LOGISTICAL A INTERPRETIVE REPORT ON SPECTRAL -IP AND RESISTIVITY SURVEY CONDUCTED ON THE GLENWATER PROPERTY, THE HORNE PROPERTY AND THE BATEMAN LAKE PROPERTY CONMEE AND HORNE TOWNSHIPS THUNDER BAY AREA ONTARIO FOR AVALON VENTURES LIMITED 52A12SE0007 2.17459 HORNE 010
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LOGISTICAL A INTERPRETIVE REPORT
ON
SPECTRAL -IP AND RESISTIVITY SURVEY
CONDUCTED ON
THE GLENWATER PROPERTY, THE HORNE PROPERTY AND THE BATEMAN LAKE PROPERTY
CONMEE AND HORNE TOWNSHIPS
THUNDER BAY AREA
ONTARIOFOR
AVALON VENTURES LIMITED
52A12SE0007 2.17459 HORNE 010
LOGISTICAL AND INTERPRETIVE REPORT
ON
SPECTRAL-IP AND RESISTIVITY SURVEY
CONDUCTED ON
THE GLENWATER PROPERTY, THE HORNE PROPERTY
AND THE BATEMAN LAKE PROPERTY
CONMEE AND HORNE TOWNSHIPS
THUNDER BAY AREA
ONTARIO
For:AVALON VENTURES LIMITED777 Red River Road, Thunder Bay, Ontario Tel: (807)767-3012 Attention: Doug Parker
By: JVX LIMITED60 West Wilmot Street, Unit #22Richmond Hill, OntarioL4B 1M6Tel: (905)731-0972Fax: (905)731-9312
4. DATA PROCESSING...........................................................-.-......................^
5. INTERPRETATION AND DISCUSSIONS OF RESULTS ..............................5
5.1 THE GLENWATER PROPERTY...............................................................-........-.......................^
5.2 THE HORNE TOWNSHIP PROPERTY .......................................................................................8
5.3 THE BATEMAN LAKE PROPERTY .........................................................................................85.3.1 The Resistivity Data...........................................................-.......-.....-.....-.-...-.....--...--..-95.3.2 The IP-Chargeability Data..................................................................................................95.3.3 Selection of IP-Targets..........................................................................................................10
6. RECOMMENDATIONS AND CONCLUDING REMARKS ........................12
52A12SE0007 2.17459 HORNE 0 10C
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LIST OF FIGURES
Figure l : Location MapFigure 2: Grid/Claim Map - Glenwater - HorneFigure 3: Grid/Claim Map - Bateman Lake
LIST OF TABLES
Table l: Specifications for the IP/Resistivity SurveyTable 2: Line Summary for IP/ Resistivity Survey for the Glenwater PropertyTable 3: Line Summary for IP/ Resistivity Survey for the Horne Township PropertyTable 4 Line Summary for IP/ Resistivity Survey for the Bateman Lake Property
Plate la: Resistivity 0=2) Contour Map; Scale l :5000Plate l b: Chargeability (M7, n=2) Contour Map; Scale l :5000Plate CM-1: Compilation Map; Scale l :5000
Included in the Glenwater Grid are the standard pseudosection plots for the IP- lines: 3600E, 3800E, 4000E, 4200E, 4400E, 4600E, 5000E, 5400E, 5800E, 6200E, 6600E, 6800E. These plots include the four parameters: Chargeability, Resistivity, Spectral-M, and TAU (the Time Constant).
FOR THE HORNE TOWNSHIP PROPERTY:
Plate 2a: Resistivity 0=2) Contour Map; Scale l :5000Plate 2b: Chargeability (M7,11=2) Contour Map; Scale l :5000Plate CM-2: Compilation Map; Scale l :5000
Included in the Horne Grid are the standard pseudosection plots for the IP-lines: 6300E, 6700E, 71 GOE, 7500E, 7900E.
FOR THE BATEMAN LAKE PROPERTY:
Plate 3a: Resistivity 0=2) Contour Map; Scale l :5000Plate 3b: Chargeability (M7,11=2) Contour Map; Scale l :5000Plate CM-3: Compilation Map; Scale l :5000
Included in theBateman Lake Grid are the standard pseudosection plots for the IP-lines:8500E, 8600E, 8700E, 8800E, 8900E, 9000E, 91 GOE, 9200E, 9300E, 9400E, 9500E, 9600E, 9700E, 9800E, 9900E, 10000E, 10100E, 10200E, 10300E, 10400E, 10500E, 10600E, 10700E, 10800E.
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1. INTRODUCTION
JVX Ltd. conducted a time-domain Spectral Induced Polarization (IP) and Resistivity survey during the period of December 5, 1996 through February l, 1997 on behalf of Avalon Ventures Limited. The survey was located in three separate areas: (i) the Glenwater Property grid in Horne Twp. (NTS: 52A/12 ), (ii) the Horne Township Property grid (NTS: 52A/12) and (iii) the Bateman Lake Property grid in the Conmee and Horne Twps. (NTS: 52A/12). These grids are all located in the Thunder Bay Area of Ontario.
These locations are shown in the Location Map in Figure l, and the survey grids are shown in Figure 2 Se FigureS.
The Grids covered the following claims:The Glenwater Property: 1224680, 1224681, 1224683,1215010 The Horne Township Property: 1215011, 1215012
The Bateman Lake Property: 1224923, 1224922, 1224924, 1173947, 1224908, 1224907
The purpose of this survey was to locate zones of disseminated sulphide mineralization associated with gold-bearing quartz veins which may be present in the three selected areas of interest. The sulphide targets could be hosted in a series of Archean mafic flows as well as intrusives, with interbedded metasediments. Previous IP surveys in the region suggested the presence of some north-east trending zones of anomalous chargeability which cross-cut the local stratigraphy.
2. SURVEY SPECIFICATIONS & PRODUCTION SUMMARY :
IP f Resistivity ' ••"-'- '--" -' , '. ' " : ' Vi; ;v ;V\", , - ,:i
Transmitter
Receiver
Array Type
Transmit Cycle Time
Receive Cycle Time
| Number of Potential Electrode Pairs
Electrode Spacing
Scintrex IPC7/2.5 kW, Huntec 2.5 kW
ScintrexIPR-12
Pole-Dipole (some Dipole-Dipole)
2 sec
2 sec
6
25 metres
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LOCATION MAPAVALON VENTURES LTD.
HORNE GLENWATER - BATEMAN LAKE PROPERTIESHorne SL Conmee Twps., Thunder Bay area, NW Ontario
N.T.S. 52 A/12GROUND GEOPHYSICAL SURVEY
Scale: l : 1,725,000Survey by JVX Ltd. Feb., 1997 Figure l
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1 121 5011 (HORNE GRID-J. -----. J
GRID l CLAIM MAPAVALON VENTURES LTD.
HORNE GLENWATER PROPERTYHorne Twp., Thunder Bay area, NW Ontario
N.T.S. 52 A/12GROUND GEOPHYSICAL SURVEY
Scale: l : 40,000Survey by JVX Ltd. Feb.. 1997 Figure 2
BL 10000 N
LJ-LLJ-IJ-J-U 9050 N
HORNE TWP.ADRIAN TWP.
GRID l CLAIM MAPAVALON VENTURES LTD.
BATEMAN LAKE PROPERTYHorne Se Conmee Twps., Thunder Bay area, NW Ontario
N.T.S. 52 A/12GROUND GEOPHYSICAL SURVEY
Scale: l : 40,000Survey by JVX Ltd. Feb., 1997 Figure 3
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The production summary are listed in the following tables:
THE GLENWATER PROPERTY
Table 2: Line Summary for IP/Resistivity SurveyT.ine
Chris Hale (Geophysicist and Party Chief)Mr. Hale was in charge of the whole survey, and was responsible for data quality andpreliminary processing of IP data in the field.
Alex Jelenic (Geophysical Operator) Mr. Jelenic operated the IPR-12 receiver.
Gord Hume (Geophysical Operator) Mr. Hume operated the IP transmitter.
Two field assistants were also engaged by JVX : Gerald Chaput and Adam Dixon.
(B) Bateman Grid -
Fred Moher (Geophysicist and Party Chief)Mr. Moher operated the IPR-12 receiver, and was responsible for the overall dataquality of the survey.
Jean-Guy Harvey (Geophysicist Operator)Mr. Harvey operated the transmitter in this survey.
Mr. Michel Daizle and Mr. Vitali Dorodnov were field Operators. In addition two other field Assistants (Gary and Tyier) engaged by JVX, assisted in with the survey.
At JVX' head office in Richmond Hill, Ontario, the following personnel were involved in this project:
Dagmar Piska (Draftsperson):Ms. Piska carried out the manual and AC AD drafting on the figures/plates andassembled this report.
Vaso Lvmberis (Draftsperson):Ms. Lymberis carried out the manual and ACAD drafting on the figures/plates.
Irina Dorodnova (Data Processing Specialist):Ms. Dorodnova processed and plotted the data and was responsible for data storage.
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Andrew G. Hwang (Geophysicist):Mr. Hwang interpreted the survey results and wrote this report.
Blaine Webster (President. JVX Ltd.):Mr. Webster provided overall supervision of the survey.
4. DATA PROCESSING
The IP and Resistivity field data were edited and processed via industry-standard GeoSoft programmes to produce the standard pseudo-sections of the Resistivity, Chargeability (M7), Spectral-M (sometimes denoted as M-EP), and TAU (decay time-constant). These four parameters were plotted together in a standard format, for each of the lines surveyed, hi the few instances where the Spectral-M and TAU values were not computed by the EPR-12 Receiver unit itself, JVX' proprietary in-house software was utilized to complement this shortfall by finding (via a least-squares criterion) an appropriate 'best- fit' decay curve (from a large set of 'master curves' database) from which the Spectral-M and time-constant values were derived.
Next, the colour-contoured maps for the depth-level, n=2, of the Chargeability as well as the Resistivity for each of the three grids were produced, to provide a preliminary view of the distributions of these quantities in plan view. The level n=2 was a usual and standard choice (although other depth-level(s) could have been selected for contouring as well).
Finally, stacked pseudo-sections were assembled and plotted in one map, for each grid, using a universal colouring scheme, for each of the two IP-quantities (Chargeability and Resistivity). Note that the colouring scheme used in the standard pseudo-sections may differ from those of the stacked pseudo-sections because the former was applied on a line- by-line basis, to emphasize the relative contrast of the DP parameters along a given line.
5. INTERPRETATION AND DISCUSSIONS OF RESULTS
For each of the three survey areas, the EP-Chargeability and Resistivity anomalies were manually selected and prioritized by studying the standard colour pseudosections (of the Chargeability, Resistivity, Spectral-MIP and the Time Constant, TAU) for each of the lines surveyed. The locations and extents of these anomalies were compiled on the three Compilation Maps, labelled Plates CM-1 (for Glenwater Property), CM-2 (for Horne Property) and CM-3 (for Bateman Lake Property).
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5.1 THE GLENWATER PROPERTY
Plate CM-1 shows the Compilation map for the Glenwater Property. In the western region of this grid, three near-surface features representing areas having a relatively conductive overburden layer (CO-1, CO-2 and CO-3) were identified; these could have the negative effect of masking out the IP responses that may occur below the overburden layer. Thus, caution need be exercised in the interpretation of the IP data within these three shaded areas.
Striking approximately east-west across the grid, and running deeper, are two distinctly separated resistivity-low zones, RL-1 and RL-2, as interpreted from the resistivity data. Part of RL-1 are found to be in coincidence with the important chargeability zone, IP-1 (to be discussed later). A few other resistivity-low zones have been identified (see Plate CM-1); these are of smaller extent and probably of lesser significance.
A number of interesting IP-anomalous features and zones have been identified within this grid, even though the inter-line spacings were larger than usual (eg. some with up to 400 m line-spacings). As such, the correctness of the interpolation in the areas in between adjacent lines may be somewhat uncertain. Nonetheless, the following prioritized anomalous IP-chargeability regions were listed and described in the following:
Zone IP-1 : This is probably the most important chargeability-high zone in the grid (see Plate CM-1). It trends east-west from Lines 3600E to 4600E, beyond which and further to the east of Line 4600E, it extends approximately N-E, reaching at least Line 6200E, and possibly extending further eastward, till Line 6600E. Four important large Spectral- M targets (T-1 through T-4) are identified and selected within this zone:
Target T-1 is ranked low in priority. It was found to coincide with the resistivity-low zone, RL-1. It has a Spectral-M value of 209 mV/V, with a relatively long time constant (had the TAU value been short, T-1 could have been moved up in priority).
Target T-2 is ranked medium priority, requiring further detailed investigation in this locale. Its M-IP value is 238 mV/V, with a short to medium time constant (indicative of the possible presence of small to moderate grain-size mineralization). It coincides well with RL-1, hence the relative importance of this target.
Target T-3 is also ranked medium in priority (even though its location was found to be not fully coincident with RL-1), since its Spectral-M value (359 mV/V) is amongst the highest in the this grid. Its time constant is short to medium. In fact, T-3 is seen to correlate more closely with a local resistive-high layer (at n^), indicative of possible silicification process.
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Targets T-4 and T-5 are both ranked low in priority, even though their M-EP values are comparable to the previous targets. This is due to the lack of correlation with any one of the larger resistive/conductive zones at these positions. (Note, however, that T-4 correlates with a local resistive-low, whereas T-5 is located near a local resistive-high (silicification)).
Overall, it is important to state that Targets T-1 through T-5 are all reasonably well cross- correlated from Line 4600E through to Line 5800E, giving confidence to validity of the field results as well as to the interpolation/interpretation approach adopted here. Still, one would strongly recommend that the missing lines (eg. Lines 4800E, 5200E, 5600E and 6000E) be similarly surveyed in the near future, to property complete the IP picture, if at all possible.
Zone IP-2: Running roughly adjacent to and located just north of zone IP-1, lies the second anomalous chargeability zone, IP-2. This is rated as next in importance, after zone IP-1. There is no apparent correlation with either a resistive-low or -high zone in this case. Three target locations (T-6, T-7 and T-8) have been identified:
T-6: This is rated as medium priority target, having an M-IP value of 352 mV/V, with some correlation with a local resistive-low (at n=3) in the area. Its time-constant is of long duration, indicative of possibly coarser-grained mineralization.
T-7: This target area is rated as low priority since its M-IP value is quite small, at 143 mV/V. There is some evidence of the presence of a local resistive-low zone at depth ^5), and thus, this target may be of some interest.
T-8: This is also rated as low priority; its M-IP value is 254 mV/V, and the target correlates with a local resistive-high area as well. Its TAU value is of short to medium duration, possibly indicative of fine-grain mineralization.
Numerous other IP zones have been delineated and outlined (see Plate CM-1). Of note was Target T-9; this is located within the chargeability zone, IP-6. This target is rated as medium priority, with a relatively sizable Spectral-MIP value of 359 mV/V. Also, the target coincides with the second resistive-low zone, RL-2, at about the same level (n= l). Finally, Target T-10, of medium priority, was found where zone IP-1 meets RL-2 on Line 6600E. Its M-EP value is 246 mV/V, with a relatively long time-constant.
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Overall, the Glenwater Property has some well defined and interesting IP anomalies. The delineation and interpolation of the IP results in the areas located in between the lines surveyed can be improved upon by utilizing smaller line-spacings (eg. 200 m instead of 400 m), wherever possible. To balance this, one should also note that the maximum Spectral-M values detected in the area was about 350 mV/V, perhaps not sufficiently high enough to warrant a more detailed survey campaign, provided other geological and/or geophysical information were available to take into consideration. Notwithstanding, perhaps a limited geochemistry sampling survey could be recommended to be conducted over some of the near surface IP target areas identified above.
5.2 THE HORNE TOWNSHIP PROPERTY
The IP and Resistivity anomalies for the Home Township Property were compiled and plotted in the Compilation map labelled Plate CM-2. Again, the line-spacing for this grid was larger than usual, at 400 m; thus the following interpolation and interpretation could be problematic, and caution in this respect is advised.
Several resistive-low zones were identified (the shaded areas in Plate CM-2). As well, five IP zones were delineated (TP-1 through IP-5), these were generally found not to coincide with the resistive-lows. Three possible targets (T-1, T-2 and T-3) were selected; these were deemed of low priority. Their Spectral-M values range from 221 to 254 mV/V, with TAU of short to medium duration. It is recommended that Lines 6500E, 6900E, 7300E and 7700E be surveyed first before a more detailed and reliable interpretive work can proceed beyond this preliminary stage.
Relatively speaking, at the present time, the Home Township Property is ranked of lesser importance than the Glenwater Property, as far as the IP-responses are concerned.
5.3 THE BATEMAN LAKE PROPERTY
The IP-survey over the Bateman Lake Property grid, in comparison with the previous two grids, shows significantly better probability of finding possible economic mineralization. A number of promising anomalous-chargeability zones have been identified (TP-1 through IP-10, cf. Plate CM-3), and more than a dozen prioritized targets have been selected (T-1 through T-16) and recommended for further follow-up studies. Detailed discussions of these IP zones and targets shall be discussed in this section.
