l41O09NW0030 2 16410 MALLARD 010

RECE.-.VED

•L F EP 13 1996

GEOPHYSICAL/GEOLOGICAL REPORT

ON THE

1995 EXPLORATION PROGRAM

MALLARD TOWNSHIP PROPERTY

MALLARD TOWNSHIP, PORCUPINE MINING DIVISION, ONT.

2. 184 10

ky- rSubmitted by: Steven D. Anderson \f , 'J-Jan.10, 1996 -

41O09NW0030 2 16410 MALLARD 010C

TABLE OF CONTENTS

PageINTRODUCTION. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . l

LOCATION AND ACCESS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

CLAIM STATUS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

SURVEY PERSONNEL . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

PREVIOUS WORK . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3

REGIONAL GEOLOGY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3

PROPERTY GEOLOGY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3

LINECUTTING . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4

MAGNETOMETER SURVEY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4

VLF-EM SURVEY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5,6

I . P . SURVEY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6,7

PROSPECTING . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7,8

SURVEY RESULTS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 9

CONCLUSIONS AND RECOMMENDATIONS . . . . . . . . . . . . . . . . . . . . . 10

CERTIFICATION. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11

APPENDICES

APPENDIX "A" : EDA OMNI PLUS, MAGNETOMETER

APPENDIX "B" : GEONICS EM- 16, VLF

APPENDIX "C" : SCINTREX IPR-12, TIME DOMAIN I. P. RECEIVER

APPENDIX "D: : SCINTREX IPC-9, 2 . 5KW I. P. TRANSMITTER

LIST OF MAPS

MAP NO. l

MAP NO. 2

MAP NO. 3

MAP NO. 4

CONTOURED TOTAL FIELD MAGNETOMETER SURVEY

CONTOURED FRASER FILTERED VLF SURVEY

PROFILED VLF SURVEY

PROSPECTING AND SAMPLE LOCATION MAP

PLATE l of l : I. P. PSUEDOSECTIONS- L100W, L200W, L500W, L700W

INTRODUCTION

This report deals v/ith the logistics and results of an exploration program conducted on the Mallard Township Property in 1995. The claims are held by Steven D. Anderson, and the work was funded in part by an OPAP grant issued to him.

The exploration program, subject of this report, consisted of Linecutting, Mag/VLF Survey, I.P. Survey, prospecting/mapping, and blast ing/trenching.

The purpose of the I.P. Survey was to look for disseminated sulphides as well any zones of alteration or silicification. The Mag/VLF Survey was done to aid in outlining any geological units or structures within the grid. This data can then be correlated with with the I.P. results.

The program was successful in outlining several I.P. anomalies. Anomalous gold values were also obtained from the prospecting and sampling done.

Results from the exploration program were quite promising and it is felt that a much more extensive program is warranted.

•3 90 S3 •O 73

33-

30-

43-

PROJECT LOCATIONX

U.S.A.

O 30 100 130 nllet

93

90 as 80

PROVINCE OF ONTARIO

FIG l

STEVE ANDERSON OPAP 1995

MALLARD TOWNSHIP PROPERT

LOCATION MAP

LOCATION AND ACCESS

The Mallard Township property is located approximately 120km. southwest from the city of Timmins, Ontario. It is situated within the central portion of Mallard Twp. with the Opeepeesway River running through the north-eastern part of the block. The property is located in the Porcupine Mining Division, Ontario, NTS Sheet, Ridout, 410/NE, and UTM co-ordinates, 5285000mN, 403000mE.

Access to the property was gained by taking Hwy 144 south from Timmins for roughly 130km to the intersection of Hwy 144 and Hwy 667. Heading west on Hwy 667 from the junction of Hwyl44 for about 45km will bring you to the where a major logging road crosses this Hwy in a north- south direction. Going north on this logging road for 23km will bring you to where the road crosses the Opeepeesway River. At this point you are about 2km. south of the block. Logging roads heading north from here provided access to the southern and northeastern portions of the block.

CLAIM STATUS

The work program outlined in this report was done on the following unpatented mining claims held by S. Anderson:

1201578......................9 units............Ma l lard Twp.1201579. . . . . . . . . . . . . . . . . . ....l unit.............Mallard Twp.1181446......................9 units............Mallard Twp.

PERSONNELThe following personnel were directly involved with this

program, which was carried out between June, 1995 to October, 1995:

S. Anderson. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .TimminsR. Meikle...................................TimminsD. MacArthur................................TimminsA. Durham...................................TimminsK. Giroux...................................Timmins

-nL: STEVE ANDERSON OPAP 1995

Proo.r.tu: MALLARD TOWNSHIP PROPERTY

Tiil.:

REGIONAL LOCATION MAP

/

3M.- -

FIO 3

STEVE ANDERSON OPAP 1995

MALLARD TOWNSHIP PROPERTY

Titl.:

CLAIM SKETCH

400 NORTH

300 NORTH

ZOO NORTH

100 NORTH

BMC LINE

100 SOUTH

ZOO SOUTH

500 SOUTH

400 SOUTH

500 SOUTH

600 SOUTH

700 SOUTH

SOO SOUTH

400 NORTH

SOO NORTH

ZOO SOUTH

OPEEPEESWAY RIVER

300 SOUTH

400 SOUTH

SOO SOUTH

600 SOUTH

TOO SOUTH

BOO SOUTH

TTJPO LJECEM3

Cltli LU.

014Tr** L l M

FIO 4

Cli.nt: STEVE ANDERSON OPAP 1995

MALLARD TOWNSHIP PROPERTY

TiU.:

GR l D SKETCH

PREVIOUS WORKIn 1974 the northern portion of the block was held by Cominco.

The work conducted included, AEM survey that was followed up by ground work. This took the form of a linecutting program which was then covered with magnetic and electromagnetic (Max-Min) surveys. These surveys did not cover the area of interest outlined in this report as they were focused on the search for base metals.

In 1983 Adeline International Mines Limited carried out a drill program in the south-east corner of the block. This consisted of B holes drilled to test areas of trenching as well as an EM (VLF) conductor.

In 1988 this company again drilled a series of 10 holes within this same area. A number of these drill holes reported very encouraging gold vales obtained from this area. Both of these drill programs focused primarily on the south-east corner of the block. As a result, the strike length of the zone remains for the most part untested.

REGIONAL GEOLOGY

The project area outlined lies within the Superior province of the Canadian Precambrian Shield. More specifically, within the Swayze Greenstone Belt. This belt, which lies between Timmins and Sudbury, west of Hwy. 144 is made up of an assemblage of volcanics, sediments and younger intrusions ( Fig.

