Abstract:The main rare-metal structure of the region is the Kalba-Narym granitoid belt of the northwestern direction, formed in the Hercynian cycle in a post collisional (orogenic) geodynamic setting. The spatialgenetic relationship of the leading geological-industrial type of deposits of rare-metal pegmatites (Ta, Nb, Be, Li, Cs, Sn) with medium-coarse-grained biotite granites of the 1 st phase of the Kalba complex P1 is emphasized. The revealed laws of formation and spatial accommodation of deposits of rare metals in… Show more
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