Superficies de erosión neógenas y neotectónica en el borde NE de la Cuenca del Duero

  1. F. J. Gracia Prieto 1
  2. F. Nozal Martín 1
  3. P. F. Wouters de Vries 2
  1. 1 ITGE
  2. 2 EPTISA
Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 1989

Zenbakia: 7

Orrialdeak: 38-40

Mota: Artikulua

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Beste argitalpen batzuk: Geogaceta

Laburpena

In the northeastern border of the Duero Bassin two erosiona/ surfaces formed on mesozoic materials are distinguished. The oldest one, actually limited to isolated summits, is probably of middle-Miocene age. The youngest one is linked to the colmation surface of the Duero Bassin ("Páramos" limestones) and therefore of Turolian-Pliocene age. Tectonic deformations with a NW-SE strike affecting this surface in the southeastern border of the Cantabrian Chain are deduced

Datuen iturria: Dialnet