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Turbidites are syntectonic sedimentary deposits orginated by deep submarine turbidity currents, especially in foreland basins, in tectonic setting of convergent margin (active). To most part of geologists, turbidite is a sequence of layers that consist of a grano-classified set of sandstone strata/pelitic sediments, generally in fining-upward that were deposited by turbidity currents and is commonly covered by hemipelagic pelites containing assemblages of deep-water fossils.