Conditions of formation of ferruginous rocks of the Middle Bug area

Authors

  • O. Usenko S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Kyiv, Ukraine

DOI:

https://doi.org/10.24028/gzh.0203-3100.v37i4.2015.111122

Abstract

An opinion has been substantiated that the rocks of ferruginous-siliceous-carbonate formation of the Bug and Golovanev suture zone are endogenous. Their appearance is synchronous with the appearance of rocks of the Gadantsev suite of the Krivoy Rog–Kremenchug zone.  Peculiarities of this formation and of enclosing strata of the Bug series can be explained by behavior of the geodynamic  process, sharp change of composition of deep fluid which accompanied differentiation of asthenospheric melt as well as crystallization under conditions of granulite metamorphism facies. Specific composition of rocks of this formation depends on mixing of the residual water chloride-potassium and deep carbonate-fluoride-sodium fluids.

References

Bogatikov O. A., Kovalenko V. I., Sharkov E. V., 2010. Magmatism, tectonics, geodynamics of the Earth. Proceedings IGEM RAS. New series. Vol. 3. Moscow: Nauka, 606 p. (in Russian).

Venidiktov V. M., 1986. Polycyclic development of granulite facies. Kiev: Naukova Dumka, 268 p.

Geological geoelectric model of the Orekhovo-Pavlograd suture zone of the Ukrainian shield, 2005. Ed. M. Ya. Azarov. Kiev: Naukova Dumka, 190 p. (in Russian).

Gintov O. B., 2005. Field Tectonophysics and its application in the study of crustal deformation 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).

Deep structure, evolution and minerals Early Precambrian basement of the East European Platform: Interpretation materials reference profile 1-EB, 4B and TATSEYS profiles, 2010. Vol. 2. Eds. A. F. Morozov. Moscow: GEOKART:GEOS, 400 p. (in Russian).

Gordienko V. V., 2007. Advection-polymorphous hypothesis tectonosphere processes. Kiev: Korvіn press, 172 p. (in Russian).

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

Entin V. A., 2005. Geophysical basis of tectonic maps of Ukraine the scale of 1: 1 000 000. Geofizicheskiy zhurnal 27(1), 74—84 (in Russian).

Ferruginous-siliceous formations of the Precambrian of the European part of the USSR. The genesis of iron ore, 1991. Ed. V. M. Kravchenko, D. A. Kulik. Kiev: Naukova Dumka, 216 p. (in Russian).

Ferruginous-siliceous formations of the Ukrainian shield. Vol. 2. Ed. N. P. Semenenko. Kiev: Naukova Dumka, 1978. 367 p. (in Russian).

Krivdik S. G., Tkachuk V. I., 1990. Petrology of alkaline rocks of the Ukrainian shield. Kiev: Naukova Dumka, 1990. 408 p. (in Russian).

Krivorozhskaya ultradeep well SG-8, 2011. Ed. E. M. Sheremet. Donetsk: Noulidzh, 555 p. (in Russian).

Lazko E. M., Kirilyuk V. P., Sivoronov A. A., Yatsenko G. M., 1975. Lower Precambrian western part of the Ukrainian Shield (age complexes and formation). Lviv: Vyshcha Shkola, 239 p. (in Russian).

Melnik Yu. P., 1986. Genesis of Precambrian banded iron formations. Kiev: Naukova Dumka, 236 p. (in Russian).

Petrology and Geochemistry charnockitoids Ukrainian Shield. Ed. O. M. Ponomarenko. Kiev: Naukova Dumka, 216 p. (in Ukrainian).

Purtov V. K., Anfilogov V. N., Yegorova L. G., 2002. Basalt interaction with chloride solutions and the mechanism of formation of acid melts. Geokhimiya (10), 1084—1097 (in Russian).

Ryabchikov I. D., Girnis A. V., 2005. Origin Ca-poorest kimberlite magmas. Geologiya i geofizika 46(12), 1223—1233 (in Russian).

Ryabchikov I. D., Kogarko L. N., Solovova I. P., 2009. Physical and chemical conditions of magma formation at the base of the Siberian plume according to the study of micro-melt in meimechites and alkaline pikitah Maimecha-Kotui province. Petrologiya 17(3), 311—323 (in Russian).

Semenenko N. P., 1966. Metamorphism mobile zones. Kiev: Naukova Dumka, 300 p. (in Russian).

Spetsius Z. V., Serenko V. P., 1990. Composition of the continental upper mantle and the lower crust beneath the Siberian platform. Moscow: Nauka, 271 p. (in Russian).

Precambrian stratigraphic sections of the Ukrainian shield, 1985. Ed. K. E. Esipchuk. Kiev: Naukova Dumka, 168 p. (in Russian).

Usenko O. V., 2013. Mineral deposits of the Kirovograd ore district of the Ukrainian shield: relationship with the underlying processes. Geofizicheskiy zhurnal 35(6), 129—146 (in Russian).

Usenko O. V., 2014a. Conditions of formation of granitoids Srednepridneprovsky granite-greenstone region. Geofizicheskiy zhurnal 36(2), 57—74 (in Russian).

Usenko O. V., 2015a. Conditions of formation of ferruginous-siliceous formations (Srednepridneprovsky megablock). Geofizicheskiy zhurnal 37(1), 21—41 (in Russian).

Usenko O. V., 2015b. Conditions of formation of ferruginous rocks of the Krivoy Rog-Kremenchug area. Geofizicheskiy zhurnal 37(3), 66—87 (in Russian).

Usenko O. V., 2014b. Forming Melts: geodynamic processes and physical and chemical interactions. Kiev: Naukova Dumka, 240 p. (in Russian).

Chekalyuk E. B., 1980. Thermodynamic stability of hydrocarbon systems in geo thermodynamic conditions. In: Degassing of the Earth and Geotectonics. Moscow: Nauka, P. 267—274 (in Russian).

Shcherbak N. P., Artemenko G. V., Lesnaya I. M., Ponomarenko A. N., Shumlyanskiy L. V., 2008. Geochronology Early Precambrian Ukrainian board. Proterozoic. Kiev: Naukova Dumka, 2008. 240 p. (in Russian).

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

Yaroshchuk M. A., 1983. Iron formation Belotserkovskii-Odessa metallogenic zone. Kiev: Naukova Dumka, 224 p. (in Russian).

Gudfinnsson G. H., Presnal D. C., 2005. Continuоus gradations among primary carbonatic, melilitic, basaltic, picritic, and komatiitic melts in equilibrium with garnet lherzolite at 3-8 GPa. J. Petrol. 46, 1645—1659.

Published

2015-08-01

How to Cite

Usenko, O. (2015). Conditions of formation of ferruginous rocks of the Middle Bug area. Geofizicheskiy Zhurnal, 37(4), 32–50. https://doi.org/10.24028/gzh.0203-3100.v37i4.2015.111122

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Articles