Results 31 to 40 of about 608 (138)
Combined knowledge on the magnitude as well as the orientation of paleo-stress is usually not given. Based on drilling investigations and laboratory experiments, we are able to provide both, constraints on paleo-stress magnitude as well as orientation in
Yoshitaka Hashimoto +3 more
doaj +1 more source
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
IODP-ICDP Workshop examines challenges of fault zone drilling [PDF]
No abstract available.
Behrmann, Jan Hinrich +4 more
core +3 more sources
Rheology and Biostratigraphy of the Mariana Serpentine Muds Unravel Mud Volcano Evolution
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
NanTroSEIZE Stage 3: NanTroSEIZE Plate Boundary Deep Riser 3 Expedition 348
The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) is a multidisciplinary investigation of fault mechanics and seismogenesis along subduction megathrusts 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 ...
Tobin, H. +30 more
openaire +2 more sources
High-velocity frictional properties of clay-rich fault gouge in a megasplay fault zone, Nankai subduction zone [PDF]
We conducted high-velocity friction experiments on clay-rich fault gouge taken from the megasplay fault zone in the Nankai subduction zone under dry and wet conditions.
Tsutsumi Akito +2 more
core +1 more source
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
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
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
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

