Successions caracteristiques et niveaux reperes dans le Paleozoique de la region de Carcassonne a Saint-Pons (Montagne-Noire, Aude, Herault)

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Abstract
The lower Cambrian deposits of the Carcassonne-Saint-Pons region, France, are characterized by similar sequences of lithologic units at widely spaced localities and by lithofacies marker horizons which are persistent over wide areas. Lithofacies analyses of other parts of the Paleozoic section in the region lead to the conclusion that the region constitutes a homogeneous tectonic unit.

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