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 …

The Tyrrhenian margin of central Italy has undergone Plio‐Quaternary extension,
developing NW‐SE normal faults and NE‐SW faults. The NE‐SW faults decrease in …

Po and Tevere rivers form two of the most important deltas of the whole Mediterranean area.
Detailed investigations have been carried out in the last decade beneath the present delta …

Zones of advanced argillic alteration with general low permeability (ie, lithocaps) are
common place in the shallow parts of porphyry and epithermal ore deposits and active …

The site of Ficoncella, in northern Latium (Italy), represents a great opportunity to investigate
the modalities of a short occupation in a fluvial context during Lower Palaeolithic. From the …

The presence of young, highly explosive volcanoes in the densely populated Roman area
(central Italy), makes the evaluation of the long-term volcanic hazard a crucial point. The …

During the Messinian Lago-Mare event, in the central Mediterranean area, compression-and
extension-related basins developed as a consequence of the post-Tortonian evolution of the …

In this work, we studied the hydrothermal agates from the Neogene–Quaternary volcanic
district of Allumiere-Tolfa, north-west of Rome (Latium, Italy) using a combination of micro …

The Ficoncella site in northern Latium (Italy) represents a unique opportunity to investigate
the modalities of a short occupation in an alluvial setting during the Lower Palaeolithic. The …

Stratigraphic and thermochronologic data are used to study the processes that shaped the
topography of the central Apennines of Italy. These are part of a major, active mountain belt …