Skip to main content
Log in

Florencite-(Sm)—(Sm,Nd)Al3(PO4)2(OH)6: A new mineral species of the alunite-jarosite group from the subpolar urals

  • New Minerals
  • Published:
Geology of Ore Deposits Aims and scope Submit manuscript

Abstract

Florencite-(Sm), a new mineral species of the florencite subgroup, was found in association with xenotime-(Y) in quartz veins of the Maldynyrd Range of the Subpolar Urals as thin zones within rhombohedral crystals of florencite-(Ce) with faceting by \(\{ 01\bar 11\} \) and \(\{ 10\bar 12\} \). The thickness of particular florencite-(Sm) zones is 0.01–0.1 mm, and the total thickness of a series of such zones is 1–3 mm. Florencite-(Sm) is colorless and pale pink or pale yellow with white streaks; its Mohs hardness is 5.5–6.0. Its measured and calculated densities are 3.70 and 3.743 g/cm3, respectively. The mineral is transparent, nonpleochroic, and uniaxial (positive), and ω = 1.704(2) and ɛ = 1.713(2). The electron beam’s fluorescence spectrum was 592 nm (intense green luminescence of Sm3+) and 558 nm (yellow luminescence of Nd3+). The chemical composition was as follows (microprobe, average of 2 WDS, wt %): 0.62 La2O3, 3.29 Ce2O3, 1.05 Pr2O3, 10.31 Nd2O3, 12.62 Sm2O3, 0.41 Eu2O3, 2.30 Gd2O3, 0.13 Dy2O3, 0.71 SrO, 0.35 CaO, 29.89 Al2O3, 26.14 P2O5, 0.85 SO3, 0.09 SiO2, 88.76 in total; 10.74 H2O (meas.). The empirical formula based on 14 oxygen atoms is (Sm0.38Nd0.32Gd0.07Ce0.10Pr0.03La0.02Eu0.01Sr0.04Ca0.03)1.0Al3.04(P1.91S0.05Si0.01)1.97O14H5.92. The idealized formula is (Sm,Nd)Al3(PO4)2(OH)6. Mineral is trigonal, space group R3m, a = 6.972(4), c = 16.182(7) Å, V = 681.2 Å3, Z = 3. The XRD pattern is as follows: dln (I) (hkl): 2.925 (10) (113), 1.881 (6) (303), 2.161 (5) (107), 5.65 (4) (101), and 3.479 (4) (110). The IR spectrum: 466, 510, 621, 1036, 1105, 1223, 2957, and 3374 cm−1.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Chukanov, N.V., Contribution of the IR Spectroscopy to the Characterization of New Mineral Species, in Abstracts of the 19th General Meeting of the IMA, Kobe, 2006, p. 19.

  • Florencite-(Nd). http://www.webmineral.com/dataFloren-site-(Nd).shtml

  • Labuntsov, A.N., The Crystals of Florencite, Tr. Miner. Muzeya AN SSSR, 1949, no. 2, pp. 135–136.

  • Mel’nikova, E.M., Kokarev, G.N., and Knyazeva, D.N., Florencite from Hydrothermal Metasomatic Rocks of the Subpolar Urals, Zap. Vsesoyuzn. Mineral. O-va, 1975, vol. 104, no. 3, pp. 341–343.

    Google Scholar 

  • Moralev, G.V., Borisov, A.V., Surenkov, S.V., Nagaeva, S.P., Tarbaev, M.B., Kuznetsov, S.K., Onishchenko, S.A., Efanova, L.I., and Soboleva, A.A., Distribution and Modes of Occurrence of REE at the Chudnoe and Nesterovskoe Au-Pd-REE Ore Occurrences in the Maldynyrd Range, the Subpolar Urals, Geokhimiya, 2005, vol. 43, no. 11, pp. 1175–1195 [Geochem. Int. (Engl. Transl.), 2005, vol. 43, no. 11, pp. 1078–1097].

    Google Scholar 

  • Plyusnina, I.I., Infrakrasnye spektry mineralov (Infrared Spectra of Minerals), Moscow: Moscow State Univ., 1977.

    Google Scholar 

  • Popov, V.A. and Kanonerov, A.A., Gems of Glimmerite of the Glinka Deposit, in: Ural Summer Mineralogical School-2000, Yekaterinburg, 2000, pp. 190–194.

  • Repina, S.A., Zoning and Sectoriality of the Florencite- and Xenotime-Group Minerals from Quartz Veins, the Subpolar Urals, Zap. Ross. Mineral. O-va, 2010, vol. 139, no. 1, pp. 19–39. [Geol. Ore Deposits (Engl. Transl.), 2010, vol. 52, spec. issue 8, Zapiski Russian Mineral. Soc., pp.821–836].

    Google Scholar 

  • Repina, S.A. and Yuzeva, N.S., Florencite in the Rocks of the Interformational Unconformity at the Subpolar Urals, in Ural Mineralogical Collection, Miass: Inst. Miner., 2005, vol. 13, pp. 91–113.

    Google Scholar 

  • Schwab, R.G., Gotz, C., Herold, H.., and de Oliveira, N.P., Compounds of the Crandallite Type: Synthesis and Properties of Pure Rare Earth Element-Phosphates, Neues Jahrb. Mineral., 1990, Hft. 6, S. 241–254.

  • Silaev, V.I., Filippov, V.N., and Sokerin, M.Yu., The Woodhouseite-Svanbergite-Florencite Solid Solutions in Hydrothermal Quartzite Zap. Vseross. Mineral. O-va 2001, vol. 130, no. 1, pp. 99–110.

    Google Scholar 

  • Somina, M.Ya. and Bulakh, A.G., Florencite from Carbonatites of East Sayan and Certain Problems of Chemical Constitution of Crandalite Group, Zap. Vsesoyuzn. Mineral. O-va, 1966, vol. 95, no. 5, pp. 537–550.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to S. A. Repina.

Additional information

Original Russian Text © S.A. Repina, V.I. Popova, E.I. Churin, E.V. Belogub, V.V. Khiller, 2010, published in Zapiski RMO (Proceedings of the Russian Mineralogical Society), 2010, No. 4, pp. 16–25.

A new mineral species florencite-(Sm) and its name were recommended by the Commission on New Minerals and Mineral Names of the Russian Mineralogical Society on September 9, 2009 and approved by the Commission on New Minerals, Nomenclature, and Classification of the International Mineralogical Association on November 30, 2009 (IMA no. 2009-074).

Rights and permissions

Reprints and permissions

About this article

Cite this article

Repina, S.A., Popova, V.I., Churin, E.I. et al. Florencite-(Sm)—(Sm,Nd)Al3(PO4)2(OH)6: A new mineral species of the alunite-jarosite group from the subpolar urals. Geol. Ore Deposits 53, 564–574 (2011). https://doi.org/10.1134/S1075701511070191

Download citation

  • Received:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1134/S1075701511070191

Keywords

Navigation