Magma Overpressure

Magma Overpressure is a mechanical condition in volcanic plumbing systems characterized by the excess pressure exerted by magma relative to the surrounding rock stress, resulting from processes such as magma injection, degassing, or crystallization-induced volume changes.

154

Publications

10.7K

Citations

462

Authors

233

Institutions

Publications per year

2017–2026

40

Authors

462

  1. RS
    R. S. J. Sparks

    University of Bristol, United Kingdom

    9 publications · 825 citations

    9

    h-index

  2. BV
    B. Voight

    Pennsylvania State University, United States

    8 publications · 897 citations

    8

    h-index

  3. DE
    Derek Elsworth

    Pennsylvania State University, United States

    7 publications · 803 citations

    7

    h-index

  4. AB
    A. B. Clarke

    Arizona State University, United States

    6 publications · 522 citations

    6

    h-index

  5. ÁG
    Ágúst Guðmundsson

    Royal Holloway University of London, United Kingdom

    6 publications · 934 citations

    6

    h-index

1–5 of 462

Venues

  1. Geophysical Research Letters

    19 publications · 1.1K citations

    18

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 16 publications · 1.3K citations

    16

    h-index

  3. Journal of Volcanology and Geothermal Research

    16 publications · 1.4K citations

    15

    h-index

  4. Earth and Planetary Science Letters

    14 publications · 1.4K citations

    13

    h-index

  5. Journal of Geophysical Research Solid Earth

    13 publications · 424 citations

    12

    h-index

1–5