The central-western Mediterranean area is a key region for understanding the complex
interaction between igneous activity and tectonics. In this review, the specific geochemical …

We present here a comprehensive petrological investigation of products emitted during the
December 2020–February 2022 paroxysmal sequence occurred at the South East Crater of …

We present a geodynamic reconstruction of the Central–Western Mediterranean and
neighboring areas during the last 50Myr, including magmatological and tectonic …

Crystals formed prior to a volcanic event can provide evidence of processes leading to and
timing of eruptions. Clinopyroxene is common in basaltic to intermediate volcanoes …

Deciphering the evolution of the internal dynamics of magmatic plumbing systems and
identifying the key parameters that drive such dynamics are major goals of modern …

A correct description and quantification of the geochemical behaviour of REE+ Y (rare earth
elements and Y) and HFSE (high field strength elements) is a key requirement for modeling …

A systematic study of textural and compositional zoning (An% and FeO variation) in
plagioclase phenocrysts of historic (pre-1971) and recent (post-1971) lavas at Mount Etna …

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 …

Magma ascent velocities, v (d H/dt; where H is depth and t is time), can be determined from
decompression rates (d P/dt), and rates of cooling (d T/dt):, where ρ is magma density, P is …

Abstract Large-scale Upper Eocene plutons in the Western Alborz–Azarbaijan orogenic belt
mostly show calc-alkaline and I-type geochemical features contrasted by the Tarom complex …