Download original image
A two-steps evolution of the North Iberia distal margin from geological constraints provided by the Urdach and Saraillé mantle bodies and adjacent formations (see companion paper Lagabrielle et al., 2019, for data relative to the Urdach massif). Syn-metamorphic extensional deformation continued in the Saraillé area (beneath a cover of Albian-Cenomanian flysch) once extension ceased in the Urdach area (See Clerc et al., 2016 for more details of such evolution).
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.