PALEOZOIC GRANITOID MAGMATISM OF THE URALS: THE REFLECTION OF THE STAGES OF THE GEODYNAMIC AND GEOCHEMICAL EVOLUTION OF A COLLISIONAL OROGEN

The Ural mobile belt is an intracontinental epioceanic orogen that has already gone through all stages of the geodynamic development. Igneous rocks formed during each stage are important indicators for understanding evolution this and determining potential ore contents its segments. We consolidated large datasets on petrogeochemistry isotope geochronology Paleozoic (490–250 Ma) granitoids associated with opening paleoocean subsequent formation collisional orogen. Using these data, we have revised ages several tectono-magmatic events, clarified paleogeodynamic settings generation different compositions, described roles mantle-crust interactions plume factor in mature continental crust study area. results can be useful geological mapping improving assessment granitoid complexes differ origin composition.