1742 OA LOGISTICAL AND INTERPRETIVE REPORT
ON
SPECTRAL IP AND RESISTIVITY
SURVEYS
CONDUCTED ON THE
MACKENZIE ISLAND PROPERTY
DOME TOWNSHIP
NORTHWESTERN ONTARIO
RED LAKE MINING DIV.
JVXLtd.
52N04SW0144 2.17420 DOME 010
A LOGISTICAL AND INTERPRETIVE REPORT
ON
SPECTRAL IP AND RESISTIVITY SURVEYS
CONDUCTED ON THE
MCKENZIE ISLAND PROJECTDOME TOWNSHIP
NORTHWESTERN ONTARIO
For: Freewest Resources Canada Inc.800 Rene Levesque Blvd. W Ste. 1525Montreal, QuebecH3B 1X9Attention: Mac WatsonTel: (514) 878-3551Fax:(514)878-4427
Freewest Resources Canada Inc.855 Field Street Thunder Bay, Ontario P7B 6B6Attention: Don Hoy Tel: (807) 346-0777
By: JVXLtd.60 West Wilmot St, Unit #22 Richmond Hill, Ontario L4B 1M6
Contact: Blaine Webster Tel: (905) 731-0972 Fax:(905)731-9312 JVX Ref: 9602 February 17, 1996
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TABLE OF CONTENTS
1 INTRODUCTION..................................................^
1.1 GENERAL....................................................................................................................................................61.2 PURPOSE.....................................................................................................................................................6
2 DATA ACQUISITION .......................................................................................................................................7
2.1 SURVEY SPECIFICATIONS ......................................................................................................................72.2 GRID SPECIFICATIONS ............................................................................................................................72.3 PRODUCTION SUMMARY........................................................................................................................72.4 PERSONNEL................................................................................................................................................92.5 FIELD INSTRUMENTATION ..........................................................................................^.......Zl..^^^
3 DATA PROCESSING............................................^
3.1 IP AND RESISTIVITY .............................................................................................................................. 10
4 INTERPRETATION METHODOLOGY......................................................................................................12
4.1 IP AND RESISTIVITY ..............................................................................................................................12
5 DISCUSSION OF RESULTS...........................................................................................................................14
5.1 ANOMALY DESCRIPTIONS ...................................................................................................................14
6RECOMMENDATIONS..................................................................................................................................17
52N04SW01442.17420DOME 0 1 OC
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FIGURES
Figure l: Location Map
Figure 2: Grid Map
TABLES
Table l: Specifications for the IP/Resistivity Survey
Table 2: Summary for IP/Resistivity Survey (a^25 m )
APPENDICES
Appendix A: Background to the Geophysical Methods
Appendix B: Plates
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PLATESGRID l
Black and White Line Plots:
Plate l: Chargeability Contour Plan Map (11=2), Scale l :2400
Plate 2: Resistivity Contour Plan Map (11=2), Scale l :2400
Plate 3: Stacked Spectral IP Pseudosections; Chargeability and Apparent Resistivity; L 1200E to L O, Scale 1:2400
Plate 3a: Stacked Spectral IP Pseudosections; MIP and Tau L 1200EtoLO, Scale 1:2400
Plate 4: Stacked IP Pseudosections; Chargeability and Apparent Resistivity; L 300W to L 1500W, Scale 1:2400
Plate 4a: Stacked Spectral IP Pseudosections; Chargeability and Apparent Resistivity; L 300W to L 1500W, Scale 1:2400
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GRID 2
Black and White Line Plots:
Plate l: Chargeability Contour Plan Map (^1=2), Scale l :2400
Plate 2: Resistivity Contour Plan Map (11=2), Scale l :2400
Plate 3: Stacked Spectral IP Pseudosections; MIP and Tau L 2400N 8c L 2100N, Scale 1:2400
Plate 4: Stacked Spectral IP Pseudosections; Chargeability and Apparent Resistivity; L 1800n to L 1200N, Scale 1:2400
Plate 4a: Stacked Spectral IP Pseudosections; MIP and Tau L ISOONtoL 1200NO, Scale 1:2400
Plate 5: Stacked IP Pseudosections; Chargeability and Apparent Resistivity; L 900N to L 300N, Scale 1:2400
Plate 5a: Stacked Spectral IP Pseudosections; Chargeability and Apparent Resistivity; L 900N to L 300N, Scale 1:2400
Plate 6: Stacked Spectral IP Pseudosections; Chargeability and Apparent Resistivity; L O to L 900S, Scale 1:2400
Plate 6a: Stacked Spectral IP Pseudosections; MIP and Tau L O to L 900S, Scale l :2400
Plate 7: Stacked Spectral IP Pseudosections; Chargeability and Apparent Resistivity; L 1200S to L 1800S, Scale 1:2400
Plate 7a: Stacked Spectral IP Pseudosections; MIP and Tau L 1200S to L 1800S, Scale 1:2400
GRID l Si GRID 2
Plate 8: Compilation Map, Scale l :2400
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l INTRODUCTION
1.1 GENERAL
JVX Ltd. conducted time-domain spectral induced polarization (IP) and resistivity surveys from January 15 to February l, 1996, on behalf of Freewest Resources Canada Inc. The surveys were done on McKenzie Island, on the McQuaig Red Lake Gold Mine Property and joining properties in Dome Township, Northwestern Ontario (N.T.S. 52 N/4). The area is accessible by winter road from Balmertown., Ontario.
1.2 PURPOSE
The purpose of this survey was to map the sulphide iron formation and to relate known gold mineralization to various structures on the property. Two possible mineralization trends exist; one parallel to lithologic strike and one crosscutting geologic strike. Two grids were surveyed one crosscutting geologic strike and one crosscutting a mineralization trend from the Campbell and Dickenson Mines.
The data from the grid crosscutting lithothology gave better line to line correlation of the IP anomaly zone. The spectral data located several targets some of which were drilled previously with gold intersected. ( No. l Vein)
-- SURVEY AREA
LOCATION MAP
FREEWEST RESOURCES INC.MCKENZIE ISLAND PROPERTY
Red Lake Area, Ontario N.T.S. 52 N/4
GROUND GEOPHYSICAL SURVEY
Surveyed by ]VX Ltd. February 1996
Scale : 1 : 2,500,000
Figure l
Lake
L a k
McKenzie Island.**0
Lake
BASE LINE O GRID 2
GRID MAP
FREEWEST RESOURCES INC. MCKENZIE ISLAND PROPERTY
Red Lake Area, Ontario N.T.S. 52 N/4
0 GROUND GEOPHYSICAL SURVEY
Surveyed by JVX Ltd. February 1996
Figure 2
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2 DATA ACQUISITION
2.1 SURVEY SPECIFICATIONS
Table 1: Specifications for the IP/Resistivity Survey
I.P.7Resi5tivity
Transmitter
Receiver
Array Type
Transmit Cycle Time
Receive Cycle Time
Number of Potential Electrode Pairs
Electrode Spacing (a spacing)
Number of Lines Surveyed
Survey Coverage
Scintrex TSQ3/3.0 kW
ScintrexIPR-12
Pole-Dipole
2 sec
2 sec
8
100 feet
Grid 1 - 9 lines
Grid 2- 15 lines
60 600 ft (18 483m)
2.2 GRID SPECIFICATIONS
The survey grid, located on McKenzie Island in Dome Township, Balmertown area , Red Lake District of Northwestern Ontario, is shown in Figure 2.
2.3 PRODUCTION SUMMARY
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Total IP coverage was 60600ft (18 483metres). The following table lists the survey coverage in detail:
Line
1200 E600 E300 E
0 E-300 W-600 W-900 W
-1200 W-1500 W
Line
2400 N2100 N1800 N1500 N1200 N900 N600 NSOONON
-300 S-600 S-900 S
-1200 S-1500 S-1800 S
- J:.,; 1:.::-:^ '-^iiVi;-;^^"^ -
Station from
1300 S1500 S1600 S1700 S1800 S1900 S1900 S1900 S1900 S
;-:-.-:: ::j?-. "-** 1 1.)? " ' .' ' ; ??"*; * ': '- '
Station from
100 E100 E100 E400 E700 E800 E1000 E1300 E1600 E1900 E1600 E1300 E600 E600 E600 E
TOTAL ALI
iCftiiJok S^: - .
to
400 S3000 N2800 N2400 N2000 N1900 N800 N800 N700 N
SubtotalISIiJlr '7
to1200 W1200 W800 W1400 W1600 W1600 W1200 W1200 W900 W1500 W1800 W1800 W1400 W1000 W1000 W
Subtotal, GRIDS
- ^X'l'-'^mDistance
(ft)
100045004400410038003800270027002600
29600-:; ' " •'/fff'^-f^,fjgf^
Distance (ft)
13001300900180023002400220025002500340034003100200016001600
3100060600
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2.4 PERSONNEL
Fred Moher (Geophysical Party Chief):Mr. Moher operated the Scintrex IPR-12 receiver and was responsible for data quality and theday-to-day operation and direction of the survey.
Four field assistants were also engaged by JVX.
Alexandra Savic (Geophysicist):Ms. Savic processed the data, prepared the plots, and is responsible for the data storage.
Dagmar Piska (Draftsperson):Ms. Piska carried out all manual drafting, and assembled and bound the report.
Slaine Webster (President, JVX Ltd.):Mr. Webster provided overall supervision of the survey, interpreted the data, and wrote thereport.
2.5 FIELD INSTRUMENTATION
JVX supplied the geophysical instruments described below. Additional information about the geophysical methods may be found in Appendix A.
2.5.11.P. TransmitterThe Scintrex TSQ3/3.0 kW Time Domain Transmitter powered by a ten-horsepower motor generator was used. The transmitter generates square wave current output with a period of 4, 8, or 16 seconds. A digital multimeter in series with the transmitter is used to measure the magnitude of the current output.
2.5.2 I. P. ReceiverThe Scintrex IPR-12 Time Domain Receiver was used. This unit samples the voltage decay curve as measured by the potential electrodes at ten points in time. Readings are repeated until they converge to within a tolerance level, and the data are stored in solid-state memory.
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3 DATA PROCESSING
After being transferred to a field computer at the end of each survey day, the data were examined, corrected, and organized by the instrument operator. The results were plotted on the following printers:
* STAR NX-80 colour dot-matrix printer ' EPSON FX-80 dot-matrix printer
These plots were used to monitor progress and data quality, and to make an initial interpretation. Thus survey parameters and design were altered when necessary.
The data were sent by courier to the head office of JVX in Richmond Hill, Ontario. They were processed and results were plotted on the following printers as was necessary:
* HEWLETT PACKARD DESIGNJET 750C 36 inch colour plotter* NICOLET ZETA 36 inch pen plotter* TEKTRONIX COLORQUICK ink jet printer" FUJITSU DL2400 colour dot-matrix printer* TEXAS INSTRUMENTS MicroLaser Pro 600 Laser printer
The processing procedure is outlined below.
3.1 IP AND RESISTIVITY
Steps l and 2 were performed both in the field and in the head office. Steps 3 and 4 were performed at the head office.
1) The GEOPAK IPSECT Package was used to generate colour pseudosections of chargeability and resistivity data.
2) JVX software was also used to perform spectral analysis of the time-domain data. This step was crucial to maximizing the information that can be obtained from IP data. This software analyses the shape of the IP decay curve, giving information about:
(a) the grain size (indicated by the parameter T),(b) the uniformity of the grain size (indicated by c}, and(c) the magnitude of the chargeable source (indicated by M-IP).
(Please see Appendix A for more information about spectral analysis.)
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3) The pseudosections from 2 above were aligned in AUTOCAD, then plotted. Since chargeability values are quite low over this grid, none are presented in this report.
4) Contoured plan maps of both chargeability and resistivity data from one dipole were produced using JVX in-house software and the GEOPAK or GEOSOFT Line Processing Package. Additional drafting on these maps was done manually or through AUTOCAD.
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4 INTERPRETATION METHODOLOGY
JVX uses its many years of experience in geophysical interpretation to extract the most accurate information from the data. The procedures involved are simplified for the sake of clarity. The SPECTRAL data was extensively used to further define the grain size (fine or coarse- grained). The high chargeability amplitude associated with the iron formation made it difficult to select drill targets on chargeability alone therefore IP anomalies with fine-grained SPECTRAL responses were given a high priority for drilling.
4.1 IP AND RESISTIVITY
The IP and resistivity data are interpreted using the following procedure:
1) Chargeability anomalies are picked on the pseudosections and classified using the following scheme as a guide:
Very Strong (^ 30 mV/V) and well defined
Strong (20 to 30 mV/V) and well defined
Moderate ( 10 to 20 mV/V) and well defined
Weak (5 to 10 mV/V) and well defined
Very Weak (3 to 5 mV/V) and poorly defined
x x x x Extremely Weak ^3 mV/V) and very poorly defined
The peak of the anomaly provides a qualitative indication of the depth to the top of the anomalous source and the location of the centre of the body. Where possible, the location and dipole number of the peak are written beside the anomaly bar.
2) The SPECTRAL characteristics of the anomalies are examined. The peak value of M- IP is noted, and T is classified according to the following scheme:
L Long (? 3 0.0 sec)
M Medium ( l.0 to 30.0 sec)
S Short ^ l .0 sec)
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3) Resistivity anomalies are picked on the pseudosections and classified using the
following scheme as a guide:
no symbol VH(n) Very High ^ 30, 000 Qm) highly silicified
no symbol H(n) High p 1 0 000 Qm) probably silicified
no symbol WH(n) Weak High ^ 1 0 000 Qm) - relative increase comparedto surrounding material
SL(n) Strong Low — strong decrease in resistivity
- - - ML(n) Medium Low — medium decrease in resistivity
' ' " " WL(n) Weak Low — weak resistivity decrease relative to surroundingmaterial,
where n is the dipole number at which the anomaly peak is located.
4) The anomalies from steps l to 3 are marked on the Compilation Map.
5) Resistivity anomalies on the Compilation Map are joined into conductive and resistive
zones.
6) Zones of high chargeability are interpreted based on resistivity and geometric
information.
7^1 The chargeability anomalies are further prioritized employing the^SPECTRAL } parameters paying particular attention to the relative amplitude of the Mff response
and the length of the time constant.
8) The IP and Resistivity data is reviewed on the compilation map with ancillary
geologic and geochemical data.
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5 DISCUSSION OF RESULTS
The interpretation of the geophysical data was compiled onto a single map, and is summarized in the sections following. This Compilation Map and all data plots are included in Appendix B.
Three main IP chargeability zones have been mapped out on Grid 2 whose wing lines cross the stratigraphy. The anomalies are correlatable from line to line therefore it is assumed Grid 2 is the best map to use for stratigraphic correlation. The chargeability anomalies, resistivity responses drill holes and gold showings are identified on the Compilation Map (Plate 8).
