Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment)
Abstract This article is devoted to describing the theory, technique, and first experimental results of a control source electromagnetic (CSEM) study of the Earth’s crust and ionosphere with the use of two mutually orthogonal industrial transmission lines 109 and 120 km in length in the frame of FEN...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhamaletdinov, A. A. [verfasserIn] |
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| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
extremely low frequency band (ELF) |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2015 |
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| Übergeordnetes Werk: |
Enthalten in: Izvestiya - Moscow : MAIK Nauka/Interperiodica Publ., 2006, 51(2015), 8 vom: Dez., Seite 826-857 |
|---|---|
| Übergeordnetes Werk: |
volume:51 ; year:2015 ; number:8 ; month:12 ; pages:826-857 |
| Links: |
|---|
| DOI / URN: |
10.1134/S0001433815080083 |
|---|
| Katalog-ID: |
SPR020054238 |
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| 100 | 1 | |a Zhamaletdinov, A. A. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment) |
| 264 | 1 | |c 2015 | |
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| 337 | |a Computermedien |b c |2 rdamedia | ||
| 338 | |a Online-Ressource |b cr |2 rdacarrier | ||
| 500 | |a © Pleiades Publishing, Ltd. 2015 | ||
| 520 | |a Abstract This article is devoted to describing the theory, technique, and first experimental results of a control source electromagnetic (CSEM) study of the Earth’s crust and ionosphere with the use of two mutually orthogonal industrial transmission lines 109 and 120 km in length in the frame of FENICS (Fennoscandian Electrical Conductivity from Natural and Induction Control Source Soundings) experiment. The main part of the measurements is executed on the territory of the Fennoscandian shield at distances from the first hundreds kilometers up to 856 km from the source with the purpose of the deep electromagnetic sounding of the Earth’s crust and upper mantle. According to the results of these studies clarifying the parameters of “normal” (standard) geoelectric section of the lithosphere to a depth of 60–70 km, the anisotropy parameters are evaluated and a geothermal and rheological interpretation in conjunction with the analysis of the seismic data is executed. Furthermore, to study the propagation of ELF–LLF waves (0.1–200 Hz) in an “Earth–Ionosphere” waveguide, the measurements are carried out apart from Fennoscandian shield at distances up to 5600 km from the source (in Ukraine, Spitsbergen, Poland, Kamchatka, and other areas). According to the results of these studies, the experimental estimates of the influence of the ionosphere and of the displacement currents on the propagation of ELF–ULF waves in the upper half-space at the different azimuths generation of the primary field are obtained. | ||
| 650 | 4 | |a electromagnetism |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a deep sounding |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a controlled sources |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a extremely low frequency band (ELF) |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a ultra low frequency band (ULF) |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a industrial power lines |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a resistivity |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a normal resistivity section |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a numerical modeling |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a inverse problem |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a interpretation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Moho boundary |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a geothermal section |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a rheology |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Shevtsov, A. N. |4 aut | |
| 700 | 1 | |a Velikhov, E. P. |4 aut | |
| 700 | 1 | |a Skorokhodov, A. A. |4 aut | |
| 700 | 1 | |a Kolesnikov, V. E. |4 aut | |
| 700 | 1 | |a Korotkova, T. G. |4 aut | |
| 700 | 1 | |a Ryazantsev, P. A. |4 aut | |
| 700 | 1 | |a Efimov, B. V. |4 aut | |
| 700 | 1 | |a Kolobov, V. V. |4 aut | |
| 700 | 1 | |a Barannik, M. B. |4 aut | |
| 700 | 1 | |a Prokopchuk, P. I. |4 aut | |
