Concerning the discussion about the Bug series of the Middle Bug (Ukrainian shield)
DOI:
https://doi.org/10.24028/gj.v45i2.278337Keywords:
Ukrainian Shield, Bug area granulite complex, series, formations, folding, dynamometamorphism, rearrangementAbstract
The materials of several articles and reports published in 2022 by the authors of this work and V.P. Kirilyuk (Kirilyuk, 2022 a,b), who discussed the structure and stratigraphy of the Вug area granulite complex of the Ukrainian Shield. The authors, relying on their geological, geophysical and geochemical studies, isotopic geochronology data, as well as on the world experience in studying the Early Precambrian complexes of the Canadian and Australian shields, argue that during 3.8—1.7 Ga, the Bug area granulite complex underwent at least a threefold structural metamorphic processing. Its modern structural plan, as well as, to a large extent, the composition and structural and textural features of metamorphic rocks, are of Early Proterozoic age. Therefore, its division into suites of primary sedimentary-volcanogenic rocks and their vertical distribution by age does not make sense. Only a division into two series is possible — the Dniester-Bug and the Bug, between which there is a tectonic contact. Contrary to this, V.P. Kirilyuk, relying on the experience of his stratigenic-metamorphogenic studies and the authority of the well-known school of L.I. Salopa, E.M. Lazko et al., defends the point of view on the stratigenic nature of the Bug area granulite complex, in which the primacy and stability of the position of strata-formations relative to each other were preserved throughout the entire time. According to V.P. Kirilyuk, there are no breaks and disagreements between the suites, so he proposes to abandon the identification of the early Precambrian USh Bug Group. And the seven suites identified by him, the youngest of which is 3.8 billion years old, are proposed to be attributed to a single Dniester-Bug series. The authors of both alternative points of view apply to the National Stratigraphic Committee of Ukraine with a proposal to revise the stratigraphic scheme of the Early Precambrian of the USh.
References
Bobrov, A.B., Kirilyuk, V.P., Goshovsky, S.V., Stepanyuk, L.M., Gursky, D.S., Lysak, A.M., Sivoronov, A.A., Bezvinny, V.P., Zultsle, V.V., Prikhodko, V.L., & Shpilchak, V.A. (2010). Granulite structural-formational complexes of the Ukrainian shield — European standard. Guide of geological excursions of the International scientific-practical conference «Stratigraphy, geochronology and correlation of the Lower Precambrian rock complexes of the basement of the East European platform», May 31— June 4, 2010. Kyiv, 160 p. (in Russian).
Gintov, O.B. (2005). Field tectonophysics and its applications in the study of deformations of the Earth’s crust of Ukraine. Kyiv: Feniks, 572 p. (in Russian).
Gintov, O.B. (2022). What happened to the Early Precambrian granulite complexes of the Bug region (Ukrainian shield) and the Limpopo belt (South Africa) and how to stratify them? A tectonist’s view. Geofizicheskiy Zhurnal, 44(1), 55—82. https://doi.org/10.24028/gzh.v44i1.253711 (in Ukrainian).
Gintov, O.B., Entin, V.A., Mychak, S.V., Pav¬lyuk, V.N., & Zyultsle, V.V. (2016). Structural-petrophysical and tectonophysical base of geological map of crystalline basement of the central part of Golovanevsk suture zone of the Ukrainian Shield. Geofizicheskiy Zhurnal, 38(3), 3—28. https://doi.org/10.24028/gzh.0203-3100.v38i3.2016.107777 (in Russian).
Gintov, О.B., Entin, V.A., Mychak, S.V., & Farfuliak, L.V. (2020). The Bug mining area of the Ukrainian shield. Structural-petrophysical map of the crystalline basement and some problems of the Early Precambrian geology. Geofizicheskiy Zhurnal, 42(3), 16—46. https://doi.org/10.24028/gzh.0203-3100.v42i3.2020.204699 (in Ukrainian).
Gintov, O.B., Mychak, S.V., & Usenko, O.V. (2022). Regarding ideas about the Bug granulite complex, developed within the Gayvoron-Zavally adistrict. Geological structure and minerals of Ukraine. Collection of theses of the All-Ukrainian scientific conference (Kyiv, October 12—13, 2022). Kyiv: Institute of Geochemistry, Mineralogy and Ore Formation named after M.P. Semenenko of the National Academy of Sciences of Ukraine, 397 p. (in Ukrainian).
Gintov, O.B., & Usenko, O.V. (2022). Peculiarities of the present structure of the Bug granulite complex developed within the Middle Bug area and its partitioning into series and suits. Geofizicheskiy Zhurnal, 44(4), 3—37. https://doi.org/10.24028/gj.v44i4.264839 (in Ukrainian).
