Japan Geoscience Union Meeting 2024

Presentation information

[J] Oral

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

[S-CG46] New Insights of Fluid-Rock Interactions: From Surface to Deep Subduction Zone

Wed. May 29, 2024 9:00 AM - 10:30 AM 301B (International Conference Hall, Makuhari Messe)

convener:Atsushi Okamoto(Graduate School of Environmental Studies), Jun Muto(Department of Earth Sciences, Tohoku University), Ikuo Katayama(Department of Earth and Planetary Systems Science, Hiroshima University), Junichi Nakajima(Department of Earth and Planetary Sciences, Tokyo Institute of Technology), Chairperson:Ikuo Katayama(Department of Earth and Planetary Systems Science, Hiroshima University), Junichi Nakajima(Department of Earth and Planetary Sciences, Tokyo Institute of Technology)

9:00 AM - 9:15 AM

[SCG46-10] Recent crustal earthquakes in Japan related to fluid movement

★Invited Papers

*Keisuke Yoshida1 (1.Tohoku University)

Keywords:crustal fluid, seismicity, fault strength, crustal stress

It has long been pointed out that the fluid movement within the crust may influence the occurrence of earthquakes. In fact, there are abundant known examples of earthquakes occurring when fluids are injected into the subsurface. The primary mechanism thought to be responsible for this was the reduction in frictional strength when a fluid, such as water, intrudes into the fault, but more recently, attention has focused on the effects of fluid-induced aseismic slip.
Recent studies have shown that there are many instances in which crustal fluid movement appears to have contributed to earthquake occurrences in Japan. In this talk, I will introduce several recent examples of such earthquake sequences. Examples include the earthquake swarms in NE Japan triggered by the Tohoku earthquake, the 2017 M5.3 Kagoshima Bay earthquake, the 2019 M6.7 Yamagata-Oki earthquake, and the 2020-2023 Noto Peninsula earthquake swarm and related recent earthquakes.