BUTLER LAKE PROPERTY - geologyontario.mndmf.gov.on.ca€¦ · 3.0 1998 EXPLORATION 3.1 Line Cutting...

42A08SW2009 2.20306 BLACK 010

Geophysical Report of Work

on

BUTLER LAKE PROPERTYBlack Township

District of Timiskaming Northeast Ontario

" 0

for

DRIVER RESOURCES INC.

October 15, 1998 Geoserve Canada Inc. Richard Daigle

1.0 SUMMARY

Driver Resources completed a preliminary investigation on their claims in Black Township, Larder

Lake Mining Division, Northeast Ontario.

Geoserve Canada Inc. of South Porcupine, ON, was retained to do line cutting, magnetics, and

induced polarization surveys. The objective of the work is an attempt to locate geological settings

favourable for base metal occurrences.

The results of the 1998 surveys encourage further work. A geological survey is recommended

before testing the targets discussed here-in.

(1)

42A08SW2009 2.20306

TABLE OF CONTENTS

BLACK 010C

1.0 Summary 2.0 Introduction 3.0 1998 Exploration

3. l Line Cutting3.2 Total Field Magnetics

3.2.1 Procedure3.2.2 Results

3.3 Induced Polarization Survey3.3.1 Procedure3.3.2 Results

4.0 Conclusion 5.0 Certification 6.0 Equipment Specification 8c

Theories

O)(3)(4)(4)(5) (5) (5) (5)(5)(6)(7)(8)

(9)

PLANS, FIGURES AND SECTIONS

Plan l Base MapPlan 2 1998 Magnetics SurveyPlan 3 Induced Polarization SurveyPlan 4 Induced Polarization Survey

Figure l Location MapFigure 2 Butler Lake Grid

Sections (l5) 1:5000

(Pocket)

(2) (4)

(Pocket)

(O

Figure 1ONTARIO MINING DIVISIONS

PROPERTY BEING REPORTED ON

N

(2)

2.0 INTRODUCTION

Geoserve Canada Inc., of South Porcupine, ON was retained by Driver Resources Inc., of Vancouver, B. C., to do work on their Butler Lake Property. The property being reported on comprises eight (8) contiguous claims in Black Township, Larder Lake Mining Division, Northeast Ontario. Geoserve Canada Inc. completed line cutting and geophysical surveys from August 25, 1998 to September 15, 1998 covering approximately 200 hectares west of Butler Lake. Butler Lake is approximately 30 km north of Kirkland Lake, ON, along Highway 101.

The objective of the 1998 work is to locate geological targets favourable for base metal occurrences. A preliminary geological investigation completed in August 1998 by Mr. R. Barber located base metal showings along with precious metal occurrences on the property being reported on. Mr. Barber emphasises two main showings which are on present claims 1227946 and 1227924. The reader is asked to refer to the Preliminary Report, R. Barber, August 1998 for a description of commodities located on the property being reported on.

(3)

3.0 1998 EXPLORATION

3.1 Line Cutting

Geoserve's line cutting crews established a baseline on the Black Township Claims on August 25,

1998. The local grid co-ordinate 0+00/0+00 on claim 1227923 is at UTM location

551512E/5354289N. From this start point, the baseline was cut 1550 m with an Azimuth of N135 0T (SE). Crews then cut the baseline NW (Az. N315 0T) up to 200N then offset the baseline 100 m SW.

Crews also offset the baseline at 600N. This was necessary to keep the survey lines on the claims. Lines were then turned 900 off the baseline at 100 metre intervals. From 100N to 300S lines were

established at 50 m intervals. The entire grid was picketed at 25 metres.

FIGURE 2BUTLER LAKE GRID

BLACK TOWNSHIP

(4)

3.2 TOTAL FIELD MAGNETICS

3.2.1 Procedure

Geoserve's geophysical crews read the total field magnetics on September 8 and 9,1998. Crews

used the GSM-19 Overhauser magnetometers for base station and mobile units. All surveyed lines

were read at a 12.5 m interval. The base station location was along the access road near Butler

Lake. The diurnal drift was monitored at 30 second intervals.

DATA: blkmag.xyz

RANGE: 55989 nT to 66146 nT

MEAN: 57797 nT

STATIONS READ: 1682 @ 12.5 metres

3.2.2 Results

The 1998 Ground Magnetics Survey is presented here-in on Plan 2. The data from file BLKMAG was

translated to UTM coordinates using;

XO:: 55103 IE YO: 5353408 -a^ 45 0

The magnetics infers gabbroic rocks bisecting the claims centrally located. The intensities over these

rocks range from 57500nT to near 62000nT. The lowest magnetic background which flanks north

with values below 57400 nT are believed to represent felsic volcanics . The magnetic intensities from

57600 nT to 57900 nT that flank south of the said gabbroic rocks delineates underlaying cobalt group

sediments.

3.3 INDUCED POLARIZATION SURVEY

3.3.1 Procedure

Geoserve's geophysical crews read the time domain induced polarization survey from September 9

to September 15, 1998. Crews read fifteen cross-lines with the Pole Dipole Array, with 3=50111 and

levels n^ to n=6. The Androtex TDR-6 receiver was used in conjunction with the Scintrex TSQ-3.

(5)

3.3.2 Results

The results are presented on fifteen l :5000 sections here-in

The survey results are also presented on Plan maps to simplify interpretation.

Chargeabilities Plan 3

The apparent chargeabilities show two significant areas of highs values beyond 20mVA^ seen on

claim 1227946 which is referred to as the "MAIN SHOWING" by Mr. R. Barber. The contours

follow a strike of approximately N315 0T. The core of chargeability highs flanks just east of a pit

located on the property.

Another area of significant high IP effects flanks north of the magnetically inferred gabbro and bisects

claims 1227924 and 1227923. This zone is open (undefined) to the north. This area is referred to

as the north zone. A N315 0T strike is favoured.

Other aberrative responses is seen on the southern traverses but are believed to be cultruly influenced

(eg: bedrock highs).

Resistivity Plan 4

The apparent resistivities which are presented in ohms/50 meters are strongly influenced by the

surficial geology. The lowest resistivities bisect the grid near and along line 400S where a creek bed

is present. The south part of the survey shows a narrow high resistivity trending across lines 1400S

to 1000S. This low occurs in conjunction with a weak chargeability high. There is a narrow

resistivity high which parallels this low from line 1400S to 900S between l SOW and 200W (local grid

coordinate). North of the creek at 400S a large resistive underlying unit occurs in the area of the said

gabbroic rocks. The author suspects that the area delineated by the resistivity high is influenced by

the surficial geology.

(6)

4.0 CONCLUSION

The high chargeabilities are reflecting the mapped sulfide mineralization. If assay results returned

from Swastika Laboratories are favourable than the drilling of the EP highs is warranted.

The author recommends a regional study of the geology. The property warrants additional

exploration. A geological survey would help delineate mineralized zones located on the claims being

reported on.

Respectfully submitted for approval,

Q v/

Date

Richard Daigle

(7)

5.0 CERTIFICATION

I Richard J Daigle residing at 900 Government Road, Porcupine, ON,certiry that;

1. This is my 19th year of practice in mining exploration.

2. I am registered with the Ontario Association of Certified Technologist.

3. I am presently owner operator of Geoserve Canada Inc.

4. I was employed by MC Exploration Services Inc., of Timmins, ON, as geophysical evaluator from 1992 to 1997.

5. I accomplished geophysical contracts (IP, HLEM, TFM, SP) and property assessments in Eastern Canada, 1987 to 1992.

6. I accomplished geophysical contracts in northeastern ON, 1985-87.

7. I was employed as a Geophysicist Assistant/Senior Technician for Kidd Creek Mines under the supervision of Mr. D. Londry, 1981-85.

8. I experienced Max-Min (HLEM) surveys/interpretations under the supervision of Mr. J. Betz, 1979-81.

9. I received an Electronic Technologist Certificate in 1979.

10. I have no direct interest in the property reported on, or the company worked for.

R. JTBaigle

(8)

GEM Systems Advanced Magnetometers GSM-19 V 4.0GEN Systems Inc52 Uest Beaver Creek Road, Unit 14Richmond Hill, Ontario Phone; (905) 764- 8008Canada, L4B-1L9 Fax ; (905) 764- 9329

Instrument Description The sensor is a dual coil type designed to reduce noise and improve gradient tolerance. The coils are electrostatically shielded and contain a proton rich liquid in a pyrex bottle, which also acts as an RF resonator. The sensor cable is coaxial, typically RG-58/U, up to 100m long. The staff is made of strong aluminum tubing sections. This construction allows for a selection of sensor elevations above the ground during surveys. For best precision the full staff length should be used. Recommended sensor separation in gradiometer mode is one staff section, although two or three section separations are sometimes used for maximum sensitivity. The console contains all the electronic circuitry. It has a sixteen key keyboard, a 4x20 character alphanumeric display, and sensor and power input/ output connectors. The keyboard also serves as an ON-OFF switch. The power input/output connector also serves as a RS232 input/output and optionally as analog output and contact closure triggering input. The keyboard front panel, and connectors are sealed (can operate under rainy conditions) The charger has two levels of charging, full and trickle, switching automatically from one to another. Input is normally 110V 50/60HZ. Optionally, 12V DC can be provided. The all-metal housing of the console guarantees excellent EM protection.

