Japan Geoscience Union Meeting 2018

Session information

[EJ] Oral

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

[S-CG58] Investigation of inputs to subduction zones: Influence of tectonic processes on the incoming plate

Wed. May 23, 2018 10:45 AM - 12:15 PM 302 (3F International Conference Hall, Makuhari Messe)

convener:Makoto Yamano(Earthquake Research Institute, the University of Tokyo), Tomoaki Morishita(School of Natural System, Colleage of Science and Technology, Kanazawa University), Gou Fujie(海洋研究開発機構), Chairperson:Yamaguchi Asuka(Atomosphere and Ocean Research Institute, The University of Tokyo), Fujie Gou(Japan Agency for Marine-Earth Science and Technology)

Various tectonic processes occur on the seaward side of the trench associated with bending of the incoming oceanic plate, e.g., fracturing of oceanic crust, infiltration of water, and intraplate volcanism. Investigation of these processes and their influence on the incoming plate provides important information on the boundary condition at the trench, inputs to subduction zones. We welcome contributions from a broad range of earth science (geophysics, geology, petrology, and so on) discussing topics related to inputs to subduction zones such as occurrence of tectonic processes due to bending of the incoming plate, modification of the incoming plate by the processes, relationship between the processes and the inherited structure of the incoming plate, and influence of the processes on the subduction plate interface. We hope discussions are made on studies of a variety of subduction zones, including the Japan Trench and the Nankai Trough, and comparative studies among different subduction zones.

10:45 AM - 11:00 AM

*Koichiro Obana1, Gou Fujie1, Yasuyuki Nakamura1, Tsutomu Takahashi1, Yojiro Yamamoto1, Yuka Kaiho1, Seiichi Miura1, Yasushi Ishihara1, Shuichi Kodaira1, Masanao Shinohara2 (1.Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology, 2.Earthquake Research Institute, University of Tokyo)

12:00 PM - 12:15 PM

*Atsushi Nakao1, Hikaru Iwamori2,3, Tomoeki Nakakuki4, Yujiro Suzuki1, Hitomi Nakamura2,3,5 (1.Earthquake Research Institute, The University of Tokyo, 2.Japan Agency for Marine-Earth Science and Technology, 3.Department of Earth and Planetary Sciences, Tokyo Institute of Technology, 4.Department of Earth and Planetary Systems Science, Hiroshima University, 5.Ocean Resource Research Center for Next Generation, Chiba Institute of Technology)

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