9:00 AM - 9:15 AM
*Koichi Yamauchi1, Masahiro Ishikawa2, Hiroshi Sato1, Takaya Iwasaki1, Tsuyoshi Toyoshima3 (1.Earthquake Research Institute, The University of Tokyo, 2.Yokohama National University, 3.Niigata University)
Oral
Symbol S (Solid Earth Sciences) » S-CG Complex & General
Mon. May 23, 2016 9:00 AM - 10:30 AM 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:Tohru Watanabe(Gradudate School of Science and Engineering, University of Toyama), Masaoki Uno(Graduate School of Environmental Studies, Tohoku University)
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.
9:00 AM - 9:15 AM
*Koichi Yamauchi1, Masahiro Ishikawa2, Hiroshi Sato1, Takaya Iwasaki1, Tsuyoshi Toyoshima3 (1.Earthquake Research Institute, The University of Tokyo, 2.Yokohama National University, 3.Niigata University)
9:15 AM - 9:30 AM
*Tulay Kaya1, Yasuo Ogawa1, Takafumi Kasaya2, Mustafa Kemal Tuncer3, Yoshimori Honkura1, Naoto Oshiman4, Masaki Matsushima1, Weerachai Siripunvaraporn5 (1.Tokyo Institute of Technology, 2.Japan Agency for Marine-Earth Science and Technology, 3.Istanbul University, 4.Kyoto University, 5.Mahidol University)
9:30 AM - 9:45 AM
*Tohru Watanabe1 (1.Gradudate School of Science and Engineering, University of Toyama)
9:45 AM - 10:00 AM
*Mineo Kumazawa1 (1.ELSI, Tokyo Institute of Technology)
10:00 AM - 10:15 AM
*Masaoki Uno1, Syuntaro Masuda1, Nobuo Hirano1, Atsushi Okamoto1, Noriyoshi Tsuchiya1 (1.Graduate School of Environmental Studies, Tohoku University)
10:15 AM - 10:30 AM
*Yoshihisa Iio1, Sho Aoki1, Hiroshi Katao1, Itaru Yoneda1, Masayo Sawada1, Tsutomu Miura1 (1.Disater Prevention Research Institute, Kyoto University)