5.1 ANOMALY DESCRIPTIONS
S.la ZONE IP -1 (Line 900S/800E to Line 1800N/200W)
IP zone IP-1 is a moderate to very strong, north/south trending, chargeability zone located on the eastern part of the grid. This zone strikes to the north extending between lines 900S and l SOON traversing a wide zone of high resistivities on the eastern part of the grid. The trend of IP-1 is parallel with the direction that drill holes l, 2, 5, 9, 10, l land 12 were drilled. The SPECTRAL data shows that even though the volume of sulphide is high the mineralization is fine-grained. In our experience this is a very good area to test for gold. Normally the alteration zone associated with a an auriferous sulphide body gives a short time constant. The section of IP-1 on line 300N which crosses with vein number l has a short time constant thereby indicating that the auriferous sulphide mineralization has a short time constant response and is therefore fine-grained. The combination of very high MIP (greater than 1,000 mV/V) with a short time constant is a very good gold indicator.
RECOMMENDATIONS:
Five targets have been selected on IP zone IP-1.
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TARGET l (Tla&Tlb) ( 300E/300N) High Priority
On grid l at 300E/300N the SPECTRAL response on a line surveyed parallel to geologic strike had a very high MIP response (zero time chargeability) with mixed time constants. Tib occurs 100 feet north of gold showing number 5 and 100ft. south of vein number l indicating the high MIP and short time constant is important in selecting drill targets.
The anomaly on line 300N/100E Grid 2 has a strong chargeability response with high resistivities (10-20,000 ohm-m) indicating a silicified environment. The SPECTRAL parameter Tau indicates that the source is fine-grained. Tla/Tlb occur near the projected western extension of the number l vein which makes this a high priority target. The anomaly should be drilled on line 300N. Geology should be used to further refine this target.
Tla and Tib are high priority drill targets.
TARGET T-3 (1200N/100E) Medium Priority
T-3 is a strong chargeability anomaly with low time constants correlating with a narrow resistivity high. The short tune constants and resistivity high indicate a fine-grained silicified source.
T-3 is a medium priority drill target.
TARGET T-4 (300S/300S) Very High Priority
T-4 is a very strong chargeability anomaly which is associated with a slight resistivity increase and moderate-to-high SPECTRAL MIP indicating a very high volume percent of fine-grained sulphides.
T-4 is a very high priority gold target. The anomaly should be drilled on line 300S. Geology should be reviewed to further prioritize the targets.
TARGET T-5 (1800N/200W) Medium Priority
T-5 is a very strong shallow chargeability response located on the east flank of a resistivity low near gold showing number l.
T-5 should be evaluated geologically and geochemically
Target T-5 could be moved to either line l SOON or l SOON.
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Target T-6 (600S/900E) Medium Priority
T-6 is a very strong chargeability anomaly with a moderate SPECTRAL MIP response and an associated long time constant (TAU). A narrow weak resistivity high (3,000 ohm-m) occurs on its west flank.
Gold showing #4 is located 400ft. to the east and may have a relationship with T-6. Drill holes 7 and 8 may partially explain T-6 and should therefore be evaluated for sulphides and alteration.
5.2 IP Zone-2 (Line 1500S/100W to Line 900S/500W)
IP Zone 2 is a moderate to strong chargeability anomaly zone associated with a resistivity high located on the southwest part of the grid on a small island. The short time constant indicates the source to be fine grained; this together with the high associated resistivity suggests that the sulphide source may be silicified.
Recommendation:
TARGET 2 (1200s7300W) Very High Priority
The SPECTRAL MIP is moderately high but the SPECTRAL TAU indicates a fine-grained source. Strong chargeabilities occur on the western contact of a very highly resistive body. The anomaly is duplicated on line 9W/4S.
The geology associated with IP Zone 2 is quartz porphyry, andesite agglomerate, and iron formation, an excellent gold environment.
5.3EPZone-3a (Line 600W/600S to Line 00/400S) IP Zone -3b (Line 900W/500S to Line 1500W/600S)
IP Zones 3a and 3b are strong chargeability anomaly zones associated with a resistivity high located on the southwestern part of the grid and situated on the northeastern part of a small island.
The associated geology should be reviewed and further evaluation made after target T-2 is drilled.
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6 RECOMMENDATIONS
All target areas should be visually inspected and sampled. The present drill program will test the defined target areas. Prior to drilling, we recommend IP modelling of relevant anomalies.
The core should be logged with special attention paid to fine grained and coarse grained sulphides and their association with silicification/alteration and gold mineralization so that the spectral data can be correlated to grain size. Explanations of targets should be given to JVX as a further guide in its spectral interpretation.
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If there are any questions with regard to the conducting of the survey or the interpretation of the data, please call the undersigned at JVX Ltd.
Respectfully submitted,
JVX Ltd.
Blaine Webster, B.Sc. President
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APPENDIX A
Background
to the
Geophysical Methods
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INDUCED POLARIZATION AND RESISTIVITY
l THE IP EFFECT
The induced polarization (IP) phenomenon is primarily caused by:
1) electrical polarization at the boundary between the rock or soil and the pore fluids, and
2) electrical polarization at the boundary between metallic minerals (particularly sulphides) within pores and the pore fluids.
This polarization occurs when a current is applied across these boundaries. Its magnitude can be measured in two ways:
1) in the frequency domain (also known as phase IP), in which the applied current is sinusoidal, or
2) in the time domain, in which the applied current is a modified square wave.
JVX conducts IP surveys in the time domain because spectral analysis, a powerful interpretive tool, can only be performed in the time domain.
Generally, the current is transmitted as a modified square wave with a period of eight seconds (two seconds positive, two seconds off, two seconds negative, two seconds off). The voltage measured in the ground will have the form shown in figure IP-1. The IP effect is manifested as a roughly exponential voltage decay after the current is turned off, similar to the relaxation effect of a discharging capacitor. The IP receiver samples this voltage decay curve at a number of points.
The SCINTREXIPR-11 receiver repeats and averages the following measurements until they converge:
Vp The primary voltage (the steady-state amplitude of the voltage while the current is being transmitted).
IP-1
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SP The self-potential (the steady state voltage when no current is being transmitted).
mO to m9 The chargeabilities (measures of the IP effect at different times along the decay voltage curve Vs(t) ).
Each chargeability value (mO to m9) is the ratio of the average secondary voltage over a time window to the primary voltage. Mathematically, this is given by:
f"m = 1 000 l Vs(t) dt
Vp(Vt,) J t,
wherem = chargeability (in mV/V)
Vs(t) = secondary voltage (i.e. the voltage decay) Vp = primary voltage t, = beginning of time window t2 = end of time window
The IPR-11 uses the ten time windows, also known as time slices, listed in table IP-1 and shown in figure IP-2. Unless otherwise stated, the term chargeability refers to the eighth time window (m7).
IP-2
Vp
T3 do
SP
Vs(t)
Figure IP-1 : The I.P. Waveform
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SLICE
mO
ml
m2
m3
m4
m5
m6
m8
m9
DURATION (msec)
30
30
30
30
180
180
180
360
360
FROM (msec)
30
60
90
120
150
330
510
1050
1410
TO (msec)
60
90
120
150
330
510
690
1410
1770
MIDPOINT (msec)
45
75
105
135
240
420
600
1230
1590
Table IP-1 : Time slices recorded by the IPR-11 receiver
Nominal total receive time: 0.2.1.2,4 sec.
y.
i; ;i s.
0-3 4 5
11111 6t 6t A Delay
M
6t
7
12t
M8
12t
M,'9
12t Window Width
IPR-11 TransienlWindows
Figure IP-2 : IP effect decay curve with IPR-11 time slices
IP-4
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2 SPECTRAL ANALYSIS
With the ability to sample the decay curve at a number of points, the shape of the decay curve can be analysed. This gives important information about the characteristics of the source.
Spectral analysis utilises the Cole-Cole model of the IP effect (Pelton et al., 1978). This model uses the following four parameters (described in Johnson, 1984) to calculate a theoretical IP decay curve:
pa Resistivity (Qm)This quantity is described in detail later in this appendix.
M-IP Chargeability Amplitude (mV/V)This quantity is related to the volume percent of the chargeable source, although there is no simple quantitative relationship.
T Time Constant (seconds)The time constant is related to the grain size of the source. A short time constant (0.01 to 0.3 s) indicates a fine-grained source. A long time constant (30 to 100 s) indicates a coarse-grained, interconnected, or massive source.
c Exponent (dimensionless)A high value (e.g. 0.5) indicates that the grain size is uniform. A low value (e.g. 0.1) indicates that there is a mixture of grain sizes.
Conventional chargeability is a combination of these spectral parameters. A change in any one parameter will produce a change in the apparent chargeability. In the absence of spectral analysis, such changes are always ascribed to a change in the volume percent of the chargeable source, even though the cause may be a shiftfromjme-grained to coarse- grained material.
JVX has developed a software package called SOFT n which determines the spectral parameters by comparing the measured decay curve with a library of model curves. The quality of the fit is given as a root-mean-square difference (expressed as a percentage). A low value (e.g. l 07o) indicates high quality data of medium to high amplitude. A high value (e.g. greater than 10 07o) indicates poor quality or low amplitude data. If the fit is greater than 5 9-6, the spectral parameters are considered to be of poor quality, and therefore are usually discarded.
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3 ARRAY CONFIGURATION
As mentioned above, a current must be flowing through the ground in order for the IP effect to occur. This current is applied using two electrodes, which are called CI and C2, and the voltage decay is measured using two potential electrodes, PI and P2. The distance separating PI and P2 is known as the a-spacing, or o, and generally remains constant during the survey.
The three most common electrode array configurations are:
1) GradientCI and C2 are located at an "infinite" distance (i.e. very far) from the grid, with one on each side. The potential electrodes move throughout the grid.
2) Dipole-DipoleC l and C2 are separated by a distance of o, and move along with the potential electrodes.
3) Pole-DipoleC2 is located at "infinity". CI moves along with the potential electrodes throughout the grid.
The gradient array allows for fast reconnaissance surveys. However, no depth information is obtained (described below), and the resolution is much lower because all of the ground between CI and C2 is energised. Furthermore, the current will be channelled through conductive zones, which could result in inaccurate chargeability and resistivity values. Thus, great care must be used when using a gradient array.
In JVX1 experience, the pole-dipole array is superior to the dipole-dipole array. Since C2 is located at an infinite distance, a greater volume of ground is energised. This results in better depth penetration (i.e. higher quality data), and is particularly important in the presence of thick and/or conductive overburden. However, the pole-dipole array does not have the disadvantages of the gradient array. Since CI is located near the potential electrodes, depth information is obtained (see below), and resolution is high.
4 A-SPACING AND NUMBER OF DIPOLES
The resolution of the data depends on o, the electrode spacing. The smaller a is, the greater the resolution. However, the depth of penetration is also smaller. A larger a results in greater depth, but less resolution. Thus, both factors must be considered when selecting the electrode spacing.
The standard pole-dipole array is shown in figure IP-2. Seven potential electrodes are used to measure the voltage simultaneously across six electrode pairs (P1-P2, P2-P3, P3-
IP-6
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P4, etc.). Each pair is labelled using an integer, n, where na is the distance between the first potential electrode and the nearest current electrode.
The depth of investigation is greater when the potential electrode pair is farther from the current electrode (i.e. larger n). However, a greater separation distance also results in greater signal attenuation, limiting the number of dipoles which could be used effectively.
5 RESISTIVITY
The DC apparent resistivity (pa) is a measure of the bulk electrical resistivity of the subsurface. Electricity flows primarily through the groundwater within fractures and pore spaces. Therefore, fault zones can be detected as low resistivity zones. However, sulphide minerals, some oxides, and graphite are also good conductors and so produce low resistivity zones. The current flow is electronic in these minerals rather than electrolytic as it is in groundwater. Sometimes, the geometry of the low resistivity zone can distinguish between a fault zone and a mineral source. In other cases, additional geological information is needed. Silicates, the most common rock forming minerals, are very poor conductors of electricity, producing high resistivity zones.
The resistivity is measured simultaneously with the IP data. For a homogeneous and isotropic subsurface, it is given by the following formula:
wherepa = apparent resistivity (Qm)
Vp = primary voltage (measured while current is on) (mV) k :: k-factor (m)
The k-factor is an array-dependant component. For a pole-dipole array, it is given by:
k s 27cn(n*l)a
wheren = dipole multiple (dimensionless) a = electrode separation (m)
Although the assumption of a homogeneous and isotropic earth is unrealistic, the calculated value of pa can be used qualitatively to map changes in rock type (even to identify the rock type in some cases), and to map low resistivity fault zones.
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References
Johnson, I.M. Spectral I.P. Parameters as Determined through Time Domain Measurements, pp. 1993-2003 Geophysics 49, 1984
Johnson, I.M., B. Webster, R. Mathews, and S. McMullan Time Domain Spectral IP Results from Three Gold Deposits in Northern Saskatchewan, The Canadian Mining and Metallurgical Bulletin, Feb. 1989
Pelton, W.H., S.H. Ward, P.G. Hallof, W.P. Sill, P.H.Nelson Mineral Discrimination and Removal of Inductive Coupling with Multifrequency IP. pp. 588-609, Geophysics 43, 1978
IP-8
APPENDIX B
Plates
GRID 1
l T96925 i
1209693 '^r^
FREEWEST RESOURCES CANADAFigure!
Claim Location SketchMcCuaig Red Lake Property
McKenzie Island, Dome TownshipRed Lake Mines 8i Minerals Division
RECEIVED
JUN 20 1997
MINING LANDS BRANCH
GRID 2
GRID 1 SL G RID 2
Compilation Map
D OhtariO 1̂ ******* Declaration of Assessment Work A and Mines Performed on Mining Land
Mining Act, Subsection 65(2) and 66(3), R.S.O. 1990
Transaction Number (ellice use)
Assessment Files Research Imaging
Personal information colled Mining Act, the Information i Questions about this colle 933 Ramsey Lake Road, Si
of the Mining Act. Under section 8 of the nd correspond with the mining land holder, ern Development and Mines, 6th Floor,
52N04SW0144 2.17420 DOME 900
Instructions: - For work performed on Crown Lands before recording a claim, use form 0240. - Please type or print in ink.
1 . Recorded holder(s) (Attach a list if necessary)
AyName Client Number
Address Telephone Number
Fax Number
NameEiUrfgl
Client Number
Address Telephone Number
Fax Numbe
2. Type of work performed: Check ( ^ ) and report on only ONE of the following groups for this declaration.
Geotechnical: prospecting, surveys, assays and work under section 18 (regs)
Physical: drilling, stripping, trenching and associated assays [ l Rehabilitation
Work Type It -Z /9^ kil*e4r6 k ^f^*t Jw&a*1- fyt6frt*4n*
j^^/5-fv/ly 5uMfe ( io .̂ )
Dates Work . f . T Performed From * ' *ai '
Day Month Year n 7 If DayGlobal Positioning System Data (if available) Township/Area
GrJ*
Month Year
M or G-Plan NumberG-T7M-8
Office Use
Commodity
Total S Value of f̂ f-\ ' 7 ^^ Work Claimed ^(. i ^T^f -
NTS Reference f) 3/1 7 xi (̂-56t
Mining Division A J^ -/^O
Resident Geologist /} s x District A^td fa*~#-i^
Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.