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5.3.1 The Resistivity Data
From the resistivity results, the areas showing resistivity-highs are labelled (eg. H, VH, WH, etc.) along each of the survey lines. No apparent overall resistive trends are readily observed from the compilation map (see Plate CM-3). Thus, only localized association of a resistive-high with each of the target areas will be discussed, if and when such a concurrence existed.
ha contrast, numerous resistivity-low zones (RL-1 through RL-13) have been delineated; some of these have partial correlation with the various identified IP-anomalous zones. Owing to the selected line-spacing of only 100 m over the entire grid, the interpolation here (for both the RL- and IP-zones) should be quite acceptable. As an overview, it was noted that the grid could be divided into two distinct regions: an area to the north of the grid, and an area to the south, separated by a central zone (which roughly range from Station Nos. 10000N to 10400N) where no apparent resistivity-lows are observed. In contrast, both the northern and southern regions have numerous zones of resistivity-lows, mostly trending approximately east-west, with a few trending north-east as well (cf. Plate CM-3).
In the northern region of the grid, a large resistivity-low zone, RL-1, striking roughly east- west, as well as north-easterly in the mid-region, was identified as one of the prominent geoelectric features in the area. It extended from Lines 9400E to 10700E, and was observed to be partially correlated with the chargeable zones IP-6, IP-7 and IP-8. Additionally, four important target areas (T-12, T-13, T-14 and T-15) were located within RL-1. These targets shall be discussed subsequently in more detail. A second, but less extensive resistive-low zone is RL-2; this is located near the south-east corner of the grid, from Lines 10400E to 10700E. Two important targets (T-4 and T-5) are positioned within RL-2, which correlate well with the chargeability zone, IP-3.
Numerous other resistivity-low zones have been identified, with quite good line-to-line correlation in their resistivity values (eg. RL-4, RL-5, RL-6, RL-7, RL-8 and RL-9). However, these generally do not appear to follow closely the various defined IP zones. Also, there are several occurrences where the resistivity-lows are apparently very localized (across 1-2 lines only); these probably have little geologic significance.
5.3.2 The IP-Chargeability Data
In this grid, at least ten anomalous IP-zones have been delineated from the chargebility data. Some of these are relatively extensive in strike-length, albeit somewhat narrow in width ^ 100 m ); a number of these notable anomalies can become wider at depth (cf. the colour-plotted standard pseudo-sections attached). The zones trend generally east- west, with occasional ones striking north-east (eg. IP-1 and DP-4).
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In the soth-west comer of the grid, a long, anomalous-chargeability region was identified and labelled as DM; it extends from Lines 8500E to 9800E, striking roughly in the north easterly direction (Plate CM-3). This is an IP-zone of moderate priority; it encompasses four target locations (T-7 though T-10), whose details are discussed in the next sub section 5.3.3. To the east of IP-1, three other chargeable zones have been identified: IP- 2, IP-3 and IP-10. IP-2 has two important targets, T-1 and T-2; and this zone is ranked high in priority. Adjacent to and just north of IP-2 is zone IP-3; wherein three target- areas (T3, T-4 and T-5) are located. IP-3 is ranked medium priority. Just north of IP-3 is the small, localized zone, labelled IP-10; this is associated with a medium-priority target, T-6. Finally, in the southern-half of this grid, to the north and west of IP-1, two other chargeable areas have been identified: EP-4 and IP-5; the latter has a target, T-11, contained therein. These zones are ranked low and medium priority respectively.
In the northern-half of the grid, at least four anomalous-chargeability zones have been identified (IP-6, IP-7, IP-8 and D?-9). IP-6 is ranked high priority, since it contains three important targets, T-12, T-13 and T-14. IP-7 and IP-8 each has one target (T-15 and T- 16 respectively), both zones are ranked medium priority. Finally, the last chargeable zone is IP-9, located to the northern edge of the grid. It is ranked low in priority, and even though no target has been selected, this zone appears to correlate well with the resistivity-low zone, RL-10.
5.3.3 Selection of IP-Targets
In this important grid, as many as 16 IP-Targets have been selected and prioritized. These were recommended for detailed follow-up studies in the near term. The particulars of each of these targets are listed and described in the following:
Targets T-1 and T-2: Both of these are ranked high priority; they are encompassed within the chargeable zone, IP-2. Their Spectral-M values are just over 540 mV/V, amongst the largest in the grid (indeed, the highest M-D? values of all three grids). Their decay time-constants (TAU) are short to medium in duration, suggestive of the possible presence of fine-grain mineralization. There is apparently some association with nearby resistivity-highs, indicative of possible silicification/alteration process in this vicinity. Further, T-1 and T-2 are positioned right next to each other (on the two adjacent Lines 9900E and 10000E, close to Station No.~9200N); this correlation would tend to suggest that these two target areas should be ranked somewhat higher in priority than the other high priority targets. Adjacent and to the north of T-1 and T-2, the standard pseudo- section plots of Lines 9900E and 10000E show possible shear zones, indicative of geologic alterations, eg. hydrothermal processes which may be relevant to fine-grain sulphide and possibly gold formation (it would be even more desirable if the Spectral-M values were found to exceed, say 800 mV/V — which could improve the odds, considerably).
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Targets T-3, T-4 and T-5: these three targets are located in EP-3, and are ranked medium priority. Their Spectral-M values are in the range of 350-420 mV/V; with relatively long time-constants, suggestive of coarser-grained mineralization in these target areas. T-3 appears to be associated with local resistivity-high, whereas T-4 and T-5 are more closely related to resistivity-lows (RL-2).
Target T-6 : this is ranked of medium priority, and is located within IP-10. Its M-DP value is 370 mV/V, with a long time-constant. Deeper (^6) and just north of T-6, a localized resistivity-low is observed.
Targets T-7. T-8, T-9 and T-10 : these four targets are located in the IP-1 zone. Interestingly, not one of them are seen to associate with the resistivity-low zone, RL-7. These targets are ranked of low priority (compared to the other targets in this region), despite their moderate M-D? values of 268-358 mV/V. They are found to mostly associate with resistive zones, apart from T-8 and T-9. All have long time-constants, except T-8.
Target T-ll: this is ranked medium priority; it is situated in a resistive zone (silification), within the IP-5 zone. Its M-D? value is a respectable 390 mV/V, but it has a long time-constant.
Targets T-12, T-13 and T-14 : these three important targets are located within the IP-6 anomalous zone. T-12 is rated high priority; its Spectral-M value is quite large, at 488 mV/V. Additionally, it has a short time-constant ^0.1 sec), suggestive of fine-grained mineralization. To its southern flank, the presence of a shear zone is suggested based on a study of the standard pseudo-section plot for Line 9400E. This would imply the presence of some geologic alteration in the vicinity. Along the line, to the south, a moderately resistive zone is observed, indicative of possible silicification process. Hence the importance of this target area. T-13 and T-14 are both rated of medium priority; their M-IP values range from —450-466 mV/V, with short to long time-constants. Owing to the lack of evidence for the presence of moderately high resistivity values in the vicinity of these targets (they apparently coincide more closely with resistivity-lows defined by the RL-1 zone), they are rated medium instead of high priority.
Target T-15 : this is rated medium in priority. It is located within the IP-7 zone, roughly correlating with the resistivity-low section of RL-1. Its Spectral-M is high, at 536 mV/V; but its time-constant is of long duration.
Target T-16 is also rated of medium priority. It is located within the EP-8 anomalous zone. Its Spectral-M value is a respectable 439 mV/V, with an associated long time- constant. Since there is no resistive anomaly seen in this locale, silicification may be less prominent, hence the rating assigned to this target.
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As a final comment, one should note that the IP and Resistivity responses of the Bateman Lake Property area show rather complex distributions of the Chargeability- and Resistivity-anomalous zones. Additionally, one should note that there are numerous other instances wherein locations having rather high posted M-IP values may not be included within any IP-zone, nor have they been selected as targets. In such cases, the corresponding pseudo-sections themselves should be studied to appreciate the implied reasonings behind their de-selection (eg. the IP-anomalies may be too localized and limited in extent, to be of interest).
6. RECOMMENDATIONS AND CONCLUDING REMARKS
Of the three grids in this IP/Resistivity Survey, the Bateman Lake Property Grid shows the most promise in the search of possible economic mineralization. Over a dozen targets have been selected for follow-up work in this area; many of their Spectral-M values are in excess of 450 mV/V, with short to medium time-constants (probably relating to the presence of fine-grained mineralization), and often with closely associated resistivity- highs which could be indicative of possible silicification process. Many of these targets are ranked medium to high priority, and strongly recommended for more detailed studies in the near term. To further prioritize these IP targets and zones, a geochemistry sampling program is recommended. The sampling should be taken 'down-ice', along the defined IP trends/zones. In areas of deep overburden (eg. n=2 or deeper), enzyme leach techniques may be employed.
Next, the Glenwater Property Grid is ranked second in importance, as far as the IP/Resistivity responses are concerned. About half a dozen targets had been selected here, mostly of low to medium priority, the maximum Spectral-M values being below 360 mV/V in this area.
Finally, the Horne Township Property apparently show less significant IP-responses, and is ranked last in importance.
However, one should be aware that both the Glenwater Property and the Horne Township Property were surveyed with the larger line-spacings of 200-400 m, hence the above overall conclusions about these two properties should be regarded as somewhat preliminary, ie., more definitive conclusions could only be drawn if and when the EP/Resistivity data were acquired at the standard 100 m line-spacings, as per the Bateman Lake Property.
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If there are questions with regard to the survey or its interpretation, kindly contact the undersigned.
Respectfully submitted,
JVX LIMITED
rT Andrew G. Hwang, Ph.D Geophysicist
Mr. Slaine Webster, B.Sc. President
[cc7CW7a:glenwtr.rep]
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APPENDIX A
i IPR-12 Time Domain Induced Polarization/Resistivity Receiver
l Brief Description
l l l l l l l l l l l l l l l
The IPR-12 Time Domain IP/Resistivity Receiver is principally used in exploration for precious and base metal mineral deposits. In addition, it is used in geoelec- trical surveying for groundwater or geothermal resources, often to great depths. For these latter targets, the induced polarization measurements may be as useful as the high accuracy resistivi ty results since it often happens that geo logical materials have IP contrasts when resistivity differences are absent.
Due to its integrated, lightweight, micropro cessor based design and its large, 16 line display screen, the IPR-12 is a remarkably powerful, yet easy to use instrument. A wide variety of alphanumeric and graphical information can be viewed by the operator during and after the taking of readings. Signals from up to eight potential dipoles can be measured simultaneously and recorded in solid-state memory along with automatically calculated parameters. Later, data can be output to a printer or a PC (direct or via modem) tor processing into profiles and maps.
The IPR-12 is compatible with Scintrex IPC and TSQ Transmitters, or others which output square waves with equal on and off periods and polarity changes each half cycle. The IPR-12 measures the pri mary voltage (Vp), self potential (SP) and time domain induced polarization (Mi) characteristics of the received waveform. Resistivity, statistical and Cole-Cole parameters are calculated and recorded in memory with the measured data and time.
Scintrex has been active in induced polar ization research, development, manufac turing, consulting and surveying for over thirty years. We offer a full range of instru mentation, accessories and training.
The IPR-12 Receiver measures spectral IP signals from eight dipoles simultaneously then records measured and calculated parameters in memory.
Benefits
Speed U p Surveys
The IPR-12 saves you time and money incarrying out field surveys. Its capacity to measure up to eight dipoles simultaneous ly is far more efficient than older receivers measuring a single dipole. This advantage is particularly valuable in drillhole logging where electrode movement time is mini mal.
The built-in, solid-state memory records all information associated with a reading, dis pensing with the need for any hand written notes. PC compatibility means rapid elec tronic transfer of data from the receiver to a computer for rapid data processing.
Taking a reading is simple and fast. Only a few keystrokes are virtually needed
since the IPR-12 features automatic circuit resistance checks, SP buckout and gain setting.
High Quality Data
One of the most important features of the IPR-12 in permitting high quality data to be acquired, is the large display screen which allows the operator easy real time access to graphic and alphanumeric displays of instrument status and measured data. The IPR-12 ensures that the operator obtains accurate data from field work.
The number and relative widths of the IP decay curve windows have been carefully chosen to yield the transient information required for proper interpretation of spec tral IP data. Timings are selectable to per mit a very wide range of responses to be measured.
Specifications
Inputs1 to 8 dipoles are measured simultaneously.
Input Impedance16 Megohms
SP Bucking 10 volt range. Automatic linear correction operating on a cycle by cycle basis.
Input Voltage (Vp) Range50 uvoltto 14 volt
Chargeability (M) RangeO to SOOmillivolt
Tau Range1 millisecond to 1000 seconds
Reading Resolution of Vp, SP and MVp, 10 microvolt; SP, 1 millivolt; M, 0.01 millivolt/volt
Absolute Accuracy of Vp, SP and MBetter than 1 "/o
Common Mode RejectionAt input more than 100db
Vp Integration Time1007o to 8007o of the current on time.
IP Transient Program Total measuring time keyboard selectable at 1, 2, 4, 8, 16 or 32 seconds. Normally 14 windows except that the first four are not measured on the 1 second timing, the first three are not measured on the 2 sec ond timing and the first is not measured on the 4 second timing. (See diagram on page 2.) An additional transient slice of minimum 10 ms width, and 10ms steps, with delay of at least 40 ms is keyboard selectable.
Transmitter TimingEqual on and off times with polarity change each half cycle. On/off times of 1, 2, 4, 8, 16 or 32 seconds. Timing accuracy of 100 ppm or better is required.
External Circuit TestAll dipoles are measured individually in sequence, using a 10 Hz square wave. The range is O to 2 Mohm with O.lkohm resolution. Circuit resistances are dis played and recorded.
SynchronizationSelf synchronization on the signal received at a keyboard selectable dipole. Limited to avoid mistriggering.
FilteringRF filter, 10 Hz 6 pole low pass filter, sta tistical noise spike removal.
Internal Test Generator1200 mV of SP; 807 mV of Vp and 30.28 mV/V of M.
Analog MeterFor monitoring input signals; switchable to any dipole via keyboard.
Keyboard17 key keypad with direct one key access to the most frequently used functions.
Display16 lines by 42 characters, 128 x 256 dots, Backlit Liquid Crystal Display. Displays instrument status and data during and after reading. Alphanumeric and graphic dis plays.
Display HeaterAvailable for below -15"C operation.
Memory CapacityStores approximately 400 dipoles of infor mation when 8 dipoles are measured simultaneously.
Real Time ClockData is recorded with year, month, day, hour, minute and second.
Digital Data OutputFormatted serial data output for printer and PC etc. Data output in 7 or 8 bit ASCII, one start, one stop bit, no parity format. Baud rate is keyboard selectable for stan dard rates between 300 baud and 51.6 kBaud. Selectable carriage return delay to accommodate slow peripherals. Hand shaking is done by X-on/X-off.
Standard Rechargeable BatteriesEight rechargeable Ni-Cad D cells. Supplied with a charger, suitable for 110/230V, 50 to 60 Hz, 10W. More than 20 hours service at -i-25'C, more than 8 hours at -30'C.
Ancillary Rechargeable BatteriesAn additional eight rechargeable Ni-Cad D cells may be installed in the console along with the Standard Rechargeable Batteries. Used to power the Display Heater or as back up power. Supplied with a second charger. More than 6 hours service at-30'C.
Use of Non-Rechargeable BatteriesCan be powered by D size Alkaline batter ies, but rechargeable batteries are recom mended for longer life and lower cost over time.
Operating Temperature Range-30'C to 4-50'C
Storage Temperature Range-30'C to -t-50'C
DimensionsConsole: 355 x 270 x 165 mm Charger: 1 20 x 95 x 55mm
WeightsConsole: 5 .8 kgStandard or Ancillary RechargeableBatteries: 1 .3 kgCharger: 1 .1 kg
Transmitters availableIPC-9 200 W TSQ-2E 750 W TSQ-3 3 kW TSQ-4 10kW
where /-'a r apparent resitivity (ohra.m)n = dipole number (dimensionless)a ^ dipole spacing (m)Vp - primary voltage (mV)I - p rimary current (raA)
Pole-Dipole Array Array Geometry and Formula for Apparent Resistivity
l l l l l l l l l l l l l l l l l l l
and Commutated DC Resistivity Transmitter System
DANGER HIGH VOLTAGE
Function
The IPC-7/2.5 kW is a medium power transmitter system designed (or time do main induced polarization or commutated DC resistivity work. It is the standard power transmitting system used on most surveys under a wide variety of geophysical, topographical and climatic conditions.
The system consists of three modules: A Transmitter Console containing a transformer and electronics, a Motor Generator and a Dummy Load mounted in the Transmitter Console cover. The purpose of the Dummy Load is to accept the Motor Generator output during those parts of the cycle when current is not transmitted into Ihe ground, in order to improve power out put and prolong engine life.
