中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
3D density structure of lithosphere beneath northeastern margin of the Tibetan Plateau

文献类型:期刊论文

作者Wang Xin-Sheng1,2,3; Fang Jian2; Hsu Hou-Tse2
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
出版日期2013-11-01
卷号56期号:11页码:3770-3778
关键词Northeastern margin of the Tibetan Plateau Density structure Gravity inversion Crustal-mantle decoupling
ISSN号0001-5733
DOI10.6038/cjg20131118
文献子类Article
英文摘要We obtained the three dimensional velocity and density structures of lithosphere beneath northeastern margin of the Tibetan Plateau (TP) using gravity and seismic data, and discussed its geodynamic implication. Firstly, P wave velocity structures are determined by seismic tomography using P wave travel time data, and then converted to initial density model for the following gravity inversion. Subsequently, the density structures in lithosphere are inverted by Bouguer gravity anomaly. Our density model shows that the crustal density structures are critical for the occurrence of earthquakes as well as the lower crustal flow. The trend of density isopleths is coherent with that of surface fractures in the crust. However, it presents a clockwise rotation in the mantle. This phenomenon may indicate the decoupling between curst and mantle. In 80 similar to 100 km depth, P wave velocity anomalies are significantly lower than density anomalies. This may demonstrate the partial melting and increase of rock water content. The combined effects of the subduction of Indian plate and the obstruction force from Ordos and Alashan blocks made a strong tectonic squeezing, inducing the asthenosphere upwelling, and providing conditions for the crustal-mantle decoupling, partial melting, and reduction of the P velocity.
WOS关键词QINGHAI-XIZANG PLATEAU ; WAVE VELOCITY STRUCTURE ; UPPER-MANTLE BENEATH ; CRUSTAL STRUCTURE ; NORTH CHINA ; AREA ; CALIFORNIA ; ANISOTROPY ; INVERSION ; FLOW
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000327753000018
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/87568]  
专题中国科学院地质与地球物理研究所
通讯作者Wang Xin-Sheng
作者单位1.Natl Earthquake Infrastruct Serv, Beijing 100036, Peoples R China
2.Chinese Acad Sci, State Key Lab Geodesy & Earths Dynam, Inst Geodesy & Geophys, Wuhan 430077, Peoples R China
3.Chinese Acad Sci, Key Lab Earths Deep Interior, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Wang Xin-Sheng,Fang Jian,Hsu Hou-Tse. 3D density structure of lithosphere beneath northeastern margin of the Tibetan Plateau[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2013,56(11):3770-3778.
APA Wang Xin-Sheng,Fang Jian,&Hsu Hou-Tse.(2013).3D density structure of lithosphere beneath northeastern margin of the Tibetan Plateau.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,56(11),3770-3778.
MLA Wang Xin-Sheng,et al."3D density structure of lithosphere beneath northeastern margin of the Tibetan Plateau".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 56.11(2013):3770-3778.

入库方式: OAI收割

来源:地质与地球物理研究所

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