Geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of Ukraine

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Бібліографічні деталі
Дата:	2010
Автори:	Starostenko, V., Gintov, O., Kutas, R., Pashkevich, I.
Формат:	Стаття
Мова:	English
Опубліковано:	Інститут геофізики ім. С.I. Субботіна НАН України 2010
Назва видання:	Геофизический журнал
Онлайн доступ:	http://dspace.nbuv.gov.ua/handle/123456789/103103
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Назва журналу:	Digital Library of Periodicals of National Academy of Sciences of Ukraine
Цитувати:	Geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of Ukraine / V. Starostenko, O. Gintov, R. Kutas, I. Pashkevich // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 162-165. — Бібліогр.: 18 назв. — англ.

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Digital Library of Periodicals of National Academy of Sciences of Ukraine

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spelling	irk-123456789-1031032016-06-14T03:04:01Z Geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of Ukraine Starostenko, V. Gintov, O. Kutas, R. Pashkevich, I. 2010 Article Geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of Ukraine / V. Starostenko, O. Gintov, R. Kutas, I. Pashkevich // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 162-165. — Бібліогр.: 18 назв. — англ. 0203-3100 http://dspace.nbuv.gov.ua/handle/123456789/103103 en Геофизический журнал Інститут геофізики ім. С.I. Субботіна НАН України
institution	Digital Library of Periodicals of National Academy of Sciences of Ukraine
collection	DSpace DC
language	English
format	Article
author	Starostenko, V. Gintov, O. Kutas, R. Pashkevich, I.
spellingShingle	Starostenko, V. Gintov, O. Kutas, R. Pashkevich, I. Geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of Ukraine Геофизический журнал
author_facet	Starostenko, V. Gintov, O. Kutas, R. Pashkevich, I.
author_sort	Starostenko, V.
title	Geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of Ukraine
title_short	Geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of Ukraine
title_full	Geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of Ukraine
title_fullStr	Geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of Ukraine
title_full_unstemmed	Geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of Ukraine
title_sort	geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of ukraine
publisher	Інститут геофізики ім. С.I. Субботіна НАН України
publishDate	2010
url	http://dspace.nbuv.gov.ua/handle/123456789/103103
citation_txt	Geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of Ukraine / V. Starostenko, O. Gintov, R. Kutas, I. Pashkevich // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 162-165. — Бібліогр.: 18 назв. — англ.
series	Геофизический журнал
work_keys_str_mv	AT starostenkov geodynamicsoflithosphereasoneofthecrucialfactorsofmineraldepositsformationofukraine AT gintovo geodynamicsoflithosphereasoneofthecrucialfactorsofmineraldepositsformationofukraine AT kutasr geodynamicsoflithosphereasoneofthecrucialfactorsofmineraldepositsformationofukraine AT pashkevichi geodynamicsoflithosphereasoneofthecrucialfactorsofmineraldepositsformationofukraine
first_indexed	2025-07-07T13:17:35Z
last_indexed	2025-07-07T13:17:35Z
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fulltext	�� 2� �� !"# $ %& '( )�& �� Geodynamics�of�lithosphere�as�one�of�the crucial�factors�of mineral�deposits formation�of�Ukraine V��Starostenko��O��Gintov��R��Kutas��I��Pashkevich, 2010 Institute of Geophysics, National Academy of Sciences of Ukraine, Kiev, Ukraine earth@igph.kiev.ua kutro@ndc.org.ua oleg.gintov@gmail.com; innap@34mail.ru Comprehensive�studies�of�the�lithosphere�struc- ture�of�Ukraine�have�been�performed�lately�at�the Institute�of�Geophysics�NASU�in�connection�with solving�the�problems�of�metallogeny��diamond-,�gas- and�oil-bearing �Starostenko et al., 2007��These studies�included��thourough�analysis�of�geological� geophysical�data�on�tectonics�and�deep�structure of�the�Earth s�crust�and�upper�mantle �plotting�the comprehensive�three�dimensional�geophysical�and geodynamic�model�of�lithosphere �generalization�of global experience in application of geophysical, in- cluding tectonophysical, methods for the search and prospecting of different kinds of mineral deposits. The�results�of�studies�allow�drawing�some�conclu- sions�on�the�character�of�geodynamic�processes� having an influence on formation and distribution of deposits on the territory of Ukraine. It�has�been�shown�by�the�examples�of�the�Ukrai- nian�Shield��the�Dnieper�Donets��the�Carpathian�and Azov�Black�Sea�oil�gas�bearing�provinces�that�the