Abstract
The Paleoproterozoic igneous complexes of the western part of the Volga-Don orogen are considered. The Don terrane developed as a volcanic arc on the continental crust, while the Losevо terrane developed on the oceanic one. This is evidenced by granitoids with different geochemical and isotope-geochemical characteristics, they were formed by postcollisoin extension of the orogen crust.
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