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《Seismology and Geology》 2004-03
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CO-SEISMIC SLIP DISTRIBUTION OF THE 2001 WEST OF KUNLUN MOUNTAIN PASS EARTHQUAKE INVERTED BY GPS AND LEVELING DATA

WAN Yong ge 1,2) WANG Min 3) SHEN Zheng kang 1,4) CHEN Jie 1) ZHANG Zu sheng 5) WANG Qing liang 6) GAN Wei jun 1) 1) State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China 2) College of Disaster Prevention Techniques, China Earthquake Administration, Yanjiao, East of Beijing 101601,China 3) Institute of Earthquake Prediction, China Earthquake Administration, Beijing 100036, China 4) Department of Earth and Space Sciences,University of California, Los Angeles, CA 90095 1567, USA 5) First Crustal Deformation Monitoring and Application Center, China Earthquake Administration, Tianjin 300180, China 6) Second Crustal Deformation Monitoring and Application Center, China Earthquake Administration, Xi'an 710054, China  
The co seismic displacement field of the 2001 west of Kunlun Mountain Pass earthquake is obtained through the analysis of GPS data mea ̄sured before and after the earthquake and leveling data measured in 1979 and 2002. Adopting these data, constrained by detail surface rupture data mea ̄sured after the earthquake, we inverted the co seismic slip distribution along the seismic fault. The result shows that the depth of rupture lower limit is 14.2~21km (with 70% confidence level), with 17km as the optimal value. The result also shows that left lateral strike slip of 2~3m exists in the area between the Sun Lake segment and the west end of the main rupture zone, although surface rupture is not observed there. This is consistent with the result of InSAR data analysis. The subsurface rupture of this earthquake is ended at the Sun Lake in the west, but it seems that left lateral slip of 1.5~ 2.0m still exists within the range of 30km to the east of the surface rupture zone. The vertical displacement inverted in this study shows that to the west of 93°E the southern side of the fault is eleva ̄ted, while to the east of 93°E the northern side of the fault is elevated. The released seismic moment estimated by geodetic data and surface rupture surveying is 6.1×10 20 N ·m, consistent with the result inverted by seismic wave records.
【Fund】: 国家自然科学基金重点项目 (4 0 3340 4 2 );; 科技部社会公益研究专项 (2 0 0 2DIA1 0 0 0 1 )共同资助。
【CateGory Index】: P228.4
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