{"id":1379,"date":"2019-10-15T13:04:18","date_gmt":"2019-10-15T10:04:18","guid":{"rendered":"http:\/\/www.g-o-f.org.ua\/?page_id=1379"},"modified":"2020-01-20T20:28:37","modified_gmt":"2020-01-20T18:28:37","slug":"source-of-sodium-and-uranium","status":"publish","type":"page","link":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2012-2\/source-of-sodium-and-uranium\/","title":{"rendered":"Source of sodium and uranium of uraniferous albitites (\u043en the example of dokuchaevka deposit of ingul megablock of USh)"},"content":{"rendered":"<p><strong>Stepanyuk L.M.<sup>1<\/sup>, Bondarenko S.N.<sup>1<\/sup>, Somka V. A.<sup>1<\/sup>, Kotvitskaja I.N.<sup>1<\/sup>, Andreev A.V.<sup>2<\/sup><\/strong><br \/>\n1. M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Sciences of Ukraine<br \/>\n2. Taras Shevchenko National University of Kyiv<\/p>\n<p>Language: Ukrainian<br \/>\nGeochemistry and ore formation 2012, 31-32: 99-104<br \/>\n<a href=\"https:\/\/doi.org\/10.15407\/gof.2012.31.099\"> https:\/\/doi.org\/10.15407\/gof.2012.31.099<\/a><\/p>\n<p><a href=\"http:\/\/www.g-o-f.org.ua\/wp-content\/uploads\/2012-31-32\/13_2.pdf\">Download (PDF)<\/a><\/p>\n<p style=\"text-align: justify;\">Investigations of rubidium-strontium isotopic system in subsequent series of metasomatic alterations (granite &#8211; barren albitite &#8211; mineralized albitite) from granites of Novoukrainka type to uraniferous albitites are carried out. Isotopic systems of bulk rock samples, apatite and plagioclases from rocks of Dokuchaevka deposit as well as apatite from Novoukrainka granites of Kapustjansky open pit are studied. The tendency of lowering the values of primary isotopic relation <sup>87<\/sup>Sr\/<sup>86<\/sup>Sr from nonaltered granite (0,725) to barren albitites (0,7121\u20130,7146) and subsuquently to mineralised albitites (0,7108\u20130,7088) is established. At the same time undirect logarithmic relation between values of primary <sup>87<\/sup>Sr\/<sup>86<\/sup>Sr ratio in albitites and uranium contents in them is observed, as well as direct linear relation between uranium contents in albitites and albites from them, that testify for common migration of uranium, sodium and strontium.<br \/>\nThe conclusion about absence of an\u0443 genetic relation between granites of Novoukrainka type and metasomatic fluids which have caused formation of albitites as well as deep nature of their source are made.<\/p>\n<p style=\"text-align: justify;\">References<br \/>\n1. Belevcev R.Ya., Nikolaenko V.I., Spivak S.D. i dr. Migraciya i fiksaciya urana v zone gipergeneza granitnyh<br \/>\nmassivov. Termodinamika gazovogo obmena v okruzhayushej srede. Kiev, Nauk. dumka, 2007, pp. 151\u2013199.<br \/>\n2. Geneticheskie tipy i zakonomernosti razmesheniya uranovyh mestorozhdenij Ukrainy. Belevcev Ya.N.,<br \/>\nKoval V.V., Bakarzhiev A.H. i dr.,Kiev, Nauk. dumka, 1995, 396 p.<br \/>\n3. Egorov Yu.P., Suhinin A.I. Nekotorye zakonomernosti formirovaniya i razmesheniya metasomaticheskih<br \/>\nmestorozhdenij v dokembrii. Geol. zhurn., 1969, No 2 , pp. 49\u201357.<br \/>\n4. Melnichenko B.F., Skobelyev V.M., Stepanov V.O. Geohronologiya endogennih rudoutvoryuyuchih procesiv na<br \/>\nZhovtorichenskomu rodovishi. Geohimiya ta ekologiya. Zb. nauk. pr., Vip. 5\/6, 2002, pp. 166\u2013170.