2015年5月25日(月) 09:00 〜 10:45 国際会議室 (2F)

コンビーナ:*金川 久一(千葉大学大学院理学研究科)、Demian Saffer(Dept. of Geosciences, The Pennsylvania State University, USA)、Michael Strasser(Geological Institute, Seiss Federal Insitute of Technology ETH Zurich)、山田 泰広(京都大学工学研究科都市社会工学専攻)、小平 秀一(海洋研究開発機構　地球内部ダイナミクス領域)、日野 亮太(東北大学災害科学国際研究所)、氏家 恒太郎(筑波大学生命環境系)、伊藤 喜宏(京都大学防災研究所)、座長:日野 亮太(東北大学災害科学国際研究所)、小平 秀一(海洋研究開発機構　地震津波海域観測研究開発センター)

Subduction zone megathrust earthquakes and their accompanying tsunamis, such as the Tohoku-oki earthquake on March 11 in 2011, have caused severe damage in the past. Scientists have worked for decades to understand these devastating events, mostly based on seismic, tsunami and geodetic observations. In addition to these remote monitoring studies, the challenge of drilling into and directly sampling megathrust faults at seismogenic depth, analysis of drill core and downhole logs, experiments on sampled fault materials, and borehole measurements at depth has recently been taken up or being planned by the Integrated Ocean Drilling or International Ocean Discovery Program at Nankai Trough (Nankai Trough Seismogenic Zone Experiment), Japan Trench (Japan Trench Fast Drilling Project and Tracking Tsunamigenic Slips in the Japan Trench), offshore Costa Rica (Costa Rica Seismogenesis Project), and at the Hikurangi margin. In this session, we welcome presentations based on such frontier studies, in addition to those based on seismic, tsunami and geodetic observations, numerical modeling, and analyses of fault rocks exhumed from seismogenic depth.