Geomorphologic evolution and neotectonics of the Sulmona intramontane basin (Abruzzi Apennine, Central Italy)
Tectonic geomorphology
been formed during Middle-Upper Pliocene, after the end of the main tectogenetic phases of the Apennine chain. In order to outline the geomorphologic evolution of the area, detailed geological and geomorphologic investigations have been carried out