On the composition and age relations of dykes with mineralization at the Sokolovskoye deposit
Abstract
The Sokolovskoye magnetite ore deposit is one of the largest in the Turgai Trough. It lies among sedimentary volcanogenic rocks of Lower Carboniferous age (Civ + n), monoclinally falling to the east at angles from 40 to 60°. Structurally, the deposit is confined to the eastern wing of the anticlinal fold.
Область исследования:
(Archived) Without section
References
- Kobzar P. N. et al. Some new data on Sokolovskoye magnetite deposit. Proc. Kaz. Inst. of Mineral Raw Materials, issue 7, 1962.
- Ontoev D.O. Genesis peculiarities of magnetite deposits of Kustanay region. - In the book: Magnetite Deposits of Kustanay Region and Ways of Their Utilization. PH of the AS USSR, 1958.
- Pyatunin V. К. Sokolovskoe deposit. - In the book: Magnetite Deposits of Kustanay Region and Ways of Their Utilization. PH of the AS USSR, 1958.
- Rudenko N. I. et al. About age relations of diorite porphyrites and magnetite mineralization at the Sarbaiskoye deposit. PH of the Academy of Sciences of Kaz. SSR, ser. geol. 1968, No. 5.
- Rudenko N. I., Melnikov V. V. V., Lazarenkov V. G. On the composition and structure of intra-ore and post-ore veins in the ores of the Sokolovskoye deposit. Proc. All-Union Mineral Society, vol. 4, 4969.
- Sokolov G. A. Types and Conditions of Formation of Magnetite Iron Ores of the USSR. - In the book: Iron-Ore Base of Ferrous Metallurgy of the USSR. PH of the AS USSR, 1957.
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