Methods and results of studying the velocity section of the Pechenga structure
Abstract
To study the deep structure of the Pechenga ore district, the reflected wave seismic (RWS) method has been successfully applied in recent years. Consistent complication of the tasks solved in this case, causes the need to detail the ideas about the velocity section of the studied area, for which data from both borehole and ground seismic observations are used.
Область исследования:
(Archived) Without section
References
- Lenina I. S. Refracted waves in the study of the velocity section of the Pechenga region. –Journal of Mining Institute, 1963, vol. 46, iss. 2.
- 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., PH LMI, 1969.
- Litvinenko I. V. Seismic method in the study of the deep structure of the Baltic Shield. Journal of Mining Institute, 1963, vol. 46, iss. 2.
- 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.
- Litvinenko I. V., Kokorina L. K. Crustal structure of the Pechenga area. In the book: State and Tasks of Exploration Geophysics. Proceedings of the 6th All-Union Scientific and Technical Geophysical Conference in Leningrad. M., Nedra, 1970.
- Litvinenko I. V. Nekrasova K. A. Differentiation of crystalline rocks by their elastic properties on the example of Northern Karelia. 46, vol. 2.
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