With the emergence of portable broadband seismic instrumentation, availability of digital
networks with wide dynamic range, and development of new powerful analysis techniques …

Since the 1919 foundation of the International Association of Volcanology and Chemistry of
the Earth's Interior (IAVCEI), the fields of volcano seismology and acoustics have seen …

In the past two decades, the central portion of Campi Flegrei caldera has experienced
ground uplift up to 15 mm/month, with an increase of rate, magnitude and extent of the …

Abstract Changes in seismicity with time and location are diagnostic signals for
understanding the dynamics of volcanic unrest. We used these signals at the Campi Flegrei …

This paper describes an approach to analyze ground deformation data collected by InSAR
(Interferometric Synthetic Aperture Radar) imaging the volcano feeding system (VFS) …

Fluids supplied by stored magma at depth are causal factors of volcanic unrest, as they can
cause pressurization/heating of hydrothermal systems. However, evidence for links between …

During the reawaking of a volcano, magmas migrating through the shallow crust have to
pass through hydrothermal fluids and rocks. The resulting magma–hydrothermal interactions …

Campi Flegrei caldera is an Italian high-risk volcano experiencing a progressively more
intense long-term uplift, accompanied by increasing seismicity and geochemical emissions …

An accelerating process of ground deformation that began 10 years ago is currently affecting
the Campi Flegrei caldera. The deformation pattern is here explained with the overlap** of …

One of the most effective approaches to identifying possible precursors of eruptions is the
analysis of seismicity patterns recorded at volcanoes. Accurate locations of the seismicity …