Geochemical data from drill holes 007 and 008 at the Kawich IP anomaly. There are broad intervals of elevated, hydrothermal gold within the broad intersections of pyrite alteration in both holes. The high temperature signature of Ag-Cu-Mo-W typical of magmatic porphyry systems is strongest in hole RV21-007. The pyrite alteration and contained polymetallic mineralization at Kawich are capped by impermeable andesite flows (green) and a strongly clay altered dacite tuff (yellow), and are focused along stratigraphic contacts and brecciated thrust fault boundaries (red, pink and orange).
Geochemical data from drill holes 007 and 008 at the Kawich IP anomaly. There are broad intervals of elevated, hydrothermal gold within the broad intersections of pyrite alteration in both holes. The high temperature signature of Ag-Cu-Mo-W typical of magmatic porphyry systems is strongest in hole RV21-007. The pyrite alteration and contained polymetallic mineralization at Kawich are capped by impermeable andesite flows (green) and a strongly clay altered dacite tuff (yellow), and are focused along stratigraphic contacts and brecciated thrust fault boundaries (red, pink and orange).