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Quantec Geoscience Inc. P.O. Box 580, 101 King Street Porcupine, ON PON 1CO Phone (705) 235-2166 Fax (705) 235-2255 Quantec Geoscience Inc. Geophysical Survey Assessment Report 0 o i , / C 6 l RECEIVED SEP 19,;,,; GEOSCIENCE ASSESSMENT OFFICE Regarding the DIPOLE-DIPOLE TDIP SURVEY at the RIVER VALLEY PROJECT on behalf of MUSTANG MINERALS CORPORATION Toronto, QGI-QGI-QGI-QGI D Dawson K Blackshaw D Eastcott July, 2001 Project QG-167 41I09NE2015 2.22108 MCWILLIAMS 010
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Page 1: Quantec Geoscience Inc. - Ontario · 2017-01-17 · * Report Type: Summary interpretation, suitable for OMNDM assessment filing The results from the service provided by Quantec Consulting

Quantec Geoscience Inc. P.O. Box 580, 101 King Street Porcupine, ON PON 1CO Phone (705) 235-2166 Fax (705) 235-2255

Quantec Geoscience Inc.

Geophysical Survey Assessment Report

0 o i, /C 6 l

RECEIVEDSEP 19,;,,;

GEOSCIENCE ASSESSMENT OFFICE

Regarding theDIPOLE-DIPOLE TDIP SURVEYat the RIVER VALLEY PROJECTon behalf ofMUSTANG MINERALS CORPORATIONToronto,

QGI-QGI-QGI-QGI D Dawson K Blackshaw D Eastcott July, 2001 Project QG-167

41I09NE2015 2.22108 MCWILLIAMS 010

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Quantec Geoscience Inc. TDIP Dipole-Dipole Survey

MUSTANG MINERALS CORP. River Valley PGM Project

1. INTRODUCTION..........................................................................................................................................^

2. GENERAL SURVEY DETAILS .....................................................................................................................4

2.1 LOCATION...............................................................................................................................^2.2 ACCESS..................................................................................................................................^2.3 SURVEY GRID ...........,......................................... ....................................................................5

3. SURVEY WORK............................................................................................................................................6

3.1 GENERALITIES................................. ..... ..................................................................................63.2 PERSONNEL..................................................................................................................... .......63.3 SURVEY SPECIFICATIONS .................................................................,........... .............. ....... ....63.4 SURVEY COVERAGE....................................................................... ..........................................73.5 INSTRUMENTATION............................................................ .......................................................83.6 PARAMETERS......................... ................................................................................................83.7 MEASUREMENT ACCURACY AND REPEATABILITY........................................................................... 83.8 DATA PRESENTATION.............. ..........................................,....................................................8

4. RESULTS AND INTERPRETATION.........................................................................................................10

4.1 GEOPHYSICAL RESULTS AND INTERPRETATION ..........................................................................105. CONCLUSION AND RECOMMENDATIONS........................................................................................,....11

APPENDIX A: STATEMENT OF QUALIFICATIONSAPPENDIX B: THEORETICAL BASIS AND SURVEY PROCEDURESAPPENDIX C: INSTRUMENT SPECIFICATIONSAPPENDIX D: PRODUCTION SUMMARYAPPENDIX E: EXPOLRATION TARGETSAPPENDIX F: LIST OF MAPSAPPENDIX G: MAPS AND SECTIONS

Figure 1: River Valley Project General Location Map............................................................. ................4Figure 2: River Valley Project Detailed Location Map .............. .......... ......... ............. .......... .................5Figure 3: Dipole-Dipole Array Layout.............................................................................. ........................7

Table l: Dipole-Dipole TDIP Survey Coverage.................................................................................. . .....lTable II: Decay Curve Sampling................ .................................................................... ........................8Table III: Highlighted IP/Resistivity areas............................................................................................... 10

QGI-167-July, 2001

41I09NE2015 2.22108

ii

MCWILLIAMS 010C

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Quantec Geoscience Inc. TDIP Dipote-Dipole Survey

MUSTANG MINERALS CORP. River Valley PGM Project

QGI Project No:

Project Name:

Survey Period:

Survey Type:

Client:

Client Address

Representatives:

QG-167

River Valley PGM Property - North Extension

April 16 to, April 28 2001

Dipole-Dipole Time Domain Induced Polarization

Mustang Minerals Corporation

120 Adelaide Street West. Suite 514 Toronto, Ontario M5H 1T1

Mr. Ken Lapierre Mr. Peter Wood

Objectives:

This report will detail and describe follow-up geophysical work required by Mustang Min erals Corporation on the North Grid Extension of the River Valley PGM Property.

1. To define and delineate, using TDIP\Resistivity, favourable signatures associated with contact-type and Sudbury-type magmatic PGM-bearing sulphide mineralization. This survey primarily targets the margins and floor of the River Valley intrusion that occurs on the property The Dipole-Dipole array was chosen based on its high reso lution and shallow mapping capability, due to the thin overburden cover and shallow nature of the drill targets sought after.

2. To specifically outline TDIP DPDP anomalies having higher apparent resistivities.

* Report Type: Summary interpretation, suitable for OMNDM assessment filing

The results from the service provided by Quantec Consulting Inc., April 23, 2000 through May 7, 2000, (Quantec Consulting Inc. job number QG-112) have been utilized in the evaluation of this follow-up data set to maintain some consistency in the anomaly evaluation.

QGI-167-July, 2001

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Quantec Geoscience Inc. TDIP Dipote-Dipole Survey

MUSTANG MINERALS CORP. River Valley PGM Project

2. GENERAL SURVEY DETAILS

2.1 LOCATION

* General Location:

* Country:

* Township:

* Province:

* Nearest Major Settlement:

* NTS Map Reference:

River Valley, NW of Sturgeon Falls ON (see Fig. 1)

Canada

Dana and Mcwilliams Townships

Ontario

River Valley, ON

41-1/09

Figure 1: River Valley Project General Location Mao

QGI-167-July, 2001

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Quantec Geoscience Inc. TDIP Dipote-Dipote Survey

MUSTANG MINERALS CORP. River Valley PGM Project

River Valley PGM Property Location

___ UustnmHmpdu Jv DMCOUL (M l ~26km Propwty Boun

Crerar

Figure 2: River Valley Project Detailed Location Map

2.2 ACCESS

* Base of Operations:

* Mode of Access to Grid:

* Mode of Access to Lines:

2.3 SURVEY GRID

* Established by:

* Coordinate Reference System:

* Line Direction:

* Line Separation:

* Station Interval:

* Method of Chaining:

* Claims No. Surveyed 1 :

Camp Horizon, ON

4x4 truck

4x4Truck and 4x4 quad

Previously established by Mustang Minerals Corp.

Local exploration grid (not UTM referenced)

Baseline Azimuth l100(Grid N-S)

200 -100 metres

25 metres

Metric, slope distance

1231265,1229153,1229152,1214638

1 Note: Claim numbers from River Valley Project CAD basemap (ref. River Valley Top&Claims.DWG, Mustang Min erals Corp., 05/2001).

QGI-167- July, 2001 5

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Quantec Geoscience Inc. TDIP Dipole-Dipote Survey

MUSTANG MINERALS CORP. River Valley PGM Project

3. SURVEYWORK

3.1 GENERALITIES

* Survey Dates:

* Survey Period:

* Survey Days (read time):

* Weather/Down Days:

* Survey Coverage:

* Number of Lines Surveyed:

* Approximate Area Surveyed:

3.2 PERSONNEL

* Project Manager:

* Geophysical Technician:

* Field Technicians:

3.3 SURVEY SPECIFICATIONS

* Array:

* Dipole spacing:

* Rx-Tx Separation:

* Line Interval:

* Sampling Interval:

April 16 to April 28 , 2001

13 days

9 days

3 days

16.85 km

9

3.5km2 (~3.5kmx1km)

Richard Chasse, Kirkland Lake, ON

Eric Dufour, Val-D'or, QC

Carman Vucko, Kirkland Lake.ON Eric Hotvedth, Ramore, ON Bobby Gerrie, Timmins, ON

Dipole Dipole (see Fig. 3)

50 metres (C, - C2 or PT - P2)

N ^ 1 to 6

100 - 200 metres

50 metres

QGl-167-July, 2001

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Quantec Geoscience Inc. TDIP Dipole-Dipole Survey

MUSTANG MINERALS CORP. River Valley PGM Project

DIPOLE-DIPOLE ARRAY

P2 P, C, C2-*-| a j-* Na *| a

N=3 N=4

N=5 N=6

PLOT-POINT(At Mid-Point 8.

Depth = a(N+1X2)

Figure 3: Dipole - Dipole Array Layout

3.4 SURVEY COVERAGE

* Total Line Coverage: 15.90 km (see Table l)

GRID

North Ext.North Ext.North Ext.North Ext.North Ext.North Ext.North Ext.North Ext.North Ext.North Ext.North Ext.North Ext.North Ext.

LINE28+OOE27+OOE25+OOE24+OOE24+OOE22+OOE22+OOE20+OOE20+OOE18+OOE18+OOE17+OOE16+OOE

START5+50N5+50S0+00

1+50S9+OON5+OON11+50N4+50S11+50N1+OOS

11+50N5+OOS1+50S

END

16+50N22+50N22+50N8+OON

20+50N8+50N

20+OON10+OON1 8+OON9+50N16+50N2+50N9+OON

Total Coverage

TOTAL (m)11002800225095011501350850145065010505007501050

15900

Table l: Dipole-Dipole TDIP Survey Coverage

Total Overlap Coverage:

Total Survey Coverage:

950 m

16.85 km

QGI-167-July, 2001

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Quantec Geoscience Inc. TDIP Dipote-Dipote Survey

MUSTANG MINERALS CORP. River Valley PGM Project

3.5 INSTRUMENTATION

* Receiver:

* Transmitter:

* Power Supply:

* Ground Contact:

IRIS IP-10 (10 channel /Time Domain)

Phoenix IPT-1 (3 kW l 75 - 1 200V output)

MG-2 (400 Hz 1110V l 3 phase) * Honda Gx-60 (5.5hp)

Stainless Steel

3.6 PARAMETERS

* Input Waveform: 0.125 Hz square wave at 5007o duty cycle (2 seconds On/Off)

* Receiver Sampling Parameters: Q IP custom windows (see Table II)

* Measured Parameters:

1. Chargeability in mV/V across max. 10 time-gates, plus area under decay curve.

2. Primary Voltage in millivolts and Input Current in milli-amperes for Resistivity in Q-m calculated according to dipole-dipole geometry factor (Appendix B).

SliceTdT,

T2T3

T4T5

T6T7T8

T9

Tio

Total Tp

Duration (msec)4020

3030

30180180

180

360360

360

1760

Start (msec)0

60120180240300660

1020138021002820

End (msec)40

120180240300660

10201380210028203540

Mid-Point (msec)

80150210270450840

1200174024603180

Table H: Decay Curve Sampling.

3.7 MEASUREMENT ACCURACY AND REPEATABILITY

* Chargeability:

* Resistivity:

3.8 DATA PRESENTATION

* Maps:

Pseudosections maps:

general^ 0.5 mv/V but acceptable to 1.0 mV/V.

less than 5 07o cumulative error from Primary voltage and Input current measurements.

Stacked posted contoured dipole-dipole sections and profiles (3=50 1 n^-6) of the apparent resistivity, total chargeability and metal factor, with Interpretation over lay, at 1:5000 scale (9 maps).

QGI-167-July, 2001

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Quantec Geoscience Inc. MUSTANG MINERALS CORP. TDIP Dipote-Dipote Survey River Valley PGM Project

Plans Maps: -Compiled posted contoured plans of Filtered TotalChargeability, Apparent Resistivity (using triangular (flt4leg.flt deconvolution filter) and Geophysical Inter pretation, with CAD basemap (UTM translated), plotted at 1:10000 scale (2 maps).

-Compiled Stacked Sections of Filtered Total Charge ability, Apparent Resistivity (using triangular (flt4leg.flt) plotted at 1:5000 scale (9 maps).

* Digital:

Raw data: IP-10 digital dump file (See Appendix C)

Processed data:

a) ASCII GEOSOFT .DAT file format with file-name relating to profile, for example:

7500e.DAT = L ine 75+OOE using the following format:

Linel: TitleLine 2: Header information, including Line, Array, Dipole, UnitsLine 3: Column headingsColumns 1-4: Electrode station positions (metres)Column 5: Primary Voltage (millivolts)Column 6: Transmitted Current (amperes)Column 7 Spontaneous PotentialColumn 8: Chargeability Windows (msec)

b) ASCII GEOSOFT IPPLOT file format with file-name relating to profile, and file-spec re lating to data type (RES = app. resistivity, IP = total charg., MF = metal factor), for ex ample:

7500e.RES = L ine 75+OOE Apparent Resistivity, using the following format:

Linel: TitleLine 2: Header information, including Line, Array, Dipole, UnitsLine 3: Column headingsColumn 1: Station/Plot Point (metres)Column 2: Filter Data Value (using Geosoft Flt4leg.flt)Column 3: 1^=1 Data Value (Res = ohm-metres, IP = mV/V, MF ^ unitless)Column 4: N^2 Data ValueColumn 5: ^3 Data ValueColumn 6: lv^4 Data ValueColumn 7: ^5 Data ValueColumn 8: N^6 Data Value

c) ASCII GEOSOFT .XYZ format, for Plan Map data (ex. Mmsr.XYZ), using the following format:

Header Lines: Identified by 7" in 1 st column, containing Header information, including Line, Array, Dipole, Units, etc.

Column 1: Plot-point Station Easting (metres) Column 2: Plot-point Station Northing (metres) Column 3: Station Number (optional) Column 4: Filtered Total Chargeability (millivolts per volt) Column 5: Filtered Apparent Resistivity (ohm-metres)

QGI-167- July, 2001

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Quantec Geoscience Inc. TDIP Dipole-Dipole Survey

MUSTANG MINERALS CORP. River Valley PGM Project

4. IRESULTS AND INTERPRETATION

This report will detail and describe follow-up geophysical work required by Mustang Minerals Corpo ration on the North Grid of the River Valley PGM Property. The results from the service provided by Quantec Consulting Inc., April 23, 2000 through May 7, 2000, (Quantec Consulting Inc. job number QG-112) have been utilized in the evaluation of this follow-up data set to maintain consistency in the anomaly evaluation.

The objectives of these surveys:

1. To define and delineate, using TDIP\Resistivity, favourable signatures associated with contact- type and Sudbury-type magmatic PGM-bearing sulphide mineralization. This survey primarily targets the margins and floor of the River Valley intrusion that occurs on the property. The Di pole-Dipole array was chosen based on its high resolution and shallow mapping capability, due to the thin overburden cover and shallow nature of the drill targets sought after.

2. This assessment report specifically outlines TDIP DPDP anomalies having higher apparent re sistivities.

4.1 GEOPHYSICAL RESULTS AND INTERPRETATION

A total of 33 geophysical features have been identified by the Northern Extension surveys. These features are listed in Appendix E. The following table separates the identified features that, from a geophysical perspective, may warrant further investigation.

#

11

12

18

23

24

30

LINE

18+OOE

20+OOE

24+OOE

25+OOE

25+OOE

27+OOE

STN MIN1050

1500

1300

1500

1800

1700

STN MAX1150

1600

1450

1550

1900

1750

CHARACTER

Moderate chargeabilityModerate chargeabilityModerate chargeabilityModerate chargeabilityModerate chargeabilityModerate chargeability

RESISITIVITY

Moderately high resistivityHighly resistive

Moderate resistivity

Highly resistive

Highly resistive

High resistivity

PRIORITY

1

2

2

2

2

2

COMMENTS

Underlying surface conductivityUnderlying surface conductivityUnderlying surface conductivity

Table III: Highlighted IP/Resistivity areas

QGI-167 -July, 2001 10

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CJuantec Geoscience Inc. TDIP Dipole-Dipote Survey

MUSTANG MINERALS CORP. River Valley PGM Project

The IP/Resistivity results at the River Valley Property Northern Extension have identified zones of weak to strong chargeability, which frequently correspond with zones of moderate to high apparent resistivity.

It is recommended:

1. Line 18+OOE is modeled to best define the geometric nature of the identified targets, with specific attention being paid to the zone near (L18+OOE) 11+OON.

2. Line 25+OOE is modeled to best investigate actual penetration effectiveness in the area of the apparent resistivity contact (L25+OOE near 11+50N) and also to further investi gate the nature of the identified features located near 15+25N and 18+50N.

Respectfully Submitted QUANTEC GEOSCIENCE INC.

J ' - .S• i ,' '

y ~. ' 'Kevin BlackshawGeneral Manager- Timmins

G. R. JeffWarne Senior Geophysicist

David EastcottTechnical Services - Timmins

Porcupine, ON

- David J.W. Dawson Senior Geophysicist

QGI-167-July, 2001 11

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Quantec Geoscience Inc. TDIP Dipole-Dipole Survey

MUSTANG MINERALS CORP. River Valley PGM Project

STATEMENT OF QUALIFICATIONS

l, David J W. Dawson hereby declare that:

1. l am a geophysicist with residence in Canada and am presently employed in this capacity with Quantec Geoscience Ltd.

2. l received a B Se (Geology) from Lakehead University (1985) in Thunder Bay, Ontario and have completed the required courses for any equivalent B.Se. (Geophysics) from the University of Western Ontario, (1987), London Ontario.