Locally, the property is said to be situated over mafic and ultramafic volcanic flows which strike at roughly north 55 degrees west and dip steeply north and south. Previous work done on the property has shown the area to host zones of quartz-veining as well as sulphide mineralization. Some of these zones are known to contain encouraging amounts of gold.

PROPERTY GEOLOGY

The prospecting program conducted on the Mallard Township Property showed the local geology to conform with that described above. The property was found to be underlain primarily my mafic volcanics. The degree of shearing and quartz veining within this unit varies throughout the grid. The general strike direction is north 45 degrees west, with a dip of 80 degrees to the south.

The exception to this is the presence of a mafic intrusive located in the southeast corner of the block.

NSSPS*•"W-,/- \ A

59953 '*59954

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ent: STEVE ANDERSON OPAP 1995MALLARD TOWNSHIP PROPERTY

TiiU:GEOLOGICAL COhPILATION MAP

MAP 2504 SAMPLE LOCATION

4

SURVEY PARAMETERS

LINECUTTING

A total of 12.4 km of grid lines were cut to cover the previously drilled area and its northwest extension. A baseline was cut at an azimuth of 310 degrees with cross lines turned off at 100 meter intervals to the north and south, and pickets every 25 meters. All lines were chain saw cut.

MAGNETOMETER SURVEY

The entire grid was covered by a Total Field Magnetometer Survey at a 12.5 meter reading interval for a total of 12.4 km. The following is a brief description of the method and instrument used to carry out the survey:

An EDA Omni Plus Proton Precession magnetometer was used to carry out the magnetometer survey. The instrument is synchronized with an EDA recording base station to help eliminate magnetic diurnal variation. This should ensure an accuracy of less than 10 Nt.

The Proton Precession method involves energizing a wire coil immersed in a hydrocarbon fluid. This causes the protons in the proton rich fluid to spin or precess simulating spinning magnetic dipoles. When the current is removed the protons precess about the direction of the earth's magnetic field, generating a signal in the same coil which is proportional to the total magnetic field intensity. In this way, the horizontal gradient of the earth's magnetic field can be measured and plotted in plan form with values of equal intensity joined to form a contour map.This presentation is useful in correlating with other data sets to aid in structural interpretation. Individual magnetic responses can be interpreted for dip, depth and width estimates after profiling the data.

The following parameters were employed for the survey:

Instrument - EDA Omni Plus Proton Precession MagnetometerStation Interval - 12.5mLine Interval - 100mDiurnal Correction Method - EDA Recording Base StationData Presentation - Magnetic Contours/Posting Map, 1:5000

- Contour Interval s 50 nT- Datum subtracted = 57000 nT

VLF-EM SURVEY

A Geonics EM-16 instrument was used to survey the entire property. Both the In-phase (dip angle) and Quadrature values were recorded at 12.5m intervals. A total of 11.2 km was surveyed.

While VLF stands for Very Low Frequency, it is for mineral exploration purposes a very high frequency compared to other commonly used Electromagnetic Surveys. The commonly used frequencies are in the order of 18-20 kilohertz. The VLF-EM technique employs fixed transmitter stations located at various places around the world to facilitate navigation. Because of this, one has a limited choice as to what transmitter station that can be used, depending on distance from and azimuth to the transmitter station.

For this survey, Cutler Maine (NAA) was used. It has an operating frequency of 24.0 khz and an azimuth of approximately of 130 degrees TN from the property. Very briefly, the transmitting station emits a concentric, circular wave pattern, expanding about the transmitter dipole. Being thousands of miles away from the transmitter, we deal with the tangent of this wave pattern which in this case would have a direction normal to the azimuth of 130 degrees. Thus any conductors having a general EW strike direction would be intersected by this signal which induces a signal in the conductor which in turn opposes the primary signal from the transmitter station. This elliptically polarizes the resultant field enabling detection of the conductor using a receiver coil to determine the attitude of the resultant field at various points along the grid lines.

The resultant field dips away from the conductor axis on both sides of the conductor producing a cross-over on the conductor axis. For an EW conductor, a true cross-over would occur where the field dips south and changes to a north dip as you progress from south to north. For this survey, a * /- system is used where a (+1 dip angle means the field is dipping to the south (indicating anomaly is to north) and a (-) dip angle means the field is dipping to the north (indicating anomaly is tosouth). This is the case only if all readings were taken facing north as per this survey.

The quadrature values, while not useful alone, can help distinguish between bedrock conductors which generally have a smaller out-of-phase response than overburden or short wavelength conductors. Also, the polarity of the quadrature is diagnostic, ie; if the polarity follows or is the same sense as the In-phase it gives more credibility to the conductor. Reverse quadrature often indicate overburden responses.

The following parameters were employed for the VLF survey:

Instrument - Geonics EM-16 VLFTransmitter Station - Cutler Maine (NAA), 24.0Khz. Azimuth to station - approx. 130 degrees TN Reading Direction - All reading taken facing north Station Interval - 12.5mData Presentation - Profiled In-phase and quadrature, 1:5000

- GCntounsd Fcser Filtered IptBse, 1:SDOO

INDUCED POLARIZATION SURVEY

The I.P. Survey was done on Lines lOOw, 200w, 500w, and 700w. Contact problems were encountered in the logged area due to outcrop and dry sandy soil conditions, which slowed down the survey considerably. It was necessary to use salt water to achieve proper contact in these areas. A crew of 4 men was used and the survey took 3 days to complete.

The following is a brief summary of the method used, theory, and the survey parameters:

The IP method involves applying voltage across two electrodes in a pulsed manner i.e. 2 seconds on, 2 seconds off. A second "dipole" or electrode pair, measures the residual potential or voltage between them after the voltage is shut off or during the 2 second off cycle. The potential is recorded at different times after the shut off. If, for example, there is sulphide mineralization wi thin the measuring d i poles, they wi 11 be polar i zed or charges set up on the sulphide particles. This polarization gives the zone a capacitor effect, thereby blocking the current delay giving a higher chargeability reading.

A typical signature for many gold showings would be a chargeability high, resistivity high and magnetic low. This would be characteristic of a mineralized, highly altered carbonated and/or silicified zone. However, this is by no means the only geological setting for gold, therefore every profile should be looked at individually and correlated with all other geophysical- geological data.

ELECTRODE ARRAY

The electrode array used for the survey was the Dipole-Dipole Array. In this array two current electrodes (CI, C2) and two receiver or potential electrodes are moved down a line in unison. In this case the "a" spacing or distance between each dipole was fixed at 25 meters apart. For an Nz l reading, the closest CI and Pi were 25 meters apart. The C1-C2 dipole remain in the same place while the potential dipole (P1-P2) moves ahead on "a" spacing and the array is ready for an Nz l reading.

