Geological and geophysical methods using for Syktyvkar weakened zones detection

Weakened zones detection requires complex application of geophysical methods (geoelectric and seismometry) using of geological and geotechnical data in the soil body of the upper geological section part. The area was selected as an experimental object in the Syktyvkar neighborhood Ezhva reffered to the unfavorable area of constructing according to the outside condition of buildings. Our geophysical researches determined weakened zones represented by interstratifications of plastic clays (clay loams) and watered sandy loams and/or fine-grained sands.