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  1. Explosive subglacial rhyolitic eruptions in Iceland are fuelled by high magmatic H2O and closed system degassing.

    Owen, J., Tuffen, H. & McGarvie, D. W., 02/2013, In: Geology. 41, 2, p. 251-254 4 p.

    Research output: Contribution to Journal/MagazineJournal articlepeer-review