Thermodynamic conditions of granitization and metamorphism of rocks in the northwestern part of the Ukrainian shield
DOI:
https://doi.org/10.24028/gj.v46i2.294984Keywords:
Proterozoic, Ukrainian shield, granitization, metamorphism, absolute age, conditions of metamorphismAbstract
The article examines the RT conditions of the formation of granites of the Sheremetyevo and Zhytomyr complexes and the metamorphism of rocks of the Teteriv series of the Volyn megablock of the Ukrainian Shield, the role of fluids in granitization. According to thermodynamic modeling, the appearance of granites is a link in the redistribution of heat and matter in the plume process. This proves the analysis of all known geological and petrological data. During the accumulation of the primary volcanogenic-sedimentary stratum, magmatic melts formed in the mantle’s melting centers located at different depths appeared many times. The formation of the melting layer in the crust is caused by conductive heating caused by its sublayering by ultrabasic melts. Temperatures of the melting point at a depth of 15 km exceed 650 °C. An increase in the gradient above it from 20 to 35 °C/km causes metamorphism, and the influx of melts and solutions through deformation zones ¾ metasomatic transformations and the formation of migmatites.
Where the upper part of the thermal asthenosphere is brought to the surface, you can see unmoved granites. At the intersection of several permeable zones (faults), granite massifs are formed, in which quartz-feldspar rocks crystallize. It is shown that the modern surface was on the border of metamorphosed rocks and the melting center in the Proterozoic time. Such a location does not contradict the existence of Archean rocks at greater depths — the level of thermal asthenosphere that produces granites.
References
Venidiktov, V.M. (1986). Polycyclic development of granulite facies. Kiev: Naukova Dumka, 268 p. (in Russian).
Antsiferov, A.V. (Ed.). (2009). Geological-geophysical model of the Nemyrov-Kocherov suture zone of the Ukrainian shield. Do-netsk: Weber, 235 p. (in Russian).
Gintov, O.B. (2019). Plate-plume tectonics as a single mechanism of geodynamic development of the tectonosphere of Ukraine and adjacent regions. Geofizicheskiy Zhurnal, 41(6), 3—34. https://doi.org/10.24028/gzh.0203-3100.v41i6.2019.190064 (in Russian).
Gintov, O.B., & Usenko, O.V. (2022). Peculiarities of the modern structure of the Pobuzh granulite complex, developed within the Middle Pobuzh region, and its division into series and worlds. Geofizicheskiy Zhurnal, 44(4), 3—37. https://doi.org/10.24028/gj.v44i4.264839 (in Ukrainian).
Gordyenko, V.V. (2007). The advection-polymorphic hypothesis of deep processes in the tectonosphere. Kiev: Korvin press, 170 p. (in Russian).
Yentin, V.A. (2005). Geophysical basis of the 1:1000000 scale Tectonic map of Ukraine. Geofizicheskiy Zhurnal, 27(1), 74—88 (in Ukrainian).
Kostenko, M.M. (2019). Metallogenic features and ore-bearing prospects of the basaltic dyke complexes of the Volynmegablock of the Ukrainian shield. Collection of scientific works of the UkrDGRI, (3-4), 9—23 (in Ukrainian).
Usenko, I.S. (Ed.). (1982). Metamorphism of the Ukrainian shield. Kiev: Naukova Dumka, 308 p. (inRussian).
Perchuk, L.L. (1997). Deep fluid flows and the birth of granite. Sorosovsky Educational Journal, (6), 56—63 (in Russian).
Ponomarenko, A.N., Lesnaya, I.M., Zyulzle, O.V., Gatsenko, V.A., Dovbush, T.I., Kanunikova, L.I., & Shumlyansky, L.V. (2010). Neoarchean of the Rosinsko-Tikich megablock of the Ukrainian shield. Geochemistry and ore formation, (28), 11—16 (in Russian).
Ponomarenko, A.N., Stepaniuk, L.M., & Shumlyanskiy, L.V. (2014). Geochronology and Geodynamics of the Paleoproterozoic of the Ukrainian Shield. Mineralohichnyy Zhurnal, 36(2), 48—60 (in Russian).
