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Loparite-(Ce) from the Khibiny Alkaline Pluton,Kola Peninsula,Russia
Authors:N. G. Konopleva  G. Yu. Ivanyuk  Ya. A. Pakhomovsky  V. N. Yakovenchuk  Yu. A. Mikhailova
Affiliation:1.Nanomaterials Research Center, Kola Scientific Center,Russian Academy of Sciences,Apatity,Russia;2.Geological Institute, Kola Scientific Center,Russian Academy of Sciences,Apatity,Russia
Abstract:Data on the occurrence, morphology, anatomy, composition, and formation conditions of loparite-(Ce) in the Khibiny alkaline pluton are given. Loparite-(Ce), (Na,Ce,Sr)(Ce,Th)(Ti,Nb)2O6, resulted from metasomatic alteration and assimilation of metamorphic host rocks at the contact with foyaite as well as foyaite on the contact with foidolite. This alteration was the highest in pegmatite, and albitite developed there. A decrease in temperature resulted in enrichment of the perovskite and tausonite endmembers in loparite-(Ce) owing to a decrease in the loparite and lueshite endmembers. La and Ce sharply predominate among rare earth elements in the composition of loparite-(Ce).
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