Mapa de asociaciones de facies neógenas del sector norte de la Cuenca de Teruel

  1. L. Ezquerro 1
  2. A. Luzón 1
  3. C.L. Liesa 1
  4. J.L. Simón 1
  1. 1 Universidad de Zaragoza
    info

    Universidad de Zaragoza

    Zaragoza, España

    ROR https://ror.org/012a91z28

Revista:
Geotemas (Madrid)

ISSN: 1576-5172

Any de publicació: 2016

Títol de l'exemplar: IX CONGRESO GEOLÓGICO DE ESPAÑA

Número: 16

Pàgines: 133-136

Tipus: Article

Altres publicacions en: Geotemas (Madrid)

Resum

The Upper Miocene-Quaternary sedimentary fill of the northern sector of the Teruel Basin is characterized by facies associations corresponding to alluvial fans, lakes and palustrine areas, as well as less common aeolian and deltaic environments. The map of facies associations corresponding to different sedimentary environments, and tectonic structures, reveals asymmetrical fill architecture. Alluvial fans were mainly sourced from the eastern (tectonically active) and western (passive) basin margins, connected downstream with shallow carbonate or evaporite lakes located in central basinal areas but closer to the active margin. The accommodation space created by synsedimentary intrabasinal faults enabled preservation of aeolian and deltaic associations, not very common in this type of basins.