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Many exploited mineral deposits are at the final stage of development. The depletion of mineral reserves leads to a reduction in the volume of production and output, as well as to the social tension of single-industry towns, whose activities are directly dependent on the mining and processing industries of the economy. In our research, the initial data are the materials of geological observations and testing of tailings storages of the copper ore beneficiation factories of Kazakhstan. Studies on the composition an...

The lack of new deposits with a rich copper content and the depletion of old deposits, as well as the need to comply with environmental requirements, raises the issue of the need to process the tailings of metallurgical industries. In Kazakhstan was accumulated significant stocks of tailings "Borgezsay" and "Staroye". The tailings reserves are estimated at up to 1 billion tons. Sample evaluation showed that the average copper content in the tailings is 0.15-0.2%. More than 1 million tons of copper are stored in th...

Currently, to replenish mineral resources of Kazakhstan, the discovery of mineral deposits in areas covered by Cenozoic deposits is important. They are located quite deep. The forecast of such minerals requires the creation of a reliable scientific base and the use of innovative cosmogeological research methods. The geotectonic structure and geodynamics of the Paleozoic and Proterozoic basement of the territory of Kazakhstan is now successfully explained from the position of the conventional plume tectonics. In ac...

The Sayak ore district is located in the north-eastern part of the Balkhash region and contains industrial molybdenum-copper and gold mineralization, which is represented mainly by skarn deposits, as well as smaller deposits and ore occurrences of hydrothermal-vein, porphyry and karst types. They are located mainly in the eastern part of the Sayak graben-syncline, which is composed of volcanic-sedimentary rocks of the Middle and Upper Paleozoic age. The Upper Paleozoic complex is accompanied by granitoid intrusion...

At present, more 900 million tons and 630 million tons of crushed tailings of copper ores are accumulated in tailings storages of Jeskasgan and Balkhash ore-processing plants, respectively. Micromineralogical studies of tails in cemented polished sections are showed the following copper minerals: chalcopyrite is the most common among them and the amount of its grains in cemented sections varies from 30 to 50 %; covellite - from 5 to 20 %; chalcocite - from rare grains to 20 %; bornite - from 4 to 25 %. Other miner...

Kazakhstan has rich reserves of copper. Stratiform copper sandstones and copper-porphyry deposits are the main industrial types of copper ore: The largest deposit of copper sandstones is Zhezkazgan (Central Kazakhstan), and Aktogay is a large deposit of copper-porphyry type (east Kazakhstan). This article describes these two deposits. The Republic of Kazakhstan is one of the world's most important provinces on reserves of copper. In Kazakhstan, there are large deposits of copper, as well as mining companies and st...

The deposit Kokkyia is located in the exocontact zone of granodiorite intrusion, and zones of hydrothermal alteration, which enclose gold mineralization, are controlled by small intrusions of diorite and syenite of the Upper Devonian intrusive complex and are located in volcanic rocks of sour alkali and medium composition. Practically all the difference of rocks are affected by the processes of hydrothermal changes and are shown as the processes of propylitic nature: albitization, feldspathization, chloritization,...

Kazakhstan has a special geological structure, which is not explained in full as from the position of geosyncline paradigm, and from a position of plate-tectonics. A comparison of the actual field geological research record of the paleozoic geological structures with the principles of plume tectonics shows that they are in good agreement. According to geological data, to develop superplume and its formation took place in the Paleozoic, which lasted impulsively with Ordovician to lower Permian. The Influence of thi...

With clastic sedimentary rocks associated deposits of ore, oil-and-gas, coal and non-metallic minerals. They are located in a variety of different age strata structural-tectonic stages. Sedimentary rocks composing these fields are often framework rocks or minerals themselves are economic minerals. Depending on the age and affinity to specific structural and tectonic tier breeds are in various stages of the penecontemporaneous transformation. By the degree of transformation of organic matter in the clastic rocks ca...

Considered the natural conditions for the fo rmation of gold, given the model of its deposits in the form of a schematic of industrial-genetic classification. Were shown the main types and examples of fields. We have created a model can serve as the scientific basis for prediction and exploration of new industrial facilities to enhance the mineral resource base of mining and processing enterprises of Kazakhstan.