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The wealth of the bowels of Kazakhstan has not yet been exhausted, there are promising areas that are currently insufficiently studied, especially at depth. The reason for the insufficient knowledge of geological structures in depth is the lack of a theoretical basis for geological research and justification for the forecast of prospect for minerals. In this regard, geology faces the question of creating a scientific approach for predicting new prospect areas, especially at depth. Our analysis shows that the princ...

The studied intrusive massif is an ellipse elongated in the sublatitudinal direction. Only the eastern part, 2.2x4 km in size, is exposed on the earth surface. Under the sediments, the intrusion was traced by boreholes and aeromagnetic survey. The intrusion is a sheetlike body of a fractured nature, inclined to the southwest. A zone of marmorized limestones, as well as tremolite and wolastonite hornfelses, formed at the contact with the intrusion. Among the intrusive rocks that make up the massif, three successive...

The Shu-Ile tectonic zone is located along the Jalaiyr-Naiman deep fault (geosuture). It stretches in a northwestern direction, passing in the northern part of the territory into a submeridional direction. It stretches in a narrow strip of about 600 km and is a section of the second ring structure of Kazakhstan. Deposits and occurrences of iron, chromium and non-ferrous metals, gold and rare metals are associated with this geosuture zone. In general, the tectonic structure of the area is quite complex due to the d...