. . . . . . . . . "Pirix\u00E9in\u00ED"@ga . . . . . "Piroksen adalah sebuah kelompok mineral inosilikat yang banyak ditemukan pada batuan beku dan batuan metamorf. Strukturnya terdiri dari rantai tunggal silika tetrahedral dan mengkristal monoklinik dan . Piroksen mempunyai rumus kimia umum XY(Si,Al)2O6 (X adalah kalsium, natrium, besi+2, magnesium dan sedikit seng, mangan, dan litium. Sedangkan Y adalah ion kromium, aluminium, besi+3, magnesium, mangan, skandium, titanium, vanadium dan besi+2)."@in . . . . . "I pirosseni sono dei silicati che costituiscono, insieme agli anfiboli, il gruppo degli inosilicati. La loro formula generale \u00E8 XYZ2O6 e la loro struttura di base \u00E8 costituita da catene singole di tetraedri composti da silicio e ossigeno. Sono componenti fondamentali di molte rocce ignee e metamorfiche: si stima rappresentino circa l'11% in volume dei minerali comuni. L\u2019origine del nome deriva dal greco antico \u03C0\u03C5\u03C1 (pir= fuoco) e \u03BE\u03AD\u03BD\u03BF\u03C2 (Xenos= straniero, estraneo) con il significato di pietra estranea al fuoco. Fu coniato da Ren\u00E9 Just Ha\u00FCy per descrivere dei cristalli verdi che aveva osservato in molte lave, ritenendo che fossero stati inclusi accidentalmente in queste rocce, da qui il nome \"estraneo al fuoco\", cio\u00E8 estraneo alle rocce ignee. I pirosseni si possono formare sia in rocce magmatiche che metamorfiche. I pirosseni metamorfici si possono formare per metamorfismo termico (o di contatto) o per metamorfismo regionale. Nel primo caso cristallizzano in una zona limitata, chiamata aureola di contatto, a basse pressioni e alte temperature; mentre nel secondo caso si formano in profondit\u00E0 ad alte temperature ed elevata pressione di tipo idrostatico."@it . . . . . . . . . . . . . . "Pirokseno estas minerala grupo el silikatmineraloj. La piroksenoj estas gravaj \u015Dtonformi\u011Dantoj kun diversa konsisto. Ili havas la \u011Deneralan formulon X2Si2O6, ofte ri\u0109as je kalcio, magnezio kaj fero. Ili havas la durecon inter 5 kaj 6,5. La plej oftaj piroksenoj apartenas al la enstatit\u2013ferrosilit-serio ([Mg,Fe]SiO3) a\u016D kalcientena diopsid\u2013hedenbergit-serio (Ca[Mg,Fe] Si2O6). La kristalan strukturon de la piroksenoj formas \u0109enoj el SiO4-tetraedroj, kiuj interligi\u011Das per komuna oksigenatomo."@eo . . . . . "Piroksen adalah sebuah kelompok mineral inosilikat yang banyak ditemukan pada batuan beku dan batuan metamorf. Strukturnya terdiri dari rantai tunggal silika tetrahedral dan mengkristal monoklinik dan . Piroksen mempunyai rumus kimia umum XY(Si,Al)2O6 (X adalah kalsium, natrium, besi+2, magnesium dan sedikit seng, mangan, dan litium. Sedangkan Y adalah ion kromium, aluminium, besi+3, magnesium, mangan, skandium, titanium, vanadium dan besi+2)."@in . . . "\u8F1D\u77F3"@ja . "Pirokseno"@eo . . "Pyroxen \u00E4r en samlingsbeteckning f\u00F6r ett antal silikatmineral, som \u00E4r vanligt f\u00F6rekommande i magmatiska och metamorfa bergarter och f\u00F6rekommer till exempel i basalt, diabas och gabbro. Pyroxenerna ing\u00E5r i den st\u00F6rre gruppen eller . Pyroxenerna \u00E4r viktiga bergartsbildande mineral. Den negativa jonen \u00E4r SiO3, som bildar o\u00E4ndliga kedjor i kristallens l\u00E4ngdriktning, vilket ger upphov till den karakt\u00E4ristiska spaltningen i parallellogramform d\u00E4r vinklarna \u00E4r omkring 87\u00B0 och 93\u00B0. Dessa spaltvinklar skiljer dem fr\u00E5n de n\u00E4rbesl\u00E4ktade amfibolerna, vars spaltvinklar \u00E4r cirka 124\u00B0 och 56\u00B0. I flera av pyroxenmineralen avs\u00F6ndras dessutom ofta parallella plattor vinkelr\u00E4tt mot kristallens l\u00E4ngdriktning."