ISOTOPIC SEPARATION OF SULFUR IN HIGH-TEMPERATURE CONDENSATION ZONES

dc.contributor.author	Malyshev A.I.
dc.date.accessioned	2022-07-18T00:49:01Z
dc.date.available	2022-07-18T00:49:01Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13449083
dc.identifier.citation	Doklady Earth Sciences, 2004, 395, 2, 206-209
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38194
dc.description.abstract	Considered is the process of isotopic separation capable to explain the anomalous isotopic composition of sulfur of Norilsk deposits without employing the concepts of crust sulfur contamination. The estimation of isotopic separation effect at 'gas-liquid' transition shows that the shift of isotope ratios in sulfur condensate can vary from close to zero values to δ34S=20.262. It makes impossible using sulfur isotope composition as its source evaluation criterion and easily explains the observed anomalies for Norilsk and other deposits.
dc.title	ISOTOPIC SEPARATION OF SULFUR IN HIGH-TEMPERATURE CONDENSATION ZONES
dc.type	Статья

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