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Stepanyuk L.M.1, Bondarenko S.N.1, Somka V. A.1, Kotvitskaja I.N.1, Andreev A.V.2 1. M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Sciences of Ukraine 2. Taras Shevchenko National University of Kyiv Language: Ukrainian Geochemistry and ore formation 2012, 31-32: 99-104 https:\/\/doi.org\/10.15407\/gof.2012.31.099 Download (PDF) Investigations of rubidium-strontium isotopic system in subsequent &hellip; <a href=\"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2012-2\/source-of-sodium-and-uranium\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Source of sodium and uranium of uraniferous albitites (\u043en the example of dokuchaevka deposit of ingul megablock of USh)&#8221;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":256,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-1379","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-mf","jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":1510,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2019-40\/1-2\/","url_meta":{"origin":1379,"position":0},"title":"The Institute of Geochemistry, Mineralogy and Ore Formation Semenenko NAS of Ukraine is 50 years","author":"admin","date":"27\/11\/2019","format":false,"excerpt":"{:uk}9 \u0441\u0456\u0447\u043d\u044f 2019 \u0440. 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post","link":""},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/www.g-o-f.org.ua\/wp-content\/uploads\/2020\/index.jpg?resize=350%2C200","width":350,"height":200},"classes":[]},{"id":1432,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2012-2\/trace-elements\/","url_meta":{"origin":1379,"position":1},"title":"Trace elements in drinking water of Rahiv-Tysynsk tectonic zone and their impact on public health","author":"admin","date":"25\/10\/2019","format":false,"excerpt":"{:uk}\u041f.\u0421. \u041f\u0430\u043f\u0430\u0440\u0438\u0433\u0430 \u041a\u0430\u0440\u043f\u0430\u0442\u0441\u044c\u043a\u0438\u0439 \u0431\u0456\u043e\u0441\u0444\u0435\u0440\u043d\u0438\u0439 \u0437\u0430\u043f\u043e\u0432\u0456\u0434\u043d\u0438\u043a https:\/\/doi.org\/10.15407\/gof.2012.31.159 Download (PDF) \u041f\u0440\u043e\u0432\u0435\u0434\u0435\u043d\u0435 \u0441\u0442\u0430\u0442\u0438\u0441\u0442\u0438\u0447\u043d\u0435 \u043e\u043f\u0440\u0430\u0446\u044e\u0432\u0430\u043d\u043d\u044f 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of the hydrothermal process intensity and the ore bodies precursors","author":"admin","date":"16\/10\/2019","format":false,"excerpt":"{:uk}\u041b.\u0417. \u0421\u043a\u0430\u043a\u0443\u043d, \u041d.\u041e. \u0421\u043b\u043e\u0432\u043e\u0442\u0435\u043d\u043a\u043e, \u0420.\u042f. \u0421\u0435\u0440\u043a\u0456\u0437, \u041a.\u0412. \u0421\u0430\u0441\u044e\u043a \u041b\u044c\u0432\u0456\u0432\u0441\u044c\u043a\u0438\u0439 \u043d\u0430\u0446\u0456\u043e\u043d\u0430\u043b\u044c\u043d\u0438\u0439 \u0443\u043d\u0456\u0432\u0435\u0440\u0441\u0438\u0442\u0435\u0442 \u0456\u043c\u0435\u043d\u0456 \u0406\u0432\u0430\u043d\u0430 \u0424\u0440\u0430\u043d\u043a\u0430 https:\/\/doi.org\/10.15407\/gof.2012.31.113 Download (PDF) \u0414\u043e\u0441\u043b\u0456\u0434\u0436\u0435\u043d\u043e \u043f\u0440\u043e\u0441\u0442\u043e\u0440\u043e\u0432\u0438\u0439 \u0440\u043e\u0437\u043f\u043e\u0434\u0456\u043b, \u043f\u0430\u0440\u0430\u0433\u0435\u043d\u0435\u0437\u0438\u0441\u0438 \u0442\u0430 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