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 …

We present a new data set of Moho depth estimates for peninsular Italy, obtained from
receiver functions analysis and a grid search approach. Teleseismic records from 174 …

This paper presents a velocity model of the Italian (central Mediterranean) lithosphere in
unprecedented detail. The model is derived by inverting a set of 166,000 Pg and Pn seismic …

Active deformation in southern Italy is accommodated by a distributed number of faults with
low–moderate slip rates. Outcropping extensional faults and mostly blind transcurrent faults …

A revised gravity anomaly map, generated from the EIGEN6C4 high resolution global gravity
model, has been utilized for understanding structure and tectonics over the 85° E Ridge and …

The entanglement between active tectonics and karst systems is well-known in the literature.
Karst systems are sound recorders of continental deformation in terms of brittle structures …

Understanding fault behavior in carbonates is critical because they represent loci of
earthquake nucleation. Models of fault-slip mode generally assume:(1) seismic sliding and …

The lithosphere of Italy is exposed to a number of different short‐term strain transients,
including but not limited to landslides, postseismic relaxation, and volcanic …

This study provides a lithospheric-scale model along the Ionian Subduction zone in
Southern Italy, contributing to the seismotectonic investigation of a region which is affected …

The crustal structure of central Apennines (Italy) is still poorly defined, leaving uncertainties
on the tectonic style (thin or thick-skinned) responsible for the development of the thrust-and …