Gintov, O.B., & Shevchuk, V.V. (2017). Structuring of the Ukrainian shield and the peculiarities of the Early Precambrian fracture formation on the example of the Golovanivsk suture zone. Kyiv: NVP Interservice, 162 p. (in Ukrainian).
State geological map of Ukraine. Scale 1:200,000. Geological and mineral map of the crystalline basement. Central Ukrainian series. Sheet M-36-XXXI (Pervomaysk). (2004). Kyiv: Publ. of the Ministry of Ecology and Natural Resources of Ukraine, State Geological Service (in Ukrainian).
Dobretsov, N.L. (1981). Principles of identification and classification of metamorphic formations and tasks of formation studies. In Metamorphic formations (principles of selection and classification) (pp. 6—36). Novosibirsk: Nauka (in Russian).
Report on the research work on the topic «Geological structure of the Bug mining district according to modern geophysical and geological data and assessment of its prospects for mineral resources (final)». (2020). Head of the theme is O.B. Gintov. Kyiv: Publ. of the S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, 519 p. (in Ukrainian).
Kyrylyuk, V.P. (2005). The main results of morpho-paragenetic geological formation al investigations dating back to the Lower Precambrian. Visnyk LNU. Ser. heol, (19), 52—74 (in Ukrainian).
Kirilyuk, V.P. (2020). On some aspects of the study of age ratios of rock complexes of the Ukrainian Shield. Geofizicheskiy Zhurnal, 42(2), 108—137. https://doi.org/10.24028/gzh.0203-3100.v42i2.2020.201745 (in Russian).
Kirilyuk, V.P. (2013). Peculiarities of stratigraphic studies of the Lower Precambrian. Article 2. The role of geological formation al investigations in the study of the stratigraphy of the Lower Precambrian. Heolohichnyi Zhurnal, (4), 102—114 (in Russian).
Kyrylyuk, V.P. (2022a). About the so-called «Bug series» of the Middle Bug region (Ukrainian shield). Article 1. The evolution of views and the composition of the «Bug series». Geofizicheskiy Zhurnal, 44(4), 155—170. https://doi.org/10.24028/gj.v44i4.264846 (in Ukrainian).
Kyrylyuk, V.P. (2022б). About the so-called «Bug series» of the Middle Bug region (Ukrainian shield). Article 2. Structural position of suites and strata of the «Bug series». Geofizicheskiy Zhurnal, 44(5), 151—170. https://doi.org/ 10.24028/gj.v44i5.272337 (in Ukrainian).
Kislyuk, V.V., Zyulzle, V.V., & Nikitash, L.P. (2011). Geological structure and mineral soft he watershed of the Southern Bug and Dniester rivers. Report on GDP-200 territory of sheet M-35-XXXVI (Gaivoron). Kyiv: Geolfunds, 460 p. (in Ukrainian).
Kostyuchenko, V.S., Zyulzle, V.V., & Vykhodtsev, N.K. (1990). Geological structure and mineral resources of Middle Bug. Report of GSO-37 of 1:200,000 scale GGK of sheet M-36-XXXI for 1984—1990. Kyiv, 341 p. (in Russian).
Kropotkin, P.N. (1973). Tectonic stresses in the earth’s crust according to direct measurements. In Stress state of the Earth’s crust (pp. 21—31). Moscow: Nauka (in Russian).
Lobach-Zhuchenko, S.B., Balagansky, V.V., Baltybaev, Sh.K., Stepanyuk, L.M., Ponomarenko, A.N., Lokhov, K.I., Koreshkova, M.Yu., Yurchenko, A.V., Egorova, Yu.S., Sukach, V.V., Berezhnaya, N.G., & Bogomolov, E.S. (2013). Stages of formation of the Bug granulitic complex according to the data of isotopic-geochronological investigations (Middle Bug region, Ukrainian shield). Mineralogical Journal, 36(2), 86—98 (in Russian).
Мychak, S., Bakarzhieva, М., Marchenko, A., Reshetnyk, M., Farfuliak, L., Оrlyuk, M., & Gintov, О. (2021). Gaivoron-Zavallia section of the Middle Pobuzhzhіa is the most representative part of the granulite complex of the Ukrainian Shield (structural-tectonophysical results and magnetometric studies). Geofizicheskiy Zhurnal, 43(4), 42—75. https://doi.org/10.24028/gzh.v43i4.239958 (in Ukrainian).
