1887

Abstract

The Gulf of Lion located in the Western Mediterranean has in its basin important deep water turbidity complexes, like the Rhône Deep-Sea Fan. During the Pliocene, the feeder system of this fan would have been constituted by multiple canyons; while in the Quaternary, the feeder system would have converged for a single canyon - the Petit-Rhône Canyon. However, the analysis of an isopac map of the Pliocene suggested that the pliocene sequence converges for two principal canyons - the Marti and the Petit-Rhône Canyon.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.172.SBGF0153_07
2007-11-19
2020-04-05
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.172.SBGF0153_07
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error