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

Abstrakt

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.