SIMULATION ANALYSIS OF TECTONIC DEFORMATION OF TIBETAN PLATEAU AREA
Lü Jian 1,2) ;Li Zhengyuan 3) ;Chen Zhiyao 1,2) ;Feng Guangyu 1) ; Li Guoming 4) ;Dang Xuehui 1) ; and Meng Qingxiao 1)
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.
Key words ：
GPS
finite element
strain rate
block
deformation
Received: 01 January 1900
Corresponding Authors:
Lü Jian
Cite this article:
Lü Jian,Li Zhengyuan ,Chen Zhiyao et al. SIMULATION ANALYSIS OF TECTONIC DEFORMATION OF TIBETAN PLATEAU AREA[J]. , 2012, 32(Supp.): 1-4.
Lü Jian,Li Zhengyuan ,Chen Zhiyao et al. SIMULATION ANALYSIS OF TECTONIC DEFORMATION OF TIBETAN PLATEAU AREA[J]. jgg, 2012, 32(Supp.): 1-4.
URL:
http://www.jgg09.com/EN/ OR http://www.jgg09.com/EN/Y2012/V32/ISupp./1
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