Geochronology, geochemistry, fluid inclusion and C, O and Hf isotope compositions of the Shuitou fluorite deposit, Inner Mongolia, China
文摘
The Shuitou fluorite deposit was formed at 132 ± 11 Ma. The ore-forming fluids can be mainly attributed to NaCl–H2O system. Data suggest that the Shuitou deposit is hydrothermal vein-type deposit. The nearly synchronous magmatic events might have provided the heat source for fluorite mineralization. The deposit is closely associated with the late Jurassic to early Cretaceous magmatism events in the SGXR.