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[HTML][HTML] Submarine slide blocks and associated soft-sediment deformation in deep-water basins: A review
Abstract Three-dimensional (3D) seismic and outcrop data are used to review the
significance of submarine slide blocks and associated soft-sediment deformation structures …
significance of submarine slide blocks and associated soft-sediment deformation structures …
Sixty years of anisotropy of magnetic susceptibility in deformed sedimentary rocks
The use of the Anisotropy of Magnetic Susceptibility (AMS) has become a rather common
practice in Earth Sciences since the pioneer note by Graham. The versatility of the …
practice in Earth Sciences since the pioneer note by Graham. The versatility of the …
Slow slip along the Hikurangi margin linked to fluid-rich sediments trailing subducting seamounts
Large seamounts and basement relief cause permanent deformation when they collide with
the overriding plate at subduction zones. The resulting structural and compositional …
the overriding plate at subduction zones. The resulting structural and compositional …
A review of shallow slow earthquakes along the Nankai Trough
Slow earthquakes occur at deep and shallow plate boundaries along the Nankai Trough.
Deep slow earthquakes are continuously distributed along the 30–40 km depth contours of …
Deep slow earthquakes are continuously distributed along the 30–40 km depth contours of …
Tsunamigenic potential of the shallow subduction plate boundary inferred from slow seismic slip
H Sugioka, T Okamoto, T Nakamura, Y Ishihara… - Nature …, 2012 - nature.com
At subduction zones, convergence between the two plates at shallow levels was thought to
occur aseismically, accommodated by asiesmic slip along either the megathrust plate …
occur aseismically, accommodated by asiesmic slip along either the megathrust plate …
Elevated pore pressure and anomalously low stress in regions of low frequency earthquakes along the Nankai Trough subduction megathrust
Recent seismic reflection and ocean bottom seismometer (OBS) studies reveal broad
regions of low seismic velocity along the Nankai subduction plate boundary megathrust …
regions of low seismic velocity along the Nankai subduction plate boundary megathrust …
Pitfalls and limitations in seismic attribute interpretation of tectonic features
Seismic attributes are routinely used to accelerate and quantify the interpretation of tectonic
features in 3D seismic data. Coherence (or variance) cubes delineate the edges of …
features in 3D seismic data. Coherence (or variance) cubes delineate the edges of …
Waveform tomography imaging of a megasplay fault system in the seismogenic Nankai subduction zone
We apply Frequency-domain Waveform Tomography to form quantitative, high-resolution P-
wave velocity images of a megasplay fault system within the central Nankai subduction zone …
wave velocity images of a megasplay fault system within the central Nankai subduction zone …
[HTML][HTML] Pore pressure distribution of a mega-splay fault system in the Nankai Trough subduction zone: Insight into up-dip extent of the seismogenic zone
We use the pore pressure distribution predicted from a waveform tomography (WT) velocity
model to interpret the evolution of the mega-splay fault system in the Nankai Trough off …
model to interpret the evolution of the mega-splay fault system in the Nankai Trough off …
Tectonic mélange as fault rock of subduction plate boundary
An assemblage of quantitative data sets is examined to evaluate tectonic mélange as a plate
boundary fault rocks in subduction zone. The research object is the latest Cretaceous Mugi …
boundary fault rocks in subduction zone. The research object is the latest Cretaceous Mugi …