Fig. 5From: The 3D conductive thermal field of the North Alpine Foreland Basin: influence of the deep structure and the adjacent European AlpsDepth of the Lithosphere-Asthenosphere Boundary used for this study (modified after Przybycin et al. 2015) as the lower thermal boundary for the calculation of the 3D thermal field, to which an isothermal temperature of 1300 °C is assignedBack to article page