Heavy δ26Mg values in carbonate indicate a magmatic-hydrothermal origin of Carlin-type Au deposit | |
Zhuojun Xie![]() ![]() ![]() | |
2022 | |
Source Publication | Geochimica et Cosmochimica Acta
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Volume | 333,Pages:166-183 |
DOI | 10.1016/j.gca.2022.07.009 |
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/42920512-1/13718 |
Collection | 矿床地球化学国家重点实验室 期刊图书信息中心 |
Affiliation | 1.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China 2.State Key Laboratory of Continental Dynamics, Shaanxi Key Laboratory of Early Life and Environments, Department of Geology, Northwest University, Xi’an 710069, China 3.University of Nevada Las Vegas, Las Vegas, NV 89154, USA 4.Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources of People’s Republic of China, Guiyang 550081, China 5.Guizhou Bureau of Geology and Mineral Exploration & Development, Guiyang 550018, China 6.University of Chinese Academy of Sciences, Beijing 100039, China |
Recommended Citation GB/T 7714 | Zhuojun Xie,Kang-Jun Huang,Yong Xia,et al. Heavy δ26Mg values in carbonate indicate a magmatic-hydrothermal origin of Carlin-type Au deposit[J]. Geochimica et Cosmochimica Acta,2022,333,:166-183. |
APA | Zhuojun Xie.,Kang-Jun Huang.,Yong Xia.,Jean Cline.,Qinping Tan.,...&Bing Yan.(2022).Heavy δ26Mg values in carbonate indicate a magmatic-hydrothermal origin of Carlin-type Au deposit.Geochimica et Cosmochimica Acta,333,,166-183. |
MLA | Zhuojun Xie,et al."Heavy δ26Mg values in carbonate indicate a magmatic-hydrothermal origin of Carlin-type Au deposit".Geochimica et Cosmochimica Acta 333,(2022):166-183. |
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Heavy ?26Mg values i(6168KB) | 期刊论文 | 作者接受稿 | 开放获取 | CC BY-NC-SA | View Download |
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