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《Journal of Geodesy and Geodynamics》 2008-03
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EFFECT OF KUNLUN Ms 8.1 EARTHQUAKE ON CRUSTAL DEFORMATION IN NORTHEASTERN MARGIN OF QINGHAI-TIBET PLATEAU

Cui Duxin,Wang Qingliang and Wang Wenping(Second Crust Monitoring and Application Center,CEA,Xi'an 710054)  
The seismic fault parameters can be inversed with Okada model based on the deformation data before and after earthquakes in the focal region and its adjacent area.Co-seismic displacements are simulated by use of these parameters and then the regional velocity field is obtained by deducting the co-seismic displacements from the GPS observation displacements.We processed and analyzed the data in northeastern margin of the Qinghai-Tibet plateau observed during 2001-2003 in two steps: firstly,simulated the displacements generated by Kunlun Ms{8.1 earthquake occurred in 2001 in this region,and then obtained the horizontal crustal velocity field by deducting the co-seismic displacements.The results reveal: 1) the effect of Kunlun Ms8.1 earthquake on the northeastern margin of Qinghai-Tibet plateau is obvious;2) the velocity field obtained with this method is better than the original GPS velocity field for reflecting the status of regional crustal movements and strain.
【Fund】: 国家自然科学基金(40674057);; 地震科学联合基金(A07132)
【CateGory Index】: P315.2
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