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Vol 104
Pages:
61-68
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RUS
Article

Vertical zonality and main types of altered rocks of the Aksai greisen deposit

Authors:
Yu. L. Gulbin
Date submitted:
1984-08-11
Date accepted:
1984-10-07
Date published:
1985-04-30

Abstract

Mineralized domes - one of the most common morphological types of greisen - are of interest not only from a practical point of view as concentrators of tin, tungsten, molybdenum and other rare metals, but also in terms of studying the vertical zonation.

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References

  1. Beskin S.M., Larin V.N., Marin Y.B. Rare-metal granite formations. L., Nedra, 1979. 280 p.
  2. Gulbin Yu.L., Skublov G.T. Evolution of greisen formation at the Aksai deposit (Central Kazakhstan). - In the book: Theses of reports of the 3rd Kazakhstan petrographic meeting. Alma-Ata, Nauka, 1984, p. 174-175.
  3. Rundquist D.V., Denisenko V.K., Pavlova I.G. Greisen deposits. M., Nedra, 1970. 328 p.
  4. Rusinov V.L., Omelyanenko B.I., Zotov A.V. et al. Some Aspects of the Problem of Vertical Metasomatic Zoning. - In the book: Problems of Vertical Metasomatic Zonality. Moscow, Nauka, 1982, p. 5-14.
  5. Skublov G.T. About zonality of the Aksai deposit (Central Kazakhstan). Theses of reports of the fourth conference on mineralogy, geochemistry, genesis and complex use of tungsten deposits of the USSR. L., PH LSU, 1981, p.36-38.
  6. Shirkunov V.V. Geological conditions of localization of mineralization on Akchatau ore field. Abstract of Cand. dissertation. M., PH of the Peoples' Friendship University named after P.Lumumba, 1981. 30 p.
  7. Sherba G.N. Formation of rare-metal deposits of Central Kazakhstan. Alma-Ata, PH of the Academy of Sciences of the Kazakh SSR, 1960. 379 p.

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