Compilation Map

7.2 Anomaly Classification

The anomalies are indicated on a Compilation maps. The HLEM conductors are shown as a number of small crosses grouped as a conductive zone or connected by an axis (shown as a heavy dashed line) depending on the relative strength of the response. The conductors are labelled with a letter (ei. A - l in A zone and HC - l or HD - l in C and D zone respectively.). The VLF conductors are indicated by square, triangle or dashed circle symbols usually located within the VLF fraser filter conductor (outlined by greater than 25 unit contours) and are labelled with the letters VA in A zone and VC or VD in zones C and D with an appropriate number. The magnetic anomalies are outlined by greater than 60,000 nT contour (thin dashed line), hatched and are labelled with the letter M in A zone, MG and MD in C and D zone and a number.

The conductivity thickness and depths to current axis were derived from the phase diagram found in figure 3. The diagram presumes a thin ( ^.1 of coil separation ) vertically dipping sheet conductor. The approximation is good within I QK for dips between -75 and +7S .

8.0 DISCUSSION OF RESULTS

8.1 Introduction

The HLEM survey on the east grid located 4 conductors labelled Al to A4 all had coincident VLF conductors and magnetic response. The VLF survey located seven VLF conductors labelled VA1 to VA7 with VA1, VA2, VA3, VA4,VA6 and VA7 having coincident magnetic responses. On the west grid six HLEM responses were identified,all had coincident VLF conductors and only HC-north did not have a significant magnetic association. Seven magnetic anomalies were located.

The HLEM anomalies yielded very high conductivity thickness which were verified by the drill results.


! l I l l I I I

i i ! i i i * i

tO,OOO-KJ.25O*T

O - MM PI (Mm w CM (

as-Vtr fimw fill

Ml rtn S IVM OMMU

KWO Jtenf-Moy 194? *MI hot* 1C* HC3 o* DitoOr)

COMPILATION MAP

KWG RESOURCES INC.UTOtt LAKE PROJECT uunoomn HOUSE AREA

i OnUru

GRID MAP

KALI 1 = 5391

COMPU9 VTjn LTD.MAY lt*Z

WEST GRID PUR 4

6063760367602366015560091600265997059923598865985559822597925976759747597315971659701596865966659636

gammas

l

too m

•oo ne

mse LIWC

too SK

wo s*

1200 SK

W U U W U UV) V) *I ** V) M

o o o o o eS S g S i g

BOO NE

LEGEND

Moi]n*lic high l-6O.OOO nT)

Vl-f-EM

B - StTmg in phoM

D - Medium In phm

A - Medium Out phaw

O - Weak In pNn* or Out Dhow

MntMin Conducli** Zoo*

•* "T"** Horizontal kwp EM yt-f!— ———— Conductor width

OutBho*

Conductor oxit

VLF Frewr nttar conductor t*25unit contour)

littvprvlvd foult

F0] Fold

Inco 1973 S 1974 drill hoi*

KWG Joril - May 1992 drill how ( Al (o *)O)

COMPILATION MAP

KWG RESOURCES INC.LAVOffi LAKE PROJECT

LANSDOWNE HOUSE AREA ___northwestern Ontario___

GRID MAP

SCALE 1 '- 4315

SURVEY BY JVX LTD.

MAYEAST GRID PLA1X B


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8.2 EAST GRID GEOPHYSICS

The east grid was surveyed with magnetics and VLF electromagnetics and partly with a horizontal loop survey with an intercoil separation of 200 feet and frequencies of 888 Hz and 1777 Hz.Five horizontal loop conductors were located and designated A-l, A-2, A-3, A-4 and A-5. ( Plate 8 Compilation Map )

Horizontal Loop Anomaly A-l ( 2300 SE - 325 NE l 2600 SE - 600 NE )

Conductor A-l is a moderate to strong HLEM conductor (92 Siemens) which correlates with a short strong (65 Siemens) VLF conductor. Anomaly A-l is on the northern flank of a high magnetic response. The conductivity does not appear to be associated directly with the magnetic response.

Recommendation :

Anomaly A-l has been drilled by INCO hole 49198, which intersected 5 ft of 5y, sulphides. The magnetic anomaly Ml located 100 feet to the west should be evaluated for its copper potential. The coincident fraser filter VLF conductor ( VA 6) could be checked with IP.

Horizontal Loop Anomaly A-2 ( 1200 SE - 100S f 1 500 SE - 50 N )

Anomaly A-2 is a strong horizontal loop conductor (92 Siemens) withan estimated depth of 13 metres. The conductor has a coincident weakto moderate magnetic anomaly and a moderate VLF fraser filterconductor.The VLF conductor noted as VA 2 has a much longer strike length (1000ft.) than the horizontal loop conductor (300 ft.)Anomaly A-2 has been drilled by hole A10 and A4.The sulphide zone in hole A4 from 92.5 to 96.5 ft. correlates withthe stronger VLF fraser filter response and the horizontal loopconductor.

Recomendation :

HLEM anomaly A-2 appears to be explained by the sulphides in drillhole A4 at 92 ft.Hole A10 also intersected minor sulphides at 100 ft.

Horizontal Loop Anomaly A-3 ( 1200 SE - 800 SW f 2600 SE - 100 SW )

Anomaly A-3 is a very strong (75-180 Siemens) HLEM conductor with strong coincident VLF and magnetic response.The main A-3 conductor appears to correlate with massive sulphides occuring on the northern contact of the gabbro (ie) hole A5 (350 ft.-409 ft.) A3 (400 ft.-480 ft.) A4 (612 ft.-665 ft.)


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•J VX

Recommendation :

The southwestern end of the HLEM conductor appears to be cut by faultPI.Drill holes A3 and A4 have explained the conductor.The eastern part of the conductor was very strong (90 Siemens) andwas throughly tested by holes A6, A7 and A8. The anomaly appears tobe explained by 10 ft wide zone of massive pyrrhotite and pyrite in azone of 80 ft. wide 3% po,py. Structurally the area appears to hostfold PD2 the nose of which is located at 2500 SE f 300 SW.Anomaly A-3 has been tested by INCO drill holes 54001, 54002, 54015,49101 and 49176.The VLP conductors that continue to the east of anomaly A-3 has beentested by INCO drill hole 49200.VLP conductor VA 7 correlates with HLEM conductor A-3 North.

Note : The VLF fraser filter data has resolved two conductors {VA 2 and VA 3) within the western part of HLEM conductor A3, which were both tested by holes A3 and A5.

Horizontal Loop Anomaly A-4 ( 1100 SE - 1175 SW l 1600 SE - 975 SW ) Anomaly A-5 ( 2500 SE - 600 SW / 2600 SE - 600 SW ) Anomaly A-6 ( 600 SE - 1450 SW )

The three horizontal loop conductors correlate with a strong VLF conductor VA4 and VA4 east. The peak fraser filter VLP responses correlate with the strongest horizontal loop responses.

HLEM conductor A-4 conductivity range from 33 to 73 Siemens and width of 20 ft. to 100 ft.The magnetic and HLEM data suggest a fold may exist ( PD-1 ) on the western end of anomaly A-4.

HLEM conductor A-5 is a very strong conductor with conductivities ofover 100 Siemens.Conductor A-5 correlates with a strong VLF conductor ( VA 4 east )and an associated magnetic high.Holes A7 and A8 may have intersected the zone at the bottom of thehole. Hole A7 intersected minor sulphide at 522 ft. and A8intersected 202 arsenopyrite at 385 - 388 ft.

HLEM coductor A-6 is a one line conductor occuring on the western part of VA 5 and is coincident with a magnetic high. The VLP conductor increases in strength to the west suggesting the Max-min conductor will be stronger to the west.

Recommendation :

Continue HLEM coverage to the west to extend HLEM conductor A-6.


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•u vxVLF conductor VA 6 ( 800 SE - 1900 SW / 3 100 SE - 1700 SW )

A moderate VLF conductor extends across the southern part of the grid. VA 6 correlates with a 300 to 600 gamma magnetic anomaly.

Recomendation :

HLEM coverage and IP should be extended to cover conductor VA 6.

Structure :

The compilation map shows the faults ( FI ), folds ( FD1 ) and stratigraphic horizon ( SH ) or vertical lithologic change interpreted from the geophysical data.

Faults :Four faults or stratigraphic breaks are noted as FI, F2, F3 and F4. The drill data should be reviewed to see if the interpreted faults exist.

Stratigraphic horizons :

Three stratigraphic horizons designated SH1,SH2 and SH3 are thought to be stratigraphic changes in the pile associated with sulphide horizons.

8.3 WEST GRID GEOPHYSICS

The west grid was completely surveyed at 100 line separation and 50ft station intervals with magnetics and VLF electromagnetics using Cutler Maine. Lines 13700W to 11400w were surveyed with a horizontal loop electromagnetic system utilizing a coil separation of 400ft at frequencies of 888 Hz and 1777 Hz. Lines 12400 W and 12000W were surveyed at 100 ft line intervals. Lines 12000 W to 11400 W and 12400W to 13600 W were surveyed at 200 ft intervals.

The horizontal loop survey located three very strong conductors designated D, C, and C south. The horizontal loop conductors have coincident strong VLF conductors and a 1000 nT magnetic response.

