Drill core examples from Holes 3, 4 and 8, roughly 1,700 meters apart along strike of an important, northeast-trending shear zone, and also 700 apart north-south, on opposing margins of the large mafic-ultramafic body. They demonstrate widespread chlorite-sericite-silica alteration with finely disseminated sulfides and quartz-carbonate veining related to shearing across the property. The protolith rock is nearly unrecognizable due to intense hydrothermal alteration overprint combined with ductile deformation on the structures trending northeast through the property. Drill core diameter is NQ.
Drill core examples from Holes 3, 4 and 8, roughly 1,700 meters apart along strike of an important, northeast-trending shear zone, and also 700 apart north-south, on opposing margins of the large mafic-ultramafic body. They demonstrate widespread chlorite-sericite-silica alteration with finely disseminated sulfides and quartz-carbonate veining related to shearing across the property. The protolith rock is nearly unrecognizable due to intense hydrothermal alteration overprint combined with ductile deformation on the structures trending northeast through the property. Drill core diameter is NQ.