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Vol 66 Iss. 2
Pages:
39-43
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RUS
Article

Aeromagnetic survey data on the tectonics of the south-eastern margin of the Pechenga structure

Authors:
V. P. Zakharov
Date submitted:
1973-08-20
Date accepted:
1973-10-18
Date published:
1974-02-01

Abstract

Located in the northwest of the Kola Peninsula, the Pechenga structure is a large synclinal fold composed of alternating sedimentary and volcanogenic strata.

Область исследования:
(Archived) Without section
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References

  1. Vinogradov A. N. Porphyritic granites of the northwestern part of the Kola Peninsula. In the book: Essays on Petrology, Mineralogy and Metallogeny of Granites of the Kola Peninsula. L., Nauka, 1968.
  2. Gilyarova M.A. Stratigraphy and structure of the Pechenga. PH LSU, 1967.
  3. Zagorodny V. G., Mirskaya D. D., Suslova S. N. Geologic Structure of the Pechenga Sedimentary-Volcanogenic Series. M. L., Nauka, 1964.
  4. Lyubavin L.M., Murova E.V. Complex aeroelectromagnetic survey for geologic mapping on the Kola Peninsula. - Soviet Geology, 1969, No. 2.
  5. Polyak E.A. Geological structure of the Pechenga structural zone. In the book: Geology and Deep Structure of the Eastern Part of the Baltic Shield. L., Nauka, 1968.

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