D-ZONE

Horizontal Loop Anomaly HP-1 ( 10800 W f 4000N to 12800W f 4600N )

Horizontal Loop conductor HD-1 consists of a very strong anomaly ranging from 30 to 221 Siemens. Coincident moderate VLF conductors VD-1 / VD-1 South and magnetic anomaly MD-1 correlate with the horizontal loop conductor. The fraser filter resolves two conductive sources within the wide horizontal loop anomaly which were drilled by Inco holes 54007 and 54008.


- 14 -

•u vxDrillholes DI to D7 intersected 150 to 400 ft wide sulphide zones ranging from l?i to 40?S sulphides with an average of 3?i. The higher volumes of sulphides were over smaller distances for example the 40?i sulphide intersection was over 2ft. and 20?S over 5ft. The intersected sulphides explain the conductivity and magnetic responses observed in the geophysics.

Recommendation:

Anomaly HD-1 should be extended to the west and east and drilled. VLP conductor VD-1 extends to the eastern most line 10800 W indicating significant sulphides are located to the east.

Anomaly VD-2 should also be surveyed with horizontal loop and induced polarization surveys to determine if the area has potential for disseminated sulphides which may host copper and nickel mineralization.

D ZONE NORTH ( 10800W l 4500N If 12800W f 5000N )

Horizontal Loop Anomaly HP-North { 12400 W / 5000N to 12000W f 5000N )

The D-North zone consists of a weak horizontal loop anomaly located on the western part of a weak VLP conductor VD-3 which also had an associated 200 nanotesla magnetic response. The top of hole D4 is a highly silicified gabbro containing 0.5 to 5?i chalcopyrite. The associated magnetic response suggests magnetite may have been partially destroyed suggesting possible enrichment in copper mineralization.

Recommendation

Induced polarization surveys should be conducted over the D Zone North to locate zones of significant non conductive sulphides.

D ZONE SOUTH Magnetic Anomaly MD-1 South (11900 W /3750N to 12700W /4000N)

Magnetic anomaly MD-1 south is not associated with any conductivity.

Recommendation:

Conduct an IP survey which may locate sulphides associated with magnetic anomaly MD-1 South.

C-ZONE (12100W f 3500N to 14000W f 3800N )

A strong horizontal loop conductor HC-1 ( 82 Siemens ) has an associated moderate to strong VLP conductor (VC-1) and a 500 nanotesla magnetic response (MC-1). The geophysical responses have been explained by 1992 drillholes CI, C2 and C3 and INCO holes 49172, 49197 and 54004. Hole 54004 intersected 58 ft of Q.7% Cu and G.37% Ni.


- 15 -

VX

Recommendation:

Induced Polarization surveys should be conducted to locate disseminated sulphide zones located adjacent to HC-1. The area should also be evaluated for gold. Additional drilling should be conducted along the horizontal loop conductor.

C ZONE NORTH ( 13600W / 4300N to 13200W f 3800N )

The C Zone North consists of a one line weak (35 Siemens)horizontal loop conductor (HC-1 North) and a weak VLF conductor ( VC-North ).

Recommendation:

The C Zone North should be surveyed with induced polarization to determine if significant sulphides are associated with VLP conductor VC-North.

C ZONE SOUTH ( 11100W f 2600N to 13700W f 3000N )

C Zone South consists of a long horizontal loop conductor (HC-1 South) that is strong on its eastern half with a strong VLP conductor VC—l South and a 500 nanotesla magnetic anomaly MC-1 South. Inco drill hole 54003 intersected sulphides that would explain the observed conductivity and magnetic response.

The western part of HC-1 South is much weaker (18 Siemens) than the eastern part of the conductor (83 Siemens).

Recommendation:

The eastern half of conductor HC-1 South should be drilled and its geological relationship with conductor HC-1 should be explained. Conductor HC-1 South correlates with the strongest airborne INPUT conductor on the west grid. The conductor should be traced out onto the lake in the winter. A Misse-a-la Masse survey would determine if the C-ZONE and C-SOUTH are interconnected.

The western half of conductor HC-1 South should be surveyed with an induced polarization survey to determine if there is any significant sulphides associated. Line 12300W should be tested for precious metals as it is in a structural deformation area.

Magnetic anomaly MC-2 South should be surveyed with IP to locate any associated sulphides.


- 16 -

•J V X _______________________

9.0 SUMMARY AND RECOMMENDATIONS

In April and May 1992 JVX Ltd. carried out HLEM, Magnetic, and VLF surveys on the Lavoie Lake basemetal project, Lansdowne House area, on behalf of Kewagama Gold Mines Ltd.

On the eastern grid four HLEM anomalies were identified on the grid and labelled Al to A4. Seven VLF anomalies were identified and labelled VA1 to VA7. All four of the HLEM anomalies, and six of the VLF anomalies, VA1, to VA4 and also conductors VA6 and VA7, showed coincident magnetic anomalies. Most of the HLEM anomalies exhibited coincident VLF anomalies. The VLF data also revealed some possible conductors in areas not surveyed by HLEM, including VA5. The VLF data also extended the length of HLEM conductors A2, A3, and A4.

The drilling program explained the observed conductivity and magnetic responses on HLEM conductors Al A2 and A3. Additional drilling and geophysics is required on HLEM conductor A4 in the vicinity of fold FD1, and VLF conductor VA5.

On the western grid six HLEM anomalies were identified on the grid and labelled HD-1, HD-2, HC-1, HC-1, HC-north and HC-south. Eight VLF anomalies were identified and labelled VD-1, VD-2, VD-3, VD-1 South, VC-North, VC-1, VC-1 South, and VC-2 South. Seven magnetic anomalies were identified and labelled M-l, M-2, MD-1, MD-1 South, MC-1, MC-1 South, and MC-2 South.

Five of the HLEM and VLF anomalies, showed coincident magnetic anomalies. All of the HLEM anomalies exhibited coincident VLF anomalies. The VLF data also revealed some possible conductors in areas not surveyed by HLEM, including VD-1. MC-2 south had some weak VLF conductivity associated with it and should be surveyed with IP to locate any associated disseminated sulphides.

The geophysics supports the geological correlation that the gabbro units in the C and D zones are the same which indicates the the body is very large. The relationship of the C-South zone to the C zone must be determined as it could significantly increase the size of the deposit. The VLF data also extended the length of HLEM A zone conductors A2, A3, A4 and C and D HLEM zone conductors HC-1, HC-1 south, and HD-1.

The strongest (25) Fraser filter contours when compared with the strong HLEM anomalies correlate to the main sulphide zones. For example fault F4 separates two Fraser filter anomalies VA3 east and VA3 west which correlate with good sulphide zones intersected in holes A9 and A7. Old INCO hole 49176 drilled between the two VLF anomalies intersected only limited sulphides. Therefore strong Fraser filter VLF conductors in the Lavoi Lake area should be checked with horizontal loop because they have a very good chance of being associated with sulphides especially when correlating with a magnetic response.


- 17 -

VX

Recommendations:

East Grid:

Extend HLEM coverage on strong VLP Fraser filter conductors VA-3 east, VA-4 west and VA-5. HLEM conductor A-4 should be drilled on line 1100E in the region of fold PD1 as a potential gold target.

IP should be done on some of the weaker non magnetic VLP targets. Misse A La Masse could also be done to determine if sulphides intersected by holes A-4 and A-9 are connected to sulphides in holes A-6, A-7, and A-8.

West Grid:

Extend HLEM coverage on all of the grid to the east and west. Misse a La Masse should be done to see if the D, C, and C-south zones are interconnected. IP should be done on 200 or 400 ft lines to see if there are significant disseminated sulphide zones near the main C-D zones. The area of highest potntial is on the D and D-north zones where silicification was noted. Magnetic anomaly MC-2 south should also be surveyed with IP to locate disseminated sulphides.

If there are any questions with regard to the survey or the reporting please do not hesitate to contact the author at JVX Ltd.

Respectfully submitted,

JVX LIMITED

Blaine Webster, B.Se. Geophysicist

l l l l l

Appendix l

l Instrument Specification Sheets

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Scintrex has used low power con sumption microprocessors and high density memory chips to create the IGS Integrated Portable Geophysical System; instrumentation which will change the way you do ground geophysics.

Here are the main benefits which you will derive from the IGS family of in strumentation:

1. Depending on your choice of optional sensors you can make one, two or all of: magnetic, VLF and electromagnetic measurements. Thus, you may optimize the IGS system for different geophysical conditions and production requirements.

2. You will save time and money in the ~t acquisition, processing and presen tation of ground geophysical survey data.

3. You will achieve an improvement in the quality of data through enhanced reading resolution, an increase in the number of different parameters measured and/or a higher density of observations. Further, errors which occur in manual transcription and calculation will be eliminated.

4. Your operator will appreciate the simplicity of operation achieved through automation.

Since add-on sensors are relatively less expensive, your investment in a range of IGS instrumentation may be much less than it would be with a number of different instruments, each dedicated to a different measurement.

The Scintrex IGS-2/MP-4/VLF-4/EM-4 permits one operator to efficiently measure magnetic, VLF and EM fields and to record data in computer compatible solid-state memory.

Typical Comments of IGS Users of the Scintrex Integrated Portable Geophysical System

"The two main advantages are the abili ty to take readings faster at much closer spacing and the ease in the cor rection of the data."

"Compared with analog instrumenta tion, the reading accuracy is demonstrably better and for multi- parameter measurements, the reading speed is much greater."