| 700 | 1 | |a Selivanov, V. N. |4 aut | |
| 700 | 1 | |a Kopytenko, Yu. A. |4 aut | |
| 700 | 1 | |a Kopytenko, E. A. |4 aut | |
| 700 | 1 | |a Ismagilov, V. S. |4 aut | |
| 700 | 1 | |a Petrishchev, M. S. |4 aut | |
| 700 | 1 | |a Sergushin, P. A. |4 aut | |
| 700 | 1 | |a Tereshchenko, P. E. |4 aut | |
| 700 | 1 | |a Samsonov, B. V. |4 aut | |
| 700 | 1 | |a Birulya, M. A. |4 aut | |
| 700 | 1 | |a Smirnov, M. Yu. |4 aut | |
| 700 | 1 | |a Korja, T. |4 aut | |
| 700 | 1 | |a Yampolski, Yu. M. |4 aut | |
| 700 | 1 | |a Koloskov, A. V. |4 aut | |
| 700 | 1 | |a Baru, N. A. |4 aut | |
| 700 | 1 | |a Poljakov, S. V. |4 aut | |
| 700 | 1 | |a Shchennikov, A. V. |4 aut | |
| 700 | 1 | |a Druzhin, G. I. |4 aut | |
| 700 | 1 | |a Jozwiak, W. |4 aut | |
| 700 | 1 | |a Reda, J. |4 aut | |
| 700 | 1 | |a Shchors, Yu. G. |4 aut | |
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10.1134/S0001433815080083 doi (DE-627)SPR020054238 (SPR)S0001433815080083-e DE-627 ger DE-627 rakwb eng Zhamaletdinov, A. A. verfasserin aut Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment) 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract This article is devoted to describing the theory, technique, and first experimental results of a control source electromagnetic (CSEM) study of the Earth’s crust and ionosphere with the use of two mutually orthogonal industrial transmission lines 109 and 120 km in length in the frame of FENICS (Fennoscandian Electrical Conductivity from Natural and Induction Control Source Soundings) experiment. The main part of the measurements is executed on the territory of the Fennoscandian shield at distances from the first hundreds kilometers up to 856 km from the source with the purpose of the deep electromagnetic sounding of the Earth’s crust and upper mantle. According to the results of these studies clarifying the parameters of “normal” (standard) geoelectric section of the lithosphere to a depth of 60–70 km, the anisotropy parameters are evaluated and a geothermal and rheological interpretation in conjunction with the analysis of the seismic data is executed. Furthermore, to study the propagation of ELF–LLF waves (0.1–200 Hz) in an “Earth–Ionosphere” waveguide, the measurements are carried out apart from Fennoscandian shield at distances up to 5600 km from the source (in Ukraine, Spitsbergen, Poland, Kamchatka, and other areas). According to the results of these studies, the experimental estimates of the influence of the ionosphere and of the displacement currents on the propagation of ELF–ULF waves in the upper half-space at the different azimuths generation of the primary field are obtained. electromagnetism (dpeaa)DE-He213 deep sounding (dpeaa)DE-He213 controlled sources (dpeaa)DE-He213 extremely low frequency band (ELF) (dpeaa)DE-He213 ultra low frequency band (ULF) (dpeaa)DE-He213 industrial power lines (dpeaa)DE-He213 resistivity (dpeaa)DE-He213 normal resistivity section (dpeaa)DE-He213 numerical modeling (dpeaa)DE-He213 inverse problem (dpeaa)DE-He213 interpretation (dpeaa)DE-He213 Moho boundary (dpeaa)DE-He213 geothermal section (dpeaa)DE-He213 rheology (dpeaa)DE-He213 Shevtsov, A. N. aut Velikhov, E. P. aut Skorokhodov, A. A. aut Kolesnikov, V. E. aut Korotkova, T. G. aut Ryazantsev, P. A. aut Efimov, B. V. aut Kolobov, V. V. aut Barannik, M. B. aut Prokopchuk, P. I. aut Selivanov, V. N. aut Kopytenko, Yu. A. aut Kopytenko, E. A. aut Ismagilov, V. S. aut Petrishchev, M. S. aut Sergushin, P. A. aut Tereshchenko, P. E. aut Samsonov, B. V. aut Birulya, M. A. aut Smirnov, M. Yu. aut Korja, T. aut Yampolski, Yu. M. aut Koloskov, A. V. aut Baru, N. A. aut Poljakov, S. V. aut Shchennikov, A. V. aut Druzhin, G. I. aut Jozwiak, W. aut Reda, J. aut Shchors, Yu. G. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 51(2015), 8 vom: Dez., Seite 826-857 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:51 year:2015 number:8 month:12 pages:826-857 https://dx.doi.org/10.1134/S0001433815080083 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 51 2015 8 12 826-857 |
