Magma Permeability
Magma Permeability is a physical property representing the ability of a porous or fractured magmatic system to allow the flow of fluids or melt through its interconnected pore network under a pressure gradient, distinguishing it from other transport properties by quantifying the ease of permeable flow within partially molten or volatile-saturated magmas.
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335
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2017–2026
31
135
David R. Scott, D. J. Stevenson · Journal of Geophysical Research Atmospheres · 1986 · 364 citations · Full text
Review of Microstructural Evidence of Magmatic and Solid-State Flow
R. H. Vernon · Visual Geosciences · 2000 · 281 citations
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Ludwig-Maximilians-Universität München
Munich, Germany
13 h-index
43 publications
3.6K citations

Centre National de la Recherche Scientifique
Paris, France
13 h-index
31 publications
2.7K citations

University of Bristol
Bristol, United Kingdom
12 h-index
20 publications
1.6K citations

University of Liverpool
Liverpool, United Kingdom
10 h-index
21 publications
1.5K citations
Planetary Science Institute
Tucson, United States
7 h-index
9 publications
1.3K citations
Université de Strasbourg
Strasbourg, France
7 h-index
16 publications
1.7K citations
University of Oregon
Eugene, United States
6 h-index
9 publications
1.8K citations
ETH Zurich
Zurich, Switzerland
6 h-index
10 publications
568 citations
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20 publications · 1.5K citations
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15 publications · 1.1K citations
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13 publications · 688 citations
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JGR · 11 publications · 1.5K citations
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10 publications · 986 citations
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