Surface-wave Magnitude

Surface-Wave Magnitude is a quantitative measure of an earthquake's size, belonging to the class of magnitude scales, that is distinguished by its derivation from the amplitude and period of surface waves propagating along the Earth's crust at distant seismograph stations.

137

Publications

10.4K

Citations

271

Authors

132

Institutions

Publications per year

2017–2026

14

Variants

MsSurface Wave Magnitude

Authors

271

  1. NN
    N. N. Ambraseys

    Imperial College London, United Kingdom

    7 publications · 757 citations

    7

    h-index

  2. BG
    B. Gutenberg

    California Institute of Technology, United States

    5 publications · 2.1K citations

    5

    h-index

  3. HK
    Hiroo Kanamori

    California Institute of Technology, United States

    5 publications · 485 citations

    5

    h-index

  4. JL
    J. L. Bonner

    Southern Methodist University, United States

    4 publications · 122 citations

    4

    h-index

  5. BC
    B. C. Papazachos

    Aristotle University of Thessaloniki, Greece

    4 publications · 232 citations

    4

    h-index

1–5 of 271

Venues

  1. Bulletin of the Seismological Society of America

    BSSA · 48 publications · 3.8K citations

    31

    h-index

  2. Geophysical Journal International

    GJI · 15 publications · 859 citations

    12

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 7 publications · 833 citations

    7

    h-index

  4. Science

    5 publications · 376 citations

    5

    h-index

  5. Earthquake Engineering & Structural Dynamics

    4 publications · 176 citations

    4

    h-index

1–5