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《Crustal Deformation and Earthquake》 2005-03
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TECTONIC MOVEMENT OF CHINESE MAINLAND REVEALED FROM GPS DATA

Sun Jianzhong~(1) and Yang Shaomin~(2,3,4)1)National Earthquake Infrastructure Service,Beijing1000362)Institute of Seismology,CEA,Wuhan4300713)Crustal Movement Laboratory,Wuhan4300714)Wuhan Base of Institute of Crustal Dynamics,CEA,Wuhan430071  
We have analyzed GPS observations in 1999,2001 and 2004 from more than one thousand stations in the Crustal Movement Observation Network of China including fiducial network,basis networks,regional network by GIPSY software,and calculated the crustal movement velocity field of Chinese mainland with the accuracy better than 2 mm/a of most sites and better than 1.5 mm/a at fiducial sites.Assuming that the contemporary tectonic activity can be treated as continuous, we have combined the GPS observations of areas around China, including Mongolia,Myanmar,India,Nepal and Himalayas, using a bicubic spline interpolation function to simulate the integral horizontal velocity,which shows the regional characteristics of tectonic movement of Chinese mainland,and reveal that the eastwards extrusion and interior deformation of Qinghai-Tibet plateau play dominant action in accommodating the collision of India Plate with Eurasia Plate at present day.
【Fund】: 国家自然科学基金(40274007 40304002)
【CateGory Index】: P542;P228.4
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