rpt of work on the spanride prop...loodb, other .-anti-alias, rf and spike rejection. internal test...

42A03SW2001 2.18442 ENGLISH

REPORT OF WORK010

on the 2 . A

SPANRIDE PROPERTYEnglish and Beemer Townships, ON.

Porcupine Mining Division

for

STARFIRE MINERALS INC.

April 17, 1998 Geoserve Canada Inc. Rodne

RECEIVEDMAY 1 2

ASSESSMENT OFFICE

42A03SW2001 2.18442 ENGLISH 010C

1.0 SUMMARY

A time domain induced polarization survey was completed on the Spanride Property in

September, 1997. Several areas of coincident chargeability and resistivity anomalies

were located by the survey, three of which warrant further work. The survey also helped

to define certain structural and lithological features of the property. Diamond drilling

of the IP anomalies is recommended.

i.o 2.03.0 4.0

5.0 6.0 7.0

4.14.2

TABLE OF CONTENTSSummary Introduction Previous Work 1997 IP Survey Procedure ResultsConclusion and Recommendations Certificate of Qualifications Equipment Specifications Si-

Survey Theories

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(DC)

(4)(4)(5)(6)(7)

LIST OF PLANS, SECTIONS AND FIGURES

Figure l Base Map (reduced)Figure 2 Location MapPlan l 1:5000 Base MapPlan 2 1:5000 Chargeability PlanPlan 3 1:5000 Resistivity PlanSection L2200S 1:5000 IP TraverseSection L2000S 1:5000 IP TraverseSection L1800S 1:5000 IP TraverseSection L1600S 1:5000 IP TraverseSection L1400S 1:5000 IP TraverseSection L1200S 1:5000 IP TraverseSection L1000S 1:5000 IP TraverseSection L200S 1:5000 IP TraverseSection L200N 1:5000 IP TraverseSection L400N 1:5000 IP TraverseSection L600N 1:5000 IP TraverseSection L800N 1:5000 IP TraverseSection L1000N 1:5000 IP TraverseSection L1200N 1:5000 IP Traverse

(2)(3) (Pocket)

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2.0 INTRODUCTION

Starfire Minerals Inc explored their Spanride Property in 1997 with a time domain

induced polarization survey. The property is comprised of seventeen (17) contiguous

claims (96 units) in Beemer and English Townships, Porcupine Mining Division,

northeastern Ontario. The property is roughly fifty kilometers south of Timmins, ON,

in the Peterlong Lake area. The property, situated within the Abitibi Greenstone Belt

in the Peterlong Assemblage is a good prospect for base metals and precious metals. The

Perterlong Assemblage is said to be dominantly magnesium-rich tholeiitic metavolcanic

rocks (Pyke 1978, Geology of Ontario, OGS Vol 4, part l, 1991). There are several gold

showings on the property and one copper showing (Peterlong Lake, Geological Map

2345, Pyke 1972, OGS) which encourages exploration.

3.0 PREVIOUS WORK

Exploration on the property dates back to the 1930's, when gold was discovered at the

Boychuck Showing. The showing apparently consists of quartz stringers and lenses

within an east-northeast striking shear zone in intermediate to felsic metavolcanics.

In 1995, Driver Resources completed 137 Ion of line cutting, a total field magnetics

survey and a limited induced polarization survey. The results of this work were

encouraging enough to lead to expanded IP coverage in the current survey.

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1995 Selected Grid

Boyehuek

Starfire Minerals Inc. l

(2)

IINCKS

Spanride Property^

Scale: 1:600000 Spanride Property

Location Map

Figure 2

4.0 1997 IP SURVEY

4.1 Procedure

Work in 1997 consisted of expanding the previous IP coverage on the l 995 grid. Crews

from Geoserve Canada Inc., used the Androtex TDR-6 Receiver and Scintrex TSQ-3

Transmitter to conduct the time domain Induced Polarization survey. The pole-dipole

array used a 50 m dipole separation and read n= l to 1^1 = 6 at 50 m intervals. A total of

3S".^5"km in l 4 lines were run on two separate areas of the property.

4.2 Results

Results of the survey are shown on the IP sections and plans which accompany this

report. Note that the plans also incorporate the data from the previous IP survey.

Several coincident chargeability and resistivity anomalies are seen.

The most significant of these is a wide area of high chargeability located south of

Telluride Lake. This may represent an extensive area of sulphidization associated with

the intrusion of the Peterlong Lake Batholith. Within this area, chargeability ranges

from 20 to 30 mV/V. Resistivity is highly variable. The area near the southern end of

Telluride Lake is a resistivity low and appears to extend to at least LI 600S, 350W. This

may represent a north south fault. Areas of moderate to high resistivity, up to 57993

ohm/m may represent areas of silicification and/or carbonatization. Of particular interest

is a "pant leg" chargeability anomaly centred near 0+50W on Lines 1000S and 1200S.

This anomaly is not fully defined due to the limit of the survey.

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A known gold occurrence northeast of Telluride Lake is located on the flank of a broad,

east-west trending resistivity high/chargeability high. This also trends toward another

gold showing on the shore of Telluride Lake, but swings to the south in the east end.

An isolated chargeability/resistivity high near Line 200N, 2150E is roughly coincident

with a north-south fault mapped by Pyke (1978).

A north-south trending chargeability/resistivity high from L400N, 800W to LO, 500W

coincides with a magnetic high outlined in 1995. This probably represents a diabase

dyke.

5.0 CONCLUSIONS AND RECOMMENDATIONSThe induced polarization survey was successful in outlining at least three areas of

anomalous resistivity/chargeability on the property, which may represent areas of

alteration and disseminated sulphide mineralization. The survey also more fully defined

certain structural and lithological trends.

A geological compilation, incorporating all past work in the area, especially diamond

drilling would be helpful in interpreting some of the anomalies. Following that the

anomalies south and northeast of Telluride Lake, and the one at L200N, 2150E should

be tested by diamond drilling.

Respectfully Submitted For Approval,

LRodney A Barber Date

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6.0 CERTIFICATE OF QUALIFICATIONS

I, Rodney Alan Barber, residing at 119 Lois Crescent, Timmins, ON , certify that:

1. I hold a B.Se. (Honours) in Geology, obtained from Laurentian University, Sudbury, ON in 1988

2 I have worked within the mineral exploration and mining industries since 1988, with an emphasis on northeastern Ontario for the last 7 years.

3. This report is the product of the examination of the survey results which accompany this report, published geological data and a general knowledge of the Timmins area.

4 I have no direct interest in Starfire Minerals Inc or the Spanride Property.

9/2.0Date

JLRodney A Barber

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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 2700 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 'Switchselectable delay and integration time 'Multiwindow chargeability measurements'Digital output for data logger 'Six channel input provided 'Compatible with standardtime domain transmitters 'Alpha-numeric LCD display 'Audio indicator for automaticSP compensation 'PortableSpecifications'Dipole nl to n6 simultaneously'Input Impedance 10 megohm'Input Voltage (Vp) range:100pV to 30 Volts (automatic),

accuracy : . 25?;, resolution : lOuV. '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 60/180HZ or 50/lSOHz,

lOOdB, other .-Anti-alias, RF and spike rejection. Internal Test Vp^V, I^SOmV/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 +50 0C, storage -40 0 to 4-60 0 C. Power Supply Four l.5V D cells. 'Dimensions 31x16x29 cm Weight 6.5 kg (14.31bs)

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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 ±1C^ 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 800Hz, 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 Z 1 500V'Output Current 10 amperes maximum'Output Current Stability Automatic controlled to within i.1% for up to

20 1* external load variation or up to ±10^6 input voltage variation.

•Stabilization Protection (Over-range) High Voltage shuts offautomatically if the control range exceeds 2 0^.

'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 t=l,2,, 4,8,16 and 32 seconds, optional•Stability Crystal controlled to better than . \\ with

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

•Efficiency .78•Operating Temperature Range; -30 0 C to + 50°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 Q C.•Dimensions 350cm x 530cm x 320cm (transmitter). 'Motor Briggs and Stratton, four stroke 8HP.•Alternator Permanent magnet type, 800Hz, 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"-t-" 1 "-t-*-

= 2 seconds, 0

i l

—————————————— ' ——————————l

N S OFF time. Total duty C

i i

J Lryde Used; 8 second;

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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;(l)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 i nterrupted. 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 cps. . 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 LimitationsThe 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 mSeconds (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.

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OntarioMinistry ofNorthern Developmentand Mines

Tra Numberjpff ice, use)

i'ssment Files Research Imaging

42A03SW2001 2.18442 ENGLISH

Declaration of Assessment Work Performed on Mining Land"'-i— *-* Subsection 65(2) and 66(3), R.S.O. 1990

)rity of subsections 65(2) and 66(3) of the M^ET. Under section 8 of the l 3d to review the assessment work and correspond with the mining land holder. \ ining Recorder, Ministry of Northern Development and Mines, 6th Floor,

900

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

2.18441. Recorded holder(s) (Attach a list if necessary)Name

; VC -Client Number

300 37/Address

350 rcrtrr fTelephone Number

'J l

R.cFax Number

Name Client Number

Address Telephone Number

Fax Number

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

Geotechnical: prospecting, surveys, i i Physical: drilling, stripping, assays and work under section 18 (regs) l l trenching and associated assays Rehabilitation

Work Type ^, vi? Cuff t '6 S I.P ^L'^^cV

l

Srme^ *om OT , ^7, ^- To 0 V . Of *)f JDay 1 Month | Year Day | Month | Year

Global Positioning System Data (if available) Township/Area

QLTtz/ncK- j tfr^C-Lj S 'iM or G-Plan Number'

Office Use

Commodity

Total S Value of ft ^/, . t/j , Work Claimed V iy6 y J f

NTS Reference

Mining Division -L/ tfouftc^-tj

Resident Geologist r~y District l i /jl^jj^t^jcx')

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

(~eo s c z uc \ /o cTelephone Number

Fex N umberAddress^79

4,Name Telephone Number

Address Fax Number

^

Telephone Numb

Addre; Fax Number

GEOSCItNCfcASSbSSMhNI ____ OFFICF

4. Certification by Recorded Holder or Agent PORCUPINE MINING DIVISION

M l Kg , do hereby certify that l have personal knowledge of the facts set(Print Name)

forth in this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.

J-

?~^xfs2Signature of Recorded Holder or Agent Date

Agent's Address Telephone Number Fax Number

0241 (02W6) ootMtf? ol

t,/fier* work was performed, at ihe time work was performed. A map snowing me contiguous linn musl accompany this

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oatemme toeallon number Mealed on tw etoim into.

