Underground structure of Tsukiyoshi fault in the Tono area, Central Japan; What is the feature of reverse fault in granitic regions ?

Nohara, Tsuyoshi; Miwa, Atsushi*; Shimada, Koji

no journal, , 

The spray faults are developed in the sedimentary rocks in the reverse fault zone in North East Japan. On the other hand, fault structure of the granite region is not understood well. In this research, the Tsukiyoshi fault is investigated as a case study, using core data. As a result, the spray fault of the Tsukiyoshi fault is not recognized.