The Kovdor-2015 experiment: study of the parameters of a conductive layer of dilatancy–diffusion nature (DD Layer) in the Archaean crystalline basement of the Baltic Shield
Abstract This paper addresses the Kovdor-2015 Experiment involving frequency electromagnetic soundings of the Archaean basement of the Earth’s crust in the southwestern part of the Kola Peninsula. Eleven soundings were carried out using two transmitting arrangements, 85 km apart. Each arrangement co...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhamaletdinov, A. A. [verfasserIn] |
|---|
| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2017 |
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| Übergeordnetes Werk: |
Enthalten in: Doklady earth sciences - Pleiades Publishing, 1998, 474(2017), 2 vom: Juni, Seite 641-645 |
|---|---|
| Übergeordnetes Werk: |
volume:474 ; year:2017 ; number:2 ; month:06 ; pages:641-645 |
| Links: |
|---|
| DOI / URN: |
10.1134/S1028334X17060095 |
|---|
| Katalog-ID: |
OLC2040795278 |
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| 245 | 1 | 0 | |a The Kovdor-2015 experiment: study of the parameters of a conductive layer of dilatancy–diffusion nature (DD Layer) in the Archaean crystalline basement of the Baltic Shield |
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| 520 | |a Abstract This paper addresses the Kovdor-2015 Experiment involving frequency electromagnetic soundings of the Archaean basement of the Earth’s crust in the southwestern part of the Kola Peninsula. Eleven soundings were carried out using two transmitting arrangements, 85 km apart. Each arrangement consisted of two mutually orthogonal grounded electric dipoles of 1.5 km long. The distances between the source and the receiver were 25 and 50 km. Interpretation of the results took into account the influence of displacement currents and static distortions. It is found that there is an intermediate conductive layer of the dilatancy–diffusion nature (DD layer) with a longitudinal conductivity of about one siemens at depths ranging from 1.5–2 to 5–7 km. The results are interpreted in the terms of geodynamics. | ||
| 700 | 1 | |a Velikhov, E. P. |4 aut | |
| 700 | 1 | |a Shevtsov, A. N. |4 aut | |
| 700 | 1 | |a Kolobov, V. V. |4 aut | |
| 700 | 1 | |a Kolesnikov, V. E. |4 aut | |
| 700 | 1 | |a Skorokhodov, A. A. |4 aut | |
| 700 | 1 | |a Korotkova, T. G. |4 aut | |
| 700 | 1 | |a Ivonin, V. V. |4 aut | |
| 700 | 1 | |a Ryazantsev, P. A. |4 aut | |
| 700 | 1 | |a Birulya, M. A. |4 aut | |
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10.1134/S1028334X17060095 doi (DE-627)OLC2040795278 (DE-He213)S1028334X17060095-p DE-627 ger DE-627 rakwb eng 550 000 VZ 38.00$jGeowissenschaften: Allgemeines bkl 38.55$jRegionale Geologie bkl Zhamaletdinov, A. A. verfasserin aut The Kovdor-2015 experiment: study of the parameters of a conductive layer of dilatancy–diffusion nature (DD Layer) in the Archaean crystalline basement of the Baltic Shield 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract This paper addresses the Kovdor-2015 Experiment involving frequency electromagnetic soundings of the Archaean basement of the Earth’s crust in the southwestern part of the Kola Peninsula. Eleven soundings were carried out using two transmitting arrangements, 85 km apart. Each arrangement consisted of two mutually orthogonal grounded electric dipoles of 1.5 km long. The distances between the source and the receiver were 25 and 50 km. Interpretation of the results took into account the influence of displacement currents and static distortions. It is found that there is an intermediate conductive layer of the dilatancy–diffusion nature (DD layer) with a longitudinal conductivity of about one siemens at depths ranging from 1.5–2 to 5–7 km. The results are interpreted in the terms of geodynamics. Velikhov, E. P. aut Shevtsov, A. N. aut Kolobov, V. V. aut Kolesnikov, V. E. aut Skorokhodov, A. A. aut Korotkova, T. G. aut Ivonin, V. V. aut Ryazantsev, P. A. aut Birulya, M. A. aut Enthalten in Doklady earth sciences Pleiades Publishing, 1998 474(2017), 2 vom: Juni, Seite 641-645 (DE-627)242069096 (DE-600)1422550-5 (DE-576)079718450 1028-334X nnns volume:474 year:2017 number:2 month:06 pages:641-645 https://doi.org/10.1134/S1028334X17060095 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO 38.00$jGeowissenschaften: Allgemeines VZ 106408305 (DE-625)106408305 38.55$jRegionale Geologie VZ 106407260 (DE-625)106407260 AR 474 2017 2 06 641-645 |
