report on a gradient array ip/resistivity survey

Report on a Gradient Array IP/Resistivity Survey

Grouse Grid, Fawcett Township Shining Tree Area, Ontario Goldeye Explorations Ltd.

Ref. 10-93 December, 2010

Goldeye Explorations JVX 10-93

2

Report on a Gradient Array IP/Resistivity Survey Grouse Grid, Fawcett Township Shining Tree Area, Ontario

For : Goldeye Explorations Ltd. 85 West Wilmot St., Unit 4 Richmond Hill, Ontario L4B 1K7 Phone : 905.886.2538 Fax : 905.886.8210 www.goldeye.ca

By : JVX Ltd.

60 West Wilmot Street, Unit 22 Richmond Hill, Ontario L4B 1M6 Phone : 905.731.0972 Fax : 905.731.9312 www.jvx.ca

Ref. 10-93 December, 2010

Summary A gradient array spectral IP/resistivity survey was done on the Grouse grid,

Shining Tree area, Ontario. The field work was done from November 24 to December 4, 2010. Total production was 18,125 m. The Grouse grid is within claims 1246451 and 1246454 registered to Goldeye Explorations Ltd. The results have been presented in maps of chargeability and apparent resistivity at 1:5,000.

Cover page : Mx chargeability contours

Goldeye Explorations JVX 10-93

3

Table of Contents

1. Presentation 2. Background 3. Survey 4. Discussion 5. Conclusions

Figures Figure 1 : Regional location map Figure 2 : Survey grid (base map from MNDMF claimap3) Figure 3 : Mx chargeability Figure 4 : n=2 Mx chargeability from JVX 5-33 Figure 5 : VLF offset profiles from JVX 8-79 Figure 6 : Mx chargeability and apparent resistivity. Line 10800E. JVX 5-33 Figure 7 : Mx chargeability and apparent resistivity. Line 10400E. JVX 5-33 Attachments Certificate of Qualifications Appendix 1 : Production, GPS Control Points, Data Processing and Archives Appendix 2 : Weekly Field Production Reports Appendix 3 : Map Images Instrument specification sheets Maps The results of the surveys are presented in 2 plan maps at 1:5,000. Both maps show land tenure from the MNDMF claimap3 website and drainage from Natural Resources Canada (geogratis.ca). Both maps show latitude / longitude marks and a UTM grid (NAD83, Z17N). Both maps show drill hole collar GL-06-01. Maps are

1. Mx chargeability 2. Apparent resistivity

Paper copies of these 2 maps are folded and bound with this report.

Goldeye Explorations Ltd. JVX 10-93 (Grouse grid) 1

Gradient Array IP/Resistivity Survey Grouse Grid, Fawcett Township, Shining Tree Area, Ontario

Goldeye Explorations Ltd.

A gradient array IP/resistivity survey was done on the Grouse grid, Fawcett Township, Shining Tree area, Ontario. The grid is centered 8 km east of Shining Tree and 30 km west southwest of Gowganda. The work was done for Goldeye Explorations Ltd. by JVX Ltd. under JVX job number 10‐93. The field work was done from November 21 to December 5, 2010. Total production was 18,125 m.

Figure 1. Regional location map

The Grouse grid is within claims 1246451 and 1246454 registered to Goldeye Explorations Ltd. The grid is made up of 16 north northeast lines at 100 m (10300E to 11800E). The maximum station range is 8775N to 10700N. The grid is shown in figure 2. The survey was done with fixed current electrodes separated by 2975m grid north and grid south of the survey area. Chargeability and apparent resistivity were measured every 25 m with 25 m long potential dipoles. The results are presented on plan maps of Mx chargeability and apparent resistivity at 1:5,000. The purpose of using the deep‐penetrating gradient array was to determine if deep (300m‐500m) sulphide bodies could be detected on the property. The geology on the grid is correlate able to the geology associated with Ursa Major’s Shining Tree Cu/Ni deposit located 1.5 km to the NW . Production summaries, GPS control points, instrumentation, data processing and archives are described in appendix 1. Weekly field production reports are in appendix 2. Map images are in appendix 3. Instrument specification sheets are attached. Paper copies of 2 plan maps are folded and bound with this report. 1. Presentation The results of the surveys are presented in 2 plan maps at 1:5,000. Both maps show land tenure from the MNDMF claimap3 website and drainage from Natural Resources Canada (geogratis.ca). Both maps show latitude / longitude marks and a UTM grid (NAD83, Z17N). Both maps show drill hole collar GL‐06‐01. Maps are

1. Mx chargeability

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2. apparent resistivity Chargeability contours are shown in figure 3. Digital results (this report, raw and processed ASCII data files, Geosoft database and map files, Autocad drawing files) are archived on CD.

