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Le Cretace de la plate-forme preafricaine du Maroc est classiquement subdivise en trois formations: Ifezouane (Albien?), Aoufous (Albo-Cenomanien) et Akrabou (Cenomano-Turonien). Les depots temoignent d'un environnement fluviatile ou deltaique a l'Albien?, evoluant vers une lagune cotiere ou sebkha paralique a l'Albo-Cenomanien moyen et superieur, et de plate-forme plutot ouverte au Cenomanien superieur-Turonien...
Set the date range to filter the displayed results. You can set a starting date, ending date or both. You can enter the dates manually or choose them from the calendar.