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32E04SE0035 - Geology Ontario

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17<br />

7.0 DISCUSSION OP RESULTS<br />

Interpretation of the induced polarization survey by Belanger has<br />

resulted in four anomalous I.P. zones, two of which warrant<br />

follow-up as follows:<br />

1) I.P. anomaly No. l<br />

Anomaly No. l on line 6 Bast at O to l North is a one line<br />

anomaly with low resistivity (28 OM), high phase (3 MRAD) and<br />

high metal factor (42.9).<br />

This I.P. anomaly may be caused by an alteration zone (silicified<br />

and carbonatized) along a fault zone similar to the zone in hole<br />

No. LR-87-1 on section 8E but stronger pyrite mineralization.<br />

2) I.P. anomaly No. 2<br />

Anomaly No. 2 on lines 8E, 10E, 13E and 15E at 3N to 5+50N has<br />

high phase (3.7 MRAD) and high resistivity (2249 OM). Line 10E is<br />

the exception in that this line<br />

has high phase (3.7) and high<br />

metal factor (39.4) with low resistivity (70). Line<br />

10E and 13E<br />

has the highest phase while line 13E has the highest resistivity.<br />

This I.P. anomaly may be caused by a silicified zone along a<br />

fault with disseminated pyrite.

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