KFU. Card publication. 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

Form of presentation

Articles in international journals and collections

Year of publication

2014

Authors, employees of KFU

Kadyrov Rail Ilgizarovich, author

Sungatullin Rafael Kharisovich, author

Other authors

Kuleshov Vladimir Nikolaevich

Authors, postgraduates KFU

Kadyrov Rail Ilgizarovich, postgraduate kfu

Bibliographic description in the original language

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.

Annotation

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.

Keywords

Carbon and oxygen isotope, dolomites, Syukeevo, gypsum

The name of the journal

LITHOL MINER RESOUR+

URL

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

Please use this ID to quote from or refer to the card

https://repository.kpfu.ru/eng/?p_id=84904&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Kadyrov Rail Ilgizarovich	ru_RU
dc.contributor.author	Sungatullin Rafael Kharisovich	ru_RU
dc.contributor.author	Kadyrov Rail Ilgizarovich	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/eng/?p_id=84904&p_lang=2	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	Articles in international journals and collections	ru_RU