The Crotone Basin is the exposed part of a larger Neogene forearc basin developed in the
Ionian Sea in the frame of the SE-ward migration of the Calabrian Arc, which led to the …

Abstract The Apennines-Sicilian-Maghrebian fold-and-thrust belt originated from the
subduction of the Alpine Tethys and the later collision of drifted continental blocks against …

One of the most famous criminal investigations involved the use of forensic geology to assist
law enforcement agencies in the homicide case of the Italian honorable Aldo Moro …

The Cenozoic geological evolution of the Italian area is characterized by the formation of two
major mountain chains-the Alps to the north and the Apennines throughout the peninsula …

We report on new stratigraphic, palaeomagnetic and anisotropy of magnetic susceptibility
(AMS) results from the Amantea basin, located on‐shore along the Tyrrhenian coast of the …

ABSTRACT The Late Tertiary history of the Mediterranean region exemplifies processes of
ocean basin closure and continental collision, as determined from integrated land and …

Understanding the fracture influence on the P-wave velocity and physical–mechanical
properties of brittle rocks is very useful for geotechnical characterization in a number of …

The Tindari Fault System (southern Tyrrhenian Sea, Italy) is a regional zone of brittle
deformation located at the transition between ongoing contractional and extensional crustal …

Based on new CROP seismic data, integrated with other geological-geophysical
information, an evolutive lithospheric tectono-dynamic reconstruction of the Sicilian region …

Recently acquired swath bathymetry of the Marsili basin has offered an unprecedented
opportunity to study the processes of back arc ocean basin development in the Tyrrhenian …