Instrument SpecificationsResolution 0.01 nT, magnetic field and gradientAccuracy 0.20 nT over operating rangeRange 20,000 to 120,000 nT automatic tuning, requiring initial setupGradient Tolerance over 10,000 nT/mOperating Interval 3 seconds minimum, faster optional. Reading initiated from keyboard, externaltrigger, or carriage return via RS-232Input/Output 6 pin weatherproof connectorsPower Requirements 12V, 200mA peak, 30mA standby, 300mA peak with GradiometerPower Source Internal 12V, 1.9Ah sealed lead-acid battery standard, external source optional.Battery Charger Input; 110/ 220 VAC, 50/60HZ and/or 12VDC

Output; 12V dual level charging Operating Ranges Temperatures; -40 0 C to -I-60 0 C

Battery Voltages; 10.0 V min to 15.0V maxHumidity; up to 9096 relative, non condensing

Storage Temperature -50"C to -l-65"C Dimensions Console; 223 X 69 X 240 cm

Sensor Staff; 4 x 450mm sectionsSensor; 170 x 71 mm diameterWeight; Console 2.1Kg Staff 0.9Kg Sensors; I.iKg

(9)

Magnetic SurveyTheory; e

The magnetic method is based on measuring alteration in the shape and magnitude of the earth's naturally occurring magnetic field caused by changes in the magnetization of the rocks in the earth. These changes in magnetization are due mainly to the presence of the magnetic minerals, of which the most common is magnetite, and to a lesser extent ilmenite, pyrrhotite, and some less common minerals. Magnetic anomalies in the earth's

filed are caused by changes in two types of magnetization; (l) Induced, caused by the magnetic field being altered and enhanced by increases in the magnetic susceptibility of the rocks, which is a function of the concentration of the magnetic minerals. (2) Remanent magnetism is independent of the earth's magnetic field, and is the permanent magnetization of the magnetic particles (magnetite, etc..) in the rocks. This is created when these particles orient themselves parallel to the ambient field when cooling. This magnetization may not be in the same direction as the present earth's field, due to changes in the orientation of the rock or the field. The unit of measurement (variations in intensity) is commonly known as the Gamma which is eauivalent to the nanotesla (nT).

Method;

The magnetometer, GSM-19 with an Overhauser sensor measures the Total Magnetic Field (TFM) perpendicular to the earth's field (horizontal position in the polar region). The unit has no moving parts, produces an absolute and relatively high resolution measurement of the field and displays the measurement on a digital lighted display and is recorded (to memory). Initially, the tuning of the instrument should agree with the nominal value of the magnetic field for each particular area. The Overhauser procession magnetometer collected the data with a 0.2 nanoTesla accuracy. The operator read each and every line at a 12.5 m interval with the sensor attached to the top of three (56cm) aluminum tubing sections. The readings were corrected for changes in the earth's magnetic field (diurnal drift) with a similar GSM-19 magnetometer, >>base station<< which automatically read and stored the readings at every 30 seconds. The data from both units was then downloaded to PC and base corrected values were computed.

(10)

Induced Polarization'Androtex TDR~6; The TDR-6 induced polarization receiver is a highly cost- effective instrument for the detailed measurements of IP effects and apparent resistivity phenomenon. Up to six dipoles can be measured simultaneously, thus increasing production. A wide input voltage range, up to 30V, simplifies surveys over the narrow shallow conductors of large resistivity contrast. Input signal indicators are provided for each dipole. All data are displayed on a 2x16 character display LCD module and any selected parameters con be monitored on a separate analogue meter for noise evaluation during the stacking/averaging. Although the TDR- 6 receiver is automatic it allows full control and communications with the operator at all times during measurements. Since the input signal synchronizes the receiver at each cycle, the transmitter timing stability is not critical and any standard time domain transmitter can be used. Data are stored in the internal memory with a capacity of up to 2 100 readings (450 stations). The data format is directly compatible with Geosoft without the necessity of an instrument conversion program.Features•Wide input signal range 'Automatic self-potential cancellation•Staking/averaging of Vp and M for high measurement accuracy in noisy environments•High rejection of power line interference 'Continuity resistance test 'Switch selectable delay and integration time 'Multiwindow chargeability measurements•Digital output for data logger 'Six channel input provided 'Compatible with standard time domain transmitters 'Alpha-numeric LCD display 'Audio indicator for automatic SP compensation 'Portable Specifications•Dipole nl to n6 simultaneously 'Input Impedance 10 megohm•Input Voltage (Vp) range:100uV to 30 Volts (automatic),

accuracy: .25*, resolution:lOpV.•Self Potential (SP) range:±2V, accuracy: J.%, Automatic compensation ±1•Chargeability (M) range:SOOmV/V,accuracy:.25%, resolution:.ImV/V•Automatic Stacking 2 to 32 cycles•Delay Time programmable•Integration Time programmable for each gate (10 gates)•Total Chargeability Time During integration time of all gates•Synchronization Signal programmable from channel l to 6•Filtering power lines:dual notch 60/lSOHz or 50/lSOHz,

lOOdB, other:Anti-alias, RF and spike rejection.•Internal Test Vp=lV / M=30mV/V•Ground resistance test O to 200 Kohm•Transmitting Time 1/2,4 and 8 sec pulse duration, ON/OFF. 'Digital Display Two line 16 alphanumeric LCD.•Analogue Meters Six-monitoring input signal and course

resistance testing.•Controls Push button reset, toggle start-stop, rotary

Rs-in-test, rotary (data scroll) display, rotary (data scroll) Dipole, keypad 16 key 4x4.

•Memory Capacity 2700 readings, 450 stations (nl to n6).•Data Output serial I/O RS-232 (programmable baud rate),

Geosoft compatible output format.•Temperature Range Operating:-30 0 to 4-50 0 C, storage -40 0 to 4-60 0 C.•Power Supply Four l.5V D cells.•Dimensions 31x16x29 cm•Weight 6.5 kg (14.31bs)

(11)

Scintrex TSQ-3;The Motor-Generator set consists of a reliable Briggs and Stratton four stroke engine, coupled to a brushless permanent magnet alternator. The transmitter design employs solid-state components both for power switching and control circuits. Output waveforms and frequencies are selectable; square wave continuous for frequency domain and square wave interrupted for time domain. The programmer is crystal controlled for high stability. While care still must be taken when working with high voltages, the TSQ-3 features overload, underload and thermal protection for maximum safety. Stabilization circuitry ensures that the output current (lg) is automatically controlled to within i.1% for up to 20*^ external load or ±10^ input voltage variations. Voltage, current and circuit resistance are presented on a LED digital display. The system functions as follows; The motor turn turns the generator (alternator) which produces SOOHz, three phase, 230VAC. This energy is transformed upwards according to a front panel voltage setting in a large transformer housed in the TSQ-3. The resulting AC is then rectified is a rectifier bridge. Commutator switches then control the DC voltage output according to the waveform and frequency selected.Specifications•Output Power 3000 VA maximum•Output Voltages 300,400,500,600,750,900,1050,1200,1350 S 1500V•Output Current 10 amperes maximum•Output Current Stability Automatic controlled to within t.1% for up to

20% external load variation or up to ±10* input voltage variation.

•Stabilization Protection (Over-range) High Voltage shuts offautomatically if the control range exceeds 20!?;.

•Digital Display Light emitting diodes permit display up to 1999with variable decimal point; switch selectable

to read input voltage, output current, external circuit resistance, dual current range, switch

selectable.•Current Reading Resolution 10mA on coarse range (1-lOA) and 1mA on fine

range (0-2A).•Time Domain Cycle t:t:t:t; ON:OFF:ON:OFF:automatic•Polarity Change Each 2t, automatic.•Pulse Duration Standard tsl,2,,4, 8, 16 and 32 seconds, optional•Stability Crystal controlled to better than .l 1?; with

external clock option better than 20ppm over operating temperature range.

