Vertical Deformation Characteristics of Shanxi-Hebei-Inner Mongolia Area
1 First Crust Monitoring and Application Center,CEA,7 Naihuo Road,Tianjin 300180,China
Abstract Based on collation and adjustment of the 1998, 2006 and 2013 leveling survey data of the Shanxi-Hebei-Inner Mongolia region, we obtain the vertical deformation rate and gradient for the periods of 1998-2006 and 2006-2013. We then analyze the regional geological unit of the Shanxi-Hebei-Inner Mongolia vertical deformation rates, the evolution of the gradient and the main fault zone activity properties. The result shows that the vertical deformation rise rate of Lüliang mountain increases, the vertical deformation rise rate of Taihang mountain declines, and the Yunzhong mountain and Xizhou mountain piedmont fault turns to reverse fault. The activity of Kouquan fault, North Yanggao basin fault, South Yanggao basin fault and South Weixian basin fault, all present normal fault activity.
Key words ：
vertical deformation
rate
gradient
structure activity
Shanxi-Hebei-Inner Mongolia region
Received: 06 June 2014
Published: 02 June 2015
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