Icnofacies del Neógeno superior de la Cuenca del Guadalquivir (área de Lepe-Ayamonte, Huelva, España)

  1. Muñiz, F
  2. Mayoral, E.
  3. Gámez Vitández, J.A.
Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 1998

Zenbakia: 24

Orrialdeak: 235-238

Mota: Artikulua

Beste argitalpen batzuk: Geogaceta

Garapen Iraunkorreko Helburuak

Laburpena

Thè marine arid lacustrine Upper Neogene sediments in the Southwestern sector of the Guadalquivir Basin (Lepe-Ayamonte area, Huelva, Spain), are basically characterized by four distinte ichnofacies: Cruziana, Skolithos, mixed Cruziana-Skolithos, Gnathichnus and GlóssifungiièS ichrìófacies. The stages of ichnofacial evolution provides several palaeòenviromentàl keys for these materials, as bathimetry, hydrodihamic energy, salinity and type of substratum