Origin of the Dongga Au deposit in the giant Xiongcun porphyry Cu-Au district, Tibet, China: Constraints from multiple isotopes (Re, Os, He, Ar, H, O, S, Pb) and fluid inclusions

The Dongga Au deposit (9.55 t Au; average grade = 6.9 g/t [up to 61.6 g/t]) is located in the Xiongcun giant porphyry Cu-Au district of the Gangdese porphyry Cu belt, Tibet. Its mineralization age, ore-forming processes, and relationship to adjacent porphyry mineralization remain unclear. To address this, we conducted a geological, pyrite Re-Os dating, He-Ar-H-O-S-Pb isotopic, and fluid inclusion study of the Dongga deposit. Pyrite samples from ore-bearing chlorite-sulfide veins yielded a weighted-mean Re-Os age of 178.4 +/- 2.6 Ma (MSWD=0.01), implying the deposit formed during the Early Jurassic. Fluid inclusion analyses yielded homogenization temperatures of 237-360 degrees C for quartz-sulfide veins and 125-201 degrees C for late quartz veins, with corresponding salinities of 2.7-43.8 and 0.9-9.9 wt% NaCleq, respectively. Fluid inclusion analyses of pyrite samples yielded 3He/4He and 40Ar/36Ar values of 0.50-1.08 Ra and 325.1-559.4, respectively, and delta D and delta 18Ofluid values of -86.2 %o to -72.1 %o and -5.6 %o to 3.9 %o, respectively. The He-Ar-H-O isotopic data suggest the mineralizing fluids were derived mainly from a crustal source with a small mantle contribution, and also contained a mixture of magmatic and meteoric waters. The S (delta 34S = -1.57 %o to -0.55 %o) and Pb (206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb are 18.17-18.41 %o, 15.55-15.63 %o and 38.15-38.37 %o, respectively) isotopic compositions of pyrite suggest the ore-forming metals were derived from a magma source in the mantle containing minor amounts of subducted sediment. Based on the geology, and isotopic and fluid inclusion data, we infer that mixing between magmatic and meteoric waters was the main trigger of Au precipitation. In addition, based on the geochronological, spatial, and genetic relationships with the adjacent No.2 deposit in the Xiongcun ore district, we propose that the Dongga Au deposit is a sub-epithermal deposit, which represents the transition between porphyry and epithermal deposits. The two deposits constitute a porphyry system and record the continuous evolution of hydrothermal fluids transported outwards in a porphyry system.