Fig. 8From: Thermal evolution of a Variscan syn-orogenic intracontinental basin (Servoz basin, Western Alps): RSCM geothermometry and geochronologyNumerical models of the thermal diffusion of the Montées-Pélissier granite within metagreywackes at initial temperatures of 250, 300, 350 and 400 °C. Models last 50 kyr. Red lines: initial geotherms; Blue lines: geotherms every 5 ka. RSCM temperatures from the western side of the Servoz syncline are projectedBack to article page