Le canal de Corse et les bassins nord-tyrrhéniens au Miocène supérieur et terminal (Messinien) ; leur évolution plio-quaternaire
- 1 January 1980
- journal article
- research article
- Published by PERSEE Program in Géologie Méditerranéenne
- Vol. 7 (1) , 5-12
- https://doi.org/10.3406/geolm.1980.1119
Abstract
In the Northern-Tyrrhenian Sea and Corsica Basin, the main structural framework is established and analysed in the Messinian sedimentation. In the Southern Corsica Basin Messi-nian layers are eroded by a large and deep rivers system cut at the uppermost Messinian time.Keywords
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