Purtov, V.K., Anfilogov, V.N., & Egorova, L.G. (2002). The interaction of basalt with chloride solutions and the mechanism of formation of acidic melts. Geochemistry, (10), 1084—1097 (in Russian).
Sollogub, V.B. (1986). The lithosphere of Ukraine. Kiev: Naukova Dumka, 184 p. (in Russian).
Esypchuk, K.E. (Ed.). (1985). Stratigraphic sections of the Precambrian of the Ukrainian Shield. Kiev: Naukova Dumka, 168 p. (inRussian).
Usenko, O.V. (2018). The geodynamic process and its geological manifestations on the continents. Geofizicheskiy Zhurnal, 40(5), 131—171. https://doi.org/10.24028/gzh.0203-3100.v40i5.2018.147477 (in Russian).
Usenko, O.V. (2022). Evolution of the composition of mantle fluids in the Precambrian (on the example of iron formations of the Ukrainian Shield). Geofizicheskiy Zhurnal, 44(2), 3—28. https://doi.org/10.24028/gj.v44i2.256263.
Usenko, O.V. (2013). Deposits of minerals of the Kirovograd ore region of the Ukrainian shield: connection with the deep process. Geofizicheskiy Zhurnal, 35(6), 128—145. https://doi.org/10.24028/gzh.0203-3100.v35i6.2013.116523 (in Russian).
Usenko, O.V. (2019). Reflection of the sequence of geodynamic processes in the geological structure of Pobuzhya. Geofizicheskiy Zhurnal, 41(3), 78—95. https://doi.org/10.24028/gzh.0203-3100.v41i3.2019.172425 (in Russian).
Usenko, O.V. (2017). Periodization and specific features of deep processes in Precambrian by example of the Ukrainian shield. Geofizicheskiy Zhurnal, 39(6), 41—83. https://doi.org/10.24028/gzh.0203-3100.v39i6.2017.116366 (in Russian).
Usenko, O.V. (2021). Present structure of the Near-Bug area: conditions of formation and history of development. Geofizicheskiy Zhurnal, 43(2), 96—115. https://doi.org/10.24028/gzh.v43i2.230191 (in Russian).
Usenko, O.V. (2014). Formation of melts: geodynamic process and physical-chemical interactions. Kiev: Naukova Dumka, 240 p. (in Russian).
Shumlyanskyy, L.V. (2012). Geochemistry of pyroxene plagiogneisses (enderbites) Pobuzhia and isotopic composition of hafni-um in zircons. Mineralohichnyy Zhurnal, 34(2), 64—79 (in Ukrainian).
Shumlyanskyy, L.V., Mazur, M.D., Zinchenko, O.V., & Kryvdyk, S.G. (2009). Isotopic (U-Рb according to zircons) age and geo-logical position of the Kishin massif and its bordering rocks (north-western region of the Ukranian shield). Mineralohichnyy Zhurnal, 31(2), 83—91 (in Ukrainian).
Shumlyanskyy, L.V., Stepaniuk, L.M., Claesson, S., Rudenko, K.V., & Becker, A.Yu. (2018). Uranium-lead by zircon and mona-zite geochronology of granitoids of the Zhytomyr and Sheremetyevo complexes, northwestern region of the Ukrainian Shield. Mineralohichnyy Zhurnal, 40(2), 63—85. https://doi.org/10.15407/mineraljournal.40.02.063 (in Ukrainian).
Shcherbak, N.P., Artemenko, G.V., Bartnytskiy, E.N., Verkhoglyad, V.M., Komaristyy, A.A., Lesnaya, I.M., Mytskevich, N.Yu., Ponomarenko, A.N., Skobelev, V.M., & Shcherbak, D.N. (1989). Geochronological scale of the Precambrian of the Ukrainian Shield. Kiev: Naukova Dumka, 144 p. (in Russian).