The IP survey was carried out using the following parameters:

Method: Time DomainElectrode Array: Dipole-Dipole"a" spacing: 25 metersNumber of Dipoles Read: 1-4Pulse Duration: 2 seconds on, 2 seconds offDelay Time: 500 millisecondsIntegration Tine: 420 millisecondsReceiver: Scintrex IPR-12Transmitter: Scintrex IPC-9, 200 watt.Data Presentation: Plate l of l, psuedosections, 1:2500

PROSPECTING PROGRAM

The area on and around the grid was prospected as well as a previously trenched area to the northwest called the Woman River Showing. It took four days with two men to complete.(8 man days) In addition to this, 2 days, (2 men), were spent blasting, hand trenching, and sampling five areas within the grid. In all, a total of 29 rock samples were taken. All were sent to Swastika Laboratories and assayed for Au. These assay results from these samples are included in this report.

The trench and sample locations have been plotted on the Prospecting Sketch, which can be found in the back pocket of this report (Map No.4).

The following is a brief description of the 5 trenched areas as well as all rock samples taken.

Trench ft Location Length Width Depth Direction (Grid)1 700W/160N 6 ft 2 ft l ft E-W2 175W/225N 6 ft 2 ft .5 ft E-W3 140W/210N 4 ft l ft .5 ft E-W4 150W/150N 3 ft l ft l ft E-W5 100E/65N 20 ft 3 ft 2 ft N-S

8

Sample t Location

59951599525995359954

5995559956599575995859959

5996059961599625996359964

5996559966599675996859969599705997159972599735997459975599765997759978

175W/225N575W/170NWoman RiverWoman River890W/85N100E/65N100E/65N140W/210N140W/210N100E/65N725W/250N150W/150N110W/140S100E/65N700W/160N100E/65NOE/100N175W/225N175W/225N250W/80S75W/200N100W/80N700W/160N200W/250N500W/160N950W/220S120W/140S20W/355N

Description

Mafic Volcanic, minor py Mafic Volcanic, carb Felsic Volcanic, minor py

Mafic Volcanic, minor qv, minor py, carb Mafic Volcanic Mafic Volcanic, sheared Mafic Volcanic, sheared Mafic Volcanic, sheared Mafic Volcanic, minor py, Mafic Volcanic, minor qv, Mafic Volcanic Mafic Volcanic, Mafic Volcanic,

angular float minor py

carbminor qv, 20* py

Mafic Volcanic, minor qv, minor py, carb Mafic Volcanic, minor qv, carb

carb sheared minor, py minor, py angular float

Mafic Volcanic, Mafic Volcanic, Mafic Volcanic, Mafic Volcanic, Iron Formation, Mafic Volcanic Mafic Volcanic Mafic Volcanic, Mafic Volcanic, Mafic Volcanic, Mafic Volcanic Mafic Volcanic, Mafic Volcanic,

minor qv ;shearedsheared

minor py

minor minor

py py

Swastika LaboratonesA D'ni*** at TSL/A-wm* IB*.

Assaying - Consulting - Representation

AM;

Assay Certificate

RAYAN EXPLORATION LTD

R. MeikJc

5W-4350-RA1

NOV-16-95

WP terety certify the following Assay of 28 Rock samples submitted NOV-08-95 by .

Sanple Nnber59951 59952 59953 59954 5995559956 59957 59958 59959 5996059961 59962 59963 59964 5996559966 59967 59968 59969 5997059971 59972 59973 59974 5997559976 59977 59978

Au PPB1687

3 10)1 3243

1717 10 14

137 99

Nil Nil Nil Nil 1017 7

1183 861 63103

Nil 21 10

Nil Nil 65

Au Check PPB1783

3086

21

3

960

27

-

Certified by.

P.O. Box 10, Swastika, Ontario POK ITO Telephone (705)642-3244 FAX (705)642-3300

ErtabUctwd m

Assay Certificate

RAYAN EXPLORATION LTD

R. MeUdc

Swastika LaboratoriesA DiviMMi of TSL/Ax-aym IB*.

Assaying - Consulting - Representation

5W-4350-RA1

NOV-16-95

Au;

We fe/vty critW' the following Assay of 28 Rock samples submitted NOV-08-95 by .

Saople Nnfcer59951 59952 59953 59954 5995559956 59957 59958 59959 5996059961 59962 59963 59964 5996559966 59967 59968 59969 5997059971 59972 59973 59974 5997559976 59977 59978

Au PPB1687

3 1011 3243

1717 10 14

137 99

Nil Nil Nil Nil 1017 7

1183 861 6510 3

Nil 21 10

Nil Nil 65

Au Check PPB1783

3086

21

*

3

w

960

27

-

Certified by.

P.O. Box 10. Swastika, Ontario POK1TO Telephone (705)642-3244 FAX (705)642-3300

RECOMMENDATIONS AND CONCLUSIONS

The exploration program conducted was successful in outlining a number of areas of interest that should be further tested.

If possible, the first step should be to tie the past drill holes into the current grid. A brief attempt to do this was made during the prospecting portion of the program. However, recent logging in the area made this difficult, and an accurate tie in may not be possible.

Based on the claim location, it is known that anomalous gold values were obtained from the A.E.M drilling program that was carried out in the extreme eastern portion of the grid. A number of I.P. anomalies have also been outlined in this same area. These may have some relationship to the gold values and should be further tested. I.P. anomalies located in the area of the base line on L5W and L7W may represent the western extension of these same zones.

Although prospecting over the grid outlined only general rock types, it also located a zone containing anomalous gold values at 175W/225N that may not have been tested previously. Detailed mapping of the property should be conducted in an attempt to locate additional such zones, as well as establish their relationship to the property geology.

One days prospecting around the Woman River showing to the northwest al so provided anomalous gold values. Previous dri 11 ing in this area by Noranda has shown significant gold values occurring over considerable widths. This area also remains relatively untested. Since the geophysical program conducted in this work program seems to have worked very well, the remainder of the property, including the Woman River showing should be covered with a similar program, especially I.P. This property has shown significant gold values occurring within the eastern portion of the current grid area as well as the Woman River Showing, while the majority of the ground betv/een and to the west of these showings remains for the most part untested.

Although additional work should be carried out, some of the zones outlined in this report could be tested at this point in time with a diamond drill program.

CERTIFICATION

I, Steve Anderson of Timmins, Ontario hereby certify that:

1. I hold a three year Technologist Diploma from Sir Sandford College , Lindsay, Ontario, obtained in May 1981.

2. I have been practising my profession since 1979 in Ontario, Quebec, Nova Scotia, New Brunswick, Newfoundland, NWT, Manitoba,and Saskatchewan.

