GOODWIN MINERAL EXPLORATIONSJohn R. Goodwin, MSc Consulting Geologist

42A01NE0116 63.5649 TECK010

GEOPHYSICAL REPORT

on Claim LI, 1135908

in Teck Township

for

Mr. II. Moore

.J;inu;iry 27, 1990 John R. C.ooiUvin

R.R. O , Powassan, Ontario POH 1ZO 705-724-5017

42A81NE0116 63.5649 TECK

TABLE OF CONTENTS

010C

Page INTRODUCTION . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . lPROPERTY LOCATION AND ACCESS . . . . . . . . . . . . . . . . . . . l

CLAIM LOCATION . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . l

TOPOGRAPHY . ............. . . . . . . . . . . . . . . . . . . . . . . . 5PREVIOUS EXPLORATION . . . . . . . . . . . . . . . . . . . . . . . . . . . 5

GENERAL GEOLOGY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7

STRUCTURE ...................................... 10ECONOMIC GEOLOGY . ... . . . . . . .. . . . . . . . . . . . . . . . . . . . 11GEOPHYSICAL SURVEYS ... . .. . . . . . . . . . . . . . . . . . . . . . . 12

DISCUSSION ..................... . . . . . . . . . . . . . . . . 13

RECOMMENDATION . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 14

CERTIFICATE . . . . . . . . . . . . . . . . .. . ................. 15

FIGURES

Figure l- Property Location . . . . . . . . . . . . . . . . . . . . 2Figure 2- Location and Access . . . . . . . . . . . . . . . . . . 3Figure 3- Claim Location . . . . . . . . . . . . . . . . . . . . . . . 4TABLES

Table l- Stratigraphic Section ................. 8MAPS

VLF Survey- 2 directions . . . . . . . . . . . . . . . . . . . . . . . in back pocketMagnetometer Survey . . . . . . . . . . . . . . . . . . . . . . . . . . . . in back pocketIP Survey . . . . . . . . . . . .. . .. . . .................... in back pocketAPPENDIX A- Report of Work Technical Data Statement APPENDIX B- Technical brochures- VLF, Magnetometer, IP.

John R. Goodwin, MSc Consulting Geologist

GOODWIN MINERAL EXPLORATIONSJohn R. Goodwin, MSc Consulting Geologist

INTRODUCTION

Teck township is located on the western section of the Kirkland Lake gold hearing camp that extends easterly through Kirkland Lake, Larder Lake and across the northwestern part of Quebec. Kirkland Lake ranks as the second largest gold -producing camp in Ontario. The bulk of the production has been produced by seven mines located in the eastern part of the township along the main ore zone. To date, however, no large ore bodies have been found outside of the main cam]) although future exploration in some areas may reveal commercial gold deposits.

PROPERTY LOCATION AND ACCESS

The subject claim is located in the northwest corner of Teck township in the Kirkland Lake mining camp (Figure 1). The property is located between Winnie Lake , site of a base metal occurence, and Amikougami Creek. Access is attained via Highway 66 to Goldthorpe Road, then westerly to Amikougami Creek. A bush trail leads northerly for 3 miles to the property (l ; igure 2 ) .

CLAIM LOCATION

This claim, LI, J 1 35908, was restaked after an inspection by ODM personell due to overstaking by other parties. The owner of this claim, Mr. II. Moore, has also staked a fraction immediately to the south of the subject claim but it is not included in thisreport (Fi gurc 3) .

R. R. 1/3 , Powassan, Ontario POI1 1110 705-724-5017

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.nrx,

l : igurc 1. Property Location

John R. Goodwin, MSc Consulting Geologist

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Figure 2. Location and Access

John R. Goodwin, MSc Consulting Geologist

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A r m t r Lake? . .

] ; igurc 3. C]aim Location

John R. Goodwin, MSc Consulting Geologist

-5-

TOPOGRAPHY

Precambrian rock outcrops cover the greater part of Teck township.

