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

dc.contributor.authorWebster J.D.
dc.contributor.authorKinzler R.J.
dc.contributor.authorMathez E.A.
dc.date.accessioned2021-01-12T05:15:17Z
dc.date.available2021-01-12T05:15:17Z
dc.date.issued1999
dc.description.abstractThe 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.identifierhttps://elibrary.ru/item.asp?id=13678182
dc.identifier.citationGeochimica et Cosmochimica Acta, 1999, , 5, 729-738
dc.identifier.issn0016-7037
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/22725
dc.titleCHLORIDE AND WATER SOLUBILITY IN BASALT AND ANDESITE MELTS AND IMPLICATIONS FOR MAGMATIC DEGASSING
dc.typeСтатья

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