Paleoarchean orthopyroxenites of the Bug granulite–gneiss domain at the Ukrainian shield

S. B. Lobach-Zhuchenko; V. V. Balaganskii; M. Yu. Koreshkova; K. I. Lokhov; Sh. K. Baltybaev; L. M. Stepanyuk; Yu. S. Egorova; S. A. Sergeev; I. N. Kapitonov; O. L. Galankina; E. S. Bogomolov; N. G. Berezhnaya; V. V. Sukach

doi:10.1134/S1028334X17060216

Paleoarchean orthopyroxenites of the Bug granulite–gneiss domain at the Ukrainian shield

Autores: Lobach-Zhuchenko S.B.¹, Balaganskii V.V.², Koreshkova M.Y.³, Lokhov K.I.³^,4, Baltybaev S.K.¹, Stepanyuk L.M.⁵, Egorova Y.S.¹, Sergeev S.A.³^,4, Kapitonov I.N.³^,4, Galankina O.L.¹, Bogomolov E.S.¹^,4, Berezhnaya N.G.⁴, Sukach V.V.⁵
Afiliações:
1. Institute of Precambrian Geology and Geochronology
2. Geological Institute, Kola Science Center
3. St. Petersburg State University
4. Karpinsky All-Russian Geological Research Institute
5. Semenenko Institute of Geochemistry, Mineralogy, and Ore Formation
Edição: Volume 474, Nº 2 (2017)
Páginas: 700-705
Seção: Geochemistry
URL: https://ogarev-online.ru/1028-334X/article/view/190118
DOI: https://doi.org/10.1134/S1028334X17060216
ID: 190118

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This report presents data on the geological structure and location of the orthopyroxenite inclusion in gneissic enderbites of the Bug granulite–gneiss domain. Three stages of orthopyroxenite formation were identified on the basis of studies of the mineral composition along with the U–Pb and Lu–Hf isotope systems of zircons.