Wen Liu, Fumio Yamazaki, Takashi Nonaka, Tadashi Sasagawa
33rd Asian Conference on Remote Sensing 2012, ACRS 2012 1 87-94 2012年 査読有り
After the March 11, 2011 Tohoku, Japan earthquake (Mw9.0), numerous aftershocks and induced events occurred in the source region of the main shock and its outside areas. One of the most damaging induced earthquakes with Mw7.1 occurred in Fukushima prefecture on April 11, 2011. This event caused the numerous fault scarps, with a maximum displacement of 2.3 m. In this study, two temporal TerraSAR-X images were used to detect the crustal movements in Fukushima region due to these events by two different methods. Firstly, the interferometric (InSAR) analysis was carried out to detect the crustal movement to the radar sensor direction. Due to the temporal decorrelation, InSAR fringes could be obtained in a small part of the area. Secondly, the building-based pixel-offset method, proposed by the present authors, was applied to the SAR intensity images. 2D movements were detected for a half of the study area. Finally, the results were compared with the recorded displacements from GPS ground stations. The difference between the movements detected by the second method and the records was less than 0.3 m, showing high accuracy of our method.