Intermontane basins characterize many orogenic chains, where they are originated either by crustal stretching or gravitational collapse of the axial zones of the chain. Extensional and/or transtensional mechanisms generate structures with geometries controlled by fault-bounded depressed areas, which in some cases are seismogenetic. The western sector of the Northern Apennines in Central Italy is characterized by several intermontane basins filled by continental Plio-Pleistocene sediments. At present, a few of these basins are depressed endorheic areas, whereas most of them have been captured by river upstream erosion. The morphotectonic characterization at both regional and local scale of these structures is crucial considering the associat...
The Quaternary basins of the axial zone of central Apennines represent a key areas for a better unde...
Several mountain arcs formed in the Mediterranean area during the Alpine orogeny, among them the Nor...
The southern Apennines is a fold-and-thrust belt, which was formed during the late Cenozoic converge...
Intermontane basins characterize many orogenic chains, where they are originated either by crustal s...
In the axial zone of the Umbria-Marche Apennines, several fault-bounded intermontane basins (i.e., C...
This research aims at highlighting the small- and medium-scale morphotectonic framework of an interm...
In the axial zone of the Umbria-Marche Apennines, several fault-bounded intermontane basins (i.e., C...
The Gubbio Basin is a 22 km long, 4 km wide depression located within the North-Central Apennines fo...
The Agri Valley is a NW-SE oriented intermontane basin located in the axial zone of the Southern Ape...
The opening kinematics of several Pliocene to Quaternary tectonically controlled continental basins ...
In active tectonic regions, topography results from the interaction between tectonics and surface pr...
Normal faults within orogenic belts can be pre-, syn- or post-orogenic features. We studied the Gubb...
Topography of the Apennines chain resulted from the combined action of tectonic displacements (relat...
The Umbro-Marchean Apennines form an arcuate NW–SE fold-and-thrust belt of NE convexity. The orogen ...
We present a geomorphological analysis of the recent extensional tectonics of a Quaternary continent...
The Quaternary basins of the axial zone of central Apennines represent a key areas for a better unde...
Several mountain arcs formed in the Mediterranean area during the Alpine orogeny, among them the Nor...
The southern Apennines is a fold-and-thrust belt, which was formed during the late Cenozoic converge...
Intermontane basins characterize many orogenic chains, where they are originated either by crustal s...
In the axial zone of the Umbria-Marche Apennines, several fault-bounded intermontane basins (i.e., C...
This research aims at highlighting the small- and medium-scale morphotectonic framework of an interm...
In the axial zone of the Umbria-Marche Apennines, several fault-bounded intermontane basins (i.e., C...
The Gubbio Basin is a 22 km long, 4 km wide depression located within the North-Central Apennines fo...
The Agri Valley is a NW-SE oriented intermontane basin located in the axial zone of the Southern Ape...
The opening kinematics of several Pliocene to Quaternary tectonically controlled continental basins ...
In active tectonic regions, topography results from the interaction between tectonics and surface pr...
Normal faults within orogenic belts can be pre-, syn- or post-orogenic features. We studied the Gubb...
Topography of the Apennines chain resulted from the combined action of tectonic displacements (relat...
The Umbro-Marchean Apennines form an arcuate NW–SE fold-and-thrust belt of NE convexity. The orogen ...
We present a geomorphological analysis of the recent extensional tectonics of a Quaternary continent...
The Quaternary basins of the axial zone of central Apennines represent a key areas for a better unde...
Several mountain arcs formed in the Mediterranean area during the Alpine orogeny, among them the Nor...
The southern Apennines is a fold-and-thrust belt, which was formed during the late Cenozoic converge...