Structural features of the upper part of the section of the Gorniy Altai Uimon depression according to electrotomography data using 3D software

Determining the structure of intermountain depressions in seismically active regions at different depths is important for understanding the stages of neotectonic formation of the region and seismic hazard assessment. On the territory of the Uimon depression of the Altai Mountains in different years,...

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Main Authors: Kuzina Z. Ya., Nevedrova N. N., Sanchaa А. M.
Format: Article
Language:Russian
Published: Murmansk State Technical University 2023-06-01
Series:Vestnik MGTU
Subjects:
Online Access:http://vestnik.mstu.edu.ru/show-eng.shtml?art=2173
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author Kuzina Z. Ya.
Nevedrova N. N.
Sanchaa А. M.
author_facet Kuzina Z. Ya.
Nevedrova N. N.
Sanchaa А. M.
author_sort Kuzina Z. Ya.
collection DOAJ
description Determining the structure of intermountain depressions in seismically active regions at different depths is important for understanding the stages of neotectonic formation of the region and seismic hazard assessment. On the territory of the Uimon depression of the Altai Mountains in different years, measurements were carried out by deep methods of electrical exploration, such as sounding by the formation of the field and vertical electrical soundings. However, to clarify the structure of the upper part of the section, where bedrock outcrops are observed on the day surface, it is necessary to use shallow methods, for example, electrical tomography (ET). The paper discusses the results of ET data interpretation using 2D and 3D inversion when studying basement outcrops in the western part of the basin. Taking into account a priori information and the obtained models, the geological structure of the object of study has been refined. Based on the results of the interpretation of the data of electrotomography using programs of two- and three-dimensional inversion, the geoelectric structure of one of the outcrops of the basement rocks on the day surface has been determined. The immersion of the studied object in the western direction towards the adjacent outcrop of rocks of the Baratal Formation of smaller sizes located in the immediate vicinity has been established. It can be assumed that these two exits are connected at a depth of 15–20 m and, most likely, are one structure.
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spelling doaj.art-89cf85e76bec4f598da9a3845b7a53f92023-06-29T08:29:39ZrusMurmansk State Technical UniversityVestnik MGTU1560-92781997-47362023-06-0126216016910.21443/1560-9278-2023-26-2-160-169Structural features of the upper part of the section of the Gorniy Altai Uimon depression according to electrotomography data using 3D softwareKuzina Z. Ya.0Nevedrova N. N.1https://orcid.org/0000-0003-3210-5248Sanchaa А. M.2https://orcid.org/0000-0002-4523-6661The Trofimuk Institute of Petroleum Geology and Geophysics of the Siberian Branch RAS, EngineerThe Trofimuk Institute of Petroleum Geology and Geophysics of the Siberian Branch RAS, EngineerThe Trofimuk Institute of Petroleum Geology and Geophysics of the Siberian Branch RAS, EngineerDetermining the structure of intermountain depressions in seismically active regions at different depths is important for understanding the stages of neotectonic formation of the region and seismic hazard assessment. On the territory of the Uimon depression of the Altai Mountains in different years, measurements were carried out by deep methods of electrical exploration, such as sounding by the formation of the field and vertical electrical soundings. However, to clarify the structure of the upper part of the section, where bedrock outcrops are observed on the day surface, it is necessary to use shallow methods, for example, electrical tomography (ET). The paper discusses the results of ET data interpretation using 2D and 3D inversion when studying basement outcrops in the western part of the basin. Taking into account a priori information and the obtained models, the geological structure of the object of study has been refined. Based on the results of the interpretation of the data of electrotomography using programs of two- and three-dimensional inversion, the geoelectric structure of one of the outcrops of the basement rocks on the day surface has been determined. The immersion of the studied object in the western direction towards the adjacent outcrop of rocks of the Baratal Formation of smaller sizes located in the immediate vicinity has been established. It can be assumed that these two exits are connected at a depth of 15–20 m and, most likely, are one structure.http://vestnik.mstu.edu.ru/show-eng.shtml?art=2173gorniy altaiuimon depressionelectrical resistivity tomographygeoelectrical sections2d inversion3d inversionгорный алтайуймонская впадинаэлектротомографиягеоэлектрические разрезы2d инверсия3d инверсия
spellingShingle Kuzina Z. Ya.
Nevedrova N. N.
Sanchaa А. M.
Structural features of the upper part of the section of the Gorniy Altai Uimon depression according to electrotomography data using 3D software
Vestnik MGTU
gorniy altai
uimon depression
electrical resistivity tomography
geoelectrical sections
2d inversion
3d inversion
горный алтай
уймонская впадина
электротомография
геоэлектрические разрезы
2d инверсия
3d инверсия
title Structural features of the upper part of the section of the Gorniy Altai Uimon depression according to electrotomography data using 3D software
title_full Structural features of the upper part of the section of the Gorniy Altai Uimon depression according to electrotomography data using 3D software
title_fullStr Structural features of the upper part of the section of the Gorniy Altai Uimon depression according to electrotomography data using 3D software
title_full_unstemmed Structural features of the upper part of the section of the Gorniy Altai Uimon depression according to electrotomography data using 3D software
title_short Structural features of the upper part of the section of the Gorniy Altai Uimon depression according to electrotomography data using 3D software
title_sort structural features of the upper part of the section of the gorniy altai uimon depression according to electrotomography data using 3d software
topic gorniy altai
uimon depression
electrical resistivity tomography
geoelectrical sections
2d inversion
3d inversion
горный алтай
уймонская впадина
электротомография
геоэлектрические разрезы
2d инверсия
3d инверсия
url http://vestnik.mstu.edu.ru/show-eng.shtml?art=2173
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AT nevedrovann structuralfeaturesoftheupperpartofthesectionofthegorniyaltaiuimondepressionaccordingtoelectrotomographydatausing3dsoftware
AT sanchaaam structuralfeaturesoftheupperpartofthesectionofthegorniyaltaiuimondepressionaccordingtoelectrotomographydatausing3dsoftware