{"id":980,"date":"2018-12-10T14:37:52","date_gmt":"2018-12-10T12:37:52","guid":{"rendered":"http:\/\/www.g-o-f.org.ua\/?page_id=980"},"modified":"2020-10-02T19:12:13","modified_gmt":"2020-10-02T16:12:13","slug":"5-2","status":"publish","type":"page","link":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2018-39\/5-2\/","title":{"rendered":"The Geochemical Aspects of the Origin of Ore-Bearing Albitites of the Novokonstantinovka Uranium Deposit"},"content":{"rendered":"

Mihalchenko I.I.1<\/sup>, Larikov A.L.2<\/sup>, Zaiats O.V.2<\/sup><\/strong>
\n1 – State institution Institute of Environmental Geochemistry of the National Academy of Sciences of Ukraine
\n2 – M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Science of Ukraine<\/p>\n

Language: Ukrainian
\nGeochemistry and ore formation 2018, 39: 53-65<\/p>\n

https:\/\/doi.org\/10.15407\/gof.2018.39.053<\/a><\/p>\n

According to the results of the study, it was confirmed that a sampling of values of measurements of decimal logarithms of uranium mass fractions in Precambrian albitites of the Novokostyantinovsky deposit of the Central Ukrainian Uranium Region of Ukrainian Shield is statistically inhomogeneous and consists of four groups, which estimated medians of uranium mass fractions are much higher than the geochemical background of uranium of the initial granite. The sampling of decimal logarithms of measured values of thorium mass fraction (without taking into account the values of the fourth group on the value of uranium measurements) is statistically homogeneous with the estimation of the sample median, which is close to the geochemical background of this chemical element of the initial granite. It appears that the variation in the measured values of thorium mass fraction is a consequence of thorium local redistribution from original granite in the process of albitites formation. The high values of measured thorium mass fraction and the high correlation between uranium and thorium in the fourth group (the intersection of rich ores on the deep horizon) are the basis for confirming the co-occurrence and concentration of these elements in common minerals
\nin the deep (high-temperature) part of the pneumatolithic and hydrothermal column. It is assumed that change of oxidation degree of U in the ore-bearing fluids of uranium sodium metasomatites with U4+ (in high-temperature (>350 \u00b0C) conditions) on U6+ (at medium to low temperature (<250 \u00b0C) conditions) is possible. This substantiates the endogenous origin of ore-bearing fluids in uranium-bearing sodium metasomatites formation. It is suggested to consider the deep magmatic cell, the magmatic differentiates of which were formed Korsun-Novomirgorod anorthosite – rapacivi granite pluton, in particular, pneumatolithic and hydrothermal – formation of uranium (ore-bearing) sodium metasomatites, as the probable source of fluids.
\nKeywords: uranium, thorium, classification, ore, albitites, genesis, Novokostyantinovska uranium deposit.<\/em><\/p>\n

Reference
\n1. Belevtsev, Ya.N. (1979). Metamorphogenic ore formation. M.: Nedra. 259 p. [in Russian].<\/p>\n

2. Belevtsev, Ya.N., Sukhinin, A.N. (1974). Some mineral, geochemical and genetical peculiarities of granitoids in the central part of the Ukrainian shield. Geol. Journ. 1. P. 16-33 [in Russian].<\/p>\n

3. Bondarenko, S.M., Stepaniuk, L.M., Ivanov, B.N., Somka, V.O., Kurylo, S.I., Hrinchenko, O.V. (2015). Typomorfizm and Age of pitchblende from deep horizon of the Vatutinka ore deposit. Suchasna heolohichna nauka i praktyka v doslidzhenniakh studentiv i molodykh fakhivtsiv: Materialy Vseukrainskoi naukovo-praktychnoi konferentsii. Kryvorizkyi natsionalnyi universytet, 26-28 bereznia 2015, pp. 122-127. [in Ukrainian].<\/p>\n

4. Vernadskiy, V.I. (1934). Ocherki geohimii, 4-e izd., Moskow-Leningrad-Groznyiy-Novosibirsk: Gosudarstvennoe nauchno-tehnicheskoe gorno-geologo-neftyanoe izdatelstvo, 380 p. [in Russian].<\/p>\n

