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

• Autores: Joaquín Rodríguez Vidal
• Localización: Geogaceta, ISSN 0213-683X, Nº. 11, 1991, págs. 85-86
• Idioma: español
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• Resumen

  • 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