Earth’s crust composition of the Ingul megablock of the Ukrainian Shield (types of crust) and patterns of location of ore mineral resources

Автор(и)

  • V. I. Starostenko S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Kyiv, Україна
  • P. Ya. Kuprienko S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Kyiv, Україна
  • I.B. Makarenko S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Kyiv, Україна
  • A. Savchenko S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Kyiv, Україна
  • O.V. Legostaeva S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Kyiv, Україна

DOI:

https://doi.org/10.24028/gzh.0203-3100.v39i5.2017.112338

Ключові слова:

Ingul megablock, granite, diorite, “basalt” layers of the Earth’s crust, types of the consolidated crust

Анотація

Within the Ingul Megablock of the Ukrainian Shield, according to the data of three-dimensional density modeling, at the scale of 1 : 200 000, the thickness of conditionally allocated “granite”, “diorite”, “basalt” layers, which abroad have the name of the upper, middle and lower crust, are determined and their characteristic is given. In relation to the thickness of each layer to the total crust, which is expressed in parts, four types of crust are distinguished: granite, diorite, leuco-basalt, basalt. Since the composition of the Earth’s crust is an important factor in assessing the prospects for minerals, a comparison of the location of the ore deposits of manifestations of hydrothermal and hydrothermal-metasomatic genesis with a real composition scheme is made. It is established that most of the deposits of minerals are confined to blocks of granitic-diorite and diorite types of crust, and the smaller — gravitates to blocks of leuco-basalt and basalt types.

Посилання

Alekhin V. I., Gintov O. B., 2004. Kinematic features, phases of development and metallogeny stage latitudinal fault zones of the Ukrainian Shield. Geofizicheskiy zhurnal 26(6), 83—101 (in Russian).

Bystrevskaya S. S., Pashkevich I. K., 1979. On Abyssal Transregional Zone of Tectonomagmatic Activization Within East-European Platform. Geologicheskiy zhurnal (6), 106—112 (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).

Gorlitskiy B. A., Zankevich B. A., Shmelev E. G., 2003. Classification of geochemical anomalies of the Ukrainian Shield and their structural-geological position: Proceedings of the Institute of Environmental Geochemistry (8), 202—215 (in Russian).

Ilchenko T. V., Pashkevich I. K., Karataev G. I., 1988. Relation between the composition and thickness of the Ukrainian Shield crust. Dopovidi AN URSR. Ser. B (4), 13—16 (in Ukrainian).

Kalashnik A. A., 2003. Perspectives of the diamond content of the Kirovograd geoblock. Naukovyy visnyk Natsionalnoho hirnychoho universytetu (6), 55—59 (in Russian).

The Kirovograd ore area. Deep structure. Tectonophysical analysis. Ore deposits, 2013. Eds V. I. Starostenko, O. B. Gintov. Kiev: Prastyi Ludy, 500 p. (in Russian).

Complex metallogen³c map of Ukraine. 1 : 500 000. Explanatory note, 2003. Ed. S. V. Goshovskiy. Kiev: UkrDHR², 326 p. (in Ukrainian).

Krasovskiy S. S., 1989. Gravity modeling of deep crustal structures and isostasy. Kiev: Naukova Dumka, 248 p. (in Russian).

Krasovskiy S. S., 1981. Reflection of the continental crust dynamics in the gravity field. Kiev: Naukova Dumka, 262 p. (in Russian).

Krasovskiy S. S., Kuprienko P. Ya., Krasovskiy A. S., 2001. Thickness schemes of the consolidated crust layers of the Ukrainian Shield, DDB and Donbass. Ñõåìû ìîùíîñòåé ñëîåâ êîíñîëèäèðîâàííîé çåìíîé êîðû Óêðàèíñêîãî ùèòà, ÄÄÂ è Äîíáàññà. In: Theory and practice of geological interpretation of gravity, magnetic and electric fields. Moscow: IPE RAS Publ., 52—54 (in Russian).

Kuprienko P. Ya., Krasovsky S. S., 1988. Density models of gradient-layered deep crustal structure of the Ukrainian Shield. Geofizicheskiy zhurnal 10(4), 28—39 (in Russian).

