Results 21 to 30 of about 123 (98)

Linking Faults, Fractures, and Clay Mineral Occurrence With Fluid Transport in the Accretionary Prism of the Nankai Trough, Japan

open access: yesGeochemistry, Geophysics, Geosystems, Volume 20, Issue 11, Page 4599-4612, November 2019., 2019
Abstract The interpretation of logging while drilling resistivity oriented images and geophysical logs from Hole C0002 drilled during the International Ocean Discovery Program (IODP) Expeditions 338 and 348 of the Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) project revealed a complex structure of the accretionary prism characterized by ...
Anja M. Schleicher, Maria‐Jose Jurado
wiley   +1 more source

Proceedings of the Integrated Ocean Drilling Program 319: NanTroSEIZE Stage 2: NanTroSEIZE Riser/Riserless Observatory

open access: yes, 2010
As part of the NanTroSEIZE program, operations during Integrated Ocean Drilling Program (IODP) Expedition 319 included riser drilling, analyses of cuttings and core samples, downhole measurements and logging, and casing at Site C0009 in the Kumano forearc basin as well as riserless drilling, logging while drilling (LWD), casing, and observatory ...
Saffer, Demian M.   +43 more
openaire   +1 more source

Geochemical constraints on the temperature and timing of carbonate formation and lithification in the Nankai Trough, NanTroSEIZE transect [PDF]

open access: yesGeochimica et Cosmochimica Acta, 2017
Information about diagenetic processes and temperatures during burial of sediments entering the subduction zone is important for understanding changes in physical properties and seismic behavior during deformation. The geochemistry of authigenic carbonates from accretionary prisms can serve as proxies for conditions during carbonate cementation and ...
Sample, James C.   +6 more
openaire   +7 more sources

Deformation Structures From Splay and Décollement Faults in the Nankai Accretionary Prism, SW Japan(IODP NanTroSEIZE Expedition 316): Evidence for Slow and Rapid Slip in Fault Rocks

open access: yesGeochemistry, Geophysics, Geosystems, 2020
Drilling during IODP NanTroSEIZE Expedition 316 led to the recovery of cores from the basal décollement in the frontal part of the Nankai accretionary prism and from a splay fault branching from the décollement at 25‐km landward of the prism toe.
O. Fabbri   +12 more
doaj   +1 more source

Rheology and Biostratigraphy of the Mariana Serpentine Muds Unravel Mud Volcano Evolution

open access: yesJournal of Geophysical Research: Solid Earth, Volume 124, Issue 11, Page 10752-10776, November 2019., 2019
Abstract In late 2016, the IODP Expedition 366 drilled 21 holes on summits and flanks of three serpentinite mud volcanoes (SMVs) of the Mariana Forearc: Yinazao (Blue Moon), Fantangisña (Celestial), and Asùt Tesoru (Big Blue). The drilling reached the forearc sediments underneath the SMVs only at Site U1498 where, according to data from this study, the
Walter Menapace   +4 more
wiley   +1 more source

Heat flow estimated from BSR and IODP borehole data: Implication of recent uplift and erosion of the imbricate thrust zone in the Nankai Trough off Kumano

open access: yesGeochemistry, Geophysics, Geosystems, 2011
Heat flow values were estimated in the Nankai Trough fore‐arc slope region off Kii Peninsula from the Bottom‐Simulating Reflector (BSR) and other data obtained during IODP Expeditions 315 and 316.
Masataka Kinoshita   +2 more
doaj   +1 more source

Synthesis of the Laboratory Frictional Properties of a Major Shallow Subduction Zone: The Nankai Trough, Offshore SW Japan

open access: yesJournal of Geophysical Research: Solid Earth, Volume 130, Issue 12, December 2025.
Abstract The Nankai Trough has a long history of ≥Mw 8 earthquakes and associated tsunamis. It has been the focus of decades of research, including drilling, providing the opportunity to measure the laboratory frictional properties of shallow accretionary prism samples. We collate all available friction data from the Nankai Trough and correlate it with
D. R. Faulkner   +6 more
wiley   +1 more source

Chemical and Noble Gas Isotope Compositions of Formation Gases from a 3 km Deep Scientific Borehole in the Koyna Seismogenic Zone, Western India

open access: yesGeofluids, Volume 2019, Issue 1, 2019., 2019
A 3 km deep research borehole KFD1 was drilled in the Koyna reservoir‐triggered seismicity region, Western India, between December 2016 and May 2017. The 1967 M 6.3 Koyna earthquake had generated a NNE‐SSW trending surface fissure zone in the Nanel‐Donichawadi‐Kadoli sector. KFD1 is located ~5 km south of Kadoli along the trend of the Donichawadi fault
Nagaraju Podugu   +4 more
wiley   +1 more source

State of Stress Across Major Faults in the Nankai Subduction Zone Estimated From Wellbore Breakouts

open access: yesJournal of Geophysical Research: Solid Earth, Volume 130, Issue 7, July 2025.
Abstract Quantifying the orientation and magnitude of stress at tectonically active margins and along major fault systems is integral to understanding the mechanics of faulting and earthquakes. Here we use data collected as part of the IODP (Integrated Ocean Drilling Program) Nankai Trough Seismogenic Zone Experiment to constrain in situ stress ...
Kaitlin E. Schaible, Demian M. Saffer
wiley   +1 more source

High fluid pressures and high fluid flow rates in the Megasplay Fault Zone, NanTroSEIZE Kumano Transect, SW Japan

open access: yesGeochemistry, Geophysics, Geosystems, 2012
Annular pressure while drilling data shows high fluid overpressures at Site C0001 in part of the megasplay fault zone of the NanTroSEIZE transect across the subduction zone of SW Japan.
J. Casey Moore   +2 more
doaj   +1 more source

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