The favourable power-weight ratio and com pact design of this system make it portable and highly versatile for use with a wide variety of electrode arrays.
Features
Maximum motor generator output, 2.5 kW; maximum power output, 1.85 kW; maximum current output, 10 amperes; maximum voltage output, 1210 volts DC.
Removable circuit boards.for ease i n servic ing.
Automatic on-off and polarity cycling with selectable cycling rates so that the op timum pulse time (frequency) can be selected for each survey.
The overload protection circuit protects the instrument from damage in case of an overload or short in the current dipole cir cuit.
The open loop circuit protects workers by automatically cutting off the high voltage in case of a break in the current dipole circuit.
Both the primary and secondary of the transformer are switch selectable for power matching to the ground load. This ensures maximum power efficiency.
The built-in ohmmeter is used for checking the external circuit resistance to ensure that the current dipole circuit is grounded properly before the high voltage is turned on. This is a safety feature and also allows the operator to select the proper output voltage required to give an adequate current for a proper signal at the receiver.
The programmer is crystal controlled for the very high stability required for broadband (spectral) induced polarization measurements using the Scintrex IPR-11 Broadband Time Domain Receiver
Technical Description of IPC-7/2.5 kW Transmitter System
Complete 2.5kW induced polarization system including motor-generator, reels with wire, tool kit, porous pots, simulator circuit, copper sulphate. IPR-8 receiver, dummy load, transmitter, electrodes and c lips.
IPC-7/2.SKW transmitter console with lid and dummy load.
T T
T T T T
Time Domain Waveform
Transmitter Console
Maximum Output Power
Output Current
Output Voltage
Automatic Cycle Timing
Automatic Polarity Change
Pulse Durations
1.85 kW maximum, defined as VI when cur rent is on, into a resistive load
10 amperes maximum
Switch selectable up to 1210 volts DC
T:T:T:T; on:off:on:off
Each 2T
Standard: T = 2 ,4 or 8 seconds, switchselectableOptional: T - 1,2,4 or 8 seconds, switchselectableOptional: T = 8 ,16,32 or 64 seconds, switchselectable
Voltage Meter
Current Meter
Period Time Stability
Operating Temperature Range
Overload Protection
Open Loop Protection
Undervoltage Protection
Dimensions
Weight
Shipping Weight
1500 volts full scale logarithmic
Standard: 10.0 A full scale logarithmic Optional: 0.3, 1.0, 3.0 or 10.0 A full scale linear, switch selectable
Crystal controlled to better than .01 "/o
-30"Cto + 55-C
Automatic shut-off at output current above10.0 A
Automatic shut-off at current below 100 mA
Automatic shut-off at output voltage less than 95 V
280 mm x 460 mm x 310 mm
30kg
41 kg includes reusable wooden crate
Motor Generator
Maximum Output Power
Output Voltage
Output Frequency
Motor
Weight
Shipping Weight
2.5 kVA, single phase
110V AC
400 Hz
4 stroke, 8 HP Briggs A Stratton
59kg
90 kg includes reusable wooden crate
222Snidercroft Road Concord O ntario Canada L4K 1 B5
Telephone: (416) 669-2280 Cable: Geoscint Toronto Telex: 06-964570
Geophysical and Geochemical Instrumentation and Services
HUNTEC
MA IP TRANSMITTER SYSTEM
MODEL 2500
OPERATOR'S MANUAL
l
WARNING
THE CURRENTS AND VOLTAGES PRODUCED BY THIS INSTRUMENT SYSTEM ARE DANGEROUS TO LIFE AND CAUTION SHOULD BE EXERCISED DURING USE.
31 OJO 7.0 0.10 0.10 2 1.00 0.102 0.10 7.6 0.10 0.10 0.10 UO 0.10 OJO 31 0.10
0.10 f"""") "' * W0 Wfl al0 Oil0
fc20——0.10 OJO 0.10 0.10 0.10 0.10
MO 0.10 0.10 0.10 0.10 0.10 0.10 0.10 0.10 MO MO 0.10 0.10 MO MO 0.10 0.10 OJO 0.10 OJO OJO MO MO OJO OJO 0.10 MO MO 0.10 0.10 MO MO MO 0.18 0.10 OJO OJO OJO MO MO OJO OJO 0.10 0.10 MO 16
MO OJO OJO OJO MO MO MO OJO MO MO OJO OJO MO MO OJO MO 0.10 MO MO MO OJO MO MO 0.10 0.10 MO OJO OJO MO MO MO OJO OJO 2 OJO OJO MO MOj^JJO 7J 3.9 0.10 OJO OJO
-3.9 3J OJO OJO 0.10 MO OJO 0.10 OJO MO OJO OJO MO OJO MO 0.10 OJO MO OJO MO 0.10 MO OJO OJO OJO OJO 0.10 OJO OJO OJO MO MO 10 5 OJO (jT} OJO *1^|^3^!' -x *M (^T^J^^ M" U'
OJO ^""iT^ MO MO MO MO MO OJO MO MO MO OJO OJO MO OJO OJO OJO OJO MO OJO OJO MO MO MO 0.10 MO MO OJO OJO MO MO UO OJO MO 1J OJO —
010 .W——010 7J OJO 0.10 OJO 0.10 0.10 M, M, MO OJO OJO MO OJO OJO 0.10 MO MD OJO MO MO MO OJO OJO MO OJO OJO OJO OJO U 3.9 0.10 2.5 O
OJO
Ul U. L. U. U. 0.10 0.1, 0.10 OJO OJO OJO MO MO 0.10 0.10 OJO 0.10 MO MO MO MO OJO OJO OJO 0.10 OJO OJO MO MO 110 MO MO 0.10 OJO OJO —— u
110+50 N 111+OON 111+50 N 112+00 N 112+50 N 113+00 N 113+50N 119+50N 120+00 N 120+50 N 121+00N 121+50 N 12atOON 122+SON 123+OON 123+50N 124+OON 124+5QN 125+OON 125+50 N 126+00 N
1J\2J U -^U) U U 1.6 U /U ^iy ^.74 -0.17 ^ U \3jJ UU Vj*^ 8 ) ** 9M ^
OJO ^2 7 3.0 /M/ U U U U ZJV^JI OJ2 -0.06 \ 2J U/ 1?\ 18^2/0.47^ O*,.7 v u) i (3j^w \i_u u u/ v //**/^ i " MI ^"-" j v®)/ ^ /-\ o- y) /^——* \— 1 .9 2J U' U 2-^^2J-X 4jOO /2J' 1.1——'B ^ OJ4 OJ7 2J 2.6——^^1.8 2.2 2.1 1J
U —— 1.1 —- OJ2 -OJO 0.080 OJO OJO -OJ4 OJ4 OJO OJ2
109+00 N 109+50 N 110+00 N 110+50 N 111+00 N 111+50 N 112+01
87 67 -—— 87 s 36 29 v ^ 67
109+00 N
I P -
109+50 N
IP-l
M "t
l112+50 N 113+00 N 113+50 N 114+00 N 114460 N 115+00 N 115+50 N 118+00 N 116+50 N 117+00 N 117+50 N 118+00 N 118+50 N 119+00 N 119+50 N 120+00 N 120+50 N 121+00 N 121+50 N 122+00N 122+50 N 123+00 N 123+50 N 124+00 N 124+50 N 125+00 N 125+50 N 126+00N 128+50 N 127+00 N 126+00 N
112+50 N . 113+00 K . 113+50 N . 114+00 N . 114+50 N . 115+00 N 115+50 N 116+00 N 116+50 N 117+00 N 117+50 N 118+00 N 118+50 N 119+00 N 119+50 N 120+OON '__120+50 N ^__121+00N 121+50 N . 122+00 N . 122+50 N . 123+00 N . 123+SON . 124+00N , 124+50 N . 125+00 N . 125+50 N . 129+00 N . 128+50 N , 127+00 N
110+00 N 110+50 N 111+00 N 111+50 N , 112+01IIP, ^ 112+50 N 113+00 N 113+50 N 114+00 N 114+50 N 115+00 N
IP-2
115+50 N
I P - 3
118+00 N 116+50 N 117+00 N 117+50 N 118+00 N 118+50 N 110+00 N 110+50 N 120+00 N 120+50 N 121+00 N 121+50 N 122+00N 122+50 N 123+00 N 123+50 N 124+00N 126+00 N
M= 104,1=2. 2.7
xxxxx': ns5 ,' 14=75,1=0
. 2J___ 241 s 0.92 ,^J.OO 1.1 - 0.89 1.5 1.8 v -OJ!4 IK 0.67 0.88 1.4 - Ut
4.2———4.8^^4.3——-341^ 34 v\ 1.4 14) 14^^-2.1 —— 2.T" "2.1 \ -1-S OJO 0.86^^1 1.4 \ 2.4 2.2 N. 14) 1.7
110+50 N 125+50 N 128+00 N 128+50 N 127+00 N 127+59 N 128+00 N
TAU (msec)
Spectral-M
Chargeability (mV/V)
Resistivity
Line 3800 E
Pole-Dipole Array ^5———™———?^
*——OH
a = 25.0 M
plot point
Resistivity and Chargeability Anomalies
—.—............Very Strong
————-—.......... Strong
—————•••••••••••Medium
—-----•••••••••••Weak
....... .......... Very Weak
xxxxxxxx- ......... -Extremely Weak
Scale 1:250025 O 25 SO 75 100 125 150
•J hi (meters)
TAU (msec)
Spectral-M(mV/V)
Chargeability(mV/V)
Resistivity (Ohm.m)
106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 108+00 N . 109+50 N . 110+00 K 110+50 N 111+00 N——l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————l—————H-
110+00 N 110+50 N 111+00 N 111+50 N 112+00 N 112+50 N--——'——i——i————i——i——i——i——i——i—113+00 N 113+50N 114+OON 114+50N , 115+OON , 115+50 N , 116+OON , .ilBfMJL——UW*? ,——H7+50N . IIB+OON . 118+SON , 119+OON , 119+50N t 120+50N . 121+OON 121+50N
*WTW a124+OON 124+50N 125+OON
1000
0.10
|tf 9 1, MO 0.10 OJO 0.10 0.10 0.10 0.10 OJO 62 16 31 31 31 S.. SI 31 125 2 OJO OJO 0.10 OJO 0.10 2* 0.10 0.10 OJO OJO OJO OJO OJO OJO OJO 0.10 0.10 0.1* OJO ..,0 D.,fl o.,0
0.10 0.10 OJO OJO 0.10 8.10 OJO OJO 0.10 OJO OJO OJO OJO SI 31 OJO 125 62 OSO OJO "™ " 125 OJO ^ 3J OJO OJO (JO OJO OJO OJO 0.10 0.10 OJO OJO OJO 0.10 OJO 0.10
M0 OJO 0.10 OJO OJO OJO 0.10 16 0.10 62 31 0.10 OJO 62 OJO 62 2.5 16^——B 0.1* QjO*)J) l J 62 62 (HO OJO OJO 0.10 OJO 0.10 OJO OJO 0.10 0.10 0.10 OJO 110
127+50 N
10^OJO OJO OJO OJO 0.80 OJO OJO 0.10 OJO 0.10 OJO 0.10 62
6JO OJO OJO 0.10 OJO 31 OJO OJO 31 U 62 62 125 18
0.10 62 0.10
0.1* OJO 0.20 OJO OJO 0.10 OJO 0.10 16 31 260- OJO 0.10 OJM 250
*" "-W MO 0.10 OJO 2ojo 0.10 ojo rg riisiN .
WO 82 OJO 0.1. OJO OJO OJO OJO OJO OJO u, OJO OJO 31 1,0 O.,0 6J6 0.10 31 080 e \!!L/ * 31 W **
u no ojo ij 0,10 0.30 0.10 0.10 ojo ojo ojo ojo au 0.10 16 L* oj* u 0,0 /™ M0 Ut Sl tM tM *****1 u.iu f sou i 0.1B U
6.10 OJO (J* TJ 6JO 0.10 250 ' 0.1
82 -Tau
(msec)
500___600
OJO 250 OJO OJO 62 62 OJO OJO OJO OJO OJO OJO 126
M* U 0.10 OJO- - - ^.Nx^y^'V^Iu m - a, u-^s^Vii, /s-.k\ 1-5---5
110+00 N 110+50 N 111+00 N 111+50 N 112+00 N 112+50 N 113+0)N——— . .—————,—————.—————,—————.—————,—————.—————l—————,—————l—————,—————(—————,—————l—————,—————i—————,—————j————^
I P - 2
113+50 N 114+OON . 114+50 N 115+OON . 115+50 N 117+50N 118+50 N 119+OON 119+50 N*——i——i——i——i——i——i——i——i——i——i—
n=l 11=176,1=1
11=1 M=208,T=4.0
i 15
IB ^- 17
0.040 OJO 0.44 U 0.91 OJO
M= 111,1=01.3 1.7 x 2.7 2.9 2J 2.1 2J
1J 1.9 \ 2J
11=90,7=0.0025U
M=94 > T=0122+50N | ia4flo N 12wsnM
- MlM
^
9J'
0.46 OJ5 . LO U
0.61 Ut 1.9 1.8 1.8 2 L7J 2.8' 3J
0.71 0.99 LI UJ8^-2.__^^1.8 /2— 2.4 2.9 SJ -—4^^3.6/4.4 4J
(T-S.N. l l LS \ 2.8 2J X 1J 2.7 2.4 SJ f M 4.4 4.6 6 6J ^ 7.1
110+50 N 111400 N 111+50 NH——————l——————l——————l——————l——————I-
112+00 N 112+50N 113+00 N 113+50 N 114+00 N 114+50N . 115+OON | 115+SON | 116+OON , 116+50N | 117+OON | 117+SON | 118+OON ; 118+508 t 119+OON ; 119+SON 120+00 N 121+00 N . 121+50 N | 122+00 N 122+50 N 129+00N 123+50 N 124+00 N 124+5QN 125+OON 125+50N 126+OON
250 iSf} 125, 0.10 0.10 0.10 OJO OJO OJO 16 OJO OJO C 25?\\ OJ6~~——OJO 8.10 3.9
0.10 1.00 010 7J 62 __.31 62 SI \\260 \" 82 62 SSTl26 SI '' ^ \\ N ^ j&eg^^ y62
IM OJO SISI C
O x 290 x 126
^@)55 260
125 '^~250 260 ^CsS^V^ 8-* "-W
250 Oa —— 125 v^ 16 62 OJO
^ 600^^260 ^~-~ 260 ^62 16
02 0.106.18 OJO 1.00 62 ( (ajfi \ 82 61
OJO 050 SI OJO 62 62 ("iS N 62 J
1.00 0.10 16 OJO 82 -125^ 82^- 126 W
7J 1A 7.8 1.00 31 OJO OJO 6.16 6JM 8.18 3.9 0.16 3.9 125 \^**L——-J1 x iog v 1ZB K
31 62 SI * 62 82 SI 7.8 6.16 O M 2 7.8 19 42 62__62 Vl25^U6 r 25T^ 6.10 \^256 .^U^ls
126 f 268 \ 82 62 82 16 82 62 6.16 0.20 OJO 1.08 SI 31 16 62 y' 266 0s 82 18 .ttS l f^^\ " l l f^^~^---
L — V .. - - M 82 OJO 31 16 0.10 16 7J ( M\ K f 250 ZSJL^X*? J25 ^-126 —— i25
126 -
86
125 600
C 82
SI 82
^-16 82
OJO 31
l /72500s 82 t OJO 31
125- 250 ^ 31 125 OJO 62
82 18 040 0.10 0.10 — OJO 0.10
H 0 ] 82^^S18\ \ 26fl\ S-^ \ v \ v s*:^PX82^2503 m?Z*}
82 31^-- 125 /T/6oT\\ It-^^•s V \ \\ \V-^-SOB-CN K \ m\ 500 N
^260 ' 82 ^ 268 --'126 IB 1.00 U6 "^1000 — 1800
110+50 N 111+00N 111+50 N 112+00N 112+50 N 113+00 N 113+50 N 114+00 N 114+50 N 115+00 N 115+50 N 116+00 N 116+50 N 117+OON 117+50 N 116+00 N 118+50 N 118+00N 119+50 N 120+00 N 120+50 N 121+00N 121+50 N 122+00 N 122+50 N 123+00 N 123+50 N 124+00 N 124+50N 125+OON 125+50N 126+OON
K 116 y 53 51 46 47 SB 45
64" ^.59 42 45 ' /) 65-67 92
'i 66 l 63 46 /s 96 ' s 39 37 ^ 67 89
109 121 ^^109 92 -^ 7S 64
101 121 133 ~"',. l"
121 188 " 75 83 62 , "-y/
