Upload
others
View
4
Download
0
Embed Size (px)
Citation preview
\\'assennar Properly Strathcona Twp. 2.20529NTS 31 M/4
31M04SE2007 2.20529 RIDDELL 010
MINERAL EXPLORATION PROJECT 1999 WASSENAAR PROPERTY
Strathcona Township
Geophysical Surveys Magnetometer, VLF-EM, Induced Polarization, Beep Mat
Geological Surveys Geological Mapping and Prospecting
Sudbury Mining District, Ontario
RECEIVED
SEP 1 5 r:iGEOSCIENCE ASSESSMENT
OfFICE
Meegwich Consultants Inc. Box 482 Temagami. Ont. POH 2HO tel (705)569-2904
ff/7/ew Wassenaar OPAP Final Submission Wassenaar Pr.nnertv Strathcona Twp.
TABLE OF CONTENTS
INTRODUCTION:Page
CO H 1O O
Property LocationAccessProperty DescriptionSummary of Work Done
PROSPECTING SURVEY:
IntroductionBeep Mat ProspectingProspecting
GEOPHYSICAL SURVEYING:
Magnetometer SurveyVLF-EM SurveyI.P. SurveyConclusions and RecommendationsInstrument specifications MagnetometerInstrument specifications VLF-EMCertificate of AuthorReferences
456
7891112121314
toU)
lf
O H OO
LIST OF FIGURES
Figure l Figure 2 Figure 3
Location Map Claim Map Geology
LIST OF MAPSMAP l Prospecting and Compilation Map MAP 2 Total Field Magnetic Contour Map MAP 3 VLF-EM Profile Map MAP 4 I.P. Pseudo sections L 550 W, 300 W, 50 W and O
Mecgvvich Consultants Inc. Box 482 Temagami. Ont. POH 2HO lei. (705)569-2904
\V\\lemWassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
APPENDIX I
Geological Mapping Report- A.W. Beecham consultant Dec 1999.-report and geology map (pond area)
APPENDIX II
Assay Certificate
Meegwich Consultants Inc. Box 482 Temagami, Ont. POH 2HO tel. (705)569-2904
MANITOBA,,''
X
ONTARIO
QUEBEC
TIMMINS-
.SAULT
,STE. MARIE O
.SUDBURY
TEMAGAM l
AREA
150ml
200 Km
FIGURE l '. LOCATION MAP TEMAGAMI PROJECT
PROPOSED ZONE 2 GRID
I23I4ZI'I (EXISTING)
-•A—,-~. ~
CLAIM fc GRID LOCATION MAP
WASSENAR PROPERTY,V -/tftJii
STRATHCONA TP
-^N'
U'illem Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
Property Location:
NTS: 31M/4Township: Strathcona (Upper Twin Lake)Mining Division: SudburyResident Geologist: Cobalt/Kirkland Lake - Gary GrabowskiLatitude: 47-00-00Longitude: 79-46-00Nearest town: Temagami (7 km to the north-northwest)
Access:
The property is situated 7 km south-southeast of Temagami as the crow flies Access to the claims is by traveling eastward on a logging road departing Hwy 11 about 10 km south of Temagami where the Trans Canada Pipeline crosses the highway. At a point 4 km east of the highway an equipment trail (where a backhoe has traveled) winds in another 300 meters to stripped showings which was the central area of detailed gridwork, geophysics, geological mapping and comprehensive sampling ( Zone 1).
Property Description:
The property consists of a group of 14 contiguous claims for a total area of 830hectares (54 units of+/-16 hectares). The claim numbers of the property are asfollows:1191010 16 units 1140888 4 units1191002 l unit 1191004 l unitl 191005 l unit 1191006 3 unit1191007 3 units 1191008 l unit1076960 l unit 1076969 l unit1076974 l unit 1231421 5 units1140887 4 units 1191009 12 units
Summary of Work Done:
Basically the northwest corner of an 830 hectare property was covered with a detailed grid pattern with line spacings of 25, 50 and 100 meters. 14.50 km of line was chainsawed and picketed at 25 meter intervals. Magnetometer and VLF-EM covered the entire grid. I.P., Geological, Beep Mat and Prospecting covered
Meegwich Consultants Inc. Box 482 Temagami, Ont. POH 2HO tel. (705)569-2904
ll'illem IVassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
areas that are considered high priority for followup from the current Mag/VLF-EM survey and previous geological work.
Totals Dates Preliminary kmLinecutting 14.50 July 1-25,1999 Magnetometer survey 13.90 Aug. 15-22, 1999 VLF-EM Survey 12.90 Aug 15-22, 1999 DetailedGeological Survey 4.00 Nov. 14,15, 1999 Prospecting 3.00 May 23, Aug l, 1999 Beep Mat Survey 5.00 Oct 23,24, 1999 I.P. Survey 2.425 Dec. 17
The primary objective of the program was to outline and explore for significant gold mineralization over Zone 2 where a 59 g/tonne assay was picked up and also to do Phase Two followup (I.P.) over the anomalous base metal Zone l. The results of the surveys have indicated drill targets near Zone l. The results over Zone 2 are not as conclusive at present however there are faint indications of a zone trending east to west.
Zone l should be drilled for a base metal deposit while Zone 2 should be only x-ray drilled for more geologic information and to test for continuity of the high grade gold occurrence. In total there are 5 drill targets based on thorough surface work funded by the applicant and the OPAP program.
Thanks to the OPAP program the option status of the property has been moved along to the drill stage.
Meegwich Consultants Inc. Box 482 Temagami. Out. POH 2HO tel. (705)569-2904
ll'il/eni H'assenaar OPAP Final Submission Wassenaar Propertv Strathcona Twp.
Beep Mat Surveying and Prospecting ReportWassenaar Property
Strathcona Twp.
Meegwich Consultants Inc. Box 482 Temagami, Ont. POH 2HO tel. (705)569-2904
Willeni Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
January 04, 2.ooa
BEEP MAT SURVEYING AND PROSPECTING REPORT
BEEP MAT SURVEY:
Introduction: ^
A beep mat survey was carried out on Oct 23,24 with a travel day on the 22nd and , 1999. The prospectors were Willem Wassenaar, Sy Wassenaar and Siek Wassenaar. The beep mat was borrowed from the MNDM in Kirkland Lake. The objective of the beep mat survey was to explore for sulphide mineral along the length of the conductors picked up by the VLF-EM survey and to prospect in general. There was about 5.0 km covered.
Instrument:
The beep mat i s a mini-EM system with a transmitter and a receiver enclosed in a durable plastic sled about 3 ft in length. When the mat is dragged over a sulphide occurrence by hand the unit will indicate such by a beeping noise. The location of the beeping is then dug up to investigate. It is only successful in area of light overburden cover. This method was successful in detecting the main showing area at O, O on the grid in the past. The sled is dragged across the conductor at right angles at approximately along the length.
The targets surveyed are as follows:
Conductor G: This anomaly was covered with the beep mat with no hits. The west end of the conductor is high and dry while the eastern part of it drops off into a low lying area. While there were no hits from the beep mat there could still be mineralization down past the 5 ft limit of the beep mat. This anomaly should be checked with HLEM.
Conductor H: This feature was field checked for sulphides with no hits. Part of the anomaly lies in a small pond so it was not totally resolved however the land portion has been covered.
Conductor M: This feature lies in a topographic low. It was covered along the full length to the lake from the end of the "boot bay".
Conclusion and Recommendations:
The results of the beep mat surveying were disappointing. There were no significant or 1 ' detectable sulphides encountered. This means there are no occurrences within 5 ft. of surface. A more sophisticated unit such as HLEM should be deployed to investigate the possibility of deeper occurrences. (SEE COVERAGE ON MAP ONE)
Meegwich Consultants Inc. Box 482 Temagami. Ont. POH 2HO tel. (705)569-2904
inilem Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
PROSPECTING SURVEY:
(Only a minor amount of prospecting was done by the applicant due to a heavy work schedule from other commitments). The areas prospected (stripping and sampling) are discussed as follows:
Main showing area Augl:
25 W, 25S Following a property visit by Wayne Benham of Queenston in May 99 it was thought some higher grade samples within chemical sediments with abundant sulphides (chalcopyrite, pyrite, pyrrhotite) near the main showing would indicate a more widespread picture and expand the dimensions of the zone. W. Wassenaar spent Aug l stripping and sampling. Of the 10 samples taken one was assayed at X-RAL Laboratories. A whole rock analysis was done and the more interesting results were 563 ppm Co, 772 ppm Ni and 308 ppm Cu.
Beaver Pond area May 23:
May 23 was spent prospecting a rock ledge on L 550 and 600 W at 300 N. There was gossan staining along the face containing minor pyrite. The rock type was mafic volcanic.
The northwest side of the pond was prospected and a 2 cm quartz vein in diabase containing abundant chalcopyrite along fractures was discovered but not assayed.
(see Map One for areas covered)
Meegwich Consultants Inc. Box 482 Temagami, Ont. POH 2HO tel. (705)569-2904
Willem Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
GEOPHYSICAL REPORT
Magnetometer/VLF-EM/Induced PolarizationWassenaar Property
Strathcona Twp.
