Magmatic and postmagmatic mineral associations of the Malyutka massif rocks (Khudolazovkiy complex of the South Urals)

The results of detailed mineralogical studies of the Malyutka massif altered rocks of the Khudolazovskiy differentiated complex are presented. The morphology and chemical composition of many rock-forming and accessory minerals are described. According to the study, the magmatic and post-magmatic (hydrothermal-metasomatic) stages of rock formation are distinguished. The problems associated with the genetic interpretation of a number of rock-forming and ore minerals are discussed. The conclusion about the polygenic nature of the formation of spinelids is made. The equilibrium temperature in the «Ti-magnetite-ilmenite» system (633-650 °C), as well as the crystallization temperature of chlorite, replacing phlogopite and hornblende (145-185 °C), were estimated.