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Sedimentary Facies Model of Turbidites: ABSTRACT
AAPG Bulletin, 1963Deposits of turbidity currents are characterized by alternating layers of sandstone and shale, in which a unit layer is defined as the sandstone together with its overlying shale. Studies of turbidites of different ages, and from many different localities in Europe, make it clear that turbidites are characterized by one sedimentary facies model, which ...
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Sedimentary environments and facies
Palaeogeography, Palaeoclimatology, Palaeoecology, 1981+4 more sources
Facies Associations of Riphean Sedimentary Sequences
Lithology and Mineral Resources, 2002Large-scale facies associations typical of intra- and pericratonic Riphean sections of the Volga–Ural region, western slope of the Urals, Timan–Pechora region, Kola Peninsula, outer and inner parts of the Siberian, North American, and Indian platforms are considered.
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Facies Architecture in Clastic Sedimentary Basins
1988Clastic deposits can be subdivided into microforms, mesoforms, and macroforms [using Jackson’s (1975) terminology], reflecting a range of physical scales of deposit and the time scale during which they form. A formal three-dimensional subdivision of some types of deposit, which clarifies these physical and temporal scales, can now be attempted using ...
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Sedimentary Environments and Facies
PALAIOS, 1986David J. Bottjer, H. G. Reading
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Sedimentary environments and facies
Earth-Science Reviews, 1987F SCHOEMAN, J THORNTON
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