{"id":619,"date":"2018-05-19T20:39:36","date_gmt":"2018-05-19T17:39:36","guid":{"rendered":"http:\/\/www.g-o-f.org.ua\/?page_id=619"},"modified":"2019-05-28T11:18:30","modified_gmt":"2019-05-28T08:18:30","slug":"%d0%b0%d0%bf%d0%be%d1%84%d0%b5%d0%bd%d1%96%d1%82%d0%be%d0%b2%d1%96-%d0%b0%d0%bb%d1%8c%d0%b1%d1%96%d1%82%d0%b8%d1%82%d0%b8-%d1%83%d0%ba%d1%80%d0%b0%d1%97%d0%bd%d1%81%d1%8c%d0%ba%d0%be%d0%b3%d0%be","status":"publish","type":"page","link":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2017-2\/%d0%b0%d0%bf%d0%be%d1%84%d0%b5%d0%bd%d1%96%d1%82%d0%be%d0%b2%d1%96-%d0%b0%d0%bb%d1%8c%d0%b1%d1%96%d1%82%d0%b8%d1%82%d0%b8-%d1%83%d0%ba%d1%80%d0%b0%d1%97%d0%bd%d1%81%d1%8c%d0%ba%d0%be%d0%b3%d0%be\/","title":{"rendered":"Apofenitic albitites of the Ukrainian Shield"},"content":{"rendered":"<p style=\"text-align: center;\"><strong>Summary<\/strong><\/p>\n<p><strong>Apofenitic albitites of the Ukrainian Shield<\/strong><\/p>\n<p><em>Kryvdik S.G. M.<\/em><br \/>\nM.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Science of Ukraine<\/p>\n<p>Language: Ukrainian<br \/>\nGeochemistry and ore formation 2017, 38: 58-69<\/p>\n<p><a href=\"https:\/\/doi.org\/10.15407\/gof.2017.38.058\">https:\/\/doi.org\/10.15407\/gof.2017.38.058<\/a><\/p>\n<p style=\"text-align: justify;\">Apofenitic albitites were discovered in the Azov Sea area (the Chernigivka carbonatite massif, the fenites of Dmitrovka village, Tunikova ravine), in the western part of the Ukrainian shield (Proskurivska massif of alkaline rocks, Beryozovaya Gat\u2019s fenites) and in the Middle Dnieper region (Mala Tersa alkaline massif). These albitites form on pyroxene fenites (more often as vein-like bodies), whereas in the Chernigivka massif they occur in the endocontact of carbonatite bodies. During formation of apofenitic albitites process, such metasomatic alteration of fenites occur most often: instead of alkaline perthite feldspars a granoblastic aggregate predominantly with albite and subordinate amount of microcline and calcite is formed, and alkaline pyroxene is replaced by Fe-Mg biotite. Sometimes the Ca-Al-amphibole of the edenite-hastingsite composition crystallize. In comparison with initial fenites these albitites have lower alkalinity ((Na + K)\/Al), because the alkaline pyroxene is replaced by biotite, and instead of aluminumless and alkaline amphiboles (richterites, riebeckites, arfvedsonites) Ca-Al-amphiboles (edenite-hastingsite series) are crystallized. The most interesting feature of apofenitic albites is increased in or high Zr, Nb and U concentration (in comparison with fenites or even carbonatites) which are concentrated in zircon, columbite, pyrochlore group minerals the formation of apofenitic albitites is due to the increasing acidity (and water enrichment) of the primary ultralkalinity fluids at the early stages the fenitization of granitoids caused, and at the final stages (during cooling, lowering of alkalinity and water enrichment) led the alteration of the fenites with the formation of ore-bearing albitites. The enriched in Zr and Nb apofenitic albitites in the geochemical aspect are similar to the mariupolites, but they differ significantly from the latter. The nepheline as main mineral of mariupolites is absent in albitites, but the latter have Fe-Mg-micas and amphiboles. The secondary micas from mariupolites are presented by strongly enriched in Fe and Mn biotites. Marioupolites in comparison with albitites are enriched in REE and depleted in Sr. Apofenitic albitites are the original metasomatites for Ukraine and they can be considered as new type of ore-bearing rocks for such rare metals as Nb, Ta and Zr.