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《Crustal Deformation and Earthquake》 2004-03
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STUDY ON PRESENT-DAY DEFORMATION AND STRAIN FIELD IN NORTH CHINA BY USE OF GPS DATA

Zhang Jinghua,Li Yanxing,Guo Liangqian and Zhang Zhongfu (First Crust Monitoring and Application Center, CEA, Tianjin 300180)  
Based on the GPS data of the North China and its adjacent areas surveyed in the past more than ten years and the elastic motion model of Eurasia plate, the horizontal deformation field and local horizontal deformation field in the North China area are obtained. The horizontal deformation field in the North China exhibits a rather consistent movement along the SE while the motion direction turns gradually with clockwise, and the movement rate raises from west to east.The motion rates of Ordos, North China plain and Eastern Shandong Huanghai blocks are 4.8 mm/a, 5.0 mm/a and 5.2 mm/a and their motion directions are SE50°, SE40° and SE35°respectively. Besides the deformation rate for local deformation field in the North China is about 50% of that of the horizontal deformation field.The local deformation directions of Ordos, North China plain and eastern Shandong-Huanghai blocks are SE, SSE and SSW, respectively. The relative motion on both sides of major fault zones and the principal strain field in each block are calculated by use of the model with rotation of entire block and linear strain. Basically, the EW and NWW trending faults in the North China are left lateral strike slip ones and the slip rates decrease from east to west,while the NNE and NE trending faults in the North China are right lateral strike slip ones and the slip rates decrease from north to south. The basic frame of strain field in the North China is that: the compression is NEE SWW directional and the extension NNW SSE directional and the principal compressive strain rate increases gradually from west to east and the principal tensile strain rate decreases gradually from west to east. It is inferred on the basis of general characteristics of horizontal deformation field and strain field in the whole area that the main driving forces of the tectonic movement and deformation in the North China are: the NE directional pushing force from Qinghai Tibit plateau, the west directional pushing force to the crust of the North China coming from the underthrust Pacific plate to Eurasia plate, and the NW SE directional extension caused by the uplifting crust.
【Fund】: 国家自然科学基金 (4 0 1742 0 9);; 中国地震局第一监测中心人才培养基金
【CateGory Index】: P228.4
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