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To determine distributive provinces for the Late Paleozoic-Mesozoic sedimentary basins of South Verkhoyanye, U-Pb (LA-MC-ICPMS) isotope dating of 522 detrital zircon grains from five samples was made. It was established that during the late Paleozoic and Early Mesozoic there existed a major PaleoА.В. ПРОКОПЬЕВ, Х. ТОРО, Э.Л. МИЛЛЕР 6 ПРИРОДНЫЕ РЕСУРСЫ АРКТИКИ И СУБАРКТИКИ, Т. 26, No4, 2018 Aldan river system that formed after Middle Paleozoic rifting (following the Early Carboniferous) and was traceable within South Verkhoyanye from south to north toward the Verkhoyansk passive continental margin. The main distributive provinces for sedimentary basins were the Siberian craton basement (Aldan shield and Okhotsk terrane), volcanites of the East Asian active continental margin, Precambrian terrigenous rocks of South Verkhoyanye, Angara-Vitim batholith, and Cisbaikalian Caledonides. Paleogeographic reconstructions of northeast Asia for Late Carboniferous, Permian, Early Triassic, and Early Jurassic times were compiled.

Late Paleozoic-Mesozoic paleogeography of South-Verkhoyansk region from U-Pb dating of detrital zircons