Figure 2. Survey grid (base map from MNDMF claimap3)

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Figure 3. Mx chargeability

2. Background The following comments have been taken from the 2004 Qualifying Report on the Fawcett Property, Fawcett Township, Larder Lake M. D., Ontario by G. A Harron for Goldeye Explorations Ltd.

Three types of mineral deposits are relevant to this property, based on historical exploration results. Lode gold occurrences are known in the extreme northwestern part of the property, magmatic Ni-Cu-(PGE) mineralization occurs on the adjacent Ft. Knox property and Cu-Zn-Pb-Ag mineralization occurs in the southeastern part of the Goldeye property and on the Ft. Knox claims. At the district scale, exploration for quartz-carbonate lode gold deposits focuses on broad shear zones located along terrane boundaries or adjacent to felsic intrusions. At a more local scale mapping of alteration mineral assemblages can delineate favourable portions of shear zones. The low sulphides content of the quartz veins and the associated wall rock alteration is detectable by IP/resistivity methods. Carbonatization causes destruction of magnetic minerals in mafic rocks, creating a negative magnetic feature coincident with alteration surrounding the lode deposit. The Ni-Cu-(PGE) mineralization on the Ft. Knox property occurs within a complex tecto-magmatic breccia zone developed within a gabbroic-anorthositic intrusion. The mineralized zone is a pipe-shaped body having dimensions of approximately 30 m wide, about 100 m in strike length and a known depth of about 500 m. The core of the zone commonly consists of disseminated pyrite with low Ni and Cu values. The margins of the zone contain the highest

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grade mineralization, which typically occurs as net-textured or nearly massive sulphides 2 to 5 m thick. The deposit model indicates that IP/resistivity in conjunction with magnetics are suitable geophysical methods for the discovery of additional mineralization. The base metal occurrences in the southeastern part of the property and on the adjacent Ft. Knox property may not be base metal volcanogenic massive sulphide type mineralization. There is a greater potential to discover “Five Element (Ni-Co-As-Ag-Bi) Vein” mineralization similar to the silver deposits in the Cobalt, Ontario area.

Figure 4. n=2 Mx chargeability from JVX 5-33

Earlier ground geophysical surveys by JVX for Goldeye Explorations on the Grouse grid include JVX 98‐53 : Profile IP/resistivity (5 km) on 4 lines (10900E, 11500E, 11900E, 12300E) JVX 5‐33 : Profile IP/resistivity (4.3 km), HLEM (1.575 km) and magnetics/VLF (2.95 km) JVX 6‐05 : Bore hole IP/resistivity (GL‐06‐01) JVX 8‐79 : Fixed loop TDEM (16.8 km), TerraTEM (8.3 km) and magnetics/VLF (21.05 km)

2006 Goldeye drill hole GL‐06‐01 was set to test an IP zone from 5‐33. GL‐06‐01 is at 499635 e, 5267231 n (NAD83, Z17N), azimuth 225°, dip ‐50°, length 191 m. The n=2 Mx chargeability from 5‐33 is shown in figure 4. VLF offset profiles from 8‐79 are shown in figure 5.

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Figure 5. VLF offset profiles from JVX 8-79

Reading from the JVX 6‐05 report on dhip surveys on GL‐06‐01 ‐

Target T1 on Grouse grid was drilled from northeast. The collar was about 50 m northeast of the probable trace of the target center (30 m southeast of line 10800E). If the target is vertical and if it continues southeast of line 10800E, it should be intersected at a down hole depth of 78 m. If the target dips 45º to the northeast (i.e. towards the drill hole), it should be intersected at a down hole length of 39.6 m. The target will not be intersected for dips to the southwest at a dip less than 63.6º. Below the 8.5 m of overburden, most of this hole passes through mafic and felsic volcanics (80 %). There are two intersections of intrusives (total 13 %) and one of metasediments (7 %). Geophysical features of note include 77.4 to 78.75 : 1 – 2 % pyrite in volcanics 141.5 to 151.35 : 1 – 2 % pyrite in volcanics 162.8 to 170.6 : 1 to 4 % pyrite in volcanics 170.6 to 182.6 : graphitic metasediments If the target is the combination of 1 to 4 % pyrite + graphitic sediments over 20 m centered around 172 m down hole, the target dips at 65° to the southwest. In this case, the target was drilled down dip.

