Los corredores de fallas de Regua-Verin y VilariçaZonas detransferencia de la deformación intraplaca en la Península Ibérica
- R. Vegas 1
- G. de Vicente 1
- A. Muñoz Martín 1
- R. Palomino 1
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1
Universidad Complutense de Madrid
info
ISSN: 1576-5172
Argitalpen urtea: 2004
Zenbakien izenburua: VI CONGRESO GEOLÓGICO DE ESPAÑA, ZARAGOZA, 12-15 JULIO, 2004
Zenbakia: 6
Orrialdeak: 245-248
Mota: Artikulua
Beste argitalpen batzuk: Geotemas (Madrid)
Laburpena
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