РУДОНОСНОСТЬ ДУНИТ-ГАРЦБУРГИТОВОЙ И ЧЕРНОСЛАНЦЕВОЙ ФОРМАЦИЙ ПОГРАНИЧНОЙ ЗОНЫ МЕЖДУ ЮЖНЫМ И СРЕДНИМ УРАЛОМ

In the article chromite mineralization of the most large ultramafic massives of dunite-harzburgite formation is considered in a transitional area between the South and Middle Urals. It is shown, that all deposits of chromite ore were formed on the stage of high temperature evolution of mantle ultramafites and then exposed to metamorphism in the earth's crust conditions. Some ultramafic massives and black shale formation are perspective for finding out new gold bearing objects.