Compressional Tectonics

Compressional Tectonics is a geological process characterized by the deformation of planetary crustal and lithospheric materials under convergent stress regimes, distinguished from other tectonic styles by the dominance of shortening structures such as folds, thrust faults, and reverse faults in response to horizontal compressive forces.

626

Publications

43.2K

Citations

1.9K

Authors

645

Institutions

Publications per year

2017–2026

98

Authors

1.9K

  1. PC
    P.R. Cobbold

    Université de Rennes, France

    8 publications · 772 citations

    8

    h-index

  2. MP
    M. P. Searle

    University of Oxford, United Kingdom

    6 publications · 542 citations

    6

    h-index

  3. CB
    Christopher Beaumont

    Dalhousie University, Canada

    6 publications · 1.3K citations

    6

    h-index

  4. RH
    Richard H. Sibson

    University of Otago, New Zealand

    5 publications · 559 citations

    5

    h-index

  5. CF
    Claudio Faccenna

    Roma Tre University, Italy

    5 publications · 595 citations

    5

    h-index

1–5 of 1.9K

Venues

  1. Tectonics

    64 publications · 6K citations

    42

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 44 publications · 7.4K citations

    34

    h-index

  3. Geological Society London Special Publications

    42 publications · 2K citations

    28

    h-index

  4. Tectonophysics

    20 publications · 2.1K citations

    18

    h-index

  5. Journal of the Geological Society

    JGS · 19 publications · 1.2K citations

    17

    h-index

1–5