Meegwich Consultants Inc. Box 482 Temagami, Ont. POH 2HO tel. (705)569-2904
7
IVil/em ll'assenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
Geophysical Surveying
MAGNETOMETER SURVEY^—^^-——-^^——^——^^^^^————
Instrument specifications:;
A total of 13.9 km ( l 150 readings) was surveyed using a micro-processor based GEM Systems GSM-19 Mag/VLF unit. The instrument is capable of +I- 1 7100th of a gamma resolution. The instrument was used in the mobile mode The diurnal variation was corrected for using a base station set up near the grid. This base instrument was an EDA Omnf IV capable of 1710th of a gamma resolution.
Dates of survey:
The survey was done by D. Laronde of Meegwich Consultants Inc. from Aug. 15-22, 1999
Results and Interpretation:
The data set is presented in colour contour format on plans at 1:2500 scale and discussed as follows: Readings were taken at 12.5 meter intervals.
The most obvious feature outlined is a massive high and low combination or di-polar response trending ESE across the north part of the grid. This is interpreted as a concentrated magnetic mineral band, probably magnetite, within a diabase or gabbro intrusion. This feature is linear and might be indicating a lineament or fault. The values on the low side range down to 56,360 nT while the high side range is as high as 58,291 nT.Further to the north and again in the diabase are a few isolated highs and lows that can be again attributed to pockets of magnetite concentrations. Co-incidently there is a drop in topography where the magnetic low trend occurs and a definite east-west lineament flanks the low to the north.
The area around the north part of the pond contains a few isolated highs on L 550 W at 475 N and on L 300 W at 300 N. Also the area between these two highs is elevated in magnetism. A similar situation occurs between L 210 W at 450 N and O at 600 N. These highs suggest the magnetic mineral content of the diabase varies in a massive fashion.
The central part of the grid is fairly uniform with a few outliers of a few hundred gammas.
At the south end of the grid a linear magnetic high runs from L 300 W at 162 S to L 200 E at 75 S. One could interpret a narrow (5-10 meter) dike here. The area to the north of this feature has a very irregular magnetic pattern. Within this pattern however are several subtle possibilities of linears and masses.
Meegwich Consultants Inc. Box 482 Temagami. Out. POH 2HO tel. (705)569-2904
8ll'illem Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
VLF SURVEY_____________________________________________
Instrument specifications:
A total of 12.90 km was surveyed (1070 readings) with the same GEM Systems GSM-19 Mag/VLF-EM receiver unit. The transmitting station was Cutler, Maine at 24.0 kHz This instrument measures the in-phase of the vertical magnetic field as a percentage of the horizontal primary field. The resolution is +I- I 07o.
Dates of Survey:
The survey was done by D. Laronde of Meegwich Consultants Inc. on the following dates: August 15-22, 1999. Readings were taken in detail at 12.5 meter stations.
Results and Interpretation:
The interpretation of VLF conductors is based on whether or not the source of the anomaly is metallic.
The survey picked up seven new conductors and some very weak responses. The labeling is a continuation in sequence from a previous survey which used the A-F labels on a detailed grid over the 0,0 showing area. The anomalies from this survey are G-M and are discussed as follows:
Conductor G: This weak anomaly is short along strike, 200 m, with the strongestresponse on L 210 W at 120 S. It trends northwest which is the strike of a local fractureset. The source would appear to be non-metallic.Conductor H: This conductor occurs on a lineament marked by a topographic lowtrending due east. This is a strong indication that this anomaly could have a non-metallicsourceConductor I: Anomaly I occurs within the pond and seems to be indicating a nearhorizontal conductive layer such as the sediment in the lake bottom and/or the trend issimilar to H and it could be a continuation. In any regard the source is likely non-metallic.The I.P. survey has confirmed there is no metallic anomaly here so the source is definitelynon-metallic.Conductor J, K and L: These anomalies are in the pond area as well and are not welldefined due to the closeness. Although the location is suspicious for having a non-metallicsource, it cannot be determined from VLF. The I.P. survey did not detect an anomalyover this area.Conductor M: C onductor M is a strong response that runs along a topographic low It has been field checked with a beep mat survey along its length and no mineral wasdetected.
Meegwich Consultants Inc. Box 482 Temagami, Out. POH 2HO tel. (705)569-2904
\VilleniWassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
INDUCED POLARIZATION SURVEY
Instrument Specifications and Survey Configuration:
A total of 2.425 km was surveyed with a di-pole di-pole, 3=25 meters configuration. N 1- 6 was read to better the chances of detecting small pockets of mineralization associated with Zone 2 containing a 59 g/tonne assay. The depth penetration is down to 225 feet or 68 meters. The survey employed the following state-of-the-art equipment:
-an IP T-3 Phoenix Transmitter 3.0 kW-an IP V-5 Receiver (Phase)-a MG-1 Phoenix Generator 2.0 kW
Dates of the survey:
The survey was done by Remy Belanger Geophysique of Rouyn-Noranda, P.Q.. There were seven crew members from the Belanger team and D. Laronde supervised and selected lines based on results at the end of each line. Crew members were Remy Belanger, Carl Belanger, Jean Yves Robin, Mario Robin, Jean-Marc Raymond, Steve Lacourse and Mike Kirovac.
Results and Interpretation:
The system is designed to respond to conductive horizons such as inter-connected metallic grains and also metallic grains that are not connected electrically. The latter is the great advantage over conventional EM systems. The results incorporate a resistivity profile that is compared in contrast to the phase profile. Anomalies with a drop in resistivity and an increase in phase are considered priority. There were four profiles or lines done and are discussed individually as follows:
L 550 W
Objective: This line was to test a series of three VLF-EM conductors occurring in or near an east-west trending structure that is thought to be a possible controlling factor in the deposition of a gold deposit. The 59 g/tonne Au assay is on trend.
Results: At 650 N there is a drop in resistivity accompanied by a wide phase anomaly. The peculiar thing about this anomaly is that the phase zone is much wider than the
Meegvvich Consultants Inc. Box 482 Temagami, Ont. POH 2HO tel. (705)569-2904
Willeni Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
resistivity low. The underlying rock is probably diabase or gabbro. Surface prospecting has uncovered some chalcopyrite which may be in this particular feature. The anomaly is probably caused by mineralization which should be followed up. This is a low prioritydrill target.
L 300 W;
Objective: This line crosses over the area of the 59 g/tonne Au assay. The purpose was to define a drill target over this zone. Since disseminated pyrite is a common accessory mineral.
Results: The zone does have a co-incident response centered at 325 N. There is a slight elevation in the phase and also the resistivity. This is not what was expected however it is a response that is over the projected zone. H igh priority drill target.
The north end of the line centered on 675 N is a wide chargeability zone with a wide high resistivity zone which is typical of the underlying diabase or gabbro. This anomaly is a priority target.
L 50 W
Objective: To test the area of base metal mineralized showings on surface for continuity along strike and at depth.
Results: There is a shallow, N^l,2, phase anomaly from 200 S to 100 S. The corresponding resistivity low is in the order of 500 to 1000 ohms/meters. This location is co-incident with the end of a VLF-EM anomaly. There is some correlation to a magnetic high here. Another anomaly, only narrow, occurs at 25 S. This is co-incident with the strike of the mineralized showings. The resistivity response is shallow. These two drill targets are high priority.
LO
Objective: To test the area of base metal mineralized showings on surface for continuity along strike and at depth.
Results: There are two strong increases in phase accompanied by a low in resistivity centered on 150 S and at 25 N. These are encouraging since there are surface showings around 0,0 grid co-ordinates. These are h igh priority drill targets.An increase in phase occurs at 150 N but is accompanied by a resistivity high as well Low priority anomaly.
Meegwich Consultants Inc. Box 482 Temagami. Ont. POH 2HO tel. (705)569-2904
nH'/Hern Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
Conclusions and Recommendations:^^———^^^^———^—^——^^^^—-^^-^^
Zone 2 (beaver pond area and north half of grid):
The magnetic survey and VLF-EM survey from the OPAP phase of work did not define any massive sulphide bodies. Most of the conductors seem to have non-metallic sources. All the conductors were followed up with I.P. and beep mat prospecting with disappointing results. The surveys over the beaver pond gold zone 2 have faint indications of corresponding responses that are quite marginal at best, nevertheless present in magnetics, VLF-EM and I.P. . Because of the high assay it would still be advisable to at least x-ray drill ( small core, portable drill) for geologic information. The gold zone may be very narrow but high grade enough to be economical.
Zone l
The IP survey lit up four targets to drill on a high priority basis This is encouraging The IP. anomalies flank existing VLF-EM conductor zones with widths up to 15 meters One l.P. response on L 50 W at 150 S may be as wide as 50 meters. Some of the assays from previous work are Cu 4070 ppm, Au, 3.98 g/tonne, Ag 18 g/tonne, Pb 1190 ppm, Zn 8790 ppm, Co 1460 ppm.
There has been enough surface work done geologically and geophysically with the end result of 5 locations to drill test. The holes need only be 300-400 feet deep amounting to a total of 1500-2000 feet. This could be done for about SIS/foot on present prices for a grand total of 522,500-530,000. It is advisable to approach mining development corporations at this time since to finance the drill project.
End
Meegvvich Consultants Inc. Box 482 Temagami, Ont. POH 2HO tel. (705)569-2904
INSTRUMENT SPECIFICATIONS
MAGNETOMETResolution:
Ace u ra c/:
Range:
Gradient Tolerance:
Operating interval:
Input/Output:
Power Requirements:
Power Source:
Battery Charger:
Operating Ranges:
Storage Temperature:
Display:
Dimensions:
ER 7 GRADIOMETER0.01 nT (gamma), magnetic field and gradient.
