Seismicity in the area of the electrical conductivity anomaly in the western part of the Priazovsky megablock
According to the data of magneto-telluric sounding and magneto-variation profiling a structure with high electric conductivity in the earth's crust has been revealed in the eastern part of the USh within the territory of the Priazovian mega-block. Three-dimensional deep model has been plotted c...
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Subbotin Institute of Geophysics of the NAS of Ukraine
2010
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journalsuranua-geofizicheskiy-article-1175762020-10-07T10:57:50Z Seismicity in the area of the electrical conductivity anomaly in the western part of the Priazovsky megablock Burakhovich, T. K. Kulik, S. N. Kushnir, A. N. Zaitsev, G. N. According to the data of magneto-telluric sounding and magneto-variation profiling a structure with high electric conductivity in the earth's crust has been revealed in the eastern part of the USh within the territory of the Priazovian mega-block. Three-dimensional deep model has been plotted comprised by two main elements: subsurface sub-longitudinal system, correlating with Azovo-Pavlograd and West-Priazovian deep faults and isometric anomaly at the depth from 2 to 10km in the South of West-Priazovian block. The Donbas and the Priazovian electro-conducting anomalies are specific by small amount of earthquakes with magnitude less than 4 points. Subbotin Institute of Geophysics of the NAS of Ukraine 2010-02-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/117576 10.24028/gzh.0203-3100.v32i1.2010.117576 Geofizicheskiy Zhurnal; Vol. 32 No. 1 (2010); 144-154 Геофизический журнал; Том 32 № 1 (2010); 144-154 Геофізичний журнал; Том 32 № 1 (2010); 144-154 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/117576/111618 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| institution |
Geofizicheskiy Zhurnal |
| baseUrl_str |
|
| datestamp_date |
2020-10-07T10:57:50Z |
| collection |
OJS |
| language |
rus |
| format |
Article |
| author |
Burakhovich, T. K. Kulik, S. N. Kushnir, A. N. Zaitsev, G. N. |
| spellingShingle |
Burakhovich, T. K. Kulik, S. N. Kushnir, A. N. Zaitsev, G. N. Seismicity in the area of the electrical conductivity anomaly in the western part of the Priazovsky megablock |
| author_facet |
Burakhovich, T. K. Kulik, S. N. Kushnir, A. N. Zaitsev, G. N. |
| author_sort |
Burakhovich, T. K. |
| title |
Seismicity in the area of the electrical conductivity anomaly in the western part of the Priazovsky megablock |
| title_short |
Seismicity in the area of the electrical conductivity anomaly in the western part of the Priazovsky megablock |
| title_full |
Seismicity in the area of the electrical conductivity anomaly in the western part of the Priazovsky megablock |
| title_fullStr |
Seismicity in the area of the electrical conductivity anomaly in the western part of the Priazovsky megablock |
| title_full_unstemmed |
Seismicity in the area of the electrical conductivity anomaly in the western part of the Priazovsky megablock |
| title_sort |
seismicity in the area of the electrical conductivity anomaly in the western part of the priazovsky megablock |
| description |
According to the data of magneto-telluric sounding and magneto-variation profiling a structure with high electric conductivity in the earth's crust has been revealed in the eastern part of the USh within the territory of the Priazovian mega-block. Three-dimensional deep model has been plotted comprised by two main elements: subsurface sub-longitudinal system, correlating with Azovo-Pavlograd and West-Priazovian deep faults and isometric anomaly at the depth from 2 to 10km in the South of West-Priazovian block. The Donbas and the Priazovian electro-conducting anomalies are specific by small amount of earthquakes with magnitude less than 4 points. |
| publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
| publishDate |
2010 |
| url |
https://journals.uran.ua/geofizicheskiy/article/view/117576 |
| work_keys_str_mv |
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| first_indexed |
2025-07-17T11:09:23Z |
| last_indexed |
2025-07-17T11:09:23Z |
| _version_ |
1837892175200780288 |