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
626
Ronald E. Wilcox, T. P. Harding, D. R. Seely · AAPG Bulletin · 1973 · 1.1K citations
Achim Kopf · Reviews of Geophysics · 2002 · 861 citations · Full text
1–5 of 626
1.9K
8
h-index
6
h-index
6
h-index
5
h-index
5
h-index
1–5 of 1.9K
645

Centre National de la Recherche Scientifique
Paris, France
31 h-index
132 publications
8.3K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
14 h-index
60 publications
3.6K citations

Université de Montpellier
Montpellier, France
12 h-index
23 publications
1.3K citations
Géosciences Rennes
Rennes, France
11 h-index
29 publications
3.4K citations
University of Oxford
Oxford, United Kingdom
11 h-index
18 publications
1.3K citations
Institut de Recherche pour le Développement
Marseille, France
9 h-index
26 publications
1.2K citations

Chinese Academy of Sciences
Beijing, China
9 h-index
30 publications
1.2K citations
Institut des Sciences de la Terre
Grenoble, France
9 h-index
19 publications
935 citations
1–8 of 645
64 publications · 6K citations
42
h-index
JGR · 44 publications · 7.4K citations
34
h-index
42 publications · 2K citations
28
h-index
20 publications · 2.1K citations
18
h-index
JGS · 19 publications · 1.2K citations
17
h-index
1–5