•Efficiency .78•Operating Temperature Range; -30 0 C to H-50 0 C•Overload Protection Automatic shut-off at 3000VA.•Underload Protection Automatic shut-off at current below 85mA.•Thermal Protection Automatic shut-off at internal temp, of 85 0 C.•Dimensions 350cm x 530cm x 320cm (transmitter).•Motor Briggs and Stratton, four stroke 8HP.•Alternator Permanent magnet type, SOOHz, three phase

230VAC at full load. 'Output Power 3000 VA maximum.•Dimensions 520cm x 715cm x 560cm (generator assembly).•Weight Transmitter;25.Okg, Generator Assembly 72.5kg.Output DC interrupted squarewave used for survey.

*-t-* 1 "-t-*-T

f1 1 i'1 II L

t= 2 seconds, ON Se OFF time. Total duty Cycle Used; 8 seconds.(12)

IP MethodThe phenomena of Induced Polarization (IP) was reported as early as 1920 by Schlumberger. The IP survey technique allows a variety of arrays (which all have advantages and disadvantages) and reads two separate elements;(1)The chargeability or IP effect (M) and Apparent Resistivity. The IP technique is useful for detecting sulphide bodies and is also useful as a structural mapping tool. The IP effect is the measurement of the residual voltage in rocks that remains after the interception of a primary voltage. It includes many types of dipolar charge distributions set up by the passage of current through consolidated or unconsolidated rocks. Among the causes are concentration polarization and electrokinetic effects in rocks containing electronic conductors such as metallic sulphides and graphite. The term overvoltage applies to secondary voltages set up by a current in the earth which decays when it is interrupted. These secondary effects are measure by a receiver via potential electrodes. The current flow is actually maintained by charged ions in the solutions. The IP effect is created when this ionic current flow is converted to electronic current flow at the surface of metallic minerals (or some clays, and platy silicates). The IP method is generally used for prospecting low grade ( or disseminated) sulphide ores where metallic particles, sulfides in particular, give an anomalous response. Barren rock (with certain exceptions) gives a low response. In practice, IP is measured in one or two ways;(1) In a pure form, a steady current of some seconds (nominally 2 seconds) is passed and abruptly interrupted. The slowly decaying transient voltage existing in the ground are measured after interruption. This is known as the time domain method. The factor Vs/ Vp is the integrated product for a specified time, and several readings are averaged (suppressing noise and coupling effects). The resultant chargeability, M is essentially an unitless value but it is usually represented in mV/V. The second method entails a comparison of the apparent resistivity using sinusoidal alternating currents of 2 frequencies within the normal range of 0.1 to 10.0 ops.. The factor used to represent the IP effect by this frequency domain method is the percent frequency effect (PFE) and is defined by (R1-R2)/RlxlOO% where RI and R2 are the apparent resistivities at the low and high frequencies. Use and Iiinii.iiati.onsThe effective depth of penetration of any IP survey is a function of the resistivity of the surface layer('s) with respect to the resistivity of the lower layer. All arrays have different effects from this resistivity contrast, some are less affected than others. When the surface layer is 0.01 of the lower layer, the effective penetration is very poor hence the term masking. Masking occurs most often in areas of thick clay cover. The size of the target therefore becomes important when detection is desirous under a conductive surface layer. The frequency domain methods are the most adversely affected by masking as inductive coupling can be much greater than the response.Standard Definitions of ChargeabilityThe IP parameter, chargeability (M) varies with time. For practical reasons the entire decay curve is not sampled. Instead the secondary voltage is sampled one or more times at various intervals. Because the secondary voltage is received at extremely low levels in many prospecting situations, measurements of its amplitude at any given time is extremely susceptible to noise. Therefore, the secondary voltage is usually integrated for a period of time called a gate. Thus, if the noise has a zero mean, the integration will tend to cancel the noise. The Newmount M Factor is a standard time domain IP parameter. The gate delay, of 80 mSecorids (used by the TDR-6) was chosen to allow time for normal electromagnetic effects and capacitive coupling effects between the transmitter and receiver to attenuate so that the secondary voltage consists only of the IP decay voltage.The TDR-6 total integration time of 1580 milliseconds (gate) is divided into ten individual gates. The time-constant of the IP dispersion curve, Cole-Cole dispersion (W H Pelton, 1977), obtained from the ten individual gates (windows) is directly related to the physical size of the metallic particles. This data is available at the clients request since all of the obtained field data is archived (downloaded) to computer.

(13)

Ontario n ^ ~.Northern Developmentand MinosDeclaration of Assessment Work Performed on fining Land

Mlnlna Act Subsection 65(2) and 66(3), R.S.O. 1990

Transaction Number (office use)

W or 80. cc -^3Assessment Files Research Imaging

^sections 65(2) and 66(3) of the Mining Act. Under section 8 of the Mining Act, this *nt work and correspond with the mining land holder. Questions about this collection Tent and Mines. 3rd Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 6B5.

42A08SW2009 2.20306 BLACK 900

instructions: - For work performed on Crown Lands before recording a claim, use form 0240. - Please type or print in ink.

1. Recorded holders) (Attach a list if necessary)Name ^p

D&iu&z. K&foutc&j' /A'c .Address

(JrtWouUt*L ft, (L U CCL /er/Name

Address

—————————————————————————— 6 ——— —— ——

Client Number

Telephone Number3 -J /O/

Fax Number ~* .

Client Number

Telephone Number

Fax Number

2. Type of work performed: Check (*0 and report on only ONE of the following groups for this declaration.

^^Geotechnical: prospecting, surveys, " assays and work under section 18 (regs) D Physical: drilling stripping,

trenching and associated assays D Rehabilitation

Work Type

A/AJeCuTTl

Dates Wot* From Performed

Global Positioning Sys

i*C , r/NftiC st/twcy ^ i .P Sotêy,

ji5 of ffi? TO 25" /^ /97,p

Day | Month | Year Day | Month | Year

em Data (K available) Township/Area o * A i^ "7"^ ÎÂc/C. X ^-/rMorO-PlanNumber

Office Use

Commodity

Total S Value of Work Claimed o?C , *4O8

NTS Reference

Mining Division \ Afr L J( f

Resident Geologist , District t-K i f r^lo fid. r\G k-Q

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

/Cd*Telephone Number

~7o rAddress /~\

r*iFax Number

Name

Address.*

Telephone Numb* r

Fax Number

Name Telephone Number

Address Fax Number

4. Certification by Recorded Holder or Agentl, ____/T-?/^"^ C'/^.O^______, do hereby certify that l have personal knowledge of the facts set forth in

{Print Nftnw)

this Dedaration 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.

Signature of Recorded Holder or Agent Date*3f-ixNu

02.

ents Address(CO

..Telephone Number' Fax Number

0241 (03/97)

b. Work to be recorded and cJistriDuted. vvorx can oniy Lie assgnt-d to Claims tnai are contiguous (aujom/ngy iu i,,t n,....,.j land where work was performed, at the time work was performed. A map showing the contiguous link must accompany this form.

Mining Claim Number. Or Ifwork was done on other eligible mining land, show In this

column the location number indicated on the claim map.

eg

•oeg

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

1.

TB 7827

1234587

1234568

L- /2.Z.79/5"L- izzrfti-iL- ILISl^ZJ—^./2,7-79Z,3t -i^î0} **yL-IZ3-~) ci2,^~Z.-/Z.L79 ISL,— y 2. 2— ~̂ J ^v

Column Totals

Number of Claim Units. For other mining land, Ut* hectares.

16 ha

12

2

5111

1i\l

y 2.

Valin of work performed on this claim or other mining land.

526,825

0

S 8,892

y p 0 ^2 "*

9 -7S2. 00

y /sYtt.**f Z Hl?.^sS Z J t f. 25~^ 5//. fo

J>^ l3> Li1 o0g /sffZ.^

*Zo,yoX' 0*

Value of work applied to this Claim.

N/A

124,000

54,000

-0-

-d-

t^-

-0 ——

^~

-e--t^-•^-~

-fr-

Value of work assigned to other mining claims,

524,000

0

0

-eS2-

-0-

CJ

-C3—TS-

-o--0-^,

-r3—

Bank. Value of work to be distributed at s future date

52.825

0

54,892- . f~f ^ O' m tj fy '-^*J

tv o . o*J^.-

^ 75-2,0*

K /,yfi-^S 2t ^?. ̂ ^f Z,lff.* Sy s*//.^"XZ3V9. 00

gr X^/-?,00

VZo,^.0*

/W 1 JC& C^/tfcO/v . do hereby certify that the above work credits are eliaible 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 RecordedJ-lolder 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:

S-TTCredits 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 D 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):

CDNote: If you have not indicated how youfjcredits are to be deleted, credits will be cut back from the Bank first,

followed by option number 2 if necessary.

