Nigel L. Banks; The origin and significance of some downcurrent-dipping cross-stratified sets. Journal of Sedimentary Research ; 43 (2): 423–427. doi: https://doi.org/10.1306/74D72784-2B21-11D7-8648000102C1865D
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Formed by migration of large-scale ripples, fluvial, Precambrian sandstone, Norway
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