Abstract
The integrated use of natural resources creates a necessary condition for the development of the industry of the mineral resource base of Kazakhstan. In the mineral resource complex, lead-zinc deposits are of paramount importance. The article discusses the features of mineralization, and also presents the geological structure of the Dyusembay deposit. The formation of the modern appearance of the tectonic structures of the region is due to very complex and lengthy geological processes. During the research, stock materials and modern geological materials on the Dyusembay deposit were considered.The conditions of formation and placement, metallogeny of the lead-zinc deposit Dyusembay were studied. The study area is located within the development of the Ulutau-Arganata meganticlinorium, which is subdivided into the Karsakpai synclinorium, the Maytyubinsk anticlinorium, and the Baikanur synclinorium. The Dyusembay deposit is located within the eastern wing of the Maytyubinsk anticlinorium.
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