@sv . "\u041F\u0456\u0440\u043E\u043A\u0441\u0435\u043D\u0438 (\u0432\u0456\u0434 \u0433\u0440\u0435\u0446. \u03C0\u03B9\u03C1\u03BF\u03C2 \u2014 \u0432\u043E\u0433\u043E\u043D\u044C \u0456 \u0433\u0440\u0435\u0446. \u03BE\u03B5\u03BD\u03BF\u03C2 \u2014 \u0447\u0443\u0436\u0438\u0439) \u2014 \u0433\u0440\u0443\u043F\u0430 \u043F\u043E\u0440\u043E\u0434\u043E\u0442\u0432\u0456\u0440\u043D\u0438\u0445 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432 \u043A\u043B\u0430\u0441\u0443 \u0441\u0438\u043B\u0456\u043A\u0430\u0442\u0456\u0432, \u043F\u0456\u0434\u043A\u043B\u0430\u0441\u0443 \u043B\u0430\u043D\u0446\u044E\u0433\u043E\u0432\u0438\u0445 \u0441\u0438\u043B\u0456\u043A\u0430\u0442\u0456\u0432."@uk . . . . . "\u041F\u0438\u0440\u043E\u043A\u0441\u0435\u043D\u044B"@ru . . . "I pirosseni sono dei silicati che costituiscono, insieme agli anfiboli, il gruppo degli inosilicati. La loro formula generale \u00E8 XYZ2O6 e la loro struttura di base \u00E8 costituita da catene singole di tetraedri composti da silicio e ossigeno. Sono componenti fondamentali di molte rocce ignee e metamorfiche: si stima rappresentino circa l'11% in volume dei minerali comuni."@it . "\u041F\u0438\u0440\u043E\u043A\u0441\u0435\u0301\u043D\u044B \u2014 \u043E\u0431\u0448\u0438\u0440\u043D\u0430\u044F \u0433\u0440\u0443\u043F\u043F\u0430 \u0446\u0435\u043F\u043E\u0447\u0435\u0447\u043D\u044B\u0445 \u0441\u0438\u043B\u0438\u043A\u0430\u0442\u043E\u0432. \u041C\u043D\u043E\u0433\u0438\u0435 \u043F\u0438\u0440\u043E\u043A\u0441\u0435\u043D\u044B \u2014 \u043F\u043E\u0440\u043E\u0434\u043E\u043E\u0431\u0440\u0430\u0437\u0443\u044E\u0449\u0438\u0435 \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u044B."@ru . . "Pyroxeny jsou skupinou miner\u00E1l\u016F z odd\u011Blen\u00ED , kter\u00E9 jsou tvo\u0159eny tetraedry SiO4 spojen\u00FDmi do lini\u00ED. Pyroxeny jsou a je pro n\u011B charakteristick\u00E1 t\u00E9m\u011B\u0159 dokonal\u00E1 \u0161t\u011Bpnost podle hranolu v \u00FAhlu 87,5\u00B0, \u010Deho\u017E se vyu\u017E\u00EDv\u00E1 p\u0159i makroskopick\u00E9m i mikroskopick\u00E9m pozn\u00E1v\u00E1n\u00ED hornin. Pyroxeny jsou d\u016Fle\u017Eit\u00E9 horninotvorn\u00E9 nerosty, p\u0159edev\u0161\u00EDm ve vyv\u0159el\u00FDch hornin\u00E1ch, jsou tak\u00E9 v a vznikl\u00FDch metamorfn\u00EDmi pochody. Pyroxeny jsou tvo\u0159eny jednoduch\u00FDmi \u0159et\u011Bzci tetraedr\u016F. Obecn\u00FD vzorec pyroxen\u016F je n\u00E1sleduj\u00EDc\u00ED: ABSi2O6 A = Ca, Fe2+, Li, Mg, Na.B = Al, Cr3+, Fe2+, Fe3+, Mg, Mn2+."@cs . . . "Pirokseny"@pl . . "Pyroxene triangle nomenclature of the sodium pyroxenes"@en . "\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646"@ar . "\u041F\u0456\u0440\u043E\u043A\u0441\u0435\u043D\u0438"@uk . . . "\uD718\uC11D(\u8F1D\u77F3, pyroxene)\uC740 \uC870\uC554\uAD11\uBB3C\uC758 \uD558\uB098\uB85C \uD654\uC131\uC554\uACFC \uBCC0\uC131\uC554\uC5D0\uC11C \uD3ED\uB113\uAC8C \uB098\uD0C0\uB09C\uB2E4. \uD718\uC11D\uC740 \uADDC\uC0B0\uC5FC \uC0AC\uBA74\uCCB4\uC758 \uB2E8\uC77C\uC0AC\uC2AC \uAD6C\uC870\uB85C \uC774\uB8E8\uC5B4\uC838 \uC788\uACE0, \uB2E8\uC0AC\uC815\uACC4 \uB610\uB294 \uC0AC\uBC29\uC815\uACC4\uC774\uB2E4. \uD718\uC11D\uC758 \uD654\uD559\uC2DD\uC740 \uC77C\uBC18\uC801\uC73C\uB85C XY(Si,Al)2O6\uB85C \uB098\uD0C0\uB0BC \uC218 \uC788\uB2E4. \uC5EC\uAE30\uC5D0\uC11C X\uB294 \uCE7C\uC298, \uC18C\uB4D0, 2\uAC00 \uCCA0, \uB9C8\uADF8\uB124\uC298\uC774 \uB418\uB294 \uACBD\uC6B0\uAC00 \uB9CE\uC73C\uB098 \uB4DC\uBB3C\uAC8C \uC544\uC5F0, \uB9DD\uAC04, \uB9AC\uD2AC\uC774 \uCE58\uD658\uB418\uAE30\uB3C4 \uD55C\uB2E4. Y\uB294 \uC774\uBCF4\uB2E4 \uC774\uC628\uC758 \uD06C\uAE30\uAC00 \uC791\uC740 \uD06C\uB85C\uBBB4\uC774\uB098 \uC54C\uB8E8\uBBF8\uB284, 3\uAC00 \uCCA0, \uB9C8\uADF8\uB124\uC298, \uB9DD\uAC04, \uC2A4\uCE78\uB4D0, \uD2F0\uD0C0\uB284, \uBC14\uB098\uB4D0 \uB4F1\uC758 \uC774\uC628\uC774 \uB4E4\uC5B4\uAC08 \uC218 \uC788\uB2E4. \uC54C\uB8E8\uBBF8\uB284\uC740 \uADDC\uC18C\uB97C \uCE58\uD658\uD558\uB294 \uC77C\uC774 \uB9CE\uC73C\uB098 \uD718\uC11D\uC5D0\uC11C\uB294 \uC774\uB7F0 \uACBD\uC6B0\uAC00 \uC0C1\uB2F9\uD788 \uC81C\uD55C\uC801\uC774\uB2E4. \uC9C0\uAD6C\uC758 \uC0C1\uBD80 \uB9E8\uD2C0\uC740 \uC8FC\uB85C \uAC10\uB78C\uC11D\uACFC \uD718\uC11D\uC73C\uB85C \uB418\uC5B4\uC788\uB2E4."@ko . . . . . . . "111194"^^ . "\u8F89\u77F3"@zh . . . . . . . . . "Pyroxene quadrilateral nomenclature of the calcium, magnesium, iron pyroxenes"@en . . "Gr\u00FApa m\u00F3r mianra\u00ED sileac\u00E1ite a chuims\u00EDonn cuid mhaith mianra\u00ED a foirm\u00EDodh ag carraig. Cos\u00FAil le hamfab\u00F3il, ach le strucht\u00FAr aonslabhra teitrih\u00E9adr\u00E1in sileac\u00E1ite, gan na hiain hiodrocsaile. Baill shuntasacha den ghr\u00FApa is ea eanstait\u00EDt, dia-opsa\u00EDd, pidseoin\u00EDt is s\u00E9id\u00EDt. I l\u00E1thair i gcarraigeacha doigheartha is meiteamorfacha."@ga . . "\uD718\uC11D"@ko . . "Pirox\u00E8"@ca . . . "Als Pyroxengruppe bezeichnet man eine Gruppe von Mineralen aus der Abteilung der Kettensilikate. Ihre Kristallstruktur zeichnet sich durch Einfachketten aus eckenverkn\u00FCpften SiO4-Tetraedern aus und ihre Zusammensetzung gen\u00FCgt der folgenden verallgemeinerten Summenformel: M1 M2 T2O6. In dieser Strukturformel repr\u00E4sentieren M1, M2 und T unterschiedliche Positionen in der Pyroxenstruktur. Sie werden vorwiegend durch folgende Kationen belegt: \n* M1: Mg2+, Fe2+, Mn2+, Al3+, Fe3+, Ti4+, Ti3+, V3+, Sc3+, Cr3+, Zr4+, Zn2+, \n* M2: Mg2+, Fe2+, Mn2+, Ca2+, Na+, Li+ \n* T: Si4+, Al3+, Fe3+"@de . "Piroxena"@pt . . "\u041F\u0456\u0440\u043E\u043A\u0441\u0435\u043D\u0438 (\u0432\u0456\u0434 \u0433\u0440\u0435\u0446. \u03C0\u03B9\u03C1\u03BF\u03C2 \u2014 \u0432\u043E\u0433\u043E\u043D\u044C \u0456 \u0433\u0440\u0435\u0446. \u03BE\u03B5\u03BD\u03BF\u03C2 \u2014 \u0447\u0443\u0436\u0438\u0439) \u2014 \u0433\u0440\u0443\u043F\u0430 \u043F\u043E\u0440\u043E\u0434\u043E\u0442\u0432\u0456\u0440\u043D\u0438\u0445 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432 \u043A\u043B\u0430\u0441\u0443 \u0441\u0438\u043B\u0456\u043A\u0430\u0442\u0456\u0432, \u043F\u0456\u0434\u043A\u043B\u0430\u0441\u0443 \u043B\u0430\u043D\u0446\u044E\u0433\u043E\u0432\u0438\u0445 \u0441\u0438\u043B\u0456\u043A\u0430\u0442\u0456\u0432."@uk . . . . . . . "13431"^^ . . . . . . "The pyroxenes (commonly abbreviated to Px) are a group of important rock-forming inosilicate minerals found in many igneous and metamorphic rocks. Pyroxenes have the general formula XY(Si,Al)2O6, where X represents calcium (Ca), sodium (Na), iron (Fe II) or magnesium (Mg) and more rarely zinc, manganese or lithium, and Y represents ions of smaller size, such as chromium (Cr), aluminium (Al), magnesium (Mg), cobalt (Co), manganese (Mn), scandium (Sc), titanium (Ti), vanadium (V) or even iron (Fe II) or (Fe III). Although aluminium substitutes extensively for silicon in silicates such as feldspars and amphiboles, the substitution occurs only to a limited extent in most pyroxenes. They share a common structure consisting of single chains of silica tetrahedra. Pyroxenes that