Mud volcanism and diapirism have puzzled geoscientists for∼ 2 centuries. They have been
described onshore and offshore in many places on Earth, and although they occur in various …

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 of rough seafloor and seamounts is thought to impact a broad range of
geodynamic processes, including megathrust slip behaviour, forearc fluid flow and long-term …

Abstract Comparison of mass transfer patterns, geometry and microstructures developed
within and around veins allows the interpretation of processes of fluid flow during …

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 low permeability of clays, shales, and other argillaceous lithologies makes them key
controls of transport and deformation processes in the crust but is known for being …

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 structural and microstructural observations from exhumed subduction-related rocks
exposed on Syros Island (Cyclades, Greece) to provide constraints on the length scales and …

Ocean plate stratigraphy (OPS) is essential to understanding accretionary wedges and
complexes along convergent plate margins. Mélanges within accretionary wedges and …

Dip** permeable sandstone bodies encased in overpressured low permeability mudstone
have a characteristic pressure field: sandstone pressures follow the hydrostatic gradient …