*塩原 肇1、歌田 久司1、Seung-Sep Kim2、YoungHee Kim3、馬場 聖至1、一瀬 建日1、Hogyum Kim3、HyeJeong Kim1、杉岡 裕子4、竹内 希1、川野 由貴1、川勝 均1、Sang-Mook Lee3、Onboard scientists of 2018/2019 Oldest cruises (1.東京大学地震研究所 附属海半球観測研究センター、2.Chungnam National University、3.Seoul National University、4.神戸大学)
セッション情報
[E] ポスター発表
セッション記号 S (固体地球科学) » S-IT 地球内部科学・地球惑星テクトニクス
[S-IT27] Oceanic lithosphere and asthenosphere
コンビーナ:竹内 希(東京大学地震研究所)、Ban-Yuan Kuo(Institute of Earth Sciences, Academia Sinica)、Rob L Evans(Woods Hole Oceanographic Institution)、Younghee Kim(Seoul National University)
The oceanic lithosphere/asthenosphere system (LAS) is one of the most fundamental features of plate tectonics. In recent years, the elucidation of the oceanic lithosphere/asthenosphere system has become one of the hot topics in solid earth science. New data from the ocean floor are being extensively obtained under the Pacific Array initiative (http://eri-ndc.eri.u-tokyo.ac.jp/PacificArray/) and others, and a great variety of views are proposed and discussed. In this session, we will discuss on observation technologies, views of the oceanic lithosphere/asthenosphere system, the strategies for interpretation of the observations (including seismic and/or electrical conductivity anisotropy), constraints/ideas on the role and abundance of water/melt in the mantle (including the transition zone), and other related topics for elucidating this enigmatic system. We call for contributions from diverse fields, including but not limited to seismology, magnetotellurics, petrology/mineralogy, dynamical modelling, and mineral physics.
*Hogyum Kim1、Kiyoshi Baba2、Hisashi Utada2、Sang-Mook Lee1、Hitoshi Kawakatsu2、YoungHee Kim1 (1.School of Earth and Environmental Sciences, Seoul National University、2.Earthquake Research Institute, The University of Tokyo)
*Hyunsun Kang1、Younghee Kim1、Shu-Huei Hung2、Pei-Ying Patty Lin3、Takehi Isse4、Hajime Shiobara4、Hitoshi Kawakatsu4、Sang-Mook Lee1、Hisashi Utada4、Nozomu Takeuchi4 (1.Seoul National University、2.National Taiwan University、3.National Taiwan Normal University、4.Earthquake Research Institute, The University of Tokyo)