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3. Survey Dennis Palos, senior geophysicist from JVX, was in charge of the survey. Field assistants included geophysicist Thomas Au and helper Brian Willard. Data processing at the JVX office was handled by Lily Manoukian. The survey grid was registered with a series of GPS control points. UTM coordinates from a hand held GPS receiver were collected at 87 GPS control points (appendix 1). The average distance between GPS control points is 263 m. The survey grid on which the geophysical results are registered is drawn by interpolation from these GPS control points. A gradient array was used with fixed current electrodes grid north and grid south of the survey area. Two sets of current electrodes were used – one for lines 10300E to 11000E and another for lines 11100E to 11800E. Chargeability and apparent resistivity were measured with a 25 m potential dipole, sampled every 25 m. An Elrec Pro time domain IP/resistivity receiver and a Walcer 10kVA time domain transmitter were used. A 2 second current pulse was used. The Elrec Pro records the primary voltage and the chargeability decay at 19 slices. The apparent resistivity is calculated from the primary voltage and the transmitted current. The Mx chargeability, centered at 870 msec, is calculated as the weighted average of 3 slices (M13, M14 and M15). A 6 Rx dipole string was used. Measurements were made at 845 Rx dipoles, 141 of which were repeats. Chargeability and apparent resistivity values at repeats were averaged. The average, minimum and maximum values of chargeability and apparent resistivity of the 712 unique Rx dipoles are listed in table 1.

Quantity average minimum maximum Mx 3.6 -1.4 12.5 Resistivity 21,800 826 94,470

Table 1. IP/resistivity statistics

Primary voltages were very low or negative at 11 Rx dipoles at the north ends of lines 10300E and 10400E and the south end of 11100E. Chargeability and resistivity readings at these points are considered invalid and are not shown on final maps. 4. Discussion The strong IP zone, first seen in 5‐33 and drill tested by GL‐06‐01, is clear in the gradient array results. This 300 m long IP zone runs from 10600E to 10900E near 10350N. Peak Mx chargeabilities are 20 mV/V (pole‐dipole 5‐33) and 10 mV/V (gradient 10‐93). There is no evidence in the resistivity results that this IP zone is also a conductor. 5‐33 Mx chargeability and apparent resistivity pseudosections for line 10800E are shown in figure 6. The gradient array chargeability map shows a second, parallel IP zone 100 to 200 m to the south. At 10400E, 10200N, peak Mx values are 6 mV/V (pole‐dipole 5‐33) and 8 mV/V (gradient 10‐93). There is no evidence in the resistivity results that this IP zone is also a conductor. Surficial resistivities from 5‐33 here are around 5,000 ohm.m. This weak IP zone is probably buried under thin overburden. 5‐33 Mx chargeability and apparent resistivity pseudosections for line 10400E are shown in figure 7.

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Figure 6. Mx chargeability and apparent resistivity. Line 10800E. JVX5-33

Figure 7. Mx chargeability and apparent resistivity. Line 10400E. JVX5-33

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5. Conclusions

A gradient array spectral IP/resistivity survey was done on the Grouse grid, Shining Tree area, Ontario. The field work was done from November 24 to December 4, 2010. Total production was 18,125 m. The Grouse grid is within claims 1246451 and 1246454 registered to Goldeye Explorations Ltd. The results have been presented in maps of chargeability and apparent resistivity at 1:5,000.

The gradient array survey data should be inverted to determine if there are deep chargeable conductive sources not apparent in the field data. The survey should be conducted over Grouse Lake to determine if there are any anomalies under it. Grouse Lake appears to cover the strike extension of the main chargeability anomaly.

Blaine Webster, B.Sc., P. Geo. December 16, 2010

Certificate of Qualifications

Blaine Webster President - JVX Ltd.,

60 West Wilmot Street, Unit 22 Richmond Hill, Ontario L4B 1M6

Tel : (905) 731-0972 Email : [email protected]

I, Blaine Webster, B. Sc., P. Geo., do hereby certify that

1. I graduated with a Bachelor of Science degree in Geophysics from the University of British Columbia in 1970.

2. I am a member of the Association of Professional Geoscientists of

Ontario.

3. I have worked as a geophysicist for a total of 36 years since my graduation from university and have been involved in minerals exploration for base, precious and noble metals and uranium throughout much of the world.

4. I am responsible for the overall preparation of this report.

______________________ Blaine Webster, B. Sc., P. Geo.


Appendix 1 Production, GPS control points, Instrumentation and Data Processing

A gradient array spectral IP/resistivity survey was done on the Grouse grid, Fawcett Township,

Shining Tree area, Ontario. The grid is centered 8 km east of Shining Tree and 30 km west southwest of

Gowganda. The work was done for Goldeye Explorations Ltd. by JVX Ltd. under JVX job number 10-93.

The field work was done from November 24 to December 4, 2010. Total production was 18,125 m

(table 1). Coverage is measured from the station of the first to last potential electrode (ideal grid).

