Coda Wave Attenuation

Coda Wave Attenuation is a seismic attenuation measurement method that quantifies the temporal decay rate of coda wave amplitudes following the direct seismic arrivals, distinguishing itself by its reliance on scattered waves trapped in the Earth’s heterogeneities to infer regional subsurface attenuation properties.

233

Publications

12.6K

Citations

495

Authors

212

Institutions

Publications per year

2017–2026

38

Authors

495

  1. SM
    S. Mukhopadhyay

    Indian Institute of Technology Roorkee, India

    10 publications · 352 citations

    10

    h-index

  2. ED
    Edoardo Del Pezzo

    Istituto Nazionale di Geofisica e Vulcanologia, Italy

    9 publications · 444 citations

    9

    h-index

  3. HR
    Habib Rahimi

    University of Tehran, Iran

    8 publications · 241 citations

    8

    h-index

  4. JA
    J. A. Cañas

    Universitat Politècnica de Catalunya, Spain

    8 publications · 275 citations

    8

    h-index

  5. JM
    Jesús M. Ibáñez

    Universidad de Granada, Spain

    7 publications · 351 citations

    7

    h-index

1–5 of 495

Venues

  1. Bulletin of the Seismological Society of America

    BSSA · 52 publications · 3K citations

    31

    h-index

  2. Geophysical Journal International

    GJI · 41 publications · 1.8K citations

    26

    h-index

  3. Pure and Applied Geophysics

    PAGEOPH · 22 publications · 637 citations

    16

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 18 publications · 3.5K citations

    15

    h-index

  5. Physics of The Earth and Planetary Interiors

    15 publications · 766 citations

    15

    h-index

1–5