Vibroseis works is one of the main geophysical mineral exploration techniques and one of the<br>principle methods of studying the deep structure of the earth interior. In the process of depth<br>and regional investigations, vibroseis works turned out to be most effective when correlating<br>into excitation and recording of reflected waves based on the SRM – CDP multifold reflection<br>seismic survey, which made it possible to record waves from the top of the basement to<br>Mohorovicic discontinuity. There are quite a few examples of successful regional works in<br>Russia: the intersections of the Southern Urals and the adjacent areas of the east of the<br>Russian Plain and Karelia, the traverse through Magadan region to north-east, to the ocean,<br>etc.


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