The Late Miocene- Early Pliocene succession of the Red Sea coastal area between Quseir and Mersa Alam is differentiated, from base to top, into: Abu Dabbab Evaporites and the overlying informal rock units (A), (B) and (C). The characteristic features of Unit (A) (Lithofacies, mineralogical, chemical compositions, fossil content as well as field relations) suggest that these sediments represent the ... إقراء المزيد