Shcherbak, N.P., Artemenko, G.V., Lesnaya, I.M., Ponomarenko, A.N., & Shumlyanskiy, L.V. (2008). Early Precambrian Geo-chronology of the Ukrainian Shield. Proterozoic. Kiev: Naukova Dumka, 240 p. (in Russian).
Shcherbak, N.P., Artemenko, G.V., Lesnaya, I.M., & Ponomarenko, A.N. (2005). Geochronology of the Early Precambrian of the Ukrainian Shield. Archaea. Kiev: Naukova Dumka, 244 p. (in Russian).
Shcherbakov, I.B. (2005). Petrology of the Ukrainian Shield. Lviv: ZuKts, 366 p. (in Russian).
Bogdanova, S.V., Gintov, О.В., Kurlovich, D.M., Lubnina, N.V., Nilsson, М.К.М., Orlyuk, О.І., Pashkevich, І.К., Shumlyan-skyy, L.V., & Starostenko, V.I. (2013). Late Palaeoproterozoic mafic dyking in the Ukrainian Shield of Volgo-Sarmatia caused by rotation during the assembly of supercontinent Columbia (Nuna). Lithos, 174, 196—216. http://dx.doi.org/10.1016/j.lithos.2012.11.002Bucher, К., & Grapes, R. (2011). Petrogenesis of Metamorphic Rocks. Springer-Verlag Berlin Heidelberg, 428 р. https://doi.org/ 10.1007/978-3-540-74169-5.
Сondie, K.C. (2011). Earth and evolving planetary system. Elsеvier, 574 p.
Duchesne, J.-C., Shumlyanskyy, L., & Mytro¬khyn, O.V. (2017).The jot unite of the Korosten AMCG complex (Ukrainian shield): Crust- or mantle-derived? Precambrian Research, 299, 58—74. http://dx.doi.org/10.1016/j.precamres.2017.07.018.
Griffin, W., Belousova, E., O’Neill, C., O’Reilly, S.Y., Malkovets, V., Pearson, N., Spetsius, S., & Wilde, S. (2014). The world turns over: Hadean-Archean crust-mantle evolution. Lithos, 189, 2—15. https://doi.org/10.1016/j.lithos.2013.08.018.
Gudfinnsson, G.H., & Presnal, D.C. (2005). Continuous gradationsamongprimarycarbonatic, melilitic, basaltic, picritic, andko-matiiticmelts in equilibrium with garnet lherzolite at 3—8 GPa. Journal of Petrology, 46(8), 1645—1659. https://doi.org/10.1093/petrology/egi029.
Ionov, D.A., Liu, Z., Li, J., Golovin, A.V., Korsakov, A.V., & Xu, Yi. (2020). The age and origin of cratonic lithospheric mantle: Archean dunites vs. Paleoproterozoic harzburgites from the Udachnaya kimberlite, Siberian craton. Geochimica et Cosmo-chimica Acta, 281, 67—90. https://doi.org/10.1016/j.gca.2020.05.009.
Ivanov, А.V., Mukasa, S.B., Kamenetsky, V.S., Ackersond, V., Demonterova, E.I., Pokrovsky, B.G., Vladykin, N.V., Kole-snichenko, M.V., Litasov, K.D., & Zedgenizov, D.A. (2018). Volatile concentrations in olivine-hosted melt inclusions from meimechite and melanephelinite lavas of the Siberian Traps Large Igneous Province: Evidence for flux-related high-Ti, high-Mg magmatism. Chemical Geology, 483, 442—462. https://doi.org/10.1016/j.chemgeo.2018.03.011.
Lobach-Zhuchenko, S.B., Balagansky, V.V., Baltybaev, Sh.K., Bibikova, E.V., Chekulaev, V.P., Yurchenko, A.V., Arestova, N.A., Artemenko, G.V., Egorova, Yu.S., Bogomolov, E.S., Sergeev, S.A., Skublov, S.G., & Presnyakov, S.L. (2014). The Orekhov-Pavlograd Zone, Ukrainian Shield: Milestones of its evolutionary history and constraints for tectonic models .Precambrian Research, 252, 71—87. https://doi.org/10.1016/j.precamres.2014.06.027.
