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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Evaporites of the Green River Formation, Bridger and Piceance Creek Basins: Deposition, Diagenesis, perennial, density stratified saline lakes. Primary textures in bedded trona and nahcolite indicate that they formed at the air-water interface as microcrystalline cumulate needles. Halite formed concurrently with trona and nahcolite as cumulate layers, and as basin floor crusts. Shortite formed di

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Book 2015-9 provide detailed member-scale synthesis of Green River Formation strata within the Greater Green River, Fossil, Piceance Creek and Uinta Basins, while its final two chapters address its enigmatic evaporite deposits and ichnofossils at broad, interbasinal scale..

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Introduction to the Green River Formation,s beginning to bring to tempo and origins of the pronounced cyclity exhibited by the Green River Formation into focus. Each of the 11 subsequent chapters of this book presents a suite of detailed stratigraphic and sedimentologic investigations of the Green River Formation within the Green River Formation basins.

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Initiation of Eocene Lacustrine Sedimentation in the Greater Green River Basin: Luman Member of theustrine deposition within the Greater Green River Basin during the Early Eocene. Well-drained alluvial and fluvial strata of the Wasatch Formation are overlain by carbonaceous mudstone, channelized sandstone and isolated interbedded pond deposits of the lower Luman Member, which are in turn overlain