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 …

Plagioclase is the most common phenocryst in all Etnean magmatic suites (~ 50% in
volume), as well as in most lavas erupted worldwide. Its stability field is strongly dependent …

The Apenninic foreland shows two distinct structural signatures comparing the central
Adriatic Sea and the Puglia region. During the Pliocene‐Pleistocene the central Adriatic …

We examine the tectonic geomorphology of La Sila, Calabria, southern Italy, a high-standing
(1500 m) plateau surrounded by crustal extension, with map, DEM, and field data. These …

New seismic reflection profiles of the Italian deep crust project CROP provide new insights
on the structure of the Ionian sea. In spite of the Apennines and Hellenides Neogene …

The Etna volcano is located in an apparently anomalous position on the hinge zone of the
Apennines subduction and its Na‐alkaline geochemistry does not favour a magma source …

A combination of published and new radiometric dates on uplifted Holocene fossil beaches
from northeastern Sicily and southern Calabria (southern Italy) is compared with the altitude …

The available geological, geophysical and seismological data of the Tyrrhenian-Apennines
system are briefly reviewed and synthesized in a number of sketch maps. Integrating and …

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 …

ABSTRACT The Apennines comprise a Neogen—Quaternary accretionary prism that shows
several anomalies with respect to classic alpine‐type mountain belts, namely (i) low …