Linking structure and chemistry in the schorl-dravite series

Nine tourmaline crystals for which major and minor element composition data are available have been examined by single-crystal X-ray structure refinement. The single crystals were then analyzed for major elements (by electron microprobe methods), Fe3+/Fe2+ (by synchrotron micro X-ray absorption near...

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Veröffentlicht in:The American mineralogist 1999-06, Vol.84 (5-6), p.922-928
Hauptverfasser: Bloodaxe, Erich S, Hughes, John M, Dyar, M. Darby, Grew, Edward S, Guidotti, Charles V
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Sprache:eng
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Zusammenfassung:Nine tourmaline crystals for which major and minor element composition data are available have been examined by single-crystal X-ray structure refinement. The single crystals were then analyzed for major elements (by electron microprobe methods), Fe3+/Fe2+ (by synchrotron micro X-ray absorption near-edge spectroscopy), B and Li (by secondary ion mass spectrometry), and bulk H content (by uranium extraction). Despite recent claims based on chemical analyses, structure analysis suggests that no B exists in tetrahedral coordination in these samples. Analysis of cation ordering between the Y and Z octahedral sites suggests that the occurrence of an Fe2+ atom on a Y octahedral site may be locally associated with the absence of Mg at both of the neighboring Z sites, as substitutions of Fe2+ on Y and Mg on Z require antithetic shifts of the O6 anion.
ISSN:0003-004X
1945-3027
DOI:10.2138/am-1999-5-627