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The AAPG/Datapages Combined Publications Database

Journal of Sedimentary Research (SEPM)

Abstract


Journal of Sedimentary Petrology
Vol. 33 (1963)No. 3. (September), Pages 628-632

Sizes of Naturally Abraded Materials

John J. W. Rogers, William C. Krueger, Marilyn Krog

ABSTRACT

Sand and silt are formed by two different abrasional mechanisms. Silt grains generally represent chips broken off of larger grains, and large grains are rarely abraded down to the fine sand or silt range. The sand and silt thus represent two different populations, each with a characteristic size distribution curve, and with little overlap between the two. The break between the populations probably occurs at a size of approximately 0.25 mm and accounts for the commonly observed deficiency of sedimnet within 0.05 to 0.25 mm range.


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