A combined fluid inclusion and isotopic geochemistry study of the Zhilingtou Mo deposit, South China: Implications for ore genesis and metallogenic setting
Fluid boiling induced the deposition of molybdenite. CO2-poor fluids and arc lithogeochemical affinity indicate an arc setting. H–O–Pb isotopes suggest that ore fluids were primarily magmatic in origin. The Zhilingtou deposit is an Endako-type porphyry Mo deposit in South China.