Ripple Marks is a sedimentary structure characterized by small, wave-like undulations on the surface of sedimentary beds, formed by the movement of sediment under unidirectional or oscillatory fluid flow, that serves as a paleoenvironmental indicator of depositional conditions in siliciclastic and planetary sedimentological contexts.
142
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6.2K
Citations
218
Authors
100
Institutions
Publications per year
2017–2026
7
Publications
142
Rhythmic Linear Sand Bodies Caused by Tidal Currents
Theodore Off · AAPG Bulletin · 1963 · 254 citations
Evolution and mechanics of a Miocene tidal sandwave
Philip A. Allen, Peter Homewood · Sedimentology · 1984 · 188 citations
RIPPLE MARK INDICES AND THEIR USES
William F. Tanner · Sedimentology · 1967 · 168 citations
1–5 of 142
Authors
218
- OF
5
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- WF
5
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3
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1–5 of 218
Institutions
100
Old Dominion University
Norfolk, United States
3 h-index
3 publications
599 citations
University of Cambridge
Cambridge, United Kingdom
3 h-index
5 publications
293 citations
United States Geological Survey
Reston, United States
3 h-index
4 publications
94 citations
Dalhousie University
Halifax, Canada
2 h-index
3 publications
100 citations
University of Reading
Reading, United Kingdom
2 h-index
2 publications
160 citations
The University of Osaka
Osaka, Japan
2 h-index
4 publications
121 citations
University of Tsukuba
Tsukuba, Japan
2 h-index
4 publications
77 citations
Kyushu University
Fukuoka, Japan
2 h-index
4 publications
190 citations
1–8 of 100
Venues
- Journal of Sedimentary Research
JSR · 41 publications · 1.7K citations
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- AAPG Bulletin
12 publications · 574 citations
11
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- Sedimentology
10 publications · 871 citations
10
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- The Journal of Geology
JG · 6 publications · 163 citations
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- Nature
3 publications · 60 citations
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