"\u0422\u0440\u0435\u043C\u043E\u043B\u0456\u0442 \u2014 \u043F\u043E\u0440\u043E\u0434\u043E\u0442\u0432\u0456\u0440\u043D\u0438\u0439 \u043C\u0456\u043D\u0435\u0440\u0430\u043B \u043A\u043B\u0430\u0441\u0443 \u0441\u0438\u043B\u0456\u043A\u0430\u0442\u0456\u0432, \u0441\u0456\u043C\u0435\u0439\u0441\u0442\u0432\u0430 \u0430\u043C\u0444\u0456\u0431\u043E\u043B\u0456\u0432. \u041C\u0430\u0433\u043D\u0456\u0457\u0441\u0442\u0438\u0439 \u0440\u0456\u0437\u043D\u043E\u0432\u0438\u0434 \u0430\u043A\u0442\u0438\u043D\u043E\u043B\u0456\u0442\u0443. \u041D\u0435\u0437\u0432\u0438\u0447\u0430\u0439\u043D\u0438\u0439 \u0432\u0438\u0433\u043B\u044F\u0434 \u0434\u0435\u044F\u043A\u0438\u0445 \u0440\u0456\u0437\u043D\u043E\u0432\u0438\u0434\u0456\u0432 \u0442\u0440\u0435\u043C\u043E\u043B\u0456\u0442\u0443 \u0440\u043E\u0431\u0438\u0442\u044C \u0439\u043E\u0433\u043E \u0446\u0456\u043D\u043D\u0438\u043C \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u043E\u043C \u0434\u043B\u044F \u043A\u043E\u043B\u0435\u043A\u0446\u0456\u043E\u043D\u0435\u0440\u0456\u0432. \u0423 \u043D\u0435 \u043C\u0435\u043D\u0448\u043E\u043C\u0443 \u0441\u0442\u0443\u043F\u0435\u043D\u0456 \u043F\u0440\u0438\u0432\u0430\u0431\u043B\u044E\u0454 \u0456 \u0439\u043E\u0433\u043E \u0433\u0430\u0440\u043D\u0435 \u0441\u0432\u0456\u0442\u0456\u043D\u043D\u044F. \u0421\u0432\u043E\u0457\u043C \u0456\u043C'\u044F\u043C \u0442\u0440\u0435\u043C\u043E\u043B\u0456\u0442 \u0437\u043E\u0431\u043E\u0432'\u044F\u0437\u0430\u043D\u0438\u0439 \u043C\u0456\u0441\u0446\u044E \u0437\u043D\u0430\u0445\u043E\u0434\u0436\u0435\u043D\u043D\u044F \u0439\u043E\u0433\u043E \u0437\u0440\u0430\u0437\u043A\u0456\u0432, \u043D\u0430 \u043F\u0456\u0434\u0441\u0442\u0430\u0432\u0456 \u044F\u043A\u0438\u0445 \u0431\u0443\u043B\u043E \u0437\u0440\u043E\u0431\u043B\u0435\u043D\u043E \u043F\u0435\u0440\u0448\u0438\u0439 \u0439\u043E\u0433\u043E \u043E\u043F\u0438\u0441. \u0419\u0434\u0435\u0442\u044C\u0441\u044F \u043F\u0440\u043E \u0434\u043E\u043B\u0438\u043D\u0443 \u0422\u0440\u0435\u043C\u043E\u043B\u0430 \u043F\u043E\u0440\u0443\u0447 \u0437 \u0421\u0435\u043D-\u0413\u043E\u0442\u0430\u0440\u0434\u0441\u044C\u043A\u0438\u043C \u0433\u0456\u0440\u0441\u044C\u043A\u0438\u043C \u043C\u0430\u0441\u0438\u0432\u043E\u043C (\u0428\u0432\u0435\u0439\u0446\u0430\u0440\u0456\u044F). \u041D\u0430\u0437\u0432\u0443 \u0434\u0430\u0432 J.G.H\u00F6pfner, 1790. \u0421\u0438\u043D\u043E\u043D\u0456\u043C\u0438: \u0433\u0440\u0430\u043C\u0430\u0442\u0438\u0442, \u0433\u0435\u043F\u0444\u043D\u0435\u0440\u0438\u0442, \u043A\u0430\u043B\u0430\u043C\u0456\u0442, \u043A\u0430\u0440\u0430\u043C\u0437\u0438\u043D\u0456\u0442, \u043D\u043E\u0440\u0434\u0435\u043D\u0448\u0435\u043B\u044C\u0434\u0438\u0442, \u0440\u0430\u0444\u0456\u043B\u0456\u0442, \u0441\u0435\u0431\u0435\u0441\u0438\u0442."