Abstract
The geodynamic model reflects the staged development of the geological and metallogenic structures of the Greater Altai. Spatially, the Great Altai occupies the territory of Eastern Kazakhstan. The features of the geodynamic development of the geological structures of the Greater Altai are considered. The territory covers the southeastern flanks of the Rudny Altai and Kalba tectonic zones of the Greater Altai, which are part of the general system of the Central Asian mobile belt. The spatial conjugation of geological and ore-bearing structures of different age and composition, subject to intense metamorphic and hydrothermal-metasomatic transformations under the influence of the Dzhungar massif and the Siberian Plate and subsequent thrust-shear deformations, is emphasized.
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