Line IP-From IP-To Separation Date

10300E 10100N 10700N 600 December 2, 2010

10400E 9900N 10650N 750 December 2, 2010

10500E 9500N 10700N 1200 December 4, 2010

10600E 9300N 10475N 1175 December 4, 2010

10700E 9000N 10600N 1600 December 3, 2010

10800E 8800N 10500N 1700 December 1/3, 2010

10900E 8800N 10500N 1700 December 1/2, 2010

11000E 8800N 9625N 825 December 1, 2010

10050N 10600N 550 December 2, 2010

11100E 8800N 9600N 800 November 27, 2010

11200E 8800N 9600N 800 November 27, 2010

11300E 8800N 9875N 1075 November 26, 2010

11400E 8800N 9850N 1050 November 26, 2010

11500E 8800N 10200N 1400 November 25, 2010

11600E 8900N 10300N 1400 November 25, 2010

11700E 8800N 9575N 775 November 24, 2010

11800E 8775N 9500N 725 November 24, 2010

Total 18,125 m

Table 1. Production summary

The survey was done with fixed current electrodes grid north and grid south of the survey

area. Chargeability and apparent resistivity were measured every 25 m with a 25 m receiver dipole. For

lines 10300E to 11000E, the current electrodes were set out at 10910E, 8625N and 10840E, 11600N

(current electrode separation 2975 m – ideal grid). For lines 11100E to 11800E, the current electrodes

were set out at 11600E, 8280N and 11625E, 11305N (current electrode separation 3025 m – ideal

grid). Grid

The Grouse grid is within claims 1246451 and 1246454 registered to Goldeye Explorations

Ltd. The grid is centered 8 km east of Shining Tree, Ontario - 100 km south southeast of Timmins and

125 km north of Sudbury.

Grid registration is based on UTM coordinates from a hand held GPS receiver at 2 or more well

separated points on each survey line. A total of 87 GPS control points were collected (table 2). The

average distance between GPS control points is 263 m. Range is 23 to 1323 m. The geophysical survey

results are registered with UTM coordinates interpolated or extrapolated from these GPS control

points.

Line Station UTM e UTM n elevation

10300E 10100N 488037 5267186 387

10250N 488088 5267318 389

10400N 488133 5267465 390

10550N 488182 5267607 392

10700N 488231 5267748 *

10400E 9900N 488058 5266962 *

10050N 488109 5267102 385

10200N 488160 5267246 386

10350N 488212 5267382 384

10500N 488260 5267525 391

Appendix 1: Production, GPS control points, Instrumentation and Data Processing



10650N 488306 5267665 392

10500E 9500N 487995 5266522 403

9800N 488095 5266798 388

9950N 488145 5266942 382

10100N 488213 5267085 396

10250N 488257 5267224 402

10700N 488408 5267650 *

10600E 9300N 488043 5266286 *

9450N 488095 5266430 386

9750N 488195 5266710 391

9900N 488249 5266853 391

10200N 488354 5267134 402

10325N 488397 5267251 397

10475N 488447 5267393 392

10700E 10600N 488565 5267466 391

9900N 488339 5266819 392

9450N 488189 5266398 386

9150N 488085 5266113 391

9000N 488039 5265973 *

10800E 10500N 488625 5267344 *

9600N 488335 5266505 386

9150N 488184 5266082 392

8825N 488078 5265778 *

8800N 488070 5265755 373

10900E 8800N 488151 5265725 377

9200N 488296 5266101 392

9450N 488379 5266329 393

9700N 488461 5266566 383

9825N 488520 5266735 389

9975N 488557 5266828 394

10100N 488598 5266944 387

10225N 488642 5267063 386

10325N 488689 5267179 390

10500N 488775 5267301 383

11000E 8800N 488256 5265687 377

8950N 488304 5265837 395

9050N 488340 5265936 401

9275N 488413 5266134 *

9625N 488532 5266464 393

10050N 488572 5266837 389

10100N 488600 5266875 391

10125N 488605 5266898 *

10200N 488648 5266960 389

10450N 488800 5267159 389

10600N 488886 5267280 *

11100E 8800N 488349 5265653 *

9600N 488617 5266406 *

11200E 8800N 488451 5265615 *

8950N 488497 5265762 388

9200N 488573 5265994 39

9600N 488705 5266372 *

11300E 8800N 488548 5265596 *

9375N 488730 5266132 391

9875N 488890 5266591 *

11400E 8800N 488635 5265576 *

9500N 488862 5266211 397

9850N 488987 5266540 *

11500E 8800N 488713 5265524 *

9450N 488942 5266131 390

9700N 489025 5266365 387

9900N 489099 5266562 *




10075N 489156 5266721 396

10200N 489199 5266840 395

11600E 10300N 489342 5266895 *

10100N 489289 5266726 392

9900N 489193 5266496 381

9650N 489098 5266262 385

9275N 488973 5265933 394

9025N 488885 5265699 394

8900N 488841 5265588 *

11700E 10300N 489436 5266859 *

9575N 489173 5266177 *

8850N 488919 5265502 *

8800N 488898 5265459 *

11800E 8775N 488989 5265406 *

8900N 489019 5265474 *

10300N 489527 5266820 *

Table 2. GPS control points (NAD83, Z17N), Grouse grid

Figure 1. Grouse grid (base map from MNDMF claimap3 website)

