中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Lithospheric mantle underneath the Tibetan Plateau does not escape southeastward

文献类型:期刊论文

作者Nie, Shitan1,2; Tian, Xiaobo1,3; Li, Jiangtao4; Tan, Ping5
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2021-02-01
卷号206页码:10
关键词Eastern and southeastern Tibetan Plateau Pn velocity Uppermost mantle Lithospheric mantle Eastward escape
ISSN号1367-9120
DOI10.1016/j.jseaes.2020.104629
英文摘要A mass of lithospheric shortening occurred beneath the Tibetan Plateau due to the collision between the Indian and Eurasian plates. The extrusion of the upper crust beneath the Tibetan Plateau has been widely accepted, but whether the lithospheric mantle escapes laterally by creep deformation or rigid-block extrusion remains unclear. Based on the Pn travel time data, the velocity structure of the uppermost mantle in eastern and southeastern Tibetan Plateau was obtained by using the interstation travel-time difference method. The results show an obviously high Pn velocity beneath the Sichuan Basin and Qaidam Basin, indicating that the areas are stable blocks. The high Pn velocity beneath the eastern Lhasa terrane may be related to the underplating of the Indian lithospheric plate to the north. The Qilian block located in the north of the Kunlun fault appears as a normal Pn velocity, which indicates a mean lithospheric mantle thickness. A significantly low Pn velocity with an average of similar to 7.8 km/s in eastern and southeastern Tibetan Plateau, including the eastern Songpan-Ganzi terrane, the Chuan-Dian Diamond Block, and the northern part of Yunnan Province, indicates that the lithospheric mantle is relatively thin in these regions. Combined with other geologic and geophysical results, we propose that the lithospheric mantle of the plateau did not escape to eastern and southeastern Tibetan Plateau where the crust has been thickened by adding crustal material from the interior of the plateau.
WOS关键词VELOCITY STRUCTURE BENEATH ; NORTH CHINA CRATON ; CRUSTAL DEFORMATION ; SEISMIC ANISOTROPY ; DYNAMICS ; MARGIN ; TOMOGRAPHY ; EVOLUTION ; ASIA ; COLLISION
资助项目National Key R&D Program of China[2016YFC0600301] ; National Natural Science Foundation of China[41974053] ; National Natural Science Foundation of China[41888101]
WOS研究方向Geology
语种英语
WOS记录号WOS:000609118800001
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/100035]  
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Tian, Xiaobo; Li, Jiangtao
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
4.Wuhan Univ, Sch Geodesy & Geomat, Dept Geophys, Wuhan 430079, Peoples R China
5.Inst Disaster Prevent, Sanhe 065201, Hebei, Peoples R China
推荐引用方式
GB/T 7714
Nie, Shitan,Tian, Xiaobo,Li, Jiangtao,et al. Lithospheric mantle underneath the Tibetan Plateau does not escape southeastward[J]. JOURNAL OF ASIAN EARTH SCIENCES,2021,206:10.
APA Nie, Shitan,Tian, Xiaobo,Li, Jiangtao,&Tan, Ping.(2021).Lithospheric mantle underneath the Tibetan Plateau does not escape southeastward.JOURNAL OF ASIAN EARTH SCIENCES,206,10.
MLA Nie, Shitan,et al."Lithospheric mantle underneath the Tibetan Plateau does not escape southeastward".JOURNAL OF ASIAN EARTH SCIENCES 206(2021):10.

入库方式: OAI收割

来源:地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。