5. Voinovskyi, A.S., Zhuzhoma, V.M., Kalinina, H.V., Lobanova, L.A., Churubova, S.S. (2006). Methodical recommendations for the compilation of geochemical maps (geochemical specialization of the geological formations of the Precambrian basement and predictive-geochemical) scale 1 : 200000 and 1 : 50,000 in relation to the conditions of the Ukrainian shield. Guidelines]. Kyiv. UkrDHRI, 96 p. [in Ukrainian].<\/p>\n

6. Volfson, F.I., Korolyov, K.G. (1990). Conditions for the formation of uranium deposits. Moskow. Nedra, 288 p. [in Russian].<\/p>\n

7. Belevtsev, Ya.N., Koval, V.B. (Eds). (1995). Genetic types and conformities to law of placing of uranium deposits of Ukraine. Kyiv: Nauk. dumka. 396 p. [in Russian].<\/p>\n

8. Scherbak, N.P., Artemenko, G.V., Les naya, I.M., Ponomarenko, A.N., Shumlyanskiy, L.V. (2008). Geochronology of early Precambrian of the Ukrainian shield. Proterozoic. Kyiv: Nauk. dumka. 240 p. [in Russian].<\/p>\n

9. Derzhavna heolohichna karta Ukrainy (2001). Masshtab 1:200 000. Tsentralnoukrainska seriia. Arkush M-36-XXXII (Novoukrainka). Kyiv, Departament heolohii ta vykorystannia nadr. 119 p.<\/p>\n

10. Iemets, O.V., Ponomarenko, O.M., Kiuni, M., Petrychenko, K.V., Shcherbak, D.M., Sineliu S. (2007). Mineralogical and geochemi cal features and the age of uranium constriction of the Kirovograd block albitates on the example of Novokostyantinivska uranium-bearing area (Novoukrainian granite massif, Ukrainian shield). Mineral. Journ. 29, No. 2, pp. 102-110 [in Ukrainian].<\/p>\n

11. Zhukov, M.N. (2008). Mathematical statistics and processing of geological data. Kyiv. 518 p. [in Ukrainian].<\/p>\n

12. Zaiats, O.V. (2017). Geochemistry of Ruska-Polyana rare-metal granitoids of the Korsun-Novomyrgorod pluton. On the rights of the manuscript. Kyiv. 20 p. [in Ukrainian].<\/p>\n

13. Zaiats, O.V. (2015). Geochemistry of Ruska-Polyana Rare-Metal Granites of Korsun-Novomyrgorod Pluton (Ingul Megablock, the Ukrainian Shield). Mineral. journ. 37, No. 3, pp. 67-77 [in Ukrainian].
\nhttps:\/\/doi.org\/10.15407\/mineraljournal.37.03.067<\/a><\/p>\n

14. Ivanov, B.N., Stepanyuk, L.M., Donskoy, N.A., Syomka, V.A., Bondarenko, S.N., Shevela A.Yu. (2017). Types of ore fields of the Central Ukrainian Uranium District and their comparative characteristics. Geochemistry and Ore Formation. 38, pp. 70-79 [in Russian].
\nhttps:\/\/doi.org\/10.15407\/gof.2017.38.070<\/a><\/p>\n

15. Komarov, A.N., Cherkashin, L.A. (1991). Rare metallic tectonic and metasomatic zones of the Ukrainian Shield. Kyiv: Nauk. dumka. 180 p. [in Russian].<\/p>\n

16. Krupennikov, V.A. (2008). Mantle alkaline fluid-magmatic petrogenesis as the main ore-forming process. Uran: resursyi i proizvodstvo: Tez. vtorogo mezhdunarodnogo simpoziuma (Moskow, 26-28 noyabrya 2008). Moskow, pp. 28-31 [in Russian].<\/p>\n

17. Kudryavtsev, V.E. (1991). The law of hydatogenic ore formation in the hypergenesis zone. Geologiya rudnyih mestorozhdeniy. No. 6, pp. 89-99 [in Russian].<\/p>\n

