Tectono-stratigraphic analysis of Early Syn-Rift Siliciclastic Deposits of Nakheil and Ranga Formations, based on outcrop data from Hamadat Half Graben basin, south Quseir indicates that the evolution of normal faulting was an important role on syn rift depositional patterns and sequence stratigraphic development. The Nakheil Formation was deposited in depocentres formed during the low subsidence rift initiation phase. The Nakheil ... Read more