@uk . "Tremolite"@en . "\u900F\u95EA\u77F3\u4E3A\u89D2\u95EA\u77F3\u7684\u4E00\u7C7B\uFF0C\u4F86\u81EA\u767D\u4E91\u77F3\u548C\u77F3\u82F1\u6DF7\u5408\u6C89\u79EF\u540E\u5F62\u6210\u7684\u53D8\u8D28\u5CA9\u3002\u6676\u4F53\u5E38\u8F90\u5C04\u72B6\u6216\u67F1\u72B6\u6392\u5217\u3002 \u5176\u4E2D\u7684\u9541\u79BB\u5B50\u53EF\u88AB\u88AB\u4E8C\u4EF7\u94C1\u79BB\u5B50\u90E8\u5206\u7F6E\u6362\uFF0C\u5F62\u6210\u4E0E\u9633\u8D77\u77F3\uFF08actinolite\uFF09\u3001\u94C1\u9633\u8D77\u77F3\uFF08ferro-actinolite\uFF09\u7684\u7CFB\u5217\u6DF7\u5408\u77FF\u7269\uFF0C\u540C\u65F6\u989C\u8272\u52A0\u6DF1\uFF0C\u76F4\u81F3\u6DF1\u7EFF\u3002 \u5728\u9AD8\u6E29\u4E0B\u8F6C\u5316\u6210\u900F\u8F89\u77F3\u3001\u65B9\u89E3\u77F3\u3001\u77F3\u69B4\u5B50\u77F3\u3001\u6ED1\u77F3\u548C\u86C7\u7EB9\u77F3\u7B49\u5176\u4ED6\u77FF\u7269\uFF0C\u56E0\u800C\u53EF\u7528\u6765\u5224\u5B9A\u5F62\u6210\u53D8\u8D28\u7684\u6E29\u5EA6\u3002"@zh . . . . "Measured: 86\u00B0 to 88\u00B0"@en . . "La tremolite \u00E8 un inosilicato, un anfibolo appartenente al sottogruppo degli anfiboli di calcio, strutturato con una doppia catena di tetraedri (SiO4) i quali condividono tre dei quattro ossigeni.Di genesi metamorfica da parte della dolomite in presenza di silice. Cristallizza nel sistema monoclino, formante un abito di prevalenza prismatico, sovente lanceolato. La tremolite forma una serie con l'actinolite e la ferro-actinolite nella quale il magnesio viene sostituito dal ferro (Fe2+), pi\u00F9 precisamente \u00E8 stata definita con la composizione che va da \u2610Ca2Mg5Si8O22(OH)2 a \u2610Ca2Mg4,5Fe2+0,5Si8O22(OH)2. Generalmente la suddivisione tra due specie di una serie viene stabilito con il limite del 50% dell'elemento che varia ma in questo caso \u00E8 stato stabilito un intervallo molto pi\u00F9 stretto per facilitare la distinzione della tremolite incolore dall'actinolite generalmente di colore verde, molto importante in ambito petrologico. La tremolite \u00E8 conosciuta fin dalla fine del XVIII secolo, il primo a menzionarla nel 1789 \u00E8 stato probabilmente Johann Georg Albrecht H\u00F6pfner (1759\u20141813) mentre la prima descrizione si deve a Ermenegildo Pini (1739-1825) nel 1796. In realt\u00E0 la prima descrizione di questo minerali si deve a nel 1782 in base ad un ritrovamento avvenuto nei pressi del villaggio di Sebe\u015Fu de Jos (facente parte del comune di Turnu Ro\u0219u) in Transilvania, Romania coi nomi di s\u00E4ulenspath e sternspath."@it . . . . . . . . . . "\uD22C\uC12C\uC11D(\u900F\u9583\u77F3, Tremolite)\uC740 \uAC01\uC12C\uC11D\uC5D0 \uC18D\uD558\uB294 \uADDC\uC0B0\uC5FC \uAD11\uBB3C\uC758 \uC77C\uC885\uC73C\uB85C, \uD654\uD559 \uBD84\uC790\uC2DD\uC740 Ca2(Mg5.0-4.5Fe2+0.0-0.5)Si8O22(OH)2\uC774\uB2E4. \uBC31\uC6B4\uC554\uACFC \uC11D\uC601\uC758 \uCE68\uC804\uBB3C\uC774 \uBCC0\uC131 \uC791\uC6A9\uC744 \uD1B5\uD574 \uC0DD\uC131\uB41C\uB2E4."