Passive Margin Formation
Passive Margin Formation is a geodynamic process denoting the structural and stratigraphic development of continental margins following the cessation of rifting, characterized by thermal subsidence and sediment accumulation along formerly active rifted margins, thereby distinguishing it from active tectonic margin evolution.
236
Publications
16.6K
Citations
752
Authors
349
Institutions
Publications per year
2017–2026
45
236
Passive margins through earth history
Dwight C. Bradley · Earth-Science Reviews · 2008 · 401 citations
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Universidade Federal de Minas Gerais, Brazil
4 publications · 152 citations
4
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Universidade Federal do Rio Grande do Norte, Brazil
4 publications · 204 citations
4
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Centre National de la Recherche Scientifique
Paris, France
12 h-index
39 publications
3.3K citations

University of Edinburgh
Edinburgh, United Kingdom
10 h-index
12 publications
1.1K citations

Geological Survey of Norway
Trondheim, Norway
7 h-index
10 publications
548 citations
University of Bergen
Bergen, Norway
6 h-index
10 publications
458 citations

Chinese Academy of Sciences
Beijing, China
6 h-index
25 publications
2.3K citations

Sorbonne Université
Paris, France
6 h-index
16 publications
390 citations
Universidade de Brasília
Brasília, Brazil
5 h-index
5 publications
248 citations
Géosciences Rennes
Rennes, France
5 h-index
11 publications
831 citations
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24 publications · 2.2K citations
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16 publications · 1.2K citations
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17 publications · 1.8K citations
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15 publications · 742 citations
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JGS · 9 publications · 676 citations
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