3. I have been employed directly v/ith Asamera Oil Inc. UrangelIschaft Canada Ltd.. Nanisivik Mines Ltd., R.S. Middleton Exploration Services Ltd.,and Rayan Exploration Ltd.

4. I have based conclusions and recommendations contained in this report on knowledge of the area, my previous experience and on the results of the field work conducted on the property during 1995.

January 10, 1996

Steven D.\Anderson

APPENDIX

Major Benefits of the OMNI PLUS* Combined VLF/Magnetometer/cradiometer

System9 No Orientation Required 0 Three VLF Magnetic Parameters Recorded 9 Automatic Calculation of Fraser Filter 9 Calculation of Ellipticity* Automatic Correction of Primary Field

VariationsMeasurement of VLF Electric Field

c ascriptionThe "OMNI PLUS" geophysical ytem combines the OMNI IV " 3-Line" magnetometer and g, jdiometer together with a VLF measurement capability. T 'OMNlPLUSVLF/Magneto- n -ter system has been develop ed in co-operation with Ceo- physical Surveys inc. of Quebec, C lada.This brochure concentrates on the VLF magnetic and electric fi d parameters measured and n orded by the OMNI PLUS. More information on the OMNI PLUS magnetometer system and tie- lii j capability is available in the O...NI IV brochure.

P.aturesEach OMNI PLUS incorporates the fc Dwing features:- nieasurement and recording in

memory of the following VLF ata for each field reading: total field strength,

- total dip,- vertical quadrature or,

alternately, horizontal amplitude,

-apparent resistivity, phase angle, time,

- grid co-ordinates,- direction of travel along grid

ines, and natural and cultural features.

- complete data protection for a number of years by an

iternal lithium backup ^attery.

- "Tie-Line" or "Looping" 'gorithm, unique only to ?A's OMNI iv and OMNI PLUS

beries, for the self-correction of atmospheric variations and

iriations in the primary field om the VLF transmitter.

Measurement of up to three VLF transmitting stations to provide complete coverage of an anomaly regardless of the orientation of the survey grid or of the anomaly itself. Display descriptors to monitor the quality of the VLF signal being measured. Choice of three data storage modes:- spot record, for readings without grid co-ordinates

- multi record, for multiple readings at one station

- auto record, for automatic update of station number

Output of grid coordinates with the designated compass bearing, using N, S, E, w descriptors.

Major Benefits* combined VLF/Magneto-

meter/Cradfometer SystemThe OMNI PLUS incorporates the capabilities of the OMNI lv 'Tie- Line" Magnetometer and Gradiometer System with the ability to measure the VLF magnetic and electric fields.Only one OMNI PLUS is needed to record all of the following geophysical parameters:

1. The total magnetic field2. The simultaneous gradient of

the total magnetic field3. The VLF magnetic field,

including:-the total dip- the total field strength of the VLF magnetic field

- the vertical quadrature, or alternately, the horizontal amplitude

4. The VLF electric field, including:-the phase angle- apparent resistivity

As an example, at each location the OMNI PLUS can calculate and

record in a matter of seconds, three VLF magnetic field and two VLF electric field parameters from two different transmitters, a magnetic total field reading and a simultaneous magnetic gradient reading.

No Orientation RequiredThe OMNI PLUS requires no orientation, by the operator, of the sensor head toward the transmitter station. This simplifies field procedures as well as saving considerable survey time. When two VLF transmitters are measured, the benefits of this time-saving feature are auto matically doubled. There is no requirement for the operator to orient himself and the sensor head toward the first selected transmitting station and then re orient towards the second trans mitting station.Consistent high quality data is achieved in the OMNI PLUS due to the utilization of three ortho gonal sensor coils rather than two sensor coils used in conventional systems. The quality of data is not then dependent on the operators ability to correctly orient the sensor head for optimum coupling with the transmitting station.The OMNI PLUS compensates automatically for the direction of travel along the grid lines as well as for the angle of the sensors from the vertical plane through the use of tiltmeters.

Three VLF Magnetic Parameters RecordedThe OMNI PLUS calculates and records in memory the:- total dip- total field strength- vertical quadrature The operator has the option to substitute the horizontal amplitude for the vertical

APPENDIX 'B'

VLF EM

VLh (KLANL W AY b) t M INb l KUM tN l b————

VLF RESISTIVITY METER

EMI6One of the most popular and widely used electromagnetic instruments, the EM16 VLF receiver makes the- ideal reconnaissance EM This can be attributed to its field reliability, operational simplicity, compactness and mutual compatibility with other reconnaissance instruments such as portable magnetometers and radiometric delec tors

The VlF method of EM surveying, pioneered by Geonics. has proven lo be a simple economical means of mapping geological structure and fault tracing The applications are many and varied, ranging from direct detection of massive sulphide conductors to the indirect detection of precious metals and radioactive deposits

FEATURES• The EMt6 is the only VLF instrument that measures the quad phase as well as

the m phase secondary field This has the advantage ol providing an additional piece of data for a more comprehensive interpretation and also allows a more accurate determination ol the Ml angle

• The secondary fields are measured as a ratio lo the primary field making the measurement independent of absolute field strength

• The EMI6 is the only VLF receiver thai can be adapted lo measure VLF resistivity

SpecificationsMEASURED QUANTITY In phase and quad phase components ol vertical mag

netic field as a percentage of horizontal primary field, (i e. tangent ol the tilt ancle and ellipticity)

SENSITIVITY In phase :i150*/. Quad phase : l 40V.

RESOLUTION *1V.OUTPUT Nulling by audio tone In phase indication from mechan

ical inclinometer and quad phase from a graduated dialOPERATING FREQUENCY IS 25 kHz VLF Radio Band Station selection done by

means of pfug in units.OPERATOR CONTROLS On/Off switch, battery test push button, station selector

switcn. audio volume control, quadrature dial, inclino meter.

POWER SUPPLY 6 disposable -AA' cells DIMENSIONS 42xl4x9cm WEIGHT Instrument: 1 6 kg

Shipping : S S kg

EMI6/I6RThe EM16R is a simple, button on attachment to the EM16 converting it to a direct reading terrain resistivity meter. The EM16R interlaces a pair of poten tial electrodes to the EM 16 enabling the measurement of the ratio of. and the phase angle between, the horizontal electric and magnetic fields of the plane wave propagated by distant VLF radio transmitters.

