. . "K2O"@en . . . . . . . . . "Magmo (greke: \u201Eknedita maso\u201C) signifas la maso el fandita \u015Dtona\u0135o, trovi\u011Danta en partoj de la supra termantelo kaj de la profunda terkrusto. La flukapablo de la magmo estas la ka\u016Dzo de la vulkanismo (vidu anka\u016D: vulkano) kaj havas grandan signifon por la formi\u011Do de rokoj. \u015Ctona\u0135oj formi\u011Dintaj el solidi\u011Dinta magmo nomi\u011Das a\u016D profund\u015Dtona\u0135oj."@eo . . . "\u062A\u062A\u062C\u0645\u0639 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0641\u064A\u0645\u0627 \u064A\u0639\u0631\u0641 \u0628\u0623\u0633\u0645 (\u063A\u0631\u0641 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 Magma Chembers) \u0627\u0644\u062A\u064A \u0642\u062F \u062A\u063A\u0630\u064A \u0628\u0631\u0643\u0627\u0646 \u0648\u062A\u062E\u0631\u062C \u0641\u0648\u0642 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u0648\u062A\u0633\u0645\u0649 \u0641\u064A \u062A\u0644\u0643 \u0627\u0644\u062D\u0627\u0644\u0629 (\u0644\u0627\u0641\u0627 Lava) \u0623\u0648 \u062A\u062A\u062C\u0645\u0639 \u062A\u062D\u062A \u0627\u0644\u0642\u0634\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0641\u064A \u0647\u0630\u0647 \u0627\u0644\u062D\u0627\u0644\u0629 \u062A\u0633\u0645\u0649 (\u0628\u0644\u0648\u062A\u0648\u0646 pluton). \u062A\u0639\u062A\u0628\u0631 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0642\u0627\u062F\u0631\u0629 \u0639\u0644\u0649 \u0623\u0642\u062A\u062D\u0627\u0645 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0645\u062C\u0627\u0648\u0631\u0629 \u0648\u062A\u0643\u0648\u0646 (\u0627\u0644\u0633\u062F\u0648\u062F \u0627\u0644\u0646\u0627\u0631\u064A\u0629 Igneous dikes) \u0648\u0627\u064A\u0636\u0627 \u062A\u0643\u0648\u0646 ( \u0627\u0644\u062C\u064A\u0648\u0628 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 sills) \u062B\u0645 \u062A\u0642\u0630\u0641 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u0644\u062A\u0643\u0648\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629. \u0627\u0644\u0645\u0648\u0627\u062F \u0627\u0644\u062A\u064A \u062A\u062A\u0643\u0648\u0646 \u0645\u0646\u0647\u0627 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0647\u064A \u0627\u0644\u0645\u0648\u0627\u062F \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0627\u0646\u064A\u0629 \u0648\u0647\u064A \u0645\u0648\u0627\u062F \u062A\u062D\u062A\u0648\u064A \u0639\u0644\u0649 \u0639\u0646\u0635\u0631 \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0648\u0646 \u0648\u0627\u0644\u0623\u0643\u0633\u062C\u064A\u0646."@ar . . . . . "\u30DE\u30B0\u30DE\uFF08\u82F1: magma\uFF09\u3068\u306F\u3001\u5730\u7403\u3092\u306F\u3058\u3081\u3068\u3059\u308B\u5929\u4F53\u3092\u69CB\u6210\u3059\u308B\u56FA\u4F53\u304C\u3001\u305D\u306E\u5185\u90E8\u3067\u6EB6\u878D\u3057\u3066\u3044\u308B\u3082\u306E\u3067\u3042\u308B\u3002\u5730\u7403\u306E\u30DE\u30F3\u30C8\u30EB\u3084\u5730\u6BBB\u306F\u4E3B\u306B\u30B1\u30A4\u9178\u5869\u9271\u7269\u3067\u3067\u304D\u3066\u3044\u308B\u305F\u3081\u3001\u305D\u306E\u6EB6\u878D\u7269\u3067\u3042\u308B\u30DE\u30B0\u30DE\u3082\u4E00\u822C\u306B\u30B1\u30A4\u9178\u5869\u4E3B\u4F53\u306E\u7D44\u6210\u3092\u6301\u3064\u304C\u3001\u7A00\u306B\u300C\u70AD\u9178\u5869\u300D\u9271\u7269\u3092\u4E3B\u4F53\u3068\u3059\u308B\u30DE\u30B0\u30DE\u3082\u5B58\u5728\u3059\u308B\u3002\u300C\u5CA9\u6F3F\uFF08\u304C\u3093\u3057\u3087\u3046\uFF09\u300D\u3068\u3082\u3044\u3046\u3002\u5730\u7403\u4EE5\u5916\u306E\u5929\u4F53\u3067\u30DE\u30B0\u30DE\u306E\u5B58\u5728\u306F\u63A8\u5B9A\u306E\u307F\u3067\u78BA\u8A8D\u3055\u308C\u3066\u3044\u306A\u3044\u305F\u3081\u3001\u672C\u9805\u3067\u306F\u5730\u7403\u306B\u304A\u3051\u308B\u30DE\u30B0\u30DE\u306B\u3064\u3044\u3066\u8A18\u8F09\u3059\u308B\u3002"@ja . . . . . "Magma"@de . "\u041C\u0430\u0301\u0433\u043C\u0430 (\u0434\u0440.-\u0433\u0440\u0435\u0447. \u03BC\u03AC\u03B3\u03BC\u03B1 \u2014 \u00AB\u043C\u0435\u0441\u0438\u0432\u043E, \u0433\u0443\u0441\u0442\u0430\u044F \u043C\u0430\u0437\u044C\u00BB) \u2014 \u0440\u0430\u0441\u043F\u043B\u0430\u0432\u043B\u0435\u043D\u043D\u0430\u044F \u043C\u0430\u0441\u0441\u0430 \u043F\u043E\u0434 \u0442\u0432\u0435\u0440\u0434\u043E\u0439 \u0437\u0435\u043C\u043D\u043E\u0439 \u043A\u043E\u0440\u043E\u0439. \u041F\u0440\u0438\u0440\u043E\u0434\u043D\u044B\u0439, \u0447\u0430\u0449\u0435 \u0432\u0441\u0435\u0433\u043E \u0441\u0438\u043B\u0438\u043A\u0430\u0442\u043D\u044B\u0439, \u0440\u0430\u0441\u043A\u0430\u043B\u0451\u043D\u043D\u044B\u0439, \u0436\u0438\u0434\u043A\u0438\u0439 \u0440\u0430\u0441\u043F\u043B\u0430\u0432, \u0432\u043E\u0437\u043D\u0438\u043A\u0430\u044E\u0449\u0438\u0439 \u0432 \u0437\u0435\u043C\u043D\u043E\u0439 \u043A\u043E\u0440\u0435 \u0438\u043B\u0438 \u0432 \u0432\u0435\u0440\u0445\u043D\u0435\u0439 \u043C\u0430\u043D\u0442\u0438\u0438, \u043D\u0430 \u0431\u043E\u043B\u044C\u0448\u0438\u0445 \u0433\u043B\u0443\u0431\u0438\u043D\u0430\u0445, \u0438 \u043F\u0440\u0438 \u043E\u0441\u0442\u044B\u0432\u0430\u043D\u0438\u0438 \u0444\u043E\u0440\u043C\u0438\u0440\u0443\u044E\u0449\u0438\u0439 \u043C\u0430\u0433\u043C\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u0438\u0435 \u0433\u043E\u0440\u043D\u044B\u0435 \u043F\u043E\u0440\u043E\u0434\u044B. \u0418\u0437\u043B\u0438\u0432\u0448\u0430\u044F\u0441\u044F \u043C\u0430\u0433\u043C\u0430, \u043F\u043E\u0442\u0435\u0440\u044F\u0432\u0448\u0430\u044F \u0431\u043E\u043B\u044C\u0448\u0443\u044E \u0447\u0430\u0441\u0442\u044C \u043B\u0435\u0442\u0443\u0447\u0438\u0445 \u043A\u043E\u043C\u043F\u043E\u043D\u0435\u043D\u0442\u043E\u0432 (\u0442\u0430\u043A\u0438\u0445 \u043A\u0430\u043A \u0432\u043E\u0434\u0430, \u0443\u0433\u043B\u0435\u043A\u0438\u0441\u043B\u044B\u0439 \u0433\u0430\u0437, \u0444\u0442\u043E\u0440, \u0445\u043B\u043E\u0440 \u0438 \u0434\u0440.) \u2014 \u043D\u0430\u0437\u044B\u0432\u0430\u0435\u0442\u0441\u044F \u043B\u0430\u0432\u0430."