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10.1134/S1028334X17060095 doi (DE-627)OLC2040795278 (DE-He213)S1028334X17060095-p DE-627 ger DE-627 rakwb eng 550 000 VZ 38.00$jGeowissenschaften: Allgemeines bkl 38.55$jRegionale Geologie bkl Zhamaletdinov, A. A. verfasserin aut The Kovdor-2015 experiment: study of the parameters of a conductive layer of dilatancy–diffusion nature (DD Layer) in the Archaean crystalline basement of the Baltic Shield 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract This paper addresses the Kovdor-2015 Experiment involving frequency electromagnetic soundings of the Archaean basement of the Earth’s crust in the southwestern part of the Kola Peninsula. Eleven soundings were carried out using two transmitting arrangements, 85 km apart. Each arrangement consisted of two mutually orthogonal grounded electric dipoles of 1.5 km long. The distances between the source and the receiver were 25 and 50 km. Interpretation of the results took into account the influence of displacement currents and static distortions. It is found that there is an intermediate conductive layer of the dilatancy–diffusion nature (DD layer) with a longitudinal conductivity of about one siemens at depths ranging from 1.5–2 to 5–7 km. The results are interpreted in the terms of geodynamics. Velikhov, E. P. aut Shevtsov, A. N. aut Kolobov, V. V. aut Kolesnikov, V. E. aut Skorokhodov, A. A. aut Korotkova, T. G. aut Ivonin, V. V. aut Ryazantsev, P. A. aut Birulya, M. A. aut Enthalten in Doklady earth sciences Pleiades Publishing, 1998 474(2017), 2 vom: Juni, Seite 641-645 (DE-627)242069096 (DE-600)1422550-5 (DE-576)079718450 1028-334X nnns volume:474 year:2017 number:2 month:06 pages:641-645 https://doi.org/10.1134/S1028334X17060095 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO 38.00$jGeowissenschaften: Allgemeines VZ 106408305 (DE-625)106408305 38.55$jRegionale Geologie VZ 106407260 (DE-625)106407260 AR 474 2017 2 06 641-645 |
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10.1134/S1028334X17060095 doi (DE-627)OLC2040795278 (DE-He213)S1028334X17060095-p DE-627 ger DE-627 rakwb eng 550 000 VZ 38.00$jGeowissenschaften: Allgemeines bkl 38.55$jRegionale Geologie bkl Zhamaletdinov, A. A. verfasserin aut The Kovdor-2015 experiment: study of the parameters of a conductive layer of dilatancy–diffusion nature (DD Layer) in the Archaean crystalline basement of the Baltic Shield 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract This paper addresses the Kovdor-2015 Experiment involving frequency electromagnetic soundings of the Archaean basement of the Earth’s crust in the southwestern part of the Kola Peninsula. Eleven soundings were carried out using two transmitting arrangements, 85 km apart. Each arrangement consisted of two mutually orthogonal grounded electric dipoles of 1.5 km long. The distances between the source and the receiver were 25 and 50 km. Interpretation of the results took into account the influence of displacement currents and static distortions. It is found that there is an intermediate conductive layer of the dilatancy–diffusion nature (DD layer) with a longitudinal conductivity of about one siemens at depths ranging from 1.5–2 to 5–7 km. The results are interpreted in the terms of geodynamics. Velikhov, E. P. aut Shevtsov, A. N. aut Kolobov, V. V. aut Kolesnikov, V. E. aut Skorokhodov, A. A. aut Korotkova, T. G. aut Ivonin, V. V. aut Ryazantsev, P. A. aut Birulya, M. A. aut Enthalten in Doklady earth sciences Pleiades Publishing, 1998 474(2017), 2 vom: Juni, Seite 641-645 (DE-627)242069096 (DE-600)1422550-5 (DE-576)079718450 1028-334X nnns volume:474 year:2017 number:2 month:06 pages:641-645 https://doi.org/10.1134/S1028334X17060095 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO 38.00$jGeowissenschaften: Allgemeines VZ 106408305 (DE-625)106408305 38.55$jRegionale Geologie VZ 106407260 (DE-625)106407260 AR 474 2017 2 06 641-645 |
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The Kovdor-2015 experiment: study of the parameters of a conductive layer of dilatancy–diffusion nature (DD Layer) in the Archaean crystalline basement of the Baltic Shield |
