Partial Melting

Partial Melting is a magmatic process in which a polycrystalline rock undergoes incongruent melting such that only certain mineral phases melt at lower temperatures, producing a silicate melt compositionally distinct from the bulk rock while leaving a refractory residue.

9.8K

Publications

730.7K

Citations

18.2K

Authors

3K

Institutions

Publications per year

2017–2026

1.7K

Authors

18.2K

  1. DB
    Donald B. Dingwell

    Ludwig-Maximilians-Universität München, Germany

    82 publications · 7.1K citations

    46

    h-index

  2. PJ
    Peter J. Wyllie

    University of Chicago, United States

    65 publications · 6.6K citations

    46

    h-index

  3. HB
    Harald Behrens

    Leibniz University Hannover, Germany

    65 publications · 5.3K citations

    43

    h-index

  4. FH
    François Holtz

    Leibniz University Hannover, Germany

    64 publications · 5.8K citations

    42

    h-index

  5. TL
    T. L. Grove

    Massachusetts Institute of Technology, United States

    43 publications · 6.2K citations

    37

    h-index

1–5 of 18.2K

Venues

  1. Geochimica et Cosmochimica Acta

    518 publications · 49.1K citations

    126

    h-index

  2. Journal of Petrology

    406 publications · 62.9K citations

    126

    h-index

  3. Earth and Planetary Science Letters

    438 publications · 48.6K citations

    122

    h-index

  4. Contributions to Mineralogy and Petrology

    448 publications · 49.5K citations

    117

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 343 publications · 43K citations

    116

    h-index

1–5