3. Person or companies who prepared the technical report (Attach a list if necessary)Name .
W U}^ UJi/nW 5{fV^, i/nJ^ ^22, I?idUwi^ f^l(, rf*(Wrr ^ /'ft
Name
Address
Name
Address
Tele)
Fax h
0Tele;
Fax h
hone Number 6*ti 3-3 f-d If l*-
jCtiC^-r^ L. i "w L li
tone Nurnbar, ^ JUNfi f
2 0 1997umber
MINING LANDS BRANCHTelephone Number
Fax Number
4. Certification by Recorded Holder or Agent
l, , do hereby certify that l have personal knowledge of the facts set(Print Name)
forth in this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.
5. Work to be. recorded and distributed. the* mining land where work was performed, must accompany this form.
Work can only be assigned to claims that are contiguous (adjoining) at the time work was performed. A map showing the contiguous link
L{) c{7 36 - O O /~JOMining Claim Number. Or K work wu dona on other eligible mining land, show In this column the location number indicated on the claim map.
eg
eg
eg
1
2
3
- 4
5
6
7
8
9
10
11
12
13
14
15
TB 7827
1234567
1234568
/Z0W2-
l-KXbV
{ZOW}
Number of Claim Units. For other mining land, list hectares.
16 ha
12
2
?
Z
i.
t
Column Totals
Value of work performed on this claim or other mining land.
S26, 825
0
S 8, 892
Mfr
Wb
W,
2 fc. m
Value of work applied to this claim.
N/A
S24,000
S 4,000
' 1,2-00
f 2,0017
' ff*a
O 1til A *"JU * J*^^^^
:
t/, 000
Value of work assigned to other mining claims.
S24,000
0
0
742 (\
Bank. Value of work to be distributed at a future date.
S2,825
0
S4,892
TftVf
W
8 /It?
aa^b
l, , do hereby certify that the above work credits are eligible under(Print Full Name)
subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to
the claim where the work was done.
Signature of Recorded Holder or Agent Authorized in Writing Date
6. Instructions for cutting back credits that are not approved.
Some of the credits claimed in this declaration may be cut back. Please check ( s ) in the boxes below to show how
you wish to prioritize the deletion of credits:
D 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated.
D 2. Credits are to be cut back starting with the claims listed last, working backwards; or
W 3. Credits are to be cut back equally over all claims listed in this declaration; or
D 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):
Note: If you have not indicated how your credits are to be deleted, c followed by option number*2 if necessary.
he Bank first,
For Office UseReceived Stamp
o^EGEIVEDRED LAKE MINING DIV.
JUN l fj J997
AM " W)
Deer fed Approved Date .
Date Approved '
Date Notilicatlon Sent
Total Value of Credit Approved
. h L
Ontario
Ministry otNorthern Developmentand Mines
Mmistere du Developpement du Nord et des mines
Statement of Costs for Assessment Credit
Etat des couts aux fins du credit d'evaluation
Mining Act/Loi sur les mines
Transaction No./N" de transaction
M- oo l "70
17420Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining claim(s). Questions 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.
Les renseignements personnels contenus dans la presente formule son! recueillis en vertu de la Lol sur les mines et servlront a tenir a jour un registre des concessions minieres. Adresser (oule quesiton sur la collece de ces renseignements au chef provincial des terrains miniers. minislere du Developpement du Nord et des Mines. 159, rue Cedar, 4* etage, Sudbury (Ontario) P3E 6A5. telephone (705) 670-7264.
1. Direct Costs/Couts directs
Type
Wages Salalres
Contractor's and Consultant's Fees Drolts de ('entrepreneur et de I'expert- consell
Supplies Used Fournltures utlllsees
Equipment Rental Location de mate'rlel
Description
Labour Main-d'oeuvre
Field Supervision Supervision sur le terrain
Type
J* 5c*wy
a&rfUVi^ M.4p
Type
""RECEIVHtU LAKE MININ
JUN l u |99?-.\
Amount Montan!
*1f,Wf
2,100
t
"i DIV.
PM
^S.SiWiyri^tt^&l8 Total descoUts directs
Totals Total global
'*Zw\
'is," j-'-^iV-
fyW*
2. Indirect Costs/Couts indlrects* * Note: When claiming Rehabilitation work Indirect costs are not
allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les couts indirects ne son! pas admissibles en tant que travaux d'evaluation.
Type
Transportation Transport
Food and Lodging Nourrlture et hebergementMobilization and Demobilization Mobilisation et demobilisation
Description
Type
- Amount Montant
Sub Total of Indirect Costs Total partlel des coOts Indlrects
Amount Allowable (not greater than 20tt of Direct Costs) Montant admissible (n'excedant pas 20 H des coOts directs)
Total Value of Assessment Credit Valeur totals du credit (Total of Direct and Allowable d'evaluationInrilrart rnalll (Total du COfHl dlrtetl
Totals Total global
tt Indirect* admissible*
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 les depenses demandees dans le present etat des couts dans les 30 jours suivant une demande a eel effet. Si la verification n'est pas effectuee, le ministre peut rejeter tout ou une partie des travaux d'evaluation presentes.
Filing Discounts
1. Work filed within two years of completion is claimed at 100(Vb of the above Total Value of Assessment Credit.
2. Work filed three, four or five years after completion is claimed at 5Q0fa of the above Total Value of Assessment Credit. See calculations below:
Total Value of Assessment Credit Total Assessment Claimed
x 0.50
Certification 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.
that as(Recorderf'Holder, Agent, Position in Company)
to make this certification
Remises pour dep6t
1. Les travaux deposes dans les deux ans suivant leur achevement sont rembourses a 100 ^ de la valeur totale susmentionnee du credit d'evaluation.
2. Les travaux deposes trois, quatre ou cinq ans apres leur achevement sont rembourses a 50 ah de la valeur totale du credit d'evaluation susmentionne. Voir les calculs ci-dessous.
Valeur totale du credit d'evaluati
Attestation de I'ttat de;
J'atteste par la presente :
n Evaluation totale demandee
xRC-C E 1 V E D
Co0t JUN 2 0 1997
MINING LANDS BRANCHque les montants indiques sont le plus exact possible et que ces depenses ont et6 engagees pour effectuer les travaux d'evaluation sur les terrains indiques dans la formule de rapport de travail ci-jolnt.
l am authorized Et qu'a litre de je suis autorisea mn? uo ——————.————————————————————— j~ ~— j ~ (titulaire enregistre, representant, posts occupe dans la compagnie)
a faire cette attestation.
Signature Dale
Ministry ofNorthern Developmentand Mines
August 26, 1997
EWAN STEWART DOWNIE 1529 RANKIN STREET THUNDER BAY, Ontario P7E-5Z2
Ministere du Developpement du Nord et des Mines Ontario
Geoscience Assessment Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5
Telephone: (888) 415-9846 Fax: (705) 670-5863
Dear Sir or Madam:
Subject: Transaction Number(s):
Submission Number: 2.17420
W9720.00170
StatusDeemed Approval
We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.
If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice.
Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.
If you have any questions regarding this correspondence, please contact Steve Beneteau by e-mail at [email protected] or by telephone at (705) 670-5855.
Yours sincerely,
ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section
Correspondence ID: 11276
Copy for: Assessment Library
Work Report Assessment Results
Submission Number: 2 .17420
Date Correspondence Sent: August 26, 1997 AssessorSteve Beneteau
Transaction First Claim Number NumberW9720.00170 1209692
Section:14 Geophysical IP
Township(s) l Area(s)DOME
StatusDeemed Approval
Approval Date
August 21, 1997
Correspondence to:Resident Geologist Red Lake, ON
Assessment Files Library Sudbury, ON
Recorded Holder(s) and/or Agent(s):Donald HoyTHUNDER BAY, ONTARIO
EWAN STEWART DOWNIE THUNDER BAY, Ontario
PERRY VERN ENGLISH RED LAKE, Ontario
Page: 1
Correspondence ID: 11276
AREAS W ITHDRAWN FROM DISPOSITION
MHO -M NING RIGHTS ONLY
S.R.O. SURf ACE RIGHTS ONLY
M.+ S. - I'/.iN'NGfAND SURFACE RIGHTS
Description Order No. Date Dijposition FiLa
SEC. 36 0.-M/88 30/06/88 MRO 188993
NOTE
SURFACE RIGHTS T RANSFERRED TO CANADA IN AREA
SHOWN THUS ; : AT RED LAKE AERODROIJE,
FILE 6 1894 R EF 141253 O C EO Dr LT?
LU
MCDONOUGH TOWNSHIP G 373241 M
M- - l M
3M- -
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I fxr'U l p. n U. l i l776202 776200 ' 776210 796918 ,
' l ll.MM—— —— T— ——— — ~T~ —— "T~ l KRL
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i ^8696ie— i __ __ —
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KRL ' KRL •^"869383 ! "6995 l 83900
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II97D5Ilo*507 Uo4-5-06 90*5-05-
or( str'y ^t./?
______—— i, -- -I.——
9045-3-2. J ^4.5-33
Howey90.9*1
HEYSON TOWNSHIP G 3736
CD
m
o
COrrT)
CDOJ -JOJen
o oCM
LEGENDHIGHWAY AND HOTTF \o
' --t - "(..AuS
r (- A . .fiHH . t V f . 'Mr S
l i"j AM SHIPS. B A') t L !Nfc S. L K
IO1S MlMNC, (.1 A;MS PARLt.i i
UNS' 'K . F i F !'- i !"JL S il , . : .'^ -,
PA-^ r i -ri( M/NI.AM v
Ml 1 . 'M", i.:i AIMS f- Tt.
RA!|.'.-'-. A\[) HIGH I (If WA^t
i J T l; ' - j i N t S
\. '. (.. .^ \ MAL S T M(r AM
^ Li H ' V, OH F LOUOlNCi RIGHTS
Sl'H; 'ViSION OH COMPOSITE Pi AN
RESf R'. A V IONS
ORKjINAL SHOfU LIMF
MARSH OR MUSKtG
M IN f-S
TRAVF. RSI Mi;Nl JMtNT
DISPOSITION OF CROWN LANDS
SYMBOiTYPE OF DOCUMENT
PATFNT MJHfAC.f A MINING H K ,H l 1 .
SI. J (O At l RK,M T'. (iM N
MININi, MKjH T 1 , (JNI T
LtASt suHrAii s, MINING Hit,M ' .SI iRI At;f MM ,n i S i INI t
MiNiNt, UK,M -', ONI v
t ICF NCF Of (JfX.UPA T ION
ORtH R IN l.f )UN(.ll
R l SI H VAT ION
CANCf L l f O
SAND R. GRAVf t
NOTE M INlN' . Hi' .n I'., if/ c n H I f l '. l'A I l i* i l f j P H 11'i H T i U A . (,
1411 V l ', T J ( . l ^ ''i M l - . r N A l l' A ' i 'i M l H * l M l l 1 1) H t l (
L ANOS A f l H '. i ' 'l ") f u A' 1 l"'l M '.l M nil ' l
n uT
Of
SOOMplro,
i nonMvtrx
10 O 10 J O 1 0 40 Ml (,fl /o
soo o looa vooo 3000 lone
SCALL 1.20 OOO
FOREST ACTIVITY INFORMATIONTHIS TOWNSHIP/AREA FALLS WITHIN THE
RED LAKE CROWNAND MAY BE SUBJECT TO FORESTRY OPERATIONS. THE M.N R UNIT FORESTER FOR THIS AREA CAN BE CONTACTED AT:
P.O. BOX 5003RED LAKE, ONTARIO POV^MO(807) 727-2253
ft. 1742
THE INFORMATION T IAT APPEARS ON THIS MAP HAS BLEN COMPII ED FROM VARIOUS SOURC Ef,. AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMAT-ON ON THE STATUS OF YHE LANDS SHOWN HEREON
TOWNSHIP
DOMEMMR ADMINISTRATIVE DISTRICT
RED LAKEMINING DIVISION
RED LAKELAND TITLES/ REGISTRY DIVISION
KENORA / PATRICIA
Ministry ofNaturalResources
Ministry ofNorthern Developmentand Mines
OntarioN ii m h *
SEPTEMBER I986
1600 W
1200 W
800 W
e
Strong
Strong
VVH(2) - Weak High Resistivity 1 H;1) - High Resistivity, 11=1 VHi2) - Vary High Resistivity, 0=2
Strong Resistivity Low
IP-1
vVeak l
M- l Pi TV Vi 517 . L lTimo Constant (Long,Medium or Short) —' |
Very Woak
Medium Medium Resistivity Low
Weak Resistivity Low
Very Woak Resistivity Low
DDH 1
Showing
^^
Chargcnbiiity Zono
Diamond Drill hole
Showing
CHARGEAE'LITV ANOMALY
RESISTIVITY ANOMALY
T-1" Exploration Target
VHP - Very High PriorityHP - High PriorityMP - Medium Priority
BASE LINE O GRID 2
2.l? 420
52N04SW0144 2.17420 DOME 210
FREEWEST RESOURCES INC.MCKENZIE ISLAND PROPERTY
RED LAKE AREA, ONTARIO_________N.T.S. 52 N/4_________
COMPILATION MAP
SURVEYED BY JVX LTD., FEBRUARY 1996
100 100 200 SOO
PLOTTED BYD.P.
FEE 1996SCALE I "s200' PLATE 8
JVX. ref. no. 9602
o o
2800 N
2700 N
2600 N
2500 N
2400 N
2300 N
2200 N
2100 N
2000 N
1900 N
1800 N
1700 N
1600 N
1500 N
1400 N
1300 N
1 200 N
1 100 N
1000 N
900 N
800 N
700 N
600 N
500 N
400 N
300 N
200 N
100 N
100 S
200 S
300 S
400 S
500 S
600 S
700 S
800 S
900 S
1000 S
1 100 S
1200 S
1300 S
1400 S
1500 S
1600 S
1700 S
o o CM o o 01o o10
o o o oto
o o(O
o oON
o o10
o o(N
o o en
o o(O
o oIO
UlooIO
Ulo o10
oCM CM
2800 N
2700 N
2600 N
2500 N
2400 N
2300 N
2200 N
2100 N
2000 N
1900N
1800 N
1700 N
1600 N
1500 N
1400 N
1300N
1200 N
1 100 N
1000 N
900 N
800 N
700 N
600 N
500 N
400 N
300 N
200 N
100 N
100 S
200 S
300 S
400 S
500 S
600 S
700 S
800 S
900 S
i s iooo s
1 100 S
1200 S
1300 S
420
FREEWEST RESOURCES CANADA INC.MCKENZIE ISLAND PROPERTY - GRID i
RED LAKE MINES and MINERALS DIVISION ______________N.T.S. 52 N/4
CHARGEABILITY CONTOURS (11=2)CONTOUR INTERVALS : l A 5 mV/V
TIME WINDOW 310-1050 ms
SURVEYED BY JVX LTD. USINGSCINTREX IPR-12 Rx ; IPC-7/2.5 kW Tx
WINTER 1996O 200 400 600
PLOTTED BYA.S.
