{"id":1744,"date":"2020-12-09T17:23:37","date_gmt":"2020-12-09T15:23:37","guid":{"rendered":"http:\/\/www.g-o-f.org.ua\/?page_id=1744"},"modified":"2020-12-21T19:17:13","modified_gmt":"2020-12-21T17:17:13","slug":"4-2","status":"publish","type":"page","link":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2020-41\/4-2\/","title":{"rendered":"Kaersutite lamprophyres of the Pokrovo-Kyriivo massif (the Azov area, Ukraine): petrographic features, mineral composition, geochemistry"},"content":{"rendered":"<p style=\"text-align: justify;\"><strong>V.O. Gatsenko<\/strong><br \/>\n<a href=\"https:\/\/orcid.org\/0000-0002-3229-3907\">https:\/\/orcid.org\/0000-0002-3229-3907<\/a><br \/>\n<strong>S.V. Kushnir<\/strong><br \/>\n<a href=\"https:\/\/orcid.org\/0000-0002-3449-1261\">https:\/\/orcid.org\/0000-0002-3449-1261<\/a><br \/>\nM.P. Semenenko Institute Geochemistry, Mineralogy and Ore Formation of the National Academy of Science of Ukraine<\/p>\n<p>Language: Ukrainian<br \/>\nGeochemistry and ore formation 2020, 41: 42-53<br \/>\n<a href=\"https:\/\/doi.org\/10.15407\/gof.2020.41.042\">https:\/\/doi.org\/10.15407\/gof.2020.41.042<\/a><\/p>\n<p style=\"text-align: justify;\">The paper represents results of the petrographical, geochemical and mineralogical studies of a dyke of porphyry-like mafic rock from the Pokrovo-Kyriivo massif of the Azov area, the Ukrainian Shield. This dyke of fine-grained rock has unique mineral composition as the main mineral in the groundmass is kaersutite. According to mineralogical and petrographic features, it can be identified as kaersutite lamprophyre. The Devonian Pokrovo-Kyriivo massif is located at a junction of the Azov Domain of the Ukrainian Shield and the folded structure of Donbas. This massif is composed of subalkaline (pyroxenite, gabbro) and alkaline (malignites, nepheline syenite) rocks which are cut by numerous dykes varying in composition from ultramafic to intermediate. The dyke of finegrained kaersutite lamprophyre was discovered in the bottom hole of the drillhole 36, where it is intruded into mediumgrained gabbroids and pyroxenites. The groundmass of the rock is composed of kaersutite, titanomagnetite, albite, chlorite, titanite, pyrite, chalcopyrite, apatite, monazite. The phenocrysts are represented by chlorite and talc pseudomorphoses after a diamond-shaped mineral with shortened obtuse angles. According to electron microprobe analysis, kaersutite has low TiO<sub>2<\/sub> content and intermediate mg# values of 0.54\u20140.67. According to the chemical composition, studied kaersutites differ from the same mineral in the microgabro dyke in the Pokrovo-Kyriivo massif, and from kaersutites in camptonites of the Khlibodarivka open pit in the Azov area. At the same time, it is similar to kaersutites from camptonites of the Novoukrainka dyke field of the Inhul terrane. Kaersutite lamprophyre also differ from dyke rocks of the Pokrovo-Kyriivo massif by the absence of clinopyroxene, mica, ilmenite and low content of TiO<sub>2<\/sub> in titanomagnetite, which does not exceed 6 %. This is due to a low TiO<sub>2<\/sub> content in the rocks (up to 3.5 %), relative to other dyke gabbro of the area. According to mineralogical-petrographic and chemical characteristics, kaersutite lamprophyres are unique rocks that have no direct counterparts in the Azov area or on the Ukrainian Shield in the whole.<\/p>\n<p style=\"text-align: justify;\">Keywords: <em>kaersutite lamprophyre, mafic dyke, kaersutite, the Pokrovo-Kyriivo massif, the Azov area.<\/em><\/p>\n<ol>\n<li>Gonshakova V.I. (Ed.) (1973). Mafic-ultramafic magmatism and metallogeny of the East European Platform (platformal stage of evolution). Moscow [in Russian].