We present the results of a gravity investigation conducted in the Norcia Intermountain Basin (central Italy) in order to obtain a subsurface picture of its structural setting and to estimate the thickness of the Quaternary infill sediments. Our survey resulted in 210 measurements, placed evenly in the whole Norcia Plain. We produced gravity anomaly maps that show the Quaternary thickness spatial distribution within the basin and identify buried faults affecting the bedrock in the northern basin sector. 2.5D models along close spaced profiles were used to construct a 3D density model and a map of the bedrock top surface elevation. Our results suggest that the northern sector of the Norcia Intermountain Basin has been affected by a s...
In the axial zone of the Umbria-Marche Apennines, several fault-bounded intermontane basins (i.e., C...
Our research is aimed at estimating the vertical deformation affecting late Quaternary units accumul...
The Colli Albani is a quiescent Volcanic District, located almost 20 km southeast of Rome (Italy). ...
gravity study was carried out to identify the geological and structural features of the Middle Atern...
n this study, detailed gravity survey and microtremor observations were made to map and model the th...
Ground-shaking phenomena in intermontane basins emplaced in seismically active areas are strongly af...
About the thesis. This thesis describes the results of a research approach that integrated a detaile...
Sediments infilling in intermontane basins in areas with high seismic activity can strongly affect g...
Systematic analyses of the tectonic structures of the Plio-Pleistocene units and MesoCenozoic deposi...
We investigated the structure of the Volturara Irpina Plain, a small intra-mountain basin in souther...
The Pian Grande di Castelluccio (PGC) basin is the main Quaternary depocenter of the Mt. Vettore‐Mt....
The aim of the study is to identify the active structures in the Paganica and Mt. Vettore-Mt. Bove a...
Intermontane basins characterize many orogenic chains, where they are originated either by crustal s...
The Middle Valle Umbra (central Italy) is a NW-SE 20 km long and 10 km wide Quaternary extensional b...
The Quaternary basins of the axial zone of central Apennines represent a key areas for a better unde...
In the axial zone of the Umbria-Marche Apennines, several fault-bounded intermontane basins (i.e., C...
Our research is aimed at estimating the vertical deformation affecting late Quaternary units accumul...
The Colli Albani is a quiescent Volcanic District, located almost 20 km southeast of Rome (Italy). ...
gravity study was carried out to identify the geological and structural features of the Middle Atern...
n this study, detailed gravity survey and microtremor observations were made to map and model the th...
Ground-shaking phenomena in intermontane basins emplaced in seismically active areas are strongly af...
About the thesis. This thesis describes the results of a research approach that integrated a detaile...
Sediments infilling in intermontane basins in areas with high seismic activity can strongly affect g...
Systematic analyses of the tectonic structures of the Plio-Pleistocene units and MesoCenozoic deposi...
We investigated the structure of the Volturara Irpina Plain, a small intra-mountain basin in souther...
The Pian Grande di Castelluccio (PGC) basin is the main Quaternary depocenter of the Mt. Vettore‐Mt....
The aim of the study is to identify the active structures in the Paganica and Mt. Vettore-Mt. Bove a...
Intermontane basins characterize many orogenic chains, where they are originated either by crustal s...
The Middle Valle Umbra (central Italy) is a NW-SE 20 km long and 10 km wide Quaternary extensional b...
The Quaternary basins of the axial zone of central Apennines represent a key areas for a better unde...
In the axial zone of the Umbria-Marche Apennines, several fault-bounded intermontane basins (i.e., C...
Our research is aimed at estimating the vertical deformation affecting late Quaternary units accumul...
The Colli Albani is a quiescent Volcanic District, located almost 20 km southeast of Rome (Italy). ...