Conduit Seismicity

Conduit Seismicity is a type of volcanic seismic signal characterized by high-frequency earthquakes originating within the volcanic conduit, distinguished from other volcanic seismic phenomena by its spatial localization to the active magma pathway and its association with brittle failure processes during magma ascent.

71

Publications

4K

Citations

235

Authors

99

Institutions

Publications per year

2017–2026

16

Authors

235

  1. IK
    Iván Koulakov

    Institute of Petroleum Geology and Geophysics, Russia

    5 publications · 171 citations

    5

    h-index

  2. BC
    Bernard Chouet

    United States Geological Survey, United States

    4 publications · 265 citations

    4

    h-index

  3. PD
    Phillip Dawson

    United States Geological Survey, United States

    3 publications · 128 citations

    3

    h-index

  4. ME
    M. E. West

    University of Alaska Fairbanks, United States

    3 publications · 90 citations

    3

    h-index

  5. SE
    Sami El Khrepy

    King Saud University, Saudi Arabia

    3 publications · 98 citations

    3

    h-index

1–5 of 235

Venues

  1. Geophysical Research Letters

    14 publications · 856 citations

    14

    h-index

  2. Journal of Geophysical Research Solid Earth

    10 publications · 208 citations

    10

    h-index

  3. Journal of Volcanology and Geothermal Research

    9 publications · 357 citations

    9

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 7 publications · 816 citations

    7

    h-index

  5. Geology

    3 publications · 141 citations

    3

    h-index

1–5