IP profile across the 3D inversion block model at Amsel, with the high resistivity iso-surface from Figure 1 draped on top. The zones of high resistivity correlate with a welded tuff interpreted to have formed an impermeable alteration cap above the IP anomaly. The strongest multi-element soil geochemistry anomaly including gold, silver and molybdenum within the 2 x 3 km surface grid, and the strongest concentration of high temperature muscovite and adularia alteration minerals in rocks occurs directly above the IP anomaly west of the hilltop which extends from surface to depth in 3D block model, and is the primary target for a large body of pyrite-bearing quartz vein stockworks with epithermal gold and silver mineralization, akin to the rock photograph in Figure 4.
IP profile across the 3D inversion block model at Amsel, with the high resistivity iso-surface from Figure 1 draped on top. The zones of high resistivity correlate with a welded tuff interpreted to have formed an impermeable alteration cap above the IP anomaly. The strongest multi-element soil geochemistry anomaly including gold, silver and molybdenum within the 2 x 3 km surface grid, and the strongest concentration of high temperature muscovite and adularia alteration minerals in rocks occurs directly above the IP anomaly west of the hilltop which extends from surface to depth in 3D block model, and is the primary target for a large body of pyrite-bearing quartz vein stockworks with epithermal gold and silver mineralization, akin to the rock photograph in Figure 4.