crystallize in the monoclinic system are known as clinopyroxenes and those that crystallize in the orthorhombic system are known as orthopyroxenes. The name pyroxene is derived from the Ancient Greek words for 'fire' (pyr \u03C0\u03C5\u03C1) and 'stranger' (ks\u00E9nos \u03BE\u03AD\u03BD\u03BF\u03C2). Pyroxenes were so named because of their presence in volcanic lavas, where they are sometimes found as crystals embedded in volcanic glass; it was assumed they were impurities in the glass, hence the name meaning 'fire-strangers'. However, they are simply early-forming minerals that crystallized before the lava erupted. The upper mantle of Earth is composed mainly of olivine and pyroxene minerals. Pyroxene and feldspar are the major minerals in basalt, andesite, and gabbro rocks."@en . . . . "\u041F\u0438\u0440\u043E\u043A\u0441\u0435\u0301\u043D\u044B \u2014 \u043E\u0431\u0448\u0438\u0440\u043D\u0430\u044F \u0433\u0440\u0443\u043F\u043F\u0430 \u0446\u0435\u043F\u043E\u0447\u0435\u0447\u043D\u044B\u0445 \u0441\u0438\u043B\u0438\u043A\u0430\u0442\u043E\u0432. \u041C\u043D\u043E\u0433\u0438\u0435 \u043F\u0438\u0440\u043E\u043A\u0441\u0435\u043D\u044B \u2014 \u043F\u043E\u0440\u043E\u0434\u043E\u043E\u0431\u0440\u0430\u0437\u0443\u044E\u0449\u0438\u0435 \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u044B."@ru . . . . . "\u0627\u0644\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646 (pyroxene) \u0647\u0648 \u0623\u062D\u062F \u0627\u0644\u0645\u0639\u0627\u062F\u0646 \u0627\u0644\u0634\u0627\u0626\u0639\u0629 \u0641\u064A \u0627\u0644\u0642\u0634\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0648\u064A\u0648\u062C\u062F \u0641\u064A \u0643\u062B\u064A\u0631 \u0645\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0646\u0627\u0631\u064A\u0629 \u0648\u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0645\u062A\u062D\u0648\u0644\u0629 \u0627\u0644\u0645\u0643\u0648\u0646\u0629 \u0645\u0646 \u0633\u064A\u0644\u064A\u0643\u0627. \u0648\u0627\u0644\u062A\u0631\u0643\u064A\u0628 \u0627\u0644\u0643\u064A\u0645\u064A\u0627\u0626\u064A \u0644\u0644\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646 \u0647\u0648 : XY(Si,Al)2O6 \u062D\u064A\u062B X \u062A\u0639\u0646\u064A \u0627\u0644\u0643\u0627\u0644\u0633\u064A\u0648\u0645 \u0623\u0648 \u0627\u0644\u0635\u0648\u062F\u064A\u0648\u0645 \u0623\u0648 \u0627\u0644\u062D\u062F\u064A\u062F +2 \u0623\u0648 \u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645 \u0648\u064A\u0646\u062F\u0631 \u0641\u064A\u0647\u0627 \u0648\u062C\u0648\u062F \u0627\u0644\u0632\u0646\u0643 \u0648\u0627\u0644\u0645\u0646\u062C\u0646\u064A\u0632 \u0648\u0627\u0644\u0644\u064A\u062B\u064A\u0648\u0645. \u0648\u062A\u0639\u0646\u064A Y \u0623\u064A\u0648\u0646\u0627\u062A \u0623\u0635\u063A\u0631 \u062D\u062C\u0645\u0627 \u0645\u062B\u0644 \u0627\u0644\u0643\u0631\u0648\u0645 \u0648\u0627\u0644\u0623\u0644\u0645\u0648\u0646\u064A\u0648\u0645 \u0648\u0627\u0644\u062D\u062F\u064A\u062F+3 \u0648\u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645. \u0648\u0631\u063A\u0645 \u0627\u0633\u062A\u0628\u062F\u0627\u0644 \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0648\u0646 \u0628\u0627\u0644\u0623\u0644\u0645\u0648\u0646\u064A\u0648\u0645 \u0641\u064A \u062A\u0644\u0643 \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0627\u062A \u0645\u062B\u0644\u0645\u0627 \u0641\u064A \u0627\u0644\u0641\u0644\u062F\u0633\u0628\u0627\u0631 \u0625\u0644\u0627 \u0623\u0646 \u0630\u0644\u0643 \u0627\u0644\u0627\u0633\u062A\u0628\u062F\u0627\u0644 \u064A\u0642\u0639 \u0641\u064A \u062D\u062F\u0648\u062F \u0628\u0633\u064A\u0637\u0629 \u0641\u0642\u0637 \u0641\u064A \u0627\u0644\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646. \u0648\u064A\u0648\u062C\u062F \u0627\u0644\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646 \u0641\u064A \u062D\u0645\u0645 \u0627\u0644\u0628\u0631\u0627\u0643\u064A\u0646\u060C \u0648\u064A\u0648\u062C\u062F \u0623\u062D\u064A\u0627\u0646\u0627 \u0645\u062A\u0628\u0644\u0648\u0631\u0627 \u0641\u064A \u0632\u062C\u0627\u062C \u0627\u0644\u0628\u0631\u0627\u0643\u064A\u0646. \u0648\u062A\u062A\u0643\u0648\u0646 \u0628\u0644\u0648\u0631\u0627\u062A\u0647 \u062D\u062A\u0649 \u0642\u0628\u0644 \u0623\u0646 \u064A\u0634\u062A\u062F \u0627\u0644\u0646\u0634\u0627\u0637 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A \u0648\u062A\u0633\u064A\u0644 \u0627\u0644\u062D\u0645\u0645. \u064A\u062A\u0643\u0648\u0646 \u0627\u0644\u062C\u0632\u0621 \u0627\u0644\u0639\u0644\u0648\u064A \u0645\u0646 \u0627\u0644\u063A\u0644\u0627\u0641 \u0627\u0644\u0623\u0631\u0636\u064A \u0645\u0646 \u0627\u0644\u0645\u0639\u062F\u0646\u064A\u0646 \u0627\u0644\u0631\u0626\u064A\u0633\u064A\u064A\u0646 \u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 \u0648\u0627\u0644\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646. \u0648\u062A\u0628\u064A\u0646 \u0627\u0644\u0639\u064A\u0646\u0629 \u0641\u064A \u0627\u0644\u0635\u0648\u0631\u0629 \u0648\u062C\u0648\u062F \u0627\u0644\u0623\u0631\u062B\u0648\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646 \u0627\u0644\u0623\u0633\u0648\u062F \u0648\u0627\u0644\u062F\u064A\u0648\u0628\u0633\u064A\u062F \u0627\u0644\u0645\u062D\u062A\u0648\u064A \u0639\u0644\u0649 \u0627\u0644\u0643\u0631\u0648\u0645 \u0648\u0644\u0648\u0646\u0647 \u0623\u062E\u0636\u0631 \u0641\u0627\u062A\u062D \u0648\u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 (\u0623\u062E\u0636\u0631 \u0645\u0635\u0641\u0631)\u060C \u0648\u064A\u063A\u0644\u0628 \u0641\u064A \u0627\u0644\u0639\u064A\u0646\u0629 \u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646. \u0648\u064A\u063A\u0644\u0628 \u0648\u062C\u0648\u062F \u0627\u0644\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646 \u0648\u0627\u0644\u0641\u0644\u062F\u0633\u0628\u0627\u0631 \u0641\u064A \u0627\u0644\u0628\u0627\u0632\u0644\u062A. \u062A\u062A\u0645\u064A\u0632 \u0645\u0639\u0627\u062F\u0646 \u0627\u0644\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646 \u0628\u062E\u0648\u0627\u0635 \u0643\u064A\u0645\u064A\u0627\u0626\u064A\u0629 \u0645\u062A\u0628\u0627\u064A\u0646\u0629 \u0648\u0647\u064A \u062A\u0648\u062C\u062F \u0641\u064A \u0643\u062B\u064A\u0631 \u0645\u0646 \u0627\u0644\u0637\u0628\u0642\u0627\u062A \u0627\u0644\u062C\u064A\u0648\u0644\u0648\u062C\u064A\u0629. \u0648\u0647\u064A \u062C\u0632\u0621 \u0647\u0627\u0645 \u0641\u064A \u062A\u0643\u0648\u064A\u0646 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0623\u0648 \u0641\u064A \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0645\u062A\u062D\u0648\u0644\u0629. \u0648\u064A\u062A\u0645\u064A\u0632 \u0627\u0644\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646 \u0628\u0635\u0644\u0627\u062F\u0629 \u0628\u064A\u0646 5 \u0648 5\u06486."@ar . . "Gr\u00FApa m\u00F3r mianra\u00ED sileac\u00E1ite a chuims\u00EDonn cuid mhaith mianra\u00ED a foirm\u00EDodh ag carraig. Cos\u00FAil le hamfab\u00F3il, ach le strucht\u00FAr aonslabhra teitrih\u00E9adr\u00E1in sileac\u00E1ite, gan na hiain hiodrocsaile. Baill shuntasacha den ghr\u00FApa is ea eanstait\u00EDt, dia-opsa\u00EDd, pidseoin\u00EDt is s\u00E9id\u00EDt. I l\u00E1thair i gcarraigeacha doigheartha is meiteamorfacha."