The carbonatites of the Ufaley block are polygenous and polychro-nous. The age of the early ones (calcite composition) is 1100-1200 Ma (Riphean rifting). They have Y-specialization and high content of rare-earth metals. In early PZ (oceanic stage, 400-395 Ma) carbonatites formed in connection with ultrabasite-sienite complex, and they have calcite and calcite-dolomite composition and Ct-specialization. During collision process (375-240 Ma) carbonatites were plastically deformed and recrystallized with forming of polygonal structures of carbonate grains. At last, during later collision stage with xenotime (calcite-dolomite composition) formated in composition of metasomatic zonation, which appeared as a result of formation of «egustinskiy» type of quartz veines.