0.2 nT over operating range.
20,000 to 1 20,000 nT.
Over 10,000 nT/m
3 seconds minimum, faster optional. Readings initiated from keyboard,
external trigger, or carriage return via RS-232-C.
6 pin weatherproof connector, RS-232C, and (optional) analog output.
12 V, 200 mA peak (during polarization), 30 mA standby. 300mA peak
in gradiometer mode.
Internal 12 V, 2.6 Ah sealed lead-acid battery standard, others op
tional. An External 12V power source can also be used.
Input: 1 10 VAC, 60 Hz. Optional 110/220 VAC, 50/60 Hz.
Output: dual level charging.
Temperature: -40 "C to +60 "C
Battery Voltage: 1 0.0 V minimum to 15V maximum.
Humidity: u p to 90"Jo relative, non condensing.-500CtoH-650C
LCD: 240 x 64 pixels, or 8 x 30 characters. Built in heater for opera
tion below -200C
Console: 2 23 x 69 x 240mm.
Sensor staff: 4 x 450mm sections.
Sensor: 170 x 71 m m dia.
Weight: Console 2.1kg, Staff 0.9kg, Sensors 1.1 kg each.
VLFFrequency Range: Parameters Measured:
Resolution: Number of Stations: Storage:
Terrain Slope Range: Sensor Dimensions: Sensor Weight:
15 -30.0kHz.Vertical In-phase and Out-of-phase components as percentage of totalfield.2 componenis of horizontal field.Absolute amplitude of total field.Q.1%.Up to 3 at a time.Automatic with: time, coordinates, magnetic field/gradient, slope, EMfield, frequency, in- and out-of-phase vertical, and both horizontalcomponents for each selected station.O0 - 900 (entered manually).14x15x9 cm. (5.5 x 6 x 3 inches).1.0 kg (2.2 Ib). ________________
Systems lin .
13ll'illem ll'assenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
CERTIFICATE OF AUTHOR
. David Laronde of the town of Temagami, Ontario hereby certify':
1. That I am a geology engineering technologist and have been engaged in mineral
exploration for the past 20 years.
2. That I am a graduate of Cambrian College in Sudbury
with a diploma in Geology Engineering Technology 1979
3. That my knowledge of the property described herein
was acquired by field work and documentation.
Dated at Temagami this 12th day of January 2000.
Dand Laronde
Meegwich Consultants Inc. Box 482 Temagami. Ont. POH 2HO tel. (705)569-2904
14WilleinWassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
References
1978 Bennett. G. Geologic Report - Geology of Northeast Temagami Area Ontario Geologic Survey
Meegwich Consultants Inc. Box 482 Temagami, Out. POH 2HO tel. (705)569-2904
ll'illem H'assenaar OPAP Final Submission Wassenaar Properly Strathcona T\\p.
APPENDIX l
Geologic Report
A.W. Beecham
Meegwich Consultants Inc. Box 482 Temagami. Out. POH 2HO tel. (705)569-2904
It'i/leni Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.
APPENDIX II
Assay Certifcate
Meegwich Consultants Inc. Box 482 Temagami. Ont. POH 2HO tel. (705)569-2904
F. JBB XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order: 056245 Date: 1 7/08/99 FINAL Pigc l of J
Mrfcod. Det-Lon-Unit*.
O1-99 •Dup l 99
AuFA301
1PI*
PiFAJOt
10PI*
PdFA301
1PI*
ft*. •H:ICF70
O.Sppol
NaICF70
0.01*
MlICP70
001*
AJ1CP70
0.01"V
P1CP70
0.01*
K1CT70
0.01*
CaICF70
0.01n
StICF70
O.Sppm
TlICT7*
0.01f
VICT70
1PPtn
Oricrro
ippm
Mnicrn
2ppm
FeICT70
0.01*
4648
1412
n15
•COS 0.040.04
0.660.69
0.860.91
•CO.Ol•COOI
001001
0.22024
2.5 2.8
0.04005
3637
5455
579603
17.8 IS.7
XRALO
XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order: 056245 Date: 1 7/08/99 FINAL Page 2 of 3
O
^
o o
Mdhut DeUUm. UnM*
CoICPTO
1ppm
r*ICPT*
1ppm
diICPTO
0-5ppm
ZaICPTO
O.Sppm
AsICT70
3ppm
STICPTO
•Jppm
YICFTi
OSPP"
ZrICPTO
0-Sppm
MBicrw
ippm
*fICT7D
0.2ppm
CtICPTO
1Ppm
SkICPTO
10ppm
SbICPTu
Sppm
' B*
ICPT*1
ppm
LaICPTO
0.5ppm
WICPTO
10ppm
199 •Dup l 99
553 748772
297308
67.5710
o 1920
4.7 5.1
•CO.S•COS
5.558
12 l!
2430
8.57.2
XRALK}O
XRAL LaboratoriesA Division of SOS Canada Inc.
Work Order: 056245 Dale: 1 7/08/99 FINAL Pjgr 3 of 3
Ekmtrt. Q Mrtbod
Dints.
Pta Bt ACICPTO ICT7O AA73
2 5 03ppm ppm
l 99•Dup 1-99
118122
2724 4 4
invoice/Facture No.: 081:031658
XRAL XRAL LaboratoriesA Division of SQS Canada inc.
INVOICE
Invoice To/Facture A:W. Wassenaar MD Attn: Willem Wassennar
7 Roxville AvenueTORONTOONTARIO, CANADA M4G 3P7
Submitted By/Soumettez Par:W. Wassenaar MD Attn: Willern Wassannar
7 Roxville AvenueTORONTOONTARIO, CANADA M4G 3P7
Work Order:. Invoice Date: Date Submitted: Shipped Via:
Qnty
1
1
1
1
1
Code
PG205
FA301
ICP70
AA73
GST
056245 Customer No.: 401705 17/08/99 Your P.O. No.: 06/08/99 Your Project No.: SELF Waybill No. :
Description
Drying, Crushing St m illing { hardened st
1AT Au Inst. Fire Assay
ICP, Aqua RegieSilver by AA
T& G ST Rg No. R105082572
# Ele Unit Cost
55.25
3 51 3.30
31 58.15
1 54.75
$2.20
Amt/Montant
$5.25
$13.30
$8.15
$4.75
52.20
PREPAY Advance Payment Received 533.65
TOTAL IN CANADIAN FUNDS l TOTAL EN DOLLARS CANADIEN 533.65
PI**** r*mtt to / S.V.P. *nvoy*f votr* p*J*m*nt i:P.O. Box 9581 Station 'A' Toronto, ON Canada M5W 2K3
PI**.** courier to l S .V.P. *nvoy*r par courl*r *:1885 Leslie StreetDon Mills, ONCanada M3B 3J4Tel: (416)445-5755Fax: 1416)445-4152
Please Quote I nvoice Number l S .V.P. Specifier le numero de facture 081:031658
Note/N.B.: 1 .5** per month interest on Overdue Accounts l I marSt de sur Comptes Arrieras de 1 . S 1* Par Mois: Terms Net 30 days
ORIGINAL INVOICE
Member of the SGS Group (Societ* Generals d* Surveiltanc*)
XRAL XRAL LaboratoriesA Division of SOS Canada Inc.
1 885 Leslie Street Don Mills, Ontario Canada MSB 3J4 Telephone (416) 445-5755 Fax (416) 445-4152 CERTIFICATE OF ANALYSIS
Work Order: 056245To: W. Wassenaar MD
Ann: Wlllem Waasennar
7 Roxville AvenueTORONTOONTARIO, CANADA M4G 3P7
Date 17/08/99
Copy 1 to
Copy 2 to
P.O. No. Project No. No. of Sample* Date Submitted Report Comprise*
1 ROCKS 06/08/99 Cover Sheet plus Pages 1 to 3
Distribution of unused material:Pulps: Discarded After 90 Days Unless Instructed!!!Rejects: Discarded After 90 Days Unless Instructed!!!
Certified By
Dr. Hiifeh de Souza, General Manager XRAL Laboratories
ISO 9002 REGISTERED
Report Footer: L.N.R. - Listed not received l.S. ~ Insufficient Sample n.a. - Not applicable -- - No result •INF - Composition of this sample makes detection impossible by this method M a fter a result denotes ppb to ppm conversion, "ft denotes ppm to "ft conversion
Member of the SOS Group (Sodete Genera* de Survvtlarx*)
. 2 O 5Wassenaar Claims SE. Strathcona Township,, Temagami Area, NE. Ontario
DI H 10Oo -J
MO U1
Geological ObservationsS gIntroduction gp
The Wassenaar claim group is located in southeastern Strathcona and southwestern Riddell townships, some 7 km. (map distance) south of the village of Temagami. Regionally this area is part of the Southern Province of the Canadian Shield. The basement rocks are Archean and consist of complexly folded mafic volcanics intruded by trondhjemite (Na-granite) batholifhs. This is overlain 0 unconformably by the Proterzoic Gowganda Formation sediments. Gently g undulating, gabbro sills, known as Nipissing diabase intrude mainly the Gowganda Formation, but also extend into the Archean basement rocks. In the area of the claims most of the Gowganda Formation has been eroded, but a sill of Nipissing Diabase remains in the northern part of the group.
