Figure 11 – Typical Au-Ag-Cu mineralisation in drill hole CHT-DDH-044 (Breccia Clint)
Chaotic to shingle quartz-tourmaline breccia with local clasts being replaced by pyrite and chalcopyrite with chalcopyrite-pyrite-arsenopyrite mineralisation. From a sample interval (183.86 to 184.8 m) that returned 0.35 g/t Au, 15.4 g/t Ag and 1.87 % Cu. Photograph is of a selected interval and is not necessarily representative of mineralisation hosted throughout the property.
Format
PNG
Quelle:
Turmalina Metals Corp.