Fig. 11

Cross sections extracted from the 3-D conductive temperature distribution that is modeled using the mean formation thermal conductivities and a basal heat flow value of 78.44 mW m⁻², running through profile lines A–A′ (a) and B–B′ (b) (see Fig. 8a for the location of profile lines). The lithology and their mean thermal conductivities are also superimposed on the temperature cross sections