i geophysical sulvey i interpretation...i i .403 i ~uantec geoscience ltd. i i geophysical sulvey i...

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I ~uantec Geoscience Ltd. I I Geophysical SUlVey I Interpretation Report I

Quantec Geoscience Ltd.

5825 King Street Porcupine, ON PON 1 CO

Phone (705) 235-2 166

Fax (705) 235-2255

.1 :1 I

I I I I I I I I I I

Regarding the BOREHOLE TRAN.SIENT EL,ECTROMAGNETIC SURVEYS over the KAMISKOTIA PROJEC7; near Timmins~ ON, onbehaHof CLAIM POST RESOURCES INC. Toronto~ ON

•

RECE\VED

GEOSCIENCE ASSESSMENT OFFICE

S.T: Coulson January 2009

Project CA00626C

537liOOON

5374000N

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42464~ I I , I

4209598

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General Information and limitations Contact Infom'l atJ'on : Provincial Mini09 RKOfdera' Oflioo

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452000E

Toll Free Map Datum: NAD 83 Tol: 1 (BBB) 415-11845 o1ll57l'lbjodion: UTM (6 dog-l

4209591

Tho .. wi"'ng to 5take mln£ng clalml should consult ~th the ProvindQI Mining Recorders' OMu of the Mlnillry ot Northern Dovelopment and Mines (or additional itlfofl1ultion on the ttlitu. oftha 'anda "'awn hereon. Thl .. map is nollntonded for nalAgatlonal, -.uvey. or land tiUI!t determination purpo6es as the InformaUan &;hown on this map 1& complritd from various sources. Completeness and acruracy ar. not guaranteed. Additlonallnfonnatlon may also be obtained through the I(leal Land Titles or Reo1llry Office. or tho Ministry ot Natural Resources. fax: , (877) 670-1444 TopographIc Data SOurce: Land tntonnaUon Ontarto

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Tho In(ann_t!on &hown Is dertved trom drQtt&J data available in the Provincial Mining Recordors' Office at the tfme ot downlosdlng trom the Minllby of Northern Development and Mines web efte.

WiIIM. Green Miller Centre 933 Ram.tey Lake Road Sudbury ON P3E 68S Mining Land Tenu.re Source: Provinaol Mining Recorders' otftee

Thta map may nOl illhow unreghsl erod land tenure ond interests In land Indudlng certain polenta, 1 . .. _ , easement .. right of ways, ftoodlng right Ifcenc:es, or Olher forms ot dlspostion ot rights and i"t&rest from the Crown. AlI50 OItftaln 'and tenure and lend UN. that retitrlct or prohibIt t oe entty to &take minIng dalm. may not be Illustrated. Harne Page: WNW.mndm.gov.on.ca1MNOM~INESIlANOSImlsmnpge.htm

ONT. 10 CANADA

MINISTRY Of NORTHERN D£VElOPMfltT AND MINES

PROVINCIAL MINING RECORDER'S OFFice

Date I TIme of ,"sue: Mon Dec 2913:22:32 EST 2008

TOWNSHIP I AREA TURNBULL

Mining Land Tenure Map

PLAN G-3250

ADMINISTRATIVE DISTRICTS I DIVISIONS

Mining Division

Land Titles/Registry Division

Ministry 01 Natural Resources District

TOPOGRAPHIC

r~

Conceq,loo. Lol

o Provtndsl Pn

CIII. F'It&PIor

" Road

rllli

+

&caN , :21"1

lOOm Om

CLAIMS WORKED

Porcupine

COCHRANE

TIMMINS

land Tenure

EI U ... .... ~ [!] Surt.ce And. MInIng Righta

m Su~ Righta Only EI _ RIQhIO OrO,

EJ u..t u" Poml.! EJ Onlor In CouOd! (l*i q>un for ,~) EJ W~ Powc lMM Agt'Iernn; ,--------j : 1234S67 :

---------.-- ------j L __ i~~_J LAND TENURE WITHDRAWALS

~ w.m Ws w'" w"mn woo WOm

AreI:I wrh*1!wn from Diapodlon _ _ _ .ar r,...

S..c.t.thlllIlinitlg Al~'MhImm s..-_aory_ --"""-""""In CoundI_rypn -"""-----"",-.on - "-"""-

IMPORTANT NOTICES

... m

Ns FLtGrf(T L I N IE C

I I I I I I I I I I I I I I I I I I I

QUANTEC GEOSCIENCE LTD. Borehole TEM Surveys

CLAIM POST RESOURCES INC. Kamiskotia Project

1. INTRODUCTION ................... ................................................................................................................... 3

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

2.1 LOCATION ... ..... .... .. ........ .. ... ..... ... .. .... .. .... .. .... .. .. .. ..... ..... ............... .. ... ........ ..... .. .... .. ..... .... .. ... ... .. ... .. 4 2.2 ACCESS ......... ............. .. ..... .. .... ...... .. ........ .. ... .. .. ..... ..... ..... .. .. .. " .. " .... " .... " ... ..... ............ ........... .. ... .. 5 2.3 SURVEY GRID ..................... ................... " ......... ... .. ....... .................... .. ...... . , ........ .... .. ..... .. ............ . 5

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

3.1 GENERALITIES ............ .... ... ....... ........... ...... .. .. .. .... ............. ... ......... ... ..... .... .. ' '''''''''''' '''''' ''' .. .. ........ 6 3.2 PERSONNEL .............. ... .. ... .. ................. ............ .. ....... ....... .. ..... .... ....... ..... .. ... ... ... ............. .. .... .. ...... '6 3.3 SUR.VEY SPECiFiCATIONS .... ...... .... .................................... .. .... , .. ..... .. " "" """" ........ .... .. ... .. ............ 6 3.4 SURVEY COVERAGE ........... .... .. .......... .. .... ... .. .. "'" '"'''''''' .. .. ........ .. ................ .... ...... ....................... 6 3.5 INSTRUMENTATION ..... ........ , ............................................... ... " ...... ...... ... """"" """""""" .. ........... 6 3.6 SURVEY PARAMETERS .... ........ ..................................................... " ...... .. , .... , ..... ............................ 7 3.7 MEASUREMENT ACCURACY AND REPEATABILITy ...................... ........... .. .... . "'"'''' ................. .. ......... 7 3.8 DATA PRESENTATION ............. .... ................................ ....... ............... .... ... ............................ ........... 7

4. SURVEY RESUL TS ... .. .. ........................................................................... ............................................... 9

5. CONCLUSIONS AND RECOMMENDATIONS .................................................................................. 11

LIST OF APPENDICE

APPENDIX A: Statement of Qualifications APPENDIX B: Theoretica. Basis and Survey Procedures APPENDIX C: Instrument specifications APPENDIX D: Production log APPENDIX E: List of Maps APPENDIX F: Profiles

Figure 1: General Location of the Kamiskotia Project.. ...... ......... .. .. ............................... .. ..... .. ...... .. ........ 4 Figure 2: 4-Axis Borehole TEM Profile :=ormat ......... .. .............. ..... ... .. ................... .. .............................. . 8

Table I: Borehole TEM Survey Coverage ..... .. .... ........ .. ...... ..... .... .... ..... .......... .... .................................... 6 Table 11: System Parameters for Borehole TEM Survey .. ...... .. ..... .. ... .. ........... .. ...... ............... .. .............. .7 Table 1\1 : Coil Conventions for Borehole TEM Survey .... ....... ............. .. .. .... , .................................. ........ 7

CA00626C - January 2009 ii



• QGL Project No:

• Project Name:

• Survey Period:

• Survey Type:

• Client:

• Client Address

• Representatives:

• Objectives:

CLAIM POST RESOURCES INC.

CA00626C

Kamiskotia Project

December 101h, 2008 to January 24th, 2009

Borehole Transient EM


55 University Avenue Toronto, ON rv15J 2H7

Charles Gryba

Kamiskotia Project

The objective of the borehole TEM survey is to determine the extent of sulphide min-eralization intersected in drill holes and the existence of other conductive mineraliza-tiol') up to 50 meters radius of the holes.