@ru . . . . . "2.6"^^ . "MgO"@en . . . . . . . "SiO2"@en . . . . . "\u041C\u0430\u0433\u043C\u0430"@ru . . . . . . . . "\u5CA9\u6F3F"@zh . . "73.2"^^ . . . . . . . . . . . . . . . . "\u041C\u0430\u0301\u0433\u043C\u0430 (\u0432\u0456\u0434 \u0433\u0440\u0435\u0446. \u03BC\u03AC\u03B3\u03BC\u03B1 \u2014 \u0442\u0456\u0441\u0442\u043E) \u2014 \u043F\u0440\u0438\u0440\u043E\u0434\u043D\u0438\u0439, \u043F\u0435\u0440\u0435\u0432\u0430\u0436\u043D\u043E \u0441\u0438\u043B\u0456\u043A\u0430\u0442\u043D\u0438\u0439 \u0432\u0438\u0441\u043E\u043A\u043E\u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u043D\u0438\u0439 \u0440\u043E\u0437\u043F\u043B\u0430\u0432, \u044F\u043A\u0438\u0439 \u0443\u0442\u0432\u043E\u0440\u044E\u0454\u0442\u044C\u0441\u044F \u0432 \u043D\u0430\u0434\u0440\u0430\u0445 \u0417\u0435\u043C\u043B\u0456."@uk . . "Rhyolite magma"@en . . . . . . "0.2"^^ . . . "Magma (g\u00E9ologie)"@fr . "53.8"^^ . "P2O5"@en . . . "Magma (do grego \u03BC\u03AC\u03B3\u03BC\u03B1; \"pasta\") \u00E9 a designa\u00E7\u00E3o dada nas geoci\u00EAncias \u00E0s massas de rocha em fus\u00E3o total ou parcial que existem debaixo da superf\u00EDcie da Terra e provavelmente de outros planetas tel\u00FAricos. Os magmas s\u00E3o constitu\u00EDdos por uma mistura de rocha em estado vari\u00E1vel de fus\u00E3o com materiais vol\u00E1teis, composta maioritariamente por silicatos a alta press\u00E3o e temperatura acompanhados por um conjunto vari\u00E1vel, em propor\u00E7\u00E3o e tipo, de i\u00F5es met\u00E1licos e compostos vol\u00E1teis ricos em enxofre, podendo ainda conter cristais em suspens\u00E3o, gases dissolvidos e por vezes bolhas de g\u00E1s. Os magmas acumulam-se em geral dentro de c\u00E2maras magm\u00E1ticas situadas entre os 15 e os 150 km de profundidade, com temperaturas que variam entre 650 e 1 200 \u00BAC, mas podendo atingir 1 560 \u00B0C. Quando expelido por um vulc\u00E3o, o magma d\u00E1 origem \u00E0 lava e \u00E0s rochas extrusivas, que quando ejectadas em erup\u00E7\u00F5es explosivas produzem tefras e outros piroclastos. Quando o magma solidifica em profundidade d\u00E1 origem a intrus\u00F5es nas rochas adjacentes, podendo formar diques e soleiras."@pt . . "Tholeiitic basalt magma"@en . . . . "Magma je term\u00EDn ozna\u010Duj\u00EDc\u00ED sm\u011Bs roztaven\u00FDch hornin a plyn\u016F, kter\u00E1 se nach\u00E1z\u00ED pod povrchem Zem\u011B a dal\u0161\u00EDch terestrick\u00FDch t\u011Bles. Vyjma roztaven\u00FDch hornin m\u016F\u017Ee magma obsahovat i krystaly r\u016Fzn\u00FDch miner\u00E1l\u016F, rozpu\u0161t\u011Bn\u00E9 plyny \u010Di bublinky. Magma je hlubinn\u00FD ekvivalent l\u00E1vy; jakmile se magma dostane na povrch t\u011Blesa, pou\u017E\u00EDv\u00E1 se pro jeho ozna\u010Den\u00ED term\u00EDn l\u00E1va. Magma, kter\u00E9 vznik\u00E1 v zemsk\u00E9m pl\u00E1\u0161ti, se naz\u00FDv\u00E1 prim\u00E1rn\u00ED; sekund\u00E1rn\u00ED (\u017Eulov\u00E9) vznik\u00E1 horotvornou \u010Dinnost\u00ED. Prim\u00E1rn\u00ED magma je pon\u011Bkud \u0159id\u0161\u00ED a snadno pronik\u00E1 k zemsk\u00E9mu povrchu, kde tuhne. Vznikaj\u00ED z n\u011Bj v\u00FDlevn\u00E9 horniny, nap\u0159. \u010Dedi\u010D. Sekund\u00E1rn\u00ED se v\u011Bt\u0161inou tvo\u0159\u00ED ve velk\u00FDch hloubk\u00E1ch a tuhne pomalu pod povrchem Zem\u011B. Vytv\u00E1\u0159\u00ED velk\u00E1 t\u011Blesa (plutony), kter\u00E1 prostupuj\u00ED star\u0161\u00EDmi horninami. Podle m\u00EDsta utuhnut\u00ED magmatu se rozd\u011Bluj\u00ED vyv\u0159el\u00E9 horniny na hlubinn\u00E9, v\u00FDlevn\u00E9 a \u017Eiln\u00E9. Na Zemi je magma nej\u010Dast\u011Bji k\u0159emi\u010Dit\u00E1 hornina s obsahem rozpu\u0161t\u011Bn\u00FDch fluidn\u00EDch slo\u017Eek, konkr\u00E9tn\u011B aluminio-silik\u00E1tov\u00E1 tavenina obsahuj\u00EDc\u00ED sope\u010Dn\u00E9 plyny (nap\u0159\u00EDklad voda, CO2, chl\u00F3r a fluor) z pl\u00E1\u0161t\u011B Zem\u011B. Magma vznik\u00E1 v oblastech zemsk\u00E9ho pl\u00E1\u0161t\u011B, nebo taven\u00EDm z hornin spodn\u00ED zemsk\u00E9 k\u016Fry. Magma m\u016F\u017Ee dosahovat r\u016Fzn\u00FDch teplot (na Zemi v\u011Bt\u0161inou mezi 650\u20131200 \u00B0C). Vlivem rozd\u00EDlu hustoty magmatu v\u016F\u010Di okoln\u00EDmu prost\u0159ed\u00ED stoup\u00E1 magma k povrchu, jeliko\u017E m\u00E1 men\u0161\u00ED hustotu. Cestou proch\u00E1z\u00ED skrze k\u016Fru t\u011Blesa, kde \u010Dasto utv\u00E1\u0159\u00ED magmatick\u00E9 krby \u2014 m\u00EDsta hromad\u011Bn\u00ED, ze kter\u00FDch pak vystupuje na povrch skrze \u017E\u00EDly. P\u0159i pr\u016Fniku na povrch doch\u00E1z\u00ED k sope\u010Dn\u00E9 \u010Dinnosti maj\u00EDc\u00ED \u010Dasto za n\u00E1sledek vznik sopek. B\u011Bhem v\u00FDstupu doch\u00E1z\u00ED takt\u00E9\u017E k postupn\u00E9mu chladnut\u00ED magmatu, postupn\u00E9 krystalizaci miner\u00E1l\u016F a k poklesu okoln\u00EDho litostatick\u00E9ho tlaku, co\u017E zp\u016Fsobuje postupn\u00E9 uvol\u0148ov\u00E1n\u00ED rozpu\u0161t\u011Bn\u00FDch plyn\u016F v magmatu a vzniku bublinek. Pokud je mno\u017Estv\u00ED rozpu\u0161t\u011Bn\u00FDch plyn\u016F dostate\u010Dn\u00E9 \u010Di magma na sv\u00E9 cest\u011B potk\u00E1 zdroj podzemn\u00ED vody, m\u016F\u017Ee doj\u00EDt k jeho fragmentaci a vzniku . Je-li ale mno\u017Estv\u00ED plyn\u016F mal\u00E9 \u010Di plyn m\u00E1 mo\u017Enost snadno z magmatu unikat, magma se po povrchu za\u010Dne vyl\u00E9vat a tvo\u0159it l\u00E1vov\u00E9 proudy."@cs . . . . . . . . . . . . . "MnO"@en . . "1.3"^^ . "7.9"^^ . "Magma is het vloeibare gesteente dat zich onder het aardoppervlak of het oppervlak van een andere aardse planeet bevindt. De meeste magma's in de Aarde zijn complexe silica-oplossingen met (normaal gesproken) temperaturen tussen de 650 \u00B0C en 1200 \u00B0C. Wanneer magma stolt ontstaat stollingsgesteente. Wanneer magma tot aan het oppervlak omhoog komt wordt het gesmolten gesteente geen magma maar lava genoemd."@nl . . . "Magma (stgr. \u03BC\u03AC\u03B3\u03BC\u03B1 \u2019g\u0119sta ma\u015B\u0107\u2019) \u2013 gor\u0105ca, stopiona masa krzemian\u00F3w i glinokrzemian\u00F3w z domieszkami tlenk\u00F3w i siarczk\u00F3w, z du\u017C\u0105 ilo\u015Bci\u0105 wody i gaz\u00F3w, powstaj\u0105ca w g\u0142\u0119bi Ziemi; magma, kt\u00F3ra wydobywa si\u0119 na powierzchni\u0119 Ziemi, nazywana jest law\u0105."