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
Experience of application of spatial DOM observation systems in the study of the southeastern pericline of the Pechenga structure
1974 L. M. Dvoretskaya, I. V. Litvinenko, M. E. Melamud
About the possibility of using industrial currents in geological mapping and searching for ore deposits
1974 V. S. Muzylev
Methods and results of studying the velocity section of the Pechenga structure
1974 L. K. Kokorina, I. V. Litvinenko, M. D. Lizinsky, Z. Kh. Telyakova