regularities�of�formation��redistribution�and�concen- tration�of�mineral�deposits�are determined in many cases by special features of tectonosphere evolu- tion arising from the mechanisms of global and re- gional movements of lithosphere plates. The Ukrainian Shield (USh). Practically all large fault zones of the USh are zones of shift with acute predominance of horizontal component of banks displacements [Gintov, 2005]. They were arised in Neo-Archean and Early Proterozoic as right and left shifts, strike-slip and upthrow faults with amplitude of displacement as kilometers and tens of kilometers and transcending far beyond the li- mits of the Shield. Their roots according to different geophysical characteristics are relaited to in the mantle up to the depth of �� km and more [Gintov, Pashkevich, 2010]��Existence of such an- cient extensive zones�of shift may be only explained by convective movements in the mantle, which took place as early as in Neo-Archean�and Early Pro- terozoic. In Proterozoic numerous fault zones were also formed as listric ones or gently sloping over- thrust. According to the results of tectonophysical and paleomagnetic studies of dynamics of lithosphere of the USh a conclusion has been drawn that the Shield as a consolidated structure has existed since the boundary of 1.8—1.6 Ga. According to paleo- magnetic data [Elming et al., 1998], it existed be- fore and moved autonomously and even earlier, ac- cording to tectonophysical data [Gintov, Pashkevich, 2010], it was divided into several megablocks, which had their own trajectories of movements. Joint analysis of kinematic and three-dimensional geophysical model of the Shield as well as of VP to- mographic model of the mantle up to the depth of 850 km [Geyko et al., 2006], allows to correlate the results of metallogenic studies of fault zones of the USh with materials of geodynamic reconstructions. Within the limits of the USh more than 75 percent of known metallogenic zones, ore areas and ore fields belong to well studied large fault zones. These are mainly the areas of development of mineralization and deposits of non-ferrous, rare, noble metals, uranium, rare earths et al. [Starostenko et al., 2007]. Dnieper-Donets oil-gas province (DDOGP). Numerous oil-gas deposits within non-anticline, the so-called "non-traditional" traps — on monoclines, half-anticlines, sub-thrust zones, within crystalline basement etc. have been discovered here lately. The majority of such deposits are related to the frac- tures of fault-, shift and upthrow (shear) fault types. These considerations brought a lot of scientists to the idea of great perspectives of anorganic hypo- thesis of oil origin and of important role of tangential forces and horizontal movements of lithosphere in formation of traps for hydrocarbons. Numerical modeling of the process of the Dnie- per-Donets aulacogene (DDA) formation by the back-stripping method within the limits of continen- tal lithosphere stretching concept of D. McKenzie testifies the possibility of its formation in the Late �� !"# $ %& '( )�& �� �2) +,� �-.�,/�0 ��. �� 1��, ��0. 0� 0��,� �� Devonian by the type of rift basins with formation of sub-oceanic crust [Stifenson et al., 1997]. Impor- tant role has been proved of shifting processes in formation of contemporary structure of DDOGP and of many types of oil-gas deposits. The system of faults of the DDA manifested during Alpine time as the largest right shift, which is the result of super- regional sub-longitudinal contraction, which covered during Meso-Cenozoic time the territories of the south and south-west of the East-European Plat- form (EEP). The explanation can be found in the known plate tectonic reconstructions: the pressure on the EEP from the south as a result of move- ments of the African and Arabian plates is passed through West-Black Sea and East Black Sea mi- cro-plates [Nikishin et al., 2001; Patalaha et al., 2003; Kazmin et al., 2004]. The suture zone of the Donets Folded Structure (DFS) with the south slope of the Voronezh crysta- lline massif (Starobelsk-Millerov monocline) can be considered as an example of the influence of the processes of compression and shifting upon forma- tion of hydrocarbon deposits. The suture zone is revealed by the series of over-thrusts of Carbonife- rous-Cretaceous deposits of the DFS upon the mon- ocline — Krasnopopovskiy, Severodonetskiy, Mari- evskiy, Almaznyi, Iliychevskiy and other ones. Here, within the stripe not less than 50 km wide, a whole set of non-anticline type deposits within the limits of the monocline itself, in Krasnorechensk and Li- sichansk gas-bearing areas have been discovered [Gintov, 2005; Starostenko