@pl . . . "Magma (fr\u00E5n grekiska f\u00F6r \"salva\" eller \"kn\u00E5dad massa\") best\u00E5r oftast av sm\u00E4lt bergartsmassa blandat med gaser och kristaller. Bergarter kan aldrig sm\u00E4lta totalt s\u00E5 magma kan d\u00E4rf\u00F6r aldrig best\u00E5 av endast sm\u00E4lt material. Magma kan bildas genom att bergarter i den l\u00E4gre delen av jordskorpan eller den \u00F6vre delen av manteln, astenosf\u00E4ren, sm\u00E4lter d\u00E5 de uts\u00E4tts f\u00F6r h\u00F6gt tryck och h\u00F6g temperatur. D\u00E5 magma tr\u00E4nger upp ur jordskorpan genom ett vulkanutbrott eller n\u00E4r en vulkan bildas kallas den lava och sedan den stelnat bildar magman en eruptiv magmatisk bergart. Magmatiska bergarter kan \u00E4ven bildas genom att magman stelnar under jord till en intrusiv magmatisk bergart."@sv . "( \uB2E4\uB978 \uB73B\uC5D0 \uB300\uD574\uC11C\uB294 \uB9C8\uADF8\uB9C8 (\uB3D9\uC74C\uC774\uC758) \uBB38\uC11C\uB97C \uCC38\uACE0\uD558\uC2ED\uC2DC\uC624.) \uC554\uC7A5(\u5DD6\u6F3F), \u540C\u610F\uB9C8\uADF8\uB9C8(\uC601\uC5B4: magma \u2190 \uADF8\uB9AC\uC2A4\uC5B4 \u03BC\u03AC\u03B3\u03BC\u03B1 m\u00E1gma '\uB450\uAEBC\uC6B4 \uC5F0\uACE0'\uC5D0\uC11C \uC720\uB798 , \uBB38\uD654\uC5B4: \uB3CC\uBB3C)\uB294 \uC554\uC11D\uC774 \uB179\uC740 \uAC83\uC774\uB2E4. \uAC00\uC7A5 \uAC04\uB2E8\uD55C \uACBD\uC6B0 \uC554\uC11D\uC774 \uB179\uB294 \uC870\uAC74\uC740 \uC77C\uBC18\uC801\uC778 \uC5F4\uC5ED\uD559\uC758 \uBC95\uCE59\uC5D0 \uB530\uB77C \uC628\uB3C4\uC640 \uC555\uB825\uC5D0 \uC758\uD574\uC11C \uACB0\uC815\uB41C\uB2E4. \uD558\uC9C0\uB9CC \uC2E4\uC81C \uC9C0\uAD6C\uC5D0\uC11C \uC77C\uC5B4\uB098\uB294 \uD604\uC0C1\uC740 \uC628\uB3C4, \uC555\uB825\uACFC \uD568\uAED8 \uBB3C\uC758 \uD568\uB7C9\uACFC \uC554\uC11D\uC758 \uC131\uBD84\uC744 \uD568\uAED8 \uACE0\uB824\uD558\uC5EC\uC57C \uD55C\uB2E4. \uC628\uB3C4\uAC00 \uB192\uC544\uC9C0\uBA74 \uC554\uC11D\uC774 \uB179\uAE30 \uC2DC\uC791\uD55C\uB2E4. \uC555\uB825\uC774 \uB192\uC544\uC9C0\uBA74 \uB354 \uB192\uC740 \uC628\uB3C4\uAC00 \uB418\uC5B4\uC57C \uC554\uC11D\uC774 \uB179\uAE30 \uC2DC\uC791\uD55C\uB2E4. \uBB3C\uC774 \uD3EC\uD568\uB41C \uC554\uC11D\uC740 \uD6E8\uC52C \uB0AE\uC740 \uC628\uB3C4\uC5D0\uC11C \uB179\uC744 \uC218 \uC788\uB2E4. \uC77C\uBC18\uC801\uC73C\uB85C \uC18C\uB4D0(Na), \uD3EC\uD0C0\uC298(K)\uC774 \uB9CE\uC774 \uD3EC\uD568\uB41C \uC554\uC11D\uBCF4\uB2E4 \uCCA0(Fe), \uB9C8\uADF8\uB124\uC298(Mg)\uC774 \uB9CE\uC774 \uD3EC\uD568\uB418\uC5B4\uC788\uB294 \uC554\uC11D\uC774 \uB354 \uB192\uC740 \uC628\uB3C4\uC5D0\uC11C \uB179\uB294\uB2E4. \uD574\uB839\uC5D0\uC11C \uBD84\uCD9C\uB418\uB294 \uB9C8\uADF8\uB9C8\uB294 \uB9E8\uD2C0 \uBB3C\uC9C8\uC774 \uB300\uB958\uC5D0 \uC758\uD574 \uC0C1\uC2B9\uD558\uBA74\uC11C \uC555\uB825\uC774 \uB0AE\uC544\uC9C0\uC790 \uB179\uC544\uC11C \uB41C \uB9C8\uADF8\uB9C8\uC774\uB2E4. \uD574\uB839 \uBC14\uB85C \uC544\uB798\uC758 \uB9E8\uD2C0 \uC548\uC5D0\uB294 \uC218\uBD84 \uD568\uB7C9\uC774 \uB9E4\uC6B0 \uB0AE\uAE30 \uB54C\uBB38\uC5D0 \uD574\uB839\uC758 \uB9C8\uADF8\uB9C8\uB294 \uC628\uB3C4\uAC00 \uB9E4\uC6B0 \uB192\uB2E4. \uADF8\uB9AC\uACE0 \uD574\uB839\uC758 \uB9C8\uADF8\uB9C8\uB294 \uB9E4\uC6B0 \uAC15\uD55C \uC5FC\uAE30\uC131\uC774\uB2E4."@ko . . . . . . "Magma"@ga . . "0.4"^^ . . . . . . . . . . . . "Magma"@es . . . . . . . "Magma"@en . "Un magma est une roche enti\u00E8rement ou partiellement fondue. Il comporte n\u00E9cessairement une phase liquide, g\u00E9n\u00E9ralement compos\u00E9e de silicates et contenant des gaz dissous. Il comporte souvent aussi, en suspension dans le liquide, une phase gazeuse (des bulles) et une ou plusieurs phases solides (des cristaux), qui proviennent respectivement de l'exsolution partielle des gaz dissous et de la solidification partielle du liquide par d\u00E9compression et refroidissement."@fr . "CaO"@en . . . "Magma is het vloeibare gesteente dat zich onder het aardoppervlak of het oppervlak van een andere aardse planeet bevindt. De meeste magma's in de Aarde zijn complexe silica-oplossingen met (normaal gesproken) temperaturen tussen de 650 \u00B0C en 1200 \u00B0C. Wanneer magma stolt ontstaat stollingsgesteente. Wanneer magma tot aan het oppervlak omhoog komt wordt het gesmolten gesteente geen magma maar lava genoemd."@nl . "1.7"^^ . . . . . "\u041C\u0430\u0301\u0433\u043C\u0430 (\u0434\u0440.-\u0433\u0440\u0435\u0447. \u03BC\u03AC\u03B3\u03BC\u03B1 \u2014 \u00AB\u043C\u0435\u0441\u0438\u0432\u043E, \u0433\u0443\u0441\u0442\u0430\u044F \u043C\u0430\u0437\u044C\u00BB) \u2014 \u0440\u0430\u0441\u043F\u043B\u0430\u0432\u043B\u0435\u043D\u043D\u0430\u044F \u043C\u0430\u0441\u0441\u0430 \u043F\u043E\u0434 \u0442\u0432\u0435\u0440\u0434\u043E\u0439 \u0437\u0435\u043C\u043D\u043E\u0439 \u043A\u043E\u0440\u043E\u0439. \u041F\u0440\u0438\u0440\u043E\u0434\u043D\u044B\u0439, \u0447\u0430\u0449\u0435 \u0432\u0441\u0435\u0433\u043E \u0441\u0438\u043B\u0438\u043A\u0430\u0442\u043D\u044B\u0439, \u0440\u0430\u0441\u043A\u0430\u043B\u0451\u043D\u043D\u044B\u0439, \u0436\u0438\u0434\u043A\u0438\u0439 \u0440\u0430\u0441\u043F\u043B\u0430\u0432, \u0432\u043E\u0437\u043D\u0438\u043A\u0430\u044E\u0449\u0438\u0439 \u0432 \u0437\u0435\u043C\u043D\u043E\u0439 \u043A\u043E\u0440\u0435 \u0438\u043B\u0438 \u0432 \u0432\u0435\u0440\u0445\u043D\u0435\u0439 \u043C\u0430\u043D\u0442\u0438\u0438, \u043D\u0430 \u0431\u043E\u043B\u044C\u0448\u0438\u0445 \u0433\u043B\u0443\u0431\u0438\u043D\u0430\u0445, \u0438 \u043F\u0440\u0438 \u043E\u0441\u0442\u044B\u0432\u0430\u043D\u0438\u0438 \u0444\u043E\u0440\u043C\u0438\u0440\u0443\u044E\u0449\u0438\u0439 \u043C\u0430\u0433\u043C\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u0438\u0435 \u0433\u043E\u0440\u043D\u044B\u0435 \u043F\u043E\u0440\u043E\u0434\u044B. \u0418\u0437\u043B\u0438\u0432\u0448\u0430\u044F\u0441\u044F \u043C\u0430\u0433\u043C\u0430, \u043F\u043E\u0442\u0435\u0440\u044F\u0432\u0448\u0430\u044F \u0431\u043E\u043B\u044C\u0448\u0443\u044E \u0447\u0430\u0441\u0442\u044C \u043B\u0435\u0442\u0443\u0447\u0438\u0445 \u043A\u043E\u043C\u043F\u043E\u043D\u0435\u043D\u0442\u043E\u0432 (\u0442\u0430\u043A\u0438\u0445 \u043A\u0430\u043A \u0432\u043E\u0434\u0430, \u0443\u0433\u043B\u0435\u043A\u0438\u0441\u043B\u044B\u0439 \u0433\u0430\u0437, \u0444\u0442\u043E\u0440, \u0445\u043B\u043E\u0440 \u0438 \u0434\u0440.) \u2014 \u043D\u0430\u0437\u044B\u0432\u0430\u0435\u0442\u0441\u044F \u043B\u0430\u0432\u0430."