Magmas near the critical degassing pressure drive volcanic unrest towards a critical state
Magmas may migrate through hydrothermal fluids, but magma-hydrothermal interactions are poorly understood. Here, Chiodini et al. use physical and volatile models showing that at a critical degassing pressure the release of magmatic gases can heat hydrothermal fluids triggering deformation leading to...
Main Authors: | , , , , , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Nature Publishing Group
2016-12-01
|
Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/ncomms13712 |