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Sedimentary facies as indicators of Mesozoic palaeoclimate
1994Sedimentary facies alone provide equivocal, and qualitative, evidence about Mesozoic climates and climate changes. The most climatically informative sediments are laterites, evaporites and aeolianites. Tills would also be unequivocal where present. A range of other criteria (e.g.
B. W. Sellwood, G. D. Price
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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
Palaeogeography, Palaeoclimatology, Palaeoecology, 1981+4 more sources
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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Distinguishing between Deep-Water Sediment Facies: Turbidites, Contourites and Hemipelagites
Geosciences (Switzerland), 2020Dorrik A V Stow, Zeinab Smillie
exaly