HANDBOOK ON THE PHYSICS AND CHEMISTRY OF RARE EARTHS

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HANDBOOK ON THE PHYSICS AND CHEMISTRY OF RARE EARTHS ( handbook-onphysics-and-chemistry-rare-earths )

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REE Mineralogy and Resources Chapter 279 237 TABLE 15 Representative Apatite-Group Minerals—Cont’d Endmember Formula Space Supergroup Mineral Name (Reduced) Group Type Fluorcalciobritholite (Ca,REE)5(SiO4,PO4)3F P63/m Britholite Chlorellestadite Ca5(SiO4,SO3)3Cl P63 or Ellestadite P63/m Fluorellestadite Ca5(SiO4,SO3)3 F P63/m Ellestadite Hydroxylellestadite Ca5(SiO4,SO3)3(OH) P21/m Ellestadite Mattheddleite Pb5(SiO4,SO4)3Cl P63/m Ellestadite Borosilicate Melanocerite-(Ce) Ce5(Si,B)3O12(OH,F)  nH2O ? Britholite Tritomite-(Ce) Ce5(Si,B)3(O,OH,F)13 P63/m Britholite Tritomite-(Y) Y5(Si,B)3(O,OH,F)13 P63/m Britholite Sulfate Aiolosite Na2(Na2Bi)(SO4)3Cl P63/m Hedyphane Cesanite (Na,Ca)5(SO4)3(OH) P63/m Hedyphane Caracolite (Na,Pb)5(SO4)3Cl P21/m Hedyphane Vanadate Vanadinite Pb5(VO4)3Cl P63/m Apatite After Pan, Y., Fleet, M.E., 2002. Compositions of the Apatite-group minerals: substitution mechanisms and controlling factors. In: Kohn, M.J., Rakovan, J., Hughes, J.M. (Eds.), Phosphates— Geochemical, Geobiological, and Materials Importance, Reviews in Mineralogy and Geochemistry, vol. 48, 13–49; Pekov, I.V., Zubkova, N.V., Husdal, T.A., Kononkova, N.N., Aqakhanov, A.A., Zadov, A.E., Pushcharovsky, D.Y., 2012. Carlgesecieite-(Nd), NaNdCa3(PO4)3F, a new belovite- group mineral species from the Il ́ımaussaq alkaline complex, south Greenland. Can. Mineral. 50, 571–580; Hughes, J.M., Rakovan, J.F., 2015. Structurally robust, chemically diverse: apatite and apatite supergroup minerals. Elements 11, 165–170. compounds with apatite structure have been reported (Pan and Fleet, 2002). According to the differences in formation environment of the natural apatite-group minerals, various chemical substitutions occur among them to yield varieties of the chemical compositions in apatite-group minerals. Hence it is fundamentally important to understand the substitution mechanisms and other factors, both intrinsic and extrinsic, that control the compositional varia- tions in the apatite (Pan and Fleet, 2002). Based on which anion, ie, fluorine, OH, or chlorine is dominant on the halogen site, apatite is, respectively, divided into fluorapatite, hydroxyapatite,

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