Abstract
Ten detailed sections have been logged and studied from the "Infra-Cenomanian'' to the Cenomanian-Turonian deposits in the Errachidia-Boudnib-Erfoud Basin between Tazzouguerte and Anounizme(SE Morocco). They show variations in their lithology and microfacies that reflect changes in the depositional environment from the base to the top of the sedimentary record. Indeed, depositional setting grades from a fluvial environment marked by sandstone deposits of the Ifezouane Formation to an alluvial plain and coastal lagoon environment comprising an alternation of red clay, gypsum, and green marl beds of the Aoufous Formation and, finally, towards shallow to moderately deep marine environments with the deposition of the carbonates of the Akrabou Formation. Correlations between the studied sections show variations in the thickness of strata throughout the basin. The variations recorded in the so-called "Infra-Cenomanian" series may be related to the structuration of the basement. The Cenomanian-Turonian carbonate platform shows deeper marine and thicker sediments towards the east, while it thins towards the west until its disappearance in Anounizme. This reflects the global Cenomanian-Turonian transgression in the Errachidia-Boudnib-Erfoud Basin from the eastern Tethyan realm towards the west. The regional correlation of the Errachidia-Boudnib-Erfoud Basin with the Ouarzazate and Agadir basins shows an eastward thinning of the Cenomanian-Turonian marine deposits of Agadir. This suggests the presence of a paleorelief at the Anounizme locality. This could be the boundary between the Errachidia-Boudnib-Erfoud Basin, with Tethyan influence, to the east and those of Ouarzazate and Agadir, with Atlantic affinity, to the west.