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Geology of Ore Deposits

, Volume 54, Issue 8, pp 674–675 | Cite as

Finding of zonal wolframoxiolite and its genetic implication

  • V. I. AlekseevEmail author
  • Yu. B. Marin
Minerals and Parageneses of Minerals
  • 55 Downloads

Abstract

Wolframoxiolite with a sectorial distribution of components is described from Li-F granite. The ontogenetic features provide evidence for the primary origin of wolframoixiolite and geochemical evolution of the mineral-forming medium.

Keywords

Marin Geochemical Evolution Sectorial Distribution Granitic Pegmatite Light Zone 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

References

  1. Alekseev, V. I., Gembitskaya., I. M., and Marin Yu. B., Wolframoixiolite and Niobian Ferberite from Zinnwaldite Granitic Rocks of the Chukchi Peninsula, Geol. Ore Deposits, 2011, vol. 53,spec. issue 7 (Zapiski Russian Mineral. Soc.), pp. 639–648.CrossRefGoogle Scholar
  2. Voloshin, A.V., Tantalo-niobaty. Sistematika, kristallokhimiya i evolutsiya mineraloobrazovaniya v granitnykh pegmatitakh (Tantalo-Niobates. Systematics, Crystal Chemistry, and Evolution of Mineral Formation in Granitic Pegmatites), St. Petersburg: Nauka, 1993.Google Scholar
  3. Ginzburg, A.I., Gorzhevskaya, S.A., and Sidorenko, G.A., Wolframoixiolite—a Variety of Ixiolite, Zap. Vses. Miner. O-va, 1969, vol. 98, no. 1, pp. 63–73.Google Scholar
  4. Kornetova, V.A., Borisovsky, S.E., Boyarskaya, R.V., et al., On the Nature of Wolframoixiolite, in Novye dannye o mineralakh (New Data on Minerals), Moscow, 1982, no. 30, pp. 117–130.Google Scholar

Copyright information

© Pleiades Publishing, Ltd. 2012

Authors and Affiliations

  1. 1.St. Petersburg Mining UniversitySt. PetersburgRussia

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