Metasomatic Rocks of Gold Deposits and Their Connection with Ore Process of Mountain Auminzatau (Central Kyzylkum)

The metasomatic rocks of gold-ore deposits of the Auminzatau Mountains (Central Kyzylkum), which are similar in mineral composition and their features of the formation, are distinguished. The corresponding stages of ore mineralization are associated with certain types of metasomatic rocks, which are their typomorphic signs. They reflect the features of the evolution of the stages of a unified mineral-forming system, which can be used as search criteria.

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