Vegas Martínez, RamónVicente Muñoz, Gerardo DeMuñoz Martín, AlfonsoPalomino, R.2023-06-202023-06-2020041576-5172https://hdl.handle.net/20.500.14352/52547A 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.spajournal articlehttp://www.sociedadgeologica.es/publicaciones_geotemas.htmlopen access551.24Intraplate strike-slip beltsNW Iberian PeninsulaGeodinámica2507 Geofísica