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Tin-rich garnet, pyroxene, and spinel from a slag

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Zeitschriftentitel: Mineralogical Magazine
Personen und Körperschaften: Butler, B. C. M.
In: Mineralogical Magazine, 42, 1978, 324, S. 487-492
Format: E-Article
Sprache: Englisch
veröffentlicht:
Mineralogical Society
Schlagwörter:
Geochemistry and Petrology
author_facet Butler, B. C. M.
Butler, B. C. M.
author Butler, B. C. M.
spellingShingle Butler, B. C. M.
Mineralogical Magazine
Tin-rich garnet, pyroxene, and spinel from a slag
Geochemistry and Petrology
author_sort butler, b. c. m.
spelling Butler, B. C. M. 0026-461X 1471-8022 Mineralogical Society Geochemistry and Petrology http://dx.doi.org/10.1180/minmag.1978.042.324.11 <jats:title>Summary</jats:title><jats:p>Garnet containing up to 26% SnO<jats:sub>2</jats:sub>, and pyroxene and spinel containing 12% and 10% SnO<jats:sub>2</jats:sub> 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 Sn<jats:sup>4+</jats:sup> in the structure of these minerals. The absence of tin from coexisting melilite suggests that Sn<jats:sup>4+</jats:sup> is only able to substitute for ions in octahedral co-ordination.</jats:p> Tin-rich garnet, pyroxene, and spinel from a slag Mineralogical Magazine
doi_str_mv 10.1180/minmag.1978.042.324.11
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imprint Mineralogical Society, 1978
imprint_str_mv Mineralogical Society, 1978
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series Mineralogical Magazine
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title Tin-rich garnet, pyroxene, and spinel from a slag
title_unstemmed Tin-rich garnet, pyroxene, and spinel from a slag
title_full Tin-rich garnet, pyroxene, and spinel from a slag
title_fullStr Tin-rich garnet, pyroxene, and spinel from a slag
title_full_unstemmed Tin-rich garnet, pyroxene, and spinel from a slag
title_short Tin-rich garnet, pyroxene, and spinel from a slag
title_sort tin-rich garnet, pyroxene, and spinel from a slag
topic Geochemistry and Petrology
url http://dx.doi.org/10.1180/minmag.1978.042.324.11
publishDate 1978
physical 487-492
description <jats:title>Summary</jats:title><jats:p>Garnet containing up to 26% SnO<jats:sub>2</jats:sub>, and pyroxene and spinel containing 12% and 10% SnO<jats:sub>2</jats:sub> 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 Sn<jats:sup>4+</jats:sup> in the structure of these minerals. The absence of tin from coexisting melilite suggests that Sn<jats:sup>4+</jats:sup> is only able to substitute for ions in octahedral co-ordination.</jats:p>
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author Butler, B. C. M.
author_facet Butler, B. C. M., Butler, B. C. M.
author_sort butler, b. c. m.
container_issue 324
container_start_page 487
container_title Mineralogical Magazine
container_volume 42
description <jats:title>Summary</jats:title><jats:p>Garnet containing up to 26% SnO<jats:sub>2</jats:sub>, and pyroxene and spinel containing 12% and 10% SnO<jats:sub>2</jats:sub> 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 Sn<jats:sup>4+</jats:sup> in the structure of these minerals. The absence of tin from coexisting melilite suggests that Sn<jats:sup>4+</jats:sup> is only able to substitute for ions in octahedral co-ordination.</jats:p>
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id ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTE4MC9taW5tYWcuMTk3OC4wNDIuMzI0LjEx
imprint Mineralogical Society, 1978
imprint_str_mv Mineralogical Society, 1978
institution DE-105, DE-14, DE-Ch1, DE-L229, DE-D275, DE-Bn3, DE-Brt1, DE-Zwi2, DE-D161, DE-Gla1, DE-Zi4, DE-15, DE-Pl11, DE-Rs1
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match_str butler1978tinrichgarnetpyroxeneandspinelfromaslag
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physical 487-492
publishDate 1978
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series Mineralogical Magazine
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spelling Butler, B. C. M. 0026-461X 1471-8022 Mineralogical Society Geochemistry and Petrology http://dx.doi.org/10.1180/minmag.1978.042.324.11 <jats:title>Summary</jats:title><jats:p>Garnet containing up to 26% SnO<jats:sub>2</jats:sub>, and pyroxene and spinel containing 12% and 10% SnO<jats:sub>2</jats:sub> 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 Sn<jats:sup>4+</jats:sup> in the structure of these minerals. The absence of tin from coexisting melilite suggests that Sn<jats:sup>4+</jats:sup> is only able to substitute for ions in octahedral co-ordination.</jats:p> Tin-rich garnet, pyroxene, and spinel from a slag Mineralogical Magazine
spellingShingle Butler, B. C. M., Mineralogical Magazine, Tin-rich garnet, pyroxene, and spinel from a slag, Geochemistry and Petrology
title Tin-rich garnet, pyroxene, and spinel from a slag
title_full Tin-rich garnet, pyroxene, and spinel from a slag
title_fullStr Tin-rich garnet, pyroxene, and spinel from a slag
title_full_unstemmed Tin-rich garnet, pyroxene, and spinel from a slag
title_short Tin-rich garnet, pyroxene, and spinel from a slag
title_sort tin-rich garnet, pyroxene, and spinel from a slag
title_unstemmed Tin-rich garnet, pyroxene, and spinel from a slag
topic Geochemistry and Petrology
url http://dx.doi.org/10.1180/minmag.1978.042.324.11