中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Distinct formation history for deep-mantle domains reflected in geochemical differences

文献类型:期刊论文

作者Doucet, Luc S.3; Li, Zheng-Xiang3; Gamal El Dien, Hamed2,3; Pourteau, Amaury3; Murphy, J. Brendan3,4; Collins, William J.3; Mattielli, Nadine8; Olierook, Hugo K. H.6,7; Spencer, Christopher J.3,5; Mitchell, Ross N.1,3
刊名NATURE GEOSCIENCE
出版日期2020-07-01
卷号13期号:7页码:511-+
ISSN号1752-0894
DOI10.1038/s41561-020-0599-9
英文摘要The Earth's mantle is currently divided into the African and Pacific domains, separated by the circum-Pacific subduction girdle, and each domain features a large low shear-wave velocity province (LLSVP) in the lower mantle. However, it remains controversial as to whether the LLSVPs have been stationary through time or dynamic, changing in response to changes in global subduction geometry. Here we compile radiogenic isotope data on plume-induced basalts from ocean islands and oceanic plateaus above the two LLSVPs that show distinct lead, neodymium and strontium isotopic compositions for the two mantle domains. The African domain shows enrichment by subducted continental material during the assembly and breakup of the supercontinent Pangaea, whereas no such feature is found in the Pacific domain. This deep-mantle geochemical dichotomy reflects the different evolutionary histories of the two domains during the Rodinia and Pangaea supercontinent cycles and thus supports a dynamic relationship between plate tectonics and deep-mantle structures. Earth's deep-mantle domains are geochemically distinct. The African domain is enriched in subducted material, which suggests a different history from the Pacific domain and a dynamic relationship between plate tectonics and deep-mantle structures.
WOS关键词LARGE IGNEOUS PROVINCES ; HELIUM-ISOTOPES ; CONTINENTAL BREAKUP ; HE-3/HE-4 RATIOS ; VOLCANIC-ROCKS ; PLUME ; ORIGIN ; SHEAR ; SR ; EVOLUTION
WOS研究方向Geology
语种英语
出版者NATURE PUBLISHING GROUP
WOS记录号WOS:000544997400013
源URL[http://ir.iggcas.ac.cn/handle/132A11/97144]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Doucet, Luc S.
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
2.Tanta Univ, Geol Dept, Fac Sci, Tanta, Egypt
3.Curtin Univ, Sch Earth & Planetary Sci, Earth Dynam Res Grp, TIGeR, Perth, WA, Australia
4.St Francis Xavier Univ, Dept Earth Sci, Antigonish, NS, Canada
5.Queens Univ, Dept Geol Sci & Geol Engn, Kingston, ON, Canada
6.Curtin Univ, John Laeter Ctr, Perth, WA, Australia
7.Curtin Univ, Ctr Explorat Targeting Curtin Node, Timescales Mineral Syst, Perth, WA, Australia
8.Univ Libre Bruxelles, Lab G Time, ULB, Brussels, Belgium
推荐引用方式
GB/T 7714
Doucet, Luc S.,Li, Zheng-Xiang,Gamal El Dien, Hamed,et al. Distinct formation history for deep-mantle domains reflected in geochemical differences[J]. NATURE GEOSCIENCE,2020,13(7):511-+.
APA Doucet, Luc S..,Li, Zheng-Xiang.,Gamal El Dien, Hamed.,Pourteau, Amaury.,Murphy, J. Brendan.,...&Mitchell, Ross N..(2020).Distinct formation history for deep-mantle domains reflected in geochemical differences.NATURE GEOSCIENCE,13(7),511-+.
MLA Doucet, Luc S.,et al."Distinct formation history for deep-mantle domains reflected in geochemical differences".NATURE GEOSCIENCE 13.7(2020):511-+.

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来源:地质与地球物理研究所

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