Lateral Accretion
Lateral Accretion is a fluvial sedimentation process in which sediment is progressively deposited on the inner bank of a meandering channel, resulting in the gradual lateral migration and buildup of point bars within a river system.
119
Publications
6.5K
Citations
328
Authors
166
Institutions
Publications per year
2017–2026
19
Parents
119
1–5 of 119
328
5
h-index
4
h-index
2
h-index
2
h-index
2
h-index
1–5 of 328
166

University of Leeds
Leeds, United Kingdom
6 h-index
7 publications
737 citations
Dalhousie University
Halifax, Canada
5 h-index
9 publications
629 citations
Utrecht University
Utrecht, The Netherlands
4 h-index
7 publications
490 citations
ExxonMobil (United States)
Irving, United States
3 h-index
9 publications
1.9K citations
Southwest Petroleum University
Chengdu, China
3 h-index
4 publications
105 citations

University of Manchester
Manchester, United Kingdom
3 h-index
5 publications
309 citations
The University of Texas at Austin
Austin, United States
3 h-index
7 publications
244 citations
United States Geological Survey
Reston, United States
3 h-index
3 publications
266 citations
1–8 of 166
JSR · 16 publications · 1K citations
16
h-index
15 publications · 1.1K citations
15
h-index
6 publications · 414 citations
6
h-index
5 publications · 353 citations
5
h-index
4 publications · 356 citations
4
h-index
1–5