{"id":1920,"date":"2021-12-15T21:56:52","date_gmt":"2021-12-15T19:56:52","guid":{"rendered":"http:\/\/www.g-o-f.org.ua\/?page_id=1920"},"modified":"2021-12-15T21:56:57","modified_gmt":"2021-12-15T19:56:57","slug":"1-5","status":"publish","type":"page","link":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2021-42\/1-5\/","title":{"rendered":"KAERSUTITIS IN AZOV AREA ROCKS (UKRAINIAN SHIELD): PETROLOGICAL ASPECT"},"content":{"rendered":"

V.O. Gatsenko <\/strong>1<\/strong><\/sup>
https:\/\/orcid.org\/0000-0002-3229-3907<\/a><\/p>\n

S.I. Kurylo <\/strong>2<\/strong><\/sup>
https:\/\/orcid.org\/ 0000-0003-4466-6851<\/a><\/p>\n

1. M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine,
03142, ave. acad. Palladina 34, Kyiv, Ukraine<\/p>\n

2. Earth Science Institute, Slovak Academy of Sciences
97411, \u010eumbierska 1, Bansk\u00e1 Bystrica, Slovakia<\/p>\n

Language: Ukrainian
Geochemistry and ore formation 2021, 42: 48-60<\/p>\n

https:\/\/doi.org\/10.15407\/gof.2021.42.048<\/a><\/p>\n

\u00a0<\/p>\n

\u00a0<\/p>\n

The paper presents the results of new studies of kaersutites from lamprophyres of the Pokrovo-Kyriivo massif (PKM) of the Azov area (Ukrainian Shield). The comparison of mineralogical-petrographic and chemical features of kaersutites of lamprophyres with those of other dyke (microgabroid) and plutonic (pyroxenite) rocks of PKM is carried out and also, with this mineral from the camptonites of the Khlibodar quarry and the pyroxenites of the Chomutov massif. The paper presents the results of new studies of kaersutites from lamprophyres of the Pokrovo-Kyriivo massif (PKM) of the Azov area (Ukrainian Shield). The comparison of mineralogical-petrographic and chemical features of kaersutites of lamprophyres with those of other dyke (microgabroid) and plutonic (pyroxenite) rocks of PKM is carried out and also, with this mineral from the camptonites of the Khlibodar quarry and the pyroxenites of the Chomutov massif. The crystal chemical characteristics of the studied kaersutites were compared with those of other amphiboles in the Azov area. According to the chemical composition of kaersutites, the conditions of kaersutite formation in the mafic rocks of the Azov area region were estimated. Microprobe studies of the chemical composition of kaersutites from kaersutite lamprophyres were performed on JXA- 8520F (JEOL) X-ray microanalyzer equipped with five wave dispersion spectrometers (WDS) at the Institute of Natural Sciences of the Slovak Academy of Sciences (Bysterka Branch). The main characteristics of the chemical composition of kaersutite from kaersutite lamprophyres of PKM are low content of TiO2 (0.5-0.68 f.o.) and Al2O3 (up to 11.4%). Due to the low Al2O3 content, they are similar to kaersutites from afir gabroid and pyroxenite PKM. Kaersutites from other rocks of the Azov area are characterized by a higher content of Al2O3 (more than 12.3%, more often \u2014 13%). The sample of kaersutites from PKM lamprophyres is not homogeneous, which indicates fluctuations in the conditions of rock formation. Most of the studied kaersutites of the Azov area are characterized by #Mg higher than 0.55. The exception is the measured ferrokaersutite from Hlibodarivka camptonite megacrysts (# Mg = 0.43). The vast majority of Azov area kaersutites have a high alkali content (more than 3%). According to their crystal chemical characteristics, kaersutites of the Azov area region differ significantly from other amphiboles of the district. The most highly baric are ferrokaersutites from Hlibodarivka camptonite megacrysts and kaersutite from porphyry amphibole-titanomagnetite microgabrroid PKM. The formation of kaersutite from the mafi\u0441 rocks of the Azov area corresponds to the conditions of high oxygen fugacity. Ferrokaersutite from Hlibodarivka camptonite was formed under conditions of medium oxygen fugacity. Keywords: kaersutite, lamprophyre, mafic dyke, pyroxenites, the Pokrovo-Kyriivo massif, camptonites of the Khlibodar quarry, Azov area.<\/p>\n

