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Anatectic melt inclusions in ultra‐high temperature granulites

Abstract : Partial 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 polycrystalline
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https://hal.archives-ouvertes.fr/hal-02959289
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Submitted on : Thursday, December 24, 2020 - 7:23:25 PM
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Omar Gianola, Omar Bartoli, Bernardo Cesare, Fabio Ferri, Andrea Galli, et al.. Anatectic melt inclusions in ultra‐high temperature granulites. Journal of Metamorphic Geology, Wiley-Blackwell, inPress, ⟨10.1111/jmg.12567⟩. ⟨hal-02959289⟩

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