Abstract:The Marmoucha syncline is located in the eastern part of the Middle Atlas. In this syncline, the “Gypsum marls ” (Bathonian-? Callovian) are covered by red detrital deposits which outcrop in Aït Bazza locality. The upper limit of these detrital deposits is below the transgressional unconformity of the Albian? - Cenomanian marine series. The present work introduces a synthesis of stratigraphical, sedimentological and micropalaeontological studies, which has led to new dating and to the identification of differen… Show more
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