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Modelling the rapid near-surface expansion of gas slugs in low-viscosity magmas
2008
Geological Society Special Publication
Preserved Fulltext
Experimental insights suggest that meniscus oscillation can only be a source mechanism for volcano-acoustic signals for non-explosive events. We suggest that the explosive source mechanism is a rapid pressure increase driven by slug expansion, and that any following oscillations represent a system-specific response.
doi:10.1144/sp307.9
fatcat:x4on56cyrng5vep3vzj3uri4ui