Volcanic stratigraphy is a fundamental component of geological map** in volcanic areas
as it yields the basic criteria and essential data for identifying the spatial and temporal …

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 …

Italian Plio-Quaternary magmatism exhibits a very wide petrological, geochemical and
radiogenic-isotope variability, which makes magma genesis and geodynamic significance …

The new geological map of Etna volcano at 1: 50,000 scale represents a significant progress
in the geological studies of this volcano over the last 30 years, coming after Waltershausen's …

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 …

Il Foglio 641 “Augusta” della Carta Geologica d'Italia in scala 1: 50.000 è stato realizzato
nell'ambito del Progetto CARG (Legge 226/99) tramite Convenzione tra APAT (ora …

An updated geological evolution model is presented for the composite basaltic stratovolcano
of Mount Etna. It was developed on the basis of the stratigraphic setting proposed in the new …

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 …

This paper uses a coupled morphometric and stratigraphic analysis of several tens of
parasitic pyroclastic cones of the SE flank of Mt. Etna volcano, Italy, to explain the structure of …

By using new high-resolution (2 m) digital elevation model derived from the 2005 LiDAR
survey of Mt. Etna volcano (Italy), our study measured the classical morphometrical …