<\/p>\n<p>Key words: apofenitic albitites, biotite, Ca-Al-amphibole, zircon, columbite, pyrochlore<\/p>\n<p><strong>References<\/strong><\/p>\n<p>1. Belevcev, Ya.N. (Ed.) (1995). Ge netical types and regularities in the location of the uranium deposits in Ukraine [Henetycheskye typy y zakonomernosty razmeshhenyya uranovyh mestorozhdenyj Ukrayny]. Kyiv, Naukova dumka. 396 p. [in Russian].<\/p>\n<p>2. Hlevasskyj, E.B., Kryvdyk, S.H. (1981). Precambrian carbonatite complex of the Azov Sea area [Dokembryjskyj karbonatytovyj kompleks Pryazov&#8217;ya]. Kyiv, Naukova dumka. 227 p. [in Russian].<\/p>\n<p>3. Donskoj, A.N., Sharkyn, O.P . (1986). 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Geohemistry and Ore Formation. 33. pp. 3-17 [in Ukrainian].<\/p>\n<p>7. Kryvdyk, S.H., Braclavskyj, P. F . (1987). Fenites of the Proskurovsky massif (Dnister-Bug area) [Fenyty Proskurovskoho massyva (Prydnestrov&#8217;e)]. Geol. Journ. 17, No. 2. pp. 111-124 [in Russian].<\/p>\n<p>8. Kryvdik, S.H., Dubyna, O.V. (2005).Chemical peculiarities of minerals from alkali-ultramafic complexes of the Ukrainian Shield as an indicator of their depth formation [Typohimizm mineraliv luzhno-ul&#8217;traosnovnyh kompleksiv Ukrayins&#8217;koho shhyta yak indykator hlybynnosti yih formuvannya]. Mineral. Journ. (Ukraine). 27. No. 1. pp. 64-76 [in Ukrainian].<\/p>\n<p>9. Kryvdyk, S.H., Tkachuk, V.Y. (1990). Petrology of alkaline rocks of the Ukrainian shield [Petrolohyya shhelochnyh porod Ukraynskoho shhyta]. Kyiv, Naukova dumka. 408 p. [in Russian].<\/p>\n<p>10. Kryvdik, S.H., Morhun, V.H., Dubyna, O.V. (2012). Alkaline metasomatite types of the Ukrainian shield and depth their formation [Typy luzhnyh metasomatytiv Ukrayins&#8217;koho shhyta ta faciyi yih hlybynnosti]. Geohemistry and Ore Formation. No. 31-32. pp. 4-11 [in Ukrainian].<\/p>\n<p>11. Kryvdik, S.H., Morhun, V.H., Sharyhin, V.V. (2010). Micas of fenites and alkaline metasomatites of the Eastern Azov [Slyudy fenitiv i luzhnyh metasomatytiv Shidnoho Pryazov&#8217;ya]. Mineral. Journ. (Ukraine). No. 4. pp. 3-11 [in Ukrainian].<\/p>\n<p>12. Kryvdyk, S.H., Tsymbal, S.N., Hejko, Yu.V. (2003). Proterozoic alkaline-ultrabasic magmatism in the northwestern part of the Ukrainian shield as an indicator of kimberlite formation [Proterozojskyj shhelochno-ul&#8217;traosnovnoj mahmatyzm severo-zapadnoj chasty Ukraynskoho shhyta kak yndykator kymberlytoobrazovanyya]. Mineral. Journ. (Ukraine). 25, No. 5\/6. pp. 57-69 [in Russian].<\/p>\n<p>13. Kryvdyk, S.H., Sharyhyn, V.V., Morhun, V.H. (2011). 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Geochemistry of niobium and uranium ore albitites of the Novooleksiyivka occurrence, Ukrainian Shield [Heohimiya niobiyu i uranu v al&#8217;bitytah Novooleksiyivs&#8217;koho rudoproyavu, Ukrayin s&#8217;kyj shhyt]. Geohemistry and Ore Formation. 