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________ _________, do hereby certify that the above work credits are eligible under

subsection 7 (1) of tne Assessment Work Regulation 6/96 for assignment lo contiguous claims or for application to the claim i

where the work was done.

Slgnaiue of Recorded howe/ or l

6. Instructions for cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check (O'" in* boxes below to showjyov*vojLwish to - - ..^ . prioritize the deletion of credits: ' FJ r"*x*\|"" t \ t r"^f^

&L 1 . Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated ** V^ C l V t LJ

O 2. C redits are to be cut back starting with the claims listed last, working backwards; or

Q 3. Credits are to be cut back equally over all claims listed in this declaration: or

O 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describ

MAY t 1 1398

kEOSCIENCE^ASSESSMENTj

Note: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary.

For Office Use Only_____ _____ftecOvtd-

MAY u m^;W^-

PORCUPINE MINING DIVISION

D*em*d AppfWM Ottt D*tt NcUfutioA S.nl

Total Valu* o

Approved for Recording by Mining Recorder (Signature)

3Mjr5 fe?Slff ?

For Office Use Only

ii f t ! iff

Received Star

1 (03/97)


Deemed Approved Date

Date Approved

Date Notification Sent

Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

RECEIVEDMAY 1 1 \

GEOSCIENCE ASSESSMENT _____ QFFICF

Ontario Ministry o) 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 Wining Act, this Information Is a public record. This Information will be used to review the assessment work and correspond with (he mining land holder. Questions about Ihis 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

/^tT FIX'5 iSfi+C Zv^J"

I.P Su.-CL/evf

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.

"9 j~" i-J ^ ^

3^-y^-/^

2.... ..-i- 4. 1 *

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

Transportation Costs

Food and Lodging Costs

Cost Per Unit of work

/^O, fitfK.

JSOO. 0" j)0rt^

3f-yf A — O 3 ^ - ^

**

Total Value of Assessment Work

Total Cost

^.3/7. ^^r"? /TC v f

^Wfi**

Calculations of Filing Discounts:

1. Work filed within two years of performance is claimed at 1rjO.% 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"7o 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 S value of worked claimed.

Note: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:

_____C'^O^J______, do hereby certify, that the amounts shown are as accurate as may reasonably(please print Full name)

be determined and the costs were incurred while conducting assessment work on the lands indicated on the accompanying

Declaration of Work form as ______y i \^ i—\-y____ t__________.————.—.———————.——.———-———(recorded~helder, agent, or *fale company position wHh signing authority)

l am authorized to make this certification.

0212(03/97)

\ P ORCUPINE MINING DIVISION

q'.5* rn \ 2 698

GEOSCIENCE ASSESSMENT OFFICE

Ministry of MIntstere duNorthern Development Developpement du Nordand Mines et des Mines Ontario

Geoscience Assessment Office 933 Ramsey Lake Road

July 27, 1998 6th Floor

Sudbury, Ontario

STARFIRE MINERALS INC. P3E 6B5

BOX 10Suite 301, 850 WEST HASTINGS STREET Telephone: (888) 415-9846

VANCOUVER, B.C. Fax: (705) 670-5881

V6C-1E1Visit our website at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm

Dear Sir or Madam: Submission Number: 2 .18442

Status

Subject: Transaction Number(s): W9860.00505 Deemed Approval

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The

attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS

SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any

steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the

Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day

Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment

Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in

Section #6 of the Declaration of Assessment work form.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the

response date on the summary.

If you have any questions regarding this correspondence, please contact Steve Beneteau by e-mail at

[email protected] or by telephone at (705) 670-5855.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 12592

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2 .18442

Date Correspondence Sent: J uly 27, 1998 Assessor: Steve Beneteau

Transaction Number

W9860.00505

Section:14 Geophysical IP

First Claim Number

1206699

Township(s) l Area(s)

BEEMER, ENGLISH

Status

Deemed Approval

Approval Date

July 23, 1998

Correspondence to:

Resident Geologist South Porcupine, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):

Mike Caron PORCUPINE, ONTARIO

STARFIRE MINERALS INC. VANCOUVER, B.C.

Page: 1

Correspondence ID: 12592

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THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED

i FROM VARIOUS SOURCES, AND ACCURACY IS NOT

i GUARANTEED THOSEWISHING TO STAKE M1N- ING CLAIMS SHOULD CON

i SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP

' M ENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE

. LANDS SHOWN HEREON

en*

5?

cL

O W f*O

-3 Twp. ivl.

122889-^'

i"—

00h-*^

Q.

to 6*C

LLJ

O'' 00"

20' 00"

(15 UNITS)

Moher Twp. M .S68

THE TOWNSHIP OF

C

DISTRICT OF

SUDBURY


SCALE: 1-^^ = 40 CHAINSjteaaKr.*f*aauamsaSK-^.''as.~Tets*' w " mnrM*—g* 'sst --i^*r-*t t&fs* - ,'*~ " ~-~

LEGEND

PATENTED LAND

CRC*N LAND i *i.ELtASES

i. CCAi tO LAHO

LtCEN^: OF OCCJ?ATtON

MiNJHG R iGhi'S 0**LY

SURFACE RIOKTS O*LY

^ l

o '1 y HL "

LO

KING'S nici-'Xi'S

RAILWAYS K..(t,R , ",cSMARSH cr, "T; p- EGMINtS

LAND USE PERMIT

•ii

NOTES

4OO( Surtoce T fi^s, Reseivcfijr ;.c-u

bf'os o r:d rivers.

Flooding Rights in Peterong and Kapiskonq

'akes assigned to KE.P.C. LO 7191

File No. 1162 VoL 4

THIS TWP CHR.E'-I T O FOflEST ACTIV/TY IN 1994/95"FURTHER INFORMATION ON FILE. .^~-'j-

DATE OF

JUL O 6 1998PROVINCIAL RECORDlNb

PLAN NO. l

DEPARTMENT OF MINES

- ONTARIO -

42A03SW2001 2.18442 ENGLISH 210

Beemer Twp.1203993 English

1203994

203992

Muskasena

VaW ;

1995 Selected Grid

137km of Survey Lines

Baseline Azimuth N3CTT

PLAN lStarfire Minerals Inc.

Spanride Property Base Map

English &C Beemer Twp's. NTS: 41 -A Porcupine Mining Division

SW

42A03SW2001 2.16442 ENGLISH 220 Plotted: Apr 7/ 98 Geoserve Canada Inc.

Beemer English! Twp..1203993

1203994

1203992

Telluride

2623024362231792199721 12420194

94768685

179351733916654161081545514933

430513791131791256712054114261090402519704901984247673688261645234436231791996

128 LEGENDApparent Resistivity Plan

Filtered Productn-1 to n=4 Levelohm's/ 50 metersPole Dipole Array

Q- 5 0m Time Domain Equipment

Apparent Resistivityohms/m

Scale 1:10000O 200 4-00

PLAN 2

Starfire Minerals he.Induced Polarization Survey

Spanride PropertyAndrotex TDR-6 Receiver

Scintrex TSQ-3 TransmitterEnglish b Beemer Twp's. MTS: 41-A / SW

Porcupine Mining Division42A03SW2001 2 .18442 BKOLISH

Geoserve Canada Inc ,

262302436223179219972112420194194761868517935173391665416108154551493314305137911317912567120541142610904102519704901984247573688261645234436231791996

123

Beemer Twp. 1203993 EnglishJL

Apparent Resistivityohms/m

42A03SW2001 2.18442 ENGLISH 240

LEGENDApparent Resistivity Plan

Filtered Productn^ to n-4 Levelohm's/ 50 metersPole Dipole Array

a= 50m Time Domain Equipment

Androtex TDR-6 Receiver Scintrex TSQ-3 Transmitter

Scale 1:10000O 200 400 600

(meters)

PLAN 3

Starfire Minerals Inc.Induced Polarization Survey

____Spanride Property_____ English Se Beemer Twp's. NTS: 41-A 7 SW

Porcupine Mining DivisionGeoserve Canada Inc . Nov. 1997.

S 1 2K-j

IP59K

RES 5933

Topo

Interpretation

Chargeability

Interpretation

Resistivity ohm/meters

58K- 0.. 0.

. . . . . s' . . . \ .

l l l l - l r i i l l i l

6.8.

.H 12K r

MF .6.8

RES .5933

O ^0 -58K

IP 59K

13+00 W 12+00 W

n-1

n=24.1

11+00 W | 10+00 W 9+00 W f 8*00 ff | 7400 W | 6+OOW | MOW | 4400 W 3+00 V^ | 2+00 W 1+00 1H | WO

12 H IS 17 H 13 12 11 9.3 10 10 9.1 It tt 9.9 9-3 10 9.7 8,* 8.4 7.S 7 6,4 5.9

19- — .22 ^17 13 t ,j,g 5.9 ^7.8 i 10 \ ^.-^Jii\ ^S 9 ' 2 "^v 1 X2 __ 7' 5 8' 4 "X11 V'fl 4' 4 —— 4-8 5' 3 5J 5'' S- 3

"-^ 12 \ I9^^"z*xjiv S-7 ^^?-'/ 10 8- 9 ^" 1 0 ( 8'5 7-8 \ 1 2 ^^\ 7' 9 *- 1 \ t2 \J-* ——— 7.5 ^S.7 S.3 5.t 5.8 S .

rPXX 13 ——— 15\ Z* \12 — "l' 'O 7-' 8-*\ 'S W 7.9 8.7\ 13 11 y 7.9 B.S^v 12^^*9.8 8.5^^7.4 6.8 6.1

^Xs-SVVIZ 16 ^ ^J2 s\ 14 1Z 9.6 7.7 9.7 13 10 ^^ 9.2^ , 1 0 13 11 . 8 M\. ' 3 " \ B l8 7.6^^8.7 5.5 S 4.

12 V\8.3 \\ W 16 . \ 33 \\ H 11 9- 9 ^. 8' 8 " \ 1 J " 1 1 I0 " 1 ! \ 8' 4 8'*\ 1 S w v 8'9 8^\ S' S f 4'7

13 ^ 6.8\ 14 17 ^" 3* ^ 13 M 1 1^ 8.4 9.1 14 13 11 f~*Va 13 10 8.5 9.3 13 10 ""~ n""N B.J 5.8

——— ! —————— l —————— l —————— l —————— l —————— l ————————————— l —————— l —————— l ————————————— P —————— . —————— l —————— l —————— l ————————————— l —————— l —————— l —————— l —————— l —————— l —————— l —————— l —————— l —————— i —————— P —————— i —————— ( ————————————— l —————— l —————— l —————— l —————— l ———— -l —————— l —————— l —————— l —————— . —————— l —————— l —————— l —————— l —————— l —————— l —————— l

Topo

Interpretation

9.8 8.9

•7.8—"8.

