Schematic section of high temperature mineral alteration vectors towards Kawich in the covered valley off the western flank of the range as the potential center and proximal source area for the overall polymetallic mineral system at Reveille based on data from the complete hyperspectral scanning of each of the 9 drill holes shown in Figure 1, in their entirety. Clay alteration and jasperoid development are stronger, occur over wider intervals, and are found at greater depths within the Kawich target area.
Schematic section of high temperature mineral alteration vectors towards Kawich in the covered valley off the western flank of the range as the potential center and proximal source area for the overall polymetallic mineral system at Reveille based on data from the complete hyperspectral scanning of each of the 9 drill holes shown in Figure 1, in their entirety. Clay alteration and jasperoid development are stronger, occur over wider intervals, and are found at greater depths within the Kawich target area.