Surface Deformation Monitoring of Linfen Basin with Sentinel-1 Data
Abstract Based on previous work, this paper uses a stacking technique with 12 scenes and 27 interferograms to obtain the deformation rate in 2015-2016. The results demonstrate main subsidence area is distributed between Luoyunshan and Emei-Zijinshan fault zones. The value is greater than 40mm in the subsidence center, which is assembled with the underground contour. The deformation is caused by excessive pumping and the active fault zone.
Key words :
Linfen basin
sentinel-1
deformation rate
stacking
Cite this article:
WANG Xiaying,ZHAO Chaoying,LIU Yuanyuan et al. Surface Deformation Monitoring of Linfen Basin with Sentinel-1 Data[J]. jgg, 2018, 38(7): 734-737.
WANG Xiaying,ZHAO Chaoying,LIU Yuanyuan et al. Surface Deformation Monitoring of Linfen Basin with Sentinel-1 Data[J]. jgg, 2018, 38(7): 734-737.
URL:
http://www.jgg09.com/EN/ OR http://www.jgg09.com/EN/Y2018/V38/I7/734
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