CRUSTAL MATERIAL DENSITY CHANGE BENEATH SHANXI
RIFT AND ITS ADJACENT AREAS FROM 1999 TO 2008
1)Key Laboratory of Earthquake Geodesy, Institute of Seismology, CEA,Wuhan 430071
2）Wuhan Base of Intitute of Crustel Dynamics,CEA，Wuhan 430071
3)School of Geodesy and Geomatics, Wuhan University,Wuhan 430079
4)Geophysical Exploration Centre, China Earthquake Administration,Zhengzhou 450002
Abstract In order to find out the characteristics of crustal material migration in Shanxi rift and its adjacent areas, we got the crustal material density changes based on gravity variations from 1999 to 2008 in the area of Shanxi province, the weight with depth and flatness of the model are taken into account in the inversion process. The result showed the basic characteristic that material accumulation locates in the region of Lüliang Mountain and the middle of Linfen Basin, and material loss locates between the Taihang mountain and the centralsouthern Shanxi rift.
Xuan Songbai,Tan Hongbo,Feng Jianlin et al. CRUSTAL MATERIAL DENSITY CHANGE BENEATH SHANXI
RIFT AND ITS ADJACENT AREAS FROM 1999 TO 2008[J]. jgg, 2013, 33(5): 7-10.
Xuan Songbai,Tan Hongbo,Feng Jianlin et al. CRUSTAL MATERIAL DENSITY CHANGE BENEATH SHANXI
RIFT AND ITS ADJACENT AREAS FROM 1999 TO 2008[J]. jgg, 2013, 33(5): 7-10.