@ga . "De groep mineralen die pyroxenen genoemd worden, is een groep belangrijke silicaten in magmatische en metamorfe gesteenten . Karakteristiek is een structuur van enkele silica ketens in tetra\u00EBders; inosilicaat. Twee kristalstelsels zijn mogelijk: \n* monoklien \n* orthorombisch"@nl . . "Pyroxene nomenclature"@en . . . . . . . . "Pyrox\u00E8ne"@fr . "Piroxeno"@eu . . . . "\u0627\u0644\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646 (pyroxene) \u0647\u0648 \u0623\u062D\u062F \u0627\u0644\u0645\u0639\u0627\u062F\u0646 \u0627\u0644\u0634\u0627\u0626\u0639\u0629 \u0641\u064A \u0627\u0644\u0642\u0634\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0648\u064A\u0648\u062C\u062F \u0641\u064A \u0643\u062B\u064A\u0631 \u0645\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0646\u0627\u0631\u064A\u0629 \u0648\u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0645\u062A\u062D\u0648\u0644\u0629 \u0627\u0644\u0645\u0643\u0648\u0646\u0629 \u0645\u0646 \u0633\u064A\u0644\u064A\u0643\u0627. \u0648\u0627\u0644\u062A\u0631\u0643\u064A\u0628 \u0627\u0644\u0643\u064A\u0645\u064A\u0627\u0626\u064A \u0644\u0644\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646 \u0647\u0648 : XY(Si,Al)2O6 \u062D\u064A\u062B X \u062A\u0639\u0646\u064A \u0627\u0644\u0643\u0627\u0644\u0633\u064A\u0648\u0645 \u0623\u0648 \u0627\u0644\u0635\u0648\u062F\u064A\u0648\u0645 \u0623\u0648 \u0627\u0644\u062D\u062F\u064A\u062F +2 \u0623\u0648 \u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645 \u0648\u064A\u0646\u062F\u0631 \u0641\u064A\u0647\u0627 \u0648\u062C\u0648\u062F \u0627\u0644\u0632\u0646\u0643 \u0648\u0627\u0644\u0645\u0646\u062C\u0646\u064A\u0632 \u0648\u0627\u0644\u0644\u064A\u062B\u064A\u0648\u0645. \u0648\u062A\u0639\u0646\u064A Y \u0623\u064A\u0648\u0646\u0627\u062A \u0623\u0635\u063A\u0631 \u062D\u062C\u0645\u0627 \u0645\u062B\u0644 \u0627\u0644\u0643\u0631\u0648\u0645 \u0648\u0627\u0644\u0623\u0644\u0645\u0648\u0646\u064A\u0648\u0645 \u0648\u0627\u0644\u062D\u062F\u064A\u062F+3 \u0648\u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645. \u0648\u0631\u063A\u0645 \u0627\u0633\u062A\u0628\u062F\u0627\u0644 \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0648\u0646 \u0628\u0627\u0644\u0623\u0644\u0645\u0648\u0646\u064A\u0648\u0645 \u0641\u064A \u062A\u0644\u0643 \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0627\u062A \u0645\u062B\u0644\u0645\u0627 \u0641\u064A \u0627\u0644\u0641\u0644\u062F\u0633\u0628\u0627\u0631 \u0625\u0644\u0627 \u0623\u0646 \u0630\u0644\u0643 \u0627\u0644\u0627\u0633\u062A\u0628\u062F\u0627\u0644 \u064A\u0642\u0639 \u0641\u064A \u062D\u062F\u0648\u062F \u0628\u0633\u064A\u0637\u0629 \u0641\u0642\u0637 \u0641\u064A \u0627\u0644\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646. \u0648\u064A\u062A\u0645\u064A\u0632 \u0627\u0644\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646 \u0628\u0635\u0644\u0627\u062F\u0629 \u0628\u064A\u0646 5 \u0648 5\u06486."@ar . . "Pyroxengruppe"@de . "As piroxenas (portugu\u00EAs europeu) ou pirox\u00EAnios (portugu\u00EAs brasileiro) s\u00E3o um importante grupo de 21 inossilicatos de cadeia simples encontrados em m\u00FAltiplas rochas \u00EDgneas e metam\u00F3rficas, em muitas das quais constituem o grupo mineral dominante."