Causal processes of shallow and deep seismicity at Campi Flegrei caldera

Abstract The increase of ground deformation, seismicity, and gas emission is underlining a remarkable unrest at Campi Flegrei caldera. The direct involvement of magma has been invoked to explain the deformation and space/time changes of velocity anomalies at shallow crustal depths. Here, we show tha...

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Main Authors: Genny Giacomuzzi, Rossella Fonzetti, Aladino Govoni, Pasquale De Gori, Claudio Chiarabba
Format: Article
Language:English
Published: Nature Portfolio 2025-01-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02045-2
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author Genny Giacomuzzi
Rossella Fonzetti
Aladino Govoni
Pasquale De Gori
Claudio Chiarabba
author_facet Genny Giacomuzzi
Rossella Fonzetti
Aladino Govoni
Pasquale De Gori
Claudio Chiarabba
author_sort Genny Giacomuzzi
collection DOAJ
description Abstract The increase of ground deformation, seismicity, and gas emission is underlining a remarkable unrest at Campi Flegrei caldera. The direct involvement of magma has been invoked to explain the deformation and space/time changes of velocity anomalies at shallow crustal depths. Here, we show that detailed imaging of seismicity, improved by phase detection with machine-learning algorithms, and velocity models shed light on the active processes at the unresting caldera. Shallow seismicity tracks the fluids uprise, while deeper seismicity, aligning on an almost continuous ring on the top of the inferred magmatic source, indicates deep-seated-related, induced stresses. Our results offer valuable constraints to the challenging aspects of tracking upward migration of magma and magmatic fluids from depth, crucial in terms of hazard assessment and forecasting at Campi Flegrei.
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issn 2662-4435
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spelling doaj-art-c77718cb4d56479799af95febba5bec62025-02-02T12:44:11ZengNature PortfolioCommunications Earth & Environment2662-44352025-01-016111010.1038/s43247-025-02045-2Causal processes of shallow and deep seismicity at Campi Flegrei calderaGenny Giacomuzzi0Rossella Fonzetti1Aladino Govoni2Pasquale De Gori3Claudio Chiarabba4Istituto Nazionale di Geofisica e Vulcanologia (INGV)Istituto Nazionale di Geofisica e Vulcanologia (INGV)Istituto Nazionale di Geofisica e Vulcanologia (INGV)Istituto Nazionale di Geofisica e Vulcanologia (INGV)Istituto Nazionale di Geofisica e Vulcanologia (INGV)Abstract The increase of ground deformation, seismicity, and gas emission is underlining a remarkable unrest at Campi Flegrei caldera. The direct involvement of magma has been invoked to explain the deformation and space/time changes of velocity anomalies at shallow crustal depths. Here, we show that detailed imaging of seismicity, improved by phase detection with machine-learning algorithms, and velocity models shed light on the active processes at the unresting caldera. Shallow seismicity tracks the fluids uprise, while deeper seismicity, aligning on an almost continuous ring on the top of the inferred magmatic source, indicates deep-seated-related, induced stresses. Our results offer valuable constraints to the challenging aspects of tracking upward migration of magma and magmatic fluids from depth, crucial in terms of hazard assessment and forecasting at Campi Flegrei.https://doi.org/10.1038/s43247-025-02045-2
spellingShingle Genny Giacomuzzi
Rossella Fonzetti
Aladino Govoni
Pasquale De Gori
Claudio Chiarabba
Causal processes of shallow and deep seismicity at Campi Flegrei caldera
Communications Earth & Environment
title Causal processes of shallow and deep seismicity at Campi Flegrei caldera
title_full Causal processes of shallow and deep seismicity at Campi Flegrei caldera
title_fullStr Causal processes of shallow and deep seismicity at Campi Flegrei caldera
title_full_unstemmed Causal processes of shallow and deep seismicity at Campi Flegrei caldera
title_short Causal processes of shallow and deep seismicity at Campi Flegrei caldera
title_sort causal processes of shallow and deep seismicity at campi flegrei caldera
url https://doi.org/10.1038/s43247-025-02045-2
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