DOI: https://doi.org/10.24028/gzh.0203-3100.v38i3.2016.107777

Structural-petrophysical and tectonophysical base of geological map of crystalline basement of the central part of Golovanevsk suture zone of the Ukrainian Shield

O. B. Gintov, V. A. Entin, S. V. Mychak, V. N. Pavlyuk, V. V. Zyultsle

Abstract


One of the most important areas of geological and geophysical studies of the Ukrainian shield (Ush) — estimation of the prospects of the Golovanevsk suture zone (GSZ) for the ferrous, non-ferrous, precious and rare metals and diamonds has been considered here.  The central part of GSZ (CPGSZ) is an essential part of the Pobuzhya mining area. The Earth’s crust of the CPGSZ (Pervomaisk- Golovanevskiy-region) is transpierced with mafic-ultramafic intrusions and extrusions, in paragenesis with which there are iron-carbonate ore series and ferruginous quartzites, chromite-bearing peridotites. The CPGSZ is currently the most promising and uniform throughout the central and western parts of the Ukrainian Shield region with wide occurrences of gold mineralization. In addition, manifestations of platinoids, rare earths, yttrium, uranium, manganese, titanium, tungsten, copper, molybdenum, apatite, sillimanite, vermiculite, serpentinite refractories, dinas quartzites, primary kaolin, mineral waters are found within this area. Pyrope and diamonds are also met in schlich samples collected in the basins of the  Southern Bug, Sinyukha, Yatran rivers.

It is shown that the reasons of weakly efficient search operations conducted in the region are not only in an extremely weak state of their financial support, but also in the absence of an updated concept of the geological structure of the GSZ. Geological maps of scale 1: 50 000, built on the results of the survey made here in the 60—70ieth, were based on outdated petrological data. Maps in the scale 1: 200 000, built later on the structural-formational basis, do not reflect in enough details the real composition of geologic complexes, as they insufficiently use the possibility of detailed geophysical surveys. The area of CPGSZ is poorly lit by the data of the present isotopic-geochronological studies.

It is proposed to begin evaluating CPGSZ prospects for building an up-to-date geological map of its crystalline basement on the basis of the present petrographic, petrological, geochemical and geophysical data, as well as current isotopic age of rocks. The article presents the structural and petrophysical, and tectonophysical basis of such a map that reflects the geological and petrophysical taxa and structural and kinematic data for the surface of the Precambrian basement in the region. The principles of the construction of the foundation and a brief analysis of its content have been developed here.


Keywords


Ukrainian Shield; Medium Pobuzhye; geological map; petrophysics; tectonophysics; ultrabasites; iron ore; diamonds

References


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

Bornyakov S. A., 1980. Modelling of shear zones in viscoelastic materials. Geologiya i geofizika (11), 75—84 (in Russian).

Geological map of the crystalline base of the scale of 1 : 200 000. Sheet M-36-XXXI (Pervomaisk), 1990. Kiev: Foundation of GP "Ukrainian Geological Company" (in Russian).

Geological Dictionary, 1973. Moscow: Nedra, Vol. 2, 456 p. (in Russian).

Geological and geophysical model of Krivoy Rog-Kremenchug suture zones of the Ukrainian Shield, 2006. Ed. A. V. Antsiferov. Kiev: Naukova Dumka, 196 p. (in Russian).

Geological and geophysical model of Golovanevsky suture zones of the Ukrainian Shield, 2008. Ed. A. V. Antsiferov. Kiev: Naukova Dumka, 308 p. (in Russian).

Geochronology of Early Precambrian of the Ukrainian Shield. Archean, 2005. Ed. N. P. Shcherbak. Kiev: Naukova Dumka, 244 p. (in Russian).

Geochronology of Early Precambrian of the Ukrainian Shield. Proterozoic, 2008. Ed. N. P. Shcherbak. Kiev: Naukova Dumka, 240 p. (in Russian).

Gintov O. B., 2012. Ukrainian Precambrian shield and plate tectonics. Geofizicheskiy zhurnal 34(6), 3—21 (in Russian).

Gintov O. B., 2005. Field Tectonophysics and its application in the study of the deformation of the Earth’s crust of Ukraine. Kiev: Feniks, 572 p. (in Russian).

Gintov O. B., 2015. Problems of Ukrainian Precambrian geodynamics. Geofizicheskiy zhurnal 37(5), 3—21 (in Russian).

Gintov O. B., 2014. Scheme of stage periodizations of faulting in the Earth’s crust of the Ukrainian shield — new data and investigations. Geofizicheskiy zhurnal 36(1), 3—18 (in Russian).

Gintov O. B., Gonchar V. V., 2004. Modelling of intra- and near-fault folds in Precambrian complexes from the position of misalignment progressive deformation. Geofizicheskiy zhurnal 26(2), 62—72 (in Russian).

