Conodontos del Paleozoico Gomáride (Rif Septentrional, Marruecos). Nota preliminar

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A moderately tectonised stratigraphic section pertaining to the Ghomarides, NW of Tetuan, Morocco, is formed by platy limestones and slates, and contains interesting associations of conodonts of uppermost Silurian to upper Devonian age
Una sección estratigráfica moderadamente tectonizada relacionada con Gomáride, NO de Tetuán, Marruecos, se forma de caliza laminada y pizarra, y contienen interesantes asociaciones de conodontos del Alto Silúrico al Alto Devónico.

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