Comparison between Miocene and Pliocene facies distribution related to Syn Rift tectonics along the Egyptian Red Sea coastal area
Two different regimes of Neogene sedimentation can be recognized along thr Red Sea coastal area: 1- The first regime comprises the Pre-Abu Dabbab Evaporite Miocene sediments. The distribution of the facies is mainly governed by the main western Miocene NW fault bounding the edge of the Red Sea rift as well as the NW trending fault-blocks. Carbonates were mainly deposited ... Read more