Hydrogeology of the artesian basins of the southern part of the Kara sea and Yamal-Gydansk megasaddle

Background. In hydrogeological terms, the territory of the Barents-Kara shelf has not been studied in sufficient detail. The data on its hydrogeological zoning are based mainly on the results of research undertaken in the 1970s, when attempts were made to isolate artesian shelf basins according to a...

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Published in:Proceedings of higher educational establishments. Geology and Exploration
Main Author: S. S. Vlasenko
Format: Article in Journal/Newspaper
Language:Russian
Published: Sergo Ordzhonikidze Russian State University for Geological Prospecting 2022
Subjects:
Online Access:https://doi.org/10.32454/0016-7762-2022-64-2-92-99
https://doaj.org/article/b48277088a6440caad21820410f40ca0
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spelling ftdoajarticles:oai:doaj.org/article:b48277088a6440caad21820410f40ca0 2023-05-15T15:18:20+02:00 Hydrogeology of the artesian basins of the southern part of the Kara sea and Yamal-Gydansk megasaddle S. S. Vlasenko 2022-10-01T00:00:00Z https://doi.org/10.32454/0016-7762-2022-64-2-92-99 https://doaj.org/article/b48277088a6440caad21820410f40ca0 RU rus Sergo Ordzhonikidze Russian State University for Geological Prospecting https://www.geology-mgri.ru/jour/article/view/774 https://doaj.org/toc/0016-7762 https://doaj.org/toc/2618-8708 0016-7762 2618-8708 doi:10.32454/0016-7762-2022-64-2-92-99 https://doaj.org/article/b48277088a6440caad21820410f40ca0 Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 2, Pp 92-99 (2022) баренцево-карский шельф гидрогеологическое районирование артезианские бассейны подземные воды водоносные комплексы нефтегазоносные структуры Geology QE1-996.5 article 2022 ftdoajarticles https://doi.org/10.32454/0016-7762-2022-64-2-92-99 2023-03-19T01:40:25Z Background. In hydrogeological terms, the territory of the Barents-Kara shelf has not been studied in sufficient detail. The data on its hydrogeological zoning are based mainly on the results of research undertaken in the 1970s, when attempts were made to isolate artesian shelf basins according to a set of hydrogeological indicators of oil and gas content. Currently, the position of the basin boundaries can be adjusted using current data from oil and gas and geological zoning and the hydrogeological testing of wells.Aim. To conduct the hydrogeological zoning of the territory of the southern part of the Kara Sea and the north of the West Siberian geosyneclise, including oil and gas structures — the South Kara syneclise and the Yamal-Gydan megasaddle, as well as to carry out a chemical analysis of groundwater of the Jurassic-Cretaceous aquifer complexes composing the sediments of the sedimentary cover of the West Siberian sedimentary basin.Materials and methods. A cartographic method was used to analyze earlier maps and schemes of hydrogeological and oil and gas geological zoning of the Russian sector of the continental slope of the Arctic Ocean, and then to determine the boundaries of the identified artesian basins. For a chemical analysis of groundwater, the results of hydrogeological testing of wells drilled at the Zapolyarnoye oil and gas condensate field were used.Results. The boundaries of two artesian basins — the South Kara submarine and the Yamal-Gydan semi-marine, corresponding to the same-name oil and gas prospective structures and having the same geological structure, were determined. Both basins are characterised by the presence of the main aquifer complexes of the Mesozoic hydrogeological floor of Western Siberia. When studying the composition of groundwater of the Zapolyarnoye deposit, it was found that the types of water change regularly with depth and an increase in the content of the hydrocarbonate ion due to the possible migration of fluids enriched with carbonic acid dioxide from the rocks of ... Article in Journal/Newspaper Arctic Arctic Ocean Carbonic acid Kara Sea Siberia Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Kara Sea Proceedings of higher educational establishments. Geology and Exploration 2 92 99
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language Russian
topic баренцево-карский шельф
гидрогеологическое районирование
