Hydrous Phase Stability
Hydrous Phase Stability is a thermodynamic construct in experimental petrology that defines the pressure-temperature-hydrogen fugacity conditions under which hydrous minerals remain stable relative to their anhydrous breakdown products during metamorphic and igneous processes.
92
Publications
7.4K
Citations
263
Authors
126
Institutions
Publications per year
2017–2026
14
Parents
92
Plagioclase-melt equilibria in hydrous systems.
Todd B. Housh, James F. Luhr · American Mineralogist · 1991 · 272 citations
1–5 of 92
263
15
h-index
6
h-index
6
h-index
5
h-index
5
h-index
1–5 of 263
126

Tohoku University
Sendai, Japan
13 h-index
48 publications
4.5K citations
Ehime University
Matsuyama, Japan
9 h-index
13 publications
547 citations
University of Bayreuth
Bayreuth, Germany
8 h-index
13 publications
1.8K citations
University of Chicago
Chicago, United States
6 h-index
10 publications
420 citations

Carnegie Institution for Science
Washington, United States
6 h-index
11 publications
681 citations
Tokyo Institute of Technology
Tokyo, Japan
5 h-index
10 publications
851 citations

Chinese Academy of Sciences
Beijing, China
5 h-index
6 publications
787 citations
Geophysical Laboratory
Washington, United States
5 h-index
9 publications
387 citations
1–8 of 126
11 publications · 743 citations
11
h-index
8 publications · 376 citations
8
h-index
9 publications · 717 citations
8
h-index
7 publications · 538 citations
7
h-index
JGR · 6 publications · 1K citations
6
h-index
1–5