• Survey Type: Interpretation

CA00626C - January 2009 3


QUANTEC GEOSCIENCE L TO. Borehole TEM Surveys


:2. GENERAL SURVEY DETAIL=S _______________ ~~~ ___ ____'

2.1 LOCATION

• Township:

• Province:

• Country:

• Nearest Settlement:

• NTS Map Reference #:

rs Al 15

Turnbull

Ontario

Canada

Timmins

42A112

h



2.2 ACCESS

• Base of Operations:

• Mode of Access:

2.3 SURVEY GRID

• Coordinate Reference System:

• Established:

• Line Direction:

• Line Separation:

• Station Interval:

• Method of Chaining:

• Claims Surveyed:

CA00626C January 2009


QGL office, Porcupine, ON

Truck to holes

UTM Reference NAD83

na

na

na

na

na

4206321,4212440,4246165

5



3.1 GENERALITIES

• Survey Dates:

• Survey Period:

• Survey Days (read time):

• Standby Days:

• Survey Coverage:

3.2 PERSONNEL

• Project Supervisor:

• Project Managers

• Technicians:

3.3 SURVEY SPECIFICATIONS

• Configuration:

• Output Power Stage:

• Dimension:

• Loop Sizes and Locations:

• Sampling Interval:

3.4 SURVEY COVERAGE

Hole # Collar (NAD83) CPOB-09 450130E, 5376230N CP08-10 451426E 5375616N CP08-11 451320E,5375590N


December 10th , 2008 to January 24th , 2009

6 days

6

o

883m

Woody Coulson, Porcupine, ON

Woody Coulson, Porcupine, ON

Nick Hnotchuk, Timmins, ON

Borehole Profiling

Low Power

3 Component (X,Y and Z)

200m x 200m

5 and 10 meters

AzlDip Start End Total 1m) 166°/_45° 130 509 379 270°/-45° 50 285 235 90°/_60° 40 274 234

Table I: Borehole TEM Survey Coverage

3.5 INSTRUMENTATION

• Receiver: Geonics Digital Protem 30 channel capability

• Coils: BH43-3D Probe (100 m2 effective area)

• Transmitter: Geonics EM-57 (1.8 kW output)

CA00626C - January 2009




• Power Supply: Honda EU2000 motor generator (60Hz)

3.6 SURVEY PARAMETERS

Pulse repetition frequency: 30Hz Gain: 2-5 Integration number: 15 sec Loop Size: 200m x 200m Current: 15 Amps Tum-off time: 4751.1s Receiver Delav -801ls Gate positions 8-61361.1s (see Appendix C) Synchronization mode: Crystal

Table II: System Parameters for Borehole TEM Survev

• Coil Conventions: (see Appendix C) COMPONENT COIL ORIENTATION

Z Positive Axiallv Up X Positive Orthogonal Up along DDH azimuth

(north) y Positive Orthogonal Horizontal and left of

DDH axis (west)

Table III: Coil Conventions for Borehole TEM Survey

• Measured Parameters: dB/dt, mV.

• Data Reduction 1: nanoVolts/metre2 (nV/m2)

3.7 MEASUREMENT ACCURACY AND REPEATABILITY

• Number of Repeats per Station: 0-1

• Number of Repeats per Day: 0-3

• Average Repeatability: 1-2% in early channels

• Worst Repeatability: 3% in early channels

3.8 DATA PRESENTATION

• Profiles: X,Y,Z components, and Total EM Field 4-axis and linlog profiles @ 1 :2500 scale with variable vertical (profile) scales to best display data.

1 Equivalent to Crone units of nanoTesla/second normalized to a unit current.

CAO0626C - January 2009 7

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Borehole CP08-l0 - Z Component

Scale 1 :2000 25 25 50 70

(metr .. ,

ClAIM POST RESOURCES INC. KAMISKOTIA PROPERTY

TIMMINS. ON

3D FIXED - '.OOP BOREHOLE TEM SURVEY

Secondocy Electromognebc Field (dB/dt)

Tronsm;\\~ r rn: quem:)I; ~o 11 : (~ dIJ\y er t le) h loop Sill!': 2001"1"1 }( 100m

h Loop LocotiOll: 275E - 47SE:5t6N- 716N

TrO'"*3rnitle ,- Cutrent: 1!:1 Amps

h lu rn-Off -llf'fl& and Rx Deloy: 465 us _ - SO u~

BorehOle l oca tion : 451 4Z6E . 5J 756 16N

Borllhole Azimu th , Dip: 266 . -4 5

StOlion Inle,...,ol; 5 - 10 me lers

Profile- Unit'S nonQvon/rTY2

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The objective of the drilling in Turnbull Twp. was to test the source of airborne conductors #2 and #4 outlined in the Fugro Airborne Surveys report of March 2007. Borehole TEM surveys were carried out in three (3) drill holes CP08-09, 10 and 11. Separate transmit loops were positioned for each hole to provide optimum coupling with the expected targets. Details concerning the bedrock geology and the full extent of exploration on the property are limited by the present author and, as such, this interpretation is based solely on the TEM survey results . Maxwel12 modeling of the TEM results has been conducted to assist in determining conductor size, depth, dip, orientation and conductivity thickness . These results are presented as 3D models. All locations are based on the collar locations referenced to UTM NAD83.

Hole CP08-09

The objective of the drill hole 09 was to test airborne target #2 outlined by Fugro in report. The hole was logged from a single 200m x 200m transmit loop centred over the drill collar. The hole was actu-ally logged 3 times due to extensions of the drill hole. Upon completion of the first logging pass to 320m, which was short of the bottom of the hole at 365m due to a blockage, the TEM results indicated a building response suggesting a possible conductor beyond the end of the hole. In additior, sulphides encountered in the core at the end of the hole supported this theory. The hole was subsequently deepened to 425m and re-Iogged ; but again the TEM response was strong at the end of the hole and indicated the hole was close to the centre of the conductor. The hole was deepened a second time to 506m. The subsequent TEM log indicated the hole was past the conductor.

The TEM results were modeled with Maxwell to determine conductor parameters . The complete TEM log of the hole outlined two (2) responses; an off-hole conductor at 170m and an in-hole conductor from 41 Om to 4 70m. Based on modeling, the off-hole conductor at ... 70m is located below (down dip and right (west) of the drill hole approximately 100m. The model utilized a plate measuring 150m strike extent by 100m depth extent, dipping NNE at 47° and having a conductance of 150 Siemens. The centre of the plate is located approximately 195m vertically below 450070E, 5376187N. This is interpreted as the possi-ble source of airborne target #2.

The in-hole conductor located between 410m and 470m is interpreted as a conductor package comprised of several parallel conductors. Evidence of extensive sulphide mineralization in the core corre-sponds to this conductor. Modeling of the response utilized plates measuring 200m strike extent by 140m depth extent, dipping NW at 62° and having a conductance of 200 Siemens. The hole appears to have penetrated the celltre of the conductor and is interpreted to continue up and down dip and along strike in both directions .

Holes CP08-10 and 11:

The objective of hoie 10 was to test the source of airborne target #4 outlined in the Fugro report. The hole was logged from a single 200m by 200m transmit loop positioned to couple with a shallow east dipping conductor. The response obtained from the TEM survey outlined a strong (20 channel) off-hole conductor at 70 in the drill hole. Based on modeling, it was determined that the hole passed over the con-ductor, which lies below (down dip) and sub-parallel to the hole (see model at the back of the report). The Maxwell model utilized a plate measuring 60m strike extent by 190m depth extent, dipping 68° WNW and having a conductance of 500 Siemens. The interpreted centre cif the conductor is located at -116m verti-cally below 451360E, 5375578N.

Based on these results, hole 11 , dipping east, was recommendeo to test the source of this conduc-

2 Maxwell 4.9.25 Forward/Inverse Modeling, Presentation and Visualization software develoDed by Electromagnetic Imaging Technology, Australia

CA00626C - January 2009 9

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tor. The TEM results indicate the hole penetrated the centre portion of the conductor at -105m in the hole. Evidence of sulphides in the core correspond to this conductor. The TEM results of hole 11 were imported directly into the Maxwell model of hole 10. Although the model and field responses don't match perfectly, the overall character does, confirming this to the be the source of the off-hole conductor in hole 10.

In addition to the above in-hole response, a moderate to strong. off-response was detected at 255m in the hole 11. The source is interpreted as small surface area conductor located below (down dip) the drill hole. Modeling with Maxwell utilized a BOm by 50m plate dipping 70° to the west and having con-ductance of 100 Siemens. The interpreted centre of the conductor is located -250m vertically below 451425E,53755BON.

