Explosive subglacial rhyolitic eruptions in Iceland are fuelled by high magmatic H2O and closed-system degassing
Rhyolitic eruptions beneath Icelandic glaciers can be highly explosive, as demonstrated by Quaternary tephra layers dispersed throughout northern Europe. However, they can also be small and effusive. A subglacial rhyolitic eruption has never been observed, so behavioral controls remain poorly unders...
Published in: | Geology |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2013
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Subjects: | |
Online Access: | https://oro.open.ac.uk/35269/ https://oro.open.ac.uk/35269/1/G33647-Owen-edited.pdf https://doi.org/10.1130/G33647.1 |