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Vol 64 Iss. 2
Pages:
23-29
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RUS
Article

Distribution and migration of trace elements in metamorphic rocks of the Chupinsky district (North Karelia)

Authors:
G. M. Arutyunov
Date submitted:
1973-08-28
Date accepted:
1973-10-08
Date published:
1974-02-01

Abstract

Long-term prospecting and exploration works in the Kola-Karelian region have established the confinement of mica-bearing pegmatites to alumina gneisses, theoretically substantiated by G. I. Buntin, D. I. Buntin, and D. I. Buntin. I. Buntin, D. S. Korzhinsky, V. D. Nikitin.

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References

  1. Nikitin V. D. Influence of host rocks on the type of mineralization of endogenous deposits. ZVMO, 1959, pt. 88, vol. 5.
  2. Nikitin V. D. Modern state of the doctrine of processes and conditions of pegmatite formation. Journal of Mining Institute, 1959, v. 40, iss. 2.
  3. Nikitin V. D. Processes of recrystallization and metasomatosis in mica-bearing and ceramic pegmatites. Journal of Mining Institute, 1952, 27, vol. 2.
  4. Shmakin B.M., Makrygina V.A. Geochemical Features of Muscovite Pegmatites and Their Contact Halo. Nauka, 1969.
  5. Shurkin K. A. et al. The White Sea Complex of Northern Karelia and the South-West of the Kola Peninsula. AS USSR, 1962.

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