Authors:
Authors’ team
Reviewers:
O.M. Ponomarenko
M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of NAS of Ukraine, Kyiv
https://orcid.org/0000-0002-5179-6091
R.I. Kutas
S. Subbotin Institute of geophysics National Academy of Sciences of Ukraine, Kyiv
https://orcid.org/0000-0002-3505-0599
L.M. Shymkiv
State enterprise “Ukrainian Geological Company”
Affiliation:
Project: Scientific book
Year: 2024
Publisher: PH "Naukova Dumka"
Pages:
DOI:
https://doi.org/10.15407/978-966-00-1959-1
ISBN: 978-966-00-1959-1
Language: Ukrainian
How to Cite:
Abstract:
New ideas about the formation of the structure of the crystalline basement of the views on the genetic features of certain types of ore deposits are presented. The general metallogenic features of the Bug mining area are determined by the Eoarchean history of its formation and the processes of early Proterozoic transformation. It is shown that the structural and textural paragenesis of the rocks of the district was formed about 2.0 ± 0.3 billion years ago, although the age of formation of the Middle Bug granulite complex, judging by the U-Pb age of individual zircon grains, is Paleo- or even Eoarchean. These parageneses reflect mainly horizontal compression or extension of the Earth’s crust. The mechanism of their formation is not related to the Archean sequential rhythmic layering of volcanics and sediments and their subsequent metamorphism with preservation of the relative position of the strata in the section, as some researchers believe, but with the transformation of tangential compression forces into simple and pure shear deformations. The latter lead to the movement of matter at the atomic and molecular level (with mineral transformation of rocks) and rock masses at the regional level. This results in the formation of new parageneses that overlap, but more often erase, the structural tissue of rocks from previous stages of deformation. On these principles, the structural and petrophysical map of the study area at a scale of 1:100,000 was constructed, which is presented in this monograph.
Keywords:
Ukrainian Shield, Middle Bug, Golovanivsk suture zone, Tarasivka structure zone, fault zones, Structural-petrophysical map
References:
Burakhovich, T. K., Ilyenko, V. A., Kushnir, A. M., & Shirkov, B. I. (2018). Three-dimensional deep geoelectric model of the Tarasivka structure of the Golovanivsk suture zone. Geofizicheskiy Zhurnal, 40(2), 108–122. (in Ukrainian). https://10.24028/gzh.0203-3100.v40i2.2018.128934
Burakhovich, T., Nikolaev, I., Sheremet, E., & Shirkov, B. (2015). Geoelectric anomalies of the Ukrainian shield and their relation to mineral deposits. Geofizicheskiy Zhurnal, 37(6), 42–63. https://doi.org/10.24028/gzh.0203-3100.v37i6.2015.111171
Burakhovych, T., Ganiev, O., & Shyrkov, B. (2023). Deep structure modeling of Golovanivsk suture zone on the basis of geoelectric data. Visnyk of Taras Shevchenko National University of Kyiv. Geology, 2(69), 39-45. https://doi.org/10.17721/1728-2713.69.06
Chulliat A., Alken P., Nair M. et al. The Enhanced Magnetic Model 2015—2020, National Centers for Environmental Information, NOAA. 2015. https://doi.org/10.7289/V56971HV
Entin, V. A., Gintov, O. B., Mychak, S. V., Belskyi, V. N., Geyko, Y. V., Polyachenko, E. B., Guskov, S. I., & Marchenko, A. V. (2019). «The Great» dyke of the Bug area. Geofizicheskiy Zhurnal, 41(4), 77–96. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v41i4.2019.177368
Entin, V., Gintov, O., Myschak, S., & Yushin, A. (2015). The structure of the Moldovan iron ore deposit (The Ukrainian shield) according to geological-geophysical data and its possible endogenous nature. Geofizicheskiy Zhurnal, 37(4), 3–18. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v37i4.2015.111118
Gintov, O. B. (2014). Scheme of periodization of faulting stages in the Earth’s crust of the Ukrainian shield – new data. Geofizicheskiy Zhurnal, 36(1), 3–18. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v36i1.2014.116145
Gintov, O. B., Entin, V. A., Mychak, S. V., Pavlyuk, V. N., & Guskov, S. I. (2018). Unique basite-metabasite structures of the Pobuzhsky ore mining region, their geological significance and ore-bearing prospects (by geophysical and geological data). Geofizicheskiy Zhurnal, 40(3), 3–26. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v40i3.2018.137170
