Modern carbonate formation in low-mineralized flowing waters

dc.contributor.author	Korolev E.
dc.contributor.author	Eskin A.
dc.contributor.author	Khuzin I.
dc.contributor.author	Petrova D.
dc.contributor.author	Barieva E.
dc.contributor.author	Korolev A.
dc.date.accessioned	2020-01-15T22:15:08Z
dc.date.available	2020-01-15T22:15:08Z
dc.date.issued	2019
dc.identifier.issn	2555-0403
dc.identifier.uri	https://dspace.kpfu.ru/xmlui/handle/net/157250
dc.description.abstract	© The Authors, published by EDP Sciences, 2019. 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.
dc.relation.ispartofseries	E3S Web of Conferences
dc.title	Modern carbonate formation in low-mineralized flowing waters
dc.type	Conference Paper
dc.relation.ispartofseries-volume	98
dc.collection	Публикации сотрудников КФУ
dc.source.id	SCOPUS25550403-2019-98-SID85067271191

Файлы в этом документе

Имя: SCOPUS25550403-20 ...

Размер: 44.25Kb

Формат: PDF

Публикации сотрудников КФУ Scopus [24551]
Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.