H2O-rich melt inclusions in fayalitic olivine from Hekla volcano: Implications for phase relationships in silicic systems and driving forces of explosive volcanism on Iceland-Reference-Cited by-同舟云学术

H2O-rich melt inclusions in fayalitic olivine from Hekla volcano: Implications for phase relationships in silicic systems and driving forces of explosive volcanism on Iceland

Published:2012-12 Issue: Volume:357-358 Page:337-346
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Portnyagin Maxim,Hoernle Kaj,Storm Sonja,Mironov Nikita,van den Bogaard Christel,Botcharnikov Roman

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference67 articles.

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3. An experimental investigation of the influence of water and oxygen fugacity on differentiation of MORB at 200MPa;Berndt;J. Petrol.,2005

4. Silicic magma petrogenesis in Iceland by remelting of hydrothermally altered crust based on oxygen isotope diversity and disequilibria between zircon and magma with implications for MORB;Bindeman;Terra Nova,2012

5. Ascent-driven crystallisation of dacite magmas at Mount St Helens;Blundy;Contrib. Mineral. Petrol.,2001

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