10:45 AM - 11:00 AM
*Keisuke Yoshida1, Akira Hasegawa2, Toru Matsuzawa2 (1.National research institute for earth science and disaster prevention, 2.Tohoku University)
Oral
Symbol S (Solid Earth Sciences) » S-CG Complex & General
Tue. May 24, 2016 10:45 AM - 12:15 PM A08 (APA HOTEL&RESORT TOKYO BAY MAKUHARI)
Convener:*Yukitoshi Fukahata(Disaster Prevention Research Institute, Kyoto University), Norio Shigematsu(Research Institute of Earthquake and Volcano Geology, Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology), Aitaro Kato(Graduate School of Environmental Studies, Nagoya University), Hikaru Iwamori(Geochemical Evolution Research Program, Japan Agency for Marine-Earth Science and Technology), Yasutaka Ikeda(Department of Earth and Planetary Science, Graduate School of Science, University of Tokyo), Toru Takeshita(Department of Natural History Sciences, Graduate School of Science, Hokkaido University), Chair:Aitaro Kato(Graduate School of Environmental Studies, Nagoya University), Keisuke Yoshida(National research institute for earth science and disaster prevention)
Since the target of dynamics in mobile belts ranges from seismic and volcanic activities, which we can experience during our lifetime, to orogeny and formation of large-scale fault systems, which take place for more than several millions of years, the integration of geophysics, geomorphology and geology is necessary. In order to understand the dynamics in mobile belts from microscopic fracture and flow to macroscopic deformation, we must clarify the spatial and temporal development of stress fields due to plate motion and other tectonic causes and rheological properties of the materials that constitute mobile belts, by using observational, theoretical and experimental approaches. In addition to this, since the rheological properties are greatly affected by fluids in the crust and reactions via fluids, petrological and geochemical approaches are also important. After the 2011 great Tohoku-oki earthquake, we observe large scale changes in seismic activities and crustal movements. The present is the best timing to work on dynamics in mobile belts. This session welcomes presentations from different disciplines, such as seismology, geodesy, tectonic geomorphology, structural geology, petrology, geofluids, etc.
10:45 AM - 11:00 AM
*Keisuke Yoshida1, Akira Hasegawa2, Toru Matsuzawa2 (1.National research institute for earth science and disaster prevention, 2.Tohoku University)
11:00 AM - 11:15 AM
*Aitaro Kato1, Kazushige Obara2, Shin'ichi Sakai2, Tetsuya Takeda3, Takashi Iidaka2, Takaya Iwasaki2 (1.Graduate School of Environmental Studies, Nagoya University, 2.Earthquake Research Institute, The University of Tokyo, 3.National Research Institute for Earth Science and Disaster Prevention)
11:15 AM - 11:30 AM
*Hiroshi Mori1, Shintaro Abe1, Yasuhira Aoyagi2 (1.National Institute of Advanced Industrial Science and Technology (AIST), 2.Central Research Institute of Electric Power Industry (CRIEPI))
11:30 AM - 11:45 AM
*Satoshi Matsumoto1, Takuya NISHIMURA2 (1.Institute of Seismology and Volcanology, Faculty of Sciences, Kyushu University, 2.Disaster Prevention Research Institute, Kyoto University)
11:45 AM - 12:00 PM
*Atsushi Takahashi1, Manabu Hashimoto2 (1.Graduate School of Science, Kyoto University, 2.Disaster Prevention Research Institute, Kyoto University)
12:00 PM - 12:15 PM
*Yuji Himematsu1, Masato Furuya1 (1.Graduate School of Science, Hokkaido University)