| Reference Type | Journal (article/letter/editorial) |
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| Title | A thermal and X-ray investigation of scarbroite |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Duffin, W. J. | Author |
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| Goodyear, J. | Author |
| Year | 1960 (March) | Volume | 32 |
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| Issue | 248 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_32/32-248-353.pdf+ |
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| DOI | doi:10.1180/minmag.1960.032.248.01 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5547 | Long-form Identifier | mindat:1:5:5547:9 |
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| GUID | 0 |
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| Full Reference | Duffin, W. J., Goodyear, J. (1960) A thermal and X-ray investigation of scarbroite. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (248) 353-362 doi:10.1180/minmag.1960.032.248.01 |
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| Plain Text | Duffin, W. J., Goodyear, J. (1960) A thermal and X-ray investigation of scarbroite. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (248) 353-362 doi:10.1180/minmag.1960.032.248.01 |
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| In | (1959) Mineralogical Magazine Vol. 32 (248) Mineralogical Society |
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| Abstract/Notes | SummaryScarbroite, a fine-grained but compact deposit obtained from fissures in the sandstone on the north Yorkshire coast, is shown by chemical analysis to have an idealized formula Al2(CO3)3·12Al(OH)3. X-ray and electron diffraction data indicate a triclinic cell with a 9·94 Å., b 14·88 Å., c 26·47 Å., α 98·7°, β 96·5°, and γ 89·0°. A layer structure consisting of gibbsite-type sheets of Al(OH)3 and sheets of Al2(CO3)3 is proposed. The structure is stable from room temperature to about 125° C. |
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