High Pressure and Low Temperature Metamorphism along the North-Eastern Margin of the Bohemian Massif From: Geolines | Date: January 1, 2005| Author: Zà ¡ ckovà ¡ , Eliska; Faryad, Shah Wali; Konopà ¡ sek, Jirà ­ | Copyright Institute of Geology 2005. Provided by ProQuest LLC.Copyright information

Several occurrences of high-pressure low-temperature rocks are known from the northern and western margins of the Bohemian Massif. They form a discontinuous belt rimming the KrkonoseJizera complex from east and south and occur also in the Krusné hory Mts. In the later, only relicts of blue amphibole with phengite and stilplomelane were found in metabasites (Holub and Soucek, 1994).

The largest metabasite body with relicts of blueschist-facies assemblage (blue amphibole+ epidote + albi...

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