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Dyment 3

The Dyment 3 zone is located west-southwest of the 55 Zone in a similar sedimentary geological setting. Mineralization is hosted in discrete quartz and quartz-carbonate veins and stringers of varying widths and orientations, accompanied by sericite/ankerite alteration. Several syenitic and quartz feldspar porphyry dykes have been intersected. Pervasively hematized, moderately sericitized and blocky intervals (fault zones) were also intersected close to the ultramafic volcanic/Timiskaming sediment contact.

Drill hole intercepts from seven historical holes (1,459 metres) include 2.08 g/t over 2.55m and 5.04 g/t over 0.4m.

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This page was created on Tue Dec 12, 2017 at 5:43:05 PM Pacific Time.