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
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.
Similar articles
Depth of electrical exploration by methods of dipole inductive profiling and ungrounded loop
1974 V. H. Zakharov
About macro- and microrelief of the Mohorovičić discontinuity on the Baltic Shield
1974 I. V. Litvinenko, L. N. Platonenkova, N. I. Suvorova