"We have characterized ferroaxinite (up to 95 mol.% of end-member composition) from a contaminated granitic pegmatite cutting the magnetite-rich portion of an Fe-skarn body near Male\u0161ov, Czech Republic, by means of electron-microprobe analysis, single-crystal X-ray diffraction, infrared spectroscopy and temperature-dependent 57Fe M\u00F6ssbauer spectroscopy. The following crystal-chemical formula was obtained: VI[Ca2.00 Ca2.00 (Fe2+1.83Mn0.10Mg0.06)S1.99 (Al1.97Fe3+0.04)S2.01 Al2.00] IV[B2.00Si8.00] O30 OH2.00. The crystal structure was refined to R(F) = 0.0184 for 4667 observed reflections with Fo > 4s(Fo). We obtained the following unit-cell parameters: a 7.152(1), b 9.206(2), c 8.962(2) \u00C5, a 91.84(3), b 98.17(3), g 77.33(3)\u00B0, V 569.86(19) \u00C53. Relative to the other end-members of axinite group, the only significant differences of structural parameters occur at the Y site, where Fe2+ atoms predominate; the mean Y?O bond length is 2.229 \u00C5. The unusually long Fe?O(14) bond (2.704 \u00C5) o"@en . . . . . "The crystal structure of near-end-member ferroaxinite from an iron-contaminated pegmatite at Malesov, Czech Republic" . "RIV/61989592:15310/06:00003343!RIV10-MSM-15310___" . "1"^^ . "12"^^ . "Kolitsch, Uwe" . . "ferroaxinite; axinite group; elektron-microprobe analysis; structure refinement; (57)Fe M\u00F6ssbauer spectroscopy; granitic pegmatite; Malesov; Czech Republic"@en . . "Canadian Mineralogist" . . "0008-4476" . . . . . . . "15310" . . "RIV/61989592:15310/06:00003343" . "5" . "We have characterized ferroaxinite (up to 95 mol.% of end-member composition) from a contaminated granitic pegmatite cutting the magnetite-rich portion of an Fe-skarn body near Male\u0161ov, Czech Republic, by means of electron-microprobe analysis, single-crystal X-ray diffraction, infrared spectroscopy and temperature-dependent 57Fe M\u00F6ssbauer spectroscopy. The following crystal-chemical formula was obtained: VI[Ca2.00 Ca2.00 (Fe2+1.83Mn0.10Mg0.06)S1.99 (Al1.97Fe3+0.04)S2.01 Al2.00] IV[B2.00Si8.00] O30 OH2.00. The crystal structure was refined to R(F) = 0.0184 for 4667 observed reflections with Fo > 4s(Fo). We obtained the following unit-cell parameters: a 7.152(1), b 9.206(2), c 8.962(2) \u00C5, a 91.84(3), b 98.17(3), g 77.33(3)\u00B0, V 569.86(19) \u00C53. Relative to the other end-members of axinite group, the only significant differences of structural parameters occur at the Y site, where Fe2+ atoms predominate; the mean Y?O bond length is 2.229 \u00C5. The unusually long Fe?O(14) bond (2.704 \u00C5) o" . . . . "P(1M0512), Z(AV0Z20410507), Z(MSM6198959218)" . . "The crystal structure of near-end-member ferroaxinite from an iron-contaminated pegmatite at Malesov, Czech Republic"@en . . . . "Schneeweiss, Old\u0159ich" . "[006323E4F28C]" . . "44" . "CA - Kanada" . "Filip, Jan" . "470047" . "Nov\u00E1k, Milan" . "The crystal structure of near-end-member ferroaxinite from an iron-contaminated pegmatite at Malesov, Czech Republic"@en . "The crystal structure of near-end-member ferroaxinite from an iron-contaminated pegmatite at Malesov, Czech Republic" . . "4"^^ .