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The Present Space-Time Motion and Deformation Features of the Northeastern Margin of the Qinghai-Xizang(Tibet) Block and Its Adjacent Area
作者姓名:Zhang  Xiaoliang
作者单位:[1]TheSecondCrustalDeformationMonitoringCenter,CEA,Xi'an710054,China [2]CenterforAnalysisandPrediction,CEA,Beijing100036,China [3]InstituteofSeismology,CEA,Wuhan430071,China [4]TheSecondCrustalDeformationMonitoringCenter,CEA,Xi'an710054,China
基金项目:ThisresearchwassponsoredbytheNationalKeyFoundationResearch“StrongEarthquakeMechanismandPredictionontheChineseMainland”(G1998040703)andtheJointEarthquakeScienceFoundation(603002),China.
摘    要:On the basis of Discontinuous Deformation Analysis (DDA), and considering the moderate intrusion of specific block boundaries to different extents, the first-order block motion model is established for the northeastern margin of Qinghai-Xizang(Tibet) block and the kinematical model for depicting deformation of small regions as well by using GPS observations of three periods (1991, 1999 and 2001). By simulating, we obtained the motion features of the firstorder blocks between the large WWN faults on the sides of the studied region, the distribution features of the principal strain rate field and the inhomogeneous motion features with spacetime of the faults in the northern boundary of the Qinghai-Xizang (Tibet) block.

关 键 词:青海-西藏  不连续变形  GPS观测  活动板块  地壳运动

The Present Space-Time Motion and Deformation Features of the Northeastern Margin of the Qinghai-Xizang(Tibet) Block and Its Adjacent Area
Zhang Xiaoliang.The Present Space-Time Motion and Deformation Features of the Northeastern Margin of the Qinghai-Xizang(Tibet) Block and Its Adjacent Area[J].Earthquake Research in China,2004,18(2):161-170.
Authors:Zhang Xiaoliang
Institution:Zhang Xiaoliang 1),Jiang Zaisen 2),Wang Shuangxu 1),Zhang Xi 1),Wang Qi 3) and Chen Bing 1) 1)The Second Crustal Deformation Monitoring Center,CEA,Xi'an 710054,China 2)Center for Analysis and Prediction,CEA,Beijing 100036,China 3)Institute of Seismology,CEA,Wuhan 430071,China
Abstract:On the basis of Discontinuous Deformation Analysis (DDA), and considering the moderate intrusion of specific block boundaries to different extents, the first-order block motion model is established for the northeastern margin of Qinghai-Xizang(Tibet) block and the kinematical model for depicting deformation of small regions as well by using GPS observations of three periods (1991, 1999 and 2001). By simulating, we obtained the motion features of the first-order blocks between the large WWN faults on the sides of the studied region, the distribution features of the principal strain rate field and the inhomogeneous motion features with space-time of the faults in the northern boundary of the Qinghai-Xizang (Tibet) block.
Keywords:The northeastern margin of Qinghai-Xizang(Tibet) block  Discontinuous Deformation Analysis  GPS observations  Active block
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