| Reference Type | Journal (article/letter/editorial) |
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| Title | Vochtenite, (Fe2+,Mg)Fe3+[UO2/PO4]4(OH)·12–13H2O, a new uranyl phosphate mineral from Wheal Basset, Redruth, Cornwall, England |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Zwaan, P. C. | Author |
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| Arps, C. E. S. | Author |
| de Grave, E. | Author |
| Zwaan, P. C. | Author |
| Arps, C. E. S. | Author |
| de Grave, E. | Author |
| Year | 1989 (September) | Volume | 53 |
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| Issue | 372 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_53/53-372-473.pdf+ |
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| DOI | doi:10.1180/minmag.1989.053.372.07Search in ResearchGate |
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| Generate Citation Formats |
| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 1532 | Long-form Identifier | mindat:1:5:1532:9 |
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| GUID | 0 |
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| Full Reference | Zwaan, P. C., Arps, C. E. S., Zwaan, P. C., Arps, C. E. S., de Grave, E. (1989) Vochtenite, (Fe2+,Mg)Fe3+[UO2/PO4]4(OH)·12–13H2O, a new uranyl phosphate mineral from Wheal Basset, Redruth, Cornwall, England. Mineralogical Magazine, 53 (372) 473-478 doi:10.1180/minmag.1989.053.372.07 |
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| Plain Text | Zwaan, P. C., Arps, C. E. S., Zwaan, P. C., Arps, C. E. S., de Grave, E. (1989) Vochtenite, (Fe2+,Mg)Fe3+[UO2/PO4]4(OH)·12–13H2O, a new uranyl phosphate mineral from Wheal Basset, Redruth, Cornwall, England. Mineralogical Magazine, 53 (372) 473-478 doi:10.1180/minmag.1989.053.372.07 |
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| In | (1989, September) Mineralogical Magazine Vol. 53 (372) Mineralogical Society |
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| Abstract/Notes | Vochtenite, a new mineral from the Basset Mine, southeast of Camborne in Cornwall, England, is a ferrous-ferric magnesium-bearing hydroxy uranyl phosphate mineral. It is monoclinic with a = 12.606, b = 19.990, c = 9.990 Å, β = 102.31° Z = 3; the ideal formula is:The strongest lines in the X-ray powder diffraction pattern are: 9.998(100)(020), 4.999(30)(040), 4.892(45)(002), 3.475(70)(311), 3.333(50)(060), 3.087(40)(232), and . Vochtenite is brown in colour with a bronzy lustre and is non-fluorescent. Mohs hardness is 2.5 and the density (calc.) = 3.663 g/cm3. There is a prominent (010) cleavage. Vochtenite is optical biaxial negative, 2V (calc.) = 89(3)° its dispersion is indiscernible. Refractive indices are α = 1.575(2), β = 1.589(2), γ = 1.603(2), and the pleochroism is very weak. Orientation X(α)∥b is perpendicular to (010) and Z(γ)∧c is small. The mineral occurs as subparallel (0.5–1.0 mm) crystal aggregates with a pseudo-quadratic outline. The mineral is named vochtenite after Prof. Dr. Ing. R. F. C. Vochten of the State University of Antwerpen, Belgium. |
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