Modern carbonate formation in low-mineralized flowing waters
Continental carbonate formation in low-mineralized flowing waters of temperate latitude is rare phenomenon. Taking this into account a study was conducted of crustate and stalactite-like authigenic calcite aggregates formed in the thalwegs of the ravines of the Volga Upland. According to chemical an...
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EDP Sciences
2019-01-01
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Online Access: | https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_01030.pdf |
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doaj-ce4ae6273fd94d8ca4a5c8791f0fddee2021-02-02T05:54:14ZengEDP SciencesE3S Web of Conferences2267-12422019-01-01980103010.1051/e3sconf/20199801030e3sconf_wri-162018_01030Modern carbonate formation in low-mineralized flowing watersKorolev Eduard0Eskin Aleksey1Khuzin Ilnur2Petrova Dariya3Barieva Enza4Korolev Albert5Kazan Federal UniversityKazan Federal UniversityKazan Federal UniversityKazan Federal UniversityKazan Federal UniversityKazan Federal UniversityContinental carbonate formation in low-mineralized flowing waters of temperate latitude is rare phenomenon. Taking this into account a study was conducted of crustate and stalactite-like authigenic calcite aggregates formed in the thalwegs of the ravines of the Volga Upland. According to chemical and isotopic analysis, modern carbonates are formed from poorly mineralized, meteoric waters of medium hardness, hydrocarbonate-magnesium-calcium hydrochemical type. It has been established that newly formed carbonate aggregates are characterized by the predominance of lightweight carbon and oxygen in the crystal structure. The osmotic hypothesis of the formation of lime-calcite aggregates is proposed.https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_01030.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Korolev Eduard Eskin Aleksey Khuzin Ilnur Petrova Dariya Barieva Enza Korolev Albert |
spellingShingle |
Korolev Eduard Eskin Aleksey Khuzin Ilnur Petrova Dariya Barieva Enza Korolev Albert Modern carbonate formation in low-mineralized flowing waters E3S Web of Conferences |
author_facet |
Korolev Eduard Eskin Aleksey Khuzin Ilnur Petrova Dariya Barieva Enza Korolev Albert |
author_sort |
Korolev Eduard |
title |
Modern carbonate formation in low-mineralized flowing waters |
title_short |
Modern carbonate formation in low-mineralized flowing waters |
title_full |
Modern carbonate formation in low-mineralized flowing waters |
title_fullStr |
Modern carbonate formation in low-mineralized flowing waters |
title_full_unstemmed |
Modern carbonate formation in low-mineralized flowing waters |
title_sort |
modern carbonate formation in low-mineralized flowing waters |
publisher |
EDP Sciences |
series |
E3S Web of Conferences |
issn |
2267-1242 |
publishDate |
2019-01-01 |
description |
Continental carbonate formation in low-mineralized flowing waters of temperate latitude is rare phenomenon. Taking this into account a study was conducted of crustate and stalactite-like authigenic calcite aggregates formed in the thalwegs of the ravines of the Volga Upland. According to chemical and isotopic analysis, modern carbonates are formed from poorly mineralized, meteoric waters of medium hardness, hydrocarbonate-magnesium-calcium hydrochemical type. It has been established that newly formed carbonate aggregates are characterized by the predominance of lightweight carbon and oxygen in the crystal structure. The osmotic hypothesis of the formation of lime-calcite aggregates is proposed. |
url |
https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_01030.pdf |
work_keys_str_mv |
AT koroleveduard moderncarbonateformationinlowmineralizedflowingwaters AT eskinaleksey moderncarbonateformationinlowmineralizedflowingwaters AT khuzinilnur moderncarbonateformationinlowmineralizedflowingwaters AT petrovadariya moderncarbonateformationinlowmineralizedflowingwaters AT barievaenza moderncarbonateformationinlowmineralizedflowingwaters AT korolevalbert moderncarbonateformationinlowmineralizedflowingwaters |
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