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DOI10.1002/2017JB014184
Internal Deformation of Lithosphere Beneath Central Tibet
Zhang, Heng; Zhao, Dapeng; Zhao, Junmeng; Hu, Zhaoguo
通讯作者Zhang, H (通讯作者)
发表日期2017
ISSN2169-9313
EISSN2169-9356
起始页码7329
结束页码7342
卷号122期号:9
英文摘要We use a large number of high-quality P wave arrival time data recorded by the Hi-CLIMB project to determine a 3-D model of azimuthal anisotropy tomography beneath central Tibet. In the Himalayan block, variations of fast velocity orientation (FVO) are revealed from the crust to the upper mantle. In contrast, the FVO in the Lhasa block exhibits only a slight difference between the lower crust and upper mantle, reflecting a coherent deformation there. Different FVOs are revealed near the Bangong-Nujiang suture, which may reflect anisotropies in different parts of the underthrusting Indian plate. In the upper mantle beneath the Qiangtang block, a strong anisotropy is revealed in the shallower part, whereas a weak anisotropy appears in the deeper part, suggesting that a two-layer anisotropy model is applicable there. A layered lithosphere is detected in the eastern part of the Lhasa block, whereas a consistent FVO is revealed in its western part. Our results indicate that strong deformation has occurred in both the Indian and Eurasian lithospheres.
关键词JAPAN SUBDUCTION ZONEAZIMUTHAL ANISOTROPYSEISMIC ANISOTROPYVELOCITY STRUCTURESOUTHERN TIBETTOMOGRAPHYMANTLECRUSTALCONSTRAINTSFLOW
语种英语
WOS研究方向Geochemistry & Geophysics
WOS类目Geochemistry & Geophysics
WOS记录号WOS:000412881700020
来源期刊JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/258994
推荐引用方式
GB/T 7714
Zhang, Heng,Zhao, Dapeng,Zhao, Junmeng,et al. Internal Deformation of Lithosphere Beneath Central Tibet[J]. 中国科学院青藏高原研究所,2017,122(9).
APA Zhang, Heng,Zhao, Dapeng,Zhao, Junmeng,&Hu, Zhaoguo.(2017).Internal Deformation of Lithosphere Beneath Central Tibet.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,122(9).
MLA Zhang, Heng,et al."Internal Deformation of Lithosphere Beneath Central Tibet".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 122.9(2017).
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