3:30 PM - 3:45 PM
[SCG61-07] Relative significance of Si-, Mg- and CO2-metasomatism at shallow mantle wedge
★Invited Papers
*Atsushi Okamoto1, Ryosuke Oyanagi2, Shunya Okino1 (1.Tohoku Univ., 2.Kokushikan Univ.)
[J] Oral
S (Solid Earth Sciences ) » S-CG Complex & General
Wed. May 28, 2025 3:30 PM - 5:00 PM 103 (International Conference Hall, Makuhari Messe)
convener:Yukitoshi Fukahata(Disaster Prevention Research Institute, Kyoto University), Hikaru Iwamori(Earthquake Research Institute, The University of Tokyo), Kiyokazu Oohashi(National Institute of Advanced Industrial Science and Technology ), Chairperson:Hikaru Iwamori(Earthquake Research Institute, The University of Tokyo), Satoshi Matsumoto(Institute of Seismology and Volcanology, Faculty of Sciences, Kyushu University)
The dynamic behaviors 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 associated with plate motion and other causes, which are connected through the rheological properties of the materials. To understand the full physical system, an integration of geophysics, geomorphology, geology, petrology, and geochemistry is necessary, as is the integration of observational, theoretical and experimental approaches. In particular, rheological properties, which are physically affected by fluids in the crust and chemical reactions assisted by fluids, can be resolved only through such an interdisciplinary approach. Frequent large earthquakes, such as the 2011 Tohoku-oki, the 2016 Kumamoto, and the 2024 Noto Peninsula Earthquakes, which were accompanied by significant changes in seismic activity and crustal deformation, 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, geochemistry and hydrology, as well as interdisciplinary studies, that relate to the dynamic behaviors of mobile belts.
3:30 PM - 3:45 PM
*Atsushi Okamoto1, Ryosuke Oyanagi2, Shunya Okino1 (1.Tohoku Univ., 2.Kokushikan Univ.)
3:45 PM - 4:00 PM
*Dyuti Prakash Sarkar1, Jun-ichi Ando2, Hirokazu Kato3, Akihiro Kano4, Kaushik Das2, Gautam Ghosh5 (1.Yamaguchi University, 2.Hiroshima University, 3.Tokyo University, 4.Teikyo University, 5.Presidency University Kolkata)
4:00 PM - 4:15 PM
*Ryotaro Fujimura1, Tomomi Okada1, Martha Savage2, Ayaka Tagami1,3, Harumi Uchida1, Mako Ohzono3, Hiroaki Takahashi3 (1.Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science, Tohoku University, 2.Victoria University of Wellington, 3.Institute of Seismology and Volcanology, Faculty of Science, Hokkaido University)
4:15 PM - 4:30 PM
*Reina Akiyama1, Ryosuke Doke2, Koji Umeda2 (1.Graduate School of Sustainable Community Studies, Hirosaki University, 2.Graduate School of Science and Technology, Hirosaki University)
4:30 PM - 4:45 PM
*Satoshi Matsumoto1 (1.Institute of Seismology and Volcanology, Faculty of Sciences, Kyushu University)
4:45 PM - 5:00 PM
*Mitsuhiro Matsuura1 (1.University of Tokyo)
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