Current Ripples
Current Ripples is a type of small-scale sedimentary structure characterized by wave-like undulations on the bedding surface of sedimentary deposits, formed by the migration of bedforms under unidirectional fluid flow, distinguished from other ripples by their asymmetrical profile and alignment parallel to flow direction.
546
Publications
24.7K
Citations
1.6K
Authors
580
Institutions
Publications per year
2017–2026
234
Variants
Current Ripple Marks
Parents
546
1–5 of 546
1.6K
15
h-index
13
h-index
9
h-index
8
h-index
6
h-index
1–5 of 1.6K
580
Aalborg University
Aalborg, Denmark
12 h-index
33 publications
991 citations

Zhejiang University
Hangzhou, China
11 h-index
32 publications
3.4K citations

North China University of Technology
Beijing, China
11 h-index
41 publications
3.2K citations

Centre National de la Recherche Scientifique
Paris, France
10 h-index
33 publications
536 citations

İstanbul Nişantaşı Üniversitesi
Istanbul, Turkey
10 h-index
12 publications
400 citations

Ajou University
Suwon, South Korea
9 h-index
24 publications
860 citations

University of Leeds
Leeds, United Kingdom
8 h-index
11 publications
651 citations

Huazhong University of Science and Technology
Wuhan, China
8 h-index
27 publications
886 citations
1–8 of 580
83 publications · 5.7K citations
43
h-index
35 publications · 2.8K citations
28
h-index
22 publications · 1.8K citations
20
h-index
22 publications · 1.1K citations
19
h-index
21 publications · 1.7K citations
18
h-index
1–5