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Oxide nanolitisation-induced melt iron extraction causes viscosity jumps and enhanced explosivity in silicic magma

Oxide nanolites crystallisation in natural magma increases melt, and hence bulk magma viscosity mainly due to iron extraction. This increase can be sufficient to drive magma fragmentation depending on magma degassing and ascent dynamics.

Francisco Cáceres
Kai-Uwe Hess
Donald B. Dingwell
ResearchOpen Access19 Jan 2024
Nature Communications

Volume: 15, P: 1-11

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Oxide nanolitisation-induced melt iron extraction causes viscosity jumps and enhanced explosivity in silicic magma

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