3 l have practiced my profession continuously since 1987 in Canada, South and Central America, and Europe

4. l have no interest, nor do l expect to receive any interest, in the properties and securities of M ustang Minerals Corp.

5. l reviewed and interpreted the data, prepared the interpreted sections and the text of Section 4 of the report. The statements in this report represent my professional opinion based on my consideration of the information available to me at the time of writing the report.

Timmins, Ont, Canada July, 2001

'~ David J.W. Dawson l) Senior Geophysicist, QGL

3G-167 - July. 2001

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Quantec Geoscience Inc. MUSTANG MINERALS CORP. "DIP Dipole-Dipole Survey River Valley PGM Project

STATEMENT OF QUALIFICATIONS

l, David Eastcott, hereby declare that:

1 l am a staff geophysical operator with residence in Porcupine, Ontario and am presently employed in this capacity with Quantec Geoscience Ltd of Porcupine, Ontario.

2. l have practiced my profession continuously since January of 1996.

3 l have no interest nor do l expect to receive any interest, direct or indirect, in the properties or securities of Mustang Minerals Corp.

4 l am the editor of the report and am responsible for the compilation and final map creation. The state ments made in this report represent my professional opinion based on my consideration of the information available to me at the time of writing this report.

Porcupine, Ontario July, 2001

David Eastcott.Technical Services

Quantec Geoscience Inc.

3G-167 -July. 2001

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Quantec Geoscience Inc. MUSTANG MINERALS CORP. "i DIP Dipole-Dipde Survey River Valley PGM Project

STATEMENT OF QUALIFICATIONS

l Kevin Blackshaw, declare that:

l am a technologist, with residence in Timmins, Ontario, and am currently employed by Quantec Geoscience Inc. of Waterdown, Ontario, as General Manager of the Canadian operational office, in Porcupine, ON.

1 l graduated from Cambrian College in Sudbury, Ontario with a Geological Engineering Technology diploma in 1983

o l have continuously been employed in this field since graduation,

^ l have no interest nor do l expect to receive any interest in the properties or securities of M ustang Minerals Corp.

l \ was the project manager and was responsible for the data acquisition, validation and plotting in the field. The statements made in this report represent my professional opinion based on my consideration of the information available to me at the time of writing this report.

Porcupine, Ontario July, 2001

Kevin Blackshaw General Manager, Timmins

OG-167-July, 2001

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Quantec Geoscience Inc. TDIP Dipde-Dipole Survey

MUSTANG MINERALS CORP. River Valley PGM Project

THEORETICAL BASIS AND SURVEY PROCEDURES

DIPOLE-DIPOLE TDIP

The collected data sets are reduced, using the Geosoft program I PRED™ to apparent resistivity, total chargeability and metal factor as explained in the following figures and equations: Using the following diagram (Fig. C1) for the electrode configuration and nomenclature:

DIPOLE-DIPOLE ARRAY

P2 P, C, C2- --*-i a j-*- na—i*-j a j-*——

II

Figure E1: Dipole-Dipole Electrode Array

*he apparent resistivity is given by:

pa = (n + 2)aVP

ohm - metres

where: "a" is the MN dipole spacing (metres)"n" is the separation parameter between CiC2 and PtP2 "Vp" is the primary voltage measured between P-|P2 (volts) "l" is the output current between CiC2 (amperes)

From Telford, et al., Applied Geophysics, Cambridge U Press, New York, 1983..

QG-167-July, 2001

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Quantec Geoscience Inc. TDIP Dipote-Dipcte Survey

MUSTANG MINERALS CORP. River Valley PGM Project

Using the following diagram (Figure C2) for the Total Chargeability:

Measured Voltage Line

negative

One half of Transmit Cycle

"Off Time"

1 tt"On Time" t(0) t,,

Figure E2: Measurement of the IP Effect in the Time-Domain

4 .The total chargeability: is given by:

lMTotal

1=11010L Vs (t) dt millivolt - seconds per volt

where f/, f^ are the beginning and ending times for each of the chargeability slices.

The sets are then ready for plotting, profiling using the Geosoft Sushi™ program. The Apparent Resis tivity, total Chargeability and Metal Factor results of the dipole-dipole surveys are presented in pseudo section format (see Fig. 2). All resistivities are in Q-metres and the chargeabilities in mVW.

3 From Terraplus\BRGM, IP-6 Operating Manual. Toronto, 19874 From Telford, et al., Applied Geophysics. Cambridge U Press, New York, 1983..

QG-167-July, 2001

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Quantec Geoscience Inc TDIP Dipde-Dipole Survey

MUSTANG MINERALS CORP. River Valley PGM Project

INSTRUMENT SPECIFICATIONS

PHOENIX IP TRANSMITTER MODEL IPT-1

Power Sources

Output Voltage:

Output Power:

Maximum Current:

Ammeter Ranges:

Meter Display:

Current regulation:

Output waveform:

Operating Temperature:

Frequency Stability:for

Transient Protection:

Dimensions:

Weight:

Phoenix MG-3 (2.5KVA, 60V, 3 phase, 400 Hz) motor generator

75 to 1200V in 5 steps.75 -150 -300 -600 -1200VVoltage is continuously variable 200Xo from each nominal step value.

Maximum continuous output power is 2.5KW.

10 Amps

50m A, 100m A, 500mA, 1A, 3A, and lOAfull scale.

A meter function switch selects the display of current level, regulation status, input frequency, output voltage, line voltage

The change in output current is less than Q.2% for a 100Xo change in input voltage or electrode impedance. Regulation is achieved by feedback to the alternator of the motor generator unit.

Either DC, single frequency, two frequencies simultaneously, or time domain duty cycle). Frequencies of 0.078, 0.156, 0.313, 1.25, 2.5 and 5.0 Hz are standard, whereas 0.062, 0.125, 0.25, 1.0, 2.0 and 4.0 Hz are optionally available. The simulta neous transmission mode has 0.313 and 5.0 Hz as standard, whereas 0.156 and 2.5 Hz are optional

-400C to -t-600C

1 0Xo from -400C to -n600C is standard. A precision time base is optionally available

coherent detection and phase IP measurements.

Current is turned off automatically if it exceeds 150^0 full scale or is less than 50Xo full scale.

1 8cm x 40cm x 53cm

4kg

3G-167-July, 2001

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Quantec Geoscience Inc. TDIP Dipole-Dipote Survey

MUSTANG MINERALS CORP. River Valley PGM Project

INSTRUMENT SPECIFICATIONS:

Iris ELREC 10 Receiver(From Iris ELREC 10 Operating Manual)

Weather proof case

Dimensions:Weight:Operating temperature:Storage:Power supply:

Input channels:Input impedance:Input over voltage protection:Input voltage range:

SP compensation: Noise rejection:

Primary voltage resolution: accuracy:

Secondary voltage windows:

Sampling rate: Synchronization accuracy: Chargeability resolution:

accuracy:

Battery test: Grounding resistance: Memory capacity: Data transfer:

31.0 cm x 21.0 cm x 25.0 cm 9.0 kg (with internal battery) -30"C to 700C (-30"C to 500 C)1 x 12.0 V external battery (30 hr. @ 20 0 C) or2 x 6.0 V NiCad rechargeable (20 hr. @ 250C) or 1010 Mohm up to 1000 volts 10V maximum on each dipole 15 V maximum sum over eh. 1 to 10 Automatic 15 V with linear drift correction 100 dB common mode rejection (for Rs^ 0) automatic stacking 1 u.V after stackingD.3% typically; maximum 1 over whole temperature rangeup to 20 windows; preset window specs for Cole- Cole parameter analysis. 10 ms10 ms, minimum 40 nV 0.1 mV/Vtypically Q.6%. maximum 20Xo of reading 1 mV/VforVp> 10 mVmanual and automatic before each measurement 0.1 to 100 kohm 3200 records, 1 dipole/record serial link @ 300 to 19200 baud

3G-167-July, 2001

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Quantec Geoscience Inc. TDIP Dipote-Dipote Survey

MUSTANG MINERALS CORP. River Valley PGM Project

Iris EIrec 10 Dump File Format:

Channel:! 0316:12/15/199808:59:25 Spacing (foot): XP : 13500 li.P: 20400 Rs: 1.61 kohm

D : 50 XA : 12900 XB : 16400 I.AB: 20400

M1/5 M6/10 M11/15 M16/20

70.93 :50.69 :43.96 :38.95 :3493 :

31.57 :28.69 :26.19 :24.00 :2199 :

20.10 :18.34 :16.71 :15.25 :1389 :

12.6311.4410.329.238.21

Sp: -2.05 mV In: 1400.00 mA Vp: 652.204 mV Tau: 4 560 s

Rho: 6645.39 ohm.mMg: 16.81 mV/V

Mcc: 199.87 mV/V

#: 20Q: 0.04 mV/V

rms: 0.25 "h

Channel. 2 Date: 12/15/199808:59:25Spacing (foot): XP : 13550 li.P: 20400 D : 50 XA : 12900 XB : 16400 I.AB: 20400Rs: 2.54 kohm

M1/5

69.9850.3643.7538.823486

M6/10

31.5328.6826.2024.0322.03

Sp: -67.15 mV In: 1400.00mA Vp: 552.303 mV Tau: 5.378 s

M11/15

20.1518.3916.7815.3213.96

M16/20

12.70 :11.52 :10.39 :9.31 :828 :

Rho: 6504.35 ohm.m #: 20Mg: 16.85 mV/V Q: 0.05 mV/V

Mcc: 199.85 mV/V rms: 0.28 *

QG-167-July, 2001

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Quantec Geoscience Inc. TDIP Dipole-Dipole Survey

MUSTANG MINERALS CORP. River Valley PGM Project

PRODUCTION SUMMARY

PropertySurveyDATE16-Apr17-Apr

18-Apr

19-Apr

20-Apr

21 -Apr

22-Apr24-Apr

25-Apr26-Apr

27-Apr

28-Apr

29-Apr

Mustang Minerals Corp./River ValleyDipole-Dipole l. P.DESCRIPTIONMobilizationIP. survey (1/2 day)Transmitter problems 4066 chip was blown, 1/2 day down.l. P. survey (1 day)

l. P. survey (1 day)

l. P. survey (1 day)Change A set up on L^OE/long cross over had to go around lake point.I.P.survey (1 day)Line extension not cut. Bush crashed along westside.I.P.survey (1/4 day)I.P.survey (1 day)Line extension not cut/bush crashed 1 50m southI.P.survey (1/4 day)I.P.survey (1 day)Line 28E stopped at bottom of cliff at 1650N800m dead walk to 2050N on 2400E.I.P.survey (1day)

I.P.survey (1day)Used boat.

Other grid area on siteTotal Coverage

GRID

North Ext.

North Ext.North Ext.North Ext.

North Ext.North Ext.

North Ext.North Ext.

North Ext.North Ext.North Ext.

North Ext.North Ext.North Ext.

North Ext.North Ext.North Ext.North Ext.North Ext.North Ext.North Ext.

LINE

27+OOE

27+OOE25+OOE25+OOE

24+OOE22+OOE

20+OOE18+OOE

17+OOE17+OOE16+OOE

27+OOE27+OOE28+OOE

24+OOE24+OOE22+OOE20+OOE18+OOE24+OOE22+OOE

START

3+OON

8+OON22+50N15+50N

1+50S5+OON

4+50S9+50N

2+50N0+001+50S

5+50S1+OOS5+50N

20+50N14+50N11+50N1 8+OON11+50N1+50N8+50N

END

8+OON

22+50N15+50N

0+00

5+OON5+OOS

10+OON1+OOS

1+OOS5+OOS9+OON

1+OOS4+OON16+50N

14+50N9+OON

20+OON11+50N16+50N8+OON1+OON

TOTAL (m)

500

14507001550

6501000

14501050

3505001050

4505001100

600550850650500650750

16850

QG-167 -July, 2001

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Quantec Geoscience Inc. TDIP Dipole-Dipole Survey

MUSTANG MINERALS CORP. River Valley PGM Project

NORTHERN EXTENSION GRID PRIORITY EXPLORATION TARGETS

#

1

23

4

5

67

8

9

10

11

12

13

14

15

16

17

18

19

2021

22

23

LINE

16+OOE

16+OOE16+OOE

17+OOE

17+OOE

17+OOE18+OOE

18+OOE

18+OOE

18+OOE

18+OOE

20+OOE

22+OOE

22+OOE

22+OOE

22+OOE

22+OOE

24+OOE

24+OOE

24+OOE24+OOE

25+OOE

25+OOE

STN MIN-50

300900

-350

-150

50350

525

650

850

1050

1500

?

-250

-100

1150

1450

1300

1500

17001850

1100

1500

STN MAX50

4001000

-300

-50?

100450

625

750

950

1150

1600

-350

-150

0

1250

1650

1450

1600

18001950

1200

1550

CHARACTER

Weak chargeability

Weak chargeabilityHigh chargeability

Weak chargeability

Very weak chargeability

Weak chargeabilityWeak chargeability

Moderate chargeability

Weak chargeability

Strong chargeability

Moderate chargeability

Moderate chargeability

Weak chargeability

Very weak chargeability

Very weak chargeability

Moderate chargeability

Moderate chargeability

Moderate chargeability

Moderate high chargeability

Weak chargeabilityModerate

chargeability

Moderate chargeability

RESISITIVITY

Highly resistive

Highly resistiveModerate resistivity

Highly resistive

Highly resistive

Highly resistiveModerate resistivity

Highly resistive

Highly resistive

Highly resistive

Moderately high resistivity

Highly resistive

Moderate high resistivityModerate resistivityModerate resistivity

Highly resistive

Moderate resistivity

Highly resistive

Highly resistiveHighly resistive

Highly resistive

PRIORITY

2

22

3

2

32

1

2

2

1

2

3

3

3

2

2

2

2

22

2

COMMENTS

Well defined resistivity

Well defined chargeability

Small and shallow

Likely associated with contactSmall and shallow

Well defined chargeability

Off end of line

Chargeability assoc. with con

tact

Questionable

Penetration contact?

Under surface conductivity

OG-167-July, 2001

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Quantec Geoscience Inc. TDIP Dipote-Dipote Survey

MUSTANG MINERALS CORP. River Valley PGM Project

24

2526

27

28

29

30

31

32

25+OOE

25+OOE27+OOE

27+OOE

27+OOE

27+OOE

27+OOE

27+OOE

27+OOE

1800

210050

500

1250

1400

1700

1950

2150

1900

150

600

1450

1750

2000

?

Moderate charge ability

Weak chargeability

Moderate charge ability

Weak chargeability

Moderate charge ability

Moderate charge ability

Weak chargeability

Highly resistive

Moderate resis tivity

Moderate resis tivity

Moderate resis tivity

High resistivity

Highly resistive

High resistivity

2

2

3

2?

2

2

Under surface conductivityQuestionable

Penetration con tact?

Under surface conductivity

Offend of line

QG-167- July, 2001

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Quantec Geoscience Inc. Dipole-Dipde Survey

MUSTANG MINERALS CORP. River Valley PGM Project

LIST OF MAPS

Plan Maps at scale of 1:10000

DESCRIPTION1.2.3.

North Ext. Grid: Posted/Contoured Filtered Total ChargeabilityNorth Ext. Grid: Posted/Contoured Filtered Total ResistivityNorth Ext. Grid: Interpretation over Filtered Total Chargeability

TOTAL PLANS

DRAWING NUMBERQG167-PLAN-NEXT-CHGQG167-PLAN-NEXT-RESQG167-PLAN-NEXT-INT

3

* Posted/contoured Profiled Pseudosections at a scale of 1:5000

LINE28+OOE27+OOE25+OOE24+OOE22+OOE20+OOE18+OOE17+OOE16+OOETOTAL

Drawing NumberQG-167-IP-DP-Line 2800 E-50 mQG-167-IP-DP-Line 2700 E-50 mQG-167-IP-DP-Line 2500 E-50 mQG-167-IP-DP-Line 2400 E-50 mQG-167-IP-DP-Line 2200 E-50 mQG-167-IP-DP-Line 2000 E-50 mQG-167-IP-DP-Line 1800 E-50 mQG-167-IP-DP-Line 1700 E-50 mQG-167-IP-DP-Line 1600 E-50 m

9

TOTAL PLANS= 3 TOTAL PSEUDOSECTIONS= 9

QG-167 -July. 2001

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Quantec Geoscience Inc. 'DIP Dipole-Dipole Survey

MUSTANG MINERALS CORP. River Valley PGM Project

MAPS AND SECTIONS

C G-167-July. 2001

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ONTARIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No:

Recording Date:

Approval Date:

Client(s):303851

Survey Type(s):

W0170.30745

2001-SEP-19

2001-OCT-19

Work Report Summary

Status: APPROVED

Work Done from: 2 001 -MAR-24

to: 2001-JUL-01

MUSTANG MINERALS CORP.

IP

Work Report Details:

Claim*

S

S

S

S

1214638

1229152

1229153

1231265

Perform

S3, 077

S1 1,571

32,016

52,228

318,892

Perform Applied Approve Applied Approve

S3

S11

S2

S2

318

,077

,571

,016

,228

,892

30

SO

SO

so

so

sososo30

SO

Assign Assign Approve

SO

sososo

so

0

0

0

0

so

Reserve

53,077

S1 1,571

32,016

52,228

518,892

Reserve Approve

53,077

311,571

52,016

52,228

518,892

Due Date

2003-NOV-05

2002-NOV-16

2002-NOV-16

2003-NOV-05

Status of claim is based on information currently on record.