M 1 3

14 10

13 13 12 11

1KB E

S.1 4.4 fj|ter

4.4

n-4

Chargeability mV/V

Interpretation

12K 10K 8572 8324 9506 8194 6460 5738 5407 4508 5454 4747 4490 9231 12K 15K 17K 19K 19K 17K 20K 18K 20K 14K 11K 9829 9973 9434 8650 8491

7235 ^ 4:18 J400* UK UK 12K

14K 7131 ^.409* 5974 111K

l* \ 6735 6106 974 3353 52S8 ^, 2603 ^ 3599 7200 1* 9565

OK 7095 5619

1 7256 494914 4701 8433 -^4027 3876

3281 7105 '

16K 25K t I7K 15K (IK 13X

19K 16K 19K - 24K ^ 33K ' 21K

0=2

tIK l 7469 9980 4863

0=4 o-5 0-6


L- 2200S

l

^ P ole-Dtpole Array

Ow

o o

M

Ha•b* h)

na

'——CD-i

0=50^1

plot point

Filter* n1

* * n2* * * n3

* * * * n4

Coni. Intervois Resistivity ; Logarithmic Chargeability ; Logarithmic Metal Factor ;

10Ulo

Profiles

INSTRUMENTSAndrotex TDR6. Time Domain Receiver

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

Scintrex T5Q-3 Transmitter BSecond Total Duty Cycle, 2Sec On/Off Time.

INTERPRETATIONl Low Effect

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

| Moderately Low Effect

l Moderately High Effect

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

Scale 1:500050 O 50 100 150 200 250 300 ~"~ -i " *c

(m stars)

StarGre Mineral fncInduced Polarization Survey

Spanride-1-95 Grid English ft Beemer, NTS: 42- A/ SW

Porcupine Mining DivisionGeoserve Canada Inc Sept. 97.

OJ 0. i i i i i i i i i i t ...i. .i

— ~e~bility —v, V

^—— /i—sters

..1.8 r9470 fe

MF ..88

RES .4735

.0 LO -58K

14400 W 13*00 W 12-KK) W 11400 W 10+00* 9+00 W 8400 W 6400W 5400 W 4+00 W 3400 W 2+00 W 1+OQW 0+00 1400 E

filter 20n-1 19

n~2

n^J

n-4

r^5

12 11 s. 7.7 5,2 7.S

20 18 \ 9^ " - v.19 15 10 13 13 v-

V *. ^

8.9 8.2 ' .p 1sS7i 12 f~5n ^^.^X 17 K 26 26 V IS 19 \ I3\^

^Z^-^— 18^^- IS ^ II 7.4 O^ li ^ 17 V 27 Z* X ™ 20 \ 13

14

is jo

14 N, 23 \ i v^—- m - o ^ ii v*~^x v ^ " \ u o x. " a \ 1J \ 1 !l \ u " "x" \ '? " " '* ^^^ÎL—J ' ^ i

18 "15 1f\ H \(r( ( '63 i } 13-? 18 17, ".VlXX" \ ™v * 2*\ " 1 9 \ !^ " \ " " \ a . \ 9 "~'^v11 1 4 " 1 3 K

18 X,5 ^\7 13 NS*—— f.*' ^4—— .4-^,3 \.SM.7\ ,XV 27 ,\ 17 ^^ ,,V 1Z V^ ,Uf^ ,, tt 9.6 1,

l r"6.7

' filter7.3 n-1

n-4 n=5

n-6

14-KWW 13+00 W 12+00 W moo w 10+0) W 9+00 W 7+00 W 6+00 W 5+OOW 4+OOW 3+00 W 2+00 W 1+00 W 0+00 1+00 E

filter 1 6K

0=1 1*

0=2 n-3 n=4 n=5

17K IK 1 6K 11K 9726 65(2 7151 7111 (638

*6?

tBK f m' m15K 17K

18K

l SK

// J1j ~

14K

.^M. "^

6290 5972

48S2 -, 4209

6185 6217

6438 5029

7136 7927 8212 8115 B561 (0*0 9151 17K 1(K

SiO* 6962

^\

(485 6Z43

8*14 ^ 8234 TUT

53351.9544 ^-

1SK 15K

19K 15K

49*

3761 5467 5994

p^*. 6870 5633 8178 x 6653 "^^ 4708 5255 77S2

5813 ( ?887\ B224X S884 8153 7974 4928 6161 \ 8545\\^ \\ V X. t \

" 5640 - 2108 x 10K ^ 6743 9745 8239

s 2997^^ 5256 6993 v

— 7585 -^M60 8603

17K

1tK 1tK

7529

\

^ — 6762 /âT^"" 8798

— - ÎOK — - M43 I2X

8442

8863 9628

6326 6640

8848 14K 1QK

IOK——"M1K 13K

12K \8236 9639

I4X ^ 8197 8600

12K MK

9278 — 89

7351

5388

W . 12K I5K

1* 15K I3K WK 5868

} sf BBS

S21Z

7348

ens6535

6068 f ilter

6061 n**1

n-3

n^4

n~5

IP .59K

Topo

Interpretation

Chargeability mV/V

Interpretation


L- 2000S oiS l

Pole-Dipole Array

0=501^V'

plot point

niter* n1

* t n2** *^ ^-t * ^r ,T|4L '^' ' ^

K ea

f** ^"OJH

N

O

M*

Cent. Intervals Profiles Resistivity ; Logarithmic — — — — Chargeability ; Logarithmic Metal Factor ;

INSTRUMENTSAndrotex TDR6, Time Domain Receiver

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

Sctntrex TSQ-3 Transmitter SSecond Total Duty Cycle. 2Sec On/Off Time.


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

Moderately Low Effect

Moderately High Effect

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

Scale 1:500050 100 150 200 250 300

•l b (meters)

Sitarfine Mineral JncInduced Polarization Survey

Spanride-1-95 Grid English A Beemer, NTS: 42- A/ SW


9318.

IP 59KL,

RES4659.

58K-. 0.

Topo


fjjter 9,3

r-1 5.2

Chargeability ns3

filter

[1=2

..2.5 j-9318 ..60K

.1.3RES

,0 uO

14+00 W 13+00 W 12+00 W 11+00 W 10+00 W 9*03 W 8+00 W 7+00 W 6+00 W 5+00 W 0+00 1+00 E

9.7 12

5.2

12 II li 13 H IS 15 It

1Z 1 2

__

11 l'

9.2 7 .8 8.1 8.7 ^8l5

i2 u

J6 __ 17 vtt -- 1*

13 s""- 1S 20 16

H n )1J 11 13 12 14 11 1 Z ,/ " " l

'12 15 ..

14 IJ 1C ' 13 14 x

15 13 13 S 1 9

20^15 li

16 IB 8.3

16 15 20 25 26 25 24 26 25 24 23 22 23

28 24 .. J4

!8 1 9 19 1 3 filter

19

"

23 ^ 17 11 18 25 28 28 26 30 27 28 28 24 .. J4 y 1 4 20 14

y 16 , C*'s.sll IP) 24 26 25 28 28 26 24 22 29 V 17 T ^

' \2' l.l'/.M 28 Z3 22 27 27 26 22 -.-""a 28 -Xie y 22 J

f 33 ^—^ /-p:C 1' 25 26 26 22 X^ 19 29 X 12 X^- ZZ v/ '

31 37 j loj),. 22 34 25 24 f 19 27 S 1 6 X^IS 7 17

10 11 -^ 24 29 27 20 —'' 26 24 25 13 -" 18 ' 28 -18 20—16 - 22 ' 12

17

0=6

lj+00W14K 16K

13+00 W16K 14K

11+OOW

14K 15K

10+00 W

16K 14K

l4fJOE . ^7546 8793 ff,ter

0 = 1

11=3

^=4

0=510K

IP .59K

Topo

ChargeabilitymV/V

Interpretation

Resistivity

ohm/meters

L- 1800S

t O /*o i O 'i;

Pole-Dipole Array o no a

Cont. Intervals Resistivity ; Logarithmic Chargeability ; Logarithmic Metal Factor :

Profiles

n ra

n** a rfM

O

ims


1760mSec Total Intergration Time, 80mS Delay. \~ ( 80+80+80+80+160+160+160+320+320+320 ) mSec

Scintrex TSQ-3 Transmitter BSecond Total Duty Cycle, 2Sec On/Off Time.


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

~\ Moderately Low Effect

] Moderately High Effect


Scale 1:5000O 50 100 150 200 250 300——————-l L.————————————————

(maters)

Starfire Mineral JhcInduced Polarization Survey

Spanride-1-95 Grid English k Beemer, NTS: 42- A/ SW

Porcupine Mining DivisionGeoserve Canada inc Sept. 97^

i——i——i——i——i——r——i——i——i——i——i .5 1 2K .60K

MF l RES 1.7 L5956

Interpretation

14400 W 13+00 W 12+00 W 11+OOW 10+00 W 9+OOW 5*00 W 7+00 W &400W won 4+OOW 3+00 W 0+00 1+00 E

Chargeability mV/V

filtern-1 12 f

^=2 *n^n-4

n=5

n-6

13 15 11 11 13 13 15 IS IS 15 IS 14 IS

12 .-— 9.7 12 H - 1 5 1.5 16 It 11

16 IS

10

24 24 2* 25 W H 24 20 20

12 ( 7.sJ 1 3 IS 16 l 1 4 J 17 .X 12 11 14 11 S

M ^^—— 11-—-15 18 15-^16/^12 12 T4 14 /M

16 IS 15 17 7 12 12 14 14A .- .^~V .S11 12 10 16 16 17 16 17 7 13 12 16

12 11 H ^- 16 18 17 l* H 13 14 15 ' j7

21 29 27 27 26 30 21 21 20 \ 14

28 22 24 28 24 28 22

18 -i 22 23 ?6 26 28 22

14 14 12 11 filtertl 11 N.9.1 9 n-1

U 14 14 12 11 r^2

5 -l 13 1! ^=3

16 IS 16 IS IS 13 n-4

11=5

"terpretation -H———*———l-

filter0=1

11=2

[1=3

22K

23K

14+00 W DC 12K

, 13+OOW14K 16K

12+00 W

IK 13K

t 11+OOW

14K I2K

| 10+00 W17K 14K

^ 9+OOW13K 13K

8*00 W13K 13K

7+OOW

13K 10K

6+pOW

7480 7728

Resistivity oh-n/meters

IOK , m^ 1 3K 12K '* V-s^j vNN?" ; i11K v J787 1 4K 1 3K 1/* ^J f** U K ^MH^-'lSt Ilit^^JBB NIBK J lin 12K I4K 13K/ 18K

0+00 1+00 E ———l——i——l—————l——i——i——iUK 8252 6506 W18 479 f[|^er

.2790 n"1

19K

1BK

W\ 1 4K

ITK' IK 'H.' 'i*

8757 M18K

-j"- ivn nf\ ^^^ QafU. T* IOK l

19K j 1 2K 13K 12K 15K ~^^1iK UK 14K

-—-'IK laC/tTXX ItK 18K \ 13K tIK 15K ——— 14K S 6782 -

— ^ — — —' "'NTS f 8640 9529

B203~^ UK

6001 6574 ^ 7688 8764 9388 ,

JTl/ .f l IR .

