Distribution and migration of trace elements in metamorphic rocks of the Chupinsky district (North Karelia)
Authors:
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
- Nikitin V. D. Influence of host rocks on the type of mineralization of endogenous deposits. ZVMO, 1959, pt. 88, vol. 5.
- Nikitin V. D. Modern state of the doctrine of processes and conditions of pegmatite formation. Journal of Mining Institute, 1959, v. 40, iss. 2.
- Nikitin V. D. Processes of recrystallization and metasomatosis in mica-bearing and ceramic pegmatites. Journal of Mining Institute, 1952, 27, vol. 2.
- Shmakin B.M., Makrygina V.A. Geochemical Features of Muscovite Pegmatites and Their Contact Halo. Nauka, 1969.
- 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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