Shape Preferred Orientation

Shape Preferred Orientation is a tectonic fabric characterized by the systematic alignment of elongated or flattened mineral grains or rock components, resulting from deformation processes that impart a directional dependence to the shape distribution within a rock mass.

124

Publications

5.4K

Citations

337

Authors

197

Institutions

Publications per year

2017–2026

16

Variants

Spo

Authors

337

  1. PL
    Patrick Launeau

    Nantes Université, France

    5 publications · 434 citations

    5

    h-index

  2. HK
    H. Kern

    Christian-Albrechts-Universität zu Kiel, Germany

    3 publications · 173 citations

    3

    h-index

  3. BT
    Basil Tikoff

    University of Wisconsin–Madison, United States

    3 publications · 90 citations

    3

    h-index

  4. DS
    David Shelley

    University of Canterbury, New Zealand

    3 publications · 74 citations

    3

    h-index

  5. BI
    Benoı̂t Ildefonse

    Université de Montpellier, France

    3 publications · 236 citations

    3

    h-index

1–5 of 337

Venues

  1. Journal of Structural Geology

    15 publications · 836 citations

    15

    h-index

  2. Geophysical Journal International

    GJI · 6 publications · 116 citations

    6

    h-index

  3. Contributions to Mineralogy and Petrology

    4 publications · 178 citations

    4

    h-index

  4. Geological Society London Special Publications

    4 publications · 164 citations

    4

    h-index

  5. Journal of Metamorphic Geology

    4 publications · 176 citations

    4

    h-index

1–5