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10.1134/S0001433815080083 doi (DE-627)SPR020054238 (SPR)S0001433815080083-e DE-627 ger DE-627 rakwb eng Zhamaletdinov, A. A. verfasserin aut Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment) 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract This article is devoted to describing the theory, technique, and first experimental results of a control source electromagnetic (CSEM) study of the Earth’s crust and ionosphere with the use of two mutually orthogonal industrial transmission lines 109 and 120 km in length in the frame of FENICS (Fennoscandian Electrical Conductivity from Natural and Induction Control Source Soundings) experiment. The main part of the measurements is executed on the territory of the Fennoscandian shield at distances from the first hundreds kilometers up to 856 km from the source with the purpose of the deep electromagnetic sounding of the Earth’s crust and upper mantle. According to the results of these studies clarifying the parameters of “normal” (standard) geoelectric section of the lithosphere to a depth of 60–70 km, the anisotropy parameters are evaluated and a geothermal and rheological interpretation in conjunction with the analysis of the seismic data is executed. Furthermore, to study the propagation of ELF–LLF waves (0.1–200 Hz) in an “Earth–Ionosphere” waveguide, the measurements are carried out apart from Fennoscandian shield at distances up to 5600 km from the source (in Ukraine, Spitsbergen, Poland, Kamchatka, and other areas). According to the results of these studies, the experimental estimates of the influence of the ionosphere and of the displacement currents on the propagation of ELF–ULF waves in the upper half-space at the different azimuths generation of the primary field are obtained. electromagnetism (dpeaa)DE-He213 deep sounding (dpeaa)DE-He213 controlled sources (dpeaa)DE-He213 extremely low frequency band (ELF) (dpeaa)DE-He213 ultra low frequency band (ULF) (dpeaa)DE-He213 industrial power lines (dpeaa)DE-He213 resistivity (dpeaa)DE-He213 normal resistivity section (dpeaa)DE-He213 numerical modeling (dpeaa)DE-He213 inverse problem (dpeaa)DE-He213 interpretation (dpeaa)DE-He213 Moho boundary (dpeaa)DE-He213 geothermal section (dpeaa)DE-He213 rheology (dpeaa)DE-He213 Shevtsov, A. N. aut Velikhov, E. P. aut Skorokhodov, A. A. aut Kolesnikov, V. E. aut Korotkova, T. G. aut Ryazantsev, P. A. aut Efimov, B. V. aut Kolobov, V. V. aut Barannik, M. B. aut Prokopchuk, P. I. aut Selivanov, V. N. aut Kopytenko, Yu. A. aut Kopytenko, E. A. aut Ismagilov, V. S. aut Petrishchev, M. S. aut Sergushin, P. A. aut Tereshchenko, P. E. aut Samsonov, B. V. aut Birulya, M. A. aut Smirnov, M. Yu. aut Korja, T. aut Yampolski, Yu. M. aut Koloskov, A. V. aut Baru, N. A. aut Poljakov, S. V. aut Shchennikov, A. V. aut Druzhin, G. I. aut Jozwiak, W. aut Reda, J. aut Shchors, Yu. G. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 51(2015), 8 vom: Dez., Seite 826-857 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:51 year:2015 number:8 month:12 pages:826-857 https://dx.doi.org/10.1134/S0001433815080083 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 51 2015 8 12 826-857 |
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10.1134/S0001433815080083 doi (DE-627)SPR020054238 (SPR)S0001433815080083-e DE-627 ger DE-627 rakwb eng Zhamaletdinov, A. A. verfasserin aut Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment) 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract This article is devoted to describing the theory, technique, and first experimental results of a control source electromagnetic (CSEM) study of the Earth’s crust and ionosphere with the use of two mutually orthogonal industrial transmission lines 109 and 120 km in length in the frame of FENICS (Fennoscandian Electrical Conductivity from Natural and Induction Control Source Soundings) experiment. The main part of the measurements is executed on the territory of the Fennoscandian shield at distances from the first hundreds kilometers up to 856 km from the source with the purpose of the deep electromagnetic sounding of the Earth’s crust and upper mantle. According to the results of these studies clarifying the parameters of “normal” (standard) geoelectric section of the lithosphere to a depth of 60–70 km, the anisotropy parameters are evaluated and a geothermal and rheological interpretation in conjunction with the analysis of the seismic data is executed. Furthermore, to study the propagation of ELF–LLF waves (0.1–200 Hz) in an “Earth–Ionosphere” waveguide, the measurements are carried out apart from Fennoscandian shield at distances up to 5600 km from the source (in Ukraine, Spitsbergen, Poland, Kamchatka, and other areas). According to the results of these studies, the experimental estimates of