The following comments are based on only 2 days (14th and 15th Nov. 1999) field work under somewhat adverse weather conditions. The comments are intended to accompany a more comprehensive report rather than as a 'stand-alone report. (No location map, property description or detailed description of previous work is included.) The purpose of the work was to examine the geology and evaluate the mineral occurrences at the following localities: (1) around the SE corner of the Beaver Pond where significant gold values had been obtained under the water line of the pond; (2) outcrop area west of the Beaver Pond; (3) the "quartz pits" along the stream between the Beaver Pond and Upper Twin Lake and (4) quartz veins in the northeast area around Line 100W and SOON.
The author is familiar with the general area from work done around Lowell Lake in late 1970's for St. Joseph Explorations (a subsidiary of the old American mining company St. Joe Minerals previously St. Joe Lead.) and from updating the Mineral Deposits Inventory for the MNDM in 1990-1991.
Description of Work Done
David Laronde of Temagami described the property and provided copies of relevant maps and reports describing previous work, mostly by the present owners. He also guided the author to property.
On the 14th the area around the southeast corner of the Beaver Pond was examined and part of the outcrop mapped. This was a reasonably good day for observation, but there was some snow on the northwest outcrop slope on the large outcrops over-looking the southeast corner of the Beaver Pond and these outcrops
could not be examined properly because of the danger of slipping into the pond. On the second field day, 15th November, a heavy snow squall held up work early in the morning and dropped 2 to 3 cm. of wet snow. The outcrops could not be brushed clear of this snow and the only way to view the surface of the outcrop was to strip off areas of moss. This made for slow progress. However, something was accomplished. On the west side of the Beaver Pond, one cross section was roughly mapped along line 600W. A cursory examination of two quartz veins in Nipissing Diabase were made, one on line 600W, northwest of the Beaver Pond and the other referred to as Showing "D" along the stream, north of the Beaver Pond. A rough cross-section was also mapped east of the Beaver Pond on the return traverse to locate the diabase volcanic contact.
Five chip samples of mineralization and veins were taken. Mapping and observations are shown on the accompanying map at a scale of 1:2500. The legend has been expanded to allow for other rock types in case more mapping is done.
The data provided by D. Laronde were reviewed and summaries of the more significant assays from work by the claim owners were added to the 1:2500 scale map. No review of data in the MNDM assessment files was made.
General Geology
A major contact striking about grid EW passes through the south part of the Beaver Pond. South of this contact the rocks are mainly fine grained pillowed and flow structured to massive mafic volcanics. North of the line, the area is underlain by a coarse to medium coarse grained gabbro. This gabbro has the textures of the Nipissing Diabase sills seen elsewhere in the Temagami and Cobalt areas and it is recognized as a Nipissing Diabase sill by Bennett. Towards the south, this gabbro seems lighter- coloured and contains areas of varied textured to pegmatite-like material. Northward it seems a little darker and generally finer grained. i.e. The diabase seems to be differentiated or layered. On line 100W at about 350N on a west facing scarp face, an Archean assemblage of mafic volcanics and feldspar porphyry intrusive appears to overlie Nipissing diabase. (This observation was made late in the afternoon and it was a bit rushed in order to get out of bush before nightfall.) This observation combined with the previous comment on apparent differentiation of the diabase, suggests that the Nipissing diabase here is a gently south dipping sill and this contact marks the top of the sill.
The pillowed to massive flows exposed south and east of the 'Beaver Pond' are typical Archean mafic volcanics, except that they contain irregular patches and streaks of silicification and some sort of feldspar (probably albite) alteration, and they are relatively hard. The impression was gained that they have been hornfelsed (rock that has been re-crystallized around an intermediate to felsic intrusive.). The hornfelsing would not be due to the Nipissing diabase, but likely the large surrounding trondhjemite batholiths.
Structural Geology
The mafic volcanics, where examined, except for pillows, are fairly massive and no strikes and dips were measured on them. In places the fine grained mafic flows grade into medium to coarse grained (gabbro-like) rocks. These units usually mark certain individual flows and cores of thick flows and mapping their contacts with the fine grained units usually give strike directions. However, none of these contacts were traced far enough to indicate a strike direction for the flows. Bennett does show the mafic volcanics trending about grid E-W and dipping south.
Three prominent fault and fracture directions are recognized. A nearly N-S set is most conspicuous southeast and east of Beaver Pond. The second, a HO0 trend is marked by the south contact of the Nipissing Diabase and parallel structures within the sill to the north. Although the prominent scarps along this contact seem to be caused by contrast in the weathering resistance of the diabase and altered mafic volcanics, this 110" trend is a regional fracture set and the diabase at this point may be intruding along these pre-existing fractures. A third set is recognized at the quartz vein (showing "D") located between 'Beaver Pond' and Upper Twin Lake. Here a prominent valley sub- parallel to the quartz vein marks a common regional 0700 trend.
Mineralization and Hydrothermal Alteration
Within the area examined, as noted above, there is wide spread, pale brown- grey alteration of the mafic volcanics. This is a combination of silicification and some sort of feldspar alteration (probably albite). This occurs as irregular patches and in pillow selvages along fractures. No particular orientation was noted. Pyrite, as trace amounts up to a few percent, accompanies this alteration . Although some of the alteration follows pillow selvages, this is not a common primary volcanic feature. It is the author's opinion that it is due to a later hydrothermal event. This type of alteration is, typically associated with gold mineralization and one of the two samples, B-3 from near the southeast corner of the Beaver Pond, does carry anomalous gold levels (74 ppb Au).
The two showings examined in the Nipissing Diabase consist of massive white, glassy quartz, with variable amounts of pyrite and chalcopyrite. On the NW showing, a 70 cm. wide quartz vein is accompanied by calcite and there is a wide (alteration) selvage of dark chlorite along the vein and pyrite and chalcopyrite (with malachite) are fairly abundant. This vein strikes NW-SE and dips vertically. A sample of the vein containing pyrite and chalcopyrite, returned a surprising 953 ppb gold. It also contained anomalous levels of both Ag, 5.6 ppm and Co, 95 ppm. This veins does not appear to be related to any prominent nearby structure. The veins at Showing D, (along the stream), on the other hand, occur along a prominent topographic feature which probably marks a major fracture or fault. These veins dip at about 450 and appears to occupy fractures subsidiary to the main structure along the stream valley. A grab sample from showing "D" returned anomalous Co, 102 ppm, but no gold or silver.
Table I List of Samples and AssaysField
#
B-2
B-3
B-4
B-8
B-9
Lab.#
14968
14969
14970
14971
14972
N
190N
314N
340N
642N
770N
Ref. Line
3 50 W
350W
300W
600W
400W
from line
10W
17E
16W
9W
8E
ppb Au
7
74 34
2
953
9383
ppm Ag
n/a
n/a
n/a
5.6
0.1
ppm Co
n/a
n/a
n/a
95
102
Remarks
sil, f.sp.alt'n patches & streaks with minor Py
tt U
check assay of original pulp'flat' fault, with earthy, red hematite, gossan, qv.70cm. glassy, white qv + blebs Py, Cp, mal
check assay of original pulp30-40 cm glassy, white rusty, calcite-qtz vein
n/a = not analyzed
Discussion
Because of the very limited field work, and the poor field conditions, conclusions reached are necessarily tentative. However a few comments can be made.
Quartz and quartz calcite veins in the Nipissing Diabase are fairly common. An example is the Gosselin vein located 11 kilometres to the NNE in Cassels Township. The Gosselin contains sections of heavy chalcopyrite, some cobalt mineralization, low silver values and isolated gold values. In spite of a lot of exploration no ore shoots have been found in the Gosselin vein. North of Lowell Lake, a St. Joseph Explorations, 1978 drill hole intersected significant gold values in quartz carbonate veins in a Nipissing Diabase intrusive (6.5 g/t Au over 30cm . All the mineralization is from a 2.5 cm vein diluted in a 30 cm. sample and one would expect selected grabs from this to be as high as 10 times this assay;). To the east, between Upper Twin Lake and Wagkich Lake, another St. Joseph drill hole intersected some low gold values in mineralized Huronian sediments, (0.85 g/t Au over 0.5 to 1m as well as I can remember). This information is in the assessment files and also in the OGS Mineral Deposit Inventory. The veins on the Wassenaar claims and at Lowell Lake appear to be similar to the Ag-Co arsenide veins in the Cobalt and Silver Centre areas except that silver and cobalt levels are lower, gold levels are higher and the veins are mainly quartz instead of mainly calcite.
The quartz (+S- calcite) veins on the Wassenaar property seem to be fairly strong structures and at least one of them is well mineralized with Py and Cp. The gold values reported at the southeast corner of the Beaver Pond are unusually high. Although there has been no gold production from quartz-carbonate veins in the Nipissing diabase, the possibility of such a deposit cannot be ruled out.
This general area carries mineralization with elevated gold levels, both in the Proterozoic (Huronian sediments and Nipissing Diabase) and in the older Archean rocks. Whether or not the area has potential for economic gold deposits is not known.
The high values reported from veins in the Nipissing Diabase seem encouraging. However, it is important to look at the geometry and grade of these structures to see if there is a chance of economic concentrations. It must be borne in mind that minimum mining width is about 1.5m and that a 30 cm. wide vein would have to grade something like 40 to 60 g/tonne gold to be economically viable and there would have to be sufficient volume to pay for development and plant costs. These diabase hosted quartz veins are not typical gold bearing structures in the Canadian Shield. This could however, be a new type of mineralization, possibly an epithermal type of gold mineralization which is common in the younger fold belts, such as the Cordilleran or Appalachian belts.
