Long section through the high-grade Copper Hill deposit demonstrating the relationship between veins hosting the high-grade mineralisation and low angle structures. These b-veins are zoned symmetrically around Nanooks Fault strongly suggesting they formed during movement on that fault. Mapping this fault and others of similar orientation through the Mining lease becomes a critical tool for identifying and expanding high-grade mineralisation.
Long section through the high-grade Copper Hill deposit demonstrating the relationship between veins hosting the high-grade mineralisation and low angle structures. These b-veins are zoned symmetrically around Nanooks Fault strongly suggesting they formed during movement on that fault. Mapping this fault and others of similar orientation through the Mining lease becomes a critical tool for identifying and expanding high-grade mineralisation.