دورية أكاديمية
Rapid shifting of a deep magmatic source at Fagradalsfjall volcano, Iceland
| العنوان: | Rapid shifting of a deep magmatic source at Fagradalsfjall volcano, Iceland |
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| المؤلفون: | Halldórsson, Sæmundur A., Marshall, Edward W., Caracciolo, Alberto, Matthews, Simon, Bali, Enikő, Rasmussen, Maja B., Ranta, Eemu, Robin, Jóhann Gunnarsson, Guðfinnsson, Guðmundur H., Sigmarsson, Olgeir, Maclennan, John, Jackson, Matthew G., Whitehouse, Martin J., Jeon, Heejin, van der Meer, Quinten H.A., Mibei, Geoffrey K., Kalliokoski, Maarit H., Repczynska, Maria M., Rúnarsdóttir, Rebekka Hlín, Sigurðsson, Gylfi, Pfeffer, Melissa Anne, Scott, Samuel W., Kjartansdóttir, Ríkey, Kleine, Barbara I., Oppenheimer, Clive, Aiuppa, Alessandro, Ilyinskaya, Evgenia, Bitetto, Marcello, Giudice, Gaetano, Stefánsson, Andri |
| المساهمون: | Department of Geosciences and Geography |
| بيانات النشر: | Nature Publishing Group |
| سنة النشر: | 2024 |
| المجموعة: | Helsingfors Universitet: HELDA – Helsingin yliopiston digitaalinen arkisto |
| مصطلحات موضوعية: | Geosciences |
| الوصف: | Recent Icelandic rifting events have illuminated the roles of centralized crustal magma reservoirs and lateral magma transport1–4, important characteristics of mid-ocean ridge magmatism1,5. A consequence of such shallow crustal processing of magmas4,5 is the overprinting of signatures that trace the origin, evolution and transport of melts in the uppermost mantle and lowermost crust6,7. Here we present unique insights into processes occurring in this zone from integrated petrologic and geochemical studies of the 2021 Fagradalsfjall eruption on the Reykjanes Peninsula in Iceland. Geochemical analyses of basalts erupted during the first 50 days of the eruption, combined with associated gas emissions, reveal direct sourcing from a near-Moho magma storage zone. Geochemical proxies, which signify different mantle compositions and melting conditions, changed at a rate unparalleled for individual basaltic eruptions globally. Initially, the erupted lava was dominated by melts sourced from the shallowest mantle but over the following three weeks became increasingly dominated by magmas generated at a greater depth. This exceptionally rapid trend in erupted compositions provides an unprecedented temporal record of magma mixing that filters the mantle signal, consistent with processing in near-Moho melt lenses containing 107–108 m3 of basaltic magma. Exposing previously inaccessible parts of this key magma processing zone to near-real-time investigations provides new insights into the timescales and operational mode of basaltic magma systems. ; Peer reviewed |
| نوع الوثيقة: | article in journal/newspaper |
| وصف الملف: | application/pdf |
| اللغة: | English |
| ردمك: | 978-85-13-78875-2 85-13-78875-9 |
| العلاقة: | We are grateful for the analytical help of C. Bosq and D. Auclair during the Sr and Nd isotope measurements. We thank G. Pedersen for providing shape-files of the lavas and M. T. Guðmundsson, H. Geirsson, F. Sigmundsson, B. Brandsdóttir, P. Einarsson, K. Grönvold, N. Óskarsson and K. Sæmundsson for helpful discussions and support. We thank S. Johnson, H. Rúnarsdóttir and Á. Ásmundsdóttir for assistance with sample preparation. The NordSIMS ion microprobe facility acknowledges support by the Swedish Research Council (grant no. 2017-00671), the Swedish Museum of Natural History and the University of Iceland; this is NordSIMS publication no. 713. The involvement of S.A.H. was partly in relation to H2020 project EUROVOLC, funded by the European Commission (grant no. 731070). This work was supported by the Icelandic Research Fund, grant no. 228933-051. We gratefully acknowledge constructive comments provided by A. Kent and K. Rubin that helped to improve this work. A.A. ackowledges funding from Italian Ministero Istruzione Università e Ricerca (Miur), grant PRIN2017-2017LMNLAW. We are grateful for the analytical help of C. Bosq and D. Auclair during the Sr and Nd isotope measurements. We thank G. Pedersen for providing shape-files of the lavas and M. T. Guðmundsson, H. Geirsson, F. Sigmundsson, B. Brandsdóttir, P. Einarsson, K. Grönvold, N. Óskarsson and K. Sæmundsson for helpful discussions and support. We thank S. Johnson, H. Rúnarsdóttir and Á. Ásmundsdóttir for assistance with sample preparation. The NordSIMS ion microprobe facility acknowledges support by the Swedish Research Council (grant no. 2017-00671), the Swedish Museum of Natural History and the University of Iceland; this is NordSIMS publication no. 713. The involvement of S.A.H. was partly in relation to H2020 project EUROVOLC, funded by the European Commission (grant no. 731070). This work was supported by the Icelandic Research Fund, grant no. 228933-051. We gratefully acknowledge constructive comments provided by A. Kent and K. Rubin that helped to improve this work. A.A. ackowledges funding from Italian Ministero Istruzione Università e Ricerca (Miur), grant PRIN2017-2017LMNLAW.; Halldórsson , S A , Marshall , E W , Caracciolo , A , Matthews , S , Bali , E , Rasmussen , M B , Ranta , E , Robin , J G , Guðfinnsson , G H , Sigmarsson , O , Maclennan , J , Jackson , M G , Whitehouse , M J , Jeon , H , van der Meer , Q H A , Mibei , G K , Kalliokoski , M H , Repczynska , M M , Rúnarsdóttir , R H , Sigurðsson , G , Pfeffer , M A , Scott , S W , Kjartansdóttir , R , Kleine , B I , Oppenheimer , C , Aiuppa , A , Ilyinskaya , E , Bitetto , M , Giudice , G & Stefánsson , A 2022 , ' Rapid shifting of a deep magmatic source at Fagradalsfjall volcano, Iceland ' , Nature , vol. 609 , no. 7927 , pp. 529-534 . https://doi.org/10.1038/s41586-022-04981-xTest; ORCID: /0000-0003-3685-334X/work/154009264; http://hdl.handle.net/10138/571469Test; 91136078-50d2-45f3-9d37-44ec1aedad82; 85137887596 |
| الإتاحة: | http://hdl.handle.net/10138/571469Test |
| حقوق: | cc_by ; info:eu-repo/semantics/openAccess ; openAccess |
| رقم الانضمام: | edsbas.18363095 |
| قاعدة البيانات: | BASE |
| ردمك: | 9788513788752 8513788759 |
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