中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
S wave velocity and Poisson's ratio tomography of the Tibetan Plateau

文献类型:期刊论文

作者Qu Chen3; Liu XiaoYu4; Yu ChangQing3; Xu Yi1,2; Yang WenCai2
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
出版日期2020-10-01
卷号63期号:10页码:3640-3652
ISSN号0001-5733
关键词Tibetan Plateau S wave Poisson's ratio Three-dimensional tomography Volcanic rock belt Crustal detachment Cenozoic rift Eastern structural syntaxis
DOI10.6038/cjg2020N0236
英文摘要In this study, three-dimensional tomographic studies of crustal seismic wave velocity structure beneath the Tibetan Plateau were carried out using seismic travel time data from China Digital Seismograph Network (CDSN) (2009-2016) seismic stations. The three-dimensional S-wave velocity structure and Poisson's ratio distribution of the Tibetan Plateau with a resolution of 1 degrees X 1 degrees X 20 km were obtained. The results show that the negative anomalous zones of S-wave velocity and high Poisson's ratio zones could be found from the upper crust to the lower crust under the high-potassium and potash volcanic belts of Kekexili and northern Qiangtang. This indicates that during the Tertiary Tibetan Plateau uplift, the East Kunlun Triassic suture zone reruptured due to continental collisions, resulting the upwelling of massive crust-mantle mixed molten material and volcanic eruption. This further reveals that the existence of Cenozoic volcanic belts in the northern Tibetan Plateau is closely related to the formation and uplift of the Tibetan Plateau. The Cenozoic rift zones of the Tibetan Plateau are located at both sides of the S-wave velocity negative anomaly zones in middle-lower crust, the Poisson's ratio below the rift zones in middle-lower crust are less than 0. 22. From the anomalous distribution of S-wave velocity and Poisson's ratio in middle-lower crust under the Cenozoic rift zones of Tibetan Plateau, it could be deduced that the Cenozoic rift of Tibetan Plateau had reached the bottom of the middle crust. This is consistent with the conclusions from the crustal density imaging study of the Tibetan Plateau using gravity inversion. The S-wave velocity and Poisson's ratio of the Tibetan Plateau change sharply with depth from lower crust to crust-mantle boundary, which indicates that large-scale interlayer detachment and horizontal shear occurred in the crust. The Poisson's ratio of the eastern tectonic syntaxis in the Tibetan Plateau is as high as 0. 29-0. 33, and the S-wave velocity perturbation under eastern tectonic syntaxis is negative. This infers that the crust below the eastern tectonic syntaxis is mainly composed of hard serpentinized peridotite. The negative anomalous zones of the S-wave velocity in the middle and lower crust of the Tibetan Plateau is widely expanded, and the bottom of the crust under Tibetan Plateau is almost covered by the negative anomalous zones of the S-wave velocity. Such characteristic of distribution of anomalous of the S-wave velocity may reflect the influence of pipeline flow in the lower crust.
WOS关键词LITHOSPHERE BENEATH ; AMBIENT NOISE ; CRUSTAL ; EASTERN ; LONGMENSHAN ; DYNAMICS ; SOUTHERN ; CHINA
WOS研究方向Geochemistry & Geophysics
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:000575879600005
源URL[http://ir.iggcas.ac.cn/handle/132A11/98296]  
专题中国科学院地质与地球物理研究所
通讯作者Yang WenCai
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Zhejiang Univ, Sch Earth Sci, Hangzhou 310027, Peoples R China
3.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China
4.China Univ Geosci Beijing, Sch Geophys & Informat Technol, Beijing 100083, Peoples R China
推荐引用方式
GB/T 7714
Qu Chen,Liu XiaoYu,Yu ChangQing,et al. S wave velocity and Poisson's ratio tomography of the Tibetan Plateau[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2020,63(10):3640-3652.
APA Qu Chen,Liu XiaoYu,Yu ChangQing,Xu Yi,&Yang WenCai.(2020).S wave velocity and Poisson's ratio tomography of the Tibetan Plateau.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,63(10),3640-3652.
MLA Qu Chen,et al."S wave velocity and Poisson's ratio tomography of the Tibetan Plateau".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 63.10(2020):3640-3652.

入库方式: OAI收割

来源:地质与地球物理研究所

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