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Investigation of former and new sections in the classic Riphean region of the Bashkirian Anticlinorium (BA) revealed that this Palaeozoic segment of the passive margin of the East European Platform (EEP), during its Proterozoic history was initially formed as an intracratonic aulacogen basin which developed as an inter-cratonic half-structure only after the Early Ordovician opening of the Uralian...