41I09NE2015 2.22108 MCWILLIAMS 900

2001-Oct-29 16:27 Armstrong-d Page 1 of 1

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Ministry ofNorthern Developmentand Mines

Date: 2001-OCT-22

Ministers du Developpement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E6B5

MUSTANG MINERALS CORP. 1351 E. KELLY LAKE RD. UNIT 8 SUDBURY, ONTARIO P3E 5P5 CANADA

Tel: (888) 415-9845 Fax:(877)670-1555

Dear Sir or Madam

Submission Number: 2 .22108 Transaction Number(s): W0170.30745

Subject: Approval of Assessment Work

We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

If you have any question regarding this correspondence, please contact LUCILLE JEROME by email at [email protected] or by phone at (705) 670-5858.

Yours Sincerely,

Ron GashinskiSupervisor, Geoscience Assessment Office

Gc: Resident Geologist

Ken J. Lapierre (Agent)

Mustang Minerals Corp. (Assessment Office)

Assessment File Library

Mustang Minerals Corp. (Claim Holder)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:16500

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MINING LAND TENURE

MAP

o o

CA

5

inr~J

o

__ l

Dale/Time of Issue Sap 17 2001

TOWNSHIP; AREA

MCWILLIAMS

16:12h Eastern

PLAN

G-2910

ADMINISTRATIVE DISTRICTS ; DIVISIONSMining Division Sudbury

Land Titles/Registry Division NIPISSING

Ministry of N atural Resource* D istrict NORTH SAY

1 TOPOGRAPHIC

DQn

LAND TENURE

S-.4**et nriM.nr.il S fllitt

Sfal

Q

EQ

LAND TENURE WITHDRAWALS

IMPORTANT NOTICES

LAND T ENURE WITHDRAWAL DESCRIPTIONS

tHIm, DIM______nm* ———DqtiWhn^—^—————————

l JIM 1 Bil AP 1

i SiS, Htar

i WAV P^atfW wtm ** w WM

IMPORTANT NOTICES

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MINING LAND TENURE

MAP

oH

H

l

CN

CN

en o

f v '-' - *-w(••mm

.-f-"^1' -fr/H^J-^ir^;^ , ; ;'- ;:V --"::-;;':.:' ; ; ti--'" ' .^:; i . J:':J^;i;[' 5V, ^ \ :^vf'.-^;- --r-.-'-Js: ^ *V^4 ;''^'X : '

rf^'-"^;: --j ;^J^v'V.,'\ \

K''--]; r : fC: vt2|73^^^|^^

feSK^^' i^-^'MS^M^^s!

Ipi^li^iifilll

General Information and LimKalians

Date ; Time of Issue Apr 26 2001

TOWNSHIP l AREA

DANA

14i08h Eastern

PLAN

G-2904

ADMINISTRATIVE DISTRICTS f DIVISIONSMining Division Sudbury

Land Tlttes'ftegistry Division NIPISSING

j Ministry of Natural Resource Dittrict NORTH BAY

i TOPOGRAPHIC

O'

r j

LAND TENURE

Q S j i f *;* a-1-9 H r-tr-if i* oHl

Csirtfu -

Shnl*

M .AJJIBTV j:*qr'1 "**i

B Q

LAND T ENURE WITHDRAWALS

IMPORTANT NOTICES

LAND TENURE WITHDRAWAL DESCRIPTIONS

Jail ail QPJ4H1IHP

J*H l 70*1 &K 3) *-LL C 16 J 9* OUT HASM H t.

IMPORTANT NOTICES; AriM amw mtEh iHtttl rentiMU*n*. iMtt AWW DI cwHlrtop* nnt ** *l*ct nonmi ot

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RIVER VALLEY PGM PROPERTY - TDIP INTERPRETATION over FILTERED TOTAL CHARGEABILITY

Property Bound

41I09NE2015 2.22108 MCWILLIAMS

LEGEND

CHARGEABILITY ANOMALES

Interpretation by Quantec Geoscience - Du

Dipole-Dipole Array

pioi point Scale T: 10000

RIVER VALLEY PGM PROPERTYNorth Grid Ext., Dana S Mcwilliams Twps.. ON

TIME DOMAIN IP SURVEY

DIPOLE-DIPOLE ARRAY (3=5001, n^1-

INTERPRETATION PLAN MAPOver Filtered Total Chargeability

Transmitter FrequencyTransmitter Current

Decay C urve:

0.125 Hz (SOSfc duty cycle) 0.1 to 1 .0 Amps

QIP IP-10 Custom Semilogarithmic Windows

20 Gates (20ms to 3840ms)

50 metres

April. 2001

^ IRIS/BRGM IP-10

DWG. #: QG-167-PLAN-NEXT-INT

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41I09NE2015 2.22108 MCWILLIAMS 230

RIVER VALLEY PGM PROPERTY - FILTERED TOTAL CHARGEABILITY (mV/V)

Property Bound

99 l, )6 /w *Qo

Dipole-Dipole Array

250

plot point

Scale 1:10000O 250 500

(metres)

enerated by DE 117.25/01

RIVER VALLEY PGM PROPERTYNorth Grid Ext, Dana S Mcwilliams Twps., ON

TIME DOMAIN IP SURVEY

DIPOLE - DIPOLE ARRAY , 11=1-6)

FILTERED TOTAL CHARGEABILITY

Transmitter Frequency: 0.125 Hz (50"A duty cycle)

Transmitter Current: 0.1 to 1.0 Amps

Decay Curve: QIP IP-10 Custom Semilogarithmic Windows

20 Gates (20ms to 3840ms)

Station Interval: 50 metres

Gridding Method: Grid Cell Size: Contour Interval: Colour Scale:

Bi-Directional25 units (2x Manning Filter Applied)

0.5, 2.5 mV/V

Equal Area Zoning

Survey Date: April, 2001

Instrumentation: Rx ^ IRIS /' BRGM IP-10

Tx s Phoenix IPT-1 DWG. #: QG-167-PLAN-NEXT-CHG

Surveyed A Processed by:

GEOPHYSICS W O R L D W l D

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41I09NE2015 2.22108 MCWILLIAMS240

RIVER VALLEY PGM PROPERTY - FILTERED APPARENT RESISTIVITY (ohm-m)

property Bound

Map Generated by DE 07/25/01

Dipole-Dipole Array

Filter

250

plot point

Scale 1:10000O 250 500

(metres)

RIVER VALLEY PGM PROPERTYNorth G rid Ext., Dana & Mcwilliams Twps., ON

TIME DOMAIN IP SURVEY

DIPOLE - DIPOLE ARRAY (3=50171, 11=1-6)

FILTERED APPARENT RESISTIVITYTransmitter F requency: 0 .125 Hz (SO'ft duty cycle) Transmitter Current: 0.1 to 1.0 Amps Decay Curve: Q IP IP-10 Custom Semilogarithmic Windows

20 Gates (20ms to 3840ms) Station Interval: 60 metres

Gridding M ethod: Grid Cell Size: Contour Interval: Colour Scale:

Bi-Directional25 units (2x Manning F ilter Applied)

10 levels/log decadeEqual Area Zoning

Survey Date: April, 2001 Instrumentation: Rx ~ I RIS t BRGM IP-10

Tx = Phoenix IPT-1 DWG. #: QG-167-PLAN-NEXT-RES

Surveyed A Processed by:

O F H V L D

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oin

00o

in H o

RES IP MF 19K- 13 3.7

MF IP RES

931 Oj 6, 3J 1.8.

Oj Oj 0. -J———L- l l ^-. l

.1.8 L6.3 .9310

.0 Lo uo

InterpretationA

H———————l———i———l———i———l- H———i———l———i———l———'———l———i———l———————l———i———I- Interpretation

0+00 1+pON. 2+00 N 3+OONApparent Resistivity ,_H(ohm-m) F!lter 1 7K 1 W 1 5K 1 5K 1 1X 9076 9 145 1 2K 1 4IC

0=1 !5K// ^593^ 3238 2907 5337 4532 848B 17K

0=2 6583 S*~W, "~10K?-X 5745

4+00 N 5+OON B+OON 7+XMN 9+OON 9+00 N 10+OON 11+00 N, . iZjOQN , , 13+03 N | | 14+00 N | Apparent ResistivityI4K IIK 8457 8624 7272 6652 5245 6309 8150 8407 7639 6921 6318 6954 6655 549S 6574 5B30 4319 3464 2855 1758 1139 Filter (ohm-mi

m^^-19K/ 9015 9599 6379 6873 5666 6645 8728 - 5429 3293 3653 3789 7906 - 10Ky 5330 4536 — 2410 2103 2135___2241 1034 \ 475 0 = 1

23X /16K 10K,. 10K 9371 7631 5353 W73 8234 f"lO*K. 7634 ^ 5651 3960 f 7344 8525 - 4946 4682 f 1 0K \ 2954 2426 ' 3516 ] 2003 x' ^ Vx ^—^ t ^~^ v i \ v V \ \ s \ /s st \\\\ i ) \9615 f 6D04~ 92D3 i 4547 5227 5113 8360^""* 10K 11K \ 5335 6418 CjplB 4321 4494 8718 -~ 9999 ^2659 2994 —' 2505 1B53

'542 8013^, 7408 f 13K ) 6815 V 4144 5101 5280 7894 . W SIMA" 7H7S 6481 ^ .imw *04* 7917 BUS SW!1 \ m

1271

"""

24K 21K 6267 - 9133 7254 515B 7833 6120 7734 7705

. 7876 5461 ^3888 4046 7917 8146 9591 2862 -- I9D3

9831 8816 9632 — 7*46 7595 6211 8077 7135 """MM 3918 5432 5626 996S 10K 1ZK\ 7779 f 2863 ~- 3563 f S922 — 7301 ^7325 86*9 \ 1745 — ——— --~ ———\ V i ——— -l \ S l \ J \

9071 8225 ^ 4454 - 6503 7452 8373 14K 1ZK ' 3278 2621 594* 6596 6615 "^ --

4046 7917 8146 9591 \ 2 1 909 2110

1523

7270 "" 5073"^" 1379

0=4

0=5

0=6

Interpretation Interpretation

12+00 N 13+00 N 14+00 NTotal ChargeabilityFilter S.9 4.2 5.2 4,4 4.4 4.5 4.6 4.9 5.1 4!8 4,8 5.7 6 6.6 6.1 7.6 8.2 8.8 10 12 11 11 8.5 7.7 7.6 7.8 8.7 9.4 7.8 5,2

f " "V-1 r4.1 3,3 5.3 3.1 3,9 4.6 4.8 5.9 5,8 i 3 .4 6.3 6.4^—5.8 8.3' 6.4 7.8

5.3 4.3 l 6.2 3.1 4.3 4.6 5.5 4.3 5.5 C 1.7 5,1 5.5\ 7,3

5,2 -3.9 —— 3,9 , 6 -O 5- B t-S') 6.7 6.i /—5.9^ 6.9^^.8,1 l 1 2 13 14 12 S 9 .4 9.6 9,5 ^,

4,6 3.B 3,9 '7.1 6.J 5.B "-"7.3 7.3 5.5 4.7' f 10 '—— 11 11 l H ' 11 ' l - 7.8 9.9 ' 1 3

Total ChargeabilityJ Filter (mV/V)

Interpretation

Metal Factor (IP/Res)*! 000

0+00 1*00 N 2+00 N JtODN 4400 N E400N S+OON 9+00 N tO+OON 11+CON 12+00 N 15+00 N 14+00

Filter 0.40 0.39 0.56 0.47 0.47 0.5S 0.52 0.44- 0.43 0.43 0.50 0.60 0.66 0.86 1,2 1.2 1.2 1 l 1.5 2 2,1 1.7 1.5 1.5 1.3 1.7 2.6 3.3 3.2 3 Filter

Interpretation

Metal Factor (IP/Res)* 1000

n = ] 0 .40 - 0.63 . •V.1.4J' 0.76 0.68 -~ 0.98 0,55 0,30 0.31 0,24 0.27 0.48 - 0.50 L 1.1—— O.S7 0.73 s 1 .1 l 0,73 0,87 \1,9 2,3 2.6 , 1 .2 V 0.71 1.1 - 0.80 - 1.2. i 2 .S 4.9 3.5 -*.2.1 \i\-0.5l 0 = 1, * \ \ \ _ ( j ^ -

2 13 1.7 1.1^- O0=2 0.62 0.26 - 0.53 ^ 0.54" 0.45 0.71 0.46 0.29 0.26 0,21 0,39 ' 0.58. - J.64 - 0.82 7 1.2 1.2 1.00 l 0,5! ; 1

0=3 0.32 O.ZO 0,45 " B.+B^ 0.46 ^ 0.58 X 0.44 0.20 0.25 0.30 , 0.57 s 0.28 ^ 0.56 ' f 1.2 1.4 t.2 f 0 .87___0.91

[1 = 4 0.24 0.15 0.47 0.57 s 0.41 N 0.58 ' 0.44 0.41 0.39 -' 0.65 0,84 0.70 - 0.80 v I.S.^—.1.5 1.00 1.2 1 1.5 ^ "" 1.

[1=5

.4 2.2 M.4-

j l s \0.87. 1.3 J ' 0,46 \

J - - l l3.9

,0.24 0.15 0.47 0.57 . 0.41 N 0.58 '0.44 0.41 0.39 - '' 0.65 0,84 0.70 - 0.8o' v I.S"^—1.5 I'.flO " 1.2-' \ \y 2.3 2.1

\0.25 0.20 0.55 0.56 0,47 0.59 0.40^.0,49 0.81 0.90 f 0 .61 J 0.93 0.76. 1.5 1.3 1,4 1,2 1.3 1.1 1.5 7 , 3.3 ^ 2.7 l 1 .4____M 1.8 \ 1

0.29 0.22 ' 0.53 ^0.41 0.50 0,49 ^0.76 " 0.90 —1 0.75 ' ' 0.95 0.81 0.76—1.1 1.5^ 1.5 1.3 0.98 0.90 ' ' l.l 3 1.7 2 1.6 —'U

2.3 4.8

"0,92 \V'4 J——' 3' 2 4' 3

0,74 X 1,4—^^1.5x^3 3.4 3.5

0=2

0=3

0=4

[1=5

Line 1600 E

Dipole-Dipole Arraya no a

Filter*

* * ~* * *

* * * *

r0!a = 50 M

plot point

IWJTERPRETAT1D3JW•^v Strong increase in polarization

i----?-u Well defined increase in polarization

t t Poorly defined polarization increase

s'srK/ityfe ;, WeekHigh resistivity feature. . A A A Strong, Modferate, Weak

MAP SPECIFICATIONS ResisbMiy: Logarithmic Contours (1, 1.5, 2, 3, 5, 7.5, 10,..)

Chargeability: Linear Contours (every ZmV/v) Metal Factor Logarithmic Contours (1, 1.5, 2, 3, 5, 7.5, 10,,,)

SURVEY SPECIFICATIONSInstrumentation: Rx = IRIS ELREC-10, Tx = PHOENIX iPT-1

Input Waveform: 0.125 Hz. 507. duty cycle

50Scale 1:5000

50 100 150 200 250 300 l U. (metres)

MUSTANG MINERALS CORP.INDUCED POLARIZATION SURVEY RIVER VALLEY PGM PROPERTY

North Grid, Mcwilliams &L D ana Twps. , ONSurvey Date: April, 2001

Drawing Number: QG-167-IP-DP-Line 16QO E-50m~d QVANTEC GEOSCIENCE INC. ~~~~

H Geosoft Software for the Earth Sciences - Processed byoHH *

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OvoCN

o H tM

O M

mo

RES IP MF 11 K- 6.9 1.8.,

5734 j 3.5' 0,92.