8674 9717 9202 8751 ^ 3454 M06 ' 9183 ) 5238^ 3458 2161 l I Mt//

,., . 4019 y 6599 7213 ~~ 5937 3642 3135^- 6830 l Z1K

/W"t 6809 748S 8177 ~" "" —— '""

UK' l/K \ lin IK \ iai H* iai —— lw s e"" x* B* s' * X llw* x DWB 7 x^ '"™ X yI4K^ 18K 15K—~1!K 17KJ 13K 12K 13K /^KK , 8640 9529 9W5 9849 ^ 4019 y 6599 7213 —' 5937 3642 3135^ 6830'S 1 BK 15K 19K ^ 13K 14)t 13K 11K-"'589* 7870 9325 8938 9980 -"388T 6809 748S 8177 3118 3148 /B822 -^

l v——-—— l *——^ I3K 17K I*K ' 8030 IOK

n-3

n=4

n~5

ns6

IP U59K

-O LO L58K

Topo

Interpretation

Chargeability mVA

Interpretation


L- 1600S

2.1 f:/*(ft* Xs.'

Poie-Dipole Arrayno

a=50M

plat point

Filter* nl

* * n2* * * n3

* * * * n4

Cont. Intervals Profiles Resistivity ; Logarithmic Chargeability ; Logarithmic Metal Factor : ——————


1760mSec Total Integration Time, BOmS Defay. ( 80+80+80+80+160+160+160+320+320+320 ) mSec

Scintrex TSO-3 Transmitter SSecond Total Duty Cycle, 2Sec On/Off Time.


50

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




Scale 1:500050 100 150 200 250 300

-i "C- (meters)

Starfire WneralbicInduced Polarization Survey


Porcupine Mining DivisionGeoserve Canada Inc. __ Sept. 97.

mo ft

IP 59KJ

58KJ

Topo

Interpretation

RES i MF 6452 J 1 .3.

l l l l l . l l L l———l———l———l———

Chargeability

Interpretation


oJ

MF t RES .1,3 L6452

.0

14^00 W 13+00* 12+00 W 11+00 W 1Q+OOW 9+03 W| 8KB W 7+03 W 6+00 W | 5+03W 4+OOW 3+00 W 2+00 W 1+00 W 0+00 1+00 E 2400 E

filter ' 3 14 14

11 12

14 14 15 16 18 17 20

n-1 10 10 11 12 11 9.

11=2 14 13 13 12 13 11

0=3 15—^14 13 14

'*^— 15

11=5

15' f I B 20

13

tt/

13 14 ' 18

14 IS 19

IB , 11. - x 23 -- W

/.H

IB 16 ] IS ^ IS 19 IS

18 21 22 24 22 18 14 8.6 6.5 6.7 8.3 9.7

20 17,x 25 25 \ IS 4 12 . i 3.3 ^ 2.6 v , 5.8 B.6.

14 s 1 8

15 —— 17

16 ' 26 17 17

25 .18 ^ 12 ,

f S ^~) " f** ® 27 2 \ 17 8.4

'14/17 IB 27 28 23 20 l 1 1

.. J - ^ .. M y/x* 4J

25 28 23

26 26

26 22 21

8/11 11 - ———

12 13 13 14 15 14 11 13

1 8 .4 f 1 0 ——— 10 12 12 12 14 13 1287 )X'2 11

\ l /^ 1Z 1Z 'Z '3 '5^ __ 15 __ 15 12 U 14 II

3.4 j l 1 3 13 12 13 y/1* 'l 'S 14 ^ I B — 14 14""^

1WBW 12+00 W 1HOOW 10+OOW-l—————l—————h-

9+O3W 8*ODW 7+00 W 6+00 W 5+COW 4+OOW J+OOW 2*00 W 1+00 W 0+00 1+00 E

2IK 13K 22K 22K 21K

2+pOE,17K m fjjter

10K 1QK 12K 11K 12K 12K 11K 6626 4078 6933 10K 11K 12K 14K 17K 21K 21K12K 11K 12K 12K 11K

— 5630, 75M ,J7S2 - 59*1 — 6227 v 9447

10K 7852 5539^- 8815^ •X*laT\ 7998 f

814 /j, 11K 11K 10K ——— 11

S I 2K

HlK-x^aiSMJS

^--

IK -, 11K ^ 19K v 9746 j- 1 6K n-1

8708 9221 . 12K ^ 9329 -" 12K

1511 f 7583 ^ 13K ^^, 1g

/6191 6234'' 37K -

18K 12K IS VZW

IP L59K

L58K

Topo

Interpretation

Chargeability mV/V

Interpretation


L- 1400S

i c^ole Array

a^SOM

Vplot point

Filter* n1

* * n2* * * n3

* * * * n4

Cent. Intervals Profiles Resistivity ; Logarithmic — — — — Chargeability ; Logarithmic Metal Factor : ——————

INSTRUMENTSAndrotex TOR6, Time Domain Receiver

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

Scintrex TSQ-3 Transmitter SSecond Total Duly Cycle. 2Sec On/Off Time.

INTERPRETATION

50

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




Scale 1:500050 100 150 200 250 300

ISH (maters)

Starfire Mineral hieInduced Polarization Survey


Porcupine Mining DivisionGeoserve Canada Inc Sept, 97.

o0\

60K- 17K.

IP 59KJ

RES 8338j

58KJ OJ

Topo

Interpretation

Chargeability

Interpretation


Ji -17K -60K

MF j

RES.8338

1J+OOW 12^00 W 11-KX) W 10*00 W 8+00 W 7*00 W 6+00 W 5*OOW 4+QOW 2400 W 1400W 0*00 1+OOE

12 13

0—1

0=2 0=3 o-4 0=5 0=6

15 IS 14 U 16

12 14 12 s 8.5-9.6

17 18 18 20

18 14 12 . 1 6

IS 13 - 16 19

5.1 4.9 5.1 6.4 8.2 9.8 U IB 23

18 20 2* 2dy 22

20 25 20 ^ 2222 2J

4.2 3.2. 2.5 ^ 3.8 y 5.7- 4.2

23 26 21 i 1 8 18 17

5.2 -9

14+OOW 1W10W 12+00 W It+OOW tO+OOJ^ 17K

9+OOJ^14K 14K

7+00 W 6KPW 5+OOW 4+00 W 3+OOW 2+00 W 1+00 W 0+00 1+OOE

filter12K ^ B4g4 sMK i UK i 3964 o-t

13K 11K\^17K' S1SB 0=2

14K 14K y B161 — 6326

isK m

~ 15K 8S90 x J238i i t',LI9K ' 10K f 3494

0=4

o-5

0-6

IP L59K

LO L58K

Topo

Interpretation

Chargeability mV/V

Interpretation


L- 1200S

2Pole-Dipole Array

no

Vplot point

Filter* n1

* * n2* * * n3

* * * * n4

Cont. IntervalsResistivity ; Logarithmic — Chargeability ; Logarithmic Metal Factor ;

Profiles


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


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



High EffectGood Chargeability mV/V. I PHigh Apparent Resistivity, rho

50Scale 1:5000

50 100 150 200 J"-* (maters)

250 300

Starfire Mnera/ JncInduced Polarization Survey

Spanride-1-95 Grid English Se B eemer, NTS: 42- A/ SW

Porcupine Mining DivisionGeoserve Canada Inc ______Sept, 97.

o oCO

HJ

o o

oM

60K. 1 8K- 1 .3-

. J

tP 59K-

Topo

interpretation

Chargeability mV/V

Interpretation


RES MF 8777- .66.

58KJ OJ OJ

-1BK ,60K

MF RES.8777 ,59K

-O

14+00 W 13+00 W 12+00 W 11+00 W 10+00 W MOW 8+00 W 7*00 W 6+Q3W 54QO W r 4+OOW 3*001* 2+00 WH———i———*- 1+pOlff Oj+00

filter 8.2 8 ,5 4.1 3.S J.2 3.5 4.3 9.4 12 li tt 14 12

3.1 3.7 y2.5 2 1.4 .80 /]?#^X J */ S'V S Wx-__X " ""•S^ l' 1 \

4 3.8 \ 2.5 \).9 r5^'^ .30jJ^4.2-^8.8.-^ 10 y/19 \ 13 13 ^9.2 \ 6

^ ^ B^

" 8- 3 filter2.9 n~1

17 ' 7 S.9

^ j^4X/ 6.9 9.3 -'IS 20 17 17 li

3.2 '7.4 10 14^ 20 ""^ 18 17 15 11

10

n-2

[1=3

n-4

n=5fn-6

7+00 W 6+OOW 5+COW 4+OOff 3+ODW 2+00 W 1+00 W 0+00 1+00 E

4909 5508 7247 8895 10K 11K 1JK 16K 16K W 15K 1W 18K 8W7 2700

2916 1683^^ 182( — 222S —

2613 3104 ^ 573?

1JI1 - J731 — 38M 302J i 8827 - 13K' 28K ^ 13

B593 2870 'S, 8489*^- !1K -

3649 ' 7350 "" 9J10 — 9584 , 4217, ^12K ^— 16K 16K

m13K

^ /6811. j^ / ^xl UK/6811 f I1K' 27K /,13

B224 ^^-2*" 21i(^^20K 1fl(___I9K

12K 14K /. S261.-V.19ir 24K 24K 24K 23K

UK '-'(488"''-'24K 27K 27K 2K 24K -^ 3(K

'/7 "/X^v'yLzxxf™/s2861

2138

filternH ^=2

n^ 0=4

n-5

IP

O L58K

Topo

Interpretation

Chargeability mV/V

Interpretation


L- 1000S

Pole-Dipole Arrayna

r8!