The EM16R is direct reading in ohm meters ol apparent ground resistivity II the phase angle is 45". the resistivity leading is the I'ue value and Hie e.vth is uniloim lo Ihe depth ol exploration (i e a skin depth) Any departure Irom 45* ol phase m dicates a layered earth Two layer interpretation curves are supplied with each in slrument lo permit an interpretation based on a two layer earth model

This highly portable resistivity meler makes an ideal tool lor quick geological map pmg and has been used successfully lor a variety ol applications

• Detection ol massive and disseminated sulphide deposits• Overburden conductivity and thickness measurements• Permaliosl mapping• Detection and delineation ol industrial mineral deposits• Aqm'er mapping

ATTACHMENT

• Apparent Resistivity of the giound in ohm meters•Phase angle between E, and H in degrees

• 10- 300onm meters• 100 - 3000 ohm melers• 1QOO - 30000 ohm melers

O 90 degrees• Resistivity * 2'.'. lull scale• Phase 'Ob'

Null by audio tone. Resistivity and phase angle read Irom graduated dialsIS 25 KM/ VLF Radio Band Station selection oy means ot rotary switch10 melers100 Mi) in parallel with OS picofarads19x11 SxlOcm(attached lo side olEMl 6)1 .S kg (including probes and cable)

MEASURED QUANTITY

RESISTIVITY RANGES

PHASE RANGE

RESOLUTION

OUTPUT

OPERATING FREQUENCY

INTERPROBE SPACING

PROBE INPUT IMPEDANCE DIMENSIONS

WEIGHT

APPENDIX 'C'

l PR-12 Time Domain Induced Polarization/Resistivity Receiver

Brief DescriptionThe IPR-12 Time Domain IP/Resistivity Receiver is principally used in exploration for precious and base metal mineral deposits. In addition, it is used in geoelec- trical surveying for groundwater or geothermal resources, often to great depths. For these latter targets, the induced polarization measurements may be as useful as the high accuracy resistivi ty results since it often happens that geo logical materials have IP contrasts when resistivity differences are absent.

Due to its integrated, lightweight, micropro cessor based design and its large. 16 line display screen, the IPR-12 is a remarkably powerful, yet easy to use instrument. A wide variety of alphanumeric and graphical information can be viewed by the operator during and after the taking of readings. Signals from up to eight potential dipoles can be measured simultaneously and recorded in solid-state memory along with automatically calculated parameters. Later, data can be output to a printer or a PC (direct or via modern) for processing into profiles and maps.

The IPR-12 is compatible with Scintrex IPC and TSQ Transmitters, or others which output square waves with equal on and off periods and polarity changes each half cycle. The IPR-12 measures the pri mary voltage (Vp), self potential (SP) and time domain induced polarization (Mi) characteristics of the received waveform. Resistivity, statistical and Cole-Cole parameters are calculated and recorded in •nemory with the measured data and time.

Scintrex has been active in induced polar ization research, development, manufac- uring, consulting and surveying for over hirty years. We offer a full range of instru mentation, accessories and training.

IFF- '2 Receive' measures spectral iP signals from eight aipdes ' recorcs measures and ca'cmated parameters ir, memory.

BenefitsSpeed Up Surveys

The IPR-12 saves you time and money in carrying out field surveys. Its capacity to measure up to eight dipoles simultaneous ly is far more efficient than older receivers measuring a single dipole. This advantage is particularly valuable in drillhole logging where electrode movement time is mini mal.

The built-in, solid-state memory records all information associated with a reading, dis pensing with the need for any hand written notes. PC compatibility means rapid elec tronic transfer of data from the receiver to a computer for rapid data processing.

Taking a reading is simple and fast. Only a few keystrokes are virtually needed

since the IPR-12 features automatic circuit resistance checks. SP buckout and gain v setting.

High Quality Data

One of the most important features of the IPR-12 in permitting high quality data to be acquired, is the large display screen which allows the operator easy real time access to graphic and alphanumeric displays of instrument status and measured data. The IPR-12 ensures that the operator obtains accurate data from field work.

The number and relative widths of the IP decay curve windows have been carefully chosen to yield the transient information required for proper interpretation of spec tral IP data. Timings are selectable to per mit a very wide range of responses to be measured.

Specifications

Inputs1 to 8 dipoles are measured simultaneously.

Input Impedance16 Megohms

SP Bucking±10 volt range. Automatic linear correction operating on a cyde by cycle basis.

Input Voltage (Vp) Range50 p volt to 14 volt

Chargeability (M) RangeO to 300millivolt

Tau Range1 millisecond to 1000 seconds

Reading Resolution of Vp, SP and MVp, 10 microvolt; SP. 1 millivolt; M. 0.01 millivolt/volt

Absolute Accuracy of Vp, SP and MBetter than 1 0Xo

Common Mode RejectionAt input more than 100db

Vp Integration Time1007o to 800Xo of the current on time.

IP Transient ProgramTotal measuring time keyboard selectable at 1, 2, 4, 8, 16 or 32 seconds. Normally 14 windows except that the first four are not measured on the 1 second timing, the first three are not measured on the 2 sec ond timing and the first is not measured on the 4 second timing. (See diagram on page 2.) An additional transient slice of minimum 10 ms width, and 10ms steps, with delay of at least 40 ms is keyboard selectable.

Transmitter TimingEqual on and off times with polarity change each half cyde. On/off times of 1,2,4, 8, 16 or 32 seconds. Timing accuracy of ±100 pom or better is required.

External Circuit TestAll dipoles are measured individually in sequence, using a 10 Hz square wave. Fhe range is O to 2 Mohm with O.lkohm resolution. Circuit resistances are dis- olayed and recorded.

SynchronizationSelf synchronization on the signal received at a keyboard selectable dipole. Limited to avoid mistriggering.

FilteringRF filter, 10 Hz 6 pole low pass filter, sta tistical noise spike removal.

Internal Test Generator1200 mV of SP; 807 mV of Vp and 30.28 mV/V of M.

Analog MeterFor monitoring input signals; switchable to any dipole via keyboard.

Keyboard17 key keypad with direct one key access to the most frequently used functions.

Display16 lines by 42 characters, 128 x 256 dots, Backlit Liquid Crystal Display. Displays instrument status and data during and after reading. Alphanumeric and graphic dis plays.

Display HeaterAvailable for below -15"C operation.

Memory CapacityStores approximately 400 dipoles of infor mation when 8 dipoles are measured simultaneously.

Real Time ClockData is recorded with year, month, day, hour, minute and second.

Digital Data OutputFormatted serial data output for printer and PC etc. Data output in 7 or 8 bit ASCII, one start, one stop bit, no parity format. Baud rate is keyboard selectable for stan dard rates between 300 baud and 51.6 kBaud. Selectable carriage return delay to accommodate slow peripherals. Hand shaking is done by X-on/X-off.

