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 …
DA Ferrill, AP Morris, RN McGinnis, KJ Smart… - Journal of Structural …, 2017 - Elsevier
Mechanical stratigraphy encompasses the mechanical properties, thicknesses, and interface properties of rock units. Although mechanical stratigraphy often relates directly to …
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 …
We present a conceptual model to explain the development of damage zones around faults in high-porosity sandstones. Damage zone deformation has been particularly well …
VF Bense, MA Person - Water Resources Research, 2006 - Wiley Online Library
We argue that the observed conduit‐barrier behavior of fault zones in siliciclastic sedimentary aquifer systems can be understood by considering a strongly anisotropic …
SS Berg, T Skar - Journal of Structural Geology, 2005 - Elsevier
Outcrop data has been used to examine the spatial arrangement of fractures in the damage zones of a segment of the large-scale Moab Fault (45km in length), SE Utah. The …
Abstract The Sand Hill fault is a steeply dipping, large-displacement normal fault that cuts poorly lithified Tertiary sediments of the Albuquerque basin, New Mexico, United States. The …
G Yielding - Norwegian petroleum society special publications, 2002 - Elsevier
At the 1996 NPF Conference on Hydrocarbon Seals we gave the first presentation of results of a fault-seal study using the Shale Gouge Ratio algorithm, describing a project undertaken …