112 111 119 "121 136 143 124 t 75 66^ 52 —— 40
69 64 ( f ffl| } .95 43 56 42 ^x 71l l s~^ 'M S 62——IB J 66 -^^W s 39 37 ^ 67 89 64 V 96 i 71 61 V
11=13371=0.5 11=92/1=0.0624.7 4.9 . v l.6: ""7x B\ 4\\:\
•U-^t* U \ 4.B 4J\
5.3 V 4J
113+00N 113+50 N 114+00N 114+50 N 115+OON 115+50 N 116+OON 116+50 N 117+00 N 117+50 N 118+00 N 118+50N 119+00 N | 119+50 N 120+00 N 120+50N 121+00N 121+50 N 122+00N 122+50 N 123+00 N
— 3
. 123+50 N 124+OON 124+50N 125+OON 125+50 N 126+OON
11=108.1=0.031 11=2 11=98,1=0.125
ns2 n=l 11=97 11=84 11=104,1=2
11=6" "0=6"" 11=110,1=0.5 14=89,1=0.5
1.9
1J U 2- Ul 1.6 ^ 2.1 i O
n=4 11=122,1=2
0.78 — 1.00 __ 1.5 y 2J
2.7 2.3 3.5
.*T^4
^1.00 U 2Jy^('7j^^V3J -- 4.1>SN^U l tJttA/ U M ^-'M tS 6.2 l"/ M "S \'\\"N"*\ " ^~ S ( 1J J U u ^ 2J U ' 2.6 X^":^*^4J8 4.1 4JI 4J ^ U t ' 6J ' vT ^ 7 7 6,5' 'u M ' 74 \ S 3.9 U ' te U t8 2.1
L7 U L9 1.8- 2.1
U N 6J \ 4J " 4.6 ? "^ 3.7 3J 3.1 3.7 16"
X \M l. 5.1 \ 8.8 ~
S2 3.8 4.6 4* \ 5J1 \ 3.3 \W ^^ -
3.7 U ^ U 4.1 4^ M^ 2J 3J ^5 ^ M 6J -^~vi~-
Possible Shear/Fault
110+50N 111+00 N 111+50 N 112+00 N 112+50 N 113+00 N 113+50 M 114+00 N 114+50 N 115+OON 115+50 N 116+00 N 116+50 N 117+OON 117+50 N 118+00 N 118+50N
- 1160 99511=1 236 ^ 148 v N 480 i l
432 282 ^ 178 ^^ 377^ 1281 1095 ^ IBM
-VWH(3)-119+00 Ni——l——i i 119+50 N 120+00 N 120+50N 121+00N 121+50 N 122+00 N 122+50 N 123+00N 123+50 N 124+OON 124+50 N 125+OON 125+50N 126+OON
11=6 11=4
2679 2261 1374
1929 \ 1317 l 738 V 1488
.~\^ ^ \V^,-'^ 2045 1147 \941 V 8B7 l ( 3116 1B4S v- 1490 ^^1379 981
aso , w j im 0=10.10 0.10 0.10 0.10 0.10 0.10 0.10 0.20 0.10 0,50 0.10 3.9 62 31 M . W , W s 10. .tsa s ant' . tMH7.6 7J 0.10 7J 0.10 0.10 0.10 0.10 0.10 0.10 0.10 0.20 0.10 7J 1.00 16 11 82/290
108+50 N | 1 07+00 N | 107+50 N | 1 08+50 N ( 1 0WMK 1 10+00 N 110+50 N 111+00 N 111+50 N
VI 87 17 17 17 11
10&+50N 107+00 N 107+50 N 1GB+OON 106+50 N lOft+OON 108+50 N 110+00 N 110+50 N
I P - l
111+00 N 111+50 Nn=l
14=192,1=11.00 U OJO 0.60 OJO 0.40 0,40 OJO OJO 1.2 - 0.90 v 2.7 14
U l J l S 1 .1 .OJO OJO 0.70 9.80 l 1 .1 l J M \ 3 17. u.w ,m ^ .. ..w y 1.1 ij M \ s1JO Lt U U \ 3
^ U 1.1 U
l.7'\ 2.7 !J^ 1.4 U ^ l 3'3 'S" OJO 1-00 Ci5 U 1J
2 '" tJt 2.7 U —— Z it —— 1.1 x OJO
8.1 U 1.00 0.70 0.70 OJO
2J 2J \ 1.4 1.1 \__OJO ,-l-0
U U 2.1
106+50 UT | 107+00 S | 107+SON f 106+00 N [ 10B+50N ^ lO+OOW t 1 09^50 N 110+00 N uo+soy | 111+00 N 111+50 N
TAU(msec)
Spectral-M(mVA)
Chargeability (mV/V)
Resistivity (Ohm.m)
1083 1605 \ 208
6429 2041 (to -s. 13)9
0=1 HI 130 133 100 -67 — 199
199 —— 199 —— 212— 243 2M-—-SW
27e 287-- 358 293——296 372 394
363 401 466 ^" 839~~~ *77 3M 491 MO— 687 U9
6H 805 ,710. 681 590 860 J88 — UK 793
66* 129 794 882 B4S ——77J HI BM W7 U7
0=1
0=2 0=3
0=4
0=5
11=6
Line 4400 E
Pole-Dipole Arraya na a
'—®n
a s 25.0 M
plot point
Resistivity and Chargeability Anomalies
........Very Strong
........Strong....... .Medium
........Weak
........Very Weak•••••••Extremely Weak
25Scale 1:2500
26 50 __75 100 125 150•d i ha (metres)
AVALON VENTURES LTD.INDUCED POLARIZATION SURVEY
GLENWATER TWP./SHABAQUATHUNDER BAY AREA, ONT.
Date: 97/03/21
JVX LTD. (Ref. 9680, Jan 1997)
TAU(msec)
Spectral—M (mV/V)
Chargeability (mV/V)
Resistivity (Ohm.m)
110+00 N 110+50 N 111+00 N 111+50 N 112+OON 112+50N 113+OOK , 113+50N114+flON 114+50N 116+OON , 115+50 N , 116+OON , 118+50N , 117+OQN , Itt+SON , IM+OON , 11B+50N , 11B+OON , 119+50N , 120+OON 120+50N 121+OON f 121+50N | 122+OON | 122+50N | 123+OON 123+50N 124+OON 124+50N 125+OON 125+50 N
0=1 OJO 31 0.1, 31 62
0=2 16 OJO 62 0.10 250
0=3 16 OJO 16 jjP^ 18W
0=5ns:6 no ino no l Sn - ino"
ow | 10 OJO 0,0 Oilfl OJO OJO OJO 2 0.10 WO OJO OJO OJO OJO OJO OJO 0.10 OJO OJO OJO OJO OJO OJO OJO 0.10 OJO OJO OJO OJO OJO OJO OJO 16 250 62 126 125 260 5OJO 0.10 0.10 OJO ^w MO u u B 10 U8 8 U o u ut 9M 0 10 , 10 wo U9 0 10 jj, wo U9 fllo D 10 jjj 7J OJO 7J 62 0.30 62 82 125 2SO__ 10 ^n,-^ 10
125 500 2i OJO 250 OJO 0.10 OJO OJO OJ, 0.10 OJO OJO OJO 0.10 OJO U 500 OJO 110 16 62 125 16 62 OJO 126 250 5ojo au 7J 0.10 ojo ojo 0.10 0.10 0.10 siu 7.8 2 6.10 OJO OJO OJO OJO OJO SI 0.10 OJO
OJO 7.8 OJO 0.10 OJO OJO OJO 16 OJO 7J
20 7J 0.10 WO OJO OJO 18 OJO OJO OJ, OJO 0.10 62
IQH 1000 1000
62 62 SI 31 02 2n 0=1
OJ, 250 62 82 2n 0=8
\ "//\""/ li" B — B B 0=3 wo ojo 1ZS 0.10 0.10 aifl 2J nO 250 2J 110 OJO OJO OJO OJO OJO OJO OJO OJO OJO OJO OJO OJO OJO 0.20 OJO OJO S 250 OJO 125 OJO 250 0.10 OJO 5^) 1000 500 -^ IONTTlOOO
MO e.io ojo ojo u w 10 u sn 5 us ojo 62 si ojo ojo 0.10 5 ojo ojo ojo m ojo u ,.i, u 62 ojo ij ij 62 mo u ,.u sn. to y ino sn looogg OJO 5 500 125 125 IM'^~~m'^ 16 0.00 2.5 OJO OJO 0.10 OJO OJO OJO OJO OJO OJO 1JO 2J 2.6 OJO 0.0 16 U 125 250 125 125 ' 1000 1000 500 1000 1000 ^1*5^ \
110+00 ir 110+50N 111+00 N 111+50 N 112+00N 112+50 H . 113+001! 113+50 N 114+00N 114+50N 115+00 N 115+50 N 116+OON 118+50N 117+OON 11+50N | 11B+OON | 118+50N 119+00 N 119+50 N 120+00 H 120+50 N 121+00 N 121+50 N 122+00 N 18Z+50N 123+OON 123+50 N 124+00 N 124+50 N | 125+00 N 125+50 N
0=1 147 i M
0=2 80
0=3 W^V W.-^ l" 04
0=4 111 M 106 y^ M/ /217 217
0=5 in in/ la f i68\ 217 at0=0 124 14S 156 1M- 2n 214
+50N 111+00 N 111+50 N 112+00 N 112+50 K 113+00 K 113+60 N 114+00 N 114+50 N 115+00 N 115+50 N 118+00 N 118+80 y 117+00N 1150N 118+00 N' 118+50N 119+00N 119+50N 120+00 N 120+50 N 121+00N 121+50 N 122+00 N 122+50 N 123+00 N 123+90 N 124+00 N 124+50 N 125+00 N 125+50 N
110+00 N 110+50 N 111+00 N- 111+80 N 112+00 N 112+50 N 113+00 N 113+50 N 114+00 N 114+50 N 115+OON . 115+50N 116+OON , 116+SON 117+OON 117+50 N 118+00 N 118+50 N 1UWJON
82 OJO 7.B 82 31 600 260 , 2000 i 20 128 OJO 0.10 0,10 0.20 0.10 0.20 0.10 7.8 1.00 1.00 31 34 SI SI 2900 , MM- 128 OJO OJO OJO 0.10 OJO 0.10 0=1
7.8 0.20 0.10 0.10 OJO OJO 2 1.00 82 31 0.80 128 82 128 OJO 2.6 M 018^? 800 -\JMO, ' 125 O6 OJO OJO OJO OJO OJO
1000 y^2dflO———2000 X P-W W* *1* 0-1B "O O.W S.* 82 U 82 125 2,6 280 OJO 25^-580 C^IMO 109)) 0.28,__ 28__126 260 — OJO OJO OJO OJO
2000 2000 20*0 r 2080 ^"-W W* '-l* *J* B-W Z M W W MO O-10 1.3 ^ 600 500. 1080 l 18\ 1000/20
.000 /f~4m^j OJO 0.10 0.10 OJO OJO SZ IB 0.10 5 0.10 OJO j' 1000 l 5S"——"X. \ l l f f f ^fflll l
U 1080 ' 4000 f' 1000 0.10 0.10 OJO 0.10 260 18 128 2* 'lMc
10 OJO 10 0.11
m 0.10 0.101000 "V 10 280 288 31 OJOe
(M 600 OJO 0.10 0.10 0.10 10 ' 1000 1000 ION ^ 125 129
11=2
0=3 0=4 n=5 0=8
110+00 N 110+50 N 111+00 N | 111+50 N | 112+00 N | 112+50 N [ 113+00 N | 113+50 N | 114+00 W , ,115+OON 115+SON 116+OON 116+50 W 117+OON 117+50 N 118+00 N 11B+50N 119+00 N
180 151 .x ut ^ aa -^at , n 10* -*^68ya ^^ ^m ^,254 223. \117^__^120 108 158^^88 _^
3Xr\W 216 278 204——' 184 J f 77 A 153 "~-~ 141 207^^136
' '"—-^129^^94 l us m' 2*8 \ 182386 \ 268 241 215' 151-
118 1S3. 118 \ \ 231 231
132 138 184^ 133^ SOS 272
TAU (msec)
Spectral-M (mV/V)
Chargeability (mV/V)
Resistivity (Ohm.m)
line 4600 E
Pole-Dipole Arraya na a
a = 25.0 M
plot point
Resistivity and Chargeability Anomalies
-Very Strong
. Strong
•Medium
. .Very Weak
.Extremely Weak
Scale 1:250025 O 25 50 75 100 125 150
•d . H5 (meters)
AVALON VENTURES LTD.INDUCED POLARIZATION SURVEY
GLENWATER TWP./SHABAQUATHUNDERBAY AREA, ONT.
Date: 97/01/26 Scintrex IPR-11 Rx
JVX LW. (Ref.9680, Jan 1097)
TAU(msec)
Spectral-M (mVA)
Chargeability (mV/V)
Resistivity (Ohm.m)
0=2
0=3
0=4
0=5
0=6
11=1 11=2 11=3 11=4 11=5 0=6
100+50 If 110+00 N 110+50 N [ 111+00 N | .111+50? | 11Z+OON | 112+50 N | 113+00 N 113+50 N 11*400N | 114+50 N | 115+00N 115+50 N 118+00 N | 116+50 N 117+00N 117+50N 118+00 N 118+50 N
7.8 0.60 0.10 0.10 31 OJO 0.20 31 ION
16 I.N 0.10 0.10 o.ifl 0.10 ojo ^ "".Js^HS.020 31 2 0.10 OJO
62 16 2 OJO 82 /if 20N 20N, ION
OJO 3.9 2
125 1JM
— 2000/0.10 0.10 2 31 600 \ 0.10 20 ^ ION 20H ^ 7.8 16 i ION ~~
OJO SI i
OJO 125 500 ^ 1000 (10
5 i^itS^T^ 0.402. U 1. U 250 ^ 5N 0.19128/1000 /"" 1000 1000
ION ION 1000 600-^7.8 020 82 260 OJO 0=1
1(00 6N^ ION ION \ 82 3.9 250^-SN 0=2
500 250 20) ION O- 62 31 ION 0=8
0=4
0=6
109+50 N 110+00 N 110+50 N 111+00 N 111+50 N 112+00N 112+50 N 113+00 N 113+50 N 114+00 N 114+50 N 115+00N 115+50 N 118+00N 116+50 N 117+00 N 117+50 N 118+00 N 118+50 N
110+50 N t —^111+00 N ( .mf50 ? i , 112+OON | f112+50N 113+00 N M^nv llft+OON H6+50N 117+OON . Itt+StN IIB+OON 11B+50N 119+OON 113+50 N .nVT" .u+finw 115+00 N , 115+50 N————HW** ,——li?™*!——————————————————.————. .————————i——————— 119+50 N 120+00 K | 180+50 N . 121+00 N
2SOv -SOB^aO j K 0.10 0.50 K E 0,50 E 125.,,,, ION y, 250
5^ "\^ 0.10 02
0.10 f f .600 \^ (2 -^XSO-——260^15)
02 3.9
0=3 0=4 0=5 0=6
11+00 N +50N 112+00 N 112+50 N 113+00 N 113+50 f 114+OON 114+50N . 115+OON 115+50N 116+00 N 116+50N | 117+OON ^17+SON .116+00 N 118+50 N 119+00 N 119+50 N 120-00 N J20+50N . 121+OON
1000 = 1000 j ,, 500 , i IS 0.10 0.10 0.10 0.10 0.10 0.10 O
0.10 0.10 0.10 0.10 0.10 0.10
0.50 0.20 0.10 0.10 0.20
0.10 0.10 0.10 0.10
0.10 0.10 0.10
0=10=2
11=3 0=4
11=5 11=6
116+00 N 116+50 N 117+00 N 117+50 N 118+00 N 118+50 N 119+00N 119+50 N 120+00 Nl————l————c————l————————l————i————l————,————l————————l————i————l————————l————c————l————c————l————i————\————,————l————c————l————l————l————.————l————l————l————l————l————l
11=1 H2 j
11=2 187
11=3
0=4
0=5
0=6
143 -__ 117 111 ~JS*-V m - 8M ' 172 x 111 92 ~~- 672^wSjttfS(2 l'"214 178 143 152 S 200 ' 237 2M V 133( v y /^ s
J 162 ^~ 153
92 85 91
143 ^ 187 216 214- — 204 209
176 186 171 ^ 206 ^ 221 ( 189 199 161 \ N 103 100
182 187 '223 x 202 202 191 195 174 N 98 117 143 —^ IK
\ ~c -— _ C — f ^^~
-148 J 1 16 ^ 138\ \ 67 65 87 67 (ClW
S^UZ 121 118-^-80 67 67 64\,1 106 S, -"^^~ - -
\ \ 103 100 \
11=111=2 11=3 11=4 0=5 0=6
IP-1116+00 N
IP-l
116+50 N 117+00 N 117+50 N 118+00 N 118+50 NH————l————h-
119+00 N 119+60 N 120+00 N
11=1 1^=202,1=0.5
0=1 8.7 , 7.4
0=2 0=3 0=4 0=5 0=6
14=220,1=1
) l J^\\\12 f 14 l 12 A\\V x \\\\\\12 -^14 IS ^ \ X 11
0.70 0.90^-1,2 , 0.90 0.60 -. 0 .40 11=1
0=2 0=3 0=4 0=5 0=6
11 X 8.3 g\\ 1.5 . -0.20 0.50 0.90 0.30 l 2.1
0.90 0.50
3 \ 0.50
116+00 N 116+50 N 117+00 N 117+50 N 118+00 N 118+50 N 119+00N 119+50 N 120+00 NVH(2)-
^^ \((7^^^ \r^\^^ 1 000 f 40 Ut 4000 ) 2000 l 0.40 J 201^ \ N^feV/// //^^ 10 S s 1000 20 ^^ 2000 Vk 20 W/ 4000 ^^^ \ f ,. ^\\f^i^ y^
..._ . ^80 ^ 40 ^ 2000 ' 20 1000 2000
92+50 N———l———————H 93+00 N 93+50 N 94+00 N 94+50 N 95+00 N 95+50 N 96+00 N 96+50 N 97+00 N 97+50 N 98+00 N 98+50 N 99+00 N————l————l————l————'————l————l—
99+50 N 100+00 N
0=1 204^—214 j 148 _ , 171 \y\ 278^^196^-^^142 __ 143 y 105 108 , 91 i 117 v 86 103 85^ 108 97 - 74 g 412i. 108 ^ 78 82-
BATEMAN LAKE PROPERTY, OntarioConmee ft Horne Twp., NTS; 52A/12
Date: 97/03/11
JVX LTD (Ret. 9680, March 1997)
TAU(msec)
Spectral—M (mV/V)
Chargeability (mV/V)
Resistivity(Ohm.m)
95+00 N 96+50N 96+00 N 96+50 N 97+00 N 97+60 N 96+00 N 96+50 N flfltOON | 99+50 N | 100+00 N | 100+50 N | 101+00 N | 101+50 N
0=2 0=3 0=4 0=6 0=6
V v\ V.UNX\ON . -_ ^ION ^N5 OJO -~- 250 —' 0.10 j^J25
1000 j^ 0.10 2J 0.10'0.10 250, 0.10 ST!