V plot point

Filter* n1

* * n2* * * n3

* * * * n4

ProfilesConi. Intervals Resistivity ; Logarithmic Chargeability ; Logarithmic Metal Factor ;


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

Scintrex TSQ-3 Transmitter SSecond Total Duty Cycle, 2Sec On/Off Time.


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

50




Scale 1:500050 100 150 200 250 300

•i b " (moters)

StarGre Mineral hieInduced Polarization Survey


Porcupine Mining DivisionGeoserve Canada Inc __ Sept. 97.

(D W

E* S-

's

^

II II

II I

II II

-*0

IB

^

lil

IsJ

-"

CD

l g—

xa

x^s

sS

I g)

f O

l ^

y J

..^

rs )

gy^s

i-A a

// ^i/

iV/4

* il

II d

II II

II H

O)

Ol

^

U

M

—

q (D

•C

S2.

3 w'

j rt-

j i!

3 ^

(D -i

"D r-t- D CD CD i-i-

Q

O :r Q

333333

~II

II l

II II

H rt

-cn

m

-l*

oi

lo

-t

(D

S\

f

S

r/

w

ut/

i

tl l

p

3

3

3

,P-'

l II

11 l

*f

*

oj

M

--

(g

O 3-

o 3 (D

(O "D T

(t i-i-

Q

O -o o

01 00g

T;

•l en

*-*-

O) -D

(6 r*r

Q

SO

TJ O

O

^-

w"

o"

CD

LQ w

*Q

.

CD

Q-

——

v ^-—

a

^^

3

ex o

,CD

CD

Q

r* ' —

-^ i

c^^ C

n o

*•'

C7

^

-^ Z

!. C

/)

,UT

g

O

30D

8^

g"

5-

o. 3.

CO

o

3^[1

8 n

o Q.

O) s ar "

o Q- (e ST

"o '

!L

o ;

—l

S3

-H

2.

s-s? ?

a s-

^ s.

i- 95

s- x.

o —

5^ 5-

31

Q o)

* S

"* "D

U1

S's

O

03.*?

2

S-q

cb

n

w n S-iaS

m

*"

5; w

-z]

w

go

8 i" ^

^^ u^

™

f?1 !

^It

S f o

' l

5 ^

g-

#w-

* w

**

*Z!

^

at

"2.

'o

f

OJ

S3

5. oT

o

O J P

50

l"iS

l(B

O

i1

CO TJ 3O II U

l o

T)

Q C^ CD l O

Q

O (T

>-

3

ro

o

o

to

42A

03SW

2001

2

.184

42EN

GLI

SH320

6QK, 20K-, 1.7-

IP 59Kj

RES 9942

1——l——l——l——f

l l l l l l l———l———i———l———l———i———l———l———l———l———l———L.-.-I-. -l- - l l l l l l li tl l l l 1. /l l l l l l l l 1. l L ll——L- l l 1. l L l l l . l l l l t l

r1.7 ..20K ^

58Kj Oj O- ———l———l ,rH,———t——l , 'j———Li-,.]———l———l———L-..I- . I.. l . l .1 i l l l

r20

MFL.85

RES .9942

Interpretation

14400 W 13KB W 12*00 W 11*00 W 10*00 W WDW fttOOW 7+00 W 6+flOW 5+OOW 4+OOW 3+OOW •4- 2+00 W 1+00 W 0+00 1+00 E 2+OOE 3+OOE 4+DOE 5+00 E—i——p—f- 6+OOE 7+00 E 8+OOE 9+OOE 10+00 E^ ^ 'W , 12+00 E 13+00 E 14+OOE 15+00 E 16*00 E 17r" E . 18*00 E

Chargeability

filter

0=2

S.I 3.5 5.2 4,8 4.5 3.7 3.5 3.5 3.6 3.5 3 .1 5.4 1.9 10

4.8 6.1 5.1, 4.* 4.1 4.3 2.9 —— J.1 3.1 3.8

5.8 S.4 J 4.9 4.9^ S.S J 3,4 3.4 3.3 3.6 3.1

5-—"4.9 Xs.3 6 y/4.3 3.6 3.7 4 3.1

4.7 /5.2 6.4 4.9 4 3.9 4.5 3.1 ^-2.

It 15 IS 13 11 (.2 1.5 S.4 4.9 4.3 3.3 2.6

3.S 4.4

n-6

/ s-\vjL^ y s* " /-" 15 1 Z l \ \4S 3 " * 3;5 7~—-1.8' 15 II y 14 13 9,3 \ 6.1 \ 3.4 3.5 4 3.5/^P/ ' r "r-*' 1J\ "- " "

.^^-- ^^. . j.a^p^.401%? 11 ^- a is 12 / *A s'\ 7 -4 *sy ,3 (]g[77) *\@t{" u yffiffly/* l r' 1J ^ (" v*^-l 5.1 -S 4.6 4.3 5.3 4,4 ^2.5 -^4.1 5.1 5.7 -^-.20^^14 /21 " 17 * 13 11 ^ W 11 13^8.

4.3 3.8 S.3

* 4.1 -X S.7

8.8 ' 6 .8

11 9.4 8.7 7.S 7.5 t.l 8 .1 9.3 9,7 9.2 8.8 7.7

-2.7 i^rwr.

1.6 5.8 S.S 5.5 1.5 7.2 8.3 10 12 12 13

5 5.6 6.4 y 9.9

13

*~

9.7-^ ^S.I 1.1 8.S 8.6^6.4 5.8 S.Sv 3.

10 12 II N.9.1 S 8.9 9.2 7.7 (.5 S-T^5.4 e.8 10 12 II N.9.1

5.3 f'-* I " n 11\U

4.S ^ 7.) -11 12 12 tA 9.1 9.1

9.t

. . __ ..^

X8.2 /^ll \sX U

't 1 .8 11 ^^9.9 M ' 4.7- 6.6

8.7 s 2.4 N. 1.8-2.7 2.3 i 4.4 , 1i 4.4 , 1 0 16 __ 18, \ ___j 1 1 N 5.5.5 6.3 \ 3.1 5.2 6.5 7.7 -l.

5.3 6.1 5.3 —— 5.2 ^ 4.3

L 11.45^.2.5^ 1.8 7 4.3 N .Si,,X^s,.,^;. ~, \u

. . .^ . - ^ __ —— v i . s^ . N. 1.-^. 2. i .

1.1 4.7 6,4 5.1 l t.sf 1 3 !4 J 1 8 17 ^s~ 14 ^ 29 ^ 13 iXr.B N. 2.7, '-5 \ 3"^ — 1J l 7J ^

5 5.5 7.2. — -7.8 l II 12 15' 12 ___ It 13 v T \ "v S? \W ' -S \ V 3.S -- 5.3 7,4-^77— TSJ\ 15 11 10

4-8^ 5,7 8.2 l \.\ __ 9.8.^ 11 13 H /*^8 10 14 \22 N. II ^ 8.9 sXj-T ^2.3 [6.2 5 ^ 5.S 5,9

. 15 23

.6 ' 9.8 13 16^ 24 \ IS

. . . 5,9^ 2"T) .

\t-S V *'' ("iT^^S.I 3.8 ^ 5.9\^ 14 J

7 ^ 4.7 8^ 3.9^ 5.6"- 4 5.r--- 10

t.9 5.1 S.4'

8.7 B.44.2 6.4 4.3 4.3

8.7 10 " 3.9~^- 5.6' 3.4 ^ 5.

Interpretation H——————l——————i———p———i-

12+00 W 11+00 W 10+00 W 9+OOW 8+pomf 7+00 W 6+OOW 5+OOW 2+00 W 1*00)11 0+00 1+OOE^ 2+OOE 3tOOEx 4+00 E 5+OOE 6+OOE 7+00 E^ 9+OOE ( 10+00 E f1+00 E 12+00 E 14+00 E 16*00 E 17+00 E 18*00 E 19+00 E 20+00 E 21+00 E 22+00 E 23+00 E 24+00 E 25+OOE 26+00 E 27+00 E 28+00 E 29+00 E11K 11K IK 18K I9K 1* 8878 10K 13X IK 18K 18K 1SK 14K UK 14K MK t(K (SK 8332 8125 SOW 24K 23IC

Resistivity ohrm/meters

0=1

0=2

0=3

2* 32K 25K 25K 29KIK 18X I6K 18K 19K I7K 21K 2SK 74K 29K I* 3* 38K 3*K 31IC 33X11K IOK 1IK 9073 9412

41(7 — 1418,1 17K , 23! -17K- 12K

8334 ..111(1 2IK 24K/ V/ I3X ' /

17K 18K 73C-" 2935 40B

IBK IK 17K m lTK 3J58 /- /

\

2IK MX 2SK \ TMt 75X UK

\162* -3843 6421 tiK 17K

18K 20K 20X MK 24K 21K

2SK 27K

V" \\VI5K—- W( V|7ti\Nl9K 30K 22K 23K XaitJ 28(1 tBK \ 1343•N N\\\

17K ISKy^ 7289

wu \ iiw irt ^. \" ^. ~"\""v — — \

•w WK\\ 6490* XMK an m Ow vx ,, .u.^^Vv *s i \

*879

9134 7823 1916 6748 8788 929 8621 14K

4*90

2tK IK 1*K 14K

, 5705 4885 — 5185 ^W

JJ47 ^031 61*3 6222 " 4*1 " (612

9S27 752* — 7420 — 7232 6781 l

14K 1WV... 8807 9190 ^0 7J69

IBI^ 13X 11K HK Ut

11K 7119 5182 4953 1027 2S92 2085 1616 1270 MJ

6752 83*1

\ v I7K . 29X S ^J/ 51SO

83*1 IWZlTw /U2S 4456

9013 5683 — 8154 85S 5387 5805^-26131(1*2 1299 3263

8701

fn\\ S968

5"~" 7981 - S871

5387 5805^-2613x1(1*2 1299 3263

1ltJ 8987 30SS 4710 6SB ^- 7351 j 304 2222^1324 1727^ ^" ' ^^

4947 —

2278 3418 944^' 1400 X — ——

2180 x 14S3 ^33W 2293 x 4885 4783 4138 4618 2739 v 7*9 0=6

IP L59K

LO i-O L58K

Topo

Interpretation

Chargeability mV/v

Interpretation


L- 200N

Pole-Dipole Arrayno

0=501^

plot point

Filter* m

* * n2* * * n3

* * * * n4

Cont. Intervals Resistivity ; Logarithmic Changeability ; Logarithmic Metal Factor ;

Profiles


1760mSec Total Intergration Time, 80mS Delay.kfi^ ( 80+80+80+804-160+160+160+320+320*320 ) mSec

Scintrex 75Q-3 Transmitter SSecond Total Duty Cycle, 2Sec On/Off Time.

