RPT ON DIAMOND DRILLING HUTT TP€¦ · Dean Rogers 41P14NE2011 2.23526 HUTT 010. Diamond Drilling...

2.23526

Report on Diamond Drilling Falconbridge Limited - Exploration

Hutt Twp., Timmins, Ont. Porcupine Mining Division

NTS 41P/14

thMay 14, 2002

RECEIVED

MAY 1 6 20C2

8EOSCIENCE ASSESSMENT OFFICE_____

Prepared by:Dean Rogers

41P14NE2011 2.23526 HUTT 010

Diamond Drilling Assessment Report Hutt Twp, Porcupine Mining Division

Contents

1) FL Rock Code Legend2) Diamond Drill Logs w/ assays and whole rock geochemistry

HUT 12-013) Assay and Whole Rock Geochemistry Certificates4) Crone Borehole EM Survey Report5) FL Property Map6) l :2,000 DDK Plan Map - Back Pocket7) 1:1,000 DDK Section - Back Pocket

TIMMfftg'EXPLORATION - AMENDED ROCK LEGEND - v7.0

1. MAIN ROCK DIVISIONS

15 [To be Announced

14 | Huronian Supergroup

13 | Metamorphic (Unknown)

12 [Gneiss

11 [Schist

10 l Diabase

9 [Felsic Intrusive

8 | Intermediate Intr. Rocks

7 [Mafic Intrusive Rocks

6 |Ultramafic Intr. Rocks

5 [Sedimentary Rocks

5,s |Sulphide (MO0/,)

4 | Felsic Volcanic Rocks

3 |Intermediate Volcanic Rocks

3,C [Heterolithic Volcanic Rocks

2 | Mafic Volcanic rocks

1 [Ultramafic Volcanic Rocks

2. TEXTURAL/GEOCHEMICAL MODIFIERS

abbxcdef

ghi

jkl

mnPqrstuV

wx

yz

Fine GrainedMedium GrainedBrecciaCoarse GrainedQuartz-Feldspar PhyricAmygdaloidal/VesicularPrimary FragmentalsGraphitic/ArgillaceousTholeiiticAlkalicCalc-AlkalicKomatiiticFlows (banded)MassiveVariolitic/SpheruliticPillowedQuartz PhyricOxide Iron FormationSulphides, ExhallitesPyroclasticHigh MgHigh FeHigh AlAndesiteIcelanditeHighly Evolved (Y^O)

AB

CDEFGH

JKLMNPQRSTUVWxYZ

Primitive (Y^O)Evolved (Y^(X60)

HeterolithicFeldspar PhyricChertWackeLeucoxene BearingBasaltic Komatiite

PyroxeniteNet TexturedPeridotiteDuniteOphiticPorphyritic

PolysuturedFracturedGabbroic TexturedPyroxene SpinifexOlivine SpinifexSkeletal/CrescumulateAdcumulateMesocumulateOrthocumulate

ROCK NAMES MUST HAVE ALL MODIFIERS COMMA DELIMITED AND CANBE NO LONGER THAN 15 CHARACTERS, COMMAS INCLUDED. Example:

3,*y,d,*DAC:-,*t

3. ALTERATION MODIFIERS

Ab AlbitizationBl Bleached^ CarbonaceousCb CarbonatizationCh ChloritizationEp EpidotizationF> Iron CarbonatizationHe Hematization^ Potassic AlterationKa KaolinitizationRs Rust StainedSe SericitizationSi SilicificationSr SerpentinizationTc Talc-CarbonatizationTk Talc

4. Textural./Structural MODIFIERS

*a Tuff (67"Xo*b Lapilli Tuff (2-64mm)*c Lapillistone (76"Xo*ct Cataclastic*d Block ^64mmXXenolith*e Autoclastic/Hyaloclastic*f Thickly Laminated*g Thinly Laminated*h Clast Supported*i Matrix Supported*j Granule (grit 2-4mm)*k Pebble (4-64mm)*l Cobble (64-256mm)

*m Boulder ^256) ̂ ^ ^

*n Graded Bedding*o Cross bedding*p Fault Gouge*q Augen*r Porphyroblastic*s Hornfels*t foliated/sheared*u folded*v boudinage*w fragmental (felsi^mafic)*x fragmental (mafic>felsic)*y Crystal Tuff (>50% of frags)*z Lithic Tuff (>50% of frags)

ALTERATION CODES

FORMS SpotsF Fracture/vein controlled P Pervasive

STRENGTH S Strong M Moderate W Weak

MINERALIZATION CODES

FORMD Disseminated/Blebs F Fracture/vein controlled M Massive B Bedded C Clasts/Fragments

PERCENTAGE

Numeric pecentage, or percentagerange (i.e. 1-3"Xo), must always be

specified

Example: EpPW = Epidote,Pervasive.Weak Example: CpB3"Xo = Chalcopyrite, Bedded, 3"7o

Amended Timmins ROCK Legend

5. MINERALOGICAL NAMES

AkAlbAl

AmAhAdAyApAr

AspAsbAugAzBabiBiBoGaCnGcCpChlCl^Gr

CpxCoCvCtDpDolEpiFeiFI

ActinoliteAlbiteAlmandineAmphiboliteAnhydriteAndalusiteAnthophylliteApatiteArgentiteArsenopyriteAsbestosAugiteAzuriteBariteBismuthiteBiotiteBorniteCalciteChalcedonyChalcociteChalcopyriteChloriteChloritoidChromiteClinopyroxeneCobalt MineralsCovelliteCordieriteDiopsideDolomiteEpidoteFeldsparFluorite

