Alluvial Facies
Alluvial Facies is a sedimentary facies characterized by deposits formed in terrestrial fluvial and floodplain environments through the action of rivers and streams, distinguished from other facies by its association with channelized flow, variable grain size, and architectural elements such as point bars, levees, and overbank deposits.
196
Publications
14.5K
Citations
532
Authors
255
Institutions
Publications per year
2017–2026
25
196
1–5 of 196
532
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255

University of Leeds
Leeds, United Kingdom
6 h-index
10 publications
1.2K citations

University of Birmingham
Birmingham, United Kingdom
5 h-index
6 publications
476 citations
Universidad Complutense de Madrid
Madrid, Spain
5 h-index
11 publications
423 citations
University of Cambridge
Cambridge, United Kingdom
4 h-index
5 publications
197 citations
United States Geological Survey
Reston, United States
4 h-index
9 publications
763 citations
ExxonMobil (United States)
Irving, United States
4 h-index
6 publications
1.2K citations

Birkbeck, University of London
London, United Kingdom
3 h-index
4 publications
483 citations
University of Brighton
Brighton, United Kingdom
3 h-index
3 publications
497 citations
1–8 of 255
25 publications · 1.8K citations
22
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JSR · 20 publications · 2.3K citations
17
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13 publications · 935 citations
13
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6 publications · 283 citations
6
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5 publications · 214 citations
5
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1–5