A combined fluid inclusion and isotopic geochemistry study of the Zhilingtou Mo deposit, South China: Implications for ore genesis and metallogenic setting

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• 作者：Guo-Guang Wang^a ; Pei Ni^a ; ^{peini@nju.edu.cn} ; Chao Zhao^a ; Hui Chen^a ; ^b ; Hui-Xiang Yuan^b ; Yi-Tao Cai^a ; ^c ; Li Li^a ; An-Dong Zhu^a
• 关键词：Fluid inclusion ; H&ndash ; O&ndash ; Pb isotopes ; Zhilingtou Mo deposit ; Endako type ; South China
• 刊名：Ore Geology Reviews
• 出版年：2017
• 出版时间：March 2017
• 年：2017
• 卷：81
• 期：part_P2
• 页码：884-897
• 全文大小：3549 K
• 卷排序：81

文摘

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.