FcGnGtVGGfGSGypHemHbHyII

I-FJrKyLsLm

MagMeMaMiMkMiMoMuNeNeNiOvOr

OpxPIPg

FuchsiteGalenaGarnetGoldGraphiteGravel & sandGypsumHematiteHornblendeHyperstheneIlmeniteIron FormationJarositeKyaniteLimestoneLimoniteMagnetiteMalachiteMarcasiteMicaMicroclineMilleriteMolybdeniteMuscoviteNephelineNiccoliteNickel mineralsOlivineOrthoclaseOrthopyroxenePhlogopitePlagioclase

PnPyPxPoQtRoRuSurSeShSidSil

SimSpsSphTiAgSp

SpdStSbSulS-MS-DTkTeTt

Ta-CITITr

WoZr

PentlanditePyritePyroxenePyrrhotiteQuartzRhodochrositeRutileSerpentineSericiteScheeliteSideriteSilicaSilliminiteSpessariteSphaleriteSphene (Titanite)SilverSpinelSpodumeneStauroliteStibniteSulphidesMass. SulphidesDiss. SulphidesTalcTellurideTertrahedriteTantalite-ColumbiteTourmalineTremoliteWollastoniteZircon

6. ROCK TYPE 1 PROTOLITH

<QFG><QTZ><MAR><SKA><PHY>Ô^<SYN><GRA>Ôl^<GRD><APL><FEL>^D^<GAB><NOR>^N^^^

QuartzofeldspathicQuartziteMarbleSkarn(Calc-Silicate)PhylliteTonaliteSyeniteGraniteMonzoniteGranodioriteApliteFelsiteQuartz DioriteGabbroNoriteAnorthositeDiorite

<PER><SER>ÛN^<PRX><LMP>*SS^^R^^C^<CGL>^Ll^<ARG>^X^^Ô^^^<CIF><SHA>*1S^

PeridotiteSerpentiniteDunitePyroxeniteLamprophyreSandstoneArkosic sandstoneGraywackeConglomerateSiltstoneMudstone-argilliteChert/exhaliteSilicate IFOxide IFSulphide IFCarbonate IFShaleLimestone

<CHM><SLA>^ll\^<CAR><AMP>^^<PEG>ÊOÊU*-:UN^<UMF><MAF><AND><DAC><RYD><RHY><SCL><RWV>

Chem. Precip.SlateKimberliteCarbonatiteAmphiboliteMigmatitePegmatiteLeucocraticMelanocraticUnknown ProtolithUltramaficMaficAndesiteDaciteRhyodaciteRhyoliteSulphide ClastsReworked Volcanic Debris

HOLE NUMBER: HOT12-01FALCONBRIDGE LIMITED DRILL HOLE RECORD IMPERIAL CHITS:

OS/13/2002 METRIC OMITS: X

PROJECT NAME: (292 PROJECT BOMBER: 8292CLAIM NOMBER: '"VlZIC, 5 7/

LOCATION: Hutt 12 Grid

PLOTTING COORDS GRID: DIM Zone 17NORTH: 5309S13.00NEAST: 487(03.COEELBV: 300.00

ALTERNATE COORDS GRID:NORTH: 10+20S EAST: 17*40E ELEV: 300.00

COLLAR DIP: -55' 'LENGTH OP THE HOLE: 165.SON

START DEPTH: O.OOMFINAL DEPTH: 165.SOU

COLLAR ASTRONOMIC AZIMUTH: O* O' GRID ASTRONOMIC AZIMUTH: 349" O'

DATE STARTED: 12/01/1900DATE COMPLETED: 12/03/1900

DATE LOOSED: 12/03/1900

COLLAR SURVEY: NOROD LOG: NO

HOLE MAKES HATER: NO

PULSE EM SURVEY: NOPLUGGED: NO

HOLE SIZE: BQ

CONTRACTOR: NDS Diamond DrillingCASINO: left in hole - 4m

CORE STORAGE: Mineaite UTM COORD.:

COMMENTS : HEDGES AT:

DIRECTIONAL DATA:

Depth (M)

Astronomic Azimuth

Dip Type of FLAG degrees Test

Depth (M)

Astronomic Azimuth

Dip Type of degrees Test

20.00 3' O- O" -S3' O' O" S OK70.00 2* O' O" -S3' O' O' S OK137.00 359' O 1 O' -52' O' O" S OK165.00 S' O' O" -51' O' O' S OK

ROLE NUMBER: HOT12-01 DRILL ROLE RECORD

HOLE NUMBER: HUT12-01 DRILL HOLE RECORD DATE: 05/13/2002

FROM TO

0.00 TO

4.00

4.00 TO

165.60

ROCK TYPE

*2,m,bx* Mafic Volcanic, massive, in-situ brecciated

TEXTURE AND STRUCTURE

-dark greenish gray -wkly fol'd *45-60deg. TCA -mod. to strongly broken core to "17m

-fine grained with mm-sized mafic phenocryst* comprising *^\ of unit -bx'd hyaloclastitic/glasay cone b/t 16. 4-16. 801 w/ calcitic amygdule* along lower margin of zone

fll7.0-17.Bj*-jFAIf-* -broken, gritty core w/ bull qtx veining

-discontinuous bx'd pillow selvages apparent locally -bleached, glassy hyaloclastite bx'n with ropey textures locally

-more typical massive textures w/ weak in-situ bx'n below 61m

-Simla r bx'n as between 56. 4-60. 5m

fl87.4-87.6fc*-|FAlf-* broken, gritty core

-quartz feldspar porphyry dyke -30-40* phenocrysts are sub-rounded and 2 -5mm in diameter -sharp but sheared uphole contact -faulted lower contact

-pastey gouge w/ fault breccia

-bx'd mafic volcanic below porphyry dyke, grading to more massive textures below 110m

{132. 0-132. Sf.SMS.

