Geochronological constraints on the tectonometamphic development of the West Sudetes (Bohemian Massif)

Abstract

Tectonometamphic evolution of the West Sudetes is constrained basen on Ar-Ar data on micas from different lithotectonic units of the West Sudets. The model of NW vergent thrusting and later shearing is suggested.

Keywords

• Kachlík
• 2137