Open-system Magmatic Evolution
Open-System Magmatic Evolution is a magmatic process model in which magma composition and thermal state evolve through the dynamic exchange of material and energy with surrounding crustal environments, distinguishing it from closed-system models by incorporating external inputs such as assimilation, magma mixing, and recharge.
56
Publications
4.4K
Citations
181
Authors
108
Institutions
Publications per year
2017–2026
9
Parents
56
1–5 of 56
181
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h-index
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108
University of California, Santa Barbara
Santa Barbara, United States
5 h-index
11 publications
1.1K citations
Southern Methodist University
Dallas, United States
5 h-index
9 publications
681 citations

Central Washington University
Ellensburg, United States
5 h-index
9 publications
847 citations

University of Hawaii System
Honolulu, United States
4 h-index
6 publications
275 citations

Rice University
Houston, United States
3 h-index
4 publications
84 citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
3 h-index
7 publications
414 citations
Oregon State University
Corvallis, United States
3 h-index
3 publications
134 citations

Massey University
Palmerston North, New Zealand
2 h-index
2 publications
153 citations
1–8 of 108
13 publications · 1.7K citations
13
h-index
6 publications · 532 citations
6
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6 publications · 378 citations
6
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5 publications · 246 citations
5
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3 publications · 81 citations
3
h-index
1–5