中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Varying deformation patterns in central Tibet revealed by radial anisotropy tomography

文献类型:期刊论文

作者Yu, CQ (Yu, Chunquan)3; Zhao, DP (Zhao, Dapeng)1; Zhang, H (Zhang, Heng)2,3; Zhang, H; Zhao, JM (Zhao, Junmeng)2
刊名JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
出版日期2016
卷号121期号:5页码:3445-3461
关键词Upper-mantle Beneath Indian Lithosphere Beneath Seismic Anisotropy Southern Tibet Surrounding Regions Velocity Structure Collision Zone Azimuthal Anisotropy Crustal Structure Uppermost Mantle
DOI10.1002/2016JB012832
文献子类Article
英文摘要P wave radial anisotropy tomography of the upper mantle beneath the central Tibetan plateau is derived using a large number of traveltime data of teleseismic events. Our results show a prominent high-velocity (high-V) zone which is separated by a low-velocity (low-V) anomaly beneath the Himalayan block, extending to similar to 33 degrees N, and a low-V zone down to similar to 300 km depth beneath the northern Qiangtang block. The upper mantle beneath northern Qiangtang exhibits a significant positive radial anisotropy (i.e., horizontal V-p > vertical V-p), implying lateral material flow rather than material upwelling in the upper mantle. In the central part of the study region, a prominent high-V zone exists at depths of 150 to 300 km and exhibits a negative radial anisotropy (i.e., horizontal V-p > vertical V-p), reflecting the subducting Indian lithospheric mantle. Variations of shear wave splitting in this region revealed by previous studies may be attributed to the low-V layer above the Indian lithospheric mantle. A high-V zone with a positive radial anisotropy is located beneath the southern Lhasa block, which is interpreted to be the northward underthrusting Indian lithospheric mantle. Multilayer radial anisotropy is detected beneath southern Tibet, which may reflect a complex deformation pattern there.
学科主题地球物理学
语种英语
WOS记录号WOS:000381626900017
源URL[http://ir.itpcas.ac.cn/handle/131C11/7701]  
专题青藏高原研究所_图书馆
通讯作者Zhang, H
作者单位1.Tohoku Univ, Dept Geophys, Sendai, Miyagi, Japan
2.Chinese Acad Sci, Lab Continental Collis & Plateau Uplift, Inst Tibetan Plateau Res, Beijing, Peoples R China
3.MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA
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Yu, CQ ,Zhao, DP ,Zhang, H ,et al. Varying deformation patterns in central Tibet revealed by radial anisotropy tomography[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2016,121(5):3445-3461.
APA Yu, CQ ,Zhao, DP ,Zhang, H ,Zhang, H,&Zhao, JM .(2016).Varying deformation patterns in central Tibet revealed by radial anisotropy tomography.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,121(5),3445-3461.
MLA Yu, CQ ,et al."Varying deformation patterns in central Tibet revealed by radial anisotropy tomography".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 121.5(2016):3445-3461.

入库方式: OAI收割

来源:青藏高原研究所

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