Closed-system Magmatic Evolution
Closed-System Magmatic Evolution is a theoretical framework in igneous petrology that models the chemical and mineralogical differentiation of magma through fractional crystallization without addition or removal of materials, distinguishing it from open-system processes by assuming thermodynamic isolation of the evolving melt.
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2.6K
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149
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85
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2017–2026
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Scott E. Bryan, Luca Ferrari, Peter W. Reiners et al. · Journal of Petrology · 2007 · 124 citations · Full text
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University of Bristol
Bristol, United Kingdom
3 h-index
12 publications
1.7K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
3 h-index
7 publications
531 citations
University of Tennessee at Knoxville
Knoxville, United States
2 h-index
4 publications
178 citations

The Open University
Milton Keynes, United Kingdom
2 h-index
2 publications
210 citations

Université Clermont Auvergne
Clermont-Ferrand, France
2 h-index
2 publications
170 citations
Lancaster University
Lancaster, United Kingdom
2 h-index
4 publications
520 citations
Brown University
Providence, United States
2 h-index
4 publications
237 citations

British Geological Survey
Nottingham, United Kingdom
2 h-index
5 publications
759 citations
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7 publications · 488 citations
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3 publications · 384 citations
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JGR · 3 publications · 290 citations
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3 publications · 283 citations
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2 publications · 70 citations
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