The manifestation of a global mechanism of orogenesis in the Baikal rift zone (using the Tunkinsky rift as an example)

Using the Tunkinsky rift as an example, this paper examines the morphostructural and geomorphological aspects concerning the manifestation of the elements of the Gobi orogenesis mechanism that is responsible for the formation of inversion uplifts in the rift hollows, a process that complicates the recent intracontinental riftogenesis in the south of East Siberia.