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...
| Κύριοι συγγραφείς: | , , , , |
|---|---|
| Μορφή: | Journal article |
| Έκδοση: |
Nature Research
2016
|