We discuss techniques to represent groundwater flow in carbonate aquifers using the three
existing modeling approaches: equivalent porous medium, conduit network, and discrete …

Springs sustain groundwater-dependent ecosystems and provide freshwater for human use.
Springs often occur because faults modify groundwater flow pathways leading to discharge …

Deep fluids play active roles during the preparatory phases of large earthquakes and,
through their chemical signature, carry information about deep processes within the …

Fault zones commonly have spatially variable fault rocks and brittle structures. Differing fault-
rock attributes may retard or increase cross-and along-fault permeability. Our work analyzed …

This study uses a 3D exposure of a fault zone in the Rio do Peixe Basin (NE Brazil) to
investigate the impact of deformation band connection on permeability in porous …

Analyzing the factors that affect the fault damage zone parameters and the impact of
deformation on host rock permeability is fundamental for predicting the fluid flow behavior in …

In permeability modeling of fault damage zones affecting porous sandstones, deformation
bands are commonly considered low-permeability structures that influence fluid flow …

We present new insights on the geometry, initiation and growth of the Thyolo fault, an 85 km
long active border fault in the southern Malawi Rift, from high-resolution topography, field …

Hydrothermal silicification and deformation bands influence the physical properties of
porous siliciclastic rocks. However, the impacts generated by the coexistence of these two …

The earthquake sequence, with a maximum earthquake magnitude of MW 3.8, that occurred
during January–February 2022 at the northern Dead Sea fault, is shown to be induced by …