Geological, fluid inclusion, H-O-S-Pb isotope, and Ar-Ar geochronology constraints on the genesis of the Nancha gold deposit, southern Jilin Province, northeast China
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- 作者：Peng Chaia ; b ; cx001chaipeng@163.com" class="auth_mail" title="E-mail the corresponding author ; Jing-gui Sunb ; sunjinggui@jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Zeng-qian Houa ; Shu-wen Xingc ; Zhong-yu Wangb
- 关键词：Nancha gold deposit ; Fluid inclusions ; Isotope geochemistry ; Ar&ndash ; Ar geochronology ; Orogenic gold deposit ; Jilin Province ; NE China
- 刊名：Ore Geology Reviews
- 出版年：2016
- 出版时间：January 2016
- 年：2016
- 卷：72
- 期：part_P1
- 页码：1053-1071
- 全文大小：5521 K
文摘
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A typical orogenic gold deposit located in the Jiao–Liao–Ji belt, North China Craton.
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Metamorphic fluid was the initial ore-forming fluid for the Nancha deposit.
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Boiling and mixing of fluids controlled the mineralization process.
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Metallogenic materials sourced from Proterozoic rocks and ore-forming metamorphic fluids.
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Gold mineralization occurred during Middle Jurassic accretionary orogen regime.
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