Barham Parkash; Downcurrent changes in sedimentary structures in Ordovician turbidite greywackes. Journal of Sedimentary Research ; 40 (2): 572–590. doi: https://doi.org/10.1306/74D71FD7-2B21-11D7-8648000102C1865D
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Cloridorme formation, sole marks, deposition by low concentration, highly turbulent currents, Gaspe, Quebec
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