Mud Volcanism

Mud Volcanism is a geological process characterized by the extrusion of mud, water, and gases from subsurface formations to the seafloor, distinguished from magmatic volcanism by the absence of molten rock and driven primarily by overpressured fluids and tectonic or sedimentary loading in marine environments.

340

Publications

19.6K

Citations

1.1K

Authors

439

Institutions

Publications per year

2017–2026

68

Variants

Sedimentary Volcanism

Authors

1.1K

  1. MI
    M.K. Ivanov

    Lomonosov Moscow State University, Russia

    13 publications · 996 citations

    13

    h-index

  2. AK
    Achim Kopf

    University of Bremen, Germany

    13 publications · 1.4K citations

    12

    h-index

  3. GB
    Gerhard Bohrmann

    University of Bremen, Germany

    12 publications · 661 citations

    12

    h-index

  4. JF
    Jean‐Paul Foucher

    Ifremer, France

    11 publications · 1.1K citations

    11

    h-index

  5. JW
    John Woodside

    Vrije Universiteit Amsterdam, Netherlands

    10 publications · 584 citations

    10

    h-index

1–5 of 1.1K

Venues

  1. Marine Geology

    27 publications · 2.4K citations

    22

    h-index

  2. Marine and Petroleum Geology

    22 publications · 1.3K citations

    19

    h-index

  3. Geo-Marine Letters

    19 publications · 1.2K citations

    17

    h-index

  4. Geology

    11 publications · 1.2K citations

    11

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 10 publications · 1.1K citations

    10

    h-index

1–5