Aproximación al paleorelieve Tortoniense del margen ibérico meridional (depresión occidental del Guadalquivir).

  1. Rodríguez Vidal, Joaquín
Revue:
Geogaceta

ISSN: 0213-683X

Année de publication: 1991

Número: 11

Pages: 85-86

Type: Article

D'autres publications dans: Geogaceta

Résumé

During the Middle•Upper Tortonian, the southern edge of the Iberian Massif was affected by a marine transgression. So the planated topography (pre-Tertiary erosion surface). tilted to the south (1% - 3%), was cutting by N-S fluvial pattern. The uneven relief conditioned the local sedimentation with little deltas, beaches and others related environments, as well as cliffs and marine benches