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

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.

Language	:	Japanese
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Meeting title	:	北淡活断層シンポジウム2008
Held date	:	2008/01
Location (city)	:	淡路
Location (country)	:	日本
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Registration No. : BB20072932
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