
In this study the evolution of metamorphism in harbey complex is proposed. The evolution characterized by regressive direction of the crystallization temperature, increasing of the dynamic factor values in the early stages of metamorphic changes and spatial localization of metamorphic phenomena.
Показано, что эволюция метаморфизма пород харбейского комплекса выражается в регрессивной направленности температурных условий кристаллизации, в возрастании роли динамического фактора на ранних стадиях метаморфических изменений и в пространственной локализации метаморфических проявлений.
МЕТАМОРФИЗМ, ТЕРМОДИНАМИЧЕСКАЯ ЭВОЛЮЦИЯ, АМФИБОЛИТЫ, МИНЕРАЛЬНЫЕ ПАРАГЕНЕЗИСЫ
МЕТАМОРФИЗМ, ТЕРМОДИНАМИЧЕСКАЯ ЭВОЛЮЦИЯ, АМФИБОЛИТЫ, МИНЕРАЛЬНЫЕ ПАРАГЕНЕЗИСЫ
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