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;1060°;C and ~22 kbar. Ultrahigh-temperature conditions persisted even after a significant drop in pressure. We dated monazite, zircon, rutile, garnet and apatite from felsic granulite by U;Pb, biotite from retrogressed felsic granulite by Rb;Sr, and titanite from mafic granulite by U;Pb. Zircon and titanite give within analytical uncertainties the same age at 341·;5 ±; 0·;8 Ma (2{sigma}) and 342·;0 ±; 0·;8 Ma (2{sigma}), respectively, demonstrating (1) a similar closure temperature for both minerals in dry systems and (2) a closure temperature for titanite considerably higher than 550°;C. Monazite plots discordantly and yields a 207Pb/206Pb age at 338·;0 ±;0·;5 Ma (2{sigma}), which represents a minimum age because of the possibility of excess 206Pb. Rutile, garnet and apatite have little radiogenic lead and show a wide range of apparent 206Pb/238U ages, which reflects initial isotopic heterogeneities originating from the reaction history rather than later disturbances. Biotite yields an Rb;Sr age at 323·;0 ±; 2·;3 Ma (2{sigma}). The age data in combination with the P;T path demonstrate that exhumation of the Saxon Granulite Massif to a middle- to upper-crustal level proceeded at a fast average rate (>9;18 mm/yr) and subsequently slowed down significantly (<2 mm/yr).