中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Seismic imaging of the crust and upper mantle beneath the North China Craton

文献类型:期刊论文

作者Tian, You1,2,3; Zhao, Dapeng2; Sun, Ruomei1; Teng, Jiwen1,3
刊名PHYSICS OF THE EARTH AND PLANETARY INTERIORS
出版日期2009-02-01
卷号172期号:3-4页码:169-182
关键词North China Craton Seismic tomography Asthenospheric upwelling Crust and mantle heterogeneity
ISSN号0031-9201
DOI10.1016/j.pepi.2008.09.002
文献子类Article
英文摘要We determined three-dimensional (3D) P-wave velocity structure down to 600km depth beneath the North China Craton using 149,054 arrival times from 7940 local and regional earthquakes, and 193,085 data from 12,657 teleseismic events. which were recorded by 585 seismic stations ill our study region. Our-tomographic images show some new features. Prominent low-velocity (low-V) and high-velocity (high-V) anomalies are imaged beneath the North China Basin, Trans-North China Orogen, and the cratonic Ordos Block. A lithospheric root of over 250 km thick is imaged clearly beneath the Ordos block. A high-Vanomaly which may represent the subducting Pacific slab is imaged in the mantle transition zone beneath the eastern edge of the study area. A few other high-V zones are also imaged in the deep portion of the upper mantle, which may reflect the stagnant Pacific slab and detached Archaean continental lithosphere. Two prominent low-V anomalies are imaged beneath the North China Basin, which may reflect asthenospheric upwelling associated with the deep subduction of the Farallon and Pacific plates since late Mesozoic. We consider that the lithospheric thinning of the eastern part of the North China Craton was Caused by the long-term replacement, metamorphism, and chemical and thermal erosion of the ancient lithosphere by the hot asthenosphere. Crown Copyright (C) 2008 Published by Elsevier B.V. All rights reserved.
WOS关键词SINO-KOREAN CRATON ; JAPAN SUBDUCTION ZONE ; DEEP-STRUCTURE ; SOUTHERN CALIFORNIA ; VELOCITIES BENEATH ; TRAVEL-TIMES ; LITHOSPHERE ; EVOLUTION ; EARTHQUAKE ; HETEROGENEITY
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000262801200004
出版者ELSEVIER SCIENCE BV
资助机构Japanese Ministry of Education and Science(Kiban-A 17204037) ; Japanese Ministry of Education and Science(Kiban-A 17204037) ; National Natural Science Foundations of China(40434009 ; National Natural Science Foundations of China(40434009 ; 40504005) ; 40504005) ; Japanese Ministry of Education and Science(Kiban-A 17204037) ; Japanese Ministry of Education and Science(Kiban-A 17204037) ; National Natural Science Foundations of China(40434009 ; National Natural Science Foundations of China(40434009 ; 40504005) ; 40504005) ; Japanese Ministry of Education and Science(Kiban-A 17204037) ; Japanese Ministry of Education and Science(Kiban-A 17204037) ; National Natural Science Foundations of China(40434009 ; National Natural Science Foundations of China(40434009 ; 40504005) ; 40504005) ; Japanese Ministry of Education and Science(Kiban-A 17204037) ; Japanese Ministry of Education and Science(Kiban-A 17204037) ; National Natural Science Foundations of China(40434009 ; National Natural Science Foundations of China(40434009 ; 40504005) ; 40504005)
源URL[http://ir.iggcas.ac.cn/handle/132A11/71590]  
专题中国科学院地质与地球物理研究所
通讯作者Tian, You
作者单位1.Jilin Univ, Coll Geoexplorat Sci & Technol, Changchun 130026, Peoples R China
2.Tohoku Univ, Dept Geophys, Sendai, Miyagi 9808578, Japan
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 10029, Peoples R China
推荐引用方式
GB/T 7714
Tian, You,Zhao, Dapeng,Sun, Ruomei,et al. Seismic imaging of the crust and upper mantle beneath the North China Craton[J]. PHYSICS OF THE EARTH AND PLANETARY INTERIORS,2009,172(3-4):169-182.
APA Tian, You,Zhao, Dapeng,Sun, Ruomei,&Teng, Jiwen.(2009).Seismic imaging of the crust and upper mantle beneath the North China Craton.PHYSICS OF THE EARTH AND PLANETARY INTERIORS,172(3-4),169-182.
MLA Tian, You,et al."Seismic imaging of the crust and upper mantle beneath the North China Craton".PHYSICS OF THE EARTH AND PLANETARY INTERIORS 172.3-4(2009):169-182.

入库方式: OAI收割

来源:地质与地球物理研究所

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