UN \
125 0.20 OJO S.1 0.10 0.10 250 .^2J U 2500.10 3J OJO 0.10 0.10 0.10 8.100.10 5
125 0.10 0.10 OJO 2
s* '-w woo loo -loooojo 0.10 0.10 ow —
C V.1V
82 ^ 3.8 ^500
5—— olio 2.5 125 2J OJO 3.0
5 0.10 0.10 U 0.10 0..0 82
—""xT v v
250 0.10\\(gv)) W 0.10 125 OJO 0.10 0.10 C-——^S-
K ojo
92+50 N 93+00 N 93+50 N 94+00 N 94+50 N 95+00 N 95+50 N 96+00 N 96+50 N 87400N 97+80 N 98+00 N 98+50 N 9800 N 99+50 N 100+00 N 100+50 N 101+00 N 101+50 N
14. 7-198-^107 102 104 104 .vl
\ 112 X 109 y 114 118
v X 88 \^ 113 112 J 124
115 114 114 v/^ 100 ) 118 /-" 124
204 XVSN 135' x 100 110 110 116 117 ' 120
—-M0 102
IP - 299+50 N | 100+00 N | 100+50 N | 101+00 N 101+60 N
9322 10K 161 171 v 21K X "* 6058^* UK^ 6370 6835 ~ 5600 ^ s 30K 53K 52K 63S
TAU(msec)
Spectral—M(mV/V)
Chargeability(mV/V)
Resistivity(Ohm.m)
Line 9800 E
Pole-Dipole Array
a = 25.0 M
plot point
Resistivity and Chargeability Anomalies
xxxxx xxxxxxx.
1 Very Strong
1 Strong
1 Medium
'Weak
- Very Weak
- Extremely Weak
Scale 1:250025 O 25 50 75 100 125 150
^^^^E (metres)
AVALON VENTURES LTD.INDUCED POLARIZATION SURVEY
BATEMAN LAKE PROPERTY, OntarioConmee k Horne Twp., NTS: 52A/12
Date: 97/03/11
JVX LTD (Ref. 9880, March 1997)
TAU (msec)
Spectral-M (mV/V)
Chargeability (mVA)
Resistivity (Ohm.m)
91+00 N 91+50 N 82+00 N 88+50 N 93+00 N 03+50 N 94+00 N 94+50N 95+00N 95+50 N 96+00 N 95+50N 97+00N——i——i——i——i——i——i——t- 97+50 N 9B40Q N 96+50 N 99+00N 99+50 N 100+00N
0=1 20 0.10
xi—2 n=3 n=4 11=5 11=6
10 0.100.10
40 ^250 82 590-^2.5 31 16 OJO 31 OJO 125 0.50 2 3.9 0.10 5M OJO 0.10 16 31 (2 125 500 125 13 125 500 0=1
0.40 .1000^^.82 0.10 V ION J 250 250 OJO l J l J 125 250 5 0.20 OJO OJO 3.9 0.10 82 82 0.60 12S OJO 2.5 5 250 500 0=2
0.10 V 1000 ) 24 18 (v^WjOTjOOO/ 0.10 OJO 0.10 0.10 0.10 OJO 7J 0.10 0.10 7J U Ut NO HO B 0.10 VJOflO^) 260 2J 62 125 1=20.10 0.10 I 1000 ' 0.10 \ 1000\\lf ^-^ )0.10 OJH 0.10 80=500 1000 x- 0.10 600 OJM^Ilf 0.10 041 0.10 SI 0.60 18 0.10 16 0.10 0.10 62 U 500 5 0.10 500 ^ U
0.10 688 250 0.60 OJO OJO 1.00 8.10 1.00 0.20 31 0.10 7M 7J 125 126 82 SO 10 0.10
—— 250 0.10 U OJO 0.10 0.10 1.00 li 82 7J 31 31 125 500
0.10 0.10 1.00 M IB OJO 1.00 U IB 0.10 250 82 OJO 250 125
1000 \ U
6 250 250 250
500 500 500
5 250 500
500 126^— 500 500 BOO
1=3
1=4
1=6
1=6
92+00N 92+50 N 93+00N 93+50 N 94+00 N 94+50 N 95+00 N 95+50 N 98+00 N 98+50N 97+00N 97+50 N 98+00N 96+50 N 99+00 N 99+50 N 100+00N 100+50 N 101+00N
16 , y68 __ 50 i 105 .—— 117 - 98 116 v- 87 y y 130—- 133 . 203 ivy
^^W \ t\rn ,r^\S^Jjir:^x 62 -—— 44 67 67
" ^DX 4* ^f"^/^i 44 56
87 87 s 54 48 i 69 i 97 109 107 N. 143 \ 118- ^l \
39-X 54 —— 54 48 H.' 63 103 t 133
vV) /^\ u a \*\ m\ uV T43l J ^A^ ^ U ^
/ A49 M ' 128 8, \ 112 ^ 143 ^ 113 ^ 152 161
I P - 2Possible Shear Zone
l
T-2,HP v92+50 lA 93+00 N 93+50 N 94+00 N 94+50 N 95+00N 95+50N 98+00 N 96+50N 97+00 N 97+50 N 98+00N 98+50 N 99+00 N-H—————i——i——i——i——^ 99+50 N 100+00N 100+50N 101+00N
n=2 111=239,1=1
2.3 22 2 2JI\ M L8
2.9 3.1 2J 24 2.1 2J
24 2.9 U 2.6 24
u 1J i U 5.4, 6.6
y 2J
2.8
2.7 2.9 4
"]
U j 44 tt
-^4* v 7.6 7J U 44 4.9 4J
7.7 ^ 5.6 8^~- 7J 6.8
* 8.5 M
u \
7.1 7J M * 8.5 M 's^J J U S
7.3 7J U \ 6.9 8.7^^7.7 U
8.95.7 7.1 STe-i44 5.5 - 12 \ U 12
\ ™ r\7.7
64
5.6 1=1
1=2
1=3
11=4
1=5 11=6
92+00 N 92+50 N 93+00 N'VH(I)
93+50N 94+00 N 94+50N 95+00 N'VH'(S)' 95+50N 96+00 N 98+50 N 97+00N 97+50 N 98+00 N 98+50 N 99+00 N 99+50 N 100+00 N 100+50 N 101+00 N
92+50 N 93+00 N 93+50N 94+00 N 94+50 N 95+00 N 95+501
96+00 N 98+50 N 97+00 N 97+50 N | | 96+00 N | | 98+50 K 99+00 N "t901! . 100+00 N 100+50 N 101+00 N 101+50 Ni———l———i———l———i———l———i———l———i———l———i———l———i———l———i———h- 102+00 N 1 102+50 y 103+00 N 103+50 N 104+00 N 105+00 IT 105+50 N 106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 109+00 N 109+50 N 110+50 N 111+00 N 111+50N
600 900 -^ 0.10 20 y 1000 ^-900——.250 250 l 1000 i 2000
1000 1000 1000 ^^ 10 ^ ION J 260 250
260 126 600 10 0.10 0.10 10
600 ^ 2000 ' ' 10 ^ 1000 " 0.10
MHW" -i 0'10 JS. *MOr^\"^^l 2000 V M* "" ^-'/l
2000 "J 1000 600 40 =
iOOO 1000 1000
900-^JOOO 1000 N 290 ——-900 129 0.10 0.10 0=1
-~ 1000 j (2 0.10 0.10 0=2
000 ^2000/^129 129 0.10 0=8
1000 ^~ H 0.10 600 0=4
0=5
0=6#~\ a- \1000 IB*260- x 2000
96+50 N 97+00 NH———i———l———i———I- 96+00 N ; , 98+50 N 99+00N " 801* 101+00N ,101+90 N | 1102+00 N | 1102+50 N | |108+00N 1 103+50 N | 104+00 N 1 105+00 N | 1105+50 N ; 106+00 N 106+50 N 107+00 N 107+50 N 106+00 N 108+50 N 109+00 N 109+50N N . 110+50 N 111+00 N 111+50 N
73 78__80 60 xl02 111 98
108 V 70 f 107 \ 80 78 A 104 (O 107
159^*0105 101 106 111 \ 76 82 109 108
j 128 118 —-* 106 c 72
M 148 —— 146 \ 98 .
216 ^ 167-^-227 i 171 ^ 133 ^-186(7 87 67 67
87 87
C ys' ™ v 1^. 176 S .* 244 5 23S\~98 87 87 07 07 87 87 , 169v 138 ' C// 1^
92+50 N 93+00 N 93+50 N 94+00 N 94+50 N 95+50 H 96+00 N 96+50 N———l———l———h- 97+00 N'VH(I)-
97+50N 88+00 N "t" f . 99+00 N "t8011 . 100+00 N 100+50 NHtO
101+00 N 101+50 Ni———l———i———l———^—rt———'———HVH(2)
102+00 N 102+50 N 103+00 N 103+50 N 104+00 N 104+11 N 105+00 N 105+50N 106+00 N 106+50 Ni——l——-——l—————l——.——l——i——l n^\ '——'——'——'——l——'——'——'——i——'——^^F-1——'——'—-"——'——i——'——i——'——l——'——i--l--i-.l-J——•~ 107+00N 107+50 N 108+00 N 108+50 N 109+00 N 109+50 N HMDO NVH(1)
110+50 N 111+00 NVH(1)
•l-—i——l——i——l——i——^- 111+50 N
MX S5I^ 94K *2I i 4(1 411 871 , 221 141 231 , . 4(36 4360//r\ r&fv9813 5160 8077 V V 2(1
BATEMAN LAKE PROPERTY, OntarioConmee ft Horne Twp., NTS; 52A/18
Date: 97/03/12
JVXLTD. (Kef. 9680, March 1997)
TAU (msec)
Spectral—M (mV/V)
Chargeability(mV/V)
Resistivity (Ohm.m)
11=1 11=2 11=3 11=4 11=5 11=8
99+00 N 99+50 N 100+00 N 100+50 N 101+00 H 101+50 N 102+00N 102+50 N 103+00N 103+50 N 104+00N 104+50 N 105+50N 106+00 N 106+50 N 107+00N 107+50N 108+00N 108+50 N 108+00N 100+50N 110+00N 110+50 K 111+00 N 111+50N
99+00N 99+50 N 100+00 N 100+50 N 101+00 N 101+50N 102+00N 102+50 N 103+00 N 103+50 N 104+00N 104+50 N 105+00 N 105+50 N | 108+00 N 108+50 N 107+00 N 107+50 N 108+00N 108+50 N 109+00 N 109+50 N 110+00N 110+50 N 111+00 N 111+50 N
99+00 N 99+50 N 100+00 N 100+50N 101+00N 101+50 N 102+00N | 102+50 N 1(0+00 N 103+50 N 104+00 N 104+50 N 105+00 N0=2
14=359,1=2/4
r^{los+sote | ki
- 6
.06+00 N 108+50 N 107+00N 107+50N 108+00 N 108+50 N 108+00N 100+50 N 110+00N 110+50 N 111+00 N 111+50N
14=466,1=008/8 11=410,1.01/212 11
)
4.1 4J 4.6 6.0 7.7 ^
.4 4J y M ti l' 8.7 —— 0.8 -. 12 '
X 6J 7J 10 yTJ ^BJV "12 \
74 U \8J^-^ 11
3.0 4.2 ' 3.8
4.7 f SJ/ SM t.\i ..o y
3.7 - 6,7 ' 7.1 X 8J X 7.1 U M
/l U 7.1 ^ U
99+00 N 99+50 N 100+00 N 100+50N 101+00N 101+50 N 102+00 N 102+50N 103+00N 103+50 N 104+00 N 104+50 N 105+00 N 105+50 N 108+00N 106+50 N 107+00 N 107+50 N 108+00N 108+50 N 109+00 N 109+50 N 110+00N 110+50 K VH(3)
111+00N 111+50 K
0733 __ 141 x , S040 3408 3342
'iP7r^/vv-^^^v^JIOV J 268 X 1167 ~- 1660 5783——-BOO ——
108+50 N 109+00 N 109+50 N 110+001 110+60 N 111+00 N
3.4 SA j 6 /O- —— 9J B.3 Ji^.2^//. a N^vT
3.9 U 4.1 t 7.1" "x" llUlf
42 ,__ 43 vvv- M yiW9J 3.8 --.3.2
__ 9.8 ( —— 6 4.0 4.7J
5.6 l 3.S
3.B 5.0 - 3.8 2.4
11 ^ 8.6 .—11 ^ 7.9 ^ U . 4.7•^^ZS// ^
i i M^ 7 / ^ / \^r-^-^ s6.8 ^ 8.7 f 12 f 19 15 16 15 f
1 SM x^ u u^— u u l K -——^17 8.4 - II -"8.8 7.9 7J 8.823 S^N 8.4 7.6 8.8 N 5.2 4j 6.3 —— 8.8 ' 2.9 ^ 4.7 5.8 4.5 ' 2.9 4.3
92+50 N 93+00N 93+50 N 94+00 N 94+60 N 95+00 N 95+50 11 98+00 N 98+50 N 97+00 N 97+50 N 98+00 N 98+50 N 99+00 N 99+50 N 100+00 N 100+50 N 101+00 N 101+50 N 102+00 N 102+50 K 103+00 N 103+50 NVH(2) " 11=1,2" VH(1,2)
4448 v 898 M 4662 -^ 111 8807 5460 i 171 261-,x- UK—— 9189 —. 7114 ^ 976'
J^^'(a^ jiY Z /Co *0^f^^^Srl^^ifc^ ^./ra^iM. L^v^i^^/^^i^L^r^
104+50 N 105+00 N 105+50 N 106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 109+00 N 109+50 N 110+001 110+50 N 111+00 N
1000
0=1
0=2 0=3 0=4 0=5 0=6
104+50 N 105+00 N 105+50 N 106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 109+00 N 109+50 N 110+50 N 111+00 N
10 ON 104+50 N 105+00 N 105+50 N 106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 109+50 N 110+001 110+50 N 111+00 N
WO 1000-040L^f^0=1 0.89 250 250 16 250 5 500 x 500 ION , 18 OJO 16 500 1000 040 20—.