<\/li>\n<li>Vishnevskaya E.A. (2016). Petrology of the dykerocks from Bobrynets Belt (Ingul megablock of the Ukrainian Shield):Thesis of PhD in geol. sciences. Kyiv. 23 p. [in Ukranian].<\/li>\n<li>Gatsenko V.O., Kryvdik S.G., Kushnir S.V. (2019). Peculiarities of the composition of the high-titanium ultramafite dyke rock in the Andriivka open pit (the Eastern Azov area of the Ukrainian shield). Geochemistry and Ore Formation. Iss. 40. P. 40-47 [in Ukranian].<br \/>\n<a href=\"https:\/\/doi.org\/10.15407\/gof.2019.40.040\">https:\/\/doi.org\/10.15407\/gof.2019.40.040<\/a><\/li>\n<li>Geological map of Domozozoic formations (2007). Responsible exec. B.V. Borodinya. Priazovskaya KGP [in Ukranian].<\/li>\n<li>Kryvdik S., Hatsenko V., Lunyov Ye. (2016). Amphiboles from the malignites of the Pokrovo-Kyriyivo massif (Azov Sea region, Ukraine) Mineralogical collection. Ivan Franko National University of Lviv. 66, Iss. 1, P. 109-118 [in Ukranian].<\/li>\n<li>Kryvdik S.G., Sharygin V.V., Gatsenko V.O., Lunev E.S. (2016). Pyroxene of the Pokrovo-Kyriyivo massif (Azov Sea region, Ukraine), Mineral. Journ. (Ukraine). Vol. 38, No. 3, P. 24-38 [in Ukranian].<br \/>\n<a href=\"https:\/\/doi.org\/10.15407\/mineraljournal.38.03.024\">https:\/\/doi.org\/10.15407\/mineraljournal.38.03.024<\/a><\/li>\n<li>Makukhina G.O. (1961) Petrography of the dyke-effusive complex of southwest Donbass. Kyiv [in Ukranian].<\/li>\n<li>Matviychuk M.V., Donsky M.O. (2006). Geochemical peculiarities of dyke rocks in the Khlebodarovka quarry. Geochemistry and Ore Formation. No. 24 [in Russian].<\/li>\n<li>Mitrokhin A.V., Vishnevskaya E.A., Gatsenko V.A., Mitrokhina T.V., Mikhalchenko I.I., Shumlyanskyy L.V. Petpology, gejchemistry and ore potential of ultramafic dykes of the Novjukrainka dyke field (Ingul terrain of the Ukrainian Shield). Mineral. Journ. (Ukraine). Vol. 38, No. 1, P. 42-57 [in Russian].<br \/>\n<a href=\"https:\/\/doi.org\/10.15407\/mineraljournal.38.01.042\">https:\/\/doi.org\/10.15407\/mineraljournal.38.01.042<\/a><\/li>\n<li>Shcherbakov I.B. (Ed.) (1999). Petrographic code of Ukraine [in Ukranian].<\/li>\n<li>Phanerozoic magmatizm of Eastern Asov area of Ukrainian Shield and related commercial minerals (petrology, geochemistry and ore potential) (2015). Kyiv [in Russian].<\/li>\n<li>Yuriev L.D. (1967) Kaersutitis and some secondary changes of lamprophyre with. Hlibodarivky: (East. Priazovya). Dopov. AN URSR. Ser. B. No. 10. P. 912-916 [in Ukranian].<\/li>\n<li>Bogdanova S.V., Gintov O.B., Kurlovich D., Lubnina N.V., Nilsson M., Orlyuk M.I., Pashkevich I.K., Shumlyanskyy L.V., Starostenko V.I. (2013). Late Palaeoproterozoic mafic dyking in the Ukrainian Shield of VolgoSarmatia caused by rotation during the assembly of supercontinent Columbia (Nuna). Lithos. Vol. 174. P. 196-216.<br \/>\n<a href=\"https:\/\/doi.org\/10.1016\/j.lithos.2012.11.002\">https:\/\/doi.org\/10.1016\/j.lithos.2012.11.002<\/a><\/li>\n<li>Maitre R.W. Le (Ed.). (2002), Igneous rocks. A Classification and Glossary of Terms.<br \/>\n<a href=\"https:\/\/doi.org\/10.1017\/CBO9780511535581\">https:\/\/doi.org\/10.1017\/CBO9780511535581<\/a><\/li>\n<li>Leake B.E., Woolley A.R., Arps C.E.S. et al. (1997). Nomenclature of amphiboles: report of the Subcommittee on amphiboles of the International Mineralogical Association Commission on new minerals and mineral names. Mineral. Magazine. 61. P. 295-321<\/li>\n<\/ol>\n<p>&nbsp;<\/p>\n<p><a href=\"http:\/\/www.g-o-f.org.ua\/wp-content\/uploads\/2020\/2020-4.