Oj Oj Oj i i i i

wr IP RESJ.8 6 .9 - 11K

-0.92 p . 5 L5734

.o Lo LO

Interpretation

Apparent Resistivity(ohm-m) Filter

0 = 1

Interpretation

JtOOS 2+00 S 1+00 S 0+OD 1+00 N ^ Apparent Resistivity5266 1DK 9574 6742 9478 10K 3S13 8233 9765 9755 6966 8481 Filter fohm-m)

3439 ^ 15K 13K f \ 5919 1JK^-^

0=2 2445 f ;iOK Ij. 19K J 8862 t ill ^

0=3 4I96\^11K 13K l 7580 ^72 C\.m

\ "6 ^ f "A 1 7S44 6506 l 15K J 8249 8831--.—i x—y/

9129 7808 — 6799 6573

[1=4

[1=5

[1=6

4580 ^ 6936 ^ 8733 J 64W 5844 \~ 10I( 13K 11K l 4)68^ 7192

3162 ^5216 7085 7236 5590 '\ * I2K f 16K ; H20 -. 4593U7 /r2304 4261 7300 7062 7504 14K 9092 7197

10K 0=1

0=2

0=4 0=5

11=6

Interpretation

Total Chargeability(mv/v) Filter

Interpretation

1*00 S 0+00 1+00 N

t.3 5 .1 5.4 4.7 5,6 5.6 5.1-^ Total Chargeability

5.1 4.7 4.1 5.4 Filter (mV/V)

9.7,- J.4 6.8- 4,8 6,3 6.7- 5.1 4.9 5.5 5.1 4.5 6 0=1

V 6.6 f 4 .4 5 W 6.9 ^4.4 4.8 5 5.2 ^/T^ 5.4 0=2

4.9 5.5 5 5.2.JS-7,5 "\ 4.6 5.1 5.2 S 2 .9' /4.9

3.7 """j^ 4.7 .5.9,

2.3 ( 5 .7 5.6. ^ "9*7^,2.9.^ 5.1.^^6.7^/3.1 ^4.6 0=5

3.7 4.9 4———5.1 - 7.3 •-"'""9.8 l /Z.B 5 .2 n =6

Interpretation

Metal Factor(tP7Res)*1000

1+OS 1+00 N

Filter

0 = 1

0=2 0=3n=4

[1=5 0=6

1,7 0.61 Q.6S 0.75 0.66 0,58 0.55 0.64 0.55 0.53 0.60 0.66 niter

Interpretation

Metal Factor (IPXRes)*1000

2.8 j j 0 .43 0.51 0.81 . 0.38 'f '^ \ ^ ^-~

0.35 0.49 .0.52 - v (

0.90

~ fl - 62 y 0' 86 \0.33 \0, 63 '-0.77

r 0 ' M 0' 59 ^ =10.56 0.61 0=2

f s ^ \'.90 v 0.43 0.44 ' 0,65, 0.94^.0.60 ^ 0.41 - 0.56 0.66 "v 0.43 0.75

0.82 '0.47 - 0^53 ^'0.92^/^.010 \S 0 ,37 "0^56 0.53" 0.66

.72 x--U ^"6779 ( 1.3 ^p 0.51 - 0.43 _ 0.43 0^49 , 0^99

1.6 1.1 r 0 .55 - 0.72 ' 0 .97'~ 0,71 ' 0.31 0.73

0=4 0=5

[1=6

Line 1700 E

Dipole-Dipole Arrayna a

Filter

* ** * *

* * * * a = 50 M•o'

plot point

IIWIERPRETAT1G3NJmmmm Strong increase in polarization

i---;'- i Well defined increase in polarization

i___i Poorly defined polarization increase

Low resistivity feature, . T T v Strong, Moderate, Weak

High resistivity feature. . A A a Strong, Moderate, Weak

MAP SPECIFICATIONS Resistivity: Logarithmic Contours (1, 1.5, 2 , 3 , 5, 7.5, 10,.,)

ChargeabiiV: Linear Contours (every 2mVyV) Metal Factor Logarithmic Contours (1, 1.5, 2, 3, 5, 7.5, 10,.,)

SURVEY SPECIFICATIONSInstrumentation: fa = I RIS ELREC-10, Ix = PHOENIX IPT-1

Input Waveform: 0.125 Hz, 50% duty cycle

Scale 1:500050 O 50 100 150 200 250 300""———-l L.

(metres)

MUSTANG MINERALS CORP.INDUCED P OLARIZATION SURVEY

RIVER VALLEY PGM P ROPERTYNorth Grid, McWillioms Se D ana Twps. , ON

Survey Date: April, 2001 Drawing Number: QG-1 67-IP-DP-Line 1700 E-50m

QUAffTJSC GSOSCrSNCS fJVC,Geosoft Software for the Earth Sciences - Processed by 1(8(01/05/08)

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Or-

Ul

iH

00oM M

O (4

g

RES IP MF 3QK-, 12- 3.9.,

J

15K-, 6. 2 J 2.

, j

MF

O.,

IP RES .12 ^30K

.2 Le.2

Lo

.15K

.-O

interpretation

Apparent Resistivity l tOON(ohm-m) Filter

2+00 N 3+OON 4+00 N 5+00 N 6+00 N 7400 N 8+OON 9+OON, | 10+00 N 11+00 N 12+00 K 13+00 N 14+00 N 15+00 N7444 7695 7443 8190 8370 9120 10K 7636 l OK 15K 17K 22K 25K 26K 2BK 27K 25K 23K 16K 8824 8203 5944 5519 6404 7494 9724 8382 1337

(1 = 1

(1=2

(1=3

(1=4

(1=5 11K

6533

...J ^o,1ZK 11K-^-19K

5389" 7033 4836 3182-^9121 "6007 \ 2200 \X 12K ( 28K l 15K\ ^ 35K___ 30K 27K l 40K 33K 36K 35K ' /, ,74S9

7883 — 9331 7411 4B4Q 1 3K UK] 4MB -- 2950 VI 21K Z7K\ 15K"^-21K 24K (33K 38K 30K ' ~26K

2229 L\12K l 7507 5702 /16K W . 7774 608B "~ 5358 C\21X 26K\ ) 10K J^ 18K ^ 27K 29K ^ 33K J 20K ^\ ^^J j //S J / I±r~\ vO\\ J l\^ 3096 \ 9115 5362 f /m m/ 8915 10K 12X A 6324 \ 22K^/ 16K . ,,, .... ^.,., —. - y f --

--" — -- - S — - - X ssfi7 11k - TrlPN 12K""- 6671^~~~ 15K ' 13K 11K 15K ^ 21K ' 1 7K ^ 5441 ~~

3817

2688 3230 , !

\ 2323 l 45.1 5378 3933

2111 17K 19K ^ 8567 17K

UK 12K\ 5699 J054 4192

11K 9501 ~X"K-^7m\ 27lT~~~ 31.

26K 21K// 4770"^ 7902^ 9499

'36 -, 14t1\((^ ) 1 038 1713 0=2

1047 0=3

Interpretation

Apparent Resistivity nlter (ohm-m)

0 = 1

w/r ^2540 — 1923

2262

6238 6540 ^~ 7846 2656

0=5

1=6

Interpretation

Total Chargeability(mv/v) Filter

^ = 1 0=2

Interpretation

1+25 N 2+26 N 3+25 N 4+25 N 5+25 M 6+25 N 7+25 N 8+00 N 9+OON IQtOON 11+00 N 12+00 N^ 1J+OON 14+00 N 15+00 N4.3 3.9 3.S 4.3 4.7 5,4 5.4 5.8 7.4 7.7 7.6 7.4 7.8 B 8.4 8.4 8.1 7.8 6.9 7.7 7.5

Total Chargeability8-6 10 II II 9.6 5.8 Filter (mV/V)

4,3 ^-3.9

v4.4 \

0=6 5.5

6.9 8.3 *7,7 7.5 7.1 7.7 7.1 7.4v^8.4 , 4 .2 s 6 .7 6.8 6.3 -^ 4.9 , 8 10 9.7 __ 8.9 ^-4.83.5 2.8 3.7 2,8^-- 4,2 4.3 —— .4.6

V.3 8 7,1 7.5 83.5 3.8 2.4 3.S-S.3 4.5 2,5 l 5.7 ( 1 0 7.3 7.5 .5.9 7.6——.7.4 8.8 14 — 16

7.7 9.4 \ 6.3 7.5 7.9 7.9 B.9 10 8,4 f 4 .9 J 8 ,

5.9 f 9 .B 8.3 !.6v 6.1 688 7.8 l 8 .6 9.6 9.4 7 5.2 B.I 9.2 ; 6.1 ———-6 7 9 ^\ 10

9.3 8 ,9 S '7,5 5 .3 8.7 / 15 ^ 14 -W 5,4 6.1

'S. 2 9.9 7.5 8.1 9.4 9.1

3.B^ 4.4 f 2 ,9 3.5 ^ S.i/ B.B/ 4.

4.4 \_j.g j.7 3.2 7 5.6-— 8.1 4,4 5,9' 7.2 ——— 7,2 7:7 B."4__J./ '7 3-'-—^ ".l *.* 3,B f.i '.i! ' \ B.l^ O.

4.5 ^ 4 --^ 5.4 ' 6.K 5 •^7.8 ——8.3 7.2 6 7^ 8.9"

7,7 ^8.2 9.2 8.9

6.6 7.8 ^ 8.1 8.4

Interpretation

Metal Factor (IP/Res)*! 000

H——i——l——i——l——————l——i——l——i——h-

1+00 N 2+00 N 3+OOf 4+00 H 5+OON 6HJON 7+00 N &+OON 9+00 N 10+00 N 11+00 N 12+00 N i —— i 1J+00 N 14+00 N 15+00 N

Filter

0=1

0=2

0=4

0=5

0=6 0.6

0.83 0.69 0.72 0.58 0.65 0.73 0.61 0.92 0.71 0.64 0.53 0,44 0,37 0.32 0.34 0.41 0.50 0.56 0.71 0.82 1 1.7 1,9 1.7 1,9 2 1.7 2.4 3.6 Filter

Interpretation

Metal Factor (IP7Res)*1000

1.1 0.74 0.9292 1.5 j 0 ,87 1.5 \ D.39 D.5J . 0.38 0.22 0.19 0.25 0.22 0.26 0.20 D,19 0,30 - 0.57 N*1.4 x 2.5 1.9 , 0.85^ 1.6 3 , 0.95 y 1 ^- 3.4

^1,1X^0^58 0.75 \ LI'0 6,48 0.36 0,48 0.23 0.25 0.2B 0.20 0.27 0.24 0.22 ' 0.75 0.58^ \ 1.3 \. 2.6 \L7-~-1,4 2.3 1.9^ , D.97 7 S'!T~\ Z,!065 0,55 '0.49 . M.1x^ 0,58 0.75 \ 1,1X^.0,48 0.36 0,48 0.23 0.25 0.2B 0.20 0.27 0.24 0.22 ' 0.75 0.58 ^\1.3,\. 2.6 \L7-~_ 1,4 .2.3 1.9' , D.97 X 5.;,~---' ; ^-- x --~N \ A ^v,\ i \ \ v^CxS^ v——i—J^^-^sS ^//I f0,54 0.42 0.42 0.66 ^0.46 0.47 0.81 1.5 N. 0.36 0.35 0.41 0.35 0.33 0.24 0.23 0.33 0,33 -- 0,59 0.79 - . ^0.69 -- 0^97 ^. 2.1 2.5 2.1^ 1.5^^. 1.00 //4,2V,

1.7 V 0.36 0,38 ' 0.62 ' O .J" 0,42 0,53 ^ ^0,97 \ 1.5^*0.39 0.34 ^0.59 s 0.38 0.29 0.29 0.29 0.47-^-1-^ 0.71' 0.97 ^.58 Vfl,84 l 3.3 3.3 l 1.3*^0.75 //1.7 ^

0.40. N. 1.2 NX- 0.41 ^ 0.59 ^ 0 .30 0.35 0.49 0.57 1.63 X 1.1 N^ 0.35 0.54 0.70 ^0.44 0.35 0.35 0.42 Vl.4 1,2*^0.93 0.92^ 0.57 i 1.4 \ 4.4 J 2.1 | 'l).57 l 1 .7 V 2,7

61 0.40 ^TT^'tl.e? ' 'o.31 0.3' O'58 0.73 0.4} ^ 0^3 0.90^ 0.51 0.66 0.61 0.53 0.40 0.50' ' '\,l 1 .5 Li 0.95 0.91"" ~" fl.94 '2.1-——2.7 ' ' 0 .67 ' \.l ^-1,5

0=1

2.9 0=2

5,8 0=3

0=4 0=5 0=6

Line 1800 E

Dipole-Dipole Arrayo noq

Filtert

* * ~* * *

* * * * a = 50 MV

plot point

INTERPRETATION

Strong increase in polarization

Well defined increase in polarization

r~" ~i Poorly defined polarization increase

Low resistjvl T T v strong, MoaUgh resistivity fe L A A Strong, Moaerat

MAP SPECIFICATIONS Resistivity: Logariltimic Contoure (1, 1.5, 2, 3, 5, 7.5, 10,..)

Chargeability Linear Contours (every 2mV7v) Metal Factor: Logprithmic Contours (1, 1.5, 2, 3, 5, 7.5, 10,..)

SURVEY SPECIFICATIONS

Instrumentation: Rx ^ IRIS ELREC-10, Tx = PHOENIX IPT-1input Waveform: 0.125 Hz, 50?5 duty cycle

Scale 1:500050 O 50 100 150 200 250 300—————-l L.

(metres)

MUSTANG MINERALS CORP.INDUCED POLARIZATION SURVEY

RIVER VALLEY PGM P ROPERTYNorth Grid. Mcwilliams A Dana Twps. , ON

Survey Date: April, 2001Drawing Number: QG-167-IP-DP-Line 1800 E-50m

QUANT&C GSOSCIENCS INC.Geosort Software for tte Earth Sc/ences - Processed by

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O 00

l

RES IP MF 14. 2.2.

13K.I

\ l

oJ

1.1.

oJ oJ

MF IP RES ^2.2 ^14 ^26K

.1.1 \-7.2 - 13K

Lo Lo

Interpretation

Apparent Resistivity(ohm-m)

3+OCS 1+OOS 0+00 1+00 N 2+00 N 3+OON 4+00 Nt .jTuu j | | ^TUU j f | irm;.;______ UTUU | | | .Tuun | | /.-nju n ( f jnm n. ( | TTW n | __^ ^ 5+00 N | 6+00 N^ | 7+00 N 8+00 N^ | 9+001^ 10*00 N

Filter ™ 10K 8429 9993 8965 8285 7949 7994 5568 5633 2727 3437 3339 3387 3553 3650 4021 4898 8768 8094 8891 8214 12K 1IK 13K I5K 11K I2K 8552

I5K I2K y 3858 ^ IOK i 7826 S7B3 - 6371 — 5905 2973 s. JOK^ , 1463 1266 y 281 275 473 - . 916 -y 2749

y/5506 /,11K IOK 7873 5313 f 9907 6820V 3835 W20 \ 1575 — 1613 ^-3R9 , 633 •"•'"T'TlfiB s 2499

11+OON 12+00 N 15+00 N 14+00 N 15+00 N 1&+OON 17+00 N

9314 8599 6406 7608 6B44 6972 18K 18K 19K 20K 24K 1*K 13K 6054 Filter

Interpretation

Apparent Resistivity (ohm-m)

12K' S5UB 'y, UK li* 7873 5313 j 9907 6820\ 383?"" W20 \ X |s75 — 1613 - r- , .., , .... , ,—y/ l / s~\ *-s \ r^r-vA \ ^S^r^^/X/ i[1=3 5874 'x'12K 11K f 8004 J 4125 ^ 8653 IOK — -•" '- —— ~~ —- ^-"•OC-... ' ^

' / X S //s~\ l[1=4 13K 12K 9385 , 4097 A 12K \ 8716

B195 - 4287 B510

[1=5

[1 = 6

13K

9385 , 4097 ,

9873 f 4803 s 9202 -

K '"'5223 X'12K' 8621

i 1 106 N 3208 . 1734 (If V\\\ '

90Z —— - 1479 '272* 2827 5780 ^ 4761—, \ ,

2232 1042 x 3099 2264 ' 4747 ^ 279S — 3304 2982 3824^ 2645 62J1 V 13K^ 8301 9852 —— IOK f 21K/N. 11K J 1 9KN\ \ ^ — ' 7 s- —— ^^ l ^ V\ ~ ^^

B144 BIBS - 42B/ BB10 /^ IK V

) - ( ^ 7 X X \l 11K.A 402W 8871 ' I OK 11K

15K y 6636 i 16K x 5890 6951__7012 5466 ^HK^j 4261 3957

4898 ( 14K 9492 8081 — 7326 7153 f UK \ 6275 4354- \ 8684 ) 2730 7217- J ^ ~^\f r'S \\\ \ ^ (--^ ^

12K 13K \ l 5330 7939. * i 2K 12K. \ 4689, 4788 — S341 __S781

11K I3K X 3853 ^ 2244 \ 1113 v 3743 4405III ^^^ \ \ l. \ l ^r

\ 1113 \ ^ \\ \\

14K ' 4781 3631 2458 1437

\\\ 9087

™ . ™,.

939 ' ! 2K 12K \t ^s \*.

8770 l 1 8K N. 22K ~~^ 18K S 1 3K 11K ———

^ 6729 f I 3K 9075 6243 -^ 5717 3018, \

6184 KJK ] 35186175 ^ 3552 3865 f 1 769 l 3984 5463 20K N 9087 8770 /',,., . m - ,.,. , l ul , ,,., ,,,,- -.™ .,,, ,,., , ..,, . -.-. . ,,y y ) ) \\\\ ^vv. j i\ \ f C *-^ \ ~ i ^—^ \\ \ \ ^ v\^_//L v—^4411 1791 2806 4305 ' 8728 18K - 7791 ' 15K 17K x 34K \ 12K 14K 15K ' 6538 5993 7675 - 6409 7143 8916 ^ 20K N 8245 ' 14K ——22K ~ 12K 9932

31 K V 12K 35K 18K 20K ) "5600

Interpretation -H———i———H —l———————I- —l———————H -l———————l———i———l———i———H Interpretation

Total Chargeability ^ (mV/V) Filter 5

J+25S 2+25 S 1+25 Of 25 S 0+75 l 1+75 N 2+75 N J+75N 4+75 N 5+75 N 7+00 M 8+OQN 9+00 N 10+00 N 11+00 12+00 N 1J+QON 14+00 N 15+CON 16+00 N 17+OON

+-B 4.2 4.5 3.9 3.7 3.9 3.5 i 3.3 2.8 2.4 1.9 2 2.3 3.1 3.9 5.1 5.6 6.2 6.7 4.8 5.5 5.7 6.4 5.9 5,1 5.7 5.8 7.5 8.5 9.3 n 11 11

6.1 —— 5.9 i 3.3^ 5 3,7

{1=2

^=5

5.6 5.7 4,9 7.4

3.6 3 s 5.2 3.5 2.5

3.2

t,6 1.3 1.9 5,9 4.7 6.9 v^ 9.

