In this work, mineralogy and evolution of granitic pegmatites of the Lipovsky vein field (ordinary and lithic quartz-feldspar as well as apogranite plagioclasites) are considered. The author has established 23 minerals, previously not described on this object. Formation of classical granite pegmatites Lipovka occurred in the Middle Permian times. The introduction of lithium-bearing pegmatites appears to have occurred at the Permian-Triassic boundary (257-250 Ma), incidentally, under the influence of heat flow, ordinary pegmatites lying in ultrabasites were desilicated to plagioclasites. The Middle Triassic ages in the Lipovsky pegmatites are most likely the consequence of the formation of the youngest pegmatites of the Aduisky massif.