| Reference Type | Journal (article/letter/editorial) |
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| Title | On the existence of monoclinic NaAlSi3O8 s at elevated temperatures |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Grundy, H. D. | Author |
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| Brown, W. L. | Author |
| MacKenzie, W. S. | Author |
| Year | 1967 (March) | Volume | 36 |
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| Issue | 277 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_36/36-277-83.pdf+ |
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| DOI | doi:10.1180/minmag.1967.036.277.13Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6039 | Long-form Identifier | mindat:1:5:6039:8 |
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| GUID | 0 |
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| Full Reference | Grundy, H. D., Brown, W. L., MacKenzie, W. S. (1967) On the existence of monoclinic NaAlSi3O8 s at elevated temperatures. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (277) 83-88 doi:10.1180/minmag.1967.036.277.13 |
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| Plain Text | Grundy, H. D., Brown, W. L., MacKenzie, W. S. (1967) On the existence of monoclinic NaAlSi3O8 s at elevated temperatures. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (277) 83-88 doi:10.1180/minmag.1967.036.277.13 |
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| In | (1966) Mineralogical Magazine Vol. 36 (277) Mineralogical Society |
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| Abstract/Notes | SummaryMeasurements from powder diffraction patterns recorded at temperatures up to 950° C for the supposed equilibrium forms of albite synthesized at 800°, 900°, and 1000° C by MacKenzie (1957) indicate that only the form synthesized at 1000° C becomes monoclinic. Single-crystal measurements on heated pure natural albite (Ab99·26) show that it becomes truly monoclinic, both in geometry and intensity distribution, at 930° C, the same temperature as for the highest-temperature synthetic form. These experiments were carried out in conditions that exclude possible contamination by potassium. |
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