{"id":1774,"date":"2020-12-09T18:52:48","date_gmt":"2020-12-09T16:52:48","guid":{"rendered":"http:\/\/www.g-o-f.org.ua\/?page_id=1774"},"modified":"2020-12-21T20:54:48","modified_gmt":"2020-12-21T18:54:48","slug":"7-2","status":"publish","type":"page","link":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2020-41\/7-2\/","title":{"rendered":"Uranium-lead age of granites Chigirin massif"},"content":{"rendered":"<p style=\"text-align: justify;\"><strong>L.M. Stepanyuk <sup>1<\/sup><\/strong><br \/>\n<a href=\"https:\/\/orcid.org\/0000-0001-5591-5169\">https:\/\/orcid.org\/0000-0001-5591-5169<\/a><br \/>\n<strong>N.M. Konoval <sup>1<\/sup><\/strong><br \/>\nE-mail: nasa246@ukr.net, <a href=\"https:\/\/orcid.org\/0000-0002-5645-0110\">https:\/\/orcid.org\/0000-0002-5645-0110<\/a><br \/>\n<strong>O.B. Visotskiy <sup>1<\/sup><\/strong><br \/>\n<a href=\"http:\/\/orcid.org\/0000-0002-3542-4685\">http:\/\/orcid.org\/0000-0002-3542-4685<\/a><br \/>\n<strong>T.I. Dovbush <sup>1<\/sup><\/strong><br \/>\n<a href=\"https:\/\/orcid.org\/0000-0002-3512-3313\">https:\/\/orcid.org\/0000-0002-3512-3313<\/a><br \/>\n<strong>O.V. Bilan <sup>2<\/sup><\/strong><br \/>\n<a href=\"https:\/\/orcid.org\/0000-0003-0964-6003\">https:\/\/orcid.org\/0000-0003-0964-6003<\/a><br \/>\n<sup>1<\/sup> M.P. Semenenko Institute Geochemistry, Mineralogy and Ore Formation of the National Academy of Science of Ukraine<br \/>\n<sup>2<\/sup> Taras Shevchenko National University of Kyiv, Institute of Geology<\/p>\n<p>Language: Ukrainian<br \/>\nGeochemistry and ore formation 2020, 41: 77-82<br \/>\n<a href=\"https:\/\/doi.org\/10.15407\/gof.2020.41.077\">https:\/\/doi.org\/10.15407\/gof.2020.41.077<\/a><\/p>\n<p style=\"text-align: justify;\">The age of granites of the Chyhyryn massif &#8211; 2040.0 \u00b1 1.1 million years &#8211; was determined by the uranium-lead isotope method for accessory monazite. According to the results of mineral studies of zircon crystals, the conclusion that granites this mass, as well as granitoids of Novoukrainsky, is formed due to the crust, which indicates the presence of relict nuclei of substrate rocks in the middle of the crystals of this mineral. It is proposed to combine in one (for example, Kropyvnytskyi) complex All two-field spar granitoids of the Ingul megablock, leaving in the composition of the new Ukrainian just gabbroids, intrusive nature and a deep source that does not create doubts. The Chyhyryn massif has an area of over 3,500 km2, located in the northern part of the Ingul megablock. The main volume of rocks that make up the array is occupied by granites, which in their composition correspond to the granites of the Kirovograd complex. According to structural features, trachytoid and porphyritic granites differ among them, and biotite and garnet-biotite granites differ in composition. The inclusions are usually represented by a microcline (occupying 40-50% of the rock volume), having a tabular shape, 3-8 mm in size, which often contain small inclusions of quartz and plagioclase. Large plate crystals of the microcline are often crushed from the edges. In addition to the microcline, plagioclase crystalline crystals up to 5 mm in size occur in areas. Porphyry-like granites of the Chyhyryn massif, common within the Golovkivsky quarry. Monocytes from biotite granite were dated to determine the time of formation of the Chyhyryn massif. Granite was selected in the Golovkivsky quarry, located south of the village. Skelivka.