FEB. 1996SCALE 1:2400 PLATE l
JVX ref. no. 9602
o oIf)
O O
2800 N
2700 N
2600 N
2500 N
2400 N
2300 N
2200 N
2100 N
2000 N
1900 N
1800 N
1700 N
1600 N
1 500 N
1400 N
1 300 N
1200 N
1 100 N
1000 N
900 N
300 N
700 N
600 N
500 N
400 N
300 N
200 N
1 00 N
100 S
200 S
300 S
400 S
500 S
600 S
700 S
800 S
900 5
1000 S
1 100 S
1200 S
1300 S
1400 S
1500 S
1600 5
1 700 S
o oO)
o o(O
o o
UJo oK)
g(O
o oCN
o oo oCN
o oO)
o o(O
o oO O ro
UJO O (O
2800 N
2700 N
2600 N
2500 N
2400 N
2300 N
2200 N
2100N
2000 N
1900N
1800 N
1700 N
1600N
1500 N
1400 N
1300N
1200 N
1 100 N
1 000 N
900 N
800 N
700 N
600 N
500 N
400 N
300 N
200 N
100 N
100 S
200 S
O CO (N
300 S
400 S
500 S
600 S
700 S
800 S
900 S
1000 S
1 100 S
1200 S
FREEWEST RESOURCES CANADA INC.
MCKENZIE ISLAND PROPERTY - GRID iRED LAKE MINES and MINERALS DIVISION
______ ______N.T.S. 52 N/4 ___________
RESISTIVITY CONTOURS (11=2)CONTOUR INTERVALS : 500 fc 2500 ohm m
SURVEYED BY JVX LTD. USINGSCINTREX IPR-12 Rx ; IPC-7/2.5 kW Tx
WINTER 1996O 200 400 600
PLOTTED BYA.S.
FEB. 1996SCALE 1:2400 PLATE 2
JVX ret. no. 960Z
LINE : O E
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRflY
DEPTH'VoiNT
N z l . 2. 3. 4. ... •fi" SPBCING : 100.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND, GRID-1
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE = l : 2400
JVX LTD.
15CJ05 | MODS | 13C|OS t 12CJOS | HOPS | l OOPS | 90pS | 80pS | 70pS , 60pS | SOpS | 40pS | 30pS | 20pS , IQpS | ON | IQpN | 20pN | 30pN t 40pN | SOpN | 60pN | 7PpN | 80pN L 90pN | IQ^ON | ll^DN | 12(]ON [ 13(|ON | HC]ON 15(|ON | 160DN | 1TCJON | 18QON | 19QON | 20QON t 21DON
RESISTIVITYNil
N:2
N:3
Ni4
NiS
N:6
2. OK
nra.
.0 102.0 108.0 221.0 188
n:-j 19.0,361.O 27
RESISTIVITY265.0 .582J) 708-0 56.7-0,199.0 161.0 123-0 119.0 161.0 193-0-^s^s / /y ^--i ^— oo z-"*
DN
MX CHG.Nil
Ni2
N:3
N:4
N:5
N:6
7.7
10t]OS , 90pS | 60pS , 70pS | 60pS t 50pS 20pN t 30pN | 40pN | SQpN | 60pN | 70pN14C)OS | 13(|OS 2ops i tops 11CJON | 12(|ON t laqON | 14CJ N | 16C|ON | 17(]DN | IBtjON , 19C|ON | 20C)ON | 2KJ
r 31714.6 26-4
16.1 ^ 27.8
16.3 18.1/ 29.3 20
19. ff 30g) 22.2
MX CHO. Nil
N;2
Ni4
Ni6
LINE : 300 E
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRflY
--o.DEPTH"*POINT
N r l . 2, 3. 4. •R" SPRUNG : 100.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND, GRID-1
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE = l: 2400JVX LTD.
15C]OS t 1 4^05 90pS | SOpS | 70pS , 60ps~~~~""~
40pS | 30pS t 20pS 20pN | 30pN 60pN | 70pN , BOpN , 90pN IBCj ON 2DQON 230^ | 24()ON , 250| ON , 260^~
RESISTIVITY
N:2
N:3
N:4
NiS
N:6
MX CHG.Nil
N:2
Ni3
N:4
N:5
N:6
60pN | 70pNS , 50pS | 40pS t 30pS | 20pS | IQpS N , 20pN | 30)N , 40pN 19CJON | 20C)ON 220| ON , 230| ON , 24C|DN , 250| ON | 26CJON | 270( ON
n-.'l't&'T-'tef'-) H-aj7 ~i*(s) .6, 24.8 27^2 -58.1 11.1 9
0 *28.
23.5 23.5
2.9 /24.1 21.3 23
4.7 22-0 21-7
RESISTIVITYNil
Ns2
Ni3
N)4
N:5
N:6
35.0
MX CHG. 12.t ,,,7 1.7 1.4 .8 .5 .1 .5 .6 .4 Nil
1.5 1.0 .3 .6 .8 .0 Ni2
.0 1-5 .9 .8 .9 -.1 Ni3
1.2 1.5 1.3 1.1 .1 Nt4
1-3 1.6 1.6 .6 N:5
Zv.0 1.5 2-0 .9 N:6
LINE : 600 E
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRRY
DEPTH POIMT
N ; 1. 2. 3. 4. "fi" SPRCING : 100.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND, GRID-1
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE = l: 2400JVX LTD.
14(]OS 12qOS lO IjOS t 9 0pS , 80pS t 7 0ps t SOpS | SOpS t 4 0pS L 30pS , 20pS--- — --- -""- - —— - ON , lOpN t 20pN , SOpN t 40pN | SOpN t 60pN t 70pN— — .-... 90N
RESISTIVITY
12(]ON 14(]ON | ISOCON 20QON | 220| ON , 23QON | 240| ON t 250| ON t 260) ON t 270| ON t 280( ON | 29QON
Nil
Nt2
Nt3
Ni4
NiS
N)6
5.4K
MX CHG.
N:2
Ni3
N)4
N)5
N:6
9.roo4.3K 8
10. IK *
Sops | 70pS pS | 40pS | 30ps , 20pS 20QN 8 3QpN , 40pN | SOpN ( 6QpN | 70pN | 80pN , 90p 230| ON t 240| ON | 250| ON | 260| ON | 270( ON , 28CJON t 290( ON
19.1 24.4 23.3 20.2 24
RESISTIVITY Nil
Ni2
Ni3
N:4
NiS
NiB
MX CHG. Nil
37.2
1.0 1.0 1.2 .9 .7 .4 -.1 -.4 -.4 -2.0
1.3 1-4 1.4 1.2 1.0 .8 .1 -.4 -.6 -2-2 Ni2
1-6 1.7 1.4 1.3 1.0 .3 -.3 -.6 -2-2 Ni3
9 1.8 1.3 1.3 .6 .0 -.4 -2.0 N:4
1.8 1.4 .8 .4 -.2 -1.7 NiS
1.9 1-8 1.0 .4 .3 -1.5 N:6
LINE : 1200 E
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRRY
Dcrrx'VoiNT
N r 1. 2. 3. 4. ... •fi" SPRCING = 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND, GRID-1
RED LflKE flREflOflTE i WINTER 1996 REF : 9602
SCflLE = l : 2400JVX LTD-
RESISTIVITY
12QQS (11DQS t l ODDS | 900S | BOOS | 7005 t 60QS t 5003 | 40DS , 30pS VHO") ~~""n-."i~ "M H fl)
Nil
N:2
N:3
N:4
43.7K
N:6
RESISTIVITY 4.2K Nil
N:2
N:3
Ni4
NiS
Ni6
MX CHG. MX CHG Nil
Ni2
NO
Ni4
Ni5
8.17*20
52N04SW0144 2 17420 DOME 240
Grid lPlate 3
LINE : O E
INDUCED POLflRIZfiTION SURVEY
POLE-DIPOLE RRRflY
N r 1. 2. 3. 4. ... "fl" SPHCING = 100.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND.GRID-1
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCRLE ^ 1: 2400
JVX LTD-
1600S 14(|OS , 130,05 , 120,05 100,05 , 90p5 , 80pS , 70ps , 60pS | 50pS i 40pS i 30pS , 20pS , lops , ON , IPpN | 20pN , 30pN , 40pN , 50pN , 60pN | 70pN , 80pN , 90pN lOqON , liqON , 12CJON , 13qON , 14qON 16(}ON , 17tjON 19qON , 20(}ON 2KJON
TflU THU
N:2
N:3
N:4
N:5
N:6
•3 -l -l .0 .0 .0 .0 .1 -O -l -O .0 v .2.0, -O -O N:l
•5 -l -l .1 .0 .0 .0 .5 .1 .0 -O .0 -5 .0 -O .0 Ns2
•3 -5 .3 .0 -O .0 1-0 .1 -l .0 .0 .5 .0 -O -O 1.0 N:3
• 5 -l -5 .0 .5 .3 1.0 -3 -l .1 .1 .5 -O .0 .0 .1 .0 N;4
•3 -3 .0 .1 .1 -O .3 .3 .3 .3 .5 .1 .0 .0 .3 .0 N:5
• 5 -3 -O .1 .3 /2tf^^tt^\ . 3 .3 .3 .5 .1 .1 .0 .1 .0 N:6
16QOS 13qOS , 120,05 , liqOS 90pS , 80pS | 70pS 40pS 20pS , IQpS , ON , 10pN , 20pN , 30pN , 40pN t 50pH , 60pN t 70pN 12qDN | 13qON , 14qON 17ON 19qON , 20qON , 2iqON
SPECTRflL MNil
N:2
N:3
N:4
N:5
N:6
221.8 336.8 /52.9
340.1 2X1-6 .827.6*,'
279.3
4.0, 200.9 171.0 183
168.1 183.7
5.6 165.4
.3 160.1 194.6^^^\\
'86.4 IB'7.6 159-3 188-5/^76.4 35).2 60.7
166^5 159.6 191.7/^1.2 5V^3/ 53.7/^34.1
.8 149.4 119.3. .44,8 . 62.4 48,1 .16.9 13.9
l 64.3 65.4
50.3 67.5 62.6 59
15
121.7 l
l 128.9 120
07.4 .85.7
''106.7 "
120.1 96/
.3 109.4
14.7 102.
2 115.3
,7*4 33.4
38.0
llSfl101?4 96.4
SPECTRflL M Nil
Ni2
N:3
N:4
N:5
N:6
LINE : 300 E
INDUCED POLflRIZfiTION SURVEY
POLE-DIPOLE RRRflY
DEPTH POINT
N ^ 1. 2. 3. 4. ..-
•fl" SPflCING - 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND-GRID-1
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE - 1 : 2400
JVX LTD-
14(OS 90pS 70fS , 60pS 40pS , 30pS t 20pS 20pN , 30pN t 40pN , 50pN , 60pN 70pN 90pN , IQtjON 12()ON , 13qON , 14qON . 16(|ON , 17qON , ISqON , 19(jON , 20qON , 2iqON 230^ , 24CJON , 25qON . 26IJON 27qON
TflU8-0
N:2
N:3
N:4
N:5
N:6
O 8^ 4-0^ 2-0 4-0 i^^ 4.0 2-0 ^-OJS 1-0 .3 -O I-O .5
O .0 -O .1
-l .0 .0 .3
O .5 .0 .0 m.o .o .0
TflU -O N:l
N:2
N:3
N:4
N:5
N:6
ISQOS 13^03 | 12QOS t H OPS t 1 0QOS | 90pS i BOpS | 70pS , 60pS 40pS | 30pS i 20pS 20pN [ 30pN t 40pN | SOpN | 60pN | 70pN g B OpN , 90pN 120ON M^ON , IStjON 19qON | 200| OH i 2 10| ON | 220| ON | 23^ t 2 40| ON | 25(jON 2600N 27QON
SPECTRflL MNsl 230.8-1000.0 172,5, 234.1. 458.1__341.6 398.2 264.2 265.9
N:2 176.5 l
Ni3
N;4
N;5
N:6
189.
y 30.2 23.1
291
136^4 141.1 .277.1. 299.8 -633.1 137.7 124.4 8SPECTRflL M
N:l
N:2
N:3
N:4
N:5
N:6
LINE : 600 E
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
H = l . 2. 3. 4, ... *H" SPHCING = 1 00.0 FEET
FREEWEST RESOURCES
MCKENZIE ISLflND.GRID-1
RED LflKE flREflDflTE i WINTER 1996 REF : 9602
SCfiLE - l : 2400JVX LTD.
TflU
N:2
N:3
N:4
N:5
N:6
14QOS 13DOS | 12QOS HOPS l OOPS 9005 80QS 70pS | 600S t SOpS | 40pS | 30ps | 20pS t lOps [ Of) | IPpN [ 20pN | 30pN t 40pN | SOpN t 60pN 70pN g BOpN | 90QN | 10QON | UPON [ 12qON t 1 300N | 14qON | ISqON | ISqON | 17qON | IBqON 19qON | 20QON 2iqON | 22QON | 23QON 24QON
B O 16J) - 1. 2-0 Z.. - . ^
250[ ON | 260| ON | 27(|ON | 2BO| ON | 2900N
-O ^ 48-0 1&- 5 .0 .0 .1 .0 .0
.0 -O .0 .0 -O .0
O .0 -O .1 .1 -O -O -O
-O// .0 .0 .0 .0 l .0 -O .0 .0 -O .1 .0 -O -O -O
.0 .0 .0 .0 .0 .0 .0 .0 .0 .0 .1 .0 .0 .0
-o .o -o .o .o .o -o .o -o .o -i .o -o -o
TflU N:l
N:2
N:3
N:4
N:5
N:6
140,05 ,130,0s t 12qOS 90pS , 80pS , 70D5 , 60pS 40pS , 30pS , 20pSflu ''
ci OM
N , 20pN , 30pN , 40pN , 50pN , 60pN , 70pN , 80pN T 90pN , 10()ON , HCJON , IZCjONfl"
N , 17()ON 2i qON 23qON , 24(]ON , 25CJON . eeqON | 270| ON 2800N 2900N
SPECTRRL M225.4 273-3 262-9 233.3 279.6 240-6, .88^4^105.9
N:2
N:3
N:4
N:5
N:6
289.1 299-4 238-2 300
i.3 /266-325. .3 296-
271.8 yg&.Z 3 64.4
332-1 379.5
394.0
31^.8 406.1 257^^09.0 354.3 258.2 fl9
" 450.4 467.4 446.8 355.3 2^2.2 19J.8
6 465.0 463.1
408
3 428.5
481-9 460.7
.0 470-1 5 J(L^ 2 97
408-5 500.1 316-
2 ^18.0, 23.1 V8.32i).6 29.7
25.2 22.4 25.4
3 30-3 ^,28-Q 23.6
28.4 34-6
22
9.6
1.0 35-7 42.3
31-5 33-9
SPECTRflL M N:l
N:2
N:3
N:4
N:5
N:6
LINE : 1200 E
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
, NO . R ,
•-HD, ^
DCPTH'VaiNT
N r 1 . 2. 3. 4. ... "H" SPHCING = 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND, GRID-1
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE r 1 : 2400JVX LTD.
