Abstract

Summary Considered theoretical and practical aspects of disposal of pyrite mineralization within Ural North. Disclosed leading geodynamic processes responsible for the formation of massive sulfide mineralization which are convergent and divergent conditions producing undifferentiated and differentiated (contrasting and continuous) volcanic formation. Compact in tabular form practiced ranking ore objects, the characteristic of near ore metasomatic rocks, ores on the main (Cu, Zn, Pb) elements including noble (Au, Ag, Pt, Pd) metals. Developed regional (structural-tectonic, formational) and local (structural and morphological facial, petrophysical, petro-geochemical) paleovolcanic criteria for a positive predictive assessment pyrite family, within which four ore-formational type isolated (Cyprus, the Urals, orealtay, Filizchay) established their spatial position and age. The presence of two metallogenic epochs of massive sulfide formed on North Urals in relation to the total of the geodynamic evolution of the territory of several different from the Middle and South Urals

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