For Office Use OnlyReceived Stamp

0241 (03*87)

Deemed Approved Date

Date Approved

Date Notification Sent

Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

r ' \

i?) Ontario Ministry ofNorthern Developmentand Mines

Statement of Costs for Assessment Credit

Transaction Number (office use)

Personal information collected on this form Is obtained under the authority of subsection 6 (1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining Act, this Information Is a public record. This information will be used to review the assessment work and correspond wtth the mining land holder. Questions about this collection should be directed to a Provincial Mining Recorder, Ministry of Northern Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury Ontario P3E 6B5.

Work Type

Li/ê. O OT7./-6StTK. Suêv\,p s****

Units of workDepending on the type of work, list the number of hours/days worked, metres of drilling, kilometres of grid line, number of samples, etc.

Z } k^2 , IU" l r"vi

//. l k^

Associated Costs (e.g. supplies, mobilization and demobilization).

Transportation Costs

Food and Lodging Costs

Cost Per Unit of work

*35-o, 00

* //S.* 0

9 ?f*. 0 0

•l

-C O

Total Value of Assessment Work

Total Cost

* 7, 3 SO . 00

r z, y/f. 00

*/* . 6fr. "*

' '" 'r '-^

*ê,V<?S. 0

Calculations of Filing Discounts:

1. Work filed within two years of performance is claimed at 1000Xo of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at 50 0Xo of the Total

Value of Assessment Work. If this situation applies to your claims, use the calculation below:

TOTAL VALUE OF ASSESSMENT WORK x 0.50 = Total $ value of worked claimed.

\lote:Work older than 5 years is not eligible for credit.A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.

Certification verifying costs:

, do hereby certify, that the amounts shown are as accurate as may reasonably

lands indicated on the accompanying

l am authorized to make this certification.

(please print full name))e determined and the costs were incurred while conducting assessment work on the lands indicated on the accompanying

Declaration of Work form as(recorded holder, agent, or state company position wHh signing authority)

212(03*7)

?-S^ 'fMT ;

Ministry ofNorthern Developmentand Mines

Ministers du DeVeloppement du Nord et des Mines

J .MB 21, 2000

DRIVER RESOURCES INC.117H FLOOR, 308 WEST HASTINGS STREETBOX 10VANCOUVER, B.C. V6G-2X4

OntarioGeoscience Assessment Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

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

Visitourwebsite at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm

L - ir Sir or Madam:

S ' ject: Transaction N umber(s):

Submission Number: 2 .20306

StatusW0080.00223 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.

L . .3 status for o transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any s::ps you C3n take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the A rêssment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day l\ :~e. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment C;; Z 3 w ithin this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in S. ::ion #6 cf the Declaration of Assessment work form.

F: vase note —y revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by theresponse date on the summary.

l: ou have rny questions regarding this correspondence, please contact BRUCE GATES by e-mail atb ce gates j}rrJ:n.gov.on.ca or by telephone at (705) 670-5856.

'-f3 s incereiy,

O

f. 3INAL CI3,\ED BYf we B. Be ete.;uA :ing Supt, visor, Geoscience Assessment OfficeK' i ng Lands Section

Correspondence ID: 14990 Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2.20306

Date Correspondence Sent: June 21, 2000 AssessorBRUCE GATES

Transaction Number

W0080.00223

Section:14 Geophysical IP 14 Geophysical MAG

First ClaimNumber

1227915

Township(s) l Area(s)

BLACK

Status

Approval

Approval Date

June 21,2000

Correspondence to:Resident Geologist Kirkland Lake, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):Mike Caron PORCUPINE, ONTARIO

DRIVER RESOURCES INC. VANCOUVER, B.C.

Page: 1Correspondence ID: 14990

REFERENCESAREAS WITHDRAWN FROM D ISPQSTION

M.R.O. - MINING RIGHTS ONLY S.R.O. - SURFACE RIGHTS ONLY M.+S. - MINING AND SURFACE RIGHTS

Description Order Mo. Date Disposition File

NO'I'hS:

froniaqe o n Butler Lake mithdrown from d isposition fat proposed s ummer resort development, J uly 6 , 1986t-ILK I6458G

THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON- SULf WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEHFON

NOTICr OF rORFSf'RY AC IIVI l YTHIS I QWNSHIP l AHKA FALLS W ITHIN T'MK

WATA61 AG MAMAGKMKNT UWIT

AND MAYflf SUBJECT TO KURrSTRY GYRATIONS. l'UK MNR UNIT F ORFS I'KH F OR TlliR ARKA CAN t^K

A l': p Q B OX 1^9SWASTIKA, ON'L POK 110

Playfair Twp.

7 /^~1222640 t

12D7783207781

22769

1225679

ia**XJW^ -v ^ l BH209B1137193 Kn3 **6

: x... .

\ i I2Q252O

l 1226907

1225788

1225289

Lee Twp

LEGEND

HIGHWAY AND ROUTE No.

OTHER ROADSTRAILS -

SURVEYED LINESTOWNSHIPS, BASE LINES, ETC. -

LOTS, MINING CLAIMS, PARCELS, ETC.

UNSURVEYED LINESLOT LINES -PARCEL BOUNDARYMINING CLAIMS ETC. ~

RAILWAY AND RIGHT OF WAY -1"

UTILITY LINES

NON-PERENNIAL STREAM --

FLOODING OR FLOODING RIGHTSSUBDIVISION OR COMPOSITE PLAN

RESERVATIONS

ORIGINAL SHORELINE

MARSH OR MUSKEG

MINES

TRAVERSE MONUMENT

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENTPATENT SURFACE St MINING RIGHTS

, SURFACE RIGHTS ONLY

" , MINING RIGHTS ONLY

LEASE, SURFACE 8, MINING RIGHTS

" , SURFACE RIGHTS ONLY

" , MINING RIGHTS ONLY

LICENCE OF OCCUPATION

ORDER-IN-COUNCIL RESERVATION

CANCELLED

SAND*GRAVEL

SYMBOL

Se o

Ei W

oc0© 0

LAND USE PERMITS FOR COMMERCIAL TOURISM, OUTPOST CAWIPSNOTE [MINING RIGHTS IN PARCELS PATENTED P RIQRTO MAY S. 1Q13,

VESTED IN ORIGINAL PATENTEE BY THE P JB LI C LANDS ACT, R .S.O. 1370, CHAP. SSO, SEC. 63, BUBSEC 1.

SCALE: 1 INCH = 40 CHAINS

MFT

Mf T

40OO imw aoao

1QDOO KMI

TOWNSHIP

BLACKM M R ADMINISTRATIVE DISTRICT

KIRKLAND LAKEMINING DIVISION

LARDER LAKELAND TITLES/ REGISTRY DIVISION

COCHRANEMinistryot LandNatural Management

Resources BranchOntario

Qiti JANUARY 19H3

DEC AHCrtVtD JULY i 5/57,

G-3197

42AOSSW2009 2.20306 BLACK 200

55IOOOE- 552000E

5354000N

orH CN

im

CM S[QOD oft

5353000N

bblOUOb

SCALE100 0.0 100

metres

200 300

Driver Resources Inc.Base Map

Butler lake Project Black Claim GroupBlack Township Larder Lake Mining Division

District of Timiskaming

Geose/ve Canada Inc tyyw Oct 19.1998

ASTRO

Magnetic Declination

11.5'W

LEGENDTotal Field Magnetics Plan

57000 nTs Base Subtracted Contours

Level 1; 25nT from 58000 to 58500nTs Level 2; 50nT from 57000 to 59000nTs Level 3; 500nT from 56000 to 65000nTs

PLAN 2Driver Resources Inc.

1*98 MagtwUcs Sunny Butler tali. Project Black Claim GroupBase Station Location; Access road

BkdiTiwitHp UnMrUktMMnaOvMon

INSTRUMENTS TerraPlus GSM-19 Overhauser 42A08SW2009 2.20306

\ - \ -\ N v \ '

LEGENDApparent Chargeability Plan

1 mV/V Contour Interval

Filtered Product n1 to 0=4 levels

Pole Dipole Array 3=50™

PLANS

Driver Resources me

BuUer lak* ProJ*ct

Black Claim Oroop

Androtex TDR-6 Receiver

Scintrex TSQ-3 Transmitter42AOSSW2Q09 2.20306

DQDDDD Apparent Resistivity Plan

Filtered Product n1 to n^4 levels

Contours25ohm750m from O to 2000ohms

lOOohm/SOm from O to lOOOOohms SOOohm/SOm from O to 45000ohms

Driver Resources meMund PdulzaOoo Suvw

Butler lakt Project

Black Claim GroupPole Dipole Array3=50171 Stock TowuMp LVKfcrUli* Urine DMtfon

Androtex TDR-6 Receiver Scintrex TSQ-3 Transmitter

2^ 34K- 2.1

IP RES l MF

6.1-4 17KJ 1.

