中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Compositional heterogeneity of the asthenosphere: Advancement and implications

文献类型:期刊论文

作者Liu ChuanZhou1,2; Yang AlexandraYang3; Liu BoDa1; Liu Tong1
刊名ACTA PETROLOGICA SINICA
出版日期2022-12-01
卷号38期号:12页码:3712-3734
ISSN号1000-0569
关键词Asthenosphere Mid-ocean ridge basalts (MORB) Abyssal peridotites Ophiolite
DOI10.18654/1000-0569/2022.12.11
英文摘要Asthenosphere is the mechanically weak and ductile region of Earth's upper mantle, which lies beneath the lithosphere and extends as deep as the mantle transition zone. Its global convection is responsible for driving tectonic movement of the plates. The asthenosphere is an important source of magmatic rocks on the Earth and has been regarded as essential reference reservoir applied to discussion on significant geological issues, such as Earth's formation and evolution, crust-mantle interaction, and crustal growth. Previous studies on oceanic basalts have proposed that the asthenosphere is relatively homogeneous in composition. Nevertheless, compositions of abyssal peridotites have shown that the asthenosphere is strongly heterogeneous. Numerous studies have shown that ancient mantle domains are ubiquitous within the asthenosphere, which could be originated from the recycled oceanic mantle and cratonic mantle dislodged through different mechanisms. Such compositional heterogeneities of the asthenosphere have been widely documented in global ophiolites of different ages. This paper summarized the relevant studies on mid-ocean ridge basalts, abyssal peridotites and ophiolites to disclose various origins of the mantle heterogeneities of the asthenosphere. Effects of these heterogeneities on partial melting of asthenosphere beneath mid -ocean ridges have also been discussed.
WOS关键词OCEANIC UPPER-MANTLE ; BENEATH GAKKEL RIDGE ; MIDOCEAN RIDGE ; CONTINENTAL-CRUST ; MELT EXTRACTION ; PERIDOTITE ; OPHIOLITE ; ANCIENT ; SUBDUCTION ; ISOTOPE
WOS研究方向Geology
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:000905312500011
源URL[http://ir.iggcas.ac.cn/handle/132A11/106913]  
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Liu ChuanZhou
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Ocean & Marginal Sea Geol, Guangzhou 510301, Peoples R China
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GB/T 7714
Liu ChuanZhou,Yang AlexandraYang,Liu BoDa,et al. Compositional heterogeneity of the asthenosphere: Advancement and implications[J]. ACTA PETROLOGICA SINICA,2022,38(12):3712-3734.
APA Liu ChuanZhou,Yang AlexandraYang,Liu BoDa,&Liu Tong.(2022).Compositional heterogeneity of the asthenosphere: Advancement and implications.ACTA PETROLOGICA SINICA,38(12),3712-3734.
MLA Liu ChuanZhou,et al."Compositional heterogeneity of the asthenosphere: Advancement and implications".ACTA PETROLOGICA SINICA 38.12(2022):3712-3734.

入库方式: OAI收割

来源:地质与地球物理研究所

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