Pinedale Field
DOI: 10.1306/13511891m1071510
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Sedimentology and Reservoir Characterization of the Upper Cretaceous Lance and Upper Mesaverde Intervals from Core Data in Pinedale Field, Wyoming

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Cited by 5 publications
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“…Identification of stacking patterns and grain size trends in fluvial deposits is important, because grain size and sorting exert strong controls on reservoir porosity and permeability (Selley 2000). Although grain size variance is relatively low in fine-grained fluvial reservoirs, the coarsest grained and highest energy lithofacies typically exhibit greater absolute porosity and permeability than finer-grained, lower energy lithofacies (e.g., Chapin et al 2014). Therefore, understanding the 3D distribution of porosity and permeability in reservoirs is necessary for constructing and conditioning representative reservoir models that form the basis for well-completion and field-development strategies (Ebanks 1987).…”
Section: Introductionmentioning
confidence: 99%
“…Identification of stacking patterns and grain size trends in fluvial deposits is important, because grain size and sorting exert strong controls on reservoir porosity and permeability (Selley 2000). Although grain size variance is relatively low in fine-grained fluvial reservoirs, the coarsest grained and highest energy lithofacies typically exhibit greater absolute porosity and permeability than finer-grained, lower energy lithofacies (e.g., Chapin et al 2014). Therefore, understanding the 3D distribution of porosity and permeability in reservoirs is necessary for constructing and conditioning representative reservoir models that form the basis for well-completion and field-development strategies (Ebanks 1987).…”
Section: Introductionmentioning
confidence: 99%