Eclogite-facies metamorphism at the eastern margin of the Bohemian Massif - subduction prior to continental underthrusting

Abstrakt

In garnetiferous micaschists situated at the northern termination of the Moravian domain, metabasites were found containing relics of eclogite-facies assemblage. In these rocks, minimum pressure conditions of 13 kbars at temperatures of 623-654