In the northern part of the township the topography becomes quite

rugged, especially west of Amikaugami Lake where a range of hills

rises more than 400 feet above the lake level. The high ridges are

generally found -within the areas underlain by gabbro, diorite or

massive greenstone. The Cobalt series sediments also tend to stand

out prominently. Amikougami Lake's long dimension is about parallel

to the strike of the pillow lavas in that area. A significant

feature of the topography is the way in which sheared and faulted

zones are indicated by linear rock depressions. For this reason,

streams sometimes mark the position of faults as represented by

Blanche River, Amikougami Creek and Murdock Creek. The most important

structure in the country from an economical standpoint is the

Kirkland Lake fault which is expressed topographically only in

the western part of Teck township.

PREVIOUS EXPLORATION

There is no recorded exploration work carried out on this claim.

Work carried out in the immediate area includes:

1984-Argcntex Resources Exploration Corp.-a nine claim group immediately north of the subject claim-regional geology, detailed mapping, trenching and sampling.-Archean mafic volcanics, massive diabasic basalt, pillowed flows, flow breccia, agglomerate and tuffs intruded by gabbro 'and syenite. Lesser amounts of interflow sediments including chert and graphitic chert.

-stratigraphy strikes at 030 to 035 degrees

John R. Goodwin, MSc Consulting Geologist

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-bcst precious metals were: .06 Au; 1.31 Ag/2.2 1 - in sulphide zone..07 Au; 1.0 Ag/1.7 1 - in sulphide zone. .092 Au; 0.57 Ag/ 1.6'- under shaft

- further work is pending

The Magni prospect is located in the cast-central portion of

Grenfell township and about 2^ miles southwest of the subject claim.

The prospect warrants discussion in this report because of similar

geological elements and a possibility that similar structural and

mineralogical parameters are present. The prospect contains Keewatin

mafic inctavolcanics and gabbro cut by small dykes of porphyry and

diabase. Several east-west trending mineralized zones are associated

with shearing and host quartz stringers with chalcopyrite, pyrrhotite,

pyrite and minor gold. Three zones have been identified averaging

3 feet wide by 800 feet long. The No. l zone returned assays up to

1.25 oz/ton gold. The No. 3 zone and on the 125 foot level returned assays up to 2.30 oz/ton gold.

GENERAL GliOl.OGY

The township is underlain by Precambrian age rocks and the formations

of interest belong to the earlier portions consisting of volcanics,

sediments and intrusives. Stratigraphic and structural studies

show that these rocks are greatly deformed by folding and faulting.

They arc also scpcrated by a great erosional and structural

unconformity into two main age groups (Table 1). The older group

consists of volcanics that underlie the northern and southern

parts of the area and belong to the Keewatin Period. The younger

sedimentary-volcanic complex is classified as part of the

John R. Goodwin, MSc Consulting Geologist

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Tabie l- Reg-ional Stratigraphic Section

QUATERNARYPLEISTOCENE: Clay, sand, gravel

Great unconformity PRECAMBRIANHURONIAN (COBALT SERIES): Conglomerate; arkose, greywacke, slate.

Great unconformity POST-ALGOMAN: 1 Diabase, lamprophyreIntrusive contactALGOMAN:

TIMISKAMING:

KEEWATIN:

Syonilc porphyry, quartz-feldspar porphyry, alaskite.Quartz porphyry.Basic syenite, augite syenite, and lamprophyre; augite porphyrite.Hornblendite, biotitite, diorite.Granite and syenite,Carbonated rock or "dolomite."2Diorite and gabbro; quartz diorite and quartz gabbro. 9

Intrusive contactTrachyte; trachytic breccia.Tuff and agglomerate; tuffaceous conglomerate.Conglomerate, greywacke, basal grit.

Great unconformityTuff and iron formation.Altered basic volcanics.Intermediate and basic volcanics (greenstone).

John R. Goodwin, MSc Consulting Geologist

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Timiskaming Scries. It is predominantly sedimentary in character

with several interbedded horizons of volcanics and pyroclastics.

Throughout the Keewatin Series are bodies of gabbro and diorite

that are intrusive into the basal formations of the Timiskaming

Series. Both of these Series are cut by irregular Algoman age

intrusive bodies and dykes ranging from acid to basic in composition.

