{"id":2175,"date":"2023-12-17T19:33:47","date_gmt":"2023-12-17T17:33:47","guid":{"rendered":"http:\/\/www.g-o-f.org.ua\/?page_id=2175"},"modified":"2023-12-21T13:14:24","modified_gmt":"2023-12-21T11:14:24","slug":"8-8","status":"publish","type":"page","link":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2023-44\/8-8\/","title":{"rendered":"POLYCHRONIC-POLYGENIC PARAGENETIC-SPATIAL TITANIUM ORE SYSTEM OF THE SEDIMENTARY COVER OF THE SOUTH-WESTERN PART OF THE KORSUN-NOVOMYRHOROD PLUTON"},"content":{"rendered":"

Yu.V. Kroshko<\/strong>, e-mail: ykrosh.79@ukr.net, https:\/\/orcid.org\/0000-0002-7601-7760<\/a>
\nM.S. Kovalchuk<\/strong>, e-mail: kms1964@ukr.net, https:\/\/orcid.org\/0000-0001-9265-9707<\/a>
\nInstitute of Geological Sciences of the National Academy of Sciences of Ukraine, 01601, O. Honchara Str., 55b, Kyiv, Ukraine<\/p>\n

https:\/\/doi.org\/10.15407\/gof.2023.44.063<\/a><\/p>\n

Information is provided on the titanium-zirconium ore content of the weathered crust and continental and coastal Mesozoic- Cenozoic deposits within the Byrzulivska, Valuivska, Likarivska, Andriivska, Novomyrgorodska, Vytiazivska areas, which are located in the southwestern part of the Korsun-Novomyrhorod pluton within the Novomyrgorod massif. On the basis of the coordinates, description and results of testing wells for the specified areas, a target database was created on the basis of which cartographic constructions were made. The results of studies of the spatial distribution of the thickness of the weathering crust, sands and redeposited kaolins of the Lower Cretaceous within the Byrzulivska, Valuivska, Likarivska, Andriivska areas are presented; sands and redeposited kaolins of the lower-middle Eocene within the boundaries of the Novomyrhorodska area; Quaternary sands within the Vytiazivska area. It was found that the lateral distribution of the thickness of the weathering crust is due to the relief of the surface of the crystalline rocks of the foundation and the partial erosion of the eluvium during the geological development of the territory. Instead, the uneven distribution of the thickness of Mesozoic-Cenozoic sediments is caused by the amount of terrigenous material entering the sedimentation basin, facies conditions of formation, and erosion and redeposition of sediments to higher stratigraphic levels. The lateral distribution of the average content of ilmenite, rutile, and zircon and the correlations between these minerals in the weathering crust, redeposited kaolins, and sands of the specified areas were studied. It was found that the ore bearing of the weathered crust and the Mesozoic-Cenozoic continental and coastal marine sediments is paragenetically and spatially related to each other and is determined by the ore bearing of the crystalline rocks of the foundation. The average content of ilmenite, rutile and zircon in the weathering crust is determined by their average content in the parent rocks of the crystalline basement, in the continental and coastal formations of the Mesozoic and Cenozoic \u2014 by the content of minerals in the weathering crust and intermediate reservoirs (for deposits that do not lie on the weathering crust), facial conditions of formation. As a rule, aureoles of increased mineral content do not coincide spatially, and correlations between their average content are mostly very weak or absent. The obtained results confirm and complement the results of previous studies on ore bearing capacity and prospects for increasing the mineral-raw material base of critical raw materials within the Novomyrhorod massif. Research results can serve as an information base for forecasting, prospecting and mining operations within the investigated areas.<\/p>\n

Keywords:<\/strong> Korsun-Novomyrhorod pluton, Novomyrhorod massif, weathering crust, Lower Cretaceous, Lower Middle Eocene and Quaternary sediments, thickness, ilmenite, rutile, zircon, content, lateral distribution of content.<\/em><\/p>\n