Gintov, O. B., Entin, V. A., Mychak, S. V., Pavlyuk, 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. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v38i3.2016.107777
Gintov, O., & Mychak, S. V. (2014). Kinematics of formation of the Ukrainian Shield during the period 1,80-1,73 Ga ago according to the results of studies of rock fracturing of the Korosten and Korsun-Novomirgorod plutons. Geofizicheskiy Zhurnal, 36(4), 24–36. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v36i4.2014.116006
Gintov, O., Yentin, V., & Mychak, S. (2017). On plotting the scheme of fracture-mega-block tectonics of the Ukrainian Shield in a scale 1 : 500 000. Geofizicheskiy Zhurnal, 39(5), 63–82. (in Ukrainian). https://doi.org/10.24028/gzh.0203-3100.v39i5.2017.112340
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. (in Ukrainian). https://doi.org/10.24028/gzh.0203-3100.v42i3.2020.204699
Gintov, О. B., Orlyuk, M. I., Entin, V. A., Pashkevich, I., Mychak, S. V., Bakarzhieva, M. I., Shimkiv, L. M., & Marchenko, A. V. (2018). The structure of the Western and Central parts of the Ukrainian schield. Controversial issues. Geofizicheskiy Zhurnal, 40(6), 3–29. (in Ukrainian). https://doi.org/10.24028/gzh.0203-3100.v40i6.2018.151000
Kushnir, A. M., Burakhovych, T. K., Ilyenko, V. A., & Shyrkov, B. I. (2018). Geoelectric researches of the Tarasivka structure of the Golovanivsk suture zone. 17th International Conference on Geoinformatics – Theoretical and Applied Aspects, Kiev, Ukraine. Volume 2018, p. 1 – 5. https://doi.org/10.3997/2214-4609.201801779
Kushnir, A.M., Burakhovich, T.K., Ilyenko, V.A., Shyrkov, B.I. and Nikolayev, I.Y. (2019). Deep geoelectric studies of the Troyankiv and Tarasivka metabasite massifs of the Golovaniv suture zone. Geofizicheskiy Zhurnal. 41, 6, 56–72. (in Ukrainian). https://doi.org/10.24028/gzh.0203-3100.v41i6.2019.190066
Kyrylyuk, V. (2020). On some aspects of the study of age ratios of rock complexes of the Ukrainian Shield. Geofizicheskiy Zhurnal. 42, 2, 108–137. (in Ukrainian). https://doi.org/10.24028/gzh.0203-3100.v42i2.2020.201745
Kyrylyuk, V. P. (2017). The open letter to the members of the bureau of the national stratigraphic committee of Ukraine and all fellow Precambrian geologists. Geologìčnij Žurnal, 0(4), 88–99. (in Ukrainian). https://10.30836/igs.1025-6814.2017.4.122797
Mychak S.V. (2016). Geodynamic development of the Ukrainian shield and the formation of mineral deposits according to geophysical and geochronological studies: According to the materials of scientific report at the meeting of the Presidium of NAS of Ukraine March 2, Visnik Nacional Noi Academii Nauk Ukrai Ni, (6), 77–85. (in Ukrainian). https://doi.org/10.15407/visn2016.06.077
Mychak S.V., Cherkes S.I., Farfuliak L.V. et al. (2018). The ratio of defor-mation structures and magnetic textures of rocks Pobuzhsky ore mining district. 17th International Conference on Geoinformatics — Theoretical and Applied Aspects, 14—17 May 2018, Kiev, Ukraine. Volume 2018, p.1 – 5. https://doi.org/10.3997/2214-4609.201801851
Mychak, S. (2015). Kinematics of formation of the western and central parts of the Ukrainian shield between 2,02—2,05 Ga ago. Geofizicheskiy Zhurnal, 37(1), 83–99. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v37i1.2015.111327
Mychak, S., Kurylо S., & Murovskaya, A. (2023). Structural features of the Golovanevsk suture zone crystalline basement in the Yatran river basin based on tectonophysical data. Visnyk of Taras Shevchenko National University of Kyiv. Geology, 1(80), 23-32. (in Ukrainian). https://doi.org/10.17721/17282713.80.03
Mychak, S.V., Murovskaya, G.V., Polyachenko, E.B., & Belskyi, V.M. (2018). Stress-deformed state of the Earth crust of the Bug mining area in the section Gayvoron—Zavalye. Geofizicheskiy Zhurnal, 40(2), 95–107. (in Ukrainian). https://doi.org/10.24028/gzh.0203-3100.v40i2.2018.128933
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. (in Ukrainian). https://doi.org/10.24028/gzh.v43i4.239958
Nechaev, S.V., Gintov, O.B., & Mychak, S.V. (2019). On the relation between the rare-earth — rare-metal and gold ore mineralization and fault-block tectonics of the Ukrainian Shield. 1. Geofizicheskiy Zhurnal, 41(1), 3–32. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v41i1.2019.158861
