Late-stage volatile saturation as a potential trigger for explosive volcanic eruptions
Magma reservoirs are thought to grow relatively slowly, assembling incrementally under volatile-saturated conditions. Eruptions may be triggered by injections of volatile-rich melt, or generation of over-pressure due to protracted crystallization. Here, we analyse fluorine, chlorine and water in apa...
| Päätekijät: | , , , , |
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| Aineistotyyppi: | Journal article |
| Julkaistu: |
Nature Research
2016
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