{"id":1556,"date":"2019-11-28T14:55:49","date_gmt":"2019-11-28T12:55:49","guid":{"rendered":"http:\/\/www.g-o-f.org.ua\/?page_id=1556"},"modified":"2020-12-21T17:52:43","modified_gmt":"2020-12-21T15:52:43","slug":"8-2","status":"publish","type":"page","link":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2019-40\/8-2\/","title":{"rendered":"Isotop-Geochemistry properties of carbonate formations of Crimea"},"content":{"rendered":"

V.M. Zagnitko<\/strong><\/em>
\nInstitute of Geology Taras Shevchenko National University of Kyiv
\nORCID 0000-0003-0165-0534
\nE.V. Naumenko<\/strong><\/em>
\nNational Science Museum of the NAS of Ukraine
\nV.S. Moroz<\/em><\/strong>
\nM.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine
\nL.I. Proskurka<\/strong><\/em>
\nM.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine<\/p>\n

Language: Ukrainian
\nGeochemistry and ore formation 2019, 40: 64-69
\n https:\/\/doi.org\/10.15407\/gof.2019.40.064<\/a><\/p>\n

Considered the features of the isotope, physical properties and Genesis carbonate formations of Crimea: sedimentary, hydrothermal recycled and metamorf\u043czations limestone, siderit and calcite concretions and sekrec\u043cons, displays of crystalline calcite, carbonate veins and displays of Onyx. Some of them have unique isotope properties, such as d13\u0421, which range between +18.6 and \u201337.71 \u2030. There are striking differences in the isotopic composition of individual parts of sectionsin the same crystals, and several genetic types of carbonates are distinguished by their isotopic and mineralogical features: 1 \u2014 Ordinary limestone, 2 \u2014 carbonate formations with Mobilizedandre-deferred local sources, 3 \u2014 low temperature, 4 \u2014 medium- temperature cores, 5 \u2014 shell separium and secretions, 6-relatively potent carbonates lived with anabnormally high severe carbon isotope 13\u0421.<\/p>\n

References
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\n2. For G. (1989). Osnovy isotopnoi geologii. Moskow, Mir, 590 p.
\n3. Zagnitko V.M., Lugovaja I.P. (1989). Isotopnaya geochemija karbonatnyh i zhelezisto-kremnistyh porod Ukrainskoho Schita. Kyiv, Naukova dumka, 316 p.
\n4. Zagnitko V.M., Emets O.V. (2004). Geokhimichni i mineralogenichni osoblyvosti karbonatnyh porid Ukrainskoho Schita. Mineral. Journ. (Ukraine). 26, No. 3. pp. 112-119.
\n5. Zagnitko V.M., Mikhailov V.A. (2014). Geokhymchni osoblyvosti hasovoi skladovoi hasonosnyh slanzevych tovsch Ukrainy. Visnyk Universytetu imeni Tarasa Shevchenka. Geologija. 214, No. 1 (64), pp. 11-17.
\n6. Mamchur G.P. (1978). K geochimiji uhleroda v endogennych obrasovanijach. In: Uhlerod i eho soedinenija v processah mineraloobrasovania. Kyiv, Naukova dumka, pp. 25-30.
\n7. Galimov E.M., Migdisov A.A., Ronov A.B. (1975). Variatziji isotopiv karbonatnnoho i organichnoho uhleroda osadocshnych porod v istorii Zemli. Geochimija. No. 3, pp. 323-343.
\n8. Tyschenko A.I. (2015). Myneraly Kryma. Simferopol, Bisnes-inform, 204 p.
\n9. Zagnitko V., Kvasnytsya I., Moroz V., Proskurka L. (2018). Krystalomorphologija, geochimija i genesis karbonatnych obrasovaniy gornoho Kryma. Mineralogischny zbirnyk, No. 68, Iss. 1, pp. 118-121.
\n10. Dovgy S.\u041e., Pavlyshyn V.I., Kvasnytsya I.V. 100 Mineraliv Ukrainy. Kyiv, 286 p.<\/p>\n

\"\"<\/a><\/strong><\/p>\n","protected":false},"excerpt":{"rendered":"

V.M. Zagnitko Institute of Geology Taras Shevchenko National University of Kyiv ORCID 0000-0003-0165-0534 E.V. Naumenko National Science Museum of the NAS of Ukraine V.S. Moroz M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine L.I. Proskurka M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine … Continue reading “Isotop-Geochemistry properties of carbonate formations of Crimea”<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":1498,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-1556","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-p6","jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":1510,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2019-40\/1-2\/","url_meta":{"origin":1556,"position":0},"title":"The Institute of Geochemistry, Mineralogy and Ore Formation Semenenko NAS of Ukraine is 50 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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":8,"url":"http:\/\/www.g-o-f.org.ua\/gb\/%d1%80%d0%b5%d0%b4%d0%ba%d0%be%d0%bb%d0%b5%d0%b3%d0%b8%d1%8f\/","url_meta":{"origin":1556,"position":1},"title":"Editorial Board","author":"admin","date":"05\/10\/2017","format":false,"excerpt":"{:uk}\u0421\u041a\u041b\u0410\u0414 \u0420\u0415\u0414\u0410\u041a\u0426\u0406\u0419\u041d\u041e\u0407 \u041a\u041e\u041b\u0415\u0413\u0406\u0407 \u0437\u0431\u0456\u0440\u043d\u0438\u043a\u0430 \u043d\u0430\u0443\u043a\u043e\u0432\u0438\u0445 \u043f\u0440\u0430\u0446\u044c \"\u0413\u0415\u041e\u0425\u0406\u041c\u0406\u042f \u0422\u0410 \u0420\u0423\u0414\u041e\u0423\u0422\u0412\u041e\u0420\u0415\u041d\u041d\u042f (Geochemistry and Ore Formation)\" \u00a0\u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a \u041b\u0435\u043e\u043d\u0456\u0434 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post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":176,"url":"http:\/\/www.g-o-f.org.ua\/gb\/","url_meta":{"origin":1556,"position":5},"title":"Geochemistry and ore formation","author":"admin","date":"09\/10\/2017","format":false,"excerpt":"{:uk}{:uk}\u0413\u0435\u043e\u0445\u0456\u043c\u0456\u044f \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f: \u0437\u0431. \u043d\u0430\u0443\u043a. \u043f\u0440. \/ \u041d\u0430\u0446. \u0430\u043a\u0430\u0434. \u043d\u0430\u0443\u043a \u0423\u043a\u0440\u0430\u0457\u043d\u0438, \u0406\u043d-\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. \u2013 \u041a\u0438\u0457\u0432: [\u0431. 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