Regularities of the structure of the volcanogenic-sedimentary strata of the Sarbaiskoye deposit
Authors:
Abstract
The Sarbaiskoye deposit of magnetite ores in the Kustanay region lies among deformed and metamorphosed Paleozoic rocks of monoclinal bedding, dipping 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‑hosting volcanogenic‑sedimentary sequence to the Lower Carboniferous (Middle‑Upper Viséan–Namurian).
Область исследования:
(Archived) Without section
Funding:
None
References
- Geologic structure of the Turgai trough. Tr. VSEGEI, nov. ser., 1961, vol. 53.
- Korzhinsky D.S. Sketch of metasomatic processes. Sbornik Osnovnye problemy v uchenii o magmatogennykh rudnykh mestorozhdeniyakh. , Izd-vo AN SSSR, 1958.
- Kochergin I. A. Structural control of magnetite mineralization in the Turgai trough. Proc. of the Academy of Sciences of Kaz. SSR. Ser. geol., Izv. AN 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. , Sbornik Magnitovye rudy Kustanayskoy obl. i puti ikh ispolzovaniya. , Izd-vo AN SSSR, 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. Tr. VSEGEI, ., nov. ser., 1961, vol. 43.
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