Stratigraphic position of the limestones and conglomerates around the Marimana granodiorite, Central Pyrenees, Spain

Abstract

Limestones bounding the Marimaña granodiorite, in the Central Pyrenees, which have until recently been correlated with the Cambro-Ordovician 'Calcaire métallifère" or "Calcaire de Bentaillou", have been proved to be of Devonian age. Conglomerates occurring at some distance below should be correlated with the main conglomerate level of the Cambro- Ordovician of the Pyrenees.