@ko . . "300"^^ . . "\u0422\u0440\u0435\u043C\u043E\u043B\u0438\u0442 \u2014 \u043B\u0435\u043D\u0442\u043E\u0447\u043D\u044B\u0439 \u0441\u0438\u043B\u0438\u043A\u0430\u0442 \u0433\u0440\u0443\u043F\u043F\u044B \u043C\u043E\u043D\u043E\u043A\u043B\u0438\u043D\u043D\u044B\u0445 \u0430\u043C\u0444\u0438\u0431\u043E\u043B\u043E\u0432. \u041D\u0430\u0437\u0432\u0430\u043D \u043F\u043E , \u043A\u043E\u0442\u043E\u0440\u0430\u044F \u043D\u0430\u0445\u043E\u0434\u0438\u0442\u0441\u044F \u0432 \u0428\u0432\u0435\u0439\u0446\u0430\u0440\u0438\u0438, \u043E\u043A\u043E\u043B\u043E \u0421\u0435\u043D-\u0413\u043E\u0442\u0430\u0440\u0434\u0441\u043A\u043E\u0433\u043E \u0433\u043E\u0440\u043D\u043E\u0433\u043E \u043C\u0430\u0441\u0441\u0438\u0432\u0430, \u0432 \u043A\u043E\u0442\u043E\u0440\u043E\u0439 \u0431\u044B\u043B \u0432\u043F\u0435\u0440\u0432\u044B\u0435 \u043E\u0431\u043D\u0430\u0440\u0443\u0436\u0435\u043D."@ru . "n\u03B1 = 1.599 - 1.612 n\u03B2 = 1.613 - 1.626 n\u03B3 = 1.625 - 1.637"@en . . "\u0422\u0440\u0435\u043C\u043E\u043B\u0438\u0442 \u2014 \u043B\u0435\u043D\u0442\u043E\u0447\u043D\u044B\u0439 \u0441\u0438\u043B\u0438\u043A\u0430\u0442 \u0433\u0440\u0443\u043F\u043F\u044B \u043C\u043E\u043D\u043E\u043A\u043B\u0438\u043D\u043D\u044B\u0445 \u0430\u043C\u0444\u0438\u0431\u043E\u043B\u043E\u0432. \u041D\u0430\u0437\u0432\u0430\u043D \u043F\u043E , \u043A\u043E\u0442\u043E\u0440\u0430\u044F \u043D\u0430\u0445\u043E\u0434\u0438\u0442\u0441\u044F \u0432 \u0428\u0432\u0435\u0439\u0446\u0430\u0440\u0438\u0438, \u043E\u043A\u043E\u043B\u043E \u0421\u0435\u043D-\u0413\u043E\u0442\u0430\u0440\u0434\u0441\u043A\u043E\u0433\u043E \u0433\u043E\u0440\u043D\u043E\u0433\u043E \u043C\u0430\u0441\u0441\u0438\u0432\u0430, \u0432 \u043A\u043E\u0442\u043E\u0440\u043E\u0439 \u0431\u044B\u043B \u0432\u043F\u0435\u0440\u0432\u044B\u0435 \u043E\u0431\u043D\u0430\u0440\u0443\u0436\u0435\u043D."@ru . . "La tremolita \u00E9s un mineral de la classe dels silicats, a dins de la qual pertany al grup dels amf\u00EDbols. Va ser anomenada l'any 1789 per Johann Georg Albrecht H\u00F6pfner amb el nom del lloc del seu descobriment, la vall de Tremola, als Alps su\u00EFssos."@ca . . "a = 9.84 \u00C5, b = 18.02 \u00C5"@en . . "Tremolita silikatoen taldeko anfibola da, asbesto taldekoa. Bere izena Suitzako haranetik dator non Tremolita meatoki bat dagoen."@eu . "Tr\u00E9molite"@fr . . . "La tr\u00E9molite est une esp\u00E8ce min\u00E9rale du groupe des silicates (sous-groupe des inosilicates, famille des amphiboles), de formule id\u00E9ale Ca2Mg5[Si4O11(OH,F)]2 avec des traces de Ti, Mn, Al, Na, K et Cl. La tr\u00E9molite magn\u00E9sienne pure est blanche, mais les diff\u00E9rentes teneurs en fer vont lui donner des tons de vert. Elle forme une s\u00E9rie avec l'actinote, la (en) et la ."@fr . . "White"@en . . . . "Tremoliet"@nl . "\u900F\u9583\u77F3\uFF08\u3068\u3046\u305B\u3093\u305B\u304D\u3001tremolite\u3001\u30C8\u30EC\u30E2\u30E9\u30A4\u30C8\uFF09\u306F\u9271\u7269\uFF08\u30B1\u30A4\u9178\u5869\u9271\u7269\uFF09\u306E\u4E00\u7A2E\u3067\u3001Ca\u89D2\u9583\u77F3\u306E\u306A\u304B\u307E\u3002 \u5316\u5B66\u7D44\u6210\u306F Ca2(Mg,Fe)5Si8O22(OH)2 (Mg/(Mg+Fe)=1.0-0.9) \u3067\u3001\u9244\uFF08Fe\uFF09\u306E\u5272\u5408\u304C\u591A\u304F\u306A\u308B\u3068\u7DD1\u9583\u77F3\u306B\u306A\u308B\uFF08Mg/(Mg+Fe)=0.5-0.9\uFF09\u3002\u9244\uFF08Fe\uFF09\u304C\u30DE\u30B0\u30CD\u30B7\u30A6\u30E0\uFF08Mg\uFF09\u3088\u308A\u3082\u591A\u304F\u306A\u308B\u3068\u3002 \u5909\u6210\u5CA9\u3092\u69CB\u6210\u3059\u308B\u9020\u5CA9\u9271\u7269\u3002"@ja . "Tremolit (IMA-Symbol Tr) ist ein h\u00E4ufig vorkommendes Mineral aus der Mineralklasse der \u201ESilikate und Germanate\u201C mit der chemischen Zusammensetzung \u2610Ca2(Mg5.0-4.5Fe2+0.0-0.5)Si8O22(OH)2 und damit chemisch gesehen ein komplexes Calcium-Silikat mit zus\u00E4tzlichen Hydroxidionen sowie Magnesium und Eisen mit in gewissen Grenzen variierenden Gehalten. Strukturell geh\u00F6rt Tremolit zu den Kettensilikaten und dort zur Gruppe der Calcium-Amphibole. Tremolit kristallisiert im monoklinen Kristallsystem und entwickelt meist s\u00E4ulige, nadelige und radialstrahlige Kristalle. er findet sich aber auch in Form faseriger bis k\u00F6rniger Mineral-Aggregate. Das Mineral kann je nach Art und Menge von Fremdbeimengungen verschiedene Farben annehmen. Bei 100 % Magnesium erscheint er meist wei\u00DF, bei geringen Beimengungen von Eisen gr\u00FCnlich. Daneben kommen auch graue, braune und rosa bis violette Farbt\u00F6ne vor. Mit steigendem Eisengehalt wird die Farbe immer dunkler. Die Strichfarbe des Minerals ist dagegen immer wei\u00DF. Unverletzte Kristalle sind meist durchsichtig und zeigen einen glas\u00E4hnlichen Glanz auf den Oberfl\u00E4chen. Aggregatformen sind dagegen eher durchscheinend mit einem seiden\u00E4hnlichen Oberfl\u00E4chenschimmer. Tremolit ist das Endglied der Tremolit-Aktinolith--Mischreihe mit variabel austauschbaren Magnesium-Ionen (Tremolit) und Eisen-Ionen (Ferro-Aktinolith)."@de . . . . . "Tremolit"@de . . . "Simple or multiple, common parallel to {100}; rarely parallel to {001}"@en . . . "Transparent to translucent"@en . . . "Het mineraal tremoliet ofwel grijze asbest is een calcium-magnesium-inosilicaat met de chemische formule Ca2Mg5Si8O22(OH)2. Het behoort tot de amfibolen."@nl . "Tremolite"@pt . . . "\u900F\u95EA\u77F3\u4E3A\u89D2\u95EA\u77F3\u7684\u4E00\u7C7B\uFF0C\u4F86\u81EA\u767D\u4E91\u77F3\u548C\u77F3\u82F1\u6DF7\u5408\u6C89\u79EF\u540E\u5F62\u6210\u7684\u53D8\u8D28\u5CA9\u3002\u6676\u4F53\u5E38\u8F90\u5C04\u72B6\u6216\u67F1\u72B6\u6392\u5217\u3002 \u5176\u4E2D\u7684\u9541\u79BB\u5B50\u53EF\u88AB\u88AB\u4E8C\u4EF7\u94C1\u79BB\u5B50\u90E8\u5206\u7F6E\u6362\uFF0C\u5F62\u6210\u4E0E\u9633\u8D77\u77F3\uFF08actinolite\uFF09\u3001\u94C1\u9633\u8D77\u77F3\uFF08ferro-actinolite\uFF09\u7684\u7CFB\u5217\u6DF7\u5408\u77FF\u7269\uFF0C\u540C\u65F6\u989C\u8272\u52A0\u6DF1\uFF0C\u76F4\u81F3\u6DF1\u7EFF\u3002 \u5728\u9AD8\u6E29\u4E0B\u8F6C\u5316\u6210\u900F\u8F89\u77F3\u3001\u65B9\u89E3\u77F3\u3001\u77F3\u69B4\u5B50\u77F3\u3001\u6ED1\u77F3\u548C\u86C7\u7EB9\u77F3\u7B49\u5176\u4ED6\u77FF\u7269\uFF0C\u56E0\u800C\u53EF\u7528\u6765\u5224\u5B9A\u5F62\u6210\u53D8\u8D28\u7684\u6E29\u5EA6\u3002"@zh . . . . . . . . "Perfect on {110} at 56\u00B0 and 124\u00B0; partings on {010} and {100}"@en . "Tremolita"@ca . "Ca2Si8O222"@en . "Tremolit (Hoffner, 1790), chemick\u00FD vzorec Ca2Mg5[OH|Si4O11]2, je jednoklonn\u00FD miner\u00E1l ze skupiny klinoamfibol\u016F."@cs . . . "Tremolite"@en . . "Tremolit \u2013 minera\u0142 z gromady krzemian\u00F3w, z grupy amfiboli. Minera\u0142 pospolity i szeroko rozpowszechniony. Nazwa pochodzi od doliny Tremola w masywie St. Gotthard w Alpach Szwajcarskich, gdzie minera\u0142 ten wyst\u0119puje."@pl . "Tr"@en . "Tremolite is a member of the amphibole group of silicate minerals with composition: Ca2(Mg5.0-4.5Fe2+0.0-0.5)Si8O22(OH)2. Tremolite forms by metamorphism of sediments rich in dolomite and quartz. Tremolite forms a series with actinolite and ferro-actinolite. Pure magnesium tremolite is creamy white, but the color grades to dark green with increasing iron content. It has a hardness on Mohs scale of 5 to 6. Nephrite, one of the two minerals of the gemstone jade, is a green variety of tremolite."@en . . . "Tremolit, \u00E4r ett icke ovanligt hydroxidhaltigt kalcium- och magnesium-silikat. Den \u00E4r en amfibol och upptr\u00E4der ofta som l\u00E5ngsmala kristaller i metamorfa bergarter."@sv . "Tremolite"@en . "Tremolit (IMA-Symbol Tr) ist ein h\u00E4ufig vorkommendes Mineral aus der Mineralklasse der \u201ESilikate und Germanate\u201C mit der chemischen Zusammensetzung \u2610Ca2(Mg5.0-4.5Fe2+0.0-0.5)Si8O22(OH)2 und damit chemisch gesehen ein komplexes Calcium-Silikat mit zus\u00E4tzlichen Hydroxidionen sowie Magnesium und Eisen mit in gewissen Grenzen variierenden Gehalten. Strukturell geh\u00F6rt Tremolit zu den Kettensilikaten und dort zur Gruppe der Calcium-Amphibole. Tremolit ist das Endglied der Tremolit-Aktinolith--Mischreihe mit variabel austauschbaren Magnesium-Ionen (Tremolit) und Eisen-Ionen (Ferro-Aktinolith)."@de . . . . . . . "\u0422\u0440\u0435\u043C\u043E\u043B\u0456\u0442 \u2014 \u043F\u043E\u0440\u043E\u0434\u043E\u0442\u0432\u0456\u0440\u043D\u0438\u0439 \u043C\u0456\u043D\u0435\u0440\u0430\u043B \u043A\u043B\u0430\u0441\u0443 \u0441\u0438\u043B\u0456\u043A\u0430\u0442\u0456\u0432, \u0441\u0456\u043C\u0435\u0439\u0441\u0442\u0432\u0430 \u0430\u043C\u0444\u0456\u0431\u043E\u043B\u0456\u0432. \u041C\u0430\u0433\u043D\u0456\u0457\u0441\u0442\u0438\u0439 \u0440\u0456\u0437\u043D\u043E\u0432\u0438\u0434 \u0430\u043A\u0442\u0438\u043D\u043E\u043B\u0456\u0442\u0443. \u041D\u0435\u0437\u0432\u0438\u0447\u0430\u0439\u043D\u0438\u0439 \u0432\u0438\u0433\u043B\u044F\u0434 \u0434\u0435\u044F\u043A\u0438\u0445 \u0440\u0456\u0437\u043D\u043E\u0432\u0438\u0434\u0456\u0432 \u0442\u0440\u0435\u043C\u043E\u043B\u0456\u0442\u0443 \u0440\u043E\u0431\u0438\u0442\u044C \u0439\u043E\u0433\u043E \u0446\u0456\u043D\u043D\u0438\u043C \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u043E\u043C \u0434\u043B\u044F \u043A\u043E\u043B\u0435\u043A\u0446\u0456\u043E\u043D\u0435\u0440\u0456\u0432. \u0423 \u043D\u0435 \u043C\u0435\u043D\u0448\u043E\u043C\u0443 \u0441\u0442\u0443\u043F\u0435\u043D\u0456 \u043F\u0440\u0438\u0432\u0430\u0431\u043B\u044E\u0454 \u0456 \u0439\u043E\u0433\u043E \u0433\u0430\u0440\u043D\u0435 \u0441\u0432\u0456\u0442\u0456\u043D\u043D\u044F. \u0421\u0432\u043E\u0457\u043C \u0456\u043C'\u044F\u043C \u0442\u0440\u0435\u043C\u043E\u043B\u0456\u0442 \u0437\u043E\u0431\u043E\u0432'\u044F\u0437\u0430\u043D\u0438\u0439 \u043C\u0456\u0441\u0446\u044E \u0437\u043D\u0430\u0445\u043E\u0434\u0436\u0435\u043D\u043D\u044F \u0439\u043E\u0433\u043E \u0437\u0440\u0430\u0437\u043A\u0456\u0432, \u043D\u0430 \u043F\u0456\u0434\u0441\u0442\u0430\u0432\u0456 \u044F\u043A\u0438\u0445 \u0431\u0443\u043B\u043E \u0437\u0440\u043E\u0431\u043B\u0435\u043D\u043E \u043F\u0435\u0440\u0448\u0438\u0439 \u0439\u043E\u0433\u043E \u043E\u043F\u0438\u0441. \u0419\u0434\u0435\u0442\u044C\u0441\u044F \u043F\u0440\u043E \u0434\u043E\u043B\u0438\u043D\u0443 \u0422\u0440\u0435\u043C\u043E\u043B\u0430 \u043F\u043E\u0440\u0443\u0447 \u0437 \u0421\u0435\u043D-\u0413\u043E\u0442\u0430\u0440\u0434\u0441\u044C\u043A\u0438\u043C \u0433\u0456\u0440\u0441\u044C\u043A\u0438\u043C \u043C\u0430\u0441\u0438\u0432\u043E\u043C (\u0428\u0432\u0435\u0439\u0446\u0430\u0440\u0456\u044F). \u041D\u0430\u0437\u0432\u0443 \u0434\u0430\u0432 J.G.H\u00F6pfner, 1790. \u0421\u0438\u043D\u043E\u043D\u0456\u043C\u0438: \u0433\u0440\u0430\u043C\u0430\u0442\u0438\u0442, \u0433\u0435\u043F\u0444\u043D\u0435\u0440\u0438\u0442, \u043A\u0430\u043B\u0430\u043C\u0456\u0442, \u043A\u0430\u0440\u0430\u043C\u0437\u0438\u043D\u0456\u0442, \u043D\u043E\u0440\u0434\u0435\u043D\u0448\u0435\u043B\u044C\u0434\u0438\u0442, \u0440\u0430\u0444\u0456\u043B\u0456\u0442, \u0441\u0435\u0431\u0435\u0441\u0438\u0442."@uk . "Tremolita silikatoen taldeko anfibola da, asbesto taldekoa. Bere izena Suitzako haranetik dator non Tremolita meatoki bat dagoen."@eu . . . . "Tremolit \u2013 minera\u0142 z gromady krzemian\u00F3w, z grupy amfiboli. Minera\u0142 pospolity i szeroko rozpowszechniony. Nazwa pochodzi od doliny Tremola w masywie St. Gotthard w Alpach Szwajcarskich, gdzie minera\u0142 ten wyst\u0119puje."@pl . . . "\u0422\u0440\u0435\u043C\u043E\u043B\u0438\u0442"@ru . "\u900F\u9583\u77F3"@ja . "La tremolita \u00E9s un mineral de la classe dels silicats, a dins de la qual pertany al grup dels amf\u00EDbols. Va ser anomenada l'any 1789 per Johann Georg Albrecht H\u00F6pfner amb el nom del lloc del seu descobriment, la vall de Tremola, als Alps su\u00EFssos."@ca . . . "Tremolit"@pl . . . "\u03B4 = 0.026"@en . "Tremolit"@sv . . . "Het mineraal tremoliet ofwel grijze asbest is een calcium-magnesium-inosilicaat met de chemische formule Ca2Mg5Si8O22(OH)2. Het behoort tot de amfibolen."@nl . "\u900F\u95EA\u77F3"@zh . . . . "La tremolita es un mineral perteneciente al grupo de los silicatos. M\u00E1s concretamente, pertenece a los anf\u00EDboles y al grupo del asbesto. La tremolita fue descubierta por primera vez en en el en el Canton Ticino, Suiza y fue descrita en 1790 por ,\u200B que dio nombre al mineral despu\u00E9s de permanecer en el que hab\u00EDa documentado por error como localidad tipo.\u200B (M\u00E1s tarde (\u00CDndice Mineral de Hey (1993)), se encontr\u00F3 que el mineral tambi\u00E9n en el Val Tremola). El topotipo fue encontrado por Saussure en 1821.