the influence of the ionosphere and of the displacement currents on the propagation of ELF–ULF waves in the upper half-space at the different azimuths generation of the primary field are obtained. electromagnetism (dpeaa)DE-He213 deep sounding (dpeaa)DE-He213 controlled sources (dpeaa)DE-He213 extremely low frequency band (ELF) (dpeaa)DE-He213 ultra low frequency band (ULF) (dpeaa)DE-He213 industrial power lines (dpeaa)DE-He213 resistivity (dpeaa)DE-He213 normal resistivity section (dpeaa)DE-He213 numerical modeling (dpeaa)DE-He213 inverse problem (dpeaa)DE-He213 interpretation (dpeaa)DE-He213 Moho boundary (dpeaa)DE-He213 geothermal section (dpeaa)DE-He213 rheology (dpeaa)DE-He213 Shevtsov, A. N. aut Velikhov, E. P. aut Skorokhodov, A. A. aut Kolesnikov, V. E. aut Korotkova, T. G. aut Ryazantsev, P. A. aut Efimov, B. V. aut Kolobov, V. V. aut Barannik, M. B. aut Prokopchuk, P. I. aut Selivanov, V. N. aut Kopytenko, Yu. A. aut Kopytenko, E. A. aut Ismagilov, V. S. aut Petrishchev, M. S. aut Sergushin, P. A. aut Tereshchenko, P. E. aut Samsonov, B. V. aut Birulya, M. A. aut Smirnov, M. Yu. aut Korja, T. aut Yampolski, Yu. M. aut Koloskov, A. V. aut Baru, N. A. aut Poljakov, S. V. aut Shchennikov, A. V. aut Druzhin, G. I. aut Jozwiak, W. aut Reda, J. aut Shchors, Yu. G. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 51(2015), 8 vom: Dez., Seite 826-857 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:51 year:2015 number:8 month:12 pages:826-857 https://dx.doi.org/10.1134/S0001433815080083 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 51 2015 8 12 826-857 |
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10.1134/S0001433815080083 doi (DE-627)SPR020054238 (SPR)S0001433815080083-e DE-627 ger DE-627 rakwb eng Zhamaletdinov, A. A. verfasserin aut Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment) 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract This article is devoted to describing the theory, technique, and first experimental results of a control source electromagnetic (CSEM) study of the Earth’s crust and ionosphere with the use of two mutually orthogonal industrial transmission lines 109 and 120 km in length in the frame of FENICS (Fennoscandian Electrical Conductivity from Natural and Induction Control Source Soundings) experiment. The main part of the measurements is executed on the territory of the Fennoscandian shield at distances from the first hundreds kilometers up to 856 km from the source with the purpose of the deep electromagnetic sounding of the Earth’s crust and upper mantle. According to the results of these studies clarifying the parameters of “normal” (standard) geoelectric section of the lithosphere to a depth of 60–70 km, the anisotropy parameters are evaluated and a geothermal and rheological interpretation in conjunction with the analysis of the seismic data is executed. Furthermore, to study the propagation of ELF–LLF waves (0.1–200 Hz) in an “Earth–Ionosphere” waveguide, the measurements are carried out apart from Fennoscandian shield at distances up to 5600 km from the source (in Ukraine, Spitsbergen, Poland, Kamchatka, and other areas). According to the results of these studies, the experimental estimates of the influence of the ionosphere and of the displacement currents on the propagation of ELF–ULF waves in the upper half-space at the different azimuths generation of the primary field are obtained. electromagnetism (dpeaa)DE-He213 deep sounding (dpeaa)DE-He213 controlled sources (dpeaa)DE-He213 extremely low frequency band (ELF) (dpeaa)DE-He213 ultra low frequency band (ULF) (dpeaa)DE-He213 industrial power lines (dpeaa)DE-He213 resistivity (dpeaa)DE-He213 normal resistivity section (dpeaa)DE-He213 numerical modeling (dpeaa)DE-He213 inverse problem (dpeaa)DE-He213 interpretation (dpeaa)DE-He213 Moho boundary (dpeaa)DE-He213 geothermal section (dpeaa)DE-He213 rheology (dpeaa)DE-He213 Shevtsov, A. N. aut Velikhov, E. P. aut Skorokhodov, A. A. aut Kolesnikov, V. E. aut Korotkova, T. G. aut Ryazantsev, P. A. aut Efimov, B. V. aut Kolobov, V. V. aut Barannik, M. B. aut Prokopchuk, P. I. aut Selivanov, V. N. aut Kopytenko, Yu. A. aut Kopytenko, E. A. aut Ismagilov, V. S. aut Petrishchev, M. S. aut Sergushin, P. A. aut Tereshchenko, P. E. aut Samsonov, B. V. aut Birulya, M. A. aut Smirnov, M. Yu. aut Korja, T. aut Yampolski, Yu. M. aut Koloskov, A. V. aut Baru, N. A. aut Poljakov, S. V. aut Shchennikov, A. V. aut Druzhin, G. I. aut Jozwiak, W. aut Reda, J. aut Shchors, Yu. G. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 51(2015), 8 vom: Dez., Seite 826-857 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:51 year:2015 number:8 month:12 pages:826-857 https://dx.doi.org/10.1134/S0001433815080083 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 51 2015 8 12 826-857 |
