Las superficies de erosión neógenas en el sector central de la Cordillera Ibérica

  1. F.J. Gracia Prieto 1
  2. M. Gutiérrez Elorza 12
  3. B. Leránoz Istúriz 12
  1. 1 Instituto de Estudios Turolenses
    info

    Instituto de Estudios Turolenses

    Teruel, España

  2. 2 Universidad de Zaragoza
    info

    Universidad de Zaragoza

    Zaragoza, España

    ROR https://ror.org/012a91z28

Journal:
Revista de la Sociedad Geológica de España

ISSN: 0214-2708

Year of publication: 1988

Volume: 1

Issue: 1-2

Pages: 135-142

Type: Article

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Abstract

In the Central Iberian Chain four planation surfaces are recognized whose respective ages are: lower-middle Miocene, Turolian-Ruscinian, middle Pliocene and middle Villafranchian. These ages are stablished through their lateral relations with correlative deposits corresponding to sedimentary accumulations of neogene tectonic depressions and their dating. After the elaboration of each surface, tectonic movements have deformed these planes. It is deduced that the neogene planation surfaces of this area are old pediplanes elaborated in arid environments.

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