Instrumentation

Iris Instruments Elrec Pro IP/resistivity receiver, SN 2315-3102519783-187

Walcer TX KW10 time domain IP transmitter

Honda 24 HP MG set

The Elrec Pro time domain IP receiver can take readings with up to 10 receiver dipoles. The IP

decay is measured in millivolts/volt over up to 20 programmable windows. For this survey, the IP

decay was measured over 19 windows. Time settings for these 19 windows are listed in table 3. All



times are in milliseconds after current shut off. A 2 second current pulse was used throughout.

Specification sheets are attached.

slice start end duration mid point

M1 50 70 20 60

M2 70 110 40 90

M3 110 150 40 130

M4 150 190 40 170

M5 190 230 40 210

M6 230 270 40 250

M7 270 310 40 290

M8 310 380 70 345

M9 380 450 70 415

M10 450 530 80 490

M11 530 610 80 570

M12 610 690 80 650

M13 690 780 90 635

M14 780 900 120 840

M15 900 1050 150 975

M16 1050 1210 160 1130

M17 1210 1380 170 1295

M18 1380 1570 190 1375

M19 1570 1770 200 1670

Table 3. Elrec Pro chargeability windows

For each receiver dipole, the Elrec Pro records line/stations of the current and potential

electrodes, the primary voltage (mV), self potential (mV), 19 chargeability values (mV/V) and the

transmitted current (mA). The apparent resistivity is calculated from the primary voltage and

transmitted current using K factors based on array geometry.

Mx chargeability, the IP slice most often presented in surveys done with the Scintrex IPR12

receiver, is centered at 870 msec (690 to 1050 msec). M14 at 840 msec (780 to 900 msec) from the

Elrec Pro is the closest IP slice to Mx. Mx may be calculated as the weighted average of M13, M14 and

M15 as (M13*90+M14*120+M15*150)/360.

The Walcer Geophysics Ltd. Walcer TX KW10 transmitter outputs up to 10 kVA (voltage to

3200V, current to 20 Amps). Line voltage and current are shown on an LED display. The transmitter was

powered by a 24 hp Honda motor generator.

Data Processing and Presentation

Grid

GPS control points are loaded into a Geosoft database (gps.gdb) as UTM coordinate –

line/station pairs. The IP/resistivity results are registered with UTM coordinates interpolated or

extrapolated from gps.gdb.

Base Map

Claim fabric has been downloaded as *.shp files from the MNDMF claimap3 website (Copyright

Queen’s Printer for Ontario). A topographic base map and claim fabric are available as a *.png image

from the same source. Lakes, rivers and roads have been downloaded as 1:50,000 *.shp files from

NRCAN geogratis.ca (Earth Sciences Sector of Natural Resources Canada). There are minor differences

in these topographic elements from federal and provincial sources.

IP/Resistivity

At the end of every survey day, the IP/resistivity data are dumped from the Elrec Pro to a PC.

Output is an ASCII text file with the job and line numbers as the file name. These data are transferred to



a MS Excel workbook.The data are reformatted into a new worksheet called ‘GeosoftReadyFormat’. Mx

chargeability and apparent resistivity are added to this worksheet. Duplicate values are averaged.

Mx has been calculated as Mx = (M13*90 + M14*120 + M15*150)/(90+120+150).

Office data processing is based largely on Geosoft Oasis Montaj v6.3 (www.geosoft.com). The

GeosftReadyFormat worksheets are loaded into a Geosoft database and merged with the position data

in gps.gdb.

Plan maps of Mx chargeability and apparent resistivity are prepared with Oasis Montaj.

Random gridding is used in all cases. Plan maps show the interpolated grid, station numbers, posted

values and line + colour contours. Colour contour intervals are decided by an equal area distribution of

all of the chargeability or apparent resistivity readings on any grid.

