Detail publikace

Trace element composition in olivine from the 2022 Meradalir eruption of the Fagradalsfjall Fires, SW-Iceland

KRMÍČEK, L. TROLL, V.R. VAŠINOVÁ GALIOVÁ, M. THORDARSON, T. BRABEC, M.

Originální název

Trace element composition in olivine from the 2022 Meradalir eruption of the Fagradalsfjall Fires, SW-Iceland

Typ

článek v časopise ve Web of Science, Jimp

Jazyk

angličtina

Originální abstrakt

This study focuses on determining the trace element composition in olivine from olivine tholeiitic basalts sampled in Iceland during the 2022 Meradalir eruption of the 2021-ongoing Fagradalsfjall Fires. The chemistry of Meradalir olivine is characteristic for a volcanic origin where olivine crystals represent the product of crystallisation. Olivine from the Meradalir basalt magma falls within the field characteristic for the melting of a dominantly peridotitic mantle source. However, the data show that the 2022 Meradalir olivine crystalized from a compositionally more evolved magma than olivine from the preceding 2021 Geldingadalir eruption of the Fagradalsfjall Fires.

Klíčová slova

olivine; Reykjanes Peninsula; Meradalir lava; LA-ICP-MS

Autoři

KRMÍČEK, L.; TROLL, V.R.; VAŠINOVÁ GALIOVÁ, M.; THORDARSON, T.; BRABEC, M.

Vydáno

15. 2. 2023

Nakladatel

MASARYK UNIV PRESS

Místo

Brno

ISSN

1805-0689

Periodikum

Czech Polar Reports

Ročník

12

Číslo

2

Stát

Česká republika

Strany od

222

Strany do

231

Strany počet

10

URL

https://journals.muni.cz/CPR/article/view/33531/28606

BibTex

@article{BUT183235,
  author="Lukáš {Krmíček} and Valentin R. {Troll} and Michaela {Vašinová Galiová} and Thor {Thordarson} and Marek {Brabec}",
  title="Trace element composition in olivine from the 2022 Meradalir eruption of the Fagradalsfjall Fires, SW-Iceland",
  journal="Czech Polar Reports",
  year="2023",
  volume="12",
  number="2",
  pages="222--231",
  doi="10.5817/CPR2022-2-16",
  issn="1805-0689",
  url="https://journals.muni.cz/CPR/article/view/33531/28606"
}