CA00626C - January 2009 10

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The borehole TEM surveys were successful in guiding the drill program at Kamiskotia . Based on the results of hole CP08-09, the source of airborne conductor #2 remains unexplained but is assumed to have been detected by the borehole TEM survey (off-hole conductor at 170m). Should it be considered geologically favourable, consideration should be given to drill testing tris off-hole conductor at the following location:

Collar Location: Azimuth : Dip:

450090E, 5376300N 1900

_600

In addition, the TEM results indicate the hole tested the centre region of an unexpected, large area, strong conductor much deeper ir the hole (450m). Follow-up drilling may be warranted should assay re-sults prove favourable.

The borehole TEM survey of hole CP08-1 0 was successful in detecting a strong off-hole conductor at 70m in the drill hole, the probable source of airborne conductor #4. The follow-up hole, CP08-11 was successful in testing the source of this conductor in the drill hole as seen by the strong in-hole response at -105m . In addition, a moderate to strong, small area, off-hole conductor was detected at 255m in the hole. Should this conductor be significant, follow-up drUling may be considered.

CA00626C - January 2009 11

ESPECTFULL Y SUBMITTED TEC GEOSCIENCE LTD.

S.T. Coulson, P.Geo. Senior Geophysicist



STATEMENT OF QUALIFICATIONS

I, Sherwood T. Coulson, hereby declare that:


1. I am a consulting geophysicist with residence ir Porcupine, Ontario and am presently employed in this capacity witr Quantec Geoscience Inc. of Porcupine, Ontario.

2. I am a graduate of Cambrian Col,ege, Sudbury, Ontario in 1974 with an Honours Diploma in Geophysical Engi-neering Technology.

3. I am a practicing member of the Association of Professional Geoscientists of Ontario (Member #0944) since 2003.

4. I have practiced my profession in Europe and North and South America continuously since graduation.

5. I am a member of the Canadian Society of Exploration Geophysicists and the Prospectors and Developers As-sociation.

6. I have no interest nor do I expect to receive any interest, direct or indirect, in the properties or securities of CLAIM POST RESOURCES INC.

7. I supervised the survey execution and reviewed the data as it was collected. I am the author of this report and I interpreted the data . The statements made by me represent my best opinion and judgment based on the infor-mation available to me at the time of the writing.

Porcupine, ON

~-r-Janua'Y U S.T. Coulson, P.Geo. Senior Geophysicist


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THEORETICAL BASIS AND SURVEY PROCEDURES

TEM SURFACE AND BOREHOLE PROFILING


TEM profiling is conducted on lines either adjacent to (Off-Loop mode) or surrounded by (In-Loop mode) a large fixed rectangular transmit loop. Current is passed through the loop which following the Turn-Off, produces a primary magnetic field (H) both inside and outside (Figure 81), This primary field induces vortex current patterns, which energize conductors and which in turn create their own secondary magnetic field (8s). The rate of change of the decaying secondary magnetic flux (d8sJdt) is measured as the vertical (Hz), in-line horizontal (Hx) and/or cross line horizontal (Hy) vector components on surface using an air-c.ore sensor coil. These measurements of the TEM decay (20 log-time slices) are taken during the "Off-Time", using a 30 cycle/sec, base repetition rate.

In keeping with the industry standard, the primary field is always considered positive up inside the loop and negative down outside . Similarly, for secondary EM fields, the receiver coil is oriented positive vertical up for the Hz component. The convention for In-Loop surveys, has the in-line component, Hx oriented either positive east (for grid EW lines) or north (for grid NS lines). The Off-Loop survey convention differs, with the receiver coil orientation for Hx pointing positive away from the transmit loop (for EW or NS lines). Finally, the sign convention in all cases, has the Hy component pOinting positive orthogonal to the left of the Hx, according to the right-hand-rule.


Primary Field Sign Convention

- ---- - ---'.//./ / / ------ .-' -/// / / --~---'---/// / / 1 / - - - ----------/// / / / / .-----/////// I - - . - _ .----- / .//,/,/,/ / / - --- -//// // // - ------//////// - - - .-// / / / //// / ~--///// / /////

.--.--// // / / //// /

Figure 81: Primary field sign convention for TEM surveys.



Grid N

! Off-Loop

,--r-:::.:::::::=-'Survey Lines +Hz=up

Fixed Off-Loop Survey Configuration +Hx=Grid South (away from loop)


+Hy=Grid East

Figure 82: Loop Configuration and Polarity Conventions for Off-Loop Profiling Surveys

The borehole survey is particulany useful to detennine the geometrical relationship between a conductor or a complex swarm of conductors around the drill hole. Of particular importance is its application in cases where the drilling is believed to have missed the target of interest. A 3-D borehole survey can effectively detennine the direc-tion and distance from the drill hole to the conductor by measuring two orthogonal secondary field components in addition to the axial component. Additionally, conductors located below the end of a drill hole, which either may be too deep and/or have gone previously undetected from surface, may be discovered during the course of a borehole survey.

The probe is manually lowered down the borehole at the end of a cable and, at successive depths, moas-urements of three (3-~) orthogonal components of the TEM field (Hx, Hy, Hz) are individually obtained in succes-sion by electronically switching the sensor coils in the borehole antenna through the use of a relay/switching system from surface, via the borehole-cable shield. As the probe is free to rotate on its vertical axis, a correction is later applied to the 3-D data in order to rotate the components into their respective coordinate axis.

Tx Loop

DDH

Y +ve left, orthogonal to .::--. station hole and horizontal __ Intervals

X +ve uP. orthogonal to hole :",\,lCU t and along BH azimuth ~ Jz +ve uP. along axis of DDH

Figure 83: Loop Configuration and Polarity Conventions for 3-D Borehole Surveys

The secondary fields induced decay at a rate proportional to the conductivity-thickness and are then meas-ured and profiled by the borehole sensor-probe.

a) Hz is positive up along the axis of borehole,





b) Hx is positive perpendicular to the borehole axis and pointing upward, in a vertical plane, in the direction ofthe azimuth of the hole,

c) Hy is positive 90° counterclockwise to Hx and horizontal, according to the right-hand rule.

At the end of each survey day, the stored data are transferred to a microcomputer where they corrected for the tum-off time, loop area, system gain and current, and converted from millivolts to nanoVolts per ampere meter squared or nanoVolts per meter squared. The data are then transferred to disk for storage and processing. Report quality field plots are generated on site, using a 24-pin printer in order to monitor the data characteristics and to pro-vide a preliminary interpretation capability.

The following equations govern the transient EM response for buried plate-like conductive bodies 1

1 -( emf = - e·/ 7:

T

Target Response to Transmitter Current Waveform: where: t flXedtime

e exponential decay

T = time constant of conductor

Equation 1: Conductor Response to the Transient EM Waveform

The time constant of the response is alternatively defined as the slope of the lin-log decay curve (Geonics) or, more exactly, as the time channel where the amplitude of the decay collapses to 37% (1/e) of its maximum value. Both ""t and the analogous decay strength (I.e., the number of anomalous channels above background), are com-monly used as indicators of conductor quality. This relationship between decay-strength and the conductivity-thickness can easily be demonstrated in the following equation for a vertically dipping conductive sheet:

T = (j~h for a thin plate

where (j = conductivity of target p. = magnetic susceptibility t = thickness of plate

h = vertical extension of plate Equation 2: Transient EM Decav Time Constant

1 From Geonics Limited, EM-37 TEM System Design Parameter. Mississauga, Ont., 1982.


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thereby giving, for an infinite vertical sheet:


crt = ,r r ~ rl mhos / metre (siemens) ph 10.31

Equation 3 Conductivity Thickness

From these equations and relationships, it therefore becomes obvious of the common use of the anomaly strength of decay as a simple, rule-of thumb indicator of the relative conductivity-thickness product for TEM SUMlYS.

In addition, the total secondary field is calculated using the three components (Hx, Hy and Hz) in the follow-ing formula


Htot = JHx2 +Hy2 + Hz2nanoVoit I Am 2. Equation 4: Transient EM Total Secondary Field

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INSTRUMENT SPECIFICATIONS

Measured Quantity:

Sensors:

Geonics Limited Digital Protem Ground Transient Electromagnetic System

Technical Specifications

Receiver

Time rate of decay of magnetic flux along 3 axes

1. (L.F.): Air-cored coil of bandwidth 60 kHz; 100 cm diameter 2. (H.F.):Air-cored coil of bandwidth 850 kHz; 100 cm diameter 3. (30-3): Three orthogonal component sensor; sirrultaneous operation 4. (30-1): Three orthogonal component sensor; sequential operation

Kamiskotia Project

Time channels: 20 geometrically spaced time gates for each base frequency gives range from 6 I-lsec to 800 msec.