Apparent Resistivity

From Telford et al, 1990, the potential at any point in a uniform half space due to a current pole

at any point in that half space is given by

V = Iρ (1/4π) [1/r + 1/r’]

Where

V is the potential in volts (or millivolts)

I is the transmitted current in amps (or milliamps)

ρ is the apparent resistivity in ohm.m

r is the distance from the point to the current pole

r’ is the distance from the point to an image current pole

The imaginary ‘image’ current pole is in free space directly above the current pole and at a height equal

to the depth to the current pole.

With two current and two potential electrodes in a half space, the potential difference between

the two potential electrodes is given by

ΔV = Iρ (1/4π) [ (1/r1c1 + 1/r1c1’) – (1/r1c2 + 1/r1c2’)

- (1/r2c1 + 1/r2c1’) + (1/r2c2 + 1/r2c2’) ]

Where ricj is the distance from the ’i’ potential electrode to the ‘j’ current electrode and ricj’ is the

distance from the ‘i’ potential electrode to the image of the ‘j’ current electrode. The apparent

resistivity is then

ρa = K4πΔV/I

where the geometry factor

K = [ (1/r1c1 + 1/r1c1’) – (1/r1c2 + 1/r1c2’) - (1/r2c1 + 1/r2c1’) + (1/r2c2 + 1/r2c2’) ]-1

For the gradient array where all current and potential electrodes are on surface and that surface is

assumed to be flat, the geometry factor

K = 0.5 [ (1/r1c1 – 1/r1c2) – (1/r2c1 – 1/r2c2) ]-1

Reference

Telford, W.M., Geldart, L.P. and R.E. Sheriff, 1990, Applied Geophysics, Second Edition. Cambridge

University Press

Archives

The results of the survey are archived on CD. Included on the CD is the Oasis Montaj viewer.

File types include

ASCII *.txt or *.prn or *.xyz – text files, including instrument data dumps

MS Excel *.xls – Excel workbooks, reformatted IP data (one workbook for each line)

*.gdb - Geosoft databases (gps, IP/resistivity)

*.map – Geosoft format maps included with this report

MS WORD *.doc and Adobe Acrobat *.pdf – this report


Appendix 2 Weekly Field Production Reports

JVX Ltd.

Weekly Field Production Report – Gradient Array IP/Resistivity

Project No 10-93 Client: Goldeye Area: Grouse Lake Week Ending: Nov 27, 2010

Day Line From To Length

Sun Nov 21

OFF

Mon Nov 22

Road icy – We did not travel until after the sand truck passed; the logging trucks did the same. Picked up equipment at Crip Lake. At Grouse Lake set up C1 and did grid recon, and opened up road to the south, then ran out of time.

Tue Nov 23

Picked up wire south of Breeze Lake and went to Grouse Lake to complete the C2 and lay out wire between C1 and C2

Wed Nov 24

Set up Tx and started survey. It went well with 25 m dipole; there was no need to go to 50 m because Vp was adequate. Brian mobilized from Kirkland Lake in the afternoon.

11800E 11700E

9500N 8800N

8775N 9575N

725 775

Thu Nov 25

Set up Tx tent because bad weather was expected. Read two lines

11600E 11500E

10300N 8800N

8900N 10200N

1400 1400

Fri Nov 26

Gradient IP. It snowed most of the day. On L11400E we skipped from 9400N to9300N because of a pond with slush and dubious ice. On L11300E, chainage error: picket 9800N had been skipped, hence picket labeled 9825 is really 9850N

11400E 11300E

9850N 8800N

8800N 9875N

1050 1075

Sat Nov 27

Gradient IP. We went as far west as we could while still getting useable readings with the existing gradient electrodes. We will move the southern gradient the next day. It snowed last night and it warmed up today, the ground was very slippery. Lines 11200E and 11100E are in bad shape; they are blocked with deadfall and many pickets have fallen (and are hard to find under the snow).

11200E 11100E

8800N 9600N

9600N 8800N

800 800

Production : X Mobilization : M Standby : S Logistics & Preparation : L

Name Position S M T W T F S Dennis Palos Geophysicist X X X X X X Thomas Au Geophysicist X X X X X X Brian Willard Helper M X X X

Appendix 2: Weekly Field Production Reports

Goldeye Explorations Ltd. JVX 10-93 (Grouse grid)

2

JVX Ltd. Weekly Field Production Report – Gradient Array IP/Resistivity

Project No 10-93 Client: Goldeye Area: Grouse Lake Week Ending: Dec 4, 2010


Sun Nov 28

Day off (go to New Liskeard, but groceries, go to Canadian Tire, buy supplies for surface IP and BHIP) (at house begin Walcer Tx dummy load repair, look at gravity proposal for two hours).

Mon Nov 29

Diagnose and repair dummy load for Walcer Tx. Move southern current electrode to the west so that the western lines could be read.

