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Segmented lateral dyke growth in a rifting event at Bárðarbunga volcanic system, Iceland.
Nature. 2015 Jan 8;517(7533):191-5. doi: 10.1038/nature14111. Epub 2014 Dec 15.
Nature. 2015.
PMID: 25517098
Free article.
Gradual caldera collapse at Bárdarbunga volcano, Iceland, regulated by lateral magma outflow.
Gudmundsson MT, Jónsdóttir K, Hooper A, Holohan EP, Halldórsson SA, Ófeigsson BG, Cesca S, Vogfjörd KS, Sigmundsson F, Högnadóttir T, Einarsson P, Sigmarsson O, Jarosch AH, Jónasson K, Magnússon E, Hreinsdóttir S, Bagnardi M, Parks MM, Hjörleifsdóttir V, Pálsson F, Walter TR, Schöpfer MP, Heimann S, Reynolds HI, Dumont S, Bali E, Gudfinnsson GH, Dahm T, Roberts MJ, Hensch M, Belart JM, Spaans K, Jakobsson S, Gudmundsson GB, Fridriksdóttir HM, Drouin V, Dürig T, Aðalgeirsdóttir G, Riishuus MS, Pedersen GB, van Boeckel T, Oddsson B, Pfeffer MA, Barsotti S, Bergsson B, Donovan A, Burton MR, Aiuppa A.
Gudmundsson MT, et al. Among authors: fridriksdottir hm.
Science. 2016 Jul 15;353(6296):aaf8988. doi: 10.1126/science.aaf8988.
Science. 2016.
PMID: 27418515
Free article.
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Unexpected large eruptions from buoyant magma bodies within viscoelastic crust.
Sigmundsson F, Pinel V, Grapenthin R, Hooper A, Halldórsson SA, Einarsson P, Ófeigsson BG, Heimisson ER, Jónsdóttir K, Gudmundsson MT, Vogfjörd K, Parks M, Li S, Drouin V, Geirsson H, Dumont S, Fridriksdottir HM, Gudmundsson GB, Wright TJ, Yamasaki T.
Sigmundsson F, et al. Among authors: fridriksdottir hm.
Nat Commun. 2020 May 15;11(1):2403. doi: 10.1038/s41467-020-16054-6.
Nat Commun. 2020.
PMID: 32415105
Free PMC article.
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Fracturing and tectonic stress drive ultrarapid magma flow into dikes.
Sigmundsson F, Parks M, Geirsson H, Hooper A, Drouin V, Vogfjörd KS, Ófeigsson BG, Greiner SHM, Yang Y, Lanzi C, De Pascale GP, Jónsdóttir K, Hreinsdóttir S, Tolpekin V, Friðriksdóttir HM, Einarsson P, Barsotti S.
Sigmundsson F, et al. Among authors: fridriksdottir hm.
Science. 2024 Mar 15;383(6688):1228-1235. doi: 10.1126/science.adn2838. Epub 2024 Feb 8.
Science. 2024.
PMID: 38330140
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