"We will probably add the VLF E-field capability next year to help discriminate overburden responses and get resistivity information."

"We can take two stations of VLF data in the time it takes to read and record one with the EM-16."

"l would estimate that IGS VLF dip angles are accurate to i 1 /2" or better, whereas analog units are ± 1 " with a good operator and ±3" with an inex perienced one.",

"l estimate that the IGS has reduced the cost of a combined mag/VLF survey by 500Xo. Regardless of line and station spacing, an IGS operator can survey approximately two-thirds as much as two operators on two in struments. In addition, with our in- house computer and plotting facilities, manual data entry is eliminated."

The above statements were all made by experienced exploration geophysicists and are documented in Scintrex' files.

Brief Description

The heart of the Scintrex Integrated Portable Geophysical System is the IGS-2 System Control Console. This in strument contains a powerful CMOS microprocessor, EPROM and RAM memory and peripheral electronics which permit a single operator to ex ecute three major functions. First, he can control a variety of sensors, either individually or in combination. Second, at the push of a button, he can record data in solid-state memory. Then, at the end of a day's surveying, he can use the IGS-2 to playback, calculate, list and plot data on a simple digital printer, often to report level quality.

To perform ground geophysical surveys, the IGS-2 System Control Con sole is complemented by especially designed IGS Sensor Options which permit the IGS-2 to become a magnetometer, a VLF receiver, an EM receiver or combinations of these. Each of these Sensor Options com prises an external sensor as well as electronic circuit boards and software program EPROMS which may be in stalled inside an IGS-2 console either at the Scintrex plant or by the end user.

The IGS-2/MP-4 combination is used as a Pro ton Magnetometer with portable, base station and mobile survey applications

The EM-4 Sensor Option permits the IGS-2 to make both Genie and Horizontal Loop elec tromagnetic measurements.

When the VLF-4 Sensor Option is added to the IGS-2. the result is an advanced VLF EM Receiver.



Common Features 0*35-2, M P-3 and VLF-3 Instrumentation

well as hour, minute and second. It is accurate to one second over 12 hours over the full operating range of the in strument. It is easily reset, if required. Time can be shown on the display, after two keystrokes.

Records header information. At the beginning of a survey, or of a day of surveying, header information such as: 1) instrument serial number, 2) grid number, 3) job number, 4) date and 5) operator code can be entered. When data are output, this header informa tion is repeated at the beginning of the data list or profile for each line, to en sure that all data are properly and unambiguously labelled.

Accepts ancillary data. In addition to automatically recorded geophysical parameters such as magnetometer and VLF values, a great deal of ancillary data can be manually entered. Such data is entered in up to eight blocks of up to five digit, signed decimal numbers.

Recalls data. By keystroke entry, any recorded value can be called up on the display. For example, over an anomaly it might be useful to compare values recorded on an adjacent line. To do this, the operator enters the adjacent line and station numbers and depresses a memory key. Instantly, the recalled value appears on the lower line of the display. Once one value is recall ed, he can move up or down the line recalling data, station by station, with a single keystroke per station.

Permits revision of data. It is notnecessary to record every measured value. Several readings can be taken before one is selected for recording. Alternatively, more than one value can be recorded with identical coordinates at different times.

To change information already in the memory, the Edit Mode can be used to change line and station numbers or header data. If it is desired to repeat a measurement, a new reading can be recorded and the old one deleted.

Outputs to many peripheral devices. The RS-232C port plus keypad selec table baud rates and carriage return delays, permit data to be output to many commonly available devices. A

digital printer can be used to print data as listings or as profile plots. A modern can be used to transmit data to head office via a telephone line or a magnetic tape recorder can store data for future computer processing.

Data can be output directly into por table microcomputers so that data ar chiving on floppy disk or additional processing can be done in the field. Some microcomputers with which the IGS-2, MP-3 and VLF-3 have been inter faced include Apple Ile, Apple III, Osborne, IBM PC, HP-85, Corona and Compaq. Several data dumps can be made sequentially from the memory.

Simple, automatic field plots. To plot data in the field you do not need a computer. A printer is all that is re quired to output header information as well as data listings or profile plots. This immediate, error-free output enhances in-field quality control and saves time and effort, compared to manual data compilation.

Organizes data. When data are output, whether as listings or profiles, they are first sorted by grid number, then in order of increasing line number and, within each line, by increasing station number. In this way the data are pro perly organized, regardless of the se quence in which they were taken, for easy comparison. For example, printer output profiles can be easily 'stacked' by placing them side by side.

Four power supply options. For base station applications, an IGS-2, MP-3 or VLF-3 can be powered from a 12 V DC external source such as a vehicle bat tery or from a specially designed Heavy Duty Rechargeable Battery Pack with built-in charger. For portable applica tions, the Non-rechargeable Battery Pack includes a battery holder and 10 disposable C cell batteries. The Rechargeable Battery Pack is entirely non-magnetic and so is recommended for most magnetometer applications as well as for work at low temperatures.

When data are output to a cassette recorder, they are stored in a computer compatible medium lor future processing.

When pseudo-analog profiles are out put onto a printer, any two parameters can be selected for simultaneous plot printing. One of several full scale sen sitivities can be selected for each pro file. The scales can be either zero centered or have their zero at the left- hand side of the space allotted to the profile. In the profile displays, the ac tual station numbers and data values are also printed numerically.

In some cases, these digital printer outputs may be sufficient for presenta tion in reports, eliminating the expense of further data processing or drafting.

Fail-safe power supply. The battery voltage can be checked anytime to be sure that there is enough power left. When the batteries are almost ex hausted, a warning indicator will ap pear on the display during a measure ment. If the batteries are not replaced or recharged, then the instrument will eventually stop measuring in order to eliminate the chance of corrupted data being measured and recorded.

Wide operating temperature range. Allspecifications are met over the range -40 0 C to + 50 0 C. For use below -20 0 C the Display Heater Option, Recharge able Battery Pack and Low Temperature Battery Extender Kit should be used.

System Options and Accessories

222 Snidercroft Road Concord Ontario Canada L4K 1B5

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

A. Console and Power Supply

A-1 IGS-2 System Control Console with 16K RAM memory and manual. Note that no battery pack is included so that one of items A-2, A-3 or A-4 should be selected unless the IGS is to be run from an external 12 V DC power source. The battery packs are interchangeable by the user.

A-2 Non-rechargeable Battery Pack in cludes battery holder and 10 disposable 'C' cell batteries. Used in normal portable operation unless temperatures are below -20 0 C in which case the Rechargeable Battery Pack and Charger should be chosen.

A-3 Rechargeable Battery Pack and Charger includes battery holder, 6 rechargeable non-magnetic batteries, charger and one spare cap for the bat tery charging plug. This is the best battery pack for portable total field and gradiometer magnetics since the non-magnetic property of these bat teries ensures a minimum of noise. Also used for light duty (slow cycling) magnetic base station applications and in cold weather where disposable batteries lose power.

A-4 Heavy Duty Rechargeable Battery Pack includes heavy duty recharge able batteries installed in a console with a built-in charger. Useful for rapid cycling base station or mobile applications.

A-5 Low Temperature Battery Extender Kit designed so that battery pack can be worn inside coat in cold weather conditions. Kit includes bottom cover for console, console to battery pack interconnecting cable, cover for bat tery pack and waist belt.

B. Memory Expansion Options

B-1 IGS Memory Expansion l. An addi tional 16K RAM is added to the ex isting memory board for a system total of 32K RAM.

B-2 IGS Memory Expansion II. A further 16K RAM is added to the existing memory board for a system total of 48K RAM.

B-3 IGS Memory Expansion III. An addi tional board is required on which memory can be added in up to six 16K RAM groups. Not available with all sensor options.

B-4 Further Memory Expansion. Memory expansion to a system total of 192K RAM is feasible for some applica tions.

C. Accessories

C-1 RS-232 Cable and Adaptors. Includes a special RS-232 data transfer cable and two IGS-2 to RS-232 cable adap tors. Used for communicating bet ween the IGS-2 and peripheral devices such as a digital printer, microcomputer, cassette recorder, modern or a second IGS-2 (or MP-3 Proton Magnetometer) for diurnal corrections.

C-2 Minor Spare Parts Kit consisting of two keyboard diaphragms and two 2A quick acting fuses.

C-3 Display Heater Option. Required to heat the LCD display on the IGS-2 Console for operation at temperatures below -20 0 C.

C-4 Digital Printer for use with 110 V AC power supply and with X-on/X-off interfacing for use with IGS-2, MP-3 or VLF-3 instruments, one box of paper, ribbon and manual. Note that the RS-232 Cable and Adaptor are re quired.

C-5 Conversion of Digital Printer for use with 220 V AC power supply.

D. MP-4 Proton Magnetometer Sensor Option

D-1 MP-4 Magnetometer Signal Process ing Board and Magnetometer Pro gram EPROM for mounting in IGS-2 Control Console, manual.

D-2 Portable Total Field Sensor Option including sensor for total field measurements, sensor staff, two sen sor cable assemblies, backpack sen sor harness, spare non-magnetic sensor clamp screw.

D-3 Base Station Sensor Option, in cluding 50 m sensor cable assembly, sensor for total field measurements, sensor tripod, external power cable, analog chart recorder cable and spare non-magnetic sensor clamp screw.

