Passive Margin Deformation
Passive Margin Deformation is a geological process denoting the mechanical alteration and structural evolution of lithospheric segments at continental margins without active plate boundary forces, distinguished from active margin tectonics by the dominance of gravitational, thermal, and sediment-loading mechanisms in the absence of significant convergence or subduction.
169
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13.4K
Citations
528
Authors
274
Institutions
Publications per year
2017–2026
28
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274

Centre National de la Recherche Scientifique
Paris, France
14 h-index
37 publications
2.3K citations

Chinese Academy of Sciences
Beijing, China
6 h-index
22 publications
1.2K citations
Géosciences Rennes
Rennes, France
5 h-index
12 publications
743 citations

Australian National University
Canberra, Australia
5 h-index
5 publications
674 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
5 h-index
13 publications
957 citations

Geological Survey of Norway
Trondheim, Norway
4 h-index
4 publications
350 citations
United States Geological Survey
Reston, United States
4 h-index
5 publications
576 citations
Geological Survey of Canada
Ottawa, Canada
4 h-index
6 publications
502 citations
1–8 of 274
18 publications · 2.3K citations
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15 publications · 1.5K citations
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15 publications · 822 citations
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11 publications · 539 citations
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9 publications · 642 citations
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