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Vol 52 Iss. 2
Pages:
53-57
Download volume:
RUS
Article

Structure of the Vuorijärvi massif

Authors:
F. P. Semilyakin
Date submitted:
1966-08-21
Date accepted:
1966-10-06
Date published:
1966-12-09

Abstract

The Vuoriyarvi massif belongs to the Paleozoic intrusive complex of ultrabasic alkaline rocks and carbonatites of the Kola Peninsula and Northern Karelia. Deposits and ore deposits of various ore and non-metallic minerals are confined to such massifs. Each type of minerals belongs to certain rocks composing a complex complex: ultrabasic rocks - titanium and phlogopite-vermiculite mineralization, carbonatites - rare elements. The issues of mineralogy, petrography and genesis of Vuorijärvi massif were paid much attention by many researchers. We have made an attempt on the basis of field studies to present the structure of the massif and the history of its formation ...

Область исследования:
(Archived) Without section
Funding:

None

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References

  1. Borodin L. S. To petrography and genesis of the Vuoriyarvi massif. Tr. IMGRE, vol. 9, 1962.
  2. Bolotovskaya N. A. Magmatic complex of ultrabasic, alkaline and carbonatite rocks of the Vuoriyarvi massif. Zapiski VMO, pt. 87, vol. 3, 1958.
  3. Bolotovskaya N. A., Kukharenko A. A. About types of carbonatite deposits and their connection with massifs of ultrabasic alkaline rocks. Izv. AN SSSR, ser. geol. 1, 1959.
  4. Ginzburg A. I. et al. Geology of deposits of rare elements. Iss. 1, Gosgeoltekhizdat, 1958.
  5. Egorov L. S. Geology and petrography of igneous rocks of the Tulinskaya intrusion. Tr. NIIGA, vol. 122, 1961.
  6. Eliseev N. A. Structural Petrology. Izd-vo LGI, 1953.
  7. Kukharenko A. A. et al. Paleozoic complex of ultrabasic alkaline rocks and carbonatites of the Kola Peninsula and Northern Karelia. M., Nedra, 1965.
  8. Moiseev. On the question about the process of formation of the Lovozero alkaline massif. Tr. IMGRE, vol. 9, 1962.
  9. Anderson E. M. Proc. Roy. Soc. Edinburgh, V. 57.2, 1936,
  10. Ресоra W. T. Bull. Geol. Soc. America, vol. 67, 1956.

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