Marine Faults
Marine Faults is a geological structure representing a planar discontinuity within the Earth's crust beneath marine environments, distinguished by measurable displacement of rock units due to tectonic stresses acting along the fault plane.
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2017–2026
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Central role of detachment faults in accretion of slow-spreading oceanic lithosphere
J. Escartı́n, Deborah K. Smith, J. Cann et al. · Nature · 2008 · 505 citations
Architecture of Marine Rift-Basin Successions
AAPG Bulletin · 1998 · 327 citations
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379

Centre National de la Recherche Scientifique
Paris, France
20 h-index
83 publications
9.1K citations
University of Bergen
Bergen, Norway
15 h-index
36 publications
1.9K citations

Istanbul Technical University
Istanbul, Türkiye
13 h-index
31 publications
3.1K citations
Equinor (Norway)
Stavanger, Norway
11 h-index
14 publications
627 citations
Centre de Recherche et d’Enseignement de Géosciences de l’Environnement
Aix-en-Provence, France
9 h-index
17 publications
1.4K citations

University of Leeds
Leeds, United Kingdom
9 h-index
13 publications
2K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
8 h-index
19 publications
1.2K citations

Institut de physique du globe de Paris
Paris, France
8 h-index
25 publications
2.8K citations
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35 publications · 1.8K citations
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16 publications · 991 citations
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15 publications · 1.6K citations
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