Deformation bands are common subseismic structures in porous sandstones that vary with
respect to deformation mechanisms, geometries and distribution. The amount of cataclasis …

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 …

Although it is well documented that during faulting there is an overall fault zone porosity loss
in porous sandstone, little is known about the effect of shear-induced compaction on …

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

The objective of this study is to analyze the influence of brittle reactivations of continental-
scale Precambrian ductile shear zones on the evolution of deformation band damage zones …

Cataclastic bands in high-porosity sandstones significantly influence fluid flow, thus
impacting the exploration and development of oil and gas. However, little experimental …

We present the results of meso-and micro-structural analyses performed on fault-related soft-
sediment deformation structures affecting poorly lithified, high-porosity siliciclastic sediments …

Clusters of deformation bands associated with fault damage zones modify the petrophysical
properties of rocks and influence fluid migration. Many works discuss the influence of …

Deformation bands (DB) are ubiquitous structural elements that can be found in Miocene pre-
and syn-rift sediments of the extensional Pannonian Basin, central Europe. Across the field …

In this contribution we show the variation of the uniaxial compressive strength (UCS) and
petrophysical properties of different architectural elements of fault zones affecting poorly …