| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9532465 | Marine Geology | 2005 | 31 Pages |
Abstract
The variation of relative sea level remains an important factor controlling the evolution of the Rhone delta after 6000 BP. The local (?) stabilization of the relative sea level between 4585 BP and 3520 BP played an important role in the triggering of coastal progradation (Saint-Ferréol lobe, eastern margin Rhône delta).
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Claude Vella, Thomas-Jules Fleury, Guillaume Raccasi, Mireille Provansal, François Sabatier, Michel Bourcier,