Japan Geoscience Union Meeting 2023

Presentation information

[J] Online Poster

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

[S-CG56] Dynamics in mobile belts

Thu. May 25, 2023 3:30 PM - 5:00 PM Online Poster Zoom Room (6) (Online Poster)

convener:Yukitoshi Fukahata(Disaster Prevention Research Institute, Kyoto University), Hikaru Iwamori(Earthquake Research Institute, The University of Tokyo), Kiyokazu Oohashi(Graduate School of Sciences and Technology for Innovation, Yamaguchi University)

On-site poster schedule(2023/5/26 17:15-18:45)

3:30 PM - 5:00 PM

[SCG56-P08] Three-dimensional resistivity structure around Earthquake Swarm Region in the Northeastern Noto Peninsula

*Ryokei Yoshimura1, Yoshihiro Hiramatsu2, Tada-nori Goto3, Takafumi Kasaya4, Rintaro Miyamachi1, Nakagawa Jun1, Nagi Yamashita3, Rei Amano3, Masato Fukata2, Amane Sugii2, Taisei Inui1, Ken'ichi Yamazaki1, Shintaro Komatsu1, Takuya Iwahori1, Masahiro Yoshikawa1, Ayako Namigishi1, Nagaoka Airi1, Yasuto Tatsuyama1, Akihiro Sawada2, Ce Zhang2, Mitsuteru Fukuoka2, Yuya Jinde2, Yuki Oshima3, Momoka Kanazawa3 (1.Disaster Prevention Research Institute, Kyoto University, 2.Kanazawa University, 3.University of Hyogo, 4.Japan Agency for Marine-Earth Science and Technology)

Keywords:Noto, seismic swarm, resistivity structure

Earthquake swarm activity and localized non-steady crustal deformation have continued near Suzu city, Ishikawa Prefecture, since the end of 2020. This activity began around June 2018, with a M5.1 (maximum seismic intensity of 5-lower) earthquake on September 16, 2021, and a M5.4 (maximum seismic intensity of 6-lower) earthquake on June 19, 2022, and has shown no sign of abating.
We are conducting a subsurface resistivity structure survey to elucidate the structural location of this swarm activity and to determine whether there are structural differences from the area where the 2007 Noto Hanto earthquake occurred. The resistivity structure inferred from the onshore broadband electromagnetic field data reveals the existence of a continuous low resistivity zone from the southern cluster, where a series of seismic activity started, to the northern cluster, which is currently the most active, strongly suggesting fluid involvement in this activity.
In this presentation, we will report the results of the reanalysis with the addition of data from supplemental observations conducted at sea and land for the purpose of improving the resolution of the subsurface structure (three observations on the ocean bottom: from September to October 2022 and 23 observations on the land: from November 2022 to February 2023).