et al., 2009]. The Carpathian Meso-Cenozoic Oil-Gas Pro- vince (COGP)�is characterized by over-thrust struc- ture of the Meso-Cenozoic strata, doubled and tri- pled cross-section of the Cretaceous, Paleogene and Neogene, is considered by the majority of geo- logists and geophysicists from the positions of plate tectonics. According to the data of seismic tomography high-velocity lithosphere of EEP sinks under rela- tively low-velocity mantle of the Volyno-Podolian plate and the Carpathians from the depth of 50 to 250—300 km [Geyko et al., 2006]. It has been found by geothermic studies [Kutas, 2005] that for deposits and the areas of oil-gas ac- cumulation, concentrated within the limits of Pre- Carpathian depression (in this case within the Ex- ternal zone of depression gas and gas-condensate deposits predominate, and within Internal one — oil deposits), increased temperature and heat flows are specific. Deposits form two stripes, narrow enough in zones of Carpatian direction Pre-Carpathian and Scole faults which are at a distance of 20—30 km from each other. In the periphery of EEP accumulation of hydro- carbons in the deposits of accretion wedge could occur as early as Cretaceous and Paleogene. Du- ring collision stage redistribution of hydrocarbon po- tential occurred.�Migration�processes� influenced essentially�on�hydrodynamic�conditions�� thermal regime��physical parameters�of sedimentary strata. These�parameters�can�be�used�for�determination�of the�ways�of�migration�and�zoning of oil-gas areas. With�the�help�of�numerical�tectonophysical�mo- deling�the�connection�of�formation�and�distribution of�oil�gas�deposits�COGP�with�plate�tectonic�mech- anism of region formation has been analyzed �Gon- char, 2007��Palinspastic�sections�of�the�frontal�part of�the�Flish�Carpathians�and�Pre�Carpathian�depres- sion�have�been�complited��They reconstruct the pro- cess of formation of deposits under conditions of lateral accretion and formation of covers in case of obduction-subduction mechanism and explain zo- ning in distribution of oil and gas deposits within Pre-Carpathian depression. Application of modern geodynamic concepts of the Carpathian region formation allows considerable widening of its perspectives of oil- and gas-bearing. North-western part of the External zone of Pre-Car- pathian depression (Krukenitskaya sub-zone), au- tokhtonous deposits of Folded Carpathians, plat- form Meso-Cenozoic deposits of south-eastern part of External zone under the over-thrust of the Folded Carpathians, Trans-Carpathian depression are worth to be paid special attention. Azov-Black Sea Oil-Gas Province (ABSOGP). A considerable part of the Province is located within the water areas. Therefore analysis of geodynamic processes in it is possible only on the background of geodynamic development of the whole Black Sea- Caucasian segment of the Alpine belt. ABSOGP and COGP have got some common geophysical peculiarities. It allows treating them from similar geodynamic positions. ABSOGP ad- joins to the southern tectonic border of EEP and here, as well as in the COGP, according to the data of seismic tomography [Geyko et al., 2006] sub- mergence can be observed of relatively high-veloci- ty lithosphere of the Craton under relatively low-velo- city mantle of Dobrogea, Scythian plate, the Black Sea. The studies of geothermal regime of the re- gion shows that oil-gas deposits are localized wi- thin the areas of increased heat flows, forming in this case two sub-parallel stripes: gas deposits are located within the zones of high heat flows and the oil ones — in their periphery. The important role is played by tectono-thermal activization in case of shift displacements of micro-plates [Kutas et al., 2002; 2007]. �� 2% �� !"# $ %& '( )�& �� For the studies of ABSOGP conditions of forma- tion the main interest belongs to Oligocene-Quater- nary stage, which began 35—40 million years ago. The results of geothermal studies in the region show that for this period there is strong enough correla- tion between location of oil-gas deposits and ano- malies of heat flow [Kutas et al., 2002; 2007]. At this stage the Black Sea — Caucasian region de- velops in the indentor regime under the action of Arabian, Pannonian and Adriatic plates [Patalaha et al., 2003]. In addition, the movement of the Black Sea plate within northern points of compass was of reverse character that is indicated by tectonophys- ical data on the Crimean peninsula: the phases of sub-longitudinal contraction was interrupted by shorter phases of even stretching [Gintov, 2005]. For promising areas of ABSOGP — north-western shelf of the Black Sea and the Kerch-Tamanian