@ru . "Magma"@it . "FeO"@en . . . . . "\u5CA9\u6F3F\uFF08Magma\uFF09\u662F\u7194\u5316\u7684\u5CA9\u77F3\uFF0C\u901A\u5E38\u4F4D\u65BC\u5730\u8868\u4E4B\u4E0B\u7684\u5CA9\u6F3F\u623F\u4E2D\u3002\u5CA9\u6F3F\u662F\u4E00\u7A2E\u8907\u96DC\u7684\u9AD8\u6EAB\u7845\u9178\u76D0\u6EB6\u6DB2\uFF0C\u662F\u5404\u7A2E\u706B\u6210\u5CA9\u7684\u524D\u8EAB\uFF0C\u706B\u6210\u5CA9\u662F\u7531\u5CA9\u6F3F\u51B7\u537B\u800C\u6210\u7684\u3002\u5CA9\u6F3F\u53EF\u4EE5\u4FB5\u5165\u9130\u8FD1\u7684\u5730\u6BBC\u5CA9\u77F3\u6216\u662F\u5192\u51FA\u5730\u8868\u3002 \u5CA9\u6F3F\u6EAB\u5EA6\u53EF\u4F4E\u81F3650 \u00B0C\uFF0C\u9AD8\u81F31400 \u00B0C\u3002\u7194\u5CA9\u4E2D\u542B\u67091 ~ 8 %\u7684\u6325\u53D1\u6027\u7269\u8D28\u3002\u5CA9\u6F3F\u8655\u65BC\u9AD8\u58D3\u4E4B\u4E2D\uFF0C\u6709\u6642\u6703\u7D93\u7531\u706B\u5C71\u53E3\uFF08\u6216\u8B6F\u706B\u5C71\u7BA1\u3001\u706B\u5C71\u6D41\u53E3\u3001\u706B\u5C71\u9053\uFF09\u4EE5\u7194\u5CA9\u6D41\u6216\u662F\u4EE5\u706B\u5C71\u788E\u5C51\u7269\u7684\u706B\u5C71\u5674\u51FA\u7269\u7684\u5F62\u5F0F\u5192\u51FA\u3002\u9019\u4E9B\u706B\u5C71\u5674\u767C\u7684\u7522\u7269\u901A\u5E38\u5305\u62EC\u4E86\u5F9E\u6C92\u5230\u904E\u5730\u8868\u7684\u6DB2\u9AD4\u3001\u7D50\u6676\u9AD4\u53CA\u6EB6\u89E3\u6C23\u9AD4\u7B49\u3002\u5CA9\u6F3F\u6703\u5728\u5730\u6BBC\u4E2D\u5404\u81EA\u5206\u96E2\u7684\u5CA9\u6F3F\u5EAB\u5167\u96C6\u7D50\uFF0C\u4E0D\u540C\u5730\u65B9\u7684\u5CA9\u6F3F\u7D44\u6210\u6210\u4EFD\u6703\u7A0D\u6709\u4E0D\u540C\u3002 \u9019\u4E9B\u5730\u65B9\u5305\u62EC\u4E86\u96B1\u6C92\u5E36\u3001\u3001\u4E2D\u6D0B\u810A\u6216\u662F\u5730\u51FD\u71B1\u67F1\u7684\u71B1\u9EDE\u4E4B\u4E0A\u3002\u53EA\u6709\u5728\u5730\u7403\u7684\u8EDF\u6D41\u5708\u5167\u7684\u7279\u5B9A\u689D\u4EF6\u4E4B\u4E0B\u5CA9\u6F3F\u624D\u6703\u5F62\u6210\u3002"@zh . . . . "Magma (grezieraz: \u03BC\u03AC\u03B3\u03BC\u03B1, \"ukendu lodia\"), Lurrarren edo beste planeten barneko arroka urtuen masak hartzen duen izena da. Tenperatura handiko nahasketa faseanitza da, osagai likido, gas eta solidoz osaturik dagoena. Bere sorreratik, gainazalean solidotu baino lehenago goraka doan magmari, laba deritzo. Magma hozten denean arroka igneoak sortzen dira."@eu . . . . . . "El magma \u00E9s un tipus de roca format per la fusi\u00F3 parcial o total d'una font pariental (principalment, la part superior del mantell i la base de l'escor\u00E7a terrestre). El magma t\u00E9 composicions diverses tractant-se d'una mescla multi fase d'alta temperatura (depenent de la seva composici\u00F3 i evoluci\u00F3, des de menys de 700 \u00B0C fins m\u00E9s de 1500 \u00B0C) de s\u00F2lids (cristalls i fragments de roca), l\u00EDquida (en la seva majoria silicats) i gas\u00F3s (ric en H, O, C, S i Cl),. El magma ascendent que, des de la seva generaci\u00F3 fins abans de la seva solidificaci\u00F3, brolla a la superf\u00EDcie, rep el nom de lava."@ca . . "0.6"^^ . . "37508"^^ . . . "TiO2"@en . . . . . "Magma"@sv . . . "Magma (s\u00E4chlich; von altgriechisch \u03BC\u03AC\u03B3\u03BC\u03B1 m\u00E1gma, deutsch \u201Ageknetete Masse\u2018) hei\u00DFen Gesteinsschmelzen, die in Teilen des oberen Erdmantels und der tieferen Erdkruste vorkommen. Die Flie\u00DFf\u00E4higkeit des Magmas ist die Ursache des Vulkanismus (siehe auch Vulkan) und hat eine gro\u00DFe Bedeutung f\u00FCr die Gesteinsbildung, da sich aus dem erstarrenden Magma die magmatischen Gesteine oder Magmatite bilden."@de . . . . . . . . "Carraig le\u00E1ite a chrutha\u00EDtear tr\u00ED mhaintl\u00EDn an Domhain a ph\u00E1irtle\u00E1 le teas \u00F3n gcro\u00EDleac\u00E1n. Faoi ch\u00FAins\u00ED geola\u00EDocha ar leith, d\u00E9anann an charraig le\u00E1ite seo imirce suas tr\u00EDd an screamh go reonn ina ions\u00E1 doigheartha, n\u00F3 go n-\u00E9ir\u00EDonn l\u00E9i an dromchla a shroichint, \u00E1it a gcailleann s\u00ED a comh\u00E1bhair inghalaithe is a mbr\u00FAchtann amach mar laibhe."@ga . . "\u039C\u03AC\u03B3\u03BC\u03B1"@el . . "\u03A4\u03BF \u03BC\u03AC\u03B3\u03BC\u03B1 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C6\u03C5\u03C3\u03B9\u03BA\u03CC \u03B4\u03B9\u03AC\u03C0\u03C5\u03C1\u03BF \u03C0\u03B5\u03C4\u03C1\u03C9\u03BC\u03AC\u03C4\u03C9\u03BD \u03C0\u03BF\u03C5 \u03B2\u03C1\u03AF\u03C3\u03BA\u03B5\u03C4\u03B1\u03B9 \u03C3\u03C4\u03B1 \u03AD\u03B3\u03BA\u03B1\u03C4\u03B1 \u03C4\u03B7\u03C2 \u0393\u03B7\u03C2, \u03C4\u03BF \u03BF\u03C0\u03BF\u03AF\u03BF \u03C6\u03B8\u03AC\u03BD\u03BF\u03BD\u03C4\u03B1\u03C2 \u03C3\u03C4\u03B7\u03BD \u03B5\u03C0\u03B9\u03C6\u03AC\u03BD\u03B5\u03B9\u03B1, \u03B4\u03B7\u03BB\u03B1\u03B4\u03AE \u03C3\u03C4\u03B7 \u03BB\u03B9\u03B8\u03CC\u03C3\u03C6\u03B1\u03B9\u03C1\u03B1, \u03C3\u03C4\u03B5\u03C1\u03B5\u03BF\u03C0\u03BF\u03B9\u03B5\u03AF\u03C4\u03B1\u03B9 \u03B4\u03B7\u03BC\u03B9\u03BF\u03C5\u03C1\u03B3\u03CE\u03BD\u03C4\u03B1\u03C2 \u03C4\u03B1 \u03B5\u03BA\u03C1\u03B7\u03BE\u03B9\u03B3\u03B5\u03BD\u03AE \u03AE \u03C0\u03C5\u03C1\u03B9\u03B3\u03B5\u03BD\u03AE \u03C0\u03B5\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1, \u03C0\u03BF\u03C5 \u03BB\u03AD\u03B3\u03BF\u03BD\u03C4\u03B1\u03B9 \u03B5\u03C0\u03AF\u03C3\u03B7\u03C2 \u03BA\u03B1\u03B9 \u03BC\u03B1\u03B3\u03BC\u03B1\u03C4\u03BF\u03B3\u03B5\u03BD\u03AE. \u03A4\u03B7 \u03B4\u03B9\u03B5\u03B8\u03BD\u03AE \u03C3\u03AE\u03BC\u03B5\u03C1\u03B1 \u03BF\u03BD\u03BF\u03BC\u03B1\u03C3\u03AF\u03B1 \u03C4\u03BF\u03C5 \u03AD\u03BB\u03B1\u03B2\u03B5 \u03B1\u03C0\u03CC \u03C4\u03BF \u03B5\u03BB\u03BB\u03B7\u03BD\u03B9\u03BA\u03CC \u03B1\u03C1\u03C7\u03B1\u03AF\u03BF \u03C1\u03AE\u03BC\u03B1 \u03BC\u03AC\u03C3\u03C3\u03B5\u03B9\u03BD (= \u03B6\u03C5\u03BC\u03CE\u03BD\u03C9)."@el . . . . . . . . . . . "62265"^^ . . "Magma merupakan batu-batuan cair yang terletak di dalam kamar magma di bawah permukaan bumi. Magma di bumi merupakan larutan silika bersuhu tinggi (700-1300 \u00B0C) yang kompleks dan merupakan asal semua batuan beku. Magma berada dalam tekanan tinggi dan kadang kala memancut keluar melalui pembukaan gunung berapi dalam bentuk aliran lava atau letusan gunung berapi. Hasil letupan gunung berapi ini mengandung larutan gas yang tidak pernah sampai ke permukaan bumi. Magma terkumpul dalam kamar magma yang terasing di bawah kerak bumi dan mengandung komposisi yang berlainan menurut tempat magma itu didapati."