Open Access

Fig. 5


Download original image

The Clansayesian (Uppermost Aptian)-Early Albian main rifting stage and the creation of the Tardets-Mauléon Basin. A: simplified isopach map. Note the close relationship between the transverse N20 fault zones, the salt diapirs and the depocenters. B: NW–SE section showing the block tilting on an hyper-extended crust and the creation of a marine deep trough filled up with Flysch Noir sediments during the following Albian late rifting stage (Fig. 5).

Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.

Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.

Initial download of the metrics may take a while.