Abstract:<p>Contourites occur where along-slope bottom currents induce large accumulations of sediments in the deep sea (Faug&#232;res and Stow, 2008). Distinguishing among contourites and other depositional facies on continental slopes is fundamental for paleoenvironmental reconstructions like bottom current velocities. Nonetheless, reliable and easily applicable diagnostic criteria to properly differentiate between contourites and other coarse-grained and/or graded deep-water deposits such as tu… Show more
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