@in . "\u062A\u062A\u062C\u0645\u0639 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0641\u064A\u0645\u0627 \u064A\u0639\u0631\u0641 \u0628\u0623\u0633\u0645 (\u063A\u0631\u0641 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 Magma Chembers) \u0627\u0644\u062A\u064A \u0642\u062F \u062A\u063A\u0630\u064A \u0628\u0631\u0643\u0627\u0646 \u0648\u062A\u062E\u0631\u062C \u0641\u0648\u0642 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u0648\u062A\u0633\u0645\u0649 \u0641\u064A \u062A\u0644\u0643 \u0627\u0644\u062D\u0627\u0644\u0629 (\u0644\u0627\u0641\u0627 Lava) \u0623\u0648 \u062A\u062A\u062C\u0645\u0639 \u062A\u062D\u062A \u0627\u0644\u0642\u0634\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0641\u064A \u0647\u0630\u0647 \u0627\u0644\u062D\u0627\u0644\u0629 \u062A\u0633\u0645\u0649 (\u0628\u0644\u0648\u062A\u0648\u0646 pluton). \u062A\u0639\u062A\u0628\u0631 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0642\u0627\u062F\u0631\u0629 \u0639\u0644\u0649 \u0623\u0642\u062A\u062D\u0627\u0645 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0645\u062C\u0627\u0648\u0631\u0629 \u0648\u062A\u0643\u0648\u0646 (\u0627\u0644\u0633\u062F\u0648\u062F \u0627\u0644\u0646\u0627\u0631\u064A\u0629 Igneous dikes) \u0648\u0627\u064A\u0636\u0627 \u062A\u0643\u0648\u0646 ( \u0627\u0644\u062C\u064A\u0648\u0628 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 sills) \u062B\u0645 \u062A\u0642\u0630\u0641 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u0644\u062A\u0643\u0648\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629. \u0627\u0644\u0645\u0648\u0627\u062F \u0627\u0644\u062A\u064A \u062A\u062A\u0643\u0648\u0646 \u0645\u0646\u0647\u0627 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0647\u064A \u0627\u0644\u0645\u0648\u0627\u062F \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0627\u0646\u064A\u0629 \u0648\u0647\u064A \u0645\u0648\u0627\u062F \u062A\u062D\u062A\u0648\u064A \u0639\u0644\u0649 \u0639\u0646\u0635\u0631 \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0648\u0646 \u0648\u0627\u0644\u0623\u0643\u0633\u062C\u064A\u0646."@ar . . "Magma je term\u00EDn ozna\u010Duj\u00EDc\u00ED sm\u011Bs roztaven\u00FDch hornin a plyn\u016F, kter\u00E1 se nach\u00E1z\u00ED pod povrchem Zem\u011B a dal\u0161\u00EDch terestrick\u00FDch t\u011Bles. Vyjma roztaven\u00FDch hornin m\u016F\u017Ee magma obsahovat i krystaly r\u016Fzn\u00FDch miner\u00E1l\u016F, rozpu\u0161t\u011Bn\u00E9 plyny \u010Di bublinky. Magma je hlubinn\u00FD ekvivalent l\u00E1vy; jakmile se magma dostane na povrch t\u011Blesa, pou\u017E\u00EDv\u00E1 se pro jeho ozna\u010Den\u00ED term\u00EDn l\u00E1va. Magma, kter\u00E9 vznik\u00E1 v zemsk\u00E9m pl\u00E1\u0161ti, se naz\u00FDv\u00E1 prim\u00E1rn\u00ED; sekund\u00E1rn\u00ED (\u017Eulov\u00E9) vznik\u00E1 horotvornou \u010Dinnost\u00ED. Prim\u00E1rn\u00ED magma je pon\u011Bkud \u0159id\u0161\u00ED a snadno pronik\u00E1 k zemsk\u00E9mu povrchu, kde tuhne. Vznikaj\u00ED z n\u011Bj v\u00FDlevn\u00E9 horniny, nap\u0159. \u010Dedi\u010D. Sekund\u00E1rn\u00ED se v\u011Bt\u0161inou tvo\u0159\u00ED ve velk\u00FDch hloubk\u00E1ch a tuhne pomalu pod povrchem Zem\u011B. Vytv\u00E1\u0159\u00ED velk\u00E1 t\u011Blesa (plutony), kter\u00E1 prostupuj\u00ED star\u0161\u00EDmi horninami. Podle m\u00EDsta utuhnut\u00ED magmatu se rozd\u011Bluj\u00ED vyv\u0159el\u00E9 horniny na hlu"@cs . . . . . . "0"^^ . . . "2"^^ . "3"^^ . . . . . "14"^^ . "El magma \u00E9s un tipus de roca format per la fusi\u00F3 parcial o total d'una font pariental (principalment, la part superior del mantell i la base de l'escor\u00E7a terrestre). El magma t\u00E9 composicions diverses tractant-se d'una mescla multi fase d'alta temperatura (depenent de la seva composici\u00F3 i evoluci\u00F3, des de menys de 700 \u00B0C fins m\u00E9s de 1500 \u00B0C) de s\u00F2lids (cristalls i fragments de roca), l\u00EDquida (en la seva majoria silicats) i gas\u00F3s (ric en H, O, C, S i Cl),. La fusi\u00F3 parcial de les roques es produeix b\u00E0sicament a les capes m\u00E9s externes de la Terra, per aix\u00F2 els elements m\u00E9s abundants dels magmes s\u00F3n els elements m\u00E9s abundants d'aquestes zones: O, Si, Al, Ca, Fe, Mg, Na, K. Els composts s\u00F3n els \u00F2xids corresponents: SiO2 (s\u00EDlice), Al2O3 (al\u00FAmina), CaO \u2026 El m\u00E9s abundant \u00E9s el SiO\u2082 (50-70%). Tamb\u00E9 \u00E9s important la pres\u00E8ncia de vapor d'aigua (fins a un 10%). Com m\u00E9s s\u00EDlice (SiO\u2082) t\u00E9 un magma, m\u00E9s viscositat t\u00E9. La viscositat condiciona el moviment i l'ascensi\u00F3 cap a les zones m\u00E9s superficials. El magma ascendent que, des de la seva generaci\u00F3 fins abans de la seva solidificaci\u00F3, brolla a la superf\u00EDcie, rep el nom de lava. La solidificaci\u00F3 del magma dona lloc a la formaci\u00F3 de roques magm\u00E0tiques."@ca . . . . . . . . . . . . . . . . . . . "El magma (del lat\u00EDn magma y este del griego \u03BC\u03AC\u03B3\u03BC\u03B1, \u00ABpasta\u00BB) es una mezcla multif\u00E1sica natural compuesta por una fase l\u00EDquida, formada por roca fundida, otra fase s\u00F3lida, mineral, y una parte gaseosa. Los gases que conforman la fracci\u00F3n gaseosa, conocidos como vol\u00E1tiles, pueden ser muy diversos, como el vapor de agua o el di\u00F3xido de carbono.\u200B Cuando el magma se enfr\u00EDa, sus componentes se cristalizan formando las rocas \u00EDgneas, que son de dos tipos: si el magma cristaliza en el interior de la tierra se forman las rocas plut\u00F3nicas o intrusivas, pero si asciende hacia la superficie, la materia fundida se denomina entonces lava, y al enfriarse forma las rocas volc\u00E1nicas o efusivas (intrusivas y efusivas son t\u00E9rminos en desuso).\u200B"@es . . . . "Fe2O3"@en . "100"^^ . "\u041C\u0430\u0433\u043C\u0430"@uk . . . . . . . . . . . . "Magma (from Ancient Greek \u03BC\u03AC\u03B3\u03BC\u03B1 (m\u00E1gma) 'thick unguent') is the molten or semi-molten natural material from which all igneous rocks are formed. Magma is found beneath the surface of the Earth, and evidence of magmatism has also been discovered on other terrestrial planets and some natural satellites. Besides molten rock, magma may also contain suspended crystals and gas bubbles."