{"id":2425,"date":"2025-12-16T12:00:59","date_gmt":"2025-12-16T10:00:59","guid":{"rendered":"https:\/\/www.g-o-f.org.ua\/?page_id=2425"},"modified":"2025-12-18T13:30:39","modified_gmt":"2025-12-18T11:30:39","slug":"gof-2025-46-056","status":"publish","type":"page","link":"https:\/\/www.g-o-f.org.ua\/gb\/archive\/2025-46\/gof-2025-46-056\/","title":{"rendered":"AGE OF METAVOLCANIC ROCKS OF ACIDIC COMPOSITION OF THE METAMORPHIC COMPLEX OF THE NORTHWESTERN PART OF THE MARMAROSH MASSIF (UKRAINIAN CARPATHIANS)"},"content":{"rendered":"<p><strong>Stepanyuk \u00a0L.M.<\/strong>, \u00a0stepaniuk@nas.gov.ua, \u00a0<a href=\"https:\/\/orcid.org\/0000-0001-5591-5169\">https:\/\/orcid.org\/0000-0001-5591-5169<\/a><br \/>\n<strong>Dovbush<\/strong><strong> \u00a0T.I.<\/strong>,\u00a0 \u00a0tetyana.dovbush1@gmail.com,\u00a0 \u00a0<a href=\"https:\/\/orcid.org\/0000-0002-3512-3313\">https:\/\/orcid.org\/0000-0002-3512-3313<\/a><br \/>\n<strong>V<\/strong><strong>ysotsky<\/strong><strong> \u00a0O.B.<\/strong>, \u00a0alek.vysotsky@gmail.com, \u00a0<a href=\"https:\/\/orcid.org\/0000-0002-3542-4685\">https:\/\/orcid.org\/0000-0002-3542-4685<\/a><br \/>\n<strong>Baran<\/strong><strong> \u00a0A.M.<\/strong>, \u00a0baranandrew9@gmail.com, \u00a0<a href=\"https:\/\/orcid.org\/0000-0002-5326-8014\">https:\/\/orcid.org\/0000-0002-5326-8014<\/a><br \/>\n<strong>Kanuniko<\/strong><strong>v<\/strong><strong>a<\/strong><strong> \u00a0L.I.<\/strong>, \u00a0Kanunikova59@gmail.com, \u00a0<a href=\"https:\/\/orcid.org\/0000-0002-7530-969\u0425\">https:\/\/orcid.org\/0000-0002-7530-969\u0425<\/a><\/p>\n<p>M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine, 34, Acad. Palladin Ave., Kyiv, Ukraine, 03142<\/p>\n<p><a href=\"https:\/\/doi.org\/10.15407\/gof.2025.46.056\">https:\/\/doi.org\/10.15407\/gof.2025.46.056<\/a><\/p>\n<p style=\"text-align: justify;\">Metavolcanites of acidic composition are quite common formations among the rocks of the crystalline complex of the Marmarosh massif \u2014 the Dilovetska, Bredetselska, Tulgesh series, etc. Due to weak metamorphic transformations, metamorphically in greenschist facies conditions, they are easily diagnosed in the field. This report presents the results of uranium-lead isotope dating (TIMS method) of multigrain samples of zircon crystals from the metagranite-porphyry of the Saulyak deposit (Rakhiv Mountains) and the porphyroid of the Perkalab stream (Chyvchyn Mountains). According to the upper section of the concordia regression line, the age of the metagranite-porphyry is 505 \u00b1 25 Ma, the porphyroid \u2014 482 \u00b1 51 Ma. The weighted average age of the metagranite-porphyry by the isotopic ratio 207Pb\/206Pb is 515.5 \u00b1 4.3 Ma and the porphyroid \u2014 474 \u00b1 3.6 Ma.<\/p>\n<p><strong><em>Keywords:<\/em><\/strong> <em>uranium-lead isotope method, zircon, metavolcanites, Marmarosh massif, Ukrainian Carpathians.