Distinguishing Postcollisional Subsolvus and Hypersolvus Granites on the Eastern Slope of the Southern Urals

摘要

Postcollisional granitoids on the eastern slope of the Southern Urals were distinguished in the 1980s as small intrusions finishing the Upper Paleozoic tec-tonomagmatic stage [1]. Currently they are distin?guished into subsolvus and hypersolvus. Consolida?tion of granite intrusions is geodynamically related to the stage of postcollisional tectonic activization of deep faults separating submeridionally elongated large structural—formational zones of the Aral folded area (Fig. 1).