@en . "9.300000000000001"^^ . . "El magma (del lat\u00EDn magma y este del griego \u03BC\u03AC\u03B3\u03BC\u03B1, \u00ABpasta\u00BB) es una mezcla multif\u00E1sica natural compuesta por una fase l\u00EDquida, formada por roca fundida, otra fase s\u00F3lida, mineral, y una parte gaseosa. Los gases que conforman la fracci\u00F3n gaseosa, conocidos como vol\u00E1tiles, pueden ser muy diversos, como el vapor de agua o el di\u00F3xido de carbono.\u200B"@es . . . . . . "\u5CA9\u6F3F\uFF08Magma\uFF09\u662F\u7194\u5316\u7684\u5CA9\u77F3\uFF0C\u901A\u5E38\u4F4D\u65BC\u5730\u8868\u4E4B\u4E0B\u7684\u5CA9\u6F3F\u623F\u4E2D\u3002\u5CA9\u6F3F\u662F\u4E00\u7A2E\u8907\u96DC\u7684\u9AD8\u6EAB\u7845\u9178\u76D0\u6EB6\u6DB2\uFF0C\u662F\u5404\u7A2E\u706B\u6210\u5CA9\u7684\u524D\u8EAB\uFF0C\u706B\u6210\u5CA9\u662F\u7531\u5CA9\u6F3F\u51B7\u537B\u800C\u6210\u7684\u3002\u5CA9\u6F3F\u53EF\u4EE5\u4FB5\u5165\u9130\u8FD1\u7684\u5730\u6BBC\u5CA9\u77F3\u6216\u662F\u5192\u51FA\u5730\u8868\u3002 \u5CA9\u6F3F\u6EAB\u5EA6\u53EF\u4F4E\u81F3650 \u00B0C\uFF0C\u9AD8\u81F31400 \u00B0C\u3002\u7194\u5CA9\u4E2D\u542B\u67091 ~ 8 %\u7684\u6325\u53D1\u6027\u7269\u8D28\u3002\u5CA9\u6F3F\u8655\u65BC\u9AD8\u58D3\u4E4B\u4E2D\uFF0C\u6709\u6642\u6703\u7D93\u7531\u706B\u5C71\u53E3\uFF08\u6216\u8B6F\u706B\u5C71\u7BA1\u3001\u706B\u5C71\u6D41\u53E3\u3001\u706B\u5C71\u9053\uFF09\u4EE5\u7194\u5CA9\u6D41\u6216\u662F\u4EE5\u706B\u5C71\u788E\u5C51\u7269\u7684\u706B\u5C71\u5674\u51FA\u7269\u7684\u5F62\u5F0F\u5192\u51FA\u3002\u9019\u4E9B\u706B\u5C71\u5674\u767C\u7684\u7522\u7269\u901A\u5E38\u5305\u62EC\u4E86\u5F9E\u6C92\u5230\u904E\u5730\u8868\u7684\u6DB2\u9AD4\u3001\u7D50\u6676\u9AD4\u53CA\u6EB6\u89E3\u6C23\u9AD4\u7B49\u3002\u5CA9\u6F3F\u6703\u5728\u5730\u6BBC\u4E2D\u5404\u81EA\u5206\u96E2\u7684\u5CA9\u6F3F\u5EAB\u5167\u96C6\u7D50\uFF0C\u4E0D\u540C\u5730\u65B9\u7684\u5CA9\u6F3F\u7D44\u6210\u6210\u4EFD\u6703\u7A0D\u6709\u4E0D\u540C\u3002 \u9019\u4E9B\u5730\u65B9\u5305\u62EC\u4E86\u96B1\u6C92\u5E36\u3001\u3001\u4E2D\u6D0B\u810A\u6216\u662F\u5730\u51FD\u71B1\u67F1\u7684\u71B1\u9EDE\u4E4B\u4E0A\u3002\u53EA\u6709\u5728\u5730\u7403\u7684\u8EDF\u6D41\u5708\u5167\u7684\u7279\u5B9A\u689D\u4EF6\u4E4B\u4E0B\u5CA9\u6F3F\u624D\u6703\u5F62\u6210\u3002"@zh . . "In vulcanologia, il magma \u00E8 un sistema complesso di roccia fusa, compreso anche di acqua, altri fluidi, sostanze gassose in esso disciolte e fenocristalli, nel caso in cui le condizioni di pressione e temperatura di liquidus non siano state superate."@it . . . . . . . "Magma"@pl . "Magma (s\u00E4chlich; von altgriechisch \u03BC\u03AC\u03B3\u03BC\u03B1 m\u00E1gma, deutsch \u201Ageknetete Masse\u2018) hei\u00DFen Gesteinsschmelzen, die in Teilen des oberen Erdmantels und der tieferen Erdkruste vorkommen. Die Flie\u00DFf\u00E4higkeit des Magmas ist die Ursache des Vulkanismus (siehe auch Vulkan) und hat eine gro\u00DFe Bedeutung f\u00FCr die Gesteinsbildung, da sich aus dem erstarrenden Magma die magmatischen Gesteine oder Magmatite bilden. Diese unterteilt man in Plutonite, wenn das Magma in der Erdkruste langsam abk\u00FChlt und daher gr\u00F6\u00DFere Kristalle bilden kann, und in Vulkanite, wenn das Magma beim Austritt an die Erdoberfl\u00E4che (zum Beispiel als Lava oder in Form von Pyroklasten) schneller abk\u00FChlt. Zu den Plutoniten z\u00E4hlt zum Beispiel der Granit, zu den Vulkaniten der Basalt."@de . . "Magma (stgr. \u03BC\u03AC\u03B3\u03BC\u03B1 \u2019g\u0119sta ma\u015B\u0107\u2019) \u2013 gor\u0105ca, stopiona masa krzemian\u00F3w i glinokrzemian\u00F3w z domieszkami tlenk\u00F3w i siarczk\u00F3w, z du\u017C\u0105 ilo\u015Bci\u0105 wody i gaz\u00F3w, powstaj\u0105ca w g\u0142\u0119bi Ziemi; magma, kt\u00F3ra wydobywa si\u0119 na powierzchni\u0119 Ziemi, nazywana jest law\u0105."@pl . "Magma"@eu . . . . . . . . . "Magma (fr\u00E5n grekiska f\u00F6r \"salva\" eller \"kn\u00E5dad massa\") best\u00E5r oftast av sm\u00E4lt bergartsmassa blandat med gaser och kristaller. Bergarter kan aldrig sm\u00E4lta totalt s\u00E5 magma kan d\u00E4rf\u00F6r aldrig best\u00E5 av endast sm\u00E4lt material."@sv . . . . . . . "Magma"@cs . . . "Magmo (greke: \u201Eknedita maso\u201C) signifas la maso el fandita \u015Dtona\u0135o, trovi\u011Danta en partoj de la supra termantelo kaj de la profunda terkrusto. La flukapablo de la magmo estas la ka\u016Dzo de la vulkanismo (vidu anka\u016D: vulkano) kaj havas grandan signifon por la formi\u011Do de rokoj. \u015Ctona\u0135oj formi\u011Dintaj el solidi\u011Dinta magmo nomi\u011Das a\u016D profund\u015Dtona\u0135oj. Je ili oni distingas plutonitojn, kiuj ekestas, se magmo en la terinterno malvami\u011Das malrapide kaj tial povas formi kristalojn, kaj vulkanitojn, se magmo eli\u011Dante al la tersurfaco rapide malvarmi\u011Das, ekzemple kiel lafo a\u016D en formo de . Al la plutonitoj ekzemple apartenas la granito, al la vulkanitoj la bazalto."@eo . . "Magma (grezieraz: \u03BC\u03AC\u03B3\u03BC\u03B1, \"ukendu lodia\"), Lurrarren edo beste planeten barneko arroka urtuen masak hartzen duen izena da. Tenperatura handiko nahasketa faseanitza da, osagai likido, gas eta solidoz osaturik dagoena. Bere sorreratik, gainazalean solidotu baino lehenago goraka doan magmari, laba deritzo. Magma hozten denean arroka igneoak sortzen dira."@eu . . "Carraig le\u00E1ite a chrutha\u00EDtear tr\u00ED mhaintl\u00EDn an Domhain a ph\u00E1irtle\u00E1 le teas \u00F3n gcro\u00EDleac\u00E1n. Faoi ch\u00FAins\u00ED geola\u00EDocha ar leith, d\u00E9anann an charraig le\u00E1ite seo imirce suas tr\u00EDd an screamh go reonn ina ions\u00E1 doigheartha, n\u00F3 go n-\u00E9ir\u00EDonn l\u00E9i an dromchla a shroichint, \u00E1it a gcailleann s\u00ED a comh\u00E1bhair inghalaithe is a mbr\u00FAchtann amach mar laibhe."