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 structure of crust in Yunnan and its implication

文献类型:期刊论文

作者Hu, JF; Su, YJ; Zhu, XG; Chen, Y
刊名SCIENCE IN CHINA SERIES D-EARTH SCIENCES
出版日期2005-02-01
卷号48期号:2页码:210-218
关键词Yunnan S-wave Velocity Poisson's Ratio Sichuan-yunnan Diamond Block
ISSN号1006-9313
DOI10.1360/03yd0062
文献子类Article
英文摘要Receiver function of body wave under the 23 stations in Yunnan was extracted from 3-component broadband digital recording of teleseismic event. Thus, the S-wave velocity structure and distribution characteristics of Poisson's ratio in crust of Yunnan are obtained by inversion. The results show that the crustal thickness is gradually thinned from north to south. The crustal thickness in Zhongdian of northwest reaches as many as 62.0 km and the one in Jinghong of further south end is only 30.2 km. What should be especially noted is that there exists a Moho upheaval running in NS in the Chuxiong region and a Moho concave is generally parallel to it in Dongchuan. In addition, there exists an obvious transversal inhomogeneity for the S-wave velocity structure in upper mantle and crust in the Yunnan region. The low velocity layer exists not only in 10.0-15.0 km in upper crust in some regions, but also in 30.0-40.0 km in lower crust. Generally, the Poisson's ratio is on the high side, however it has a better corresponding relation to the crustal velocity structure. An obvious block distribution feature is still shown on such a high background of Poisson's ratio. It is discovered by synthetically analyzing the velocity structure and Poisson's ratio distribution that there are high Poisson's ratio and complicated crust-mantle velocity structure feature in the Sichuan-Yunnan Diamond Block with Xiaojiang fault to be the east boundary and Yulong Snow Mountain fault to be the west boundary besides the frequent seismicity. This feature differs obviously from that of surrounding areas, which would provide geophysical evidence to deeply study the eastwardly flowage of lithospheric substances in the Qinghai-Tibet Plateau.
WOS关键词WESTERN YUNNAN ; PROVINCE ; TIBET ; CHINA
WOS研究方向Geology
语种英语
WOS记录号WOS:000228190600008
出版者SCIENCE CHINA PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/65592]  
专题中国科学院地质与地球物理研究所
通讯作者Hu, JF
作者单位1.Yunnan Univ, Dept Geophys, Kunming 650091, Peoples R China
2.Seismol Bur Yunnan Province, Kunming 650041, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100101, Peoples R China
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Hu, JF,Su, YJ,Zhu, XG,et al. S-wave velocity and Poisson's ratio structure of crust in Yunnan and its implication[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2005,48(2):210-218.
APA Hu, JF,Su, YJ,Zhu, XG,&Chen, Y.(2005).S-wave velocity and Poisson's ratio structure of crust in Yunnan and its implication.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,48(2),210-218.
MLA Hu, JF,et al."S-wave velocity and Poisson's ratio structure of crust in Yunnan and its implication".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 48.2(2005):210-218.

入库方式: OAI收割

来源:地质与地球物理研究所

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