Clinoform Development
Clinoform Development is a stratigraphic process in deltaic sedimentation characterized by the progressive seaward progradation, aggradation, and lateral spreading of sedimentary deposits that form a distinctive clinoform geometry defined by a convex-upward bedslope transitioning from subaerial to subaqueous environments.
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4.4K
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190
Authors
119
Institutions
Publications per year
2017–2026
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Shelf‐margin clinoforms and prediction of deepwater sands
Erik P. Johannessen, Ron J. Steel · Basin Research · 2005 · 230 citations
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The University of Texas at Austin
Austin, United States
12 h-index
27 publications
1.5K citations
University of Washington
Seattle, United States
5 h-index
12 publications
1.1K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
4 h-index
11 publications
1.9K citations
William & Mary
Williamsburg, United States
3 h-index
4 publications
1.2K citations

University of Oslo
Oslo, Norway
3 h-index
5 publications
182 citations
Istituto di Scienze Marine del Consiglio Nazionale delle Ricerche
Venice, Italy
3 h-index
6 publications
349 citations
University of Bergen
Bergen, Norway
3 h-index
4 publications
383 citations

Ocean University of China
Qingdao, China
2 h-index
2 publications
581 citations
1–8 of 119
16 publications · 771 citations
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5 publications · 683 citations
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4 publications · 846 citations
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JSR · 4 publications · 335 citations
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4 publications · 135 citations
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