Tandai Geology

Tandai is interpreted to represent an intermediate-sulphidation system with gold-silver mineralisation hosted by a series of veins and breccias distributed over a vertical extent exceeding 500m. Three major east west trending mineralised lineaments are identified within the Tandai Area and the known strike extent approximates to >10km. These include the Toko Rotan, Lebong Tandai and Glumbuk structures. All three structures have varying grades and widths of mineralisation. A small amount of mining activity has taken place at Glumbuk, with Toko Rotan remaining undeveloped due to low surface gold grades.