Tue Nov 30

Move the northern current electrode further north, and to the west so that the western lines could be read. Waited for a window of no rain to do the work. We worked until we were soaked and miserable.

Wed Dec 1

We filled in the south part. 11000E 10900E 10800E

8800N 9850N 8800N

9625N 8800N 9075N

825 1050 275

Thu Dec 2

We read the north portion on L11000E - it does not join the south part. Please see the Mapsource file for bizarre line direction. We read the north part of L10900E and one overlap dipole over the south part. At the northern extremities of L10300E and L10400E, the Vp values were low and the Mx values were “random” because of unfavourable geometry of the current electrode.

11000E 10900E 10300E 10400E

10600N 9850N 10700N 9900N

10050N 10500N 10100N 10650N

550 650 600 750

Fri Dec 3

10800E 10700E

10500N 9000N

9075N 10600N

1425 1600

Sat Dec 4

Finished the wide spacing gradient 10500E 10600E

10700N 9300N

9500N 10475N

1200 1175


Name Position S M T W T F S Dennis Palos Geophysicist X X X X X X Thomas Au Geophysicist X X X X X X Brian Willard Helper X X X X X X

Appendix 2: Weekly Field Production Reports

Goldeye Explorations Ltd. JVX 10-93 (Grouse grid)

3

JVX Ltd. Weekly Field Production Report – Gradient Array IP/Resistivity

Project No 10-93 Client: Goldeye Area: Grouse Lake Week Ending: Dec 11, 2010


Sun Dec 6

Pick up all gradient wire, take down Tx tent and pick up Tx and MG

Mon Dec 6

Tue Dec 7

Wed Dec 8

Thu Dec 9

Fri Dec 10

Sat Dec 11


Name Position S M T W T F S Dennis Palos Geophysicist X Thomas Au Geophysicist X Brian Willard Helper X


Appendix 3 - Map Images

The results of the surveys are presented in 2 maps at 1:5,000. All but map surrounds, legend,

title block and posted values are shown below. The 2 maps are

- Mx chargeability

- apparent resistivity

Appendix 3 - Map Images


Figure 1. Mx chargeability

Figure 2. Apparent resistivity

IRIS INSTRUMENTS

ELREC Pro

10 CHANNELS

IP RECEIVER FOR

MINERAL EXPLORATION

• 10 simultaneous dipoles

• 20 programmable chargeability windows

• High accuracy and sensitivity

ELREC Pro: this new receiver is a new compact and low consumption unit designed for high productivity Resistivity and Induced Polarization measurements. It features some high capabilities allowing to work in any field conditions.

Reception dipoles: the ten dipoles of the ELREC Pro offer an high productivity in the field for dipole-dipole, gradient or extended poly-pole arrays.

Programmable windows: beside classical arithmetic and logarithmic modes, ELREC Pro also offers a Cole-Cole mode and a twenty fully programmable windows for a higher flexibility in the definition of the IP decay curve.

IP display: chargeability values and IP decay curves can be displayed in real time thanks to the large graphic LCD screen. Before data acquisition, the ELREC Pro can be used as a one channel graphic display, for monitoring the noise level and checking the primary voltage waveform, through a continuous display process.

Internal memory: the memory can store up to 21 000 readings, each reading including the full set of parameters characterizing the measurements. The data are stored in flash memories not requiring any lithium battery for safeguard.

Switching capability: thanks to extension Switch Pro box(es) connected to the ELREC Pro unit, the 10 reception electrodes can be automatically switched to increase the productivity in-the-field.

ELREC Pro unit with its graphic LCD screen

Display of numeric values and IP decay curve during acquisition

Monitoring of the Primary voltage waveform before acquisition

ELREC Pro

FIELD LAY-OUT OF AN ELREC PRO UNIT

The ELREC Pro unit has to be used with an external transmitter, such as a VIP transmitter. The automatic synchronization (and re-synchronization at each new pulse) with the transmission signal, through a waveform recognition process, gives an high reliability of the measurement. Before starting the measurement, a grounding resistance measuring process is automatically run ; this allows to check that all the electrodes are properly connected to the receiver. Extension Switch Pro box(es), with specific cables, can be connected to the ELREC Pro unit for an automatic switching of the reception electrodes according to preset sequence of measurements ; these sequences have to be created and uploaded to the unit from the ELECTRE II software.

The use of such boxes allows to save time in case of the user needs to measure more than 10 levels of investigation or in case of large 2D or 3D acquisition. DATA MANAGING

PROSYS software allows to download data from the unit. From this software, one has the opportunity to visualize graphically the apparent resistivity and the chargeability sections together with the IP decay curve of each data point. Then, one can process the data (filter, insert topography, merge data files…) before exporting them to ″txt″ file or to interpretation software: RES2DINV or RESIX software for pseudo-section inversion to true resistivity (and IP) 2D section. RES3DINV software, for inversion to true resistivity (and IP) 3D data.

