Three-dimensional resistivity structure of the epicenter area of the 1997 Kagoshima earthquake doublet, Japan

松永 佳大*; 相澤 広記*; 浅森 浩一; 小川 大輝*; 宇津木 充*; 吉村 令慧*; 山崎 健一*; 内田 和也*; 山口 雅弘*; 井上 智裕*; 奥田 祐大*; 米盛 航平*; 重松 弘道*; 砂川 尋海*

Matsunaga, Keita*; Aizawa, Koki*; Asamori, Koichi; Ogawa, Hiroki*; Utsugi, Mitsuru*; Yoshimura, Ryokei*; Yamazaki, Kenichi*; Uchida, Kazunari*; Yamaguchi, Masahiro*; Inoue, Tomohiro*; Okuda, Yuta*; Yonemori, Kohei*; Shigematsu, Hiromichi*; Sunagawa, Hiromi*

We utilized broadband magneto-telluric (MT) data to analyze the 3-D resistivity structure around the epicenters of the 1997 Kagoshima earthquake doublet, Japan. We reanalyzed previous MT data and further obtained additional MT data. Our findings reveal low-resistivity zones near the eastern and western edges of the aftershock region at depths of 5-10 km. The hypocenters of the M6 earthquakes are located near the edge of the low-resistivity zones. A distinct high-resistivity zone is sandwiched between two low-resistivity zones at depths of 0-3 km, corresponding to the distribution of a granodiorite body. The slip distribution of the March M6 earthquake is located beneath this shallow granodiorite body and is sandwiched by the low-resistivity zones.