中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Origin and evolution of the slab fluids since subduction inception in the Izu-Bonin-Mariana: A comparison with the southeast Mariana fore-arc rift

文献类型:期刊论文

作者Ribeiro, Julia2; MacLeod, Christopher3; Lissenberg, Johan3; Ryan, Jeff1; Macpherson, Colin4
刊名CHEMICAL GEOLOGY
出版日期2022-07-05
卷号601页码:15
ISSN号0009-2541
DOI10.1016/j.chemgeo.2022.120813
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000797220500004
源URL[http://ir.gig.ac.cn/handle/344008/67901]  
专题中国科学院广州地球化学研究所
通讯作者Ribeiro, Julia
作者单位1.Univ S Florida, Sch Geosci, Tempa, FL USA
2.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China
3.Cardiff Univ, Dept Earth & Environm Sci, Cardiff CF10 3AT, Wales
4.Univ Durham, Dept Earth Sci, Durham, England
推荐引用方式
GB/T 7714
Ribeiro, Julia,MacLeod, Christopher,Lissenberg, Johan,et al. Origin and evolution of the slab fluids since subduction inception in the Izu-Bonin-Mariana: A comparison with the southeast Mariana fore-arc rift[J]. CHEMICAL GEOLOGY,2022,601:15.
APA Ribeiro, Julia,MacLeod, Christopher,Lissenberg, Johan,Ryan, Jeff,&Macpherson, Colin.(2022).Origin and evolution of the slab fluids since subduction inception in the Izu-Bonin-Mariana: A comparison with the southeast Mariana fore-arc rift.CHEMICAL GEOLOGY,601,15.
MLA Ribeiro, Julia,et al."Origin and evolution of the slab fluids since subduction inception in the Izu-Bonin-Mariana: A comparison with the southeast Mariana fore-arc rift".CHEMICAL GEOLOGY 601(2022):15.

入库方式: OAI收割

来源:广州地球化学研究所

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