3.1 -4.3 4,2 22 0.74 1. .2 ^-5,8 \ 6,3

5.5 4.7 3.8 2.6 3.5 V 4.3 \ 3,5 J-8 2.4 \ 1.6 -C.2B .2.1 2.7 3.1 } 4 .8^ 8.4 ^ 6.1

4,8 5,3 4.2 3.3 3,9 3.3 \ 4.2 1.5 2.7 2.3 1.2 s' 3 .2 2.9 3.9 ^ 4.8 N 7.

!3 )2 11 11

10 s. 9,9 11 12

Total Chargeability6.7 +.B Filter (mV/V)

5.5 4.6 s l.S 6 .1

4,7 4.6 f 3.4

3.B 3,8

3.9 2,7 \ 1.8 1.6 J 2.5 l 1 .7 ^ 3.9-^3.6 3,5^^ 4-' 3-B' 5,3) 6.6

3.3 3.* 2.7^ 1.3 ' 2 .9 '1.6 ' 3.7 4.6 4.5 4.7 '3,7 '4.8 '6.9 6.9 4, )

i xB.3 6.1 4,1 3.1 S . 6.7 6.Z——^i.^jr

X 6.8 6.4 6.3 . 4.7^,^-6.6 6.8 X 5,3 /j 1 2 -

7.1 ^-5.8"^ 6.4 6.9 , 7 .7 6,3. 5,6y^X.12 12

,7.3 5.8 \2.9

.6 6.5 l 4.7

12 10' 7.7 '5.59.2 tO I6\^n 11 12

13 X, 1 8 ^^ '2 \ 1 1 f 9 '

12 ""l? \\ 12 9.9 8.3 8.7

6.B ^ 4 .3 5.B 7.2 ' 9.3

^=2

^=5

,7

Interpretation

Metal Factor (IP7Res)*1000

3+OOS 2+00 S 1+00 S 1+00 N 2+OON 3+CON 5+OON 6+00 N 74WN &+OON 9+00 N 10+00 N 11+00 N 12+00 N 13+00 N 14+00 N 15+00 N 16+00 N 17+OON

Filter 0.41 0.50 0.57 0.4S 9.47 0,50 D.55 0,49 0.81 0,84 1.3 1.2 1.2 1.5 1.2 1.3 1.2 1.2 0.94 0.99 0,89 0.90 0.53 0,67 0.60 0.44 0.50 0,56 0.71 0,88 1.2 l.fi 1,6 2 2

0 = 1 0,41 0.49 t 0 ,85 0.49 0,47 0.45 ^ 0.72 0.61 , 1 , 0.51 ^ 2.4 l \ ." /' ,' f

[1=3

(1=5

11=6

•y-.. J ^~-^]L^~^L!—-^ 1A Z -1 ^x' 1 '* 0" 9'7 v 0-a -' O i63 / Oi86 ! i5 X 0- 79 ^ v lij 0- M, ' 0- 33 0' 5! D ii5:5 O i39 ' O i92 —^ li2 1-! 9' 8Z ^s^ 2 • 5 2 i * V'0.38 0.73 0.45 0.44 0.39 0^81 0.42 " 0,54 - V.W —- 1.1 V 2-1 /T-—-"'olTr^ 1.2 —v, 1.5 "^1.2 1.00 J 0.62 - 0.71 0.77 1,4 x 0.75 0.54 x 1,00 ' 0.53 0,41 0.37 0,49' /O.ft1 x O.sT , 1 /V^vV 1.1 ' l 3.43 1.7x v. /^ M\ y i^x^\\ i f S/ ,~^^~~ f - N ,^ x- 7 ^^ f/// v^ vji 7

1.4 ^0.69 -0.31/J 1.4 0.99, I.I/ 0.84 X 1.81 \ 0.58 H 1.4 ., C.74 0.53 0,41 s. 0.67 0.52 0.32 0,58 -1 0.94 ^ 0.50 0.57 f 2.3 2.4 "-—l.7 ——1.80.54 , 0 .46 0,41 0.47 0.63 ,, 0.41 0.43 0.42' . ' ^

0.36 0.43 0.45 O.BO 0.34 0.38 0.31 ^ O,

,0.37 0.77 0.39 0.44 0.23 0,71 0.73 0.54

...

flV -0.31/^1.4 0. '

0.23 0.38 0.19 0.66 1.1 ' l.\ -TJ

1 0.24 r /l N 0.52 1^0.70 0.71 ^0.37 0.33 x 0.59, 0,33 0.53 0,97 ' 0.52 0.59.

1.3 1.2. -. 0 .33 S- C.66 0.68 \ 0.40 0.27 0,35 0,5^ 0.73 •""0.61 0.64

0.79 0.37- 0.61 0.44 0.25 0.17 Ol58 0.65 0,60 0.56 -^ 2,5 ;1.5 1,3- t.6

vV

l 0.86 0.72 0.67 0.50 0.61 0.59 0.80 Filter

0.25 0.53 0.49 0.5B 0.31 ' 0.62 v 0.40 0.77 [1 = 1t v-

0.69 . . 0.66 ' 0.36 J.47 - 0.55 0.76 ^=2

(1=3

[1=5 [1=6

Interpretation

Metal Factor(IP/Res)*! 000

.35 ' 0.95^. 0.33 f 0 .5B ^ 0.38 0.9B

1.6 1.60^ O'.SQ -- 0.47 - 0.52 ' 0.48 " 0.73

.2 \ O.W—-1.1\ r?.2\\ X 0.28 ' 0.83 ^0,43,' 0.87\ 0.89—-1.1 \ 1 .1 \\ 0 .26 ' 0.83 0,43 'XV \\ VU lli'v. i ^ i ' -' '1.8 ^ 0.68 ' 1.5 1,2 x ' 0.46 0.70 0.74

Line 2000 E

Dipole-Dipole Arraya noa

Filtert

* ** * *

* * * * a = 50 M

isplot point

INTERPRETATION

^^M Strong Increase in polarization

i" - 1 M ' Well defined increase in polarization

i i Poorly defined polarization increase

Low resistwty feature, v v v strong, Moderate, weakHigh resistivity feature,

i A A Strong, Moderate, Weak

MAP SPECIFICATIONS Resistivity: Logarithmic Contours (1, 1.5, 2, 3, 5, 7.5, 10,..)

Chargeability: Linear Contours (every 2mVXV) Metal Factor: Logarithmic Contours (1, 1,5, 2, 3, 5, 7.5, 10,.,)

SURVEY SPECIFICATIONSInstrumentation: Rx ^ IRIS ELREC-10, Tx = PHOENIX IPT-1

Input Waveform: 0.125 Hz, SO/S duty cycle

2.2210Scale 1:5000

50 Q. 50 J 00 150 200 250 300 l l l l l

(tnet'es)

MUSTANG MINERALS CORP.INDUCED POLARIZATION SURVEY RIVER VALLEY PGM PROPERTY

North Grid, Mcwilliams k D ana Twps. , ONSurvey Dote: April, 2001

Drawing Number: QG-1 67-IP-DP-Line 2000 E-50mGSOSC1SNCB INC.

Geosoft Software for the Earlh Sciences - Processed by KB(01/05/08)

Page 36: Quantec Geoscience Inc. - Ontario · 2017-01-17 · * Report Type: Summary interpretation, suitable for OMNDM assessment filing The results from the service provided by Quantec Consulting

O O\ (N

o rg

RES 45HU

22K.I

IP MF 12 2.8,,

6 J 1.4.

Oj OJ

MF IPop in.2.8 f 12

.1.4 L6

RES ,-45K

1.22K

.0 LO

Interpretation Al———i———H -H———'——l

Apparent Resistivity 4+oos (ohm-m) Filter

3+00 s 2+00 S 1+OQS 0+00 1+pON, 2+00 N 3+OON 4400 N 5+00 N 5+00 N 7+00 8+00 N 9+OON 10+00 N 11+OON 12+00 N 13+00 N H+OON 15+00 N 1&+OON 17+00 N 18+00 N!4K 9643 6731 8992 12K I3K 13K 10K 7712 4822 3*92 4239 4134 W81 2J83 2659 6473

11=3

11=4

11=5 11=6

7538 8207 5273 7970 9584 7347 9000 7839 5957 336! 4638 4527 5070 5*52 11K 14K 26K 28K 34K 41K 36X 35K 28K 24K 18K 13K 9513

7 c' 11V

Interpretation

Apparent ResistivityFilter (ohm-m)

.1052^-; 1703 —.859 - 2101y -,595y 1691 __TQ^j . 2352 ^ 3272 vx 23K ^ 17K - 22K 25K 27K 43K 28K 26K 20K 21K , 8805 — 6616 xx^6K n=1

4758 ~~665i -^ 1423 1115 14H f 3099 ~~ 2464^J 3987 40B7^X15K ( f j6K X 26K 24K/ 47K 37K 33K^\ 28K 22K ' 10K~"17K \ 5320 :? 1818 n=2

1lK-iil4B01 — 5381 6531 6700 ^ 1789 A 7759' -**"l3K-—— 13KJY\ 1047 1746 2013 (9027^.3844 4182 3298 \1 SK \ 36 K \26K^/ 36* 40K 45K 32K 30K 19K S 25K j j13 /)//!

8211 7421 '/. 1 230A .6521. , 1 BK -""""aK } 6144 si 1179 \ 1918 ^ 4449 ( 14K\4S7 3287 3966 \\ 22K^\ 34K 38K 31K 51K""*] 43K 31K; 28K__ 26K ^ W A 1367 11=4

157 _ cvfifi \ infi i f w (vj cai

Interpretation

Total Chargeability(mV/V) Filter

0 = 1

0=2

0=3

0=4

0=5

0=6

nterpretation

Metal Factor (IP/Res)*! 000

14K 9619 4997 ^ 9515 — 9169 - 6441 B824__ 8492 6079 6758 5618 . 2357 , 1740 ^W —— 979 1698 — 1893 i 3414 -^.825._, 1491 2477 3367 , i 11K s Tilt.*/, 1052 ~- 1703 —.859 - 2101 , - 695 y 1691 __706 j - 2352 ^- 3272 v x 23K ^- 1 7K - 22K 25K 21s\ M x MV v. \ y /"^ -\ \ / /^s-~-~) ^^^^-* ^^^ l ^^^^y/ /-——- MI t / /^//^-rr^rsss. ^ *~* ) ^^^ / ~^^ f r~^\ f24K \ 13K l 6037 3561 \ v I2K 10K^69IO 1ZK 9Z31 9048 6364 , 1760 1638 1782 — 2031 931-^267^ 2695 l 6045 -^ 1918^^3342 392t 5362 l ™ S/ 1959 - 475fl 6851 -^ 1423 1115 14H f 3099 ~~ imj 3987 4087 SVtSK ( (36K N 26K 24K/

21K \ 8965 4116 5483 ^ UK l SK ^11K 14K 11K. 7586 f 1 943 1179 1407 'Xx'm^O 1828 C^j23 440 V^. 4414 f . 1lK-ii 4B01 _ 53B1 6531 6700 "- 1789 /^ 7759 •*^WL . '-^jH 1 M7 1746 2013 ( 9027^. 3844 4182 3298 ^18K \ 36K \26K^/ 3!

15K l 5938 6240 5637 \ UK f~W v\ 12K } 1 6K\ 8826 7^2452 1240 1126 [t^ 1 1KU 1092 ^MS \^J?^^ 7270 r^9X\ 679E__ 8211 7421 ' t 1 230^V 652! y 1BK -^*~m j 6144 si 1179 ^ 1918 ^ 4449 ( 14K\^4S7 3287 3966 \\ 22K"-x34K 38K

9379^ 8720^ 6159 5915 \ 10K 26K\J6K -—- 1 3K j j 3001 |485 ]K6 /- 8476 1 5K yy 2224 ~~ l 991 ^ 998^T 392 \\\\ I2K ( 287x^9122 8656 J1693 *s 3964 f l 14X ( 27K f 9 157 — 6766 N 1136 '/5002 6969 14K Yy 31S6 3757 4386 ^y 18X \ 45K 33

13K l 8225 72+8 ' 9590 ^ 22K '^~34K \ 13K **^4777 ^ 1748 1138 ' 10K 9792 "^2526 ' 4473 2779^^ 1K5 ~ 1488^ 18K f 35K^ 9241 -- 2107 — 4963 ' 7233 ' 20K —^10K 9181 6555^ 3092 ^ 6751 7S90 11K^ 3565 4084 3696 ' ' 24K 38K

i . i L. , j i i isl———————l———i———l———i———l———i———l———i———l———————l———————l———i———l———i———————i———(———i———l———————l———l———l———i———l———,———l———i———l———,———l———i———l———————l———————l———————l———i———l——,———————,———l———,———l———,———l———,———l———,———————i———l———i———————i———T'""""! 1 " l i,———,———H———,———,———,———l———————p———

4+OOS ^ | 5tOQS | t | 2+OOS_____1+00 S | | 0+00 | 1+00 N | | 2+00 N | | 3+00 N | ; 4+00 N | t 5+00 N t 6+00 N 7-KX) N | StpON | &+OON ( 10+00 N | | 11+OON t | 12+00 N | | 13+00 N | | 14+00 N4.8 4,1 3.4 3,5 4.1 4.3 4.1 4.3 3.8 3.6 3.2 2.3 2.7 2.9 3 1.3 3.6 2.6 3 5.6 5.5 4.7 4.5 3.8 3.4 3,8 3.2 3.5 3 3.9 5.2 9.8 10 10 10 11 11 1

4.7 4,4' 3,5 3.6 v 4.4 4.6 -—4,1 5,2 4,4 5.3 6^ 2.9 2.9 1.9 2.4 3.1 v 8^ x-1.4 —^- 3 i 5,7 4,5 4,6 6 4,8 2.3 2,6 -0.3 -^3.9 2.3 2.7 -1.7,^9.3__9.5 9.4 - 1.^ 9 8.9 l.

6,3x 4.B l 3 ,! 2.7 3.6! 5 3^7 \4,3 4,6 (^Tj 5.4 y/2,2——.2,1—^2,5 2.4' 1.1 \. 4\ 7.7^^3.3 '4,9 if 6,8\ 4.1 5.3 4.5^^ 3,8 3,4 Vl.3\ 2,9 f 0 .28 -0.08*^9.! 11 8.6 10 ——9.9.__g.g'^lT^

6.7 ( 3.7 2.4 3.1 4.1 4,9 \3.7 J) 4.T 4,3 4.1 2.2 1.3 1y/ /VX 1.6 0.27^_4-3 ^33 8.9 V\ 4,1 6.5 6.2-^^S.2 4.1 / Q.52 j 3 'TT 77X 2.4 .-1.5 -2.9^)11 _ II ^-9.5 B.6 "l3~^x 11 11 1

5.6 \ 3 2.9 3.5 4.1 5.2 4.1 4.2 4,6 ' 1.5 1.3 1 f 4 .5 5,5 N. 3.9^^0.59 -38 ^9.lN^"4.4 5.5 7 A 4.1 1.9—— 2.3 3.i /6.8 | 4.8 /I -1.7 -^8J Xjsj 8,2 8.8 J11 V. 14 12 11

4.6\3.4 3,8 2.7 4.2 5.3 4.2 4.4/2.5 o',59 Q .S!, S S ( 5 .3 ,3.6 4-———3.1 -1.6 V) 9,1 \\ 3.9, 6.1 __.5.9 \3.2 3.4 1.5' 5.9 —— 5.9 l il -2.3/78.3 9.J-xll \ B.7 y/11 11 \ TT N 12 1'

5,1 s 3.7 3 3.6 \ 4.3 5.7 4.5 ' 2.3 ' 1.4 -0.63 '4.2——- 3.6'——"3.8 3.5 5.9 4.2 l O^*^ B.4^ 4.5 5.1 5.3^^4^ 3.7 ' 4 ,9 5 3.8 ' -0.46 ^6.9 9.5 * 7.7^ 11 11 11 11 ^ 15- 11

r^3

28K 26K s 1 8K 7. 1367\ S—N //s#/

45K 33K 39K 47K 41K 30K 37K l 17K /? 1 829

3565 4084 3696 ' ' 24K 38K 40K 37X 44K 42K 37K ' 24K l 1955

17K /^)j(4L n^5

0=6

Interpretation

14+00N t r 15+00N | 16+OON | 17+00N | i 1&+QOM | 19+oQM Tota | ChargeabilityFilter (mV/V)11 11 10 9.9 9.1 8.B 8.3 7,9 7.6 6.2 5.6

1.3 8.4 8 -8.1 -7.7

~icT\9.5 9.3 \J-tl 8 -6 J 7-5

11 10 8.9 8.2 8.1 ——

11 11 l 9.7 9.5 7.8' 8.9

10 10 10~\ 9.2 8.9

8.2

7.8 8.9

8.9

10 8.4

0=2

0=3

0=5

3+pOS l 2+COS 1+00 S 0+00 1+00 N 2+00 N 3+OON 4+OON 5+00 N4+OOSt——i——Filter 0.36 0.45 0.55 0.45 0.40 0.43 0.35 0.41 0.41 0.57 0,76 0.87 0.95 1.5 1.4 -21 -10 -21 -11 1.5

&+OOM 7+00 N &+OON 9+OON 10+00 N 11+OON 12+00 N 13+00 N 14+00 N 15+00 N 16+OON —*- 17+OON 18+00 N-t- 19+00 N

0=2 0.26 0.37 0.51 0.75 \ 0.31 0.46,^0^.54 0,35 0.50 0,42 0.85 1.2 1.3 1.4 —— 1.2"

