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Primary terms
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carbon
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Tertiary
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Tullock Member (1)
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Chordata
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upper Albian (2)
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Aptian (1)
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Cloverly Formation (1)
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Mancos Shale (13)
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Middle Cretaceous (1)
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Upper Cretaceous
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Campanian (10)
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lower Cenomanian (1)
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Ferron Sandstone Member (17)
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Frontier Formation (1)
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Maestrichtian (2)
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Mesaverde Group (4)
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Price River Formation (2)
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Senonian (7)
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Star Point Sandstone (3)
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Turonian
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middle Turonian (2)
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Jurassic
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Carmel Formation (3)
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Middle Jurassic
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Summerville Formation (1)
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Upper Jurassic
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Brushy Basin Member (3)
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Entrada Sandstone (3)
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Morrison Formation (7)
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Salt Wash Sandstone Member (2)
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Navajo Sandstone (1)
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Triassic
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Lower Triassic
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Permian-Triassic boundary (1)
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Moenkopi Formation (2)
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plate tectonics (2)
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weathering (1)
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Emery County Utah
Alkaline sill intrusions in sedimentary basins: emplacement of the Mussentuchit Wash Sill in San Rafael Swell, Utah
Paralic sedimentology of the Mussentuchit Member coastal plain, Cedar Mountain Formation, central Utah, U.S.A.
The problem of paleo-planforms
Stratigraphic architecture within delta plain deposits in the Upper Cretaceous Neslen and Farrer Formations, Book Cliffs, Utah
Coarse-grained meandering distributive fluvial system of the basal Cedar Mountain Formation, U.S.A.
Bringing sedimentology and stratigraphy into the StraboSpot data management system
Zircon (U-Th)/(He-Pb) double-dating constraints on the interplay between thrust deformation and foreland basin architecture, Sevier foreland basin, Utah
Glossifungites gingrasi n. isp., a probable subaqueous insect domicile from the Cretaceous Ferron Sandstone, Utah
Tidal estuarine deposits of the transgressive Naturita Formation (Dakota Sandstone): San Rafael Swell, Utah, U.S.A.
Sedimentology, diagenesis, and reservoir characterization of the Permian White Rim Sandstone, southern Utah: Implications for carbon capture and sequestration potential
Lacustrine cyclicity in the early Eocene Green River Formation, Uinta Basin, Utah: Evidence from X-ray fluorescence core scanning
Red-bed bleaching in a CO 2 storage analogue: Insights from Entrada Sandstone fracture-hosted mineralization
Dip, layer spacing, and incision rate controls on the formation of strike valleys, cuestas, and cliffbands in heterogeneous stratigraphy
Detrital-Zircon U-Pb Paleodrainage Reconstruction and Geochronology of the Campanian Blackhawk–Castlegate Succession, Wasatch Plateau and Book Cliffs, Utah, U.S.A.
Erosional surfaces in the Upper Cretaceous Castlegate Sandstone (Utah, USA): Sequence boundaries or autogenic scour from backwater hydrodynamics?
A siltstone reaction front related to CO 2 - and sulfur-bearing fluids: Integrating quantitative elemental mapping with reactive transport modeling
TRANSGRESSIVE EROSION EXPRESSED AS A GLOSSIFUNGITES -BEARING WOODGROUND: AN EXAMPLE FROM THE BLACKHAWK FORMATION, UTAH
A large pterodactyloid pterosaur from the Late Cretaceous Ferron Sandstone of Utah
Abstract: Three associated incomplete wing bones of a large pterodactyloid pterosaur from the Ferron Sandstone Member of the Mancos Shale Formation of Utah are described. Based on the morphology of the bones’ articular ends, the specimen is referred to the Pteranodontoidea. Associated ammonites indicate that the specimen’s age is Middle Turonian, so it adds to the sparse worldwide record of Turonian pterosaurs. The record of pteranodontoid pterosaurs in the Western Interior Seaway of North America is reviewed, and it is suggested that pteranodontoids were not diverse.
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.