Roland Delcey, Jean Claude Limasset, Pierre Routhier; Les bassins sedimentaires du nord de la Corse; essai de synthese stratigraphique et apercu tectonique. The Saint Florent, Balagne, and Francardo basins of northern Corsica, surrounded by Paleozoic granitic and metamorphic rocks, are occupied by Permian to Triassic arkosic clastics and rhyolite overlain by dolomitic limestones, Jurassic limestones and spilite pillow lavas, Cretaceous flysch and overlying Globotrunca marly and sandy limestones, Eocene arkosic clastics, Nummulite limestone, and flysch. Although the paleogeographic history of the three basins differs in details, it was essentially the same in major features. The tectonic history, however, differed considerably depending on the structural nature of the underlying basement rocks of the basins. Presence of nappes of distant origin is suspected from relationships of the Cretaceous flysch and the Paleozoic schists east of Francardo.
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Auzende, J. Rehault, L. Pastouret, B. Szep, J. Olivet; Les bassins sedimentaires de la mer d'Alboran. Shibboleth Sign In. OpenAthens Sign In. Institutional Sign In. Sign In or Create an Account. User Tools. Sign In. Advanced Search. Article Navigation. Close mobile search navigation Article navigation. Previous Article Next Article. Other March 01, Les bassins sedimentaires de la mer d'Alboran J.
Auzende ; J. Google Scholar. Rehault ; J. Pastouret ; L. Szep ; B. Olivet J. Article history first online:. This content is PDF only. Please click on the PDF icon to access. First Page Preview. Close Modal. You do not currently have access to this article. You could not be signed in. Librarian Administrator Sign In. Buy This Article. Email alerts Article activity alert. New issue alert. View Full GeoRef Record. Citing articles via Google Scholar. Related Articles.
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