Tectonic Cleavage

Tectonic Cleavage is a geological structure, specifically a planar fabric formed within rocks due to the alignment of mineral grains or the development of submicroscopic foliation under directed pressure during regional metamorphism and deformation, distinguishing it from primary sedimentary layering or other non-tectonically induced anisotropies.

148

Publications

8.7K

Citations

425

Authors

219

Institutions

Publications per year

2017–2026

13

Authors

425

  1. PS
    Peter Stringer

    Radboud University Nijmegen, Netherlands

    3 publications · 121 citations

    3

    h-index

  2. WG
    Wen‐Chun Ge

    Jilin University, China

    3 publications · 363 citations

    3

    h-index

  3. TN
    Timothy N. Debacker

    KU Leuven, Belgium

    3 publications · 34 citations

    3

    h-index

  4. MJ
    M. J. Rickard

    Australian National University, Australia

    2 publications · 74 citations

    2

    h-index

  5. DR
    David R. Gray

    Monash University, Australia

    2 publications · 136 citations

    2

    h-index

1–5 of 425

Venues

  1. Tectonophysics

    15 publications · 1.6K citations

    15

    h-index

  2. Geological Magazine

    9 publications · 314 citations

    9

    h-index

  3. Geological Society of America Bulletin

    9 publications · 633 citations

    9

    h-index

  4. Journal of Structural Geology

    8 publications · 282 citations

    8

    h-index

  5. American Journal of Science

    6 publications · 287 citations

    6

    h-index

1–5