Fig. 5From: Sequence stratigraphy and depositional environments of Late Cretaceous–Early Palaeogene succession, North Eastern Desert, EgyptIdealized Late Cretaceous–Palaeogene sea-level fluctuation curve in southern Galala Sub-Basin, as deduced from integrated lithostratigraphy, micropaleontology, paleobathymetrical parameters, organic geochemistry, and microfacies analysis, and compared with regional and global sea-level variations (Haq et al. 1987; Lüning et al. 1998)Back to article page