Keewatin Series

This series is mainly composed of andesite-basalt lavas. The flows

are massive and show primary structures such as vesicles, amygdules,

spherules and pillows. Fragmental volcanics are widely distributed

and narrow bands of volcanic breccia probably represent fragmental

tops of lava flows. Throughout the Keewatin volcanic series it is

difficult to distinguish between the coarse grained thick flows

and intrusive diorite and/or gabbro. Narrow bands of bedded cherty

tuff and iron formation are occasionally interbedded with the lava

flows. The iron formation contains narrow seams of fine grained

magnetite. The tuffs show differential weathering, are thin bedded,

and in some areas are sufficiently ferruginous to weather a rusty

gossan.

Timiskaming Series

This series consists of interbedded sedimentary and volcanic units

which Jie with great unconformity on the Keewatin Series. These

rocks represent a continuous belt that may extend west to Matachewan

under the Cobalt Series and easterly through Larder Lake and

northwestern Quebec. The Timiskaming is divided into two distinct

lithologic units consisting of conglomerate and greywacke in one

and pyroclastics with trachytic volcanics in the other. The

John R. Goodwin, MSc Consulting Geologist

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pyroclastics consistiof agglomerates and water-laid tuffs. In Teck

township the Timiskaming strata face south and rest unconformably

on Keewatin::volcanics to the north and are in fault contact with

the same volcanics to the south.

Algoman In tru s i ve s

A variety of Algoman intrusivcs have invaded rocks of the Timiskaming

and Keewatin Series, These intrusivcs include: diorite and gabbro, quartz diorite, quartz gabbro; granite and syenite; hornblendite,

biotite and diorite; syenite and quartz feldspar porphyry. It is

often difficult to establish relative ages of the intrusions

because contact relationships cannot be observed.

Carbonated flocks

The carbonated rocks were formed by the replacement of pre-existing

rocks by siliceous carbonate materials. The type and degree of

alteration varies from place to place and the bodies are quite

irregular in outline. The carbonated rocks are composed mainly of

silica and carbonates of magnesium, calcium and iron. The rock

frequently contains a bright green fuchsite or mariposite and is

intersected by a network of quartz vcinlets. Most of the carbonated

bodies occur as elongated ban.ds and lenses along sheared zones

that strike about paralic] to the stratigraphy. The strongest and

most persistent sheared zone is localized along or near the south

margin of the Timiskaming Series in Teck township and is believed to be the westerly extension of the Larder Lake "break".

STRUCTURE

Faults are of great economic importance owing to the fact that the

John R. Goodwin, MSc Consulting Geologist

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seven ore bodies in the Kirkland Lake area are located along a fault system. It is also significant to note the*relative age of the fault with respect to the time of ore formation. The strike faults arc generally more liable to be pre-ore and thus of economic interest while the cross faults are usualy known to be post-ore. The strike faults have a thrust displacement and probably originated during the long period of regional folding and igneous intrusions. Faults may be represented by a wide zone of shearing or brecciation and in some instances has been followed by carbonatization, silicification and vein formation. The Kirkland Lake and Larder Lake faults are significant strike faults in the area.

ECONOMIC GHOLOGY

In tlic past all of the gold production has come from mines in Teck township and are located on a major structural "break". In nearly all of the occurcnccs, gold is found in quartz veins or stringer zones, syenite porphyry and carbonate alteration adjacent to the structure isinvariably present. The mineralization consists mainly of pyrite with lesser amounts of chalcopyrite, galena, molybdenum and specularite. In some places high gold values are associated with patches of heavy sulphide mineralization with some native gold reported.

Widespread exploration throughout the Kirkland Lake- Larder Lake gold belt has shown that orebodies have a closer relationship to structures than to rock type. Emphasis should thus be placed on the tracing out and investigating pre-ore fault structures (strike faults). The close association between the productive veins and

John R. Goodwin, M Se Consulting Geologist

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the Kirkland Lake fault systemhas focused attention on its extension westward across the country. The development of important subsidiary

veins on the south side of the main fault sysytem suggests that

similar interesting conditions might be found at other places along

the fault system west of the Macassa mine.

GEOPHYSICAL SURVEYS

A program of geophysical surveys was carried out on the subject

clain to locate and trace potential gold-bearing shear/fault zones

containing disseminated sulphides. The program includeddtime-domain

I.P., VLF and magnetometer surveys carried out by Oxsics Exploration

Ltd. on .January 16, 17 and 18, 1990. The property owner, Mr. II. Moore,

arranged for the linecutting at 200' line spacing and 100' stations

for a total of 1.87 line miles. The survey results are enclosed in

the back pocket.

