| Reference Type | Journal (article/letter/editorial) |
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| Title | A thermal study of thaumasite |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Font-Altaba, M. | Author |
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| Year | 1960 (September) | Volume | 32 |
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| Issue | 250 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_32/32-250-567.pdf+ |
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| DOI | doi:10.1180/minmag.1960.032.250.06 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5577 | Long-form Identifier | mindat:1:5:5577:6 |
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| GUID | 0 |
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| Full Reference | Font-Altaba, M. (1960) A thermal study of thaumasite. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (250) 567-572 doi:10.1180/minmag.1960.032.250.06 |
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| Plain Text | Font-Altaba, M. (1960) A thermal study of thaumasite. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (250) 567-572 doi:10.1180/minmag.1960.032.250.06 |
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| In | (1959) Mineralogical Magazine Vol. 32 (250) Mineralogical Society |
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| Abstract/Notes | SummaryA differential thermal analysis curve of thaumasite shows an endothermal peak at 206° C., correspinding to the loss of H2O and CO2, and a weak exothermal peak at 709° C., corresponding to recrystallization to a mixture of anhydrite and larnite, as is shown by X-ray powder photographs of material heated to 950° C. Improved powder data for thaumasite are given: the three strongest lines are at 9·66, 3·79, and 4·58 Å., and the cell-dimensions are a 10·992, c 10·311 Å. |
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These are possibly similar items as determined by title/reference text matching only.
