In understanding the evolution of siliciclastic systems, Late Quaternary analogs may enable
reliable predictive models of facies-tract architecture. The Po Plain–Adriatic Sea system …

To properly frame the seismic data acquired with the CROP Project, the geophysical and
geological characteristics of the Italian region and a review of magmatism are briefly …

The large scale structure of the earth is caused by geodynamic processes which are
explained using energetic, kinematic and dynamic descriptions. While" geodynamic …

The geometry, kinematics and rates of active extension in Lazio–Abruzzo, Italian Apennines,
have been measured in order to gain a better understanding of the spatial and temporal …

The Meso-Cenozoic stratigraphical successions that crop out in central Italy are part of the
sedimentary wedge developed on the southern Neotethyan passive margin. On the previous …

The Emilia‐Romagna coastland south of the Po River delta, Italy, has experienced a
dramatic land settlement mainly due to the large groundwater withdrawal related to the local …

Deltas are highly dynamic coastal systems that over the last few decades have generally
experienced a substantial area loss caused by trap** of river sediments in upland …

Over the last century the Ravenna area has been affected by a widespread land subsidence
process of both natural and anthropogenic origin which has become a matter of increasingly …

The Po Plain is a low-relief area characterised by active shortening accommodated by blind
thrust faulting. In this almost flat region depositional rates are similar to tectonic rates and …

The Venetian–Friulian Plain is the eastern part of the foreland basin of the Southern Alps
and is characterized by the presence of alluvial megafans. Existence of these large …