| Reference Type | Journal (article/letter/editorial) |
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| Title | Tin-rich garnet, pyroxene, and spinel from a slag |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Butler, B. C. M. | Author |
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| Year | 1978 (December) | Volume | 42 |
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| Issue | 324 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_42/42-324-487.pdf+ |
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| DOI | doi:10.1180/minmag.1978.042.324.11Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 2963 | Long-form Identifier | mindat:1:5:2963:0 |
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| GUID | 0 |
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| Full Reference | Butler, B. C. M. (1978) Tin-rich garnet, pyroxene, and spinel from a slag. Mineralogical Magazine, 42 (324) 487-492 doi:10.1180/minmag.1978.042.324.11 |
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| Plain Text | Butler, B. C. M. (1978) Tin-rich garnet, pyroxene, and spinel from a slag. Mineralogical Magazine, 42 (324) 487-492 doi:10.1180/minmag.1978.042.324.11 |
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| In | (1978, December) Mineralogical Magazine Vol. 42 (324) Mineralogical Society |
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| Abstract/Notes | SummaryGarnet containing up to 26% SnO2, and pyroxene and spinel containing 12% and 10% SnO2 respectively, occur in a tin-refining slag in association with cassiterite. These tin contents probably represent minimum values for the limit of ionic replacement of Sn4+ in the structure of these minerals. The absence of tin from coexisting melilite suggests that Sn4+ is only able to substitute for ions in octahedral co-ordination. |
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