Problèmes posés par le Sédimentaire allochtone de Macinaggio (Corse) et par l'origine de ses détritus

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Abstract
Stratigraphical analysis (carbonated Trias-Lias, siliceous — "lydians" — and detrital late Cretaceous with Praeglobotrun¬ cana and Rotalipora. These sedimentary outliers overlie with tectonic contact the previously tectonized "Schistes lustrés". The Tamarone brecciae seem to be related to the Cretaceous : most clasts are blocks derived from a material similar to that found in the Autochthon of western Corsica. Discussion of the origin of the Allochthon : arguments in favor of an external origin.

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