18. Kushev, V.G. (1972). Schelochnyie metasomatityi dokembriya. Leningrad: Nedra. 189 p. [in Russian].<\/p>\n

20. M\u0456halchenko, I.I. (2016). Correlation of Uranium and Thorium in Ore Albitites of the Partyzan Deposit, the Ukrainian Shield. Mineral. journ. 38. No. 4, pp. 54-65. [in Ukrainian].
\nhttps:\/\/doi.org\/10.15407\/mineraljournal.38.04.054<\/a><\/p>\n

21. Mihalchenko, \u0406.\u0406., Andreiev O.V., Zagorodn\u0456i, V.V., Zayats, O.V. (2016). Modeling migration of chemical elements during formation of thorium-uranium ore-bearing albitites of the Novooleksiivka oredeposit, Central-Ukrainian uranium orebearing district of The Ukrainian Shield. Geochemistry and Ore Formation. 37, pp. 86-99 [in Ukrainian].
\nhttps:\/\/doi.org\/10.15407\/gof.2016.37.086<\/a><\/p>\n

22. M\u0456halchenko, I.I., Andreiev O.V. (2017). Monazites in the Thorium-Uranium Ore-Bearing Albitites of the Novo \u2013oleksiivka Ore Deposit (the Ukrainiane Shield). Geochemistry and Ore Formation. 38, pp. 32-49 [in Ukrainian].
\nhttps:\/\/doi.org\/10.15407\/gof.2017.38.032<\/a><\/p>\n

24. Obrizanov, V.N. Basic features of the geochemistry of Vatutinka uranium deposit and some problems of sodium metasomatites. Cand. geol.-mineral. sci. dis. Berezovka, 27 p. [in Russian].<\/p>\n

25. Naumov, G.B., Vlasov, B.P., Golubev, V.N., Mironova O.F. (2017). The Schlema-Alberoda five-element uranium deposit, Germa ny: An example of self-organizing hydrothermal system. Geologiya rudnyih mestorozhdeniy. 59. No. 1, pp. 3-16 [in Russian].<\/p>\n

26. Ronenson, B.M., Royzenman, V.M., Ortenberg, N.A. (1976). Methods for dismembering metamorphic complexes. Leningrad: Nedra. 191 p. [in Russian].<\/p>\n

27. Ryibalov, B.L., Omelyanenko, B.I. (1986). Sources of ore material of endogenous uranium deposits. Moskow: Nauka. 275 p. [in Russian].<\/p>\n

28. Stepaniuk, L.M., Bondarenko, S.M., Somka, V.O., Kotvitska, I.M., Andreiev, O.V. (2012). Source of sodium and uranium of uraniferous albitites (on the example of Lokuchaevka deposit of ingul megablock of USh). Geochemistry and Ore Formation. 31-32, pp. 99-104 [in Ukrainian].<\/p>\n

29. Shestopalova, O.Ye. (2017). Geochronology of Korsun-Novomirgorod Pluton. Kyiv. 20 p. [in Ukrainian].<\/p>\n

30. Shmuraeva, L.Ya. (1991). Genetic model of the formaition of carbonate alkaline metasomatites in fault zones. Blagoveschensk. 24 p. (Preprint\/DVO AN SSSR. AmurKNII DVO AN SSSR).[in Russian].<\/p>\n

31. Fraley, C., Raftery, A., Scrucca, L. (2012). Mclust Version 4 for R: Normal Mixture Modeling for Model-Based Clus te ring, Classification, and Density Estimation. Technical Report 597. Department of Statistics. University of Washington. 57 p.<\/p>\n

32. Mihalchenko, I.I., Shumlyanskyy, L.V., Soesoo, A. (2016). Rare earth elements in Th-U-bearing albitites of the Novooleksiivka occurrence, the Ukrainian Shield. Problemi teoretichnoyi i prikladnoyi mineralogiyi, geologiyi, metalogeniyi girnichovidobuvnih regioniv. Kriviy Rig, pp. 34-38.<\/p>\n

33. Shumlyanskyy, L., Mitrokhin, O., Billstrom, K., Ernst, R., Vishnevska, E., Tsymbal, S., Cuney, M., Soesoo, A. (2015). The ca. 1.8 Ga mantle plume related magmatism of the central part of the Ukrainian shield. GFF. XX. No. X, pp. 1-17.<\/p>\n

