Metamorphism of Paleoproterozoic paragneisses in the Belarus-Podlyasie granulite belt: Prograde-retrograde evolution
Metasedimentary granulites from the central portion of the Belarus-Podlyasie granulite belt were studied with the purpose to reproduce the Paleoproterozoic tectono-thermal evolution in the western part of the East European craton. The regularities identified in the compositional variations in minerals (particularly, garnet), textural relations between minerals, and thermobarometric data point to t