35. pp. 19-28 [in Ukrainian].<\/p>\n<p>18. Morhun, V.H. (2012). Petrology of alkaline metasomatites of the Eastern Azov [Petrolohiya luzhnyh metasomatytiv Shidnoho Pryazov&#8217;ya]. Thesis for a PhD degree in geological science. Kyiv . 24 p. [in Ukrainian].<\/p>\n<p>19. Nechelyustov, H.N., Pozharyckaya, L.K. (1986). Pyrochlore composition evolution in one of the carbonatite complexes of the East European Platform [Evolyucyya sostava pyrohlora v odnom yz karbonatytovyh kompleksov VostochnoEvropejskoj platform]. Mineral. Journ. (Ukraine). 8. No. 5. pp. 38-48 [in Russian].<\/p>\n<p>20. Stepaniuk, L.M., Bondarenko, S.M., S&#8217;omka, V.O., Kotvic&#8217;ka, I.M., Andreyev , O.V. (2012). The source of sodium and uranium in the uranbearing albitites (for example Dokuchayevsk deposit in the Ingulskiy megablock of the Ukrainian Shield) [Dzherelo natriyu ta uranu uranonosnyh al&#8217;bitytiv (na prykladi Dokuchayivs&#8217;koho rodovyshha Inhul&#8217;s&#8217;koho mehabloku Ukrayins&#8217;koho shhyta)]. Geohemistry and Ore Formation. No. 31-32. pp. 99-104 [in Ukrainian].<\/p>\n<p>21. Tymoshenko, O.D. (1975). Geology, composition and ore mineralization prospects in the Malotersyansky alkaline massif (Middle Pridneprovie) [Heolohyya, veshhestvennyj sostav y perspektyvy rudonosnosty Malotersyanskoho shhelochnoho massyva (Srednee Prydneprov&#8217;e)]. Thesis for a PhD degree in geological and mineralogical science. Khar&#8217;kov . 24 p. [in Russian].<\/p>\n<p>22. Tsymbal, S.N., Shherbakov, Y.B., Kryvdyk, S.H., Labuznyj, V.F . (1997). Alkaline-ultramafic rocks of Gorodnitskaya intrusion (northwest of the Ukrainian shield) [Shhelochno-ul&#8217;traosnovnye porody Horodnyckoj yntruzyy (severo-zapad UShh)]. Mineral. Journ. (Ukraine). 19. No. 3. pp. 61-81 [in Russian].<\/p>\n<p>23. Cirelu, Sandrine (2008). Metasomatose sodique et Mineralisations uraniferes associees: Exemples du district de Kirovograd-Novoukrainsk (Ukraine), du Gatholite du Kurupung (Guyana), et du Gisement d&#8217;Espinharas (Bresil). These, Docteur de l&#8217;Universite Henri Poincare, Nansy I en Geosciences. pp. 59-63.<\/p>\n<p><a href=\"http:\/\/www.g-o-f.org.ua\/wp-content\/uploads\/2017\/6.pdf\">Download (PDF)<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Summary Apofenitic albitites of the Ukrainian Shield Kryvdik S.G. M. M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Science of Ukraine Language: Ukrainian Geochemistry and ore formation 2017, 38: 58-69 https:\/\/doi.org\/10.15407\/gof.2017.38.058 Apofenitic albitites were discovered in the Azov Sea area (the Chernigivka carbonatite massif, the fenites of Dmitrovka village, &hellip; <a href=\"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2017-2\/%d0%b0%d0%bf%d0%be%d1%84%d0%b5%d0%bd%d1%96%d1%82%d0%be%d0%b2%d1%96-%d0%b0%d0%bb%d1%8c%d0%b1%d1%96%d1%82%d0%b8%d1%82%d0%b8-%d1%83%d0%ba%d1%80%d0%b0%d1%97%d0%bd%d1%81%d1%8c%d0%ba%d0%be%d0%b3%d0%be\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Apofenitic albitites of the Ukrainian