Flux Melting
Flux Melting is a process of partial melting in magma genesis wherein the addition of volatile components, such as water or carbon dioxide, to a mineral assemblage reduces the solidus temperature of the rock, thereby enabling melt formation at lower temperatures than would occur under dry conditions.
51
Publications
3.2K
Citations
180
Authors
95
Institutions
Publications per year
2017–2026
6
Variants
Flux-induced Melting
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1–5 of 51
180
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Rutgers, The State University of New Jersey, United States
2 publications · 159 citations
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2
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2
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2
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1–5 of 180
95

Akita Prefectural University
Akita, Japan
3 h-index
5 publications
127 citations

Tohoku University
Sendai, Japan
3 h-index
7 publications
245 citations

Massey University
Palmerston North, New Zealand
2 h-index
2 publications
135 citations
Leiden University
Leiden, The Netherlands
2 h-index
5 publications
972 citations
Los Alamos National Laboratory
Los Alamos, United States
2 h-index
4 publications
678 citations
University of Cambridge
Cambridge, United Kingdom
2 h-index
7 publications
635 citations

University of Birmingham
Birmingham, United Kingdom
2 h-index
4 publications
1.4K citations
Rutgers, The State University of New Jersey
New Brunswick, United States
2 h-index
5 publications
369 citations
1–8 of 95
PRB · 7 publications · 298 citations
7
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4 publications · 398 citations
4
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2 publications · 40 citations
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2 publications · 35 citations
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2 publications · 83 citations
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