@ga . . . . . . . . . . . . "\u0635\u0647\u0627\u0631\u0629"@ar . . "\u30DE\u30B0\u30DE\uFF08\u82F1: magma\uFF09\u3068\u306F\u3001\u5730\u7403\u3092\u306F\u3058\u3081\u3068\u3059\u308B\u5929\u4F53\u3092\u69CB\u6210\u3059\u308B\u56FA\u4F53\u304C\u3001\u305D\u306E\u5185\u90E8\u3067\u6EB6\u878D\u3057\u3066\u3044\u308B\u3082\u306E\u3067\u3042\u308B\u3002\u5730\u7403\u306E\u30DE\u30F3\u30C8\u30EB\u3084\u5730\u6BBB\u306F\u4E3B\u306B\u30B1\u30A4\u9178\u5869\u9271\u7269\u3067\u3067\u304D\u3066\u3044\u308B\u305F\u3081\u3001\u305D\u306E\u6EB6\u878D\u7269\u3067\u3042\u308B\u30DE\u30B0\u30DE\u3082\u4E00\u822C\u306B\u30B1\u30A4\u9178\u5869\u4E3B\u4F53\u306E\u7D44\u6210\u3092\u6301\u3064\u304C\u3001\u7A00\u306B\u300C\u70AD\u9178\u5869\u300D\u9271\u7269\u3092\u4E3B\u4F53\u3068\u3059\u308B\u30DE\u30B0\u30DE\u3082\u5B58\u5728\u3059\u308B\u3002\u300C\u5CA9\u6F3F\uFF08\u304C\u3093\u3057\u3087\u3046\uFF09\u300D\u3068\u3082\u3044\u3046\u3002\u5730\u7403\u4EE5\u5916\u306E\u5929\u4F53\u3067\u30DE\u30B0\u30DE\u306E\u5B58\u5728\u306F\u63A8\u5B9A\u306E\u307F\u3067\u78BA\u8A8D\u3055\u308C\u3066\u3044\u306A\u3044\u305F\u3081\u3001\u672C\u9805\u3067\u306F\u5730\u7403\u306B\u304A\u3051\u308B\u30DE\u30B0\u30DE\u306B\u3064\u3044\u3066\u8A18\u8F09\u3059\u308B\u3002"@ja . . "Na2O"@en . . . . "3.9"^^ . . . . "\uB9C8\uADF8\uB9C8"@ko . . . . . "1116058475"^^ . . . . "Magma merupakan batu-batuan cair yang terletak di dalam kamar magma di bawah permukaan bumi. Magma di bumi merupakan larutan silika bersuhu tinggi (700-1300 \u00B0C) yang kompleks dan merupakan asal semua batuan beku. Magma berada dalam tekanan tinggi dan kadang kala memancut keluar melalui pembukaan gunung berapi dalam bentuk aliran lava atau letusan gunung berapi."@in . "\u30DE\u30B0\u30DE"@ja . . . . . "Magmo"@eo . . . . "In vulcanologia, il magma \u00E8 un sistema complesso di roccia fusa, compreso anche di acqua, altri fluidi, sostanze gassose in esso disciolte e fenocristalli, nel caso in cui le condizioni di pressione e temperatura di liquidus non siano state superate. Dal punto di vista geochimico, il magma \u00E8 distinto dalla lava, poich\u00E9 possiede ancora la componente gassosa disciolta. Il magma \u00E8 presente solo in situazioni ipogee dal momento che, quando il magma fuoriesce dalla crosta attraverso apparati vulcanici, diviene lava, perdendo alcuni suoi componenti volatili quali acqua e gas disciolti, non essendoci pi\u00F9 le condizioni di pressione sufficienti a mantenerli in soluzione nella massa fusa."@it . . . "\u041C\u0430\u0301\u0433\u043C\u0430 (\u0432\u0456\u0434 \u0433\u0440\u0435\u0446. \u03BC\u03AC\u03B3\u03BC\u03B1 \u2014 \u0442\u0456\u0441\u0442\u043E) \u2014 \u043F\u0440\u0438\u0440\u043E\u0434\u043D\u0438\u0439, \u043F\u0435\u0440\u0435\u0432\u0430\u0436\u043D\u043E \u0441\u0438\u043B\u0456\u043A\u0430\u0442\u043D\u0438\u0439 \u0432\u0438\u0441\u043E\u043A\u043E\u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u043D\u0438\u0439 \u0440\u043E\u0437\u043F\u043B\u0430\u0432, \u044F\u043A\u0438\u0439 \u0443\u0442\u0432\u043E\u0440\u044E\u0454\u0442\u044C\u0441\u044F \u0432 \u043D\u0430\u0434\u0440\u0430\u0445 \u0417\u0435\u043C\u043B\u0456."@uk . . . . . . . . . . . . . . . . . . "Magma"@in . "Un magma est une roche enti\u00E8rement ou partiellement fondue. Il comporte n\u00E9cessairement une phase liquide, g\u00E9n\u00E9ralement compos\u00E9e de silicates et contenant des gaz dissous. Il comporte souvent aussi, en suspension dans le liquide, une phase gazeuse (des bulles) et une ou plusieurs phases solides (des cristaux), qui proviennent respectivement de l'exsolution partielle des gaz dissous et de la solidification partielle du liquide par d\u00E9compression et refroidissement. Le magma peut aussi comporter des \u00E9l\u00E9ments solides provenant des roches \u00E0 travers lesquelles le magma est remont\u00E9 : fragments de roches mantelliques ou crustales (x\u00E9nolithes) et/ou cristaux isol\u00E9s (x\u00E9nocristaux). Les magmas se forment \u00E0 haute temp\u00E9rature et sous haute pression par fusion partielle de la cro\u00FBte terrestre ou du manteau. Moins denses que les roches solides de la lithosph\u00E8re, ils sont entra\u00EEn\u00E9s vers le haut par la pouss\u00E9e d'Archim\u00E8de, sous forme de dykes ou de diapirs. Selon le contraste entre leur densit\u00E9 et celle des roches travers\u00E9es, les magmas s'arr\u00EAtent \u00E0 une certaine profondeur (plutons) ou s'\u00E9panchent en surface (laves). Leur refroidissement complet conduit \u00E0 la formation de roches magmatiques (roches plutoniques pour les plutons, roches volcaniques pour les laves)."@fr . "Magma (do grego \u03BC\u03AC\u03B3\u03BC\u03B1; \"pasta\") \u00E9 a designa\u00E7\u00E3o dada nas geoci\u00EAncias \u00E0s massas de rocha em fus\u00E3o total ou parcial que existem debaixo da superf\u00EDcie da Terra e provavelmente de outros planetas tel\u00FAricos. Os magmas s\u00E3o constitu\u00EDdos por uma mistura de rocha em estado vari\u00E1vel de fus\u00E3o com materiais vol\u00E1teis, composta maioritariamente por silicatos a alta press\u00E3o e temperatura acompanhados por um conjunto vari\u00E1vel, em propor\u00E7\u00E3o e tipo, de i\u00F5es met\u00E1licos e compostos vol\u00E1teis ricos em enxofre, podendo ainda conter cristais em suspens\u00E3o, gases dissolvidos e por vezes bolhas de g\u00E1s. Os magmas acumulam-se em geral dentro de c\u00E2maras magm\u00E1ticas situadas entre os 15 e os 150 km de profundidade, com temperaturas que variam entre 650 e 1 200 \u00BAC, mas podendo atingir 1 560 \u00B0C. Quando expelido por um vulc\u00E3o"@pt . . . "Magma"@ca . "1.5"^^ . . . . . "Magma (gesteente)"@nl . . . . . . . . . "\u03A4\u03BF \u03BC\u03AC\u03B3\u03BC\u03B1 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C6\u03C5\u03C3\u03B9\u03BA\u03CC \u03B4\u03B9\u03AC\u03C0\u03C5\u03C1\u03BF \u03C0\u03B5\u03C4\u03C1\u03C9\u03BC\u03AC\u03C4\u03C9\u03BD \u03C0\u03BF\u03C5 \u03B2\u03C1\u03AF\u03C3\u03BA\u03B5\u03C4\u03B1\u03B9 \u03C3\u03C4\u03B1 \u03AD\u03B3\u03BA\u03B1\u03C4\u03B1 \u03C4\u03B7\u03C2 \u0393\u03B7\u03C2, \u03C4\u03BF \u03BF\u03C0\u03BF\u03AF\u03BF \u03C6\u03B8\u03AC\u03BD\u03BF\u03BD\u03C4\u03B1\u03C2 \u03C3\u03C4\u03B7\u03BD \u03B5\u03C0\u03B9\u03C6\u03AC\u03BD\u03B5\u03B9\u03B1, \u03B4\u03B7\u03BB\u03B1\u03B4\u03AE \u03C3\u03C4\u03B7 \u03BB\u03B9\u03B8\u03CC\u03C3\u03C6\u03B1\u03B9\u03C1\u03B1, \u03C3\u03C4\u03B5\u03C1\u03B5\u03BF\u03C0\u03BF\u03B9\u03B5\u03AF\u03C4\u03B1\u03B9 \u03B4\u03B7\u03BC\u03B9\u03BF\u03C5\u03C1\u03B3\u03CE\u03BD\u03C4\u03B1\u03C2 \u03C4\u03B1 \u03B5\u03BA\u03C1\u03B7\u03BE\u03B9\u03B3\u03B5\u03BD\u03AE \u03AE \u03C0\u03C5\u03C1\u03B9\u03B3\u03B5\u03BD\u03AE \u03C0\u03B5\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1, \u03C0\u03BF\u03C5 \u03BB\u03AD\u03B3\u03BF\u03BD\u03C4\u03B1\u03B9 \u03B5\u03C0\u03AF\u03C3\u03B7\u03C2 \u03BA\u03B1\u03B9 \u03BC\u03B1\u03B3\u03BC\u03B1\u03C4\u03BF\u03B3\u03B5\u03BD\u03AE. \u03A4\u03B7 \u03B4\u03B9\u03B5\u03B8\u03BD\u03AE \u03C3\u03AE\u03BC\u03B5\u03C1\u03B1 \u03BF\u03BD\u03BF\u03BC\u03B1\u03C3\u03AF\u03B1 \u03C4\u03BF\u03C5 \u03AD\u03BB\u03B1\u03B2\u03B5 \u03B1\u03C0\u03CC \u03C4\u03BF \u03B5\u03BB\u03BB\u03B7\u03BD\u03B9\u03BA\u03CC \u03B1\u03C1\u03C7\u03B1\u03AF\u03BF \u03C1\u03AE\u03BC\u03B1 \u03BC\u03AC\u03C3\u03C3\u03B5\u03B9\u03BD (= \u03B6\u03C5\u03BC\u03CE\u03BD\u03C9)."