@pt . . "Les pyrox\u00E8nes (du grec \u03C0\u03C5\u03C1 (feu) et \u03BE\u03B5\u03BD\u03BF\u03C2 (\u00E9tranger) : \u00AB \u00E9tranger au feu \u00BB) sont une famille de min\u00E9raux du groupe des inosilicates. Ce sont des composants courants des roches magmatiques et m\u00E9tamorphiques. Ils sont apparent\u00E9s aux amphiboles, dont ils se distinguent notamment par leur caract\u00E8re anhydre (absence de groupes OH) et leurs directions de clivage. Les pyrox\u00E8nes appartiennent en g\u00E9n\u00E9ral au syst\u00E8me monoclinique (clinopyrox\u00E8ne), parfois orthorhombique (orthopyrox\u00E8ne), avec une forme cristalline en prismes trapus, caract\u00E9ris\u00E9s par deux clivages pratiquement orthogonaux (93\u00B0 ou 87\u00B0)."@fr . "Piroxeno"@es . "The pyroxenes (commonly abbreviated to Px) are a group of important rock-forming inosilicate minerals found in many igneous and metamorphic rocks. Pyroxenes have the general formula XY(Si,Al)2O6, where X represents calcium (Ca), sodium (Na), iron (Fe II) or magnesium (Mg) and more rarely zinc, manganese or lithium, and Y represents ions of smaller size, such as chromium (Cr), aluminium (Al), magnesium (Mg), cobalt (Co), manganese (Mn), scandium (Sc), titanium (Ti), vanadium (V) or even iron (Fe II) or (Fe III). Although aluminium substitutes extensively for silicon in silicates such as feldspars and amphiboles, the substitution occurs only to a limited extent in most pyroxenes. They share a common structure consisting of single chains of silica tetrahedra. Pyroxenes that crystallize in the"@en . . . "As piroxenas (portugu\u00EAs europeu) ou pirox\u00EAnios (portugu\u00EAs brasileiro) s\u00E3o um importante grupo de 21 inossilicatos de cadeia simples encontrados em m\u00FAltiplas rochas \u00EDgneas e metam\u00F3rficas, em muitas das quais constituem o grupo mineral dominante."@pt . . "1115529924"^^ . . . "Pirokseny \u2013 grupa bardzo rozpowszechnionych minera\u0142\u00F3w ska\u0142otw\u00F3rczych o strukturze wewn\u0119trznej odpowiadaj\u0105cej krzemianom \u0142a\u0144cuchowym i og\u00F3lnym wzorze: AB[Si2O6]gdzie:A to najcz\u0119\u015Bciej wap\u0144, s\u00F3d, lit;B to najcz\u0119\u015Bciej magnez, \u017Celazo, glin. Pirokseny stanowi\u0105 cz\u0119sty sk\u0142adnik ska\u0142 magmowych i metamorficznych, a najwi\u0119ksz\u0105 rol\u0119 ska\u0142otw\u00F3rcz\u0105 odgrywa augit. Spotykane s\u0105 w ska\u0142ach na ca\u0142ym \u015Bwiecie.Nazw\u0119 wprowadzi\u0142 Ren\u00E9-Just Ha\u00FCy od s\u0142\u00F3w greckich pyr = ogie\u0144 i xenos = obcy. Uwa\u017Ca\u0142 bowiem, \u017Ce pirokseny nie tworz\u0105 si\u0119 w chwili erupcji, lecz p\u00F3\u017Aniej."@pl . . . "Les pyrox\u00E8nes (du grec \u03C0\u03C5\u03C1 (feu) et \u03BE\u03B5\u03BD\u03BF\u03C2 (\u00E9tranger) : \u00AB \u00E9tranger au feu \u00BB) sont une famille de min\u00E9raux du groupe des inosilicates. Ce sont des composants courants des roches magmatiques et m\u00E9tamorphiques. Ils sont apparent\u00E9s aux amphiboles, dont ils se distinguent notamment par leur caract\u00E8re anhydre (absence de groupes OH) et leurs directions de clivage. La structure des pyrox\u00E8nes est celle des plus simples inosilicates, c'est-\u00E0-dire un assemblage de cha\u00EEnes simples de complexes t\u00E9tra\u00E9driques SiO4. De ce fait, le rapport Si/O vaut 1/3, avec une p\u00E9riode de cha\u00EEne de (SiO3)n. La formule g\u00E9n\u00E9rale d'un pyrox\u00E8ne est par cons\u00E9quent XY(SiO3)2, o\u00F9 X est un gros cation (Na+, Ca2+, Li+, Mg2+, Fe2+, Mn2+...) et Y un cation de taille moyenne (Mg2+, Fe2+, Mn2+, Fe3+, Al3+, Cr3+, Ti4+...) Les pyrox\u00E8nes appartiennent en g\u00E9n\u00E9ral au syst\u00E8me monoclinique (clinopyrox\u00E8ne), parfois orthorhombique (orthopyrox\u00E8ne), avec une forme cristalline en prismes trapus, caract\u00E9ris\u00E9s par deux clivages pratiquement orthogonaux (93\u00B0 ou 87\u00B0)."