0000000000379613

AUTHOR

Andri Stefánsson

showing 3 related works from this author

Rapid shifting of a deep magmatic source at Fagradalsfjall volcano, Iceland

2022

AbstractRecent 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 associate…

REYKJANES PENINSULA3705 GeologySOLUBILITY/140/128/140/125ERUPTION/704/2151/431/132Multidisciplinaryiceland volcanism volatiles Fagradalsfjall/704/2151/213/704/2151/598PRESSURESarticleCONSTRAINTS37 Earth SciencesEVOLUTION3703 GeochemistryINSIGHTS[SDU]Sciences of the Universe [physics]MIDOCEAN RIDGE BASALTSOLIVINE/704/2151/2093706 GeophysicsGENERATION
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Chemical weathering of volcanic rocks at the island of Pantelleria, Italy: Information from soil profile and soil solution investigations

2007

Abstract Concentrations of major, minor and trace elements were determined in soil profiles and soil solutions from the island of Pantelleria, Sicily Channel, to evaluate the weathering extent of soils evolved on trachytic and pantelleritic rocks and the aqueous transport of elements by their soil solutions. The chemical index of alteration (CIA) indicates a low-to-moderate degree of weathering; consistently, the mineralogical and geochemical imprints of the parent rocks are generally preserved. The chemical weathering appears to be incongruent, owing to primary minerals and glass dissolving to a variable degree while secondary minerals have formed. Based on the calculated saturation state …

PedogenesisGeochemistry and PetrologySoil production functionParent materialGeochemistrySoil horizonKaoliniteMineralogyGeologyWeatheringParent rockClay mineralsGeologyChemical Geology
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Ground-Based measurements of the 2014-2015 holuhraun volcanic cloud (Iceland)

2018

he 2014–2015 Bárðarbunga fissure eruption at Holuhraun in central Iceland was distinguished by the high emission of gases, in total 9.6 Mt SO2, with almost no tephra. This work collates all ground-based measurements of this extraordinary eruption cloud made under particularly challenging conditions: remote location, optically dense cloud with high SO2 column amounts, low UV intensity, frequent clouds and precipitation, an extensive and hot lava field, developing ramparts, and high-latitude winter conditions. Semi-continuous measurements of SO2 flux with three scanning DOAS instruments were augmented by car traverses along the ring-road and along the lava. The ratios of other gases/SO2 were …

Eldgos010504 meteorology & atmospheric sciencesLavaHoluhraun; Bárðarbunga; gas; SO<sub>2</sub>; cloud height; eruption monitoring; fissure eruptionBárðarbunga; cloud height; eruption monitoring; fissure eruption; gas; Holuhraun; SO2GaEarth and Planetary Sciences(all)SO2Fissure eruption010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesSO 2GosmökkurLava fieldgasBrennisteinsdíoxíðPrecipitationTephraHoluhraun/dk/atira/pure/subjectarea/asjc/19000105 earth and related environmental sciencesSOgeographygeography.geographical_feature_categoryConjunction (astronomy)eruption monitoringfissure eruptionlcsh:QE1-996.5Sprungugoscloud heightPlumelcsh:GeologyBárðarbunga13. Climate actionGasCloud heightGeneral Earth and Planetary SciencesEruption monitoringLofttegundirCloud heightEarth and Planetary Sciences (all)GeologyVolcanic ash
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