Geoelectric studies of the south Voronezhcrystalline massif


  • I. Logvinov S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Ukraine
  • V. I. Tregubenko Ukrainian State Geological Survey Institute of the Ministry of Ecology and Natural Resources of Ukraine, Ukraine
  • V. N. Tarasov S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Ukraine



electrical conductivity, the crust Voronezh Massif


The first results of interpretation of magnetic variation data, focused on the three profiles in the southern part of the Voronezh crystalline massif by the two-dimensional inversion have been pre-sented. Several objects of low resistance, the roof of which is located at the depth of less than 10 km have been subdivided. The most reliable object spatially correlates with the Belgorod-Mikhailovsk greenstone belt (and the spread of ferruginous quartzites of the Kursk Magnetic Anomaly).


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How to Cite

Logvinov, I., Tregubenko, V. I., & Tarasov, V. N. (2014). Geoelectric studies of the south Voronezhcrystalline massif. Geofizicheskiy Zhurnal, 36(2), 75–84.




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