Magma Permeability

Magma Permeability is a physical property representing the ability of a porous or fractured magmatic system to allow the flow of fluids or melt through its interconnected pore network under a pressure gradient, distinguishing it from other transport properties by quantifying the ease of permeable flow within partially molten or volatile-saturated magmas.

135

Publications

10.6K

Citations

335

Authors

180

Institutions

Publications per year

2017–2026

31

Authors

335

  1. DB
    Donald B. Dingwell

    Ludwig-Maximilians-Universität München, Germany

    10 publications · 1.2K citations

    10

    h-index

  2. FB
    Fabian B. Wadsworth

    Ludwig-Maximilians-Universität München, Germany

    7 publications · 456 citations

    7

    h-index

  3. KV
    K. V. Cashman

    University of Oregon, United States

    6 publications · 1.1K citations

    6

    h-index

  4. MJ
    Michael J. Heap

    Université de Strasbourg, France

    6 publications · 607 citations

    6

    h-index

  5. YL
    Yan Lavallée

    University of Liverpool, United Kingdom

    6 publications · 561 citations

    6

    h-index

1–5 of 335

Venues

  1. Journal of Volcanology and Geothermal Research

    20 publications · 1.5K citations

    19

    h-index

  2. Earth and Planetary Science Letters

    15 publications · 1.1K citations

    14

    h-index

  3. Geophysical Research Letters

    13 publications · 688 citations

    13

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 11 publications · 1.5K citations

    11

    h-index

  5. Bulletin of Volcanology

    10 publications · 986 citations

    10

    h-index

1–5