КФУ. Карточка публикации. Isotope (δ13C and δ18O) Compositions of Dolomites from the Permian Evaporitic Sequences of the Eastern Russian Plate: Evidence from the Syukeevo Gypsum Deposit

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ISOTOPE (δ13C AND δ18O) COMPOSITIONS OF DOLOMITES FROM THE PERMIAN EVAPORITIC SEQUENCES OF THE EASTERN RUSSIAN PLATE: EVIDENCE FROM THE SYUKEEVO GYPSUM DEPOSIT

Форма представления

Статьи в зарубежных журналах и сборниках

Год публикации

2014

Авторы, сотрудники КФУ

Кадыров Раиль Илгизарович, автор

Сунгатуллин Рафаэль Харисович, автор

Другие авторы

Кулешов Владимир Николаевич

Авторы, аспиранты КФУ

Кадыров Раиль Илгизарович, автор

Библиографическое описание на языке оригинала

Sungatullin R. Kh., Kuleshov V. N. and Kadyrov R. I. Isotope (δ13C and δ18O) Compositions of Dolomites from the Permian Evaporitic Sequences of the Eastern Russian Plate: Evidence from the Syukeevo Gypsum Deposit // Lithology and Mineral Resources. 2014. Vol. 49, No. 5, pp. 406–415.

Аннотация

Carbon and oxygen isotope compositions has been studied in dolomites of the Syukeevo gypsum deposit located in the Eastern Russian Plate. Values of δ13C in the dolomites vary from 0.3 to 6.6 ?; δ18O, from 28.0 to 36.6?. It is shown that the dolomites were formed in the epicontinental evaporitic basin in dif ferent paleoecological settings. This led to the formation of diverse lithological types of dolomites with pecu liar isotopegeochemical features.

Ключевые слова

Carbon and oxygen isotope, dolomites, Syukeevo, gypsum

Название журнала

LITHOL MINER RESOUR+

URL

http://www.maik.rssi.ru/cgi-perl/journal.pl?name=lit&lang=eng

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https://repository.kpfu.ru/?p_id=84904

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Кадыров Раиль Илгизарович	ru_RU
dc.contributor.author	Сунгатуллин Рафаэль Харисович	ru_RU
dc.contributor.author	Кадыров Раиль Илгизарович	ru_RU
dc.date.accessioned	2014-01-01T00:00:00Z	ru_RU
dc.date.available	2014-01-01T00:00:00Z	ru_RU
dc.date.issued	2014	ru_RU
dc.identifier.citation	Sungatullin R. Kh., Kuleshov V. N. and Kadyrov R. I. Isotope (δ13C and δ18O) Compositions of Dolomites from the Permian Evaporitic Sequences of the Eastern Russian Plate: Evidence from the Syukeevo Gypsum Deposit // Lithology and Mineral Resources. 2014. Vol. 49, No. 5, pp. 406–415.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/?p_id=84904	ru_RU
dc.description.abstract	LITHOL MINER RESOUR+	ru_RU
dc.description.abstract	Carbon and oxygen isotope compositions has been studied in dolomites of the Syukeevo gypsum deposit located in the Eastern Russian Plate. Values of δ13C in the dolomites vary from 0.3 to 6.6 ?; δ18O, from 28.0 to 36.6?. It is shown that the dolomites were formed in the epicontinental evaporitic basin in dif ferent paleoecological settings. This led to the formation of diverse lithological types of dolomites with pecu liar isotopegeochemical features.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Carbon and oxygen isotope	ru_RU
dc.subject	dolomites	ru_RU
dc.subject	Syukeevo	ru_RU
dc.subject	gypsum	ru_RU
dc.title	Isotope (δ13C and δ18O) Compositions of Dolomites from the Permian Evaporitic Sequences of the Eastern Russian Plate: Evidence from the Syukeevo Gypsum Deposit	ru_RU
dc.type	Статьи в зарубежных журналах и сборниках	ru_RU