DOI: https://doi.org/10.24028/gzh.0203-3100.v41i3.2019.172425

Reflection of sequence of geodynamic processes in geological structure of the Bug area

O. V. Usenko

Abstract


The age of formations composing granulite blocks of the Ukrainian Shield is a pro-blem for disputes. In order to ascertain the primary genesis and conditions of transduction of the Bug area rocks it is proposed to find out how was deep process realized according to composition of magmatic and chemogenic-sedimentary rocks. Description of formations was used and sequence of geological events, given in the paper [Venidictov, 1986] for the Upper Bug area. During the period that began not later than 2.5 Ga and lasted up to 2.0 Ga three tectono-magmatic cycles happened that can be compared with a regime “folded area”. Application of over-all schemes allows to ascertain composition and temperatures of melts and fluids sup-plied to the crust (thermodynamic regime), and to appraise the character of interactions (metasomatic substitution, crystallization, melting-dissolution etc.) between deep material (of the known composition and temperature) and crust material at the ascertained depth (with known lithostatic pressure and temperature). Regime “folded area” is cha-racterized by magmatic rocks generated at depths 220, 150, 100, 50 km. Underlaying of the crust by mantle (ultrabasic) melts and replenishment of melting layers with their upper edge at depths 50 and 20 km, occurs repeatedly, that assumes complication of ba-sic regime. It has been determined that in the Bug area temperatures and pressures of metamorphic transformations exceeded those ones needed for production of the layer of partial melting in the crust. To present-day erosion section the level of asthenosphe-re position, where granites attached to the berdychiv complex was drawn. Sequence of occurrence was replaced by the order of incorporation and substitution. Primary sedimentary rocks were not preserved and there is no relation between occurrence of rocks and their age.


Keywords


Proterozoic; metamorphism; granulite area; melting; metasomatic substitution; isotopic age

References


Bogatikov, O. A., Kovalenko, V. I., & Sharkov, E. V. (2010). Magmatism, tectonics and geodynamics of the Earth: connection in time and in space. Moscow: Nauka, 606 р. (in Russian).

Venidiktov, V. M. (1986). Polycyclic development of granulite facies. Kiev: Naukova Dumka, 267 p. (in Russian).

Antsiferov, A. V. (Ed.). (2008). Geological and geophysical model Golovanevsk suture zones of the Ukrainian Shield. Donetsk: Weber, 308 p. (in Russian).

Gerya, T. V. (1990). PT trends and model forming complexes granulitovyh Precambrian: Author's abstract of the dis. of Dr. geol.-min. sci. Moscow: Moscow State University, 35 p. (in Russian).

Gintov, O. B. (2005). Field Tectonophysics and Its Applications for the Studies of Deformations of the Earth's Crust of Ukraine. Kiev: Feniks, 572 p. (in Russian).

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. https://doi.org/10.24028/gzh.0203-3100.v40i3.2018.137170 (in Russian).

Usenko, I. S. (Ed.). (1985). Granulite facies of the Ukrainian Shield. Kiev: Naukova Dumka, 220 p. (in Russian).

Entin, V. A., Gintov, O. B., Mychak, S. V., & Yushin, A. A. (2015). The structure of the Moldovan iron ore deposit (Ukrainian Shield) according to geological and geophysical data and its possible nature. Geofizicheskiy zhurnal, 37(4), 3—18. https://doi.org/10.24028/gzh.0203-3100.v37i4.2015.111118 (in Russian).

Kirilyuk, V. P. (2015). Once again about the problems of the stratigraphy of the Pobuzh granulite complex (on the occasion of the adoption of a new regional stratigraphic scheme of the lower Precambrian of the Ukrainian Shield). Article 2. The ratio of retinues of the pobozhsky stratigraphic complex. Collection of scientific works UkrGGRI, (3), 147―168 (in Ukrainian).

Lazko, E. M., Kirilyuk, V. P., Sivoronov, A. A., Yatsenko, G. M. (1975). Lower Precambrian of the Ukrainian Shield. Lviv: Vysshaya shkola, 239 p. (in Russian).

Lobach-Zhuchenko, S. B., Baltybaev, Sh. K., Glebovitsky, V. A., Sergeev, S. A., Lokhov, K. I., Yegorova, Yu. S., Balagansky, V. V., Skublov, S. G., Galankina, O. L., & Stepanyuk, L. M. (2017a). U-Pb-SHRIMP-II-Age and origin of zircon from lhertzolite of the Bug Paleoarchean complex (Ukrainian Shield). Doklady RAN, 477, 567―571. doi: 10.7868/S0869565217350134 (in Russian).

Lobach-Zhuchenko, S. B., Ryborak, M. V., Saltykova, T. E., Sergeev, S. A., Lokhov, K. I., Bobrova, E. M., Sukach, V. V., Skublov, S. G., Berezhnaya, N. G., & Albekov, A. Yu. (2017b). The Archean formation of the Sarmatian continental crust. Geologiya i geofizika, 58(12), 1886—1914. doi: 10.15372/GiG20171204 (in Russian).

