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Renium-osmiy-silver-copper deposits of Zhezkazgan type with zinc and lead have magmatogenhydrothermal nature and are localized in terrigenous-sand thicker in the upper intra-continental sedimentary basins. Localisation of rich complex ores in nodes of contacts of ultradeep fractures with radical breaks is determined by the raise of deep ore bearing fluids along these nodded areas. Granitogen deposits of rare metals and rare lands genetically is linked to deeply specialized potassium-plumazit and alkali granites.
The large skarnovo-magnetite deposits of Torgay belt are associated with high calcic andesit-basalt-gabbro-diorit formation in postoceanic grooves. Sodium-silicon- ferriferous solutions separated as a result of early crystallization of plagioclase and calcium-magnesium femic minerals and then concentrated at the base of magma center by gravitational accumulation as well as squeezing out on consolidation downwards. This led to the formation of iron sodium-enriched silicon fluid in the foot of magma columns. These fluids raised following the gabbro-diorit small intrusions and replaced carbonate rocks in andesit-basalt volcanogen-sedimentary cut.
Metasomatic and hydrothermal sedimentary- volcanogen gold ores of stepnyakskiy type (North Kazakhstan) arising from the hydrothermal island arched andesit-basalt and gabbro-sienodiorit-granosienit formations of lateoceanic stage. The second type of large-scale gold mineralization is linked to the border depth zones at the junction of the ocean - the continent. Industrial gold-is the result of tectonic-deformation, plutono-mobilization metamorophogen and hydrothermal-metasomatic conversion of gold containing thickness. Examples of such large deposits - Kumtor (Kyrgyzstan), Muruntau (Uzbekistan), Sukhoi Log (Russia). The third type is related to the peripheral areasd of continental-margin volcanic belts and are formed by means of metamorphogen mobilization of gold thickness. The fourth type is revealed in the inner area of continental-margin volcanic belts and associated with hydrothermal-riolit volcanism in the form of land-stratovolkanos.
The fifth gold mineralization type is revealed in axial paleooceanic zones along the periphery bazit-hyperbazit- alpine types belts.
The large chromite deposit with titanium-magnetite-nickel-vanadium mineralization is genetically linked to dunit- troktolit-gartsburgity formation, formed in the original bundle of oceanit-gartsburgit magma system on gravitational model.
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