Stratiform copper mineralization of hydrothermal-sedimentary type in the Kachar ore field
Abstract
In recent years, several zones and points of copper mineralization have been established at the Kachar magnetite deposit (North Kazakhstan) and adjacent territory.
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References
- Butuzova G.Yu. To the problem of modern hydrothermal ore formation in the rift zone of the Red Sea. - In the book: Conditions of formation of rare-metal and lead-zinc stratiform deposits. Moscow, Nauka, 1982, p. 37-38.
- Veselov E.V. Relation of copper mineralization of the Kachar deposit with acidic submarine volcanism. – Journal of Mining Institute, 1985, vol. 104, p.20-26.
- Veselov E.V. Types of copper mineralization at the Kachar magnetite deposit. - Proc. of the Academy of Sciences of the Kazakh SSR, ser. geol., 1983, No. 6, p. 34-41.
- Porotov G.S., Veselov E.V. Formation features of the Kachar deposit in the Turgai trough. - Proc. of AUMS, 1983, issue 5, p. 535-547.
- Porotov G.S., Veselov E.V. About genesis of acidic rocks of the Kachar magnetite deposit. - Geology and Geophysics, 1972, No. 3, p. 123-127.
- Skripchenko N.S. Hydrothermal-sedimentary sulfide ores of basaltoid formations. M., Nedra, 1972. 214 p.
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