Evolución megasecuencial del relleno mio-plioceno del sector norte de la cuenca de Teruelinteracciones entre tectónica y sedimentación

  1. Lope Ezquerro 1
  2. Mª Aránzazu Luzón 1
  3. Carlos L. Liesa 1
  4. José 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: 2012

Títol de l'exemplar: VIII Congreso Geológico de España, Oviedo, 17-19 de julio, 2012.

Número: 13

Pàgines: 218-221

Tipus: Article

DIALNET GOOGLE SCHOLAR

Altres publicacions en: Geotemas (Madrid)

Resum

The Upper Miocene-Pliocene syn-tectonic sedimentary fill of the Teruel Basin in the northern sector is characterized by alluvial fans, mainly fed from the eastern and western margins of the basin, and by the development of palaeosols and shallow lakes in central basinal areas. The study of 21 stratigraphic sections, the correlation and specially the analysis of vertical changes in clast size and lithofacies allow to propose a sequential evolution in which six megasequences have been distinguished. Several lines evidences such us progressive unconformities, development of highly incised channels, abrupt changes of palaeocurrent directions or syn-sedimentary faulting affecting to the contemporary lacustrine facies suggest that extensional tectonics was an important factor controlling this evolution.

Fuente de los datos: Dialnet