中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Deep electrical structure beneath the Sichuan-Yunnan area in the eastern margin of the Tibetan plateau

文献类型:期刊论文

作者Cheng Yuan-Zhi1,2; Tang Ji1; Cai Jun-Tao1; Chen Xiao-Bin1; Dong Ze-Yi1; Wang Li-Bo3
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
出版日期2017-06-01
卷号60期号:6页码:2425-2441
关键词Eastern Himalayan syntaxis Magnetotellurics Electrical structure Lithospheric tectonic deformation
ISSN号0001-5733
DOI10.6038/cjg20170631
文献子类Article
英文摘要In response to the ongoing convergence between the Indian and Eurasian plates, significant intracontinental deformation has been accommodated by crustal thickening on large-scale strike slip faults. Several models have been proposed to explain the deformation of the eastern Tibetan plateau, including: (1) lateral extrusion of rigid blocks, in which deformation is primarily localized along strike-slip faults that bound the blocks; (2) continuous deformation of lithosphere; and (3) ductile channel flow in the mid-lower crust. The major characteristics are dominated by the large-scale clockwise rotation around the eastern Himalayan syntaxis in the southeast margin of the Tibetan plateau. However, the mechanisms for Tibetan plateau's deformation and expansion remain enigmatic due to the resolution limitations of methods and data. The debates of these models center on whether the deformation is localized to the mantle or to the upper crust. The southeast margin of the Tibetan plateau, which has undergone significant crustal thickening and tectonic extrusion, is particularly important for understanding the kinematics and dynamics of intracontinental deformation.
WOS关键词MANTLE VELOCITY STRUCTURE ; RAYLEIGH-WAVE DISPERSION ; AMBIENT SEISMIC NOISE ; LOWER CRUSTAL FLOW ; MAGNETOTELLURIC DATA ; WESTERN YUNNAN ; TECTONIC IMPLICATIONS ; RECEIVER FUNCTIONS ; SE TIBET ; ARRAY TOMOGRAPHY
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000403744600031
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/52852]  
专题地质与地球物理研究所_中国科学院地球与行星物理重点实验室
通讯作者Tang Ji
作者单位1.China Earthquake Adm, Inst Geol, State Key Lab Earthquake Dynam, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.Jiangxi Earthquake Adm, Nanchang 330039, Jiangxi, Peoples R China
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Cheng Yuan-Zhi,Tang Ji,Cai Jun-Tao,et al. Deep electrical structure beneath the Sichuan-Yunnan area in the eastern margin of the Tibetan plateau[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2017,60(6):2425-2441.
APA Cheng Yuan-Zhi,Tang Ji,Cai Jun-Tao,Chen Xiao-Bin,Dong Ze-Yi,&Wang Li-Bo.(2017).Deep electrical structure beneath the Sichuan-Yunnan area in the eastern margin of the Tibetan plateau.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,60(6),2425-2441.
MLA Cheng Yuan-Zhi,et al."Deep electrical structure beneath the Sichuan-Yunnan area in the eastern margin of the Tibetan plateau".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 60.6(2017):2425-2441.

入库方式: OAI收割

来源:地质与地球物理研究所

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