Resumen de Los corredores de fallas de Regua-Verin y Vilariça: Zonas detransferencia de la deformación intraplaca en la Península Ibérica

Ramón Vegas Martínez, Gerardo de Vicente Muñoz, Alfonso Muñoz Martín, R. Palomino

• A substantial part of the intraplate deformation in the Iberian Foreland is transferred from theCantabro-Pyrenean border by means of two strike-slip deformation belts, the Regua-Verin andVilariça fault corridors. The Neogene and recent tectonic activity along these intraplate strike-slip belts is responsible for the onset of a geomorphic barrier between the Duero Basin and the Atlantic Margin