Abstract
The characteristics of mineral composition and features of metasomatic rocks of gold ore deposits of the Auminzatau mountains in the Central Kyzylkum are identified. The corresponding stages of ore mineralization are associated with certain types of metasomatites, which are their typomorphic features and reflect the features of the evolution of the stages and stages of a single mineral-forming system, which can be used as search criteria.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
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
