The origin of magma encountered during drilling of geothermal well KJ-39, Krafla, Iceland and the relationship with the nearby IDDP-1 magma
In July 2008, well KJ-39 encountered magma at 2571 metres below the surface while drilling into the geothermal system within the Krafla central volcano, north-eastern Iceland. The magma was returned to the surface as quenched glass along with a resorbed mineral assemblage consisting of bytownite wit...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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University of Canterbury
2020
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| Online Access: | https://dx.doi.org/10.26021/10115 https://ir.canterbury.ac.nz/handle/10092/101052 |