| Reference Type | Journal (article/letter/editorial) |
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| Title | The thermal expansion of the sodalite group of minerals |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Taylor, D. | Author |
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| Year | 1968 (June) | Volume | 36 |
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| Issue | 282 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_36/36-282-761.pdf+ |
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| DOI | doi:10.1180/minmag.1968.036.282.02Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6154 | Long-form Identifier | mindat:1:5:6154:8 |
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| GUID | 0 |
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| Full Reference | Taylor, D. (1968) The thermal expansion of the sodalite group of minerals. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (282) 761-769 doi:10.1180/minmag.1968.036.282.02 |
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| Plain Text | Taylor, D. (1968) The thermal expansion of the sodalite group of minerals. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (282) 761-769 doi:10.1180/minmag.1968.036.282.02 |
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| In | (1966) Mineralogical Magazine Vol. 36 (282) Mineralogical Society |
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| Abstract/Notes | SummaryThermal expansion data up to 920° C by powder X-ray diffraction methods are presented for four noseans, five haüynes, and one sodalite. The rate of thermal expansion is at first high and increases with temperature; this is interpreted as due to the untwisting of the partially collapsed framework. Above a certain temperature (which depends on the mineral and its composition) the rate of thermal expansion is much lower and is linear with temperature; this corresponds to the rate of thermal expansion of the more fully expanded framework. Sodalite does not show this second stage below 920° C. The thermal expansion behaviour of other framework silicates is interpreted in analogy to that of the sodalite group. |
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