Publication: Los corredores de fallas de Regua-Verin y Vilariça: Zonas de
transferencia de la deformación intraplaca en la Península Ibérica
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Publication Date
2004
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Sociedad Geológica de España.
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Abstract
A substantial part of the intraplate deformation in the Iberian Foreland is transferred from the Cantabro-Pyrenean border by means of two strike-slip deformation belts, the Regua-Verin and Vilariça fault corridors. The Neogene and recent tectonic activity along these intraplate strikeslip belts is responsible for the onset of a geomorphic barrier between the Duero Basin and the Atlantic Margin.