Formation and destabilization of the high pressure assemblage garnet-phengite-paragonite (Krušné hory Mountains, Bohemian Massif): The significance of the Tschermak substitution in the metamorphism of pelitic rocks

Abstract

Petrology of high-pressure metasediments

Keywords

• Jiří Konopásek
• tel. 1525 phengite
• paragonite
• Tschermak substitution
• high-pressure metamorphism
• Bohemian Massif