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Coronitic metagabbros of the Mariánské Lázně Complex and Teplá Crystalline Unit: inference fro the tectonometamorphic evolution of the western margin of the Teplá-Barrandian Unit, Bohemian Massif

Publication at Faculty of Science |
2002

Abstract

Gochemistry, metamorphic evolution of metagabbross of the Early Palaeozoic Mariánské Lázně Complex were studied due to reconstruction of pre-Variscan and Variscan history of the teplá suture zone.