El control del Paleorrelieve durante la Transgresión Tortonienseun caso de estudio emn el Margen Pasivo de la Cuenca del Guadalquivir (Sur de España)

  1. Pendón Martín, José Gabriel
  2. Abad de los Santos, Manuel
  3. Cáceres Puro, Luis Miguel
  4. Rodríguez Vidal, Joaquín
  5. Ruiz Muñoz, Francisco
  6. Cantano Martín, Mercedes
Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 2005

Zenbakia: 38

Orrialdeak: 163-166

Mota: Artikulua

Beste argitalpen batzuk: Geogaceta

Laburpena

The Guadalquivir foreland basin has a complex temporal and spatial evolution which is shown in its facies architecture and its paleogeographical distribution during Tortonian. In this work we emphasize the control that exerted paleorelief on sedimentation (volume, location and type) and distribution of sedimentary environments in the Tortonian transgression. Four types of paleotopographic configurations have been differenced in the Paleozoic substrate, which are related to the different deposits deposited on the passive margin of the basin during sea-level fluctuation.