Hydrous Magmatism

Hydrous Magmatism is a type of magmatic process occurring in plutonic environments characterized by the significant presence and influence of water-rich fluids on magma generation, evolution, and crystallization.

628

Publications

58.4K

Citations

1.8K

Authors

588

Institutions

Publications per year

2017–2026

148

Authors

1.8K

  1. JB
    Jon Blundy

    University of Bristol, United Kingdom

    11 publications · 3.5K citations

    11

    h-index

  2. EO
    Eiji Ohtani

    Tohoku University, Japan

    10 publications · 1.2K citations

    10

    h-index

  3. EH
    E. H. Hauri

    Carnegie Institution for Science, United States

    10 publications · 1.9K citations

    10

    h-index

  4. TL
    T. L. Grove

    Massachusetts Institute of Technology, United States

    10 publications · 1.8K citations

    10

    h-index

  5. DJ
    D. J. Frost

    University of Bayreuth, Germany

    8 publications · 845 citations

    8

    h-index

1–5 of 1.8K

Venues

  1. Earth and Planetary Science Letters

    43 publications · 4.3K citations

    33

    h-index

  2. Journal of Petrology

    36 publications · 6.5K citations

    30

    h-index

  3. Contributions to Mineralogy and Petrology

    41 publications · 4.1K citations

    29

    h-index

  4. Geochimica et Cosmochimica Acta

    29 publications · 2.2K citations

    25

    h-index

  5. Geophysical Research Letters

    33 publications · 2.5K citations

    25

    h-index

1–5