Magnetometer Survey

A magnetometer survey using an lil)A OMNI-IV total field unit was used

over the grid. This instrument has an accuracy of" - l nnno-tcsla.n

and all readings were diurnally corrected by a base station recorder.

A reference field of 59,092 was selected and for plotting purposes

a datum value of 58,000 wns subtracted from all readings. The data

was contoured at 100 to 400 nano-tesla intervals.

The magnetic pattern indicates a change in magnetic suscepability

from the north half to the south half. The known regional geology

supports this response with volcanics to the north and gabbro/diorite

to the south.

John R. Goodwin, MSc Consulting Geologist

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VLF Survey

The VLF survey was read in two directions using an EDA OMNI-PLUS

with in-phase dip angle and quadrature being recorded. Two fixed

transmitter stations using a frequency of 24.0 (Cutler, Maine)

and 21.4 (Annapolis, Md.) were plotted. The readings from Cutler,

Maine gave the best response with a wide response on LO+00 possibly

due to two conductors. At L4+OOW the response is strongest and is due to a single conductive source. West of this line the response is

very weak possibly due to conductive overburden or it is very deep.

IP Survey

A dipole-dipole time domain IP survey was conducted over the claim

using an l i DA IP-2 receiver and a Scintrex IPC-9 transmitter at an "a" spacing of TOO". Pseudo-sections of resistivity and chargeability

are plotted and a chargeability profile for each line is presented. An anomaly is identified as u zone of low resistivity and high

chargeability in response to disseminated semi-conductors such as

pyrite. A conductive zone is identified on the pseudo-sections from LO+00 to L12+OOW. The anomaly from LO+00 to L6+OOW is a wide,

chargeable zone with direct VLF correlation. Beyond this point

the response is less clear and. may be due to end of conductor effects.

The geophysical surveys carried out to date indicate a moderate

conductor trending east -northeast to west-southwest through the

central portion of the property. The conductor has good IP and VLF

correlation and does not appear to have any direct magnetic

association indicating that magnetite and/or pyrrhotite is not

John R. Goodwin, MSc Consulting Geologist

-J4-

present in the structure. The magnetic patterns indicate the claim

is underlain by volcanics in the north half and diorite/gabbro in

the south.

The anomaly response is typical of disseminated sulphides and it

is not known at this time if the anomaly is a contact or structural

feature. This property warrants further exploration in the summer

to carry out detailed geological mapping, prospecting, trenching

and diamond drilling if warranted.

RECOMMENDATIONS

This conductive zone warrants detailed surface exploration as follows Phase .1

Geological mapping- l man for 2 days

Trenching- 2 men for 2 days

Assaying . . . . . . . . . . . . . . . . . . . . . . . . . . .

Accomodati on/Transportation

Drafting/Assessment report

Total Phase l

Phase 2

Diamond Drilling- 2,500 feet in 5-500 1 holesall inclusive @ iZO.OO/foot .

Assaying . . . . . . . . . . . . . . . . . . . .

Drill Supervision/Assessments

Total Phase 2

$1,000.00

1,000.00

500.00

500.00

2,000.00

S5,000.00"

$50,000.00

1,000.00

5,000.00

S56,000.00

John R. Goodwin, MSc Consulting Geologist

-15-

CERTlFJCATli

I, John R. Goodwin of R. li. #3 powassan, District of Parry Sound in the Province of Ontario DO HEREBY CERTIFY THAT:

1. I am a Consulting Geologist

2. I have practiced my profession since 1969.

3. I am a graduate of Laurentian University in Sudbury, Ontario where J obtained a MMc degree in Geological Sciences.

4. I am a Fellow of the Geological Association of Canada.5. This report, dated January 27, 1990 on Claim LL 1135908 in

Teck Township, Kirkland Lake District, Ontario is based on data compiled by the author on published government reports, maps and assessment records on file at the Resident Geologists office in Kirkland Lake and survey data collected and copiled by Exsics Exploration Ltd, who carried out the surveys.

6. l have no interest in this property or any securities held by Mr. 11. Moore.