Repetition Rate:

Synchronization :

0.3 Hz, 0.75, 3, 7.4, 30, 75 or 285 Hz for 60 Hz power-line networks (Base Frequency)

1) reference cable. 2) high stability (oven controlled) quartz crystals. (Switch selectable)

Integration time:2 , 4, 8,15,30,60,120,240 sec.

Calibration: Internal self-calibration External Q coil calibration (optional)

Keyboards Two 3 x 4 matrix sealed key pads with. positive tactile feedback

Gain: Autometic or manual control

Dynamic Range: 23 bits (132 dB)

Display Quantity: (1) Table of time rate of decay of magnetic flux (dB/dt) (2) Curve of rate of decay of magnetic flux (dB/dt) (3) Table of apparent resistivity (Pa)

(4) Curve of apparent resistivity (Pa) (5) Profile of dB/dt (6) Real time noise monitor (7) Calibration curve (8) Data acquisition statistics (real t.me)

Storage: Solid state memory with capacity for over 3000 data sets

Display: 8 .ines by 40 character (240 x 64 dot! graphic LCD

Data Transfer: Standard RS-232 communications port.

Processor: CMOS 68HCOOO 8 MHz CPU

Receiver Battery: 12 volts rechargeable battery for 8 hours continuous operation. 6 hours in XTAL mode


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Receiver Size:

Receiver Weight:

Operating Temp.:

Transmitters:

34 x 38 x 27 em

15 kg

(1) Geonics TEM47 (2) Geonics TEM57 (3) Geonics TEM37

l$itj' width start

mode 0 2.000 32.00 0 2.625 40.00

50.50 4 13.70 15.90 4.375 63.50 5 -18,00 . 20.80 5.500 81.00

: 6 23.50 27.00 7.000 103.0 I 7 30.50 34.80 8.500 131.0

7.S/6.25Hz

",nte' I width I start 36.00 80.00 45.25 100.0 57.00 13.00 126.3 72.25 17.50 158.8 92.00 22.00 202.5 117.0 28.00 257.5 148.0 34.00 327.5

I 8 39.00 44.40 10.75 165.0 I 186.5 43.00 412.5 I 9 49.80 56.30 13.00 208.0 234.0 52.00 520.0

10 62.80 70.30 15.00 260.0 290.0 60.00 650.0 11 77.80 85.90 16.25 320.0 352.5 65.00 800.0 12 94.10 104.7 21.25 385.0 427.5 85.00 963.0 13 115.3 129.1 27.50 470.0 525.0 110.0 1175 14 142.8 159.7 33.75 580.0 647.5 135.0 1450 15 176.6 198.4 43.75 715.0 802.5 175.0 1788 16 220.3 248.6 56.25 890.0 1002.5 225.0 2225 17 276.6 312.3 71.25 1115 1257.5 285.0 2790 18 }47,8 393.5 91.25 1400 1582.5 365.0 3500 19 439.0 497.1 116.2 1765 1997.5 r 465.0 4413 20 555.3 629.0 147.5 2230 2525.0 590.0 5575 21 702.8 797.3 188.7 2820 3197.5 755.0 7050 22 891.5 1012 240.0 3575 4055.0 i 960.0 8940 23 1131 1285 306.2 4535 5147.5 1225 11338 24 1438 1634 391.2 5760 6542.5 1565 14400 25 1829 2079 498.7 7325 8322.5 1995 18310 26 2328 2645 636.2 9320 10592 2545 23300 27 2964 3370 812.5 11865 13490 3250 29663 28 3776 4295 1036 15115 17187 4145 37800 29 4813 5473 1321 19260 21902 5285 48150 30 6134 6978 1685 24545 27915 I 6740 61360

7819 31285 I 78200 Note: All trmes In mIcroseconds

CLAIM POST RESOURCES INC. Kamiskotia I"reject

312.SHz center width

90.00 20.00 113.1 26.25 142.5 32.50

!HI 230.0 292.5 466.3 107.5 585.0 130.0 725.0 150.0 881.3 162.5 1069 212.5 1313 275.0 1619 337.5 2006 437.5 2506 562.5 ! 3144 712.5 3957 912.5 4994 1162 6313 1475 ! 7994 1887

. 1Q~38 2400 12870 3062 16350 3913 20806 4987 26475 6363 33725 8125 42975 10362 54750 13212 69800 16850

Table C1: Digital Protem Gate Locations

This Table applies to both synchronization modes regardless of which ofTEM37, TEM47 and TEM57 transmit-ters is used, provided that correct Tx model is selected in Header (2.4).

Note: 7.5/6.25 and 0.75/0.625 Hz proportional to 75/62.5 Hz 3/2.5 and 0.3/0.25 Hz proportional to 30125 Hz



QUANTEC GEOSCIENCE LTD. Borehole TEM SUlVeys


Current Waveform:

Base Frequency:

Turn-off Time(t):

Transmitter Loop:

Output Current:

Output Voltage:

Geonics limited EM-57 Transient Electromagnetic Transmitter

Technical Specifications

Bipolar rectangular current with 50% duty cycle

0.3,0.75,3, 7.5 or 30 Hz where power line frequency is 60 Hz 0.25, 0.625, 2.5 or 25 Hz where power line frequency 50 Hz Rates below 1 Hz available from PROTEM receiver through reference cable

Fast linear tum-off maximum of 450 I-tsec. at 25 amps into a 300x600 meter loop. De-creases proportionally with current and the root of the loop area to a maximum of 20 11 sec. Actual value of t read on front panel meter.

Up to 2,000 x 2,000 m single turn

25Amaximum

18 to 150 V continuously adjustable

Synchronization: Reference cable or, optionally. quartz crystal

Power Supply: Variable 2,OOOW to 4,500 W. 115 or 110/220 V. 50/60 Hz, single phase motor generator

Transmitter Protection: Electronic and electromechanical protection

Dimensions: 43 x 25 x 25 cm (TEMS7-MK2); 42 x 20 x 31 cm (EM-67 Power Module)

Component Dimensions and Weights

Weight: 15 kg (TEM57-MK2); 12 kg (EM-67 Power Module)





GEONICS LIMITED

BH-43 3-D Borehole Probe with Tilt Sensors Technical Specifications

Measured Quantity: Time derivative of axial and radial magnetic field

Sensors: Three orthogonal coils (one axial, two radial)

Overall Length: 334 cm

Maximum Diameter: 3.8 cm

Weight: 9.5 kg

Sensor-Preamplifier Resonant Frequency: 10kHz

Sensor Areas: 100 m2

Operating Temperature: -30 degrees C to +80 degrees C

Probe Rotation Correction: Two orthogonal tilt meters with range ±1 0 to ±80· from vertical

Kamiskotia Project

Battery: Rechargeable NiCd sealed pack for 15 hours continuous operation

Cable

Type: Two-conductor shield polyurethane jacket Kevlar membrane

Diameter: 5.6 mm

Weight: 40 kg/km

Length: 540m


I I I I I I I I I I

I I I I I I I I


PEND IX 0

PRODUCTION LOG KAMISKOTIA PROJECT BOREHOLE TEM SURVEYS

Date Description 10-Dec-08 Mob to property. Transport gear to first hole but not finished

yet. Lay loop. Half survey day. 11-Dec-08 Return to property at 1pm. Shut down hole at 287m. Wait for

drillers to pull rods. Dummy and log hole successfully. Pull loop and all gear back to staging area.

9-Jan-09 Mob to property. Set up loop for hole 9. Dummy to 320m where dummy becomes lodged and left in the hole. LOg hole to 320m. Retrieve loop.

12-Jan-09 Mob to property. Set up loop for hole 11. Dummy cleanly to the bottom. Log hole and retrieve loop.

16-Jan-09 Mob to property. Lay loop for hole 9 extension. Dummy cleanly but lose dummy at the bottom of the hole. Re-dummy cleanly and 10Q hole.

24-Jan-09 Return to property at 1 pm. Lay 200m loop. Dummy and log hole successfully. Retrieve loop and all gear and demob property.



