TY - JOUR
T1 - Abuite, CaAl2(PO4)2F2, a new mineral from the hinomaru-nago mine, Yamaguchi Prefecture, Japan
AU - Enju, Satomi
AU - Uehara, Seiichiro
PY - 2017
Y1 - 2017
N2 - Abuite was found in hydrothermally altered rocks in the Hinomaru-Nago mine, Kiyo area, Abu, Abu County, Yamaguchi Prefecture, Japan (34°53'N 131°52'E). Abuite is often included in aluminum phosphate rich samples, embedded with quartz and augelite and/or trolleite, and is often accompanied by other phosphates especially apatite and crandallite. Abuite is transparent and colorless with white streak and vitreous luster. It is very difficult to find them in bare eyes, since the dominant phases in aluminum phosphate rich samples, augelite, trolleite, and quartz, are all also transparent and colorless. The empirical formula of abuite (based on 10 anions pfu, O = 8, F + OH = 2) is (Ca0.99Sr0.01)1.00Al1.96P2.03O8(F1.89OH0.11). H2O was calculated by stoichiometry. The simplified formula is CaAl2(PO4)2F2. Abuite is the calcium analogue of SrAl2(PO4)2F2, which was synthesized by hydrothermal methods (Le Meins and Courbion, 1998). The crystal structure is orthorhombic, with space group P212121. Unit cell parameters refined from the obtained X-ray diffraction pattern are a = 11.818(2), b = 11.993(3), c = 4.6872(8) Å and V = 664.3(2) Å3, with Z = 4.
AB - Abuite was found in hydrothermally altered rocks in the Hinomaru-Nago mine, Kiyo area, Abu, Abu County, Yamaguchi Prefecture, Japan (34°53'N 131°52'E). Abuite is often included in aluminum phosphate rich samples, embedded with quartz and augelite and/or trolleite, and is often accompanied by other phosphates especially apatite and crandallite. Abuite is transparent and colorless with white streak and vitreous luster. It is very difficult to find them in bare eyes, since the dominant phases in aluminum phosphate rich samples, augelite, trolleite, and quartz, are all also transparent and colorless. The empirical formula of abuite (based on 10 anions pfu, O = 8, F + OH = 2) is (Ca0.99Sr0.01)1.00Al1.96P2.03O8(F1.89OH0.11). H2O was calculated by stoichiometry. The simplified formula is CaAl2(PO4)2F2. Abuite is the calcium analogue of SrAl2(PO4)2F2, which was synthesized by hydrothermal methods (Le Meins and Courbion, 1998). The crystal structure is orthorhombic, with space group P212121. Unit cell parameters refined from the obtained X-ray diffraction pattern are a = 11.818(2), b = 11.993(3), c = 4.6872(8) Å and V = 664.3(2) Å3, with Z = 4.
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U2 - 10.2465/jmps.170131
DO - 10.2465/jmps.170131
M3 - Article
AN - SCOPUS:85021750361
SN - 1345-6296
VL - 112
SP - 109
EP - 115
JO - Journal of Mineralogical and Petrological Sciences
JF - Journal of Mineralogical and Petrological Sciences
IS - 3
ER -