Standard Rechargeable BatteriesEight rechargeable Ni-Cad D cells. Supplied with a charger, suitable for 1107230V. 50 to 60 Hz. 10W. More than 20 hours service at *25'C. more than 8 hours at -30*C.

Ancillary Rechargeable BatteriesAn additional eight rechargeable Ni-Cad D cells may be installed in the console along with the Standard Rechargeable Batteries. Used to power the Display Heater or as back up power. Supplied with a second charger. More than 6 hours service at-30'C.

Use of Non-Rechargeable BatteriesCan be powered by D size Alkaline batter ies, but rechargeable batteries are recom mended for longer life and lower cost over time.

Operating Temperature Range-30'C to *50'C

Storage Temperature Range-30'C to *50'C

DimensionsConsote:355 x 270 x 165 mm Charger: 1 20 x 95 x 55mm

WeightsConsole: 5 .8 kgStandard or Ancillary RechargeableBatteries: 1 .3 kgCharger: 1 .1 kg

Transmitters availableIPC-9 200 W TSQ-2E 750 W TSQ-3 3 kW TSQ-4 10kW

Ut Canada

222 Snidercroft Rd. Concord, Ontario Canada, L4K1 BS

tatteU.SJL

85 River Rock Drive Unit/202 Buffalo, N.Y. U.SA 14207

IPR-12/94

Tel.: (905)669-2280 Fax; (905) 669-6403 Telex: (905) 06-964570

Tel.: (716)298-1219 Fax: (716)298-1317

APPENDIX 'D'

IPC-9/200U

INDUCED POLARIZATION AND P.C. KESIST1VITY TRANSMITTER

2.0 SPECIFICATIONS

Maximum Output Power

Output Voltage

Output Current

Meter Ranges

Automatic Cycle Timing

Automatic .Polarity Change

Pulse Durations

Period Tine Stability and Accuracy

Open Loop Protection

Synchronization Output

Internal Power Sources

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

Switch selectable at nominal settings of 15, 150, 210, 300, 425, 600 or 850 V.

1.5 A maximum.

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

T:T:T:T; on:off:on:off.

Each 2T.

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

Crystal controlled to better than 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 testing purposes. This protection is not effective at the 15 V output.

". i - 1 :" ' ' : i

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

External Power Sources

Two battery packs 'are standard, each containing 4 GC 660-1 lead-acid 'gel-type batteries' giving 24 V at 12Ah. :--.:-::3i- ; •-•' ' ;

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 Hz, 100 W.

Transmitters with two batterypacks i140 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 mm; 5.5 kg

-30'C to *55'C.

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

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

46 kg Includes reusable wooden shipping case.

2-2

Ministry ofNorthern Developmentand Mines

Ontario

Report of Work Conducted After Recording Claim

Mining ActPersonal Information collected on this form is obtained under the authority of the Mining Act. This information will be used for correspondence. Questions about this collection should be directed to the Provincial Manager. Mining Lands. Ministry of Northern DevetopMnt and Mines. Fourth Floor. 159 Cedar Street, Sudbury. Ontario. P3E 6A5. telephone (705) 670-7264. ^ - "" ^* '

Instructions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for requin

Recorder.- A separate copy of this form must be completed fc

-- Technical reports and maps must accompany this-A sketch, showing the claims the work is assigned "

l Mines. Fourth164

1O09NW0030 2 16410 MALLARD 900

Work Performed (Check One Work Group Only)WorkGroup

l/ Geotechnical Survey

Physical Work, Including Drilling

Rehabilitation

Other Authorized Work

Assays

Assignment from . Reserve -^

Type

LotJl^ M** VL? 7P Aei^oJj.* /?MA// ^ "'

'

RECEIVED

FtB i 3 1996

MINING LANDS BRANCH

*

- ';

* **

( -

Total Assessment Work Claimed on the Attached Statement of CostsNote: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded

holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report) .Name Address

) T -tfZ

(attach a schedule H necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse sidel certify that at the time the work was performed, the claims covered in this workreport were recorded In the current holder's name or held under a beneficial interest^ —-*^by the current recorded holder.

Date l Holder or (Signature)

Certification of Work Reportl certify that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after its completion and annexed report is true.

Name and of Pereon

QJ3 OkBy (Signature)releponeNo. Oate

For Office Use Only

Date Notice for Amendments Sent

0241 (03*1)

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Credits you are claiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (^) one of the following:

rt/ "x '^ST~1. W Credits are to be cut back starting with the claim listed jaw, working backwards.2. D Credits are to be cut back equally over all claims contained in this report of work.3. D Credits are to be cut back as priorized on the attached appendix.

In the event that you have not specified your choice of priority, option one will be implemented.

Note 1: Examples of beneficial Interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.

Note 2: If work has been performed on patented or leased land, please complete the following:

l certify that the wonted holder had a beneficial interest In the patented or (eased land at the time the work was performed.

Signature Date

Ontario

Ministry ofNorthern Developmentand Mines

Minister* du Devetoppement du Nord et des mines

Statement of Costs for Assessment Creditttat des couts aux fins du credit d'evaluation

Mining Act/Loi sur les mines

Transaction NoJN* de transaction

Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining daim(s). Questions about this collection should be directed to the Provincial Manager. Minings Lands, Ministry of Northern Development and Mines. 4th Floor. 159 Cedar Street. Sudbury. Ontario P3E 6A5. telephone (705) 670-7264.

164 loLes renseignements personnels contenus dans la presents formule sont recueidis en vertu de la Lo! sur les mines et serviront a tenir a Joor un registre des concessions minieres. Adresser toute quesiton sur la cdtece de ces renseignements au chef provincial des terrains miniers, ministere du Devetoppement du Nord et des Mines. 159. rue Cedar, 4e elage. Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Direct Costs/CoQts directs

Type

Wage* Salalre*

Contractor's and Consultant's Fees Drottsde ('entrepreneur et de ('expert- Cornell

Supplies Used Foumltures utlHsees

Equipment Rental Location de materiel

Description

Labour Main-d'oeuvreField Supervision Supervision sur le terrain

T*P* 1 Ijh.s.ri/'tl^

Pwp *xr ju.4 .M.^ VULffzP

U-l.tin'T'

Typ* l

Type

Amount Montant

3/oafyeo100V

Total Direct Costs Total des couts directs

Totals Total global

:" r '-' ' r

Ift W

;i...'..-- ;

: - ffi" , -

firn

2. Indirect Costs/CoOts Indirecto* * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work.Pour le remboursement des travaux de rehabilitation, les couts indirects ne son! pas admissibtes en tant que travaux devaluation.

