Rifted Margin Architecture
Rifted Margin Architecture is a geological framework that characterizes the structural configuration and stratigraphic organization of continental margins formed through lithospheric extension and rupture, distinguished by the arrangement of fault systems, crustal thinning patterns, and syn- to post-rift sedimentary sequences resulting from continental breakup and seafloor spreading initiation.
408
Publications
26.4K
Citations
1.3K
Authors
525
Institutions
Publications per year
2017–2026
113
Parents
408
1–5 of 408
1.3K
21
h-index
14
h-index
9
h-index
6
h-index
6
h-index
1–5 of 1.3K
525

Centre National de la Recherche Scientifique
Paris, France
33 h-index
117 publications
7.6K citations
Université de Strasbourg
Strasbourg, France
23 h-index
66 publications
5.1K citations

Geological Survey of Norway
Trondheim, Norway
18 h-index
32 publications
2.2K citations

University of Oslo
Oslo, Norway
15 h-index
39 publications
2.5K citations
China University of Geosciences
Wuhan, China
15 h-index
43 publications
2.5K citations
Total (France)
Paris, France
13 h-index
23 publications
1.6K citations

China National Offshore Oil Corporation (China)
Beijing, China
12 h-index
25 publications
1K citations

University of Leeds
Leeds, United Kingdom
10 h-index
16 publications
1.4K citations
1–8 of 525
54 publications · 4.2K citations
33
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34 publications · 2.3K citations
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22 publications · 1.6K citations
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24 publications · 2.9K citations
21
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13 publications · 1.2K citations
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