Solubility of niobium in the system CaCO3–CaF2–NaNbO3 at 0.1 GPa pressure: implications for the crystallization of pyrochlore from carbonatite magma
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[1] R. Mitchell,et al. EXTREME COMPOSITIONAL VARIATION OF PYROCHLORE-GROUP MINERALS AT THE OKA CARBONATITE COMPLEX, QUEBEC: EVIDENCE OF MAGMA MIXING? , 2004 .
[2] R. Linnen,et al. A filler-rod technique for controlling redox conditions in cold-seal pressure vessels , 2003 .
[3] B. Kjarsgaard,et al. Solubility of niobium in the system CaCO3–Ca(OH)2–NaNbO3 at 0.1 GPa pressure , 2002 .
[4] R. Mitchell. Preliminary studies of the solubility and stability of perovskite group compounds in the synthetic carbonatite system calcite-portlandite , 1997 .
[5] J. Gittins,et al. Pyrochlore crystallization in carbonatites; the role of fluorine , 1993 .
[6] D. H. Watkinson. Experimental studies bearing on the origin of the alkalic rock-carbonatite complex and niobium mineralization at Oka, Quebec , 1970 .
[7] O. F. Tuttle,et al. The system CaF 2 -Ca(OH) 2 -CaCO 3 , 1964 .