Geochronology, fluid inclusions and isotopic characteristics of the Chaganbulagen Pb-Zn-Ag deposit, Inner Mongolia, China
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- 作者：Tiegang Lia ; b ; Guang Wub ; wuguang65@163.com" class="auth_mail" title="E-mail the corresponding author ; Jun Liub ; Guorui Wangb ; Yanqing Huc ; Yunfu Zhangc ; Dafeng Luoc ; Zhihao Maoa ; Bei Xud
- 关键词：Sericite 40Ar ; &minus ; 39Ar age ; Zircon U&ndash ; Pb age ; Fluid inclusion ; H&ndash ; O&ndash ; S&ndash ; Pb isotopes ; Chaganbulagen Pb-Zn-Ag deposit ; Inner Mongolia
- 刊名：Lithos
- 出版年：2016
- 出版时间：15 September 2016
- 年：2016
- 卷：261
- 期：Complete
- 页码：340-355
- 全文大小：4778 K
文摘
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The dating data indicate that the Chaganbulagen deposit formed approximately 138 Ma ago.
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The ore-forming fluids of the deposit are moderate-temperature and low-salinity fluids.
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The ore-forming fluids of the deposit consist dominantly of meteoric water.
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The ore-forming materials of the deposit mainly came from the Mesozoic magma.
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The Chaganbulagen deposit is a low-sulfidation epithermal deposit.