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