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Origin of the Shanggong gold deposit, the southern margin of the North China Craton: Constraints from Rb-Sr ages of sericite, and trace elements and sulfur isotope of pyrite
Lei Meng; Caiyun Lan; Qiang Zhan; Qiang Wu; Taiping Zhao
2022
Source PublicationOre Geology Reviews
Volume142Pages:104728
DOI10.1016/j.oregeorev.2022.104728
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Indexed BySCI
Language英语
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Cited Times:13[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/13719
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 550081, China
2.Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
3.CAS Center for Excellence in Deep Earth Science, Guangzhou 510640, China
4.State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China
Recommended Citation
GB/T 7714
Lei Meng,Caiyun Lan,Qiang Zhan,et al. Origin of the Shanggong gold deposit, the southern margin of the North China Craton: Constraints from Rb-Sr ages of sericite, and trace elements and sulfur isotope of pyrite[J]. Ore Geology Reviews,2022,142:104728.
APA Lei Meng,Caiyun Lan,Qiang Zhan,Qiang Wu,&Taiping Zhao.(2022).Origin of the Shanggong gold deposit, the southern margin of the North China Craton: Constraints from Rb-Sr ages of sericite, and trace elements and sulfur isotope of pyrite.Ore Geology Reviews,142,104728.
MLA Lei Meng,et al."Origin of the Shanggong gold deposit, the southern margin of the North China Craton: Constraints from Rb-Sr ages of sericite, and trace elements and sulfur isotope of pyrite".Ore Geology Reviews 142(2022):104728.
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