{"id":1784,"date":"2020-12-09T19:10:09","date_gmt":"2020-12-09T17:10:09","guid":{"rendered":"http:\/\/www.g-o-f.org.ua\/?page_id=1784"},"modified":"2020-12-21T21:00:44","modified_gmt":"2020-12-21T19:00:44","slug":"8-2","status":"publish","type":"page","link":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2020-41\/8-2\/","title":{"rendered":"U-Pb geochronology by zircon of fine-grained granite of the Osnitsky complex. (Volinsky megablok US)"},"content":{"rendered":"<p style=\"text-align: justify;\"><strong>Vysotsky O.B.<\/strong><br \/>\nE-mail: alek.vysotsky@gmail.com, <a href=\"https:\/\/orcid.org\/0000-0002-3542-4685\">https:\/\/orcid.org\/0000-0002-3542-4685<\/a><br \/>\n<strong>Stepanyuk L.M.<\/strong><br \/>\n<a href=\"https:\/\/orcid.org\/0000-0001-5591-5169\">https:\/\/orcid.org\/0000-0001-5591-5169<\/a><br \/>\n<strong>Dovbush T.I.<\/strong><br \/>\n<a href=\"https:\/\/orcid.org\/0000-0002-3512-3313\">https:\/\/orcid.org\/0000-0002-3512-3313<\/a><br \/>\n<strong>Kovalenko N.O.<\/strong><br \/>\n<a href=\"https:\/\/orcid.org\/0000-0002-3203-7145\">https:\/\/orcid.org\/0000-0002-3203-7145<\/a><br \/>\nM.P. Semenenko Institute Geochemistry, Mineralogy and Ore Formation of the National Academy of Science of Ukraine<\/p>\n<p style=\"text-align: justify;\">Language: Ukrainian<br \/>\nGeochemistry and ore formation 2020, 41: 83-86<br \/>\n<a href=\"https:\/\/doi.org\/10.15407\/gof.2020.41.083\">https:\/\/doi.org\/10.15407\/gof.2020.41.083<\/a><\/p>\n<p style=\"text-align: justify;\">The article presents the results of uranium-lead dating of zircon from fine-grained granite of the Osnytsia block of the Volyn megablock of the Ukrainian Shield. The variety of granites of the Osnitsky complex is manifested starting from their appearance. They are dominated by massive medium-grained rocks, limitedly developed fine-grained, even less common coarse-grained varieties. The age of typical Osnitsky granites, determined by the uranium-lead method according to zircon, is 1980-1950 million years. Granitoids after gabbroids were formed, and their rooting took place in two stages. At the first stage, depending on the physicochemical and tectonic conditions, a whole range of acid rocks was formed &#8211; from leptitelike (fine-grained) to large-medium-grained granites. In the second stage, coarse-grained, typical Osnitsky granites took root. One of the most characteristic macroscopic features of Osnitsky granites is that quartz is almost always represented by lilac-gray rounded grains. According to the results of uranium-lead isotope dating, the age of zircon from fine-grained granite is 1973.6 \u00b1 8.4 million years, and 14 \u00b1 24 million years, according to the lower. The weighted average value of the isotopic age in the isotope ratio 207Pb\/206Pb is 1969.3 \u00b1 6 million years. The obtained age for zircon from fine-grained granite of the Osnitsky complex corresponds to the time of formation of granites of the Osnitsky block.<\/p>\n<p style=\"text-align: justify;\">Keywords: <em>Osnitsky block, granite, zircon, isotope age, Ukrainian shield<\/em><\/p>\n<ol>\n<li>Aksamentova N.V. (2002). Magmatizm i paleogeodinamika ranne-proterozoiskogo Osnytsko-Mikashevichskogo vulkanoplutonicheskogo poyasa. Minsk [in Russian].<\/li>\n<li>Bartnitskiy E.N., Bibikova E.V., Verhoglyad V.M., Legkova G.V., Skobelev V.M., Terets G.Ya. (1995). IGMR-1. Mezhdunarodnyj standart cirkona dlya uran-svincovyh izotopnyh issledovanij. Geohimiya i rudoobrazovanie. No. 21. P. 164-167 [in Russian].<\/li>\n<li>Artemenko G.V., Bartnickij E.N., Verhoglyad V.M., Komaristyj A.A., Lesnaya I.M., Mickevich N.YU., Ponomarenko A.N., Skobelev V.M., Shcherbak D.N., Shcherbak \u041c.P. Geohronologicheskaya shkala dokembriya Ukrainskogo shchita. (1989). Kyiv, Nauk. dumka [in Russian].<\/li>\n<li>Dovbush T.I., Skobelev V.M., Stepanyuk L.M. (2008). Metodychni rekomendatsiyi z uran-svyntsevogo, rubidiystrontsiyevogo ta samariy-neodymovogo izotopnogo datuvannya geologichnyh ob\u2019ektiv pry GRR. Kyiv [in Ukrainian].