Closed-system Magmatic Evolution

Closed-System Magmatic Evolution is a theoretical framework in igneous petrology that models the chemical and mineralogical differentiation of magma through fractional crystallization without addition or removal of materials, distinguishing it from open-system processes by assuming thermodynamic isolation of the evolving melt.

38

Publications

2.6K

Citations

149

Authors

85

Institutions

Publications per year

2017–2026

6

Authors

149

  1. MJ
    M. J. Rutherford

    Brown University, United States

    2 publications · 145 citations

    2

    h-index

  2. CD
    Carol D. Frost

    University of Wyoming, United States

    1 publications · 121 citations

    1

    h-index

  3. MD
    Matthew D. Hacker

    Oregon State University, United States

    1 publications · 35 citations

    1

    h-index

  4. JW
    J. W. Head

    Brown University, United States

    1 publications · 46 citations

    1

    h-index

  5. LL
    Lei Liu

    Nanjing University, China

    1 publications · 61 citations

    1

    h-index

1–5 of 149

Venues

  1. Journal of Petrology

    7 publications · 488 citations

    7

    h-index

  2. Lithos

    3 publications · 384 citations

    3

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 3 publications · 290 citations

    3

    h-index

  4. Contributions to Mineralogy and Petrology

    3 publications · 283 citations

    3

    h-index

  5. American Mineralogist

    2 publications · 70 citations

    2

    h-index

1–5