Anatectic melt inclusions in ultra high temperature granulites

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 (European Central Alps)...

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Veröffentlicht in:	Journal of metamorphic geology 2021-04, Vol.39 (3), p.321-342
Hauptverfasser:	Gianola, Omar, Bartoli, Omar, Ferri, Fabio, Galli, Andrea, Ferrero, Silvio, Capizzi, Luca S., Liebske, Christian, Remusat, Laurent, Poli, Stefano, Cesare, Bernardo
Format:	Artikel
Sprache:	eng
Schlagworte:	Aluminosilicates Aluminum silicates Biotite Carbon dioxide Carbonates Coexistence Continental crust Degassing Dehydration Diameters Earth Sciences Feldspars Fluid inclusions Garnet Geochemistry granites Gruf Complex High temperature Immiscibility Melting Melts Mica Mineral assemblages Miscibility Muscovite nanogranitoids Plagioclase Planetology Potassium oxides Quartz Rheological properties Sciences of the Universe Silica Silicon dioxide Temperature Thermal structure Ultrahigh temperature
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