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dc.contributor.authorPankhurst, MJ
dc.contributor.authorScarrow, JH
dc.contributor.authorBarbee, OA
dc.contributor.authorHickey, J
dc.contributor.authorColdwell, BC
dc.contributor.authorRollinson, GK
dc.contributor.authorRodríguez-Losada, JA
dc.contributor.authorLorenzo, AM
dc.contributor.authorRodríguez, F
dc.contributor.authorHernández, W
dc.contributor.authorFernández, DC
dc.contributor.authorHernández, PA
dc.contributor.authorPérez, NM
dc.date.accessioned2022-03-21T09:05:35Z
dc.date.issued2022-01-10
dc.date.updated2022-03-18T16:38:40Z
dc.description.abstractHow and why magmatic systems reactivate and evolve is a critical question for monitoring and hazard mitigation efforts during initial response and ongoing volcanic crisis management. Here we report the first integrated petrological results and interpretation provided to monitoring authorities during the ongoing eruption of Cumbre Vieja, La Palma, Canary Islands, Spain. The first eruptive products comprised simultaneous Strombolian fountain-fed lava flows and tephra fall from near-continuous eruption plumes. From combined field, petrographic and geochemical analyses conducted in the 10 days following sample collection, we infer low percentage mantle melts with a variably equilibrated multimineralic crystal-cargo and compositional fractionation by winnowing during eruptive processes. Hence ‘rapid response’ petrology can untangle complex magmatic and volcanic processes for this eruption, which combined with further study and methodological improvement can increasingly assist in active decision making.en_GB
dc.format.extent1-10
dc.identifier.citationVol. 5(1)en_GB
dc.identifier.doihttps://doi.org/10.30909/vol.05.01.0110
dc.identifier.urihttp://hdl.handle.net/10871/129096
dc.identifierORCID: 0000-0002-5391-3415 (Hickey, James)
dc.identifierORCID: 0000-0002-0655-6304 (Rollinson, Gavyn K)
dc.identifierScopusID: 25645060100 (Rollinson, Gavyn K)
dc.language.isoenen_GB
dc.publisherVolcanicaen_GB
dc.relation.urlhttps://doi.org/10.21203/rs.3.rs-963593/v1en_GB
dc.rights© The Author(s) 2022. Open access. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License, which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commonslicense, and indicate if changes were made.en_GB
dc.subjectLava-tephraen_GB
dc.subjectPetrological monitoringen_GB
dc.subjectQEMSCANen_GB
dc.subjectMineral chemistryen_GB
dc.subjectCrystal cargoen_GB
dc.titleRapid response petrology for the opening eruptive phase of the 2021 Cumbre Vieja eruption, La Palma, Canary Islandsen_GB
dc.typeArticleen_GB
dc.date.available2022-03-21T09:05:35Z
dc.identifier.issn2610-3540
dc.descriptionThis is the final version. Available on open access from Volcanica via the DOI in this recorden_GB
dc.descriptionData availability: Full datasets are available at Research Square: https: //assets.researchsquare.com/files/rs-963593/ v1/9f174d00-262e-4f21-b0d2-6825cf131538.pdf?c= 1634295351 (doi: 10.21203/rs.3.rs-963593/v1).en_GB
dc.identifier.eissn2610-3540
dc.identifier.journalVolcanicaen_GB
dc.relation.ispartofVolcanica, 5(1)
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_GB
rioxxterms.versionVoRen_GB
rioxxterms.licenseref.startdate2022-01-10
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2022-03-21T09:01:18Z
refterms.versionFCDVoR
refterms.dateFOA2022-03-21T09:08:27Z
refterms.panelBen_GB
refterms.dateFirstOnline2022-01-10


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© The Author(s) 2022. Open access. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License, which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commonslicense, and indicate if changes were made.
Except where otherwise noted, this item's licence is described as © The Author(s) 2022. Open access. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License, which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commonslicense, and indicate if changes were made.