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) |