Japan Geoscience Union Meeting 2014

Presentation information

Oral

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

[S-CG67_2AM1] Ocean Floor Geoscience

Fri. May 2, 2014 9:00 AM - 10:45 AM 418 (4F)

Convener:*Kyoko Okino(Ocean Research Institute, University of Tokyo), Keiichi Tadokoro(Research Center for Seismology, Volcanology and Earthquake and Volcano Research Center, Nagoya University), Osamu Ishizuka(Institute of Geoscience, Geological Survey of Japan/AIST), Tomohiro Toki(Faculty of Science, University of the Ryukyus), Narumi Takahashi(Earthquake and Tsunami Research Project for Disaster Prevention, Japan Agency for Marine-Earth Science and Technology), Chair:Yukihito Osada(Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science, Tohoku University), Yusuke Yokota(Japan Coast Guard, Hydrographic and oceanographic department)

9:15 AM - 9:30 AM

[SCG67-12] Postseismic seafloor movements following the 2011 Tohoku-oki earthquake detected by GPS/acoustic positioning

*Shun-ichi WATANABE1, Mariko SATO1, Yusuke YOKOTA1, Naoto UJIHARA1, Tadashi ISHIKAWA2, Masashi MOCHIZUKI3, Akira ASADA3 (1.Hydrographic and Oceanographic Department, Japan Coast Guard, 2.Japan Coast Guard Academy, 3.Institute of Industrial Science, University of Tokyo)

Keywords:seafloor geodetic observation, the 2011 Tohoku Earthquake

The Hydrographic and Oceanographic Department, Japan Coast Guard, have been developing precise seafloor positioning systems using the GPS/acoustic combination technique and carrying out campaign observations along the major trenches in the Pacific Ocean, such as the Japan Trench and the Nankai Trough. For example, after the 2011 Tohoku-oki earthquake (Mw = 9.0), we detected a huge coseismic displacement of 24 m toward ESE at MYGI which is located above the epicenter. We have been continued the geodetic observations along the Japan Trench in order to detect postseismic deformation. The results of the observations show that the displacements vary with the sites even in the directions. MYGI and KAMS had moved toward west-northwest at constant rate. MYGW had moved toward south-southeast. KAMN had moved toward northwest. FUKU and CHOS had moved toward east-southeast. In addition, the displacements at FUKU and CHOS decay with time. For vertical component, significant subsidence was detected at all sites except CHOS where no vertical displacement was detected within the accuracy range.In this presentation, we will report and discuss the latest results of the seafloor geodetic observation along the Japan Trench.