Zones Localization of Hazardous Geological Processes Habit of the Coastal Cliff According to 3D Seismotomography Sounding Data
The article presents a methodology for conducting 3D seismic tomography of rock massifs. This technique has been developed for the identification and localisation of zones of development of dangerous geological processes formed within the rock massif of a coastal cliff. An example of the application...
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| Format: | Article |
| Language: | English |
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Russian Academy of Sciences, The Geophysical Center
2025-02-01
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| Series: | Russian Journal of Earth Sciences |
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| Online Access: | http://doi.org/10.2205/2025es000993 |
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| author | Glazunov Vladimir Vasil'evich Efimova Natal’ia Zelikman Danil Bukatov Andrei |
| author_facet | Glazunov Vladimir Vasil'evich Efimova Natal’ia Zelikman Danil Bukatov Andrei |
| author_sort | Glazunov Vladimir Vasil'evich |
| collection | DOAJ |
| description | The article presents a methodology for conducting 3D seismic tomography of rock massifs. This technique has been developed for the identification and localisation of zones of development of dangerous geological processes formed within the rock massif of a coastal cliff. An example of the application of the technique is provided by the results of seismic tomography, which were used to study the state of a coastal cliff in Crimea that is subject to abrasion. The seismic tomographic inversion process has been utilised to generate maps depicting the distribution of 𝑃 and 𝑆 velocity values of seismic waves within the rock massif at varying depths. Furthermore, the dynamic moduli of elasticity, which are indicative of the physical and mechanical properties of the rocks constituting the cliff, have been calculated. The maps that have been generated by the seismic tomographic inversion process reflect the spatial distribution of these parameters, and the maps also localise the zones that have been weakened, presumably as a consequence of the formation and development of negative geological processes that are dangerous for the cliff's stability. |
| format | Article |
| id | doaj-art-b76b376fb0b74f5bbdb481c97de0098e |
| institution | DOAJ |
| issn | 1681-1208 |
| language | English |
| publishDate | 2025-02-01 |
| publisher | Russian Academy of Sciences, The Geophysical Center |
| record_format | Article |
| series | Russian Journal of Earth Sciences |
| spelling | doaj-art-b76b376fb0b74f5bbdb481c97de0098e2025-08-20T02:39:48ZengRussian Academy of Sciences, The Geophysical CenterRussian Journal of Earth Sciences1681-12082025-02-0125111210.2205/2025es000993Zones Localization of Hazardous Geological Processes Habit of the Coastal Cliff According to 3D Seismotomography Sounding DataGlazunov Vladimir Vasil'evich0https://orcid.org/0000-0001-5816-0507Efimova Natal’ia1Zelikman Danil2https://orcid.org/0009-0003-0044-2298Bukatov Andrei3Empress Catherine II Saint Petersburg Mining UniversityA.P. Karpinsky Russian Geological Research InstituteEmpress Catherine II Saint Petersburg Mining UniversityGosudarstvennyy istoriko-arheologicheskiy muzey-zapovednik «Hersones Tavricheskiy»The article presents a methodology for conducting 3D seismic tomography of rock massifs. This technique has been developed for the identification and localisation of zones of development of dangerous geological processes formed within the rock massif of a coastal cliff. An example of the application of the technique is provided by the results of seismic tomography, which were used to study the state of a coastal cliff in Crimea that is subject to abrasion. The seismic tomographic inversion process has been utilised to generate maps depicting the distribution of 𝑃 and 𝑆 velocity values of seismic waves within the rock massif at varying depths. Furthermore, the dynamic moduli of elasticity, which are indicative of the physical and mechanical properties of the rocks constituting the cliff, have been calculated. The maps that have been generated by the seismic tomographic inversion process reflect the spatial distribution of these parameters, and the maps also localise the zones that have been weakened, presumably as a consequence of the formation and development of negative geological processes that are dangerous for the cliff's stability.http://doi.org/10.2205/2025es000993Seismic tomography seismic sounding 3D inverse modeling stress-strain properties competence cliff Crimea coast landslide tension joint |
| spellingShingle | Glazunov Vladimir Vasil'evich Efimova Natal’ia Zelikman Danil Bukatov Andrei Zones Localization of Hazardous Geological Processes Habit of the Coastal Cliff According to 3D Seismotomography Sounding Data Russian Journal of Earth Sciences Seismic tomography seismic sounding 3D inverse modeling stress-strain properties competence cliff Crimea coast landslide tension joint |
| title | Zones Localization of Hazardous Geological Processes Habit of the Coastal Cliff According to 3D Seismotomography Sounding Data |
| title_full | Zones Localization of Hazardous Geological Processes Habit of the Coastal Cliff According to 3D Seismotomography Sounding Data |
| title_fullStr | Zones Localization of Hazardous Geological Processes Habit of the Coastal Cliff According to 3D Seismotomography Sounding Data |
| title_full_unstemmed | Zones Localization of Hazardous Geological Processes Habit of the Coastal Cliff According to 3D Seismotomography Sounding Data |
| title_short | Zones Localization of Hazardous Geological Processes Habit of the Coastal Cliff According to 3D Seismotomography Sounding Data |
| title_sort | zones localization of hazardous geological processes habit of the coastal cliff according to 3d seismotomography sounding data |
| topic | Seismic tomography seismic sounding 3D inverse modeling stress-strain properties competence cliff Crimea coast landslide tension joint |
| url | http://doi.org/10.2205/2025es000993 |
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