Fluid inclusions and isotopic characteristics of the Jiawula Pb–Zn–Ag deposit, Inner Mongolia, China
Journal of Asian Earth Sciences（2015）
Abstract
•The sulfide Rb–Sr isochron age of the Jiawula deposit is ca. 143–142Ma.•The ore-forming fluids are medium–low temperature and variable salinity fluids.•The ore-forming fluids are mainly meteoric water with minor magmatic water.•The ore-forming materials mainly came from the Mesozoic magma.•The deposit is a low-sulfidation epithermal Pb–Zn–Ag deposit.
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Key words
Sulfide Rb–Sr dating,Fluid inclusion,H–O–S–Pb isotopes,Low-sulfidation epithermal Pb–Zn–Ag deposit,Jiawula,Inner Mongolia,Northern Great Xing’an Range
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