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Contemporary Depositional Environments of the Omo Delta
Nature, 1970Geomorphological and sedimentological studies of depositional environments of the modern Omo River delta and floodplain are essential to an understanding of the Pliocene to Pleistocene Mursi, Nkalabong and Kibish Formations of the Lower Omo Basin (southwestern Ethiopia).
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Deposit Insurance in a Sequential-Service Constrained Environment
Mathematical Social ScienceszbMATH Open Web Interface contents unavailable due to conflicting licenses.
Fernando A. Barros Jr. +3 more
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Carbonate Depositional Environments
2004Knowing where modern carbonates occur, what they are composed of, and what their controls are is essential for evaluating microfacies data. The objectives of this chapter are to summarize the settings and environments in which carbonate sediments are formed and to document which classifications are used for differentiating these environments.
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Section 9 Depositional Environments of Evaporite Deposits
1987Abstract Evaporites are sedimentary deposits composed of minerals precipitated from brines concentrated by evaporation. Some evaporites were deposited from the waters of inland desert basins. Others are products of evaporitic concentration within the interstitial waters of bodies of sediment located along the margins of the sea. Still
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Depositional Environments and Sedimentary Geology Coal Depositional Systems
1998Abstract Depositional systems affect the thickness, geometry, extent, quality of coal seams, and the integrity of the associated roof and floor rocks. Moreover, post-depositional compaction may add complexities to coal seam geometry and impact economic recovery of coal and/or coalbed methane (CBM).
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Journal of Sedimentary Environments, 2020
Faiz Ahmad, M. Quasim, A. Ahmad
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Faiz Ahmad, M. Quasim, A. Ahmad
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Coal Facies and Depositional Environment
1992In the preceding chapters coal components have been classified on the basis of physical, chemical and genetic relationships. In the following discussion these will be employed in a filtering process that is designed to detect the signatures left behind by depositional environments in the form of a distinctive coal facies.
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