Abstract
The article discusses the patterns of distribution of gold mineralization in the Central Kyzylkum desert of the Southern Tien Shan. As a result of applying the methods of statistical metallogenic analysis, quantitative characteristics of the localization of gold-bearing objects were obtained, explaining some of the features of their formation in connection with the stages of the geological development of the region. It was found that the formation of the gold source and the gold deposits of the Central Kyzyl Kum itself involved all stages, from the stage of formation of the oceanic crust in the spreading zones to the stage of collision and associated metamorphism.
Sign-in/Register to access full text options 
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