D-4 Gradiometer Sensor Option including second sensor cables, two 0.5 m staff extenders to complement Portable Sensor Option and spare non magnetic sensor clamp screw.

D-5 Spare section for Portable Total Field Sensor Staff (0.5 m length).

E. VLF-4 VLF Electromagnetic Sensor Option

E-1 Two VLF-4 Signal Processing Boards and VLF program EPROM for mount ing inside IGS-2 System Control Con sole, dual coil VLF-magnetic field sensor with level compensator, sensor-console interconnecting cable, harness and support for back mount ing of sensor, manual.

E-2 VLF EM Primary Field Drift Correction Option consisting of two program EPROMS which replace the standard VLF program EPROMS in each of the portable and base station VLF units.

E-3 VLF Electric Field Sensor Option for VLF resistivity measurements. In cludes two capacitive electrodes with integral preamplifiers and 5 m of cable. Longer cable lengths on request.

F. EM-4 Genie/Horizontal Loop Electromagnetic Sensor Option

F-1 Two EM-4 Signal Processing Boards for mounting either inside IGS-2 System Control Console or the EM-4 Genie/Horizontal Loop Expansion Module, one program EPROM for mounting inside IGS-2, one receive coil, one interconnecting cable, manual.

F-2 EM-4 Tiltmeter/lntercom Module. Per mits Horizontal Loop measurements to be made with magnetics but without VLF.

F-3 EM-4 Genie/Horizontal Loop Expan sion Module. Permits Horizontal Loop measurements to be made with both magnetics and VLF.

F-4 Genie/Horizontal Loop Portable Elec tromagnetic Transmitter complete with heavy duty battery pack, battery charger, manual.

F-5 TM-2 Tiltmeter/lntercom Module used with TM-2 when Horizontal Loop measurements are to be made.

F-6 Transmitter-Receiver Interconnecting Cables for Horizontal Loop measure ments are made to order, in any lengths up to 300m.

G. Carrying Cases

A variety of carrying cases are available to suit different combinations of console and sensor options.


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— ._J Lir-

u Five frequencies: 222, 444, BBS, 1777 and 3555 Hz.b Maximum coupled C horizontal-loop l operation with

reference cable.u Minimum coupled operation with reference cable. k Vertical-loop operation without reference cable.k Coil separations: 25, 50,100,150, SOO and SSOm

C with cable 3 or 1OO, 200,300,400, BOO and BOO ft.LI Reliable data from depths of up to ISO m CBOOft}.y Built-in voice communication circuitry with cable,b Tilt meters to control coil orientation.

SPECIFICATIONS :

Frequencies: 222. 444. BBS, 1777 and 3535Hz.

Modes of Operdc ion: MAX: Tranamittep coil plane and re ceiver coil plane horizontal [Max-coupled ; Horizontal-loop mode). Used with refer, cable .

M IN: Transmitter coil plans horizon tal and receiver coil plane ver tical (Min- coupled mode). Used with reference cable .Transmitter coil plane verti cal and receiver coil plane hori zontal t Vertical -loop mode). Used without reference cable , in parallel linea.

Coil Separationt.:

Paramo Lor t.

Reudoutt.:

Scale Ranget. :

NOW ALSO i QUADRATURE FULL SCALE.

Readability :

V. L.

25.50.100.150,200 S 25Om l or 1OO. 2OO. 3OO, 4OO,6OOand BOO ft. (MMnF). Coil separations in VL.mode not re stricted to fixed values.

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

- Tilt-angle of the total field in V.L. mode .

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

- Tilt angle and null in SO mm edge- wiae meters in VL.mode .

In-Phase: *2OV..*1CX^ by push button switch .

Quadrature: ±2O If,, 1 1OOV. by push button switch.

Tilt: 175V. slope.NulKVLJ: Sensitivity adjustable

by separation switch.

Trunumittur

Voice Uink :

Indicator Lights:

Receivur

iO.25'/.tollVo normally, depending on conditions, frequencies and coil separation used .

: - 222HZ : 22O Atm2- 4 44 Hz : SCO Atm2- BBBHz i 12OAtm2- 1777Hz : BOAtm2-3555 Hz s 3D Atm2

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

12V 6 Ah Gel- type rechargeable battery. tCharger supplied)

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

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lBuilt-in intercom system for. voice communication between re j ceiver and transmitter operators L In MAX end MIN modes, via re ference cable .

Built-in signal end reference wam-l ing lights to indicate erroneous' readings .

: -4O'C tO+BO'C C-

: Skg (13 Ibs.)

Trtinbmitter Weigiit: 13kg (2SlbS.)

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

In-Phase and Quadrature : O.S5 V.to 0 .5 V. ; Tilt: 1V. . Specifications subject to cnano.e without notificetior

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iP A RI A M t^ T ft l C S 1.1 nil i'f B DeOO STEELCXXS6 RD. E., MARKHAM. ONT.. CANADA. L3R

liPhone: (416) 495-1618 Cables: APEXPARA TORONTO

l l l• Appendix 2

Plates, scale I"r200' (1:2400)

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West Grid

Plate la: Total Field Magnetics Contours

Plate l b: Total Field Magnetics Profiles


l Plate 2b: Fraser Filtered VLF Cutler 24.0kHz

Plate 3a: HLEM Profiles 888Hz, c.s.r400ft

l Plate 3b: HLEM Profiles 1777Hz, c.s.r400ft


East Grid

l Plate 5a: Total Field Magnetics Contours

Plate 5b: Total Field Magnetics Profiles

l Plate 6a: VLF-EM Profiles - Cutler 24.0kHz

— Plate 6b: Fraser Filtered VLF Cutler 24.0kHz

" Plate 7a: HLEM Profiles 888Hz, c.s.r200ft

l Plate 7b: HLEM Profiles 1777Hz, c.s.r200ft


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ntario 43oasNE99aa 2 .14777 SPRINGER LAKE 900

Ministry of Ministere du Geoscience Approvals section Northern Development D6veioppement du Nord g^ Miner Centre and Mines et des Mines 9 33 Ramsey Lake Rd., 6th Fir

Sudbury, OntarioP3E 6B5

Telephone: (705) 670-5853 Fax: (705) 670-5863

December 11, 1992

Our File: 2.14777 Transaction #: W9240.195

W9240.196

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

Dear Sir

RE: Approval of Assessment Work on mining claims TB 1133764 et al. in th* Springer Lake Area.

The assessment credits for geophysics, section 14 of the Mining Act Regulations, as listed on the original Report of Work, have been approved as of December 9, 1992.

If you have any questions concerning this matter please contact Dale Messenger at (705) 670-5858.

Yours sincerely,

Ron C. GashinskiSenior Manager, Mining LandsMines and Minerals Division

ONTARIO GEOLOGICAL SURVEYGIS-ASSESSMENT HIES

JAN l j 1993

Branc i RECEIVED

nclosures:

cc: ^/Assessment Files Office Toronto, Ontario

Resident Geologist Thunder Bay, Ontario

Ministry ofNorthern Development

Mine*Ontario

Report of Work Conducted After Recording Claim

Mining Act

Transaction Number

•*f*on*J Information collected on trds form Is obtained under trie authority of the Mlnlr^Me collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street..udbury, Ontario, P3E SA5, telephone (705) S70-7264.

O^ *nstructlona: - Please type or print and submit In duplicate.- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining

Recorder.- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form In duplicate.- A sketch, showing the claims the work Is assigned to, must accompany this form.

/Yortc Performed (Check One Work Group Only)Work Group

V ^Geotechnical SurveyPhysical Work, Including Drilling

RehabilitationOther Authorized Work

AssaysAssignment from Reserve

Type

hft^*L-iYc s, vLl^tfl a^J t""lrfy^1'"TT Sofi^ys

RECEIVEDI I tvm^^tmml ~*

NOV 2 - 1992

MINING LANDS BRANCH

Total Assessment Work Claimed on the Attached Statement of Costs lit^ote: The Minister may reject for assessment work credit all or part of the assessment work submitted If the recorded

holder cannot verify expenditures claimed In the statement of costs within 30 days of a request for verification.

'arsons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address

JVV L-fet Ji/U4

(attach a schedule H necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse sidel certify that at the time the work was performed, the claims covered In this work report were recorded In the current holder's name or held under a beneficial Interest by the current recorded holder. __ ^^^^

Date Recorded Holder or

Certification of Work Report1 certify that 1 have a personal knowledge of the facts set forth In this Work report, having performed the work or witnessed same during and/or after tt* completion and annexed report Is true.

Nam*.and Addrsst of Person Certifying

Tetepone No.

?o 7-Date Certmed

For Office Uae OnlyTotal Value Cr. Recorded Date Recorded

ffi t* 11/92- .Deemtd Approval Date

Mining Recorder ^

Dst* Approved

Dst* Notice for Amendments Sent

Received StampGhOTUU hi .10026,

;.":- ? SIAIG e?"::' 1/:.'.'.'G U3(l'| : ;..l.

3241 (OOT1)

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) ^ O (T

Note 2)

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edits

you

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claim

ing

in th

is re

port

may

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cut b

ack.

In or

der t

o m

inim

ize th

e ad

vers

e ef

fects

of s

uch

delet

ions,

pleas

e In

dicat

e fro

m

which

clai

ms

you

wish

to p

rioriz

e th

e de

letion

of c

redit

s. Pl

ease

mar

k (^

) on

e of

the

follo

wing

:1.