The author did not examine the Area 004 mineralization and hence, the following comments are speculative. Most of this mineralization as described by Hart appears to be within or closely associated with interflow sediments or exhalite beds. This mineralization is similar to showings west and southwest of Lowell Lake.. Here sub-economic Cu and Zn occur in pyrrhotite-rich cherty, exhalite beds within mafic flows. This mineralization has been mapped SSW towards Herridge Lake to about Highway 11. From this point a series of airborne EM anomalies (from an unpublished survey by St. Joseph Explorations cl977) extends eastward for about 3.5 km and then through a series of folds into the area just south of the Wassenaar claims. One of these conductors, not far east of Highway 11 was drilled. Sulphides similar to the Lowell Lake showings were intersected and the EM anomalies to the east are thought to mark similar sulphide-rich beds. At Lowell Lake the beds have been fairly extensively sampled and some drilling has been done without locating any economic mineralization. The best values encountered here are 0.65 "/o Cu, and 0.39 % Zn over about 5 m. The pyrrhotite beds at Lowell Lake are very similar both in their make up and in their geological setting to the interflow sediments that commonly form the 'roots' of many silver veins in the Cobalt camp. Here, too a lot of exploration has been done for base metals, but the best concentrations found have grades of only about 2% Zn and 0.5 to 0.75 9o Cu over 3 to 5 m thickness. Even this grade is well below economic levels. The Lowell Lake and Cobalt interflows are similar to the exhalite beds that mark productive horizons in Archean, massive sulphide base metal camps, except that here they occur within mafic volcanics rather than in close association with felsic volcanics as in the productive camps.
Recommendations
More work is warranted on the auriferous quartz veins in the Nipissing Diabase. It is recommended that one or two of the best veins be well exposed and systematically channel sampled to determine grade and continuity of mineralization.
Some re-examination of the showings in Area 004 is recommended. Although the base metal potential is not rated very good, the gold values could be interesting if they are actually in the exhalite where values could have better continuity than in veins.
Airphotographs would help in mapping and particularly in identifying faults and prominent fractures, which may control the quartz veins in the Nipissing Diabase in the north part of the property.
Soil geochemistry could be helpful on this property. Sampling of small areas around and 'down ice' (in the direction of Pleistocene ice movement) from known gold showings could be useful to see if the technique works. The B-2 soil horizon generally provides the best sample medium. The author has had some technical success with soil geochemistry in locating a large low grade gold deposit (as yet sub-economic) in the Tyrrell-Knight area west of Gowganda. The technique should detect major, subcropping gold concentrations.
In summary, although no mineralization typical of known gold ore bodies has been recognized, the unusually high gold values found in some of the quartz veins warrant further exploration. In this case where the geological model is unfamiliar, it is generally best to be guided by metal values.
A.W. Beecham Haileybury, Ontario 2 Dec. 1999
References
Beecham, A.W.April 1978
Bennett, G. 1978
Born, P.1989
Hart, I.R.May 1998
Laronde, D.Aug. 1999
Drill log 189-1, St. Joseph Explorations Ltd. MNDM assessment files;
Geology of the Northeast Temagami Area, Dist, of Nipissing, Rep. 163 and Map 2324, Ont. Geol Survey Geol.;
Precambrian Geology, Cassels and Riddell Townships Report 271 and map 2526, Ont. Geol. Survey
Geological Report, Wassenaar Property NTS 31-L-13, Strathcona Twp.
Wassenaar Property, Strathcona Township, Ontario, Ground Geophysical Surveys, Meegwich Consultants Inc. Map 1:2500;
Appendix
Assay Certificate
Swastika LaboratoriesA Division of Assayera Corporation Ltd.
Established 1928 Assaying - Consulting - Representation
Geochemical Analysis Certificate 9W-3653-RG1Company: A .W. BEECHAM Date: NOV-23-99Project: WassenaarAttn: A.W. Beecham
We hereby certify the following Geochemical Analysis of 5 Grab samples submitted NOV-17-99 by .
Sample Au Au Check Ag Co Number PPB PPB PIM PIM14968""""""""""""""""""""?"""""""-""""""""-""""""-""""""""""""""""
14969 74 3414970 214971 953 938 5.6 9514972 3 - 0.1 102
One assay ton portion used.
Certified by
l Cameron Ave., P.O. Box 10, Swastika, Ontario POK l TO Telephone (705)642-3244 Fax (705)642-3300
andMinesDeclaration of Assessment Work Performed on Mining LandMining Act, Sub**ctlon 65(2) and 66(3), R. S. O. 1990
Transaction Ni,T.t*r (office
UJOO'fOAssessment F iles Pessaran 'r.ag -i g
)l subsections 65(2) and 66(3) of ihe Mining Act. Under sociion 8 of :f a review the assessment work and correspond wiih ihe m n r g lane! hcice' Recorder, Ministry ol Northern Development aid Mines, 5;i Flo;-
31M04SE2007 2.20529 RIDDELL 9QQ 2.2052Instructions: - For work performed on Crown Lands before recording a claim, use form 0240.
- Please type or print in ink.
1. Recorded holder(s) (Attach a list if necessary)o t,
Name . ^ ' ^^^\ ~m j* * ^ "C
to So Address f — s\?tt- 'oft 9 1? S t ^ fc C*J t"SS *- ^ ^ * ^ jrSc*'**- ^ " '
'~*6n J . U . U/* iJ^^^r- (^^ /9 - T20JJ
'~*lT9 ^ ^l^~ (sJ ^sx-^**-r J /9- rZoJ-7/^ ? 6 Tf?^ f _______ -^ —- —————
AOCress "7 /T o X" \ it(e- /O^c-.
"7~oro^7u, 0^^. M ij- G- S ?7
Client Number ,2d^ ^*// ( U/t-lt^
Telephone Number
Fax Numbeff^,cj ^v-- 3y?2-Client Number
Telephone Number
Fax Number
2. Type of work performed: Check (^) and report on only ONE of the following groups for this declaration.Physical: drilling stripping, n RehabilitationGeotechnical: prospecting, surveys,
assays and work under section 18 (regs)n *-* trenching and associated assays D
Work Type /** - f 0
Oates Work From ^ x o— ^^ ^o 3 / S i- ^9Performed Day | Montti | Year Day | Montn | Year
Global Positioning System Data (rf available) Township/Area ^~j-rc,jj, c.e^x? ~7^ .
M or O-Plan Number
Office UseCommodity
Total S Value of Work Claimed /G", ^7C
NTS Reference
Mining D,v,s,on ^d^(l ^ (J
Resident Geologist , 7 District *?(,rlkfansJ ACL^-^
Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.
3. PersonName
Aodress
Name
or companies who prepared the technical report (Attach a list if necessary)
MEEGWICH INC.P.O. BOX 482
POH 2HOAddress
Name
Address
Telephone Number "7 o 5^ -TV? - 2 9o Y
Fax Number
Telephone Number
Fax Number
Telephone Number
Fax Number
4. Certification by Recorded Holder or Agentt do hereby certify that l have personal knowledge of the facts set forth in
(Pnnt Name)
this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, tlje annexed report is true.Signature of Recorded Holder or Agent Date
Agent's Address Telephone Number Fax Number
3211 (03*71 RECtlVbbSEP 15 :::3
GEOSCIENCE ASSESSMENT OfFlCE
5. Work to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to tie mining land where work was performed, at the time work was performed. A map showing the contiguous link must accompany form
Mining Claim Number. Or if work was done on other eligible mining land, show in this
column the location number indicated on the claim map
eg
eg
eg
i,/
i *'•C-'
30.'"
" J1
5 }
6 ^
7 ,)
8 ,J
9 ^
1C
1 1
12
13
14
TB7827
1234567
1234568
/o 7t ?6a/o-?Z 969
/o7t ??Y/(*tl o o 2-f l f f oo Y
f (*i l oo S
X/ f/ *30^
//?/ 0 ^7//f/ o of
15
Column Totals
Number of Claim Units. For other mining land, list hectares.
16 ha
12
2
Xs
/7ff
fyf
/jr
Value of work performed on this claim or other minjng land.
526,825
0
S 8,892
Vo3ff/,t7fZ,?-'?*'
2-,2-Oc
/.rros 7 004 0&
z&r 2*0
/t, *7* -
Value of work applied to this claim.
N/A
324,000
54,000
2., o ^ 02,ooo
Z , OCJe.
2 , ^o "
2 , ** t*o
2. ,oo o
/, ^^o
S, Z&&(,2--7* **
St*7o -
Value of work assigned to other mining claims
524.000
0
0
Z y ^2^
- —
2.7
Zclti
' ——
. —
- —
*/^er —
- —
2.?y2.^
Bank. Value of -vcxk :c De districted ai a future date
S2625
3
S4B9C
OS
)
—— ±i ————
, do hereby certify that the above work credits aie eligible underl.___________________(Pnnt Full Name)
subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the c;aim
where the work was done.
Signature of Recorded Holder oi/"^ ~\
^gentAjJthorized inytfrhidox' Date M/J^, 2.o*o -——————————————————————————— --(^ ~ —— ————— -- ——— — —————— . ——— -y- • ••••-
6. Instruction for cutting back credits that are not approved.
Some of the credits claimed in this declaration may be cut back. Please check fV) in the boxes below to show how you v/ish topnontize the deletion of credits:
® 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated. D 2 Credits are to be cut back starting with the claims listed last, working backwards; or fas 3 Credits are to be cut back equally over all claims listed in this declaration; or D 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):
C? ;P| t^ ^ Q
Note: if you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary.