<\/p>\n<p style=\"text-align: justify;\">Keywords: <em>porphyry-like granites of the Chyhyryn massif, uranium-lead isotope system, Ukrainian shield.<\/em><\/p>\n<ol>\n<li>Bartnitskiy E.N., Bibikova E.V., Verkhoglyad V.M., Legkova G.V., Skobelev V.M., Terets G.Ya. (1995). International zircon standard for uranium-lead isotope studies. Geochemistry and Ore Formation. Iss. 21. P. 164-167 [in Russian].<\/li>\n<li>Yesypchuk K.Yu. (1988). Petrological and geochemical foundations of the formation analysis of Precambrian granitoids. Kyiv, Nauk. Dumka [in Russian].<\/li>\n<li>Yesipchuk K.Yu., Bobrov O.B., Stepanyuk L.M., Shcherbak M.P., Glevaskiy \u0404.B., Skobelev V.M., Drannik A.S., Geychenko M.V. (Eds). (2004). Korelyatsiyna chronostratigraphic diagram of the early Precambrian Ukrainian Shield. Kyiv. 30 p. [in Ukrainian].<\/li>\n<li>Stepanyuk L.M., Andriynko O.M., Dovbush T.I., Bondarenko V.K. Crystallogenesis in zircon and monazite in the rocks of the Novoukrainka massiv. Collection scientific works of UkrDGRI. No. 1, 2004. P. 64-72 [in Ukrainian].<\/li>\n<li>Stepanyuk L.M., Kurilo S.I. Dovbush T.I. (2015). Uranium-lead geochronology on the granite monazite of the Dolyna massif of the Ingul megablock of the Ukrainian Shield. Visn. Nac. Akad. Nauk Ukr. No. 10. P. 46-49 [in Ukrainian]. <a href=\"https:\/\/doi.org\/10.15407\/visn2015.10.046\">https:\/\/doi.org\/10.15407\/visn2015.10.046<\/a><\/li>\n<li>Stepanyuk L.M., Siomka V.O., Kurilo S.I., Bondarenko S.M., Dovbush T.I. (2016). Uranium-lead isotope age of granites of the Voznesensk massif (Ingul megablock of the Ukrainian shield). Doopov. of the NAS of Ukraine. No. 8. P. 79-84 [in Ukrainian].<\/li>\n<li>Stepanyuk L.M., Kurilo S.I., Siomka V.O., Bondarenko S.M., Kovalenko O.O., Dovbush T.I., Vysotsky O.B. (2017). Features of U-Pb isotope systems of zircons and monazites of the granite-xenolite association: petrological and geological consequences. Mineral. Journ. Vol. 39, No. 1. P. 63-74 [in Ukrainian]. <a href=\"https:\/\/doi.org\/10.15407\/mineraljournal.39.01.063\">https:\/\/doi.org\/10.15407\/mineraljournal.39.01.063<\/a><\/li>\n<li>Shcherbak N.P., Artemenko G.V., Bartnitskiy E.N., Verhoglyad V.M., Komaristy A.A., Lesnaya I.M., Mitskevich N.Yu., Ponomarenko A.N., Skobelev V.M., Shcherbak D.N. (1989). Geochronological scale of the Precambrian of the Ukrainian Shield. Kyiv, Nauk. Dumka [in Russian].<\/li>\n<li>Shcherbakov I.B. (2005). Petrology of the Ukrainian Shield. Lviv, ZUKTS. [in Russian].<\/li>\n<li>Krough T.E. (1973). A law contamination method for hedrotermal decomposition of zircon and extraction of U and Pb for isotopic age determination. Geochim. Cosmochim. Acta. Vol. 37. No. 3. P. 485-494. <a href=\"https:\/\/doi.org\/10.1016\/0016-7037(73)90213-5\">https:\/\/doi.org\/10.1016\/0016-7037(73)90213-5<\/a><\/li>\n<li>Ludwig K.R. (1989). Pb Dat for MS-DOS, version 1.06. U.S. Geol. Survey Open-File Rept. No. 88. 542. P. 40.<\/li>\n<li>Ludwig K.R. (1990). ISOPLOT for MS-DOS, version 2.0. U.S. Geol. Survey Open-File Rept. No. 88. 557. P. 38.<\/li>\n<li>Stepanyuk L.M., Kurylo S.\u0406., Dovbush T.