INTERPRETATION| | Low Effect————— Poorly Chargeable mV/V, IP effect

Low Apparent Resistivity, rho

L.... 1 Moderately Low Effect

l l Moderately High Effect

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

High Apparent Resistivity, rho

Scale 1:500050 O 50 100 150 200 250 300

.aEsssi(meters)

StarGre Mneral JncInduced Polarization Survey



o m

SH

rtf

60K-, 51 K. 2.2..

IP 59K.

RES 26K.

Topo

Interpretation

ChargeabilitymV/V

Interpretation

Resistivity o h m/meters

OJ O

i——i——i——i——i——f—i—i——i——i——i—i——i——i——i——i——i

1.1,

H———i———l———i———l———————l———l———l———i———h-

14+OOW 13+00 W 12*00* 11+OOW 10+00 W 9+OOW fttOOW 7+00* 6+OOW 5HJOW 4+OOW 3+QOW 2*00 W 1*00 W 0+00 MM E 2+00 E 3tOOE 4+OOE 5+OOE &+OOE 7+00 E 10*00 E 12+00 E 13+00 E 14+00 E 15+OOE 17*00 E 18*00 E 19*00 E 20+COE 21+00 E 22+00 E 23+OOE 24*00 E 25+OOE 26*00 E 27+00 E 2S+OOE 29+OOEfilter

0=1 3.5 3.6 3.5y 2.7 J.*/ 2.3 3.1 2.7 3.5 3.7 4.1 J.I 6.3 6.5

2.3—-''l.B 2.1 3.1 3.3 3.3 "^ 2.8 X 6,7 X^ 7.3-1 3.1 "2.6

7.1 8.2 7.4 7.5

3.1 3.3- 2.7 —— 3.2- 7.5 B.9 7.7

10 s 5 .4 6.8 4.4 J.2 .2.8.^- 1.7 ^.3.2 4.1- 2.7 5.4 6 5.8, 3.6 4,2^^,4,9 3.8 , 2.5 , 1.7 -1.45.6 7.4 6.3 \ 3 .7 3.! /1.6//3.9 4.7 / 5.3 6.6 5 3.9 4.S./5.6 5.S\ J.3 1.9 1.9.__1J S 2 .8 4.

7^-^sT \ 6.7 5 2.8 1.1^/4.*-^^ /(dy/* ™ M s 2~5 .5.1 6,J 5.8 5 2.7 ^2' 2.3 2.2 \3.4

i.* i .t z .o^- 1. 1

\ 3 .7 3.2 /L6//3.:

5 2^8 2.3.X*-J'X'^-^ \ X v————-"^ STPN, 8.5 S.4 3.3 3.6 ^.5.1 5.6

7 /s s7.9 5.2 |2.8 /e.5/ 8.9^—^7,3 6.5 5.4 ) 4 .7'

3.7 ' 8 .7 7.9' 5.9' 3.5 * 8 .6 7.t '' - I.I

2.4

2.7 4.7 7.8-^-3.5 i

y 3.7 \ 5.9 f 10 \^ 5.4li

.10, 3.1 2.9V 3.4

M 6.3 x 3.5

t,

Z.1 3.1 4

—— 2.9' 3.6 y 5 .5 6.5 5.2

4.2 3.6 -^6.3 6.4 5 4.6 6.5-^2.2 x 1.^ 13

4.6. s . 2.5 2.3 2.8 3.7'\ f

9.3 82 5.3 2.8 2.7y 3.3 -^2.6

4.2 3.7 3.8 4.2 4.B 10 10 j 5 .1 5.2 Ll) 3 ' 4

4.9 - 5.8 V W ^ * I 5 S.8 3.2 3.7 4.4 4.4

F-T t.* J, f JiO

O 3.6 4.5 4.2 4

5 5 —4.8 i.3 -3.9 \ 1,7 -2.8 3.7 3.4 J.3 4.5 4.53.1 4.3 /2.6 .,3.|--v 2.7 2-t 2.3 l 3.7 4.7 f 6 8.7 6.4 7.4

2.3__ 2.4 /J.3 3.3 \-2.9 —— 2.9———3 4.4 j 5.4 7.1 ^~^T~~~~ 7 .7 8.3

2.8 ,l 1.4 \ 2.7 3.8 3.6 3.7 3.8 3.8 5.1 6.4 f 8.2 9.5 8.5 9.1 X 6.1^X1.9 \ 4.2 r" 5.3 ""4.1 4.3 l 6 5.2rrT4.1X 6.11.7 1.8. 3 3.8 4.2 4.1 4.3 4.5 \ 5.7 7.5 9.2 S.8 9 9.6 \ 8.4 0s 2.4) 4.9 6 5.1——5.3 5.1 ^f^0^3.7\ 6.3 6.2 6.4 \ 3.7

3 ^-4.3^ 2.2 12 \3.4 4.4 5 4.8 4.7 4.9 6.8 ' 8.3 9.7^ tt- 9 .7 10 N 7 x 3.4 5.4 6.3 5.7 4.7 -l

5.5 8.2 J.4 4.5

6.7

6.4\3.7 i 5.6 6.6 (.3 6.2 5.8

5.8 7.1\ 4,2 ^ 6 5.* 5.5 7.4 6.1 6. 1 4.4-

filter

0=2

(1=3 11=4 11=50=6

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

14+00 W 13+00 W 12*00 W 11+OOW 10+00 W 9+00 W 8+OOW 6+OOW 5+OOW 4+OOW 3+00 W 2+00 W 1*00 W 0+00 1+00 E 2+00 E 3*ODE 4+00 5+OOE 6*OOE | 7+00 E

filter 6713 7666 8365 7B25 6545 8833 6911 8607 9036

6944

l IK 33K

/"" jf9302 9258 v^ 5200 V 9233 \ 4613

6643 — 7918 ( 11K V \5640 ^ 8076. 3121 201

r^ l 1388 90^- 1744 ~- 3842 663? ^ 2414 ^ 8137 . 3171

0=2 2203 -- 4157

0=3 M72 ^

0=4 16K—— m 11 UK *\ KST*} 6554 J 9476 ifKi it *"./ 0=5 \*'/ SK /.,W~i 8317

0=6

' 6501 -X 8498 l 2172 l"— //isl\ r^\-11K 9674 f 3Ms 6643 — 7918 ( 11Kv N

l——14K //418B mT^t 6554 ) 9476 11116K —— 14K j l 418B ', 8297 l 6554

f t 6081 -^'(*^ S317 8948 S396 9074 3081 —.3376

7678 ^^HK 9891 -^TlT^ 7555 7612 5325 2195

2K 20K I2K 2825 2156 IKK 1630 1679 1573 1453 4538 4231 5818 13K 12K 15K

10K 12K——-121

aH)OE | ; | 10*00 E 11|00 E r | 12+OOE ^ 1 3+COE | 14+ODE ^ ^ 15+OOEm m at 24K 21K ISK lw i* I+K

16400 E | 17*00 E _^ JBtQOE t6314 S886 5371

19+00 E 20+00 E——l———l———F———i———1———t—21+00 E 22+00 E 23+OOE 24*00 E 25KXJE 2WOE 27+00 E 28+OOE 29+OOE

——- 12K ,, 1 759 ^ 1104 e i 4TO 298 341 __342 431~^\\((( ^ \ S\N——-——————HT^'30K)). 274) 2073 1131 V. 676 —- 833 ~L864__882 ((, l///// ' ' ' —————'46K //^4537 -.2608 1497 1?94 ^ 1450 — 1446 —

3711S 1752 ^- 1496 x 2K3 2196^^^2497

4581 225B 1652 S 2566, 3063 3610

— 4106 2691 2011 2838 3527 4654

2896 4241 ^ S794 7727

J551 l SB3 7382 7861

4230 4487 6545 7228 7299

30K V13K I4K 9019 84IB ^- IOK

27K \ 12K(f**n*\ 1 IK ^1*

23K 2K\\ 6722 5752 l 18K ^24K H V\ \ \ \ l

6132 6810

4896 4800

\ \ l \3287 6821 7892

1646 " 2430 3526 ^ inn (

1241 ~~~ ISy, 2475 3454

2289

5223

1232

6067

4053

4131

1669

1382

1135

2103

3518

2183 1694

1767 ^ - e

^

1484

I2K 13K 8722

6017

B7 ~

1150

f" 877 .\2184A

30B5

2713

1062

1709

1259 filter

306 0=1

n=2 0=3 0=4 0=5 0=6

Topo

Interpretation

ChargeabilitymV/V

Interpretation

Resistivityohm/meters

L- 400No •* m

Pole-Dipole Arrayo no Q

wmH

- — On

\ , ' 0 =50*4

^plot point

Filter* n1

* * n2 * * * n3* * * n4

Cont. Intervals Resistivity ; Logarithmic Chargeability ; Logarithmic Metal Factor ;

Profiles


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


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


J Moderately High Effect

50


Scale 1:500060 100 150 200 250 300 JJi" ""i"*-

(meters)

Starfine Mineral hieInduced Polarization Survey

Spanride-1-95 Grid English k Beemer. NTS: 42- A/ SW


^ 14K 2.6.,

IP59Kj

RES l MF 6834J 1.3.

58Kj OJ 0.

