Alluvial Fans
Alluvial Fan is a sedimentary landform composed of unconsolidated clastic material deposited by gravity-driven, distributive fluvial processes radiating from a confined source point, typically at a mountain front, distinguished from other fluvial depositional systems by its characteristic conical topography and proximal-to-distal grain size diminution.
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774
Institutions
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2017–2026
119
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Centre National de la Recherche Scientifique
Paris, France
22 h-index
97 publications
5K citations
Planetary Science Institute
Tucson, United States
19 h-index
33 publications
2K citations
United States Geological Survey
Reston, United States
19 h-index
49 publications
4.6K citations
Utrecht University
Utrecht, The Netherlands
16 h-index
27 publications
2.2K citations

University of Liverpool
Liverpool, United Kingdom
16 h-index
20 publications
1.3K citations

Institut de physique du globe de Paris
Paris, France
13 h-index
37 publications
1.8K citations

Chinese Academy of Sciences
Beijing, China
12 h-index
27 publications
715 citations
University of Arizona
Tucson, United States
12 h-index
27 publications
1.1K citations
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56 publications · 3.1K citations
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JSR · 30 publications · 3.3K citations
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