AMSLETO ra————

ALTERATION———————————————————————————————

-strongly epidote altered, pervasive and fracture-controlled -weak to mod. qtc/calcite veining -weak gash chlorite fractureing with weak pervasive chlorite throughout -weakly carbonatized (pervasive) locally

'

-strong epidote alteration within bx'd zone with mod. fracture controlled chlorite defining brecciation

-pinkish hematite alteration/oxidation

MINERALIZATION

-tr.-lt Py as clots/knots disseminated sporadically throughout unit -granular Py clots up to lcm in diameter

-5-7* diss. Py

-nil sulphides within dyke

REMARKS

ROLE NUMBER: HUT12-01 DRILL HOLE RECORD LOGGED BY: Dean Rogers PAGE:

HOLE NUMBER: HDT12-01 DRILL HOLE RECORD DATE: 05/13/2002

FROM TO

165.80TO

165.80

ROCK TYPE

•E. O.H.IEnd-Of-Role

TEXTURE AND STRUCTURE

-zone of 15-25* fracture controlled PoV-tr.-l*Py -explanation of weak, TEM conductor -pale brown, largely non-magnetic Po - ' res inous ' appearance -sulphides surround angular fragments of in-situ brecciated mafic volcanic-tr. Cpy7

-similar Po*X-Py rich tones between 133. 9-134. Om, 145. 9-146. 9m t 151 .6-154 .9m-S-10% sulphides within minor zones

fll36. 4-137. Ol*6,b,m*-thin dyke w/ sharp contact WSdeg. TCA -med. to coarse grained, pinkish brown unit -mottled, cumulate textures locally

-uniform and massive textured mafic volcanic for remainder of hole

ANGLE TO CA ALTERATION

-wkly carbonatised dyke

-epidote alteration decreasing slightly below 140m where epidote veinleta dominate and pervasive epidote alteration ends

MINERALIZATION———————————————————————————————————

-2-3* Py w/in gabbro dyke

REMARKS

HOLE NUMBER: HDT12-01 DRILL HOLE RECORD LOGGED BY t Dean Rogers PAGE: 3

HOLE NUMBER : HUT12-01 ASSAYS SHEET DATBi 13/05/2002

Sample From (M)

To (M)

Leng. (M)

Cu ppm

Zn ppn

Pb ppn

Hippm

Au ppb

Ag

AD033BB 132.00 132.50 0.50AU033B9 133.90 134.00 0.10AU03390 145.90 146.90 1.00AU03391 154.60 155.00 0.40

290200117103

1369881

13 t57

38404034

21177

27

0.8 0.5 0.3 0.2

HOLE NUMBER: HOT12-01 ASSAYS SHEET

HOLE NUMBER : HDT12-01

Sample From To Leng.

KA03450 23.00 26.00 3.00 AU06399 80.00 63.00 3.00 AU03385 104.00 106.00 2.00 AU06400 128.00 131.00 3.00 AU03387 136.40 137.00 0.60 AU03396 158.00 161.00 3.00

(3EOCHEMICAL ASSAY DATS: 13/05/2002

SI02 AL203 GAO MOO NA2O K20 FB203 TI02 P205 MHO LOISDMYZR CO ZN HI CR FIELD CHEM ALUM

| ——————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————48.110 11. COO S. 9400 4.4200 3.2200 0.3800 K. 870 1.7800 0.2600 0.2600 4.6100 3S.OOO 142.00 98.000 90.000 33.000 60.000 49.620 12.040 7.0400 .1100 3.4200 0.1800 15.880 1.8800 0.2600 0.2100 4.3700 32.000 140.00 103.00 80.000 36.000 66.000 71.460 13.410 0.8500 .3500 5.9400 1.4300 2.9700 0.3600 0.0900 0.0400 1.1600 8.0000 67.000 3.0000 48.000 9.0000 164.00 47.590 12.590 5.8700 .8900 3.8200 0.1900 18.840 1.9700 0.2400 0.2600 3.2700 37.000 134.00 69.000 94.000 26.000 64.000 58.430 13.380 6.0500 .0200 4.9100 2.6700 6.0400 0.6700 0.3600 0.0900 1.3400 14.000 127.00 19.000 17.000 36.000 247.00 49.470 11.860 6.3200 .2600 3.8500 0.2600 17.720 1.9000 0.2300 0.2SOO 2.9200 34.000 131.00 103.00 76.000 24.000 48.000

.

'

HOLE NUMBER: HUT12-01 GEOCHEMICAL ASSAY

HOLE NOMBER : HDT12-01 GEOCHEMICAL ASSAYS DATE: 13/05/3002

Sample Prom To (H) (M)

Leng. (H)

CO PPM

V PPM

KA03450 23.00 26.00 3.00A006399 80.00 83.00 3.00AD03385 104.00 106.00 2.00AU06400 128.00 131.00 3.00AD033B7 136.10 137.00 0.60A003386 158.00 HI.00 3.00

44.00042.0009.000044.00015.00039.000

0.2300 174.000.1000 196.000.0050 21.0000.1400 209.000.3700 37.0000.0800 194.00

HOLE NDMBER: HOT12-01 GEOCHEMICAL ASSAYS

HOLE NUMBER : HOT12-01 GEOCHEMICAL ASSAYS DATE: 13/05/2002

Sample From To (M) (H)

Leng. (H)

SC PPM

MOO* CA/AL NI/MGO ISHIKN ZN/NA2PPM

KA034SO AU06335 AU03385 AU06400 A0033B7 AU03366

23.0080.00

104.00128.00136.40158.00

26.0013.00

106.00131.00137.00161.00

3.003.002.003.000.603.00

7.0000e.oooo 2.50002.50002.50007.0000

10.000 10.000 2.0000 10.000 2.0000 B.0000

HOLE NUMBER: HUT12-01 GEOCHEMICAL ASSAYS

Swastika Laboratories LtdEstablished 1928 Assaying - Consulting - Representation

Geochemical Analysis Certificate 1W-0028-RG1

company: FALCONBRIDGE LTD EXPLORATION Date JAN-09-01Project: 292Attn: D. Rogers

We hereby certify the following Geochemical Analysis of 4 Core samples submitted JAN-04-01 by .

