Deformation along faults in the shallow crust (< 1 km) introduces permeability heterogeneity
and anisotropy, which has an important impact on processes such as regional groundwater …

Deformation bands are the most common strain localization feature found in deformed
porous sandstones and sediments, including Quaternary deposits, soft gravity slides and …

Coupling the basics of hygrogeology with analytical and numerical modeling methods,
Hydrogeology and Groundwater Modeling, Second Edition provides detailed coverage of …

We evaluate the benefits of space‐derived ground deformation measurements for basin‐
wide characterization of aquifer‐system properties and groundwater levels. We use …

We argue that the observed conduit‐barrier behavior of fault zones in siliciclastic
sedimentary aquifer systems can be understood by considering a strongly anisotropic …

Faults can be either conduits or retarders for fluid flow. As the presence of faults increases
the risks for hydrocarbon exploration, the sealing behaviour of a fault zone has been a focus …

Groundwater management typically relies on water‐level data and spatially limited
deformation measurements. While interferometric synthetic aperture radar has been used to …

Clay smear is a collection of fault processes and resulting fault structures that form when
normal faults deform layered sedimentary sections. These elusive structures have attracted …

The distribution of deformation bands in damage zones of extensional faults in porous
sandstones has been analyzed using 106 outcrop scanlines along which the position and …

The concept of fault facies is a novel approach to fault description adapted to three-
dimensional reservoir modeling purposes. Faults are considered strained volumes of rock …