Geologic cross-section of the Wilder creek target, and hand sample photograph of copper-silver sulfide melt interstitial to quartz and K-feldspar grains in granite dyke, Junction Property, Nevada. The schematic drill hole targets the high resistivity core of the concentric magnetic ring anomaly shown in the previous two figures, as a potential mineralized source body to the numerous copper-bearing dykes mapped at surface.
Geologic cross-section of the Wilder creek target, and hand sample photograph of copper-silver sulfide melt interstitial to quartz and K-feldspar grains in granite dyke, Junction Property, Nevada. The schematic drill hole targets the high resistivity core of the concentric magnetic ring anomaly shown in the previous two figures, as a potential mineralized source body to the numerous copper-bearing dykes mapped at surface.