Plan map (upper) and north-south section (lower) of the recent 3D array DCIP survey at Silverback, with locations for drill holes completed in the spring of 2024, and for those planned and now underway in 2025. The plan map shows IP isoshells at 12.5 mV/V (orange) and 15 mV/V (red) on a basemap with inferred shear-zones and outline of the mafic dykes and intrusions with copper-nickel sulfides which span the entire property. The central and largest IP anomaly, CZ, correlates with the strongest shear-fabrics observed in outcrop, and magnetic destruction evident in the gap in magnetic contours on the plan map and are potentially the result of hydrothermal alteration.
Plan map (upper) and north-south section (lower) of the recent 3D array DCIP survey at Silverback, with locations for drill holes completed in the spring of 2024, and for those planned and now underway in 2025. The plan map shows IP isoshells at 12.5 mV/V (orange) and 15 mV/V (red) on a basemap with inferred shear-zones and outline of the mafic dykes and intrusions with copper-nickel sulfides which span the entire property. The central and largest IP anomaly, CZ, correlates with the strongest shear-fabrics observed in outcrop, and magnetic destruction evident in the gap in magnetic contours on the plan map and are potentially the result of hydrothermal alteration.