FEATURES TECHNICAL SPECIFICATIONS

• Input voltage: Max. input voltage: 15 V Protection: up to 800V

• Voltage measurement: Accuracy: 0.2 % typical Resolution: 1 µV Minimum value: 1 µV

• Chargeability measurement: Accuracy: 0.6 % typical

• Induced Polarization (chargeability) measured over to 20 automatic or user defined windows

• Input impedance: 100 MΩ • Signal waveform: Time domain (ON+,OFF,ON-,OFF)

with a pulse duration of 500 ms - 1 s - 2 s - 4 s - 8 s • Automatic synchronization and re-synchronization

process on primary voltage signals • Computation of apparent resistivity, average

chargeability and standard deviation • Noise reduction: automatic stacking number in relation

with a given standard deviation value • SP compensation through automatic linear drift

correction • 50 to 60Hz power line rejection • Battery test GENERAL SPECIFICATIONS.

• Data flash memory: more than 21 000 readings • Serial link RS-232 for data download • Power supply: internal rechargeable 12V, 7.2 Ah

battery ; optional external 12V standard car battery can be also used

• Weather proof • Shock resistant fiber-glass case • Operating temperature: -20 °C to +70 °C • Dimensions: 31 x 21 x 21 cm • Weight: 6 kg

IRIS INSTRUMENTS - 1, avenue Buffon, B.P. 6007 - 45060 Orléans Cedex 2, France Phone: +33 (0)2 38 63 81 00 - Fax: +33 (0)2 38 63 81 82 E-mail: [email protected] - Web site: www.iris-instruments.com

Extension Switch Pro box able to drive 24 - 48 - 72 or 96 electrodes

Walcer Model TX 9000 Transmitter The Walcer Tx 9000 transmitter is used for time-domain Induced Polarization survey. Its switching times are 1 sec., 2 sec., 4 sec., and 8 sec. It can operate in extreme climatic conditions. The Walcer Tx 9000 transmitter is powered by MG-12 Honda generator (125V input). It transmits up to 20Amps and 100-3200V in 10 steps.

Walcer Model TX 9000

Power Input 125V line to neutral 400 Hz / 3 phase

Powered by MG-12 Output

100 - 3200V in 10 steps 0.05 - 20 Amps

Tested to 9.25 kVA Switching

1 sec., 2 sec., 4 sec., 8 sec. Metering

LED for line voltage and output current

Size 63cm. x 54cm. x 25cm.

Weight 44 kg.

Walcer Motor Generator

MG-12

Output 120 / 220V AC

400 Hz / 3 phase Generator

Bendix Aircraft Type Very durable

Forced Air Cooled Engine

24 HP Honda,Twin Cylinder Size

75cm. x 70cm. x 25cm. Weight 125 kg.

Walcer Geophysics Ltd.

2106 Regional Road 3 Enniskillen, OntarioCANADAL0B 1J0

Phone: (905) 263-8767,Fax: (905) 263-8766

Email: [email protected]

mailto:[email protected]

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Scale 1 :5000 100

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200

GOLDEYE EXPLORATION LTD .

300

SPECTRAL IP I RESISTIVITY SURVEY GROUSE LAKE GRID -FAWCETT TWP.

SHINING TREE AREA- ONTARIO NTS: 41 P/11

CHARGEABILITY Array: Gradient, a=25 m

Contours: 0.05, 0.5 & 5 mVN Value posted: Rigth, Stations posted: Left

lnst: Rx(2 sec) IRIS ELREC PRO & Tx(2 sec) Topographic base map copyright."© Department of Natural Resources Canada

Claims provided by:© Queen's Printer for Ontario, 2010

JVX LTD. ref. no. 10-93, December 2010

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Scale 1 :5000 100

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GOLDEYE EXPLORATION LTD.

300

SPECTRAL IP I RESISTIVITY SURVEY GROUSE LAKE GRID -FAWCETT TWP.

SHINING TREE AREA- ONTARIO NTS: 41 P/11

RESISTIVITY (n=2) Array: Gradient, a=25 m

Contours: 5, 50 & 200 ohm-m Value posted: Rigth, Stations posted: Left

lnst: Rx(2 sec) IRIS ELREC PRO & Tx(2 sec) Topographic base map copyright© Department of Natural Resources Canada

Claims provided by:© Queen's Printer for Ontario, 2010

JVX LTD. ref. no. 10-93, December 2010

report on a gradient array ip/resistivity survey

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