Regularities of the structure of the volcanogenic-sedimentary strata of the Sarbaisky deposit
Authors:
Abstract
Sarbaiskoye deposit of magnetite ores in the Kustanay region lies among dislocated and metamorphosed Paleozoic rocks of monoclinal bedding, falling to the west at an angle of 45-50° and overlain by horizontally bedded Meso-Cenozoic sediments with a thickness of 70-130 m. E. A. Mazina attributes the ore-bearing volcanogenic-sedimentary strata to the Lower Carboniferous (middle-upper Vise-Namur).
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References
- Geologic structure of the Turgai trough. Proc. VSEGEI, new series, 1961, vol. 53.
- Korzhinsky D.S. Sketch of metasomatic processes. Coll.: Basic Problems in the Doctrine of Magmatogenic Ore Deposits. PH of the AS USSR, 1958.
- Kochergin I. A. Structural control of magnetite mineralization in the Turgai trough. Proc.of the Academy of Sciences of Kaz. SSR. Ser. geol., 1961, vol. 1 (42).
- Kochergin I.A. and Pyatunin V. K. The latest data on the geology of Sarbaisky and Sokolovskiy iron-ore magnetite deposits. Coll.: Magnetite ores of Kustanay region and ways of their utilization. PH of the AS USSR, 1958.
- Mazina E. A. and Ksenofontov O. K. Features of magmatism of the northern part of the Turgai Trough and the main stages of its development. Proc. VSEGEI, new ser., 1961, vol. 43.
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