0=2 MO 5 250 290 900 125 500. 1000 S m 62 OJO 2
1^3 0.10 2.5 0.10 5 250 125 125 0.10 2.5 OJO
nZ4 tx (^an~~^m 0.10 m K at m m (^IOBO oainsS 110 —- 500 s\ 500 U 250 7J OJO 125 10
0=6 6 800 1J 1J 800 18 1000 "^~2000 40
e-i/r^f^iP^ioUjf
OJO
2000
0=40=5 0=6
101+00 N 101+SON 102+OON KB+SON 03+5011 106+gQN 107+50N
111 M' 114 100 101 1ZO- 107 111 07 ^.
M -^ 101 -^ 100 ( 133 \ 103
117 105 m 136 \ \ 84
111 x' 12* 18* __ 181
121 107 US 121 114
0=1
0=2 0=3 0=4 0=5 0=6
I P - 6
101+00 N 101+50 N 102+00 N 102+50 N 103+00 N 103+50 N 104+00 N 104+50N 106+50N 106+OON 108+50 N 107+OON 107+50 N 106+OONH———"———I- D8+50N
11=1 u . 0.111=2 11=3 11=4 11=5 0=6
6.8 U ^ — U li M 8.4 - M 4.8 --^2-4 *-3 __ "/-^ ll VA 21 ^^Ji^" *
u M" w-^^wA w 7 — u 5.0 u * 'J (tMU-— ' B Uy^" 8 "^-V* " S 8 ^ "
: a u JKv* n^ o iir
101+00N 101+50 N 102+00 N 102+50 N 103+OON 103+50 Nt._'. . '——'——i——'——i——'——i——i——i——'——i——'——i——'——i- 104+00 N 104+50 N 105+00 N 105+50 K 106+flO N 106+50 N 107+00 N 107+50 N iff)
B6+50N
0=1 0=2 0=3 0=4 0=5 0=6
SM
1388 — 1(45 V 0198 \ W03
2546 — 2084 v 3H3 8276
TAU (msec)
Spectral-M(mV/V)
Chargeability (mV/V)
Resistivity (Ohm.m)
Line 9700 E
Dipole-Dipole Arrayf a na a
J±]___C±la s 25.0 M
plot point
Resistivity and Chargeability Anomalies
. Very Strong
-jjedium
ixm TOXXXXX.
-Very Weak
. Extremely Weak
Scale 1:250025 O 25 50 75 100 125 150
-l LJ
(metres)
AVALON VENTURES LTD.INDUCED POLARIZATION SURVEY
BATEMAN LAKE PROPERTY, OntarioConmee A Horne Twp., NTS; 52A/12
Date: 97/03/12
JVXLTD. flgef. ggflq JfarcA 1 997)
TAU (msec)
Spectral—M (mV/V)
Chargeability (mVA)
Resistivity (Ohm.m)
101+50 N 102+00N 102+50 N 103+00N 103+50 N 104+00 N 104+50 N 105+00 N 105+50 Ni——i——c——i——i——i——i——i- 106+00 N 106+50 N | 107+00 N 107+80 K 108+0011 108+50N 108+OON 109+50N 110+OON 111+OON 1I1+50N
101+50N 102+00 N 102+50 N 103+00N 103+50 N 104+00N 104+9)N 105+00 N 105+50 N 107+00 N 107+50 N | 1106+00 N 108+50 N 109+OON 109+50N 110+OON 110+50 N 111+00 N 111+50 N
11=1 111 104 113 104 103. " -— 112
11=2 l" "Z HI W 104 ^-124.
11=3 l" 116 111 107 X 136 l 103
nr:4 104 ^ 121-^J04y 140 i 110
137 . 110~^v\ ^~-
"\\TT06 ^ ' 166 104 116
^*L ^r^^}//^.ir. .A i /.Z////
101+50N 102+00N 102+50 N 103+00 N 103+50 N 104+00 N 104+90 N 105+00N
I P - 8105+50 N 106+00 N 108+50 N 107+00 N 107+50 N
I P - 7
106+00N 108+50 N
IP - 9
109+00 N 109+50 N 110+00 N 110+60 N 111+00 N 111+50 Nn^
M=350,T=211=1 7.4 0.0 7.B tA U ^ M
n-Z 73 7.3 li 7 B.B
n^3 0.1 6.0 7J 7
0=4
0=50=6
114=541.1=4-8 W. --M.ss-i W *^r 31
11=^13^1=216 ,2.4 .^ U v. 1.7 -0.44
' /11 ^ 22 ss~ 10 ^ 16 17 l 20
101+50N 102+00 N 102+50 N 103+00N 103+50N 104+00 N 104+90 N 109+OON 105+50N 106+00N 106+60 N 107+00 N 107+50N 108+00 N 108+50NVH(3) n=2,3
— —— —— ^ mn=l n=l1 109+OON 'VH(2) ' 109+50 N 110400 N 110+50 N 111+00 N 111+60 N
VH(2)
m 0115r—s ,— — x""/' /~7 LIl^— — ^^--^S^— "SJ —101/201 271 231' 7 111 X 5502 6204 s ***7 l 0620 ^1iT\ 11-^* i f J f ^~- ~~ ~—. ^s.^ y i
23t 23t 2K 7 la/^OJM -^W^ 0025
2tt^-lB ; 7240^111 (JJ61
SS /^ 131 10I"*1**12I IK Itt^ Ttt\ 1117/ y^^\ X \
18E '6534 Iffi^ 111 16K 211
1040 11=1
11=2
11=3 0=4
11=5 0=6
TAU (msec)
Spectral-M (mV/V)
Chargeability (mV/V)
Resistivity (Ohm.m)
Line 9800 E
Dipole-Dipole Array. a . na a
[±La = 25.0 M
plot point
Resistivity and Chargeability Anomalies
xzxzz xxxxxzx.
•Very Strong
•Strong
•Medium
•Weak
•Very Weak
•Extremely Weak
25Scale 1:2500
25 50 75 100 125 150^fsmassim(metres)
AVALON VENTURES LTD.INDUCED POLARIZATION SURVEY
BATEMAN LAKE PROPERTY, OntarioConmee tt Horne Twp., NTS: 52A/12
Date: 97/03/19
JVXLW. (Ref. 9680, March 1997)
TAU (msec)
Spectral-M
Chargeability (mV/V)
Resistivity (Ohm.m)
99+50 N 100+00 N 100+50N 101+OON , 101+5™ , 102*0™ . ^50N - M**'f - t0W————^}^L 104+50 N 106+00 N 105+50 N 106+00N lOB+SO M . 107+00 N 107+50 N . 108+00 N , 108+6011 109+00 N 109+50 N 110+00 N 110+50N 111+00 N
11=2 0=3 0=4
0=6
(2 5 5 0.10 __ JOG 82 290 250- 1(1011,10001 OJO 250
Zi5 u 10 WJfflj), 5?1 —— *"* * ( 1MO f** W——'W 20
0.1* MO 0.10 0.10 1.3 U U U 0.10 0.10 125 10 loj 1*60 J 0.1* 11 ^ 1900
01B 25* B.1B 62 125 500 500 tt 259 5BB B [ f /2WO) J 590 C M ^ 508
nz i 0.10 16 0.10 0.10 0.10 5 5 7.8 82
n-2 25 0.1* 0.10 0.10 500 125 125 0.10
0=3
0=4
0=5
aw 0=1
0.10 1.3 is 0.10 0.10 ' low ut 2to
OJO 580 18 -- 300 U. J { ^;** ^
2i 31 X. 1000 x 259 261
99+50 X 100+00 N 100+50 N 101+00 M 101+50 N 102+00N 102+50N 103+00 N 103+50 N 104+00N 104+50N 105+00 N 105+50N 106+OON ^ 108+SOK . 107+00 N . 107+501? . 108+00 N 108+50 N 109+OON . 109+50 N 110+OON 110+50N 111+00 N
117 145 162 162 M 10!
133 '148 148 115 94
I P - 6 P - IP-9
99+50N 100+00 N 100+50 N 101+00 N 101+SQK , 102+OON 102+SON 103+OON 103+50K 104+OON 104+50N 106+OON 105+60 N 106+00 N 106+50 N 107+00 N 107+50 N 106+00 N 106+50 N 109+OON 109+50 N 110+00 N 110+50 N 111+00 N
8J j1 /6 Asjl M ' 9Jl^M (u 4J1 4.1 | 1.8 ( Jl/3-*^-"
-^65 6.8 8^^ 9A 9.7 7.7 ^-6 U S.4,
.1 7Ji 7
0=1
0=20=3
0=4 0=5 0=6
99+50N 100+00N 100+50 N 101+00 N 101+50 N 102+OON 108+50 N 103+OON 103+50 N 104+OON 104+50 N 105+00 N 106+50 N 106+OON 106+50 N 107+00 N 107+50 N 108+00 N 106+50 N 109+OON 109+50 N 110+00 N 110+50 N 111+00 N
1437198 2676 ' 3324 ^W8^- 1714 0=1
0=2 0=3
0=4
0=5
0=6
TAU (msec)
Spectral-M (mV/V)
Chargeability (mV/V)
Resistivity (Ohm.m)
Line 9900 E
Dipole-Dipole Arrayna
/' a = 25.0 M
plot point
Resistivity and Chargeability Anomalies
xxxxx xxxxxxx
Very Strong
Strong
Medium
Weak
Very Weak
Extremely Weak
25Scale 1:2500
25 50__75 100 125 150se^nf-ia(metres)
AVALON VENTURES LTD.INDUCED POLARIZATION SURVEY
BATEMAN LAKE PROPERTY, OntarioConmee fc Home Twp., NTS: 52A/18
Date: 97/03/12
JVX LTD. (Ref. 9680, March 1997)
TAU (msec)
Spectral—M (mV/V)
Chargeability(mV/V)
Resistivity(Ohm.m)
99+OON 99+50 N 100+00N 100+50 N 101+00 N 101+90 N 102+00 N 102+50 N 103+00 N 103+50 N 104+00 N 104+50 N 105+00 N , 106+50 N | 106+00 N | lOt+SON | 107+00 N | 107+50 N | 106+00 N | 108+50 N | 109+00 N | 109+50 N | 110+00 N | 110+50 N | 111+00 N
0=1
11=2
11=3
0=4
n=5 0.10
11=6 0.10 3.*
2 S
0.10 1.3 0.10 31 290 0.10 62 OJO 125
20 —— 0.10 250 0.10 500 129 16 16 290
((T^^V250 0.10 290 250 62 62 31
260 —— 260 125^^600 1000 ) UK 260 62 f r*--——^31 10 ( 1000 ) 290 1.3 290 129
looT"^ 129 126 2.5 0.10 250 500
900 18 0.20 290__ 10 tt 3.9 3.0 02 0.10 129 i i 2000 aNOx/SM 2.5 0.10 0.10 10
290 129 129
129 1.3
2.9 K
( 1000 \ 31M^-- UM
OJO 0.50 82 16
•900 129 0.10 82 16 31
125 500 280 250 16 7.6
250 2.5 250 500 250 0.60 120
0.10 1Z6 U 5 62 62
500 "\aO 250 10
1000 500 U
1DOO ~ 1000 500 290
1000 \ 10 290 9
1000 -~ 900 290
11=1
11=2 0=3 0=4 0=5 0=6
99+00 N 99+50 N 100+00 N 100+50 N 101+00 N 101+50N 102+00 N 102+50 N 103+OON 103+50N 104+00 N . 104+50 N 105+00 N 105+90N | 106+OON | 110H50 N | 107+OON | 107+50N | 10B+OON | ,109+SON | ,109+OON | M9+50N | HO+flON | 110+50N { , 111+OON
109 v 73 74 106 , 189 189 -^ 14378 ^ 100 116 v 124 l 111
102+00 N 102+50 N 103+00 N 103+50N 104+00 N 104+50 N 105+00 N 105+50 N 106+OON 10I+50N 107+OON 107+50 N 106+OON 106+50 N 109+00 N 109+50 N 110+00 N 110+50 N 111+00 N11=5
11=148,1=1.0x 7.2 6.2 iU U 40 41 5.2 y 6.8
5.1 6.1 t* ^ 47 47 3A 5.1 6.1
ll^— j
.1=2 14=26^1=4 11=451,1=2
6J B.B U .6/ 46 5.2
0=6 2-0 4.8 4.0 ' 8.5
5.6 3.7 3^ 4.1 46 U 42
7.1 6* 47 3.0 45 3.6 4.2 U 4.S
041 B.B 45
\6J
8J 6.8 7.8
4J 5.2 f 6J \ 14
^^6J 5.0
7.1 6.1 62 6.3 s 6.1 4J ' - 12
5.4 46
11=434,1=0.04-83J 64 6.1 IS 13 ^ 10 B.S -^ H i i 26
99+00 N 90+90 N 100+00 N 100+50 N 101+00 N 101+50 N 102+00 N 102+50 N 103+00 N 103+50N 104+00 N 104+50 N 105+00 N 105+50 N 106+00N 101+50 N 107+OON 107+50 N 106+00 N 109+00 N 109+50 N 110+00 N 110+50 N 111+00 N
11=1
11=2 0=3
11=4
0=8 H72
^ 38* \;,OPJ^ -Z 6M8 , 8470 "~778J
' 2\m \\ 2541 — 2304 7031 Toi
111 111 0=6
TAU (msec)
Spectral-M (mV/V)
Chargeability (mv/v)
Resistivity (Ohm.m)
Line 10000 E
Dipole-Dipole Array, a | na a
r^i r^na = 25.0 M
plot point
Resistivity and Chargeability Anomalies
. Very Strong
-strong
ZXZXX XXXXXXXi
. . . . . . . . . . Weak
. . . . . . . . . . Very Weak
, . . . . . . Extremely Weak
25Scale 1:2500
25 50 75 100 125 150S3* I-(metres)
AVALON VENTURES LTD.INDUCED POLARIZATION SURVEY
BATEMAN LAKE PROPERTY, OntarioConmee A Horne Twp., NTS: 52A/12
Date: 97/04/08
JVXLW. (Ref. 9880, March 1997)
TAU (msec)
Spectral—M (mV/V)
Chargeability(mV/V)
Resistivity (Ohm.m)
91+50N 92+00 N 92+50 N 93+00 N 93+50 N 94+00N 94+50 N
91+50 N 92+00 N 92+50 N 93+00 N 93+50 N 94+00 N 94+50 N
0=1
0=2 0=3 0=4 0=5 0=8
195 (3j!V-31
IP - 291+90 N 92+00 N
99+00 N 99+90 N 98+00 N 96+50 N 97+00 N 97+50N 96+00 N 96+50 N | 99+00 N 99+50 N 100+00 N 100+50 N 101+00 N 101+90 N 102+00 N 102+50 N 103+00 Ni——i——i——i- 103+50K 104+00 N ; 1Q4+50N | 105+00 N ( 105+50 N | 106+00 N | 106+50 N | 107+00 N lOB+OOy 109+OON 109+90N ,110+OOW 11Q+50N 111+50N
l
WOO — 2000 2000 ,, x 0.10 1.00 16 IM0.10 0.10 10.
0.10 0.10 260
2000 ^ 4000 A\ ItOO ^ 0.10 0.10 0.10 0.10
20
11 J.10
0.10 0.10 O
OJO 82 O 0.10
31 31 16 16 125 82 OJO 3J 16 OJO 0.10 82 250 0.60 185 0.10 62 OJO 0.49 0.10 0.10 31 1J
O 0.10 /""lOoT^ OJO 1.00 3.9 OJO OJO 860 250 1.3 500 600 0.10 10 0.10 l J OJO 0.10 250 10 '"ionT^ 0.10 62 0.80 0.10 S gM^ 1.10 ' "lOOo""1"* li, s ' 1000 1000 1000 -- 500 l
95+00 N 95+50 N 96+00 N 96+50 N 97+00 N 97+50 N 98+00 N | 96+50 N ( 99+00 N ( | 99+50 N | { 100+00 N | 100+50 N 101+00 N 101+50 N IQZ+OON ; 102+50 N 103+00 N 103+50^, 1 104+00 N ; 04+501? 105+00 N | 105+50N 106+00N ^Oe+MN t ^07+OON | ^07+SON | ^OS+OON | ^OB+SON 109+00 N 109+50 N . ^ilO+00 N 110+50N 111+00 N 111+50 N
n=2 n^a S 11=1 ns5Ms370,Ts4 M=336J=fr^=541,T=2 lO539,Ts.OB/!
'/P,') a ' 9^L.U. v \'.4 - W \ 9 ^-M
7 ,7 3^ ^7- 3J 6.
