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

• Autores: Carlos Fernández Rodríguez
• Localización: Geogaceta, ISSN 0213-683X, Nº. 9, 1990, págs. 50-52
• Idioma: español
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• Resumen

  • 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