Aeromagnetic survey data on the tectonics of the southeastern frame of the Pechenga structure
Authors:
Abstract
Located in the northwest of the Kola Peninsula, the Pechenga structure is a large synclinal-type 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 (in Russian)
- Gilyarova M. A. Stratigraphy and structure of the Pechenga. Izd. LGU ,1967 (in Russian)
- Zagorodny V. G., Mirskaya D. D., Suslova S. N. Geological Structure of the Pechenga Sedimentary-Volcanogenic Series. M.–L., Nauka, 1964 (in Russian)
- Lyubavin L. M., Murova E. V. Complex aeroelectromagnetic survey for geological mapping on the Kola Peninsula. Sovetskaya geologiya , 1969, No. 2 (in Russian)
- 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 (in Russian)
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