Any effective volcanic risk mitigation strategy requires a scientific assessment of the future
evolution of a volcanic system and its eruptive behavior. Some consider the onus should be …

The dynamic behavior of magmatic hydrothermal systems entails coupled and nonlinear
multiphase flow, heat and solute transport, and deformation in highly heterogeneous media …

Abstract The central Campanian Plain is dominated by the structural depression of Acerra
whose origin is tectonic, but may have been enlarged and further depressed after the …

We model the location, geometry and density of the source of the recent geological unrest at
Campi Flegrei caldera (Italy) by inverting levelling, trilateration and gravity measurements …

The Campi Flegrei caldera is a complex structure in which resurgence occurs through a
simple shearing mechanism. The most uplifted block inside the caldera is the La Starza …

The Campi Flegrei (CF) Caldera experiences dramatic ground deformations unsurpassed
anywhere in the world. The source responsible for this phenomenon is still debated. With the …

We have analyzed a multiparametric data set of seismological, geodetic and geochemical
data recorded at Campi Flegrei caldera since 1982. We focus here on the period 1989 …

Satellite radar interferometry of Campi Flegrei caldera, Italy, reveals a pattern of subsidence
during the period 1993–1998. Interferograms spanning the first half of the observation …

We develop a numerical algorithm for simulation of wave propagation in linear
nonisothermal poroelastic media, based on Biot theory and a generalized Fourier law of …

Phlegrean Fields is an active and densely populated caldera near Naples (Italy). Two major
unrest episodes characterized its recent history, each leading to remarkable ground uplift …