Methods and results of studying the velocity section of the Pechenga structure
Abstract
To study the deep structure of the Pechenga ore district, seismic exploration by the reflected-wave method (RWM) has been successfully applied in recent years. The consistent complication of the tasks being solved causes a need to detail the ideas about the velocity section of the studied area, for which data from both downhole and surface seismic observations are used.
Область исследования:
(Archived) Without section
Funding:
None
References
- Lenina I. S. Refracted waves in the study of the velocity section of the Pechenga region. Zapiski Gornogo Instituta, 1963, vol. 46, issue 2 (in Russian)
- Lizinsky M. D. Features of the methodology and some results of seismic logging in the Pechenga area. In the book: New Research in Geology. L., Izd. LGI , 1969 (in Russian)
- Litvinenko I. V. Seismic method in the study of the deep structure of the Baltic Shield. Zapiski Gornogo Instituta, 1963, vol. 46, issue 2 (in Russian)
- Litvinenko I. V., Lenina I. S. Some results of the study of the deep structure of the Pechenga structure by seismic survey. In the book: Geology and Deep Structure of the Eastern Part of the Baltic Shield. L., Nauka, 1968 (in Russian)
- Litvinenko I. V., Kokorina L. K. Structure of the Earth's crust of the Pechenga area. In the book: State and Tasks of Exploration Geophysics. Materialy VI Vsesoyuzn. nauchn.-tekhn. geofiz. konf. v g. Leningrade. M., Nedra, 1970 (in Russian)
- Litvinenko I. V., Nekrasova K. A. Differentiation of crystalline rocks by elastic properties on the example of Northern Karelia. Zapiski Gornogo Instituta, 1963, vol. 46, issue 2 (in Russian)
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