Geochemical variability as an indicator for large magnitude eruptions in volcanic arcs

Abstract Caldera-forming eruptions have the potential to induce drastic socioeconomic change. However, the criteria to identify volcanoes capable of producing large magnitude eruptions in the future are not well constrained. Here we compile and analyse data, revealing that volcanoes which have produ...

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Main Authors: Gregor Weber, Tom E. Sheldrake
Format: Article
Language:English
Published: Nature Portfolio 2022-09-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-022-19902-1
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author Gregor Weber
Tom E. Sheldrake
author_facet Gregor Weber
Tom E. Sheldrake
author_sort Gregor Weber
collection DOAJ
description Abstract Caldera-forming eruptions have the potential to induce drastic socioeconomic change. However, the criteria to identify volcanoes capable of producing large magnitude eruptions in the future are not well constrained. Here we compile and analyse data, revealing that volcanoes which have produced catastrophic caldera-forming eruptions in the past, show larger ranges of erupted magma geochemistry compared to those that have not. This suggests geochemical variability is related to the size of magmatic systems. Using heat transfer simulations, we show that differences in magma flux result in a dependency between chemical diversity and magma volume that is consistent with these observations. We conclude that compositional spread should be included in the catalogue of criteria to identify volcanoes with greater probability of producing future large eruptions. Importantly, this allows to identify stratovolcanoes with caldera-like geochemical signatures, which have not yet been recognized as systems with greater likelihood of producing large magnitude eruptions.
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spelling doaj.art-87ef8cbb69734d1abca4a645b1b660fb2022-12-22T03:18:12ZengNature PortfolioScientific Reports2045-23222022-09-0112111110.1038/s41598-022-19902-1Geochemical variability as an indicator for large magnitude eruptions in volcanic arcsGregor Weber0Tom E. Sheldrake1Department of Earth Sciences, University of OxfordDepartment of Earth Sciences, University of GenevaAbstract Caldera-forming eruptions have the potential to induce drastic socioeconomic change. However, the criteria to identify volcanoes capable of producing large magnitude eruptions in the future are not well constrained. Here we compile and analyse data, revealing that volcanoes which have produced catastrophic caldera-forming eruptions in the past, show larger ranges of erupted magma geochemistry compared to those that have not. This suggests geochemical variability is related to the size of magmatic systems. Using heat transfer simulations, we show that differences in magma flux result in a dependency between chemical diversity and magma volume that is consistent with these observations. We conclude that compositional spread should be included in the catalogue of criteria to identify volcanoes with greater probability of producing future large eruptions. Importantly, this allows to identify stratovolcanoes with caldera-like geochemical signatures, which have not yet been recognized as systems with greater likelihood of producing large magnitude eruptions.https://doi.org/10.1038/s41598-022-19902-1
spellingShingle Gregor Weber
Tom E. Sheldrake
Geochemical variability as an indicator for large magnitude eruptions in volcanic arcs
Scientific Reports
title Geochemical variability as an indicator for large magnitude eruptions in volcanic arcs
title_full Geochemical variability as an indicator for large magnitude eruptions in volcanic arcs
title_fullStr Geochemical variability as an indicator for large magnitude eruptions in volcanic arcs
title_full_unstemmed Geochemical variability as an indicator for large magnitude eruptions in volcanic arcs
title_short Geochemical variability as an indicator for large magnitude eruptions in volcanic arcs
title_sort geochemical variability as an indicator for large magnitude eruptions in volcanic arcs
url https://doi.org/10.1038/s41598-022-19902-1
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AT tomesheldrake geochemicalvariabilityasanindicatorforlargemagnitudeeruptionsinvolcanicarcs