|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.