Denudation of the continental shelf between Britain and France at the glacial–interglacial timescale

The erosional morphology preserved at the sea bed in the eastern English Channel dominantly records denudation of the continental shelf by fluvial processes over multiple glacial–interglacial sea-level cycles rather than by catastrophic flooding through the Straits of Dover during the mid-Quaternary...

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Detalles Bibliográficos
Autores principales: Mellett, Claire L., Hodgson, David M., Plater, Andrew J., Mauz, Barbara, Selby, Ian, Lang, Andreas
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Elsevier 2013
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3990419/
https://www.ncbi.nlm.nih.gov/pubmed/24748702
http://dx.doi.org/10.1016/j.geomorph.2013.03.030

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3990419/
https://www.ncbi.nlm.nih.gov/pubmed/24748702
http://dx.doi.org/10.1016/j.geomorph.2013.03.030

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