The Murman-2018 Experiment on Remote Sensing in Order to Study the “Impenetrability” Boundary at the Transition between Brittle and Plastic States of the Crystalline Earth’s Crust
Abstract This paper describes the Murman-2018 experiment on remote electromagnetic sounding in combination with frequency and audio magnetotelluric soundings. The experimental results made it possible to quantify for the first time in the scientific literature the position of the boundary of a sharp...
Ausführliche Beschreibung
Autor*in: |
Zhamaletdinov, A. A. [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2019 |
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Anmerkung: |
© Pleiades Publishing, Ltd. 2019 |
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Übergeordnetes Werk: |
Enthalten in: Doklady earth sciences - Pleiades Publishing, 1998, 486(2019), 1 vom: Mai, Seite 575-579 |
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Übergeordnetes Werk: |
volume:486 ; year:2019 ; number:1 ; month:05 ; pages:575-579 |
Links: |
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DOI / URN: |
10.1134/S1028334X19050301 |
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Katalog-ID: |
OLC2040801669 |
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700 | 1 | |a Kolesnikov, V. E. |4 aut | |
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10.1134/S1028334X19050301 doi (DE-627)OLC2040801669 (DE-He213)S1028334X19050301-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 Murman-2018 Experiment on Remote Sensing in Order to Study the “Impenetrability” Boundary at the Transition between Brittle and Plastic States of the Crystalline Earth’s Crust 2019 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2019 Abstract This paper describes the Murman-2018 experiment on remote electromagnetic sounding in combination with frequency and audio magnetotelluric soundings. The experimental results made it possible to quantify for the first time in the scientific literature the position of the boundary of a sharp increase in rock resistivity at a depth of 10–15 km. The nature of the established boundary (the “impenetrability” boundary for direct current) is related to the transition of rock properties in the Earth’s crust from the fragile state in the upper crust to a plastic state at a depth of 10–15 km or more. Velikhov, E. P. aut Shevtsov, A. N. aut Skorokhodov, A. A. aut Kolobov, V. V. aut Ivonin, V. V. aut Kolesnikov, V. E. aut Enthalten in Doklady earth sciences Pleiades Publishing, 1998 486(2019), 1 vom: Mai, Seite 575-579 (DE-627)242069096 (DE-600)1422550-5 (DE-576)079718450 1028-334X nnns volume:486 year:2019 number:1 month:05 pages:575-579 https://doi.org/10.1134/S1028334X19050301 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 486 2019 1 05 575-579 |
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10.1134/S1028334X19050301 doi (DE-627)OLC2040801669 (DE-He213)S1028334X19050301-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 Murman-2018 Experiment on Remote Sensing in Order to Study the “Impenetrability” Boundary at the Transition between Brittle and Plastic States of the Crystalline Earth’s Crust 2019 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2019 Abstract This paper describes the Murman-2018 experiment on remote electromagnetic sounding in combination with frequency and audio magnetotelluric soundings. The experimental results made it possible to quantify for the first time in the scientific literature the position of the boundary of a sharp increase in rock resistivity at a depth of 10–15 km. The nature of the established boundary (the “impenetrability” boundary for direct current) is related to the transition of rock properties in the Earth’s crust from the fragile state in the upper crust to a plastic state at a depth of 10–15 km or more. Velikhov, E. P. aut Shevtsov, A. N. aut Skorokhodov, A. A. aut Kolobov, V. V. aut Ivonin, V. V. aut Kolesnikov, V. E. aut Enthalten in Doklady earth sciences Pleiades Publishing, 1998 486(2019), 1 vom: Mai, Seite 575-579 (DE-627)242069096 (DE-600)1422550-5 (DE-576)079718450 1028-334X nnns volume:486 year:2019 number:1 month:05 pages:575-579 https://doi.org/10.1134/S1028334X19050301 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 486 2019 1 05 575-579 |
