[EE] Evening Poster
S (Solid Earth Sciences) » S-SS Seismology
[S-SS04] Nankai Trough Seismogenic Zone Experiment toward the final challenge
Tue. May 22, 2018 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall7, Makuhari Messe)
The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) is a multidisciplinary investigation of fault mechanics and seismogenesis along the megathrust at the Nankai Trough subduction zone, and includes reflection and refraction seismic imaging, direct sampling by drilling, in situ measurements, and long-term monitoring in conjunction with laboratory and numerical modeling studies. During the past 11 IODP expeditions off Kii Peninsula since 2007, 15 sites have been drilled by D/V "Chikyu" down to depths from 100s of meters to more than 3000 meters below seafloor, where the inner and outer wedge of the Nankai margin has been sampled extensively, and two state-of-the-art real-time downhole observatories are now in operation. NanTroSEIZE is now at the final stage with only two more expeditions planned for another downhole observatory installation at the toe site in early 2018, and for resuming riser drilling toward the megathrust at ~5200 meters below seafloor starting from late 2018.
In this session jointly held with AOGS, we expect presentations on scientific outcomes from the NanTroSEIZE project and discussions toward the final challenge. We welcome presentations on, but are not limited to, seismic imaging, borehole logging and monitoring, chemical analyses of pore water and mud gas, lithology, structures, physical properties and laboratory experiments of cuttings and core samples, and theoretical and numerical modeling.
*Mikiya Yamashita1, Ayako Nananishi1, Gregory F. Moore2, Shuichi Kodaira1, Yasuyuki Nakamura1, Seiichi Miura1, Yoshiyuki Kaneda3 (1.R&D Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology, 2.School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, 3.Research Center for Regional Resilience, Kagawa University)
*Rina Fukuchi1, Kan-hsi Hsiung1, Drake Singleton2, Asuka Yamaguchi3, Qing Chang1, Jun-Ichi Kimura1, Yoshitaka Nagahashi4, Gaku Kimura5 (1.Japan Agency for Marine-Earth Science and Technology, 2.San Diego State University, 3.The University of Tokyo, 4.Fukushima University, 5.Tokyo University of Marine Science and Technology)
*Suguru Yabe1, Rina Fukuchi1, Baiyuan Gao2, Ginta Motohashi3, Mari Hamahashi4, Yoshitaka Hashimoto5, Gaku Kimura6 (1.Japan Agency for Marine-Earth Science and Technology, 2.The University of Texas at Austin, 3.Univ. of Tsukuba, 4.Earth Observatory of Singapore, 5.Kochi Univ., 6.Tokyo University of Marine Science and Technology)
*Hasegawa Ryota1, Asuka Yamaguchi1, Rina Fukuchi2, Yohei Hamada3, Yujin Kitamura4, Gaku Kimura5, Juichiro Ashi1, Tsuyoshi Ishikawa3 (1.Atmosphere and Ocean Research Institute, The University of Tokyo, 2.Research and Development (R&D) Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology, 3.Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology, 4.Graduate School of Science and Engineering KAGOSHIMA UNIVERSITY, 5.Tokyo University of Marine Science and Technology School of Marine Resources and Environment)
*Tsuyoshi Ishikawa1, Asuka Yamaguchi2 (1.Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology, 2.Atmosphere and Ocean Research Institute, The University of Tokyo)