Shield&#8221;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":242,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-619","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-9Z","jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":954,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2018-39\/","url_meta":{"origin":619,"position":0},"title":"2018. Vol 39","author":"admin","date":"10\/12\/2018","format":false,"excerpt":"{:uk}\u0417\u041c\u0406\u0421\u0422 \u0417 \u043d\u0430\u0433\u043e\u0434\u0438 \u0441\u0442\u043e\u0440\u0456\u0447\u043d\u043e\u0433\u043e \u044e\u0432\u0456\u043b\u0435\u044e \u041d\u0430\u0446\u0456\u043e\u043d\u0430\u043b\u044c\u043d\u043e\u0457 \u0430\u043a\u0430\u0434\u0435\u043c\u0456\u0457 \u043d\u0430\u0443\u043a \u0423\u043a\u0440\u0430\u0457\u043d\u0438 \u041b.\u041c. \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a, \u0421.\u0413. \u041a\u0440\u0438\u0432\u0434\u0456\u043a \u0413\u0435\u043e\u0445\u0456\u043c\u0456\u044f \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f 2018, 39: 3-5 \u0413\u0435\u043e\u0445\u0456\u043c\u0456\u044f \u0456 \u043f\u0435\u0442\u0440\u043e\u043b\u043e\u0433\u0456\u044f \u043f\u0440\u043e\u0446\u0435\u0441\u0456\u0432 \u043f\u043e\u0440\u043e\u0434\u043e- \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f \u0428\u0435\u0440\u0435\u043c\u0435\u0442 \u0415.\u041c., \u041d\u0438\u043a\u043e\u043b\u0430\u0435\u0432 \u0418.\u042e., \u0421\u0435\u0442\u0430\u044f \u041b.\u0414., \u0410\u0433\u0430\u0440\u043a\u043e\u0432\u0430 \u041d.\u0413. \u0412\u0438\u0434\u0456\u043b\u0435\u043d\u043d\u044f \u043f\u0440\u043e\u0433\u043d\u043e\u0437\u043d\u0438\u0445 \u043f\u043b\u043e\u0449 \u0437\u043e\u043d \u043c\u0435\u0442\u0430\u0441\u043e\u043c\u0430\u0442\u0438\u0442\u0456\u0432 \u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u043e\u0433\u043e \u0449\u0438\u0442\u0430 \u0433\u0435\u043e\u0435\u043b\u0435\u043a\u0442\u0440\u0438\u0447\u043d\u0438\u043c\u0438 \u043c\u0435\u0442\u043e\u0434\u0430\u043c\u0438 \u0413\u0435\u043e\u0445\u0456\u043c\u0456\u044f \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f 2018, 39: 6-15 https:\/\/doi.org\/10.15407\/gof.2018.39.006\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":242,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2017-2\/","url_meta":{"origin":619,"position":1},"title":"2017.Vol 38","author":"admin","date":"09\/10\/2017","format":false,"excerpt":"{:uk}\u0417\u041c\u0406\u0421\u0422 \u0413\u0435\u043e\u0445\u0456\u043c\u0456\u044f \u0456 \u043f\u0435\u0442\u0440\u043e\u043b\u043e\u0433\u0456\u044f \u043f\u0440\u043e\u0446\u0435\u0441\u0456\u0432 \u043f\u043e\u0440\u043e\u0434\u043e- \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a \u041b.\u041c., \u041a\u0443\u0440\u0438\u043b\u043e \u0421.\u0406., \u0414\u043e\u0432\u0431\u0443\u0448 \u0422.\u0406., \u0413\u0440\u0456\u043d\u0447\u0435\u043d\u043a\u043e \u041e.\u0412., \u0421\u044c\u043e\u043c\u043a\u0430 \u0412.\u041e., \u0411\u043e\u043d\u0434\u0430\u0440\u0435\u043d\u043a\u043e \u0421.\u041c., \u0428\u0443\u043c\u043b\u044f\u043d\u0441\u044c\u043a\u0438\u0439 \u041b.