Faciès sédimentaires et évolution paléogéographique de la Meseta marocaine au silurien

Silurian deposits of Moroccan Meseta domain were the subject of a sedimentological study. Facies analysis allows to recognize several sedimentary facies that are related to wave and storm influenced delta, tide dominated littoral and storm dominated shelf. The palaeogeographic evolution indicate that during the Silurian the sedimentation was controlled by distensive tectonic and glacio-eustatism.