Fluid inclusion and H-O-S-Pb isotopic evidence for the Dongxiang Manto-type copper deposit, South China
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- 作者：Yi-Tao Caia ; b ; Pei Nia ; peini@nju.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Guo-Guang Wanga ; Jun-Yi Pana ; Xiao-Ting Zhua ; b ; Hui Chena ; c ; Jun-Ying Dinga
- 关键词：Ore genesis ; Fluid inclusions ; H&ndash ; O&ndash ; S&ndash ; Pb isotopes ; Dongxiang copper deposit ; South China ; Manto deposit
- 刊名：Journal of Geochemical Exploration
- 出版年：2016
- 出版时间：December 2016
- 年：2016
- 卷：171
- 期：Complete
- 页码：71-82
- 全文大小：2540 K
文摘
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Ore bodies in sandstone and shale occur as stratoid and lenticular massive sulfide.
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Ore-forming fluids are derived from magmatic waters.
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Fluid boiling induced metal precipitation from hydrothermal solutions.
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It is a Jurassic manto-type deposit instead of a Carboniferous Sedex deposit.