Fig. 14From: Geochemical signature of paleofluids in microstructures from Main Fault in the Opalinus Clay of the Mont Terri rock laboratory, Switzerland(modified from Pirkenseer 2007)A regional sketch of the paleo-structural situation of the Delémont Basin and its neighborhood during the Rupelian. On the left sketch are indicated the study area and the SSE-NNW cross-section with the location of the drillings (vertical bars) on which the stratigraphic interpretation was basedBack to article page