\u0406., Grinchenko O.V., Syomka V.O., Bondarenko S.M., Shumlyanskyy L.V. (2017). Geochronology of granitoids of the eastern part of the inhul terraine (the Ukrainian shield). Geochemistry and Ore Formation. Iss. 38. P. 3-13. <a href=\"https:\/\/doi.org\/10.15407\/gof.2017.38.003\">https:\/\/doi.org\/10.15407\/gof.2017.38.003<\/a><\/li>\n<li>Stepanjuk L.M., Hrinchenko O.V., Siomka V.O., Bondarenko S.M., Kurylo S.I., Dovbush \u0422.I. (2018). Geochronology of granitoides of Ingul megablock as to their lithium content. Visnyk KNU, Geology. Vol. 82 (3). P. 23-28. <a href=\"https:\/\/doi.org\/10.17721\/1728-2713.82.03\">https:\/\/doi.org\/10.17721\/1728-2713.82.03<\/a><\/li>\n<\/ol>\n<p><a href=\"http:\/\/www.g-o-f.org.ua\/wp-content\/uploads\/2020\/2020-7.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","protected":false},"excerpt":{"rendered":"<p>L.M. Stepanyuk 1 https:\/\/orcid.org\/0000-0001-5591-5169 N.M. Konoval 1 E-mail: nasa246@ukr.net, https:\/\/orcid.org\/0000-0002-5645-0110 O.B. Visotskiy 1 http:\/\/orcid.org\/0000-0002-3542-4685 T.I. Dovbush 1 https:\/\/orcid.org\/0000-0002-3512-3313 O.V. Bilan 2 https:\/\/orcid.org\/0000-0003-0964-6003 1 M.P. Semenenko Institute Geochemistry, Mineralogy and Ore Formation of the National Academy of Science of Ukraine 2 Taras Shevchenko National University of Kyiv, Institute of Geology Language: Ukrainian Geochemistry and ore formation &hellip; <a href=\"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2020-41\/7-2\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Uranium-lead age of granites Chigirin massif&#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-1774","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-sC","jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":2345,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2024-45\/gof-2024-45-064\/","url_meta":{"origin":1774,"position":0},"title":"URANIUM MINERALIZATION IN ROCKS OF THE PETRIVSK IRON ORE DEPOSIT (INGUL MEGABLOCK, UKRAINIAN SHIELD)","author":"admin","date":"18\/12\/2024","format":false,"excerpt":"{:uk}\u041e.\u0412. \u041a\u043e\u0432\u0442\u0443\u043d 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\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.2024.45.044 \u0412\u0438\u043a\u043b\u0430\u0434\u0435\u043d\u043e \u0440\u0435\u0437\u0443\u043b\u044c\u0442\u0430\u0442\u0438 \u0432\u0438\u0432\u0447\u0435\u043d\u043d\u044f \u0433\u0440\u0430\u043d\u0456\u0442\u0443 \u043d\u0435\u0440\u0456\u0432\u043d\u043e\u043c\u0456\u0440\u043d\u043e\u0437\u0435\u0440\u043d\u0438\u0441\u0442\u043e\u0433\u043e (\u043f\u0440\u043e\u0431\u0430 14\/23), 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\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":2124,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2023-44\/4-4\/","url_meta":{"origin":1774,"position":3},"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 1 E-mail: nataliya.kryuchenko@gmail.com, https:\/\/orcid.org\/0000-0001-8774-90 \u0415 \u042f. \u0416\u043e\u0432\u0438\u043d\u0441\u044c\u043a\u0438\u0439 1 E-mail: zhovinsky@ukr.net, https:\/\/orcid.org\/0000-0003-1601-5998 \u041f.\u0421. \u041f\u0430\u043f\u0430\u0440\u0438\u0433\u0430 2 E-mail: paparyga.ps@ukr.net, https:\/\/orcid.org\/0000-0002-4021-0809 \u041e.\u0410. \u0416\u0443\u043a 1 E-mail: igmof.zhuk@gmail.com, https:\/\/orcid.org\/ 0000-0002-5264-0750 \u041c.