ABSTRACT

This contribution describes the most important locality of polymetallic mineralization in the Svratka Dome (the Moravicum), the so-called Stepánov ore district, comprising Pb-Zn-(Sb) and Cu-Pb-(Zn) types of mineralization. The genetic process which best supports all the observed patterns within the studied mineralizations is a mobilization of hydrothermal fluids by the Early-Variscan metamorphic processes.