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

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Resumen

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

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