Relics of the Eoarchean Continental Crust of the Anabar Shield, Siberian Craton

In the northern part of the Anabar Shield, orthopyroxene plagiogneisses of the granulite Daldyn Group host lenses of mafic rocks surrounded by melanocratic rims. According to their chemical composition, the mafic rocks correspond to subalkaline gabbro, the plagiogneisses correspond to granodiorites contaminated with mafic material, and the rims are diorites. The orthopyroxene plagiogneisses of granodiorite composition have Sm-147/Nd-144 = 0.1097, epsilon(Nd)(T) = 1.6, T-Nd(DM) = 3.47 Ga and are metamorphosed anatectic granitoids with an age of 3.34 Ga. The mafic rocks have high Zr, Th, and Pb contents, are enriched in REE (sigma REE = 636 ppm), with a high degree of fractionation [(La/Yb)(N) = 17.73] and a well-defined Eu minimum (Eu/Eu* = 0.51), and have Sm-147/Nd-144 = 0.099, epsilon(Nd)(T) = 1.4 and T-Nd(DM) = 3.65 Ga. It is assumed that these rocks crystallized from melt derived from an enriched mantle (plume) source. Based on U-Pb (SHRIMP-II) dating of 50 zircon grains from the mafic rocks, a group of grains with concordant ages from 3567 to 1939 Ma was distinguished, along with a large number of discordant values. Multiple measurements in zircon grains with discordant age values make it possible to identify seven grains of Eoarchean age, with upper intercepts of the discordia corresponding to 3987 +/- 71 to 3599 +/- 33 Ma. The Lu-Hf systematics of 14 zircon grains is characterized by epsilon(Hf)(T) = +3.7 and by close values of T-Hf(DM) = 3.95 and = 3.93 Ga (3.99 Ga for the oldest zircon). The Paleoarchean (3.57 Ga) zircons are characterized by negative values of epsilon(Hf)(T) = -5.3 and -6.8, T-Hf(DM) = 3.92-3.98 Ga, and = 4.14-4.24 Ga, which indicate recycling of the preexisting Eoarchean and Hadean continental crust. The younger zircon (3287-2410 Ma) was also formed when the preexisting crust was recycled.