Tectonic Evolution of the Tuvinian Trough (Northern Part of Central Asian Orogenic Belt): Synthesis of Geological Data and Results of Feldspar Ar‒Ar Dating

The Tuvinian rift trough, located in the northern part of the Central Asian orogenic belt (CAOB), arose in the Early Devonian on Late Proterozoic (?)‒Early Paleozoic terranes as a result of Altai–Sayan mantle plume activity. The sedimentary record from the Middle Paleozoic to the Middle Mesozoic, pr...

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