Hole # Start End Total (m)

CP08-10

CP08-10 50 285 235

CP08-09 135 320 185

CP08-11 40 274 234

CP08-09 300 420 120

CP08-09 400 509 109

I I I I

I I I I I I I I I I I I


LIST OF MAPS


• LPTEM Borehole Profiles: Multi-Channel 4-Axis and LinLog Profile Plots: showing time rate of decay of the secondary electromagnetic field, for X, Y , Z and Total Field components, 1 :2000 scale, ch. 1-

2 20 divided according to 4 vertical (linear) axes and ch 1-20 from a single axis , nVlm

Drawing #s:


CA00626C-BH4AXIS-TiLT-K-Borehole#, where K=Z, X, Y, TF (Total Field). CA00626C-BHLL-TILT-K-Borehole#, where K=Z, X, Y, TF (Total Field)

BOREHOLES TOTAL PROFILES CP08-09 8 CP08-1 0 8 CP08-11 8

Total Profiles: 24

I QUANTEC GEOSCIENCE L TO. CLAIM POST RESOURCES INC. Borehole TEM Surveys Kamiskotia Project

I I PROFILES AND MODELS I I I I II I

II :1 I

I I I I I I II I

II CA00626C - January 2009

'I


QUANTEC GEOSCIENCE LTD. Boceho6e TEM Surveys

........ _ ........ _ ..... JLaod IlnII _ \\, ..

IS \:I.I:J ,:-:. ? ~ ~~ .. ' . . ••••• 'eJC!:I ,+ .... 'iii l; a.

Maxwell Model Results fo

Off-holeconductor - j ' probable source of airborne anomaly #2

Recommended drillhole

View Looking Southeast

• • start " :. i:j r: It • !l ~ :-- ' _. .

CAOO626C - January 2009

CLAIM POST RESOURCES INC. Kamiskolia Project

. ~. AC_

Field & Model Responses fo_~r~C~h~~7i-

".. • Ill! 111 . .

..... . -


QUANTEC GEOSCIENCE L lD_ 8ofehole TEM Surveys

_ ....... _ S-/lOOII n- __

IS \:.~ ':'. ', ')r ~ .... ' •• e lie tic!:! ' + .... ;, .,. ".

Maxwell Model Results for CP08-10

- . Conductor Parameters Dimensions: 60m x 190m Dip: 68° NW

... - . Azimuth: 2020

Conductance: 500 Siemens -. ..

Recommended drillhole .. ..... ....

View Looking South


..

...

CLAIM POST RESOURCES INC. Kamiskolia Project

' '-Field & Model Responses for Ch 15 - 20

.. . " II a .. Q .. •

• 11 & II' g lD

.'1l_._l'Q:a:»~ __ rt_31 -uc_

•• ., .... f» •• !tt ' ••• ft:3l3; .:s.!'Ia:. -,-l;~ 1.,1.,. 1". .....J. I •• , _ .. If ~


QUANTEC GEOSCIENCE LTD. Borehole TEM SUNeys

~ _PnIjItt _ SMIIOII DIM _ .....

IS \:I.~ '1:.:r .;, ')r ~ \00 • • ' ••••• tic!] , .;. I.I."Ii l; A.

Maxwell Model Results for CP08-11

conductor

View looking Southeast

_ : 119.S._: 1W), __ : "'"


ClAIM POST RESOURCES INC. Kamiskotia Project

A'-Field & Model Responses for Ch 15 - 20

.. -u'-

.~ • a . ~ .. : :s:. . :. -YC_

-------------------CP08-09 BOREHOLE & LOOP LOCATION MAP

o 100E 200E

200N - 200N

100N CP08-09 100N

o - - 0

Nap Cenerated by

Scale 1 :2500 25 a 25 50 75 100 125 ......... i

(metres)

CLAIM POST RESOURCES INC. KAMISKOTIA PROPERTY

TIMMINS. ON

3D FIXED-LOOP BOREHOLE TEM SURVEY

BOREHOLE &: LOOP LOCATION MAP CP08-09

Borehole Porometers: DDH # 1 = Locotion = Azimuth & Dip =

CP08-09 450130E,5376230N

166, -45

Survey Dote:

DDH #2 = Locotion = Azimuth & Dip =

DDH #3 = Locotion -Azimuth & Dip =

Instrumentotion:

Jon 9, 2009

Rx = Digitol Protem (3x20 Channels)

Geonics 3D probe + SOOm coble

Tx = Geonics EM-57 1 . 8 kW

Surveyed & Processed by:

QUANTEC GEOSCIENCE LTD. owe. #: CA00626C-BHT£M-LOOPLOC-CP08-09

- -"D

~ 3 0000 . rz.. >, '-

------------------------ -------------------------------- -

I

150

AlaI' em.rated by

- -

I

200

-

I

250

-

I

300

- -

I 350

D E P T H (metres)

-

I

400

- -

I

450

-

I

500

- -10000

1000

100

til ...J

10 « u Cf)

5 til .....

...J ~ ~ ......

0 0 l1 0:: ~ 0... 0 c

·5 {) D C

0 .....,

...J ·10 I

Z :3

·100

·1000

·10000

- - - - --I-I

Borehole CPOB-09 - Z Component

Scale 1 :2000 25 0 25 50 75

~--(metres)

CLAIM POST RESOURCES INC . KAMISKOTIA PROPERTY

TIMMINS. ON

3D FI XED-LOOP BOREHOLE TEM SURVEY

Secondary Electromagnetic Field (dB/dt)

Transmitter Frequency:

r x Loop Size : Ix Loop Location:

Transmitter Current :

30 Hz (507. duty cycle )

200m, 200m

S5/1 08;7/302;202/349 ;251 / \ 46

Tx Turn-Of(-Time and R)( Delay :

15 Amps

480 uS - 80 us

450 \ 30£ . 5376230N

\ 66. - 45

5 - 10 meters

nonoVoltjm"'2

Hz - positive up

Borehole Locatio n:

Borehole Azimuth, Dip:

Station Interval:

Profil e uni ts :

Receiver Coil Orientation:

Hx - positive south, Hy - positi ve we st

C(O~S Component Rotation: using T::t Meter Aflgles

Survey Date:

Instrumentation:

Jon g . \ 6 . 24. 2009

R, : O;g ;to l Protem (3,20 Channels)

Geonics 30 proce l' SOOm coble

" : Ceon;cs EM -57 (1.8 kW)

Surveyed & Processed by: QUANTEC CEOSCIENCE LTD.

OWG. NO. CA00626C-BHLL-Z- TiIl -CP08-09-f/

-

o

I ;J)

(f)

..c U

o (\1

I co

In ..c u

-

-500 .

30 .

- 30.

Nap Cerurated by

- -

I I

150 200

- -

1

250

-

I 300

- -

I

350

o E P T H (metre.)

- - - -

I

500

-

2 C:.J.

100 . 0 :r (f)

0 ()l

-1 0 0 .

- - - - -j-

Borehole CP08-09 - X Component

Scale 1 :2000 25 0 25 50 75 ~=-- .-

(metres)

ClAIM POST RESOURCES INC. KAMISKOTIA PROPERTY

TIMMINS. ON


Secondary Electromagnetic Fiel d (dB/d t )

Transmitter Frequency: 30 Hz (50% duty cyc le )

Tx Loop Size: 200m x 200m

T, Loop Locot;on55E/1 08N: TEI 302N:202EI 349N:251 El l 56N Transmitter Current:

Ix Turn-Otf - Time and Rx Deloy:

15 Amps

480 ,us. -80 us

450 I JOE. 53762JON

166, -45

Borehole Location :

Borehole Azimuth , Dip:

Station Interval : 5 - 10 meters

Profi le Units: nonoVolt!m"2

Receiver Coil Or ient ation : Hz - positive up

Hx positive south. Hy - positive west

Cross Component Rotation using Til t Meter Angles

Survey Dote:

Instrumentation:

Jon 9,16,24, 2009

Rx :.:. Digital Protem (3,.;20 Channels)

Geonics 3D probe .. 500m co ble

T, = Geon;c. EM-57 (t , B kW)

Surveyed & Processed by.

QUANTEC GEOSCIENCE LTD. oW(; , NO . CAOD626C-BH4A-TiJlro/-X-CPOB-09-ty

- - -

N ap Cen~rated hy

-

200

-

I

250

-

I

300

- -

I

350

D E P T H (metres)

-

I

400

- -

I

450

-

I

500

- -10000

1000

100

~ ....J

10 ~ U rn

5 ~ ~ ....J r;: "-0 0 l!

