Resumen de Conodontos del Paleozoico Gomáride (Rif Septentrional, Marruecos): Nota preliminar

M.R. Rodríguez Cañero, Ali Maate, Agustín Martín Algarra

• A moderately tectonised stratigraphic section pertaining to the Ghomarides, NW of Tetuan, M orocco, is formed by platy limestones and slates, and contains interesting associations of conodonts of uppermost Silurian to upper Devonian age.