D C

redit

s ar

e to

be

cut b

ack

starti

ng w

ith th

e cla

im li

sted

last,

work

ing b

ackw

ards

.2.

[^C

redi

ts a

re to

be

cut b

ack

equa

lly o

ver a

ll cla

ims

cont

ained

In th

is re

port

of w

ork.

3. D

Cre

dits

are

to b

e cu

t bac

k as

prlo

rized

on

the

atta

ched

app

endix

.

In th

e ev

ent t

hat y

ou h

ave

not s

pecif

ied y

our c

hoice

of p

riorit

y, op

tion

on* w

ill b*

Imple

men

ted.

Note

1:

Exam

ple*

of b

enef

icial

Inte

rest

are u

nrec

orde

d tra

nsfe

rs, o

ptio

n agr

eem

ent*,

mem

oran

dum

of ag

reem

ent*,

etc.,

with

resp

ect

to th

e m

inin

g cl

aim

*.

Note

2:

If wo

rk h

a* b

een

perfo

rmed

on

pate

nted

or l

ease

d lan

d, p

lea*

* com

plet

e th

e fo

llowi

ng:

l cer

tify

that

the

reco

rded

hol

der h

ad a

ben

efici

al In

tere

st In

the

pate

nted

or

iMM

d te

nd a

t th*

tim

e in

* wo

rfc W

M p

erfo

rmed

.Si

gnat

ure

Date

Report of Work Conducted After Recording Claim

Mining Act

Transaction Number

/A)

Ministry o*Northern Development

•Mint* .

•ersonal Information collected on this form Is obtained under the authority of the Mining Act. This Informatkw win be ueed for corresporKkrKe.Chiesttons about its eotactton should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 1M Cedar Street, '.udbury, Ontario, P3E 6A5. telephone (70S) 670-7264.

nstructlona: - Please type or print and submit In duplicate. Q ^ J. T: C C C- Refer to the Mining Act and Regulations for requirements of ftnflg assessment work or consult the Mining

Recorder.- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work Is assigned to, must accompany this form.

Work Performed (Check One Work Group Only)

V

Work Group

Geotechnical Survey.physical Work, Including Drilling

RehabilitationOther Authorized Work

AssaysAssignment from Reserve

Type

/FOJLrmcvffi**. REC&-

^40* "v,f\G Rf\AN^

w\uu

s 2-;//y 3.Total Assessment Work Claimed on the Attached Statement of Coststote: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded

holder cannot verify expenditures claimed In the statement of costs within 30 days of a request for verification.

'ersona and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address'

ZcCo*

attach a schedule If necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse sidel certify that at the time the work was performed, the claims covered In this work report were recorded In the current holder's name or held under a beneficial Interest by the current recorded holder.

Date Recorded Holder or Agent (Signature)

*fr-

^rtlfleaUon of Work Reportl certify that l have a personal knowledge of the facts set forth In this Work report, having performed the work or witnessed same during and/or after Its completion and annexed report Is true.

Name and Address of Pereon Certifying

R ^. 0^.TeleponeNo.

For OWc* UM OnlyTotal Value Cr. Recoraea Dan Recorded

21

eM1(OMI)

Deemed Approval Date

Date Notice for Amendmenti Sent

Mining Recorder

Data Approved

""""" "GrTniuu HI 10026,

^

' fi ir i fi ir r| to* * '* w* l C* C o

l

f

- ' ;

•' *

't^

.

s' •^

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III* iilr

s*. l* N

^ i

SS t ^^ r0

^ *r * vj^

^^ I

W ^ P-

Cred

its y

ou a

re cl

aiming

in th

is re

port

may

be c

ut b

ack.

In or

der t

o m

inim

ize th

e ad

vers

e ef

fects

of s

uch

delet

ions,

pleas

e In

dicat

e fro

m

which

cla

ims

you

wish

to p

rioriz

e th

e de

letion

of c

redit

s. Pl

ease

mar

k (**

) one

of t

he fo

llowi

ng:

1. D

Cre

dits

are

to b

e cu

t bac

k sta

rting

wtth

the

claim

liste

d las

t, wo

rking

bac

kwar

ds.

2. Ga

Cre

dits

are

to b

e cu

t bac

k eq

ually

ove

r all c

laim

s co

ntain

ed In

this

repo

rt of

wor

k.3.

D C

redi

ts a

re to

be

cut b

ack

as p

rioriz

ed o

n th

e at

tach

ed a

ppen

dix.

In th

e ev

ent t

hat y

ou h

ave

not s

pecif

ied y

our c

hoice

of p

riorit

y, op

tion

one

will

be Im

plem

ente

d.

Note

1:

Exam

ples

of be

nefic

ial In

tere

st ar

e unr

ecor

ded

trans

fers

, opt

ion

agre

emen

ts, m

emor

andu

m o

f agr

eem

ents

, etc

., wtth

resp

ect

to th

e m

inin

g cl

aim

*.

Note

2:

If wo

rk h

as b

een

perfo

rmed

on

pate

nted

or t

ease

d lan

d, p

lease

com

plet

e th

e fo

llowi

ng:

l cer

tify th

at th

e re

cord

ed h

older

had

a b

enef

icial

Inter

act I

n th

e pa

tent

ed

or iM

Md

land

at th

e tim

e th

e wo

rk wa

s pe

rform

ed.

Sign

ature

Date

Ontario

•Ministry ofNorthern Developmentand Mine*

dulopp*ment du Nord

et dea mines

Statement of Costs for Assessment Creditl-tat des coOts aux fins du credit d'e valuation

Mining Act/Lol sur le* mines

Transaction NoJN* de transaction

Personal Information collected on this form la obtained under the authority of the Mining Act. This Information will be used to maintain a record and ongoing status of the mining clalm(s). Question* about this collection should be directed to the Provincial Manager, Minings Lands, Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5. telephone (705) 670-7264.

Lea renselgnements personnel* content)* dan* la present* formule sent recuelllls en vertu de la Lot aur tea mine* et aervlront a tenir A (our un reglstre des concessions mlnieres. Adre*ser toute queslton sur la codec* d* ces renseignements au chef provincial des terrains mlnlers, minister* du Developpement du Nord et des Mine*, 159, rue Cedar, 4* etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Direct Costs/Gouts directs

Type

Wage* SelaJrea

Contractor'* and Consultant'* Fee* Drottede ('entrepreneur et de ('expert-ntinmmMvQnavn

8uppne*U*ed FoumHure* irtttlae**

Equipment Rental Location de materiel

Description

Labour Main-d'oeuvreField Supervision Supervision sur le terrain

TypV JS /-meLiftiin.*

(^Cupl^U^S ^

Typ*

Typ*

Amount Montant

^/,*fn.2/i, (tic

Total Direct Coat** Total de* coOt* directs

Totals Total global

-*\ lv*

31,4^1,*:

2. Indirect Costs/CoOts Indlrects* * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work. Pour le remboursement des travaux de rehabilitation, tes coOts irtdirects ne sent pas admissible* en tant que travaux d'evaluation.

Type

Transportation Transport

Food and Lodging Nourrttur* *t htbergementMobilization end Demobilization Mobilisation et demobilisation

Description Amount Montant

Typ*

REOPr fcr^

——— mnr-

MINING LAND

TV "'C f- Ak4

A4V cUrt"

wz

Totals Total global

3BRANOH

?4, tt.-*

Sub Total of Indirect Costs Total partial des eouts Indirect*

Amount Allowable (not greater than 20H of Direct Costs) Montant admissible (n'excMant pa* 20 M de* coots direct*)Total Velu* of As*e**m*nt Credit Vileur total* du credit 1 (Total of Direct and Allowable devaluation indirect costs) (Total d** eoOto aVeets

M Mkwtt admlMMM

^tJH.^J

&W.11^<,ti *r)

^^'f

Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.

Note : Le titulaire enregistre sera tenu de verifier tes depenses demandees dans le present etat des coOts dans las 30 jours suivant une demande a cet effet. Si la verification n'est pas effectuee, le ministre peut rejeter tout ou une partie des travaux d'evaluation preserves.

Filing Discounts

1 . Work filed within two years of completion is claimed at the above Total Value of Assessment Credit.

of

2. Work filed three, four or five years after completion Is claimed at SQto of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimedx 0.50 -

Remlaes pour dtpotcr

1. Les travaux deposes dans les deux ans stmjant leur achevement sontrembourses a 100 4b de la valeur totate susmeotkxtnee du credit d'evaluation.

—^ —. .::

2. Les travaux deposes trois, quatre ou cinq t^ aprf/s leur pchevement sont rembourses a 50 to de la valeur totale du^Alij devaluation susmentionne. Voir les calculs ci-dessousS -r cr r '.

Valeur total* du credit d'evaluation EtatbatiorT to(B* damandeex 0,50 -

Certificatlon Verifying Statement of Costs

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

(^•corded Ho)d*r7Ag*nt, Position In Company)

to make this certification

Attestation de I'etat des coOts

J'atteste par la presente :que les montants indiques sont le plus exact possible et que ces depenses ont etd engagers pour effectuer les travaux d'evaluation sur les terrains indiques dans la formule de rapport de travail ci-joint.

l am authorized Et qu'ajitre de je suis autorise(tltulalr* *nr*gl*tr*, r*pr***ntant, post* occupi dent l* compagni*)

a faire cette attestation.