\u200B"@es . . . "5"^^ . . . "Tremolit"@cs . . . . "Tremolit, \u00E4r ett icke ovanligt hydroxidhaltigt kalcium- och magnesium-silikat. Den \u00E4r en amfibol och upptr\u00E4der ofta som l\u00E5ngsmala kristaller i metamorfa bergarter."@sv . . . . "\uD22C\uC12C\uC11D"@ko . . . "A tremolita ou tremolite \u00E9 um mineral de silicato de c\u00E1lcio, magn\u00E9sio e ferro, do grupo da anf\u00EDbola, com f\u00F3rmula qu\u00EDmica Ca2Mg5Si8O22(OH)2. \u00C9 usada como isolante e como gema. Descoberta na regi\u00E3o de Tremola, na It\u00E1lia, \u00E9 tamb\u00E9m denominada abcasita, em refer\u00EAncia \u00E0 Abc\u00E1sia (Abkhazia, em portugu\u00EAs), terra dos abc\u00E1sios, na Ge\u00F3rgia, onde igualmente se encontraram dep\u00F3sitos do mineral. A tremolita se forma por metamorfismo de sedimentos ricos em calcita, dolomita e quartzo. Forma uma solu\u00E7\u00E3o s\u00F3lida com a actinolita. A tremolita magnesiana pura \u00E9 branca; com o aumento do teor de ferro, sua cor se aproxima do verde escuro. Possui dureza entre 5 e 6. O nome do mineral deriva da regi\u00E3o de Tremola, na It\u00E1lia, onde foi descoberto. Outro nome dado ao mineral, inclu\u00EDdo no Vocabul\u00E1rio Ortogr\u00E1fico da L\u00EDngua Portuguesa, \u00E9 abcasita, que faz refer\u00EAncia \u00E0 Abc\u00E1sia (Abkhazia, em portugu\u00EAs), terra dos abc\u00E1sios, na Ge\u00F3rgia, onde igualmente se encontraram dep\u00F3sitos do mineral. A tremolita \u00E9 um indicador de m\u00E9dio grau metam\u00F3rfico em rochas calciossilic\u00E1ticas, ou seja, f\u00E1cies anfibolito."@pt . "2.99"^^ . . "La tremolita es un mineral perteneciente al grupo de los silicatos. M\u00E1s concretamente, pertenece a los anf\u00EDboles y al grupo del asbesto. La tremolita fue descubierta por primera vez en en el en el Canton Ticino, Suiza y fue descrita en 1790 por ,\u200B que dio nombre al mineral despu\u00E9s de permanecer en el que hab\u00EDa documentado por error como localidad tipo.\u200B (M\u00E1s tarde (\u00CDndice Mineral de Hey (1993)), se encontr\u00F3 que el mineral tambi\u00E9n en el Val Tremola). El topotipo fue encontrado por Saussure en 1821.\u200B"@es . "C2/m"@en . . . "La tremolite \u00E8 un inosilicato, un anfibolo appartenente al sottogruppo degli anfiboli di calcio, strutturato con una doppia catena di tetraedri (SiO4) i quali condividono tre dei quattro ossigeni.Di genesi metamorfica da parte della dolomite in presenza di silice. Cristallizza nel sistema monoclino, formante un abito di prevalenza prismatico, sovente lanceolato."@it . . "Vitreous and silky"@en . "\uD22C\uC12C\uC11D(\u900F\u9583\u77F3, Tremolite)\uC740 \uAC01\uC12C\uC11D\uC5D0 \uC18D\uD558\uB294 \uADDC\uC0B0\uC5FC \uAD11\uBB3C\uC758 \uC77C\uC885\uC73C\uB85C, \uD654\uD559 \uBD84\uC790\uC2DD\uC740 Ca2(Mg5.0-4.5Fe2+0.0-0.5)Si8O22(OH)2\uC774\uB2E4. \uBC31\uC6B4\uC554\uACFC \uC11D\uC601\uC758 \uCE68\uC804\uBB3C\uC774 \uBCC0\uC131 \uC791\uC6A9\uC744 \uD1B5\uD574 \uC0DD\uC131\uB41C\uB2E4."