 <\/p>\n

References<\/strong><\/p>\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n
1. Gurskyi, D.S., Esipchuk, K.E., Kalinin, V.I. etc. (2005). Metallic and non-metallic minerals of Ukraine. Metallic minerals. Center of Europe, Kyiv-Lviv. Vol. 1. 785 p. [in Ukrainian].<\/td>\n<\/tr>\n
<\/td>\n<\/tr>\n
2. Kovalchuk, M.S., Kroshko, Yu.V. (2015). Aptian-Lower Albian and Eocene river valleys of the central part of the Ukrainian Shield, Lviv University Bulletin. Geological series, 29, pp. 67-76 [in Ukrainian].<\/td>\n<\/tr>\n
<\/td>\n<\/tr>\n
3. Kovalchuk, M.S., Sukach, V.V. (2018). Spatial-paragenetic, polygenic-polychronic gold ore system of the Solonyan ore field, Tectonics and stratigraphy, No. 45, pp. 123-132 [in Ukrainian].
\nhttps:\/\/doi.org\/10.30836\/igs.0375-7773.2018.170100<\/a><\/td>\n<\/tr>\n
<\/td>\n<\/tr>\n
4. Kroshko, Yu.V. (2016). Digital structural and lithological model of the Birzuliv ilmenite placer (Middle Dnieper region), First independent scientific journal, No. 5 (2), pp.4-7 [in Ukrainian].<\/td>\n<\/tr>\n
<\/td>\n<\/tr>\n
5. Kroshko, Yu. (2016). Digital structural and lithological models of Aptian-Lower Albian and Middle Eocene continental ilmenite placers within the Korsun-Novomyrhorod pluton, Mineral. coll., No. 66, pp. 30-39 [in Ukrainian].<\/td>\n<\/tr>\n
<\/td>\n<\/tr>\n
6. Kroshko, Yu.V. (2016) Ilmenite bearing of Eocene continental formations within Novomyrhorod placer, Materialy tenth sciences readings named after Acad. Evgeny Lazarenko, Lviv, pp. 53-55 [in Ukrainian].<\/td>\n<\/tr>\n
<\/td>\n<\/tr>\n
7. Kroshko, Yu.V. (2016). The ilmenite content of the subduction crust and its erosion products within the upper paleoterra of the Lebedyn-Balakliiv paleovalley (the central part of the Ukrainian shield), Materialy tenth sciences readings named after Acad. Yevhen Lazarenko, Lviv, pp. 55-57 [in Ukrainian].<\/td>\n<\/tr>\n
<\/td>\n<\/tr>\n
8. Kroshko, Yu.V. (2016). Digital structural and lithological models of Lower Cretaceous continental ilmenite placers of the upper paleocurrent of the Lebedyn-Balakliiv paleovalley (central part of the Ukrainian shield). Geoinformatics, 3(59), pp. 49-57 [in Ukrainian].<\/td>\n<\/tr>\n
<\/td>\n<\/tr>\n
9. Kroshko, Yu.V., Kovalchuk, M.S. (2021) Structural and lithological modeling of ilmenite deposits in weathering crusts and products of their erosion and redeposition within the Novomyrgorod titanium-bearing region, Proc. of the All-Ukrainian Conference \u00abFrom Mineralogy and Geognosy to Geochemistry, Petrology, Geology and Geophysics: Fundamental and Applied Trends of the XXI Century\u00bb (MinGeoIntegration XXI), Kyiv, pp. 189-193 [in Ukrainian].
\nhttps:\/\/doi.org\/10.59911\/mgg.2786-7994.2021.2(3).261990<\/a><\/td>\n<\/tr>\n
<\/td>\n<\/tr>\n
10. Kroshko, Yu.V., Kovalchuk, M.S. (2023). Ore-bearing of the Likarivskyi placer (Korsun-Novomyrgorod pluton), Problems of applied geological sciences and ways to overcome them (to the 160th anniversary of the birth of V.I. Vernadsky): Collection of materials of the scientific conference of the National Academy of Sciences of Ukraine, Institute of Geochemistry, Mineralogy and Ore Formation. M.P. Semenenko, pp. 70-74 [in Ukrainian].<\/td>\n<\/tr>\n
<\/td>\n<\/tr>\n
11. Semenenko, N.P., Veklich, M.F. (Ed.). (1967). Titanium and titanium-zirconium placers of the Ukrainian SSR. Kyiv. 850 p. [in Russian].<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n

