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

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dc.contributor.authorO'Neill, Hugh
dc.contributor.authorMavrogenes, John
dc.date.accessioned2015-12-13T23:41:19Z
dc.date.issued2002
dc.date.updated2015-12-12T09:32:02Z
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.identifier.issn0022-3530
dc.identifier.urihttp://hdl.handle.net/1885/94845
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.bibliographicCitation.issue6
local.bibliographicCitation.lastpage1087
local.bibliographicCitation.startpage1049
local.contributor.affiliationO'Neill, Hugh, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationMavrogenes, John, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidO'Neill, Hugh, u8101317
local.contributor.authoruidMavrogenes, John, u9415694
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.ariespublicationMigratedxPub24542
local.identifier.citationvolume43
local.identifier.scopusID2-s2.0-0036081862
local.type.statusPublished Version

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