中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Reconstruction of the S-wave velocity structure of crust and mantle from seismic surface wave dispersion in Sichuan-Yunnan Region

文献类型:期刊论文

作者Zhang Zhi1; Chen Yun2; Li Fei2
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
出版日期2008-07-01
卷号51期号:4页码:1114-1122
关键词frequency-time analysis surface wave dispersion crustal and upper mantle structure thickness of the crust S wave velocity
ISSN号0001-5733
文献子类Article
英文摘要We apply the technique of matched filter frequency time analysis to process long period surface wave data covering Sichuan and Yunnan regions, and then obtain the surface wave group velocity dispersion in the period range 10 similar to 100 s. Then we use the grid inversion method to extract pure path dispersion in the grid of 1.5 degrees x 1.5 degrees after getting the distance and time in the grid of the study area by ray tracing, at the same time, we employ the damped least-square method to determine the crust-mantle S wave velocity structure in the Sichuan and Yunnan region. The result shows that the crust of the region is thickened and shortened. In spite of some local low velocity anomalies, the crust and uppermost mantle of the rhombic Chuan-Dian block as a whole have relatively high velocity as compared with the surrounding areas. The peripheral strike-slipping faults display negative velocity anomalies down to the top of upper mantle, which facilitates the lateral extrusion of crustal blocks along the faults. The high conductivity layer in the crust and upper mantle in western Yunnan and Sichuan is connected with partial melting or detachment structure. The average depth of Moho of Sichuan basin is about 48 kin. The Moho in Yunnan reaches 58 km in the north end and is about 51 km in the south end, which proves that different blocks are affected differently by tectonic movement.
WOS关键词SOUTHWESTERN CHINA ; RECEIVER FUNCTION ; BINCHUAN ; PROVINCE ; ZHEFANG ; PROFILE ; MALONG ; ZONE ; ASIA
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000258061300020
出版者SCIENCE CHINA PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/69856]  
专题中国科学院地质与地球物理研究所
通讯作者Zhang Zhi
作者单位1.Guilin Inst Technol, Dept Resource & Environm Engn, Key Lab Geol Engn Ctr Guangxi Prov, Guilin 541004, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Zhang Zhi,Chen Yun,Li Fei. Reconstruction of the S-wave velocity structure of crust and mantle from seismic surface wave dispersion in Sichuan-Yunnan Region[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2008,51(4):1114-1122.
APA Zhang Zhi,Chen Yun,&Li Fei.(2008).Reconstruction of the S-wave velocity structure of crust and mantle from seismic surface wave dispersion in Sichuan-Yunnan Region.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,51(4),1114-1122.
MLA Zhang Zhi,et al."Reconstruction of the S-wave velocity structure of crust and mantle from seismic surface wave dispersion in Sichuan-Yunnan Region".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 51.4(2008):1114-1122.

入库方式: OAI收割

来源:地质与地球物理研究所

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