During the past five decades, numerical modeling of subduction, one of the most
challenging and captivating geodynamic processes, remained in the core of geodynamic …

One aspect of earthquake physics not adequately addressed is why some earthquakes
generate thousands of aftershocks while other earthquakes generate few, if any …

In subduction zones, fluids are often invoked to explain slip processes on the megathrust,
from great earthquakes to slow-slip events and tectonic tremors. However, it is unclear how …

Slow slip and tremor is observed along many subduction margins and is commonly linked to
fluid pressure variations and migration. Accurate estimates of porosity and permeability …

A major goal in earthquake physics is to derive a constitutive framework for fault slip that
captures the dependence of shear strength on fault rheology, sliding velocity, and pore-fluid …

The interplay between compaction‐driven fluid flow and plastic yielding within porous media
is investigated through numerical modeling. We establish a framework for understanding the …

Time-dependent rock deformation affects both natural processes happening on the
geological time scale and subsurface engineering operations. We perform a series of …

We combined novel laboratory techniques and numerical modeling to investigate (a)
seismic preparatory processes associated with deformation localization during a triaxial …

An understanding of instantaneous and long‐term compaction of porous rocks is important
for reservoir engineering and Earth sciences. Experience from laboratory triaxial …

Several decades of field, geophysical, analogue, and numerical modeling investigations
have enabled documentation of the wide range of tectonic transport processes in …