3J 0. i i

Ji.\

MF l RES

.1 L17K (.6.1

l l l l L l l l l l l l l l l l l l l l l————i————l————l————l————l———— .0

Top o

Interpretation

7-KBW &HXIW WWW—l-

1-tQO W CWX)

Chargeability mV/V

filter 11=1{1=2

0=3

FIB*

0=5

0=6

17 " filter

H^3 U ^H^l^n 13 Qjll

14 x 13 '13 ^ I S ' 16 15 ^ 13 14 "' 6 .4

Interpretation

7+00 W 6*OOW

filter

Resistivity ohm/meters

Topo

Interpretation

Chargeability mV/V

Interpretation


L 200NPole-Dipole Array

no

l___l

0=501^•b'

plot point

Filter* n1

* * n2* * * n3

* * * * n4

Cont. Intervals Profiles Resistivity ; 500 ohm/meter — — — ~ Chargeability ; 1.0 mV/V Metal Factor ; 1 % ——————

INSTRUMENTSBRGM Elerec 6, Time Domain Receiver

1760mSec Total Integration Time, BQrnS Delay. ^ ( 80+80+80+80+160+160+160+320+320+320 ) mSec

Huntec M2, 7.5Kw Transmitter BSecond Total Duty Cycle, 2Sec On/Off Time.

INTERPRETATIONLow EffectPoorly Chargeable mV/V, IP effectLow Apparent Resistivity, rho

J Moderately Low Effect

Moderately High Effect

High EffectGood Chargeability mV/V, IP effectHigh Apparent Resistivity, rho

Scale 1:500050 O 50 100 150 200 250 300J*^*^^^*

(meters)

Butler Lake ProjectInduced Polarization Survey

Black Township, NE QntrioLarder Lake Mining Division

Geoserve Canada inc Od 1998.42A08SW2009 2.20306 BLACK 250

10- 26ie 2-3-,

IP RES i MF

5,1 J 13l 1.1.

OJ o OJ

J26K

MF i RES

.1.1 L13K

Lo

Topo

Interpretation H———————l———.———l———————t-

5+QOW 4+QOW 3+OOW 2+00 W

Chargeability mV/V

fiiter " 1 2 " 10n-1 12 xH j 1 2 ,j 8 ^

17=2 l? 13 V 7 9.1'———*'———8.9-^^9.9

(1=3 11 -"" 10 —— 10 —— w it ^=411=5 (1=6

| X .X' ^ "S. \ ^^11 ' 13 "-"^ 13 It ' 13 ~~^ 13 14 14 15 - 14 14

Interpretation

filter 35K J6K IBK 21K 20K

3+00*-i——,——i——-~ 2+00 W 1+00 W 0+00 1+00 E1SK 11K 9509 S735 7064 W50 Z2K


IP

L5.1

L.O

Topo

Interpretation

Chargeability mV/V

Interpretation


L 100NPole-Dipole Array

a na

*—CD-i

plot point

Filter* n1

* * n2* * * n3

* * * * n4

Cent. Intervals Profiles Resistfvity ; 500 ohm/meter — — — — Chargeability ,- 1.0 mV/V Metal Factor ; 1 * ——————


1760mSec Total Intengration Time, 80mS Delay.MT= ( 80+60+804^0+160+160+160+320+320+320 ) mSec

Huntec M2, 7.5Kw Tronsmitter BSecond Total Dirty Cycle, 2Sec On/Off Time.

INTERPRETATION

50

Low EffectPoorly Chargeable mV/V, IP effectLow Apparent Resistivity, rho

Moderately Low Effect


High EffectGood Chargeability rnV/V, IP effectHigh Apparent Resistivity, rho

Scale 1 :500050 100 1 50 200 25^ 300

jyjMHHM^^

(meters)


Block Township, NE QntrioLarder Lake Mining Division

Geoserve Canada he Get 1998.42A08SW2009 2.20306 BLACK 260

IP l

7.7.

17K-

RES l MF

8723J 12.

Topo

Interpretation

Chargeability

Interpretation


Oj Oj

.24

MF f RES

.12 L8723

15

TIP

.7.7

Lo LO

-H———'———t- -t———————l———i———l———i———l———————l———i———l———,———t———.———I-

MOW | 7^Wt 6-KMW 5*00 Wfilter ! -J 10 '* 1 7 21 21 1 S 1Z l i!

A ——t *i l . . T t * j f r 1** . (It 99 . *^w -97 *. . W .....M.IU. tt \ 1 1^ ft

4iOOW 3KJOW

0 = 1 5.4

ns2

0=3

0=4

0=5

11=8

8.9 1.8

t

l.j

2+00*•t——'——t—'8.9 11

VtOOW [MX) 2-KME11 11 12 14 I S K It IB 20 1 9 1C filter

o.i s.i B.} e,* v 11 n ?.s^ ^"Xx- u \*sSJ' l i

^.8 7.1 7,* 'i-^J^ \^ (1 r^~^~ '2 i \̂ ^^^ /•~~

^\ i '* V\ 7-7 l *- s f *-5 M\\ tt u ; 13 "/'il "~^ "x^ ̂

' 4.1~-^ B.z S.I i.? - 9.1 t.B" \ f^T^ W tt -^ 11 ' ^ 17 -^

5+OOW VKPW OtO)fj]êr 1426 57IJ 1W 17* 20K

5*15 asiillK ̂ -6067

0=2

(1=4

(1=5 0=6

1* 2W 11H 1W BK 19K \7K IK 16K W 19K 14K filter

Topo

Interpretation

Chargeability mV/V

Interpretation


L 0+00Pole-Dipole Array

na

Vplot point

Filter* n1

* * n2* * * n3

* * * * n4

ProfilesCoat. IntervalsResistivity ; 500 ohm/meter Chargeability ; 1.0 mV/V Metal Factor ; 1 X


1760mSec Total integration Time, 80mS Delay.MT- { 80+80+80+80+160+160+160+320+320+320 ) mSec


INTERPRETATIONLow Effect

————— Poorly Chargeable mV/V, I P effect Low Apparent Resistivity, rho

j ^ J Moderately Low Effect

\ ~ ) Moderately High Effect

l High Effect———— Good Chargeability rnV/V, IP effect

High Apparent Resistivity, rho

Scale 1:500050 O 50 100 150 200 250 300~- ~ sassssa

(meters)



Geoserve Canada inc Oct 1998.42A08SW2009 2.20306 BLACK 270

MF f RES rIP

9757J 1.1. .1.1 '9757 r

O- OJ O- ———l———l l l l l l l I.... l l l- l ...j l l l l l 11 I...,L——-L..... J l l l l l l l— --L- .1.1 l l l l .0 LO

Top o

Interpretation

Chargeability mV/V

Interpretation

Resistivityohm/meters

noow t t moo9.5 B.B 8.6

1400 E

filter

8*00 V) 7+00 W &KXJW 5403W 4+OOW 3KWW

filter

Topo

Interpretation

Chargeability mV/V

Interpretation


L 100SPole-Dipole Array

no

J±L

plot point

Filter* n1

* * n.2* * * n3

* * * * n4

ProfilesCont. IntervalsResistivity ; 500 ohm/meter Chargeability ; 1.0 mV/V Metal Factor ; 1 X


1760mSec Total Intergration Time, BOmS Delay.MT= ( 80+80+80+80+160+160+160+320+320+320 ) mSec

Huntec M2, 7.5Kw Transmitter SSecond Total Duty Cycle, 2Sec On/Off Time.

INTERPRETATION

50





Scale 1:500050 100 150 200 250 300^^•••c

(meters)



Geoserve Canada he Oct 1998.42A08SW2009 2.20306 BLACK 280

1CL, 27K 1.2.,

IP' RES'! W

5.2. 14KJ . 59.