\u0412. \u0413\u0435\u043e\u0445\u0440\u043e\u043d\u043e\u043b\u043e\u0433\u0456\u044f \u0433\u0440\u0430\u043d\u0456\u0442\u043e\u0457\u0434\u0456\u0432 \u0441\u0445\u0456\u0434\u043d\u043e\u0457 \u0447\u0430\u0441\u0442\u0438\u043d\u0438 \u0406\u043d\u0433\u0443\u043b\u044c\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 \u0413\u0435\u043e\u0445\u0456\u043c\u0456\u044f \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f 2017, 38: 3-13 https:\/\/doi.org\/10.15407\/gof.2017.38.003 \u041a\u0440\u0430\u0432\u0447\u0435\u043d\u043a\u043e \u0413.\u041b., \u0420\u0443\u0441\u0430\u043a\u043e\u0432 \u041d.\u0424. \u041d\u043e\u0432\u0456 \u0434\u0430\u043d\u0456 \u043f\u0440\u043e \u043c\u0435\u0442\u0430\u0443\u043b\u044c\u0442\u0440\u0430\u0431\u0430\u0437\u0438\u0442\u0438 \u0426\u0435\u043d\u0442\u0440\u0430\u043b\u044c\u043d\u043e\u0433\u043e \u041f\u0440\u0438\u0430\u0437\u043e\u0432\u2019\u044f \u0413\u0435\u043e\u0445\u0456\u043c\u0456\u044f \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":253,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2013-2\/","url_meta":{"origin":619,"position":2},"title":"2013. Vol 33","author":"admin","date":"09\/10\/2017","format":false,"excerpt":"{:uk}\u0417\u041c\u0406\u0421\u0422 \u0413\u0435\u043e\u0445\u0456\u043c\u0456\u044f \u0456 \u043f\u0435\u0442\u0440\u043e\u043b\u043e\u0433\u0456\u044f \u043f\u0440\u043e\u0446\u0435\u0441\u0456\u0432 \u043f\u043e\u0440\u043e\u0434\u043e- \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f \u041a\u0440\u0438\u0432\u0434\u0456\u043a \u0421.\u0413. \u041f\u0440\u043e \u0433\u0435\u043d\u0435\u0437\u0438\u0441 \u043b\u0443\u0436\u043d\u0438\u0445 \u043c\u0435\u0442\u0430\u0441\u043e\u043c\u0430\u0442\u0438\u0442\u0456\u0432 \u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u043e\u0433\u043e \u0449\u0438\u0442\u0430 https:\/\/doi.org\/10.15407\/gof.2013.33.003 \u041a\u0440\u0430\u0432\u0447\u0435\u043d\u043a\u043e \u0413.\u041b. \u041e\u0441\u043e\u0431\u043b\u0438\u0432\u043e\u0441\u0442\u0456 \u0441\u043a\u043b\u0430\u0434\u0443 \u043f\u043e\u0440\u0456\u0434 \u043e\u0441\u0438\u043f\u0435\u043d\u043a\u0456\u0432\u0441\u044c\u043a\u043e\u0457 \u0441\u0435\u0440\u0456\u0457 \u0428\u0435\u0432\u0447\u0435\u043d\u043a\u0456\u0432\u0441\u044c\u043a\u043e\u0457 \u0441\u0442\u0440\u0443\u043a\u0442\u0443\u0440\u0438 (\u0424\u0435\u0434\u043e\u0440\u0456\u0432\u0441\u044c\u043a\u0430 \u0437\u043e\u043d\u0430, \u041f\u0440\u0438\u0430\u0437\u043e\u0432\u2019\u044f) https:\/\/doi.org\/10.15407\/gof.2013.33.018 \u0406\u0432\u0430\u043d\u043e\u0432 \u0411.\u041d., \u0417\u0430\u043d\u043a\u0435\u0432\u0438\u0447 \u0411.\u041e., \u041c\u0438\u0445\u0430\u043b\u044c\u0447\u0435\u043d\u043a\u043e \u0406.\u0406., \u0428\u0430\u0444\u0440\u0430\u043d\u0441\u044c\u043a\u0430 \u041d.