Thrust-related Folding

Thrust-Related Folding is a structural geological process in which crustal shortening along a thrust fault results in the ductile deformation and buckling of overlying rock layers, distinguishing it from brittle faulting mechanisms by its characteristic development of folds synchronously with thrust displacement.

85

Publications

3.4K

Citations

245

Authors

116

Institutions

Publications per year

2017–2026

9

Authors

245

  1. FS
    Fabrizio Storti

    Roma Tre University, Italy

    4 publications · 194 citations

    4

    h-index

  2. MB
    Marco Bonini

    Institute of Geosciences and Earth Resources, Italy

    3 publications · 140 citations

    3

    h-index

  3. RW
    Robert W. Butler

    University of Leeds, United Kingdom

    3 publications · 145 citations

    3

    h-index

  4. MP
    M. P. Coward

    University of Leeds, United Kingdom

    3 publications · 336 citations

    3

    h-index

  5. GP
    Giacomo Prosser

    University of Basilicata, Italy

    2 publications · 72 citations

    2

    h-index

1–5 of 245

Venues

  1. Journal of Structural Geology

    12 publications · 463 citations

    11

    h-index

  2. Tectonics

    6 publications · 279 citations

    6

    h-index

  3. Journal of the Geological Society

    JGS · 6 publications · 163 citations

    6

    h-index

  4. Marine and Petroleum Geology

    5 publications · 146 citations

    5

    h-index

  5. Geological Society London Special Publications

    5 publications · 278 citations

    5

    h-index

1–5