Type

Transportation Transport

DescriptionTyp*

Food and Lodging Nourriture et hebergenwnt

INING LANDS BRArv 3H

Amount Montant

MoMllzatkMi and Demobilization Mobilisation et demoblllMtton _^__

Sub Total of Indirect Costs Total parcel des coOts Indirects

Amount Allowable (not greater than 20* of Direct Costs) Montant admissible (n'excedant pas 20 H des coots directs)Total Value of Assessment CredN (Told of Direct and ABowaMe Indbect costs)

Vatour totato du crsdM(Total d** coOb M Mr*** tM

Totals Total global

Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.

Note : Le Utulaireenregistre sera tenu de verifier tesdepensesdeinandses dans le present etat des couts dans les 30 jours suivant une demande a eel effet. Si la verification n'est pas effectuee. le ministre peut rejeter tout ou une partie des travaux d'evaluatton presentes.

Rllng Discounts Remises pour depot

1. Work filed within two years of completion is claimed at KXWfe of the above Total Value of Assessment Credit.

1. Les travaux deposes dans les deux ans suivant tour achievement son! rembourses a 100 % de la vateur totato susmerrbonnee du cridM d'evaluaton

2. Work filed three, four or five years after completion is claimed at SOW of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimedx 0.50

2. Les travaux deposes trois, quatre ou cinq ans apres leu r achevemeni son! rembourses a 50 "ft de la valour totale du credit d'evaluatior susmentionne. Voir les calculs ci-dessous.

Valeur totale du credit d'evaluationx 0.50 -

Evaluation totale dernandee

Certification Verifying Statement of Costs Attestation de I'etat des couts

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report ej Work form.

that as . . ,. , ^ ^ " l Holder. Hgent, Position in Company)

to make this certification

J'atteste par la presente :que les montants indiques sont le plus exact possible et que ce; depenses ont ete engagees pour effectuer les travaux d'evaluatioi sur les terrains indiques dans la formule de rapport de travail ci-joint

^ l am authorized Et qu'a litre de . je suis autoria(titulaire enregistra. reprtoentant. poste occupe dans l* compagnie)

d faire cotte attestation.

Date

0212(04/91) Nota : Dans cette formule, kxsqu'll designe des personnes, le masculin est utilise au sens

r X

-\ 0f

q

164

10

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FEB

i 3

1996

MIN

ING

LAN

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RAN

CH

OntarioMinistry ofNorthern Developmentand Mines

Ministere duDeveloppement du Nord et des Mines

Geoscience Approvals Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: (705) 670-5853 Fax: (705) 670-5863

April 04, 1996Our File: 2.16410 Transaction /: W9660.00026

Mining RecorderMinistry of Northern Development 6 Mines60 Wilson Avenue, 1st floorTimmins, OntarioP4N 2S7

Dear Mr. White:

Subject: APPROVAL OF ASSESSMENT WORK CREDITS OH MIMING CLAIMS 1201578 i 1201579 IN MALLARD TOWNSHIP

Assessment credits have been approved as outlined on the attached report of work form. The credits have been approved under Section 9 (Prospecting) and Section 14 (Geophysical) of the Mining Act Regulations.

The approval date is April 04, 1996.

If you have any questions regarding this correspondence, please contact Steven Beneteau at (705) 670-5855.

Yours sincerely, ORIGINAL SIGNED BY:

Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division

SBB/jl Enclosure:

cc: Resident Geologist Timmins, Ontario

Assessment Files Library Sudbury, Ontario

VALUE OF ASSESSMENT WORK PERFORMED ON MINING CLAIMS

APRIL 04, 1996 FILE NUMBER 2.16410 TRANSACTION NO. W9660.00026

Please note, assessment credits have been distributed to reflect the value of work performed on each claim.

CLAIM NUMBER VALUE OF ASSESSMENT WORKDONE ON THIS CLAIM

1201578 Sl2,400.001201579 $ 1,000.00

TOTAL 913,400.00

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200 SOUTH

300 SOUTH

400 SOUTH

500 SOUTH

600 SOUTH

700 SOUTH

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400 NORTH

300 NORTH

200 NORTH

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200 SOUTH

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400 SOUTH

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FOLIATION

AREA OF OUTCROP

SAMPLE NUMBER AND LOCATIONMAFIC METAVOLCANICSMAFIC INTRUSIVE

TRENCH

pnop.nH

Titl

STEVE ANDERSON - OPAP 1995

MALLARD TOWNSHIP PROPERTY

PROSPECTING SKE

RE C E i -,' E D

SDA

DoiJAN/95

ProvinceONTARIO

Sea I1 : 5000

CheckedSDA

Town.hip

NTS410/NE

Drawing290VLFG

"S.164 10

400 NORTH

300 NORTH

200 NORTH

100 NORTH

BflSE LINE

100 SOUTH

200 SOUTH

300 SOUTH

400 SOUTH

500 SOUTH

600 SOUTH

700 SOUTH

800 SOUTH

OPEEPEESWAY RIVER

951 - g•- 987•- 990

985•- 977

OLD ROAD

400 NORTH

300 NORTH

200 NORTH

100 NORTH

BRSE LINE

100 SOUTH

200 SOUTH

300 SOUTH

400 SOUTH

500 SOUTH

600 SOUTH

700 SOUTH

800 SOUTH

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LEGEND

INSTRUMENT EDA OMNI PROTON PRECESSION MAGNETOMETER

PARAMETERS MEASURED. EARTH'S TOTAL MAGNETIC FIELD (NANO-TESLAS

READING INTERVAL 12 5 M

CONTOUR INTERVAL- 50 NANO TESLAS

DIURNAL CORRECTION METHOD. RECORDING OMNI BASE STA"

DATUM SUBTRACTED: 57000 nT

CI lent STEVE ANDERSON - OPAP 1995

Property MALLARD TOWNSHIP PROPERTYTitl

TOTAL FIELD MAGNETOMETER'' Mf^VEYn

Proc*SDA

DaLaJAN/95

ProvlnctONTARIO

Scol5000

CheckedSDA

TownehipMALLARD

NTS410/NE

Drowing290MAG

2-164 10

41O09NW0030 2 16410 MALLARD 220

22SN 250N 27SN

M9 CHO.Nil

Ni2

Ni3

Ni4

75N IQpN 12SN , ISpN , 17SN

14 B.2

M9 CHO N:l

N)2

Ni3

Nt4

125J | Iff t 50,8 | 25,8 t ON ,20pN

RESISTIVITYNil

Nt2

Ni3

Ni4

8.BK 6.0K L0. .2K ^B.SK 2.61

4.OK S.BK

4.IK /-IK 6-SK

3.9K /*.Sif 4.4K 5

K 26

2K

BK

-8K 11.2K20.4K2Q.OK

10.BK37.3K IB.OK 13.SK

.OK30.7K23.7K 12.6KB3.9K

27.SK 17.7K 1S.3K72.3KB7.2K

RESISTIVITY Mtl

Ni2

Ni3

NM

izps ^opsM9 CHG.

