Fig. 9From: Thermal evolution of a Variscan syn-orogenic intracontinental basin (Servoz basin, Western Alps): RSCM geothermometry and geochronologyStratigraphic Log of the Servoz syncline showing the F1, F2 and F3 formations with representative TRSCM (this study; Boutoux et al., 2016), temperature conditions from Dobmeier (1998) and associated apparent geothermal gradients. Colour of each sample is related to its temperatureBack to article page