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

Mihalchenko I.I.1, Larikov A.L.2, Zaiats O.V.2 1 – State institution Institute of Environmental Geochemistry of the National Academy of Sciences of Ukraine 2 – M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Science of Ukraine Language: Ukrainian Geochemistry and ore formation 2018, 39: 53-65 https:\/\/doi.org\/10.15407\/gof.2018.39.053 According to the results … Continue reading “The Geochemical Aspects of the Origin of Ore-Bearing Albitites of the Novokonstantinovka Uranium Deposit”<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":954,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-980","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-fO","jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":1889,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2021-42\/1-1\/","url_meta":{"origin":980,"position":0},"title":"GEOCHEMICAL CHARACTERISTICS OF NOVOKOSTIANTYNIVKA URANIUM DEPOSIT","author":"admin","date":"15\/12\/2021","format":false,"excerpt":"{:uk} \u0413\u0415\u041e\u0425\u0406\u041c\u0406\u0427\u041d\u0406 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DISTRIBUTION OF URANIUM OF ALBITITES OF THE NOVOKOSTIANTYNIVKA AND THE PARTYZANSKE DEPOSITS","author":"admin","date":"17\/12\/2023","format":false,"excerpt":"{:uk}{:uk}\u041c.\u041e. \u0414\u043e\u043d\u0441\u044c\u043a\u0438\u0439 1 Email: nikkolai.donskoy@gmail.com; https:\/\/orcid.org\/0000-0002-3037-6346 \u0412.\u041e. \u0421\u044c\u043e\u043c\u043a\u0430 1 Email: syomka1949@gmail.com; https:\/\/orcid.org\/0000-0001-5202-4045 \u0412.\u0412. \u0421\u0443\u043a\u0430\u0447 1 E-mail: svital@ukr.net; https:\/\/orcid.org\/0000-0002-4710-7230 \u0411.\u041d. \u0406\u0432\u0430\u043d\u043e\u0432 2 \u0421.\u041c. \u0411\u043e\u043d\u0434\u0430\u0440\u0435\u043d\u043a\u043e 1 E-mail: sbond.igmr@gmail.com; https:\/\/orcid.org\/0000-0001-7948-3583 \u0412.\u041c. \u0411\u0435\u043b\u044c\u0441\u044c\u043a\u0438\u0439 1 E-mail: belskyi_vm@ukr.net; https:\/\/orcid.org\/0000-0001-7990-1386 1 \u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u0433\u0435\u043e\u0445\u0456\u043c\u0456\u0457, 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\u0412\u0430\u0441\u0438\u043b\u044c\u043a\u0456\u0432\u0441\u044c\u043a\u0430, 90, \u041a\u0438\u0457\u0432, \u0423\u043a\u0440\u0430\u0457\u043d\u0430 \u041a\u043e\u043d\u0446\u0435\u043d\u0442\u0440\u0430\u0446\u0456\u044f \u0444\u043e\u0441\u0444\u043e\u0440\u0443 \u0432 \u0440\u0456\u0437\u043d\u0438\u0445 \u0442\u0438\u043f\u0430\u0445 \u043d\u0435\u0444\u0435\u043b\u0456\u043d\u043e\u0432\u0438\u0445 \u0442\u0430 \u043b\u0443\u0436\u043d\u0438\u0445 \u0441\u0456\u0454\u043d\u0456\u0442\u0456\u0432 \u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u043e\u0433\u043e \u0449\u0438\u0442\u0430 \u0432\u0438\u0437\u043d\u0430\u0447\u0435\u043d\u0430 \u043d\u0430\u043b\u0435\u0436\u043d\u0456\u0441\u0442\u044e\u0446\u0438\u0445\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar 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\u041b\u0443\u043d\u044c\u043e\u0432\u0430 2, gerasimetsirina@gmail.com, https:\/\/orcid.org\/0000-0003-4670-0216 \u0410.