 <\/p>\n

Download (PDF)<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"

Yu.V. Kroshko, e-mail: ykrosh.79@ukr.net, https:\/\/orcid.org\/0000-0002-7601-7760 M.S. Kovalchuk, e-mail: kms1964@ukr.net, https:\/\/orcid.org\/0000-0001-9265-9707 Institute of Geological Sciences of the National Academy of Sciences of Ukraine, 01601, O. Honchara Str., 55b, Kyiv, Ukraine https:\/\/doi.org\/10.15407\/gof.2023.44.063 Information is provided on the titanium-zirconium ore content of the weathered crust and continental and coastal Mesozoic- Cenozoic deposits within the Byrzulivska, Valuivska, Likarivska, Andriivska, … Continue reading “POLYCHRONIC-POLYGENIC PARAGENETIC-SPATIAL TITANIUM ORE SYSTEM OF THE SEDIMENTARY COVER OF THE SOUTH-WESTERN PART OF THE KORSUN-NOVOMYRHOROD PLUTON”<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":2072,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-2175","page","type-page","status-publish","hentry"],"translation":{"provider":"WPGlobus","version":"3.0.0","language":"gb","enabled_languages":["uk","gb"],"languages":{"uk":{"title":true,"content":true,"excerpt":false},"gb":{"title":true,"content":true,"excerpt":false}}},"jetpack_sharing_enabled":true,"jetpack_shortlink":"https:\/\/wp.me\/P9ghyZ-z5","jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":2124,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2023-44\/4-4\/","url_meta":{"origin":2175,"position":0},"title":"GEOCHEMISTRY OF FLUORINE OF SEDIMENTARY ROCKS OF DIFFERENT MASSES OF THE CARPATIAN BIOSPHERE RESERVE","author":"admin","date":"17\/12\/2023","format":false,"excerpt":"{:uk}{:uk}{:uk}{:uk} {:uk}\u041d.\u041e. \u041a\u0440\u044e\u0447\u0435\u043d\u043a\u043e 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https:\/\/orcid.org\/0000-0001-5202-4045 \u0412.\u0412. \u0421\u0443\u043a\u0430\u0447 2 E-mail: svital@ukr.net; https:\/\/orcid.org\/0000-0002-4710-7230 \u041c.\u041e. \u0414\u043e\u043d\u0441\u044c\u043a\u0438\u0439 2 E-mail: nikkolai.donskoy@gmail.com; https:\/\/orcid.org\/0000-0002-3037-6346 \u041e.\u0411. \u0411\u043e\u043d\u0434\u0430\u0440\u0435\u043d\u043a\u043e 2 1 \u041f\u0417\u0415 \u2116 46, \u041a\u041f \u00ab\u041a\u0456\u0440\u043e\u0432\u0433\u0435\u043e\u043b\u043e\u0433\u0456\u044f\u00bb, 55222, \u0441\u043c\u0442 \u041f\u0456\u0434\u0433\u043e\u0440\u043e\u0434\u043d\u0430, \u041f\u0435\u0440\u0432\u043e\u043c\u0430\u0439\u0441\u044c\u043a\u0438\u0439 \u0440-\u043d, \u041c\u0438\u043a\u043e\u043b\u0430\u0457\u0432\u0441\u044c\u043a\u0430 \u043e\u0431\u043b., \u0423\u043a\u0440\u0430\u0457\u043d\u0430 2 \u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u0433\u0435\u043e\u0445\u0456\u043c\u0456\u0457, \u043c\u0456\u043d\u0435\u0440\u0430\u043b\u043e\u0433\u0456\u0457 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\u041a\u0440\u044e\u0447\u0435\u043d\u043a\u043e1E-mail: nataliya.kryuchenko@gmail.com, https:\/\/orcid.org\/0000-0001-8774-9089\u0415.