Abstract
Evolution of melts and fluids during the crust and mantle formation in Neo-Archean—Paleo-Proterozoic. Stratigraphic effects
Highlights
The paper presents a comparison of material composition of metamorphic complexes of the Ukrainian shield formed in Neo-Archean—Paleo-Proterozoic
During the second tectonic-magmatic cycle separation of the Ukrainian shield into blocks and suture zones took place, which differ by composition of accumulated strata and positions of material sources
During the second tectonic-magmatic cycle (on the border of Neo-Archean and Paleo-Proterozoic) separation of the Ukrainian shield into blocks and suture zones took place, which differ by composition of accumulated strata and positions of material sources
Summary
Верхняя подсвита: Кальцифиры, завальевская чередование скарноиды, Мраморы, силикатных, мраморы, пироксенкальцифиры, силикатномагнетитовые графит-биотитовые, карбонатных, железистые гранат-биотитовые, карбонатных пород; кварциты пироксеновые гнейсы, кальцифиры. Гранат-биотитовые (с кристаллосланцы; кварциты, гнейсы кордиеритом) гнейсы с амфиболиты гранат-биотитовые, прослоями гиперстен-. Биотитовые, гранатбиотитсланцев и биотитовые гнейсы амфиболовые, кальцифиров и сланцы амфиболиты
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