Isotopic (C-O-S) geochemistry and Re-Os geochronology of the Haobugao Zn-Fe deposit in Inner Mongolia, NE China

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• 作者：Yuan Liu^a ; Si-Hong Jiang^a ; ^{jiangsihong1@163.com} ; Leon Bagas^a ; ^b ; Ning Han^a ; Chun-Liang Chen^a ; Huan Kang^a
• 关键词：C&ndash ; O&ndash ; S isotopic geochemistry ; Re&ndash ; Os dating ; Electron microprobe analyses ; Haobugao Zn&ndash ; Fe deposit ; Great Xing&rsquo ; an Range ; NE China
• 刊名：Ore Geology Reviews
• 出版年：2017
• 出版时间：April 2017
• 年：2017
• 卷：82
• 期：Complete
• 页码：130-147
• 全文大小：7748 K
• 卷排序：82

文摘

Petrography and EMPA indicate that the sphalerite has three generations. The ore fluid was deep magmatic in origin mixing with minor meteoric water. The Zn-Fe mineralization is related to an extensional setting during the Mesozoic.