Fig. 1From: Sequence stratigraphy and depositional environments of Late Cretaceous–Early Palaeogene succession, North Eastern Desert, EgyptSatellite image of the Southern Galala Sub-basin, Eastern Desert, Egypt. Shown are the affecting structures, distribution of the formations, and the location of studied sections, which run in transect A-B parallel to the Gulf of Suez. The strike directions of the Wadi Araba and North Esh El-Mallaha faults (related to Mesozoic–Palaeogene tectonics) and the Gulf of Suez faults (related to the Miocene opening of the Gulf) lie perpendicular to each otherBack to article page