● Pyroxenite-hosted Ni-Cu-PGE surface showing with historical grab samples returning up to 2.64% Cu + 0.49 % Ni + 3.44 g/t Pt-Pd-Au
● Historical drill intersections (2008) including 0.38% Ni + 0.44% Cu + 0.65 g/t Pt-Pd-Au over 20.7 metres
● Nearby strongly sheared + quartz-carbonated veined mafic volcanic-hosted gold showing with historical grab samples yielding up to 24 g/t Au
Ducros Sill Complex
● Limited drilling (three holes) in the 1980’s encountered an interpreted 3.5 km long and up to 700-metre-wide ultramafic sill with anomalous nickel values
● Regional QC government geophysical data and GIS compilation work indicate over 30 line-kilometres of ultramafic sills with coincident or flanking electromagnetic anomalies never drill tested
Ducros Gabbro
● Poorly exposed ~ 5 km X 5 km mafic intrusion largely inferred from regional magnetic data
● Interpreted to be emplaced along intersecting deep-seated regional structures (regional magnetics)
● Magnetic data suggest the body is layered and/or multi-phased
● Never drilled
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