\u0412. \u041a\u0443\u0445\u0430\u0440 1 E-mail: mvk2819@gmail.com, https:\/\/orcid.org\/0000-0003-3572-5194 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\u0435\u043d\u0456 \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. \u041f\u0430\u043b\u043b\u0430\u0434\u0456\u043d\u0430, 34, \u041a\u0438\u0457\u0432,\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":2425,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2025-46\/gof-2025-46-056\/","url_meta":{"origin":1774,"position":4},"title":"AGE OF METAVOLCANIC ROCKS OF ACIDIC COMPOSITION OF THE METAMORPHIC COMPLEX OF THE NORTHWESTERN PART OF THE MARMAROSH MASSIF (UKRAINIAN CARPATHIANS)","author":"admin","date":"16\/12\/2025","format":false,"excerpt":"{:uk}\u041b.\u041c. \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a, stepaniuk@nas.gov.ua, https:\/\/orcid.org\/0000-0001-5591-5169\u00a0 \u0422.\u0406. \u0414\u043e\u0432\u0431\u0443\u0448, tetyana.dovbush1@gmail.com, https:\/\/orcid.org\/0000-0002-3512-3313 \u041e.\u0411.\u00a0 \u00a0\u0412\u0438\u0441\u043e\u0446\u044c\u043a\u0438\u0439,\u00a0 \u00a0alek.vysotsky@gmail.com,\u00a0 \u00a0https:\/\/orcid.org\/0000-0002-3542-4685 \u0410.\u041c. \u00a0\u0411\u0430\u0440\u0430\u043d, \u00a0baranandrew9@gmail.com, \u00a0https:\/\/orcid.org\/0000-0002-5326-8014 \u041b.\u0406.\u00a0 \u00a0\u041a\u0430\u043d\u0443\u043d\u043d\u0456\u043a\u043e\u0432\u0430,\u00a0 \u00a0Kanunikova59@gmail.com,\u00a0 \u00a0https:\/\/orcid.org\/0000-0002-7530-969\u0425 \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. \u041f\u0430\u043b\u043b\u0430\u0434\u0456\u043d\u0430, 34, \u041a\u0438\u0457\u0432, \u0423\u043a\u0440\u0430\u0457\u043d\u0430 https:\/\/doi.org\/10.15407\/gof.2025.46.056 \u041c\u0435\u0442\u0430\u0432\u0443\u043b\u043a\u0430\u043d\u0456\u0442\u0438 \u043a\u0438\u0441\u043b\u043e\u0433\u043e \u0441\u043a\u043b\u0430\u0434\u0443 \u0454 \u0434\u043e\u0441\u0438\u0442\u044c \u043f\u043e\u0448\u0438\u0440\u0435\u043d\u0438\u043c\u0438 \u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f\u043c\u0438 \u0441\u0435\u0440\u0435\u0434 \u043f\u043e\u0440\u0456\u0434 \u043a\u0440\u0438\u0441\u0442\u0430\u043b\u0456\u0447\u043d\u043e\u0433\u043e \u043a\u043e\u043c\u043f\u043b\u0435\u043a\u0441\u0443 \u041c\u0430\u0440\u043c\u0430\u0440\u043e\u0441\u044c\u043a\u043e\u0433\u043e\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":1766,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2020-41\/6-2\/","url_meta":{"origin":1774,"position":5},"title":"Lead-zinc mineralization of fluoriton-bearing areas of the Middle Transnistria","author":"admin","date":"09\/12\/2020","format":false,"excerpt":"{:uk}\u041d.\u041e. \u041a\u0440\u044e\u0447\u0435\u043d\u043a\u043e 1 https:\/\/orcid.org\/0000-0001-8774-9089 \u0415.\u042f. \u0416\u043e\u0432\u0438\u043d\u0441\u044c\u043a\u0438\u0439 1 https:\/\/orcid.org\/0000-0003-1601-5998 \u041e.\u0410. \u0416\u0443\u043a 1 https:\/\/orcid.org\/0000-0002-5264-0750 \u041f.\u0421. \u041f\u0430\u043f\u0430\u0440\u0438\u0433\u0430 2 https:\/\/orcid.org\/0000-0002-4021-0809 \u041c.\u0412. \u041a\u0443\u0445\u0430\u0440 1 https:\/\/orcid.org\/0000-0003-3572-5194 \u041a.\u0415. \u0414\u043c\u0438\u0442\u0440\u0435\u043d\u043a\u043e 1 https:\/\/orcid.org\/0000-0003-1001-3457 \u0422.\u0410. \u041f\u043e\u043f\u0435\u043d\u043a\u043e 1 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\u0435\u043d\u0456 \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. \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 2 \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 \u041c\u0456\u043d\u0456\u0441\u0442\u0435\u0440\u0441\u0442\u0432\u0430\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar 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