L.M. Stepanyuk. THE U-Pb ZIRCON GEOCHRONOLOGY (LA-ICP-MS) OF GEOLOGICAL PROCESSES IN GRANULITES OF MIDDLE BOUH AREA. Article 2. Rock association in the Chausove open pits
https://doi.org/10.15407/mineraljournal.42.04.084
UDC 550.93
THE U-Pb ZIRCON GEOCHRONOLOGY (LA-ICP-MS) OF GEOLOGICAL PROCESSES IN GRANULITES OF MIDDLE BOUH AREA. Article 2. Rock association in the Chausove open pits
L.M. Stepanyuk, DrSc (Geology), Corresponding member of NAS of Ukraine,
Prof., Deputy director, M.P. Semenenko Institute of Geochemistry,
Mineralogy and Ore Formation of the NAS of Ukraine
34, Acad. Palladin Ave., Kyiv, Ukraine, 03142
E-mail: stepaniuk@nas.gov.ua; https://orcid.org/0000-0001-5591-5169
L.V. Shumlyanskyy, DrSc (Geology), Senior Research Fellow, Leading
Researcher. M.P. Semenenko Institute of Geochemistry,
Mineralogy and Ore Formation of the NAS of Ukraine
34, Acad. Palladin Ave., Kyiv, Ukraine, 03142
E-mail: lshumlyanskyy@yahoo.com; http://orcid.org/0000-0002-6775-4419
S.A. Wilde, Prof. Curtin University, School of Earth and Planetary Sciences
GPO Box U1987, Perth WA 6845 Australia
E-mail: s.wilde@curtin.edu.au; http://orcid.org/0000-0002-4546-8278
А.А. Nemchin, Prof. Curtin University, School of Earth and Planetary Sciences
GPO Box U1987, Perth WA 6845 Australia
E-mail: A.Nemchin@curtin.edu.au; http://orcid.org/0000-0002-3955-3409
O.V. Bilan, Head of the Oil and Gas Geology Training Laboratory
Kyiv Taras Shevchenko National University
Educational-scientific institute "Institute of Geology"
90, Vasylkivska Str., Kyiv, Ukraine, 03022
E-mail: olenka.bilan@gmail.com; https://orcid.org/0000-0003-0964-6003
Language: Ukrainian
Mineralogical journal 2020, 42 (4): 84-103
Abstract:
The LA-ICP-MS method was applied to investigate U-Pb and Lu-Hf isotope systematics of zircon crystals from charnockitoids that crop out in the open pits near Chausove village, Pervomaisk district. The association of enderbite gneisses, mafic and ultramafic (pyroxenite) granulites and vein bodies of pink biotite granites occur in the open pits. Enderbites are rather heterogeneous, and their composition varies from leucocratic quartzite-like rocks to enderbite-diorite. The Pervomaisk open pit is located within charnockite massif. Our data indicates that the association of enderbites and charnockites crystallised at 2850-2760 Ma from juvenile material (Hf isotope composition in zircons from enderbite-diorite is 176Hf/177Hf = 0.280915 ± 12, εHf2850 = +2; from leucocratic charnockite 176Hf/177Hf = 0.280875 ± 12, εHf2760 = –1; and from charnockite 176Hf/177Hf = 0.280875 ± 12, εHf2760 = –1). These rocks represented the newly formed Meso-Neoarchean crust, in contrast to the reworked older continental crust. This association has experienced a significant transformation in Paleoproterozoic. The last stage of transformation was accompanied by crystallisation of a new generation of zircon and formation of monazite at 2.04-2.06 Ga.
Keywords: Middle Bouh area, granulite association, charnockite, U-Pb isotope age, Lu-Hf isotope systematic.
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