Kinematics of formation of the western and central parts of the Ukrainian shield between 2,02—2,05 Ga ago
On the basis of study of Umansk, Novograd-Voolynsk and Novoukrainsk granitoid massif of western and central parts of the Ukrainian shield by tectonophysical methods intensely deformed state of the earth's crust in the period between 2,02—2,05 Ga has been revealed. The single paleofield of tectonic stress for Nemirovsk and Lelekovsk stages has been restored. A refined scale of deformation stages of the north-western and central part of the Ukrainian Shield in the time interval 2,45—1,73 Ga has been composed. The idea of counter-clockwise turning the western part of the shield relative to its central part during the interval of 2,02—2,05 Ga is being substantiated.
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Belichenko P. V., Gintov O. B., 1996. Tension and deformation of the Earth's crust of the Ukrainian Shield in the period of gabbro-anorthosite-rapakivi Korsun-Novomirgorod Pluton (on tectonophysical data). Geofizicheskiy zhurnal 18(2), 59—69 (in Russian).
Gintov O. B., 1978. The structures of the continental crust at different stages of development. Kiev: Naukova Dumka, 162 p. (in Russian).
Gintov O. B., 2005. Field tectonophysics and its applications in the study of crustal deformations of Ukraine. Kiev: Feniks, 572 p. (in Russian).
Gintov O. B., 2014. Scheme of periodization phases of faulting in the crust of the Ukrainian Shield — the new data and investigation. Geofizicheskiy zhurnal 36(1), 3—18 (in Russian).
Gintov O. B., Mychak S. V., 2012. Reverse faults and thrusts in the crust of the Kirovograd ore district and bond with them uranium mineralization. Geofizicheskiy zhurnal 34(3), 84—91 (in Russian).
Gintov O. B., Mychak S. V., 2014. Kinematics formation of the Ukrainian shield between 1,80—1,73 billion years ago as a result of the study of fracturing rocks Korosten and Korsun-Novomirgorod plutons. Geofizicheskiy zhurnal 36(4), 24—36 (in Russian).
Gintov O. B., Mychak S. V. 2011. Tensions and crustal deformations of the central part of the Ingul megablock on materials of the tectonophysical study of Novoukrainian massif. Geofizicheskiy zhurnal 33(2), С. 28—45 (in Russian).
Geotectonics Volyn-Podolia. Ed. I. I. Chebanenko, 1990. Kiev: Naukova Dumka, 243 p. (in Russian).
Geochronology of the Early Precambrian of the Ukrainian shield. Proterozoic, 2008. Ed. N. P. Shcherbak. Kiev: Naukova Dumka, 240 p. (in Russian).
Isay V. M., 1989. Rheological properties of the crust and some faulting patterns (for example, the Ukrainian shield). Geofizicheskiy zhurnal 11(3), 40—52 (in Russian).
The Kirovograd ore area. Deep structure. Tectonophysical analysis. Ore deposits, 2013. Eds V. I. Starostenko, O. B. Gintov. Kiev: Prastye Ludy, 500 p. (in Russian).
Kozlov G. G., Sveshnikov K. I., 1985. Granitoid formation interfluve Teterev—Sluch. Geologicheskiy zhurnal 45(2), 58—66 (in Russian).
Tsymbal S. N., Shymlanskaya L. V., Stepanyuk L. M., 2014. Age alkaline-ultramafic rocks Gorodnitsky complex and granitoids Sheremetovsky complex north-western part of the Ukrainian shield. Geochronology and geodynamics of the Early Precambrian (3,6—1,6 billion years) Eurasian continent. Collection of abstracts of the International Scientific Conference on the 90th anniversary of academician of NAS of Ukraine N. P Shcherbak. Kiev 16—17 September 2014. …………. (in Russian).
Shevchuk V. V., Pavlov G.G., Kochetov R.V., 2005. Tectonophysical reconstruction on the basis of preferred orientations megacrystals feldspars in granitoids. Geofizicheskiy zhurnal 27(1), 55—62 (in Russian).
Shcherbakov I. B., 2000. Evolution of magmatism of the Ukrainian shield. Mineralogicheskiy zhurnal 22(2/3), 36—48 (in Russian).
Bogdanova S., Gintov O., Kurlovich D., Lubnina N., Nilsson M., Orlyuk M., Pashkevich I., Shumlyanskyy L., Starostenko V., 2012. 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.2012.11.002.
Bogdanova S., Gorbatschev R., Grad M., Guterch A., Janik T., Kozlovskaya E., Motuza G., Skridlaite G., Starostenko V., Taran L., 2006. EUROBRIDGE: New insight into the geodynamic evolution of the East European Craton. In: European Lithosphere Dynamics. Geol. Soc., London, Memoirs, 32, Р. 599—628.
Bogdanova S. V., Bingen B., Gorbatschev R., Kheraskova T. N., Kozlov V. I., Puchkov V. N., Volozh Y. A., 2008. The East European Craton (Baltica) before and during the assembly of Rodinia. Precambrian Res. 160, 23—45.
Elming S. A., Kravchenko S. N., Layer P., Rusakov O. M., Glevasskaya A. M. Mikhailova N. P., Bachtadze V., 2006. Palaeomagnetism and 40Ar/40Ar age determinations of the Ediacarian traps from the southwestern margin of the East European Craton, Ukraine: Relevance to the Rodinian breakup. J. Geol. Soc. 162(6), 131—133.
Elming S.-A., Mikhailova N. P., Kravchenko S., 2001. Palaeomagnetism of Proterozoic rocks from the Ukrainian Shield: new tectonic reconstructions of the Ukrainian and Fennoscandian shields. Tectonophysics 339, 19—38. doi: 10.1016/S0040-1951(01)00032-4.
Mogi K., 1966. Pressure dependence of rock strength and transition from brittle fracture to ductile flow. Bull. Earthquake Res. Inst., Tokyo Univ. 44, 215—232.