Fig. 7
Download original image
Comparative stratigraphic table between the formations of Pechelbronn (North URG) and the Potash Basins and Mulhouse/Sundgau horst (South URG). The Marnes à Cyrènes and the topmost part of the Couches à Mélettes (Upper Rupelian) are lacking in the GRT wells. The Calcaire à Planorbes (Lutetian) is lateraly discontinuous and was not intercepted by the wells of Rittershoffen.
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.