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Static and kinematic analysis of coseismic deformation of Wenchuan Ms8.0 earthquake
|Authors:||Xu Shaoguang; Xiong Yongliang; Liao Hua; Wu Yaoqiang; Lu Yipei|
|Author Affiliations:||Primary: |
Southwest Jiaotong University, Department of Surveying and Geo-informatics, Chengdu, China
Earthquake Administration of Sichuan Province, China
|Volume Title:||Dadi Celiang yu Diqiu Dongli Xue Journal of Geodesy and Geodynamics|
|Source:||Dadi Celiang yu Diqiu Dongli Xue = Journal of Geodesy and Geodynamics, 30(3), p.27-30,54. Publisher: Gai Kan Bianjibu, Wuhan, China. ISSN: 1671-5942|
|Note:||In Chinese with English summary. 13 refs.|
|Summary:||Before and after the Wenchuan Ms8.0 earthquake on 12th May 2008, the coseismic deformation changes greatly, the horizontal deformation at PIXI, MYAN, ZHJI and CHDU GPS stations reached 70cm, 31cm, 23cm, 20cm respectively. The most deformations are towards northwest 45°, nearly the orthogonal direction of the fault, and the right region, i.e. Chengdu plain of the fault appears downward. The results of kinematic GPS data processing show that the maximum deformation of PIXI reached about 1m during the earthquake. At last, on the basis of the region time recorded at the stations of the Sichuan GPS network, the average S wave velocities from Wenchuan to all the GPS stations of the network are computed.|
|Subjects:||Body waves; Coseismic processes; Deformation; Earthquakes; Elastic waves; Focal mechanism; Kinematics; S-waves; Seismic waves; Velocity; Wenchuan earthquake 2008; Asia; China; Far East; Sichuan China; Wenchuan China|
|Coordinates:||N311323 N311323 E1031948 E1031948|
|Copyright Information:||GeoRef, Copyright 2021 American Geosciences Institute.|
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