O- Oj O- ——i——i——l——s t i——L-.....I j j——i——i.. .1 i .1 i i i i i i i——i i i i i i i .0 LO

-27K

MF I RES

...59 LHK

r IP

.5.2

Topo

Interpretation

6+00 Wi —— i 5+00 W 4400 W 3+00 W 2+pOW^ 1+QOW 0+00 1+03 E ]

filter 1 4 7 - 4 5- 7 *- s 5.4 5 .9 6.4 6 .6 6.8 7.5 8 .7 5.Z 3.9 filter

Chargeability mV/V

0=3

11=4

0=5

11=6

2.9. 4.7 ( i 8.5__-D.I 7.3 6 .9 6.6, - 8.4 ^ 6.! \ 4.4* 3.7 [1 = 1

,aj,i n=2' 4 0=3

0=4

0=5 0=6

\v X\ iV-46.4\ 8.1 7.2 1 .1 7 .4 ^ 8.9

4.75 v 6.3 6.5 ^ 7.2 7.9.^ 7.7-^^.8/1

l 7.7 / 8.5 \ 6.8 —— 6.3s, '..1-J^r4 N 2.9 ^^ 4.4 5.1^^7,3 6.8 '^'2.6

Interpretation H————r————l————————l————i————l————i————l————r————l-


Topo

interpretation

Chargeability mV/V

Interpretation

7W 7778 90M MW 7835 7SBB 6151 W4 M12

Resistivity

ohm/meters


na

Vplot point

niter* n1

* * n2* * * n3

* * * * n4

Cont. Intervals Profiles Resistivity ; 500 ohm/meter — — — ~ Chargeability ; 1.0 mVA Metal Factor ; 1 JE ——————

INSTRUMENTSBRGM Derec 6, Time Domain Receiver

1760mSec Total Integration Time, 80mS Delay. T~ ( 80+80+80+80+160+160+160+320+320+320 ) mSec


INTERPRETATION

50



Moderately H igh Effect


Scale 1:500050 100 150 200 250 300 t^^^m^K

(meters)


Black Township, NE Ontrio Larder Lake Mining Division

Geoserve Canada he Get 1998.42A08SW2009 2.20306 BLACK 290

5.2., 2859- 19. i——i——i——i——i——i——i——i——r~~i——i——i——i——i——i i——i——i—i—i——i——i——i——t——i——i

1430J 9.5-

O- ___l l- -...L-., l l L l l l l l l l———l———l l l l l l l l l l l l ..J l l l l0-1

Topo

Interpretation

ChargeabilitymV/V

Interpretation


^2859 ..5.2Jl

MF [RES l

-9.5 L14-30 1.2.6

l l

.o L

l————r————l

440DW JKHW 2-KB W HOD W 0+CO HjME 2+OQE JrfOOE

2.3 2.1 1. 1 2 -2 2,i 2.9 2.9

1 1.2 1.1—^Z.l 2.7 -^

1.2 1.3 1.3 ( . ttj) 1 .7 1.7

1.5 1.5 1.5 1.9 1.8

2.6 2.3 3.2 [1=6

-H——'——1~

4iOOW 2-(00 W-I————————l————.————l————————h-

t-KJOE1703 3899 2041 2592 2845 2893 271* 1389 2019 1680 1385 1046 953 747 664 618 filter

0=1 283 w (J!®MKy 61574S-—— 657 570 462 ——467 —— 448-^545 761 505 1020 573 5K 633 , 4 )0 n^1

0=2 5948 llj534 — 1514 "~" ISIZ^T 1577 — 1381 ---J033 —— 946 -^JJ' 782 639 546 660 S07 683 546 11=2

2509 — 2470 •^~!m~^. 259D -~. 2249 -— 1B92 ~ 1516 ^1160 ~~ 1026 ~^!75 676 770 541 -' 625 0=3

1179 V 3W3 — 3464 4092 — 3609 ^.JOzT^- 23J4 2049 ^ 1496 ^ 1298 1010 722 723 512 0=4 \\\ (x—0=5

0=6M1457 U 4362 -^j[300 516S v^ 4443

1760 \' S2!4 — 5189 1590?— 5737 ^ 4701 - 3456^ 2596

1010 722 723 512

2424 ^ 1621 "1482 1024 618 505

'1085 843 405

.0 uO

Topo

Interpretation

Chargeability mV/V

Interpretation

Resistivityohm/rneters

42A08SW2009 2.20306 BLACK 300


no

plot point

Filter* n1

* * n2* * * n3

* * * * n4

Cant. IntervalsResistivity ; 500 ohm/meter Chargeability; 1.0 Metal Factor ; 1 X

Profiles

INSTRUMENTSBRGM Qerec 6, Time Domain Receiver

1760mSec Total Intercretion Time, 8QmS Delay. T^ ( 80+80+80+80+160+160+160+320+320+320 J mSec

Huntec M2, 7.5Kw Transmitter 8Second Total Duty Cycle, 2Sec On/Off Time.

INTERPRETATIONLow EffectPoorly Chargeable rnV/V. IP effectLow Apparent Resistivity, rho

50

Moderateiy Low Effect



Scale 1:500050 100 150 200 250 300

~i L.(meters)

BaUer Lake Projectinduced Polarization Survey

Black Township, NE OntrioLarder Lake Mining Division

Geoserve Canada Inc Oct 1998.

o, o- o.,

IP

OJ

RES l MF

Topo

Interpretation

ChargeabilitymV/V

Interpretation


oJ 0.

oJ nil i

filter

11=2

r.0

MF i RES

.0 Lo

.o Lo

filter

-9.*

3*0010

filter filter

11=2

482 1719

IP

LO

LO

Topo

Interpretation

Chargeability mV/V

interpretation

Resistivityohm/rneters


naSJ m

0=50)4 l

o f*l o rq

•s' plot point

Filter* n1

* * n2* * * n3

* * * * n4

Cont. Intervals Profiles Resistivity ; 500 ohm/meter — — — -- Chargeability ; 1.0 mV/V Metal Factor : 1 % ——————


1760mSec Total Intergration Time, BOmS Delay.MT= ( 80+80+80+80+160+160+160+320+320+320 ) mSec

Huntec M2, 7. 5Kw Transmitter BSecond Total Duty Cycle, 2Sec On/Off Time.

INTERPRETATION

50

Low EffectPoorly Chargeable mV/V, IP effectLow Apparent Resistivity, cho



High EffectGood Chargeability rrtV/V. IP effectHigh Apparent Resistivity, rho

Scale 1:500050 100 150 200 250 300

J I- (meters)

Butler Lake Projectinduced Polarization Survey



3.5.. 3739., 1.7

1 1

IP' RES] MF

11.8. 1 870J . 84.

i

l

J

lOJ oJ 0.

Topo

Interpretation

filter 4

(1=1 4

11=2Chargeability ^3

mV/V n M,

[1=6

Interpretation

filter *n-1 a

n=2

11=3 Resistivity ^4ohm/meters n--5

0=6

v /\\ y ^^\ x--.^^- v^Ss. XN:^

v^-x---.^^*^^ ^* ^ ^ '

i i i i i i i t i i i i i i i i i i t t i

2+00 W 1+00 W 0+00 1+00 E 2+00 E 3+00 E1.8 3.2 2.5 2.9 2.8 2.2 1.4 1.3 1.1 .70 .70 .80

.3 -s. 2- 9 --^ l-' 3' 3 3- 6 ~~4.6-^-2.8 3.3— 2.4 1 1 1 4.7 j l 1 .3 2 2.8 2.2^-^1.6 .90—— 1.2 1 .20 .70

' t N ( S 2.1 —— .3.9 1.9 2.8 \ 1.6 1 .10 .M .70 -M

3.2 ^M.5 12.3 2.3\ 5.3 .90 .40 .M .70

2.8 ' 1.2 1.3 1.7 - .80 - 1.3 -- - .70

2+00 W 1+00 W 0+00 1+00 E 2+00 E 3+00 E099 3854 3030 3534 2856 2047 131S 1113 7S7 558 46* 490

J45 ^^ 2WO Z580 0 'OH 1020 (321 468 361 28S 24! 398

5436^^1876 i 4034 — 3778^^1552 638^ 571 ^M3~^ 456 337 440

1338 2343 V 4397 — 48S6^V\ 977 __ 1031 .591 S5S 4S3 __ 442

1372 ^ 2248 \X 5278^/. 3078 C; 15)6 1094 879 630 618

857?*|fe 2642 — 3262 /^4663^ 1347 1053 627 727

19Sl' "1753 ''4791 433^ 1437 ^949 721

••lil

.1.7 ^3739 -3.5

1

MF r RES "IP

1.84 f.1870 .1.8

l

.0 Lo LO

Topo

Interpretation

filter

n-2

n-3 Chargeability[1=4 mVA

n=5

^=6

Interpretation

filter

[1=3 ^4 Resistivitynz5 ohm/meters

IliJHIII

L 700SPoie-Dipole Array

a na a

\ / ' a soM

plot point

niter* n1

* * n2 * * * n3

* * * * n4

Cont. Intervals Profiles Resistivity ; 500 ohm/meter — — — —Chargeabili^ ; 1.0 mV/VMetal Factor ; 1 H ——————

INSTRUMENTS BRGM Berec 6, Time Domain Receiver

1760mSec Total Intergration Time, 80mS Delay. MT= { 80+80+80+BO+1 60+160+160+320+320+320 ) mSec

Huntec M2, 7. 5Kw Transmitter BSecond Total Duty Cyde, 2Sec On/Off Time.

INTERPRETATIONl 1 Low Effect

Poorly Chargeable mV/V, IP effect Low Apparent Resistivity, rho

j | Moderately Low Effect

\ \ Moderately High Effect

\ \ H igh EffectGood Chargeability mV/V, IP effect High Apparent Resistivity, rho

Scale 1:500050 0 50 100 150 200 250 300

(meters)



Geoserve Canada Inc Oct 1998,42A08SW2009 2.20306 BLACK 320

2.4,, 5870 1.5n

IP RES] MF

l

2935 ' . 77.