1200S HDDS lOqOS 90pS 80pS TODS 60pS 50pS 40pS 30ps
TflU TflU N:l 8.0 16.0 16.0 J^O -1 4-0 ^2.0 1.0 2-0 1-0 N:l
N:2 16-0 ^̂ ^^-^^ 1 ' 0 ^— -^^y 4 " 0 \U 0 {Z^O^/l- 0 N s2
N:3 . ^2' . 0 -0^^^ "^-O^Viis.^ . \ N :3
N:5 -0 ^^V^1^/^^^ ' 0 ' 0 N S5
N:6 .0 J^^^^^ff -0 -0 N:6
1200S 11QOS 1000S SODS 80PS 70Q5 60PS 50QS 40QS 300ST —— i —— 3 —— i —— ̂ —— i —— F —— i —— F —— i —— F —— i —— F —— i —— F —— i —— F —— ' —— T
SPECTRflL M SPECTRflL M N:l 266.3 421.7 y 58,7 43-3 37^ 306-9 265-1 234-3 213-7 199-9 N:l
N:2 395.2 l^a^^A^^^^5^^.Z\^2^. 1 32a*Tcg37.7 230-2 N:2
N:3 . Q-^^^.O .̂ VM^.4 /T^S^Az. 3 Sw7^2 — *33^8 N:3
Ni4 .0 .0 fflj^l T'^^^^^^^\ (^OK N' 4
NiS .0 •0:^^v^^3.0^n) .O^Q\.6 Ni5
Ni6 .0 ^fl ^ — HJ ———— .0 ;^ Ni6
52N04SWD144 2 17420 DOME 250
Grid lPlate 3 a
LINE : -1500 W
INDUCED POLRRIZflTION SURVEY
POLE-DIPOLE flRRflY
Z?]___fl.
Dtrin'raiNTN r I. 2. 3. 4. ...
•H" SPHCING - 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND. GRID-1
RED LflKE flREflOflTE s WINTER 1996 REF : 9602
SCflLE - 1 : 2400
JVX LTD-
legos nqos isqos , isqos 14903 , isqos , i2qos ; iiqos , logos , aops , sops t vops , sops , jops 40ps , aops z^ips tops i op i iopN t 20pN t aopN , 4opN t sopn sopN- — -~ -— — — — - — —-— — — - — ——
RESISTIVITY72.0 81.0 99.0 139.0 153-0 212-0 205.0 258-021,2- 3,OK 3-7K
N:2
N:3
N:4
N:S
N:6
123-0 148-0 178.0 172-0 2^.0 262
239-0 32190.0
272.0 223.0 230.0 239-0 299-
260-0 263.0 256.0 31^xtn 243
308.0 291.0 3*fTo 272.
297
I/^T)^
247
RESISTIVITY N:l
N:2
N:3
N:4
N:5
N:6
12qOS | li 90pS i 80pS t 70pS , SOpS
MX CHO.Nil
Ni2
Ni3
N:4
N:S
N:6
.1 .1 -.2 -.2 -1-2 -1.1 -1.9 -2.7
.2 .1 -.7 -2-1 -2-7 -3.7 -4-8
.0 -1.2 -3-0 -4.7 -6-3 -6.8 -7.7
-.8 -3.5 -6-2 -8-7 -8.8 -8-6
-3.6 -7.0 -10.0 -10-3 -9.2 -6-4
-7.6 -12-0 -11.8 -9.4 -5-9
-5.9
40s IPpS pN t 20pN , 30pN N t S OpN
-6 -9.0 -10
-8.2 -9.1 -
-8-1 -5-2 -28
J 1.6 -.3 -.7 -.5 -.5 -1.7 -1.5 -.3 -1.6,,,.10,2 11-1
3 -1.0 -7 -.8 --8 -.7 -2-1 -2-3 -1.8 -1.4/^TD^ 11-2
-.8 -2-8 -O -.8 -.9 -2-3 -2-5 -2.2 -1.6,^VO 11-1
O -4-6 -3-2 .0 -.8 -2.4 -2-6 -2-3
16-4 -4-9 -3-0 -.1 -2.3 -2-8 -2.5
4 -14.4 -3- T -2.0 -1-6 -2.7 -2-6 -.9
11.3
11.6
11.8
MX CHG. N:l
N:2
N:3
N:4
N:5
N:6
LINE : -1200 W
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRflY
RESISTIVITY
legos | nqos i isqos i isqos nqos i isqos i i 2qos | iiqos t logos i gops t aops t 7ops r sops i sops t 4ops , 3ops 20ps i t opsJTs2. ''' .--.--. -j^
89-0
20pN , 30pN , 40pN 60pN
fl.
N : l . 2. 3. 4. ... fl" SPHCING = 100.0 FEET
N:2
N:3
N:4
N:5
N:6
RESISTIVITY N:l
N:2
N:3
N:4
N:6
MX CHG-
isqos t nqos i isqos j isqos f uqos , isqos t i 2qos ,iiqos ,logos t gops t aops , 7ops , sops i sops , 4pps . sops 20ps t tops*!"T- s
IQpN | 20pN , 30pN N , 60pN 70pN
FREEWEST RESOURCESMCKENZIE ISLflND, GRID-1
RED LflKE flREflOflTE : WINTER 1996 REF : 9602
N:2
N:3
N:4
N:5
N:6
.2 -2-3 -.1
-1.6
.4 .3 -.1 -1.2 -1.3 .6 1.0 .1 1.4 -2
.9 .2 -1.0 -1.3 .7 1.4 .2 l
.8 -.7 -1.0 .9 1.7 .4 1.5
-.1 -.7 1.2 2.0 .4 1.7/^
-.1 1.6^/2.4/v .4 1.9 .1
2.l/ 2.8 f . 7 2.0 -.1 2
-2.8 -.6 5. 11.4 21^ 9.0
-.9
MX CHO. N:l
N:2
N:3
N:4
N:5
N:6
SCflLE r 1: 2400
JVX LTD.
LINE : -900 W
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
N r 1. 2. 3. 4. ... "R" SPflCING = 100.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND, GRID-1
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE r Is 2400
JVX LTD.
RESISTIVITY
legos t nqos , legos t i sqos i nqos , isqos , 12^05 , nqos , logos , gops aops , ?ops t eops t sops , 4ops ^sops ^P5 , 1 0PS , Of t 1 0PN , 20PN , 30pN i 40pn i sopN . eopN ?o
941.0 546*0 480-0^654.RESISTIVITY
N:l
N:2
N:3
N:4
N:5
N:6
MX CHG.
N:2
N:3
N:4
N:5
N:6
S t SOOS , 400S , 30QS , 20pS t 1 00S N | 30pN | 40pN11QOS 10QO1800S 17QOS
S.l. 1.4.9 . 28-5 .25.0 ,17 5.6 4-3. 2.7 1.3.3 -2.5 ...6v3 8.0 1.1-0 .19-2. 26-5 .15.3 14.0 l
5.3 4.5 4.2
10.S/ 6-
11-1 f 8 -1
LINE : -600 W
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
f^•*. e*vvrm mm
N r 1. l , 3 . 4."fi" SPflClNO s^lTJO.O FEET
FREEWEST RESOURCESMCKENZIE ISLflND, GRID-1
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400
JVX LTD-
isqos i nqos , isqos T isqos^ nqos , isgos , i2qos i iiqos i logos , gops sops , 7ops i eopsRESISTIVITY
449-0 433,0 664*^X546.0 577-0 567.0 523.0 47S.o33-rfl
RESISTIVITYN: l
N:2
N:3
N:4
N:5
N:6
isqos nqos , legos , isqos , uqos i3j|os , izqos , n(|os , logos , sops , eops . ?ops , eops , sops . 4pps sops , 20p5 , tops ^ op , iopN , zppn ...30PN . 40PN . SOPN , SOPN , 70PN , 80PNMX CHG.
h-1 n-5
LINE : -300 W
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
SVDEPTH POIMT
N r 1. 2. 3. 4. ... -H" SPHCINO r 100.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND, GRID-1
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400JVX LTD.
2011.4 13
4.8 23.8 16.9. 10-3^.10.5 14.1 13-1 10.1 14.8 14,8
M^IIT", T-1 M X CHG5 l.l 1.3 1-3 1.3 1.3 1.5 1.3 1.4 1.3 1.2 1-2 1-5 1.7_,2-Q 2-1 1.9 2-1 ^.2-9 3-3
3.17420
nqos legos isqos uqos isqos izqos nqos logos gops , sops , 70ps , eops sops . 40ps , sops 2ops tops , op iopN^ ̂ 20pN , sopN , 4opN , sopN , eopN , 7opN , 800J4 - ,J"P-N-L1 "(]0^ - | 1C1QN - 1 2tP 1 3(ION isqoN
RESISTIVITYn'5 n^6
N:2
N:3
N:4
N:5
N:6
19604^^95.0362^0 23^-0203RESISTIVITY
N:l
N:2
N:3
N:4
N:5
N:6
17QJ isqos 14905 ISQOS i2qos iitjos , logos , gops
j-p-3*
S 70pS i 60pS , SOpS | 40pS t 30pS , 20pS op . iopN . 20pN , sopN , 40pN . sopN i sopN . 7opN . 8opN gopN i2oN uqoN , isqoN . leqoN , nqoN , leqoN
MX CHG.N: l
N:2
N:3
N:4
N:5
N:6
4-5 4.8 4-Q ^2-4 2-4 2-5 2.4 2-0.^1.6
2.6
n-'S S ^U- (62, T- 2(3) ^-2-0 2.92-2 2.1 2-3 2.1 2-0 ^1.9 1.4 LO8 . 4.1 . 7.0 6.8 7.4 6-2^ 4.4
3-9 5.8 5.1
13.2 14.4 11.1 11.2 10.6
9.1 8-1 7.7 6.7 7-0 7.8
9.3 8-9 8.4 7-7 8-7
8.8 6-4
8.2 6-6 9.5 7.Q
MX CHG. N-.l
N:2
N:3
N:4
N:5
N:6
O (D CM
Grid lPlate 4
LINE : -1500 W
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRRY
\ VoertH POINT
N - l . 2. 3. 4. ... •fl" SPflCING ^ 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND.GRID-1
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE - 1 : 2400JVX LTD-
TflU
N:2
N:3
N:4
N:5
N:6
SPECTRflL M
N:2
N:3
N:4
N:5
N:6
ISQOS , i7([os legos isqos , uqos 1 1 3^05 1 12^03 , iiqos , logos . gops | aop5 | 70ps .eops , sops , 40ps i sops i zops , tops iopN , 20pN i sopN i 40pN , sopN i eopN
TflU 2.0 Nil
legos , nqos , isqos i isqos , uqos , isqos t i 2qos | nqos t logos , gpps , sops , 7ops , eops , sops t 4pps sops t 20ps , iops , ON 20N 40pN
.0 .0 ^g.8 4.4 -19.7 -15.6 24-1 -35-1
.0 -10.2 'flFa.. -34.3 -47-8 -62.6 -75W ^ *~^JSf . 0 -38.9 l^p .1) -78.8 -85-2 -95-8
.0 -46.2 -78.4 -107.9 -108-8 -106-6 -86
-48.1 -88.3 -127.7 -127.0 -115-2 -82-9
-94.8 14AS3V-148.4 -116-3 -79-7 6,
•3 4J)K,y2.4 -23-3 -21-5 4.9 -41.
VoTffr^qPKl -27.2 -30-6 -23-4 Ms&Z
.4 144.6
SPECTRflL M N:l
Nt2
N:3
N:4
N:5
N:6
LINE : -1200 W
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRRY
DEPTH "
N - 1. 2. 3. 4. .-.
H" SPRCING s 100-0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND,GRID-l
RED LflKE flREflDflTE : WINTER 1996
SCflLE - 1 : 2400JVX LTD-
TRU
N:2
N:3
N:4
N:5
N:6
SPECTRflL M
legos i nqos t teqos | isqos i uqos , isqos t i zqos iiiqos , logos i sops i apps , 70ps t sops , sops t 4cps , sops i 20ps i lops , ON , iopN | 2opN i sopN i 40pN t sopN i eopN i 7ppNTRU
.o .o .o...ia.o. ..4 •o .1 .o .o
.1 .0—— .3 .0.0 .3 -O -O
.0 .0 .0 -O .0 .0
.0 .0 .0 .0
.0 .0 .0 .0
1800S | 1700S | 16QOS t 1SOOS ( 14QOS 13QOS , 1200S i H OPS | 10QOS , 90DS | 800S 7QOS | 60pS . 50pS t 40pS [ 30pS | 20pS | IQpS | ON | IPpN t 20pN | 30pN t 40pN t 50pN | 60pN t 70pN
SPECTRflL M ,253.0 136.6 N:l
LINE : -900 W
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRRY
N - 1 . 2. 3. 4. ... fl" SPflCING - 100.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND,GRID-1
RED LflKE flREflDRTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400
JVX LTD-
TflU
N:2
N:3
N:4
N:5
N:6
isqos i nqos , legos t isqos , uqos , isqos i i 2qos , iiqos t logos t gops , aops , 7ops , 60ps i sops , 4pps i sops i 20ps , tops | ON t iopN t 20pN , sopN , 4QpN , sopN t eopN t 70pNTflU
48-0 N:l
N:2
N:3
N:4
N:5
N:6
-l 1.0 .1 l
nqos t legos t i sqos 114(^05 , isqos 112^03 i nqos tioqos i gops , sops , 70ps sops , sops , 40ps , sops t 20ps t l ops t op t i opN i 2ppN i sopN t 4ppN , sopN t sopN t 7gpN
SPECTRflL M
N:2
N:3
N:4
N:5
N:6
99.9 137.4| 221.7 294.4 189^4 170-1 195SPECTRflL M
N:l
N:2
N:3
N:4
N:5
N:6
LINE : -600 W
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRflY
N s 1. 2. 3. 4. ..."fl" SPflCING = 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND.GRID-1
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE = 1: 2400
JVX LTD.
TflU
leqos i nqos , legos i isqos i uqos i isqos 112^03 t t iqos t I OCJQS i sops i aops i 7ops t eops i sops , 40ps t sops i aops i lops
4.0 . .0 -O .0 -O -O ... 4-0. ... -5 . .2.0 2-0 . 2-0 . 4-0 . 2-Q 20. 4-0
3N t IQpIQN 30pN | 40pN t 50pN , SOpN | 70pN | 80pN t 90pN nqoN i isqoN
N:3
N:4
N:5
TflU .1 -5 -l -l -O .5 -O .3 -O N:l
.1 .1 .1 .1 -l -l .3 .0 N:2
•S .0 -l -l .1 .1 -l .1 N:3
.3 -O -l .1 .3 -l .0 N:4
•3 -l .0 .1 .1 .t .0 N:5
.1 l .1 .0 N:6
isqos i nqos , legos i isqos i nqos t isqos 1 120^5 i iiqos , logos i gops , sops t 7ops i sops . sops , 4ops . sops i zops L lops t ON i iopN i 20pN t sopN t 4opN [ sopN i eopN i 70pN t sopN ( gopN N T 12^ t isqoN UPON ISOON , IBQON nooN i ISQONSPECTRflL M
45.1
N:2
N:3
N:4
N:5
N:6
126.6 129-0 . 170-3 157.3. 124.4 176.1 178-2 15.0 17.7 17-9 17.5 17.4^.20.1 16.8 17.9 16.8 15-7 17.2^^19.7 26.9, 30-6 36-1 S ———————————————-———————— ————————————^^————————-^^- ^-0^
4 24.4 26.0 28-4 29.0 25.9 26.5 25-4 24.7
142
-2 35.5 38.6 33.7 32-9 TTT*
2 48.8 43-7 43-9 41-0 38-3 37-5 36-3
45.3 44.7 42-1 42.4 42.
