Open-system Magmatic Evolution

Open-System Magmatic Evolution is a magmatic process model in which magma composition and thermal state evolve through the dynamic exchange of material and energy with surrounding crustal environments, distinguishing it from closed-system models by incorporating external inputs such as assimilation, magma mixing, and recharge.

56

Publications

4.4K

Citations

181

Authors

108

Institutions

Publications per year

2017–2026

9

Authors

181

  1. FJ
    Frank J. Spera

    University of California, Santa Barbara, United States

    6 publications · 911 citations

    6

    h-index

  2. WA
    Wendy A. Bohrson

    Central Washington University, United States

    5 publications · 675 citations

    5

    h-index

  3. WP
    William P. Leeman

    Rice University, United States

    3 publications · 73 citations

    3

    h-index

  4. GA
    Guy A. Brown

    University of California, Santa Barbara, United States

    3 publications · 325 citations

    3

    h-index

  5. MA
    M. A. Dungan

    University of Geneva, Switzerland

    3 publications · 154 citations

    3

    h-index

1–5 of 181

Venues

  1. Journal of Petrology

    13 publications · 1.7K citations

    13

    h-index

  2. Lithos

    6 publications · 532 citations

    6

    h-index

  3. Contributions to Mineralogy and Petrology

    6 publications · 378 citations

    6

    h-index

  4. Journal of Volcanology and Geothermal Research

    5 publications · 246 citations

    5

    h-index

  5. Chemical Geology

    3 publications · 81 citations

    3

    h-index

1–5