Topo

Interpretation

Chargeability mV/v

Interpretation


O J O J I l l ] l l l r .0 LO

H———i———l———i———l-

filter

r^2 n-3

n=4

3.7

fitter

[1=4 n=5

- 42AOSSW2009 2.20306

2+00 W 1+OOW CHOP 1-tOOE

2.9 3.3 2.8 Z.7 2.5 2.3 2.2 2.5 1.7

3.3 V 2.6 2.6 1.6 1.1

3.5 \ 2.5 2.5 l 1.2 s 2.1

filter

n=2

n=5

2^00 W 1+OOW CWM

Topo

Interpretation

ChargeabilitymV/V

Interpretation


BLACK 330

L 800SPole-Dfpole Array

na

0=501*1

Vplot point

Filter* n1

* * n2* * * n3

* * * * n4

Con t. Intervals Profiles Resistivity ; 500 ohm/meter — — — — Chargeability ; 1.0 mVA Metal Factor ; 1 X ——————


1760mSec Total Integration Time, 80mS Delay. N ( 80+80+80+80+160+160+160+320+320+320 ) mSec


INTERPRETATION1 Low Effect

Poorly Chargeable mV/V, IP effect Low Apparent Resistivity, rho

50




Scale 1 :500050 100 150 200 250 300

-l """"C (meters)




9035-, 1.8.,

IP"1 REST MF' l

1.5. 4517.J . 88-

TopO

Interpretation

Chargeability

ohm/meters

Oj

i r i i

0. ———l———l———l- -L- J..-....1 .J———l———l———l———l———l———L.

n 1.8

MF NES

..88 [.4517

-O In

2-tOOW VKB W 0*00 1-KJOE

2-KJOW 1-KJOW 0*00 (-KM E 2*00 E

filter11=1

11=2

(1=3

0=6

12K 1 2K 1110

n=3

0=4

3983 -

IP

1.5

Topo

Chargeability


L 900SPole-DIpole Array

na a-H———————l

0=50^

plot point

niter* n1

* * n2* * * n3

* * t * n4

Coat. Intervals Profiles Resistivity ; 500 ohm/meter — — — — Chargeability ; 1.0 mV/V Metal Factor ; 1 SE ——————


1760mSec Total Integration Time, BOmS Delay. T= ( 80+80+80+80+160+160+160+320+320+320 ) mSec


INTERPRETATION

50




High EffectGood Chargeability rnV/V, IP effectHigh Apparent Resistivity, rho

Scale 1:500050 100 150 200 250 300

-l C (meters)


Black Township, NE OntrioLarder Lake Mining DivisionGeoserve Canada Inc Oct 1 998 .

42A08SW2009 2.20306 BLACK 340,

3.6., 7345n 1 .7.,

RES l MF

1.8. 3673.] . 84.

Topo

Interpretation

ChargeabilitymV/V

Interpretation


OJ OJL-j.

p7345 r3.6

MF f RES

i

..84 [.3673 .1.8

.0 Lo

3+OOW

filter 4-' " 2-6 " 3-8H00W ~*~—i—~~,—

4 3.5

0+00

4.6 4.2

n=1 2.3._J.e.0=2 5~

n=3

0=4

0=5

0=6

- U ^^.7^3 v^ ) 3 , M 3

i.2N^2.3—-'1.1---2.6x 3.4 3.4, 2.2 y 4,1^*^.3.5 X^

6 - 3 4^L-L^" j A 1 .4.1\J.3 1.4 t 5-1^3,2

^8^^*-*J5-'-8 ^ 3-7 4.6^^-5^^-4,^,5.4 ——

1?fC^^\ /T^^^

filter "" filterS7S

Topo

Interpretation

ChargeabilitymV/V

Interpretation



ai————i- na

i l

Profiles

Vplot point

niter* n1

* * n.2* * * n3

* * * * n4

Coni. IntervalsResistivity ; 500 ohm/meter Chargeability ; 1 .0 Metal Factor ; 1 X


1760mSec Total Intergration Time, 80mS Delay.MT= ( 80+80+80+80+160+160+160+320+320+320 ) mSec

Huntec M2, 7 . 5Kw Transmitter BSecond Total Duty Cycle, 2Sec On/Off Time.

INTERPRETATION

50





Scale 1:500050 100 150 200 250 300

•l. '"•••S(meters)



Geoserve Canada Inc Oct 1998.42A08SW2009 2.20306 BLACK 350

L1^ 5606,, 2.3.,

IP

2.1.

RESl MF

2803.) 1.1-

Topo

Interpretation

ChargeabilitymV/V

Interpretation


oJ o.

5606

MF T RES

.1.1 (-2803 -2.1

j_ .o Lo

l———i———t-

4+QOW JtOOW 2-KXJW 1400 W CWMfilter 4' 7 s'3 5" 6 5" 6 4' S 3" 8 J'8 3" B 3' 2

2 v 4.3 ——— 4.4 i 2.1

\

2.4\\__- V " X " \1.9 2.7^ 3.4\

——' 2 .3 3.1 3.7

V-2.3 2.9 3.7 tf"4.1 >|/X 2.8-^ 3.6.—— 1 ,1 ^S^ t,*

1 g. t 7.4^5^7^3.1 3.6 3.1 4*6^.3.7 C 5:

B.3 A.B 7.3- S^'^l.T 3.7 ' 4.

3.6 3.7 3.3 2.9 2.9 f|| ter

3.6 3.4 2.3 y 1.6 1.6 n=1

3.4 \ 2.4 2.5 \ 3.3 3.1 2.3 2.2 ^=2

2.7) 3.6 3.2 3.3

"5.5

n=3

n=6

filterr^1

11=2

[1=3 [1=4

[1=5 n^6

4400W—.—i——.—99 2346 1884

3+QOW —i——i——i——i—2376 4197

2XBW——i———i———I-

7019 7644

HOOW——l———i———h-

5401 3B93

0+00—l——l——l——l—4170 3138

4349 v 3404 , 2651 i 762 s 1 386 , . 3777 im 1 !K ,__ 11K MSS 5152 i 3495 , 5395 ^- 2956 s\\ ///f ^-^ / ^///!itiilllllii\(((^^mm\ L ( i/ Â\\\\C4377 J 274J f ! 2S4 1354 . 2638 (U 7533 lUl 1 t3K )) 10K ffiffl 3604 V 4K2 ^ 5947 m 2 I1J//y y x -*^ S i \\\\\\\wiH\i\Uu\ niiiaim\m\\ i \ •xS—•r ;\\\\\

1H)OE | 2-KX1E^ m Ta22 f j | ter

?P iS.aSB ^ 1850 I2S^^

Z.flZ "^ 2283 ^ 1*22f

2527

1203

23W ^^2651 2651

2804 3004 2870

m 3604 v 4K2 ^ 5947 l 2112 ' 2283IJIl\^ ^ V^r^^Jl\\j65O3g53~~-420Zzr 3825 O 1993^, 2\v\\ /T:——' \V^

1 5321 \ \ 3117 2729 -^3368 \ 1 947

S4 / 4137 l MJ1 — 91M , 11My /ni//^ ^x,/ 4137 y 2021 — 2124 x/S/JII ( \\4067 S 2520 v IBM 207!

n"1

n=2

[1=3

11=4

[1=5

0=6

.-O

Topo

Interpretation

ChargeabilitymV/V

Interpretation



na

0=50^

plot point

Rlter* n1

* * n2* * * n3

* * * * n4

Cant, intervals Profiles Resistivity ; 500 ohm/meter — — — — Chargeability ; 1.0 mV/V Metal Factor ; 1 X ——————


1760mSec Total Integration Time, 80mS Delay. :* ( 80+80+80+80+160+160+160+320+320+320 ) mSec


INTERPRETATION| ~| Low Effect

Poorly Chargeable rnV/V, IP effect Low Apparent Resistivity, rho

| | Moderately Low Effect

| ~~| Moderately High Effect

| | High EffectGood Chargeability mV/V, IP effect High Apparent Resistivity, rho

Scale 1:500050 O 50 100 150 200 250 300

BKLJ-JLJui (meters)


Black Township, NE QntrioLarder Lake Mining DivisionGeoserve Canada Inc Oct 1998.

42A08SW2009 2.20306 BLACK 360

3.9- 4773 2.U

IP

1.9J

RESl MF

2386" 1.

