The stratigraphic succesions of the Hafa el Banat and of the Fahs Dohor slices (Internal Hauz, Northern Rif) are described. Both slices show stratigraphic features and a tectonic position similar to that of the Uestia II Slice of southern sectors of the Hauz belt and, as well as this latter, they were a part of a subsiding continental margin during the Mesozoic
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