Evolución sedimentaria reciente de las Tablas de Daimiel (Ciudad Real).

  1. García-Hidalgo Pallarés, José F.
  2. Temiño Vela, Javier
  3. Bustamante Gutiérrez, Irene de
  4. Segura Redondo, Manuel
Revista:
Geogaceta

ISSN: 0213-683X

Año de publicación: 1995

Número: 18

Páginas: 87-90

Tipo: Artículo

Otras publicaciones en: Geogaceta

Resumen

Two sedim entary events have been distinguished in the recent evolu tio n o f the present Tablas de Daimiel National Park. The older one is characterized by the presence of siliceous sands and silts, and mudstones; the former contain fluviatile Pelecypods and Gastropods, being interpreted as channellized deposits corresponding to the last stage of the Holocene fluvial inclssion. The mudstones sometimes contain a high content in carbonate and/or organic matter, root debris and gastropods are also common; this sediments are interpretad as deposited in a muddy alluvial plain. Finally, the younger event is dominated by peat and lime mud sedimentation in a lacustrine-palustrlne system crossed by some fluvial channels