Fluid-rock Equilibrium

Fluid-Rock Equilibrium is a geochemical state in which the mineral assemblages of a rock and the composition of an aqueous fluid phase coexist without net dissolution or precipitation, indicating thermodynamic equilibrium between the solid and fluid phases under specific temperature, pressure, and chemical potential conditions.

143

Publications

10.2K

Citations

437

Authors

211

Institutions

Publications per year

2017–2026

41

Authors

437

  1. HD
    Hassan Dehghanpour

    University of Alberta, Canada

    3 publications · 69 citations

    3

    h-index

  2. CE
    C. E. Manning

    University of California, Los Angeles, United States

    3 publications · 244 citations

    3

    h-index

  3. MS
    Mojtaba Seyyedi

    Heriot-Watt University, United Kingdom

    2 publications · 162 citations

    2

    h-index

  4. JW
    John W. Valley

    University of Wisconsin–Madison, United States

    2 publications · 43 citations

    2

    h-index

  5. JS
    Jane Selverstone

    University of New Mexico, United States

    2 publications · 58 citations

    2

    h-index

1–5 of 437

Venues

  1. Geochimica et Cosmochimica Acta

    14 publications · 829 citations

    13

    h-index

  2. Contributions to Mineralogy and Petrology

    9 publications · 363 citations

    9

    h-index

  3. Chemical Geology

    7 publications · 338 citations

    7

    h-index

  4. Geology

    7 publications · 858 citations

    7

    h-index

  5. Lithos

    6 publications · 126 citations

    6

    h-index

1–5