Mineral Equilibrium

Mineral Equilibrium is a theoretical state within mineral paragenesis denoting the condition in which the assemblage of coexisting minerals in a rock system remains stable over time, with no net change in mineral composition or phase distribution under constant physical and chemical conditions.

121

Publications

8K

Citations

257

Authors

140

Institutions

Publications per year

2017–2026

19

Authors

257

  1. TT
    Toshiaki Tsunogae

    University of Tsukuba, Japan

    8 publications · 183 citations

    8

    h-index

  2. RP
    Roger Powell

    The University of Melbourne, Australia

    6 publications · 510 citations

    6

    h-index

  3. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    5 publications · 131 citations

    5

    h-index

  4. TJ
    T. J. B. Holland

    University of Cambridge, United Kingdom

    5 publications · 525 citations

    5

    h-index

  5. SK
    Surendra K. Saxena

    Florida International University, United States

    4 publications · 115 citations

    4

    h-index

1–5 of 257

Venues

  1. American Mineralogist

    14 publications · 763 citations

    13

    h-index

  2. Contributions to Mineralogy and Petrology

    12 publications · 1.2K citations

    12

    h-index

  3. American Journal of Science

    10 publications · 880 citations

    10

    h-index

  4. Geochimica et Cosmochimica Acta

    7 publications · 799 citations

    7

    h-index

  5. Journal of Metamorphic Geology

    5 publications · 308 citations

    5

    h-index

1–5