P-T-time constraints for the Nevado-Filábride complex. A: P-T-time evolution after Augier et al. (2005b). The inset shows the temperature-time (T-t) and depth-time (Z-t) evolutions. Despite a probable slightly higher maximum temperature in the Bédar-Macael unit than in Calar Alto, available ages and error bars on the P-T estimates do not allow showing separate T-t and Z-t paths. B: other available data from Platt et al. (2006), Li and Massonne (2018) and Santamaria-Lopez et al. (2019).