0=3

0=4

0=5

0 = 6

0,32 0.4! f 0 .58 0.56 x 0.36 0,33 0,35 0.30 0.40 0.54 v 1,1 1.1 f b.Tl - - 0.44 0.86/.^^ N /\"

0,37 ' 0,51 0.47 0.63 i 0.2! 0.23 0,33 0.25 0.52 0.60' \ ,

0".93 ' 0 .33 0.49

0.49 0.40 ' 0.62 ' 0.39 0,21 0.20 0,26 0.33 0".82 0.40 ~ 0,52 - 0,36

0.38 0.45 ~ '0.41 0.38 0.2D 0,17 0.34 0^49 0.7?' -0.55 0.42 0.37 ''/\5 O jT^ 2.1

1 0,73 0,61 0,93 0.65 0.72 0,99 1.2 0.68 0.62 2.5 1.3 1.6 1,3 0.66 0,53 0.40 0.25 0,26 0.26 0.38 0.45 0.67 0.78 0.87

.4 . 0.56 0.32.^2.2-^1.5 1.5 -1.9 -.3.4-3.8 f 1 .8 s 1 .4 i O ,. ..,/f : i 'As—^-~^ ^ \2 / 1 .——. 0.99 0,30 - - - — -

-2.4*^,3.9 2.9 xv 0.42. 0.41 0.41 0.36 0.31 0.19 0.29 0.31 0.39 0.39. O5. ^ ^0.86 ^0.49

v^.84^— 0.80 '."0.50 ^ 0.88 y1 2.3 S f 6 .20 -fl.028'^3.7 2.8 2.1^X^70. 0.28 0.38 0.44 0.20 0.25 0.23 0.30 0.34 Vsi - 0.45^1.2^^0.97

tfl ft id n TT ft A ' i n * f n B'T

Filter

0=1

Interpretation

Metal Factor (IP/Res)*! 000

t / ' ^ -^ ,.---- , 'l/f l/t'i m\V / ^\S^^v ^.^— ,'l.lf 0.79 0.61:^0,29 0.39 0,33 0.42(^1.3^/0,87 -1.4 4, 1 .2 V^2.8 2.3 2.6X^0.74^ 0,30 0,42 0.31 0,25 0.20 0.26 0.27 0.42 0.30 (O.M--0.49

1.81 V ,K O .Se'^-TeS^ 0.35 0.21 0.31 , X 0.77. — 0.86 X -0.88/^2 "J 0.93 ^\ 2.2 2.7 2.(IvXS3 - D' ffi ^ 'X 0-* fll ' 9 0 lK O lffi "'^ 0 |29 "/l/ '' 70.35 0.21 0.31 i 0 .77 — 0.86 -0.88l ,' ^^ f,

3,1 fc -4.2^-0,77 , 0.14 ^ 0.66" " 0.68V' 1 - 9 7 0'.85 l 0.25 0,22 0.65 0.44 -2 A, 1.7 l'.3 - 0.77 \\ 2.7 2.9'-. '///~} f/' X

.13 0,55 -^-2.5 ' 0 .88 0.51 0.25 0.48 6.41 -0.073 14

7 \\\\\

100 0.96

. \Xxx

.6 V-"-??

2.7

0.27 0.32 0.26 0.22 0.22 0.30 0.23 0.46 jS 1 .5

O.S2 0.29 0.25 0.28 0.22 0.24 0,23 oV '''fi

Line 2200 E

Dipole-Dipole Arrayo no a

Fitter*

* * ~* * *

* * * * a = 50 M

plot point

INTERPRETATIONStrong increase in polarization

Well defined increase in polarization

Poorly defined polarization increase

resistwiT v strong. Moderate, weak High resistivity fi

MAP SPECIFICATIONS ResisMy: Logarithmic Contours (l, 1.5, 2, 3, 5, 7,5, 10,.,)

Chargeabifty: Linear Contours (every 2mVyV) Metal Factor Logorithmic Contours (1, 1.5, 2, 3, 5, 7.5, 10,,,)

SURVEY SPECIFICATIONSInstrumentation: Rx = IRS ELREC-10, Tx ^^ PHOENW IPT-1

Input Waveform: 0.125 Hz, 50^ duty cycle

Scale 1:500050 O 50 100 150 200 250 300

iZ^^S (metres)

MUSTANG MINERALS CORP.INDUCED POLARIZATION SURVEY RIVER VALLEY PGM PROPERTY

North Grid, Mcwilliams St D ana Twps. , ONSurvey Dote: April, 2001

Drawing Number: QG-167HP-DP-Line 2200 E-5Qm QUAJfTEC GEOSCISKCS INC.

Geosoft 5'offware for the Earth Sciences -Processed by 1^8(01/05/08)

Page 37: Quantec Geoscience Inc. - Ontario · 2017-01-17 · * Report Type: Summary interpretation, suitable for OMNDM assessment filing The results from the service provided by Quantec Consulting

o o ra

a\ o

RES IP MF 33K^ 10., 4.2.

17K. 5 .2-j 2.1.

oJ o.

MF IP RES -4.2 10 33K

,2.1 [.5.2

.o Lo

,17K

L.O

Interpretation

Apparent Resistivity (ohm-m)

0+25 S 0+75 N 1+75 N 2+75 N 3+75 N 4+75 N 5+75 N 6+75 N 7+75 N 8+75 N 9+75 N 10+75 N 11+75N———l———,———4———,———i———— 13+00 N 14+00 N 15+00 N 16+00 N JJ+OOJl 1B+OON 19+00 NFilter 8878 7551 8155 UK UK 10K 1IK 6799 3663 5897 4335 5483 4925 6328 6026 4105 5188 4033 2421 1992 1683 1587 1S97 1803 2250 5455 8287 11K 1BK 2* 21K 27K 30K 26K 30K 30K 24K 17K 19K 20K I5K Filter

Interpretation

Apparent Resistivity{ohm-m}

4332 — 5023 ^ 7781 -12K —— 10K 8291 17K j 5590 --. 170S , 7549 - 190B - J1SO 2402 2867 \ 8514'

0=3

0=4

0=5

0=6

3823..\9080 y 3464

j

11K

1757 - 3062

15K\\ 5069

1819 1074 ,- 436 346 300 382 1545^-7234 17K - 23K 25K'-06 ' 4764 /- 3038 \ 1075 ^^ 1546 1688' 499 —— 58B932 ) ) . 6120 L 7944 1235 ^ 6405 4134 4522

21K-~^ UK \ . 8814""^ 1905,— 2415'^ 4200 ~~ 4386 ^ 1888.\ 9018 \ 5621 ' 6207 -C" 2003 x 'WV) .S 960! J *P \^™.^\. 1 797. " 2T84 \'B83-^ 705

8047 —.6327 "" 9309'A (WK^ \ 'l 6.K, (rf. l'2?4' ' ( 8162 V2093 4008 " 5639 N 229B\\ "11K ~" 7579 '/"1268 f i 5438 ^ 9248 X 6429 3450 \N ?58 V 1968 2327 O 1140 — 1\ l ^-—' \ \ l i t*——-~- N X \ \\\ l l l Iff J l i If ' S \ NX*. X\ N ^sN-3896 6683, 3037 l 8311 7520 , N 2785 A 15K J/ 1386 -^ "~ "" ' "" "" "~ ""

11'K ~~ 8082 ^ m ~^im~ 3975 2313 -* 6196 6847 10K 6441 3385 = 2598 3828 - 6097 4954 3182 3574 3475 •"v" 737 - N 2545 4411 3890 -"" 7141 3949 - 6458 — 6558 --- 3926

22K 20K

, W s- 6347 — 6276 — 9485 ^ XX 43K 27K , , 12K _ 11K__11K 12K n=1

-wtr/ f , 9424 ' 12K 13K l '33K ) 21K'/ 5631 //30K-O^-I5K I4K ,V 46K 35K /16K 9701, / 26K 1 1 IK r^2^J i l l S f 7 l ^™x l \ f f t ^ ' ' I ^***^*** ^* .___i ^ \. t f *

^.1627 \7776 \^\K S^ W& H BK ^_25K /j 9 233 ^s 2 1K f 49K x 20K '—— 1SX

,1983 s J 7523 — 7706 f 13K 12K__ m '^/'W. 33K V 59K \/ m C ^13K^^20K' "m.'^,m 1 7K n=4

9734 / W 3636 3524 \\ 778 ^\" 1932 3040 ^'1607^2566 .5804 6132 ,- 4969 l Kjt^^ 3607 '^MSJ Y/ 43K -—50K 38K\ 60K \ ^ 20K (~677l CN 1*K /36K X 22K 0=5t ^-^s 7. ^ A ..^ /^;JJ// r.. \ .V \ \\\\i62K 58K 38K 33K 26K 0=6

Interpretation

Total Chargeability(mV/V)

o+ooFilter 4.1

4+00 N 5+OON 7+OON 8+QON—t———l———i———l———t———4———,———l———i———l———,———l———,———l———i———————i———l———,——

6.3 4.6 2.9 '3.2 3 3.7 3.1 2.3 3.1 2,7

9+00 N 10+00 N 11+OON 12+00N

Filter

n=1

Interpretation

Total Chargeabilityt i j. i , A

11 9.7 6.5 s -2.9^

2.3

Interpretation

Metal Factor (IP7Res)*1000

\ l t \ \ 7 ^ l \ ^-———x V X v—'——X3.2V 5.4/ 0.53 )2.8 /-4,1 2.7 3.5 3.5 1.8 0.99 2.3 J.B S.I' 6 .1 6.8 6.2 l 9.3 B.fl ' 5.8-^7 6,3 6.1 7.9"^ 8.1 6.2 6.3 6.5 \ 5.4 n=2

3.3^^- 2.1 ——2.3 4.2^3,7 ^TT^X 3,3 3.3 0.69 1.3 f 3.1 3.9 , 6.5 7.2 6.9 7.3———B"^ B.5 ^8.9 8.6 V. 6.8 6.7 7.9 6.7 7.9 6.6 6.3 [1=3

4.4/0.097 4.2——-3.6 3.4 2.4 0.91X. 3 2^1.l J2.4 3.6 . 6 .6 7.5 TA-^"'^^ J B.I ———-B /9.4'^^O ^ 9.1^**^ 7.7 6.4__ 6.5 j B . 4 B.2 6.9 [1=4

l 0 .65 2.3 l 5.5 j 2.5 2.2 2.1 0.69 1,7 3.2 2,2 3.4^ 6.4 7.6 7.7 3.4 ,7.Z [ 4,8 l / 9.4 ' ' 1 11 9.9 X 7 ' 1 / *- 9 J 7- 9 B' B 7- S n^

1.9 -— 2.9 3^ 4.2 M.4 2 ' 1,7 -0,24 ' 3 /^~~*T~~~~-4.1 6.1 7.5 7,6 ' 9 7,9 '5.4 ^8.5 ' 1G 11 11 9.4' '4.8 '7.4 ' 8.3 B.5 ^=6

——l——————l——————C——————l——————C——————l——————l——————l——————.——————l——————l——————l——————l——————l——————l——————\————————————l————————————]————————————(————————————l————————————~——~——————————————^——————,————————————I——————l———————————————————l——————l————————————l————————————l——————l——————l——————l——————l——————l——————l——————l——————l————————————l——————'——————H———————————l——————

0+25! 0+75 N 1+75 N 2+75 M 3+75 N 4+75 N 5+75 N 7+75 N B+75 10+75 +75N 13+00 N 14+00 N 15+OO 1&+OON 17+00 N 1&+OON 13+00 N

Filter 0.56 0.64 0.65 0.52 0.63 0.96 1,5 2.9 3,4 1.3 1.5 0.88 0.83 0.69 0.61 0.53 0,61 0.63 l 1.4 1.6 1,8 2.2 2,4 3.8 3.6 1,3 0.89 0.77 0.63 0.52 0.55 0.46 0.36 0.41 0.32 0.32 0.37 0.45 0.43 0.36 Filter

nterpretation

Metal Factor(|P7Res)*1000

0 = 1 0.83 -. 0.89 D.75 0,45 0.67 0.76 0.49 -^1.9-— ''•l'sp O ' 65 \V 2'' "~O ' 2 1.*— 1.2/ 0.66 v. 0.46 ^ 0.81

0=2 0,32 . 0.82 0.84. v 0.33 0.40 -- 0,52 .0,97 ,// 10 )) 1.5,^-0.64 l\1.4 V 0^90*^0.88 0.71 0.52 - 0.29 V JJ.59 - 0 .5!' V* 2.5

0=3

0=4

0=5

0.39 v 0.96 0,68 0.20 0.29 , - 1.3 ' t .3 l .8 0.40. , ( . . f . . . . ^ . .

0.50S -- J.81 ^ 0 .42 0.15 0^71 S 2 .9 (^-— ' 2 3j ^ 1.4 V -0.44^*-J .3 V v0.50 ~ . 0 .5

0.43 -0.39 0.34 0.32/73.6 3.22.2 2.2 0^94 -0,51 ^ 0,98 ^0.41 , ^ 0.47 - - 0,65 0.56* ' ' O.'si---'/l

0.22 0.36 ' 0 .77 "^ 1.4—— 1.4 3.8

0.90 ^ 1.8 J.5 3,2 ^ 4.4 ^ 6.1 .

2.5^-^2 "\ 4.6, 6.4

0.61 0.69 0.53 ^v. IJj^'0.46 0.43 s 0 .75 "\"1. F 1.9 1.5 ~~ s 0 .7? ,\ 2.2 V 4

0,076 ^ 0.77 ' 0.39 l fl.63 0.69 •*^jT^--1.5 . 6.87 i \ \ 2.3

. --,, -.-. -.-- , -.,. - .... -,~ -,— -.-. 0,59 0,59 v 0.89 T" 0.86^ / V I. \s-' v-'.7 - 1.4 0.63 -0.45 ~ 0.66 0.71 0.75 0.50 0.85 0.43 ~ 0.56 O

v 0.89 ^ 0.^86 -^1 1.4 ——

.49 ' -0.32 ^ 1.2 1.1 1.1

0,74 0.40 0.30 0.39 0,62 - 0.63 0.74 0.64 0.20 0.18 0.29 0.52 0.54 0.45 0,48 0=1~

.64 0.57 "~ 'O.W tt,28 0.42 l (T ; , 0.24 0^43 0.44 0.17 0.23 0.39 i 0.65 ' 0.25 0.47

O'B* 0.67 - 0 .76 V0.43 0.33 l 0 ,70 " 0^41 0.17 0.34 0.42 0.21 0.34 0.51 " 0 ,31 0.31

.00 — 0.99 0.67 0,51 "" 0,54 0.29 0.31 0.15 0.34 0.48 ^ 0.32 0.43 0,26 0.40

0.90 ~"o;S3 ~" ""0.80 l 0 .22 0.21 0.2B 0.17 0.36 , 0.72 V 0.41 0.25 0.35\ '^—————————-N ^ \ f *-.\

1,4 1.2 1.4 ' 0.34 0.17 0.19 0.29 0.19 0.49 0,98 x 0.25 0.33

0=2

0=3

n-4

0=5

0=6

Software for the Earth Sciences - Processed fay 1 8(01/05/08}

Line 2400 E

Dipole-Dipole Arraya naa

Filter*

* * ~* * *

* * * * a = 50 M

V plot point

INTERPRETATION•Mi Strong increase in polarization

t 'i Well defined increase in polarization

L i Pooriy defined polarization increase

t v v Strong, Mooerate, WeakHigh resistMty feature.

