Passive Margin Inversion
Passive Margin Inversion is a tectonic process in which a previously extensional continental margin, formed during rifting and seafloor spreading, undergoes compressional reactivation due to far-field stresses, resulting in the uplift and deformation of sedimentary basins and crustal thickening along formerly passive margins.
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188
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2017–2026
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Centre National de la Recherche Scientifique
Paris, France
12 h-index
36 publications
2K citations

Sorbonne Université
Paris, France
6 h-index
15 publications
1.6K citations

Chinese Academy of Sciences
Beijing, China
4 h-index
14 publications
594 citations
Universidade de São Paulo
São Paulo, Brazil
4 h-index
6 publications
434 citations
Géosciences Rennes
Rennes, France
3 h-index
8 publications
580 citations
Texas A&M University
College Station, United States
3 h-index
4 publications
913 citations

Australian National University
Canberra, Australia
3 h-index
3 publications
170 citations

The University of Adelaide
Adelaide, Australia
3 h-index
6 publications
397 citations
1–8 of 188
12 publications · 747 citations
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5 publications · 348 citations
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JGR · 5 publications · 530 citations
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4 publications · 541 citations
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4 publications · 256 citations
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