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GYIG OpenIR  > 环境地球化学国家重点实验室
Mineralogy and Geochemistry of the High-Cr Podiform Chromitite from the Cuobuzha Ophiolite, Yarlung Zangbo Suture Zone, Western Tibet, China: Implication for its Origin
Hui ZHAO; Jingsui YANG; Fei LIU; Fahui XIONG; Dongyang LIAN; Hu YAO
2020
Source PublicationActa Geologica Sinica 94
Volume94Issue:1Pages:75-89
DOI10.1111/1755-6724.14342
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Indexed BySCI
Language英语
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Cited Times:4[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/11857
Collection环境地球化学国家重点实验室
Affiliation1.Harbin Institute of Technology, Harbin 150001, China
2.Department of Earth and Space Sciences, Southern University of Science and Technology, Shenzhen 518055, China
3.Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
4.School of Earth Sciences and Engineering, Nanjing University, Nanjing 201123, China
5.Institute of Geochemistry Chinese Academy of Sciences, Guiyang 550081, China
Recommended Citation
GB/T 7714
Hui ZHAO,Jingsui YANG,Fei LIU,et al. Mineralogy and Geochemistry of the High-Cr Podiform Chromitite from the Cuobuzha Ophiolite, Yarlung Zangbo Suture Zone, Western Tibet, China: Implication for its Origin[J]. Acta Geologica Sinica 94,2020,94(1):75-89.
APA Hui ZHAO,Jingsui YANG,Fei LIU,Fahui XIONG,Dongyang LIAN,&Hu YAO.(2020).Mineralogy and Geochemistry of the High-Cr Podiform Chromitite from the Cuobuzha Ophiolite, Yarlung Zangbo Suture Zone, Western Tibet, China: Implication for its Origin.Acta Geologica Sinica 94,94(1),75-89.
MLA Hui ZHAO,et al."Mineralogy and Geochemistry of the High-Cr Podiform Chromitite from the Cuobuzha Ophiolite, Yarlung Zangbo Suture Zone, Western Tibet, China: Implication for its Origin".Acta Geologica Sinica 94 94.1(2020):75-89.
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