1)Key Laboratory of Earthquake Geodesy,Institute of Seismology, CEA, Wuhan 430071;2)Wuhan Base of Institute of Crustal Dynamics,CEA,Wuhan 430071;3)China Earthquake Network Center, Beijing 100045;4)Chengdu University of Technology, Chengdu 610059
Abstract：Using the CMONOC’s GPS data relative to Eurasia from 2009 to 2011, with the method of twodimensional finite element and carefully considering the blocks of second order and active fault of the geological structure in the studied area.The velocity field was analyzed, strain rate field in the Tibetan Plateau region was simulated and the deformation characteristics of the Tibetan plateau area was analyzed.