<\/em><\/p>\n<p><a href=\"http:\/\/www.g-o-f.org.ua\/wp-content\/uploads\/2025\/12\/gof.2025.46.056.pdf\"><strong>Download<\/strong><strong> (PD<\/strong><strong>F)<\/strong><\/a><\/p>\n<p><strong>Refer<\/strong><strong>ences<\/strong><\/p>\n<p>Bartnytskyi, N., Bibikova, E.V., Verkhogliad, V.M., Legkova, G.V., Skobelev, V.M., Terets, G.Ya. (1995). An international zircon standard for uranium-lead isotope studies. <em>Geochemistry and ore formation<\/em>, 21, pp. 164-167 [in Russian].<\/p>\n<p>Boyko, K. (1970). Pre-Upper Paleozoic complex of the northwestern end of the Marmarosh massif (Eastern Karapty). Lviv: Lviv University Press. 246 p. [in Russian].<\/p>\n<p>Voloshin, A. (1981). Geological structure and ore-bearing capacity of the northwestern end of the Marmarosh massif. Kyiv: Nauk. Dumka. 108 p. [in Russian].<\/p>\n<p>Matkovsky, I. (1971). Mineralogy and petrography of the Chivchin Mountains (Ukrainian Carpathians). Lviv: Lviv University Press. 224 p. [in Russian].<\/p>\n<p>Matskiv, V., Pukach, B.D., Vorobkanych, V.M. et al. (2009). State Geological Map of Ukraine. Scale 1:200,000. Carpathian Series. Sheets: M-34-XXXVI (Khust), L-34-VI (Baya Mare), M-35-XXXI (Nadvirna), L-35-I (Visheu). Kyiv. 178 \u0440. [in Ukrainian].<\/p>\n<p>Stepanyuk M. Geochronology of igneous rocks of acidic composition of the northwestern part of the Marmarosh mas- sif : author\u2019s abstract. dis. \u2026 candidate of geol.- min. sciences: 04.00.02. Kyiv, 1986. 20 p. [in Russian].<\/p>\n<p>Stepanyuk, M. (1993). Petrochemical features and age of metavolcanics of acidic composition of the metamorphic complex of the northwestern part of the Marmarosh massif. <em>Geochemistry and ore formation<\/em>, Iss. 20, pp. 48-55. [in Russian].<\/p>\n<p>Shcherbak, P., Stepanyuk, L.M., Bartnitsky, E.N., Komaristy ,A.A. (1986). Age of the most ancient volcanism in the Soviet Carpathians. <em>Reports of the Academy of Sciences of the Ukrainian SSR<\/em>, <em>Series. B<\/em>, No. 11, pp. 26-28 [in Russian].<\/p>\n<p>Gaw\u0119da, , Szopa, K., Golonka, J., Chew, D., Stepanyuk, L., Belskyy, V., Wa\u015bkowska, A., Siliauskas, L., Drakou, F. (2022). Collision with Gondwana or with Baltica? Ordovician magmatic arc volcanism in the Marmarosh Massif (Eastern Carpathians, Ukraine). <em>International Journal of Earth Sciences. <\/em>https:\/\/doi.org\/10.1007\/s00531-022-02228-8<\/p>\n<p>Krough, T.E. (1973). A law contamination method for hedrotermal decomposition of zircon and extraction of U and Pb for isotopic age Geochiica. Cosmochimica Acta. 37, No. 3. pp. 485-494.<\/p>\n<p>Ludwig, R. (1989). Pb Dating for MS-DOS, version 1.06. U.S. Geol. Survey Open-File Rept. No. 88-542. P. 40.<\/p>\n<p>Ludwig, R. (1990). ISOPLOT for MS-DOS, version 2.0. U.S. Geol. Survey Open-File Rept. 1990. No. 88-557. P. 38.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Stepanyuk \u00a0L.M., \u00a0stepaniuk@nas.gov.ua, \u00a0https:\/\/orcid.org\/0000-0001-5591-5169 Dovbush \u00a0T.I.,\u00a0 \u00a0tetyana.dovbush1@gmail.com,\u00a0 \u00a0https:\/\/orcid.org\/0000-0002-3512-3313 Vysotsky \u00a0O.B., \u00a0alek.vysotsky@gmail.com, \u00a0https:\/\/orcid.org\/0000-0002-3542-4685 Baran \u00a0A.M., \u00a0baranandrew9@gmail.com, \u00a0https:\/\/orcid.org\/0000-0002-5326-8014 Kanunikova \u00a0L.I., \u00a0Kanunikova59@gmail.com, \u00a0https:\/\/orcid.org\/0000-0002-7530-969\u0425 