Number of the records: 1  

Cyclical geothermal unrest as a precursor to Iceland’s 2021 Fagradalsfjall eruption

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    SYSNO ASEP0557212
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleCyclical geothermal unrest as a precursor to Iceland’s 2021 Fagradalsfjall eruption
    Author(s) Flóvenz, Ó. G. (IS)
    Wang, R. (CN)
    Hersir, G. P. (IS)
    Dahm, T. (DE)
    Hainzl, S. (DE)
    Vassileva, M. (DE)
    Drouin, V. (IS)
    Heimann, S. (DE)
    Isken, M. P. (DE)
    Gudnason, E. Á. (IS)
    Ágústsson, K. (IS)
    Ágústsdóttir, T. (IS)
    Horálek, Josef (GFU-E) ORCID, RID
    Motagh, M. (DE)
    Walter, T. R. (DE)
    Rivalta, A. (DE)
    Jousset, P. (FR)
    Krawczyk, C. M. (DE)
    Milkereit, C. (DE)
    Source TitleNature Geoscience. - : Nature Publishing Group - ISSN 1752-0894
    Roč. 15, May (2022), s. 397-404
    Number of pages8 s.
    Publication formPrint - P
    Languageeng - English
    CountryGB - United Kingdom
    Keywordssurface deformation ; Reykjanes peninsula ; earthquakes
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    OECD categoryVolcanology
    Method of publishingOpen access
    Institutional supportGFU-E - RVO:67985530
    UT WOS000789729500001
    EID SCOPUS85129252410
    DOI10.1038/s41561-022-00930-5
    AnnotationUnderstanding and constraining the source of geodetic deformation in volcanic areas is an important component of hazard assessment. Here, we analyse deformation and seismicity for one year before the March 2021 Fagradalsfjall eruption in Iceland. We generate a high-resolution catalogue of 39,500 earthquakes using optical cable recordings and develop a poroelastic model to describe three pre-eruptional uplift and subsidence cycles at the Svartsengi geothermal field, 8 km west of the eruption site. We find the observed deformation is best explained by cyclic intrusions into a permeable aquifer by a fluid injected at 4 km depth below the geothermal field, with a total volume of 0.11 +/- 0.05 km(3) and a density of 850 +/- 350 kg m(-3). We therefore suggest that ingression of magmatic CO2 can explain the geodetic, gravity and seismic data, although some contribution of magma cannot be excluded. Ingression of magmatic gas into a geothermal aquifer generated cyclical deformation and primed the system for the 2021 Fagradalsfjall eruption, Iceland, according to a catalogue of 39,500 precursory earthquakes combined with a poroelastic model.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2023
    Electronic addresshttps://www.nature.com/articles/s41561-022-00930-5
Number of the records: 1  

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