DATED THIS 27th DAY OF JANUARY, 1990

'JOHN R. GOODWIN

John R. Goodwin, MSc Consulting Geologist

APPENDIX A

-Report of Work

-Technical Data Statement

John R. Goodwin, MSc Consulting Geologist

Ministry ofNorthern Developmentand Mines

Ontnno

Instructions- Please type or print.- Refer to Section 77, the Mining Act (or assessment work requirement;.

and maximum credits allowed per survey type.- tt numhor ol mining clninis traversed oxcoods spurn on Ihis loini.

Of Work a ttach a list.- Technical Reports and maps in duplicate should be submitted h Mining AC! ( Gcophysicnl. Goologicfll and Gooohomical Sllivoy:.) Mminii l uncls Koclion, Mimual Dovolopnuinl and limits HiaiH h

,[".' o f Survey(s)

^VLF, Magnetometer, IP) M nmri DIVIS on

Larder LakeTownship or Area

Teck Township'Uv.nidod Holder(s)

.-.....,.....-,^Mr..... H. Moore. ,. ...^_.........,....... ... .... . ........_,.__.Address

P.O. Box 10, New Liskeard, Ontario __.Survey Company

___lixsics Explpj'ation Ltd ^ ___fJamri and Address of Author (ol Goo-Technical Report)

John R . Goodwin R.R. #3 Powassan, Ontario

Prospector's Licence No

K 17625Telephone No.

647-5179

Dale of Survey (from ft to)

o46 J ,90Orndit.s Requested per r^-h Claim in Columns at right Mining Claims Traversed (List in numerical sequence)

.-r.' r ial Provisions

! o; fi";t su'voy

l HUM 40 days. (This includes linn culling)

F or each additional survey using the same grid:

('mer ?0 days (for each)

Man Days

Complete reverse side and mer lotal(s) here

Airborne Credits

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Etooliomac nolu:

- Magnetometer

- Other , p

Geological

Goochnmical

Goophysic.il

- Electromagnelic

- Magnelorneter

- Other

Geological

Gnocnomic.il

Electromagnet c

Magnetometer

Other

Total miles flown over claim(s). Dale Recorded Holder

27 .Jan. 90

1 )ays pei Claim

20

-2D....

Days por Claim

Days pei Claim

3r Agent (Signature)

1.

F'mlix

LI,

lining Claim

Number

1135908

-

N " - - Prolix

lining Claim

Number

- -- ..-...-- -

Mining Cl.nm

Prefix

-

. ,. .--

Tolal number ol mining claims covered by this roport ol work.

Number

|

1Ci'ililication V(Mifyiit(| llc|ioit of Work

l hi'iiiliy (;ertily Hint l liavi; n p.'i'.'inal and intimate knowkjdije ol the lads sel tuilh in tins Hupoil ci Wink, having perluiined illei il!. completion and aniH'xrt! rtiport is tine.

Name and Address ol Person Certifying

John R. Goodwin R. R. #3 Powassan, OntarioTplOf) HIIK! t in

724-5037

For Office Use Only

Days Date Recorded

l).Ill' Apllliivi"! .r. Iter.Oliii'il

Mining Recorder

t'h'vinn.il M.maqi'i, Mniiii(| l .imi:.

wilnpssod sajne riurilu] iind/ui

Hate JTertified By (Signature)

27 Jan. 1990Received Stamp

Ministry ofNorthern Developmentand Mines

Ontario

Geophysical-Geological-Geochemical Technical Data Statement

File—

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT !

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC. f

Type of Survcy(s) V LP ' Magnetometer, TPTownship or Area Teck Township Claim Holder(s) Mr t H .

Survey Company Rxsir.s F.xpl nra t i nn LtdAuthor of Report John R . Hoodwi nAddress of Author, R . R . Pnv\f,'l On t n r i n

Covering Dates of Survey Jan 2 to Jan 27 1990(linecutting to office)^ "

1.87 milesTotal Miles of Line Cut.

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

RAYS-, , . . per claimGeophysical--Electromagnetic. 40————-Magnetometer____20

-Radiometric————————— j-Other_____________ ; Geological——.—...-——.—--— Geochemical——^—..———

AIRBORNE CREDITS (SpcciaJ provision credits do not apply to airborne lurveyi)

Magnetometer. .Electromagnetic(enter dayt per

DATE: Jan. 77 1QQQ SIGNATUR:uthor of Report or Agent

Res. Geol.. .Qualifications.Previous Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

(prefix) (number)

TOTAL CLAIMS.

