Types of phenite metasomatites of contact halo of Magan massif (Maimecha-Kotui province)
Authors:
Abstract
The Magan massif belongs to the Maimecha-Kotui province of alkaline, ultramafic rocks and carbonatites.
Область исследования:
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References
- Apatite deposits of Maymecha-Kotui province and their geological and economic evaluation. Edited by Yu.N.Zanin. Novosibirsk, Nauka, 1983. 83 p.
- Bagdasarov Yu.A., Voronovsky S.N., Arakelyants M.M. About the age of ultramafic-alkaline massifs of the Maimecha-Kotui province. - Sov. geol. 1985, No. 4, 103-107.
- Danilin E.L., Bagdasarov Yu.A., Bogaditsa V.P. Eudialyte with low zirconium content from tveitosites of Magan massif. In the book: Krasnoyarsk Book Publishing House, 1977, vol. 4, 44-47.
- Danilin E.L., Bogaditsa V.P. Some regularities in ore bodies of the Magan deposit.
- in ore bodies of the Magan deposit /Maymecha-Kotui province. In the book: Alkaline magmatism and apatite-bearing capacity of the north of Siberia. L., ed. NIIGA, 1980, p. 77-83.
- Lazarenkov V.G. Geochemistry of the zonal phenite halo of the Yraas massif. – Journal of Mining Institute, 1985, v. 104, p. 46-50.
- Lazarenkov V.G., Stepanov V.A. Zonal phenite halos of alkaline massifs of the Maimecha-Kotui Province. - In the book: Metasomatism and ore formation. Moscow: Nauka, 1984, pp. 37-45.
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