Sample NumberAU03388AU03389AU03390AU03391

Au PPB21177

27

Cu PIM290200117103

Zn PFM136988188

Pb PFM13857

Ag PPM0.80.50.30.2

Ni PFM38404034

Certified by-

l Cameron Ave., P.O. Box 10, Swastika, Ontario POK l TO Telephone (705) 642-3244 Fax (705) 642-3300

CHIIVHTEC BONDAR CLEGG VAMCOUVM MANCH

Rapport Lab Gt jhimie Geochemical Lab Report

CLIENT: FALCON EXPLORATION, KIDD CREEK HINESITE REPORT: T01-57008.0 ( COMPLETE )

SAMPLE NUMBER

AU 03385 AU 03386 AU 03387 AU 03392 AU 06399

AU 06400 KA 03450

DATE RECEIVED: 08-JAN-01 DATE PRINTED: 17-JAN-01PROJECT: 292

PAGE 1A( M 2)

71.46 13|48;:0.85 ||p5.94

49.47 l;pa|;6.32 11^3.85 -

58.43 1:p3S^6.05 |^tl;::4.91

47.59 12.5^5.87 4*8^3.82

48.11 Ili.iai6.94 li?

2.97 p|36|0.09 ?:0;164 |||99.24 67

17.72

' 6.04

:; 2.77

O;,.:i9 18.84 t.:9|:0.24

Oi38::;16.87 1:178^0.26

66 |||:99.04

64 lip:99.57

60 41^11:98.49

76;

64

18

86

51

;:35l42

48 i

76:

17

68

80 \

94;90

2 *; 21

; 6 80 i

37

174

<5

<5

<5

<5

^<5

8 ;:

9

|s 14

i;: 9

6

15

3

9

16

17

16

2-

im'm-

Chimitee - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178. Fax: (819) 825-0256

CHIIVHTEC:BOIMD/VR

Rapport Lab Ge ,himie Geochemical Lab Report

CLIENT: FALCON EXPLORATION, KIDD CREEK MINESITE REPORT: T01-57008.0 ( COMPLETE } DATE RECEIVED: 08-JAN-01 DATE PRINTED: 17-JAN-01

PROJECT: 292 PAGE 1B( 2/ 2)

SAMPLE NUMBER

ELEMENT Nb UNITS PPM

AU 03385 AU 03386 AU 03387 AU 03392 AU 06399

28

23

10

AU 06400

KA 03450

1010

Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

Geophysical Survey Report

covering

Borehole Pulse EM Surveysover

Hutt Gridfor

Falconbridge Ltd.during

September -October, 2001

by

CRONE GEOPHYSICS & EXPLORATION LTD.

Survey Area: Hutt Grid,Timmins, Ontario

Survey Type: 3D Borehole Puke EM Survey

Survey Operator. Tom Myers, Dan Brazeau

Holes Surveyed: 1201

Survey Period: September 17* -October 1st, 2001

Report By: Kevin Ralph

Report Date: October 2001

Submitted To: Falconbridge Ltd.Timmins

Crone Geophysics & Exploration Ltd.

TABLE OF CONTENTS

1 INTRODUCTION

2 PERSONNEL

3 SURVEY METHOD Si EQUIPMENT

4 SURVEY PARAMETERS

5 PRODUCTION SUMMARY

Appendices

Appendix A: Plan Map and Primary Field Sections

Appendix B: Linear (5-axis) Pulse EM Data Profiles

Appendix C: Step Response Profiles

Appendix D: Pulse EM Data Profiles (Lin-Log scale)

Appendix E: Crone Instrument Specifications



1. INTRODUCTION

Crone Geophysics A Exploration Limited was contracted by Falconbridge Ltd. to conduct a 3 Dimensional Pulse Electromagnetic Borehole survey on its Hutt Grid near Timmins, Ont. This report summarizes the geophysical work carried out on the property during the period of September 17*, - October 1 st, 2001. During this time period one hole was surveyed. The initial survey of this hole was conducted on September 17th. However, the inherent noise levels in the data were unacceptable to Crone so the hole was later repeated on October l*. The appendices to this report contain the plan and section maps, step response profiles, linear profile plots, PBM profiles in a lin-log format and the Crone Instrument Specifications.

2. PERSONNEL

The following personnel were involved in the collection of the data and production of this report:

Survey Operators: Tom Myers, Dan Brazeau Report: Kevin Ralph

3. SURVEY METHOD A EQUIPMENT

Crone Pulse EM is a time domain electromagnetic method in which a precise pulse of current with a controlled linear shut off is transmitted through a large loop of wire on the ground and the rate of decay of the induced secondary field is measured across a series of time windows during the off-time. The EMF created by the shutting-off of the current induces eddy currents in nearby conductive material thus setting-up a secondary magnetic field. When the primary field is terminated, this magnetic field will decay with time. The amplitude of the secondary field and the decay rate are dependent on the quality and size of the conductor.

On this project, a 3D Borehole Pulse EM system was assembled in which an axial component (Z) probe and a cross component (XY) probe were used to measure the three components of the induced secondary field. The first pass with the 'Z' probe detects any in-hole or off-hole anomalies and gives information on size, conductivity, and distances to the edge of conductors. The second pass with the 'XY' probe measures two orthogonal components of the EM field in a plane orientated at right angles to the borehole. These results give directional information to the center of the conductive body.


