Trough Cross-Stratification is a type of sedimentary structure characterized by curved, scoop-shaped laminae that truncate and overlap one another in three dimensions, distinguished from planar cross-stratification by its concave, erosional lower boundaries and variable azimuth of foreset dips, typically formed by migrating bedforms in unidirectional or oscillatory flows.
36
Publications
1.8K
Citations
68
Authors
43
Institutions
Publications per year
2017–2026
2
Variants
Trough Cross-bedding
Parents
Publications
36
1–5 of 36
Authors
68
- GE
2
h-index
- BR
2
h-index
- CS
2
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- RK
1
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- MG
1
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1–5 of 68
Institutions
43
University College London
London, United Kingdom
3 h-index
3 publications
283 citations
The University of Adelaide
Adelaide, Australia
3 h-index
4 publications
386 citations
Birkbeck, University of London
London, United Kingdom
2 h-index
2 publications
228 citations
University of Johannesburg
Johannesburg, South Africa
1 h-index
1 publications
38 citations
ABS Consulting (United States)
Houston, United States
1 h-index
1 publications
114 citations
Czech Academy of Sciences, Institute of Botany
Průhonice, Czechia
1 h-index
1 publications
12 citations
Woodside (Australia)
Perth, Australia
1 h-index
1 publications
263 citations
Marathon Oil (United States)
Houston, United States
1 h-index
1 publications
12 citations
1–8 of 43
Venues
- Journal of Sedimentary Research
JSR · 14 publications · 645 citations
14
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- Sedimentology
5 publications · 498 citations
5
h-index
- The Journal of Geology
JG · 3 publications · 156 citations
3
h-index
- Geological Society London Special Publications
2 publications · 169 citations
2
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- AAPG Bulletin
2 publications · 63 citations
2
h-index
1–5