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A brief review of isotopically light Li - a feature of the enriched mantle?

文献类型：期刊论文

作者Tang, Yan-Jie; Zhang, Hong-Fu; Ying, Ji-Feng
刊名INTERNATIONAL GEOLOGY REVIEW
出版日期2010
卷号52期号:9页码:964-976
关键词lithium isotope geochemistry fractionation mechanisms peridotite xenoliths review of Li isotopic evolution
ISSN号0020-6814
DOI10.1080/00206810903211385
文献子类Review
英文摘要Lithium isotope geochemistry is increasingly being used to trace deep-earth processes, reflecting the observed large variation of Li isotope ratios in mantle-derived rocks, including peridotite xenoliths associated with ancient continents. We briefly review the Li isotopic compositions of major geochemical reservoirs, the assumed mechanisms of Li isotopic fractionation, and, in particular, the origins of isotopically light Li in mantle-derived rocks based on the latest developments in Li isotope geochemistry. Comparison of Li isotope data with existing Sr-Nd isotope ratios reflects the subduction-recycling of ancient oceanic crust and the reappearance of Li in volcanic rocks. This circulation may play an important role in generating the isotopically light-Li component in the mantle - perhaps the enriched mantle end member defined by the Sr-Nd isotopic compositions of oceanic basalts.
WOS关键词NORTH CHINA CRATON ; LITHIUM-ISOTOPE FRACTIONATION ; SLAB-DERIVED FLUIDS ; VOLCANIC ARC LAVAS ; SECTOR ICP-MS ; PERIDOTITE XENOLITHS ; LITHOSPHERIC MANTLE ; SUBDUCTION ZONES ; OCEANIC-CRUST ; PRECISE DETERMINATION
WOS研究方向Geology
语种英语
WOS记录号WOS:000278857000004
出版者TAYLOR & FRANCIS INC
资助机构Natural Science Foundation of China(90714008 ; Natural Science Foundation of China(90714008 ; Natural Science Foundation of China(90714008 ; Natural Science Foundation of China(90714008 ; Chinese Academy of Sciences(KZCX2-YW-103) ; Chinese Academy of Sciences(KZCX2-YW-103) ; Chinese Academy of Sciences(KZCX2-YW-103) ; Chinese Academy of Sciences(KZCX2-YW-103) ; Institute for Study of the Earth's Interior, Okayama University ; Institute for Study of the Earth's Interior, Okayama University ; Institute for Study of the Earth's Interior, Okayama University ; Institute for Study of the Earth's Interior, Okayama University ; 40773026 ; 40773026 ; 40773026 ; 40773026 ; 40534022) ; 40534022) ; 40534022) ; 40534022) ; Natural Science Foundation of China(90714008 ; Natural Science Foundation of China(90714008 ; Natural Science Foundation of China(90714008 ; Natural Science Foundation of China(90714008 ; Chinese Academy of Sciences(KZCX2-YW-103) ; Chinese Academy of Sciences(KZCX2-YW-103) ; Chinese Academy of Sciences(KZCX2-YW-103) ; Chinese Academy of Sciences(KZCX2-YW-103) ; Institute for Study of the Earth's Interior, Okayama University ; Institute for Study of the Earth's Interior, Okayama University ; Institute for Study of the Earth's Interior, Okayama University ; Institute for Study of the Earth's Interior, Okayama University ; 40773026 ; 40773026 ; 40773026 ; 40773026 ; 40534022) ; 40534022) ; 40534022) ; 40534022) ; Natural Science Foundation of China(90714008 ; Natural Science Foundation of China(90714008 ; Natural Science Foundation of China(90714008 ; Natural Science Foundation of China(90714008 ; Chinese Academy of Sciences(KZCX2-YW-103) ; Chinese Academy of Sciences(KZCX2-YW-103) ; Chinese Academy of Sciences(KZCX2-YW-103) ; Chinese Academy of Sciences(KZCX2-YW-103) ; Institute for Study of the Earth's Interior, Okayama University ; Institute for Study of the Earth's Interior, Okayama University ; Institute for Study of the Earth's Interior, Okayama University ; Institute for Study of the Earth's Interior, Okayama University ; 40773026 ; 40773026 ; 40773026 ; 40773026 ; 40534022) ; 40534022) ; 40534022) ; 40534022) ; Natural Science Foundation of China(90714008 ; Natural Science Foundation of China(90714008 ; Natural Science Foundation of China(90714008 ; Natural Science Foundation of China(90714008 ; Chinese Academy of Sciences(KZCX2-YW-103) ; Chinese Academy of Sciences(KZCX2-YW-103) ; Chinese Academy of Sciences(KZCX2-YW-103) ; Chinese Academy of Sciences(KZCX2-YW-103) ; Institute for Study of the Earth's Interior, Okayama University ; Institute for Study of the Earth's Interior, Okayama University ; Institute for Study of the Earth's Interior, Okayama University ; Institute for Study of the Earth's Interior, Okayama University ; 40773026 ; 40773026 ; 40773026 ; 40773026 ; 40534022) ; 40534022) ; 40534022) ; 40534022)
源URL[http://ir.iggcas.ac.cn/handle/132A11/72126]  
专题中国科学院地质与地球物理研究所
通讯作者Tang, Yan-Jie
作者单位Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
推荐引用方式
GB/T 7714		 Tang, Yan-Jie,Zhang, Hong-Fu,Ying, Ji-Feng. A brief review of isotopically light Li - a feature of the enriched mantle?[J]. INTERNATIONAL GEOLOGY REVIEW,2010,52(9):964-976.
APA Tang, Yan-Jie,Zhang, Hong-Fu,&Ying, Ji-Feng.(2010).A brief review of isotopically light Li - a feature of the enriched mantle?.INTERNATIONAL GEOLOGY REVIEW,52(9),964-976.
MLA Tang, Yan-Jie,et al."A brief review of isotopically light Li - a feature of the enriched mantle?".INTERNATIONAL GEOLOGY REVIEW 52.9(2010):964-976.

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来源：地质与地球物理研究所

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