THE POST ABU DABBAB EVAPORITE UPPER MIOCENE (?) PLIOCENE SEDIMENTS ALONG THE RED SEA COASTAL AREA SOUTH AND NORTH OF MERSA ALAM COULD BE SUBDIVIDED INTO THREE LITHOFACIES: FACIES A : DOMINANTLY FLUVIATILE SILICICLASTICS, WITH RESTRICTED MARINE CARBONATES AND EVAPORITES NEAR THE TOP (SAMH MB. OF MERSA ALAM FM.). FACIES B: OPEN MARINE, MIXED SILICICLASTIC-CARBONATE SEDIMENTS DEPOSITED IN BEACH, INTERTIDAL ...
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