Key words: hydrothermal mineralization, alpine paragenesis, lazulite, Tribeč This work has a recherche character and provides a comprehensive overview of mineralizations in the Tribeč Mountains. The aim of the work is to describe individual localities and characterize indivindual mineralizations and to include them in the system of hydrothermal mineralizations in Tribeč. All occurrences were classified under some type of mineralization according to characteristic geological and genetic traits and / or according to the predominant or characteristic mineral. Based on these criteria, mineralizations can be divided into the following 3 large groups: 1. Hydrothermal mineralizations in crystalline basement and mesozoic cover, 2. Hydrothermal mineralizations related to tertiary volcanics and 3. Other types of mineralizations. Each of these 3 large groups includes other types of mineralizations divided into subgroups. A characteristic type of mineralization in the studied area are alpine veins. A special feature that characterizes the Tribeč region is lazulite paragenesis, which is found in Slovakia only in this area. This paragenesis is characterized by the presence of several phosphates, some of which are rare (eg gorceixite, goyazite, svanbergite, crandallite). The work provides a summary of previous research work and knowledge from the region of Tribeč, and gives a list of available literature and points out methods of studying mineral associations. The final parts of the work also present the first partial results of own field and laboratory research work.