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• W2022206909 abstract "A Permian granitoid intrusion, exposed on Monte Mucrone, Sesia-Lanzo Zone, Italy, was metamorphosed under high-pressure conditions. To elucidate the metamorphic history of this granitoid complex, investigations have been made into the chemistry of the protolith, possible mass transfer during metamorphism, phase chemistry and implications for P-T conditions, and the age of metamorphic events. The metagranitoids contain Na-pyroxene, quartz, white mica, garnet and zoisite, and vary from rocks showing a well-preserved granitic texture to strongly deformed schists and gneisses. The rocks are of granitic to granodioritic composition and originated as an I-type granite pluton. With the exception of addition of H2O, the rock series behaved isochemicaliy throughout high-pressure metamorphism and later tectonic and retrograde transformations. P,T estimates based on Na-pyroxenes, garnet-clinopyroxene and garnet-biotite pairs give minimum pressures of ∼ 14 kbar at 600°C for the peak of the eclogite metamorphism. Age determinations by RbSr and KAr methods give 129-Ma for the rejuvenation of the total rock and 114-Ma isochrons for garnet and clinopyroxene, the first eclogite phase minerals. White-mica cooling ages scatter from 90 to 60 Ma." @default.
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• W2022206909 date "1985-07-01" @default.
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• W2022206909 title "Geochemistry, geochronology and petrology of Monte Mucrone: An example of EO-alpine eclogitization of Permian granitoids in the Sesia-Lanzo Zone, Western Alps, Italy" @default.
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• W2022206909 doi "https://doi.org/10.1016/0168-9622(85)90016-8" @default.
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