\u042f. \u0416\u043e\u0432\u0438\u043d\u0441\u044c\u043a\u0438\u04391E-mail: zhovinsky@ukr.net, https:\/\/orcid.org\/0000-0003-1601-5998\u041f.\u0421. \u041f\u0430\u043f\u0430\u0440\u0438\u0433\u04302E-mail: paparyga.ps@ukr.net, https:\/\/orcid.org\/0000-0002-4021-0809\u041e.\u0410. \u0416\u0443\u043a1E-mail: igmof.zhuk@gmail.com, https:\/\/orcid.org\/0000-0002-5264-0750\u041c.\u0412. \u041a\u0443\u0445\u0430\u04401E-mail: mvk3@ukr.net, https:\/\/orcid.org\/0000-0003-3572-5194\u041a.\u0415. \u0414\u043c\u0438\u0442\u0440\u0435\u043d\u043a\u043e1E-mail: zovin.kosta@gmail.com, https:\/\/orcid.org\/0000-0003-1001-3457\u0422.\u0410. \u041f\u043e\u043f\u0435\u043d\u043a\u043e1E-mail: tanya_simple@ukr.net1. \u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u0433\u0435\u043e\u0445\u0456\u043c\u0456\u0457, 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\u0441\u0435\u0440\u0435\u0434\u043e\u0432\u0438\u0449\u0430 \u0423\u043a\u0440\u0430\u0457\u043d\u043890600, \u0432\u0443\u043b. \u041a\u0440\u0430\u0441\u043d\u0435 \u041f\u043b\u0435\u0441\u043e,\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":1926,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2021-42\/1-7\/","url_meta":{"origin":2175,"position":4},"title":"URANIUM-LEAD GEOCHRONOLOGY ON MONACITE OF GRANITES OF THE LYPNYAZKA MASSIF AND ITS FRAMING (INGUL MEGABLOCK OF THE UKRAINIAN SHIELD)","author":"admin","date":"15\/12\/2021","format":false,"excerpt":"{:uk}\u041b.\u041c. \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a 1https:\/\/orcid.org\/0000-0001-5591-5169E-mail: stepaniuk@nas.gov.ua\u0421.\u0406. \u041a\u0443\u0440\u0438\u043b\u043e 2E-mail: kurylo.sergiy@gmail.com;https:\/\/orcid.org\/0000-0003-4466-6851\u0412.\u041e. \u0421\u044c\u043e\u043c\u043a\u0430 1E-mail: syomka1949@gmail.com;https:\/\/orcid.org\/0000-0001-5202-4045\u0422.\u0406. \u0414\u043e\u0432\u0431\u0443\u0448 1https:\/\/orcid.org\/0000-0002-3512-3313E-mail: tetyana.dovbush1@gmail.com\u0421.\u041c. \u0411\u043e\u043d\u0434\u0430\u0440\u0435\u043d\u043a\u043e 1E-mail: sbond.igmr@gmail.com;\u00a0https:\/\/orcid.org\/0000-0001-7948-3583\u041e.\u0412. \u041a\u043e\u0432\u0442\u0443\u043d 1, 3E-mail: kovtun85@ukr.net;https:\/\/orcid.org\/0000-0003-0475-8778\u0406.\u041c. \u041a\u043e\u0442\u0432\u0456\u0446\u044c\u043a\u0430 1E-mail: irinakotvitska@gmail.com1. \u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u0433\u0435\u043e\u0445\u0456\u043c\u0456\u0457, \u043c\u0456\u043d\u0435\u0440\u0430\u043b\u043e\u0433\u0456\u0457 \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f \u0456\u043c\u0435\u043d\u0456 \u041c.