Gabbross in an accretionary prism: sources emplacement environments, and metamorphic evolution of the Mariánské Lázně Complex and Teplá Crystalline Unit (NW Bohemian Massif) during the Palaeozoic.

Abstract

Geochemical characteristic of metagabbross from the Mariánské Lázně Complex and the Teplá Crystalline unit is given. Geotectonic condition of their intrusion are interpreted based on geochemistry, petrology and mineralogy of these metagabbros.