Crone Geophysics A Exploration Ltd.

The rotation of the XY probe was corrected through the use of an orientation tool, so that positive X points in the direction of the hole azimuth and positive Y is horizontal and points to the left of an observer looking down the hole.

In addition to measuring the standard Primary Pulse channel on the ramp and the 20 off-time channels, the Step Response was also calculated. Step Response requires accurate geometrical control in which the loop position and the hole geometry are accurately determined. Ideally loop geometry is supplied as GPS coordinates while hole geometry is given as Gyroscopic readings. The hole geometry data is then processed by Crone to produce a smoothly segmented hole, and together with loop geometry data, a new PBM data file is formed. The Crone Step Response transformation was then performed on the data. The calculated Step Response values are binned into an SI channel (from 0.5T to T), an S2 channel (from 0.25T to 0.5T), an S3 channel (from 0.125T to 0.25T) and an S4 channel (from 0.0625T to 0.125T, where T is the time base). The SI channel is normalized to the theoretical primary field, while S2, S3 and S4 are normalized to SI.

The equipment used on this project was a Crone Pulse EM Borehole system. This includes a 4.8kW transmitter with a 220V voltage regulator which is powered by a 11 hp motor generator. The Crone Digital Receiver was used to collect the field data. The synchronization between the Transmitter and the Receiver was maintained by direct cable sync for the borehole work. Using sync cable is the most accurate type of synchronization because it is a direct connection between the Transmitter and Receiver.

4. SURVEY PARAMETERS

Table I: Borehole Survey CoverageHole

1201

Txloop

Hutt-A, -B

Collar Location

1740 E -1020 S

Dip at collar

54"

Azimuth

15"

Depth (meters)

160

Length Read

(meters)

20-160

Component

X.Y.Z

Table II: Borehole and Surface Loop CoverageLoop

Hutt-A

Hutt-B

Size (meters)200x200

200x200

Location

1600E-1800E 960 S -1160 S1600E-1800E 985 S -1185 S

Ramp Time

1.5ms

1.5ms

Current

16.5 amps

12 amps

Time Base

16.66ms

8.33ms

Date SurveyedSeptember 1 7*, 2001

October 1 st, 2001



The following table shows the various time gates, in ms, that constitute the channel configurations set up in the Crone PEM Receiver.

Table III: Channel Configuration, 20 ChannelsChannel

PP246B10121416IS20

Start-1.982e-046.2996-051.125e-042.027eX)43.6006-046.389e-041.129e-031. 9936-033.514e-036.192e-031.091e-02

finish-9.900e4)58.550e-051.5316-042.700e-044.815e-048.505e-041.4986-032.646e-034.6666-038221e-031.4496-02

Channel135791113IS1719

Start4.950e-058.550e-051.5316-042.7006-044.815e-048.505e-041.498&032.6466-034.6666-038.2216-03

Finish6.2996-051.125e-042.0276-043.6006-046.389e-041.129e-031.993e-033.5146-036.1926-031.091e-02

5. PRODUCTION SUMMARY

Table IV: roduction SummarySeptember 17*. 2001

October l", 2001

Laid loop, surveyed hole 1201 at 16.66 ms time base, picked up loop and brought all gear from the grid.Laid loop, surveyed hole 1201 at 16.66 ms time base, picked up loop and brought all gear from the grid.

ly submitted,

l

Kevin RalphvCrone Geophysics St, Exploration Ltd.October 2001


Crone Geophysics b Exploration Ltd.

Appendix A:Plan Map and Primary Field Sections


1600E900S-

1700El

1800E l

1000S-

1201

Tx Loop Hutt-B

1100S-

Scale 1:250025 O 25 50———^—"Mi———

(metert)

1200S-

Falconbridge Ltd.Hutt Grid

3-D Borehole Pulse EM Survey Borehole Se Loop Location Map

Hole: 1201Survey Date: Oct 1, 2001

Crone Geophysics Se Exploration Ltd.

0

-100

-200

-300

-400

1750 E, 1100 S l 1 t l~l *

1

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Hole: 1201Survey Date: Oct 1 , 2001

Crone Geophysics A Exploration

Field

Ltd.

Crone Geophysics fa Exploration Ltd.

Appendix B:Linear (5-axis) Pulse EM Data Profiles


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Appendix C:Step Response Profiles


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Crone Geophysics de Exploration Ltd.

Appendix D:Pulse EM Data Profiles (Lin-Log scale)


CRONE GEOPHYSICS & EXPLORATION LTD Borehole Pulse EM Survey

Client : FALCONBRIDGEGrid : HOTDate : Oct l, 2001

Hole : 1201Tx LOOp : HUTFile name : 1201XYT.PEM

Data Corrected for Probe Rotation using Orientation Tool #13 X COMPONENT dBx/dt nanoTesla/sec - 16 of 16 channels and PP

Scale: 1:1250

-105 -104 -103 H03

CRONE GEOPHYSICS fi EXPLORATION LTD Borehole Pulse EM Survey

Client : FALCONBRIDGEGrid : HOTDate : Oct l, 2001

Hole : 1201TX Loop : HUTFile name : 1201XYT.PEM

Data Corrected for Probe Rotation using Orientation Tool #13 Y COMPONENT dBy/dt nanoTesla/sec - 16 of 16 channels and PP

Scale: 1:1250

-105 -104 -103 102 + 103 + 104-J—t. l l l IIJ————i J—' ,*fA

CRONE GEOPHYSICS 6 EXPLORATION LTD Borehole Pulse EM Survey

Client : FALCONBRIDGEGrid : HUTDate : Oct l, 2001

Hole : 1201Tx Loop : HOTFile name : 1201Z.PEM

Z COMPONENT dBz/dt nanoTesla/sec - 16 of 16 channels and PP Scale: 1:1250

-105 -104 -103 -102 -l

20m

30m

40m

50m

60m

70m

80m

90m

100m

110m

120m

l- 130m

140m

150m

160m


Appendix E: Crone Instrument Specifications



CRONE PULSE EM SYSTEM

SYSTEM DESCRIPTION

The Crone Pulse EM system is a time domain electromagnetic method (TDEM) that utilizes an alternating pulsed primary current with a controlled shut-off and measures the rate of decay of the induced secondary field across a series of time windows during the off-time. The system uses a transmit loop of any size or shape. A portable power source feeds a transmitter which provides a precise current waveform through the loop. The receiver apparatus is moved along surface lines or down boreholes.