Nechaev, S.V., Gintov, O.B., & Mychak, S.V. (2019). On the relation between the rare-earth — rare-metal and gold ore mineralization and fault-block tectonics of the Ukrainian Shield. 2. Geofizicheskiy Zhurnal, 41(2), 58–83. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v41i2.2019.164450
Orlyuk, M., Marchenko, A. V., & Romenets А. A. (2017). Spatial-temporeral changes in the geomagnetic field and seismisity. Geofizicheskiy Zhurnal, 39(6), 84–105. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v39i6.2017.116371
Orlyuk, M., Marchenko, A., & Romenets, A. (2023). Earth’s seismicity and secular changes of its magnetic field. Visnyk of Taras Shevchenko National University of Kyiv. Geology, 4(75), 50-54. (in Ukrainian). https://doi.org/10.17721/1728-2713.75.08
Orlyuk, M., Romenets, A., Marchenko, A., Orlyuk, I., & Ivashchenko, I. (2015). Magnetic declination of the territory of Ukraine: the results of observations and calculations. Geofizicheskiy Zhurnal, 37(2), 73–85. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v37i2.2015.111307
Pashkevich, I. K., Orlyuk, M. I., Marchenko, A. V., Romanets, A. A., Tsvetkova, T. A., & Bugayenko, I. V. (2020). On the possible mantle nature of the long-wave Central-European magnetic anomaly. Geofizicheskiy Zhurnal, 42(6), 100–130. (in Russian). https://10.24028/gzh.0203-3100.v42i6.2020.222288
Pavlyuk, V., Entin, V., Gintov, O., & Guskov, S. (2019). Prospects for the exploration of gold deposits in the Golovanevsk suture zone of the Ukrainian shield. Geofizicheskiy Zhurnal, 41(5), 87–104. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v41i5.2019.183632
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. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v40i5.2018.147474
Shevchuk, V., Kravchenko, D., Mazko, A., & Khabanets, I. (2013). Pervomayskaya granite-gneiss monocline in the section along river South Вug. Visnyk of Taras Shevchenko National University of Kyiv. Geology, 1(60), 5-8. (in Ukrainian). https://doi.org/10.17721/1728-2713.60.01
Shumlyanskyy L., Nosova A., Billström K. et al. The U—Pb zircon and baddeleyite ages of the Neoproterozoic Volyn Large Igne-ous Province: implication for the age of the magmatism and the nature of a crustal contaminant. GFF. 2016. Vol. 138, N 1. P. 17—30. https://doi.org/10.1080/11035897. 2015.1123289
Shyrkov, B., & Burakhovych, T. (2023). Electromagnetic methods for forecasting of mineral resources occurences. Visnyk of Taras Shevchenko National University of Kyiv. Geology, 4(79), 40-45. (in Ukrainian). https://doi.org/10.17721/17282713.79.06
Shyrkov, B., Burakhovich Т., & Kushnir, A. (2017). Three-dimensional geoelectric model of the Golovanevsk suture zones of the Ukrainian Shield. Geofizicheskiy Zhurnal, 39(1), 41–60. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v39i1.2017.94010
Starostenko V., Janik T., Lysynchuk D. et al. Mesozoic(?) lithosphere-scale buckling of the East European Craton in southern Ukraine: DOBRE-4 deep seismic profile. Geophysical Journal International. 2013b. Vol. 195, N 2. P. 740—766. https://doi.org/10.1093/gji/ggt292
Starostenko V., Janik T., Yegorova T. et al. Lithospheric structure along wide-angle seismic profile GEORIFT 2013 in Pripyat-Dnieper-Donets Basin (Belarus and Ukraine). Geophysical Journal International. 2018. Vol. 212. P. 1932—1962. https://doi.org/10.1093/gji/ggx509
Starostenko, V. I., Kuprienko, P. Y., Makarenko, I. B., Savchenko, A. S., & Legostaeva, O. V. (2018). Three-dimensional Earth’s crust density model of the central part of the Golovanevsk suture zone of the Ukrainian Shield. Geofizicheskiy Zhurnal, 40(3), 27–53. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v40i3.2018.137172
Starostenko, V. I., Kuprienko, P. Y., Makarenko, I. B., Savchenko, A. S., & Legostaeva, O. V. (2018). Three-dimensional Earth’s crust density model of the central part of the Golovanevsk suture zone of the Ukrainian Shield. Geofizicheskiy Zhurnal, 40(3), 27–53. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v40i3.2018.137172
