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  • jebel qatrani formation: Topics by Science. gov
    On the southern margin of the Tethys, Early Cretaceous sediments cover most of the Central Tunisia As a result of a Middle Cretaceous sub-aerial exposure, the Late Barremian -Early Albian interval is mainly characterized by a major stratigraphic gap (hiatus) However in the Sidi Bouzid area a continental succession has been deposited called ;Kebar Formation; The Kebar Formation was


















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