카나다 온타리오 밴크로프트의 맥도날도 페그마타이트 광산에서 산출된 Nb Sphene: 원소 치환에 관한 고찰

Niobian Sphene from the McDonald Pegmatite Mine, Bancroft, Ontarion, Canada: Consideration of Substitutions

  • ;
  • Donald R. Peacor (Department of Geological Sciences, The University of Michigan)
  • 발행 : 1989.03.01

초록

Sphene from the McDonald pegmatite near Bancroft, Ontario, Canada was analyzed using EPMA. It contains 4.3 to 6.3 weight percent of Nb2O5 with an average formula Ca1.02(Ti0.62Al0.22Nb0.07Fe0.06Ta0.01)Si0.99(O4.85F0.16). Three types of subtitutions are possible; 1)2Ti4+=(Nb, Ta)5+ + (Al, Fe3+), 2) Ti + O = (Al, Fe3+) + (F, OH), and 3) 2Ti + O = Fe2+ + (Nb, Ta)5+ + (F, OH). T재 different schemes of substitutions for balancing the analysis are considered when the iron is either all ferric or all ferrous. Assuming stoichiometry fo Ca and Si, a general formula derived from the two different schemes is Ca(Ti0.64Al0.22Fe3+0.06-X {{{{Fe_{x}^{2+} }} Nb0.01)Sio4.80-XF0.16(OH)0.04+x.

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