+7 (812) 328 9282 - Office,  +7 (812) 328 9248 - Museum    info@karpinskyinstitute.ru
Russian Geological Research Institute (VSEGEI)
Regional Geology and Metallogeny
Journal Contents
2016
66

Title


N.I. GUSEV, V.E. RUDENKO, L.YU. SERGEEVA (VSEGEI), K.I. LOKHOV (SPb State University), N.G. BEREZHNAYA, A.N. LARIONOV (VSEGEI)

Archean granulites of Dzhelinda blok Anabar Shield (Siberian Сraton): geochemistry, age, isotopic characteristics

The paper presents data on petrographic and chemical composition of the rocks, U-­Pb age of zircon (SHRIMP II), Sm­-Nd isotopic system and zircon Lu­-Hf system from hypersthene plagiogneiss (enderbitoides) and crystalline schists of Daldyn and Verhneanabar series. Also studied ultramafic crystalline schists, charnokites and pegmatoid granitoids. Crystalline schists of Daldyn series contain own magmatic zircon with a concordant age of about 3.0 Ga, model age THf (DM) of 3.27–3.39 Ga and crust extraction age TCHf of 3.37–3.61 Ga. Plagiogneiss of Daldyn and Verhneanabar series is similar to rocks of TTG­series, but have high values of Eu/Eu* 1.33–1.99, and mg# 0.43–0.57. Plagiogneiss U-­Pb age is of about 2.86 Ga. Zircon is characterized by positive values εHf (T) from +7 to +7.9, the same model age THf (DM) and crust extraction age TCHf of 2.8–2.9 Ga.
Keywords: Anabar Shield, granulites, enderbitoides, zircon, U­-Pb age, Sm-­Nd, Lu-­Hf systematics.

Яндекс.Метрика