| Reference Type | Journal (article/letter/editorial) |
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| Title | The crystal structure of gersdorffite (III), a distorted and disordered pyrite structure |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Bayliss, P. | Author |
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| Stephenson, N. C. | 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_36/36-283-940.pdf+ |
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| DOI | doi:10.1180/minmag.1968.283.036.04Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6185 | Long-form Identifier | mindat:1:5:6185:2 |
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| GUID | 0 |
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| Full Reference | Bayliss, P., Stephenson, N. C. (1968) The crystal structure of gersdorffite (III), a distorted and disordered pyrite structure. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (283) 940-947 doi:10.1180/minmag.1968.283.036.04 |
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| Plain Text | Bayliss, P., Stephenson, N. C. (1968) The crystal structure of gersdorffite (III), a distorted and disordered pyrite structure. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (283) 940-947 doi:10.1180/minmag.1968.283.036.04 |
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| In | (1966) Mineralogical Magazine Vol. 36 (283) Mineralogical Society |
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| Abstract/Notes | SummaryThe crystal structure of gersdorffite (III) has been examined with three-dimensional Weissenberg X-ray diffraction data. The unit cell is isometric with a 5·6849 ± 0·0003 Å, space group PI, and four formula units per cell. This structure has the sulphur and arsenic atoms equally distributed over the non-metal atom sites of pyrite. All atoms show significant random displacements from the ideal pyrite positions to produce triclinic symmetry, which serves to distinguish this mineral from a disordered cubic gersdorffite (II) and a partially ordered cubic gersdorffite (I). Factors responsible for the atomic distortions are discussed. |
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