Presentation Information
[G2-O-2]Paleo-earthquakes as indicated by deep-sea turbidites off Omae-zaki and their recurrence intervals in the Holocene
*Ken IKEHARA1, Toshiya KANAMATSU2, Kan-Hsi HSIUNG2, Takashi ISHIZAWA3, Yasufumi SATOGUCHI4, Yoshitaka NAGAHASHI5 (1. National Institute of Advanced Industrial Science and Technology, 2. Japan Agency for Marine-Earth Science and Technology, 3. Tohoku University, 4. Lake Biwa Museum, 5. Fukushima University)
Keywords:
earthquake,turbidite,terminal basin,Nankai Trough,Holocene
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