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Nickel isotope ratios trace the process of sulfide-silicate liquid immiscibility during magmatic differentiation
Lie-Meng Chen; Peter C. Lightfoot; Jian-Ming Zhu; Fang-Zhen Teng; Qing Duan; Runsheng Yin; Guangliang Wu; Song-Yue Yu; Rui-Zhong Hu
2023
Source PublicationGeochimica et Cosmochimica Acta
Volume353Pages:1-12
Abstract

 

 

DOI10.1016/j.gca.2023.05.013
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Indexed BySCI
Language英语
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Cited Times:2[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/14656
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.University of Western Ontario, 1151 Richmond Street, London N6A3K7, Canada
3.State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (Beijing), Beijing 100083, China
4.Isotope Laboratory, Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA
5.State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330032, China
Recommended Citation
GB/T 7714
Lie-Meng Chen,Peter C. Lightfoot,Jian-Ming Zhu,et al. Nickel isotope ratios trace the process of sulfide-silicate liquid immiscibility during magmatic differentiation[J]. Geochimica et Cosmochimica Acta,2023,353:1-12.
APA Lie-Meng Chen.,Peter C. Lightfoot.,Jian-Ming Zhu.,Fang-Zhen Teng.,Qing Duan.,...&Rui-Zhong Hu.(2023).Nickel isotope ratios trace the process of sulfide-silicate liquid immiscibility during magmatic differentiation.Geochimica et Cosmochimica Acta,353,1-12.
MLA Lie-Meng Chen,et al."Nickel isotope ratios trace the process of sulfide-silicate liquid immiscibility during magmatic differentiation".Geochimica et Cosmochimica Acta 353(2023):1-12.
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