For Office Use OnlyReceived Stamp
RECEIVEDSEP 1 5 2000
GEOSCIENCE ASSESSMENT OFFICE
Deemed Approved Date
Date Approved
Date Notification S e T.
Total Value of Credi'. Approved
Approved for Recording by Mining Recorder (Signature)
Minislry ofNorthern Developmentand Mines
Statement of Costs for Assessment Credit
Transaction Number (office us*)
Personal information collected on (his form is obtained under the authority of subsection 6(1) ol the Assessment WorK Regulation 6/96. Under section 8 ol the Mining Act, the information is a public record. This information will be used lo review tr-.e assessment work and correspono *nri the mining land holder. Questions about this collection should be directed to the Chief Mining Racordar, Minirtry of Northern Development a 10 Mines. 6th Floor, 933 Ramsey Lake Road, Sudbury, Onlario, P3E 685. rt Ci X* t-v J ,,
4b m 6 \J *J' *~' v
Work TypeUnits of Work
Depending on the type of work, list the number ol hours/days worked, metres ol drilling, kilo metres ol grid line, number of samples, etc.
Cost P er Unit of
Total Cost
A; /y.~U-
I/CF
-J^f
-To'*
. e* fc.~-
Associated Costs (e.g. supplies, mobilization and demobilization).
^ J& rri+.^J'
Transportation Costs
f
Food and Lodging Costs
Total Value of Assessment Work
Calculations of Filing Discounts:
1. Work filed within two years of performance is claimed at IOQ.% of the above Total Value of Assessment Work2. If work is filed after two years and up to five years after performance, it can only be claimed at 5 n(Vo ol the Total
Value of Assessment Work. If this situation applies to your claims, use the calculation below:
TOTAL VALUE OF ASSESSMENT WORK x 0 .50 Total S value of worked claimed.
Note: '- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 4 5 d ays of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.
Certification verifying costs:
l, hereby certify, that the amounts shown are as accurate as may(please print full name)
reasonably be determined and the costs were incurred while conducting assessment work on the lands indicated on
the accompanying Declaration of Work form as
to make this certification.(recorded holdeff agenti or state company posiiton with signing aui
RECEIVEDSEP 151;: J
GEOSCIENCE ASSESSMENT _____OFFICE
am authorized
Signature Dale
Ministry of Ministers duNorthern Development Developpement du Nordand Mines et des Mines Ontario
Geoscience Assessment Office 933 Ramsey Lake Road
January 5, 2001 6th FloorSudbury, Ontario
JOHN LIEUWES WASSENAAR P3E 6B57 ROXVILLE AVENUETORONTO, ONTARIO Telephone: (888) 415-9845M4G-3P7 Fax: (877)670-1555
Visit our website at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm
Dear Sir or Madam: Submission Number: 2 .20529
Status Subject: Transaction Number(s): W0070.00167 Approval After Notice
We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.
If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.
Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.
If you have any questions regarding this correspondence, please contact BRUCE GATES by e-mail at [email protected] or by telephone at (705) 670-5856.
Yours sincerely,
ORIGINAL SIGNED BYLucille JeromeActing Supervisor, Geoscience Assessment OfficeMining Lands Section
Correspondence ID: 15573
Copy for: Assessment Library
Work Report Assessment Results
Submission Number: 2 .20529
Date Correspondence Sent: J anuary 05, 2001 Assessor:BRUCE GATES
First Claim Number1076960
Township(s) l Area(s)STRATHCONA
StatusApproval After Notice
Transaction NumberW0070.00167
Section:14 Geophysical MAG 14 Geophysical VLF 14 Geophysical IP 9 Prospecting PROSP 12 Geological GEOL
The 45 days outlined in the Notice dated November 16, 2000 have passed.
Assessment work credit has been approved as outlined on the attached Distribution of Assessment Work Credit sheet.
Approval Date
December 31, 2000
Correspondence to:Resident Geologist Kirkland Lake, ON
Assessment Files Library Sudbury, ON
Recorded Holder(s) and/or Agent(s):David Laronde TEMAGAMI, ONTARIO
JOHN LIEUWES WASSENAAR TORONTO, ONTARIO
SIEK WASSENAAR STOUFFVILLE, ONTARIO
SYBREN L WASSENAAR TORONTO, ONTARIO
WILLEM WASSENAAR TORONTO, Ontario
Page:1Correspondence ID: 1 5573
Distribution of Assessment Work Credit
The following credit distribution reflects the value of assessment work performed on the mining land(s).
Date: January 05, 2001
Submission Number: 2.20529
Transaction Number: W0070.00167
Claim Number Value Of Work Performed
1076960 3,770.00
1076969 1,678.00
1076974 2,005.00
1191002 2,200.00
1191004 1,480.00
1191005 1,430.00
1191006 600.00
1191007 1,757.00
1191008 200.00
Total: S 1 5,120.00
Page: l
Correspondence ID: 1 5573
31M04SE2007 2.20529 RIDDELL 200
Ministry of Ministry ofNatural Northern DevelopmentResources and Mines
THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED f ROM VARIOUS SOURCES, AND ACCURACY IS HOT GUARANTEED. THOSE WISHMG TO STAKE MININGCLAIMS SHOULD CONSULT WITH THE M IM1NO RECORDER HIMSTRY OF NORTHERN DEVELOPMENT AND MINES. FOR ADDITIONAL INFORMATION OH THE STATUS OF THE LANDS SHOWN HEREOM.
1231127 INDEX TO LAND DISPOSITIONG.H A
TEMAGAMIPU*
G -3450TOWNSHIP SUDBURY
UNC Tflltl; JttBIS ^ MtUOH
NIPISSINGSTRATHCONA
AKA MEMft-M Ait* W fCH
M (WDIFWVTSU iiMj;
12307,31AREAS WITHDRAWN FROM DISPOSTiON
M.R.O. - MINING RK3HTS ONLY S-R.O -SURFACE RIGHTS ONLY M.tS. -MINING AND SURFACE RIGHTS
Boundary
Township, Meridian, Baseline
Rood allowance: surveyed . - .
Psrcel;unmrvaywl
Rlglit of way; roadrailway .
utility
^eaervatkin
g53!i V- ' * 5*-J*t i ,- ™ ' 1""rir '
•' X-'' ) ' • ^.'s- V-i-y ~i 4^29/.^ -y-r
T^tJ^^^^^^Sr ' 'l '^^^J|*37827i f ig ^g^ /J/ ^ s ]2 !9S371- j' si z ifllS^ t ,;J^ 1240260
V, ,: ;V, ..V,',' i'SJJI' 9 tt it (il()
(R;) T— l l *e*DHMBl WNEBH* nurHCIIQNnrltf CKMN.V" f l ' JWWLinu*MVtrrffxuiiitoHXFi*mY
m UTM o*-f IMIMV 'i Htiivu -i.-it marne* t-'i.•Ut. MTOT.
Road; higrnvajr, county, townshipaccess . . . . . - . . . . . . . . . . . .Ifjil.toush---------- ......
ShoreHrn (nrigirul) . . . - - . . .
SKYLINE RESERVE
DISPOSmON OF CROWN LANDSPat*nt
Surface A Wninil Rk|M* Surface N ights Only. Mining Rights Onry.....
LM6*
Surfaca 4 Mining Rights Surface R ights Only
.,v '--' ^ ^K. ,.jL*K- - . ^rf ~ ^- ^-. ' -J Al *a.— - -.- - . j J.l -
MAJOR AMENDMENTS TO NORL STAKWG
L^-:^ "? PLEASE NOT!: THK fSLAMD ON LAKE TWACAMl Nm-O^I" W|TH*'^WN AND Wlil TMMGAMIUOEonx TontDspEcrmc AND STAKING our
In. aru riwwn H SKYLINE HURVE Ma**te hurt cmnd by IM wun ut LAKE TEMAGAMI on rill* BM* will bg jubjrct to OMMM Refulilicw WWIS tradi undar rhc furlic Lnh AM.
on tte type md Tim'*! of yo*r*xplof*icn wwk you may require a Wort Permit. Ft* ftrilivniifbrnutlnripltaie contact Qw**(d Mcytf, RegfonU KMidrac G*otD|ltt it (701) X7.H42 ar
[7Wrl3*n*irr —— ——— —
TOWNSHIP
. *nod"- —"O-, drafcr- j 8i""i i Hid rv-.ipein;
NUpper
\Tw i n
/
\Lake
O C 7
V
C 7 fe 9 7 4
1^19555li
\
tx*o '
GEOLOGICAL LEGEND
PROTEROZOIC
\ l 9 Late diabase dykes (Sudbury Type)
t ' 1 8 Nipissing Diabasel -----J (a) Coarse grained gabbro mcl varied textured typesl l (b) Medium, uniform textured gabbrof "l (f) Dark fine grained, magnetic diabase
ARCHEAN
B Granitic, Plutonic Rocks(a) Trondhjemite(b) Pegmatite
___ 5 Mafic to Intermediate Intrusivesl l (a) Gabbro (b) Diorite
l l 4 Sediments(e) Sulphide rich exhalite, cherty sediment
3 Intermediate to Felsic Subvolcanic Intrusives(a) Quartz feldspar porphyry mtrusives(b) Feldspar porphyry mtrusives
en 2 Felsic Volcanics
1 Mafic Volcanics(a) Massive to foliated(b) Pillowed(d) Medium to coarse grained(c) Flow breccia
ABBREVIATIONS
aftC-9chlCpCIGhemm gmalqcqvPoPysil
SYMBOLS
X : i.
