At Wilder Creek, surface copper-silver showings are related to a concentration of granite dykes which occur within the core high of a concentric magnetic ring anomaly more than two kilometres in diameter. Figure 3 shows the correlation of the magnetic high core of concentric ring feature with a high resistivity body. Permitted drill hole locations are shown, and will provide a first pass test of the magnetic, resistive core anomaly as a potential mineralized source body to the numerous mineralized granite dykes mapped at surface (see photo in Figure 4).
At Wilder Creek, surface copper-silver showings are related to a concentration of granite dykes which occur within the core high of a concentric magnetic ring anomaly more than two kilometres in diameter. Figure 3 shows the correlation of the magnetic high core of concentric ring feature with a high resistivity body. Permitted drill hole locations are shown, and will provide a first pass test of the magnetic, resistive core anomaly as a potential mineralized source body to the numerous mineralized granite dykes mapped at surface (see photo in Figure 4).