JpGU-AGU Joint Meeting 2017

Session information

[EE] Poster

S (Solid Earth Sciences) » S-CG Complex & General

[S-CG62] [EE] Dynamics in mobile belts

Tue. May 23, 2017 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall HALL7)

The dynamic behaviours of mobile belts are expressed across a wide range of time scales, from the seismic and volcanic events that impact society during our lifetimes, to orogeny and the formation of large-scale fault systems which can take place over millions of years. Deformation occurs on length scales from microscopic fracture and flow to macroscopic deformation to plate-scale tectonics. To gain a physical understanding of the dynamics of mobile belts, we must determine the relationships between deformation and the driving stresses due to plate motion and other causes, which are connected though the rheological properties of the materials. To understand the full physical system, an integration of geophysics, geomorphology, and geology is necessary, as is the integration of observational, theoretical and experimental approaches. In addition, because rheological properties are greatly affected by fluids in the crust and fluid chemical reactions, petrological and geochemical approaches are also important. After the 2011 great Tohoku-oki earthquake, large-scale changes in seismic activity and regional scale crustal deformation were observed, making present-day Japan a unique natural laboratory for the study of the dynamics of mobile belts. This session welcomes presentations from different disciplines, such as seismology, geodesy, tectonic geomorphology, structural geology, petrology, and geofluids, as well as interdisciplinary studies, that relate to the dynamic behaviour of mobile belts.

*Tadashi Sato1, Tomomi Okada1, Yoshihisa Iio2, Satoshi Matsumoto3, Stephen C Bannister4, John Ristau4, Shiro Ohmi2,5, Tsutomu Miura2, Jarg Pettinga6, Francesca Ghisetti7, Richard Sibson8 (1.Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science, Tohoku University, Japan, 2.Disater Prevention Research Institute, Kyoto University, Japan, 3.Institute of Seismology and Volcanology, Faculty of Sciences, Kyushu University, Japan, 4.GNS Science, New Zealand, 5.Earthquake Hazards Division, Disaster Prevention Research Institute, Kyoto University, Japan, 6.Univerisity of Canterbury, New Zealand, 7.Terra Geologica, New Zealand, 8.University of Otago, New Zealand)

*Tsuyoshi Toyoshima1, Norio Shigematsu2, Yasuhito Osanai3, Masaaki Owada4, Toshiaki Tsunogae5, Tomokazu Hokada6 (1.Department of Geology, Faculty of Science, Niigata University, 2.Research Institute of Earthquake and Volcano Geology, Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, 3.Division of Evolution of Earth Environments, Faculty of Social and Cultural Studies, Kyushu University, 4.Graduate School of Science and Engineering for Innovation, Yamaguchi University, 5.Faculty of Life and Environmental Sciences (Earth Evolution Sciences), University of Tsukuba, 6.National Institute of Polar Research)

*Norio Shigematsu1, Cecile Massiot2, John Townend2, Mai-Linh Doan3, David D. McNamara4, Virginia Toy5, Rupert Sutherland2, DFDP-2 Science Team (1.Research Institute of Earthquake and Volcano Geology, Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, 2.Victoria University of Wellington, 3.University of Grenoble, 4.National University of Ireland, Galway , 5.University of Otago)

Zenshiro Saito2, *Yasuo Ogawa1, Masahiro Ichiki3, Hideyuki Satoh4, Yusuke Kinoshita2, Atsushi Suzuki2, Puwis Amatyakul1 (1.Volcanic Fluid Research Center, School of Science, Tokyo Institute of Technology, 2.Earth and Planetary Sciences, Tokyo Institute of Technology, 3.Graduate School of Science, Tohoku University, 4.National Institute of Advanced Industrial Science and Technology)

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