@ko . . "A tremolita ou tremolite \u00E9 um mineral de silicato de c\u00E1lcio, magn\u00E9sio e ferro, do grupo da anf\u00EDbola, com f\u00F3rmula qu\u00EDmica Ca2Mg5Si8O22(OH)2. \u00C9 usada como isolante e como gema. Descoberta na regi\u00E3o de Tremola, na It\u00E1lia, \u00E9 tamb\u00E9m denominada abcasita, em refer\u00EAncia \u00E0 Abc\u00E1sia (Abkhazia, em portugu\u00EAs), terra dos abc\u00E1sios, na Ge\u00F3rgia, onde igualmente se encontraram dep\u00F3sitos do mineral. A tremolita \u00E9 um indicador de m\u00E9dio grau metam\u00F3rfico em rochas calciossilic\u00E1ticas, ou seja, f\u00E1cies anfibolito."@pt . . . . "\u900F\u9583\u77F3\uFF08\u3068\u3046\u305B\u3093\u305B\u304D\u3001tremolite\u3001\u30C8\u30EC\u30E2\u30E9\u30A4\u30C8\uFF09\u306F\u9271\u7269\uFF08\u30B1\u30A4\u9178\u5869\u9271\u7269\uFF09\u306E\u4E00\u7A2E\u3067\u3001Ca\u89D2\u9583\u77F3\u306E\u306A\u304B\u307E\u3002 \u5316\u5B66\u7D44\u6210\u306F Ca2(Mg,Fe)5Si8O22(OH)2 (Mg/(Mg+Fe)=1.0-0.9) \u3067\u3001\u9244\uFF08Fe\uFF09\u306E\u5272\u5408\u304C\u591A\u304F\u306A\u308B\u3068\u7DD1\u9583\u77F3\u306B\u306A\u308B\uFF08Mg/(Mg+Fe)=0.5-0.9\uFF09\u3002\u9244\uFF08Fe\uFF09\u304C\u30DE\u30B0\u30CD\u30B7\u30A6\u30E0\uFF08Mg\uFF09\u3088\u308A\u3082\u591A\u304F\u306A\u308B\u3068\u3002 \u5909\u6210\u5CA9\u3092\u69CB\u6210\u3059\u308B\u9020\u5CA9\u9271\u7269\u3002"@ja . "\u0422\u0440\u0435\u043C\u043E\u043B\u0456\u0442"@uk . "Biaxial"@en . "c = 5.27 \u00C5; \u03B2 = 104.95\u00B0; Z = 2"@en . . "1123455528"^^ . . "La tr\u00E9molite est une esp\u00E8ce min\u00E9rale du groupe des silicates (sous-groupe des inosilicates, famille des amphiboles), de formule id\u00E9ale Ca2Mg5[Si4O11(OH,F)]2 avec des traces de Ti, Mn, Al, Na, K et Cl. La tr\u00E9molite magn\u00E9sienne pure est blanche, mais les diff\u00E9rentes teneurs en fer vont lui donner des tons de vert. Elle forme une s\u00E9rie avec l'actinote, la (en) et la ."@fr . "Tremolita"@eu . "Tremolita"@es . . . . "Short UV=yellow, Long UV=range pink"@en . . . "9"^^ . . . . . "Elongated prismatic, or flattened crystals; also as fibrous, granular or columnar aggregates"@en . . "1023396"^^ . . . . "Tremolite"@it . . . "Brittle"@en . "5664"^^ . . "Tremolite is a member of the amphibole group of silicate minerals with composition: Ca2(Mg5.0-4.5Fe2+0.0-0.5)Si8O22(OH)2. Tremolite forms by metamorphism of sediments rich in dolomite and quartz. Tremolite forms a series with actinolite and ferro-actinolite. Pure magnesium tremolite is creamy white, but the color grades to dark green with increasing iron content. It has a hardness on Mohs scale of 5 to 6. Nephrite, one of the two minerals of the gemstone jade, is a green variety of tremolite. The fibrous form of tremolite is one of the six recognised types of asbestos. This material is toxic, and inhaling the fibers can lead to asbestosis, lung cancer and both pleural and peritoneal mesothelioma. Fibrous tremolite is sometimes found as a contaminant in vermiculite, chrysotile (itself a type of asbestos) and talc."@en . . "Tremolit (Hoffner, 1790), chemick\u00FD vzorec Ca2Mg5[OH|Si4O11]2, je jednoklonn\u00FD miner\u00E1l ze skupiny klinoamfibol\u016F."@cs . . "Prismatic"@en . "White, gray, lavender to pink, light green, light yellow"@en .