Melt extraction from the partially molten mantle is among the fundamental processes
shaping the solid Earth today and over geological time. A diversity of properties and …

The interior of the Earth is quite complex due to the actual geometrical structure and the
presence of complex rheological materials, including viscoelastic rocks, porous sediments …

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 …

To reach Earth's surface, magma must ascend from the hot, ductile asthenosphere through
cold and brittle rock in the lithosphere. It does so via fluid-filled fractures called dykes. While …

Two-phase flow equations that couple solid deformation and fluid migration have opened
new research trends in geodynamic simulations and modelling of subsurface engineering …

Focused fluid flow is common in sedimentary basins worldwide, where flow structures often
penetrate through sandy reservoir rocks, and clay‐rich caprocks. To better understand the …

Gas chimneys, fluid-escape pipes, and diffused gas clouds are common geohazards above
or below most petroleum reservoirs and in some CO2 storage sites. However, the processes …

A valuable synthesis of the physics of magmatism for students and scholars Magma genesis
and segregation have shaped Earth since its formation more than 4.5 billion years ago …