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• W2112140100 abstract "AbstractDune deposits on Lake Michigan’s southeastern shore contain pin stripe laminations: thin (<3 mm) laterally continuous (10 m) layers of dark sand, with vertical separations of 0.5–100 cm between laminations. On modern dune surfaces concentrations of dark sand are observed in ripple troughs and form continuous sheets that pass under ripple crests. We explore the source of the dark grains and the processes that can concentrate them in layers, using direct field observations, textural analysis, and point counts of sand grain minerals using the energy-dispersive x-ray analysis function on an electron microprobe. Large and medium size fractions of dune sand are dominated by quartz while smaller size fractions contain high proportions of dark heavy minerals (Fe-Ti oxides, garnets, and Fe-Mg silicates). Pin stripe laminations and dark surface patches are enriched in this fine-grained component, suggesting that sorting by grain size is important in their origin. The fine-grained sand fractions of glacial t..." @default.
• W2112140100 created "2016-06-24" @default.
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• W2112140100 date "2011-09-01" @default.
• W2112140100 modified "2023-09-26" @default.
• W2112140100 title "The Origin of Dark Sand in Eolian Deposits along the Southeastern Shore of Lake Michigan" @default.
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• W2112140100 doi "https://doi.org/10.1086/661192" @default.
• W2112140100 hasPublicationYear "2011" @default.
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