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Título Fig. 11. R–T diagrams for samples of garnet-muscovite-biotite gneiss MTZ: (a) – model 996-1, (b) – model 2465v. The lines of mineral reactions were calculated by the method of "classical" thermobarometry using garnet-biotite geothermometer (GB, Holdaway, 2000), garnet-biotite-plagioclase-quartz geobarometer (GBPQ, Wu et al., 2006) and garnet-biotite-muscovite-plagioclase geobarometer (GBMP, Wu, 2015).
Submissão Metamorphic mineral reactions and mineral paragenesis in the rocks of the Meyeri tectonic zone (the south-eastern part of the Fennoscandian shield, Russia)
Tipo author.submit.suppFile.figureResearchMaterials
Data 2024-07-17
Idioma ru
Digital Object Identifier https://doi.org/10.31857/S0869-5903322195-217-4259581

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