OJ OJ 0. l__

Topo

Interpretation

Chargeability mV/V

interpretation

Resistivity

ohm/meters

.2.1 4773 -3.9

ll

MF f RES

.1 '2386 L1.9

5*00* 4+OOW 3+OOW———l———i———h- 2*OOW| 1+00 W 0+00 1+00 E

filter 4.8 5-2 5.3 5.3 4.5 1.7 1.4 3.5 3.6 I.I 2.8 2.7 2.1

2tpOE |

19 filter1.6 1.4 2..1 2.5 2,9_ 2.3 !-4 2.4 2.8 , ! .6 1.6 n=1

.2.2, 1.5 \ 2.3 2.9 3.5 \ '1.9^ 2.4 2.5 2-'N. 1' 5 " S2

2.3 2.3 2.2 n=3

2.1 l 3.9-——4—^.3,8 \2.7 2.5 ( 1.5 [1=4

U-3 4.5 "3.9 ""3^ 2.6 (1=5

3.3 "^ 4.4 4.4 4".2 J.1 [1=6?5 7 'TT~^ 7.3 6.7 4.7*

filter

0 = 1

0=2

15=3

11=4 (1=5

15 = 6

5+OOW6462 t341

4+OOW

18 2772

5+OQW

2001 2043

2+00*

3512 5162

1+00 W

6506 5959

0+00

5032 4530

1+00 E

3314 2859

8068 — 95i4

7239

95i4 JR. 3609 3658 //.919- 1157 ^4888 /5886y 8349 l i 5404 ,v 3222•^*™\ r̂ ^( - - \m\\ ( /s/// \\\\\\^r^— 7757 \\\ 2470 ^ \W 1 654 -~ 1487 Â 5309 f 8295 — 7923 \ 5369 — 4837^-w)\\\\\\\r l ^^ \\m\\\\i i ( ^\\v^^\\em ^ 5094 \ \ 1 291 l 2145 2129 — 206S * S485 S\ S160 l 76E5 -~ S435 | ....-^^/y/KvJ i ,—^ x^^j^:^ "^CNMl l v - , . xiw7 -^ 17M "^. ieiQ \ viV) vnti - iMt\ ^K AIM -^ iHAt ^ 35 i t 5.]^} \ 42JJ J252///in \ \ i t \ ^

S, (U& . 4668/3516 2929tsy/S J / 7 S f

2+00 E |

2058 1 627 fi | ter

8S2 n=1

3tcH l l \ fa\ l .iFU L \G3 —— AJD9 Vi* WOO-^y/KvJ v '—— vtai--,4257 Z* 2769 ^ 1649 \ 2532 2726 -^ 2400 ^ 6189^ ^XN \ v \ \^^s^ vx ,

2546 ^3263 \ 1874 2908 ^3002 X 2270 ^49H^ 8213i \\ V \ ̂ x. ' f—~~2901 3180 x 1676 2736 2642 1

\ 4218

1886 ^ 2145 ^ s 896

\2378 2340 \1296 [1=2

3765 \ 2228 2624 ^ \\ V

T319 ^-

n=3

— 5547 W27

IP

ii. ,o Lo LO

Topo

Interpretation

ChargeabilitymV/V

Interpretation



na

0=50^

Vplot point

nitern1 n2

* * ** * * *

Coni. Intervals Profiles Resistivity ; 500 ohm/meter — — — — Chargeability ; 1.0 mVA Metal Factor ; 1 X ——————


1760mSec Total Intergration Time, SOmS Delay. ^ ( 80+80+80+80+160+160+160+320+320+320 ) mSec


INTERPRETATION| Low Effect

Poorly Chargeable mV/V, IP effect Low Apparent Resistivity, rtio

1 Moderately Low Effect

l Moderately High Effect

l High Effect———— Good Chargeability mV/V, IP effect

High Apparent Resistivity, rho

Scale 1 :500050 O 50 1 00 1 50 200 250 300

-l " i ""C(meters)

Batier Lake ProjectInduced Polarization Survey


Geoserve Canada Inc Oct 1998.42AOSSW2009 2.20306 BLACK 370

3.8- 13K

IP' RES'!

1.9 j

MF

6508J .88.

cu oj oJ

Topo

Interpretation

ChargeabilitymV/V

Interpretation

Resistivity

ohm/meters

\ r \

l i i

..1.8 ..13K -3.8

MF

..88 L6508

WWW WWW 2+00 W 1+00 W 1X00 MX) E

filter filter3.4 3.4 3.4 3.3 3.1 2.9

2.9 2.8 ___ 2.9

5.2 5.2 5."!- 4.6 4.5 1'' 3-3 3.4 3.2 3.4

5.6 5.3 5.3 5.4 5.3 5.3 2.3 —— 2.1 3,7 3.

n=5 S.7 5.8^——6.1——6.3 ^~6

6.5 6.8 -^ 7^ "*- 6.9

... V \ ' ' - '

6.7 6 6.3 - 4.!\ 3.2 3.3 * 4.8 4.2

6+OOW 5+OOW 4400 W

filter

frOOW 2+03 W

2135

745,

24SJ

1634

1850

1813 ~ 1980 s 2906l

2856 \ 1425 l\

TS r 1813 ~ 1980 s 2906R\\\ ^ l f S \

2794 3130

2412

\ \. ^, 1874 \ 289

I - 4584^ 2965 ^ 1859^

2894 3193

2763 2B22

IP

ul-S

.0 LO i-O

Topo

Interpretation

Chargeability

Interpretation


42A08SW2009 2.20306 BLACK 3 g Q

L 1300SPole-DIpole Array

na

I±L0=50^

•B' plot point

Filter* n1

* * n2 * * * n3

* * * n4

Cont. Intervals Profiles Resistivity ; 500 ohm/meter — — — — Chargeability ; 1.0 mV/V Metal Factor ; 1 X ——————


1760mSec Total Integration Time, 80mS Dekiy.MT= ( 80+80+80+80+160+160+160+320+320+320 } mSec

Huntec M2, 7.5K* Transmitter BSecond Total Duty Cycle, 2Sec On/Off Time.

INTERPRETATION

50

Lo* EffectPoorly Chargeable mV/V, IP effectLow Apparent Resistivity, rho



High EffectGood Chargeability rnV/V, IP effectHigh Apparent Rssistivity, rho

Scale 1:500050 1OO 150 200 250 300

J J Li (meters)




3.7- 10K 1 .2.,

IP RES] MF

1.8 J 5229' .59.

O J O J O J l i i i

. . . . .: . . . t. .:. . .

i i i i i i i t

.1.2 - 10K

MF ["RES

.59 '5229

-3.7

IP

L1.8

Topo

Interpretation

5+OOW 4+OOW 3+OOW 2+00 W4.5 *.4 5 4.7 4.6 4.7 4.1 3.7 3

1+00 W 0+003.4 3.6 3.3 2.!

±1___J.6jU~S 3-7

Chargeability mV/V

(1=2

(1=4

n=5

0=6

4.3 4 .5 -3.3 3 .8 3.2-^^2.7 2.3 \ 1.7 ^3.2 3.4 C (.-.20

4.2 4.7 4.2 4.2——-4,

4,5 X 5.8 ^""-4.9---- 5.1 .. 4.2

5^ 5.8 6.5^^^ 5.B 5.5 V \3-5^ 4.9 "^N.3.5 \ 2.1

6.5 6.2 x 7.2 6.! 6.8 "^ 4.3 4.8 ^ 3.3

filter

^=2

n=5

n=6

Interpretation

5+03W 4+OOW 3+OOW 1+OOW 0*00

7196 filter


i i l Lo Lo LO

Topo

Interpretation

ChargeabilitymV/V

interpretation

2872 V 2035

33lT "^2759 2348 2611-N\ x r3871 v 2475 1923

3253 3221 l 1995 1845 C 3110

2154 ~- 2608 2302 1498 1868



na

Vplot point

Filter

* * *

n1 n2 n3 n4

ProfilesCont. IntervalsResistivity ; 500 ohm/meter Chargeability ; 1.0 Metal Factor ; 1 JE


1760mSec Total Integration Time, 80mS Delay.- ( 80+80+80+80+160+160+160+320+320+320 ) mSec


INTERPRETATIONLow Effect

————— Poorly Chargeable mV/V, IP effect Low Apparent Resistivity, rho

| | Moderately Low Effect

| ~| Moderately High Effect

| | High EffectGood Chargeability mV/V, IP effect High Apparent Resistivity, rho

Scale 1:500050 O 50 100 150 200 250 300

-J ^(meters)



Geoserve Canada Inc Oct 1998.42A08SW2009 2.20306 BLACK 390

Date post:	06-Oct-2020
Category:	Documents
Upload:	others
View:	1 times
Download:	0 times

BUTLER LAKE PROPERTY - geologyontario.mndmf.gov.on.ca€¦ · 3.0 1998 EXPLORATION 3.1 Line Cutting...

Documents