hydfothermatty alteredcoarse grainedchiorite alterationchalcopyriteclaim linegossanhematitemedium grainedmalachitequartz-calcite veinquartz veinpyrrhotitepyritesilicified, silicification
outcrop, area of outcrop
sca r p
geological contact
geological contact showing dip
sctvstosity, foliation
lineation
pillows
fault
low angle or thrust fault
topographic lineament, prominent fracture, fault
silica *Meldspar alteration. +J- pyrite
sample point; Au ppb, Ag ppm. Co ppm,
summary of assays by claim owners
rock pit, trench
earth trench
diamond drill hole
swamp
open, grassy swamp
claim post located
property boundary
all weather road
track, winter road
Note:Picket line locations, claim lines and topography modified after Laronde Aug 1999
31M04SE2007 2 .20529 R IDDELL 210
CV-. ,' 9 o p o DI ppm
l/1/assenaar PropertySE Strathcona Twp
District of Nipissing
GeologyUpper Twin Lake Area
Scale: 1:2500Drawn by. AW Beecham
Date. Nov 1999
Revisions NTS31U13, 31M/4
-v
A
x, O
Claim post, assumed
Claim post, found
Trench
Ledge
Main Showing
Conductor Axis, Defined
Conductor Axis, Interpreted
Conductor Zone
Outcrop
Gra b Sample (Aug 1, 1999 56245)
IP. Anomaly
(high priority drill target)
IP. Anomaly
(low priority drill target)
Area of beep map prospecting
Area prospected by W.Wassenaar
Upper Twin Lake
N-
(Astronomic)
1219555
Hwy.#11 4km
2.2052931M04SE2007 2 .20S29 RIDDBLL 220
Instruments: GEM Systems GSM-19 MAG / VLF Serial #806862
GEM Systems GSM-19 Base Station Serial#58479
GEM Systems GSM-19 Magnetometer Senal #58479
Scintrex EDA Omni IVBase Station Serial#228225
Geonics EM-16 VLF Receiver Serial # 10585
VLF Station: NAA 24.0 kHz Cutler Maine
50
Scale 1:250050 100 150
metre
Wassenaar PropertyStrathcona Township, Ontario
Prospecting and Compilation Map
Data Processing and Interpretation by: Meegwich Consultants Inc.
Scale 1:2500
December 1999
NTS31 L/13&31 M/
31M
04S
S20
07
2.2
05
29
O
r, c?
1191
008
Stra
thco
na T
wp.
Ridd
ell T
wp.
(Astronomic)
Conductor Axis, Defined
Conductor Axis, Interpreted
Profile Scale: 1 cm ^ 2QV,
31M04SS2007 2 .20529 RIDDELL 240
Instruments: GEM Systems GSM-19 MAG / VLF Serial #836862
GEM Syst&ns GSM-19 Base Station Serial #58479
GEM Systems GSM-19 Magnetometer Serial #58479
Sdntrex EDA Omni IV Base Station Serial #228225
Geonics EM-16 VLF Receiver Serial # 10585
VLF Station: NAA 24.0kHz Cutler Maine
50Scale 1:2500
50 100 150
motre
Wassenaar PropertyStrathcona Township, Ontario
Ground Geophysical Surveys
VLF - EM Survey Profiles of the In-Phase and Quadrature
Data Processing and Interpretation by:
Meegwich Consultants Inc.Scale 1:2500
December 1999
NTS 31 U13 A 31 M/'
2.20529
4894.
Rt 3ISTIVITY OHM-METERS
oin(N
g PHASEK M RAO
fNM W
OJ
i T~" 7 i r i 'r i ; i f T ' j j i i i rPOO RQO
_48 9738
K 24 .4894
Lo
l f 50 2+0) 2+50 3+00 N 4400 N 4+y) 5+00 N 6+00 N 6+50 N
Filter 8356 5610 S032 5631 5904
n-2
0=5
3351 3260 1867 3132 12ffi, 2tK 2453 1W 2 564 2ffii Wl 5233
975 1579 \V I6K
8698 4J84 "43 Filter
3868 3495\ / t l \ y J \ l
5910 6S7! 7438 WU ' 5473 l 3682 -^ 21i1 2448 ' 1 807 5478 ' , I 51S ^-i
7091 6116 6211 5B4B ^ 4721 ^ JJM^ 7lSB 1988 ' 2BS7 ' 1 085 1121" \J?S/ 17SC ,Xi 5SJ-^ 2255 \ ~ SQJ 1 S1E - MH " ^ 12K/, S17J 5583 6458
7IB4 4763 72M +411 , 5995 — 672t \ 27IZ
\
\ 1012 1224 \ 23i2 — 4B24 1279 21EJ 1S21'53S9 5141 5B57 5586/1*; \ 5616 — W68 //824' ( 465 ^-. B56 . (" 1907 \ 1457 ff, 1 8K \ li 3867 -, 2622 ""- 15*.! I486
5630' 4207 8231 949B 316J 1W^ ' 11E! ' 583 V 357 - 2213 S l IK ' 4920 JK4 x 1013 "^742 737 - x 5503
5060 896!
514J 7860V
11 = 4
.5+50 N 4 KX) N 4+50 N 5+00 N 5+50 N 6+00 N 6 + 50 N
Filter
11=6
5 f.E 92 l? 17 21
,1 1.3 _ 1 1.8 j i, 11 \ 23 v 4418 H , , 7J 81
~"\ f ' ( '\22 19 t 1 0 V s.B l\ l x\-J yx ^v ) \ x \ x^^— li C L-T ) n \ \ 2 6 '"-. 36 K^^^J ) V . "N,
\ \ M 43 41
4? 44 4H
14 /VV 1.6 -' 1.5 1.5 2.4 A '- 91 S ,
Filter
v..'' y?j ' M' 25 "29 36
RESISTIVITY OHM-METERS
PHASEM RA D
Line 550 WDipole-Dipole Array
no
Filter
o ^ 25.0 M
© . plot point
Logarithmic Contours 1, 1.5, 2, 3, 5, 7,5, 10,...
INTERPRETATION
Strong increase in polarization accompanied by marked decrease in resistivity.
Well defined increase in polarization without marked resistivity decrease.
Poorly defined polarization increase with no resistivity signature.
Low resistivity feature.
Scale 1:2500O 26 50 75 100 125
(metreiQ]
g . 2 052^?^ ^f ^j*^"*^^^^"W.WASSENAAR
INDUCED POLARIZATION SURVEYWASSENAAR PROPERTY
STRATHCONA TOWNSHIP , ONTARIO
BELANGER (GEDPt-frSICW- COfWVCICR)
PBOI ?K
8274.
oj
RESISTIVITYOHM-METEKS
PHASEMRAD
MOO ^
1d .
0.
Filter
n^l i
11=2
n^3
11=4
11 = 5
n=6
Filter
1^=1 t
r^2
11=3
n-4
n=5
11=6
s'\
"^-^
y,
x19K
2
' f
13
i i i i . . i i i
\_____
—— ^^\
Ot-50 N 1+00 N 1+5C
UK IOK 35T3 (Ml 6055
8795 12K IOK —i. 85J6 MO
1 672? x "86 UK ) 6715 5822\\ \ \ l X f
UK \\M9Q \ 12K B50B 673?
