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• W2048776273 abstract "The Maastrichtian-Lower Eocene sediments on both sides of the northern Gulf of Suez can be subdivided into eight formal formations (including one group) and one informal formation that are described in detail. These lithostratigraphic units reflect three different environmental regimes of deposition or non-deposition. The first regime is characterised by uplift and erosion or non-deposition resulting mostly from the uplift of the Northern Galala/Wadi Araba structure, a branch of the Syrian Arc Foldbelt. The shallow water carbonate platform and slope deposits of the Late Campanian-Maastrichtian St Anthony Formation and the Paleocene-Lower Eocene Southern Galala and Garra Formations represent the second regime and are found north and south of the Northern Galala/Wadi Araba High. The third regime is represented by basinal chalks, marls and shales of the Maastrichtian Sudr Formation and of the Paleocene-Eocene Dakhla, Tarawan and Esna Formations, the Dakhla/Tarawan/Esna informal formation and the Thebes Group. The distribution and lateral interfingering of the above mentioned environmental regimes reflect different vertical movements, changing basin morphology, sea level changes and progradation of shallow water sediments and is illustrated on 11 palæogeographic maps. Les sédiments du Maastrichtien et Eocène inférieur, affleurant de part et d'autre au nord du Golfe de Suez, peuvent être subdivisés en huit unités bien définies (incluant un groupe) et une unité plus informelle qui sont décrites en détail. Ces unités lithostratigraphiques témoignent de trois environnements sédimentaires différents. Le premier est caractérisé par une surrection et une érosion ou une absence de dépots qui résulte pour l'essentiel de la surrection de la structure du Northern Galala/Wadi Arabia, une branche de la ceinture plissée de l'arc Syrien. Un environnement de plateforme carbonatée peu profond, avec des dépots de pentes, correspondant à la formation de St Anthony du Campanien supérieur-Maastrichtien, et aux formations Paléocène-Eocène inférieur du Southern Galala et du Garra, représente le second régîme de dépôt; il est observé au Nord et au Sud du Northern Galala/Wadi Arabia High. Le troisième régîme est constitué par des craies de bassin, des marnes et des shales de la formation maastrichtienne de Sudr, des formations Paléocène-Eocène de Dakla, Tarawan et Esna, la formation informelle de Dakla/Tarawan/Esna et le groupe Thebes. La distribution des milieux de dépots précédents et leurs passages latéraux, témoignent de mouvements verticaux, de variations de la morphologie des bassins et du niveau marin, et de la progradation de sédiments d'eaux peu profondes. Ils sont illustrés par 11 cartes paléogéographiques." @default.
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• W2048776273 date "2001-02-01" @default.
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• W2048776273 title "Maastrichtian-Early Eocene litho-biostratigraphy and palægeography of the northern Gulf of Suez region, Egypt" @default.
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• W2048776273 doi "https://doi.org/10.1016/s0899-5362(01)90005-3" @default.
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