{"id":1363,"date":"2019-10-08T12:22:55","date_gmt":"2019-10-08T09:22:55","guid":{"rendered":"http:\/\/www.g-o-f.org.ua\/?page_id=1363"},"modified":"2020-01-20T20:02:28","modified_gmt":"2020-01-20T18:02:28","slug":"the-metasomatites-formed-by-fluids-of-calc-alkaline-magmas","status":"publish","type":"page","link":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2012-2\/the-metasomatites-formed-by-fluids-of-calc-alkaline-magmas\/","title":{"rendered":"The Metasomatites Formed by Fluids of Calc-Alkaline Magmas"},"content":{"rendered":"

Kigay I.N.<\/strong>
\nInstitute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry RAS (IGEM RAS)<\/p>\n

Language: Russian
\nGeochemistry and ore formation 2012, 31-32: 56-66
\n https:\/\/doi.org\/10.15407\/gof.2012.31.056<\/a><\/p>\n

Download (PDF)<\/a><\/p>\n

Acidity evolution of magmatic fluids is determined by dependence of dissociation constants of hydrolysis products of alkali metal chlorides on temperature and pressure. High-temperature supercritical fluids, derived from granitic melts are initially alkaline. Being cooled they can become acidic. But fluid\u2019s acidity sufficient for creation of acidic metasomatites is not a consequence of simple cooling of initially alkaline fluids or of an overtaking wave of acidic components suggested by D.S. Korzhinskii, \u2013 it is a result of acid gases\u2019 condensation at the upper parts of closed heterophase subcritical fluid systems. This conclusion is based on silica loss from all silicate host rocks during acidic leaching (greisening, tourmalinization etc.), as well as on close relation of acidic metasomatites with filling veins and fluids\u2019 heterogenization. All types of alkaline and acidic metasomatites formation are characterized by formation of monomineral rear zones containing no quartz; these are the K-feldspar, albite or chlorite zones in alkaline metasomatites and the topaz, muscovite, tourmaline and sericite zones in acidic ones. During a multistage mineralization, any stage of mineralization is started from formation of near-fracture metasomatic column and is terminated with precipitation of ore minerals and redeposition of previously leached silica to form quartz in veins and in altered host rocks up to formation of monomineral rear quartz zones. The latter are always secondary relative to other monomineral zones. General evolution of fluid\u2019s acidity starts from subneutral fluids through high-temperature alkaline ones to acidic fluids and finally to vertically separated low-temperature acidic and alkaline fluids. This succession is rather similar to that of D.S. Korzhinskii\u2019s “overtaking acidity wave”, but is instead a multiple multistage repetition of both alkaline metasomatism and acidic leaching with the conjugated ore assemblages. A group of mineral deposits, whose ore mineralization is related to preore acidic metasomatism and forms with the participation of heterophase fluids, comprises practically all postcollisional W, Sn, Be, Li veintype deposits genetically related to reduced calc-alkaline granitoids, and Au, Ag, Cu, Pb, Zn, As, Sb, and Hg deposits genetically related to oxidized basic magmatites of mantle origin.<\/p>\n

