Facies Cyclicity
Facies Cyclicity is a stratigraphic concept that denotes a recurring sequence of sedimentary facies within a depositional environment, distinguished by systematic vertical changes in lithology, fossil content, or sedimentary structures reflecting cyclical variations in controlling geological processes such as sea level, climate, or tectonics.
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4K
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199
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133
Institutions
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2017–2026
6
Variants
Facies Cycles
Parents
72
The stratigraphic distribution of fossils
Steven M. Holland · Paleobiology · 1995 · 273 citations
Peter G. Langdon, Keith Barber, Paul Hughes · Quaternary Science Reviews · 2003 · 175 citations
Fining‐upwards cycles in alluvial successions
J.R.L. Allen · Geological Journal · 1965 · 162 citations
Stacy C. Atchley, Lee C. Nordt, S. I. Dworkin · Journal of Sedimentary Research · 2004 · 112 citations
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Czech Academy of Sciences, Institute of Inorganic Chemistry, Czechia
2 publications · 55 citations
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1–5 of 199
133
Virginia Tech
Blacksburg, United States
3 h-index
6 publications
274 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
7 publications
444 citations
Kansas State University
Manhattan, United States
2 h-index
3 publications
102 citations

Imperial College London
London, United Kingdom
2 h-index
5 publications
129 citations
Smithsonian Institution
Washington, United States
2 h-index
2 publications
126 citations

Lamont-Doherty Earth Observatory
Sparkill, United States
2 h-index
3 publications
182 citations

University of Calabria
Rende, Italy
2 h-index
5 publications
226 citations
Universidad de Zaragoza
Zaragoza, Spain
2 h-index
7 publications
118 citations
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12 publications · 618 citations
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8 publications · 372 citations
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JSR · 6 publications · 352 citations
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4 publications · 130 citations
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3 publications · 812 citations
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