Los corredores de fallas de Regua-Verin y VilariçaZonas detransferencia de la deformación intraplaca en la Península Ibérica

  1. R. Vegas 1
  2. G. de Vicente 1
  3. A. Muñoz Martín 1
  4. R. Palomino 1
  1. 1 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

Journal:
Geotemas (Madrid)

ISSN: 1576-5172

Year of publication: 2004

Issue Title: VI CONGRESO GEOLÓGICO DE ESPAÑA, ZARAGOZA, 12-15 JULIO, 2004

Issue: 6

Pages: 245-248

Type: Article

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Abstract

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

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