Genetic types of mineral deposits of the formation of ultramafic-alkaline rocks and carbonatites of the Kola Peninsula
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- Leningrad Mining Institute
Abstract
Only 50 years ago in the world were known single massifs composed of the original complex of ultramafic-alkaline rocks and carbonatites. Now there are more than 200 of them, and it should be expected that their number in the coming decades will increase significantly. The search for and study of such massifs are increasingly expanding both in the USSR and abroad, mainly due to the discovery of large and sometimes unique deposits of tantalum-niobates, iron, apatite, phlogopite, etc.
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