Aeolian Stratification
Aeolian Stratification is a sedimentary structure formed by the deposition and accumulation of wind-transported particulate matter in distinct, layer-parallel strata, distinguished from other sedimentary stratifications by its genesis in aeolian (wind-driven) geomorphic processes and characteristic bedforms such as cross-bedding, grainfall laminae, and avalanche-derived layers observed in dune and desert environments.
31
Publications
1.5K
Citations
81
Authors
56
Institutions
Publications per year
2017–2026
6
Parents
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1–5 of 31
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Institute of Geographic Sciences and Natural Resources Research, China
2 publications · 55 citations
2
h-index
1–5 of 81
56
The University of Texas at Austin
Austin, United States
3 h-index
9 publications
1K citations

Chinese Academy of Sciences
Beijing, China
2 h-index
4 publications
99 citations
Institute of Geographic Sciences and Natural Resources Research
Beijing, China
2 h-index
4 publications
99 citations
Utrecht University
Utrecht, The Netherlands
2 h-index
2 publications
81 citations

Indian Statistical Institute
Kolkata, India
2 h-index
2 publications
66 citations

Consejo Nacional de Investigaciones Científicas y Técnicas
Buenos Aires, Argentina
1 h-index
1 publications
21 citations
Changchun University
Changchun, China
1 h-index
2 publications
28 citations
Laboratoire de Géologie de Lyon : Terre, Planètes et Environnement
Lyon, France
1 h-index
4 publications
68 citations
1–8 of 56
6 publications · 639 citations
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2 publications · 60 citations
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2 publications · 50 citations
2
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2 publications · 41 citations
2
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2 publications · 61 citations
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