61-7 S3.r\49.2 48-0 46.4 47.3
81
84.8 93-6
80-2 81.3 lltf.8 159.3
-6 92.1 ^rfS.2 16CX6
99-4/124.7 106^8
SPECTRRL M N:l
N:2
N:3
N:4
N:5
N:6
LINE : -300 W
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRRY
- l
N = 1. 2. 3. 4. ... "fl" SPflCING - 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND.GRID-1
RED LflKE flREflDflTE s WINTER 1996 REF : 9602
SCflLE r 1: 2400JVX LTD.
2.1742015CJOS 90pS 70S SOpS t 40pS ( 30pS t 20pS ON | 10pN 30pN | 40pN 90pN t 1C(|ON 12(]ON 17QQN | I800N 19QON
TflU TflU
N:2
N:3
N:4
N:5
N:6
2-0 . 1.0 . 2.0 . . .5 l .0 ^ l .0 . 2-0 . . .5.5 .3 .1 -l 2-0 . 1.0 , 2.0 2.0 2-0, , .3 .3 -l .3 -O .0 .0 -O .3 .Q .Q .o
1-0 .5 .3 -3 2.0^ 2.0 2.0 2-0 / ^ .3 .5 .0 -l .0 -l -O
ri-o__i.o i.5 .5 .3 .3
.5 .5 .5 .3
1.0 -5 .5 .5 -5 .s i.\o r.q f re1-0 .5 1-0 • O /I.O 1-0
2.0
1-0
1.0 1.0 -5 .5 .5 l
.1 .0 .0 -l -l .1 .0
.1 .1 .0 -l -l .1 .0
.1 .0 .1 .1 .1 .3
l .0 .3 .0 -l -l
N:2
N:3
N:4
N:5
N:6
90pS t 80pS | 70pS | 60pS 40pS t 30ps t 20pS N i IQpIQN 30pN | 40pN 60pN | 70pN 80pN | 90pN | 10C|ON 15C|ON | 1600N i 1 7QON | 18QON i 19Q ON
SPECTRflL M
N:2
N:3
N:4
N:5
N:6
58-9 60.3 51-4 31.2 31.3 36.9 32-3
51.3 73.S 64.8
50.2 ?'l.l^^7^ri^^64.2 67.5 67
80.9 94.7 88.0
'O/ 117.0 110.7 108-1 -"-89.8
78.9 51.2
122-1
31.9 128-6 120.3
138.0 130.5 116
141.0 137.2 125.6
139.8 130.1 100
4.6 28.1^28^7 30.2 .2JL-0 26.2 24-2
38.4 40.7 38.5 35-8 34.
47.1 45-4 42.5 39.7 35-1
53.1 SIT*-^ 48.1 45.8 42-5 38.0 35-3
64-8 57.1 53.7 SIS^ 46.7 42.7 41.1 37-1
68.4 59.0 56.1 53-5N47.8 45.4 42-2 43.0 8 118.6 133.9 100-2
SPECTRflL *
Ns2
N:3
N:4
N:5
N:6
O N. CM
Grid lPlate 4a
o oCO
O O
O O (M
O O O
o oOD
O O CO
O O
O O CM
UJ CO CC CD
O O (M
O O
O O CO
LU
O O CO
UJ
O Oo
UJ
o oCM
UJ
o o o
oCD
2400 N 2400 N
1200 N
O
300 S
600 S 600 S
900 S 900 S
52N04SWD144 2.17420 DOME 280
1800 S 1800 S
o oCO
o o
o oCM
o o o
o o00
o oCO
o o
o o(NJ
UJ
LU COcr03
UJ
ooCM
UJ
o o
o oCO
UJ
o oCO
o o o
UJ
o oCM
FREEWEST RESOURCES CANADA INC.
MCKENZIE ISLAND PROPERTY - GRID zRED LAKE MINES and MINERALS DIVISION
______________N.T.S. 52 N/4 ___________-
CHARGEABILITY CONTOURS (11=2)CONTOUR INTERVALS : 2 it 1 0 mV/V
TIME WINDOW 310-1050 ms
SURVEYED BY JVX LTD. USINGSCINTREX IPR-12 Rx ; IPC-7/2.5 kW Tx
WINTER 1996
200 400 600
PLOTTED BYA.S.
FEB. 1 996SCALE 1 :2400 PLATE l
JVX ref. no. 9602
LINE : -1200 S
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRflY
ffl.
acrm'nunN : 1. 2. 3. 4. ...
•R" SPflCINO = 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND,GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE = 1: 2400JVX LTD-
RESISTIVITY
MX CHO.
N:2
N:3
N:4
N:5
N:6
N:2
N:3
N:4
N:5
N:6
1300N 12QOH , IIQON , 1000H , 900H , 80QH1 * * 60QH 40 VofP"d(A 0p"dl\ 10pH—"E-'-'.gPJ-'JiT 30 P E - 40 P E 50P E
6K
RESISTIVITY O N:l
N:2
N:3
N:4
N:5
N:6
OE , IPpE , 20pE , 30pE , 40pE , 50pE
MX CHG. 5.,l 8.2 N:l
N:2
N:3
N:4
N:5
N:6
LINE : -1500 S
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRRY
DEfTM'VoillT
N r 1. 2. 3. 4, ...
'IT 8PHCING ^TTJOTQ -Hit T
FREEWEST RESOURCESMCKENZIE ISLflND.GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400JVX LTD-
90HpH | 80pH | 70pN | 60J3H 2DpE . 30pE 40pE | 50pE
RESISTIVITY
N:2
N:3
N:4
N:5
N:6
7K
9K
RESISTIVITY N:l
N:2
N:3
N:4
N:5
N:6
MX CHG.
90H 80H
-3.5
20pE . 30pE , 40pE , 50pE
MX CHG. N:l
N:2
N:3
N:4
N:5
N:6
LINE : -1800 S
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
V'DEPTH POINT
N = l, 2, 3, 4 . ...
"fl" SPflCINO - 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND-GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE = 1: 2400JVX LTD-
20pE . 30pE 40pE { 50pE
RESISTIVITY
N:2
N:3
N:4
N:5
N:6
RESISTIVIT N:l
N:2
N:3
N:4
N:5
N:6
20pE : 30pE : 40pE | 50pE
MX CHG.
N:2
N:3
N:4
N:5
N:6
X CHG. N:l
N:2
N:3
N:4
N:5
N:6
O O) CM
Grid 2Plate 7
LINE : -1200 S
INDUCED POLflRIZRTIQN SURVEY
POLE-DIPOLE flRRRY
ffl.
N s 1. 2. 3. 4. ... •fl" SPHCINB s 100.0 FEET
FREEWEST RESOURCESMCKENZIEISLflND, GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE = 1: 2400JVX LTD-
13(OH13(] 80pH SOpH H | 20pH IQDE | 20pE , 30pE , 400E , 50PE
THU TflUNil
N:2
N:3
N:4
N:5
N:6
13(OH 12(DH 90H SOpH 20pE ; 3QpE | 40pE
SPECTRflL M
N:2
N:3
N:4
N:5
N:6
SPECTRflL M 6 N:l
N:2
N:3
N:4
N:5
N:6
LINE : -1500 S
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRRY
DEPTH'ValMT
N r 1. 2. 3. 4. ... •H" SPHCING = 1 00.0 FEET
FREEWEST RESOURCESMCKENZIEISLflND,GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400JVX LTD.
H i 70pH u | 40pH | 30pH , 20pH IQpE | 20pE . 30pE , 40pE
TflU TflU.1 LO
N:2
N:3
N:4
N:5
N:6
l .3 1.0 .3
N:2
N:3
N:4
N:5
N:6
80pH t 70pH | 60pH 40pU | 30pH 20pE . 30pE , 4ppE [ 50pE
SPECTRflL (1
N:2
N:3
N:4
N:S
N:6
SPECTRflL M 51.2 N:l
N:2
N:3
N:4
N:5
N:6
LINE : -1800 S
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
N s 1. 2. 3. 4. ... •fl" SPRCING :; 100.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND, GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE - 1 : 2400
JVX LTD-
20pE , 30pE , 40pE , 50pE
TflU
N:2
N:3
N:4
N:5
N:6
90pH , 80pH | 70pH , 60pH 0pH 10pV4 , 20pE | 30pE , 40pE { 50pE
SPECTRflL M
N:2
N:3
N:4
N:5
N:6
51
60
SPECTRflL M N:l
N:2
N:3
N:4
N:5
N:6
O O CO
Grid 2Plate 7a
LINE : O N
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRflY
-0,
OtPTH POINT
N r 1. 2. 3. 4. ... •R- SPflCIMO - 1 00.0 FEET
FREEWEST RESOURCES
MCKENZIE ISLflND.GRID-2
RED LflKE flREflDflTE : WINTER 1995 REF : 9602
SCflLE r 1: 2400
JVX LTD-
TRU
Nt2
Nt3
N:4
N:5
N:6
SPECTRflL MNil
N:2
Ni3
N:4
N:5
N:6
80pH 60pH 50pH , 40pH —— 30pH i 2DpM IQpH OE 20pE 30pE , 40pE , SOpE 60pE 70pE 80pE i 90pE , IQtjOE 12()OE , 13qOE | 14()OE
4-0 . 2,0 2-0 N:I
48.0 \\ V O .0 .3
.0 -O .3 .5 -3 -O
80pH , 70pH M 30pH 20pH OE , IQpE 20pE 30pE 40pE , 50pE 60pE , 70pE , 80pE | 90pE 12QOE , 1300E L 1400E
24-1 25.5 27.8 27.4 l 122. .9 142.4 170.5
-40.3
292.1^78.5.9, 1 39 - 7
279.3 27L8MOOO.O
'/m 249.7 23Ts2
281.^447.0
l
C^B^rHlS -4
SPECTRRL M N:1
N:2
N:3
N:4
N:5
N:6
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRflY
fi.\ .' V
DEPTH POINT
N - L 2. 3. 4. ...
•fl" SPflCING r 100.0 FEET
FREEWEST RESOURCES
MCKENZIE ISLflND.GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400JVX LTD-
H , 121JOH H , 7DpH | 60pH , SOpH , 40pH [ 30pH OE , IQpE | 20pE t 30pE , 40pg , 50pE , 60pE , 70pE | 80pE | 90pE 12(}OE 1400E 16qOE 17qOE
TflU4-0 . 2..0 v LO LO
N:2
N:3
N:4
N:5
N:6
8.0 .1 .5 .5 LO ,1,.0
.1 .5 LO J l .t^T~
O -3 -S LO LO
.5 .5 .5 LO .5 LO .5 LO l -0,^, LO
.5 -5 .5 .5 .5 LO .5 .5 MJ ,-
.5 li
.4-0
.5 .5 .5 .3 .5 LO .5
TflU O, 16.0 N:l
N:2
N:3
N:4
N:5
N:6
SPECTRRL M
| 13qOH t 12Q.OH { HOOK IpqOH | 90pH , 80pH | 70pH t 60pH t 50pH , 40pH | 3DpU i 20pH , 10pH , OE | IPpE i 20pE 30pE , 40pE , 50pE | 60pE | 70pE t 80pE t 90pE , IQCJOE , HOPE , IZ^OE t 13(]OE | 14C|OE | ISqOE t IStjOE | 17CJOE
N:5
N:6
o ^—— -^ 74.6 95.2 /i(5feQ3 78-5 d23-6 130-7 116.3 102.2 122.7 136.3 112.0 124.1 119.0
72.0 1021.4/84.4 85.3\ 141.-.3 145.1 127.8 110.1 141.0 152-1 125.5 121.5 115.3 125-6 114.5 138
61.7, 103..5 123.5
106.4 127-0
.1 5L5 56.7 59-7 73.4 299-6
1.3 W.B-224.
119.3
94-8 l-WL-6 125-8 10
3 87.5 9TV7 129.8 133.9 125.
84.1 84.6
77.8 80-• 2 llO.O 18L6 172.3
SPECTRflL M N:l
N:2
N:3
N:4
M:5
N:6
LINE : -600 S
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRflY
fl.
OEPTH^POINT
N - L 2. 3. 4. .-. •fl* SPflCING - 1 00.0 FEET
FREEWEST RESOURCES
MCKENZIE ISLflNDpGRID-2
RED LflKE flREflDRTE : WINTER 1996 REF : 9602
SCflLE = 1: 2400
JVX LTD-
1700H 12QOH 40H | 30U | 20H . OE | 10pE \ 20pE t 30pE , 40pE 70pE i 80pE t 90pE
TflU
N:2
N:3
N:4
N:5
.0 .0 .0 .1 .0 .3 -5 -O LO .3 ^.0 -3 .0 .5 LO 1^0 v 2-^—— L
'• 0 ^v^y/ft v 4 ' 0 \VyLO LO rs-fl— \ LO l V-ffj 4.0 ^^D-~^
8.0 8.0 ^ 4.0
.0 .0 .1 .3 -l .5 .5 LO 1.0 —— 1-0 .1 -S
.1 .0 .3 .5 .3 -l 1.0 1.0 1.0 .5 .3 1.0 .5 LO .5 .5
.0 .0 .5 .5 .3 LO .5 .5 .5 .3 LO .5 .5 -3 .5 LO LO
.3 .0 .5 .1 .5 .5 .5 -5 -l LO -5 -5 -l .3 LO .5
.1 .1 .3 1.0 .5 .5 -5 .1 .5 —rS— —^J -l———-rt .S .0
-' -L'j ^Jo^ - ~~~
8.0
LO
TflU 2-0 N:l
N:2
N:3
N:4
N:5
Ni6
90pH 60H 40H 30U 20H IPU OE 10E 2QE 30E 4QE 60E 80pE | 90pE t I QCJOE 14(OE
SPECTRflL M33-9 33.3 43.9 44.8
N:2
N:3
N:4
N:5
N:6
20
20-5 23.1
25.5
44^8 59.,8 106.1 113.2 H8
T80 oM2.4 123.0 132
.9 125.7 130.6
128.1 129.3 128
•7 130.1 128.7
255 7 300.5 306^6,^15.3
284^0 367. 5o 206.7^0346 — o o
202-4 288.6 219.5 O35L5 32i\B 247.1
611
371
.9 417
SPECTRflL M -3 .264.0 , 153.6. 283.9 153-8 N:l
N:2
N:3
N:4
N:5
N:6
LINE : -900 S
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
DEPTH'*'rOIMT
N r 1. 2. 3. 4. ... •H" SPRCING = 1 00.0 FEET
FREEWEST RESOURCES
MCKENZIE ISLflND.GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400JVX LTD.
