Les appareils sédimentaires de la marge orientale de la Corse : interprétation hydrodynamique et implications structurales

The small turbiditicsystems lying along the eastern Corsicanmargin are in many respects very similar to typical deep-seafans. In the North, they can be connected with the streams rising from the alpine part of Corsica. In the South, they seem to testify old submerged reliefs. In this area, channel and canyontrends reveal both the Hercynian structures of the basement and the tectonic influence of the opening of the Tyrrhenian basin