Magma decompression rate correlates with explosivity at basaltic volcanoes — Constraints from water diffusion in olivine-Reference-Cited by-同舟云学术

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Magma decompression rate correlates with explosivity at basaltic volcanoes — Constraints from water diffusion in olivine

Published:2019-12 Issue: Volume:387 Page:106664
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Barth Anna,Newcombe Megan,Plank Terry,Gonnermann Helge,Hajimirza Sahand,Soto Gerardo J.,Saballos Armando,Hauri Erik

Funder

National Sleep Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference80 articles.

1. An experimental facility for the investigation of magma fragmentation by rapid decompression;Alidibirov;Bull. Volcanol.,1996

2. Relationships between pre-eruptive conditions and eruptive styles of phonolite-trachyte magmas;Andújar;Lithos,2012

3. Hydroxide in olivine: a quantitative determination of the absolute amount and calibration of the IR spectrum;Bell;J. Geophys. Res. Solid Earth,2003

4. Üder OH-gruppen in Olivin;Beran,1969

5. Fingerprinting the water site in mantle olivine;Berry;Geology,2005

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4. Magmatic Storage and Volatile Fluxes of the 2021 La Palma Eruption;Geochemistry, Geophysics, Geosystems;2024-06

5. 3D Diffusion of Water in Melt Inclusion‐Bearing Olivine Phenocrysts;Geochemistry, Geophysics, Geosystems;2024-03

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