Abstract
The variety of sizes and morphology of grains and chemical composition of native Au, and the diversity of mineral productive associations in the new ore occurrences of the Western and Central Taimyr (the Minina–Bolshevik miogeocline and the Shrenk–Faddeevskaya accretionary mineragenic zones) indicate the complex multicomponent composition of ore-forming systems and different physicochemical conditions of the formation of gold ore mineralization. The native Au characteristics and specific features of the geological structure of the objects point to the significant gold ore potential of the Central Sector of the Russian Arctic.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
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
