Growth Faulting
Growth Faulting is a syndepositional normal faulting process in sedimentary basins wherein differential subsidence and sediment accumulation across the fault plane result in progressive thickening of strata toward the downthrown block, distinguishing it from non-growth faulting by its temporal correlation with sedimentation.
94
Publications
4.8K
Citations
226
Authors
101
Institutions
Publications per year
2017–2026
9
Variants
Syndepositional Faulting
Parents
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101
Géosciences Rennes
Rennes, France
5 h-index
20 publications
617 citations
University College Dublin
Dublin, Ireland
5 h-index
12 publications
599 citations

Bureau of Economic Analysis
Washington D.C., United States
5 h-index
12 publications
633 citations
The University of Texas at Austin
Austin, United States
5 h-index
11 publications
367 citations

Centre National de la Recherche Scientifique
Paris, France
5 h-index
16 publications
514 citations

Imperial College London
London, United Kingdom
4 h-index
6 publications
232 citations

University of Liverpool
Liverpool, United Kingdom
4 h-index
21 publications
2.4K citations
Universiti Brunei Darussalam
Bandar Seri Begawan, Brunei
3 h-index
8 publications
470 citations
1–8 of 101
23 publications · 867 citations
18
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9 publications · 622 citations
9
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6 publications · 191 citations
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6 publications · 230 citations
6
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3 publications · 107 citations
3
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1–5