The transmitter cycle consists of slowly increasing the current over a few milliseconds, a constant current, abrupt linear termination of the current, and finally zero current for a selected length of time in milliseconds. The EMF created by the shutting-off of the current induces eddy currents in nearby conductive material thus setting-up a secondary magnetic field. When the primary field is terminated, this magnetic field will decay with time. The amplitude of the secondary field and the decay rate are dependent on the quality and size of the conductor. The receiver, which is synchronized to the off-time of the transmitter, measures this transient magnetic field where it cuts the surface coil or borehole probe. These readings are across fixed time windows or "channels".

SYSTEM TERMINOLOGY

Ramp Time"Ramp time" refers to the controlled shut-off of the transmitter current Three ramp times are

selectable by the operator, 0.5ms, 1.0ms, and 1.5ms. By controlling the shut-off rather than having it depend on the loop size and current ensures that the same waveform is maintained for different loops so data can be properly compared.

The 1.5ms ramp is the normally used setting for good conductors. It keeps the early channel responses on scale and decreases the chance of overload. The faster ramp times of 1.0ms and 0.5ms will enhance the early time responses. This can be useful for weak conductors when data from the higher end of the frequency spectrum is desired.

Time BaseTime base is the length of time the transmitter current is off (it includes the ramp time). This also

equals the on time of the current Eight time bases are selectable by the operator. They include the original time bases used in the analog system as well as time bases to eliminate the effects of powerline interference. The eight time bases are as follows: compatible to analog Rx: 10.89ms, 21.79ms; 60hz powerline noise reduction: 8.33ms, 16.66ms, ft 33.33ms; 50hz powerline noise reduction: 10.00ms, 20.00ms, St 40.00ms

Since readings are taken during the off cycles, the time base will have an effect on the receiver channels. Normally, a standard time base is selected for the type of system and survey being used, but this can be changed to suit a particular situation. A longer time base is preferred for conductors of greater time constants, and in surveys such as resistive soundings where more channels are desired

Zero Time SetThe term "zero time set" or "ZTS" refers to the starting point for the receiver channel

measurements. It is manually set on the receiver by the operator thus allowing adjustments for the ramp times and fine tuning for any fluctuations in the transmitter signal.

Crone Pulse EM System Description l


Receiver ChannelsThe rate of decay of the secondary field is measured across fixed time windows which occupy

most of the off-time of the transmitter. These time windows are referred to as "channels". These channels are numbered in sequence with "l" being the earliest The analog and datalogger receivers measured eight fixed channels. The digital receiver, being under software control, offers more flexibility in the channel positioning, channel width, and number of channels.

FP ChannelThe PEM system monitors the primary field by taking a measurement during the current ramp

and storing this information in a "PP channel". This means that data can be presented in either normalized or unnormalized formats, and additional information is available during interpretation. The PP channel data can provide useful diagnostic information and helps avoid critical errors in field polarity.

SynchronizationSince the PEM system measures the secondary field in the absence of the primary field, the

receiver must be in "sync" with the transmitter to read during the off-time. There are three synchronization methods availablercable connection, radio telemetry, and crystal clock This flexibility enhances the operational capabilities of the system.

SURVEY METHODS

The wide frequency spectrum of data produced by a Pulse EM survey can be used to provide structural geological information as well as the direct detection of conductive or conductive associated ore deposits. The various types of survey methods, from surface and borehole, have greatly improved the chances of success in deep exploration programs. There are eight basic profiling methods as well as a resistivity sounding mode.

Moving CoilA small, multi-turn transmitter loop (13.7m diameter) is moved for each reading while the

receiver remains a fixed distance away. This method is ideal for quick reconnaissance in areas of high background conductivity.

Moving LoopSame as Moving Coil method, but with a larger transmit loop (100 to 300 meters square). This

method provides deeper penetration in areas of high background conductivity, and works best for near-vertical conductors. This method can be used in conjunction with the Moving In-loop survey for increased sensitivity to horizontal conductors.

Moving In-LoopA transmit loop of size 100 to 300 meters square is moved for each reading while the receiver

remains at the center of the loop. This method provides deep penetration in areas of very high background conductivity, and works best for near-horizontal conductors. It can be used in conjunction with the Moving Loop survey.

Large In-LoopA very large, stationary transmit loop (800m square or more) is used, and survey lines are run

inside the loop. This mode provides very deep penetration (700m or more) and couples best with shallow dip conductors (^5 deg.) under the loop.

Crone Pulse EM System Description 2

Crone Geophysics cfc Exploration Ltd.

DeepemA large, stationary transmit loop is used, and survey lines are run outside the loop. This mode

provides very deep penetration, and couples best with steeply dipping conductors (M5 deg.) outside the loop.

Borehole (Z Component only)Isolated Borehole: A drill hole is surveyed by lowering a probe down a hole and surveying it with

a number of transmit loops laid out on surface. The data from multiple loops gives directional information on the conductors.