depres- sion the detailed schemes of fault tectonics of conso- lidated crust have been compile [An integrated …, 2006]. They emphasize the leading role of shift defor- mations during formation of fault and fold structures of the Meso-Cenozoic cover, to which (especially to the knots of fault crossing) hydrocarbon deposits are re- lated. It has also been found by marine geophysical studies that zones of deep faults and neo-tectonic dis- turbances connected with them are the channels of migration of gas-fluid flows [Kobolev, Kutas, 1999]. References An integrated three-dimensional geophysical model of the lithosphere of the Ukrainian Shield in con- nection with magmatism, tectonics and the forma- tion of minerals // Report of the Institute of Geophys- ics by S.I. Subbotin of NASU / Ed. V. I. Starostenko. — Kiev, 2006. — 510 p. — Fund of UkrNIINTI, � state registration 102U002478 (in Russian) Elming S. A., Mikhailova N. P., Kravchenko S. N. The Ñonsolidation of the East European Craton; a Pa- leomagnetic Analysis of Proterozoic Rocks from the Ukrainian Shield and Tectonic reconstructions Ver- sus Fennoscandia // Geophys. J. — 1998. — 20, � 4. — P. 71—74 (in Russian). Geyko V. S., Shumlanskaya L. A., Bugaenko I. V., Za- yets L. N., Tsvetkova T. A. Three-dimensional mo- del of the upper mantle of Ukraine on the arrival time of P-waves // Geophys. J. — 2006. — 28, � 1. — P. 3—16 (in Russian). Gintov O. B. Field tectonophysics and its application in studying the crustal deformation of Ukraine. — Kiev: Phoenix, 2005. — 572 p. (in Russian). �� . .�� !��"��#��$%&��'�� (�� // Geophys. J. — 2009. — 31, � 5. — P. 3— 31 (in Russian). Gintov O. B., Pashkevich I. K. Tectonophysical analy- sis and geodynamic interpretation of the three-di- mensional geophysical model of the Ukrainian Shield // Geophys. J. — 2010. — 32, � 2. — P. 3— 27 (in Russian). Gonchar V. V. Rheological control of the accretion and cover styles of deformation and stress state of su- prasubduction orogen // Geophys. J. — 2007. — 29, � 6. — P. 116—137 (in Russian). Kazmin V. G., Lobkovsky L. I., Pustovitenko B. G. Con- temporary kinematics of the microplates in the Black-sea-South-Caspian region // Okeanology. — 2004. — 44, � 4. — P. 600—610 (in Russian). Kobolev V. P., Kutas R. I. Geophysical researches of gas release structures on the northwestern part of the Black Sea // Tectonics and oil- and gas-content of the Azov-Black-sea region. — Simferopol, 1999. — P. 53—55 (in Russian). Kutas R. I. Geodynamic processes and thermal state of lithosphere of the Carpathian region // Research of modern geodynamics of the Ukrainian Car- pathians. — Kiev: Nauk. dumka, 2005. — P. 132— 139 (in Russian). Kutas R. I., Kobolyev V. P., Paliy S. I. Geothermal con- ditions and oil- and gas bearing of the North-Black- sea — Ciscaucasian region // Oil and Gas Indus- try. — 2002. — � 5. — P. 9—11 (in Russian). Kutas R. I., Kravchuk O. P., Bevzyuk M. I., Stakho- va L. I. Results of geothermal studies in the nor- thern part of the Black Sea // Geophys. J. — 2007. — 29, � 4. — P. 45—65 (in Russian). Nikishin A. M., Korotayev M. V., Bolotov S. N., Yer- shov A. V. Tectonic history of the Black-sea basin // BMOIP. — 2001. — 76, issue 3. — P. 3—17 (in Rus- sian). Patalakha E. I., Gonchar V. V., Senchenkov I. K., Cher- vinko O. P. Indenter mechanism in geodynamics of the Crimean-Black-sea region. Forecast of HC and seismic hazard. — Kiev: Publishing house PP "EMKO", 2003. — 226 p. (in Russian). �� V� ��intov O� B�� I� K�� k�� T� K�� S� N�� P� Ya�� I� B��O��y�� M� I�� a T. A��)��'�� �� '�� #� �� mineral� �� !"# $ %& '( )�& �� �2� +,� �-.�,/�0 ��. �� 1��, ��0. 0� 0��,� �� "�� �� '��'�� � �� # ��#��+,��&���--�.�� /��0� ��1� 0�� 2��0�P� 3034 (in Russian). Starostenko V� I��Lukin A� E��Kobolyev V� P��Rusa- kov O� M��Orlyuk M� I��Shuman V� N��Omelchen- ko V� D��Pashkevich I� K��Tolkunov A� P��Bogda- nov Yu� A��Burkinsky I� B��Loiko N� P��Fedoto- va I� N��Zakharov I� G��Chernyakov A� M��Kupri- enko P� Ya��Makarenko I� B��Legostayeva O� V�� Lebed T� V��Savchenko A� S��Model of deep struc- ture of the Donets folded construction and sur- rounding structures according to the regional geo- physical observations // Geophys. J. — 2009. — 31, � 4. — P. 44—68 (in Russian). Stephenson R. A., Van Weiss Ja. D., Stovba S. N., Shy- manovsky V. A. One-dimensional numerical mo- deling of tectonic immersion of DD within the con- cept of extension of the continental lithosphere by Mac Kenzie // Geophys. J. — 1997. — 19, � 3. — P. 25—41 (in Russian).

Geodynamics of lithosphere as one of the crucial factors of mineral deposits formation of Ukraine

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