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 Nakanishi2, Koichiro Obana2, Mikiya Yamashita2, Takashi Tonegawa3, Kentaro Imai4, Takeshi Iinuma5, Eiichiro Araki6, Takane Hori7 and Shuichi Kodaira7, (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, Yokosuka, Japan, (4)JAMSTEC Japan Agency for Marine-Earth Science and Technology, Research Institute for Marine Geodynamics, Kanagawa, Japan, (5)Japan Agency for Marine-Earth Science and Technology, Research and Development Center for Earthquake and Tsunami, Yokohama, Japan, (6)Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Research Institute for Marine Geodynamics, Yokosuka, Japan, (7)Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama, Japan