\u0412. \u0427\u0443\u043c\u0430\u043a 3, chymak209@ukr.net, https:\/\/orcid.org\/0009-0000-9225-278X 1 \u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u0433\u0435\u043e\u043b\u043e\u0433\u0456\u0447\u043d\u0438\u0445 \u043d\u0430\u0443\u043a \u041d\u0410\u041d \u0423\u043a\u0440\u0430\u0457\u043d\u0438 01054, \u0432\u0443\u043b. \u041e\u043b\u0435\u0441\u044f \u0413\u043e\u043d\u0447\u0430\u0440\u0430, 55 \u0411, \u041a\u0438\u0457\u0432, \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 \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\u0438 03142, \u043f\u0440\u043e\u0441\u043f. \u0410\u043a\u0430\u0434.\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":8,"url":"http:\/\/www.g-o-f.org.ua\/gb\/%d1%80%d0%b5%d0%b4%d0%ba%d0%be%d0%bb%d0%b5%d0%b3%d0%b8%d1%8f\/","url_meta":{"origin":980,"position":5},"title":"Editorial Board","author":"admin","date":"05\/10\/2017","format":false,"excerpt":"{:uk}\u0421\u041a\u041b\u0410\u0414 \u0420\u0415\u0414\u0410\u041a\u0426\u0406\u0419\u041d\u041e\u0407 \u041a\u041e\u041b\u0415\u0413\u0406\u0407 \u0437\u0431\u0456\u0440\u043d\u0438\u043a\u0430 \u043d\u0430\u0443\u043a\u043e\u0432\u0438\u0445 \u043f\u0440\u0430\u0446\u044c \"\u0413\u0415\u041e\u0425\u0406\u041c\u0406\u042f \u0422\u0410 \u0420\u0423\u0414\u041e\u0423\u0422\u0412\u041e\u0420\u0415\u041d\u041d\u042f (Geochemistry and Ore Formation)\" \u00a0\u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a \u041b\u0435\u043e\u043d\u0456\u0434 \u041c\u0438\u0445\u0430\u0439\u043b\u043e\u0432\u0438\u0447 (\u041a\u0438\u0457\u0432) \u2014 \u0433\u043e\u043b\u043e\u0432\u043d\u0438\u0439 \u0440\u0435\u0434\u0430\u043a\u0442\u043e\u0440, \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\u0438, \u0437\u0430\u0441\u0442. \u0434\u0438\u0440\u0435\u043a\u0442\u043e\u0440\u0430 \u0437 \u043d\u0430\u0443\u043a\u043e\u0432\u043e\u0457 \u0440\u043e\u0431\u043e\u0442\u0438, \u0434\u043e\u043a\u0442\u043e\u0440 \u0433\u0435\u043e\u043b\u043e\u0433\u0456\u0447\u043d\u0438\u0445 \u043d\u0430\u0443\u043a,\u00a0 \u0447\u043b.-\u043a\u043e\u0440. \u041d\u0410\u041d \u0423\u043a\u0440\u0430\u0457\u043d\u0438, \u043f\u0440\u043e\u0444\u0435\u0441\u043e\u0440. \u0411\u043e\u0431\u0440\u043e\u0432 \u041e\u043b\u0435\u043a\u0441\u0430\u043d\u0434\u0440 \u0411\u043e\u0440\u0438\u0441\u043e\u0432\u0438\u0447 (\u041a\u0438\u0457\u0432) \u2014\u041f\u0412\u041d\u0417 \u00ab\u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u0422\u0443\u0442\u043a\u043e\u0432\u0441\u044c\u043a\u043e\u0433\u043e\u00bb, \u043f\u0440\u043e\u0440\u0435\u043a\u0442\u043e\u0440\u2026","rel":"","context":"In \"Editorial Board\"","block_context":{"text":"Editorial Board","link":"http:\/\/www.g-o-f.org.ua\/gb\/tag\/editorial-board\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]}],"_links":{"self":[{"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/pages\/980","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/comments?post=980"}],"version-history":[{"count":7,"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/pages\/980\/revisions"}],"predecessor-version":[{"id":1663,"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/pages\/980\/revisions\/1663"}],"up":[{"embeddable":true,"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/pages\/954"}],"wp:attachment":[{"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/media?parent=980"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}