Anatectic melt inclusions in ultra‐high temperature granulites

International audiencePartial melting up to ultra-high temperature (UHT) conditions is one of the major processes for the geochemical differentiation and reworking of the mid-to lower continental crust, with relevant implications on its rheological behaviour. UHT granulites from the Gruf Complex (Central Alps) display garnet and sapphirine porphyroblasts containing a variety of primary melt inclusions. Typically, melt inclusions in garnets occur as glassy and polycrystallin