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The Kovdor-2015 experiment: study of the parameters of a conductive layer of dilatancy–diffusion nature (DD Layer) in the Archaean crystalline basement of the Baltic Shield |
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Zhamaletdinov, A. A. |
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Zhamaletdinov, A. A. Velikhov, E. P. Shevtsov, A. N. Kolobov, V. V. Kolesnikov, V. E. Skorokhodov, A. A. Korotkova, T. G. Ivonin, V. V. Ryazantsev, P. A. Birulya, M. A. |
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the kovdor-2015 experiment: study of the parameters of a conductive layer of dilatancy–diffusion nature (dd layer) in the archaean crystalline basement of the baltic shield |
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The Kovdor-2015 experiment: study of the parameters of a conductive layer of dilatancy–diffusion nature (DD Layer) in the Archaean crystalline basement of the Baltic Shield |
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Abstract This paper addresses the Kovdor-2015 Experiment involving frequency electromagnetic soundings of the Archaean basement of the Earth’s crust in the southwestern part of the Kola Peninsula. Eleven soundings were carried out using two transmitting arrangements, 85 km apart. Each arrangement consisted of two mutually orthogonal grounded electric dipoles of 1.5 km long. The distances between the source and the receiver were 25 and 50 km. Interpretation of the results took into account the influence of displacement currents and static distortions. It is found that there is an intermediate conductive layer of the dilatancy–diffusion nature (DD layer) with a longitudinal conductivity of about one siemens at depths ranging from 1.5–2 to 5–7 km. The results are interpreted in the terms of geodynamics. © Pleiades Publishing, Ltd. 2017 |
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Abstract This paper addresses the Kovdor-2015 Experiment involving frequency electromagnetic soundings of the Archaean basement of the Earth’s crust in the southwestern part of the Kola Peninsula. Eleven soundings were carried out using two transmitting arrangements, 85 km apart. Each arrangement consisted of two mutually orthogonal grounded electric dipoles of 1.5 km long. The distances between the source and the receiver were 25 and 50 km. Interpretation of the results took into account the influence of displacement currents and static distortions. It is found that there is an intermediate conductive layer of the dilatancy–diffusion nature (DD layer) with a longitudinal conductivity of about one siemens at depths ranging from 1.5–2 to 5–7 km. The results are interpreted in the terms of geodynamics. © Pleiades Publishing, Ltd. 2017 |
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Abstract This paper addresses the Kovdor-2015 Experiment involving frequency electromagnetic soundings of the Archaean basement of the Earth’s crust in the southwestern part of the Kola Peninsula. Eleven soundings were carried out using two transmitting arrangements, 85 km apart. Each arrangement consisted of two mutually orthogonal grounded electric dipoles of 1.5 km long. The distances between the source and the receiver were 25 and 50 km. Interpretation of the results took into account the influence of displacement currents and static distortions. It is found that there is an intermediate conductive layer of the dilatancy–diffusion nature (DD layer) with a longitudinal conductivity of about one siemens at depths ranging from 1.5–2 to 5–7 km. The results are interpreted in the terms of geodynamics. © Pleiades Publishing, Ltd. 2017 |
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The Kovdor-2015 experiment: study of the parameters of a conductive layer of dilatancy–diffusion nature (DD Layer) in the Archaean crystalline basement of the Baltic Shield |
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Velikhov, E. P. Shevtsov, A. N. Kolobov, V. V. Kolesnikov, V. E. Skorokhodov, A. A. Korotkova, T. G. Ivonin, V. V. Ryazantsev, P. A. Birulya, M. A. |
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Velikhov, E. P. Shevtsov, A. N. Kolobov, V. V. Kolesnikov, V. E. Skorokhodov, A. A. Korotkova, T. G. Ivonin, V. V. Ryazantsev, P. A. Birulya, M. A. |
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