Moho Discontinuity

The "Moho Discontinuity" is a seismological boundary surface within the Earth's interior that demarcates the base of the crust and the onset of the mantle, distinguished by an abrupt increase in seismic wave velocity due to a change in rock composition and density.

302

Publications

16.3K

Citations

931

Authors

324

Institutions

Publications per year

2017–2026

49

Variants

MohoMohorovičić Discontinuity

Authors

931

  1. RK
    R. Kind

    GFZ Helmholtz Centre for Geosciences, Germany

    9 publications · 1K citations

    10

    h-index

  2. XY
    Xiaohui Yuan

    GFZ Helmholtz Centre for Geosciences, Germany

    8 publications · 737 citations

    8

    h-index

  3. ME
    Mehdi Eshagh

    KTH Royal Institute of Technology, Sweden

    5 publications · 88 citations

    5

    h-index

  4. ZZ
    Zhongjie Zhang

    Chinese Academy of Sciences, China

    5 publications · 435 citations

    5

    h-index

  5. MG
    M. Grad

    University of Warsaw, Poland

    5 publications · 202 citations

    5

    h-index

1–5 of 931

Venues

  1. Geophysical Journal International

    GJI · 43 publications · 2.1K citations

    28

    h-index

  2. Tectonophysics

    28 publications · 1.5K citations

    25

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 24 publications · 2.1K citations

    20

    h-index

  4. Geophysical Research Letters

    20 publications · 1.2K citations

    18

    h-index

  5. Bulletin of the Seismological Society of America

    BSSA · 16 publications · 979 citations

    15

    h-index

1–5