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- W1992179448 abstract "Eolian sands which accumulated along the eastern margin of the Iraq Southern Desert show variable grain-size distributions. Samples from different parts of a dune have distinctly different amounts of the three basic genetic populations of clastic grains. Bimodal grain-size distribution is relatively widespread. The origin of bimodal distribution is explained by the infiltration of fine fractions transported by dust storms. The variation of the statistical parameters is in contrast with the previously reported low variability of these parameters in eolian sands. Carbonate content is variable, reaching a maximum of 30%. Carbonate is concentrated in the finest fraction, which is derived from alluvial sediments and desert soils. The association of heavy minerals in eolian sands is characterized by large amounts of opaque and unstable minerals of the hornblende, epidote, and pyroxene groups. The local accumulation of celestite is remarkable. The association of heavy minerals is generally similar to that of sediments of the Lower Mesopotamian Plain, which were probably the main source of eolian clastics." @default.
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- W1992179448 date "1972-08-01" @default.
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- W1992179448 title "Grain-size distribution, carbonate content and heavy minerals in eolian sands, southern desert, Iraq" @default.
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- W1992179448 doi "https://doi.org/10.1016/0037-0738(72)90040-1" @default.
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