Petrology and geochemistry of the 2014–2015 Holuhraun eruption, central Iceland: compositional and mineralogical characteristics, temporal variability and magma storage-Reference-Cited by-同舟云学术

Petrology and geochemistry of the 2014–2015 Holuhraun eruption, central Iceland: compositional and mineralogical characteristics, temporal variability and magma storage

Published:2018-07-23 Issue:8 Volume:173 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Halldórsson Sæmundur A.,Bali Enikő,Hartley Margaret E.,Neave David A.,Peate David W.,Guðfinnsson Guðmundur H.,Bindeman Ilya,Whitehouse Martin J.,Riishuus Morten S.,Pedersen Gro B. M.,Jakobsson Sigurður,Askew Rob,Gallagher Catherine R.,Guðmundsdóttir Esther R.,Gudnason Jónas,Moreland William M.,Óskarsson Birgir V.,Nikkola Paavo,Reynolds Hannah I.,Schmith Johanne,Thordarson Thorvaldur

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/article/10.1007/s00410-018-1487-9/fulltext.html

Reference120 articles.

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2. Bali E, Hartley ME, Halldórsson SA, Guðfinsson GH, Jakobsson S (2018) Melt inclusion constraints on volatile systematics and degassing history of the 2014–2015 Holuhraun eruption, Iceland. Contrib Mineral Petrol 173:9

3. Bindeman IN (2008) Oxygen isotopes in mantle and crustal magmas as revealed by single crystal analysis. Rev Mineral Geochem 69:445–478

4. Bindeman IN, Sigmarsson O, Eiler J (2006) Time constraints on the origin of large volume basalts derived from O-isotope and trace element mineral zoning and U-series disequilibria in the Laki and Grimsvötn volcanic system. Earth Planet Sci Lett 245:245–259

5. Bindeman IN, Gurenko A, Sigmarsson O, Chaussidon M (2008) Oxygen isotope heterogeneity and disequilibria of olivine crystals in large volume Holocene basalts from Iceland: evidence for magmatic digestion and erosion of Pleistocene hyaloclastites. Geochim Cosmochim Acta 72:4397–4420

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