Deformation, metamorphism and metasomatism in the Gemer-Vepor Contact Zone in the Western Carpathians and the possible links to the Greywacke Zone in the Eastern Alps
Název práce v češtině:
Deformace, metamorfóza a metasomatóza v gemersko-veporské kontaktní zóně v Západních Karpatech a možné vazby na Greywacke Zone ve Východních Alpách
Název v anglickém jazyce:
Deformation, metamorphism and metasomatism in the Gemer-Vepor Contact Zone in the Western Carpathians and the possible links to the Greywacke Zone in the Eastern Alps
Klíčová slova:
Centrální Západní Karpaty, Greywacke Zone, Ochtinská jednotka, Veitschský příkrov, U-Pb datování zirkonů, modelování fázových rovnováh
Klíčová slova anglicky:
Central Western Carpathians, Greywacke Zone, Ochtiná Unit, Veitsch Nappe, U-Pb zircon dating, Phase equilibrium modelling
The cause and effect of magnesium mobility will be studied in ancient zones of active deformation. The study area is located in Eastern Alps - West Carpathians orogenic system known for magnesite deposits along the Veitsch-Noetsch-Szabadbattyán-Ochtiná zone. This zone has been recognised as the crustal-scale tectonic boundary of first order importance for the Cretaceous (Alpine) convergent processes. In this zone, the relationship between deformation structures/phases and Mg-metasomatism responsible for the magnesite deposits will be sought.