Magma Overpressure
Magma Overpressure is a mechanical condition in volcanic plumbing systems characterized by the excess pressure exerted by magma relative to the surrounding rock stress, resulting from processes such as magma injection, degassing, or crystallization-induced volume changes.
154
Publications
10.7K
Citations
462
Authors
233
Institutions
Publications per year
2017–2026
40
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233

Centre National de la Recherche Scientifique
Paris, France
18 h-index
42 publications
2.5K citations

University of Bristol
Bristol, United Kingdom
16 h-index
33 publications
2.2K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
13 h-index
39 publications
2.5K citations
Institut des Sciences de la Terre
Grenoble, France
9 h-index
15 publications
566 citations

Pennsylvania State University
State College, United States
8 h-index
26 publications
2.5K citations
Institut de Recherche pour le Développement
Marseille, France
8 h-index
13 publications
630 citations

Institut de physique du globe de Paris
Paris, France
7 h-index
19 publications
2.2K citations
Université Gustave Eiffel
Champs-sur-Marne, France
7 h-index
13 publications
498 citations
1–8 of 233
19 publications · 1.1K citations
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JGR · 16 publications · 1.3K citations
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16 publications · 1.4K citations
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14 publications · 1.4K citations
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13 publications · 424 citations
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