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>V.O. Gatsenko https:\/\/orcid.org\/0000-0002-3229-3907 S.V. Kushnir https:\/\/orcid.org\/0000-0002-3449-1261 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: 42-53 https:\/\/doi.org\/10.15407\/gof.2020.41.042 The paper represents results of the petrographical, geochemical and mineralogical studies of a dyke of porphyry-like mafic rock from the Pokrovo-Kyriivo massif of &hellip; <a href=\"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2020-41\/4-2\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Kaersutite lamprophyres of the Pokrovo-Kyriivo massif (the Azov area, Ukraine): petrographic features, mineral composition, geochemistry&#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-1744","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-s8","jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":2084,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2023-44\/1-1\/","url_meta":{"origin":1744,"position":0},"title":"AGE OF QUARTZ SYENITES OF THE NIZYANKA STRUCTURE OF THE WEST AZOV REGION","author":"admin","date":"17\/12\/2023","format":false,"excerpt":"{:uk}{:uk}{:uk}\u0413.\u0412. \u0410\u0440\u0442\u0435\u043c\u0435\u043d\u043a\u043e 1 E-mail: regulgeo@gmail.com; https:\/\/orcid.org\/0000-0002-4528-6853 \u0411.\u0412. \u0411\u043e\u0440\u043e\u0434\u0438\u043d\u044f 2 E-mail: boris.priazov@gmail.com \u041b.\u0421. \u0414\u043e\u0432\u0431\u0438\u0448 1 E-mail: dovbyshls@ukr.net; https:\/\/orcid.org\/0000-0003-4529-448X \u041e.\u0411. \u0412\u0438\u0441\u043e\u0446\u044c\u043a\u0438\u0439 1 E-mail: alek.vysotsky@gmail.com; https\/\/orcid.org\/0000-0002-3542-4685 \u0412.\u041e. \u0412\u0456\u043b\u044c\u043a\u043e\u0432\u0441\u044c\u043a\u0438\u0439 1 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, \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 2 \u041a\u041f \u00ab\u041f\u0456\u0432\u0434\u0435\u043d\u0443\u043a\u0440\u0433\u0435\u043e\u043b\u043e\u0433\u0456\u044f\u00bb 49000,\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":1920,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2021-42\/1-5\/","url_meta":{"origin":1744,"position":1},"title":"KAERSUTITIS IN AZOV AREA ROCKS (UKRAINIAN SHIELD): PETROLOGICAL ASPECT","author":"admin","date":"15\/12\/2021","format":false,"excerpt":"{:uk}\u0412.\u041e. \u0413\u0430\u0446\u0435\u043d\u043a\u043e 1E-mail: vera.gatsenko@ukr.net,https:\/\/orcid.org\/0000-0002-3229-3907\u0421.\u0406. \u041a\u0443\u0440\u0438\u043b\u043e 2\u0415-mail: kurylo.sergiy@gmail.com,https:\/\/orcid.org\/ 0000-0003-4466-68511. \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. \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 p\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, \u0421\u043b\u043e\u0432\u0430\u0447\u0447\u0438\u043d\u0430 \u0412\u0438\u043a\u043b\u0430\u0434\u0435\u043d\u043e \u0440\u0435\u0437\u0443\u043b\u044c\u0442\u0430\u0442\u0438 \u043d\u043e\u0432\u0438\u0445 \u0434\u043e\u0441\u043b\u0456\u0434\u0436\u0435\u043d\u044c \u043a\u0435\u0440\u0441\u0443\u0442\u0438\u0442\u0456\u0432 \u0456\u0437 \u043b\u0430\u043c\u043f\u0440\u043e\u0444\u0456\u0440\u0456\u0432 \u041f\u043e\u043a\u0440\u043e\u0432\u043e-\u041a\u0438\u0440\u0456\u0457\u0432\u0441\u044c\u043a\u043e\u0433\u043e \u043c\u0430\u0441\u0438\u0432\u0443 \u041f\u0440\u0438\u0430\u0437\u043e\u0432\u2019\u044f (\u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0438\u0439 \u0449\u0438\u0442),\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar 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\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 2 \u041a\u0438\u0457\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 \u0422\u0430\u0440\u0430\u0441\u0430 \u0428\u0435\u0432\u0447\u0435\u043d\u043a\u0430 \u041d\u0430\u0432\u0447\u0430\u043b\u044c\u043d\u043e-\u043d\u0430\u0443\u043a\u043e\u0432\u0438\u0439 \u0456\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u00ab\u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u0433\u0435\u043e\u043b\u043e\u0433\u0456\u0457\u00bb \u0432\u0443\u043b. \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, 03022 \u00a0https:\/\/doi.org\/10.15407\/gof.2024.45.021 \u041f\u0440\u0435\u0434\u0441\u0442\u0430\u0432\u043b\u0435\u043d\u0456\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":1744,"position":3},"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":2025,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2022-43\/7-2\/","url_meta":{"origin":1744,"position":4},"title":"RARE-EARTH DEPOSITS OF A NON-TRADITIONAL TYPE IN THE AZOV PART OF THE UKRAINIAN SHIELD","author":"admin","date":"20\/12\/2022","format":false,"excerpt":"{:uk} \u041b.\u0414. \u0421\u0454\u0442\u0430\u044fE-mail: lasetaya@gmail.com, https:\/\/orcid.org\/0000-0002-2996-0289\u0406.\u042e. \u041d\u0456\u043a\u043e\u043b\u0430\u0454\u0432E-mail: oemidonetsk@gmail.com, https:\/\/orcid.org\/0000-0003-2208-0032\u0421.\u041c. \u0421\u0442\u0440\u0435\u043a\u043e\u0437\u043e\u0432E-mail: ssss21161@gmail.com, https:\/\/orcid.org\/0000-0002-1421-4910\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\u0430 https:\/\/doi.org\/10.15407\/gof.2022.43.074 \u0420\u043e\u0437\u0433\u043b\u044f\u043d\u0443\u0442\u043e \u0433\u0435\u043e\u043b\u043e\u0433\u0456\u0447\u043d\u0443 \u0431\u0443\u0434\u043e\u0432\u0443 \u0442\u0430 \u043f\u0435\u0440\u0441\u043f\u0435\u043a\u0442\u0438\u0432\u043d\u0456\u0441\u0442\u044c \u043d\u0435\u0442\u0440\u0430\u0434\u0438\u0446\u0456\u0439\u043d\u043e\u0457 \u0434\u043b\u044f \u043f\u0440\u043e\u043c\u0438\u0441\u043b\u043e\u0432\u043e\u0441\u0442\u0456 \u0423\u043a\u0440\u0430\u0457\u043d\u0438 \u0433\u0440\u0443\u043f\u0438 \u043e\u0431\u2019\u0454\u043a\u0442\u0456\u0432 \u0440\u0456\u0434\u043a\u0456\u0441\u043d\u043e\u0437\u0435\u043c\u0435\u043b\u044c\u043d\u043e\u0457 \u0441\u0438\u0440\u043e\u0432\u0438\u043d\u0438 \u0435\u043a\u0437\u043e\u0433\u0435\u043d\u043d\u043e\u0433\u043e \u043f\u043e\u0445\u043e\u0434\u0436\u0435\u043d\u043d\u044f. \u041d\u0430 \u0434\u0443\u043c\u043a\u0443 \u0430\u0432\u0442\u043e\u0440\u0456\u0432, \u0446\u0435 \u043f\u0435\u0440\u0435\u0432\u0430\u0436\u043d\u043e \u0433\u043b\u0438\u043d\u0438\u0441\u0442\u0430 \u043a\u043e\u0440\u0430 \u0432\u0438\u0432\u0456\u0442\u0440\u044e\u0432\u0430\u043d\u043d\u044f\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":1774,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2020-41\/7-2\/","url_meta":{"origin":1744,"position":5},"title":"Uranium-lead age of granites Chigirin massif","author":"admin","date":"09\/12\/2020","format":false,"excerpt":"{:uk}\u041b.\u041c. \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a 1 https:\/\/orcid.org\/0000-0001-5591-5169 \u041d.\u041c. \u041a\u043e\u043d\u043e\u0432\u0430\u043b 1 E-mail: nasa246@ukr.net, https:\/\/orcid.org\/orcid.org\/0000-0002-5645-0110 \u041e.\u0411. \u0412\u0438\u0441\u043e\u0446\u044c\u043a\u0438\u0439 1 https:\/\/orcid.org\/0000-0002-3542-4685 \u0422.\u0406. \u0414\u043e\u0432\u0431\u0443\u0448 1 https:\/\/orcid.org\/0000-0002-3512-3313 \u041e.\u0412. \u0411\u0456\u043b\u0430\u043d 2 https:\/\/orcid.org\/0000-0003-0964-6003 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\u0438\u0457\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 \u0422\u0430\u0440\u0430\u0441\u0430 \u0428\u0435\u0432\u0447\u0435\u043d\u043a\u0430, \u041d\u0430\u0432\u0447\u0430\u043b\u044c\u043d\u043e-\u043d\u0430\u0443\u043a\u043e\u0432\u0438\u0439 \u0456\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u00ab\u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar 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