Starostenko, V. I., Kuprienko, P. Y., Makarenko, I., Savchenko, A., & Legostaeva, O. (2015). Density heterogeneity of the Earth’s crust of the Ingul megablock of the Ukrainian Shield according to the data of three-dimensional gravity modeling. Geofizicheskiy Zhurnal, 37(3), 3–21. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v37i3.2015.111089
Starostenko, V. I., Kuprienko, P. Y., Makarenko, I., Savchenko, A., & Legostaeva, O. (2015). Density heterogeneity of the Earth’s crust of the Ingul megablock of the Ukrainian Shield according to the data of three-dimensional gravity modeling. Geofizicheskiy Zhurnal, 37(3), 3–21. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v37i3.2015.111089
Starostenko, V. I., Kuprienko, P. Y., Makarenko, I., Savchenko, A., & Legostaeva, O. (2017). Earth’s crust composition of the Ingul megablock of the Ukrainian Shield (types of crust) and patterns of location of ore mineral resources. Geofizicheskiy Zhurnal, 39(5), 27–46. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v39i5.2017.112338
Starostenko, V. I., Legostaeva, O., Makarenko, I., & Savchenko, A. (2015). Software system for automated data interpretation of potential fields (GMT-Auto). (in Russian). Geofizicheskiy Zhurnal, 37(1), 42–52. https://doi.org/10.24028/gzh.0203-3100.v37i1.2015.111322
Starostenko, V. I., Legostaeva, O., Makarenko, I., & Savchenko, A. (2015). Software system for automated data interpretation of potential fields (GMT-Auto). Geofizicheskiy Zhurnal, 37(1), 42–52. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v37i1.2015.111322
Starostenko, V. I., Sharypanov, V. M., Sharypanov, A. V., Savchenko, A. S., Legostayeva, O. V., Makarenko, I. B., & Kuprienko, P. Y. (2016). Interactive software package Isohypse for three-dimensional geological and geophysical models, and its practical use. Geofizicheskiy Zhurnal, 38(1), 30–42. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v38i1.2016.107720
Starostenko, V. I., Sharypanov, V. M., Sharypanov, A. V., Savchenko, A. S., Legostayeva, O. V., Makarenko, I. B., & Kuprienko, P. Y. (2016). Interactive software package Isohypse for three-dimensional geological and geophysical models, and its practical use. Geofizicheskiy Zhurnal, 38(1), 30–42. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v38i1.2016.107720
Stepaniuk, L. M., M.P. Dovbush, T. Y., Kurylo, S. Y., Lesnaya, Y. M., Petrychenko, K. V. (2016). The final stage of granitoid magmatism in the Dniester-Bug megablocks Ukrainian shield. Geochemistry and Ore Formation, 36, 72–81. (in Ukrainian). https://doi:10.15407/gof.2016.36.072
Stepanyuk, L. (2018). Problems of stratigraphy and geochronology of the Ukrainian shield. Mineralogical Journal, 40(1), 16–31. (in Ukrainian). https://doi:10.15407/mineraljournal.40.01.016
Stepanyuk, L. M., Kurylo, S. I., Dovbush, T. I., Ziultsle, O. V., Syomka, V. A. (2018). Uranine-lead age on the monacite of the crystal rocks of the lower plant r. Yatran (the Yatran unit of the Dnister-Bug megablok Ukrainian shield). Geochemistry and Ore Formation, 39, 24–35. (in Ukrainian). https://doi:10.15407/gof.2018.39.024
Trypolsky, O. A., Topoliuk, O. V., & Gintov, O. B. (2019). The structure of the Earth’s crust of the central part of the Holovanivsk suture zone according to the reinterpretation of materials of IV geotraverse of DSS (PK 295—400). Geofizicheskiy Zhurnal, 41(1), 172–179. https://doi.org/10.24028/gzh.0203-3100.v41i1.2019.158870
Usenko, O. (2015). Conditions of formation of ferruginous rocks of the Middle Bug area. Geofizicheskiy Zhurnal, 37(4), 32–50. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v37i4.2015.111122
Usenko, O. (2018). Geodynamic process and its geologic manifestations in the continents. Geofizicheskiy Zhurnal, 40(5), 137–171. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v40i5.2018.147477
Usenko, O. V. (2019). Reflection of sequence of geodynamic processes in geological structure of the Bug area. Geofizicheskiy Zhurnal, 41(3), 78–95. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v41i3.2019.172425
Usenko, O. V. (2019). To the problem of origin of the Bug series rocks. Geofizicheskiy Zhurnal, 41(4), 60–76. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v41i4.2019.177365
Yushin, A. (2015). On the prospects of identifying magmatogene-hydrothermal iron-ore deposits in the Ukrainian Shield. Geofizicheskiy Zhurnal, 37(4), 19–31. (in Russian). https://doi.org/10.24028/gzh.0203-3100.v37i4.2015.111121
