32E04SE0035 - Geology Ontario

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8.0 CONCLUSIONS AND RECOMMENDATIONS
Hole No. PR-91-1 on grid A-3 investigated the coincident HEM,
magnetic and gold in humus geochemical anomaly. The magnetic
conductor is caused by ID-15% disseminated pyrrhotite, minor
pyrite and traces of chalcopyrite over a width of 1.62
metres in
a cherty banded tuff. The gold and copper assays of the core are
very low. The gold in humus geochemical anomaly of seven times
background over the conductor is unexplained.
Hole No. PR-91-2 on grid A-8-9 explored the coincident weak HEM
and gold in humus geochemical anomaly. The weak conductor is
caused by 2-3% disseminated pyrite over a width of 5.85 metres in
a banded intermediate to mafic tuff. The gold in humus
geochemical anomaly of eight times background is unexplained.
Hole No. PR-91-3 on grid A-6-7 investigated the strong HEM
anomaly on line 1+OOE. The conductor is caused by three
bands of
sulphide-magnetite-cherty iron formation over widths of 0.5 to
2.13 metres in amphibolitic basalt. The cherty iron formation
contains 15% pyrrhotite and 20% magnetite. The best assay of
cherty iron formation is 306 ppb Au over 0.91 metres. This drill
hole is a follow-up to hole No. PR-90-1 on section 2+OOW which
returned an assay of 396 ppb over a metre. The assays from the
two holes 300 metres apart are comparable but weak.