Fluoro-sodic-ferropedrizite, NaLi2(Fe2+2Al2Li)Si8O22F2, a new mineral of amphibole group from Sutlug River, Tuva Republic, Russia: description and crystal structure. (Articolo in rivista)

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  • Fluoro-sodic-ferropedrizite, NaLi2(Fe2+2Al2Li)Si8O22F2, a new mineral of amphibole group from Sutlug River, Tuva Republic, Russia: description and crystal structure. (Articolo in rivista) (literal)
Anno
  • 2009-01-01T00:00:00+01:00 (literal)
Alternative label
  • Oberti R.; Boiocchi M.; Ball N.; Hawthorne F. (2009)
    Fluoro-sodic-ferropedrizite, NaLi2(Fe2+2Al2Li)Si8O22F2, a new mineral of amphibole group from Sutlug River, Tuva Republic, Russia: description and crystal structure.
    in Mineralogical magazine (Print)
    (literal)
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  • Oberti R.; Boiocchi M.; Ball N.; Hawthorne F. (literal)
Pagina inizio
  • 487 (literal)
Pagina fine
  • 494 (literal)
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  • 73 (literal)
Rivista
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  • In: Mineralogical Magazine, vol. 73 (3) pp. 487 - 494. Dr S.A.T. Redfern of the University of Cambridge, 2009. (literal)
Note
  • ISI Web of Science (WOS) (literal)
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  • CNR-IGG, Pavia, Centro Grandi Strumenti, Universita` di Pavia, Pavia, Italy., Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba, Canada. (literal)
Titolo
  • Fluoro-sodic-ferropedrizite, NaLi2(Fe2+2Al2Li)Si8O22F2, a new mineral of amphibole group from Sutlug River, Tuva Republic, Russia: description and crystal structure. (literal)
Abstract
  • Fluoro-sodic-ferropedrizite, ideally ANaBLi2C(Fe2+2 Al2Li)TSi8O22WF2, is a new mineral of the amphibole group from the Sutlug River, Tuva Republic, Russia. It occurs at the endogenic contact of a Li-pegmatite with country rocks near to a diabase dyke and formed by reaction of the pegmatitic melt with the country rock. Fluoro-sodic-ferropedrizite occurs as prismatic to acicular crystals, ranging in length from 0.1?3 cm and widths of up to 50 mm. Crystals occur inparallel to sub-parallel aggregates up to 5 mm across ina matrix of calcite and plagioclase feldspar. Crystals are pale bluish-grey with a greyish-white streak. Fluoro-sodic-ferropedrizite is brittle, has a Mohs hardness of ~6 and a splintery fracture; it is non-fluorescent with perfect {110} cleavage, no observable parting, and has a calculated density of 3.116 g cm?3. Inplan e-polarized light, it is pleochroic, X = pale purple-grey, Y = light grey, Z = colourless; X^ a = 71.2º (in b acute), Y || b, Z^c = 83.4º (in b obtuse). Fluoro-sodic-ferropedrizite is biaxial positive, a = 1.642(1), b = 1.644(1), g = 1.652(1); 2V(obs) = 68.0(3)º, 2V(calc) = 56.4º. Fluoro-sodic-ferropedrizite is monoclinic, space group C2/m, a = 9.3720(4) A ? , b = 17.6312(8) A ? , c = 5.2732(3) A ? , b = 102.247(4)º, V = 851.5(2) A ? 3, Z = 2. The strongest ten X-ray diffraction lines in the powder patternare (d inA? ,(I),(hkl)): 8.146,(10),(110); 2.686,(9),(151); 3.008,(8),(310); 4.430,(7),(021); 2.485,(6),(2¯ 02); 3.383,(4),(131); 2.876,(3),(1¯ 51, 3¯ 11); 2.199,(3),(3¯ 12); 4.030,(2),(111) and 3.795,(2),(1¯31). Analysis by a combination of electron microprobe and crystal-structure refinement gives SiO2 59.81, Al2O3 12.66, TiO2 0.09, FeO 10.32, MgO 5.56, MnO 0.73, ZnO 0.17, CaO 0.20, Na2O 2.81, Li2O 4.80, F 2.43, H2Ocalc 1.10, sum = 99.65 wt.%. The formula unit, calculated on the basis of 24(O,OH,F) is A(Na0.68)B(Li1.92Na0.05Ca0.03)C(Fe2+1.16Mg1.10Mn2+0.08Zn0.02Al1.97Ti0.01Li0.66) T(Si7.98Al0.02)O22W(F1.03OH0.97). Crystal-structure refinement shows Li to be completely ordered at the M(3) and M(4) sites. Fluoro-sodic-ferropedrizite, ideally ANaBLi2C(Fe2+2 Al2Li)TSi8O22WF2, is related to the theoretical end-member 'sodic-pedrizite', ANaBLi2C(Mg2Al2Li)TSi8O22W(OH)2, by the substitutions CFe2+ ? CMg and WF ? W(OH). (literal)
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