Understanding the structure and development of calderas is crucial for predicting their
behaviour during periods of unrest and to plan geothermal and ore exploitation. Geological …

Diverse subsidence geometries and collapse processes for ash-flow calderas are inferred to
reflect varying sizes, roof geometries, and depths of the source magma chambers, in …

A compilation of the Marine Isotope Substage (MIS) 5.5 high stand (∼ 125Ka) sites
spanning the coastline of Italy allows a picture of the vertical displacement pattern affecting …

Scaled experiments have been carried out on caldera collapse mechanisms, using silicone
as analogue magma and dry sand as analogue rock. Experiments were carried out in two …

Physical properties of some weathered/altered volcanic rocks and their variation with the
degree of alteration are described in detail. A series of tests was performed to identify and …

A clear and detailed understanding of gas migration mechanisms from depth to ground
surface is fundamental to choose the best locations for CO2 geological storage sites, to …

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 …

Structures at calderas may form as a result of precursory tumescence, subsidence due
withdrawal of magmatic support, resurgence, and regional tectonism. Structural reactivation …

The peninsular and insular Italy are punctuated by Quaternary volcanoes and their rocks
constitute an important aliquot of the Italian Quaternary sedimentary successions. Also away …

Abstract Vulsini Volcanic district in Northern Latium (Central Italy) is characterized by high
natural radiation background resulting from the high concentrations of uranium, thorium and …