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

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

Using image logs from horizontal wells in the asymmetric East Painter Reservoir anticline in
Wyoming, scanlines and petrographic observations from nearby outcrops, and methods that …

Shallow marine carbonate sedimentation dominated during the Albian in the western part of
the Basque Cantabrian Basin in Northern Spain, forming the large Ramales Platform. This …

Relay ramps associated with overlap** faults are commonly regarded as efficient conduits
for fluid flow across potentially sealing intra-reservoir fault zones. The current study …

Frictional slip along bedding planes contributes to fault-related folding of layered rocks. We
use numerical experiments to investigate the deformation of frictional bedding planes near …

The three-dimensional meter-scale fracture networks, observed on exposed folds between
the towns of Tata and Akka, western Moroccan Anti-Atlas, consist mostly of planar …

Since 2000, China has been ranked as one of the top countries in gas production.
Nevertheless, the domestic gas production can hardly satisfy the need of national economic …

Cataclastic deformation bands, which are common in sandstone reservoirs and which may
negatively affect fluid flow, are generally associated with notable thickness variations. It has …

The mechanics of deformation in multilayer flexures is analysed by comparing field
observations of joint clusters from the East Kaibab Monocline, Utah with fracture patterns …