0:: ~ 0- g

·5 ~ 0 c:

0 '-'" ....J

·10 I Z :J

·100

·1000

·10000

- - - - -j-


Scale 1 :2000 25 0 25 50 75 ---.---

(metres)

CLAIM POST RESOURCES INC . KAMISKOTIA PROPERTY

TIMM INS. ON

3D FIXED- LOOP BOREHOLE TEM SURVEY

Secondary Elect romagnetic Field (dB/ dt)


Tx Loop Size :

T x Loop loco r," on

Tra nsmitter Current:

30 Hz (507. duty eyel. )

200m, 2COm

55/ 108:7/302:202/349:25 1/146

Ix Tum-Oft - Time and R)C Oelay:

'15 Amps

480 us -80 uS

450 130E, 53762 30N

166 , -4 5

5 - 10 meters

nonoVoltjrrY'2

Hz - posit ive up

Boreh ole Location :

Borehole Azimuth, Dip :

Station In terval:

Profile units :

Rec eiver Coil Orien ta tion;

Hx - positive south . Hy - positive wes t

Cros s Component Rolation: u sing Tilt Meter An g les

Survey Date :

Ins trumentation;

Jan g, 16,2 4, 2009

ax - Digita l Pro te m ( 3x20 Chann els) Geo"ics 3D probe ... SOOm coble

Ix = Gean;es EM - 5 7 ( 1 , 8 kW)

Surveyed &: Processed by: QUANTEC GEOSCIENCE LTD.

OWl>. NO. CAOO626C- BHLL-X-TiIl-

--0

Q)

~

>,

- -

I

150

Nap Cenerated 6y

- -

I

200

-

I

250

-

I

300

- -

I

350

D E P T H (metres)

-

I

400

- -

I

450

p

-

I

500

P

- -10000

1000

100

W ....J

10

- - - - - - - - - - - - - -'"0

~ 30000. Co.

>,

~ O. ~4-4-~~~~~~~-+-+-==:~~~~~~~~~~~~~~~~~~~~gg~~~~~ [

CL.

-300 00

5000. 0

I co rJ) 0

..c: u

-5mSO.

I 00. 0 C\I I

co

rJ) 50.

..c: u

0

- 50 .

Nap Ceneratea by

I

~-

--=====--

I

150 I

200 I

250 I

300 I

350

o E P T H (metree)

I

400

1--

I

45 0

, ,

I

500

f 30000 n

I ::r rJ)

O. I 0\

800.000.

400. n ::r rJ)

200.

CJl

- - - - --1-

Borehole CPOB-09 - Tolal Field

Scale 1 :2000 25 0 25 50 75 --- (metres)


TIMMINS. ON


Secondary Electromagneti c Field (dB/dt)

Transmitter frequency: JO Hz (507. duty cyCle)

h Loop Size: 200m x 200m

ix LOOp Locotion55£/ 1 08N; 7EjJ02N.202E/349N;25 1 E/ 156N

Transmitter Current:

Tx Turn-O f(-Time and Rx De fo y:

15 Amp,

480 us. -80 uS

4501 JOE , 53762JON

166 . -45

') -- 10 meters

nanoVult/m'"'2

~z - positive up

Borehole Location :

Borehole Azimuth. DiD:

Stotion If' tervcl:

Profile units :


Hx - positive south. Hy - po sitive wes t

Cross Component Rotation" using Till Meter Anqles

Survey Dote :

Instrumenta tion :

Jon 9 . 16.24 . 2009

Rx = Uiqi to l Protem (3x20 Chann els)

Geo nics .30 probe + SOOm coble

Tx = Geonic, EM-57 (1 8 kW)

G Surveyed & Processed by QUANTEC GEOSCIENCE LTD. """ OING _ NO . CAOD626C-BH4A-THlrol - TF- CPOB-D9-rI

- -

I 150

N ap Cen eralea by

-

I

200

- -

I

250

-

I

300

- -

I 350

D E P T H (metres)

- - - -

I I I I I I I I I I I I I I I I I I I I I II

I 400

I

450 I

500

- -10000

1000

100

~ .....:l

10 . NO, CAOO626C-BHLL -TF- TiJt~P08-09-tI

-----'--------------CP08-10 - BOREHOLE & LOOP LOCATION MAP

700N

600N

Jlap Cenerated by

300E

t(As Shown)

300E

400E

- 7001\1

CP08-

SOON

400E

Scale 1 :2500 25 0 25 50 75 100 125 ....... -.

(metres)


TIMMINS, ON



Borehole Parameters: DOH # 1 = CP08- 10

Survey Dote:

Location = 451426E, 53756 16N Azimuth & Dip = 266, -45

DOH #2 = Location = Azimuth & Dip =

DOH #3 = Location = Azimuth & Dip =

Instrumentation:

Dec 11, 2008

Rx = Digital Protem (3x20 Channels)

Geanics 3D probe + 500m cable

Tx = Geonics EM-57 (1,8 kW) Surveyed & Processed by:

QUANTEC CEOSCIENCE LTD. owe , #: CA00626C-BHT£M-LOOPLOC-CP08- 10

- -~ 50000 . (])

. ~

r:z.. >, h co o. E h

- -j - I-+--+-~

0.. _______

- - - - - - - - -1 . - I-I--+---+--+-- I-- +1 ---+---1-+---+1 ---+-- -1 I 1

-50000 . 50000

~

o

I CD

[j)

..c u

o C\J I

CD

[j)

..c u

-5000.

200.

o -+--!-~

-200. I

50

Nap Cenerated by

I

100

1

-t---t- t--+---'---t-i- - !-j---r----t--t--

I 150

I

200

o E P T H (metres)

I

250

t- -

o

n ;:::r' (J)

-50000

500 .

o

- 500

n ;:::r' (J)

- - - - - -a

Borehole CP08-10 - Z Component

Scale 1 :2000 25

(metres)

50 75 .5


TIMMINS, ON




Tx Loop Size:

Tx Loop Loca tion :


Tx Turn-Off-Time and Rx Delay:

30 Hz (50% duty cycle)

200m x 200m

275E -4 75E;516N-716N

15 Amps

465 us. -80 uS

451426E.5375616N

266. -45

5 - 10 meters

nanoValt/m"2

Hz - positive up

Borehole Location :

Borehole Azimuth. Dip :

Station Interval :

Profile Units:

Receiver Coi l Orientation:

Hx - positive west . Hy - positive south

Cross Component Rotation: using Tilt Meter Angles

Survey Date :

Instrumentation:

Dec 11 . 2008

Rx = Digitat Protem (3

I

50

Nap Cenerated by

I 100

I

150 I

200

D E P T H (metres)

-----~

I

250

10000

1000

100

~ ~

10 .c:x: U (f)

5 ~ ""' ~ ~ -~ ........

0 0 l! ~ ~ 0... 0 c

-5 0 g 0

....... ~

-10 I Z -~

-100

-1000

·10000

-B Borehole CPOB-10 - Z Component

Scale 1 :2000 25 0 25 50 75 ----- (metres)


TIMMINS. ON

3D FIXED· LOOP BOREHOLE TEM SURVEY


Transmitter Frequency: 30 ::z (50% duty cycle) T x Laop Size :

Tx Loop Location :

Transmitter Current :

Tx Turn-Olf-Time and Rx Delay:

200m x 200m

275E -4 75E;516N -71 6N

1 S Amps

465 uS -80 uS

451426E,5375616N

266. -45

5 - 10 meters

nonoVoltj m-2

Hz - positive up

Borehole Location :


Stotion Interval:

Profile Units :

Receiver Coil Orientotion:

Hx - positive west, Hy - positive south

Cross Component Rotation : using Tilt Meter Angles

Survey Dote :

Instrumentation :

Dec 1 t, 2008


Geanics 3D probe + SOOm coble

Tx = Geonics EM-57 (1.8 kW)

Surveyed & Processed by: QUANTEC CEOSCIENCE LTD.

owe. NO. CA00626C-BHLL-Z-Tilt-CPOB-rJm-W

- -:.s 5 0000

ClJ

~

» ;..... (1j

E 0

h 0...

-5 0000.