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10.1134/S1028334X19050301 doi (DE-627)OLC2040801669 (DE-He213)S1028334X19050301-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 Murman-2018 Experiment on Remote Sensing in Order to Study the “Impenetrability” Boundary at the Transition between Brittle and Plastic States of the Crystalline Earth’s Crust 2019 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2019 Abstract This paper describes the Murman-2018 experiment on remote electromagnetic sounding in combination with frequency and audio magnetotelluric soundings. The experimental results made it possible to quantify for the first time in the scientific literature the position of the boundary of a sharp increase in rock resistivity at a depth of 10–15 km. The nature of the established boundary (the “impenetrability” boundary for direct current) is related to the transition of rock properties in the Earth’s crust from the fragile state in the upper crust to a plastic state at a depth of 10–15 km or more. Velikhov, E. P. aut Shevtsov, A. N. aut Skorokhodov, A. A. aut Kolobov, V. V. aut Ivonin, V. V. aut Kolesnikov, V. E. aut Enthalten in Doklady earth sciences Pleiades Publishing, 1998 486(2019), 1 vom: Mai, Seite 575-579 (DE-627)242069096 (DE-600)1422550-5 (DE-576)079718450 1028-334X nnns volume:486 year:2019 number:1 month:05 pages:575-579 https://doi.org/10.1134/S1028334X19050301 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 486 2019 1 05 575-579 |
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the murman-2018 experiment on remote sensing in order to study the “impenetrability” boundary at the transition between brittle and plastic states of the crystalline earth’s crust |
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The Murman-2018 Experiment on Remote Sensing in Order to Study the “Impenetrability” Boundary at the Transition between Brittle and Plastic States of the Crystalline Earth’s Crust |
abstract |
Abstract This paper describes the Murman-2018 experiment on remote electromagnetic sounding in combination with frequency and audio magnetotelluric soundings. The experimental results made it possible to quantify for the first time in the scientific literature the position of the boundary of a sharp increase in rock resistivity at a depth of 10–15 km. The nature of the established boundary (the “impenetrability” boundary for direct current) is related to the transition of rock properties in the Earth’s crust from the fragile state in the upper crust to a plastic state at a depth of 10–15 km or more. © Pleiades Publishing, Ltd. 2019 |
abstractGer |
Abstract This paper describes the Murman-2018 experiment on remote electromagnetic sounding in combination with frequency and audio magnetotelluric soundings. The experimental results made it possible to quantify for the first time in the scientific literature the position of the boundary of a sharp increase in rock resistivity at a depth of 10–15 km. The nature of the established boundary (the “impenetrability” boundary for direct current) is related to the transition of rock properties in the Earth’s crust from the fragile state in the upper crust to a plastic state at a depth of 10–15 km or more. © Pleiades Publishing, Ltd. 2019 |
abstract_unstemmed |
Abstract This paper describes the Murman-2018 experiment on remote electromagnetic sounding in combination with frequency and audio magnetotelluric soundings. The experimental results made it possible to quantify for the first time in the scientific literature the position of the boundary of a sharp increase in rock resistivity at a depth of 10–15 km. The nature of the established boundary (the “impenetrability” boundary for direct current) is related to the transition of rock properties in the Earth’s crust from the fragile state in the upper crust to a plastic state at a depth of 10–15 km or more. © Pleiades Publishing, Ltd. 2019 |
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container_issue |
1 |
title_short |
The Murman-2018 Experiment on Remote Sensing in Order to Study the “Impenetrability” Boundary at the Transition between Brittle and Plastic States of the Crystalline Earth’s Crust |
url |
https://doi.org/10.1134/S1028334X19050301 |
remote_bool |
false |
author2 |
Velikhov, E. P. Shevtsov, A. N. Skorokhodov, A. A. Kolobov, V. V. Ivonin, V. V. Kolesnikov, V. E. |
author2Str |
Velikhov, E. P. Shevtsov, A. N. Skorokhodov, A. A. Kolobov, V. V. Ivonin, V. V. Kolesnikov, V. E. |
ppnlink |
242069096 |
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hochschulschrift_bool |
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doi_str |
10.1134/S1028334X19050301 |
up_date |
2024-07-04T03:09:42.889Z |
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1803616342931144704 |
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