Shear Zone Evolution

Shear Zone Evolution is a geological process that describes the progressive development and transformation of a localized region of intense ductile to brittle deformation within the Earth's crust or mantle, distinguished by time-dependent changes in strain, fabric, geometry, and kinematics in response to tectonic forces.

1K

Publications

55.7K

Citations

2.7K

Authors

810

Institutions

Publications per year

2017–2026

188

Authors

2.7K

  1. RF
    Roberto F. Weinberg

    Monash University, Australia

    14 publications · 677 citations

    13

    h-index

  2. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    9 publications · 582 citations

    9

    h-index

  3. KW
    Klaus Wemmer

    University of Göttingen, Germany

    9 publications · 479 citations

    9

    h-index

  4. MP
    M. P. Searle

    University of Oxford, United Kingdom

    8 publications · 1.2K citations

    8

    h-index

  5. CC
    Chris Clark

    Curtin University, Australia

    8 publications · 375 citations

    8

    h-index

1–5 of 2.7K

Venues

  1. Journal of Structural Geology

    105 publications · 6.2K citations

    45

    h-index

  2. Tectonics

    67 publications · 5.7K citations

    42

    h-index

  3. Tectonophysics

    50 publications · 4.2K citations

    33

    h-index

  4. Journal of Metamorphic Geology

    47 publications · 2.7K citations

    30

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 25 publications · 2.9K citations

    25

    h-index

1–5