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10.1134/S0001433815080083 doi (DE-627)SPR020054238 (SPR)S0001433815080083-e DE-627 ger DE-627 rakwb eng Zhamaletdinov, A. A. verfasserin aut Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment) 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract This article is devoted to describing the theory, technique, and first experimental results of a control source electromagnetic (CSEM) study of the Earth’s crust and ionosphere with the use of two mutually orthogonal industrial transmission lines 109 and 120 km in length in the frame of FENICS (Fennoscandian Electrical Conductivity from Natural and Induction Control Source Soundings) experiment. The main part of the measurements is executed on the territory of the Fennoscandian shield at distances from the first hundreds kilometers up to 856 km from the source with the purpose of the deep electromagnetic sounding of the Earth’s crust and upper mantle. According to the results of these studies clarifying the parameters of “normal” (standard) geoelectric section of the lithosphere to a depth of 60–70 km, the anisotropy parameters are evaluated and a geothermal and rheological interpretation in conjunction with the analysis of the seismic data is executed. Furthermore, to study the propagation of ELF–LLF waves (0.1–200 Hz) in an “Earth–Ionosphere” waveguide, the measurements are carried out apart from Fennoscandian shield at distances up to 5600 km from the source (in Ukraine, Spitsbergen, Poland, Kamchatka, and other areas). According to the results of these studies, the experimental estimates of the influence of the ionosphere and of the displacement currents on the propagation of ELF–ULF waves in the upper half-space at the different azimuths generation of the primary field are obtained. electromagnetism (dpeaa)DE-He213 deep sounding (dpeaa)DE-He213 controlled sources (dpeaa)DE-He213 extremely low frequency band (ELF) (dpeaa)DE-He213 ultra low frequency band (ULF) (dpeaa)DE-He213 industrial power lines (dpeaa)DE-He213 resistivity (dpeaa)DE-He213 normal resistivity section (dpeaa)DE-He213 numerical modeling (dpeaa)DE-He213 inverse problem (dpeaa)DE-He213 interpretation (dpeaa)DE-He213 Moho boundary (dpeaa)DE-He213 geothermal section (dpeaa)DE-He213 rheology (dpeaa)DE-He213 Shevtsov, A. N. aut Velikhov, E. P. aut Skorokhodov, A. A. aut Kolesnikov, V. E. aut Korotkova, T. G. aut Ryazantsev, P. A. aut Efimov, B. V. aut Kolobov, V. V. aut Barannik, M. B. aut Prokopchuk, P. I. aut Selivanov, V. N. aut Kopytenko, Yu. A. aut Kopytenko, E. A. aut Ismagilov, V. S. aut Petrishchev, M. S. aut Sergushin, P. A. aut Tereshchenko, P. E. aut Samsonov, B. V. aut Birulya, M. A. aut Smirnov, M. Yu. aut Korja, T. aut Yampolski, Yu. M. aut Koloskov, A. V. aut Baru, N. A. aut Poljakov, S. V. aut Shchennikov, A. V. aut Druzhin, G. I. aut Jozwiak, W. aut Reda, J. aut Shchors, Yu. G. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 51(2015), 8 vom: Dez., Seite 826-857 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:51 year:2015 number:8 month:12 pages:826-857 https://dx.doi.org/10.1134/S0001433815080083 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 51 2015 8 12 826-857 |
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Izvestiya |
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Zhamaletdinov, A. A. @@aut@@ Shevtsov, A. N. @@aut@@ Velikhov, E. P. @@aut@@ Skorokhodov, A. A. @@aut@@ Kolesnikov, V. E. @@aut@@ Korotkova, T. G. @@aut@@ Ryazantsev, P. A. @@aut@@ Efimov, B. V. @@aut@@ Kolobov, V. V. @@aut@@ Barannik, M. B. @@aut@@ Prokopchuk, P. I. @@aut@@ Selivanov, V. N. @@aut@@ Kopytenko, Yu. A. @@aut@@ Kopytenko, E. A. @@aut@@ Ismagilov, V. S. @@aut@@ Petrishchev, M. S. @@aut@@ Sergushin, P. A. @@aut@@ Tereshchenko, P. E. @@aut@@ Samsonov, B. V. @@aut@@ Birulya, M. A. @@aut@@ Smirnov, M. Yu. @@aut@@ Korja, T. @@aut@@ Yampolski, Yu. M. @@aut@@ Koloskov, A. V. @@aut@@ Baru, N. A. @@aut@@ Poljakov, S. V. @@aut@@ Shchennikov, A. V. @@aut@@ Druzhin, G. I. @@aut@@ Jozwiak, W. @@aut@@ Reda, J. @@aut@@ Shchors, Yu. G. @@aut@@ |