837 (85/12)

GEOPHYSICAL TECHNICAL DATA

•^i^

Number of Static VLl ; - 392 Mag- 196_______Number of Readings VLF-392 Mag- 196 Station interval-——-—SO.fcct__________________Line spacing 200fect_____________ Profile scale —————————————————————————————————————————————————————— Contour interval 100 nao-teslas___________________________________

Instrument EDA OMNI- IV____________________________________________ Accuracy - Scale constant - One 119310- tesla_________________________________ Diurnal correction method RDA OMNI IV Base station recorder—————-——--—.——- Base Station check-in interval (hours) 30 seconds^___^__________________________Base Station location and value _____L Q at 0 + 00.

Instrument iqiA OMNH -P1.1IS

Coil configuration Coil separation —.Accuracy ————Method: Q Fixed transmitter Q Shoot back O In line CD Parallel line Frequency, 24. O Cutler Maine—-..——21.4 Annapolis Md.—————-—————————

(specify V.L.F. station)

Parameters measured^..,...Jj3lRh.aA^^iR

Instrument.Scale constant.Corrections made.

Base station value and location

Elevation accuracy.

Instrument Reelevcr-BDA IP-2__________Transmitter- Scintrex IPC-9Method E Time Domain CD Frequency DomainParameters — On time 2 sec.___________________ Frequency —-————..—.—.——

- Off time 2 see.____________________ Range ___________-- Delay time 500 milliseconds———m.——.- Integration timp 420 milliseconds—————

Power 200 watts______________________________________________ Electrode array___Dlpol e-DipOle————————————————————————————————-——— Electrode spacing _LQJI feot————Nf l , 2 , 5——————————————————————-———— Type of electrode Stainless steel____________—————————————————————

APPENDIX B

-Technical Brochures- VLF, Magnetometer, IP

John R. Goodwin, MSc Consulting Geologist

IP-2 TWO DIPOLETIME DOMAIN IP RECEIVER

MAJOR B ENEFITS

*

*

*

A

*

TWO DIPOLES SIMULTANEOUSLY MEASURED

SOLID STATE MEMORY

AUTOMATIC PRIMARY VOLTAGE (Vp) RANGING

AUTOMATICALLY CALCULATES APPARENT RESISTIVITYCOMPUTER COMPATIBLE

fO/V instrument* Inc., l load Of f Ice: A Thorncllffc P.irK Drive, Toronto, Can.irf,i Mill iHt iclpplionc: MIE) /125-7800, Telex: 06 2 3 121 EDA TOR. Cables: INSTRUMENTS 1iniiwv, rnAiin(ruiiipiifsinc.,5l5IWarclRoa(J, Wlic.n uuge,

Specifications ,Dipoles ....... .. .... ... ...... .Twosimultaneous input dipoles.Input Voltage (Vp) Range ......... .40 microvolts to 4 volts, with automatic ranging andovervoltage protection.Vp Resolution ... ..,............ 10 microvolts.Vp Accuracy ,.......,,..,..... .D.3% typical; maximum 1 0Xo over temperature range.Chargeability Resolution ......,,. .1 0Xo.Chargeability Accuracy .......... .D.3% typical; maximum 1 0Xo over temperature rangeforVp^OmV.Automatic SP Compensation ....... ± 1 V with linear drift correction up.to 1 mV/s.Input Impedance .,......,....... 1 Megohm. -.-.Sample Rate ...............,... 10 milliseconds.Automatic Stacking ...... .,...... 3 to 99 cycles.Synchronization.. .............. .Minimum primary voltage level of 40 microvolts.Rejection Filters.. ............. .. 50 and GO Hz power line rejection greater than100 do. . 'Grounding Resistance Check ....,. . 100 ohm to 128 kilo-ohm. -,Compatible Transmitters......... .Any time domain waveform transmitter with a pulseduration of 1 or 2 seconds and a crystal timing stability of 100 pprn.Programmable Parameters ........ Geometric parameters, time parameter, intensity ofcurrent, type of array and station number.Display... . .. . .. . .., . . . . .. ...., Two line, 32-characl.er alphanumeric liquid crystaldisplay protected by an internal healer for low temperature conditions.Memory Capacity ...... . ......,. 600 sets of readings.RS-232C Serial I/O Interface ........ 1200 baud, 8 data bits, 1 stop bit, no parity.Console Power Supply .. . . ... . ... .Six-1.5V "D" cell disposable batteries with amaximum supply current of 70 mA and auto power save.Operating Environmental Range .... - 2f) 0C to -i 550C; Q-100% relative humidity;weatherproof.Storage Temperature Range ,..,...-400C to-f 600C. '-

