Magmatic-hydrothermal evolution of the Donggou porphyry Mo deposit at the southern margin of the North China Craton: Evidence from chemistry of biotite | ||
Chang Jin; Xin-Yu Gao; Wei Terry Chen; Tai-Ping Zhao | ||
2018 | ||
Source Publication | Ore Geology Reviews
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Volume | 92Pages:84-96 | |
Abstract |
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Keyword | Biotite magmatic Fluid halogen Fugacity oxygen Fugacity donggou Porphyry Mo Deposit | |
Indexed By | SCI | |
Document Type | 期刊论文 | |
Identifier | http://ir.gyig.ac.cn/handle/42920512-1/8665 | |
Collection | 矿床地球化学国家重点实验室 | |
Affiliation | 1.Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China 2.University of Chinese Academy of Sciences, Beijing 100039, China 3.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China | |
Recommended Citation GB/T 7714 | Chang Jin;Xin-Yu Gao;Wei Terry Chen;Tai-Ping Zhao. Magmatic-hydrothermal evolution of the Donggou porphyry Mo deposit at the southern margin of the North China Craton: Evidence from chemistry of biotite[J]. Ore Geology Reviews,2018,92:84-96. | |
APA | Chang Jin;Xin-Yu Gao;Wei Terry Chen;Tai-Ping Zhao.(2018).Magmatic-hydrothermal evolution of the Donggou porphyry Mo deposit at the southern margin of the North China Craton: Evidence from chemistry of biotite.Ore Geology Reviews,92,84-96. | |
MLA | Chang Jin;Xin-Yu Gao;Wei Terry Chen;Tai-Ping Zhao."Magmatic-hydrothermal evolution of the Donggou porphyry Mo deposit at the southern margin of the North China Craton: Evidence from chemistry of biotite".Ore Geology Reviews 92(2018):84-96. |
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