Experience in dissection and correlation of the buried Paleozoic sedimentary-volcanogenic strata in the iron-ore regions of the Turgai Trough
Authors:
Abstract
The areas under consideration are located in the western part of the Turgai trough, within the Valerianov structural-formation zone. Intensive geologic and exploration works on revealing and exploration of skarn-magnetite deposits and other minerals are carried out in the areas. Deposits lie in the folded Paleozoic basement overlain by a cover of Mesozoic and Cenozoic sediments.
Область исследования:
(Archived) Without section
References
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- Galperov G. V., Pertsov A. V., Brusnichnica N. A. Aeromethods of geologic study of areas of two-tier structure (on the example of the Turgai Trough). L.: Nedra, 1979, 111 p.
- Moskalenko A. I. On partitioning of sedimentary-volcanogenic strata and principles of correlation of lithologic-stratigraphic sections at magnetite deposits of the Sokolovsko-Sarbaisky ore cluster // Issues of geology and magmatism of the Urals / Ural Branch of the USSR Academy of Sciences. Sverdlovsk, 1970. P. 44-48.
- Porotov G. P. Relation of magnetite deposits of the Turgai Trough with paleovolcanic structures // Geology and genesis of iron ore deposits. / Ural Scientific Center of the USSR Academy of Sciences. Sverdlovsk, 1981. P. 25-34.
- Porotov G. S., Veselov E. V. Formation features of the Kachar deposit in the Turgai trough // Notes of All-Union Mineral Society. 1983. Iss. 5. P. 535-547.
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