SOLUBILITY AND PARTITIONING OF NE, AR, KR AND XE IN MINERALS AND SYNTHETIC BASALTIC MELTS

dc.contributor.author	Broadhurst C.L.
dc.contributor.author	Drake M.J.
dc.contributor.author	Hagee B.E.
dc.contributor.author	Bernatowicz T.J.
dc.date.accessioned	2020-11-09T02:14:14Z
dc.date.available	2020-11-09T02:14:14Z
dc.date.issued	1992
dc.identifier	https://elibrary.ru/item.asp?id=31546582
dc.identifier.citation	Geochimica et Cosmochimica Acta, 1992, , 2, 709-723
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18692
dc.description.abstract	The solubilities of Ne, Ar, Kr, and Xe gases were measured in natural samples of anorthite, diopside, forsterite, spinel, and synthetic basaltic melts, the samples which represent equilibrium pairs in the Fo-An-Di-SiO2 system. Results show that, in natural minerals, the solubilities of these gases increase with increasing atomic number. In contrast, the solubilities of noble gases in the synthetic basaltic melts decreased with increasing atomic number. The partition coefficients increased with increasing atomic number for all mineral/melt pairs.
dc.title	SOLUBILITY AND PARTITIONING OF NE, AR, KR AND XE IN MINERALS AND SYNTHETIC BASALTIC MELTS
dc.type	Статья

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