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GEOTECTONIC POSITION, AGE AND ORE POTENTIAL OF INTRUSIVE-DYKE BELTS IN EAST KAZAKHSTAN
Abstract
With the theoretical concepts of mobilism discusses the features of the geological structure, age and ore potential of intrusive-dyke belts in the Carboniferous-Permian of Eastern Kazakhstan. Emphasizes the genetic relation of gold deposits with prebatholithic belts the North-Western direction, represented fault small intrusions and dykes Qunush complex (C3) collisional type, and spatial distribution in them later imposed rare metal mineralization of the contact-metasomatic nature. Rare metal deposits are characterized by great variety. Most of the studied morphogenetic types of spatial and genetically associated with Late Hercynian granites of normal and high alkalinity. Most fully manifested in Qalba-Narym zone, the model objects are also inherent in the Zharma-Saur, Chingiz-Tarbagatai, Irtysh and Holzyn-Sarymsakty zones. The characteristic of rare metal and rare earth mineralization of Keregetas-Espinsky complex (P1-P2), which associated with altered alkaline granites (by example on Verkhnee Espe deposit).
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