Tectonic Shortening
Tectonic Shortening is a geological deformation process characterized by the horizontal compression of the Earth's crust, resulting in the reduction of crustal volume through the formation of folds, thrust faults, and crustal thickening within continental collision zones and thrust belts.
492
Publications
42K
Citations
1.5K
Authors
571
Institutions
Publications per year
2017–2026
107
492
1–5 of 492
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571

Centre National de la Recherche Scientifique
Paris, France
25 h-index
110 publications
8.8K citations

Chinese Academy of Sciences
Beijing, China
16 h-index
43 publications
2.7K citations
ETH Zurich
Zurich, Switzerland
15 h-index
28 publications
2.4K citations
China Earthquake Administration
Beijing, China
15 h-index
37 publications
3.7K citations

Chinese Academy of Geological Sciences
Beijing, China
15 h-index
42 publications
1.8K citations
Planetary Science Institute
Tucson, United States
14 h-index
23 publications
3K citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
13 h-index
24 publications
1.9K citations
University of Oxford
Oxford, United Kingdom
11 h-index
17 publications
2.3K citations
1–8 of 571
70 publications · 6.9K citations
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JGR · 31 publications · 7.4K citations
28
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19 publications · 2.5K citations
18
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18 publications · 1.5K citations
18
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19 publications · 1.3K citations
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