E. C. Willey; Supposed cross-lamination in the Mesozoic strata of South Wales. Journal of Sedimentary Research ; 37 (1): 233–235. doi: https://doi.org/10.1306/74D716A9-2B21-11D7-8648000102C1865D
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Structures consisting of intersecting bandings have been interpreted as being produced by the development of low-angle jointing in laminated sediments. Similar structures have been previously described as cross-lamination.
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