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Fluid inclusion and stable isotope (C, O and S) constraints on the genesis of the high-grade Langdu Cu skarn deposit in Yunnan, SW China
Tao Ren; Hong Zhong; Xing-chun Zhang
2020
Source PublicationOre Geology Reviews
Volume118Pages:10335
DOI10.1016/j.oregeorev.2020.103354
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Indexed BySCI
Language英语
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Cited Times:11[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/11835
Collection矿床地球化学国家重点实验室
Affiliation1.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550018, China
2.Faculty of Land Resources Engineering, Kunming University of Science and Technology, Kunming 650093, China
Recommended Citation
GB/T 7714
Tao Ren,Hong Zhong,Xing-chun Zhang. Fluid inclusion and stable isotope (C, O and S) constraints on the genesis of the high-grade Langdu Cu skarn deposit in Yunnan, SW China[J]. Ore Geology Reviews,2020,118:10335.
APA Tao Ren,Hong Zhong,&Xing-chun Zhang.(2020).Fluid inclusion and stable isotope (C, O and S) constraints on the genesis of the high-grade Langdu Cu skarn deposit in Yunnan, SW China.Ore Geology Reviews,118,10335.
MLA Tao Ren,et al."Fluid inclusion and stable isotope (C, O and S) constraints on the genesis of the high-grade Langdu Cu skarn deposit in Yunnan, SW China".Ore Geology Reviews 118(2020):10335.
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