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

Authors

263

  1. EO
    Eiji Ohtani

    Tohoku University, Japan

    15 publications · 1.4K citations

    15

    h-index

  2. AS
    Akio Suzuki

    Tohoku University, Japan

    6 publications · 526 citations

    6

    h-index

  3. JT
    Jun Tsuchiya

    Ehime University, Japan

    6 publications · 314 citations

    6

    h-index

  4. NH
    Naohisa Hirao

    Japan Synchrotron Radiation Research Institute, Japan

    5 publications · 469 citations

    5

    h-index

  5. TK
    Tadashi Kondo

    National Cancer Research Institute, United Kingdom

    5 publications · 352 citations

    5

    h-index

1–5 of 263

Venues

  1. Geophysical Research Letters

    11 publications · 743 citations

    11

    h-index

  2. Contributions to Mineralogy and Petrology

    8 publications · 376 citations

    8

    h-index

  3. American Mineralogist

    9 publications · 717 citations

    8

    h-index

  4. Earth and Planetary Science Letters

    7 publications · 538 citations

    7

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 6 publications · 1K citations

    6

    h-index

1–5