STUDY OF THE TRANSFORMATION OF HYDROGEN-CONTAINING CENTERS IN DIAMOND AT HIGH PT PARAMETERS

dc.contributor.author	Kupriyanov I.N.
dc.contributor.author	Pal'yanov Yu.N.
dc.contributor.author	Shatsky V.S.
dc.contributor.author	Kalinin A.A.
dc.contributor.author	Nadolinnyi V.A.
dc.contributor.author	Yur'eva O.P.
dc.date.accessioned	2024-10-23T07:15:48Z
dc.date.available	2024-10-23T07:15:48Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13509526
dc.identifier.citation	Doklady Earth Sciences, 2006, 406, 1, 69-73
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46120
dc.description.abstract	The influence of hydrogen is considered in many geological processes, and the special role of hydrogen is emphasized in deep geodynamics in the ascent of mantle plumes. Some models of diamond formation also assume an interaction between the reduced methane–hydrogen fluid and more oxidized rocks. As has been shown by experiments, hydrogen may be a reductant of CO2 during diamond crystallization as a result of carbonate–silicate interaction.
dc.title	STUDY OF THE TRANSFORMATION OF HYDROGEN-CONTAINING CENTERS IN DIAMOND AT HIGH PT PARAMETERS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X0601017X

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