Nechaev, S.V., Voynovsky, A.S., Isakov, L.V., Anishchenko, T.M., Kukshina, L.V., Churubrov, S.S., & Parfenova, A.Ya. (2005). Report on the research work «Compilation of a prognostic metallogenic map of rare metal mineralization of the Ukrainian shield on a scale of 1:500,000». Kyiv: Ukrgeoinform, 315 p. (in Ukrainian).
Ponomarenko, O., Gintov, O., & Stepanyuk, L. (2018). On the so-called «leukogranulite formation» and «greenlevada suite» of Early Precambrian of the Ukrainian Shield. Geofizicheskiy Zhurnal, 40(5), 47—70. https://doi.org/10.24028/gzh.0203-3100.v40i5.2018.147474 (in Russian).
Ponomarenko, O.M., Lisna, I.M., & Gulko, V.V. (2022). The possible variant of formation of the oldest rocks of the tonalite-trondyemite-granodioritic series was considered. Proc. of the All-Ukrainian conf. «From mineralogy and geognosytogeochemistry, petrology, geology and geophysics: fundamental and applied trends of the 21st century» (MinGeoIntegration XXI), September 28—30, at the Institute of Geology of Taras Shevchenko Kyiv National University (pp. 59—63). Kyiv (in Ukrainian).
Popov, V.I. (1966). Experience of classification and description of geological formations: Classification of formations. Leningrad: Nedra, 208 p. (in Russian).
Stepanyuk, L.M., Shumlyansky, L.V., Ponomarenko, O.M., Dovbush, T.I., Vysotsky, O.B. (2010). To the question of the age limits of the formation of the Kosharo-Olexandrian suite of the bug series of the Bug area. Geochemistry and ore formation, (28), 4—10 (in Ukrainian).
Syomka, V.O., Bondarenko, S.M., Pavlyuk, V.M., & Kornienko, P.K. (2006). Gold-bearings karns of the Kapitaniv ore field (Dniester-Bug region of the Ukrainian Shield). Mineralogical Journal, 28(2), 94—97 (in Ukrainian).
Tectonic map of Ukraine. Scale 1:1000 000. Part I. Explanatory note. (2007). Kyiv: UkrDGRI, 97 p. (in Ukrainian).
Terkot, D., & Shubert, J. (1985). Geodynamics. Moscow: Mir, 730 p. (in Russian).
Usenko, O.V. (2021). Tonalite-trondjemite-gra¬no¬diorite formation of the Archaean. Special features of composition and conditions of for¬mation, Ukrainian Shield as an example. Geo¬¬fizicheskiy Zhurnal, 43(1), 38—68. https://doi.org/10.24028/gzh.0203-3100.v43i1.2021. 225541 (in Russian).
Shumlyansky, L.V. (2012a). Age and isotopic composition of hafnium of zircons from the quartzites of the Middle Bug region of the Ukrainian shield. Geochemistry and ore formation, (31-32), 136—142 (in Ukrainian).
Shumlyansky, L.V. (2012b). Geochemistry of pyroxene plagiogneisses (enderbites) of the Bug area and isotopic composition of hafnium in zircons. Mineralogical Journal, 34(2), 64—79 (in Ukrainian).
Shcherbakov, I.B. (1975). Petrography of the Precambrian rocks of the central part of the Ukrainian Shield. Kiev: Naukova Dumka, 280 p. (in Russian).
Shcherbakov, I.B. (2005). Petrology of the Ukrainian shield. Lviv: ZUGTS, 366 p. (in Russian).
Condie, K.C., Beyer, E., Belousova, E., Griffin, W.L. & O’Reilly, S.Y. (2005). U-Pb isotopic ages and Hf isotopic composition of single zir¬cons: the search for juvenile Precambrian con¬tinental crust. Precambrian Research, 139(1-2), 42—100. https://doi.org/10.1016/j.precamres. 2005.04.006.
Hamilton, W.B. (2007). Earth’s first two billion years — the era of internally mobile crust (pp. 233—296). Geol. Soc. of America, Memoir 200. https://doi.org/10.1130 /2007.1200(13).
Myers, J.S. (1990). Western gneiss terrane. In Geology and Mineral Resources of Western Australia (pp. 13—31). Western Australia Geological Survey.
Wilde, S.A., & Spaggiari, C. (2007). Chapter 3.6 The Narryer Terrane, Western Australia: A Review. Developments in Precambrian Geology, 15, 275—304. https://doi.org/10.1016/S0166-2635(07)15036-2.
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 2023 O.B. Gintov, S.V. Mychak, O.V. Usenko, O.E. Lazarenko
This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.
Authors who publish with this journal agree to the following terms:
1. Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.
2. Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.
3. Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access).