, ' ' ' K ThortKUffc Park Drive,Weight and Dimensions.........., 5.5 kg, 310x230x210 mm. Toronto,Canada M4H 1111Standard System Complement ..... Instrument console with carrying strap, batteries and Ic!? ?G ";" r;(w) ,operations manual. : StfSXS* 1oro"toAvailable Options...... . . . ...... .Stainless steel transmit! ing electrodes, copper in us Asulphate receiving electrodes, alligator clips, bridge ' s l'"r"'sl"c leads, wire spools, interface cables, rechargeable viat batteries, charger and software programs.

(503)4229112

ri lot c J In Canada

HA,-*/ /tlUW

INDUCED FOIARIZATION AND D. C. RESISTIVITY TRAHSM1TIER

2.0 SPECIFICATIONS

Maxitnun Output Power

Output Voltage

Output Current

Meter Ranges

Automatic Cycle Timing

Automatic Polarity Change

Pulse Durations

Period Time Stability and Accuracy

Open Loop Protection

Synchronization Output

Internal Power Sources

External Power Sources

200W defined as when current is on and into a resistive load*

Switch selectable at nominal nettings of 15, 150, 210, 300, MS, 600 or 850 V,

l.5 A maximum,

Switcli selectable at 50 mA, 150 mA, 500 mA, 1500 mA full neale with accuracy of *3X of full scale*

T:T:T:T; onsofftontoff*

Each 2T.

T is switch selectable at l, 2, 4, 8, 16 or 32 seconds.

Cryntfll controlled to better thnn 0.002 percent of the selected pulse duration.

High voltage is automatically turned off if the output power is less than 2 W. This can be overridden manually for tenting purposes. This protection in not effective at the 15 V output.

Optically Isolated, suitable for external synchronization of the I PR-11 multichannel IP Receiver.

Two battery packs are ntnndard, each containing 4 GC 660-1 lead-acid gel-type batteries giving 24 V at 12 Ah.

One Penlite battery, Eveready E91 or equivalent.

24 V DC supply at maximum 10A.

2 -

Power for Battery Charger

Dimensions and Weights

Operating Temperature Range

Standard Equipment

Optional Equipment

Shipping Weight

115 or 230 VAC, 50 to 400 lit, 100 W.

Transmitters with two batterypacks:140 x 300 x 460 mm; 16.0 kg

Single battery pack:140 x 300 x 150 mm; 6.2 kg

Charger:140 x 300 x 150 tnm; 5.5 kg

-30"C to *55'C.

Console, 2 battery packs, battery charger, carrying harness. Two giant banana plugs, minor spare parts kit.

, wire, porous pots, electrodes, major spare parts kit, radio transceivers, back pack.

46 kg includes reusable wooden shipping case.

2-2

r?,,.

Specifications*Frequency Tuning Range.

Transmitting stations Measured.

Recorded VLF Magnetic Parameters

.15 to 30 kHz, with bandwidth of 150 Hz; tuning range accommodates new Puerto Rico station at 28.5 kHz. up to 3 stations can be automatically measured at any given grid location within frequency tuning range

Standard Memory capacity.

Display

,. Total field strength, total dip, vertical quadrature (or alternately, horizontal amplitude).. 800 combined VLF magnetic and VLF electric measurements as well as gradiometer and magnetometer readings

.. .Custom designed, ruggedized liquid crystal display with built-in heater and an operating temperature range from -400Cto 4-55cC. The display contains six numeric digits, decimal point, battery status monitor, signal strength status monitor and function descriptors.RS232C Serial I/O Interface ...... 2400 baud rate, 8 data bits, 2 stop bits, no parityTest Mode ................... .A. Diagnostic Testing (data and programmablememory)

B. Self Test (hardware)Sensor Head .................. contains 3 orthogonally mounted coils withautomatic tilt compensationOperating Environmental Range ...................... -40ccto *55 0C;

