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More model informationBedding geometry, changes in bedform size, angle, and shape of laminae, along with the presence of mud drapes, is all indicative of the cyclic changes in the velocity of tidal currents. Orientation of lamination records a dominant paleoflow towards the NW, which in this case means towards the open sea, and therefore leads to the conclusion that the bedforms were formed by ebb tidal currents. Roda Sandstone (Eocene, South-Pyrenean Foreland Basin, Aragón)
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