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Electromagnetic sounding of the Earth’s crust in the vicinities of the SG-6 and SG-7 superdeep boreholes in the fields of natural and powerful controlled sources |
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| Authors: | A A Zhamaletdinov M S Petrishchev A N Shevtsov V V Kolobov V N Selivanov O A Esipko E A Kopytenko V F Grigorjev |
| Institution: | 1. Pushkov Institute of Earth??s Magnetism, Ionosphere, and Propagation of Radio Waves, Russian Academy of Sciences, St. Petersburg Branch, St. Petersburg, Russia 2. Geological Institute, Kola Science Center, Russian Academy of Sciences, Murmansk oblast, Apatity, Russia 3. Center for Physical-Technical Problems of the North, Kola Science Center, Russian Academy of Sciences, Murmansk oblast, Apatity, Russia 4. OAO NPTs Nedra, Yaroslavl, Russia 5. OOO VEGA, St. Petersburg, Russia 6. Polar Geophysical Institute, Kola Science Center, Russian Academy of Sciences, Murmansk oblast, Apatity, Russia |
| Abstract: | The results of electromagnetic sounding of the Earth??s crust in the vicinities of the SG-6 and SG-7 superdeep boreholes (Yamal-Nenets Autonomous Okrug) are presented. The studies were conducted in the fields of natural sources (AMT-MTS) and in the field of the Zevs ULF antenna located at a distance of more than 2000 km from the receiver points. In the vicinity of the SG-7 superdeep borehole, where the small industrial noise was observed, the results of inverse problem solution are completely consistent with the electric logging data. The conducting layers have been identified at the depths of 150 m and 1.1 km. The roof of rocks having small electrical conductivity and belonging to the Permian-Triassic trappean complex has been found at the depth of about 7 km. The response of the Zevs signal (the frequency range of 44?C182 Hz) has indicated the properties of the upper part of the geoelectrical section better than audiomagnetotelluric sounding for both boreholes. Based on the sounding in the vicinity of the SG-6 superdeep borehole, with the data of the Novosobirsk observatory taken into account, the distribution of resistivity down to about 800 km depth has been obtained. This distribution can serve as additional information in calculation of the temperature and rheological regime of the lithosphere and the upper mantle in the region of Western Siberia. |
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