O -10096 relative humidity; weatherproofPower supply ..............,.. Non-magnetic rechargeable sealed lead-acid 18VDC battery cartridge or belt; 18V DC disposable battery belt; 12V DC external power source for base station operation only.Weights and Dimensions Instrument Console .......... 2.8 kg, 128 x 150 x 250 mmSensor Head................. 2.1 kg, 130 dia. x 130 mmVLF Electronics Module........ 1.1 kg, 40 x 150 x 250 mmLead Acid Battery cartridge ... 1.8 kg, 235 x 105 x 90 mm M|d Acid Battery Belt ........ 1.8 kg, 540 x 100 x 40 mm^posable Battery Belt ....... 1.2 kg, 540 x 100 x 40 mm•Preliminary

EDA instruments inc., 4 Thorncllffe Park Drive, toronto, Ontario Canada M4H 1H1 Telex: 06 23222 EDA TOR. Cables: Instruments Toronto (416) 425-7800in USA,EDA instruments inc.,5151 Ward Road,Wheat Ridge, ColoradoU.S.A. 80033(303)422-9112

Printed In Canada

SpecificationsDynamic Range

Tuning Method . Automatic Fine Tuning ,Display Resolution Processing Sensitivity Statistical Error Resolution . Absolute Accuracy

Standard Memory Capacity Total Field or Gradient Tie-Line Points Base Station

Display

RS 232 Serial I/O interface Gradient Tolerance Test Mode

Sensor

j Gradient Sensors

Sensor Cable . . .Cycling Time (Base Station Mode) . .Operating Environmental Range Power supply

Battery Cartridge/Belt Life .

Weights and Dimensions instrument Console Only NiCad or Alkaline Battery Cartridge NiCad or Alkaline Battery Belt Lead-Acid Battery Cartridge Lead-Add Battery Belt . Sensor Gradient Sensor

(0.5 m separation - standard) Gradient Sensor

(1. 0 m separation- optional) . System complement

Base Station Option Gradiometer Option

18,000 to 110,000 gammas. Roll-over display feature suppresses first significant digit upon exceeding 100,000 gammas.Tuning value is calculated accurately utilizing a specially developed tuning algorithm ± 1594 'relative to ambient field strength of last stored value

.0.1 gamma . ± 0.02 gamma .0.01 gamma± 1 gamma at 50,000 gammas at 23 0 C ± 2 gamma over total temperature range1,200 data blocks or sets of readings100 data blocks or sets of readings5,000 data blocks or sets of readingsCustom-designed, ruggedized liquid crystal display with anoperating temperature range from -40*C to -f 55"C. Thedisplay contains six numeric digits, decimal point, batterystatus monitor, signal decay rate and signal amplitudemonitor and function descriptors.2400 baud, 8 data bits, 2 stop bits, no parity6,000 gammas per meter (field proven)A. Diagnostic testing (data and programmable memory)B. Self Test (hardware)

Optimized miniature design. Magnetic cleanliness Isconsistent with the specified absolute accuracy.0.5 meter sensor separation (standard), normalized togammas/meter, optional 1.0 meter sensor separationavailable. Horizontal sensors optional.Remains flexible in temperature range specified, includesstrain-relief connectorProgrammable from 5 seconds up to 60 minutes In 1second increments-40"C to -i- 55 0 C; D-100% relative humidity; weatherproofNon-magnetic rechargeable sealed lead-acid batterycartridge or belt; rechargeable NiCad or Disposable batterycartridge or belt; or 12V DC power source option for basestation operation.2,000 to 5,000 readings, for sealed lead acid power supply,depending upon ambient temperature and rate ofreadings

2.8 kg, 238 x 150 x 250mm 1.2kg, 235 x 105 x 90mm

,1.2kg, 540 x 100 x 40mm 18 kg, 235 x 105 x 90mm 1.8 kg, 540 x 100 x 40mm 1.2 kg, 56mm diameter x 200mm2.1 kg, 56mm diameter x 790mm2.2 kg, 56mm diameter x 1300mminstrument console; sensor; 3-meter cable, aluminumsectional sensor staff, power supply, harness assembly,operations manual.Standard system plus 30 meter cablestandard system plus 0.5 meter sensor

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