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  • Rhodes, Emma,1990-Uppsala universitet,Mineralogi, petrologi och tektonik,Uppsala Univ, Ctr Nat Hazards & Disaster Sci, Uppsala, Sweden. (author)

Rapid Assembly and Eruption of a Shallow Silicic Magma Reservoir, Reyðarártindur Pluton, Southeast Iceland

  • Article/chapterEnglish2021

Publisher, publication year, extent ...

  • American Geophysical Union (AGU),2021
  • electronicrdacarrier

Numbers

  • LIBRIS-ID:oai:DiVA.org:uu-461136
  • https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-461136URI
  • https://doi.org/10.1029/2021GC009999DOI
  • https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-199539URI

Supplementary language notes

  • Language:English
  • Summary in:English

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  • Subject category:ref swepub-contenttype
  • Subject category:art swepub-publicationtype

Notes

  • Although it is widely accepted that shallow silicic magma reservoirs exist, and can feed eruptions, their dynamics and longevity are a topic of debate. Here, we use field mapping, geochemistry, 3D pluton reconstruction and a thermal model to investigate the assembly and eruptive history of the shallow Reyoarartindur Pluton, southeast Iceland. Primarily, the exposed pluton is constructed of a single rock unit, the Main Granite (69.9-77.7 wt.% SiO2). Two further units are locally exposed as enclaves at the base of the exposure, the Granite Enclaves (67.4-70.2 wt.% SiO2), and the Quartz Monzonite Enclaves (61.8-67.3 wt.% SiO2). Geochemically, the units are related and were likely derived from the same source reservoir. In 3D, the pluton has a shape characterized by flat roof segments that are vertically offset and a volume of >2.5 km(3). The pluton roof is intruded by dikes from the pluton, and in two locations displays depressions associated with large dikes. Within these particular dikes the rock is partially to wholly tuffisitic, and rock compositions range from quartz monzonite to granite. We interpret these zones as eruption-feeding conduits from the pluton. A lack of cooling contacts throughout the pluton indicates rapid magma emplacement and a thermal model calculates the top 75 m would have rheologically locked up within 1,000 years. Hence, we argue that the Reyoarartindur Pluton was an ephemeral part of the wider plumbing system that feeds a volcano, and that timeframes from emplacement to eruption were rapid.

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Added entries (persons, corporate bodies, meetings, titles ...)

  • Barker, AbigailUppsala universitet,Mineralogi, petrologi och tektonik,Uppsala Univ, Ctr Nat Hazards & Disaster Sci, Uppsala, Sweden.(Swepub:uu)abiba516 (author)
  • Burchardt, Steffi,1982-Uppsala universitet,Mineralogi, petrologi och tektonik,Uppsala Univ, Ctr Nat Hazards & Disaster Sci, Uppsala, Sweden.(Swepub:uu)stebu734 (author)
  • Hieronymus, Christoph F.,1967-Uppsala universitet,Geofysik(Swepub:uu)chrhi266 (author)
  • Rousku, S. N.Uppsala universitet,Institutionen för geovetenskaper (author)
  • McGarvie, D. W.Univ Lancaster, Lancaster Environm Ctr, Lancaster, England. (author)
  • Mattsson, TobiasStockholms universitet,Institutionen för geologiska vetenskaper,University of St Andrews, UK,Univ St Andrews, Sch Earth & Environm Sci, St Andrews, Fife, Scotland.;Stockholm Univ, Dept Geol Sci, Stockholm, Sweden.(Swepub:su)toma4827 (author)
  • Schmiedel, TobiasUppsala universitet,Mineralogi, petrologi och tektonik(Swepub:uu)tobsc370 (author)
  • Ronchin, E.Sapienza Univ Rome, Dept Earth Sci, Rome, Italy. (author)
  • Witcher, TaylorUppsala universitet,Mineralogi, petrologi och tektonik(Swepub:uu)taywi125 (author)
  • Uppsala universitetMineralogi, petrologi och tektonik (creator_code:org_t)

Related titles

  • In:Geochemistry Geophysics Geosystems: American Geophysical Union (AGU)22:111525-2027

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