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32E04SE0035 - Geology Ontario

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5<br />

intermediate tuff. The anomaly on grid A-6-7 is explained by<br />

three bands of sulphide-magnetite-cherty iron formation over a<br />

width of 0.5 to 2.13 metres. The best assay was in the cherty<br />

iron formation which returned a value of 306 ppb Au over a width<br />

of 0.91 metres from the core.<br />

A total of four diamond drill holes on grids A-3, A-6-7 and A-8-9<br />

during 1990<br />

and 1991 adequately investigated the conductors with<br />

negative rsults. No further exploration on the grids is<br />

recommended.<br />

Anomaly A-5 has not been adequately tested by previous diamond<br />

drilling (See Map No. S-91-304- Compilation Map). The new<br />

airborne<br />

electromagnetic survey by the <strong>Ontario</strong> government more<br />

adequately defines this anomaly. A small grid of 3.2 km is<br />

recommended to explore this anomaly on the ground with HEM and<br />

magnetic surveys.

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