Results 11 to 20 of about 416 (127)
NanTroSEIZE Stage 3: NanTroSEIZE Plate Boundary Deep Riser 2 [PDF]
, 2014 The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) is a multidisciplinary scientific project designed to investigate fault mechanics and seismogenesis along subduction megathrusts through reflection and refraction seismic imaging, direct ...
M. Strasser +5 more
core +5 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 +15 more
doaj +3 more sources
Thermal Conductivity Profile in the Nankai Accretionary Prism at IODP NanTroSEIZE Site C0002: Estimations From High‐Pressure Experiments Using Input Site Sediments [PDF]
Geochemistry, Geophysics, Geosystems, 2020 Depth profiles of sediment thermal conductivity are required for understanding the thermal structure in active seismogenic zones. During the Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE), a scientific drilling project of the International Ocean
Weiren Lin +5 more
doaj +2 more sources
Coring Technology to be applied in IODP NanTroSEIZE [PDF]
OCEANS 2008 - MTS/IEEE Kobe Techno-Ocean, 2008 JAMSTEC/CDEX has started the first drilling operation of CHIKYU for the Nankai Trough Seizmogenic Zone Experiment (NanTroSEIZE) at offshore Kumanonada conducted by the Integrated Ocean Drilling Program (IODP) in September 2007. The majority of coring objectives principally involve that of "continuous" wireline coring operations.
Kazuyasu Wada
openaire +2 more sources
Geochemistry, Geophysics, GeosystemsObtaining 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 +8 more
doaj +2 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.
H. Tobin +8 more
core +6 more sources
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
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 +7 more
wiley +1 more source
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 +1 more
wiley +1 more source