Abstract
Complex study of the U–Pb and Lu–Hf systems of zircon from a lhertzolite lens of Archean gneiss enderbites of the Bug complex, Ukrainian Shield, showed that ultramafic magma was contaminated by the material of the country gneiss enderbites. The age of the zircons of 2.81 ± 0.05 Ga corresponds to the period of ultramafic magmatism within the Bug complex. Previously, this peak of endogenic activity was considered the stage of manifestation of metamorphism and magmatism of mafic composition.
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Original Russian Text © S.B. Lobach-Zhuchenko, Sh.K. Baltybaev, V.A. Glebovitsky, S.A. Sergeev, K.O. Lokhov, Yu.S. Egorova, V.V. Balagansky, S.G. Skublov, O.L. Galankina, L.M. Stepanyuk, 2017, published in Doklady Akademii Nauk, 2017, Vol. 477, No. 5, pp. 567–571.
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Lobach-Zhuchenko, S.B., Baltybaev, S.K., Glebovitsky, V.A. et al. U–Pb SHRIMP II age and origin of zircon from lhertzolite of the bug Paleoarchean complex, Ukrainian Shield. Dokl. Earth Sc. 477, 1391–1395 (2017). https://doi.org/10.1134/S1028334X17120157
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DOI: https://doi.org/10.1134/S1028334X17120157