@el . . . . . "Magma (from Ancient Greek \u03BC\u03AC\u03B3\u03BC\u03B1 (m\u00E1gma) 'thick unguent') is the molten or semi-molten natural material from which all igneous rocks are formed. Magma is found beneath the surface of the Earth, and evidence of magmatism has also been discovered on other terrestrial planets and some natural satellites. Besides molten rock, magma may also contain suspended crystals and gas bubbles. Magma is produced by melting of the mantle or the crust in various tectonic settings, which on Earth include subduction zones, continental rift zones, mid-ocean ridges and hotspots. Mantle and crustal melts migrate upwards through the crust where they are thought to be stored in magma chambers or trans-crustal crystal-rich mush zones. During magma's storage in the crust, its composition may be modified by fractional crystallization, contamination with crustal melts, magma mixing, and degassing. Following its ascent through the crust, magma may feed a volcano and be extruded as lava, or it may solidify underground to form an intrusion, such as a dike, a sill, a laccolith, a pluton, or a batholith. While the study of magma has relied on observing magma after its transition into a lava flow, magma has been encountered in situ three times during geothermal drilling projects, twice in Iceland (see ) and once in Hawaii."@en . "Al2O3"@en . . . . . "Magma"@pt . "( \uB2E4\uB978 \uB73B\uC5D0 \uB300\uD574\uC11C\uB294 \uB9C8\uADF8\uB9C8 (\uB3D9\uC74C\uC774\uC758) \uBB38\uC11C\uB97C \uCC38\uACE0\uD558\uC2ED\uC2DC\uC624.) \uC554\uC7A5(\u5DD6\u6F3F), \u540C\u610F\uB9C8\uADF8\uB9C8(\uC601\uC5B4: magma \u2190 \uADF8\uB9AC\uC2A4\uC5B4 \u03BC\u03AC\u03B3\u03BC\u03B1 m\u00E1gma '\uB450\uAEBC\uC6B4 \uC5F0\uACE0'\uC5D0\uC11C \uC720\uB798 , \uBB38\uD654\uC5B4: \uB3CC\uBB3C)\uB294 \uC554\uC11D\uC774 \uB179\uC740 \uAC83\uC774\uB2E4. \uAC00\uC7A5 \uAC04\uB2E8\uD55C \uACBD\uC6B0 \uC554\uC11D\uC774 \uB179\uB294 \uC870\uAC74\uC740 \uC77C\uBC18\uC801\uC778 \uC5F4\uC5ED\uD559\uC758 \uBC95\uCE59\uC5D0 \uB530\uB77C \uC628\uB3C4\uC640 \uC555\uB825\uC5D0 \uC758\uD574\uC11C \uACB0\uC815\uB41C\uB2E4. \uD558\uC9C0\uB9CC \uC2E4\uC81C \uC9C0\uAD6C\uC5D0\uC11C \uC77C\uC5B4\uB098\uB294 \uD604\uC0C1\uC740 \uC628\uB3C4, \uC555\uB825\uACFC \uD568\uAED8 \uBB3C\uC758 \uD568\uB7C9\uACFC \uC554\uC11D\uC758 \uC131\uBD84\uC744 \uD568\uAED8 \uACE0\uB824\uD558\uC5EC\uC57C \uD55C\uB2E4. \uC628\uB3C4\uAC00 \uB192\uC544\uC9C0\uBA74 \uC554\uC11D\uC774 \uB179\uAE30 \uC2DC\uC791\uD55C\uB2E4. \uC555\uB825\uC774 \uB192\uC544\uC9C0\uBA74 \uB354 \uB192\uC740 \uC628\uB3C4\uAC00 \uB418\uC5B4\uC57C \uC554\uC11D\uC774 \uB179\uAE30 \uC2DC\uC791\uD55C\uB2E4. \uBB3C\uC774 \uD3EC\uD568\uB41C \uC554\uC11D\uC740 \uD6E8\uC52C \uB0AE\uC740 \uC628\uB3C4\uC5D0\uC11C \uB179\uC744 \uC218 \uC788\uB2E4. \uC77C\uBC18\uC801\uC73C\uB85C \uC18C\uB4D0(Na), \uD3EC\uD0C0\uC298(K)\uC774 \uB9CE\uC774 \uD3EC\uD568\uB41C \uC554\uC11D\uBCF4\uB2E4 \uCCA0(Fe), \uB9C8\uADF8\uB124\uC298(Mg)\uC774 \uB9CE\uC774 \uD3EC\uD568\uB418\uC5B4\uC788\uB294 \uC554\uC11D\uC774 \uB354 \uB192\uC740 \uC628\uB3C4\uC5D0\uC11C \uB179\uB294\uB2E4. \uD574\uB839\uC5D0\uC11C \uBD84\uCD9C\uB418\uB294 \uB9C8\uADF8\uB9C8\uB294 \uB9E8\uD2C0 \uBB3C\uC9C8\uC774 \uB300\uB958\uC5D0 \uC758\uD574 \uC0C1\uC2B9\uD558\uBA74\uC11C \uC555\uB825\uC774 \uB0AE\uC544\uC9C0\uC790 \uB179\uC544\uC11C \uB41C \uB9C8\uADF8\uB9C8\uC774\uB2E4. \uD574\uB839 \uBC14\uB85C \uC544\uB798\uC758 \uB9E8\uD2C0 \uC548\uC5D0\uB294 \uC218\uBD84 \uD568\uB7C9\uC774 \uB9E4\uC6B0 \uB0AE\uAE30 \uB54C\uBB38\uC5D0 \uD574\uB839\uC758 \uB9C8\uADF8\uB9C8\uB294 \uC628\uB3C4\uAC00 \uB9E4\uC6B0 \uB192\uB2E4. \uADF8\uB9AC\uACE0 \uD574\uB839\uC758 \uB9C8\uADF8\uB9C8\uB294 \uB9E4\uC6B0 \uAC15\uD55C \uC5FC\uAE30\uC131\uC774\uB2E4. \uD574\uAD6C \uBD80\uADFC\uC758 \uD654\uC0B0\uC740 \uB300\uB959 \uC9C0\uAC01\uC774\uB098 \uD574\uC591 \uC9C0\uAC01\uC774 \uB9E8\uD2C0 \uC548\uC73C\uB85C \uC0BD\uC785\uB418\uC5B4 \uB4E4\uC5B4\uAC00\uBA74\uC11C \uBB3C\uC774 \uD3EC\uD568\uB41C \uC554\uC11D\uC774 \uB179\uC544\uC11C \uB41C \uB9C8\uADF8\uB9C8\uC774\uB2E4. \uC0C1\uB300\uC801\uC73C\uB85C \uC628\uB3C4\uAC00 \uB0AE\uACE0 \uC911\uC131 \uB0B4\uC9C0\uB294 \uC0B0\uC131\uC778 \uACBD\uC6B0\uAC00 \uB9CE\uB2E4. \uC810\uC131\uC774 \uB192\uAE30 \uB54C\uBB38\uC5D0 \uC6A9\uC554\uB958\uB294 \uB113\uAC8C \uD37C\uC9C0\uC9C0 \uBABB\uD558\uACE0 \uD55C \uACF3\uC5D0 \uC9D1\uC911\uB418\uC5B4 \uC6D0\uCD94 \uBAA8\uC591\uC758 \uD654\uC0B0\uCCB4\uB97C \uD615\uC131\uD55C\uB2E4. \uCE84\uCC28\uCE74\uBC18\uB3C4, \uC77C\uBCF8 \uC5F4\uB3C4, , \uC548\uB370\uC2A4 \uC0B0\uB9E5\uC758 \uC5EC\uB7EC \uD654\uC0B0\uB4E4\uC774 \uADF8 \uC608\uC774\uB2E4. \uC5F4\uC810\uC5D0\uC11C\uC758 \uD654\uC0B0\uB4E4\uB3C4 \uD574\uB839\uC758 \uB9C8\uADF8\uB9C8\uC640 \uBE44\uC2B7\uD55C \uACFC\uC815\uC744 \uD1B5\uD574 \uD615\uC131\uB418\uC9C0\uB9CC \uADF8 \uAE30\uC6D0\uC740 \uB9E8\uD2C0\uC758 \uB354 \uAE4A\uC740 \uACF3\uC73C\uB85C \uC5EC\uACA8\uC9C4\uB2E4. \uC5F4\uC810\uC740 \uB9CE\uC740 \uC591\uC758 \uB9C8\uADF8\uB9C8\uB97C \uBD84\uCD9C\uD558\uAE30 \uB54C\uBB38\uC5D0 \uADF8 \uC704\uC5D0 \uD070 \uD654\uC0B0\uCCB4\uB97C \uB9CC\uB4E0\uB2E4. \uC5FC\uAE30\uC131 \uB9C8\uADF8\uB9C8\uB294 \uC628\uB3C4\uAC00 \uB192\uACE0 \uC774 \uBC1C\uB2EC\uB418\uC5B4\uC788\uC9C0 \uC54A\uAE30 \uB54C\uBB38\uC5D0 \uC810\uC131\uC774 \uB0AE\uC544\uC11C \uB113\uAC8C \uD37C\uC838\uC11C \uD750\uB974\uBA70 \uADF8 \uACB0\uACFC 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"4.1"^^ . . . "13.9"^^ . . .