Main Sections of the Earth Crust and Upper Mantle of the Greater Caucasus by New Technologies. 2. Deep Seismic Sounding, Micro Seismic Sounding
The work reviews the possibility of application of the seismic tomography method for processing the materials of deep seismic sounding (DSS). It presents comparative results by various softwares as GeoGiga Seismic PRO 7.0 (Canada), XTomo-LM (St. Petersburg). The work shows the possibility of using t...
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| Дата: | 2016 |
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| Автори: | , , , , , |
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S. Subbotin Institute of Geophysics of the NAS of Ukraine
2016
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| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/107805 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| _version_ | 1856543108753260544 |
|---|---|
| author | Ghonghadze, S. A. Chelidze, T. L. Mindeli, P. Sh. Ghlonti, N. I. Kiria, J. K. Yavolovskaya, O.V. |
| author_facet | Ghonghadze, S. A. Chelidze, T. L. Mindeli, P. Sh. Ghlonti, N. I. Kiria, J. K. Yavolovskaya, O.V. |
| author_sort | Ghonghadze, S. A. |
| baseUrl_str | |
| collection | OJS |
| datestamp_date | 2020-10-07T11:20:03Z |
| description | The work reviews the possibility of application of the seismic tomography method for processing the materials of deep seismic sounding (DSS). It presents comparative results by various softwares as GeoGiga Seismic PRO 7.0 (Canada), XTomo-LM (St. Petersburg). The work shows the possibility of using tomography together with the data of the micro seismic sounding (MSS) method. The basic section of the Earth's crust and upper mantle by tomographic sections. It is determined that the cover of the foundation is strongly indented, i.e., all the foundation is fragmented into blocks, which are enclosed by the net of faults formed according to the gradient zones of speeds and fragmentation of speed inhomogeneity in the tomography section. The thickness of the earth crust under the Greater Caucasus increases to 60—70 km. It reveals the speed image obtained as a result of seismic tomography, earlier constructed speed models of the DSS profiles of Bakuriani—Stepnoye and Nakhchivan—Volgograd reinterpreted by Pavlenkova G. A, also correlative analysis of the method of deep seismic sounding (DSS) and the method of micro seismic sounding (MSS) of the profile of Tskhinval—Ardon. |
| first_indexed | 2025-07-17T11:04:33Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-107805 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:04:33Z |
| publishDate | 2016 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-1078052020-10-07T11:20:03Z Main Sections of the Earth Crust and Upper Mantle of the Greater Caucasus by New Technologies. 2. Deep Seismic Sounding, Micro Seismic Sounding Ghonghadze, S. A. Chelidze, T. L. Mindeli, P. Sh. Ghlonti, N. I. Kiria, J. K. Yavolovskaya, O.V. the Greater Caucasus Earth's crust deep seismic sounding seismic tomography micro seismic sounding The work reviews the possibility of application of the seismic tomography method for processing the materials of deep seismic sounding (DSS). It presents comparative results by various softwares as GeoGiga Seismic PRO 7.0 (Canada), XTomo-LM (St. Petersburg). The work shows the possibility of using tomography together with the data of the micro seismic sounding (MSS) method. The basic section of the Earth's crust and upper mantle by tomographic sections. It is determined that the cover of the foundation is strongly indented, i.e., all the foundation is fragmented into blocks, which are enclosed by the net of faults formed according to the gradient zones of speeds and fragmentation of speed inhomogeneity in the tomography section. The thickness of the earth crust under the Greater Caucasus increases to 60—70 km. It reveals the speed image obtained as a result of seismic tomography, earlier constructed speed models of the DSS profiles of Bakuriani—Stepnoye and Nakhchivan—Volgograd reinterpreted by Pavlenkova G. A, also correlative analysis of the method of deep seismic sounding (DSS) and the method of micro seismic sounding (MSS) of the profile of Tskhinval—Ardon. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2016-07-15 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/107805 10.24028/gzh.0203-3100.v38i4.2016.107805 Geofizicheskiy Zhurnal; Vol. 38 No. 4 (2016); 100-112 Геофизический журнал; Том 38 № 4 (2016); 100-112 Геофізичний журнал; Том 38 № 4 (2016); 100-112 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/107805/102877 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | the Greater Caucasus Earth's crust deep seismic sounding seismic tomography micro seismic sounding Ghonghadze, S. A. Chelidze, T. L. Mindeli, P. Sh. Ghlonti, N. I. Kiria, J. K. Yavolovskaya, O.V. Main Sections of the Earth Crust and Upper Mantle of the Greater Caucasus by New Technologies. 2. Deep Seismic Sounding, Micro Seismic Sounding |
| title | Main Sections of the Earth Crust and Upper Mantle of the Greater Caucasus by New Technologies. 2. Deep Seismic Sounding, Micro Seismic Sounding |
| title_full | Main Sections of the Earth Crust and Upper Mantle of the Greater Caucasus by New Technologies. 2. Deep Seismic Sounding, Micro Seismic Sounding |
| title_fullStr | Main Sections of the Earth Crust and Upper Mantle of the Greater Caucasus by New Technologies. 2. Deep Seismic Sounding, Micro Seismic Sounding |
| title_full_unstemmed | Main Sections of the Earth Crust and Upper Mantle of the Greater Caucasus by New Technologies. 2. Deep Seismic Sounding, Micro Seismic Sounding |
| title_short | Main Sections of the Earth Crust and Upper Mantle of the Greater Caucasus by New Technologies. 2. Deep Seismic Sounding, Micro Seismic Sounding |
| title_sort | main sections of the earth crust and upper mantle of the greater caucasus by new technologies. 2. deep seismic sounding, micro seismic sounding |
| topic | the Greater Caucasus Earth's crust deep seismic sounding seismic tomography micro seismic sounding |
| topic_facet | the Greater Caucasus Earth's crust deep seismic sounding seismic tomography micro seismic sounding |
| url | https://journals.uran.ua/geofizicheskiy/article/view/107805 |
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