Perchuk, A. L. (2002). Eclogites of the Bergen-Arks complex, Norway: petrology and mineral chronometry. Petrologiya, 10(2), 115—136 (in Russian).

Perchuk, L. L. (1997). Deep Fluid Flows and Granite Birth. Sorosovskiy obrazovatel'nyy zhurnal, (6), 56―63 (in Russian).

Ponomarenko, A. N., Gintov, О. B., & Stepanyuk, L. M. (2018). On the so-called «leucogranulite formation» and «zelenovadov Formation» 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).

Purtov, V. K., Anfilogov, V. N., & Egorova, L. G. (2002). The interaction of basalt with chloride solutions and the mechanism of formation of acid melts. Geokhimiya, (10), 1084―1097 (in Russian).

Stepanyuk L. M., Shumlyansky L. V., Ponomarenko A. N., Dovbush T. I., Vysotsky A. B., Dyuym Br. On wikis limits the formation of Koshar-Alexandrov worlds Pobuzhya Bug series. Heokhimiya ta rudoutvorennya, (28), 4―10 (in Ukrainian).

Usenko, O. V. (2018). Geodynamic process and its geologic manifestations in the continents. Geofizicheskiy zhurnal, 40(5), 137—171. https://doi.org/10.24028/gzh.0203-3100.v40i5.2018.147477 (in Russian).

Usenko, O. V. (2013). The development of the Ingul megablock of the Ukrainian Shield during the formation of the Novoukrainsky and Korsun-Novomirgorod Plutons. Geofizicheskiy zhurnal, 35(3), 54—69. https://doi.org/10.24028/gzh.0203-3100.v35i3.2013.116394 (in Russian).

Usenko, O. V. (2015a). Conditions of formation of ferruginous rocks of the Middle Bug area. Geofizicheskiy zhurnal, 37(4), 32—56. https://doi.org/10.24028/gzh.0203-3100.v37i4.2015.111122 (in Russian).

Usenko, O. V. (2014). Formation of melts: a geodynamic process and physical-chemical interactions. Kiev: Naukova Dumka, 240 p. (in Russian).

Usenko, O. V. (2015b). Evolution of mantle melts and fluids in Precambrian. Dopovidi NAN Ukrainy, (7), 99―104 (in Russian).

Shatskiy, V. S., Buzlukova, L. V., Yagoutts, E., Kozmenko, O. A., & Mityukhin, S. I. (2005). The structure and evolution of the lower crust of the Daldyn-Alakitsky region of the Yakutsk diamondiferous province (according to a study of xenoliths). Geologiya i geofizika, 46(12), 1273―1289 (in Russian).

Shumlyanskiy, L. V. (2012). Age and isotopic composition of hafnium zircons from quartzite from the Middle Pobuzh'ya Ukrainian Shield. Heokhimiya ta rudoutvorennya, (31-32), 136―143 (in Russian).

Scherbak, 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).

Scherbak, N. P., Artemenko, G. V., Lesnaya, I. M., Ponomarenko, A. N., & Shumlyansky, L. V. (2008). Geochronology of the Early Precambrian of the Ukrainian Shield. Proterozoic. Kiev: Naukova Dumka, 240 p. (in Russian).

Shcherbakov, I. B. (2005). Petrology of the Ukrainian Shield. Lviv: ZuKTs, 366 p. (in Russian).

Chukhrov, F. V. (Ed.). (1991). Endogenous sources of ore matter. Moscow: Nauka, 248 p. (in Russian).

Yaroshchuk, M. A. (1983). Iron-ore formations of the Belotserkov-Odessa metallogenic zone. Kiev: Naukova Dumka, 224 p. (in Russian).

Belousova, E. A., Kostitsyn, Y. A., Griffin, W. L., Begg, G. C., O'Reilly, S. Y., & Pearson, N. J. (2010). The growth of the continental crust: constraints from zircon Hf-isotope data. Lithos, 119(3-4), 457―466. https://doi.org/10.1016/j.lithos.2010.07.024.

Bogdanova, S. V., Gorbatschev, R., & Garetsky, R. G. (2016). EUROPE|East European Craton. In Reference Module in Earth Systems and Environmental Sciences (pp. 3―17). Elsevier.

Carlson, R. W., Pearson, D. G., & James, D. E. (2005). Physical, chemical and chronological characteristics of continental mantle. Reviews of Geophysics, 43(1), 1—24. http: dx.doi.org.10.1029/2004RG000156.

Сondie, K. C. 2011. Earth and evolving planetary system. Elsеvier, 574 p.

Ionov, D. A., Carlson, R. W., Doucet, L. S., Golovin, A. V., & Oleinikov, О. B. (2015). The age and history of the lithospheric mantle of the Siberian craton: Re-Os and PGE study of peridotite xenoliths from the Obnazhennaya kimberlite. Earth and Planetary Sciences Letters, 428, 108―119. https://doi.org/10.1016/j.epsl.2015.07.007.

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.

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.




Creative Commons License
Licensed under a Creative Commons Attribution 4.0 International License.

Flag Counter