Gintov O. B., Yentin V. A., Isay V. M., 1985.New data about the features of the formation of the folded structure of magnetite deposits of the Middle Bug. Doklady AN USSR. Ser. B (4), 15—17 (in Russian).

Gintov O. B., Yentin V. A., Isay V. M., 1984. About kinematics of Yadlov-Traktemirovsky fault. Geofizicheskiy zhurnal 6(6), 43—48 (in Russian).

Gintov O. B., Isay V. M. 1988. Tectonophysical studies of consolidated crust faults. Kiev: Naukova Dumka, 228 p. (in Russian).

Gintov O. B., Isay V. M., Kovalenko V. N. 1990.Tectonophysical data on the mechanism of formation of folds of the first order of the Kryvyi Rig basin on the example of Lihmanovska structure. Geologicheskiy zhurnal (5), 115—123 (in Russian).

Gintov O. B., Mychak S. V., 2011a. Geodynamic development of Ingul megablock of the Ukrainian Shield on geological and geophysical and tectonic data. I. Geofizicheskiy zhurnal 33(3), 102—118 (in Russian).

Gintov O. B., Mychak S. V., 2011b. Strained state and deformation of the Earth’s crust of the central part of the Ingul megablock according to Materials of tectonophysical study of Novoukrainsky massif. Geofizicheskiy zhurnal 33(2), 28—45 (in Russian).

Gintov O. B., Pashkevich I. K., 2010.Tectonophysical analysis and geodynamic interpretation of three-dimensional geophysical model of the Ukrainian shield. Geofizicheskiy zhurnal 32(2), 3—27 (in Russian).

Glevasskiy E. B., 2005.The solution of some problems of petrology and stratigraphy of the Ukrainian shield from the standpoint of plate tectonics. Mineralogicheskiy zhurnal 27(3), 57—66 (in Russian).

Glevasskiy E. B., Kalyaev G. I., 1998. Precambrian and plate tectonics (the problem of plate tectonic reconstructions of the south-western segment of the East European Platform). In: Geology and stratigraphy of Precambrian Ukrainian Shield. Kiev, P. 38—40 (in Russian).

Glevasskiy E. B., Kalyaev G. I., 2000. Tectonics of the Precambrian Ukrainian Shield. Mineralogicheskiy zhurnal (2), 77—91 (in Russian).

Gonchar V. V., 2001. Progressive deformation and misalignment issues of diagnosis structures. Dopovidi NAN Ukrainy (9), 108—114 (in Russian).

State geological map of Ukraine. Scale 1 : 200 000. Geological map and a map of minerals of the crystalline basement. Central Ukrainian series. Letter M-36 XXXI (Pervomaysk), 2004. Kiev: Ministry of ecology and mineral resources of Ukraine, State Geologіcal Service (in Ukrainian).

Dobrohotov M. N., Gintov O. B., Yentin V. A., Solonina I. N., 1971. The report on the theme: "The synthesis and reinterpretation of geological and geophysical data on the Ukrainian shield to determine areas perspective on iron". Kiev: Geolfond, 412 p. (in Russian).

Yentin V. A., 2005. Geophysical base of tectonic map of Ukraine in scale 1 : 1 000 000. Geofizicheskiy zhurnal 27(1), 74—84 (in Russian).

Yentin V. A., 2012.Natural geophysical phenomena in Ukraine. Kiev: Publ. House of UkrGGRI, 76 p. (in Russian).

Yentin V. A., 1987. Abstract of thesis for the degree of geological-mineralogical sciences. Kiev. 32 p. (in Russian).

Yentin V. A., Gintov O. B., Mychak S. V., Yushin A. A., 2015. The structure of the Moldovian iron ore deposits (Ukrainian shield) on geological and geophysical data and its possible endogenous nature. Geofizicheskiy zhurnal 37(4), 3—18 (in Russian).

Zavoyskiy V. I., 1982. Using of tensor of magnetic susceptibility for the solutions of structural geology problems. Izvestiya AN SSSR. Ser. Fizika Zemli (3), 76—84 (in Russian).

Zaika-Novatskiy V. S., 1986. Structural analysis and development of the Ukrainian shield stratigraphic scheme. Geologicheskiy zhurnal 46(3), 6—10 (in Russian).

Kanevskiy A. Ya., Gintov O. B., 1972. Finding of a new species of iron ore in the Bug area of the Ukrainian shield. Geologicheskiy zhurnal 32(is. 5), 140—141 (in Russian).

Kropotkin P. N., 1973.The tectonic stresses in the Earth's crust according to direct measurements. Stress state of the Earth's crust. Moscow: Nauka, P. 21—31 (in Russian).

Krutikhovskaya Z .A., Pashkevich I. K., Silina I. M., 1977. Map of the anomalous magnetic field of the Ukrainian shield at a scale of 1 : 50 000. Kiev, 100 p. (in Russian).

