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The Redox State of Incipient Oceanic Subduction Zones: An Example From the Troodos Ophiolite (Cyprus)
Wen-Jun Hu; Mei-Fu Zhou; Julia M. Ribeiro; John Malpas; Ya-Dong Wu; Zhong-Jie Bai
2023
Source PublicationJournal of Geophysical Research: Solid Earth
Volume128Issue:4
Abstract


 

DOI10.1029/2022JB025008
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Indexed BySCI
Language英语
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Cited Times:6[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/14740
Collection矿床地球化学国家重点实验室
Affiliation1.School of Earth Resources, China University of Geosciences, Wuhan, China
2.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, China
3.Department of Earth Sciences,The University of Hong Kong, Hong Kong, China
4.State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Science, Guangzhou, China
5.State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
Recommended Citation
GB/T 7714
Wen-Jun Hu,Mei-Fu Zhou,Julia M. Ribeiro,et al. The Redox State of Incipient Oceanic Subduction Zones: An Example From the Troodos Ophiolite (Cyprus)[J]. Journal of Geophysical Research: Solid Earth,2023,128(4).
APA Wen-Jun Hu,Mei-Fu Zhou,Julia M. Ribeiro,John Malpas,Ya-Dong Wu,&Zhong-Jie Bai.(2023).The Redox State of Incipient Oceanic Subduction Zones: An Example From the Troodos Ophiolite (Cyprus).Journal of Geophysical Research: Solid Earth,128(4).
MLA Wen-Jun Hu,et al."The Redox State of Incipient Oceanic Subduction Zones: An Example From the Troodos Ophiolite (Cyprus)".Journal of Geophysical Research: Solid Earth 128.4(2023).
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