Sedimentary aggregates in the Peoria Loess of Nebraska, USA
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Mason, Joseph A
Jacobs, Peter
Greene, Richard
Nettleton, WD
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Elsevier
Abstract
Loess grain size data used to infer transport direction or wind strength are generally derived from vigorously disaggregated samples. However, these data may not adequately represent the effective particle size distribution during loess transport, if the
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