TflU
N:2
N:3
N:4
N:5
N:6
SPECTRflL M
N:2
N:3
N:4
N:5
N:6
H , 14qON 200H 30H OE , 10pE t 20pE , 30pE , 40pE 60pE t 7 0pE [ 80pE 9QpE t 10(}OE 12t|O
TflU.0 .0 .0 -O -O .0 .3 .0
.0 .0 -O -O -O .5 .0
.0 .0 .0 .0 -5 .0 LO
.0 .0 -O -l
.0 .0 .0 .3
LO -O -3 .0 8-0. 2.0 2-0 4.0 4.0 N:l
• O -5 -O .0
.0 .0 .0 .0
.5 .0 .0 -O
-O -O -O .0.0 .0 .0 -O -3 ^ ).
.0 .0 .0 .0 .0 .0 .0 .0 .1 .3 -O .0 -O -O -O -O
1700H 70H OE , IQpE t 20pE | 30pE t 4 0pE 60pE t 70pE t 80pE 90pE , IQCJOE , li
LOK,, -O,,. 15 13B..7 208.-6 426-8
j:s~-*e6.
SPECTRflL M N:l
N:2
N:3
N:4
N:5
N:6
7420
oCO
Grid 2Plate 6 a
LINE : O N
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
fl.N - 1 . 2. 3. 4. -..
•fl" SPRCING - 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND, GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE = l: 2400JVX LTD.
RESISTIVITY
Ni6
U 2DpH —— LOpH , OEH i 70pM , 60pH | 50pH 20pE , 30pE r 40pE , SOpE , 60pE 70pE , 80pE , 90QE 1000E , 1100E 1200E' ---61.3K 72.6K 28..0K
^TTR^,
N:l 133.0 85.0 62.0 56-0 65.0 86.0 170.p,,862.0 795.0 563.0, ,2
N:2 203-0
Ns3 154.0 328xKf^22l2lZ3?*^Lll?TrO—2*2TU285.0^^375.0X377.0| 863.0\ ]f.6K——l
N:4 210.0\ f ^"^-^ "———"^ i
Ni5 295.0\ 734.0 934.0 72?7TJ*--*62i0548.063*reN 549.0 704.0 \L1K\ 2\ x-——-—^ ———— V—**S
832395
RESISTIVITY 950.0 N:l
N:2
M:3
N:4
N:5
N:6
^M ~
IH 70pH , 60pt4 , SOpH 40pH 30pn 20pH IPpH OE , IQpE , 20pE , 30pE , 40pE SOpE 60pE , 70pE 80pE , 90pE , IPqOE , HOPE , 1200E ISqOE MODE
MX CHG. MX CHO-
N:2
N:3
N:4
N:5
N:6
2.1 2-3 2.6X ,4.5 B.7. ..31.5 23-5 29.6 16.3
L. l INC.
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
Z?]V'
DEPTH raiHT
N r 1. 2. 3. 4. ... 'H" SPHCING - 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND.GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400
JVX LTD-
1300H 70pH 20pt4 IQE 30pE , 40pE 60pE | 70pE , 80pE 12QDE 14 (|OE 16QOE , 1700E
RESISTIVITY453.0
N:2
N:3
N:4
N:5
N:6
09713
l.OK
l 697.0 864.0 882-0 455.0^58^0 191-0.^136
.0 615-(L 705-0 894-0 59g/S ""^-S.
572/0 494.0 ^B-0 941.
.0 \539-0 5 11.0 Sg2.0
756.0 666TD** COU8^ 857.
.0 971.0 848.0 754.0
11.8K
SK
4K
RESISTIVITY N:l
N:2
N:3
N:4
N:5
N:6
r P-
14QOH p 1300H | 12QOH 10QOH | 900H | 80pH 40pH 20pU | IQpH OE 70pE t 80pE , 90pE , IQCJOE | liqOE | 12QOE , 13QOE
MX CHG.
N:2
N:3
N:4
N:5
N:6
14-9
8.6 . 3,8, 1.9 2.3 , 3.4 3.2. 6-1 .2*6 2.4 1.7 2-7 2
10-2 ^6-3 6.0 5.2 S-SX' 6.8"S^ 5-1 5 -7^" 7 .2 8-5 \5-2 ^xC.7 7.8 10
7.0 6-7 7.3 ^6^3 7.6 8.4 7.1 7.0 8.9 9.4 7.4 8.3 9
5."S\ 7.6 8.0 6-2 9.7 ^---te-^L^ 9-1 8-0 9.6/^ii'^J^s^ 8.8 9-8 9-5
5-^\ 8-2 6-5 6.7 li.l 11.5 ^Q.O 8.4 li.l 12-5 ^9-8 9.5 9
* o.
15QOE 17QO
7.7 9.9 4.9 4.0 4.4
6-7 6-3 7.5 \12-1 12-0 11.3
.5 5/8* ^r\.l 9-ft 13-1 13.3
MX CHG. N:l
N:2
N:3
Ni4
N:5
N:6
LINE : -600 S
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
Z?]____fl
N - l . 2. 3. 4. ... fl" SPRCING : 100-0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND.GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE - 1 : 2400JVX LTD.
1700U II OOH 30n OE 10E 30E 40E 70p 90pE 12CIOE
RESISTIVITY
N:2
N:3
N:4
N:5
N:6
^876-0 920.0 9j
896 O 1.3JS-——UgK 1.2K 1-2K l .3K
l.OK/ 1-7K -2.1K "M-SM——^ .SK 1 .3K
RESISTIVITY 24.IK N:l
N:2
N:3
N:4
N:5
N:6
1700H ISOOU 12QOH 90pH OE 20pE . 30pE
MX CHG.8.5 9.,l
N:2
N:3
N:4
N:5
N:6
10.6
.4 .2 .6 .5 -7 1.4, 2
.7 .4 .9 1.0 1-51-
1.0 .7 1.2 1.5/ 2.
1.2 1-0 1-7 y 2 -2
1.5 1.4 7 2-3 2-
1.7 119 2-7
4 13.0
11.3 12.5 12.9 14.2 12
9.8—-^.
.9 10-2 10.5 10.4 li.'
10.8 10.6 10.2 11.1 13'
.8 11.2 10.3 10-8 12-S"
21,5
10.8 f 1 9.5 16..^
18vl 25.
0 - X17\6 28.6
19.7 j)9.4 30.6(———121.7 22.3 27.6
MX CHG. N:l
N:2
N:3
N:4
N:5
N:6
LINE : -900 S
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRRY
Ifl___fl.\ s
OErTH m l NT
N - 1 . 2. 3. 4, ... •R" SPRCING = 1 00.0 FEET
FREEWEST RESOURCESMCKENZIEISLflND, GRID-2
RED LflKE flREflORTE : WINTER 1996 REF : 9602
SCflLE - 1 : 2400
JVX LTD.
H 90pH SOpH , 70pH | eopu , SOPH , 40pU t 30pu 20pH
RESISTIVITY
10pE , 20pE , 30pE , 40pE , SOpE | 60pE t 70pE , 80pE , 90pE ~~ ~ 12qOE
N:2
N:3
N:4
N:5
N:6
109.0 126.0 147.0 95.0 93.0 118.0 J/76.Q 414,0
194 .fl^^52^ol^369^^?30ja—22^ ^?75jj)^-^58xO
308^\A3^o |2aIq^jHra^n 39a-a--^72TQ 501462.0^/692.0 986-0
674-0 98^0
902
4K
0 754 IK 2-7K
RESISTIVITY N:l
N:2
N:3
N:4
N:5
N:6
rp- 1TP-12QOE
MX CHG.
N:2
N:3
N:4
N:5
N:6
pE t 70pE ; 80pE . 90pE1400M 1300M 12QOU lf\-ivia,r-M-306, T
26.9 25 10.2 12-1 .4.a 7.6 5.85 .1 .2 .2
8.7 8VVH-1.6.0 .3 .4
-.1 .4 .7
MX CHG.14.9
28-8 26.0\19M 28-0
31-53TT5--^29.6 23-8
-4 34.9 33.9 34.5
37.8 37.0 34.8
N:2
N:3
N:4
N:5
N:6
742
Grid 2Plate 6
oCM CO
LINE : 900 N
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
ffl.
DEPTH'VaiMT
N - 1. 2. 3. 4. ... •fl" SPHCING = 1 00.0 FEET
FREENEST RESOURCES
MCKENZIE ISLflND.GRID-2 RED LflKE flREfl
DflTE : WINTER 1996 REF : 9602
SCflLE = 1: 2400JVX LTD-
15(jOH 4 14(|OH t 1 3(}OH , 12(]OH | 1KJOH | 10(|OH , 90pn 70pH 50pH 30pH OE , IQpE ( 20pE , 30pE t 40pE ( 50pE | 60pE , 70pE
TflUNil
N:2
N:3
Ni4
NsS
N:6
SPECTRflL hNil
Ni2
Ni3
Ni4
Ni5
Ni6
.5 .1 .0 .1 .0 .0 .0 .0 .1 .3 -3 .5 .3
.5 .1 -l -l .1 -l -l .1 -3 .3 .3 -S .5
.3 .1 .1 .1 .1 .1 .1 .1 .3 -3 .5 1.0 .5
.3 .1 .1 -l -l .3 .3 -3 -3 .5 .5 1.0 LxD 7 2 .0 2-0 2.0 2-0
2.0 2.0 2.0 2.0 2.0 2.0. .1-0
2-0 2.0 2.0 2-0 2.0
2-0 2-0 2.0 2 .1
.3 .1 .1 .1 .1 .3 .3 .3 .5 .5 1^0 C 2 .0 2.0 2.0 2.0^ ^0 1.0 '
.3 .1 .1 .1 .3 .3 .3 .3 .5 1.0 N.(K 2.0 2.0 2-0 2^0 A 1.0 l
——'J \1-r* * 1.0 N1.0
TflU 512.0 Nil
Ni2
Ni3
Ni4
NiS
N:6
13(|OH , 12CJOH IQCjOH | 90pH 70H 50pH 20pH , IQpH , OE t IQpE , 2QpE t 30pE 60pE | 70pE
2 40.
49.7 37.7 40.8 33.2 35.4 22.2 20.8 21.2 25.8,^28
4-0 41.4
.6 41.8 47-6^-6*
A9-J}——52.8 56.9
.6 61.7 61-3 66
75.0 69-3 72-4
.8 29.5 32.4 42
40.4 41
245.6 251.4 254.1 285.4 292.8
SPECTRflL M Nil
Ni2
Ni3
Ni4
Ni5
Ni6
LINE : 600 N
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
fl.\ *
OEPTH'VoiNT
N —— It t* di 4* BBI
•H" SPHCINB - 1 00.0 FEET
FREEWEST RESOURCES
MCKENZIE ISLflND.GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE = li 2400JVX LTD.
90pH | 60pH , SOpH | 40pH | 30pM t 2 0pH 10pH t OE pE , 70pE , BOpE i 90p
TflUNil
Ni2
Ni3
Ni4
NiS
Ni6
2.0 - 5 - 1 - 0 ' 0 - 1 - 0 - 1 - 0
.5 .0 .1 .1 .0 .1 .0
.5 .0 .5 .5 .0 .0 .0 .1
.0 .5 1.0 .0 .1 .0 -3 .0
~"~~ -3 1.0 .0 -O -O .0 .0 .0
1.0 .0 .0 .0 .0 .0 .0 .0
.0 -O .0 Nil
Ni6
IQCDH BOpH , 70pH t 60pH 30pH , 20pN , IQpH , OE 20pE , 30pE , 40pE , SOpE , SOpE | 70pE , BOpE | 90pE
SPECTRflL MNil
Ni2
Ni3
NU
Nt5
Ni6
18.7 229.3 263,1 427.4.1,39.3 176.77 229.3 263.1 42
353^T*-304o-* 340.7 P.3' 81.8 106.4k o
43
353
•8 339.9 366.4 340-0 428.'
325.9 326.0 360.4 353.3 410-tb \M4^8 150-9
-O 323-3 320-8 409-4 392.2 401^^45.6
18-1 321.0 321.5 443.4 397.6 399.7
82.1 79.9SPECTRflL h
Nil
Ni2
Ni3
Ni4
NiS
Ni6
O CO CO
LINE : 300 N
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
^ f'
OEPtHHrolMT
N ^ 1. 2. 3. 4. ... •H" SPHCINO = 100.0 FEET
FREENEST RESOURCESMCKENZIE ISLflND.GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE = l: 2400
JVX LTD.
BOpH , 70pH , 60pH 40pH [ 30pH , 20pH OE ^ IQpE t 20pE , 30pE , 40pE | SOpE , 60pE , 70pE 90pE , IQIJDE
TflU
N:2
N:3
N:4
N:5
N:6
1KJOH t l OQOM t 90pH , 80pH , 70pH , 60pN , SOpH , 40pN | 30pH , 20pH ZOpE , 30pE | 40pE 60pE , 70pE t BOpE , 90pE , 10(|OE 12 CJOE
SPECTRflL MNil
Ni2
Ni3
N:4
Ni5
Ni6
10.9 19.2 18.6 18.7__17SPECTRflL M
109.0 Nil
Ni2
N:3
Ni4
NiS
Ni6Grid 2
Plate 5 a
LINE : 1800 N
INDUCED POLARIZATION SURVEY
POLE-DIPOLE flRRRY
N = 1. 2 , 3 . 4. .-. "R" SPPCINO r 100.0 FEET
FREENEST RESOURCES
MCKENZIEISLAND.GRID-2
RED LAKE AREADflTE i WINTER 1996 REF i 9602
SCALE r l s 2400
JVX LTD-
70pH , 60pH t 50pH , 40pH , 30pH , H | OE
TflU
N:2
Ni3
Ni4
N:5
N:6 .0 ^ .0
TflU N:l
N:2
N:3
N:4
N:5
N:6
60pM t 50pH | 30pH OE
SPECTRflL M62.4
N:2
N:3
N:4
N:5
N:6
SPECTRflL M 187.3 Nsl
Ns2
N:3
N:4
Ns5
N:6
LINE : 1500 N
INDUCED POLARIZATION SURVEY
POLE-DIPOLE flRRRY
DEPTH'VolNT
N r i. 2. 3. 4. ...
