At subduction zones, fluid flow, pore pressure, and tectonic processes are tightly
interconnected. Excess pore pressure is driven by tectonic loading and fluids released by …

Deepwater fold and thrust belts (DWFTBs) are classified into near-field stress-driven Type 1
systems confined to the sedimentary section, and Type 2 systems deformed by either far …

Subduction thrust faults generate earthquakes over a limited depth range. They are aseismic
in their seaward updip portions and landward downdip of a critical point. The seaward …

Seismic reflection profiles reveal steeply landward–dipping splay faults in the rupture area of
the magnitude (M) 8.1 Tonankai earthquake in the Nankai subduction zone. These splay …

A growing body of evidence suggests that fluids are intimately linked to a variety of faulting
processes. These include the long term structural and compositional evolution of fault zones; …

Mudstone permeabilities vary by ten orders of magnitude and by three orders of magnitude
at a single porosity. Much of the range at a given porosity can be explained by differences in …

The thickness of an active plate boundary fault is an important parameter for understanding
the strength and spatial heterogeneity of fault behavior. We have compiled direct …

We report characteristic P wave spectra and stress drops of very low frequency (VLF)
earthquakes that occurred within the accretionary prism along the Nankai Trough …

Down‐hole geochemical anomalies encountered in active accretionary systems can be
used to constrain the timing, rates, and localization of fluid flow. Here we combine a coupled …

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 …