| Reference Type | Journal (article/letter/editorial) |
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| Title | Synthesis and study of diaboleïte |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Winchell, R. E. | Author |
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| Wenden, H. E. | Author |
| Year | 1968 (September) | Volume | 36 |
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| Issue | 283 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_36/36-283-933.pdf+ |
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| DOI | doi:10.1180/minmag.1968.283.036.03Search in ResearchGate |
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| Generate Citation Formats |
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| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 6184 | Long-form Identifier | mindat:1:5:6184:5 |
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| GUID | 0 |
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| Full Reference | Winchell, R. E., Wenden, H. E. (1968) Synthesis and study of diaboleïte. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (283) 933-939 doi:10.1180/minmag.1968.283.036.03 |
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| Plain Text | Winchell, R. E., Wenden, H. E. (1968) Synthesis and study of diaboleïte. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (283) 933-939 doi:10.1180/minmag.1968.283.036.03 |
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| In | (1966) Mineralogical Magazine Vol. 36 (283) Mineralogical Society |
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| Abstract/Notes | Diaboleïte has been synthesized between 25 and 100° C at atmospheric pressure and approximate water vapour partial pressures of 14·7 lb/in2. Under similar conditions at 170° C cumengéite appears to be the stable phase produced from a diaboleïte composition. Synthetic diaboleïte is much simpler morphologically than the natural mineral but the hemimorphic symmetry is more clearly demonstrated morphologically in the artificial specimens. A comparison of X-ray powder data for natural and synthetic diaboleïte shows almost exact detailed correspondence in line position and intensity between 0 and 180° 2θ. The cell dimensions obtained from X-ray powder data are a 5·869 ± 0·002 Å and c 5·495 ± 0·003 Å. |
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