0212 (04/91) Nota : Dans c*tt* formul*. torsqu'll d**lo.n* d** persBrmes, l* masculin *st utilise au sans neutr*.

ioi oO)

O)J*o-JE(D

Q. O

87*45' e??3o'

52030'-

87045

n^n—'1149^30

1133767——— ——J M, .___ ————

1133764

f 1145244 1145205.—-1145243

j o i fi -* -* rt. A if* i*iiT^- J m n TiVi- i v i v t l M— l U i JP J J ^L. i Ml "J l U l- J- " — ~~~~ — — '— — "H" — r—' "n

-520 30'

ALDRED LAKE G-188

'30

CDro

lO (D

o; ^cD -J

C CD?O

Sob K . Blow-up

S

LEGENDHIGHWAY AND R OUTE N o

OTHER fUJADS

TRAILS

TOWNSHIPS, B ASE LINES, ETCLOTS. MINING CI AIMS, P ARCELS, ETC

UNSURVFYFH l INES

l OT LINfcSPA R Tt L BCtiNDARYMINING CLAIMS f TC

RA.; A AY AN:I RIGHT OF WAY

UTILIT t LINES

NUN Pt RF. NNIAt STREAM

FLOODING OR FLOODING RIGHTS

SUBDIVISION OR COMPOSITE PLAN

RESERVATIONS

ORIGINAL SHORELINE

MARSH OH MUSKEG

MtNFS

TRAVERSE MONUMENT

-~^j^

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOL

PATENT, SURFACE Si M INING RIGHTS.... ,.

, SURFACE RIGHTS ONLY. ...^ . ,. ...

, MINING RIGHTS ONLY ,. .. . . . . . ..LEASE, SURFACE 8t M INING RIGHTS, .

" , SURFACE RtGHTSONLY........ . . . .

" , MINING RIGHTSONLY...^,... ... . .

LICENCE OF OCCUPATION ^.... .,.. . .... ... . .... ..ORDER IN COUNCIL .... . ... .... .

RESERVATION .^.... . . . .CANCELLED ....

SAND&GRAVEL . .. .....,..... ....... . .. . .LAND USE PHRM'TS F OR COMMERCIAL TOURI3M.OOTPOST CAMPS

NOTE M INING HiTiHlS IN P ARCELS P ATENTED **RIOR TO MAY fc 1913. VtSTEO IN ORIGINAL PATENTEE Bv THK PUBMC LANDS ACT R5O 1970. C HAP 380. S EC 63.

H

B

0

T

OC

W ®

SCALE: 1 INCH 40 CHAINS

'000 AHJO -U10O tiOOO 80 OO

100O i KM 1 \7 K M

AREA

SPRINGER LAKEMN R ADMINISTRATIVE DISTRICT

GERALDTONMINING DIVISION

THUNDER BAYLAND TITLES/ REGISTRY DIVISION

KENORA/PATRICIA PORTION

Ministryof LandNatural Managnmetit

Resources BranchOntario

N ii m h

G-413

43D05NE9902 2. l 4777 SPRINGER LAKE S00

5600 N

5600 N

540D N

5200 N

5000 N

4800 M

4600 N

4400 N

4200 N

4000 N

3800 N

3600 N

3400 N

3200 N

3000 N

2600 N

2600 N

2400 N

oD O

O O O

43DB5NE99fc2 2 .14777 SPRINGER LAKE

O O en m

o o(Oro

oD

O O IDm

o o ir? en

o o

oD COen

o oCMro

o o

o oCOon

o oOD

o t—m

o oIDm

oDLOrn

o o m m

oD CMen

o o o m

oo en

o oODeg

o o r-CSJ

oD

D OinCvj

DotSJ

a o enCM

a aCM

D O

O OoCM

OoCD

O O CO

O O

a a m

o oCM

O D

O Or-

o oCD

O O LO

5800 N

56GO N

5400 N

S200

5000 N

4800 N

4600 N

44DD N

4200 N

4000 N

3800 N

3600 N

3400 N

3200 N

3000 N

280D N

2600 N

2400 N

2.14777

KWG RESOURCES INCLAVOIE LAKE PROJECT


TOTAL FILED MAGNETIC CONTOURSCONTOUR INTERVALS : 50, 250, ft 1500 nT

GRID CELL SIZE : 20 ft * 20 ft RELATIVE CONTOUR LOW :

__________SCINTREX IGS-2/MP-4——^————-

SCALE 1:2400

SURVEY BYJVX LTD.

MAY 1992WEST GRID PLATE la

210

rt IE

0 D 0 0a m -r m

5800 N

5600 N

5400 N

5200 N

5000 N

4BOO N

4600 N

4400 N

4200 N

3000 N

2800 N

2600 N

2400 N

160

190

174

183

163

174

187

- 192

- 199

-- 239

- 299

- 295

284

224

195

- .7,

- IBS

102

- 182

155

151

150

146

- 142

- 143

' 139

148

161

175

194

208

208

201

203

202

229 l

2SB J

318 j

415 f

l W- SB*

- 551

- 479 \

- 443

*~ 972" — ——

331

314

-- 334

- 359

- 401

" 470

- 55* I

SOSJ

848J

BM

J

T- 81 1

' SI B

- K 3

si

1-- eil

- B9D

i"t

-- 139

•- 141

-. 150

•- 149

•- 170

-- 177

- 187

•- 194

•- 203

-- 21)

•- 214

•- 20B

•- 220

-. 224

-- 215

-- 202

-- 194

-- 183

-- IBS

•- 100

•- ISfl

-- 160

- 159

-- 159

-- 162

•- 185

- 183

•- 170

•- 187

-- 220

- 222

- 207

- 212

-- 208

•- 219

•- 234

.-273

-- 314

-- 409

- 49 1/

•- Si l

- S 4

•- 4

- 3!

-- /30—

- i 359

\. 377\

•- 381

-- 393

-- 455

-J

•- 5 1BJ

•- 5881

- 6lJ

-J

- HSJ

-- ssi

- si

•- BM

-.1

1- 61*"i"l

-•638 3

o a enrn

1 II

ooCOrn

o aa or- tom m

a oin m

o o CM m

o o

r~ rn

a o LD rn

a o in rn

o oo am CMro m

o a o m

o enC\J

o oOD CM

OO

o oOD Osl

D D LT) CM

O O

D Oo aCO CMt\j eg

a o

CD O

"- O CM CM

O Den

a aCO

o o

a c m

aD CNJ

Oo r-

o oCD

a oin

m rht hr nth**

5800 N

5600 N

5400 N

5200 N

5000 N

4800 N

4600 N

4400 N

4200 N

4000 N

3800 N

3600 N

3400 N

32QQ N

3000 N

2800 N

2600 N


UNSDOWNE HOUSE AREA Northwestern Ontario

2400

TOTAL FIELD MAGNETICS PROFILESBASE VALUE : 2000 nT

PROFILE SCALE : l in - 2000 nTPOSITIVE PROFILE DIRECTION : WEST

SCINTREX IGS-2/MP-4

SCALE I:a400

SURVEY BYJVX LTD.

MAY 1992WEST GRID P1ATE . 1 b

43D05NE9902 2.54777 SPRINGER LAKE 220

DOo

o o m m

o aCO (O

o o r- m

o ID en

o a in en

o o -t rn

o o en en

o o(Nlrn

o o

5800 N

5600 N

5400 N

5200 N

5000 N

480Q N

4600 N

4400 N

4200 N

4000 N

3800 N

3600 N

3400 N

32QQ N

3000 N

2800 N

2600 N

2400 N

" 71 -If S l - li * l -|0 B

7 l ''l '13' -I 4 IS/ it 15 l 1 rt l '7

V a/Vu it.l-n M

' r 'y' ' Yt 0 -- K , 31

-l -rf -l -l*/ lV -IS ' l

-M -10 - ' -\ -4 4\ -U - S

\: l '\ \ h -"f/--"'i tli .B . Jl) ^J .1,15 l J

1 \ '-2 If - 16 '-3 -N-1S ' l

D O CD CO

O O COen

o o r-cn

o o

oD

o o

o of"ri

o o CM

Do

o o o on

o mCsJ

oD OD

o oCsJ

o oCD (N

O O LD Csj

Oa

o a m

o o CsJ

ooCM

O O OOJ

d CD 05

O O CO

o o o

CO

ooC\j

o o

o o

o oOD

o oLD

o o o

5800 N

5600 N

5400 N

5200 N

5000 N

4800 N

4600 N

4400

4200 N

4000 N

3800 N

__3600 N

3400 N

3200 N

3000 N

2. l2800 N

2600 N

2400 N


LANSDOWNE HOUSK AREA Northwestern Ontario

VLF-EM PROFILES, 24.0 kHzVLF STATION : NAA (Cutler, Maine)

PROFILE SCALE : l in - 50 7.POSITIVE PROFILE DIRECTION : WEST

_______SCINTREX IGS-2/VLF-4______

SCALE 1:2400

SURVEY BYJVX LTD.

MAY 1992m fM kr A** Vtafevt.

43DeSWE99B2 2.14777 SPRINGER LAKE

WEST GRID PLATE 2 a

230

o oo oO CD-W ro

O OO OCD r-(T) CO

o o toIT)

o aLDrn

D O

o oro ro

o oCSJcr.