Multiple Boreholes: One large transmit loop is used to survey a number of closely spaced holes. The change in anomaly from hole to hole provides directional information. These methods have detected conductors to depths of 2500m from surface and up to 200m from the hole.

3-D BoreholeDrill holes are surveyed with both the Z and the XY borehole probes. The X and Y components

provide accurate direction information using just one transmit loop.Since the probe rotates as it moves down the hole a correction is required for the X-Y data. This

is accomplished in one of two ways. The standard approach is to use the measurement of the primary field from the "PP" channel, apply a "cleaning" algorithm to remove most of the secondary field contamination, and compare this to theoretical values. The amount of probe rotation is then calculated, and the correction can be made. The second method involves the use of an optional orientation device for the X-Y probe which is produced in co-operation with IFG Corp. This attachment uses dipmeter? to calculate the probe

, rotation.

Underground BoreholeUnderground drill holes can be surveyed in any of the above mentioned borehole methods with

one or more transmit loops on the surface. Near-horizontal holes can be surveyed using a push-rod system.

Resistivity SoundingsBy reading a large number of channels in the centre of a transmit loop it is possible to perform a

decay curve analysis giving a best-fit layer earth model using programs such as ARRTI or TEMDC.

EQUIPMENT

Transmit LoopsThe PEM system can operate with practically any size of transmit loop, from a multi-turn

circular loop 13.7m in diameter, to a l or 2 turn loop of any shape up to l or 2 kilometers square using standard insulated copper wire of 10 or 12 gauge. The multi-turn loop is made in two sections with screw connectors. The 10 or 12 gauge loop wire comes on spools in either 300m or 400m lengths. The spools can be mounted on packframe winders for laying out or retrieving.

Power SupplyThe PEM system normally operates with an input voltage from 24v to 120v. Modifications have

recently been made to increase the power to 240 volts. The maximum current is still 20 amps. For low power surveys a 20amp7hr 24v battery can be used. The power supply requires a motor generator and a voltage regulator to control and filter the input voltage to the transmitter.

Specifications: PEM Motor Generator- 4.5 hp Wisconsin, (2 kw) - 11 hp Honda (4 kw); 4 cycle engine- belt drive to D. C. alternator- cable output to regulator


Crone Geophysics 6 Exploration Ltd.

- maximum output: 120v, 20amp (2 kw); 240v, 20amp (4 kw)- fuse type overload protection-steel frame- external gas tank- unit weight: 33kg (2 kw); 52kg (4 kw)- optional packframe- wooden shipping box- shipping weight: 47kg (2 kw); 80kg (4 kw)

Specifications: PEM Variable Voltage Regulator- selectable voltage between 24v and 120v or 48v and 240v- 20amp maximum current- fuse and internal circuit breaker protection- cable connections to motor generator and transmitter- anodized aluminum case- unit weight 10kg; shipping weight 18kg- padded wooden shipping box

TransmitterThe transmitter controls the bi-polar on-off waveform and linear current shut-off ramp. The latest

2000w PEM Transmitter has the following specifications:

Specifications: PEM Transmitter-timebases: 10.89ms, 21.79ms, 8.88ms, 16.66ms, 33.33ms, 10ms, 20ms, 30ms- ramp times: 0.5ms, 1.0ms, 1.5ms- operating voltage: 24v to 120v (2 kw); 48v to 240v (4 kw)- output current: Samp to 20amp- monitors for input voltage, output current, shut-off ramp, tx loop continuity, instrument temperature,

and overload output current- automatic shut-off for open loop, high instrument temperature, and overload- fuse and circuit breaker overload protection- three sync modes: 1) built-in radio and antenna

2) cable sync output for direct wire link to receiver or remote radio3) connectors for the crystal clock

- anodized aluminum case- optional packframe- unit weight 12.5kg; shipping weight 22kg- padded wooden shipping box

ReceiverThe receivers measure the rate of decay of the secondary field across several time channels. Three

types of receivers are available with the PEM system: Analog Rx, Datalogger Rx, and Digital Rx. The Analog Rx and Datalogger Rx read eight fixed time channels while the Digital Rx, under software control, offers a variety of channel configurations. The Digital Rx has been used in the field for contract surveys since 1987.

Specifications: Digital PEM Receiver- operating temperature -400C to 500C- optional packframe- unit weight 15kg; shipping weight 25.5kg- padded wooden shipping box


Crone Geophysics (fe Exploration Ltd.

Menu driven operating software system offering the following functions:- controls channel positions, channel widths, and number of channels- time bases: 10.89ms, 21.79ms, 8.88ms, 16.66ms, 33.33ms, 10ms, 20ms, and 30ms- ramp time selection- sample stacking from 512 to 65536- scrolling routines for viewing data- graphic display of decay curve and profile with various plotting options- routines for memory management- control of data transmission- provides information on instrument and operating status

Sync EquipmentThere are three modes of synchronization available; radio, cable, and crystal clock. The radio

sync signal can be transmitted through a booster antenna from either the PEM Transmitter internal radio or through a Remote Radio.

Specifications: Sync Cable- 2 conductor, 24awg, Teflon coated- approx. 900m per aluminum spool with connectors

Specifications: Remote Radio- operating frequency 27.12mhz- 12v rechargeable gel cell battery supply- fuse protection- sync wire link to transmitter- coaxial link to booster antenna- anodized aluminum case- unit weight 2.7kg

Specifications: Booster Antenna- 8m, 4 section aluminum mast- guide rope support- 'A wave CB fiberglass antenna- range up to 2km- coaxial connection to transmitter or remote radio

Specification: Crystal Clocks- heat stabilized crystals- 24v rechargeable gel cell battery supply- anodized aluminum case- rx unit can be separate or housed in the receiver- outlet for external supplementary battery supply

Surface PEM Receive Coil, The Surface PEM Receive Coil picks up the EM field to be measured by the receiver. The coil is j; mounted on a tripod that can be positioned to take readings of any component of the field



Specifications: Surface PEM Receive Coil- ferrite core antenna- VLF filter- 10khz bandwidth- two 9v transistor battery supply- tripod adjustable to all planes- unit weight 4.5kg; shipping weight 13.5kg- padded wooden shipping box

Borehole PEM Z Component ProbeThe Z component probe measures the axial component of the EM field The Z component data is

not affected by probe rotation so no correction are required.

