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Wycheproofite: a new hydrated sodium aluminium zirconium phosphate from Wycheproof, Victoria, Australia, and a new occurrence of kosnarite

Published online by Cambridge University Press:  05 July 2018

William D. Birch
Affiliation:
Department of Mineralogy, Museum of Victoria, 328 Swanston Street, Melbourne, Victoria, 3000, Australia
Allan Pring
Affiliation:
Department of Mineralogy, South Australian Museum, North Terrace, Adelaide, South Australia, 5000, Australia
D. J. M. Bevan
Affiliation:
School of Physical Sciences, Flinders University, Bedford Park, South Australia, 5042, Australia
Kharisun
Affiliation:
School of Physical Sciences, Flinders University, Bedford Park, South Australia, 5042, Australia

Abstract

Wycheproofite is a new hydrated sodium aluminium zirconium phosphate from a pegmatite vein in granite at Wycheproof, in northwestern Victoria, Australia. The mineral occurs as compact, finely fibrous masses in small cavities in the quartz/feldspar/muscovite/schorl-bearing pegmatite. The fibrous crystals are between 5 and 10 µm wide and up to several mm long. Accompanying minerals include two other zirconium phosphates — kosnarite and a new species, selwynite, the K-analogue of gainesite — as well as wardite, eosphorite, cyrilovite, leucophosphitc, rockbridgeite, a kidwellite-like mineral and saleeite. The wycheproofite aggregates are pale pinkish to brownish orange, with a vitreous to pearly lustre. The streak is colourless, fracture rough, cleavage not observed and the Mohs hardness is between 4 and 5. Optical data are incomplete due to the fibrous nature of the mineral; the indices of refraction are in the range 1.62–1.64. The measured density is 2.83 g cm−3. Chemical analysis gave (wt.%) Na2O 6.36, K2O 0.44, CaO 0.66, FeO 0.36, MnO 0.21, Al2O3 12.03, Cs2O 0.03, ZrO2 32.43, HfO2 1.24, P2O5 35.85, SiO2 0.23, F 0.34, H2O 9.0, less 0=F 0.14, Total 99.04. The simplified formula is NaAlZr(PO4)2(OH)2·H2O. Wycheproofite is triclinic with unit cell parameters a=10.926(5) Å, b = 10.986(5) Å, c = 12.479(9) Å, α= 71.37(4)°, β = 77.39(4)°, γ= 87.54(3)° V = 1375.9 Å3. For Z= 6, the calculated density is 2.81 g cm-3. The strongest lines in the X-ray powder diffraction pattern are [dobs (Å), Iobs,hkl] 2.603 (100) 040; 4.128 (80) 121; 3.711 (65) 023; 3.465 (60) 030; 8.865 (40) 101; 3.243 (35) 132. The crystal structure has not been solved due to the finely fibrous nature of the material available. The name is for the locality, which in the local Australian Aboriginal language means ‘witchie bushes growing on a hilltop’.

Data on the third occurrence of kosnarite, KZr2(PO4)3, at Wycheproof are also given.

Type
Mineralogy
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1994

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References

Birch, W. D. (1993) Phosphate minerals in granitic rocks. In: Phosphate Minerals of Victoria, (Birch, W. D. and Henry, D. A., Eds.), 5-39, Mineralogical Society of Victoria, Special Publication No. 3.Google Scholar
Birch, W. D., Pring, A. and Foord, E. E. (1994) Can. Mineral (in press).Google Scholar
Brownfield, M. E., Foord, E. E., Sutley, S. J. and Botinelly, T. (1993) Kosnarite, KZr2(PO4)3, a new mineral from Mt Mica and Black Mountain, Oxford County, Maine. Amer. Mineral., 78, 653–6.Google Scholar
Foord, E. E., Brownfield, M. E., Lichte, F. E., Davis, A. M., and Sutley, S. J. (1994) Mccrillisite, NaCs(Be,Li)Zr2(PO4)4-l-2H2O, a new mineral from Mt Mica, Oxford County, ME, and new data for gainesite. Amer. Mineral, (in press).Google Scholar
Moore, P. B., Araki, T., Steele, I. M., Swihart, G. H. and Kampf, A. R. (1983) Gainesite, sodium zirconium beryllophosphate: a new mineral and its crystal structure. Amer. Mineral., 68, 1022–8.Google Scholar