Direct observation of a plate boundary earthquake by a seafloor network in the Nankai Trough seismogenic zone (DONET): an example of the M=6.5 earthquake on 1st April, 2016
Narumi Takahashi1, Shin'ichiro Kamiya2, Masaru Nakano2, Kensuke Suzuki2, Ayako Nakanishi3, Koichiro Obana2, Mikiya Yamashita2, Takashi Tonegawa4, Kentaro Imai5, Takeshi Iinuma6, Eiichiro Araki7, Takane Hori8 and Shuichi Kodaira8, (1)National Research Institute for Earth Science and Disaster Prevention, Tsukuba, Japan, (2)JAMSTEC Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan, (3)JAMSTEC Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan, (4)JAMSTEC, Yokosuka, Japan, (5)JAMSTEC Japan Agency for Marine-Earth Science and Technology, Research Institute for Marine Geodynamics, Kanagawa, Japan, (6)Japan Agency for Marine-Earth Science and Technology, Research and Development Center for Earthquake and Tsunami, Yokohama, Japan, (7)Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Research Institute for Marine Geodynamics, Yokosuka, Japan, (8)Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama, Japan
