Near-surface Attenuation

Near-Surface Attenuation is a seismic attenuation phenomenon characterized by the reduction in amplitude and alteration of frequency content of seismic waves as they propagate through the uppermost layers of the Earth's crust, distinguished from deeper attenuation processes by its strong dependence on shallow subsurface heterogeneities, unconsolidated materials, and near-surface geological conditions.

93

Publications

3.2K

Citations

254

Authors

129

Institutions

Publications per year

2017–2026

14

Authors

254

  1. DB
    Dino Bindi

    GFZ Helmholtz Centre for Geosciences, Germany

    3 publications · 108 citations

    3

    h-index

  2. ED
    Edoardo Del Pezzo

    Istituto Nazionale di Geofisica e Vulcanologia, Italy

    3 publications · 133 citations

    3

    h-index

  3. TH
    Toshihiko HASHIDA

    The University of Tokyo, Japan

    3 publications · 116 citations

    3

    h-index

  4. SC
    Sean C. Solomon

    Carnegie Institution for Science, United States

    2 publications · 101 citations

    2

    h-index

  5. GL
    Guofa Li

    China University of Petroleum, Beijing, China

    2 publications · 28 citations

    2

    h-index

1–5 of 254

Venues

  1. Bulletin of the Seismological Society of America

    BSSA · 14 publications · 733 citations

    13

    h-index

  2. Physics of The Earth and Planetary Interiors

    9 publications · 244 citations

    9

    h-index

  3. Geophysical Journal International

    GJI · 6 publications · 199 citations

    6

    h-index

  4. Soil Dynamics and Earthquake Engineering

    5 publications · 208 citations

    5

    h-index

  5. Tectonophysics

    5 publications · 250 citations

    5

    h-index

1–5