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The AAPG/Datapages Combined Publications Database
Wyoming Geological Association
Abstract
Petrographic and Petrophysical Properties of the Almond Sandstone in the Washakie Basin
Abstract
The marginal marine and nonmarine Almond sandstones are mostly sublitharenite, litharenite, and lithic arkose. The sandstones are fine- to very-fine-grained, and are well-sorted. The framework composition, authigenic minerals, and porosity and permeability distributions in the Almond sandstones are different below and above 8,000 feet, resulting in a variation in hydrocarbon reservoir types. Diagenetic changes in the Almond sandstones have been affected by burial deeper than their present depths. Reconstruction of the burial history and diagenetic modeling are necessary for understanding the diagenetic evolution of the Almond sandstones.
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