Trvaní eo-alpinské metamorfní uúdalosti na základe modelovaní vícprvkové difuzi v granátu

Abstract

Rocks from the Micaschist-Marble Complex of the Wölz Tauern, which are part of the middle Austroalpine unit, contain large (up to 2 cm) garnet crystals that show clear evidence of two stage growth. Isotopic dating indicates that a Variscan (~ 270 Ma) gar

Keywords

• Cooling-exhumation rate
• multicomponent diffusion in garnet
• Austroalpine unit
• Eastern Alps