Nil

Ni2

Ni3

Ni4

225N*- ^ 25pN . 27gN . 30pN . 32SN

RESISTIVE7.2 9.4 9.7 B.3 6.6

.2 7.8 B-TV l O (20 ' 9.3 /6-3

i 7.5 6-7 7\*V^ 7.4

.5 6-5 7-5 6^--**fl

M9 CHG Nil

Ni2

NM

1258 10P6 758 5Q8 258 ON . 25N . 5QNp——t——p——t——T——* —^-——t^-^——i——^—-*——^f^——i——i

RESISTIVITYNil Hi 2 fli3 Ni 4

191-JU69-0 189.0

466

1.3K

ICON 125N ISDN 175N 20DN 225N 250N Z75N 30pN . 325N ——F-— t——f —t- —f-—t --f—4——f— t——f—t——F —i- -f---*- —F—'——F

-8K 8.SK B.5K55.5K21.7K30.5K23.1K25.4K26.2K22.1K

6.SKS.9.0K 1B.OK34.4K27.SKZ9.4K61.7K34.4K23.0K

B.4K/16.0K 13.7K 37.4K21.6K 59.OK SB.BK 25.OK

5.2Kiol.6K 11. IK 17.BK 26.OK 36.OK 50.SK 36.SK

RESISTIVITYNil

Ni2

f19 CHO.Nil

Ni2

Ni3

CONDUCTIVE IB. l

.275 175875 125S t lOp 5()8 DN

RESISTIVITY.0679.0825.0

721 O

0530.0663.0559.0

.BK 5.IK 5.7K 6-SK 7,1K 16-3K 9-2K 22.2K 10-6K 21-6K

O.OK.B.9Kp.2K 12.9K 24.2K 22.9K 17.SK 17.BK

l x- 0000 i t——x .If ^3.BK 1Z.4K/ 7-fK25.4K24.OK 33.9K

( 17.8K ff.BK K.BK23.3K 36.1K23. 3.9K

RESISTIVITY NUNi2

Ni3

NM

IH

O CO CM

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4.9

Ni4

2ops | i7pa , isps laps . sqs ( op

RESISTIVITYNil

Ni2

Nt3

Ni4

4 10pN H 125N t 15pN t 17^N t 20pN

RESISTIVITT 18.6K 2.SK NU

Ni3

Ni4

LINE : 100 W

INDUCED POLflRIZflTION SURVEY

DIPOLE-DIPOLE RRRRY

. 1 . M - 1 .

[®1 ffi^ f* * *

x * \ f

•PTH*raiHTM s 1, 2. 3. 4. -..

•fl- SPflCINO ~ 25.0 METRES

RECEIVER SC1NTHEX I PR- 12 TIME QCMAIN

RX-TX TIMING 2~e CM Zmm* OFF PUTTTED MINDOH SLICE *9

TRANSMITTER SCIHTREX IPC-9 2M NATT

RNDERSON OPflP 1995MflLLflRD PROPERTY

MflLLflRD TOWNSHIPDflTE : SEPT25/95 REF : SOU

SCRLE - 1 : 2500

PSS

LINE : 200 W

INDUCED POLfiRIZRTION SURVEY

DIPOLE-DIPOLE RRRRY

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TRANSMITTER SCINTREX IPC-9 2M NATT

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TRANSMITTER SCINTREX [PC -9 2H HATT

flNDERSON OPflP 1995

MflLLflRD PROPERTY

MflLLflRD TOWNSHIPDHTE : SEPT25/95 REF : SDH

SCflLE - 1 : 2500

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INDUCED POLflRIZflTION SURVEY

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TRANSMITTER SCINTREX IPC-9 2M WATT

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INDUCED POLARIZATION PSUEDOSECTIONS

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400 NORTH

300 NORTH

200 NORTH

100 NORTH

BflSE LINE

100 SOUTH

200 SOUTH

300 SOUTH

400 SOUTH

500 SOUTH

600 SOUTH

700 SOUTH

800 SOUTH

c

OPEEPEESWAY RIVER

OLDROAD

400 NORTH

300 NORTH

200 NORTH

100 NORTH

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200 SOUTH

300 SOUTH

400 SOUTH

500 SOUTH

600 SOUTH

700 SOUTH

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LEGEND

INSTRUMENT. GEONICS EM-16 VLF

PARAMETERS MEASURED IN-PHASE AND QUADRATURE

READING INTERVAL 12.5 M

PROFILE SCALE, l cm - 20XTRANSMITTER STATION* CUTLER MAINE (NAA) 24 O KHz

ALL READINGS TAKEN FACING NORTH

CONDUCTOR AXIS

DIRECTION TOSTATION NAA

CI lent. STEVE ANDERSON - OPAP 1995

Property * MALLARD TOWNSHI P PROPERTY

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300 NORTH

200 NORTH

100 NORTH

BRSE LINE

100 SOUTH

200 SOUTH

300 SOUTH

400 SOUTH

500 SOUTH

600 SOUTH

700 SOUTH

800 SOUTH

OPEEPEESWAY RIVER

OLD ROAD

400 NORTH

300 NORTH

200 NORTH

100 NORTH

BRSE LINE

100 SOUTH

200 SOUTH

300 SOUTH

400 SOUTH

500 SOUTH

600 SOUTH

700 SOUTH

800 SOUTH

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DC l a i ffi Line

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LEGEND

INSTRUMENT GEONICS EM-16 VLF

PARAMETERS MEASURED IN-PHASE FRASER FILTERED

READING INTERVAL 12 5 M

CONTOUR INTERVAL 5 UNITS

TRANSMITTER STATION CUTLER MAINE (NAA) 24.0 KHz

CONDUCTOR AXIS —————

ALL READINGS TAKEN FACING NORTH

A

DIRECTION TOSTATION NAA

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STEVE ANDERSON - OPAP 1995

MALLARD TOWNSHIP PROPERTY

VLF-EM SURVEY POSTED IN-PHASiPE"c~ErCONTOURED FRASER F L"1"^'"' 1 ' 1 '

SDA

JAN/95

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Scale:.5000

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Towrmhl p .MALLARD

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250