Source and dynamics of a volcanic caldera unrest: Campi Flegrei, 1983–84

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

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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.
Original languageEnglish
Article number8099
Pages (from-to)1-13
Number of pages13
JournalScientific Reports
Volume7
DOIs
Publication statusPublished - 14 Aug 2017

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caldera
volcanic eruption
fluid injection
fluid
seismic source
rupture
dike
emplacement
uplift
anomaly
earthquake
temperature

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De Siena, L., Chiodini, G., Vilardo, G., Del Pezzo, E., Castellano, M., Colombelli, S., ... Ventura, G. (2017). Source and dynamics of a volcanic caldera unrest: Campi Flegrei, 1983–84. Scientific Reports, 7, 1-13. [8099]. https://doi.org/10.1038/s41598-017-08192-7

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.

In: Scientific Reports, Vol. 7, 8099, 14.08.2017, p. 1-13.

Research output: Contribution to journalArticle

De Siena, L, Chiodini, G, Vilardo, G, Del Pezzo, E, Castellano, M, Colombelli, S, Tisato, N & Ventura, G 2017, 'Source and dynamics of a volcanic caldera unrest: Campi Flegrei, 1983–84', Scientific Reports, vol. 7, 8099, pp. 1-13. https://doi.org/10.1038/s41598-017-08192-7
De Siena L, Chiodini G, Vilardo G, Del Pezzo E, Castellano M, Colombelli S et al. Source and dynamics of a volcanic caldera unrest: Campi Flegrei, 1983–84. Scientific Reports. 2017 Aug 14;7:1-13. 8099. https://doi.org/10.1038/s41598-017-08192-7
De Siena, Luca ; Chiodini, Giovanni ; Vilardo, Giuseppe ; Del Pezzo, Edoardo ; Castellano, Mario ; Colombelli, Simona ; Tisato, Nicola ; Ventura, Guido. / Source and dynamics of a volcanic caldera unrest : Campi Flegrei, 1983–84. In: Scientific Reports. 2017 ; Vol. 7. pp. 1-13.
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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.",
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N2 - 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.

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