\u0412. \u0423\u0440\u0430\u043d\u043e\u043d\u043e\u0441\u043d\u0456 \u043d\u0430\u0442\u0440\u0456\u0454\u0432\u0456 \u043c\u0435\u0442\u0430\u0441\u043e\u043c\u0430\u0442\u0438\u0442\u0438 \u0412\u0430\u0442\u0443\u0442\u0438\u043d\u0441\u044c\u043a\u043e\u0433\u043e \u0440\u043e\u0434\u043e\u0432\u0438\u0449\u0430 (\u0441\u0442\u0440\u0443\u0442\u043a\u0443\u0440\u043d\u0430 \u043f\u043e\u0437\u0438\u0446\u0456\u044f \u0442\u0430 \u043e\u0441\u043e\u0431\u043b\u0438\u0432\u043e\u0441\u0442\u0456 \u043b\u043e\u043a\u0430\u043b\u0456\u0437\u0430\u0446\u0456\u0457 \u0431\u0430\u0433\u0430\u0442\u0438\u0445 \u0440\u0443\u0434)\u2026","rel":"","context":"In \"2013. \u0412\u044b\u043f\u0443\u0441\u043a 33\"","block_context":{"text":"2013. \u0412\u044b\u043f\u0443\u0441\u043a 33","link":"http:\/\/www.g-o-f.org.ua\/gb\/tag\/2013-%d0%b2%d1%8b%d0%bf%d1%83%d1%81%d0%ba-33\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":256,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2012-2\/","url_meta":{"origin":619,"position":3},"title":"2012. Vol 31-32","author":"admin","date":"09\/10\/2017","format":false,"excerpt":"{:uk}\u0417\u041c\u0406\u0421\u0422 \u0417\u0431\u0456\u0440\u043d\u0438\u043a\u0443 \"\u0413\u0435\u043e\u0445\u0456\u043c\u0456\u044f \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f\" \u2013 40 \u0440\u043e\u043a\u0456\u0432 \u0413\u0435\u043e\u0445\u0456\u043c\u0456\u044f \u0456 \u043f\u0435\u0442\u0440\u043e\u043b\u043e\u0433\u0456\u044f \u043f\u0440\u043e\u0446\u0435\u0441\u0456\u0432 \u043f\u043e\u0440\u043e\u0434\u043e- \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f \u041a\u0440\u0438\u0432\u0434\u0456\u043a \u0421.\u0413., \u041c\u043e\u0440\u0433\u0443\u043d \u0412.\u0413., \u0414\u0443\u0431\u0438\u043d\u0430 \u041e.\u0412. \u0422\u0438\u043f\u0438 \u043b\u0443\u0436\u043d\u0438\u0445 \u043c\u0435\u0442\u0430\u0441\u043e\u043c\u0430\u0442\u0438\u0442\u0456\u0432 \u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u043e\u0433\u043e \u0449\u0438\u0442\u0430 \u0442\u0430 \u0444\u0430\u0446\u0456\u0457 \u0457\u0445 \u0433\u043b\u0438\u0431\u0438\u043d\u043d\u043e\u0441\u0442\u0456 https:\/\/doi.org\/10.15407\/gof.2012.31.004 \u041d\u0435\u0447\u0430\u0435\u0432 \u0421.\u0412., \u0421\u044c\u043e\u043c\u043a\u0430 \u0412.\u0410. \u0420\u0443\u0434\u043e\u043d\u043e\u0441\u043d\u0456 \u043c\u0435\u0442\u0430\u0441\u043e\u043c\u0430\u0442\u0438\u0442\u0438 \u0426\u0435\u043d\u0442\u0440\u0430\u043b\u044c\u043d\u043e\u0457 \u0447\u0430\u0441\u0442\u0438\u043d\u0438 \u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u043e\u0433\u043e \u0449\u0438\u0442\u0430 (\u0423\u0429) (\u043f\u0440\u043e\u0433\u043d\u043e\u0437\u043d\u043e-\u043f\u043e\u0448\u0443\u043a\u043e\u0432\u0435 \u0442\u0430 \u0437\u0430\u0433\u0430\u043b\u044c\u043d\u043e\u0433\u0435\u043e\u043b\u043e\u0433\u0456\u0447\u043d\u0435 \u0437\u043d\u0430\u0447\u0435\u043d\u043d\u044f) https:\/\/doi.org\/10.15407\/gof.2012.31.012 \u041f\u043e\u043d\u043e\u043c\u0430\u0440\u0435\u043d\u043a\u043e \u041e.\u041c., \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":988,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2018-39\/8-2\/","url_meta":{"origin":619,"position":4},"title":"Phosphorus in syenites as an indicator of the petrogenesis and ore potential of alkaline complexes of the Ukrainian Shield","author":"admin","date":"10\/12\/2018","format":false,"excerpt":"{:uk}\u0421.\u0413. \u041a\u0440\u0438\u0432\u0434\u0456\u043a1, \u041e.\u0412. \u0414\u0443\u0431\u0438\u043d\u04301,2 1 \u2014 \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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