A A A Strong, Moderate, Weak

MAP SPECIFICATIONS Resistivity; Logarithmic Contours (1, 1.5, 2, 3, 5, 7.5, 10,..}

Chargeability: Linear Contours (every ZmV/V) Metal Factor Logarithmic Contours (l, 1.5, 2, 3, 5, 7.5, 10,, ,]

SURVEY SPECIFICATIONSInstrumentation: Rx ^ IRIS ELREC-10, Tx = PHOENIX IPT-1

Input Waveform: 0.125 Hz, 50/5 duiy cycle

Scale 1:500050 O 50 100 150 200 250 300

-l L. —(metres)

MUSTANG MINERALS CORP.INDUCED POLARIZATION SURVEY RIVER VALLEY PGM PROPERTY

North Grid, Mcwilliams &L D ana Twps. , ONSurvey Date: April, 2001

Drawing Number: QG-167-IP-DP-Llne 2400 E-50m "^| QUANTEC GfOSCIENCE INC. ~~

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oHm

ao

oM

RES

20IU

IP MF .5^ 2.6

4.7 J 1.3-

Oj oJ oJ

MF IP RES 2.6 -9.5 ^40K

.1 .3 L.7 L20K

J) L O uO

Interpretation H———^-——t—

Apparent Resistivity (ohrn-m)

1+00 N 2+00 N ——i——i——i——i——i- J+OON 4+00 N &+OON 7+00 N 8+OON 9+00 N 10+00 N 11+QON 12+OON 15+00 N 14+00 N 15*00 N 16+OON 17+00 N 18*00 N 19+00 N 20+00 N 21+00 N

Filter 69?4 5205 5737 62B8 5629 5623 5206 4186 4102 3449 4807 4533 3313 2960 2298 1755 1562 1210 140S 1710 2107 2485 658! UK 16K 17K 21K 24K 23K 26K 21K 19K 22K 29K 33K 36K 26K 25K 23K 24K 24K 24K Filter

Interpretation

Apparent Resistivity (ohm-m)

n=1

11=2

11=3

[1=4

[1=5

[1=6

UK j. 6256 2917 2717 , 1158 _.938__ 1158 1484 3301 W& ^ 6 145 6102 2965 - 5359 .-734 x 867___770 , 279 396 -^. 253 424 ^sa 1S38 xx. 15K - 13K- tTK//^-^ s—\\NX -^——s\ / j ) l f~} l r" '——^\O ( YA ^ /^^^^- ' ~~

(^y W99 3940 ^ 6345 \ 2946-^1804^^ 2785 N \ J 2456 2439, 3273 ^ VK\^ 3207 — 2956 — 2662 N^832J 1456 J 593-^.406 370^733^,. 1672 1908 ^- 8747 f f 25K

4729 3397 i 6499 6505N 4295 — 4435 3203 — 2582 2120 f 4569 _ 4810 — 4183 3153 4340 2611 ^ 1217 -—* D63 713 j 319 /104Z ^'tlisz''' 1707 1707 \Yj4K

3265 5018 — 5278 839T^~S2W , 4828 -- 5525 2431^ 4107 5424 , 2066^ 4154 4071 3644 3525 \\ 699~N 975 ) 533^1085 ^ :^~~^ -— ^ — ^—

X

2493 1779

434} 3731 , 6990 , 16K \ 9270^^7809 56*9 ^ 4468 4546 2414 2635 4985 3121 4442 y 1930 X 790 776-^x 21B6 -~ 3712 3152 ^ 2759 — 2965 2687 ^ 3803 , ( 22K

2987 4903 ''UK- l SK 14K^ 5786 8500- 5065- "2026 3043 3038 3616 3591 2285 2113^640-* 2935 -^^TSeT^ 3308 3422 4435 2701 ^ 1124"'

^, 5352 — 6240 ^16K 20K 22K -r 4835 ——14K UK s^ 26K 17K 18K——- 2GK ^^ 26K

^^^^^^m^ ^^^^^^^m 24K 28K V17K

m —— 21K 23K\ 73t|\. 15K^ 12K^X66K 46K \. 21Kv \ 7605 .\\ 29K"3*^1 25K— XX'Sir:—t////... -. \ \ \\

""XVtT/'j^Kfx ". " ) "C 1^,BOK 81K N 31K 7D16 -^ 16K N 42K 61K x 41K 34K - 21K - 10K

[1=2

[1=3

11=4

[1=5 [1=6

Interpretation

Total Chargeability (mV/V)

i+oo N 2+00 M 4+00 W 5+OON 6+OON 7+00 N 8+OON 9+00 N 10+00 NFilter 5.4 6.5 8.4 7.3 6.3 5.3 3.9 2.7 2.6 2.2

11+OON 12+OON 13+00 N I^OOJL2.8 2.6 2.7 2.3 1.8 1.7 1.4

H———i———l———i———H

1.6 2.5 3.8 5.3 6,1 6.3 5.8 6,7 6.3 6.4

15*00 N IfrtOON 17+00 N 1SKMN 19+00 N 20+00 N 21+00 N

[1 = 1 5.9^7.1 v S S,^^,! Llill^l.S 2 .1 3.9 J.6 4.5 .3.4 2,6 2,7 2.5 2.2 2.6 2 1.9 1.5 1,4

[1=2 6,3 5.3 X 7.5 ^ 9.7\M.5^ 2.8 3 \ 0.60 1,8^^,2.3 2.8 \ 4.2 2.4 2.8 3.S 1.8 \ 2,6 2.3 0.61 1.2

[1=3

11=4

[1=5 [1=6

.

.1 0.45 -0.64 l. 2 /x 4.9

s.\ -w—r ^— -~4.4 5.2 4.

— 6.9 .-7-6 6.8.

7.B 6.9 7.3 7.4 7.1 7 6.8 7.2 6.1

3,3——.4.3 , 7.2 6.9 7 6.6 7.7 6.14.4 \ 3 v -0.64 2.1-^-6.6 -v 9.2 8 9- , 3 ,3——-4.3 j

.5 5.J\J^ —— 2.4V^8'7™^-e 9.7 7.4 X5.2^-6,3 —— 6.3 6 7.2 6.6 7.2 6.7

6.3^ 5.1 ^5.3'S*8.7 9.4 8———8.3 (5.2/^8.4 8.1 6,3^5.9 7 7.5 6.6

.4 s 1 0 8.2 6.5\ 5.7 7.6 7.1

5.7 4.2 \ 7.1 5.S' 7 .3 S ; U N ll \ 8.9 / 1 ^ \ 4 .1 J /9.5-~~10 .10 8,3, 5.1—^6.3 7,7

0.17 H .3 Z.l" -^ B.Z——-S.B— 6.4 7.6 6.4 '3.1 4,5^ 6.5 B 5 S fj 13 ^ 11 ^ 7.6 ^ 4,9 7.3 \ 11 10 9,9 7.8 6.3

0.87 0.74 \ 2.8 2.9 3.3 2,7 3.5 2.7 ^Z 1--——2.1" 0.45 -0.64 1,2' s 4.9 4 .8 4.4 .6.4 \_B.6y 6.

3.9 \ 0.18 U\ 2' 6 /^- 7 3' 6 3 J 2- s 2- B l-J 0.34 -1.2 0.19y,4.8 ^ 5 : 9 5.1 ^^ 6 "^—6.1-^^6,9 5.5 / 5.8 ^ 7.. 4

1.9S. 0.95 1.6 1.6 X 2.6 4 2.1 2.5 2.1 -0.59 -0.065 0.98 '^ 4',8 f 6 .4 ?,2^ 7

3.8^ 1.1 0.64 2.2 2.7 2.B 2.2 ^"T?

9.3 9.4 J 6.2——.6.3

Interpretation

Metal Factor(IP/Res)*! 000

Interpretation

Total Chargeabil'tyFilter (mV/V)

n=1

n=2

n=3

[1=4

[1=5

[1=6

Interpretation

1+CONl———i———H 2+00 N 3+03 N 4+00 N 5+OON S+OON 7+00 N 8+OON 9+00 N 10+00 N 11+OON 12+00 N 1J+OON 14+00 N 1MOON 16+00 N 17+00 N 1&K10N 19+XN 20+00 N 21+00 N

Fiiter 0.96 1.3 1.7 1.3 1.4 1.1 0.78 0.69 0,64 0.71 0.64 0.66 0.79 l 1.3 1.3 1.4 1,8 1,4 1,9 2.1 2.3 1.6 1.1 0,78 062 0.52 0.38 0.22 0.36 0.66 0.62 0.53 0.44 0.38 0.25 0.41 0.36 0.37 0.32 0.33 0.30 FilterMetal Factor (IP/Res)* 1000

0.52 ,- 1.1 i 3.I 1,4 1,3 1.4 1.2 1.3 i 0.73 0.56 0.88 3.5 j 2 .5 3.4 v 7.1 ^- 4.8 i 5.8

1.5 —— 1,5 1,8 1.1 i 0.42 0.95 — 0.86 0,46 0.75 0,95^ 1.4^\2,1-^ l.

0,95 D.34 0,35 v 0.61 0.61 0.79 0.85

0.56 0.54- - C.46 0.50 0.72 0.54 -0.53 0.3! 1- 0.58 x 0.40 0.41 0.68 0,31 ^0.64 , 0.27 0.41 0.37 0.39 0.26\

[1=3

[1=4

[1=5 [1=6

0.93 1.4

0.49 - 0.55 0.33 0.52 0.16 0.26 0.44 0.52 '1.2 1-1 /L7 l'* y'C.83 0.95 0.71. 0,075 0.38 0.49 6.84 O.BB 0.7?' 0.69 0.80 ^^9^0^35 -2.2 0,18 V 1.4 J 2.3 2.8

0.99 /•^.^ /^.^ , o.83 0.83 ^ o.?i o'si 0.21 0.34 l o.ea 0.99 0.79 i o.ee 0.55 'l 1.1-^^0.74 -o.ow 0.45 ^/ij/ 2 23 24 j.iX"o.73" 033 0.53 LIB o.is 0.23 'l f / s v \s v. s// . . . -.. 1 .'•6 1.4 O.B3 0.87 ' 0.61 0.71 0,45 0,22 0.32 - 0.73 0.88 0.76 0.61 0.74 '0.078 -2.1 0.71 0.82 M .8 1.9

.3^\.Z^ 2 .7 2.7 \vVss" O.J5 0.38 ; 0,60 ' 0.34 V 0.60 0.28 0.45 \0.93 ^ 0.61. 0.35 \ .Si ' 0 .15 0,34 N X 0.60 v^ 0.32 0.27 0,26 0.39 [1=2

^rT""? 19 2,8 2,6 \V 0,46 0.34 j 0 .55 ' 0.34 0.47 ^ 0.26 0.42 0.41 V N '•1\X ^ - fl - 43 fl .13 0.18 0.31 V 0.78 \ D.24 0.23 0.26 [1=3

\ W\\ ' . .4 0.52^-^*1^^^5.75 0.12 0.15 " '" "" " "" " "" "" —'

'( 0.59 0.55 V 1.3 j fi 0 .22 0.15 0.16\ ^

2.4 2.8^ 'o.49 0.54 ' 0.18 0.16 0.16 0.36 0.69

0.75 0.12 0.15 0.18 0.41 0.62 0.20 0.25^ \

0.26 0.34 ^ - 0.55 , 0.23

- 6.45 0.26 0.16 0.24 0.23 0.30 " 0.60

^=4

[1=5 11=6

Line 2500 E

Dipole-Dipole Arrayna

Filter

t * ~* * *

* * * *

i___L

a = 50 M-B'

plot point

INTERPRETATIONStrong increase in polarization

Wdl defined increase in polarization

Poorly defined polarization increase

MAP SPECIFICATIONS Resistivity: Logarithmic Contours (1, 1.5, 2, 3, 5, 7.5, 10,..)

Chargeability: Linear Contours (every ZmV/V) Metal Factor Logarithmic Contours (1, 1.5, 2, 3, 5, 7.5, 10,..)

SURVEY SPECIFICATIONSInstrumentotion: Rx = I RIS ELREC-10, Tx = PHOENIX IPM

Input Waveform: 0.125 Hz, 50/5 duty cycle

Scale 1:500050 O 50 100 150 200 250 300

J" 'L.(metres)

MUSTANG MINERALS CORP.INDUCED POLARIZATION SURVEY

RIVER VALLEY PGM PROPERTYNorth Grid, Mcwilliams &C D ana Twps. , ON

Survey Date: April, 2001 Drawing Number: QG-167HP-DP-Line 2500 E-5Qm

QUANTZC GEOSCIENCE INC.^^—^^—Geosofl Software for the Earth Sciences - Processed by K^(d i/05/08)

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O 04m

H J

m Ho

RES 30 K.

15K,

IP MF 10. 4.8

J

5 J 2.4.

J

oJ oj

i——i——i——r

i i i i i i i i i i i i i ' r~r~r~r-r-r-r~ r~r~r" i—i——i——i——i——i i i i——t i \——i——i——i——i——i——i——i——i i i i....j i i i i

MF IP .4.8 -10

RES

.2.4

Lo Lo

.15K

Interpretation

Apparent Resistivity (ohm-m)

H———————l———i———l———————H Interpretation

4+QCS 3+oos 1+OOS o+oo 1+00 M 2+00 N 3+OGN 5+OON 6+00 N 7+00 N 8+OON 9+00 N 10+00 N 11+OON 12+00 N 13+00 NFilter 8578 10K 10K 9995 11K 9786 11K 12K 12K 9041 7175 5815 6240 5234 8420 5354 5955 5493 4391 3803 2915 2fl09 2569 2555

6288 N - 12K 12K 14K ^ 11K

14+00 N 15+00 Nl———i———l 16+00 N 17+00 N 18+00 N 19+00 N 20+00 N 21+CON

[1=1 7713 I6K I7X- 12K

r^2 12K

n=4 5193 5471 8573

[1=5

[1=6

13K 14K

8743 \ 18K 16K ' 7936 y 1891 ,\\ \ / s/// y/9863 x 16K ' 7397 s 3050 s 7178

\ ^-- s ^ \ /—x__,K 1*K I3K V. 8012 V 15K 17K I6K , 6903 " 2 118 J WA \ 2 134 2449 x 5591 v, 4320 f 9265 \ 4Q3B 3254 1832

X, 9665 14K UK X 8743. \ 1SK 16K ' 7936 s 1 891

—i————f————t-———l————i————i—ii.i . . .. .r————i————i——i—t-^——i————f————i————i————i————i————r^~—^" i ' i————'———t——"^-t————l————"————t————i————l————*—^—l————i————l - " ^————r————P————i—- -*..'..—(————i————i————'————i————i————i————i————i————i————i————i————i——-i————i ' ' - * "- -'f————*—

2558 2569 2262 149) 1310 1121 1099 1244 1686 2297 3806 5143 UK 17K 21K 16K 13K 14K 13K 17K l SK 17K 16K 21K 20K 28K 25K 1BK 20K

691 —— 651 j 1 644 1956 2)24 2436 y 907 s^ 460^ 241 283 ^311

343 x 2157

xM \ J

niter

Apparent Resistivity

5471 8573 . 13K 4K 9883 ^ 16K ' 7397 s W5K s 7 178—x^ \N ,^-x - ~*sy// ///-^ ,4981 4919 7956 y UK ( 16K 9034^76552 . 2208 / 7954 7507\ \\ \ \ t r^^ y y//

4989 4770 8098 16K •'iJK* ' 3679 — 22B3 " 8436 8637 '

•S 1 768 — 2560 3190 \8188 3578 4327 — 3050 2033 1713 865 -——69i-—— 651^ 1644 1956 2)24 2436 , 907 s,^^ 460 241 283 ,311 ^ 838 1736 3118 3206 \v1*K f~~ 15K ' 3 1K

1118 y'woTv 2134 2449^ 5591 v, 4320 /^ZeT^N 4Q3B 3254 1B32 . 1141 ^ 1558 — 1343 , 2157 32fl7 3557 1481 g&tT^X 609 X. 321——"402 ^S 940 1S86 2320 52dT~~ 5215 \ 1BK 29K 26K/7 \^ \ \ \\\ y \ ^—^^—-x\\ \ i i i i V -O\ / /s i f \ i \\\\ ^-x 7s 6865 5771 ~- 3369 2271 S369 6976 ~~ 7915 . 4406 f 2514 2014 — 219B 2559 X 1487 \ 2751 4358 f 2000 ^ 135Z 1071 - 730 \^.VA ^ 1 076 1405 19B3 3455 , 7148 6562 \V 31K 29K Js ^—Ox\ \ \ r~^ \ "\ \ ( ^———^ \ i \ s / ^ N ^—/s t i i \ \\\\ \/ /

7178 7154 x-10K,X 3857 2481 \ 8927 l 5239 \ 9176 2946 2581 "^ 3729 3467 2834 1933 3135 -- 2225 1858 1414 1178 "^928—— 1037 1375 j 1 691 2781 4225 7035 -^ 11KsX 29K f 1 BK -

7507 J/12K 11K\ 3721 ~ 3214 ^6646 5871 5735 3283 4577 ^~~570T 3340 386lN 2067 1482 . 1945 1979 1568 — 1445 s* 2339 x 1286 1575 2289 3144 3893 l 9964""^ 10K ~—x 17K f

3637 -^12K 13K 10K^ 5322 ^~2422 - 8135 '^Tx 6465 5917 6585 5015 3599 3897 ' 945 —— 1223 1981 2271 2206 3527 'V~293S X 1 618 2070 2483 2733 5277 -7728 7W6 ' -^26K

- 15K - 31K 15K i 6925 6618 2470 1554 -^ 1036 , 4001 , , '' ' "———' \ t ( ^~~ -^"^^ J l f

) 3200 2113 " 6884 = 5841 7200

' 29K y 16K '—— 15K /. 4849 3195 -. 8692 /^JltT^x. 8781 8230 5^3882

-z:.6189 5066 , i 13K 11=1

41K \ Y" 4194 BJ48 l 23K ^ = 2'^N-X l \ lO 5755 \\ 15K n^3^S^x

52K S J2K ^—— 31K ^-6805 11=4

31K 39K 46K ^=5

' 37K •'SSK n = 6

Interpretation

Total Chargeability(mV/V) Filter

^=2

^=3

4+OOS 3+OOS 2+00 S 1+00 S 0+00 1+00 N 2+00 N J+OON——l———i———h-

4+OON 5+OOM B+OON 7+00 N —i——i 8+00 N 9+pON 10*00 N 11+OON 12+00 N 13+00 N 14+00 N 1&+OON 16+OON 17+00 N 18+00 N 19+00 N 20+00 N 21+00 N

fl -* 4.5 4.2 3.5 4.8 5.7 7.2 7-5 B.2 6.8 5,9 6.1 5.6 6.2 6.7 7.7 B.3 9.2 7.9 7.6 7.7

8.5 9.2 8.9 7.6 v 5.t i 9.7 9.6 M. , 1 1 , 9.2 s s 1 -5 2.9 3.8 3.5 2.8

T 7.2

[1=5

[1=6

7.6 6.9 7.4 9.7 8.8

7.1 6.8 f 9 .4 9.7 8. B j

4\8' 'B.9 B.B 9.1 ' 6 '

5,2 2.6 4.2 4.1 4.B'1.7' 2,5 4.3 X 2.6

/

!.J 2.7 2.8 4 4.8 5.7 i 9.1 X^L^ 9- 7 / 6 - 7 / 5 A 3 ' 6 4- 3 1-8 - 1 - 1

2.7 3.3 2.7 4 6.3 7.3\ 8.9 9.3 7.7 ( 5.4 5.B \ 2.9 3.4 2^^2,1

1.6 3,4 J.2 2.9 5.4 7 ___7.1 i '^^} 8 .9 \ l X 5.6 5.3 X. 3.4 S 4 .9 -—7.2 ~~

3.4 3,3 3.7,_.-4.1 6-^^ 4.8^\ 8.2 9.8 8.2———'8 \ 4.9 6^^ 5.2//ID ——9.!Q)s*

nterpretatlon

Total ChargeabilityFilter (mV/V)

0=1

6.7

8.5 9.3 l 6.9,

' 6.6 6.3

Interpretation

Metal Factor (IP/Res)* 1000

4+aos 3+OOS 2+00 S 1+00 S (MX) 1+00 N 2+00 N 3+OON 4+OON 5+00 N 6+00 N 7+00 N 8+OON 9+00 N 10+00 N 11+OON 12+00 N 13+00 N———l————l————h- 14+00 N 15+00 N 16+OON 17+00 N 18+00 N 19+00 N 20+00 N 21+00 N

fitter 1.1 0.96 0.95 0.94 0.82 0.84 0.80 0.71 0.79 0.95 0.92 0.87 0,86 0.95 0.75 0.83 0.81 0.9J 1.3 1.9 2.3 2.2 2.1 1.5 1.1 1,1 1.3 2.2 2.4 3.t 4.4 4.2 2.4 1.9 1.5 1,3 0,81 0.55 0,47 0,51 0.65 0.65 0.95 0.67 0.2D 0.58 0.58 0.56 0.67 0.42 3.46 0.68 0.49

[1 = 1 1.2 . 0.54 0.55 0.72 0.71 0.