M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine, 34, Acad. Palladin Ave., Kyiv, Ukraine, 03142 https:\/\/doi.org\/10.15407\/gof.2025.46.056 Metavolcanites of acidic composition are quite common formations among the rocks of the &hellip; <a href=\"https:\/\/www.g-o-f.org.ua\/gb\/archive\/2025-46\/gof-2025-46-056\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;AGE OF METAVOLCANIC ROCKS OF ACIDIC COMPOSITION OF THE METAMORPHIC COMPLEX OF THE NORTHWESTERN PART OF THE MARMAROSH MASSIF (UKRAINIAN CARPATHIANS)&#8221;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":2361,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-2425","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-D7","jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":2345,"url":"https:\/\/www.g-o-f.org.ua\/gb\/archive\/2024-45\/gof-2024-45-064\/","url_meta":{"origin":2425,"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 kovtun85@ukr.net; https\/\/orcid: 0000-0003-0475-8778 \u041b.\u041c. \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a stepaniuk@nas.gov.ua, https:\/\/orcid.org\/0000-0001-5591-5169 \u041e.\u0412. \u0417\u044e\u043b\u044c\u0446\u043b\u0435 olegzjults@gmail.com, https:\/\/orcid.org\/0000-0002-6204-2009 \u041e.\u0411. \u0412\u0438\u0441\u043e\u0446\u044c\u043a\u0438\u0439 alek.vysotsky@gmail.com; https\/\/orcid.org\/0000-0002-3542-4685 \u0422.\u0406. \u0414\u043e\u0432\u0431\u0443\u0448 tetyana.dovbush1@gmail.com, https:\/\/orcid.org\/0000-0002-3512-3313 \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 \u0440\u043e\u0437\u0441\u0456\u043a\u0430\u0454\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":2324,"url":"https:\/\/www.g-o-f.org.ua\/gb\/archive\/2024-45\/gof-2024-45-044\/","url_meta":{"origin":2425,"position":1},"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. \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a stepaniuk@nas.gov.ua, https:\/\/orcid.org\/0000-0001-5591-5169 \u041e.\u0411. \u0412\u0438\u0441\u043e\u0446\u044c\u043a\u0438\u0439 vysotsky@nas.gov.ua, https:\/\/orcid.org\/0000-0002-3542-4685 \u0410.\u041c. \u0411\u0430\u0440\u0430\u043d https:\/\/orcid.org\/0000-0002-5326-8014 \u041e.\u0412. \u041a\u043e\u0432\u0442\u0443\u043d https:\/\/orcid.org\/0000-0003-0475-8778 \u0422.\u0406. \u0414\u043e\u0432\u0431\u0443\u0448 https:\/\/orcid.org\/0000-0002-3512-3313 \u041d.\u041e. \u041a\u043e\u0432\u0430\u043b\u0435\u043d\u043a\u043e https:\/\/orcid.org\/0000-0002-3203-7145 \u0406.\u041c. \u041a\u043e\u0442\u0432\u0456\u0446\u044c\u043a\u0430 https:\/\/orcid.org\/0000-0002-2593-3953 \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.2024.45.044 \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), \u043f\u0435\u0433\u043c\u0430\u0442\u043e\u0457\u0434\u043d\u043e\u0433\u043e \u0433\u0440\u0430\u043d\u0456\u0442\u0443\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":2151,"url":"https:\/\/www.g-o-f.org.ua\/gb\/archive\/2023-44\/6-6\/","url_meta":{"origin":2425,"position":2},"title":"U-Pb SYSTEM ZIRCON FROM CATACLAZED PLAGIOGRANITOIDS (NOVO-PAVLIVKA GREENSTONE STRUCTURE OF THE MIDDLE-DNIEPER MEGABLOCK)","author":"admin","date":"17\/12\/2023","format":false,"excerpt":"{:uk}\u0413.