Geochronology, geochemistry, fluid inclusion and C, O and Hf isotope compositions of the Shuitou fluorite deposit, Inner Mongolia, China

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• 作者：Qiuming Pei^a ; ^b ; ^{peiqm2014@cugb.edu.cn} ; Shouting Zhang^a ; ^{zst@cugb.edu.cn} ; M. Santosh^a ; ^c ; Huawen Cao^d ; Wei Zhang^e ; Xinkai Hu^a ; Liang Wang^a
• 关键词：Fluorite deposit ; Sm&ndash ; Nd dating ; Zircon U&ndash ; Pb geochronology ; C&ndash ; O isotopes ; Fluid inclusions
• 刊名：Ore Geology Reviews
• 出版年：2017
• 出版时间：April 2017
• 年：2017
• 卷：83
• 期：Complete
• 页码：174-190
• 全文大小：4351 K
• 卷排序：83

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.