Conductivity structure in and around the Deep Low-Frequency Tremors generation region beneath the western part of the Kii Peninsula in Southwest Japan.
Satoshi Katakami1, Satoru Yamaguchi2, Makoto Uyeshima3, Hideki Murakami4, Tsutomu Ogawa5, Naoto Oshiman6, Ryokei Yoshimura7, Koki Aizawa8, Ichiro Shiozaki9, Takahumi Kasaya10 and Yoshihiro Ito7, (1)Graduate School of Science, Kyoto University, Kyoto, Japan, (2)Osaka City University, Osaka, Japan, (3)Earthquake Research Institute (ERI), University of Tokyo, Tokyo, Japan, (4)University of Kochi, Kochi, Japan, (5)Earthquake Research Institute, Tokyo, Japan, (6)Kyoto University, Kyoto, Japan, (7)Disaster Prevention Research Institute, Kyoto University, Kyoto, Japan, (8)Kyushu University, Fukuoka, Japan, (9)Tottori University, Tottori, Japan, (10)Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan
