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
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