中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Seismic Azimuthal Anisotropy of Northeastern Tibetan Plateau From Ambient Noise Double Beamforming Tomography: Implications for Crustal Deformation

文献类型:期刊论文

作者Wu, Xiaoyang1,2; Guo, Zhen2,3; Li, Shilin2; Yu, Yong2; Bai, Qipeng4; Chen, Yongshun John2
刊名JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
出版日期2023-06-01
卷号128期号:6页码:16
ISSN号2169-9313
关键词seismic ambient noise tomography double beamforming northeastern Tibetan Plateau seismic azimuthal anisotropy crustal deformation
DOI10.1029/2022JB026109
通讯作者Guo, Zhen(guoz3@sustech.edu.cn) ; Chen, Yongshun John(johnyc@sustech.edu.cn)
英文摘要In this study, we obtain a three-dimensional (3-D) high resolution seismic anisotropy model of NE Tibet using ambient noise double beamforming (DBF) tomography with ChinArray-Himalaya II data. DBF tomography technique allows for the simultaneous derivation of local phase velocity and azimuthal anisotropy from ambient noise cross-correlations without performing tomographic inversion. Based on the DBF tomography results, we have constructed a high resolution 3-D azimuthal anisotropic shear wave velocity model of NE Tibet. Our model indicates the presence of prominent low velocities and strong azimuthal anisotropy in the mid-to lower crust beneath the Songpan-Ganzi belt, while the mid-to lower crust of the Qilian belt exhibits relatively weak low velocity and azimuthal anisotropy. We propose that crustal channel flow may be the primary mechanism driving crustal deformation in the Songpan-Ganzi belt, which is in the mature part of the plateau. As the Qilian belt is at an early stage of plateau formation, it is characterized by crustal shortening with the development of a sub-vertical foliation. Additionally, the misalignment between predicted and observed shear wave splitting reveals decoupled crust and upper mantle deformation west of the Ordos block where eastward mantle flow is deflected by the lithospheric keel of Ordos.
WOS关键词SURFACE-WAVE TOMOGRAPHY ; LOW-VELOCITY ZONE ; MANTLE DEFORMATION ; RADIAL ANISOTROPY ; CROSS-CORRELATION ; QILIAN-SHAN ; BENEATH ; EASTERN ; INVERSION ; EVOLUTION
资助项目National Science Foundation of China[42122027] ; National Science Foundation of China[41974052] ; National Science Foundation of China[41890814] ; National Science Foundation of China[U1901602] ; National Science Foundation of China[41904056] ; Shenzhen Sustainable Development Science and Technology Project[KCXFZ20201221173608023] ; Shanghai Science and Technology Committee[19dz1200200]
WOS研究方向Geochemistry & Geophysics
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:000999811800001
源URL[http://ir.qdio.ac.cn/handle/337002/183223]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Guo, Zhen; Chen, Yongshun John
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China
2.Southern Univ Sci & Technol, Dept Ocean Sci & Engn, Shenzhen, Peoples R China
3.Shanghai Sheshan Natl Geophys Observ & Res Stn, Shanghai, Peoples R China
4.Southern Univ Sci & Technol, Acad Adv Interdisciplinary Studies, Shenzhen, Peoples R China
推荐引用方式
GB/T 7714
Wu, Xiaoyang,Guo, Zhen,Li, Shilin,et al. Seismic Azimuthal Anisotropy of Northeastern Tibetan Plateau From Ambient Noise Double Beamforming Tomography: Implications for Crustal Deformation[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2023,128(6):16.
APA Wu, Xiaoyang,Guo, Zhen,Li, Shilin,Yu, Yong,Bai, Qipeng,&Chen, Yongshun John.(2023).Seismic Azimuthal Anisotropy of Northeastern Tibetan Plateau From Ambient Noise Double Beamforming Tomography: Implications for Crustal Deformation.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,128(6),16.
MLA Wu, Xiaoyang,et al."Seismic Azimuthal Anisotropy of Northeastern Tibetan Plateau From Ambient Noise Double Beamforming Tomography: Implications for Crustal Deformation".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 128.6(2023):16.

入库方式: OAI收割

来源:海洋研究所

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