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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

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Publications (1/1 displayed)

  • 2010Qingheiite-(Fe2+), Na2Fe2+MgAl(PO 4)3, a new phosphate mineral from the Sebastião Cristino pegmatite, Minas Gerais, Brazil7citations

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Wouters, Johan
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Philippo, Simon
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Hatert, Frédéric
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2010

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  • Wouters, Johan
  • Philippo, Simon
  • Hatert, Frédéric
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article

Qingheiite-(Fe2+), Na2Fe2+MgAl(PO 4)3, a new phosphate mineral from the Sebastião Cristino pegmatite, Minas Gerais, Brazil

  • Wouters, Johan
  • Baijot, Maxime
  • Philippo, Simon
  • Hatert, Frédéric
Abstract

<p>Qingheiite-(Fe<sup>2+</sup>), ideally Na<sub>2</sub>Fe <sup>2+</sup>MgAl(PO<sub>4</sub>)<sub>3</sub>, is a new mineral species from the Sebastião Cristino pegmatite, Minas Gerais, Brazil. It occurs as rims around frondelite grains, included in a matrix of quartz and albite. Frondelite is locally replaced by jahnsite, cyrilovite and Fe-Mn oxides. Qingheiite-(Fe<sup>2+</sup>) is transparent and exhibits a dark green colour, with a resinous lustre and with a pale to bottle green streak. It is non-fluorescent, brittle, and shows a perfect {010} cleavage. The estimated Mohs hardness is 4. The measured density is 3.6(2) g/cm<sup>3</sup>; the calculated density is 3.54 g/cm<sup>3</sup>. Qingheiite-(Fe<sup>2+</sup>) is biaxial negative, with α = 1.692(5), β; = 1.718(3), and γ= 1.720(5) (with A = 590 nm). Pleochroism is from pale pinkish brown (X) to pale green (Y) and pale bluish grey (Z). The calculated 2V angle is 31°, and a strong dispersion r &gt; v has been observed. The β index is parallel to the b crystallographic axis; α and γ lie in the (010) plane. Electron microprobe analyses gave P<sub>2</sub>O<sub>5</sub> 46.51, Al<sub>2</sub>O <sub>3</sub> 6.94, Fe<sub>2</sub>O<sub>3</sub> 10.58, FeO 11.46, MgO 6.32, MnO 11.23, CaO 0.24, Na<sub>2</sub>O 6.27, K<sub>2</sub>O 0.01, total 99.56 wt. %. The resulting empirical formula, calculated on the basis of 3 P, is (□<sub>0.65</sub>Na<sub>0.35</sub>)<sub>Σ1.00</sub>(Na <sub>0.58</sub>Mn<sup>2+</sup> <sub>0.40</sub>Cao.o2)z;i.oo (Fe<sup>2+</sup> <sub>0.68</sub>Mn<sup>2+</sup> <sub>0.32</sub>)<sub>Σ1.00</sub> (Mg <sub>0.72</sub>Fe<sup>3+</sup> <sub>0.23</sub>Fe<sup>2+</sup> <sub>0.05</sub>) <sub>Σ1.00</sub>(Al<sub>0.62</sub>Fe<sup>3+</sup> <sub>0.38</sub>) Σ<sub>1.00</sub>[PO<sub>4</sub>]3. The single-crystal unit-cell parameters are a = 11.910(2), b = 12.383(3), c = 6.372(1) Å, β = 114.43(3)°, and V= 855.6(3) Å<sup>3</sup>, space group P2 <sub>1</sub>/n. The eight strongest lines in the powder X-ray diffraction pattern [d(in Å)(I)(hkl)] are: 3.468(35)(310), 3.047(100)(112), 2.849(80)(312), 2.810(35)(222), 2.711(40)(330), 2.688(90)(240), 2.500(40)(132; 112), 2.074(30)(313). Qingheiite-(Fe<sup>2+</sup>) is the Fe<sup>2+</sup> analogue of qingheiite, and belongs to the wyllieite group of minerals. The crystal structure has been refined, based on single-crystal X-ray diffraction data, to R<sub>1</sub> = 2.91%. The mineral species and name were approved by the Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association (CNMNC-IMA) under number 2009-076.</p>

Topics
  • density
  • impedance spectroscopy
  • mineral
  • dispersion
  • grain
  • hardness
  • powder X-ray diffraction
  • space group