DD

5800 N

5600 N

5400 N

5200 N

5000 N

4800 N

4600 N

4400 N

4200 N

40QO N

3800 N

3500 N

3400 N

3200 N

3000 N

2800 N

2600

2400 No o oa o om CD r-en m en

o o to en

o oLO CO

o o "1-co

o o p-) ro

o oCMen

o oa o orn m

o o en CM

o aODCM

O Or-CM

o oCO (M

o oIT) CM

D O

Csl OJ

oCD

tXJ

DO O (M

Om

o oCO

o o

o CDCM

oo

Do r-

CD O

O O LT)

O O O

5800 N

5600 N

5400 N

5200 N

5000 N

4800 N

460G N

4400 N

4200 N

4000 N

3800 N

3600 N

340C N

3200 N

3000 N

2800 N

2600 N

2400

2.



FRASER FILTERED VLF, 24.0 kHzVLF STATION : NAA (Cutler, Maine) CONTOUR INTERVALS : 5, 25 units

CONTOURED POSTIVE VALUES ^________SCINTREX IGS-3/VLF-4.,——-.-————

SCALE 1:2400

SURVEY BYJVX LTD.

MAY 1992WEST GRID PLATE 2 b

43Dd5NE99aa 2.14777 SPRINGER LAKE 240

oDin m

o ^*rn

56DQ M

5400 N

5200 W

5000 N

4800

4600 M

4400 N

4200 N

4DDO M

3800

3600 M

3400 N

3200 M

3000 N

2800

2600 N

srr s

o oO Dt- IDrn m

o o

o o (M

o o o

o o03

Q O CD

o a

a a

o oCSJ

o oc\j

CDO

a oCO

a a to

5600 N

5400

5200 N

5QOQ M

4800 N

4600 M

44DO

42QO N

4000 M

3800

3600 LEGEND

Conductivity thickness (6"t) in Siemens

3400

3200 N

3000 M

?800 N

2600

KWG RESOURCES INC.LAVOIE IAKE PROJECT


HLEM PROFILES, 888 HzCOIL SEPARATION (Tx-Rx) : 400 ft

PROFILE SCALE ; l in - 75 70POSITIVE PROFILE DIRECTION : WEST

APEX MaxMin II

SCALE 1 :2400

SURVEY BYJVX LTD.

MAY 1992WEST GRID PLATE 3 a

43D95NE9902 2 .14777 SPRINGER LAKE 250

5600 N

5400 N

52QD M

5000 M

48DD M

4600 M

440Q M

4200 N

4000 M

3800 N

3600

3400 M

3QCO N

23QQ N

2600 N

1 43D95NE9902 2 .14777 SPRINGER LAKE m*

Oo

OoUDm

260

o o

-trn

o a CD CM

a o toCM

oD

Oo m CM

o oIN (M

O O

O O O CM

CD O CO

5600 N

5-400 N

5200 N

5QOQ N

4800 N

4600 N

4400 N

420G N

4QDD N

360D N

3600 N

3400 N

3200 N

o i 43000 N

2800 N

2600 NKWG RESOURCES INC

LAVOIE LAKE PROJECTLANSDOWNE HOUSE AREA

Northwestern OntarioHLEM PROFILES, 1777 Hz

COIL SEPARATION (Tx-Rx) : 400 ftPROFILE SCALE : l in - 75 ^

POSITIVE PROFILE DIRECTION : WESTAPEX MaxMin II

SCALE 1:2400

SURVEY BYJVX LTD.

MAY 1992WEST GRID PLATE 3 b

5800 N

56DO N

5400 N

5200 N

5000 N

4800 N

4400 N

4200 N

4000 N

3BOO N

3600 N

3400 N

3200 N

3000 N

2800 N

2600 N

2400 N

O OenCO

oCO

o or- ro

to rn

o o in rn

o oo o•w mm rn

aoCM

C 2 fone N

o oCDm

oOD

o in

o oin

o o

ro mo a

rn rn

a oa oo enn CM

r-(XI

a inCsJ

o otsjM

O CD

d CO

O O

o ar- o

LO

58DC N

5600 N

5400 N

5200 N

5000 N

40QO N

4400 N

4200 N

3BOO N

340C N

3200 N

2600 N

2400 N

LEGEND

Magnetic high

60,250nT

60,000 -60,250 nT

VLF - EM Conductors

Strong In phase 8 Reversed Out phase

Medium In phase

Medium Out phase

Weak In phase or Out phase

Max Mm Conductive Zone

VD-1

-—' Conductor width

Conductor axis

VLF Fraser filter conductor contour }

54010 Inco 1973 8 1974 drill hole

KWG April-May 1992 drill hole

( Ci to C3 and D1 to D7 )

Mineralization, vertical projection

COMPILATION MAP



GRID MAP

SCALE 1:3400

COMPILED BYJVX LTD.

KAY 1992WEST GRID PLATE 4

43D05NE9902 2 .14777 SPRINGER LAKE 2Z0

UJ(f)CD oCM

UJ (f)

Oa

UJ tooCDto

UJ 10

oCD

UJ CO

oCD CO

UJ CO

o o01

UJ CO

CD o o

UJ LO

D D

UJ CO

oCM

UJ LO

o o rn

UJ CO

o a

LUtoa a m

UJcoa oCO

UJtoa CD r-

UJtoo oCD

UJ CO

o o en

UJtoa a o(M

UJ LO

O O

CM

UJtoooCslCM

UJ CO

o oroCM

UJ CO

o o

UJtoOCDinCM

UJtoo oCD (SJ

UJ LO

o a r- CM

UJtoo oCOCM

UJ CO

o o enCM

UJtoo o oro

UJto

UJ LO

OoCMro

UJtoa o rnCO

UJto CO

o Q m en

UJcoo oCDm

UJcoO Dc-CO

UJtooCDCOro

UJ CO

Qa enrn

UJtoo o CD

1000 NE

600 WE

60D NE

400 NE

200 NE

BflSE LINE

200 SW

400 SW

BOO SW

800 SW

1000 SW

1200 SW

1400 SW

1500 SW

1800 SW

2000 SW

1000 NE

800 ME

BOO NE

4CO NE

200 NE

BRSE LIME

200 SW

400 SW

600 SW

800 SH

1000 SW

1200 SW

140Q SW

O

1600 SW

18QO SW

2000 SW

UJtoo a CM

UJ CO

CD O

UJ CO

a oCD

UJtoQ Or-

UJto oCDCO

UJtooo en

UJtoo a o

LUtoa o

UJtoo oCM

UJ CO

o o m

UJ CO

o CD UJ CO

CDo in

UJ CO

o o to

UJ CO

CD o r-

cu too aCO

Q Q CT)

UJ LO

Oa aCM

UJ CO

o o

UJ

oCD CM 00

UJ CO

oCImCM

UJ CO

a o

UJtoa o in CM

UJtoCD O CD CM

UJ CO

a o r-CM

UJ CO

oCD COCM

UJ LO

CD CDenCM

UJ CO

oCD Oen

UJtoo o

LU LO

Oa CM m

UJtoCD O CO CO

UJ CO

CD CD

UJ CO

CD Dm to

UJtoCD D CD CO

a o r- ro

UJLOo oCOro

UJ CO

oCDen to

CDo a-4-

43D05NE9902 3 ,14777 SPRINGER LAKE



TOTAL FIELD MAGNETICS CONTOURSCONTOUR INTERVALS : 100, 500, fc 2500 nT

GRID CELL SIZE : 20 ft * 20 ft RELATIVE CONTOUR LOW : V y SCINTREX ^^^

SCALE 1:2400

SURVEY BYJVX LTD.

MAY 1992EAST GRID PLATE 5 a

280

UJtoooC\J

UJ LJin coa oa o"f CD

UlCO

ooc-

LUCO

QaOD

LUtoaaCD

UJCO

ODO

UJCO

LU OCO O

CMO ™O

—

LUtoDOm

LUtoDD

—

LUCO

OOLO

LUtoOOCO

UJCO

oor-

UJtoooCO— -

UJCO

ooen—

LUCO

OooCNJ

LUCO

aa—— r

CM

LJtnooCNJCM

LUtooot1"!CM

UJCO

oo-t-CM

LUenooinCM

LUCO

OOCDCM

LJCO

Oor~CM

LUtoooCOCM

LUen

ooenCM

LUCO

DOOro

LUCO

oo— 'CO

LUCO

Oo(M01

UJCO

aaroro

LUCO

oo-1-cn

LUCO

ooLOen

LUtoOotom

LUCO

oor-rn

LJCO

CDoCOCO

LUCO

ooenCO

UJCO

ooo"^

1000 NE

800 NE

600 NE

400 NE

200 NE

BflSE LINE

200 SW

400 SW

5QQ SW

800 SN

000 SW

1200 SW

14QD SW

1600 SW

1800 SW

2GQO SW

o LUCO

oD OJ

tuCO

o o

o oCD

UJ CO

o o r~

LU CO

o oCD

IUtoa o m

LU CO

o o o

LUtoO D

LU Cn CO

DO

LU to

O CD

lU CO

O LO

LU o^

O O

LU co

O O

IJJ co

O O

LU co

D O

LU co

D O

LU co

D O

UJ to

O O

LU to

O O

uJ w

O O

Uj to

O O

uJ co

O D

Ld co

O O

LU co

O O

O O

LJ co

O O

Lu to

CD O

LJ co

LU co

D D

LU co

O O

LU to

O O

LU co

O a

LU co

O O

LU co

O D

LLJ co

D O

ljJ tn

O O

1000 NE

800 NE

600 NE

400 NE

200 NE

BflSE LINE

?00 SN

400 SW

600 5W

800 SW

1GOO SW

1?00 SW

14GG SH

l BOG SW

1800 SW

2000 SW



TOTAL FIELD MAGNETIC PROFILESBASE VALUE : 59500 nT

PROFILE SCALE : 1 in - 2000 nTPOSITIVE PROFILE DIRECTION - WEST

SCINTREX IGS-2/MP-4

SCALE 1 :2400

SURVEY BYJVX LTD.

