Results 11 to 20 of about 608 (138)

IODP Expedition 333: Return to Nankai Trough Subduction Inputs Sites and Coring of Mass Transport Deposits [PDF]

Scientific Drilling, 2012
Integrated Ocean Drilling Program (IODP) Expedition 333 returned to two sites drilled during IODP Expedition 322 on the ocean side of the Nankai Trough to pursue the characterization of the inputs to the Nankai subduction and seismogenic zone, as part of
Michael Strasser, Kyaw Thu Moe, Toshiya Kanamatsu, Pierre Henry, the IODP Expedition 333 Scientific Party   +4 more
doaj   +5 more sources

Effective Porosity Profile at IODP Site C0002 in the Heart of the Nankai Accretionary Prism, and Its Use for Predicting In Situ Seismic Velocities

Geophysical Research Letters, 2023
Using logging data and samples collected by the four expeditions of the International Ocean Discovery Program NanTroSEIZE drilling campaign that occupied Site C0002 in the Nankai margin located southwest of Japan, we determined effective porosity and ...
Mai‐Linh Doan, Jade Dutilleul, Pierre Henry   +2 more
doaj   +2 more sources

Operational Review of the First Wireline In Situ Stress Test in Scientific Ocean Drilling [PDF]

Scientific Drilling, 2012
Scientific ocean drilling’s first in situ stress measurement was made at Site C0009A during Integrated Ocean Drilling Program (IODP) Expedition 319 as part of Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) Stage 2. The Modular Formation Dynamics
Casey Moore, Masataka Kinoshita, Yasuyuki Kano, Peter Flemings, Timothy Byrne, Eiichiro Araki, Demian Saffer, Lisa McNeill, David Boutt, Mai-Linh Doan, Weiren Lin, Chee Kin Khong, Takatoshi Ito, Yoshihisa Kawamura, Moe Kyaw Thu, Nobu Eguchi, and Ikuo Sawada, Harold Tobin   +15 more
doaj   +3 more sources

NanTroSEIZE Stage 1 expeditions: introduction and synthesis of key results [PDF]

, 2009
Integrated Ocean Drilling Program Expeditions 314, 315, and 316 were carried out as a unified program of drilling collectively known as Stage 1 of the Nankai Trough Seismogenic Zone Experiment, a multistage complex drilling project. A transect of eight sites was selected for riserless drilling to target the frontal thrust region, midslope megasplay ...
Tobin, Harold, Kinoshita, Masataka, Ashi, Juichiro, Lallement, Siegfried, Kimura, Gaku, Screaton, Elizabeth, Moe, Kyaw Thu, Masago, Hideki, Curewitz, Daniel, Kitamura, Yujin, Behrmann, Jan Hinrich   +10 more
openaire   +5 more sources

Recent Advances in the Use of Drill Cuttings for Determining Subduction Zone Structure, Stratigraphy, and Stress State

Geochemistry, Geophysics, Geosystems
Obtaining in situ samples from active subduction systems is critical for assessing the material properties and geological evolution of rocks and sediments that host plate boundary deformation, and advancing our understanding of the processes that lead to
P. H. Cornard, A. M. Schleicher, C. Regalla, M. Hamahashi, M. Kitamura, R. Fukuchi, K. T. Pickering, H. Kitajima, T. Wiersberg   +8 more
doaj   +2 more sources

The IODP Nankai Trough Seismogenic Zone Experiment [PDF]

Scientific Drilling, 2007
No abstract available.
Masataka Kinoshita, Harold Tobin
doaj   +6 more sources

Steady‐State Effective Normal Stress in Subduction Zones Based on Hydraulic Models and Implications for Shallow Slow Earthquakes

Journal of Geophysical Research: Solid Earth, Volume 128, Issue 2, February 2023., 2023
Abstract The spatial distribution of effective normal stress, , is essential for understanding the fault motion. Although Rice (1992, https://doi.org/10.1016/s0074-6142(08)62835-1) proposed a steady‐state solution for a vertical strike‐slip fault zone with constant fluid properties, models that are based on the concept by Rice (1992, https://doi.org/10.
Shunya Kaneki, Hiroyuki Noda
wiley   +1 more source

Nankai Forearc Structural and Seismogenic Segmentation Caused by a Magmatic Intrusion off the Kii Peninsula

Geochemistry, Geophysics, Geosystems, Volume 23, Issue 8, August 2022., 2022
Abstract The causes for forearc basin and megathrust rupture zone segmentation are controversial. The Nankai forearc, Japan, is separated into five domains based on topography: Enshu, Kumano, Muroto, Tosa, and Hyuga. The boundaries of these domains correspond to the rupture limits of large earthquakes. We examined the geologic structure of the boundary
G. Kimura, Y. Nakamura, K. Shiraishi, G. Fujie, S. Kodaira, T. Tsuji, R. Fukuchi, A. Yamaguchi   +7 more
wiley   +1 more source

Bathymetric Signatures of Submarine Forearc Deformation: A Case Study in the Nankai Accretionary Prism

Geochemistry, Geophysics, Geosystems, Volume 22, Issue 11, November 2021., 2021
Abstract Large earthquakes and tsunamis in subduction zone forearcs occur via slip on the shallow plate boundary and upper plate faults, but the locations, geometries, and slip histories of these faults can be difficult to constrain in regions with minimal subsurface geophysical and stratigraphic data.
Emily R. Schottenfels, Christine A. Regalla   +1 more
wiley   +1 more source

Spatial Patterns in Frictional Behavior of Sediments Along the Kumano Transect in the Nankai Trough

Journal of Geophysical Research: Solid Earth, Volume 126, Issue 11, November 2021., 2021
Abstract Fault slip activity at subduction zones is governed by sediment frictional properties, which in turn are affected by diagenetic processes. To study the spatial patterns in frictional properties across the Nankai Trough, SW Japan, and their relations to fault slip activity, we used sediment samples (10%–59% clay mineral content) along the ...
Hanaya Okuda, Matt J. Ikari, Alexander Roesner, Katja Stanislowski, Andre Hüpers, Asuka Yamaguchi, Achim J. Kopf   +6 more
wiley   +1 more source