Schematic cross section adapted from Díez Fernández and Pereira (2016, their Fig. 4d) illustrating the tectonic-magmatic context of emplacement of Fregeneda-Almendra pegmatites to the north of the FCL anatectic complex. The location of the cross section is indicated in Fig. 2b. High temperature-low pressure metamorphism-related M2 isograds (Carnicero, 1982; Vieira et al., 2011) were drawn parallel to the D2 Pinhel shear zone (SZ). The size of the pegmatites is not to scale. The ages of Li-pegmatites are from this study and the ages of migmatites and granites are from Ferreira et al. (2019, 2022).