Monazite and zircon U–(Th–)Pb dating reveals multiple episodes of HT metamorphism in the Cima Lunga unit (Central Alps): implications for the exhumation of high‐pressure rocks

High- to ultrahigh-pressure (HP-UHP) rocks recording high-temperature (HT) > 700 degrees C are well exposed in the Central Alps, making it an ideal region to study the timing of metamorphic stages and the mechanisms of deep-seated rocks exhumation. Here, we report an integrated dataset of petrological and U-(Th-)Pb dating of metapelites surrounding ultramafic lenses from the Cima Lunga unit. At the interface with ultramafics preserving (U)HP-HT assemblages (1.5-3.1 GPa, 650-850 degrees C), metapelites record higher P-T values (1.3-2.7 GPa, 700-850 degrees C) and traces of partial melting, whereas the rest of the unit is dominated by amphibolite-facies conditions. U-Th-Pb dating on zircon and monazite from migmatites indicates that partial melting was episodic involving at least two stages at similar to 38 to 35 Ma and 33-30 Ma, respectively. While the 38-35 Ma stage matches the HP conditions (> 1.5 GPa) and it is recorded around only one lens with scarce volumes of melt, partial melting at 33-30 Ma is witnessed at lower pressure (similar to 1 GPa) and more widely distributed around the lenses, as within the major shear zones. Far from the ultramafics, zircon from the amphibolite-facies metasedimentary rocks record inherited pre-Variscan ages, while monazite ages at similar to 22 Ma document mineral growth during the Barrovian cooling. Field and petro-chronological evidence highlight that multiple episodes of partial melting locally developed at the rheological interface promoted by the interplay of fluids extracted from the ultramafic lenses associated with shear heating. New evidence suggests that local variation of P-T equilibria play a significant role during the exhumation history.