Geoelectric studies of the Belgorod-Sumy megablock of the northern slope of the Dnieper-Donets Trough

Authors

  • B. Shirkov S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Kyiv, Ukraine
  • O. Perestyuk S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Kyiv, Ukraine
  • A. Kushnir S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Kyiv, Ukraine

DOI:

https://doi.org/10.24028/gzh.0203-3100.v37i5.2015.111163

Keywords:

magnetotelluric sounding, magnetovariational profiling, the Dnieper-Donets Trough

Abstract

Processing of long-term Earth’s electromagnetic field observations was performed using two software systems (PRC_MTMV and PTS), frequency distribution of the amplitude and phase of impedance, apparent resistivity, horizontal components of the magnetic tensor and tipper were obtained. Minimum on the descending part of ρk curves according to the results of a qualitative assessment corresponds to the conductor at a depth of 50—150 km.

References

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Published

2015-10-01

How to Cite

Shirkov, B., Perestyuk, O., & Kushnir, A. (2015). Geoelectric studies of the Belgorod-Sumy megablock of the northern slope of the Dnieper-Donets Trough. Geofizicheskiy Zhurnal, 37(5), 176–182. https://doi.org/10.24028/gzh.0203-3100.v37i5.2015.111163

Issue

Vol. 37 No. 5 (2015)

Section

Scientific Reports

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