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Convolute laminations and load structures in turbidites as indicators of flow reflections and decelerations against bounding slopes. Examples from the Marnoso-arenacea Formation (northern Italy) and Annot Sandstones (south eastern France)
Keywords: امواج داخلی; Soft sediment deformations; Convolute laminae; Load structures; Contained-reflected beds; Internal waves; Syntectonic sedimentation