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

ISSN: 0213-683X

Year of publication: 1990

Issue: 9

Pages: 50-52

Type: Article

More publications in: Geogaceta


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