The Pb isotopic ratios and μ (238U/204Pb) values across Urals VHMS deposits display increase from fore-arc to back-arc settings.
The Pb model ages decrease from fore-arc (~700Ma) to back arc (ca. 400Ma) settings.
The most radiogenic Pb isotopic composition is similar with the Urals MORBs derived from highly depleted metasomatized mantle.
The range of Pb isotopic ratios of volcanics matches the ores, with the exception of felsic volcanics being less radiogenic.
The unradiogenic source of lead may be represented by Neoproterozic oceanic crust, or/and old Archean continental crust.