IlKX. 7495 ^ 9250 9576 l IWiC\\ \ r") x 7 v-17K \ 6100 \ 1 0K 7 3821\s \ y/ ,--
I4K N- ~ 7184 ~~ t.51'1 -~ M40
0+50 H 1 +00 N 1+5C19 20 20 22 21
16 -^ n 2 4 yj* J4 i
M 19 25 26 Z4
19 l') 7 24 21 ?2r ^^
23 20 - —— 20 l/ ^ — 15 l ^,.'-
2S 1 15 15 11
20 15 12 H
. iniiiiiiinnii
. , 1 1 , , 1 1 , , , , , 1 , 1 , r , . , . , , , , . . , , , , , , , , , ,
~"^ ——— ^^^^ ^"^——— —— ^^ /^
V
N 2+00 N 2fWN 3+00 fJ 3+50 N 4+00 H 4+50 N 5+00 N 5+50 N 6+00 N
5053 3Blb 5414 3608 2706 1134 2763 2170 1013 890 613 656 B42 872 1175 1582 16BJ 2Mlf. V92
7220 2550 . 7119 x 16E? 1226 x 5ZB8 — 46.12 1901 , 1121 U2S , , 40B , 295 M * 264 m , 537 ^ —— 895 13S4 v x !OK/SI i \ \ . N\X^ X X/ JV /. \ ^ ^- —— N \ r-} l /'^^—, \ rv \V\\\\^ 2170 6803 6.MI x 16M — 1576 ^ 3155 i254 x J 466 9?? 791 \ J27 W 5 99 \ 173 l f /, I Bt7 \ 1 ) \ -^ \ m
1B2!T 7 4591 ^ 5JOJ &I67 ''^1737 1559 \ Ji90 ' 1JJ6 1044 7 5BO 595 "~~~ i!3 716 7 BJ " ' 308 7 l' '?5ffl ^ 1446 - 1404 -- 2544 s^^ s " \ \\ i v—-' /v r — /' f — , ^ — . y ^^s ' V ^ — - \ V^\N V, 560e 4CM 4514 5571 ^ 1545 , 76T3 1817 955 x 637 7 J90 \ (900 ^"682 x 412 /^, 9 ?B ^1 1510 ^- 2202 Z3B4 1106 x 277
•^ '^^ \ ^^ ^ ' \ f f 1 1 r^N l I ///^ ——— N ^ \ \ \ ^ 44JO 311? iE90 J938 "" 5108 2367 1401 1J88 1 7Qi f 431 V 60S , ( I1IJ 1 432 -S 1 084 ' ?917 \ 1364 \ 29dli 1649 N 1161~X l' \ \ \ / M V— \ s— i " //s,// / \ \ \ ^ \
4127 3025 1175 3486 8048 x 1185 111J 1082 ' 54J 725 781 715 - 1219 ^ mi 2 715 1672 2378 IMS 110
it
1 4 1 1 4 1 h 1 1 1 1 1 i i- 1 1
1N 2tOO N 2+M N 3+00 N i+50 N 4+00 N 4+50 N 5+00 N 5+M N ^ 6(00 N
17 15 16 14 13 13 15 12 10 5.2 5.2 41 * 4ft 5; 74 10 1- 15 27
22 ^ 11 , IS i 7.2 —— 8.6 16 - 13 , 16 - 11 ID , , 3 3 , , 1.1 12 1.4 11 1.1 - S.I .'1 -, 46f/ ( \ ^ \ s f //f- t l /~'-——- ) ' v/'-"/ f \ xf l 1 1 15 15 10 ——— - 10 14 "-^ li ( 12 10 7 4.7 l ' 1.1 -' , 2 I.B ,' 1 1 1.1 ^',- 9.5 - lb ' 1'2 \. Je7 \ ^, /- \ y ( -, \^--" x. \ tf/^ -' -
14 12 x 16 IB 'V II 12 V IB 16 10 7.8 46 ^ 2,4 ; ^ IS 11 /;^, U ^-- If 16 .. 17 \
^ — \ x, v-... -^ \ ^, \ i A J s ssS -'' ' ) ' ' 17 \ ir \ is is x 11 it M iz ) g.fi B.J V j-.. ? c i9 12 - y ^ r' ia ,.' n X ;.j) -- . \ r~ ,.^r^x ^ * v-~ :^-- ^ 'i ^ '^ - ' l-
17 17 "~-- 15 * 70 20 \ 9.8' 57 ^^- 11 ^ j; 9 .7 8.9 , 7? 6.7 "'"-. 2.9 ^ i 1 j //^. 19 - —— 20 -~ ~ IS /' 1.5 /' 19 '~\ \ \ u ,'" N.X ^ f — x\ •^zystf//' \ i~~ . 1 7 '" 2I 16 JO ' 18 X ' 4.2 J9 ~"-- L '., !1 ~' 6.2 ' 9 .9 78 ' .3.6 ^ ? 1 K ?: 14 ' 13 1'
*i
III 111 II II II 11 111 III Hill Illl '
' ' ^ ' ' ' '^ \
. ^ — —
6+50 M 7+00 N
5659 7M8 7910 6697 79
5Z&5 . 9964 7159 — 776J 611 xv \
~ 7265 ^ Vm 9000 9018
9544 6597 UK 5070,\ -^ V 's 85J? 8302 IOK
\.\, \N 2Sll' \ flT^ 7SJCx\\\o
} J21.5 ^ 99W
i
E. 1 10 M 7+00 N
29 ,M i? 1? 29
ii 4.i 37 39 . 2;
.W 31* 2* ~" ~ 32
4; 36 31 \ ?5
•a w u' 20 " . J' 30
'.: J !
POO 37
.19
,0
3 Filter
S 11 = 1
0 = 2
11 = 3
0 = 4
r^5
0 = 6
filter
n^l
0 = 2
r^i
n-4
ii-S
n-^ 1:
ROD ^K
1'
.6274
l
Lo
RESISTIVITYOHM-METERS
P H AS LM RAf.i
Line 300 WOipole-Oipole Array
a ru.i o
rOH rHg^, Filter 11 11
* * t \ S
o - "'5,0 Mx /
plot point
Logarithmic , 1 , , 5 ? Contours '' ' ' Ol ^ 0 | O l X A I U —
INTERPRETATION
M Strong increase in polarization accompanied by m arked decrease in resistivity,
Q Well defined increase in polarization without marked resistivity decrease.
D Poorly defined polarization increase with no resistivity signature.
T Low resistivity feature.
Scale 1:250025 0 25 50 75 100 126
(metres)
W.WASSENAAR
INDUCED POLARIZATION SURVEY WASSENAAR PROPERTY
STRATHCONA TOWNSHIP , ONTARjQ
Dote: W /:?/]?, inteipic'tolion: [D CHARM' (CLOLOCO) PHOL'NIX VX. RX
REMY BELANGER (GEDPhffSIG^L OWRACIVR)Software fur /he forth Sciences ) 5
31M04SE2007 2.20529 RIDDELL 260
31M04SE2007
2.20529
RIDDELL
270
li
O
LO
o to-H K
oo
o
o
fi II
II li
t
S!
t
t?
CTi
PO
fe
i
CTV
en
uLi
v
s X ;-
x 2
\ fcs
N^
it
\ \
B
\ K
\
x \
S
'! K g
^\
St
\
\ 11
\s
i
-
\ \ \ // \\
M n
U:
-:.n
00 (J1
oo
g
o
T)
Vitf;
RTRE OEN
00 00 m z
. w"
IT,
^,
a 8
D
f D
LT.
~
-i 0
S o
Bg
.0 —
—
.
n
g-0
'ft
! Q
ir,
en - —
, ^.NJ
ro
b
uo
CD
'-
S o
J-
ci
O 00
aHK
in o
H tn *p oH
ROO POCr- r? 7 r. T -r
.'938 J l y
OJ Oj
RESISTIVITY OHI/-METER3
PHASE
M RAO
POO ROO
ll
.19 L2938
L
LO Lo
Filter
2 f (fi S 1+50 S HOP S 0+50 S^
676 724 S&3 I2C8 1401 1204 1*1
Of 00 Q+50 H____ l f (xj M 1+60 N 2+00 N_____ g 150 N_____|
13-76 2+75 2791 3+50 3M8 J593 4S8 5341 51)68 5087 48I + 4759 5291 Filter
i982 - 118? -— 897
0 = 2 1IM ; 413 ~—- 587 7 TT^O- '
n-3 Mi 7134 -^-., 573IK n i0=4 Ml N.—— 174
(1=6
474^^-924 v fil ? v 1626 xx 405 ^-' 90J^ 1584 ^ 3S35 3E2S HIS 5862
940 ^ T77J i VA X 666^—- 451 ' /'S\ V \ 7 ///., ^
... . ... , , ..., -— — 2749 1579 2B34 3647 +COS 7g1l \\ \ I II/' 11 i l /' \ '~J \ \ "^ \ 7
2273 N 1521 ^ ( tBTj^, 942 5063 , 5401 2461 2126 I2E2 4S62 . M52 TO* TOS l SW1 y
6C4\ X I2?7 v 20IM j 10Q8 1559 — 1/64 5SS7 ^823 "2958^ 2476 i 1050 W06 4630 ^ 624J ^ 474S -^ 740J
109i 795 16+4 ~" |j45"'--' IfiSO 2752 J087 4865 5364 34IZ 3452
4MB 302? 3596 3123 2747 ZSJl~——-- vi ^ /^^-, \ J t
3DM 3500 \, 6571 6105 -^ 3979 +917 2W4 6515
4702 42W~" 4+94 9320
2-KX) S
Filter 21
11=1
HW S 0+50 S 0+50 N I+OO N 1 + 50 2+00 N 7+50 N
3C W .51 21 50 M
v - (?4 N 37 40 - ?2 ?1
35 H 13 ^-.. J2: 31 2f' ?7 19
34 ^29 L'6 24 '"'. IB
n=5
l l j14 7 54 55
52 J5
^ \ 21 ' K ( 3 3 +S W'
UN 17 17 \ 44 43 . i5 7 X 10
\ \ l \4fi 52 \ 15 ,' 2 7 . ) 9 . ^
'- 35 \
7 V '' \ J M " '^--S2H /' 14 11 —— 15 \ 24 - 20
?4 25
31 — 28
23 21 Filter
20 16 n =]t
^j i ^
U n -- j
RESISTIVITY OHM-METERS
PHASEMRAD
Line 000 W011 x 'l*-- Dipole Act a
na
Filter
a = 2 5.0 M
Logarithmic Contours
plot point
l, 1.5. 2, 3, b, 7.5, 10,..
INTERPRETATION
Strong increase in polarization accompanied by marked decrease in resistivity.
Well defined increase in polarization without marked resistivity decrease.
D Poorly defined polarization increase with no resistivity signature.
Low resistivity feature.
Scale 1:250025 50 75 100 12525___O
(met res')
W.WASSENAAR
INDUCED POLARIZATION SURVEYWASSENAAR PROPERTY
STRATHCONA TOWNSHIP , ONTARIO
rvite: 99/12/24 Interpretation: ED CHARTRE (CtiOLOGISl) PHOENIX V--5 RX
BELANGER (GEDPW3&L COWWC1VR)