Upper Mantle Attenuation

Upper Mantle Attenuation is a geophysical phenomenon within seismic attenuation that specifically characterizes the dissipation of seismic wave energy due to anelastic processes in the Earth's upper mantle, distinguished from attenuation in other mantle layers by its dependence on temperature, composition, and partial melt in the depth range approximately 50 to 660 kilometers.

567

Publications

36.9K

Citations

1.3K

Authors

426

Institutions

Publications per year

2017–2026

57

Authors

1.3K

  1. BR
    Barbara Romanowicz

    University of California, Berkeley, United States

    14 publications · 891 citations

    14

    h-index

  2. BL
    Bryan L. Isacks

    Cornell University, United States

    13 publications · 1.6K citations

    13

    h-index

  3. MB
    Muawia Barazangi

    Cornell University, United States

    12 publications · 1.4K citations

    12

    h-index

  4. GF
    G. F. Panza

    University of Trieste, Italy

    11 publications · 371 citations

    11

    h-index

  5. BL
    B. L. N. Kennett

    Australian National University, Australia

    11 publications · 652 citations

    10

    h-index

1–5 of 1.3K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 75 publications · 8.9K citations

    57

    h-index

  2. Earth and Planetary Science Letters

    69 publications · 5.9K citations

    41

    h-index

  3. Tectonophysics

    69 publications · 3.4K citations

    34

    h-index

  4. Geophysical Journal International

    GJI · 48 publications · 2.6K citations

    30

    h-index

  5. Physics of The Earth and Planetary Interiors

    44 publications · 2.4K citations

    27

    h-index

1–5