| Reference Type | Journal (article/letter/editorial) |
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| Title | Can Ti4+ replace Si4+ in silicates? |
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| Journal | Mineralogical Magazine |
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| Authors | Hartman, P. | Author |
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| Year | 1969 (September) | Volume | 37 |
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| Issue | 287 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_37/37-287-366.pdf+ |
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| DOI | doi:10.1180/minmag.1969.037.287.09Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6298 | Long-form Identifier | mindat:1:5:6298:9 |
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| GUID | 0 |
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| Full Reference | Hartman, P. (1969) Can Ti4+ replace Si4+ in silicates?. Mineralogical Magazine, 37 (287) 366-369 doi:10.1180/minmag.1969.037.287.09 |
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| Plain Text | Hartman, P. (1969) Can Ti4+ replace Si4+ in silicates?. Mineralogical Magazine, 37 (287) 366-369 doi:10.1180/minmag.1969.037.287.09 |
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| In | (1969, September) Mineralogical Magazine Vol. 37 (287) Mineralogical Society |
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| Abstract/Notes | SummaryIt is argued on crystal-chemical grounds that Si deficiency is compensated by the entering of Al, Fe3+, or Ti4+, in this order of preference, into tetrahedral sites. It is pointed out that Ti4+ occurs in tetrahedral coordination in exceptional circumstances only, while Fe3+ relatively easily takes a tetrahedral coordination. |
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