Topo

Interpretation

ChargeabilitymV/V

Interpretation

Resistivityohm/meters

.2.6 .UK -60Kl——l——l——l——l——l——l——l——l——f——l——l——l l l——l——l——l

l I I l l l l l t ..l l ----L--l- .J - L.I l l l l J l l l t l l l l l l l l L l J- -l -l———l———i———l———i———l———l———l———l———l———l———l———l———i———l———l———l . l ...J III l l l l———l l l———l———l———l LO u58K

-l——l——l——l——l——l——p——l——l——l——l——l——l——l——l——.——l——l——1- H———i———l———i———l———i———h- ~t———-———l———i———H

4+OOW 2*00 W o+oo 1*00 E j+ooj^ 3+pOE 4+OOE^ 5+03 E | 6+OOE—i——-—i- 7+00 E—i——i——i- *f* E , 9+OOE lOtOOE 11+OOE 12+00 E 13+00 E 14+00 E 16*00 E 17+00 E 1B+OOE 19+00^ 20+OOE —i——i——i- 21-KWE—i—-——t- 23+OOE 24+00 E 25+OOE 26+OOE 27+00 E^ ^ 2StQOE 29+OOE.30

-2.5

6.8 5.5

0=4

0=5

0=6

-5.8^f3.8 xj.3 , 3-'^-' 5.8_-4.9 v 5.8 6.5 5.4

"#?y " 5^7.2 ^ i " /^^\

" -^9.4 7.3 4.6 (2.6 y 3.3,r? ,(,; -^5.8 .-—-4.9 x. 5.8 6.5 ,5.4 3.5 -v^Z.5 2.6 2.5 2.2 2.7 3.6

J.6 \2.7 2.5 2.4 2.9 4.7-" 6.1

4.4 ^.7.5 e.:/ 9.5 \ Mr Sr *A ^ 7.3 4.6 (2.6 J 3 .3 3.5 XT6 2.B 3.1 5.1 7.2-" 8.17.7 l.*/ 1 0 7 8.8 ^ IO/ 8.6 f 5.6 3.7 3.3 i.5 3.8 3.1 3.3 ,5.4 7.8 8.7 8.6 J 5 .2 6.3 6.9 7 V^7,6 5—-^ 5.6 5.7

6.4-^ 10 r *.T,jT\\ 9 .7 7.5 4.7 4.2 3.S 3.8 4 3.6/5.9 /8 9 9 9.2 i y - 3.7 ) 5.8 6.4 6.7 7 6.9 4.7 ~~- 4;9J^; 6 :10 ——9.7-"*'l2 11 ' 8.4 ' 6.3 ^5 4.8 4.2 " SI "~ 5.4 ""1.2 /t.l 9 .2 9.4 9.5 -^5 4.6 3 v 7.4 7 7.S 5.9' -79 *6.7 "—3.S 4.2

i. v\ f i \\.7" TT*- -3.7*-N 6.6 N 1.4 = .80 -.90 x N 7.

3.1 5.2 6.J 5.6 4.7

5 6.3 v 3.5 --^2-3 l Li X-TO * 1.7. 2.6 2,7

6.3 5.4 5.4 7T7-X 6.5 5.4 5.9^-4.5 NjV^-1.7. 1.1

7.2 5.6 6.5 6 \T.lX 6.6 5.9 6.1 4.7 ) 2.6 V^l.1 1.3 ^\ 2 2.4.

5.2 6.3 6.9 " ~

1..8 2,5 3.1 -—2.7 2.5 2.8 2.8 4.2^- 2.6^ ——— 4.7 3.5 i Z.7 f - 9 J z - 5 5-3 7 S 9.7 i 5.4 -2.6 4.9 -.1,9.±^^2,6

1,3.5 2.1.^^2.9^/3.2 4.1 [ 1 f\ VV CT\ \ 3.8 3 3.1 2.1 3.4 V 6.6 7.4 ^^^8 ,J \ 4.8 3.5 4.6 l VS^S//"-^

1.9 \3-8 3.5 3.3 4.4 2.8 —— 3.6V 7.4 \ 3 3.4 3.3 v 2-4^) 3-7 y 5 3 6.3^*^7.4 4.7 3.3 3.2 —— 3.5

2.1\ 4.4 3.9 4.6 2.9^-—————3 v ^~ 3N. 6.8 \. 3. l 3.4 3.3 3.7 j.5^^-5^ 5.7 ^7 v 5.7-^^4.2

4.7.--"Tj 2..9 \ 4.2 .2.7 2.8\ 6.8 \ 3.3 3.2 4 f (^Mfi^ 3.3 __ 4.2 4.2 \ 7.5 6.8 \ 4.5\ 6.2 \4.2 375SiL -2.t"*-"j.J

3, l 6 J,,l

3.7 3.3

3.2 __ 4.4 2.6

3.7 6.9 x 2.5 ^3.5 3.7^——2.5-^^.4! \

f]|ter 4316 5258 6782

638- 1161 — 15470=1

0=2

n=3

n"4

(1=5

n=6

3079 — 3147 — 2901 ^, 4055

5786 ~~ 4674 4412f

7461 S958

8632 I3K

10K

54tB ^2461 ^ 9069 — 81.62

f 'm) 6

- 1062 15J7—— ~^^ -

1767 — 204E — 2517

3293 "~ 4364

4967—4926 — 6544 16K

4826 ^ 3968

3449 ^ 5285 3588

3526 4483 5052 71*1 —

2961 '2754 5158 6472 - 12K

7+00 l 8+OOE 9HQOE 10+00 E 11fOOE J2+QDE 13*00 E 14+00 E 15+OOE 1&+OOE 17+00 E IBtOOE 19*00 E 21+00 E 22+00 E Z3+OOE 24+OOE 25+OOE 26+OOE 27+00 E 2B+OOE 29+00 E7886

3597

11K

9438

W21 V 879-\ r-N\ 9177 f 3972

UK

2976

17K

*\JZ11KVV,33K

13K'^36K ^ 19K

s-t 13K IlK-s. 8154 -^.IIK t in ia,i ,

14K \ I 5800 \ 14K , 6799 ™\\\ \\L

14K 13K

4727 -^ 21

Sis' 9533 ^ 5362

10K

904-

7947

1159

6244

3076

2391

5114 9052 U15 75*7

3937 ~ 6643 ^ 2212 , 17633^)//^-^;

1497 , U I4K -^Jvm\ i ^

5537 4737 4420 4360 3783 4359 4071 3996 2178

^\3565

4894 7954 \ 13K\ xC4455 5490 6884 12K

9347

9771

. l\

T^^T ^: m -) ^vS\\\vrp^\ - ?l ISrO 8H7 iTT^- 80M C" 2075 1 936 f 3784 -.2551 A 12* \ B10D Mtli (S^r™' r^^v I pT^^^V- 74

10K———"10K A 32K V X|7K\ 29K V 12K ^ 3215 4521 ^8456 ^^^T 21K \ *" \ 1fY..N \ .l v\S^ ^xNJi16K— 13K

\ \ \ X \ X.\"\"V X ^.—^10K A 32K , \ I7K \ 29K X 12K X; 3215

r^^VV 3^^ 3797 SS97 8415

1786 2538 5720

3185 3628 3446

3392 — 3045 3587 4129

1820

s- IW-^ 3723 1332

6551 j 1 148//y/ , ^

6237 s 1 581 1153 2330} l (f X 11,

7660/2206 1551 — 162? ( 41465285 3239 3526 4856 "3314 ^2424 2003 —' 2598

14K V 5261 2891 4878 , 2056 " 3548 2948 — 2835 ^. 3227

S721 14K^ 4941 3728 2179 2245 3952 4043 3560 35322432

11=1

0=2

0=4 0=5 0=6

Topo

Interpretation

Chargeability mV/V

Interpretation


L- SOON o in m

Pole-Dipole Arrayno

' —— On

0=501^1

Profiles

plot point

Riter* n1

* * n2* * * n3

* * * * n4

Coni. Intervals Resistivity ; Logarithmic Chargeability ; Logarithmic Metal Factor ;


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


INTERPRETATION

r*•*tCOH

M

O O

50

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



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

Scale 1 :500050 1 QQ 150 200 250 300a-"* ""c

(meters)

Wneral IncInduced Polarization Survey

Spanride-1-95 Grid English A Beemer. NTS: 42- A/ SW


5.9., 24K n 2.1,

IP 1 RES! MF

12K.J 1.

O- oJ 0.

Topo

Interpretation

Chargeability

Interpretation

T——T

: : /--^: : V ' ' ' ' . ' ' ' ' ' ' . ' ' ' " ; " " ' ' ' ' ' : ' ' ' " ' ' ' . 1 ' ' ' ' '

^-'""""""---i. -----^ ,--'"/- ~~'**/^**^ f-~~** " ---,----" i\ 7 \ ^--'"' : : : !

^\ :/^ A.^ ..... ....................y...\^.....\ :^-- : *^ : : 7

- ———— - ~-X^~' - . ^ ———— - -V - - - - - - - ; - - - - -7 ; - - - - - - - ; - - -

r24K P5.9

MF f RES*-IP

.1 J.12K

.o Lo

2400 W 1+00 W 0+00 5*ME 17' a)E IftOOE 19+00 E 2MQ E

4 - B *- 3filter 4

n-1 J.6^ -~^ 5.4 -^. \1 -1.9 i t\ l \\ N. J f

n=2 l 'W— -3.8 ^03.4=^3.5

3.2 2.S

^ 6.4 6.8 )\

J\ 6.9 (^

s - 4 s- 2 5-* 4- 5 4- T 4- 3 2.4 3.7 3.9 3.95 - 8 5- 8 s-2 5-*3.5 2.8 2.3 3.1 3.6 4.3 lî^^x'

?TN^j —— j.1 4,T^-4 X I M-^T^KS4,2 \ S.B/ 6,1 8.8 87^s-4.6y\2,7\ 4

. 4\ 1,3 M fT^^VM [

.5 j 6.8 B.' . - ^^^ . ^r*

filter

n=2

n-3

Resistivity nôhm/meters n^5

3+OOW 2+OOW 1+00 W 0+00 1+00 E 2*00 E 3+OOE 4+OOE 5+OOEi——t——i——i——i——i————p——i——i——i——i——i——i——t——i——i——i——i——i——i——i——i——i——i——i——t——i——i——i——i——i——i——i——i——i——i——i——i—23K 13K 21K BS64 9113 9225 8568 12K 12K 9994 11K KM 8616 8242 11K J3K J1K 3CK 26K 21K

7*00 E WXE ^ÔOE 10*00 E 12+00 E 13*00 E 14+00 E 15*00 E 16+00 E 17+00 E 18*00 E 1J+OOE 20+00 E

38K

1JK 17K 16K 12K 8753 8171 S532 6106 3631 53B4 5S75 7015 5086 7745 J7K J3K 28K 17K 10K 7310 14K 13K 10K 6339 5608 3671 5208 1440 2238 885 fj|ter

10K

Topo

Interpretation

Chargeability mV/V

Interpretation

n-3

nm± Resistivity n-5 ohm/meters na6

L- SOONo vo m

Pole-Dipole Arrayna

Vplot point

Filter .* n1

* * n2* * * n3

* * * * n4

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


1760mSec Total (ntergration Time, 80mS Delay. T* ( 80+80+80+80+160+160+160+320+320+320 ) mSec

Scintrex T50-3 Transmitter BSecond Total Duty Cycle, 2Sec On/Off Time.

