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1000 Titel
  • A multi-methodological approach to record dynamics and timescales of the plumbing system of Zaro (Ischia Island, Italy)
1000 Autor/in
  1. Pelullo, Carlo |
  2. Chakraborty, Sumit |
  3. Montagna, Chiara Paola |
  4. Arienzo, Ilenia |
  5. Brown, Richard James |
  6. D’Antonio, Massimo |
  7. de Vita, Sandro |
  8. D’Oriano, Claudia |
  9. Nazzari, Manuela |
  10. Pappalardo, Lucia |
  11. Petrosino, Paola |
1000 Verlag Springer Berlin Heidelberg
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-05-04
1000 Erschienen in
1000 Quellenangabe
  • 179(5):54
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1007/s00410-024-02138-9 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:title>Abstract</jats:title><jats:p>Determining the time spans of processes related to the assembly of eruptible magma at active volcanoes is fundamental to understand magma chamber dynamics and assess volcanic hazard. This information can be recorded in the chemical zoning of crystals. Nevertheless, this kind of study is still poorly employed for the active volcanoes of the Neapolitan area (Southern Italy), in particular, for Ischia island where the risk is extremely high and this information can provide the basis for probabilistic volcanic hazard assessment. For these reasons, we acquired chemical composition on clinopyroxene crystals erupted at Ischia during the Zaro eruption (6.6 ± 2.2 ka) and performed numerical simulations of the input of mafic magma into a trachytic reservoir, in order to investigate various aspects of pre-eruptive dynamics occurring at different timescales. This event emplaced a ~ 0.1 km<jats:sup>3</jats:sup> lava complex, in which the main trachytic lava flows host abundant mafic to felsic enclaves. Previous petrological investigation suggested that mafic magma(s) mixed/mingled with a trachytic one, before the eruption. In this work, the clinopyroxene zoning patterns depict the growth of crystals in different magmatic environments, recording sequential changes occurred in the plumbing system before the eruption. The evolution of the plumbing system involved a hierarchy of timescales: <jats:italic>a few hours</jats:italic> for magma mingling caused by mafic recharge(s) and likely occurred multiple times over <jats:italic>a decade</jats:italic> during which a dominant magmatic environment was sustained before the eruption. Such timescales must be considered in volcanic hazard assessment at Ischia and similar active volcanoes in densely populated areas.</jats:p>
1000 Sacherschließung
lokal Original Paper
lokal Ischia island
lokal Fe–Mg diffusion modelling
lokal Clinopyroxene zoning pattern
lokal Magma recharge
lokal Numerical simulation
1000 Fächerklassifikation (DDC)
1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/UGVsdWxsbywgQ2FybG8=|https://frl.publisso.de/adhoc/uri/Q2hha3JhYm9ydHksIFN1bWl0|https://frl.publisso.de/adhoc/uri/TW9udGFnbmEsIENoaWFyYSBQYW9sYQ==|https://frl.publisso.de/adhoc/uri/QXJpZW56bywgSWxlbmlh|https://frl.publisso.de/adhoc/uri/QnJvd24sIFJpY2hhcmQgSmFtZXM=|https://frl.publisso.de/adhoc/uri/ROKAmUFudG9uaW8sIE1hc3NpbW8=|https://frl.publisso.de/adhoc/uri/ZGUgVml0YSwgU2FuZHJv|https://frl.publisso.de/adhoc/uri/ROKAmU9yaWFubywgQ2xhdWRpYQ==|https://frl.publisso.de/adhoc/uri/TmF6emFyaSwgTWFudWVsYQ==|https://frl.publisso.de/adhoc/uri/UGFwcGFsYXJkbywgTHVjaWE=|https://frl.publisso.de/adhoc/uri/UGV0cm9zaW5vLCBQYW9sYQ==
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1000 Förderer
  1. German Academic Exchange Service |
  2. Istituto Nazionale di Geofisica e Vulcanologia |
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1000 Förderprogramm
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1000 Dateien
1000 Förderung
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    1000 Förderer German Academic Exchange Service |
    1000 Förderprogramm -
    1000 Fördernummer -
  2. 1000 joinedFunding-child
    1000 Förderer Istituto Nazionale di Geofisica e Vulcanologia |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
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1000 @id frl:6500019.rdf
1000 Erstellt am 2025-02-05T06:14:26.899+0100
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1000 Zuletzt bearbeitet 2025-09-11T18:13:46.570+0200
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