GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室
Qiu, Yifan1,2; Zhao, Taiping1; Li, Yiliang3,4
The Yunmengshan iron formation at the end of the Paleoproterozoic era
Source PublicationAPPLIED CLAY SCIENCE
ISSN0169-1317
2020-12-01
Volume199Pages:12
DOI10.1016/j.clay.2020.105888
Language英语
WOS Research AreaChemistry ; Materials Science ; Mineralogy
WOS IDWOS:000598137500003
Indexed BySCI
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Cited Times:7[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/57599
Collection中国科学院矿物学与成矿学重点实验室
Corresponding AuthorLi, Yiliang
Affiliation1.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Mineral & Metallogeny, Guangzhou 510640, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Univ Hong Kong, Dept Earth Sci, Pokfulam, Hong Kong, Peoples R China
4.Univ Sci & Technol China, Ctr Excellence Comparat Planetol, Chinese Acad Sci, Hefei 230026, Peoples R China
Recommended Citation
GB/T 7714
Qiu, Yifan,Zhao, Taiping,Li, Yiliang. The Yunmengshan iron formation at the end of the Paleoproterozoic era[J]. APPLIED CLAY SCIENCE,2020,199:12.
APA Qiu, Yifan,Zhao, Taiping,&Li, Yiliang.(2020).The Yunmengshan iron formation at the end of the Paleoproterozoic era.APPLIED CLAY SCIENCE,199,12.
MLA Qiu, Yifan,et al."The Yunmengshan iron formation at the end of the Paleoproterozoic era".APPLIED CLAY SCIENCE 199(2020):12.
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