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The sulfide capacity and the sulfur content at sulfide saturation of silicate melts at 1400˚C and 1 bar

O'Neill, Hugh; Mavrogenes, John

Description

The solubility of sulfur as S2 has been experimentally determined for 19 silicate melt compositions in the system CaOMgO-Al2O3-SiO2 (CMAS) ± TiO2 ± FeO, at 1400°C and 1 bar, using CO-CO2-SO2 gas mixtures to vary oxygen fugacity (fO2) and sulfur fugacit

dc.contributor.authorO'Neill, Hugh
dc.contributor.authorMavrogenes, John
dc.date.accessioned2015-12-13T23:41:19Z
dc.identifier.issn0022-3530
dc.identifier.urihttp://hdl.handle.net/1885/94845
dc.description.abstractThe solubility of sulfur as S2 has been experimentally determined for 19 silicate melt compositions in the system CaOMgO-Al2O3-SiO2 (CMAS) ± TiO2 ± FeO, at 1400°C and 1 bar, using CO-CO2-SO2 gas mixtures to vary oxygen fugacity (fO2) and sulfur fugacit
dc.publisherOxford University Press
dc.sourceJournal of Petrology
dc.subjectKeywords: silicate melt; solubility; sulfide; sulfur; thermodynamics Silicate melts; Sulfide capacity; Sulfur; Thermodynamics
dc.titleThe sulfide capacity and the sulfur content at sulfide saturation of silicate melts at 1400˚C and 1 bar
dc.typeJournal article
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.citationvolume43
dc.date.issued2002
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.ariespublicationMigratedxPub24542
local.type.statusPublished Version
local.contributor.affiliationO'Neill, Hugh, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationMavrogenes, John, College of Physical and Mathematical Sciences, ANU
local.description.embargo2037-12-31
local.bibliographicCitation.issue6
local.bibliographicCitation.startpage1049
local.bibliographicCitation.lastpage1087
dc.date.updated2015-12-12T09:32:02Z
local.identifier.scopusID2-s2.0-0036081862
CollectionsANU Research Publications

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