Supplemental Material: Variscan intracrustal recycling by melting of Carboniferous arc-like igneous protoliths (Évora Massif, Iberian Variscan belt)

Table S1: SHRIMP U-Pb-Th zircon data of samples from Alto de São Bento (Évora Massif); Table S2: Amphibole thermobarometry results on the microprobe analyses from plutonic rocks of Hospistais intrusion.