Japan Geoscience Union Meeting 2018

Presentation information

[JJ] Oral

S (Solid Earth Sciences) » S-SS Seismology

[S-SS15] Fault Rheology and Earthquake Physics

Mon. May 21, 2018 9:00 AM - 10:30 AM A07 (Tokyo Bay Makuhari Hall)

convener:Hideki Mukoyoshi(Department of Geoscience Interdisciplinary Graduate School of Science and Engineering, Shimane University), Wataru Tanikawa(Japan Agency for Marine-Earth Science and Technology, Kochi Instutute for Core Sample Research), Takanori Matsuzawa(国立研究開発法人 防災科学技術研究所, 共同), Keisuke Yoshida(Tohoku University), Chairperson:Yoshida Keisuke(東北大学大学院理学研究科 地球物理学専攻), Matsuzawa Takanori(National Research Institute for Earth Science and Disaster Resilience)

10:07 AM - 10:29 AM

[SSS15-11] Earthquake swarms and their relation to crustal fluid as revealed by dense seismic observation in Hakone volcano, central Japan

★Invited Papers

*Yohei Yukutake1 (1.Hot Springs Research Institute of Kanagawa Prefecture)

Keywords:earthquake swarm, crustal fluid

The occurrence of earthquake swarms has been related to crustal fluid migration (e.g., Parotidis et al., 2005) or an aseismic slip on fault planes (e.g., Lohman and McGuire, 2007). This study aims to investigate the contribution of crustal fluid to the occurrence of earthquake swarms, based on the highly resolved hypocenter distribution and seismic tomography results in Hakone volcano, central Japan, where shallow intense swarm activities and crustal deformation associated with inflation of the pressure source were often observed. The hypocenter distribution of earthquake swarms reveals thin vertical plane-like zones, each with a thickness of several tens of meters. Moreover, hypocenters of the earthquake swarms migrate following a diffusion equation that gives hydraulic diffusivity between 0.5 and 1.0 m2/s (Yukutake et al., 2015). Low stress drop and high b-values are estimated for the earthquake swarms during the initial stage of activity. These observations imply that the earthquake swarms were triggered by the diffusion of high-pressure crustal fluids within the fault damage zones. Tomographic inversion reveals a region of low P-wave velocity (Vp), low S-wave velocity (Vs), and high Vp/Vs ratios at depths of 10–20 km beneath the volcano, corresponding to the locations of the pressure sources (Yukutake et al., 2015). The high Vp/Vs ratios represent a deep magma chamber with a high content of fluid and melt, according to the theoretical modeling by Takei (2002). Above the high Vp/Vs zone, a region of low Vp, low Vs, and low Vp/Vs ratios exists at depths of 3–10 km, suggesting the presence of crack-filled water or CO2 supplied from the deep magma chamber. Most of the earthquake swarms occur in this low Vp/Vs zone. These results indicate that the crustal fluids from the magma source substantially contribute to the generation of the earthquake swarms, as well as the geothermal activity in Hakone volcano.

I used waveform data from the seismic stations of the National Research Institute for Earth Science and Disaster Resilience, the Japan Meteorological Agency, and the University of Tokyo.

Lohman RB, McGuire JJ (2007) Journal of Geophysical Research 112 doi:10.1029/2006jb004596
Parotidis M, Shapiro SA, Rothert E (2005) Journal of Geophysical Research 110:B05S10 doi:10.1029/2004JB003267
Takei Y (2002) Journal of Geophysical Research 107 doi:10.1029/2001jb000522
Yukutake Y, Honda R, Harada M, Arai R, Matsubara M (2015) Journal of Geophysical Research 120:3293-3308 doi:10.1002/2014jb011856
Yukutake Y, Ito H, Honda R, Harada M, Tanada T, Yoshida A (2011) Journal of Geophysical Research 116 doi:10.1029/2010jb008036