CHLORIDE AND WATER SOLUBILITY IN BASALT AND ANDESITE MELTS AND IMPLICATIONS FOR MAGMATIC DEGASSING

dc.contributor.author	Webster J.D.
dc.contributor.author	Kinzler R.J.
dc.contributor.author	Mathez E.A.
dc.date.accessioned	2021-01-12T05:15:17Z
dc.date.available	2021-01-12T05:15:17Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=13678182
dc.identifier.citation	Geochimica et Cosmochimica Acta, 1999, , 5, 729-738
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22725
dc.description.abstract	The solubilities of chloride (Cl−) and H2O in aluminosilicate melts of basalt, andesite, and latite compositions saturated in aqueous vapor and/or hydrosaline liquid were determined at 2000 bars and ≈1 bar by melting mixtures of NaCl, KCl, H2O, and natural and synthetic rock powders and by measuring Cl− and H2O in the run product glasses. The abundances of Cl− in several of the aqueous run product liquids were also measured, and the partitioning of Cl− between aqueous vapor and silicate melt was determined for these experiments.
dc.title	CHLORIDE AND WATER SOLUBILITY IN BASALT AND ANDESITE MELTS AND IMPLICATIONS FOR MAGMATIC DEGASSING
dc.type	Статья

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