артезианские бассейны
подземные воды
водоносные комплексы
нефтегазоносные структуры
Geology
QE1-996.5
spellingShingle баренцево-карский шельф
гидрогеологическое районирование
артезианские бассейны
подземные воды
водоносные комплексы
нефтегазоносные структуры
Geology
QE1-996.5
S. S. Vlasenko
Hydrogeology of the artesian basins of the southern part of the Kara sea and Yamal-Gydansk megasaddle
topic_facet баренцево-карский шельф
гидрогеологическое районирование
артезианские бассейны
подземные воды
водоносные комплексы
нефтегазоносные структуры
Geology
QE1-996.5
description Background. In hydrogeological terms, the territory of the Barents-Kara shelf has not been studied in sufficient detail. The data on its hydrogeological zoning are based mainly on the results of research undertaken in the 1970s, when attempts were made to isolate artesian shelf basins according to a set of hydrogeological indicators of oil and gas content. Currently, the position of the basin boundaries can be adjusted using current data from oil and gas and geological zoning and the hydrogeological testing of wells.Aim. To conduct the hydrogeological zoning of the territory of the southern part of the Kara Sea and the north of the West Siberian geosyneclise, including oil and gas structures — the South Kara syneclise and the Yamal-Gydan megasaddle, as well as to carry out a chemical analysis of groundwater of the Jurassic-Cretaceous aquifer complexes composing the sediments of the sedimentary cover of the West Siberian sedimentary basin.Materials and methods. A cartographic method was used to analyze earlier maps and schemes of hydrogeological and oil and gas geological zoning of the Russian sector of the continental slope of the Arctic Ocean, and then to determine the boundaries of the identified artesian basins. For a chemical analysis of groundwater, the results of hydrogeological testing of wells drilled at the Zapolyarnoye oil and gas condensate field were used.Results. The boundaries of two artesian basins — the South Kara submarine and the Yamal-Gydan semi-marine, corresponding to the same-name oil and gas prospective structures and having the same geological structure, were determined. Both basins are characterised by the presence of the main aquifer complexes of the Mesozoic hydrogeological floor of Western Siberia. When studying the composition of groundwater of the Zapolyarnoye deposit, it was found that the types of water change regularly with depth and an increase in the content of the hydrocarbonate ion due to the possible migration of fluids enriched with carbonic acid dioxide from the rocks of ...
format Article in Journal/Newspaper
author S. S. Vlasenko
author_facet S. S. Vlasenko
author_sort S. S. Vlasenko
title Hydrogeology of the artesian basins of the southern part of the Kara sea and Yamal-Gydansk megasaddle
title_short Hydrogeology of the artesian basins of the southern part of the Kara sea and Yamal-Gydansk megasaddle
title_full Hydrogeology of the artesian basins of the southern part of the Kara sea and Yamal-Gydansk megasaddle
title_fullStr Hydrogeology of the artesian basins of the southern part of the Kara sea and Yamal-Gydansk megasaddle
title_full_unstemmed Hydrogeology of the artesian basins of the southern part of the Kara sea and Yamal-Gydansk megasaddle
title_sort hydrogeology of the artesian basins of the southern part of the kara sea and yamal-gydansk megasaddle
publisher Sergo Ordzhonikidze Russian State University for Geological Prospecting
publishDate 2022
url https://doi.org/10.32454/0016-7762-2022-64-2-92-99
https://doaj.org/article/b48277088a6440caad21820410f40ca0
geographic Arctic
Arctic Ocean
Kara Sea
geographic_facet Arctic
Arctic Ocean
Kara Sea
genre Arctic
Arctic Ocean
Carbonic acid
Kara Sea
Siberia
genre_facet Arctic
Arctic Ocean
Carbonic acid
Kara Sea
Siberia
op_source Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 2, Pp 92-99 (2022)
op_relation https://www.geology-mgri.ru/jour/article/view/774
https://doaj.org/toc/0016-7762
https://doaj.org/toc/2618-8708
0016-7762
2618-8708
doi:10.32454/0016-7762-2022-64-2-92-99
https://doaj.org/article/b48277088a6440caad21820410f40ca0
op_doi https://doi.org/10.32454/0016-7762-2022-64-2-92-99
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