2017年5月23日(火) 10:45 〜 12:15 A07 (東京ベイ幕張ホール)

コンビーナ:大内 智博(愛媛大学地球深部ダイナミクス研究センター)、北 佐枝子(広島大学大学院理学研究科地球惑星システム学専攻)、Brent G Delbridge(Berkeley Seismological Lab)、片山 郁夫(広島大学大学院理学研究科地球惑星システム学専攻)、座長:岡崎 啓史(海洋研究開発機構)、座長:片山 郁夫(広島大学大学院理学研究科地球惑星システム学専攻)、座長:大内 智博(愛媛大学地球深部ダイナミクス研究センター)

The rheological behavior of subducting slabs contributes to the generation and occurrence of intraslab earthquakes; however, we currently lack an understanding of the physical mechanisms linking these properties to the generation of intraslab earthquakes. The purpose of this session is to share constraints and advances in the understanding of the mechanisms that generate shallow and intermediate depth earthquakes, including both brittle and ductile flow rheologies. We seek to formulate future directions of the interdisciplinary study of the occurrence of intraslab earthquakes from the viewpoint of seismology, geodynamics and mineral physics. We welcome presentations from a wide variety of scientific disciplines, including observational and theoretical seismology, seismotectonics, geodynamics, mineral and rock physics, geology, and numerical modeling. Studies related to the thermal and tectonic structures of the subducting slab are also welcomed.