There is a high resistivity body in the magnetic high core of the concentric magnetic ring feature at Wilder Creek. The concentration of more than one dozen mineralized granite dykes in the core of the ring feature have a strike length in excess of one kilometre. 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).
There is a high resistivity body in the magnetic high core of the concentric magnetic ring feature at Wilder Creek. The concentration of more than one dozen mineralized granite dykes in the core of the ring feature have a strike length in excess of one kilometre. 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).