INTERPRETATION

M** CO H

n

o o

4 fi

J Low Effect~* Poorly Chargeable mV/V, IP effect

Low Apparent Resistivity, rho

50



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

Scale 1:500050 100 150 200 250 300

J ,.S (maters)

Starfire Mineral IncInduced Polarization Survey


Porcupine Mining DivisionGeoserve Canada Inc________Sept. 97.

58K- 11K-, 1.3.,

\

tp58KJ

RES MF 5380-j .63.

58KJ OJ O,

Topo

Interpretation

Chargeability

Interpretation


MF RES ..63 [.5380

i

4+OOW 3+OOW 2+00 W 1+OOW 1+00 E 2+00 E 3+OOE 4+OOE 5+OOE 6+OOE 7*00 E 8+OQE 9+00 E 10*03 E 11+00 E. 12+00 E 1J*00 E 14+00 E 15*00 E 16+00 E 17+00 E 18+00 E 19+00 E 20+00 E

filter

n-1 2.6 2.5

0=2 3 2.9

0=3 Tl ~

2^/ 3 - 5 2- e 2' 1 2' 2 2'3y *' 5 --^. *

3.5 3.8 3.7 4.J 3.4 ^ 2.6 2.7 X' 3.7 3.9

4.2 4.6 4.3 4.8 3.8 \ 2.7 J 3 .4 3.3

5.4 4.4 3.2

\

3.8 3.9 v5.8 4.9- 5.7 ^^ 7.6 8.6

\ "NV ~ J

"\ \0=4 3.9 3.8 f,.l ^ 5.^4.7 i 5 -*\ Jt8 J-3 3-3 3-' M \ ™ \ ** ^ e - 6 5.3 " 5.2 5.4

0=5 4 4.6 \ 5.4 5.4V 4.8 j 5.5"-- 4.8 3.1 3.7 J.I 2.4. \ 6.3 \ 9.J ^6.9 S .t 6 6.2 5.4 6.7

0=6 4.7 4.8 5.8 5.7 5.1 6.4 * 4.3 3.9 4.3 3.8 3.4 \ 7 9.8 7.5 6.7 6.5 5.9 5.6 5.9 5

3.8\

.X^ N 4.

4.2 3.8 -2.4 2.6

4.9 4.7 2.8 2.8

4.9.—— 4.7 J.I 3.8

2.5 3 5.1 - j, 1 1 ^—-1 7 .8 xr-^1 -MA 1.5^^^2.1 2,4 2.2 2.6 i t 6.4.8,__a.7^-^3 7 10 /V^iTTV\ 8.3 a- 3 N^i' - 1.Z\ i-i 2.S,^--3.3 4.9 ^^4.3^^-^6,5

•-'f*^**- *-*^S~* . .\\. r B.i^X^-.IO S ; 1.l 1.2 A 2.8^ i.B 4.B 3.1 ________

LI S.Z-^VviS I -^ '.-2 1.5\ 3.4 (5.Z 3

. J.4

Z.5

3.3 2.2 3.2

filtern-1

n-2

n-4

2.3 n-5

2.7 n-6

4*OOWfilter "" 78a M 11

0=1 24*5__2J43 — 27(0 — 1815 —781

0-2 SOW

n-3

n-5

3+00 W 2+00 W 1+00 W——t———i———l———i———l———————l———i———4———i

8272 (747 tOK 9779 81

0*00 1+00 E 2*00 E WME 4+OOE 5+OOE 6*OOE 7+00 E &+OOE 10+00 E 11+OOE 12+00 E 13+00 E 14+00 E 15+00 E 16+OOE 17+00 E 18+00 E 19+00 E 20+00 E

5217 4223 8003 9982

-902 ^ 2949.

11K 12K

B511 ^ 3807 5~ 1JS7 ^ t937 — 1933 2746 — J590 -s 2S62 ^- 4066 4650 7527 3733 5*33

8751 ^ 8806 7867 —. 52B4

N 71S3 9011

7766 9435

8862 10K 9012 7514 6640 8730 7937 10K B7S2 72J2 559B S571 9349 13K

534.7 3W1 7765

m 14K

9200 7874

.3144 683J

9435 \ 5047 9899

^ 6724^ 1.

9864 8548 8140 11K

— 3742 f 71171 -^ 2BJ5 — 3176 44*7 ^, 3090

filtern-1 n-2

n-3

n-5

n-6

IP L58K

.0 LO L58K

Topo

Interpretation

Chargeability mV/V

Interpretation


L- 1000N

Pole-Dipole Arrayna

0=501*1

Vplot point

Filter* n1

* * n2* * * n3

* * * * n4

Coni. Intervals Resistivity ; Logarithmic Chargeability ; Logarithmic Metal Factor ;

Profiles


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


INTERPRETATIONLow EffectPoorly Chargeable rrMN, I P effectLow Apparent Resistivrty, rho



50


Scale 1:500050 100 150 200 250 300iZ-----^^SZ----5!fiS5i

(maters)

StarSre Mineral IncInduced Polarization Survey


Porcupine Mining DivisionGeoserve Canada Inc _______Sept. 97.

o t~M

o o

15K- 1.1.

IP RES 7305.

58Kj

Topo

Interpretation

Chargeability mVA

Interpretation


MF .55.

oJ oJ

MF .55

RES .7305

LO

4400W 1+QW Q+O 2+oaE 3+OOE 44QOE 7+00 E 6400 E 10+00 E II+OOE 1 2+00 E 15+00 E 14+00 E 15+00 E 16*00 E 17+00 E 18+00 E

filter ^^^^i*K^^^^58K5IK5BK5BKS8K58K58KS8X5SK58KS8K58K58KJ8K58K58K58KSBKi^ filter

n-1 1.6 x *-2 3.5 v 1.9 i 1.3 , 3 .B , 5.9- 4 4.4 vi.S I.I s. -8.1 4.1 5.7 7.8 7.5 7.7^ -O-8 s^ 3.9 2.4 2.8 N^. .80 j^s. 3.8 3.5v v^.90^ .90 .90 v 1.8 -^2.6 y 3.9 -B- 6.1 , 4 .1.i . F . 7 -1-9 4.7 3.8 . 7-2.3

4.B 4.5^v.2.4 3.1 3.7

. . . . . . . .

.31 4.8 i^T^X 3.7 4.4 \^ 1.7 \ 2.9 V 7.2 5.1 t.t

n-4

n=5

n-6

... .

3.7 5.3 4.9 2.9-J J.3

3.4 5.6

4.A 6.) 6.3

j5.1 2 .1

. 4 .3y 5.902.5 . . . .

^~^~ 3 4.9 5.8 *y 2.7 \ 4.2 \B.4

5.1 3. B 5.4 8.4- 3.2 4.4 \

x- . . v . -^. f . -- . j

3.9 \\ MS. .90 .. .K — "'.' J-' 5.3— -4,5 4.

.

2.8 j '

1.9 3.1 3.3^ 1.4 1.5 j 2.* 2.8 3.9 3. B 3 4.5 4.2 n-1

2.3 2.8 3.8 J.8\\1.3 \ 2 2.2 V.3.7 4.5 4.4 4.4 4.7 n"2

3.8X1.6 '-— \ 4' 2 s-'"*" S^TN 4.1 0=32,9 —— '3,1 3.9

8.8

, , . . —^^ '

5^5.1 1.3 \ J.3 3.3 4.2 4.7\^2.1 2.5 2.4\ 4.6 6,1

* *- 9 5- B \ 3 p- 3'* 3' 3 *' B 5'3 \ 2' 8 /T2-~-^-J S.3 5.4

S.I 5.6 6.1- J.S^- 3.9 4.3 ' 5.8 5.9 2.6^~- 3.4 4.3 ^-5.2

n-4

n-5

n-6

4+00 W 3+OOW 24COW 1+OOW CWM 1+00 E 2+00 E 5+OOE 4+OOE 5+OOE e+OOE 7+00 E 8+OOE 9+OOE 10+00 E 11+00 E 12+OOE 13+00 E

filter

0=2

0=4

0=6

12K 12K 10K 7124 8319 7571 6199 9239 8049 6424 11K 9709 16K 20K 24K 19K

\SRlU C /- 8'77/ 2930- 3949 -^629^ 544^^7229^^2142^^1* 9732 8712,^1840

14K 23K

1JK-, SJSJ ^ .,,^

895 A\ 16K^^llKX" 275?\ft f—XN

1032 U 26K \1

1631 '.vX 26K Nv\XJ. 447k ^X""" v

3977 ^ - iBK^WTs^A-^6K~ 20*^ 6299 ' 2609

B549 7052 5353 7789 11K

770-^28*3 28*3 3392 — 4104 .

1IK 4492 2881 3922 7433 9356 8813

14+00 E 15+00 E 16*00 E 17+00 E 18+00 E

9455 7712 5596 6855 7216 8984 9909 8051 27K fj|{er

S447iUX 48K 0=11133 ^ 4202 ^2942

1488 1374 1327 ^ 6854 —

N^^\r TN^ X mh'i"^*"M- — 1519

24K^?x* 18^8 — 2197 "J35T;* 9lfl5 ^^^ ^^.x rn -^ 27K 2*-^^* 2487 2742 ' 1398 *^ f2K

10K

n-3n^4

o-5

n-6

IP (-58K

Lo .58K

Topo

Interpretation

Chargeability mV/V

Interpretation

Resistivityohm/rneters

L- 1200N

Pole-Dipole Arrayna

0=50*1

Vplot point

Filter* n1

* * n2* * * n3

* * * * n4

Cant. Intervals Profiles Resistivity ; Logarithmic — — — — Chargeability ; Logarithmic Metal Factor ; ——————


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


INTERPRETATION

T Low Apparent Resistivity, rho

Moderately Low IP Effect (mV/V)


High EffectGood Chargeability mV/V, IP effect

Scale 1:500050 O 50 100 150 200 250 300————-J " "- ' ———

(maters)

StarBre Mineral bicInduced Polarization Survey

Spanride-1-95 Grid English b Beemer, NTS: 42- A/ SW

Porcupine Mining Division Geoserve Canada Inc_______Sept. 97.

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rpt of work on the spanride prop...loodb, other .-anti-alias, rf and spike rejection. internal test...

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