(f)

..c u

- - - - - - - - - - -~-Y ~~:J P

-l-+---+--- I I - f------t--1 f- f- I II p

~=+~~~~~~~~~~~~T-~~~~I c ~

l - 50000

-500 0. - 5 00 . o :::T (f)

o C\J I

CD ,--;

(f)

..c u

~ +-+ I -+ t +- :,~-::,~T=+, =++, ---~I ~~'~T~=1~=-q~~~l a

2 0 0 . '~ - 5 00 ~-~

o

-200 I

50 I

100 I

15 0 I

200 I

25 0

Nap Cimerated by o E P T H (metres)

- - - - - --1-

Borehole CPOB-10 - X Component

Scale 1 :2000 25 o 25 50 75 ~- (metres)

CLAIM POST RESOURCES INC. KAM ISKOTIA PROPERTY

TIMMINS. ON


Secondary Electromagnetic Field (dB/ dt)


I x Loop Size :

Tx LOOp Location :



200,-,-, x 200m


275E-475E;516N-716N

15 Amps

465 us, -80 us

451426E,5375616N

266, -45

5 - 10 meters

nonoValt/m'2

Hz - positive up

Borehole Location:


Station ·I nterval:

Profile Units:




Survey Dote :

Instrumentation :

Dec 11 , 2008


Geonics 3D probe + 500m coble



QUANTEC GEOSCIENCE LTD. OWG. NO. CA00626C-BH4A-TiJlro/-X-CP08-(Of1}-tJ

I

50

Hap Cenerated by

I

100 I

150 I

200

D E P T H (metres)

\ \

\

~ I

250

10000

1000

100

til ~

10 < U If)

5 til -~ ~ -CL. ) 0 0 ~ ~ 0.. g

-5 0 0 C

0 '-' ~

-10 I Z -~

-100

-1000

-10000


Scale 1 :2000 25 o 25 50 75 ...-..--

(metres)


TIMMINS, ON

3D FIXED--LOOP BOR[HOLE TEM SURVEY


T ronsm;t~er Frequency:

Ix Loop Size :

Tx Loop Location:


Tx Turn-Oft-Time and Rx Delay:

30 :.:z (50% duty cy~I",)

200m x 200m

2 75E -4 75E;51 6N- 716N

15 Amps

465 us -80 us

451426E.5375616N

266, - 45

5 - 10 meters

nanoVolt/ m' 2

Hz - positive up

Borehole Locat ion:


Station Interval:

Profile Units:

Receiver Coi l Orientation:



Survey Dote: .

Instrumentation :

Oec 11, 2008

Rx = Digital Protem (3x20 Channe ls)

Geonics 3D probe + 500m cable

Tx = Geonics EM-57 (1 . 8 kW)


QUANTEC GEOSCIENCE LTD. OWG. NO . CA00626C-BHLL-X-Ti/t-CPOB-IJIJ-N

- ---0 10 00U Q)

Co-

>-, h

E C.

-1 00 0U

o

I ~

(J)

-

~-1000. ~ '-'

o C\J I

CD

(J)

[3 -200 . I 50

Nap Ceneraled by

- -

I

100

- - - - - - - -p

z--£ p " ~~

+--+--+--+--+---+-1 -II --t-+---t---l-I-----=+=+=---r-~~1'_4 2 0000.

10000. n ;:::J ell

r->

I .- 0 ()l

- -1 0000 .

+- + bJ=ghjL-+--41

I

15 0 I

200

o E P T H (metres)

I

250

-500. r-> C)l

- - - - - --t-

B j

Borehole CP08-10 - Y Component

Scale 1 :2000 25 o 25 50 75

(metres)


TIMMINS, ON


Secondary Electromognetic Field (dB/dt)

T ronsmitter Frequency:

Tx Loop Size:

Tx Loop Location:


Tx Turn,..Off-Time and Rx Oeloy:

30 Hz (507. duty cycle)

200m x.200m

275E -4 75E;516N-716N

15 Amps

465 us. -80 us

451426E.5375616N

266. -45

5 - 10 meters

nanoValt/m'2

Hz - positive up

Borehole Location:

Borehole Azimuth. Dip:

Station Interval:

Profile Units:


Hx - positive west. Hy - positive south


Survey Date:

Instrumentation:

Dec 11. 2008

Rx = Digital Protem (3x20 Channels) Geonics 3D probe + 500m cable

Tx = Geanics EM-57 (1.8 kW)


QUANTEC GEOSCIENCE LTD. DWG. NO. CA00626C-8H4A-T,ltrot-Y-CPOB-(P(P-1I

I 50

Hap Cenera(ed by

I

100 I

150 I

200

D E P T H (metres)

I

250

10000

1000

100

~ .....l

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i 50 200 2 iJO

o E P T H (metres)

-

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- 7 5000.

1000. n ;::::J Ul

0 ;-0

t-'

(J1

- - - - - -8

Borehole CP08-10 - Total Field

Scale 1 :2000 25 0 25 ----- (metres) 50 75 i


TIMMINS, ON




h Loop Size :

Tx Loop Location:


Tx Turn'-Off-Time and Rx Delay:

30 Hz (507. duty cycle)

200m x 200m

275E - 4 75E ;516N-71 6N

15 Amps

465 us , -80 us

451426E.5375616N

266 , -45

5 - 10 meters

nanoVolt/mA 2

Borehole Location :


Station Interval:

Profile Units:

Receiver Coil Orientation: Hz - positive up

Hx - positive west, Hy - positive sou th

Cross Component Rotation: using Till Meter Angles

Survey Dote :

Instrumentation:

Dec 1" 2008

Rx '" Digital Protem (3x20 Channels)


Tx '" Geonics EM-57 (1 . 8 kW)

O· . Surveyed & Processed by:

QUANTEC CEOSCIENCE LTD. ';I' OWG . NO. CA00626C-BH4A-Tiflrol-TF-CPOB-tPlP-'fi

I

50

Nap Cenerated tr!l

I 100

I

150 I

200

o E P T H (metres)

I

250

I !

10000

1000

100

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10 < U r.J)

5 Cil -~ ~ -~ ) 0 0 ~ ~ 0... 0 s:

-5 c..:J 0 s:

0 '-' ~

-10 I Z -~

-100

-1000

-10000

Borehole CP08-10 - Total Field

Scale 1 :2000 25 o ----- 25 (metres) 50 75 ==s


TIMMINS. ON ~------------------------------------.



Transmitter F:requency:

Tx 'Laop Size:

Tx Loop Location:


Tx Turn-Ofl-Time and Rx Delay :

30 H. (50% duty cycle)

200m x 200m

275E-475E;516N-716N

15 Amps

465 uS -80 us

451426E.5375616N

266. ·45

5 - 10 meters

nonoValtj rTY'2

Hz - positive up

Borehole Location:

Borehole Azirnuth. Dip :

Station Interval :

Profile Units:


Hx - positive west. Hy - positive south

Cross Component Rotation : using Tilt Meier Angles

Survey Dole:

Instrumentation :

Dec 11. 2008


Geonic s 3D probe + 500m coble



QUANTEC CEOSCIENCE LTD. OWG. NO. CAOO626C-BHLL-TF-Tilt-CPOB-Ot»-N

-------------------CP08-11 BOREHOLE & LOOP LOCATION MAP

200E 300E

700N 700N Sea Ie 1 :2500

25 0 25 50 75 100 125 'IJ"' ___ :s

(metres)


TIMMINS. ON

600N 600N 3D FIXED-LOOP BOREHOLE TEM SURVEY


Borehole Porometers: DDH # 1 = CP08-11 Locotion = 451320E,5375590N Azimuth & Dip = 90, -60

DDH #2 = Location = Azimuth & Dip =

DDH #3 = SOON - - SOON Locotion =

Azimuth & Dip =

(As Shown) Su rvey Dote: Jan 13, 2009 200E 300E Instrumentotion: Rx = Digitol Protem (3x20 Channels)



G Surveyed & Processed by:

Nap Ceneraled by QUANTEC GEOSCIENCE LTD.