MAY 199243D05NE9902 2 .14777 SPRINGER LAKE 230

EAST GRID PLATE 5 b

100D NE

600 NE

600 NE

400 NE

200 ME

BRSE LINE

200

400 SH

600 SH

800

1000

1200 SW

14CO SW

1600 SW

1800 SK

2000 SN

43Da5NE9902 2 .14777 SPRINGER L AKE

2

UJ CO

D D (XI

LU CO

LU CO

o oCD

LU CO

o o r-

LUCO

D CD

UJCO

tlJLO

oCD O

CD D

UJ LO

O O CM

UJen

o m

UJ CO

D o

LU LO

oLO

UJtno oLO

UJ LO

LUto

UJ LO

O DO Or- co

o o o

UJcoo o

UJ CD

LUtooD

LU LO

O D

UJ CO

D O

UJ CO

oD

UJ CO

UJ LO

D O

UJ CO

O O

LJ CO

O O

UJ CO

O O

UJ CO

oo

UJ LO

o o

UJ CO

o o

LU LO

O O

UJ LO

O O

UJ LO

O O

LU LO

O O ODen

LU CO

o o en en

LU LO

O CD D

1000 NE

800 NE

600 NE

400 N E

2DO Nt

BflSE LINE

200 SW

400 SW

BOO SW

800 SW

1000 SW

1200 SW

1400 SW

1600 SW

1800 SW

20DO SW



VLF-EM PROFILES, 24.0 kHzVLF STATION ; NAA (Cutler, Maine)

PROFILE SCALE : l in ^ 100 ?5POSITIVE PROFILE DIRECTION : WEST

_______SCINTREX 1GS-2/VLF-4^^^^

SCALE 1 :2400

SURVEY BYJVX LTD.

MAY 1992EAST GRID PLATE 6 a

300

10QQ NE

800 NE

600 NE

400 NE

200 NE

BRSE LINE

200 SW

1000 NE

800 NE

600 NE

400 NE

200 NE

BflSE LINE

200 SW

400 SW 400 SW

600 SW 600 SW

aoo sw 6DO SW

1000 SW

1200 SH

1400 SW

1600 SH

1800 SW

LU ino oCsJ

LU ID

O O

UJtoO O CO

UJ CO

O Or-

UJ CO

o oCO

LUtoo o en

LUto oDo

LUtoDo

o oCM

UJ LO

o o m

LU CO

oD

UJtoo oLTJ

UJtoo oLO

LUtoo o r-

LUtoo oCO

CDo en

UJ CO

o o o CM

UJtoo oCM

LUtoo oCM CM

UJ CO

o o enCsJ

LU CO

o o

LUCO

o oLD CSl

UJ

o oCD CM

LU CO

o o t-(M

LUtoooCD CM

a oO) CM

UJ CO

o o oCO

LUtooo

LUtoDoCsJm

LU CO

D DCO

LU CO

o a

LU10o oLOen

UJ CO

a a to m

LU CO

D Dr-ro

UJtoD D COm

UJ CO

a o ai m

LUtoD Do"t

43D85NE990a 2 .14777 SPRINGER LAKE 310



FRASER FILTERED VLF, 24.0 kHzVLF STATION : NAA (Cutler, Maine) CONTOUR INTERVALS : 5, 25 units

CONTOURED POSITIVE VALUES _________SCINTREX IGS-2/VLF-4————-—

SCALE 1:3400

SURVEY BYJVX LTD.

MAY 1992EAST GRID PUTE 6 b

BOO NE

BOO NE

4QO NE

200 NE

BflSE LINE

200 SH

400 SH

600 SH

800 SH

1000 SW

1200 SW

1400 SW

16DO SH

1800 SW

43D05NE9902 2 .14777 SPRINGER LAKE

UJ W

Oo UJin

UJto

UJino oD Dr- CD

80D NE

600 NE \400 NE

200 NE

BRSE LINE

200 SW

400 SW

BOO SW

800 SW

LEGEND

66 - Conductivity thickness (G"t) in Siemens

1QQQ SW

1200 SW

1400 SW

^ t: ft rA.

1800 SW

1800 S H

320

KWG RESOURCES INC.LAVOIE LAKE PROJECT


HLEM PROFILES, 888 HzCOIL SEPARATION (Tx-Rx) : 200 ft

PROFILE SCALE : l in ^ 75 %POSITIVE PROFILE DIRECTION : TOST

APEX MaxMin H

SCALE 1:2400

SURVEY BYJVX LTD.

MAY 1992EAST GRID PLATE 7a

800 ME

600 NE

400 NE

200 ME

BflSE LINE ..^..^

200 SH

400 SH

600 SW

800 SH

1000 SH

1200 SW

1400 SW

1600 S H

180Q SW

UJCD

o o LU

CO

UJto

LJ

o oo or- OD

800 NE

BOO NE

ADO NE

200 NE

BRSE LINE

200 SH

400 SH

600 SW

BOO SH

1DOO SH

1200 SH

140D SH

1600 S H

1800 SH KWG RESOURCES INC

43DB5NE9982 2 .14777 SPRINGER LAKE 330

LAVOIE LAKE PROJECTLANSDOWNE HOUSE AREA

Northwestern OntarioHLEM PROFILES, 1777 Hz

COIL SEPARATION (Tx-Rx) : EOO ftPROFILE SCALE : l in ^ 75 55

POSITIVE PROFILE DIRECTION : NORTH-WESTAPEX Max-Min II

SCALE 1:3400

SURVEY BYJVX LTD.

MAY 1992EAST GRID PUTE 7 b

UJcoo oCM

Oo

UJcoD D CD

LU CQ

D Dr-

LJ CO

D O CO

LU CO

O CDen

LU CO

oo

UJ CO

oLOo

LU CD

O O

UJ CO

D LO

UJ CO

CDOC\J

UJ CO

oLD (M

UJ CO

o o

oLOm

o o

LJCO

o o

UJCO

Do

LU CO

D Or- o

OD

UJ LO

D CTJ

UJ CO

o o oC\J

UJ CO

D O

LU CO

CM Csj

LU CO

o o en c-j

UJCO

ooOsJ

LU CO

oD LO CvJ

LU CO

O O CD CM

LU CO

o o t—CM

LU CO

Oo

D O CD CM

LU CO

O O

LU LO

D D

UJ CO

o oCM

LU CO

O O

LU CO

O O

1000 NE

800 NE

600 NE

400 NE

200 NE

BflSE LIME

200 SW

400 SW

BOO SW

800 SW

laao sw

1200 SW

1400 SW

1600 SW

1800 SW

2000 SW

LUCO

o oCM

UJ CO

Oo o

CD

UJ CO

Oo r-

UJ CO

UJ CO

UJ CO

UJ CO

LU CO

aCD

o en

oo o

a o CD o o aLO O Lfl Ln

CNo ro

o o

LU CO

o oLO

LUtoooLO

LU LO

O Or-

UJto LiJ

LO

a en

LU LO

LU IO

Oo

oCM

CM CM

LU CO

oLO CM

OoCD CM

LU CO

Or-CM

LU CO

O OD CM

LUen

CDCM

LM CD

Oo o en

UJ LO

LU LO

LU CO

o CMCO

LU CO

o oLO CO

oLO CO

LUtoOo

LLJ CO

oCDm

LU CO

o o r-

UJto

o r-en

LUCO

o oCD CO

UJ CO

Den ro

oCOm

o en m

LUCO

o o o

CD Oo

1000 NE

800 NE

600 NE

400 NE

LEGEND

200 NEMagnetic high ^60,OOO nT

VLF- EM Conductors :

.BflSE LINE

200 SW

Strong In phase S Reversed Out phase

Medium IP phase

Medium Out phase

Weak In phase or Out phase

MaxMm Conductive Zone

400 SW

600 SW

VA4

Horizontal loop EM -—— Conductor width

Conductor axis

VLF Fraser filter conductor contour )

BOO 5W

SH1

F1

Gtraloqraphic horizon

Interpreted fault

1000 SW

FD1

400

Inro 1973 8 1974 drill hole

KWG April-May 1992 drill hole ( A 1 to A10 )

Mineralization, vertical projection

600 SW

COMPILATION MAP

sao SH

2030 SW


LANSDOWNE HOUSE AREA m __________Northwestern Ontario___________

GRID MAP

SCALE 1:2400

SURVEY BYJVX LTD.

MAY 1992EAST GRID PLATE 8

43DB5NE9902 2 .14777 SPRINGER LAKE 34-0

rpt on ground geophysical surveys...ground geophysical survey scale : 1 : 1,600,000 survey by jvx...

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