TIMING AND SEQUENCE OF ENDOGENOUS EVENTS IN THE BUG GRANULITE-GNEISS DOMAIN OF THE UKRAINIAN SHIELD BASED ON THE STUDY OF A COMPOSITE TECTONO-MAGMATIC BRECCIA

In the Bug gneiss-granulite region of the Ukrainian shield, a composite tectono-magmatic breccia including enderbites and various mafic rocks was studied in the gneiss-enderbite complex. Based on the assessment of the thermodynamic conditions of rock and mineral formation, and the analysis of the U—Pb and Lu—Hf isotope systems of zircon, the history of endogenous development of the gneiss-enderbite complex is deciphered. The predominant rocks are enderbites with numerous inclusions of two-pyroxene and pyroxene-amphibole crystalline schists that underwent deformation under conditions of granulite metamorphism. The most ancient zircons have a concordant U—Pb age of 3.6–3.7 Ga, which is close to the age of the protolith of the Bug enderbites. Zircons are characterized by a heterogeneous structure, negative ε(t) values from −1 to −38 and a variation in Hf/Hf isotope ratios from 0.28035 to 0.28095, which is consistent with their different ages and origins. Based on the age, geochemistry and isotope composition of zircon from composite breccia rocks, geological events from Archean to Proterozoic are distinguished: 1) 3.67–3.60 Ga, the stage of magmatic crystallization of early mineral associations. 2) 3.0–2.8 Ga, the stage of granulite metamorphism and partial melting (2.9 Ga) of gneiss-enderbites with the preservation of melt mineral phases in zircons, but a strong disturbance of its U—Pb isotope system. 3) 2.0–1.9 Ga, the stage of Proterozoic granulite metamorphism with the reorganization of cation and isotope systems of rock-forming and accessory minerals. The obtained data are consistent with the model of polychronic development of the continental crust of the Ukrainian Shield in the Paleo- and MesoArchean with its strong reworking in the Paleoproterozoic.