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Goblin Valley
Relay structure at Buckskin Spring near Goblin Valley. Oblique deformation ...
Comparison of permeability values obtained from different approaches (plug,...
Figure 1. (A) Compressive and (B) extensional deformation band stepover geo...
Synthetic diagrams summarizing the evolution of the deformation and its ass...
(A) Location of the study site at the scale of Utah: San Rafael desert. (B)...
Graph summarizing the permeability of the host rocks (HR) and their resulti...
(A, B) Grain size distribution of the host rock sandstones at Clashach Cove...
Examples of geometry and spatial distribution of band sets formed as revers...
Micro- and macrostructural observations and quantification of the deformati...
Fault surface development and fault rock juxtaposition along deformation band clusters in porous sandstones series
Scanning electron microscopy of backscattered electrons imaging of the host...
Micro- and macrostructural observations and quantification of the deformati...
A) General Jurassic chronostratigraphic section on the Colorado Plateau, c...
Near-tip stress rotation and the development of deformation band stepover geometries in mode II
The 36–18 Ma Central Nevada ignimbrite field and calderas, Great Basin, USA: Multicyclic super-eruptions
Tectonic regime controls clustering of deformation bands in porous sandstone
Jointed deformation bands may not compartmentalize reservoirs
Characterization of deformation bands associated with normal and reverse stress states in the Navajo Sandstone, Utah: Discussion
A review of deformation bands in reservoir sandstones: geometries, mechanisms and distribution
Abstract Deformation bands are common subseismic structures in porous sandstones that vary with respect to deformation mechanisms, geometries and distribution. The amount of cataclasis involved largely determines how they impact fluid flow, and cataclasis is generally promoted by coarse grain size, good sorting, high porosity and overburden (usually >500–1000 m). Most bands involve a combination of shear and compaction, and a distinction can be made between those where shear displacement greatly exceeds compaction (compactional shear bands or CSB), where the two are of similar magnitude (shear-enhanced compaction bands or SECB), and pure compaction bands (PCB). The latter two only occur in the contractional regime, are characterized by high (70–100°) dihedral angles (SECB) or perpendicularity (PCB) to σ 1 (the maximum principal stress) and are restricted to layers with very high porosity. Contraction generally tends to produce populations of well-distributed deformation bands, whereas in the extensional regime the majority of bands are clustered around faults. Deformation bands also favour highly porous parts of a reservoir, which may result in a homogenization of the overall reservoir permeability and enhance sweep during hydrocarbon production. A number of intrinsic and external variables must therefore be considered when assessing the influence of deformation bands on reservoir performance.