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...

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Bibliographic Details
Published in:Geology
Main Authors: Owen, Jacqueline, Tuffen, Hugh, McGarvie, Dave
Format: Article in Journal/Newspaper
Language:unknown
Published: 2013
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