Geological structural and petrological features of dykes and vein rocks of the Kamenushinsky massif (Middle Urals)

The Kamenushinsky Massif (the Middle Urals) of the dunite-clinopyroxenite-gabbro formation is one of the least studied massifs of the Platiniferous Belt of the Urals. This massif is characterized by the extensive distribution of dyke and vein bodies that are spatially tend to the fields of development of platinum mineralization. While, dyke and vein formations are poorly explored. The pecularities of the dyke bodies interrelations with dunites and clinopyroxenites that massif was composed of, as well as chromites that concentrate platinum mineralization could be used in studying of the geological evolution of the Kamenushinsky massif and its metallogeny. The obtained results are based on the data of microscopy and geological observations carried out during 2014-2017. For the first time complex characteristics of mineral-petrographic and geological-structural features of dyke and vein bodies of the Kamenushinsky massif are given.