8.1 7 l 49 12 - 7 j~^ ifi '
^x^
8.6 5J1 5.6 4J ^ 2.6 6.7
7.7 ——— 7.8V^^^fS^-% 12 iS^ffiVU w 17 -S5^,
7.4 7.6 k 4.7 X'/ 12 -^? 7J
42 C 8 8.4 7J 'S -23
7.4 6.8 (fc8 —- 6.6
91+50 N4-
93+00 N 94+00N 94+50 N 95+00 N 95+50 N 96+00 N 96+90 N 97+00 N 97+50 N 96+00N 96+50 N 99+00 N 111+90 N
TAU
(msec)
Spectral-M(mV/V)
Chargeability (mV/V)
Resistivity (Ohm.m)
Line 10100 E
Dipole-Dipole Arraya na a
a = 25.0 M
plot point
Resistivity and Chargeability Anomalies
xzxzx zxxxzxx
•Very Strong
Strong
Medium
Weak
•Very Weak
•Extremely Weak
Scale 1:250025 O 25 50 75 100 125 150
——" -J I- (metres)
TAU (msec)
Spectral-M (mV/V)
Chargeability(mV/V)
Resistivity (Ohm.m)
91+50IV 82+00 N 85+00 S 95+SOjf
11=1 0.10ns211=30=40=511=8
11=2 0=3 11=4 ns5 11=8
W - Ts^S^ j8^5^SbS^--54E:^^^^;^ 7^^S^^;^\^^^; ^o. (^^ <^^^^i (upe^t- ff-4*
88+CpS 97+50 N 96+00 N 96+Sfl K 99+OON 100+DOM 100+50N 101400 N 101+60 102+00N 1(8+50 N 03+00 M 104+00 K 104+50 N 105+00 N 105+50N 106+00N 108+60N 107+00 N 107+50 N 108+00 V 106+50N 108+00 109+50 ff 110+00 N 110+50N 111+00 N
6 no 250 O.U no no no no no in 0.10 no o.n 0.10 no no 0,10 0.10 no 119 no no j ion82 us O,M ae no 250 no no it st SK u IA u no no 259 no no no no ut o,ao no 0.10 0.10 no MO no no no no no no no no
u u 6 6 no no no u u 0 .20 OJB no 0,10 0.10 o.u no it no 0.10 no no no 0.10600
40 a " tM 4-u "o w ~ 0.100.10 0,10 0.10 110 0.10 0,10 40 0.40 0.10
129 0.10 62 Itt 0.10 0.10 D.10
no { ~iwj si 1.W ojo nono 0,20 126 0.10 no
10 U 20 82
91+50 N 92+00N 92+50 N 93+00 y 93+50N W+OON 14+50N 95+00 N 95+50N 96+00 N , , 96+90 N r , 97+00 N 97+50N 98+M N 100400 H 100+50 N 108f80N ,103+OON 104+OON 04*801? 105+OON 107400 N 108+OON 109+50N . UO+QON HOiSON llt+flON
1———————————l———————————l————H————^~98+00N 9&+SON 98+00N 99+60 tt 100+00N 100+50 N 101+00 H 101+50 N 102+00 N , 102+50 K 103+00 N 103+60 N 104+00 N 104+60 N ^ t IJDBtqIN 106+00 N .tpeyjog ^ 1107+00 y 107+50 N 108+00 N 106+50 N 109+00 N 109+50 N 110+00 N 110+60 N 111+00 N
114=350,1=2J?i^ a X X H-Sv.B.7 7.1 v 4 M 6.S Ij 8.8 —— 84 7.1 x 1.3
91+50 K 92+00 N 92+50N 99+00N 93+50N 94+00 N 94+50 N 95+00 N 95+50 N 96+00N 98+50 N 97+00 N 97+50 M 98+00N 98+50 N 99+OON 99+50 (f 100+00N 100+50 N 101+00 N 101+50 N 102+00N 102+5011 103+00 N 109+50 N 104+00 N 104+50 N 105+00 N 105+50 N 108+00 N 106+50N 107+00 N 107+50 N 108+00 NVH(Z) VH{4) 0=1,4
r 106+50 WLi H M v, H^
109+00 N 109+60 N 110+00 N 110+50 N 111+00 N0=1/3
,2BI 44E 391/"^\ M /r/x•t^jij^ 431/^^481
W ( 6K 671 681
m ,*f p 2 (^}2K 261^ Sil SH 881- 781
11=111=2 11=33=4
0=6
e 11=1
11=3
0=5
0=6
0=2 11=3 11=4 11=5 0=6
TAU (msec)
Spectral-M (mV/V)
Chargeability (mV/V)
Resistivity (Ohm.m)
Line 10200 E
Dipole-Dipole Arraya na a
a s 25.0 M
plot point
Resistivity and Chargeability Anomalies
xxxxx xxxxxxx.
•Very Strong
' •Strong
"Medium
ITeak
•Very Weak
•Extremely Weak
25Scale 1:2500
25 50 75 100 135 150—— "HSS55SS (metres)
AVALON VENTURES LTD.INDUCED POLARIZATION SURVEY
BATElfAN LAKE PROPERTY, OntarioConmee it Horne Twp., NTS; 52A/12
Date: 07/03/21
JVX LTD. (Ref. 9660, March 1997)
TAU (msec)
Spectral-M (mV/V)
Chargeability (mV/V)
Resistivity (Ohm.m)
——————————————————————————————————— r ——————————————————————————————————————————————————————————————————————————————————————————————— *
93+50 N 94+00 N , 94+50 N ( 96+00 N 95+50 N ( 96+00 N | 96+50^ : 97+00 N ( 97+50 N | 98+00 N | 98+50 N ( 99+00 N | 99+50 N | 100+00 N ( 100+50 N ( 101+00 N | 101+50 N ( 102+00 N | 102+50 N | 103+00 N f 103+60 N ( 104+00 N | 104+50 N f 105+00 N
1
96+50 N 108+00 N 106+90 N 107+00 N 107+50 N 108+00 N 108+50 N 109+00 N 109+50 N 110+00 N 110+90 N | H+OO N 111+50 1*r ' ' ' ' ' ' ' ' ' ' ' ' ' ' ' ' ' ' - ' - ' - ' — ' — ' — --•••" ' ' ' " - ' ' ' ' ' 'V - ' - ' -11=1 500 ^ 250 2.5 0.10 0.10 0.11
93+50 N 94+00N 94+50 N 95+00N 95+50 N 96+00 N 96+50 M 97+00 N 97+50 N 98+00N 96+50 N 99+00 N 99+50 N 100+00 N 100+50N 1+00 N 111+50 N108+50 N 109+00 N 109+50 N 110+00 N
95+50 N 96+00 N 96+501 97+00 N 97+50 N 96+00 N 98+50 N 99+00 N 99+50 N 100+00N 100+50 N 101+00 N 101+50 N 102+00 N 102+50 N 103+00 N 103+50 N 104+00N 104+50 N 105+00 N11=2 1^=382,1=2-4
106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 109+00 N 109+50 N 110+00N 110+50 N 111+00 N 111+50 Nns2
11=336,1=2-8.0 6.7 i 9J v , 3.7 4.1 6J
\u) \1 0^\\2 W, 4,
.6 7 M ——^ 7J \^ SJ ^v 6 f .
4.1 6.3 - 3.8 , 7J U 6.9 5J ^ 3J 3^/47 42 42 — 3J
6.7
49 6.1 43 44 5.8 i 3.3 3.9 2J 32 ^ 3.9 8.4 64 i 9 .5 11 U jtr^sVJ? —- 8.1 —^9.1 ' M w ^ T
3.6 5J 4.7 4.3 4.3 49 41 —— 3.9 6.2 \ 2J
6^6.61 ^
ItW l vat v*m fc
6.7 7.9 9.2 U ix^u u "vi u s r; "^W"^16^^-12 11 13 lT^ 9.4 /'1.6 -^6.7 ' ~'i IB9.6 12 ^ 7J 8.8 6J 4.9 N 7J ^ 8.7 6J
93+50 N 94+00 N 94+50 N 95+00 N 95+50 N 96+00 Nvri(s)
98+50N 97+00 N 97+50 N 96+00 N 98+50 N 99+00 N 99+50 N 100+00 N 100+50 NVE(4)
l———l———l———l———l———l———l 101+00 N 101+50 N | 102+00 N ; 102+50 N '——-VH(4) p .
103+00 N 103+50 N | 1104+00 K VE(3) -^^
104+50 N t 105+00 N —^
, 1^*5+50 N 106+00 N 106+50 N | 107+00 N 11=4,5'"'
107+50 N 108+00N 108+50 N 109+00 N 109+50 N 110+00 N 110+50 N ll+OON 111+90 N
98+50N 97+00 N 97+50 N 96+00 N 96+50 N 99+00 N 99+50 N 100+00N 100+50 N 101+00 N 101+50 N 102+00 N 102+50 N 103+00 N 103+50 N 104+00 N 104+50 N 105+00 N 105+50 N 106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 109+00 N J109+50N 110+00N 110+50N 111+00 N 111+50 N
91+50 N 92+00 N 92+50 N 93+00 N 93+50 N 94+00 N 94+501 98+00 N 96+OON 98+50 N
w-l"s\\\ 92 116 142 149 133 -110
120 148 128
l US ^^110^- 1
1 133^- 10g 107 i
13S KM 121 117
lit W__ 121 ——^33 124 133 102 146
99+00 N 99+50 N 100+00 N 100+50 N 101+00 N 101+50 N 102+00 N 102+50 N 103+00N 103+50 N 104+00 N 104+50 N 105+00 N 105+50 N 106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 109+00 N , U09+50 N
143 > 106121 148 """W^* Til 104 ——106 106
129 ^.113' 146
42 \ MOO 116 92
x .^ 1"iU \ **n133 146 171 ' 187 —-l
110+00 N 110+50 N 111+00 N 111+50 N
136 124 . —— 140 117 67 . —— 87
l t m J S. 148 143 143 133 119 106- 109 116 105 ' p ' 117^ 68
I P - 2
91+50 N 92+00 N 92+50N 93+00 N 93+50 N 94+00 N 94+501 95+00 N 96+OON 96+50 Nnsl
11=451,1=217 8.4 5.4 44
3.8
62 x 94 . 8.9 13 6.7 x 1J
64 7.3 X 6.1 ' x 11 -Ot il -i 17
7.1 4.8 3.7 ' 12 ' ' 26 21 "^ -33
97+00 N 97+50 N 98+00N 98+50 N 99+00 N 99+50 N 100+00 N 100+50 N 101+00 N 101+50 N 102+00 N 102+50 N 103+00 N 103+50 N 104+00 N 104+50 N 105+00 N 105+50 N
IP - 7106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 109+00N 109+50 N 110+00 N 110+50 N 111+00N 111+50 N
44 8,6 32 3.6
X 14 64 13
62 42 (TO 13 16 8.5 7.6 V *2 17 32
20 V\*J 6.1 42 32 6.4 84 7.4 6J 7.6 ~ 13 ^ 3.9 S 2.8 M l 6.1 64 —— 64
(^ \, u ^ i - ^14 6.6 \ 64 64 -*^ 72 X 4 V 1.9 24 l
12 y4J 32 , 7.4 ^ 6.1 46
4.7
M 3.1
3.1 4.7 N 6.3 6.7
13-* 11 8.9 94 10 x " \ " 11 \ 12 j 12
6.2- ^ 14 N 7.7 7.7 /^14^ 8.4 84 12 12 10 82
•9.4 12- 84 x 5.4 6.3 -~^*4. 12 0.72 1.9 0=1
4^~~~- 2.8. O.B5 0=2
sX ——. \ f f
72 17 /IS \ B.8 BJ f 12
74 y \L*S 10 . 8.1—^6.7 i^ \
91+50 N 92+00 N 92+50 N 93+00 N 93+50 N 94+00 N 94+50
n=3/4 H(2)95+00 N 95+50 N 96+OON 98+50 N 97+00 N 97+50N 96+OON 96+50 N 99+00 N 99+50 N 100+00 N 100+50 N 101+00 N 101+50 N 102+00 N 102+50 N 103+00 N 103+50 N
n=2/5 VH(4)- VH(2) VH(4) H(4) -H(2)
184
761-__ 691-—- 741
611 ( 1041 Hit t 871
^^J-^
3SI x/ 5W* as 4*1. Vj?Lx^ **w — 2463^, 7*88 - 111 - Itt —— 161 i; l
104+00N 104+50 N 105+00 N 105+50N 106+00 N 106+50 N 107+00 N^(3)
22* 462, 8*2^( 1836 \ 6873 y 2139 }
107+50 N 106+00N 108+50 N 109+00N 109+50 N 110+00 N 110+50 N 111+00N 111+50 N
f wii auoo X (
IB77 ' 7664 9316 ~
2171 V 8434 ' -
1812 ^4580 ' 8646 - 6408
^?13K \ \ BVAV l WW1V x. ^- wvi s^
1=1/3"
870 406 0=1
Sf-^ 573 0=2^\t~
l 8188J ;2426 0=4
--6424 0=6
2433 0=6
TAU (msec)
Spectral-M (mV/V)
Chargeability(mV/V)
Resistivity (Ohm.m)
Line 10400 E
Dipole-Dipole Array
a = 25.0
plot point
Resistivity and Chargeability Anomalies
zxzxz xxxxxxx.
Very Strong
- Strong
Medium
Weak
Very Weak
Extremely Weak
Scale 1:250025 50 75 100 125 150
S L-
(metres)
AVALON VENTURES LTD.INDUCED POLARIZATION SURVEY
BATEMAN LAKE PROPERTY, OntarioConmee A Horne Twp.. NTS; 52A/18
Date: 97/03/12
JVX LW. (Ret. 9680, March 1997)
TAU(msec)
Spectral-M (mV/V)
Chargeability (mV/V)
Resistivity (Ohm.m)
91+00 N 91+90 N 92+50 N 93+OON 93+50N 94+OON l 94+90 N 95+OON 96+50 N 97+00 N 97+50 N 98+00 N 96+50 N 99+00 N 99+50 N 100+00N . 100+90N . 101+00N . 101+50N . 102+OON . 102+50 N . J03+OON ; 103+50N | 104+00N ; 104+50N f 105+00N f 105+50N | 108+00N ( 106+60N ; 107+00 N ; 107+60N ; 106+00N 108+90 N t09ft N 109+50 N 110+00 N 110+50 N 111+00 N "l+SON
16 0.10
iMO ^ 0.10 0.10 0.10 0.10 0.10 0.10 0.10 0.10 U 1J OJO 0.10 0.10 020 0.10 3.0 OJO OJO 1.00 1.00
' OJO 0.10 0.10 0.10 0.10 0.10 0.10 0.10 0.10 62 0.10 0.80 125 0,10 0.10 OJO 31 62
+OON 91+50N 92+OON 92+S3 N 93+OON 93+50 N 94+OON ^ 94+50 N ( 95+OON , 95+50N f 96+OON ( 98+50 N ( 97+OON | ,97+SON
L98+00 N 96+50 N 99+00 N 99+50 N 100+00 N 100+50 N 101+00 N 101+50 N 102+OON 102+50 N L03+OON , 103+50 N ( 104+00 N : 104+50 N : 105+00 N : 105+50 N ( 106+00 N ( 106+50 N ( 107+00 N ( 107+50 N i 108+00 N : 108+50 N p lOSjM N t 109+50 N 110+00 N | 110+50 N 111+00 N 111+901r
74 68 7 i 116 - 123 123 f 110 121 111 117 118 116 v 121 110
100 111 121\ 118 117 \_121 111
107 117 IDS 110 110 116 100
108 / n .sim __ 108 116
l/ 86/108 (joj^ 108 - 117
M —--108 111 108 ' i 76 ^
;1 ^ 110 108 110 f 00 S 106103 110 106 121 ——119 110 121-
IP-8104+OON ; 104+50N | 109+00 N ; ^OS+SON f 106+OON | 106+90N ( 1107+00 N ( 107+SON ; 106+OON ( 106+90N ; 109^ N ( 109+50N ; 110+OON ( 110+50N ; 111+OON ( .Ul+ftON
EJ 3.8 4.2 / 7J 74 v v 2.3. 0.75 0.24 v. 4.7 s 2 .1 3.6 6.1 74 6.1 ^ -3J8 1.1 -0.77 14 nsl*,6 l IJO t# \ \ 6,3
3.9 U (jj) U \ 2J
3.9 24 If -*- 4.1
4.1 3.3 2.8 /4.0
34 U .s^ *i '
4.7 5J8 ^x
4.9 XU X -04
3.0 6.3 V t6 6.6
5.7 '
0.96 0.70 l 3.6 2.0 ~-^. 14 l 4.3 S U l 14 \ 3.9 S 74 8.6 6.7
^/;y/™//" (^12. f/ -0.61 /,5.4 6
1.4^24 r———2
s. 34 3 "44 6.1 64 —— 64 f / -0.81 /. 6.4 6 5.0 —^
4.7^ 3.1 3.9 4J 54 6 ' '-Q.K 'U 6J -^M 8.7 '
1.4 -0.80 34 6.0 \ 1.7 l 14 X — l ^ 21 -—IB T^- \ 11 77^ '
84 64 4.8 64 W / 3.3 1|
7.0 J 4.3 64 54 f 3.1 2.1
6———6.7 6.4 54 3.9
5.4 /64 54
5.4 6.1 6.8
91+00N 91+50N 92+OON 92+50 N 93+OON 93+50 N 102+90 N
6678 6110 8460 — 3706 26(6611 -411 , 271
W 401 361
171 201 141
Itf IK 171171 161 201
181 211 on J an /va. to. \ m. , Mi y in —111 181/471
IK'' W. 391 (n-"9204 Mn^ la ' ' 66122 321-- -121 ' 6080 ' 2662 2047
iOS+OON 103+50 N 104+00 N 104+50 N 105+00 N 105+90 N 106+00 N 106+90 N 107+00 N 107+50 N 108+00 N 106+50 N 109+50 N 110+00N 110+90 N 111+00 N 111+50 N-VH(2)
1754 3705 — 6841 ( ^-^ f101 Itt 829
Z^p-fr^
TAU (msec)
Spectral-M (mV/V)
Chargeability (mV/V)
Resistivity (Ohm.m)
Line 10500 E
Dipole -Dipole Arraya na a
a = 25.0 M
plot point
Resistivity and Chargeability Anomalies
•Very Strong
Strong
•Medium
•Weak
•Very Weak
•Extremely Weak
35Scale 1:2500
35 50 75 100 125 150sa^-^^s (metres)
AVALON VENTURES LTD.INDUCED POLARIZATION SURVEY
BATEMAN LAKE PROPERTY, OntarioConmee tt Horne Twp.. NTS; 52A/12
Date: 97/03/19
JVXLW. (Ret. 9680, March 1997)
TAU (msec)
Spectral-M (mV/V)
Chargeability(mV/V)
Resistivity (Ohm.m)
91+50 N 82+00 N 92+50 N 93+00 N 93+50N 04+00 N 94+50N 95+00 N 95+50 N 98+00 N 96+50 N 67+00 N 97+50 N 96+OON 98+50 N 99+00 N 99+50 N 100+00 N 100+50 N 101+00 N 101+50 N 102+00N 102+50 N 103+00 N 103+50 K 104+00 N 104+50 N 105+00N 105+50 N 106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 106+50 N 109+00 N 110+00N 110+50 N 111+00 N 111+50 N
97+00 N 97+50 N 98+00 K 96+50 N 99+00 N 99+50 N 100+00N 100+50 N 101+00 N 101+50 N 102+00 N . 102+50 N . 103+00 N . 103+50N . 104+00 K . 104+50 N . 105+00 N , 105+50 N . 106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 109+00 N 110+00N 110+50 N . 111+00 N 111+50 N
' 121 x^* 203 y t 103 86 M 100 66 * 108
J 100 "••138 J 110 VO*M J 103 ( r*// 10S
120 IN ('""w""') 108 —— 111 117-——'m (
124 t6 —— 106 1121. 107 117 \ Tt
S ia\ 1M ( ^}——146 124 t6 —"^106 y 121 107 117r—"\ \ ^ — ^ "Is
133 l 168 \ 111^/1" IU\ Ut l07 m '\ " A fTj CX 1U ~~. 148 151 n, tu 103 ^ n -^ifi X 117
106 \^J61,^- 106 lOB 111
107 /74 J 106 117 11!
