Fault activity and earthquake based on tectonic maps including subsurface structure and drilling data

在这项研究中，我们确定在日本东北部南部的构造地貌，根据长期的永久变形与重复地震板内孕震断层，高分辨率stareopair解释和现场地质。虽然该地区的滑动速率和活动断层的分布已被揭示，但弧后快速沉降盆地和/或沿海地区的盲冲断层的分布仍完全没有得到解决，应在未来的研究中进行彻底的探索。

In this study we identified tectonic landforms in southern Northeastern Japan according to long-term permanent deformation associated with repeated earthquakes on intraplate seismogenic faults, based on high-resolution stareopair interpretations and field geology. Whereas rates of slip and distributions of active faults in this region are revealed, distribution of blind thrusts in rapidly subsiding basin and/or beneath coastal areas in the back arc remain fully unresolved and should be thoroughly sought in future researches.