Vesiculation of rhyolite magma in the IDDP-1 borehole at Krafla, Iceland
In 2009 the IDDP-1 borehole at Krafla, Iceland unexpectedly intersected rhyolitic magma at 2.1 km depth [1,2], providing unprecedented opportunities to investigate silicic melt formation and storage, and potential for powerful geothermal energy production. A key objective is to constrain the nature...
Main Authors: | , , , , , |
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Format: | Text |
Language: | unknown |
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European Geosciences Union
2016
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Online Access: | https://eprints.lancs.ac.uk/id/eprint/83119/ |