| Reference Type | Journal (article/letter/editorial) |
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| Title | The nature and significance of exsolved phases in some chrome spinels from the Rhum layered intrusion |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Putnis, A. | Author |
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| Price, G. D. | Author |
| Year | 1979 (December) | Volume | 43 |
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| Issue | 328 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_43/43-328-519.pdf+ |
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| DOI | doi:10.1180/minmag.1979.043.328.12Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3075 | Long-form Identifier | mindat:1:5:3075:9 |
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| GUID | 0 |
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| Full Reference | Putnis, A., Price, G. D. (1979) The nature and significance of exsolved phases in some chrome spinels from the Rhum layered intrusion. Mineralogical Magazine, 43 (328) 519-526 doi:10.1180/minmag.1979.043.328.12 |
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| Plain Text | Putnis, A., Price, G. D. (1979) The nature and significance of exsolved phases in some chrome spinels from the Rhum layered intrusion. Mineralogical Magazine, 43 (328) 519-526 doi:10.1180/minmag.1979.043.328.12 |
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| In | (1979, December) Mineralogical Magazine Vol. 43 (328) Mineralogical Society |
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| Abstract/Notes | SummaryChrome spinels from seams in the Rhum layered intrusion, Inner Hebrides, generally contain very fine platelets of exsolved phases. Despite the low bulk Ti content (< 1%) of the spinel grains, analytical electron microscopy shows these platelets to be highly enriched in titanium. Electron diffraction indicates the presence of platelets of two different phases, one a magnesian ilmenite, the other a defect spinel intermediate phase. The platelets are the result of oxidation of the spinel at moderate (c. 600 °C) temperatures and their distribution suggests that oxygen fugacity gradients existed across some of the seams. |
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