Aeromagnetic survey data on the tectonics of the south-eastern margin of the Pechenga structure
Authors:
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
Funding:
None
References
- 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.
- Gilyarova M.A. Stratigraphy and structure of the Pechenga. PH LSU, 1967.
- Zagorodny V. G., Mirskaya D. D., Suslova S. N. Geologic Structure of the Pechenga Sedimentary-Volcanogenic Series. M. L., Nauka, 1964.
- Lyubavin L.M., Murova E.V. Complex aeroelectromagnetic survey for geologic mapping on the Kola Peninsula. - Soviet Geology, 1969, No. 2.
- 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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