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 |
DOI | 10.18654/1000-0569/2022.12.11 |
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 |
推荐引用方式 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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