中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Low-Degree Melt Metasomatic Origin of Global Upper Mantle Fe Isotope Fractionation

文献类型:期刊论文

作者Guo, Pengyuan1,2; Niu, Yaoling2; Sun, Pu1,2; Chen, Shuo1,2; Chen, Yanhong3; Duan, Meng1,2; Wang, Xiaohong1,2; Gong, Hongmei1,2
刊名GEOPHYSICAL RESEARCH LETTERS
出版日期2023-07-28
卷号50期号:14页码:10
ISSN号0094-8276
关键词mantle metasomatism upper mantle Fe isotope fractionation continental alkali basalt
DOI10.1029/2022GL102264
通讯作者Guo, Pengyuan(guopy@qdio.ac.cn)
英文摘要The upper mantle is heterogeneous in Fe isotope compositions, but the origin of the heterogeneity needs understanding. Recent studies on oceanic basalts demonstrate that the upper mantle Fe isotope heterogeneity results from low-degree melt metasomatism. However, whether this hypothesis is of global significance needs testing in continental settings. Here we present an Fe isotopic study on intraplate continental alkali basalts from continental China, which are shown to have derived from upper mantle containing more metasomatized lithologies. The results show first-order positive correlations of delta Fe-56 with indices of low-degree melt metasomatism (e.g., [La/Sm](N)), which, together with the so-far published mid-ocean ridge basalts data, define global trends, substantiating the global significance of low-degree melt metasomatism in causing upper mantle Fe isotope variation. We, thus, suggest that low-degree melt metasomatism is a globally effective process to preferentially concentrate heavy Fe isotopes in metasomatic lithologies at upper mantle conditions both today and in Earth's history.
WOS关键词OCEAN ISLAND BASALTS ; EAST PACIFIC RISE ; CENOZOIC BASALTS ; CHEMICAL-COMPOSITION ; CHINA EVIDENCE ; BENEATH ; HETEROGENEITY ; GEOCHEMISTRY ; CRUST ; MORB
资助项目We thank editorial handling by Christian Huber and constructive comments from two journal reviewers. P.Y. thank Fu-Ping Pei for providing several samples in this study. This work is financially supported by National Natural Science Foundation of China Gran[42076048] ; We thank editorial handling by Christian Huber and constructive comments from two journal reviewers. P.Y. thank Fu-Ping Pei for providing several samples in this study. This work is financially supported by National Natural Science Foundation of China Gran[91958215] ; We thank editorial handling by Christian Huber and constructive comments from two journal reviewers. P.Y. thank Fu-Ping Pei for providing several samples in this study. This work is financially supported by National Natural Science Foundation of China Gran[41776067] ; National Natural Science Foundation of China
WOS研究方向Geology
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:001093766900001
源URL[http://ir.qdio.ac.cn/handle/337002/181598]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Guo, Pengyuan
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China
2.Laoshan Lab, Qingdao, Peoples R China
3.China Univ Geosci, Sch Ocean Sci, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Guo, Pengyuan,Niu, Yaoling,Sun, Pu,et al. Low-Degree Melt Metasomatic Origin of Global Upper Mantle Fe Isotope Fractionation[J]. GEOPHYSICAL RESEARCH LETTERS,2023,50(14):10.
APA Guo, Pengyuan.,Niu, Yaoling.,Sun, Pu.,Chen, Shuo.,Chen, Yanhong.,...&Gong, Hongmei.(2023).Low-Degree Melt Metasomatic Origin of Global Upper Mantle Fe Isotope Fractionation.GEOPHYSICAL RESEARCH LETTERS,50(14),10.
MLA Guo, Pengyuan,et al."Low-Degree Melt Metasomatic Origin of Global Upper Mantle Fe Isotope Fractionation".GEOPHYSICAL RESEARCH LETTERS 50.14(2023):10.

入库方式: OAI收割

来源:海洋研究所

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