Specifications: Borehole PEM Z Component Probe- fenite core-dimensions: length- 1.6m; dia-3.02cm (3.15cm for high pressure tested probes)- internal rechargeable ni-cad battery supply- replaceable heat shrink tubing for abrasion protection- pressure tested for depths 1300m, 2000m, and 2800m- packaged in padded cover and aluminum tube- shipped in padded wooden box; total weight 17kg

Borehole PEM XY Component ProbeThe XY probe measures two orthogonal components of the EM field perpendicular to the axis of

the hole. Correction for probe rotation can be achieved by two methods. The standard approach is to use the measurement of the primary field from the "PP" channel, apply a "cleaning" algorithm to remove most of the secondary field contamination, and compare this to theoretical values. The amount of probe rotation is then calculated, and the correction can be made. The second method involves the use of an optional orientation device for the X-Y probe that uses dipmeter? to calculate the probe rotation.

Specifications: Borehole PEM XY Component Probe- ferrite core- dimensions: length - 2.01m; dia - 3.02cm- internal rechargeable ni-cad battery supply- selection of X or Y coils by means of a switch box on surface or automatic switching with Digital

receiver- replaceable heat shrink tubing for abrasion protection- pressure tested for depths to 2800m- packaged in padded cover and aluminum tube- shipped in padded wooden box; total shipping weight 20kg

Orientation DeviceThe orientation device is an optional attachment for the XY probe which measures the rotation of

the probe using two dipmeters.

Specifications: Orientation Device- 2 axis tilt sensors- sensitivity +A 0. l deg.


Crone Geophysics de Exploration Ltd.

- operating range -89.5 to -10 deg.- dimensions: length - 0.94m; dia - 28.5cm- packaged in padded cover and aluminum tube- shipped in padded wooden box; total shipping weight 11kg

Borehole EquipmentTo lower the probe down a drill hole requires a cable and spool, winch assembly frame and cable

counter. Borehole surveys also require equipment to "dummy probe" the hole before doing the survey.

Specifications: Borehole Cable- two conductor shielded cable- kevlar strengthened- lengths are available up to 2600m on three sizes of spools.- shipped in wooden box

Specifications: Slip Ring- attaches to side of borehole cable spool providing a connection to the receiver while allowing the spool to turn.

-VLF filter- pure silver contacts

Specifications: Borehole Frame- welded aluminum frame- removable axle- chain driven, 3 speed gear box- hand or optional power winding- handbrake and lock- two sizes: standard for up to 1300m cable; larger for longer cables- shipped in wooden box

Specifications: Borehole Counter- attaches to the drill hole casing- calibrated in meters- shipped in wooden box; total weight 13kg

Specifications: Dummy Probe and Cable- solid steel or steel pipe- same dimensions as borehole probe- shear pin connection to dummy cable- steel dummy cable on aluminum spool- cable mounts on borehole frame- various lengths to 2600m on 3 spool sizes.


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ONTMUO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No: Recording Date: Approval Date:

Client(s):130679

Survey Type(s):

W0260.00810

2002-MAY-15

2002-JUN-06

Work Report Summary

Status: APPROVED

Work Done from: 2000-DEC-01

to: 2001-SEP-17

FALCONBRIDGE LIMITED

ASSAY DHGEO PDRILL

Work Report Details:

Claim* Perform

P 1227824 SO

P 1236371 316,211

P 1236372 SO

316,211

External Credits:

Reserve:

Perform Applied Approve Applied Approve

SO S3.200 33,200

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30 36,400 36,400

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30 2003-MAY-22

S211 2003-MAY-20

SO 2003-MAY-20

3211

321 1 Reserve of Work Report*: W0260.0081 0

321 1 Total Remaining

Status of claim is based on information currently on record.

41P14NE2011 2.23526 HUTT 900

2002-Jun-10 13:59 Armstrongjd Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date:2002-JUN-10

Ministere duDeveloppement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5

FALCONBRIDGE LIMITEDSUITE 1200, 95 WELLINGTON STREET WESTTORONTO, ONTARIOM5J 2V4 CANADA

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

Dear Sir or Madam

Submission Number: 2.23526 Transaction Number(s): W0260.00810

Subject: Approval of Assessment Work

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

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

If you have any question regarding this correspondence, please contact STEVEN BENETEAU by email at [email protected] or by phone at (705) 670-5855.

Yours Sincerely,

Ron GashinskiSenior Manager, Mining Lands Section

Cc: Resident Geologist

Falconbridge Limited (Claim Holder)

Assessment File Library

Falconbridge Limited (Assessment Office)

Dean Rogers (Agent)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:17150

MINING LAND TENURE

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ADMINISTRATIVE DISTRICTS l DIVISIONSMining Division PorcupineLand Titles/Registry Division SUDBURY

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FALCONBRIDGE LIMITEDExploration Division Timmins, ONTARIO

Hutt-Halliday Project PN 292

Hutt 12 Grid DDH HUT12-01

1:2,00041P14NE2011 2,23526 HUTT

RPT ON DIAMOND DRILLING HUTT TP€¦ · Dean Rogers 41P14NE2011 2.23526 HUTT 010. Diamond Drilling...

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