GYIG OpenIR  > 矿床地球化学国家重点实验室
Mafic-ultramafic intrusion formed by multi-stage evolution of hydrous basaltic melts
Qi-Wei Li; Jun-Hong Zhao; Mei-Fu Zhou; Jian-Feng Gao
2022
Source PublicationGSA Bulletin
Volume134Issue:1/2Pages:526–544
DOI10.1130/B35920
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Indexed BySCI
Language英语
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Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/13661
Collection矿床地球化学国家重点实验室
Affiliation1.State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
3.Department of Earth Sciences, University of Hong Kong, Hong Kong 3State
Recommended Citation
GB/T 7714
Qi-Wei Li,Jun-Hong Zhao,Mei-Fu Zhou,et al. Mafic-ultramafic intrusion formed by multi-stage evolution of hydrous basaltic melts[J]. GSA Bulletin,2022,134(1/2):526–544.
APA Qi-Wei Li,Jun-Hong Zhao,Mei-Fu Zhou,&Jian-Feng Gao.(2022).Mafic-ultramafic intrusion formed by multi-stage evolution of hydrous basaltic melts.GSA Bulletin,134(1/2),526–544.
MLA Qi-Wei Li,et al."Mafic-ultramafic intrusion formed by multi-stage evolution of hydrous basaltic melts".GSA Bulletin 134.1/2(2022):526–544.
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