U-Pb AGE OF ZIRCON FROM PARAGNEISSES IN GRANULITE TERRANE OF THE SHARYZHALGAI UPLIFT (southwest of the Siberian craton): EVIDENCE FOR THE ARCHEAN SEDIMENTATION AND EVOLUTION OF CONTINENTAL CRUST FROM EOARCHEAN TO MESOARCHEAN
O.M. Turkina1,2, S.A. Sergeev3,4, V.P. Sukhorukov1,2, N.V. Rodionov3
1V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia 2Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia 3Center of Isotopic Research, A.P. Karpinsky Russian Research Geological Institute, Srednii pr. 74, St. Petersburg, 199106, Russia 4Institute of Geosciences, Saint Petersburg State University, Universitetskaya nab. 7/9, St. Petersburg, 199034, Russia
Keywords: Paragneisses, detrital zircon, U-Pb age, SHRIMP, sedimentation, Archean, Sharyzhalgai uplift
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