CHAOITE FORMATION FROM CARBON-BEARING FLUID AT LOW PT PARAMETERS

dc.contributor.author	Simakov S.K.
dc.contributor.author	Kalmykov A.E.
dc.contributor.author	Sorokin L.M.
dc.contributor.author	Yagovkina M.A.
dc.contributor.author	Grebenshchikova E.A.
dc.contributor.author	Novikov M.P.
dc.contributor.author	Drozdova I.A.
dc.date.accessioned	2022-08-14T03:31:08Z
dc.date.available	2022-08-14T03:31:08Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13470726
dc.identifier.citation	Doklady Earth Sciences, 2004, 399, 9, 1289-1290
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38527
dc.description.abstract	Data apparently suggest that chaoite is a high-temperature phase that can occur in nature only under superhigh temperatures, which correspond to meteorite structures and lower mantle. However, this is inconsistent with the presence of impurities of carbyne (a high-temperature carbon phase genetically related to chaoite) in natural graphites. We studied the formation of free carbon from carbon-bearing gases at 500°C and total pressure of 1000 atm.
dc.title	CHAOITE FORMATION FROM CARBON-BEARING FLUID AT LOW PT PARAMETERS
dc.type	Статья

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