Canterford, J. H., Tsambourakis, G., Lambert, B. (1984) Some observations on the properties of dypingite, Mg5(CO3)4(OH)2·5H2O, and related minerals. Mineralogical Magazine, 48 (348) 437-442 doi:10.1180/minmag.1984.048.348.15

| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Some observations on the properties of dypingite, Mg5(CO3)4(OH)2·5H2O, and related minerals | ||
| Journal | Mineralogical Magazine | ISSN | 0026-461X |
| Authors | Canterford, J. H. | Author | |
| Tsambourakis, G. | Author | ||
| Lambert, B. | Author | ||
| Year | 1984 (September) | Volume | 48 |
| Issue | 348 | ||
| Publisher | Mineralogical Society | ||
| Download URL | https://rruff.info/doclib/MinMag/Volume_48/48-348-437.pdf+ | ||
| DOI | doi:10.1180/minmag.1984.048.348.15Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 3651 | Long-form Identifier | mindat:1:5:3651:5 |
| GUID | 0 | ||
| Full Reference | Canterford, J. H., Tsambourakis, G., Lambert, B. (1984) Some observations on the properties of dypingite, Mg5(CO3)4(OH)2·5H2O, and related minerals. Mineralogical Magazine, 48 (348) 437-442 doi:10.1180/minmag.1984.048.348.15 | ||
| Plain Text | Canterford, J. H., Tsambourakis, G., Lambert, B. (1984) Some observations on the properties of dypingite, Mg5(CO3)4(OH)2·5H2O, and related minerals. Mineralogical Magazine, 48 (348) 437-442 doi:10.1180/minmag.1984.048.348.15 | ||
| In | (1984, September) Mineralogical Magazine Vol. 48 (348) Mineralogical Society | ||
| Abstract/Notes | Abstract Dypingite, Mg5(CO3)4(OH)2·5H2O, was found in materials obtained during the production of high purity magnesia from crude magnesite by the calcination/CO2-leaching process. The snow-white, finely crystalline dypingite contained 41.0% MgO; the theoretical value is 41.5%. The X-ray powder data revealed a long period structure with a strong peak at 31.0 Å. The five strongest reflections (Å) and their estimated intensities (I/I 0) were 10.4 (100), 31.0 (40), 15.62 (40), 5.86 (30), and 6.34 (20). The DTA curve showed ten endothermic reactions with maxima at 43, 50, 77, 86, 105, 127, 180, 260, 420, and 514°C and an exothermic reaction at 495°C. | ||
Mineral Pages
| Mineral | Citation Details |
|---|---|
| Dypingite | |
| Giorgiosite |
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