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 …

Abstract The Indo-Burma Ranges form an enigmatic mountain belt, with fragments of
evidence for an early accretionary history (Jurassic Jade belt HP-LT metamorphism; Early …

Active and widespread CH4 accumulations and emissions in the Nankai Trough subduction
zone are attested by numerous mud volcanoes, gas plumes, and gas hydrates containing …

The mathematization of all sciences, the fading of traditional scientific boundaries, the
impact of computer technology, the growing importance of computer modeling and the …

There is considerable variability in the thickness, structure, and macroscopic deformation
style within shale-prone major thrust zones, which also impacts the structural style in the …

Sedimentary deposits in the distal Kumano forearc basin of the Nankai accretionary margin
off Kii Peninsula, Japan, have been imaged using three-dimensional (3D) seismic data. The …

Multiple lines of evidence exist for a range of sediment mass movement processes within the
shallow megasplay fault zone (MSFZ) area and the adjacent slope basin in the outer fore arc …

Accretionary complexes host a variety of fault zones that accommodate plate convergence
and internal prism deformation, including the décollement, imbricate thrusts, and out‐of …

The temporal and spatial evolution of a seismogenic megasplay fault in the Kumano area,
Nankai Trough (southwest Japan), is revealed by detailed investigation of the three …

Geophysical observations show spatial and temporal variations in fault slip style on shallow
subduction thrust faults, but geological signatures and underlying deformation processes …