“…Generally in epithermal deposits sulfides are frequently reported as the dominant ore minerals in association with native gold; whereas significant dominance of tellurides accompanying gold is less observed. However, when highly concentrated throughout, or in limited parts of a deposit, Au-(Ag) tellurides may themselves constitute highly economic ores (Cook and Ciobanu, 2005;Cook et al, 2009). In numerous large gold deposits worldwide, Au-(Ag) tellurides comprise an abundant component of ore minerals and may also contribute a significant portion of the overall gold balance, such as observed in the Cripple Creek and Golden Sunlight deposits in USA (Thompson et al, 1985;Porter and Ripley, 1985), the Emperor deposit in Fiji (Ahmad et al, 1987;Pals and Spry, 2003), the Dongping and Dashuigou deposits in China (Mao et al, , 2003, the Acupan and Baguio deposits the GHR region (Fig.…”