Long-term washover fan accretion on a transgressive barrier island challenges the assumption that paleotempestites represent individual tropical cyclones

Barrier island overwash occurs when the elevation of wave runup exceeds the dune crest and induces landward transport of sediment across a barrier island and deposition of a washover deposit. Washover deposition is generally attributed to major storms, is important for the maintenance of barrier isl...

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Detalles Bibliográficos
Autores principales: Rodriguez, Antonio B., Theuerkauf, Ethan J., Ridge, Justin T., VanDusen, Beth M., Fegley, Stephen R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7661513/
https://www.ncbi.nlm.nih.gov/pubmed/33184392
http://dx.doi.org/10.1038/s41598-020-76521-4

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7661513/
https://www.ncbi.nlm.nih.gov/pubmed/33184392
http://dx.doi.org/10.1038/s41598-020-76521-4

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