Open-system Magmatic Processes
Open-System Magmatic Processes is a magmatic differentiation process in which the magma interacts with its surrounding country rock or external materials through mass and energy exchange, thereby altering its chemical and isotopic composition during crystallization.
49
Publications
4.6K
Citations
145
Authors
91
Institutions
Publications per year
2017–2026
6
Parents
49
1–5 of 49
145
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h-index
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91

Central Washington University
Ellensburg, United States
5 h-index
8 publications
582 citations
University of California, Santa Barbara
Santa Barbara, United States
5 h-index
10 publications
817 citations

The Open University
Milton Keynes, United Kingdom
4 h-index
6 publications
1.1K citations
Oregon State University
Corvallis, United States
3 h-index
3 publications
164 citations

Durham University
Durham, United Kingdom
3 h-index
8 publications
2.1K citations
Earth and Space Research
Seattle, United States
3 h-index
6 publications
728 citations
Southern Methodist University
Dallas, United States
3 h-index
4 publications
177 citations
University of Washington
Seattle, United States
3 h-index
6 publications
728 citations
1–8 of 91
11 publications · 1.7K citations
11
h-index
JGR · 4 publications · 257 citations
4
h-index
3 publications · 139 citations
3
h-index
3 publications · 244 citations
3
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3 publications · 148 citations
3
h-index
1–5