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32E04SE0035 - Geology Ontario

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18<br />

8.0 CONCLUSIONS AND RECOMMENDATIONS<br />

The induced polarization survey on the Lightning River property<br />

has outlined some interesting anomalies along the North Branch of<br />

the Destor-Porcupine Fault that warrants exploration for gold.<br />

The I.P. anomalies that warrant follow-up are as follows:<br />

1) Anomaly No. 1:<br />

This is a one line anomalous I.P. zone on line 6B from O to IN<br />

with moderate phase, metal factor and low resistivity but open<br />

along strike. This may be caused by pyrite and alteration along a<br />

fault.<br />

2) Anomaly No. 2<br />

This zone is an I.P. anomaly with high phase and high resistivity<br />

over a strike length of 800 metres and open. Line 10E has high<br />

metal factor, phase and low resistivity. This zone may be<br />

strongly silicified with pyrite mineralization.<br />

The model for this property is a gold-pyrite deposit associated<br />

with silicified and carbonatized alteration along the North<br />

Branch of the Destor-Porcupine Fault similar to the Harker-<br />

HolIoway model.<br />

Hole No.<br />

LR-87-1 on section 8E encountered 73 ppb Au over 3.99 m<br />

within a silicified and carbonatized zone over 22.13 m on the

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