[1=2 0.95 . 0,63 - ' 0,86 \ 0.63 0.55 l O.Sfl 0.66 0.59 C

0,80 - 0.80 0,85 0.97 — 0 .78 ^ ., ; \ ^—-.73 ' 1.4 0.77 ~ 0.

[1=3

[1=4

[1=5

[1=6

0.68 x 0.91 \ 0.57 0.53 l M .3 1.6 V i

0.73 0.63" x 0.81 0.53 , 0.89 V.1.7/. 0.74

1.2 i - 0.42 \ 0.79 0.84 ~ 0.96 1.4 \ \ v - \ f ^^^~—~

67 \1.2 0.95 v 0.55 v JJ.88/ 0.46 0,77 ^

1.2 x, U __ 1.7 3.8 3,2 4.6 7.6 8.6 s 3 .3 2.3 i 1.5 1 s 0 .48 0.66 i 1.3 jf 0 .59

Filter

11=1

Interpretation

Metal Factor (IP/Res)*! 000

0.92 -^1.1 ^ 0,89 x 0.67

1.5 1,3 ^ O.B6 ~ 0.73 0.63 x 0^81 0.53 , 0.89 x U-^ 0.74 - 0.71 0.50'

1.4 1.4 I^X 0- 72 Q-55 0,71 " 0.93 . 0.85 ~ 0.75 0.85 (l 0..50

0.92 ' 1.9^ 1.1 V 0,61 " *fl,47 * \, 5 ' ' 0^27 "" 0.49 0.85 ''0.57' 0.48 -0.58 ~~ 0^94

N 0.58 0.81 0.52 0.72 '1.8 7 3.6 3 \ 1.5 —— 1.4 0.86 0,68 V 1.5——-1.S, 3,1 3.S V 6.5 SV \ ^ f /y / ^S \\ \ l \ Y \"\ \ ^——S1.1 \ 6.47 0.7B v 0.52 ' I\A' 3 .^,^^2.8 2.5\\1.1 1.4 \ 0.65 0.76 T—-1 X 1.8 \ 3.6 / i ——— 3.3

0.91" - 0.67 V 0.87^—1.1 ( (2.5 2,4 2.1 2.3x\ 1.1 1.3\' 0,49 ~ "oTSS.^A 1.3 \ 2 X^3.2 /"T?N

0.94 '*1JS' 0.79 1,7- 1.3^-2-——1.9^ 2.2 2.5 Y 1.1 1.2 ^ D.079 O.M ' t.5 1.7——'1.5 1.5

f , 4

... , .. __, . , ..64 0.46 0.32 0.44 0.77 0.54 i 1.7 1./ S——— l -O \\ \ l .-- n \ J ri ' t - - 1 . , f ,- . . V .j. Q32 Q 30 Q 56 ^ 0 45 ^ 092 \^ 16 J O J2 g a O M ; 0 33

' s -^ "L//1 \ \ " 's', " s ' v- x' ,'0.34 0.31 0.44 O-* ^ 1-1 t .\^7t,M 0 .23 0.62 0.53 ^ 0.63.' 0.45 0.23 0,38 ^ 0.70 0,44 n=3

2,2x 1.5 1.4 \ 0 ,68~ 0,76^x0,33 0.46 0,32 ff ' l ,00-- 1,3//' 0,41 0,30 0.25 " 0.55 /-l-'\ 'd. 50 0,23 0.40 0.30 ~ 0^44 n = 4

X -l * '-- - -- ''-'- - ~' '' - -- l'ff,. \ \ 1 '\ \ -, , . -——l', 'f.3 X 1.4 1.00 , 0.55 0.69 0.50 0.33 0.89 0.66 0.44 0.23 0.31 0.24 l l\ 4 1.1\ i s^ i ^, - i ' ^ x'^v ^ / i ll y2.5 2

1.5 v 3.5 s- 2.6 2J ' 0.72 0.80 ' 0.~43 1.82 ' 0.36 ' 0.97 0.51 0.22 O .24 0.31 0.76 1.1 f 0 .65 -

0.31 0.37 0,33 0.21

0.48 0.30 0.22

[1 = 5

[1=6

Line 2700 E

Dipole-Dipole Array...a na a

Filter

* * ** * * * a = 50 M

plot point

IIM1ERPRETAT1BWI

Strong increase in polarization

Wdl defined increase in polarization

defined polarization increase

sistivity fDrig,"Wocfer(Se, weak h resistivity f?

T T V

A A A

MAP SPECIFICATIONS Resistivity; IjDgarithmic Contours (1, 1.5, 2, 3, 5, 7.5, 10,..)

Chargeability: Linear Contours (every 2m\yV) Metal Factor Logarithmic Contours (l, 1.5, 2, 3, 5, 7.5, 10,..)

SURVEY SPECIFICATIONSInstrumentation: Rx ^ I RIS ELREC-10, Tx = PHOENIX IRM

Input Waveform: 0.125 Hz, 50/5 duty cyde

Scale 1:500050 O 50 100 150 200 250 300

•J L.(metres)

MUSTANG MINERALS CORP.INDUCED POLARIZATION SURVEY RIVER VALLEY PGM PROPERTY

North Grid, McWiitiarns A Dana Twps. , ONiurvey uate: April, ^UUI

Drawing Number: QG-167~IP-DP-Line 2700 E-5QmQUANTEC GEOSCIENCE INC,

Geosorr Software for the Earth Sciences - Processed oy KB(01/05/08)

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On m

RES IP MF 19KL, 19 16.

9659^ 9.3' 7. S.

O- oj

MF IP RES -16 19 fl9K

-7.8 '9.3

.O LO

.9659

-O

Interpretation

Apparent Resistivity (ohm-m)

6+OOS 5+00 S 4+COS 3+00 S 2+00 S 1+00 S Q+oo HOON [ 2+00 N 3+00 N 4+00 N 5+OO , 7+00 N BtOON 9+ON 10+00^ 11+00 N 12+00 N 13+OON 14+00 N 15+00 NFilter 6032 8489 8676 1BK 5209 7100 6184

0 = 1 1424 - 2091 2541 — 7945 i 2284 v - l OK x. 3791

(1=3

(1=4 n=5

(1=6

10K UK 15K 15K 18K

——\ / 7277 5372

8957 9214 8119 6486 2933 3026 2480 1914 2034 2296 2309 Z543

10K 7061 398S - 5445 s 1 725 1784 ^-871 i 764 B2B -.900—— 1207 , 4651

.2309 1716 3029 — 2722///( \ J

6911 .4206: -^ 2713 V* HK'^^7415 "\13K f 1 7K 19K 15K 19K 16K-" 832.7 UJtnO l 19I(/, 6010 V 2239 2668 2380 3116 ^

9104 l 5192 ^ 5062 V 2530 \ 15K y 5850\ l SK 17K 15K 15K f 23K l 7453 7373 8811 m S W\ 5756 ^.3419 . 2118 2681 4919.

8019 6828 6021 4B04 3329**- 12K- 7016 l K ' 14K 16K 20K ' 10K ^ 6691 11K -" 17? -4204 5192 '1357 x 2810 2471

1224 2454 4303 , isl f li17 ' 4791 29271212 1751

^s X/ , . ..... \ 1508 l 3500 3149 J 1 333\ f \vr/

' 3956 5976 3325

49/1- — -

1358 1058 1091 178 934 1025 1352 2158 2990 4218 4785 5617 6693 6939 8220

261^ 187 ®\^ m j 1 316 s 7M^9541047^, 2999 7603 5055 4619

1 - 1746 "" 2743 — 3191 5363 s* 4740 8728 -~~Ss' ^ -—^ l i Sl 2249 S 4063 ^ 7015 4614 3727 l 7733 1EK

1696 f 4682 s 8759 8891 \ 3020 S6BO fi /III/ .^ l \ l l l 13/3304 9299 -^JOK f 5539 ^ 4376 8901

' l in RW* t K* linn

Interpretation

Apparent Resistivity(ohm-m)

629 V 1305

\\ \1055 \ 2054 — 1031

1986 -^"1354 11181136 1087"^ 630^ ^ 1443 3247 "~ 2730 ^ 'TOO ; l'l75' ' 2772' '6256 ^10*' 6013 7782 6530

13K

n=1

0=2

0=3

0=4

0=5

Interpretation

Total Chargeability 6t^ (wV/V) F ilter 4' 9

5+00 S 4+00 S 3+OOS 2+00 S 1-KJO S 0+00 1+00 N 2+OQN——l———*———h-3+00 N 4+00 N 5+OON 6+00 N 7+00 N B+OC N 9+OON 10+00 N 11+00 H 12+00 N 15+00 N 14+00 N 15+00 N

2.2 IA; 5 .3 4,7 B. 4 ^ 5.4 v 11

4,5 \ 6.8 6.7\v 10 J 9 ,3 \ 11

,2 8 B.7 9 ,5 9.2 B.5 8 .1 7 6.7 5 .8 4.5 5.7 5.2 5.7 6 .3 9 12 1 6 17 11 9.1 7.4 4.9 3.6 2.9 2.7

10 __ 10 -^ 7.J 6 .S 7 .9 - 4.9 ; 7.1 8 .8

2.1 1.5 1.6 2.2 !.7 4.B 4.9 5.6 5.3 4,8

0=5

8.4 6.4 7,7

9,9 12 \ B.2 6.5

11 11 V. 8.5-^ 7,6'

7. l S .J^ B.I 6.1 5.2 N 8.9—- 7.B 8.4 9.2"- 12 11 ''3.1

19.sss--0.27 1.5 -4,1^- 3.4 3.5^—2.5 3.7 3.3 1.5 1,5 V2.7 -4.3 2.4 ^ 5.1 N 3.1 j 4 .9 4.5 4.3 , 3.5

.17 l 3.7 f^~l.\ 3 .5 \ 0.

-0.45 l 4 .2 4.9 l 7 .!

3 \ O.U -1.B 2.5 4.1 6.5 6.9 \ 4,8 5.4248.6 6.4 -4.S 0.89 ^ 3.8 3.7

^ f .. ^ .

4.8^^4 4,1 2.4 N 6.3 ''•' 18 12 9.3 12 12 '—- 15

Interpretation

Total Chargeability Filter (mV/V)

0=1

89 1 .2 \2.5-^ 1.21 y 4,9 5 .5 5.2 5.4 4.4 4,2 4 .8 0=2

0=3

0=4

0 = 5

0=61.9 1.B 3.4 3 .4 - O.S8 0 .58 0 .97 ' 3.7 5 .2 5 .4 5.! '6.4

Interpretation

Metal Factor(IP/Res)* 1000

6+OOS 5+OOS 4+00 S 3+OOS 2+00 S 1+OOS 0+00 1+00 N 2+po^l l 3+00 N 4+00 N 5+OON——l———i———h- 6+OON 7+00 N B+OON J+OON 10+00 N 11+00 N 12+00 N 13+OON 14+00 N 15+00 N

pjlter 1,4 0.86 0.79 0.76 1.4 1.1 1,2 0.95 0,82 0,69 0.65 0.50 0.51 0.48 0.49 0.45 0.54 0.70 0.85 1.4 2.2 3 7.1 14 H 5.6 4.3 3.7 2.7 2,8 2,7 5.1 3.1 1.8 1,3 1.1 1.1 1.4 1.1 0.87 0.85 0.65

(1 = 1 2.1 l

0=2 1.2 ; o0=3 0=4 0=5 0=6

-'"'^"AN2 \0^l x\.81 ' s 0 .39 0.93 Vl.sV 0,78 N.1.

0.67 s. 2 v 0C 63 x x 1.4 0,72 - 0.78 0.64 0.60 - 0.37 C.46 O.J2 0.53 0.42 0,67 0.95 O.Sfl - 079 1.4 1.4__/i 4.5 s' - - \ .'^ t ' ^ ^ '' - ^ ^ l ( "sv/aff

0.67 , ' 0.41 \\1.i 1.3J-^2.9 ff l ' :2 ^ 0.81 C,52 0.79 0.52 0,27 ' 0.60 " 0.45 0,45 0.53 0,6

'.92 /' 0.31 t 0 .72 0.92

0,37 s 0 .64 .' 0,87 l.l'

0.78 ~ 0.76 /1

0.90 0,93

l 0.52 0,71 ~ 0,65 0.44 0.36 \ 0.66 ' 0.42 0,44

\ 2 \" 0.75 ' - 0.70 . . 0.68 0.63 0.57 0.56 0.40 , 0.83 l 0.34 0.54 " 0.\ v\\v ' " -. x v - ^ \ x - '1.1 \ \ 2.1 N 11 0.52 t , 1~\ 0.65 0.56 0,70 0.63 \ 0.39 0.52 , 0.41 0.46 \ V-' l V . ' C \ '^ ' \ " -

. .-' l V . '

1.3 1.6^* 0.73

i 2.4 6.1^ -^ 13 i 5.4 3.9 3.7 3,3——-3.3 5.3 1.6 i 0 .53 , - 0.35 - 0.76"" ~~28 , 31/1 -0.29

(.6 1,00 — 0.92

, 0.50 ^ 0.52 5.35^ ^ 0.35 - O.B6 /s 3,6^ 7.3 s^- 16 __- 14 8.9 V 0.87 ^ 3 .3 3.7V 6.5 \ 0,67 - 0,92 ' -0.55 Jj.1.9

3.7i\D.19 -2.4 ' 1.5-^ 0.88 - ' 0.74 ~ 0.77 l.*/ 0.9S 0.460.4- 0.29 , ,I^A 0 .20 //, 4.1 6.8 /4.4vT^8.5

au ^l.(.—— 1.6^ 2.9 .L -3.9 0.93 — 0.73 0.60 0.3.9/- 2.7. \5.8 5,5

1.1 - 0.54 0.68 0.73 0.56 0.30 v 0.72 ~ 0.37 0,21 0.58 ' 1.2 ' 2.1 ' 4.9 4.9 M.3 2^- 3.8 x 7.5' '18 ^5.8 5.9^^3,1 1,3—- 0,82 0.50 ~ 0.35 v 0.59 C.50 0.90 0.74 O,!

Filter

0.45 0=2

0=3

0=4

(1=5

(1=6

Interpretation

Metal Factor (IP/Res)* 1000

Line 2800 E

Dipole-Dipole ArrayQ no o

Filter

* * ~* * *

* * * * a ^ 50 M

Vplot point

IWI1FERPRETAT1GIW

Strong increase in polarization

Well defined increase in polarization

Poorly defined polarization increase

Low resistivity feUU-I C t ine, WeakHigh resistivity feature. , * -t A Strbng, Moderate, Weak

MAP SPECIFICATIONS Resistivity: Logarithmic Contours (1, 1.5, 2, 3, 5, 7.5, 10,..)

Chargeability: Unear ContourB (every 2mVyY) Metal Factor Logarithmic Contours (1, 1.5, 2, 3, 5, 7.5, 10,,.)

SURVEY SPECIFICATIONSInstrumentat'on: Rx = IRIS ELREC-10, Tx = PHOENIX IFT-1

Input Waveform: 0.125 Hz, 50% duty cycle

?, 103

50 O" ———

Scale 1:500050 100 150 200 250 300

-J L.

(metres)

MUSTANG MINERALS CORP.INDUCED POLARIZATION SURVEY

RIVER VALLEY PGM PROPERTYNorth Grid, McWilltams &L D ona Twps . , ON

Survey Date: April, 2001 Drawing Number: QG-1 67-IP-DP-L'ne 2800 E-50m

QUANTSC GEOSCISffCB INC,Geosoft Software tor the Earth Sciences - Processed by KBfOi/OS/OSJ


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