中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Upper mantle structure beneath central Tibet derived from teleseismic S wave tomography along the INDEPTH-III profile

文献类型:期刊论文

作者Liu Zhen1,2; Tian Xiao-Bo1; Liang Xiao-Feng1; Teng Ji-Wen1
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
出版日期2015-04-01
卷号58期号:4页码:1169-1178
关键词Tibetan Plateau Upper-mantle Structure S-wave Velocity Tomography
DOI10.6038/cjg20150407
文献子类Article
英文摘要The Tibetan Plateau is produced by the continental-continental collision between the India and Eurasian plates as well as the subsequent convergence. It has become a consensus that the crustal thickness beneath the plateau is twice of the normal continental crust, while the deformation of its mantle lithosphere, as an important part of the developing plateau, remains controversial. This ambiguity about the upper mantle structure is resulted from uneven distributed seismologic observations in Tibet, and upper mantle structure is possibly heterogeneous along the east-west direction. Another reason is that the seismic wave speed contrast between the continental mantle lithosphere and asthenosphere might not be significant to detect by current seismic methods. Because the geodynamic of mantle lithosphere is closely related to the processes of plateau uplift and the presence of volcanic rocks, revealing the geometry of Indian and Eurasian mantle lithosphere can help understanding the dynamic processes of mantle lithosphere as well as the evolution of the plateau.
WOS关键词INDIAN LITHOSPHERE BENEATH ; VELOCITY STRUCTURE BENEATH ; TRAVEL-TIME TOMOGRAPHY ; P-WAVE ; NORTHERN TIBET ; LEAST-SQUARES ; ARRIVAL TIMES ; PLATEAU ; SUBDUCTION ; CRUST
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000353664300007
源URL[http://ir.iggcas.ac.cn/handle/132A11/62536]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Liu Zhen,Tian Xiao-Bo,Liang Xiao-Feng,et al. Upper mantle structure beneath central Tibet derived from teleseismic S wave tomography along the INDEPTH-III profile[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2015,58(4):1169-1178.
APA Liu Zhen,Tian Xiao-Bo,Liang Xiao-Feng,&Teng Ji-Wen.(2015).Upper mantle structure beneath central Tibet derived from teleseismic S wave tomography along the INDEPTH-III profile.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,58(4),1169-1178.
MLA Liu Zhen,et al."Upper mantle structure beneath central Tibet derived from teleseismic S wave tomography along the INDEPTH-III profile".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 58.4(2015):1169-1178.

入库方式: OAI收割

来源:地质与地球物理研究所

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