Closed-system Magmatic Processes
Closed-System Magmatic Processes is a magmatic differentiation process in which the chemical and isotopic evolution of a magma occurs without significant exchange of material with its surrounding environment, distinguished from open-system processes by the isolation of the magma body during crystallization and differentiation.
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2017–2026
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Magmatic Processes: Physicochemical Principles
Sieger R. van der Laan · Earth-Science Reviews · 1988 · 407 citations
Magmatic processes: Physicochemical principles
S. A. Morse · Geochimica et Cosmochimica Acta · 1988 · 392 citations
Simon Large, Albrecht von Quadt, Jörn‐Frederik Wotzlaw et al. · Economic Geology · 2018 · 99 citations · Full text
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Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry, Russia
1 publications · 45 citations
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École Polytechnique Fédérale de Lausanne
Lausanne, Switzerland
2 h-index
7 publications
583 citations
University of Maryland, College Park
College Park, United States
1 h-index
3 publications
132 citations
University of California, Davis
Davis, United States
1 h-index
1 publications
65 citations
Planetary Science Institute
Tucson, United States
1 h-index
4 publications
260 citations
University of Tennessee at Knoxville
Knoxville, United States
1 h-index
3 publications
195 citations
University of Zurich
Zurich, Switzerland
1 h-index
1 publications
99 citations

University of Zagreb
Zagreb, Croatia
1 h-index
2 publications
154 citations
Oregon State University
Corvallis, United States
1 h-index
1 publications
40 citations
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3 publications · 197 citations
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2 publications · 408 citations
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2 publications · 75 citations
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1 publications · 158 citations
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