Volatile Exsolution
Volatile Exsolution is the process whereby dissolved volatiles, primarily water and carbon dioxide, partition from a silicate melt into a separate gas phase due to decreasing pressure during magma ascent, constituting a fundamental mechanism in volcanic degassing within volcanic plumbing systems.
75
Publications
5.3K
Citations
258
Authors
151
Institutions
Publications per year
2017–2026
27
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1–5 of 75
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151
University of Cambridge
Cambridge, United Kingdom
6 h-index
11 publications
1.3K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
5 h-index
8 publications
729 citations
University of Colorado Boulder
Boulder, United States
4 h-index
8 publications
134 citations
Planetary Science Institute
Tucson, United States
4 h-index
5 publications
606 citations

Australian National University
Canberra, Australia
4 h-index
7 publications
635 citations
University of Oregon
Eugene, United States
4 h-index
6 publications
662 citations
Brown University
Providence, United States
3 h-index
4 publications
145 citations
Arizona State University
Tempe, United States
3 h-index
7 publications
307 citations
1–8 of 151
9 publications · 412 citations
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5 publications · 199 citations
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JGR · 4 publications · 315 citations
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4 publications · 273 citations
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3 publications · 682 citations
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