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TitleDateSubjectDescription
1 Depositional environments of oil shale in the Green River Formation, Douglas Creek Arch, Colorado and Utah1985depositional environments; oil shale; Green River Formation; Douglas Creek Arch; stratigraphyDouglas Creek arch in western Colorado and eastern Utah separates the Uinta and Piceance Creek basins. During deposition of the lower part of the Eocene Green River Formation, the arch provided a physical barrier dividing ancient Lake Uinta into two segments. As the lake expanded, the arch became a ...
2 Hypotheses of oil-shale genesis, Green River Formation, northeast Utah, northwest Colorado, and southwest Wyoming1985oil shale; Green River Formation; tar sandstoneIn the six decades or so of oil-shale studies on the Green River Formation (Paleocene/Eocene) in northeast Utah, northwest Colorado, and southwest Wyoming, two alternative hypotheses for the paleoenvironment have dominated the literature: (1) a stratified lake in which anaerobic conditions in the hy...
3 Bituminous sandstone and limestone deposits of Utah1963The significant bituminous sandstone and bituminous Limestone deposits of Utah are located within, or on the edges of, the Uinta Basin. They are all located within the boundaries of Carbon, Duchesne, and Uintah Counties. The Sunnyside deposits in Carbon County contain the greatest reserves of bitumi...
4 Gilsonite1961-06glisonite; bitumen; asphalt-based petroleum; glisonite oreGlisonite is a black, pitch-like substance which occurs in pure form in large veins in the Tertiary sediments of the Uinta Basin. It is a homogenous petroleum substance (technically it is a predominently aromatic asphaltite) which fuses relatively easily and burns like tar. Glisonite is brittle and ...
5 Gilsonite and related hydrocarbons of the Uinta Basin, Utah1949glisonite; hydrocarbons; Uinta Basin; kerogen; bitumenHydrocarbons are important in the present study for two reasons: ( 1) An understanding of their nature and origin may lead to a better understanding of the oil possibilities in the area. (2) From gilsonite, kerogen, and associated bituminous substances there may be fractionated many still-undiscover...
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