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Kigay I.N. Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry RAS (IGEM RAS) Language: Russian Geochemistry and ore formation 2012, 31-32: 56-66 https:\/\/doi.org\/10.15407\/gof.2012.31.056 Download (PDF) Acidity evolution of magmatic fluids is determined by dependence of dissociation constants of hydrolysis products of alkali metal chlorides on temperature and pressure. High-temperature supercritical fluids, derived from … Continue reading “The Metasomatites Formed by Fluids of Calc-Alkaline Magmas”<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":256,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-1363","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-lZ","jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":2303,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2024-45\/gof-2024-45-021\/","url_meta":{"origin":1363,"position":0},"title":"MELANOCRATIC ROCK OF THE SYENITE-TVAITOSITE SERIES OF THE CHERNIHIVKA CARBONATITE MASSIF (AZOV 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\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\u0430E-mail: kryvdik@ukr.net 2 \u2014 \u041d\u041d\u0406 \u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u0433\u0435\u043e\u043b\u043e\u0433\u0456\u0457 \u041a\u041d\u0423 \u0456\u043c\u0435\u043d\u0456 \u0422\u0430\u0440\u0430\u0441\u0430 \u0428\u0435\u0432\u0447\u0435\u043d\u043a\u043003022, \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 \u041a\u043e\u043d\u0446\u0435\u043d\u0442\u0440\u0430\u0446\u0456\u044f \u0444\u043e\u0441\u0444\u043e\u0440\u0443 \u0432 \u0440\u0456\u0437\u043d\u0438\u0445 \u0442\u0438\u043f\u0430\u0445 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formation","author":"admin","date":"23\/07\/2018","format":false,"excerpt":"{:uk}\u0421.\u0413. \u041a\u0440\u0438\u0432\u0434\u0456\u043a, \u0412.\u0413. \u041c\u043e\u0440\u0433\u0443\u043d, \u041e.\u0412. \u0414\u0443\u0431\u0438\u043d\u0430 \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 03680, \u043f\u0440\u043e\u0441\u043f. \u041f\u0430\u043b\u043b\u0430\u0434\u0456\u043d\u0430, 34, \u041a\u0438\u0457\u0432, \u0423\u043a\u0440\u0430\u0457\u043d\u0430 \u041c\u043e\u0432\u0430: \u0443\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0430 \u0413\u0435\u043e\u0445\u0456\u043c\u0456\u044f \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f 2012, 31-32: 4-11 https:\/\/doi.org\/10.15407\/gof.2012.31.004 Download (PDF) \u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0438\u0439 \u0449\u0438\u0442 \u0454 \u043e\u0434\u043d\u0438\u043c \u0456\u0437 \u043d\u0430\u0439\u0431\u0430\u0433\u0430\u0442\u0448\u0438\u0445 \u043d\u0430 \u043b\u0443\u0436\u043d\u0456 \u043c\u0435\u0442\u0430\u0441\u043e\u043c\u0430\u0442\u0438\u0442\u0438 \u0440\u0435\u0433\u0456\u043e\u043d\u0456\u0432. \u0412\u0438\u0434\u0456\u043b\u044f\u044e\u0442\u044c\u0441\u044f \u0442\u0430\u043a\u0456 \u0442\u0438\u043f\u0438 \u043b\u0443\u0436\u043d\u0438\u0445 \u043c\u0435\u0442\u0430\u0441\u043e\u043c\u0430\u0442\u0438\u0442\u0456\u0432: 1) \u0444\u0435\u043d\u0456\u0442\u0438,\u2026","rel":"","context":"In \"\u041b\u0443\u0436\u043d\u0456 \u043c\u0435\u0442\u0430\u0441\u043e\u043c\u0430\u0442\u0438\u0442\u0438\"","block_context":{"text":"\u041b\u0443\u0436\u043d\u0456 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\u0412\u0441\u0442\u0430\u043d\u043e\u0432\u043b\u0435\u043d\u043e, \u0449\u043e \u043c\u0456\u043d\u0435\u0440\u0430\u043b\u044c\u043d\u0456 \u0430\u0441\u043e\u0446\u0456\u0430\u0446\u0456\u0457 \u0430\u043f\u043e\u0433\u0440\u0430\u043d\u0456\u0442\u0443 \u0439 \u0430\u043f\u043e\u0434\u0456\u0430\u0431\u0430\u0437\u0443 \u0432\u0456\u0434\u043f\u043e\u0432\u0456\u0434\u0430\u044e\u0442\u044c \u0430\u043a\u0442\u0438\u043d\u043e\u043b\u0456\u0442\u043e\u0432\u0456\u0439 \u0444\u0430\u0446\u0456\u0457 \u0432\u0435\u0440\u0442\u0438\u043a\u0430\u043b\u044c\u043d\u043e\u0457 \u0437\u043e\u043d\u0430\u043b\u044c\u043d\u043e\u0441\u0442\u0456 \u043b\u0443\u0436\u043d\u0438\u0445 \u043d\u0430\u0442\u0440\u0456\u0454\u0432\u0438\u0445 \u043c\u0435\u0442\u0430\u0441\u043e\u043c\u0430\u0442\u0438\u0442\u0456\u0432.{:}{:ru}\u041c\u0438\u0445\u0430\u043b\u044c\u0447\u0435\u043d\u043a\u043e \u0418.\u0418., \u0421\u0438\u043d\u0438\u0446\u044b\u043d \u0412.\u0410. https:\/\/doi.org\/10.15407\/gof.2012.31.077\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":1967,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2022-43\/","url_meta":{"origin":1363,"position":5},"title":"2022. Vol 43","author":"admin","date":"20\/12\/2022","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 \u0410\u0440\u0442\u0435\u043c\u0435\u043d\u043a\u043e \u0413.\u0412., \u0428\u0443\u043c\u043b\u044f\u043d\u0441\u044c\u043a\u0438\u0439 \u041b.\u0412., \u0411\u0435\u043a\u043a\u0435\u0440 \u0410.\u042e., \u0425\u043e\u0444\u0444\u043c\u0430\u043d \u0410. \u0412\u0456\u043a \u0446\u0438\u0440\u043a\u043e\u043d\u0443 \u0437 \u043c\u0435\u0442\u0430\u0440\u0456\u043e\u0434\u0430\u0446\u0438\u0442\u0456\u0432 \u043e\u043b\u0435\u043a\u0441\u0430\u043d\u0434\u0440\u0456\u0432\u0441\u044c\u043a\u043e\u0457 \u0441\u0432\u0456\u0442\u0438 \u043c\u0438\u0445\u0430\u0439\u043b\u0456\u0432\u0441\u044c\u043a\u043e\u0457 \u0441\u0435\u0440\u0456\u0457 (\u043c\u0435\u0433\u0430\u0431\u043b\u043e\u043a \u041a\u041c\u0410) \u00a0 \u0421\u0442\u0435\u043f\u0430\u043d\u044e\u043a \u041b.\u041c., \u0412\u0438\u0441\u043e\u0446\u044c\u043a\u0438\u0439 \u041e.\u0411., \u041a\u043e\u0432\u0442\u0443\u043d \u041e.\u0412., \u041a\u0443\u0440\u0438\u043b\u043e \u0421.\u0406., \u0414\u043e\u0432\u0431\u0443\u0448 \u0422.\u0406. \u0423\u0440\u0430\u043d-\u0441\u0432\u0438\u043d\u0446\u0435\u0432\u0438\u0439 \u0456\u0437\u043e\u0442\u043e\u043f\u043d\u0438\u0439 \u0432\u0456\u043a \u043c\u043e\u043d\u0430\u0446\u0438\u0442\u0456\u0432 \u043f\u043b\u0430\u0433\u0456\u043e\u0433\u043d\u0435\u0439\u0441\u0456\u0432 \u0456\u043d\u0433\u0443\u043b\u043e-\u0456\u043d\u0433\u0443\u043b\u0435\u0446\u044c\u043a\u043e\u0457 \u0441\u0435\u0440\u0456\u0457 (\u0406\u043d\u0433\u0443\u043b\u044c\u0441\u044c\u043a\u0438\u0439 \u043c\u0435\u0433\u0430\u0431\u043b\u043e\u043a \u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u043e\u0433\u043e \u0449\u0438\u0442\u0430) \u00a0\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]}],"_links":{"self":[{"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/pages\/1363","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/comments?post=1363"}],"version-history":[{"count":5,"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/pages\/1363\/revisions"}],"predecessor-version":[{"id":1365,"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/pages\/1363\/revisions\/1365"}],"up":[{"embeddable":true,"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/pages\/256"}],"wp:attachment":[{"href":"http:\/\/www.g-o-f.org.ua\/gb\/wp-json\/wp\/v2\/media?parent=1363"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}