\u041f. \u0421\u0435\u043c\u0435\u043d\u0435\u043d\u043a\u0430 \u041d\u0410\u041d \u0423\u043a\u0440\u0430\u0457\u043d\u043803142, \u043f\u0440\u043e\u0441\u043f. \u0430\u043a\u0430\u0434. \u041f\u0430\u043b\u043b\u0430\u0434\u0456\u043d\u0430, 34, \u041a\u0438\u0457\u0432, \u0423\u043a\u0440\u0430\u0457\u043d\u04302. \u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u043d\u0430\u0443\u043a \u043f\u0440\u043e \u0417\u0435\u043c\u043b\u044e \u0421\u043b\u043e\u0432\u0430\u0446\u044c\u043a\u0430 \u0430\u043a\u0430\u0434\u0435\u043c\u0456\u044f \u043d\u0430\u0443\u043a97401, \u0414\u0443\u043c\u0431\u0456\u0454\u0440\u0441\u044c\u043a\u0430, 1, \u0411\u0430\u043d\u0441\u044c\u043a\u0430-\u0411\u0438\u0441\u0442\u0440\u0438\u0446\u044f, \u0421\u043b\u043e\u0432\u0430\u0447\u0447\u0438\u043d\u04303.\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":1994,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2022-43\/2-2\/","url_meta":{"origin":2175,"position":5},"title":"URANIUM-LEAD ISOTOPIC AGE OF MONAZITES OF PLAGIOGNEYSES OF THE INGULO-INGULETSE SERIES (INGUL MEGABLOCK OF THE UKRAINIAN SHIELD)","author":"admin","date":"20\/12\/2022","format":false,"excerpt":"{:uk} \u041b.\u041c. \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a 1E-mail: stepaniuk@nas.gov.ua, https:\/\/orcid.org\/0000-0001-5591-5169\u041e.\u0411. \u0412\u0438\u0441\u043e\u0446\u044c\u043a\u0438\u0439 1E-mail: alek.vysotsky@gmail.com, https:\/\/orcid.org\/0000-0002-3542-4685\u041e.\u0412. \u041a\u043e\u0432\u0442\u0443\u043d 1E-mail: kovtun85@ukr.net; https:\/\/orcid.org\/0000-0003-0475-8778\u0421.\u0406. \u041a\u0443\u0440\u0438\u043b\u043e 2\u0415-mail: kurylo.sergiy@gmail.com, https:\/\/orcid.org\/0000-0003-4466-6851\u0422.\u0406. \u0414\u043e\u0432\u0431\u0443\u0448 1E-mail: tetyana.dovbush1@gmail.com, https:\/\/orcid.org\/0000-0002-3512-33131. \u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u0433\u0435\u043e\u0445\u0456\u043c\u0456\u0457, \u043c\u0456\u043d\u0435\u0440\u0430\u043b\u043e\u0433\u0456\u0457 \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f \u0456\u043c. \u041c.\u041f. \u0421\u0435\u043c\u0435\u043d\u0435\u043d\u043a\u0430 \u041d\u0410\u041d \u0423\u043a\u0440\u0430\u0457\u043d\u043803142, \u043f\u0440\u043e\u0441\u043f. \u0430\u043a\u0430\u0434. \u041f\u0430\u043b\u043b\u0430\u0434\u0456\u043d\u0430, 34, \u041a\u0438\u0457\u0432, \u0423\u043a\u0440\u0430\u0457\u043d\u04302. \u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u043d\u0430\u0443\u043a \u043f\u0440\u043e \u0437\u0435\u043c\u043b\u044e, \u0421\u043b\u043e\u0432\u0430\u0446\u044c\u043a\u0430 \u0430\u043a\u0430\u0434\u0435\u043c\u0456\u044f \u043d\u0430\u0443\u043a 97411, \u0414\u0443\u043c\u0431\u0456\u0454\u0440\u0441\u044c\u043a\u0430, 1, \u0411\u0430\u043d\u0441\u044c\u043a\u0430 \u0411\u0438\u0441\u0442\u0440\u0438\u0446\u044f,\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar 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