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.
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Partitioning of intermontane basins by thrust‐related folding, Tien Shan, Kyrgyzstan
Burbank, McLean, Bullen et al. · Basin Research · 1999 · 217 citations
M. P. Coward, J. H. Kim · Geological Society London Special Publications · 1981 · 145 citations
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University of Leeds
Leeds, United Kingdom
3 h-index
6 publications
672 citations
Cardiff University
Cardiff, United Kingdom
3 h-index
13 publications
473 citations
Institute of Geosciences and Earth Resources
Pisa, Italy
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3 publications
115 citations
Roma Tre University
Rome, Italy
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10 publications
393 citations

Imperial College London
London, United Kingdom
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10 publications
759 citations

Université de Pau et des Pays de l'Adour
Pau, France
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5 publications
68 citations
Institute of Geological Sciences
Kyiv, Ukraine
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2 publications
40 citations

University of Basilicata
Potenza, Italy
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2 publications
72 citations
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12 publications · 463 citations
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JGS · 6 publications · 163 citations
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