<\/li>\n<li>Shcherbak M.P., Artemenko G.V., Lesnaya I.M., Ponomarenko O.M., Shumlyanskyy, L.V. (2008). Geokhronologiia rannego dokembriia Ukrainskogo shchita. Proterozoy. Kyiv, Nauk. dumka [in Russian].<\/li>\n<li>Shcherbak M.P., Zlobenko V.G., Zhukov G.V., Kotlovskaya F.I., Polevaya N.I., Komlev, L.V., Kovalenko N.K., Nosok G.M., Pochtarenko V.I. (1978). Katalog izotopnyh dat porod Ukrainskogo shchita. Kyiv, Nauk. dumka [in Russian].<\/li>\n<li>Ludwig K.R. (1989). Pb Dat for MS-DOS, version 1.06. U.S. Geol. Surv. Open-File Rept. 542, No. 88. 40 p.<\/li>\n<li>Ludwig K.R. (1990). ISOPLOT for MS-DOS, version 2.0. U.S. Geol. Surv. Open-File Rept. 557, No. 88. 38 p.<\/li>\n<\/ol>\n<p><a href=\"http:\/\/www.g-o-f.org.ua\/wp-content\/uploads\/2020\/2020-8.pdf\" target=\"_blank\" rel=\"noopener\"><img data-recalc-dims=\"1\" loading=\"lazy\" decoding=\"async\" class=\"alignleft\" src=\"https:\/\/i0.wp.com\/www.g-o-f.org.ua\/wp-content\/uploads\/2020\/index.jpg?resize=100%2C100\" alt=\"\" width=\"100\" height=\"100\" \/><\/a><\/p>\n<p style=\"text-align: justify;\">\n","protected":false},"excerpt":{"rendered":"<p>Vysotsky O.B. E-mail: alek.vysotsky@gmail.com, https:\/\/orcid.org\/0000-0002-3542-4685 Stepanyuk L.M. https:\/\/orcid.org\/0000-0001-5591-5169 Dovbush T.I. https:\/\/orcid.org\/0000-0002-3512-3313 Kovalenko N.O. https:\/\/orcid.org\/0000-0002-3203-7145 M.P. Semenenko Institute Geochemistry, Mineralogy and Ore Formation of the National Academy of Science of Ukraine Language: Ukrainian Geochemistry and ore formation 2020, 41: 83-86 https:\/\/doi.org\/10.15407\/gof.2020.41.083 The article presents the results of uranium-lead dating of zircon from fine-grained granite of the &hellip; <a href=\"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2020-41\/8-2\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;U-Pb geochronology by zircon of fine-grained granite of the Osnitsky complex. (Volinsky megablok US)&#8221;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":1702,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-1784","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-sM","jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":2324,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2024-45\/gof-2024-45-044\/","url_meta":{"origin":1784,"position":0},"title":"ISOTOPIC GEOCHRONOLOGY OF GRANITOIDS OF THE KROPYVNYTSKYI COMPLEX, USING THE LOZUVAT QUARRY AS AN EXAMPLE","author":"admin","date":"18\/12\/2024","format":false,"excerpt":"{:uk}\u041b.\u041c. 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pravobereg@gmail.com; https\/\/orcid.org\/0000-0002-3542-4685 \u0412.\u041e. \u0412\u0456\u043b\u044c\u043a\u043e\u0432\u0441\u044c\u043a\u0438\u04391 E-mail: V.vilkovskiy@gmail.com; https:\/\/orcid.org\/0009-0007-7117-8980 1 \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, \u043c. \u041a\u0438\u0457\u0432, \u0423\u043a\u0440\u0430\u0457\u043d\u0430, \u043f\u0440\u043e\u0441\u043f. \u0410\u043a\u0430\u0434. \u041f\u0430\u043b\u043b\u0430\u0434\u0456\u043d\u0430, 34 2\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar 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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 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\u0413.\u0413. \u041f\u0430\u0432\u043b\u043e\u0432 genychpavlov@gmail.com; https\/\/orcid.org\/0000-0002-5913-042X \u041d.\u041e. \u041a\u043e\u0432\u0430\u043b\u0435\u043d\u043a\u043e https:\/\/orcid.org\/0000-0002-3203-7145 \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 \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\u0430, 03142 https:\/\/doi.org\/10.15407\/gof.2024.45.064 \u0423 \u043f\u043b\u0430\u0433\u0456\u043e\u043f\u0435\u0433\u043c\u0430\u0442\u0438\u0442\u0456, \u0449\u043e 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