Interior Anisotropy

Interior Anisotropy is a geophysical property characterized by the directional dependence of physical parameters within a planetary interior, distinguishing it from isotropic models by reflecting variations in composition, crystal alignment, or stress fields that produce measurably different behaviors along distinct spatial orientations.

9

Publications

948

Citations

27

Authors

16

Institutions

Publications per year

2017–2026

4

Authors

27

  1. AT
    Anssi T. Karttunen

    Aalto University, Finland

    1 publications · 23 citations

    1

    h-index

  2. EC
    Ernesto Contreras

    Universidad San Francisco de Quito, Ecuador

    1 publications · 50 citations

    1

    h-index

  3. KS
    Kwan San Hui

    University of East Anglia, United Kingdom

    1 publications · 46 citations

    1

    h-index

  4. AF
    Alberto Farina

    Université de Picardie Jules Verne, France

    1 publications · 35 citations

    1

    h-index

  5. KN
    Kwun Nam Hui

    University of Macau, Macao SAR China

    1 publications · 46 citations

    1

    h-index

1–5 of 27

Venues

  1. The European Physical Journal Plus

    2 publications · 89 citations

    2

    h-index

  2. Reviews of Geophysics

    1 publications · 159 citations

    1

    h-index

  3. Journal of Mathematical Physics

    1 publications · 244 citations

    1

    h-index

  4. The European Physical Journal C

    1 publications · 37 citations

    1

    h-index

  5. Journal of Materials Chemistry

    1 publications · 46 citations

    1

    h-index

1–5