M. G. Laird; Vertical sheet structures; a new indicator of sedimentary fabric. Journal of Sedimentary Research ; 40 (1): 428–434. doi: https://doi.org/10.1306/74D71F69-2B21-11D7-8648000102C1865D
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Turbidite sequence, paleocurrent indicators, matrix-deficient residue of larger grains initiated during differential settling
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