OWG. l CAOO626C-8HTEM-LOOPLOC-CP08-11

- - - - - - - - - - -p

'ti 00000 OJ .-

C:r.., p

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5 0 '00 130 :250

Map Cenerated by o E P T H (metres)

- - - - - -G-

Borehole CP08-11 - Z Component

Scale 1 :2000 25 o 25 50 75 .,----

(metres)

CLAIM POST RESOURCES INC. KAMISKOTIA PROPER1Y

TIMMINS, ON



T ransmitter Frequency:

T x Loop Size:

Tx Loop Location:




200m x 200m

170E -370E;490N-690N

15 Amps

475 us, -80 us

451320E,5375590N

90, -60

5 - 10 meters

nanoVolt/ m'2

Hz - positive up

Borehole Location:


Station Interval:

Profile Units:


Hx - positive east, Hy - positive north


Survey Dote:

Instrumentation:

Jon 13, 2009

Rx : Digital Protem (3x20 Channels)




QUANTEC GEOSCIENCE LTD. OWG. NO. CA00626C-BH4A-Tiltrot-Z-CP08-0J-f/

I

50

Nap Ceneraled by

I

100 I

150 I

200

D E P T H (metres)

I

250

10000

1000

100

~ .....:I

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- - - - - - - - - - - - -

>.... (L

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I I 150 :200 250

Map Cenera{ed by o E P T H (metres)

- - - - - -

G-Borehole CP08-11 - X Component

Scale 1 :2000 25 o 25 50 75

(metres)


TIMMINS. ON


Secondory Electromagnetic Field (dB/ dt)


Tx Loop Size :

1. Loop Location :

Transmitte·r Current :

Tx Turn-Off-Time ond Rx Delay:


200m x . 200m

170E-370E;490N-590N

15 Amps

475 us, -80 us

451320E,5375590N

90, -50

5 - 10 meters

nanoVolt / m' 2

Hz - positive up

Borehole Location :

Borehole Azimuth , . Dip:

Station Interval :

Profile Units:

Receiver Coil Orientation :



Survey Date:

Instrumentation :

Jon 13, 2009

Rx = Digital Protem (3 x20 Channels)


Tx = Geonic s EM-57 ( 1 . 8 kW)


QUANTEC GEOSCIENCE LTD. OWG. NO . CA00626C-BH4A-Tiltro/-X-CP08-fPJ-N

Nap Cenerated by

P

I

200

D E P T H (metres)

I

250

~ 10000

1000

100

~ ......:l

10

- - - - - - - - - - - - -p

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250

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- 0 (f) ,...... I

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200 0

C)l

- 20 00.

- - - - - -

Borehole CPOB-ii - Y Component

Scale 1 :2000 25 0 25 .........

(metres)

50 75 S


TIMMINS. ON



TransmiUer Frequency:

Tx loop Size:

Tx Loop Location:


Tx Turn-Off-Time and Rx Deloy:


200m x 200m

170E-370E;490N-690N

15 Amps

475 us, -80 us

451320E,5375590N

90, -60

5 - \0 meters

nonaVoltjmA 2

Hz - positive up

Borehole Location:

Borehole Azimuth, Dip :

Station Interval:

Profile Units:


Hx - positive east , Hy - positive north

Cross Com ponent Rotation: using Tilt Meter Angles

Survey Dote:

Instrumentation:

Jon 13, 2009


Geonics 3D probe + SOOm coble


Surveyed & Processed by: QUANTEC GEOSCIENCE LTD.

owe. NO. CA00626C-BH4A-Tiltro/-Y-CP08-lDJ-W

I

50

Afap Cenerated by

I

150 I

200

o E P T H (metres)

I 250

10000

1000

100

Cx.J ~

10 < U if)

5 Cx.J -~ i -~ .......

0 0 ::l ~ ~ 0... 0

~

-0 c.::J 0 ~

0 ......

~

-10 I Z -~

-100

-1000

-10000

G-Borehole CP08-11 - Y Component

Scale 1 :2000 25 o ----- 25 (metres) 50 75 2S


TIMMINS . ON



Transmitter Frequency :

T x Loop Size:

1 x Loop Location:

Tronsmitter Current:



200m x 200m

170E -370E;490N-590N

15 Amps

475 us -80 us

451320E.5375590N

90 -50

5 - 10 meters

nonoVoil/m'2

Hz - positive up

Borehole Locotion :

Borehole Azimuth. Dip :

Station Interval :

Profile Units:

Receiver Coil Orientotion:

Hx - positive eost. Hy - positive north


Su rvey Do t e:

Instrumentation:

Jan 13. 2009


Geanics 3D probe + 500m coble

Tx = Geonics EM-57 (1 .8 kW)


QUANTEC GEOSCIENCE LTD. owe. NO. CA00626C-BHLL -Y-TiI/-CP08-IPJ-tl

- -3 00000 Q)

~

o . ~

L. 0....

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- - - - - -p

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5 0 100 150

o E P T H (metres)

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0

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I

200 I

25 0

- - - - - --j-

G-Borehole CP08-11 - Total Field

Scale 1 :2000 25 0 25 ~=-

(metres)

50 75 I


TIMMINS, ON




Tx Loop Size:

Tx Loop Location:




200m x 200m

1 70E -3 70E;490N-690N

15 Amps

475 us. -80 us

4~1320E,5375590N

90, -60

5 - 10 meters

nonoVoltjm'2

Hz - positive up

Borehole Location:


Station Interval:

Profile Units:




Survey Date:

Instrumentation:

Jan 13, 2009


Geonics 3D probe + SOOm cable

Tx = Geonics EM 57 (1.8 kW)

G Surveyed & Processed by:

QUANTEC GEOSCIENCE LTD. ~ OWG. NO. CA00626C-BH4A-Tiltrot-TF-CP08-{PJ-W

I

50

Nap Cenerated by

I I I I I I I I I I I I I I I I I

I

100 I

150 I

200

D E P T H (metres)

I I I I I I Ii

I

250

10000

1000

100

10

5

o

-5

-10

-100

-1000

-10000

G-Borehole CPOB-ll - Total Field

Scale 1 :2000 25 0 25 ----- (metres) 50 75 I


TIMMINS. ON

3D FIXED-LOOP BOREHOLE TlM SURVEY



Tx Loop Size:

Tx Loop Location:


Tx Turn-Off-Time o nd Rx Delay·

Borehole Lacalion:


200m x 200m

170E-370E;490N-690N

15 Amps

475 us -80 us

451320E.5375590N

90 -60

5 - 10 meters

nanoVoll/mA 2

Hz - positive up


Station Interval:

Profile Units:


Hx - positive east. Hy - positive north


Survey Dale:

Instrumentation:

Jan 13. 2009



Tx = Geonics EM-57 (1,8 kW)


QUANTEC GEOSCIENCE LTD. Dwe, NO, CA00626C-BHLL-TF-Ti/l-CPOB-(JJ-W

2_40319_10_Downhole Geophysical Report_0012_40319_10_Downhole Geophysical Report_0022_40319_10_Downhole Geophysical Report_0032_40319_10_Downhole Geophysical Report_0042_40319_10_Downhole Geophysical Report_0052_40319_10_Downhole Geophysical Report_0062_40319_10_Downhole Geophysical Report_0072_40319_10_Downhole Geophysical Report_0082_40319_10_Downhole Geophysical Report_0092_40319_10_Downhole Geophysical Report_0102_40319_10_Downhole Geophysical Report_0112_40319_10_Downhole Geophysical Report_0122_40319_10_Downhole Geophysical Report_0132_40319_10_Downhole Geophysical Report_0142_40319_10_Downhole Geophysical Report_0152_40319_10_Downhole Geophysical Report_0162_40319_10_Downhole Geophysical Report_0172_40319_10_Downhole Geophysical Report_0182_40319_10_Downhole Geophysical Report_0192_40319_10_Downhole Geophysical Report_0202_40319_10_Downhole Geophysical Report_0212_40319_10_Downhole Geophysical Report_0222_40319_10_Downhole Geophysical Report_0232_40319_10_Downhole Geophysical Report_0242_40319_10_Downhole Geophysical Report_0252_40319_10_Downhole Geophysical Report_0262_40319_10_Downhole Geophysical Report_0272_40319_10_Downhole Geophysical Report_0282_40319_10_Downhole Geophysical Report_0292_40319_10_Downhole Geophysical Report_0302_40319_10_Downhole Geophysical Report_0312_40319_10_Downhole Geophysical Report_0322_40319_10_Downhole Geophysical Report_0332_40319_10_Downhole Geophysical Report_0342_40319_10_Downhole Geophysical Report_0352_40319_10_Downhole Geophysical Report_0362_40319_10_Downhole Geophysical Report_0372_40319_10_Downhole Geophysical Report_0382_40319_10_Downhole Geophysical Report_0392_40319_10_Downhole Geophysical Report_0402_40319_10_Downhole Geophysical Report_0412_40319_10_Downhole Geophysical Report_0422_40319_10_Downhole Geophysical Report_0432_40319_10_Downhole Geophysical Report_0442_40319_10_Downhole Geophysical Report_0452_40319_10_Downhole Geophysical Report_0462_40319_10_Downhole Geophysical Report_0472_40319_10_Downhole Geophysical Report_0482_40319_10_Downhole Geophysical Report_0492_40319_10_Downhole Geophysical Report_0502_40319_10_Downhole Geophysical Report_0512_40319_10_Downhole Geophysical Report_0522_40319_10_Downhole Geophysical Report_0532_40319_10_Downhole Geophysical Report_054

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