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Article ; Online: Source and dynamics of a volcanic caldera unrest: Campi Flegrei, 1983-84.

De Siena, Luca / Chiodini, Giovanni / Vilardo, Giuseppe / Del Pezzo, Edoardo / Castellano, Mario / Colombelli, Simona / Tisato, Nicola / Ventura, Guido

Scientific reports

2017  Volume 7, Issue 1, Page(s) 8099

Abstract: Despite their importance for eruption forecasting the causes of seismic rupture processes during caldera unrest are still poorly reconstructed from seismic images. Seismic source locations and waveform attenuation analyses of earthquakes in the Campi ... ...

Abstract Despite their importance for eruption forecasting the causes of seismic rupture processes during caldera unrest are still poorly reconstructed from seismic images. Seismic source locations and waveform attenuation analyses of earthquakes in the Campi Flegrei area (Southern Italy) during the 1983-1984 unrest have revealed a 4-4.5 km deep NW-SE striking aseismic zone of high attenuation offshore Pozzuoli. The lateral features and the principal axis of the attenuation anomaly correspond to the main source of ground uplift during the unrest. Seismic swarms correlate in space and time with fluid injections from a deep hot source, inferred to represent geochemical and temperature variations at Solfatara. These swarms struck a high-attenuation 3-4 km deep reservoir of supercritical fluids under Pozzuoli and migrated towards a shallower aseismic deformation source under Solfatara. The reservoir became aseismic for two months just after the main seismic swarm (April 1, 1984) due to a SE-to-NW directed input from the high-attenuation domain, possibly a dyke emplacement. The unrest ended after fluids migrated from Pozzuoli to the location of the last caldera eruption (Mt. Nuovo, 1538 AD). The results show that the high attenuation domain controls the largest monitored seismic, deformation, and geochemical unrest at the caldera.
Language English
Publishing date 2017-08-14
Publishing country England
Document type Journal Article ; Research Support, Non-U.S. Gov't
ZDB-ID 2615211-3
ISSN 2045-2322 ; 2045-2322
ISSN (online) 2045-2322
ISSN 2045-2322
DOI 10.1038/s41598-017-08192-7
Database MEDical Literature Analysis and Retrieval System OnLINE

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