固体地球科学(S)
セッション小記号地球内部科学・地球惑星テクトニクス(IT)
セッションIDS-IT29
タイトル和文東アジアにおけるジオダイナミクスの新展開
英文New perspectives on East Asia geodynamics
タイトル短縮名和文ジオダイナミクス東アジア
英文East Asia geodynamics
代表コンビーナ氏名和文Jonny Wu
英文Jonny Wu
所属和文University of Houston
英文University of Houston
共同コンビーナ 1氏名和文山口 飛鳥
英文Asuka Yamaguchi
所属和文東京大学大気海洋研究所
英文Atomosphere and Ocean Research Institute, The University of Tokyo
共同コンビーナ 2氏名和文沖野 郷子
英文Kyoko Okino
所属和文東京大学大気海洋研究所
英文Atmosphere and Ocean Research Institute, The University of Tokyo
共同コンビーナ 3氏名和文Timothy B Byrne
英文Timothy B Byrne
所属和文University of Connecticut
英文University of Connecticut
発表言語E
スコープ和文East Asia is one of the most tectonically active regions on Earth and includes the Eurasian continental margin, the western Pacific subduction zones and many of Earth's marginal seas. The region has a long history of subduction, collision, backarc basin opening and closing, and other plate boundary interactions. In recent years, a wide range of new observations have been collected from the land, oceans and Earth interior, including detailed geologic data, zircon age spectra, earthquakes, high resolution crustal to mantle imaging, and Big Data. These new data show the detailed space-time evolution of subduction zones, mountain building, slab stagnation, crustal deformation, continental dynamics, backarc spreading, and other East Asian geodynamics cannot be fully explained by classic theories; new perspectives are needed. Here we seek to share new insights on the geologic history, paleomagnetism, and geophysical character of East Asia since the Paleozoic. We also invite geodynamic models that integrate diverse datasets into a more holistic view of this dynamic environment.
英文East Asia is one of the most tectonically active regions on Earth and includes the Eurasian continental margin, the western Pacific subduction zones and many of Earth's marginal seas. The region has a long history of subduction, collision, backarc basin opening and closing, and other plate boundary interactions. In recent years, a wide range of new observations have been collected from the land, oceans and Earth interior, including detailed geologic data, zircon age spectra, earthquakes, high resolution crustal to mantle imaging, and Big Data. These new data show the detailed space-time evolution of subduction zones, mountain building, slab stagnation, crustal deformation, continental dynamics, backarc spreading, and other East Asian geodynamics cannot be fully explained by classic theories; new perspectives are needed. Here we seek to share new insights on the geologic history, paleomagnetism, and geophysical character of East Asia since the Paleozoic. We also invite geodynamic models that integrate diverse datasets into a more holistic view of this dynamic environment.
発表方法口頭および（または）ポスターセッション