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Stress variations and non-shear earthquakes before the 2021 Iceland eruption trace magmatic fluid flow

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F25%3A00637887" target="_blank" >RIV/67985530:_____/25:00637887 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/25:10505805

  • Result on the web

    <a href="https://www.nature.com/articles/s43247-025-02533-5" target="_blank" >https://www.nature.com/articles/s43247-025-02533-5</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1038/s43247-025-02533-5" target="_blank" >10.1038/s43247-025-02533-5</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Stress variations and non-shear earthquakes before the 2021 Iceland eruption trace magmatic fluid flow

  • Original language description

    The 2021 Fagradalsfjall eruption on Iceland's Reykjanes Peninsula was preceded by an intense seismic swarm, offering an opportunity to investigate fluid dynamics and faulting processes at divergent plate boundary. Here we analysed 1306 full moment tensors of pre-eruption dike-related earthquakes and identified three faulting regimes: strike-slip, normal and reverse, driven by variations in vertical stress and controlled by fluid dynamics and crustal heterogeneity. Systematic volumetric components of these earthquakes revealed both tensile opening and compressive closing of cracks. Notably, crack closing dominated shallow, fractured crust, associated with surface subsidence above the dike, while crack opening occurred within the impermeable crust, suggesting overpressured fluids trapped at structural barriers. These variations highlight the role of fluid-rock interactions and anisotropic permeability in driving fault behaviour. Our results demonstrate that non-double-couple components of earthquakes are sensitive indicators of evolving stress and fluid migration. They provide insights into the mechanics of seismo-volcanic unrest at the slow-spreading rift.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10507 - Volcanology

Result continuities

  • Project

    <a href="/en/project/GX25-16408X" target="_blank" >GX25-16408X: Comprehensive geophysical analysis of the ongoing volcanic eruption at the Reykjanes peninsula</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2025

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Communications Earth & Environment

  • ISSN

    2662-4435

  • e-ISSN

    2662-4435

  • Volume of the periodical

    6

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    11

  • Pages from-to

    575

  • UT code for WoS article

    001535204300001

  • EID of the result in the Scopus database

    2-s2.0-105011272399