Tectono-stratigraphic analysis of Late Oligocene-Early Miocene Nakheil and Ranga Formations, based on outcrop data from Hamadat and Zug El Bohar half-graben basins, south Quseir, indicates that the evolution of normal fault segments was an important control on syn-rift depositional patterns and sequence stratigraphic development. Sedimentological and stratigraphic analysis of the Nakheil Formation indicates that it was deposited in a series ...
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