Kuprienko P. Ya., Makarenko I. B., Starostenko V. I., Legostaeva O. V., 2007. 3D density model of the Earth’s crust and upper mantle of the Ukrainian shield. Geofizicheskiy zhurnal 29(5), 3—27 (in Russian).

Lebedev T. S., Korchin V. A., Savenko B. Ya., Shapoval V. I., Shepel S. I., 1986. Physical properties of mineral substance in the lithospheric thermobaric conditions. Kiev: Naukova Dumka, 200 p. (in Russian).

Lukiyenko O. I., 2001. Morphological tectonics (on tektonofacial basis). Tutorial. Kyiv: Publ. House of the Kiev University, 66 p. (in Ukrainian).

Lukiyenko O. I., 2002. Structural Geology with bases of paragenetic structural analysis. Textbook. Kyiv: Publ. House “Kyiv University”, 366 p. (in Ukrainian).

Lukiyenko O. I., Kravchenko D. V., Sukhorada A. V., 2008. Dislocation tectonics and tektonofaces of Precambrian Ukrainian Shield. Kyiv: Publ. House "Kyiv University", 279 p. (in Ukrainian).

Guidelines and requirements for the results of the integrated interpretation of geological and geophysical data within the Ukrainian Shield. 1999. Kiev: Publ. House of the Scientific Methodical Center of Geolkom of Ukraine, 45 p. (in Russian).

Mychak S. V. 2015. Kinematics of the formation of the western and central parts of Ukrainian shield from 2.05 to 2.02 Ga. Geofizicheskiy zhurnal 37(1), 83—99 (in Russian).

Pavlyuk V. M., Bobrov O. B., Visots’kyy B. L., Dovhan’ R. M., Zhovyns’kyy E. Ya., Kostenko M. M., Lykov L. І., Tsymbal S. M., 2008. Report "Geology, petrology, geochemistry, age and ore-bearing of mafіt-ultramafіt associations of the Western part of the Ukrainian Shield". Kiev: Foundation of State Enterprise "Ukrainian Geological Company", 683 p. (in Russian).

Patalakha E. I., Lukiyenko A. I., Gonchar V. V., 1995. Tectonic flows as a basis for understanding of the geological structures. Kiev: Feniks, 151 p. (in Russian).

Petrographic dictionary, 1963. Ed. G. D. Afanasyev. Moscow: Gosgeoltekhizdat, 447 p. (in Russian).

Stepanyuk L. M., 1999. Sequence of manifestations of geological processes in rocks of the Bug series. Mineralogicheskiy zhurnal (5/6), 86—92 (in Russian).

Stepanyuk L. M., Bibikova E. V., Klaessen S., Ponomarenko A. N., Dovbush T. I., Fedotova A. A., 2010. On the question of age lines of forming Kosharo-Alexandrov suite of the Bug series of Pobujya. Abstracts of the International scientific-practical conference "The stratigraphy, geochronology and correlation of lower Precambrian rock complexes of the foundation of the East-European platform." Kiev: UkrNIGRI, 252 p. (in Russian).

Terkot D., Schubert J., 1985. Geophysics. Part II. Moscow: Mir, 730 p. (in Russian).

Usenko O. V., 2015. Conditions of formation of ferruginous rocks of the Middle Pobuzh’ya. Geofizicheskiy zhurnal 37(4), 32—50 (in Russian).

Shakina K. A., Skakun L. Z., 2010. Mineral composition and processes of formation of graphite containing rocks of Zavallya graphite deposits. Abstracts of the International scientific-practical conference "The stratigraphy, geochronology and correlation of Lower Precambrian rock complexes of the basement of the East European platform". Kiev: UkrNIGRI, 252 p. (in Ukrainian).

Sherman S. I., Bornyakov S. A., Buddo V. Yu., 1983. Areas of dynamic influence of faults (simulation results). Novosibirsk: Nauka, 112 p. (in Russian).

Schuldiner V. I., 1982. Precambrian basement of the Pacific belt and flanking platforms. Moscow: Nedra, 226 p. (in Russian).

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

Yushin A. A., 2015. On the prospects of identifying magmatogenic hydrothermal iron ore formations in the Ukrainian Shield. Geofizicheskiy zhurnal 37(4), 19—31 (in Russian).

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

Bogdanova S. V., Gintov O. B., Dzmitry M., Kurlovich C., Lubnina L. V., Mimmi K., Nilsson M., Orlyuk M. I., Pashkevich I. K., Shumlyansky L. V., Starostenko V. I., 2012. Late Palaeoproterozoic mafic dyking in the Ukrainian Shield of Volgo-Sarmatia caused by rotations during the assembly of supercontinent Columbia (Nuna). Lithos 174, 196—216.

Chardon D., Gapais D. Cagnard F., 2009. Flow of ultra-hot orogens: a view from the Precambrian, clues for the Phanerozoic. Tectonophysics 477, 105—118.