| publishDateDaySort_date |
2015-12-01T00:00:00Z |
| hierarchy_top_id |
34232098X |
| id |
SPR020054238 |
| language_de |
englisch |
| fullrecord |
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A.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment)</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Pleiades Publishing, Ltd. 2015</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract This article is devoted to describing the theory, technique, and first experimental results of a control source electromagnetic (CSEM) study of the Earth’s crust and ionosphere with the use of two mutually orthogonal industrial transmission lines 109 and 120 km in length in the frame of FENICS (Fennoscandian Electrical Conductivity from Natural and Induction Control Source Soundings) experiment. The main part of the measurements is executed on the territory of the Fennoscandian shield at distances from the first hundreds kilometers up to 856 km from the source with the purpose of the deep electromagnetic sounding of the Earth’s crust and upper mantle. According to the results of these studies clarifying the parameters of “normal” (standard) geoelectric section of the lithosphere to a depth of 60–70 km, the anisotropy parameters are evaluated and a geothermal and rheological interpretation in conjunction with the analysis of the seismic data is executed. Furthermore, to study the propagation of ELF–LLF waves (0.1–200 Hz) in an “Earth–Ionosphere” waveguide, the measurements are carried out apart from Fennoscandian shield at distances up to 5600 km from the source (in Ukraine, Spitsbergen, Poland, Kamchatka, and other areas). 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Zhamaletdinov, A. A. misc electromagnetism misc deep sounding misc controlled sources misc extremely low frequency band (ELF) misc ultra low frequency band (ULF) misc industrial power lines misc resistivity misc normal resistivity section misc numerical modeling misc inverse problem misc interpretation misc Moho boundary misc geothermal section misc rheology Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment) |
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Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment) electromagnetism (dpeaa)DE-He213 deep sounding (dpeaa)DE-He213 controlled sources (dpeaa)DE-He213 extremely low frequency band (ELF) (dpeaa)DE-He213 ultra low frequency band (ULF) (dpeaa)DE-He213 industrial power lines (dpeaa)DE-He213 resistivity (dpeaa)DE-He213 normal resistivity section (dpeaa)DE-He213 numerical modeling (dpeaa)DE-He213 inverse problem (dpeaa)DE-He213 interpretation (dpeaa)DE-He213 Moho boundary (dpeaa)DE-He213 geothermal section (dpeaa)DE-He213 rheology (dpeaa)DE-He213 |
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Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment) |
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Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment) |
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Zhamaletdinov, A. A. Shevtsov, A. N. Velikhov, E. P. Skorokhodov, A. A. Kolesnikov, V. E. Korotkova, T. G. Ryazantsev, P. A. Efimov, B. V. Kolobov, V. V. Barannik, M. B. Prokopchuk, P. I. Selivanov, V. N. Kopytenko, Yu. A. Kopytenko, E. A. Ismagilov, V. S. Petrishchev, M. S. Sergushin, P. A. Tereshchenko, P. E. Samsonov, B. V. Birulya, M. A. Smirnov, M. Yu. Korja, T. Yampolski, Yu. M. Koloskov, A. V. Baru, N. A. Poljakov, S. V. Shchennikov, A. V. Druzhin, G. I. Jozwiak, W. Reda, J. Shchors, Yu. G. |
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study of interaction of elf–ulf range (0.1–200 hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (fenics experiment) |
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Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment) |
