Critical Refraction

Critical Refraction is a seismic refraction phenomenon in which a refracted wave propagates along the interface between two geological layers at the critical angle, resulting in the minimum angle of incidence at which the refracted ray travels parallel to the boundary, thereby enabling the detection of subsurface layer velocities and depths through first-arrival travel-time analysis.

32

Publications

1.7K

Citations

123

Authors

48

Institutions

Publications per year

2017–2026

10

Variants

Head WaveHead Waves

Authors

123

  1. PH
    Peng He

    Harbin Institute of Technology, China

    2 publications · 31 citations

    2

    h-index

  2. WM
    Wenbing Miao

    Harbin Institute of Technology, China

    2 publications · 31 citations

    2

    h-index

  3. SD
    Shiyun Dong

    Harbin Institute of Technology, China

    2 publications · 31 citations

    2

    h-index

  4. BL
    Bin Liu

    Harbin Institute of Technology, China

    2 publications · 31 citations

    2

    h-index

  5. PN
    P. N. S. O’Brien

    BP (United Kingdom), United Kingdom

    2 publications · 28 citations

    2

    h-index

1–5 of 123

Venues

  1. Geophysics

    3 publications · 141 citations

    3

    h-index

  2. The Journal of the Acoustical Society of America

    JASA · 2 publications · 167 citations

    2

    h-index

  3. Geophysical Journal International

    GJI · 2 publications · 49 citations

    2

    h-index

  4. Geophysical Prospecting

    2 publications · 28 citations

    2

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 1 publications · 183 citations

    1

    h-index

1–5