,1S6 J 103 17
( rt --v^ioo nr107 IN
to ,tt . n -\ 56 82 X 54 .^ 68 7* N 17
100 ^- U 41 . 101 - 78 -
f 64 ( IsT^^ 66 "^48 J 1
67 67 0=1143 143 107
121 ) 67 __ 74 -— 11 67 67 11 67 \ ill f 146 143 m ' l U 67 67 87 0=2
——117^ 67 87 __ 67 * r 62 ^ lU-^tt /VI*.*//, l }*-——^"
67
1
11=4
0=5
11=6
95+60 N ; 96+00 N ; 96+50 N ( 97+00 N | 97+50 N 96+OON 96+50N . 99+00 N , 99+50 N 100+00 N 100+60 N 101+00 N 101+50 N 102+00 N 102+50 N 103+00 N 103+501 104+00 N 104+50 N 105+00N
IP Zone
105+50 N 106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 106+50 N 109+00 N
15 i OJ 0.8 -- 6.7 6J 7.1 i 34 4J-8.7 6J 7.1 i 34 4J , 2 S
9 g " —— j,j __ j,4 g 3| 3 ——— 3j
16 — 1.1 1.2 5J 5.6 3.1
n=2 M=187 I T=.5
I P - 8110+00 N 110+50 N 111+00N 111+50 N
3.9 4.7 4J 3.6 44 6.3 4.6 , 2.1
4.2 3J 4.1 4.6 34 5.1 6.3 2.6 2J
3 J 3 K SJ 44 4.3 6.6 2.6 2.7
LI -.M 2
N2J
t \ V\ 13 14^ 16 N
2.7 1.6
3.6 \ 2.8 2.7 14
3.7 3.1 1.8
4 3.1 \2.B~) SJ 6.4 4.7 3.3 2.7 f 3J "^ 3 4.2 l 2.4
101+00 N 101+50 N 102+00 N 102+50 N 103+00 N 103+501 104+00N 104+50 N 105+00 N 105+50 N 108+00 N 111+50 NVH(2)
— 2M6
0=1
0=2
0=3
0=4
0=5
0=6
TAU (msec)
Spectral-M (mV/V)
Chargeability(mV/V)
Resistivity (Ohm.m)
Line 10600 E
Dipole-Dipole Arraya na a
a = 25.0 M
plot point
Resistivity and Chargeability Anomalies
xxxxx xxxxxxx
•Very Strong
Strong
'Medium
Ifeak
•Very Weak
•Extremely Weak
25Scale 1:2500
25 50 75 100 125 150 ±i* I- (metres)
AVALON VENTURES LTD.INDUCED POLARIZATION SURVEY
BATEMAN LAKE PROPERTY, OntarioConmee it Horne Twp., NTS; 52A/12
Date: 97/03/19
JVX LTD. (Ref. 9680, March 1997)
TAU
(msec)
Spectral—M (mV/V)
Chargeability(mVA)
Resistivity (Ohm.m)
92+00 N 92+90 N 93+00 N 93+50 N 94+00 N 94+50N 86+50N 96+00 V 96+50N 97+00 N 97+90 N 96+00 N 96+50 N 99+00 N 99+50 N 100+00 N 100+50 N 101+00 N 101+50 N 102+00 N 102+50N 103+00 N 1*3+50 N 104+00 N 104+50 N 105+00N 105+50 N 106+00 V 106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 109flN 109+50 N 110+00 N 110+50 N 111+00 N 111+50N
92+00 N 92+50N 93+00 N 93+50N 94+00 N 94+90 N 95+50 N 98+00 N 96+50 N 97+00 N 97+50 N 98+00 N 98+50N 99+00 N 99+50 N 100+00 N 100+50N 101+00N 101+50 N 102+00 N 102+50 N 103+00N 103+50 N 104+00 N 104+50 N 105+00 N 105+50 N 106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 109+50 N 110+00 N 110+50 N 111+00 N 111+50 N
99+00 N 99+50 N 100+00N 100+50 N 101+00 N 101+50 N 102+00 N 102+50 N 103+00 N 109+50 N 104+00 N 104+50 N 105+00 N 105+50 N 106+00 N 106+50 N 107+00 N 107+50 N 108+00 N 108+50 N 10941) N 109+50 N
Personal Information collect^ Mining Act, the Information i! Questions about this colle* 933 Ramsey Lake Road, Su
Declaration of Assessment Work Performed on Mining LandMining Act, Subsection B5(2) and 6*0), R.S.0.1MO
Transaction Number (office use)x) 9 -y'yA*3y'L
Assessment Files Research ImagImaging
52A12SE0007 2.17459 HORNE 900Instructions: - For work performed on urown uanos oeiorw
- Please type or print In Ink.
1. Recorded holder(s) (Attach a list If necessary)
(3) of the Mining Act. Under section B of the (and correspond with the mining land holder, rthern Development and Mine*, 6th Floor,
use form 0240.
2.17459
2. Type of work performed: Check ( y ) and report on only ONE of the following groups for this declaration.
re* Geotechnical: prospecting, surveys, r—i Physical: drilling, stripping UN assays and work under section 18 (regs) L-1 trenching and associated iassays Rehabilitation
Work Type Office UseCommodity
Total f Value ofWork Claimed ^ //S,
Dates Work Performed \
Dayti ,1 Month | YMT D*y | Month | YMT
NTS ReferenceGlobal Positioning System Data (H available) Township/Area
MlninoQ-Plan Number Resident Geologist ~j\
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 CosiSr4erm 0212;- provide a map showing contiguoMBjfllffljj^ands that are linked for assigning work;- include two copies of your'
3. Pereon or companies who prepared the technical
4. Certification by Recorded Holder or Agent
, do hereby certify that l have personal knowledge of the facts setforth in this Declaration of Assessment Work having caused the work to be performed or witnessed the same during
Its completion and, to the best of my knowledge, the annexed report is true.
AgerffTMdreee77*7 Telephone Numbe.
0.1*
~. **oi* it DC fecotufca ana aistnouiea. Work can only be assigned to claims that are contiguous (adjoining) to the mining land where work was performed, at the time work was performed. A map showing the contiguous link must accompany this form.
Mining Claim Number. Or ifwork was done on other eligible mining land, show in this column the location number Indicated on the claim map.
eg
eg
eg
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
TB 7827
1234567
1234568
J Z Z. If? 2-3'
li 7 3W7-i "7 *O /J CSf "7 ~"^ *
1 s\ —y fi Ci J l* *
12.2-^?^-
l 1^107'
\ Z-l 5*O/ ^'/Z) 50! l 'l ZZ^6^3 -l Z- 2.4 6^(9-12150/0-l ZZ-^tf)-
IZI 5O l 3I 2- l S O l q*-\-2~\0 "if -2-l Z- 2. f 6 7 L,l 2- ^ ^ 67 ^
Number of Claim Units. For other mining land, list hectares.
16 ha
12
2
U
V
^
2.
l
Z.
l Z1 1
6l 5l (9; 5l Z.xs
/Y' S
Column Totals-v —-^
Value of work performed on this claim or other mining land.
S26, 825
0
S 8, 892
1,1 kOW t SOO
1 O f 200
l&i ^OO
i o 3ooZ. &OO
2 & GO
lozzS 20(p5 "2-OQ
22-^72
11^17
Value of work applied to this claim.
N/A
S24,000
14,000
MOO-5-2-00^00l booLiZOOUoO
HOO5~S3
1 3 GsooS3 3sooHOO"2- fc -?Zfe 7
433
z6,S4^rr
Value of work assigned to other mining claims.
S24,000
0
0
1^33
7^33
Bunk. Value of work to be distributed at a future date.
52,825
0
14,892
1LO\ / , ?oo6,000^^oo
\~^ } 7OO^^oo2- ~2-O*9
2. O ^ 78" ^1H7c)^tf^ 7
2dP 4^9
^s.szzV i-
(Print Full Name), do hereby certify that the above work credits are eligible under
subsection 7 (1) of the Assessment Work Regulation 6/96 for assignmentto-contiguous claims or for application to
the claim where the work was done.Signature~of-^ecorded
f )
orized in Writing Data
6. Instructions for cutting back credits that are not approved.
Some of the credits claimed in this declaration may be cut back. Please check ( ^ ) in the boxes below to show howyou wish to prioritize the deletion of credits:
D 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
D 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):
^ote: 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.
:or Office Use Onlytecehrad Stamp Deemed Approved Date
y 3/,/ff?Thunder Ba,v Mining Division
MAY - 2 1997"RECFJVF.n
Data Approved
Data Notification Sent
Total Value of Credit Approved
Approved for Recording by Mining Recorder (Signature)
Personal information collected on this form Is obtained under the authority of subsection 8(1) of the Assessment Work Regulation 6/96. Under section B of the Mining Act. the information is a public record. This information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed lo the Chief Mining Recorder, Ministry of Northern Development and Mines, 6th Floor, 933 Ramsey Lake Road, Sudbury, Or.tarlo, P3E 6B5.
Work Type
IT P SlX^l/^y
SuPFTSLiyi^J/OA^
Units of WorkDepending on the type of work, list the number of hours/days worked, metres of drilling, kilo metres of grid line, number of samples, etc.
B;.3z,5k^
Associated Costs (e.g. supplies, mobilization and demobilization).
-
Transportation Costs t p /") \S
Food and Lodging Costs
iiiiindu-rh,-., -.lining Di vis;. .
Cost Per Unitof workt
^2073
35^/fcW
^r.f'.M-'-* i \™~ '- -"
MAY - 2 1QQ7 Total Value of Assessment Work
Total Cost
loipon
H,Zde
•2.I7
H2-, Hn
Calculations of Filing Discounts:
1. Work filed within two years of performance is claimed at lOO'Vb of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at 50*yb of 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 $ 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 45 days 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 verifyingcosts:
1)^ u fc L4
A i
, do hereby certify, that the amounts shown are as accurate as mayprint lull 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.holder, agent, or state company position with signing authority)
l am authorized
Date
*.' *\
o
O
Ministry ofNorthern Developmentand Mines
Ministere du Developpement du Nord et des Mines
September 22, 1997
DONALD MURRAY LEISHMAN 204 ANTEN STREET THUNDER BAY, Ontario P7B-5J6
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.
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 Lucille Jerome by e-mail at [email protected] or by telephone at (705) 670-5858.
Yours sincerely,
ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section
Work Report Assessment Results
Submission Number: 2 .17459
Date Correspondence Sent: September 22, 1997___________________Assessor:Lucille Jerome^^^^^^^^^^
Transaction First ClaimNumber Number Township(s) l Area(s) Status Approval DateW9740.00246 1224923 HORNE, CONMEE Approval After Notice September 22, 1997
Section:14 Geophysical IP
The 45 days outlined in the Notice dated July 30, 1997 have passed.
Assessment work credit has been approved as outlined on the attached Distribution of Assessment Work Credit sheet.
Correspondence to: Recorded Holder(s) and/or Agent(s):Resident Geologist Douglas P. ParkerThunder Bay, ON THUNDER BAY, ONTARIO
Assessment Files Library DONALD MURRAY LEISHMAN Sudbury, ON THUNDER BAY, Ontario
KENNETH GEORGE FENWICK THUNDER BAY, ONTARIO
SCOTT ALEXANDER CHRISTIANSON THUNDER BAY, ONTARIO
STEPHEN A STARES THUNDER BAY, Ontario
AVALON VENTURES LTD. THUNDER BAY, ONTARIO
Page: 1Correspondence ID: 11337
Distribution of Assessment Work Credit
The following credit distribution reflects the value of assessment work performed on the mining land(s).
f M,R.O. - .--'iNlNS RIGHT5 ONLY S R.O. - SURFACE RIGHTS ONLY M.+S. - taMNG A*f SURFACE RIGHTS
Dawson Road Lots G-649
o oCM
NCfTlCE:Thu tnfarmatbn that appear* on thb mop hw b*en from vortcui. .cures* and accuracy b not guarantcxL e** wUhlng lo jttqiu MINING CLMMS ificNiM ooMNlt with tt. MHNfl RECORDER. Ministry of Northwn D.vrtgpm*nt and Mto*s. for li
Information on HM VMm of tha land* *homi (raman
173911 173912
739 3
M739I41173915
224
1215013 1210316
1215012 12150141207877 I2I50II2I02
1205117120^118
1209578
i I205T;I9
l Ei 5 2 51120^244 H08245 1205173
Adrian Twp. G-640
LEGENDHIGHWAY AND ROUTE No
OTHER ROADS
TRAILS
SURVEYED LINES:TOWNSHIPS, BASE LINES, ETC.LOTS. MINING CLAIMS. PARCELS, ETC
SAND 81 GRAVEL .........._............—.———-LAND USE PERMITS FOR COMMERCIAL TOURISM. OUTPOST CAMPS
NOTE: MINING RIGHTS IN PARCELS PATENTED PRIOR TO MAY 6.1913. VESTED IN ORIGINAL PATENTEE BY THE PUBLICLANDS ACT. R.S.O. 1970, CHAP. 380. SEC. 63. SUBSEC 1.
NOTICE:The Information that appears on this map has been compiled from various sources and accuracy Is not guaranteed. Those wishing to stake MINING CLAIMS should consult with the MINING RECORDER. Ministry of Northern Development and Mines, for additional information on the status of the lands shown hereon.
LEGENDHIGH'AAv A N( [, R, j, (if M,,
OTHEH Hi;.A[)S
TRAILS
SURVEY tp LINESTOWNSHIPS HAst i 'fas t f i. lOTS MlN'.fjo -"i "Ai^ ^AP.ttriS
' JNSUR - t r 1 1- L iNr -,
LO T i iNtS PARCt l B()UN[iAR
MINING CL AIMS E 1C RAILWAY AND RIGHI OK AA -UTILITY L iNES
NON PERENNIAL STRtAM
F LOGGING OR F l OOOiNG H IGHTS
SUBDIVISION ORCCJMPOblTE PLAN
RfcStRVATHjNS
ORIGINAL SHORELINE
MARSH OR MUSK 1 1,
MINES
TRAVERSE MONUMENT
h i r
DISPOSITION OF CROWN LANDS
TYRE OF DOCUMENT SYMBOL
PATENT SURf- AC.E g, MINiN( ; HK,H TS
siiHFACE RIGHTS ONL >MINING RIGHTS ONLV w
LEASE SURFACE 81 IV1INING RIGH T S B
SURFACE RIGHTS ONL r H
MINING RIGHTS ON L r C
LICENCE'.)' OC(.v.'PA T li IN T
ORDER iN cAJiJNC li OC
RESERVATION '*
CANCEL L! "
SAND S G H AV 1 1 ' LAND USE PERMITS FOR COMMERCIAL TOURISM. OUTPOST CAMPS
NOTE It/I l N l N i i R ir'i H r S "- p A t' l t l.S " A T t N ' E : l P H - P ' V a .
'913 v e s i E n - N " ' N A i. " * T E N i e f e * ™ t ^ ' B .LANDS A( T R s "J 'O i ~ " A B 38O S fC 63 S- 8StL