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Wearing, E. (1984) Occurrence of some Ni- and Sn-rich minerals in copper converter slags. Mineralogical Magazine, 48 (347) 243-249 doi:10.1180/minmag.1984.048.347.08

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Reference TypeJournal (article/letter/editorial)
TitleOccurrence of some Ni- and Sn-rich minerals in copper converter slags
JournalMineralogical MagazineISSN0026-461X
AuthorsWearing, E.Author
Year1984 (June)Volume48
Issue347
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_48/48-347-243.pdf+
DOIdoi:10.1180/minmag.1984.048.347.08Search in ResearchGate
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Mindat Ref. ID3620Long-form Identifiermindat:1:5:3620:1
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Full ReferenceWearing, E. (1984) Occurrence of some Ni- and Sn-rich minerals in copper converter slags. Mineralogical Magazine, 48 (347) 243-249 doi:10.1180/minmag.1984.048.347.08
Plain TextWearing, E. (1984) Occurrence of some Ni- and Sn-rich minerals in copper converter slags. Mineralogical Magazine, 48 (347) 243-249 doi:10.1180/minmag.1984.048.347.08
In(1984, June) Mineralogical Magazine Vol. 48 (347) Mineralogical Society
Abstract/NotesAbstractThe chemistry of opaque spinel, delafossite (Cu2O·Fe2O3), cuprite (Cu2O), cassiterite, nickel-olivine (Ni2SiO4), and bunsenite (NiO) from some copper converter slags has been investigated by electron microprobe analysis. The spinel has a complex composition containing up to 33.89% NiO and 47.69% SnO2, ranging from essentially Ni2SnO4 to (Ni,Fe2+)O4. The associated delafossite contains up to 19.18% NiO and 38.15% SnO2. The chemical variation of the mineral phases is evaluated, and it appears that Ni2+ enters the spinel and delafossite to charge-balance the octahedrally coordinated Sn4+.


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