The possible impact origin of the Sevetin and Susice structures (Bohem
ia, Czech Republic) has been tested by searching for shock metamorphis
m in quartz. Transmission Electron Microscopy (TEM) investigation reve
aled microstructures originating only from tectonic deformation. No la
ttice defects characteristic of shock deformation have been detected,
even considering possible annealing of microstructures. An impact orig
in for Sevetin and Susice is not supported by TEM study.