С. А. Бушмин scite author profile

The proposed PT grid of mineral facies of metamorphic rocks, which retains the commonly adopted nomenclature (greenschist, epidote-amphibolite, amphibolite, granulite, glaucophane-schist, and eclogite facies), is based on original calculations and the published calculated and experimental data on mineral equilibria. To validate the facies and subfacies PT boundaries, the mineral equilibria in metapelitic and metabasic rocks have been used.

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Rb-Sr age of metasomatism and ore formation in the low-temperature shear zones of the Fenno-Karelian CRATON, Baltic Shield

Глебовицкий

Бушмин

Belyatsky

et al. 2014

Petrology

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Equation of State of the H2O–CO2–CaCl2 Fluid System and Properties of Fluid Phases at Р-Т Parameters of the Middle and Lower Crust

Ivanov

Бушмин

2019

Petrology

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Origin and composition of fluid responsible for metasomatic processes in shear zones of the Bolshie Keivy tectonic nappe, baltic shield: Carbon isotope composition of graphite

et al. 2011

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Oxygen isotopic composition of coexisting minerals of sillimanite-hypersthene rocks from the Por’ya bay area: Evidence of fluid involvement in granulite-facies metamorphism

et al. 2010

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