Caldera-forming Currents

Caldera-Forming Currents is a type of pyroclastic density current distinguished by its exceptional volume, mobility, and sustained eruptive flux, capable of inducing magma chamber roof collapse and subsequent caldera formation through the generation of large-scale, ignimbrite-depositing flows.

54

Publications

2.5K

Citations

180

Authors

101

Institutions

Publications per year

2017–2026

11

Authors

180

  1. BK
    Ben Kennedy

    University of Canterbury, New Zealand

    3 publications · 156 citations

    3

    h-index

  2. JS
    John Stix

    McGill University, Canada

    3 publications · 190 citations

    3

    h-index

  3. GG
    Guido Giordano

    Roma Tre University, Italy

    2 publications · 38 citations

    2

    h-index

  4. RC
    Raffaello Cioni

    Istituto Nazionale di Geofisica e Vulcanologia, Italy

    2 publications · 250 citations

    2

    h-index

  5. WM
    W.U. Mueller

    Université du Québec à Chicoutimi, Canada

    2 publications · 141 citations

    2

    h-index

1–5 of 180

Venues

  1. Bulletin of Volcanology

    14 publications · 781 citations

    14

    h-index

  2. Journal of Volcanology and Geothermal Research

    17 publications · 723 citations

    14

    h-index

  3. Earth and Planetary Science Letters

    4 publications · 133 citations

    4

    h-index

  4. Sedimentary Geology

    2 publications · 35 citations

    2

    h-index

  5. Geological Society of America Bulletin

    2 publications · 63 citations

    2

    h-index

1–5