セッション概要

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ID S-IT06 タイトル 和文 Geofluids and their roles in dynamics of the Earth's interior 英文 Geofluids and their roles in dynamics of the Earth's interior タイトル短縮名 和文 Geofluids 英文 Geofluids 代表コンビーナ 氏名 和文 岩森 光 英文 Hikaru Iwamori 所属 和文 東京工業大学大学院理工学研究科地球惑星科学専攻 英文 Department of Earth and Planetary Sciences, Tokyo Institute of Technology 共同コンビーナ 1 氏名 和文 ブルノ　レイナード 英文 Bruno Reynard 所属 和文 リヨン高等師範学校 英文 Ecole Normale Superieure de Lyon 共同コンビーナ 2 氏名 和文 スティーブ　カービー 英文 Stephen Kirby 所属 和文 米国地質調査所 英文 USGS 共同コンビーナ 3 氏名 和文 高橋　栄一 英文 Eiichi Takahashi 所属 和文 東京工業大学 英文 Tokyo Institute of Technology 国際セッション開催希望 国際セッションとしての開催を希望する 発表主要言語 英語 スコープ 和文 Fluids on the surface and in the interior of the Earth may play crucial roles in terrestrial dynamics and evolution of a wide spectrum of phenomena in time and space, e.g., active tectonics such as earthquakes, slow fault slip, magmatism, hydrothermal activity to long-term orogeny with metamorphic complex and continental evolution. How much and where do fluids actually exist, and which evidence is sensitive? What are the fluid pathways and how fast do fluids migrate? How much do they reduce mechanical strength, induce rock failure, or enhance melting? Geofluids must carry various (but specific) chemical components. How much do they migrate and thereby contribute to formation of ore and continental crust? Geological, geophysical and geochemical methods are all necessary to address these questions, and we highly welcome various contributions from observational, experimental and theoretical approaches. 英文 Fluids on the surface and in the interior of the Earth may play crucial roles in terrestrial dynamics and evolution of a wide spectrum of phenomena in time and space, e.g., active tectonics such as earthquakes, slow fault slip, magmatism, hydrothermal activity to long-term orogeny with metamorphic complex and continental evolution. How much and where do fluids actually exist, and which evidence is sensitive? What are the fluid pathways and how fast do fluids migrate? How much do they reduce mechanical strength, induce rock failure, or enhance melting? Geofluids must carry various (but specific) chemical components. How much do they migrate and thereby contribute to formation of ore and continental crust? Geological, geophysical and geochemical methods are all necessary to address these questions, and we highly welcome various contributions from observational, experimental and theoretical approaches. 発表方法希望 口頭および（または）ポスターセッション 招待講演 Bruno Reynard (Ecole Normale Superieure de Lyon), Stephen Kirby (USGS)