RESEARCH ON DEFORMATION CHARACTERISTICS OF WEIHE BASIN
Gao Haolin 1) ; Zhu Yiqing 2) ; Han Meitao 1) ; Dou Mali 1) ; and Li Jing 1)
1)Earthquake Administration of Shanxi Province，Xi’an 7100682)Second Crust Monitoring and Application Center, CEA, Xi’an 710054
Abstract The relations between the differences of crustal deformation of Weihe basin leveling profile from 2001 to 2008 and active fault, distribution of cities and towns,underground water level are analyzed, the differences between vertical fracture activity rate gradients on the same or different faults are studied. The activity characteristics that the trend of profile deformation is slow in Weihe basin and meanwhile there is a reverse change in the north to Jingyang since 2004 are discussed.
Key words ：
Weihe basin
leveling profile
vertical deformation
active fault
reverse change
Received: 01 January 1900
Corresponding Authors:
Gao Haolin
Cite this article:
Gao Haolin ,Zhu Yiqing ,Han Meitao et al. RESEARCH ON DEFORMATION CHARACTERISTICS OF WEIHE BASIN [J]. , 2009, 29(3): 60-66.
Gao Haolin ,Zhu Yiqing ,Han Meitao et al. RESEARCH ON DEFORMATION CHARACTERISTICS OF WEIHE BASIN [J]. jgg, 2009, 29(3): 60-66.
URL:
http://www.jgg09.com/EN/ OR http://www.jgg09.com/EN/Y2009/V29/I3/60
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