Age limits of high-grade metamorphic supracrustal complexes in the centralAldan Shield: Sm-Nd isotopic data

First investigation results on Sm-Nd isotope systems in elastic metasedimen tary and metavolcanic rocks from the high-grade metamorphic supracrustal co mplexes of central Aldan Shield are used to approximately evaluate their ma ximum age boundary. It is established that the Upper Archean rocks (model a ge T-Nd(DM) = 3.3-2.6 Ga) served as a principal source material for metapel ites of the Kurumkan Group; metapelites and metagraywackes of the Amedichi Group; and also for the metagraywackes of the Kurulta, Zverev, and Seim gro ups. Provenances with the Early Archean model age (TNd(DM)= 3.5 Ga) are fou nd to be appropriate only for few rock samples from the Kurumkan and Kurult a groups. The Early Proterozoic age (T-Nd(DM) = 2.5-2.2 Ga) is inferred for the protolith material of supracrustal rocks of the Chuga, Kholbolokh, Kyu rikan, Idzhek, and Fedorov groups. The data obtained suggest that supracrus tal rocks of the Aldan granulite-gneiss and East Olekma granite-greenstone terranes were formed not in the Early Archean, as it was formerly believed, but at the Late Archean and/or Early Proterozoic stages of geologic evolut ion of the shield.