FORMATION OF CARBON AND HYDROGEN SPECIES IN MAGMAS AT LOW OXYGEN FUGACITY

dc.contributor.author	Kadik A.
dc.contributor.author	Pineau F.
dc.contributor.author	Jendrzejewski N.
dc.contributor.author	Martinez I.
dc.contributor.author	Javoy M.
dc.contributor.author	Litvin Y.
dc.date.accessioned	2022-03-30T02:31:49Z
dc.date.available	2022-03-30T02:31:49Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13464383
dc.identifier.citation	Journal of Petrology, 2004, 45, 7, 1297
dc.identifier.issn	0022-3530
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/36720
dc.description.abstract	Studies of iron-bearing silicate melt (ferrobasalt) þ iron metallicphase þ graphite þ hydrogen equilibria show that carbon andhydrogen solubilities in melts are important for the evolution of theupper mantle. In a series of experiments conducted at 3 7GPa and1520--- 1600 C, we have characterized the nature (oxidized vsreduced) and quantified the abundances of C- and H-compoundsdissolvediniron-bearingsilicatemelts.Experimentswerecarried outin an anvil-with-hole apparatus permitting the achievement of equalchemical potentials of H
dc.title	FORMATION OF CARBON AND HYDROGEN SPECIES IN MAGMAS AT LOW OXYGEN FUGACITY
dc.type	Статья

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