Titlebook: Stratigraphy and Paleolimnology of the Green River Formation, Western USA; Michael Elliot Smith,Alan R. Carroll Book 2015 Springer Science

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Lacustrine Sedimentology, Stratigraphy and Stable Isotope Geochemistry of the Tipton Member of the ord a single shift from open to partly closed hydrology, new detailed stratigraphy and stable isotope geochemistry indicates that its strata record open, then partly closed, then open, then partly closed hydrology, which are each recorded by distinct transitions in facies associations, geochemistry,

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Lake Type Transition from Balanced-Fill to Overfilled: Laney Member, Green River Formation, Washakis the final stages of Eocene Lake Gosiute. The Laney Member comprises two main facies associations: fluctuating profundal facies of the lower LaClede Bed; and fluvial-lacustrine facies of the upper LaClede and Sand Butte Beds. The lower LaClede Bed consists of repetitive, 1–5 m scale facies successi

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Stratigraphy and Interbasinal Correlations Between Fossil and the Green River Basin, Wyoming,lution radiometric dates with small error ranges. However, lithostratigraphic correlations of coeval sedimentary units have not been previously successful. Correlations based on mapping of coeval units that can be physically traced from one basin into another would allow for more precise temporal co

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Sedimentology of the World Class Organic-Rich Lacustrine System, Piceance Basin, Colorado,in the world today (~1.5 trillion bbls in place). Based on the detailed facies and facies association study three small-scale (decimetre to metre) depositional cycles have been separated that characterize deposition along the basin margin and in the deeper part of the basin. Stacked depositional cyc

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Facies, Stratigraphic Architecture, and Lake Evolution of the Oil Shale Bearing Green River Formati resource, a predictive genetic model of the basin’s lacustrine strata has been refined here. This model provides a better understanding of facies distribution, stratigraphic architecture, and a precise history of depositional evolution of Lake Uinta in eastern Utah..This study evaluates the upper D

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Evaporites of the Green River Formation, Bridger and Piceance Creek Basins: Deposition, Diagenesis,uilibria, provide information on depositional and diagenetic conditions. Volumetrically important trona (NaHCO. ∙ Na.CO. ∙ 2H.O) and shortite (Na.CO. ∙ 2CaCO.) occur in the Wilkins Peak Member, Bridger Basin, WY, whereas nahcolite (NaHCO.) occurs in the saline facies of the time equivalent Parachute

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Jeremy Boak,Sheven Poolee clearer. This knowledge has come through normal out-patient clinic referrals, care of in-patients, and by working in a domiciliary consultative capacity. The problems that concern family physicians nowadays are somewhat different from the problems of two or three decades ago. The accent now is ver