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 Publication | Ore Geology Reviews
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Volume | 118Pages:10335 |
DOI | 10.1016/j.oregeorev.2020.103354 |
URL | 查看原文 |
Indexed By | SCI |
Language | 英语 |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://ir.gyig.ac.cn/handle/42920512-1/11835 |
Collection | 矿床地球化学国家重点实验室 |
Affiliation | 1.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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