中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Amagmatic Subduction Produced by Mantle Serpentinization and Oceanic Crust Delamination

文献类型:期刊论文

作者Yang, Jianfeng2,3; Lu, Gang1,3; Liu, Tong3; Li, Yang1,3; Wang, Kun3; Wang, Xinxin3; Sun, Baolu1,3; Faccenda, Manuele2; Zhao, Liang1,3
刊名GEOPHYSICAL RESEARCH LETTERS
出版日期2020-05-16
卷号47期号:9页码:11
关键词numerical modeling arc gap flux melting subduction zone mantle serpentinization
ISSN号0094-8276
DOI10.1029/2019GL086257
英文摘要Recycling of oceanic lithosphere and serpentinized peridotites into the mantle leads to dehydration melting and volcanic arcs. However, the mechanism of the occurrence of long-term volcanic gap in subduction zones remains poorly understood. Two-dimensional thermomechanical numerical models focusing on resisting the transport of the major hosts of hydrous minerals to mantle depths, show that thin oceanic crust together with rheologically weak and buoyant serpentinized mantle could result in hydrated lithologies piling up in the accretionary wedge and no or sparse occurrence of arc magmatism. This scenario may occur during subduction of oceanic lithosphere formed at (ultra)slow-spreading margins characterized by thin crust and extensive mantle serpentinization, which is a plausible explanation for the "arc gaps" in the Alps and southern Tibet.
WOS关键词SEISMIC-REFRACTION PROFILES ; XIGAZE OPHIOLITE TIBET ; IBERIA ABYSSAL-PLAIN ; CONTINENT TRANSITION ; DEEP-STRUCTURE ; EXHUMATION ; WESTERN ; ROCKS ; WATER ; LITHOSPHERE
资助项目NSFC[41888101] ; NSFC[91755000] ; NSFC[41625016] ; NSFC[41774112] ; Strategic Priority Research Program (B) of CAS[XDB18000000] ; CAS[GJHZ1776]
WOS研究方向Geology
语种英语
WOS记录号WOS:000536639500017
出版者AMER GEOPHYSICAL UNION
资助机构NSFC ; NSFC ; NSFC ; NSFC ; Strategic Priority Research Program (B) of CAS ; Strategic Priority Research Program (B) of CAS ; Strategic Priority Research Program (B) of CAS ; Strategic Priority Research Program (B) of CAS ; CAS ; CAS ; CAS ; CAS ; NSFC ; NSFC ; NSFC ; NSFC ; Strategic Priority Research Program (B) of CAS ; Strategic Priority Research Program (B) of CAS ; Strategic Priority Research Program (B) of CAS ; Strategic Priority Research Program (B) of CAS ; CAS ; CAS ; CAS ; CAS ; NSFC ; NSFC ; NSFC ; NSFC ; Strategic Priority Research Program (B) of CAS ; Strategic Priority Research Program (B) of CAS ; Strategic Priority Research Program (B) of CAS ; Strategic Priority Research Program (B) of CAS ; CAS ; CAS ; CAS ; CAS ; NSFC ; NSFC ; NSFC ; NSFC ; Strategic Priority Research Program (B) of CAS ; Strategic Priority Research Program (B) of CAS ; Strategic Priority Research Program (B) of CAS ; Strategic Priority Research Program (B) of CAS ; CAS ; CAS ; CAS ; CAS
源URL[http://ir.iggcas.ac.cn/handle/132A11/96651]  
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Zhao, Liang
作者单位1.Univ Chinese Acad Sci, Inst Earth Sci, Beijing, Peoples R China
2.Univ Padua, Dipartimento Geosci, Padua, Italy
3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Yang, Jianfeng,Lu, Gang,Liu, Tong,et al. Amagmatic Subduction Produced by Mantle Serpentinization and Oceanic Crust Delamination[J]. GEOPHYSICAL RESEARCH LETTERS,2020,47(9):11.
APA Yang, Jianfeng.,Lu, Gang.,Liu, Tong.,Li, Yang.,Wang, Kun.,...&Zhao, Liang.(2020).Amagmatic Subduction Produced by Mantle Serpentinization and Oceanic Crust Delamination.GEOPHYSICAL RESEARCH LETTERS,47(9),11.
MLA Yang, Jianfeng,et al."Amagmatic Subduction Produced by Mantle Serpentinization and Oceanic Crust Delamination".GEOPHYSICAL RESEARCH LETTERS 47.9(2020):11.

入库方式: OAI收割

来源:地质与地球物理研究所

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