Evolución durante el Pérmico inferior de las fallas de la región de Pálmaces de Jadraque-Angón (borde SE del Sistema Central Español).

  1. Fernández Rodríguez, Carlos
Journal:
Geogaceta

ISSN: 0213-683X

Year of publication: 1990

Issue: 9

Pages: 50-52

Type: Article

More publications in: Geogaceta

Abstract

The Permian basins in the easternmost part of the Spanish Central System have been ascribed to the tectonic activity that took place during the late Hercynian. The Pálmaces half-graben is mainly due to a complex interaction between the fault system of Angón, largely affecting the hercynian metamorphic rocks, and the well-known Sarteneja Fault