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Abstract This article is devoted to describing the theory, technique, and first experimental results of a control source electromagnetic (CSEM) study of the Earth’s crust and ionosphere with the use of two mutually orthogonal industrial transmission lines 109 and 120 km in length in the frame of FENICS (Fennoscandian Electrical Conductivity from Natural and Induction Control Source Soundings) experiment. The main part of the measurements is executed on the territory of the Fennoscandian shield at distances from the first hundreds kilometers up to 856 km from the source with the purpose of the deep electromagnetic sounding of the Earth’s crust and upper mantle. According to the results of these studies clarifying the parameters of “normal” (standard) geoelectric section of the lithosphere to a depth of 60–70 km, the anisotropy parameters are evaluated and a geothermal and rheological interpretation in conjunction with the analysis of the seismic data is executed. Furthermore, to study the propagation of ELF–LLF waves (0.1–200 Hz) in an “Earth–Ionosphere” waveguide, the measurements are carried out apart from Fennoscandian shield at distances up to 5600 km from the source (in Ukraine, Spitsbergen, Poland, Kamchatka, and other areas). According to the results of these studies, the experimental estimates of the influence of the ionosphere and of the displacement currents on the propagation of ELF–ULF waves in the upper half-space at the different azimuths generation of the primary field are obtained. © Pleiades Publishing, Ltd. 2015 |
| abstractGer |
Abstract This article is devoted to describing the theory, technique, and first experimental results of a control source electromagnetic (CSEM) study of the Earth’s crust and ionosphere with the use of two mutually orthogonal industrial transmission lines 109 and 120 km in length in the frame of FENICS (Fennoscandian Electrical Conductivity from Natural and Induction Control Source Soundings) experiment. The main part of the measurements is executed on the territory of the Fennoscandian shield at distances from the first hundreds kilometers up to 856 km from the source with the purpose of the deep electromagnetic sounding of the Earth’s crust and upper mantle. According to the results of these studies clarifying the parameters of “normal” (standard) geoelectric section of the lithosphere to a depth of 60–70 km, the anisotropy parameters are evaluated and a geothermal and rheological interpretation in conjunction with the analysis of the seismic data is executed. Furthermore, to study the propagation of ELF–LLF waves (0.1–200 Hz) in an “Earth–Ionosphere” waveguide, the measurements are carried out apart from Fennoscandian shield at distances up to 5600 km from the source (in Ukraine, Spitsbergen, Poland, Kamchatka, and other areas). According to the results of these studies, the experimental estimates of the influence of the ionosphere and of the displacement currents on the propagation of ELF–ULF waves in the upper half-space at the different azimuths generation of the primary field are obtained. © Pleiades Publishing, Ltd. 2015 |
| abstract_unstemmed |
Abstract This article is devoted to describing the theory, technique, and first experimental results of a control source electromagnetic (CSEM) study of the Earth’s crust and ionosphere with the use of two mutually orthogonal industrial transmission lines 109 and 120 km in length in the frame of FENICS (Fennoscandian Electrical Conductivity from Natural and Induction Control Source Soundings) experiment. The main part of the measurements is executed on the territory of the Fennoscandian shield at distances from the first hundreds kilometers up to 856 km from the source with the purpose of the deep electromagnetic sounding of the Earth’s crust and upper mantle. According to the results of these studies clarifying the parameters of “normal” (standard) geoelectric section of the lithosphere to a depth of 60–70 km, the anisotropy parameters are evaluated and a geothermal and rheological interpretation in conjunction with the analysis of the seismic data is executed. Furthermore, to study the propagation of ELF–LLF waves (0.1–200 Hz) in an “Earth–Ionosphere” waveguide, the measurements are carried out apart from Fennoscandian shield at distances up to 5600 km from the source (in Ukraine, Spitsbergen, Poland, Kamchatka, and other areas). According to the results of these studies, the experimental estimates of the influence of the ionosphere and of the displacement currents on the propagation of ELF–ULF waves in the upper half-space at the different azimuths generation of the primary field are obtained. © Pleiades Publishing, Ltd. 2015 |
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Study of interaction of ELF–ULF range (0.1–200 Hz) electromagnetic waves with the earth’s crust and the ionosphere in the field of industrial power transmission lines (FENICS experiment) |
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