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A dynamic mid-crustal magma domain revealed by the 2023 to 2024 Sundhnúksgígar eruptions in Iceland

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dc.contributor Háskóli Íslands
dc.contributor University of Iceland
dc.contributor.author Matthews, Simon W.
dc.contributor.author Caracciolo, Alberto
dc.contributor.author Bali, Enikő
dc.contributor.author Halldórsson, Sæmundur A.
dc.contributor.author Sigmarsson, Olgeir
dc.contributor.author Guðfinnsson, Guðmundur H.
dc.contributor.author Pedersen, Gro B. M.
dc.contributor.author Robin, Jóhann Gunnarsson
dc.contributor.author Marshall, Edward W.
dc.contributor.author Aden, Araksan A.
dc.contributor.author Gísladóttir, Bryndís Ýr
dc.contributor.author Bosq, Chantal
dc.contributor.author Auclair, Delphine
dc.contributor.author Merrill, Heini
dc.contributor.author Levillayer, Nicolas
dc.contributor.author Löw, Noëmi
dc.contributor.author Rúnarsdóttir, Rebekka Hlín
dc.contributor.author Johnson, Sóley M.
dc.contributor.author Steinþórsson, Sveinbjörn
dc.contributor.author Drouin, Vincent
dc.date.accessioned 2024-10-22T08:45:34Z
dc.date.available 2024-10-22T08:45:34Z
dc.date.issued 2024-10-17
dc.identifier.citation 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
dc.identifier.issn 0036-8075
dc.identifier.issn 1095-9203
dc.identifier.uri https://hdl.handle.net/20.500.11815/5042
dc.description.abstract 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.
dc.format.extent 309-314
dc.language.iso en
dc.publisher American Association for the Advancement of Science (AAAS)
dc.relation.ispartofseries Science;386(6719)
dc.rights info:eu-repo/semantics/openAccess
dc.subject Jarðefnafræði
dc.subject Reykjanes
dc.subject Eldgos
dc.subject Svartsengi
dc.subject Bergfræði
dc.title A dynamic mid-crustal magma domain revealed by the 2023 to 2024 Sundhnúksgígar eruptions in Iceland
dc.type info:eu-repo/semantics/article
dc.description.version Peer Reviewed
dc.identifier.journal Science
dc.identifier.doi 10.1126/science.adp8778
dc.relation.url https://www.science.org/doi/pdf/10.1126/science.adp8778
dc.contributor.department Jarðvísindastofnun (HÍ)
dc.contributor.department Institute of Earth Sciences (UI)
dc.contributor.school Verkfræði- og náttúruvísindasvið (HÍ)
dc.contributor.school School of Engineering and Natural Sciences (UI)


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