Long-term Monitoring in Deep Boreholes in the Nankai Subduction Zone [PDF]
No abstract available.
Hisao Ito
doaj +6 more sources
Weakening behavior of the shallow megasplay fault in the Nankai subduction zone
The Nankai Trough megasplay fault hosts diverse modes of fault slip, ranging from slow slip events to megathrust earthquakes, and is responsible for related phenomena such as tsunamis and submarine landslides.
Alexander Roesner +3 more
doaj +2 more sources
Deformation Process and Mechanism of the Frontal Megathrust at the Nankai Subduction Zone
The frontal megathrust of the Nankai Trough subduction zone is recognized as a seismogenic fault based on a record of frictional heating, but the underlying micromechanical processes that act on the fault surface are poorly known. Here we present a layer
Gaku Kimura +12 more
doaj +2 more sources
Ambient seafloor noise excited by earthquakes in the Nankai subduction zone. [PDF]
AbstractExcitations of seismic background noises are mostly related to fluid disturbances in the atmosphere, ocean and the solid Earth. Earthquakes have not been considered as a stationary excitation source because they occur intermittently. Here we report that acoustic-coupled Rayleigh waves (at 0.7–2.0 Hz) travelling in the ocean and marine sediments,
Tonegawa T +5 more
europepmc +4 more sources
Temperature limits to deep subseafloor life in the Nankai Trough subduction zone [PDF]
Deep, hot, and more alive than we thought Marine sediments represent a massive microbial ecosystem, but we still do not fully understand what factors shape and limit life underneath the seafloor. Analyzing samples from a subduction zone off the coast of Japan, Heuer et al.
Verena B. Heuer +42 more
openaire +7 more sources
An inhomogeneous across-slab conduit controlled by intraslab stress heterogeneity in the Nankai subduction zone. [PDF]
AbstractNonvolcanic, deep low-frequency tremors and slow-slip events occur simultaneously in the transition zone from locked to continuously creeping fault in the down-dip portion of the Nankai Trough subduction zone, southwestern Japan. The occurrence of these slow earthquakes is discontinuous along the trench and attributed to the effect of high pore
Otsubo M +3 more
europepmc +4 more sources
Fluid migration before and during slow earthquakes in the shallow Nankai subduction zone [PDF]
Fluid migration in subduction zones is a key controlling factor of slow and megathrust earthquakes at plate boundaries. During the migration, seismic velocity and heterogeneous structures in its pathways may be temporarily varied, preferably triggering slow earthquakes.
Takashi Tonegawa +3 more
openaire +2 more sources
Distribution of dehalogenation activity in subseafloor sediments of the Nankai Trough subduction zone [PDF]
Halogenated organic matter buried in marine subsurface sediment may serve as a source of electron acceptors for anaerobic respiration of subseafloor microbes. Detection of a diverse array of reductive dehalogenase-homologous ( rdhA ) genes suggests that subseafloor organohalide-respiring ...
Taiki, Futagami +4 more
openaire +2 more sources
Sedimentary inputs to the Nankai subduction zone: The importance of dispersed ash [PDF]
We examine the importance of dispersed volcanic ash as a critical component of the aluminosilicate sediment entering the Nankai Trough, located south of Japan’s island of Honshu, via the subducting Philippine Sea plate. Multivariate statistical analyses of an extensive major, trace, and rare earth element data set from bulk sediment and discrete ash ...
Rachel P. Scudder +5 more
openaire +3 more sources
The First D/V Chikyu IODP Operations: Successful Logging and Coring During NanTroSEIZE Stage 1 Expeditions [PDF]
The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) is a multi-expedition IODP drilling project aimed at drilling, coring, logging, and instrumenting the seismogenic zone of an active subduction margin , in a region thought to generate megathrust
Moe Kyaw Thu +3 more
doaj +1 more source

