Closed-system Magmatic Processes

Closed-System Magmatic Processes is a magmatic differentiation process in which the chemical and isotopic evolution of a magma occurs without significant exchange of material with its surrounding environment, distinguished from open-system processes by the isolation of the magma body during crystallization and differentiation.

18

Publications

1.9K

Citations

72

Authors

43

Institutions

Publications per year

2017–2026

4

Authors

72

  1. CA
    Christoph A. Heinrich

    ETH Zurich, Switzerland

    2 publications · 143 citations

    2

    h-index

  2. NS
    N. S. Stevens

    Montserrat Volcano Observatory, Montserrat

    1 publications · 158 citations

    1

    h-index

  3. BG
    Bronislav Gongalsky

    Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry, Russia

    1 publications · 45 citations

    1

    h-index

  4. DL
    Dominique Lattard

    Heidelberg University, Germany

    1 publications · 12 citations

    1

    h-index

  5. MC
    Madeleine C. S. Humphreys

    Durham University, United Kingdom

    1 publications · 16 citations

    1

    h-index

1–5 of 72

Venues

  1. Economic Geology

    3 publications · 197 citations

    3

    h-index

  2. Geochimica et Cosmochimica Acta

    2 publications · 408 citations

    2

    h-index

  3. Meteoritics and Planetary Science

    2 publications · 75 citations

    2

    h-index

  4. Geophysical Research Letters

    1 publications · 158 citations

    1

    h-index

  5. Annual Review of Earth and Planetary Sciences

    1 publications · 83 citations

    1

    h-index

1–5