IODP Expedition 338: NanTroSEIZE stage 3: NanTroSEIZE plate boundary deep riser 2

G. F. Moore, K. Kanagawa, M. Strasser, B. Dugan, L. Maeda, S. Toczko, Lionel Esteban, Olivier Fabbri, Jacob Geersen, Sebastian Hammerschmidt, Hiroki Hayashi, Katrien Heirman, Andre Huepers, Maria José Jurado Rodriguez, Koji Kameo, Toshi Kanamatsu, Yukari Kido, Hiroko Kitajima, Harue Masuda, Kitty MillikenRavi Mishra, Kyaw Thu Moe, Isao Motoyama, Katelyn Olcott, Kiyokazu Oohashi, Kevin T. Pickering, Sebastian Ramirez, Harunur Rashid, Yoshinori Sanada, Derek Sawyer, Anja Schleicher, Yehua Shan, Robert Skarbek, Insun Song, Toru Takeshita, Tomohiro Toki, Joanne Tudge, Susanna Webb, Dean Wilson, Hung Yu Wu, Asuka Yamaguchi

Research output: Contribution to journalArticlepeer-review

30 Citations (Scopus)


The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) is designed to investigate fault mechanics and seismogenesis along a subduction megathrust, with objectives that include characterizing fault slip, strain accumulation, fault and wall rock composition, fault architecture, and state variables throughout an active plate boundary system. Integrated Ocean Drilling Program (IODP) Expedition 338 was planned to extend and case riser Hole C0002F from 856 to 3600 meters below the seafloor (m b.s.f.). Riser operations extended the hole to 2005.5mb.s.f., collecting logging-while-drilling (LWD) and measurement-while-drilling, mud gas, and cuttings data. Results reveal two lithologic units within the inner wedge of the accretionary prism that are separated by a prominent fault zone at ̃ 1640mb.s.f. Due to damage to the riser during unfavorable winds and strong currents, riser operations were suspended, and Hole C0002F left for re-entry during future riser drilling operations. Contingency riserless operations included coring at the forearc basin site (C0002) and at two slope basin sites (C0021 and C0022), and LWD at one input site (C0012) and at three slope basin sites (C0018, C0021 and C0022). Cores and logs from these sites comprehensively characterize the alteration stage of the oceanic basement input to the subduction zone, the early stage of Kumano Basin evolution, gas hydrates in the forearc basin, and recent activity of the shallow megasplay fault zone system and associated submarine landslides.

Original languageEnglish
Pages (from-to)1-12
Number of pages12
JournalScientific Drilling
Issue number17
Publication statusPublished - 2014 Jan 1

All Science Journal Classification (ASJC) codes

  • Energy Engineering and Power Technology
  • Mechanical Engineering


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