\u0412. \u0410\u0440\u0442\u0435\u043c\u0435\u043d\u043a\u043e1 E-mail: regulgeo@gmail.com; https:\/\/orcid.org\/0000-0002-4528-6853 \u041b.\u041c. \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a1 E-mail: stepaniuk@nas.gov.ua; https:\/\/orcid.org\/0000-0001-5591-5169 \u041b.\u0421. \u0414\u043e\u0432\u0431\u0438\u04481 E-mail: dovbyshls@ukr.net; https:\/\/orcid.org\/0000-0003-4529-448X \u041e.\u0412. \u0417\u044e\u043b\u044c\u0446\u043b\u04351 E-mail: olegzjults@gmail.com; https\/\/orcid.org\/0000-0002-6204-2009 \u0410.\u0412. \u041c\u0430\u0440\u0442\u0438\u043d\u044e\u043a2 E-mail: 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 post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":1784,"url":"https:\/\/www.g-o-f.org.ua\/gb\/archive\/2020-41\/8-2\/","url_meta":{"origin":2425,"position":3},"title":"U-Pb geochronology by zircon of fine-grained granite of the Osnitsky complex. (Volinsky megablok US)","author":"admin","date":"09\/12\/2020","format":false,"excerpt":"{:uk}\u041e.\u0411. \u0412\u0438\u0441\u043e\u0446\u044c\u043a\u0438\u0439 E-mail: alek.vysotsky@gmail.com, https:\/\/orcid.org\/0000-0002-3542-4685 \u041b.\u041c. \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a https:\/\/orcid.org\/0000-0001-5591-5169 \u0422.\u0406. \u0414\u043e\u0432\u0431\u0443\u0448 https:\/\/orcid.org\/0000-0002-3512-3313 \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\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 \u041d\u0430\u0432\u0435\u0434\u0435\u043d\u043e \u0440\u0435\u0437\u0443\u043b\u044c\u0442\u0430\u0442\u0438 \u0443\u0440\u0430\u043d-\u0441\u0432\u0438\u043d\u0446\u0435\u0432\u043e\u0433\u043e \u0434\u0430\u0442\u0443\u0432\u0430\u043d\u043d\u044f \u0446\u0438\u0440\u043a\u043e\u043d\u0443 \u0437 \u0434\u0440\u0456\u0431\u043d\u043e\u0437\u0435\u0440\u043d\u0438\u0441\u0442\u043e\u0433\u043e \u0433\u0440\u0430\u043d\u0456\u0442\u0443 \u041e\u0441\u043d\u0438\u0446\u044c\u043a\u043e\u0433\u043e \u0431\u043b\u043e\u043a\u0443 \u0412\u043e\u043b\u0438\u043d\u0441\u044c\u043a\u043e\u0433\u043e \u043c\u0435\u0433\u0430\u0431\u043b\u043e\u043a\u0443 \u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u043e\u0433\u043e \u0449\u0438\u0442\u0430. \u0420\u0456\u0437\u043d\u043e\u043c\u0430\u043d\u0456\u0442\u043d\u0456\u0441\u0442\u044c \u0433\u0440\u0430\u043d\u0456\u0442\u0456\u0432 \u043e\u0441\u043d\u0438\u0446\u044c\u043a\u043e\u0433\u043e \u043a\u043e\u043c\u043f\u043b\u0435\u043a\u0441\u0443 \u043f\u0440\u043e\u044f\u0432\u043b\u044f\u0454\u0442\u044c\u0441\u044f\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar 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":2124,"url":"https:\/\/www.g-o-f.org.ua\/gb\/archive\/2023-44\/4-4\/","url_meta":{"origin":2425,"position":4},"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":1766,"url":"https:\/\/www.g-o-f.org.ua\/gb\/archive\/2020-41\/6-2\/","url_meta":{"origin":2425,"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 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