Lobach-Zhuchenko, S.B., Kaulina, T.V., Baltybaev, S.K., Balagansky, V.V., Egorova, Yu.S., Lokhov, K.I., Skublov, S.G., Sukach, V.V., Bogomolov, E.S., Stepanyuk, L.M., Galankina, O.L., Berezhnaya, N.G., Kapitonov, I.N., Antonov, A.V., & Sergeev, S.A. (2017). The long (3.7—2.1 Ga) and multistage evolution of the Bug Granulite-Gneiss Complex, Ukrainian Shield, based on the SIMS U-Pb ages and geochemistry of zircons from a single sample. In J. Halla, M.J. Whitehouse, T. Ahmad, Z. Bagai (Еds.), Crust-Mantle Interactions and Granitoid Diversification: Insights from Archaean Cratons (Vol. 449, pp. 175—206). Geol. Soc., London, Spec. Publ. http://doi.org/10.1144/SP449.3.
Mychak, S., & Farfuliak, L. (2021). Inner structure and kinematics of the Sushchany-Perga fault zone of the Ukrainian Shield according to the tectonophysical study. Geofizicheskiy Zhurnal, 43(1), 142—159. https://doi.org/10.24028/gzh.0203-3100.v43i1.2021.225496.
Ryabchikov, I.D., Solovova, I.P., Ntaflos, Th., Büchl, A., & Tikhonenkov, P.I. (2001) Subalkalinepicrobasalts and plateau basalts from Putorana plateau (Siberian CFB province). II. Melt inclusion chemistry, composition of «primary» magmas and P-T re-gime at the base of superplume. Geochemistry, (5), 484—497.
Shumlyanskyy, L.V. (2014). Geochemistry of the Osnitsk-Mikashevichy Volcanoplutonic Complex of the Ukrainian Shield. Geo-chemistry International, 52(11), 912—924. https://doi.org/10.1134/S0016702914110081.
Shumlyanskyy, L., Ernst, R.E., Albekov, A., Soderlund, U., Wilde, S.A., & Bekker, A. (2021). The early Statherian (ca. 1800—1750 Ma) Prutivka-Novogol large igneous province of Sarmatia: Geochronology and implication for the Nuna/Columbia su-percontinent. Precambrian Research, 358, 106185. https://doi.org/10.1016/j.precamres.2021.106185.
Shumlyanskyy, L., Hawkesworth, C., Billstrom, K., Bogdanova, S., Mytrokhyn, O., Romer, R., Dhuime, B., Claesson, S., Ernst, R., Whitehouse, M., & Bilan, O. (2017). The origin of the Palaeoproterozoic AMCG complexes in the Ukrainian shield: New U-Pb ages and Hf isotopes in zircon. Precambrian Research, 292, 216—239. https://doi.org/10.1016/j.precamres.2017.02.009.
Starostenko, V., Janik, T., Kolomiyets, K., Czuba, W., Środa, P., Lysynchuk, D., Grad, M., Kovács, I., Stephenson, R., Lysyn-chuk, D., Thybo, H., Artemieva, I.M., Omelchenko, V., Gintov, O., Kutas, R., Gryn, D., Guterc, A., Hegedűs, E., Kommi-naho, K., Legostaeva, O., Tiira, T., & Tolkunov, A. (2013). Seismic velocity model of the crust and upper mantle along profile PANCAKE across the Carpathians between the Pannonian Basin and the East European Craton. Tectonophysics, 608, 1049—1072. https://doi.org/10.1016/j.tecto.2013.07.008.
Walter, M.J. (2005). Melt Extraction and Compositional Variability in Mantle Lithosphere. In R.W. Carlson (Ed.), The Mantle and Core (pp. 363—394). Oxford: Elsevier. https://doi.org/10.1016/B0-08-043751-6/02008-9.
Wyllie, P.J. (1977). Effects of Н2О and СО2 on magma generation in the crust and mantle. Journal of the Geological Society, 134, 215—234. https://doi.org/10.1144/gsjgs.134.2.021.
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 2024 Olga Usenko
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).
