| Reference Type | Journal (article/letter/editorial) |
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| Title | A study of iron-bearing rutiles in the paragenesis TiO2-Al2O3-P2O5-SiO2 |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Putnis, A. | Author |
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| Wilson, M. M. | Author |
| Year | 1978 (June) | Volume | 42 |
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| Issue | 322 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_42/42-322-255.pdf+ |
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| DOI | doi:10.1180/minmag.1978.042.322.14Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 2905 | Long-form Identifier | mindat:1:5:2905:0 |
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| GUID | 0 |
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| Full Reference | Putnis, A., Wilson, M. M. (1978) A study of iron-bearing rutiles in the paragenesis TiO2-Al2O3-P2O5-SiO2. Mineralogical Magazine, 42 (322) 255-263 doi:10.1180/minmag.1978.042.322.14 |
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| Plain Text | Putnis, A., Wilson, M. M. (1978) A study of iron-bearing rutiles in the paragenesis TiO2-Al2O3-P2O5-SiO2. Mineralogical Magazine, 42 (322) 255-263 doi:10.1180/minmag.1978.042.322.14 |
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| In | (1978, June) Mineralogical Magazine Vol. 42 (322) Mineralogical Society |
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| Abstract/Notes | SummaryHydrothermal ruffles from a suite of rocks at Mount Perry, Queensland, have been studied in thin section, by electron microprobe analysis, and by transmission electron microscopy. The iron-bearing rutiles, while originally singte-phase, are found to exsolve a sequence of iron-rich precipitates on experimental annealing, with hematite being formed as the stable equilibrium precipitate. Experiments at different temperatures and annealing times enable a time-temperature-transformation plot to be drawn for the exsolution process. The kinetics of this process are used to conclude that the rutiles formed below about 450 °C. |
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