Kuprienko P. Ya., Makarenko I. B., Starostenko V. I., Legostaeva O. V., 2007à. Three-dimensional density model of the crust and upper mantle of the Ingul megablok of the Ukrainian Shield. Geofizicheskiy zhurnal 29(2), 17—41 (in Russian).

Kuprienko P. Ya., Makarenko I. B., Starostenko V. I., Legostaeva O. V., 2007b. Three-dimensional density model of the crust and upper mantle of the Ukrainian Shield. Geofizicheskiy zhurnal 29(5), 3—27 (in Russian).

The lithosphere of Central and Eastern Europe. East-European Platform, 1989. Ed. A. V. Chekunov. Kiev: Naukova Dumka, 187 p. (in Russian).

The lithosphere of Central and Eastern Europe: geo-traverse: IV, VI, VIII, 1988. Ed. A. V. Chekunov. Kiev: Naukova Dumka, 170 p. (in Russian).

The lithosphere of Central and Eastern Europe. Summary of studies, 1993. Ed. A. V. Chekunov. Kiev: Naukova Dumka, 258 p. (in Russian).

Sveshnikov K. I., Krasovskiy S. S., Kuprienko P. Ya., Krasovskiy A. S., 1998. Correlation of the near-surface and deep structure of the Earth’s crust of the Ukrainian Shield: new aspects of the synthesis of geological and geophysical data. In: Tectonics and geodynamics: general and regional aspects. Vol. 2. Moscow: GEOS, 161—163 (in Russian).

Sollogub V. B., 1986. Lithosphere Ukraine. Kiev: Naukova Dumka, 184 p. (in Russian).

Starostenko V. I., Gintov O. B., Kutas R. I., 2011. Geo-dynamic development of lithosphere of Ukraine and its role in formation and location of mineral deposits. Geofizicheskiy zhurnal 33(3), 3—22 (in Russian).

Starostenko V. I., Gintov O. B., Pashkevich I. K., Burakhovich T. K., Kulik S. N., Kuprienko P. Ya., Kutas R. I., Makarenko I. B., Orliuk M. I., Tsvetkova T. A., 2007. Metallogeny of the Ukrainian Shield: distribution of ore deposits, regularities of connection with deep structure and dynamics of lithosphere. Geofizicheskiy zhurnal 29(6), 3—31 (in Russian).

Starostenko V. I., Kuprienko P. Ya., Makarenko I. B., Legostaeva O. V., Savchenko A. S., 2012. Density heterogeneity of the Earth’s crust along latitudinal fault zones of the Ukrainian Shield and the Dnieper-Donets depression. Geofizicheskiy zhurnal 34(6), 113—132 (in Russian).

Starostenko V. I., Kuprienko P. Ya., Makarenko I. B., Savchenko A. S., Legostaeva O. V., 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).

Scheme of deep lithosphere structure in South-Western part of Eastern-European platform. 1: 1 000 000, 1992. Ed. A. V. Chekunov. Kiev: Publ. of the State Committee for Geology of Ukraine (in Russian).

Tripolskiy A. A., Sharov N. V., 2004. Structure of the Precambrian shields of the Earth’s lithosphere by seismic data. Petrozavodsk: Karelian Research Centrå, RAS. 156 p. (in Russian).

Chekunov A. V., Naumenko V. V., Kuchma V. G., 1982. A relationship between the Earth’s crust deep re-arrangement, tectonic movements, magmatism, metamorphism and metal content in the Dnieper-Donets paleorift. Geofizicheskiy zhurnal 4(3), 17—24 (in Russian).

Chekunov A. V., Sollogub V. B., Ilchenko T. V., Krasovsky S. S., Kutas R. I., Pashkevich I. K., Garetsky R. G., Karataev G. I., Nadezhka L. I., Dubyansky A. I., 1990. A depth inhomogeneities of the Earth’s crust in the south of the Eastern-European platform. Geofizicheskiy zhurnal 12(4), 3—22 (in Russian).

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Опубліковано

2017-10-26

Як цитувати

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. Геофізичний журнал, 39(5), 27–46. https://doi.org/10.24028/gzh.0203-3100.v39i5.2017.112338

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