Delineation and Fine‐Scale Structure of Fault Zones Activated During the 2014–2024 Unrest at the Campi Flegrei Caldera (Southern Italy) From High‐Precision Earthquake Locations

Abstract 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 seismicity. In this work, we perform multi‐scale precise earthquake relocation of the 2014–2024 seismicity, mapping in...

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Main Authors: Francesco Scotto di Uccio, Anthony Lomax, Jacopo Natale, Titouan Muzellec, Gaetano Festa, Sahar Nazeri, Vincenzo Convertito, Antonella Bobbio, Claudio Strumia, Aldo Zollo
Format: Article
Language:English
Published: Wiley 2024-06-01
Series:Geophysical Research Letters
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Online Access:https://doi.org/10.1029/2023GL107680
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author Francesco Scotto di Uccio
Anthony Lomax
Jacopo Natale
Titouan Muzellec
Gaetano Festa
Sahar Nazeri
Vincenzo Convertito
Antonella Bobbio
Claudio Strumia
Aldo Zollo
author_facet Francesco Scotto di Uccio
Anthony Lomax
Jacopo Natale
Titouan Muzellec
Gaetano Festa
Sahar Nazeri
Vincenzo Convertito
Antonella Bobbio
Claudio Strumia
Aldo Zollo
author_sort Francesco Scotto di Uccio
collection DOAJ
description Abstract 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 seismicity. In this work, we perform multi‐scale precise earthquake relocation of the 2014–2024 seismicity, mapping in detail activated fault zones. We relate the geometry, extent, and depth of these zones with up‐to‐date structural reconstructions of the caldera. The current seismicity is mainly driven by ground‐uplift‐induced stress concentration on pre‐existing, weaker fault zones, some of which identified for the first time. These structures are not only related to the inner caldera and dome resurgence but also to volcano‐tectonic events of the last 10 ka. The extent of imaged fault segments suggests they can accommodate ruptures up to a moment magnitude 5.1, significantly increasing seismic hazard in the area.
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spelling doaj-art-e70ba879e43f4f43a2d72583e919c6982025-08-20T01:52:06ZengWileyGeophysical Research Letters0094-82761944-80072024-06-015112n/an/a10.1029/2023GL107680Delineation and Fine‐Scale Structure of Fault Zones Activated During the 2014–2024 Unrest at the Campi Flegrei Caldera (Southern Italy) From High‐Precision Earthquake LocationsFrancesco Scotto di Uccio0Anthony Lomax1Jacopo Natale2Titouan Muzellec3Gaetano Festa4Sahar Nazeri5Vincenzo Convertito6Antonella Bobbio7Claudio Strumia8Aldo Zollo9Department of Physics Ettore Pancini Università di Napoli Federico II Napoli ItalyALomax Scientific Mouans‐Sartoux FranceDepartment of Earth and Geoenvironmental Sciences Università di Bari “Aldo Moro” Bari ItalyDepartment of Physics Ettore Pancini Università di Napoli Federico II Napoli ItalyDepartment of Physics Ettore Pancini Università di Napoli Federico II Napoli ItalyDepartment of Physics Ettore Pancini Università di Napoli Federico II Napoli ItalyIstituto Nazionale di Geofisica e Vulcanologia Osservatorio Vesuviano Napoli ItalyIstituto Nazionale di Geofisica e Vulcanologia Osservatorio Vesuviano Napoli ItalyDepartment of Physics Ettore Pancini Università di Napoli Federico II Napoli ItalyDepartment of Physics Ettore Pancini Università di Napoli Federico II Napoli ItalyAbstract 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 seismicity. In this work, we perform multi‐scale precise earthquake relocation of the 2014–2024 seismicity, mapping in detail activated fault zones. We relate the geometry, extent, and depth of these zones with up‐to‐date structural reconstructions of the caldera. The current seismicity is mainly driven by ground‐uplift‐induced stress concentration on pre‐existing, weaker fault zones, some of which identified for the first time. These structures are not only related to the inner caldera and dome resurgence but also to volcano‐tectonic events of the last 10 ka. The extent of imaged fault segments suggests they can accommodate ruptures up to a moment magnitude 5.1, significantly increasing seismic hazard in the area.https://doi.org/10.1029/2023GL107680earthquake locationscaldera Campi Flegreiimaging active faults
spellingShingle Francesco Scotto di Uccio
Anthony Lomax
Jacopo Natale
Titouan Muzellec
Gaetano Festa
Sahar Nazeri
Vincenzo Convertito
Antonella Bobbio
Claudio Strumia
Aldo Zollo
Delineation and Fine‐Scale Structure of Fault Zones Activated During the 2014–2024 Unrest at the Campi Flegrei Caldera (Southern Italy) From High‐Precision Earthquake Locations
Geophysical Research Letters
earthquake locations
caldera Campi Flegrei
imaging active faults
title Delineation and Fine‐Scale Structure of Fault Zones Activated During the 2014–2024 Unrest at the Campi Flegrei Caldera (Southern Italy) From High‐Precision Earthquake Locations
title_full Delineation and Fine‐Scale Structure of Fault Zones Activated During the 2014–2024 Unrest at the Campi Flegrei Caldera (Southern Italy) From High‐Precision Earthquake Locations
title_fullStr Delineation and Fine‐Scale Structure of Fault Zones Activated During the 2014–2024 Unrest at the Campi Flegrei Caldera (Southern Italy) From High‐Precision Earthquake Locations
title_full_unstemmed Delineation and Fine‐Scale Structure of Fault Zones Activated During the 2014–2024 Unrest at the Campi Flegrei Caldera (Southern Italy) From High‐Precision Earthquake Locations
title_short Delineation and Fine‐Scale Structure of Fault Zones Activated During the 2014–2024 Unrest at the Campi Flegrei Caldera (Southern Italy) From High‐Precision Earthquake Locations
title_sort delineation and fine scale structure of fault zones activated during the 2014 2024 unrest at the campi flegrei caldera southern italy from high precision earthquake locations
topic earthquake locations
caldera Campi Flegrei
imaging active faults
url https://doi.org/10.1029/2023GL107680
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