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References<\/strong><\/p>\n

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    V.O. Gatsenko 1https:\/\/orcid.org\/0000-0002-3229-3907 S.I. Kurylo 2https:\/\/orcid.org\/ 0000-0003-4466-6851 1. M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine, 03142, ave. acad. Palladina 34, Kyiv, Ukraine 2. Earth Science Institute, Slovak Academy of Sciences97411, \u010eumbierska 1, Bansk\u00e1 Bystrica, Slovakia Language: UkrainianGeochemistry and ore formation 2021, 42: 48-60 https:\/\/doi.org\/10.15407\/gof.2021.42.048 \u00a0 \u00a0 The paper … Continue reading “KAERSUTITIS IN AZOV AREA ROCKS (UKRAINIAN SHIELD): PETROLOGICAL ASPECT”<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":1873,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-1920","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-uY","jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":2025,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2022-43\/7-2\/","url_meta":{"origin":1920,"position":0},"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, 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\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":1926,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2021-42\/1-7\/","url_meta":{"origin":1920,"position":1},"title":"URANIUM-LEAD GEOCHRONOLOGY ON MONACITE OF GRANITES OF THE LYPNYAZKA MASSIF AND ITS FRAMING (INGUL MEGABLOCK OF THE UKRAINIAN SHIELD)","author":"admin","date":"15\/12\/2021","format":false,"excerpt":"{:uk}\u041b.\u041c. \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a 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 \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":1737,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2020-41\/3-2\/","url_meta":{"origin":1920,"position":2},"title":"Ta-Nb mineralization in rare-metal pegmatite from north-western frame of Lypniazhka granite-migmatite structure","author":"admin","date":"09\/12\/2020","format":false,"excerpt":"{:uk}\u0421.\u0406. \u041a\u0443\u0440\u0438\u043b\u043e 1, 3 \u0415-mail: kurylo.sergiy@gmail.com, https:\/\/orcid.org\/0000-0003-4466-6851 \u041d.\u041c. \u041b\u0438\u0436\u0430\u0447\u0435\u043d\u043a\u043e 2 \u0415-mail: lyzhachenko@gmail.com, https:\/\/orcid.org\/0000-0001-8598-0551 \u0421.\u041c. \u0411o\u043d\u0434\u0430\u0440\u0435\u043d\u043a\u043e 3 https:\/\/orcid.org\/0000-0001-7948-3583 \u0412.\u041e. \u0421\u044c\u043e\u043c\u043a\u0430 3 https:\/\/orcid.org\/0000-0001-5202-4045 \u041e.\u0412. \u0413\u0440\u0456\u043d\u0447\u0435\u043d\u043a\u043e 4 https:\/\/orcid.org\/0000-0003-3030-1720 1 \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\u043a 97411, \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, \u0414\u0443\u043c\u0431\u0456\u0454\u0440\u0441\u044c\u043a\u0430, 1 2 \u0414\u0435\u0440\u0436\u0430\u0432\u043d\u0430 \u0443\u0441\u0442\u0430\u043d\u043e\u0432\u0430 \u201c\u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u0433\u0435\u043e\u0445\u0456\u043c\u0456\u0457 \u043d\u0430\u0432\u043a\u043e\u043b\u0438\u0448\u043d\u044c\u043e\u0433\u043e \u0441\u0435\u0440\u0435\u0434\u043e\u0432\u0438\u0449\u0430 \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\u201d\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":2084,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2023-44\/1-1\/","url_meta":{"origin":1920,"position":3},"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 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tetyana.dovbush1@gmail.com, https:\/\/orcid.org\/0000-0002-3512-33131. \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\u04302. \u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u043d\u0430\u0443\u043a \u043f\u0440\u043e \u0437\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,\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":2137,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2023-44\/5-5\/","url_meta":{"origin":1920,"position":5},"title":"THE SPECIFIC URANIUM-LEAD ISOTOPIC SYSTEM OF MONAZITE FROM THE LEUCOCRATE GNEISS OF PRIAZOVIA","author":"admin","date":"17\/12\/2023","format":false,"excerpt":"{:uk}{:uk}\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 \u041e.\u0411. \u0412\u0438\u0441\u043e\u0446\u044c\u043a\u0438\u0439 E-mail: alek.vysotsky@gmail.com, https:\/\/orcid.org\/0000-0002-3542-4685 \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, 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.2023.44.035 \u0414\u043e\u0441\u043b\u0456\u0434\u0436\u0435\u043d\u043e \u0443\u0440\u0430\u043d-\u0441\u0432\u0438\u043d\u0446\u0435\u0432\u0443 \u0456\u0437\u043e\u0442\u043e\u043f\u043d\u0443 \u0441\u0438\u0441\u0442\u0435\u043c\u0443 \u043c\u043e\u043d\u0430\u0446\u0438\u0442\u0456\u0432 \u0456\u0437 \u043b\u0435\u0439\u043a\u043e\u043a\u0440\u0430\u0442\u043e\u0432\u043e\u0433\u043e \u0433\u043d\u0435\u0439\u0441\u0443 (\u041f\u0440\u0438\u0430\u0437\u043e\u0432\u0441\u044c\u043a\u0438\u0439 \u043c\u0435\u0433\u0430\u0431\u043b\u043e\u043a) \u0456 \u0432\u0438\u0437\u043d\u0430\u0447\u0435\u043d\u043e \u0432\u0456\u043a \u0457\u0445 \u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f. \u041c\u043e\u043d\u0430\u0446\u0438\u0442\u0438 \u0456\u0437 \u043b\u0435\u0439\u043a\u043e\u043a\u0440\u0430\u0442\u043e\u0432\u043e\u0433\u043e\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar 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