Geological, fluid inclusion and isotopic studies of the Baiyangping Pb-Zn-Cu-Ag polymetallic deposit, Lanping basin, Yunnan province, China
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- 作者：Xiao-Hu Wanga ; wangzykc@yeah.net" class="auth_mail" title="E-mail the corresponding author ; Zeng-Qian Houb ; Yu-Cai Songb ; Hong-Rui Zhangb
- 关键词：Geological features ; Fluid inclusions ; C&ndash ; O&ndash ; S&ndash ; Pb isotopes ; Baiyangping deposit ; Lanping basin ; SW China
- 刊名：Journal of Asian Earth Sciences
- 出版年：2015
- 出版时间：1 November 2015
- 年：2015
- 卷：111
- 期：Complete
- 页码：853-871
- 全文大小：6706 K
文摘
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The ore-forming fluid was derived mainly from meteoric water with formation water.
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The sulfur in ore was produced by organic thermochemical sulfate reduction and decomposed the sulfur-bearing organic matter.
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The lead and zinc were derived from the sedimentary strata and the basement rocks but indirectly from mantle.
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Two mineralization events resulted in the diversity of ore-forming elements.