“…The reported data on the igneous complexes and related metallogeny of the region allow us to update the existing evolution models of the South Ural accretionary-collisional system. Unlike those models postulating predominant suprasubduction, collisional, and postcollisional magmatism [Tevelev, Kosheleva, 2002;Puchkov, 2003Puchkov, , 2010Tevelev et al, 2006;Fershtater et al, 2007;Fershtater, 2013], we additionally distinguish a setting of transform boundaries [Vladimirov et., 2020]. The transform boundary conditions left record in many similar structures of Asia: Early Cretaceous and Eocene geodynamic complexes in eastern Asia; Jurassic -Early Cretaceous complexes in the regions of Kolyma Loop, Mongolia-Okhotsk belt, and Transbaikalia; and Devonian to Permian complexes in the Altai region [Khanchuk et al, 1997[Khanchuk et al, , 2019Martynov et al, 2002;Simanenko et al, 2006;Vladimirov et al, 2020;Martynov, Khanchuk, 2013;Kruk, 2015].…”