Titill: | A dynamic mid-crustal magma domain revealed by the 2023 to 2024 Sundhnúksgígar eruptions in Iceland |
Höfundur: |
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Útgáfa: | 2024-10-17 |
Tungumál: | Enska |
Umfang: | 309-314 |
Háskóli/Stofnun: | Háskóli Íslands University of Iceland |
Svið: | Verkfræði- og náttúruvísindasvið (HÍ) School of Engineering and Natural Sciences (UI) |
Deild: | Jarðvísindastofnun (HÍ) Institute of Earth Sciences (UI) |
Birtist í: | Science;386(6719) |
ISSN: | 0036-8075 1095-9203 |
DOI: | 10.1126/science.adp8778 |
Efnisorð: | Jarðefnafræði; Reykjanes; Eldgos; Svartsengi; Bergfræði |
URI: | https://hdl.handle.net/20.500.11815/5042 |
Tilvitnun:Simon W. Matthews et al., A dynamic mid-crustal magma domain revealed by the 2023 to 2024 Sundhnúksgígar eruptions in Iceland. Science 386, 309-314 (2024). DOI: 10.1126/science.adp8778
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Útdráttur:Mid-crustal magma domains are the source of many basaltic eruptions. Lavas from individual eruptions are often chemically homogeneous, suggesting they derive from single well-mixed magma reservoirs. The 2023-2024 eruptions at Sundhnúksgígar in the Svartsengi volcanic system, Iceland, provide an opportunity to observe the behavior of a mid-crustal magma domain at high spatial and temporal resolution by detailed sampling and geochemical characterization. We observed substantial mantle-derived geochemical variability in the products erupted in the first hours of the December 2023, January, February, and March-May 2024 eruptions, indicating the eruptions derived from multiple magma reservoirs, which mineral-melt equilibration pressures place in the mid-crust. The unusual presence of geochemical heterogeneity in the mid-crustal magma domain provides an insight into how dynamic and complex mid-crustal magma domains can be.
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