Planar Cross-stratification
Planar Cross-Stratification is a type of sedimentary structure characterized by inclined, tabular layers that truncate and overlap one another, formed by the migration of subaqueous bedforms under unidirectional flow, where the bounding surfaces are predominantly flat and parallel, distinguishing it from cross-laminations with curved or convex geometries.
30
Publications
1.2K
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51
Authors
25
Institutions
Publications per year
2017–2026
4
Variants
Planar Cross-bedding
Parents
30
Giorgio Basílici, Pedro Henrique Vieira de Luca, Daniel G. Poiré · Sedimentary Geology · 2012 · 65 citations · Full text
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Czech Academy of Sciences, Institute of Botany, Czechia
2 publications · 53 citations
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1
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University of Illinois Urbana-Champaign, United States
1 publications · 50 citations
1
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University of Ottawa
Ottawa, Canada
3 h-index
4 publications
138 citations

Consejo Nacional de Investigaciones Científicas y Técnicas
Buenos Aires, Argentina
1 h-index
1 publications
65 citations
Jagiellonian University
Krakow, Poland
1 h-index
1 publications
12 citations

Universidade Estadual de Campinas (UNICAMP)
Campinas, Brazil
1 h-index
2 publications
130 citations

Czech Academy of Sciences
Prague, Czechia
1 h-index
1 publications
15 citations

Northern Arizona University
Flagstaff, United States
1 h-index
1 publications
16 citations

Indian Statistical Institute
Kolkata, India
1 h-index
3 publications
63 citations
Czech Academy of Sciences, Institute of Geology
Prague, Czechia
1 h-index
1 publications
15 citations
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JSR · 12 publications · 639 citations
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4 publications · 172 citations
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JG · 2 publications · 85 citations
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1 publications · 12 citations
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1 publications · 15 citations
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