Practice of transition zone delineation in ores of Verkhnekairaktinskoye deposit
Authors:
Abstract
The "transition zone" of the deposit is characterized and correlated with the horizon of disintegration and reduction processes of hypergenesis zones. Visual and mineralogical criteria for determining the boundaries of intervals characterized by reduced recoveries from tungsten trioxide ores were tested.
Область исследования:
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References
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- Izoitko V.M. Technological mineralogy of tungsten ores. L.: Nauka, 1989. 232 p.
- Verkhneye Kayrakty deposit / G.I.Bedrov, S.P.Krovyakov, V.G.Li, L.B.Ivanov/ Metallogeny of Kazakhstan. Ore formations. Deposits of rare metal ores. Alma-Ata: Nauka, 1981. P. 88-93.
- On the formation affiliation of near-ore metasomatites of Verkhnekayraktinskoye deposit / V.I.Chernov, S.A.Kaiser, A.V.Ivanchuk et al. // Sov. geolog. 1984. № 4. P. 90-93.
- Rare-metal mineralization of Kazakhstan / G.N.Shcherba, A.V.Kudryashov. N.P.Senchilo et al. Alma-Ata: Nauka, 1988. P. 99-178.
- Chernov V.I., Kiseleva V.S. Experience in the application of thermal analysis to determine the mineral composition of oxidized ores of Verkhnekayraktinskoye deposit // Typomorphic features and technological properties of minerals of ore and nonmetallic deposits of useful resources. Kazakhstan and their practical significance / Kaz. Research Institute of mineral raw materials. Alma-Ata. 1984. P. 91-96.
- Yakhontova L.K., Grudev A.P. Mineralogy of oxidized ores Reference book. Moscow: Nedra, 1987. 198 p.
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