"H" SPRCINO r 100.0 FEET
FREENEST RESOURCES
MCKENZIE ISLAND,GRID-2
RED LAKE AREADflTE i WINTER 1996 REF i 9602
SCALE = 1 : 2400JVX LTD-
13C|OH t IZqOH t liqOH , 90H 60pH , 50pH , 40pH | 30pM OE 20pE , 30pE
TflU TflUNil
N:2
N:3
N:4
N:5
N:6
.0 . 48.0.......O .0 .0 -O
N:2
N:3
N:4
N:5
N:6
eopn sopH , sopn aopn , zopu , lopn , OE t iopE , zopE , aopESPECTRflL M
Nil
N:2
N:3
Ni4
N;5
N:6
SPECTRflL M Nil
Nt2
N:3
Nt4
N:5
Ns6
o •st co
LINE : 1200 N
INDUCED POLARIZATION SURVEY
POLE-DIPOLE RRRRY
VDCPTN rOINT
N r 1. 2. 3. 4. ... •H' SPHCINO = 100.0 FEET
FREENEST RESOURCES
MCKENZIE ISLAND-GRID-2
RED LAKE AREADflTE : WINTER 1996 REF : 9602
SCALE = 1 : 2400JVX LTD-
ISqOH | 14(}OM , 13(]CIH , lOqOH | 90pM , BOpH M , 50pH , 40pH t 30pH , 20pN IQpH , OE , 20pE , 30pE , 40pE , SOpE
TflU TflUNil
N:2
Ni3
Nt4
N:5
N:6
.0 .1 .1 ..O.5 .-O . -O .1 .0 .0 ^ .0 .0 .0
.1 .1 .3 ;i.oo -O .3 .0 .0
.0 .5 .0 .1
.3 .1 .1 .3 .0 .1 .1 .3
.0 o -0\ 2rfl—~. 2..3 .1 .1 .5 .1 .3
A \ Vo i..5 -l .1 .5 .1 -3
15CJOH t 1 4CJON 12()OM , llt|OH 90pM t 80pH , 70pH 30pH OE 20pE | 30pE , 40pE BOpE
SPECTRRL M27.9.5
N:2
N:3
N:4
N:5
N:6
19^^X214.5
.7 189.3
SPECTRflL M N ' !
Ns3
N:4
NsS
N:6
Grid 2Plate 4a
LINE : 900 N
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRRY
ffl.
VDtfTH POINT
N : 1. 2. 3. 4. ..-
•fl" SPflCINO s 100.0 FEET
FREEWEST RESOURCES
MCKENZIE ISLflND. GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400JVX LTD-
RESISTIVITY
MX CHG.
Ni2
N:3
N)4
N:5
N:6
Nil
Ni2
Ni3
Ni4
Ni5
Ni6
l SOON | 14I|OH 120( OH , IICJOH | H)(|OH , 90pH , 80pH , 70J1H | 60pU | 50pH | 4DpH , 30pH , 20pN 20pE , 30pE t 40pE | SOpE , 60pE t 70pE
RESISTIVITY
9K
2K 10.6K
l-SJC 2.2K Nil
Ni2
N:3
Ni4
Ni5
N:6
X P-
TC.
40pE , SOpE , 60pE t 70pE
8.2
8.7 6.5
5 "23. (
24.3
22.2 24.3 24^;Q\. 9 ' 1 M .6N 8.0
22.2 22.1 24.3 ZsVjV 10.4 15.3
22.1 22.1 24.5 26^V\ 10.4
21.4 22.1 22.0 25.1 26.3
ft* C HG. Nil
Ni2
Nt3
Ni4
Ni5
Ni6
LINE : 600 N
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRHY
N z 1. 2. 3. 4. ... •fi- SPHCINB = 1 00.0 FEET
FREEWEST RESOURCES
MCKENZIE ISLflND, GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400JVX LTD-
RESISTIVITY
Ni2
N:3
N:4
'N i o
Nt6
MX CHO.Nil
Ni2
N:3
N:4
Ni5
Ni6
11 • SOPH . 4QOH , 300H , 20DH , 10PH OE , 10PEf—— -r 20DE . 300E , 400E . SOQE . 60PE 70PE . 80QE . 90pEi*) r-^ —— —— —— ——
41-0 44.0
81.0 85-0
46.0 57.0 77.0 130.0 3Q5
94.0 122.0 163.0 2\2.
131.0 141.0 160.0 2Q3-*fr"'228.0 2!9.\)"ft43.0 695
199.Q^-*tmr~l239.0 269.0^3J1Z*6 336^8-^441.0
283.0^3*15-4)—a*e^ 348.0 355.o f27lk.o \27___ Vc^
383.0 389.0 393.0^T3lTW) 330.0 328.0
RESISTIVITY 21.OK 1 5.2K 5.SK Nil
•6K 19.SK Ni2
- 1 O
T.c.pH | 60pt4 , SOpH , 40pH 20pJ t 30pE
18.9 23.3 38.1-6 1.6 1.1 .8 .7
1.8 1.7 1.4 1.2 1.0
-^2^0 1.9 1.5 l
2.7 2.6 2T2 —— ~2T
.6 31.0 36.5 37.9
Ni3
N:4
MsS
N:6
900E
MX CHG. 4.5 3.1 Nil
Ni2
Ni3
Ni4
NiS
N:6
LINE : 300 N
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRRY
DEPTH POINT
N - l. 2. 3. 4. ..."H" SPflCINO = 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND.GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE = l: 2400JVX LTD-
2.174^0
RESISTIVITY
IICJOH t IPqOH , 90pH | BOpN | 70pH | 60pH | SOpH , 40pH , 30pH | 20pH , IQpH , 0^ i l OpE , 20pE t 30pE 40pE , SOpE , 60pE , 70pE , 80pE t 90pE IQ^OE , HOPE | 1200E
MX CHO.
Nil 50-0 46.0 43.0 45.0 47.0 63-0 86.0__9
Ni2 96.0 97.0 95.0 92.0 88.0 113JJ—T4TTO 206,
N:3 165.0 152.0 160.0 164.0 147.0 171.0 204^
N:4
N:5
N:6 489."0\387.0
252 .
2K
RESISTIVIT N:l
N:2
N:3
N:4
N:5
Ni6
rr-1 IP- i
SOpE ( 60pE t 70pE , 800E | 90pE | 10QOE | 11QOE | 12QOE
3 8.5
70pH , 60pH | SOpH , 40pH
9. 1.3 1.4 1.4 1.4 1.5 1.7 1.8
1.9/ 2.4 2.8 /3.1 3.3 3.1 3.4
2.2 2.8 J. l 3-5 3.5 3.6 4/1
MX CHO. Nil
Ni2
Ni3
Ni4
NiS
Ni6Grid 2Plate 5
o 10 co
LINE : 1800 N
INDUCED POLRRIZRTION SURVEY
POLE-DIPOLE flRRRY
ffl.
N r 1. 2. 3. 4. ... "H" SPfltlNO : 100.0 FEET
FREENEST RESOURCESMCKENZIE ISLRND,GRID-2
RED LflKE flREflDRTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400JVX LTD-
60pH [ 500H , 40JH , 30pH , H , OE
RESISTIVITY
N:2
N:3
N:4
N:5
Ni6
RESISTIVITY . O 217.0 N:l
9.0
4K
7K
N:2
N:3
N:4
N:5
Nt6
ir-
MX CHG.
N:2
Ni3
N:4
Ni5
N:6
MX CHO- 13-4 Nil
17.8 N:2
-6.7
N:4
N:5
N:6
LINE : 1500 N
INDUCED POLRRIZRTION SURVEY
POLE-DIPOLE RRRRY
ffl.
DErTH*r01HT
N - 1 . 2. 3. 4. ... •fl" SPflCING = 100.0 FEET
FREENEST RESOURCESMCKENZIE ISLRND*GRID-2
RED LRKE RRERDflTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400JVX LTD-
80pH 60pH 40DH , 30J3H "H , OE 20pE
RESISTIVITY RESISTIVITY .4K 5.3K Nil
N:2
N:3
N:4
Ns5
N:6
90pH 70pH [ 60pN | SOpH , 40pH , 30pH , 20pH , IPpH , OE | IPpE , 20pE , 30pE
MX CHO.1.6
Nt2
N:3
N:4
N)5
N:6 7.4
MX CHO- 5^7 9.3 Nsl
Ci .6 Ni2
Nt3
N:4
N:5
N:62.1,7 420
LINE : 1200 N
INDUCED POLRRIZRTION SURVEY
POLE-DIPOLE RRRflY
OEPTH'VfllMT
N r 1. 2. 3. 4. ... "H' SPnCING = 1 00.0 FEET
FREENEST RESOURCESMCKENZIE ISLRND, GRID-2
RED LRKE RRERDRTE : WINTER 1996 REF : 9602
SCRLE ^ 1: 2400JVX LTD.
i t --'?
n , 80pN , 70pH
RESISTIVITY
40pH , 30pH , 20pH , IPpH , OE | IQpE , 20pE { 30pE , 40pE , 50pE , 60pE
^r3 RESISTIVITY
MX CHO.
NM
N:2
N:3
N:4
N:5
N:6
N:2
N:3
N:4
N:5
N:6
12()OH , llt|OH , IQtjOH , 90pH , BOpH , 70pM , 60pH | 50pt4 , 40pH , 30pH 20gH^, IQpH |, _ OE ^g^,. 20Rf , 3^PE - 4 0P E j 50P E . 60P E""
2-1 1-1 1-4MX
14.1
N:2
N:3
N:4
N:5
N:6
oCO CO
Grid 2Plate 4
LINE : 2400 N
INDUCED POLflRIZRTION SURVEY
POLE-DIPOLE HRRflY
Z?]
N z 1. 2. 3. 4. ... •H" SPRCING r 100.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND.GRID-2
RED LflKE flREflOflTE : WINTER 1996 REF : 9602
SCflLE r 1: 2400JVX LTD-
TflU
N:2
N:3
N:4
N:5
N:6
SPECTRPL M
N:2
N:3
N:4
N:5
N:6
•O
50.8
44
90pH i 80pH 40pH 30pH Of
.0 .0 .0 .Q .Q .Q .Q
-o . o .o .o .o .o .o_____ -o .o .o .o .o .o .o
•O .0 .0 .0 .0 .0 .0 .0 .0
•O -O .0 .0 .0 .0 .0 .0
• O .0 .0 .0 .0 .Q .Q
TflU • O N:l
N:2
N:3
N:4
N:5
N:6
H . 40pH 20H
.0 17.5 ,-Q - Ql ' u vJI^ r u • 0\^ . 0____.0.
•Ol V .0 -O/ .0 .0 .0
.0 .0 .0 .0 .0
.0 -O .0 .0 .0
.0 .0 .0 .0
' 0 ' 0 294
.0
SPECTRflL M • O N:l
N:2
N:3
N:4
N:5
N:6
LINE : 2100 N
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRflY
a.V
DEPTH POINT
N :: 1. 2. 3. 4. ...
•H" SPflCING = 1 00.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND. GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE :: 1: 2400JVX LTD.
TflU
N:2
N:3
N:4
N:5
N:6
SPECTRflL M
N:2
N:3
N:4
N:5
N:6
80pH 40H Of
TflU• O .0 .0 .0 .0 .0 Nsl
.0 o . 0 .0 .0 .3 Ns2
.0 .0 .0 .1 1.0 .0
.0 .0* n .0 .3 .1
•O -0\ .0 .1 .3 .0 \ . 0 \ .0 ".Q .5 Ns3
•O V -O .1 .1 .0 /O .Q\ .0 1.0 N:4
.0 .0 .0 ^/Q .0 \ . 0 N:5
.0 1.0 .0 .0 .0 .Q .Q N:6
Of
35.7
3TN9N 1.0 .Q .0 .o .0
SPECTRHL M
Ns2
N:3
N:4
Ns5
N:6
LINE : 2400 N
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE flRRflY
a.OEPTI/POINT
N r 1. 2. 3. 4.. .̂ —. •H" SPflCING r 100.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND.GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE = 1: 2400
JVX LTD-
RESISTIVITY
MX CHO.
N:2
N:3
N:4
N:5
N:6
N:2
N:3
N:4
N:5
N:6
1Q[|OU | 90pH | 80pH | 700U | 60pH | 500H | 400H | 30DH | 20pH Of
""^ RESISTIVITY *0 V U46.0, 62-0 79.0 156.0 192.0 198.0 119.0 112.0^ 60-0 59.0 Nsl
^0X^85^0^/108-0 136-0 134.0 19^0—207rfl—22-4-^
f*~~9*^0 126.0 172-P 29L-fl-"j4TTtr-~3J2.0
591.D l 923^HSS3H-X 119TO—*112-0 165-0/247.0 4*B~.Q 465.0
653\
624ttN
70.0 149.0 22.0 350 O
19^.0 30/4.0 /444.0
N:2
N:3
N:4
N:5
N:6
anomaly
-.6 ..O .1 .3 .3 .5
.8 \2 --9 ' .5
2.8
9^3.
MX CHG. Nsl
N:2
N:3
N:4
N:5
Ns6
LINE : 2100 N
INDUCED POLflRIZflTION SURVEY
POLE-DIPOLE RRRRY
,
DEPTH*POINT
N r 1. 2. 3. 4, .-.
"R" SPRCING = 100.0 FEET
FREEWEST RESOURCESMCKENZIE ISLflND.GRID-2
RED LflKE flREflDflTE : WINTER 1996 REF : 9602
SCflLE - 1 : 2400
JVX LTD-
RESISTIVITY
N:2
N:3
Ns4
N:5
N:6
N:l
N:2
N:3
N:4
Ns5
Ns6
ilQOH . IPqOH . 90PH 80pH . 70pH . SOPH . 50QH 40pU . 30QH . 20PH . IQPH OET——' i ' F ' r—'- -J—'- -J-.-'—— l—.'--r————*#r±) r ^ f Mf,j rRESISTIVITY^ - m
JQfl.zrTlT.Q
W/i^i.o
Ns3
N:4
Ns5
N:6
TP- fligOM , lOqOU , 90pH , 80pM | 70pH . 60pH i 50pU | 40pH | 30pU , 20pM , lOpH , OE
"n:'r"~~ " "-' MX CHG.2.3 . 3.4 3,3 2.1 Nsl
Grid 2Plate 3
oCO
o oCD
O O
O O (M
O O O
O O 00
OoCO
o o
o oCNI
UJZ
co(Xen
oo(M
o o
UJ
a oCO
o oGO
UJ
o o o
UJ
o o(M
a a
UJ
o oCO
2400 2400 N
1500 N
1200 N 1200 N
900 N
600 S
900 S
300 N
O
300 S
600 S
900 S
420
52NO4SW0144 2.17420 DOME 380
1800 S 1800 S
o oCO
o o
o oCM
Oo o
o aCD
ooCO
o a
ooCM
UJ
UJ COcr ea
UJ
o oCM
o o
UJ
o oCO
a aCO
UJ
o o o
UJ
o oCM
FREEWEST RESOURCES CANADA INC.MCKENZIE ISLAND PROPERTY - GRID 2
RED LAKE MINES and MINERALS DIVISION______________N.T.S. 52 N/4 ————.^——
RESISTIVITY CONTOURS (11=2)RESISTIVITY CONTOURS : 500 fc 2500 ohm m
SURVEYED BY JVX LTD. USINGSCINTREX IPR-12 Rx ; IPC-7/2.5 kW Tx
WINTER 1996200 400 600
FEETPLOTTED BY
A.S. FEB. 1996
SCALE 1:2400 PLATE 2
JVX ret. no. 9602