@fr . "Pirokseno estas minerala grupo el silikatmineraloj. La piroksenoj estas gravaj \u015Dtonformi\u011Dantoj kun diversa konsisto. Ili havas la \u011Deneralan formulon X2Si2O6, ofte ri\u0109as je kalcio, magnezio kaj fero. Ili havas la durecon inter 5 kaj 6,5. La plej oftaj piroksenoj apartenas al la enstatit\u2013ferrosilit-serio ([Mg,Fe]SiO3) a\u016D kalcientena diopsid\u2013hedenbergit-serio (Ca[Mg,Fe] Si2O6). La kristalan strukturon de la piroksenoj formas \u0109enoj el SiO4-tetraedroj, kiuj interligi\u011Das per komuna oksigenatomo."@eo . . . . . . . . . "\u8F89\u77F3\u662F\u4E00\u79CD\u91CD\u8981\u7684\u7845\u9178\u76D0\u77FF\u7269\uFF0C\u662F\u8F89\u77F3\u7C7B\u77FF\u7269\u7684\u603B\u79F0\uFF0C\u5E38\u5728\u706B\u6210\u5CA9\u548C\u53D8\u8D28\u5CA9\u4E2D\u88AB\u53D1\u73B0\u3002\u6839\u636E\u6676\u4F53\u7ED3\u6784\u7684\u4E0D\u540C\uFF0C\u8F89\u77F3\u53EF\u88AB\u5206\u4E3A\u5355\u659C\u8F89\u77F3\u548C\u659C\u65B9\u8F89\u77F3\u4E24\u4E2A\u4E9A\u65CF\uFF0C\u524D\u8005\u5C5E\u4E8E\u5355\u659C\u6676\u7CFB\uFF0C\u540E\u8005\u5C5E\u4E8E\u659C\u65B9\u6676\u7CFB\u3002\u8F89\u77F3\u7C7B\u77FF\u7269\u7684\u5171\u540C\u7279\u70B9\u662F\u5176\u6676\u4F53\u4E2D\u542B\u6709\u5F62\u6210\u7684\u5355\u94FE\u7ED3\u6784\u3002"@zh . "Pyroxeny"@cs . . . . "Pirosseno"@it . . "\u8F89\u77F3\u662F\u4E00\u79CD\u91CD\u8981\u7684\u7845\u9178\u76D0\u77FF\u7269\uFF0C\u662F\u8F89\u77F3\u7C7B\u77FF\u7269\u7684\u603B\u79F0\uFF0C\u5E38\u5728\u706B\u6210\u5CA9\u548C\u53D8\u8D28\u5CA9\u4E2D\u88AB\u53D1\u73B0\u3002\u6839\u636E\u6676\u4F53\u7ED3\u6784\u7684\u4E0D\u540C\uFF0C\u8F89\u77F3\u53EF\u88AB\u5206\u4E3A\u5355\u659C\u8F89\u77F3\u548C\u659C\u65B9\u8F89\u77F3\u4E24\u4E2A\u4E9A\u65CF\uFF0C\u524D\u8005\u5C5E\u4E8E\u5355\u659C\u6676\u7CFB\uFF0C\u540E\u8005\u5C5E\u4E8E\u659C\u65B9\u6676\u7CFB\u3002\u8F89\u77F3\u7C7B\u77FF\u7269\u7684\u5171\u540C\u7279\u70B9\u662F\u5176\u6676\u4F53\u4E2D\u542B\u6709\u5F62\u6210\u7684\u5355\u94FE\u7ED3\u6784\u3002"@zh . . . "Pyroxeny jsou skupinou miner\u00E1l\u016F z odd\u011Blen\u00ED , kter\u00E9 jsou tvo\u0159eny tetraedry SiO4 spojen\u00FDmi do lini\u00ED. Pyroxeny jsou a je pro n\u011B charakteristick\u00E1 t\u00E9m\u011B\u0159 dokonal\u00E1 \u0161t\u011Bpnost podle hranolu v \u00FAhlu 87,5\u00B0, \u010Deho\u017E se vyu\u017E\u00EDv\u00E1 p\u0159i makroskopick\u00E9m i mikroskopick\u00E9m pozn\u00E1v\u00E1n\u00ED hornin. Pyroxeny jsou d\u016Fle\u017Eit\u00E9 horninotvorn\u00E9 nerosty, p\u0159edev\u0161\u00EDm ve vyv\u0159el\u00FDch hornin\u00E1ch, jsou tak\u00E9 v a vznikl\u00FDch metamorfn\u00EDmi pochody. Pyroxeny jsou tvo\u0159eny jednoduch\u00FDmi \u0159et\u011Bzci tetraedr\u016F. Obecn\u00FD vzorec pyroxen\u016F je n\u00E1sleduj\u00EDc\u00ED: ABSi2O6 A = Ca, Fe2+, Li, Mg, Na.B = Al, Cr3+, Fe2+, Fe3+, Mg, Mn2+."@cs . . . "De groep mineralen die pyroxenen genoemd worden, is een groep belangrijke silicaten in magmatische en metamorfe gesteenten . Karakteristiek is een structuur van enkele silica ketens in tetra\u00EBders; inosilicaat. Twee kristalstelsels zijn mogelijk: \n* monoklien \n* orthorombisch"@nl . . "Los piroxenos son un importante grupo de silicatos que forman parte de muchas rocas \u00EDgneas y metam\u00F3rficas.\u200B Su nombre proviene de las palabras \"piro\" y \"xeno\" del griego antiguo que significan \"fuego\" y \"extra\u00F1o\".\u200B Este nombre se lo dio Ren\u00E9 Just Ha\u00FCy debido a que este consideraba su ocurrencia en lavas como algo ajeno.\u200B"@es . "\u8F1D\u77F3\uFF08\u304D\u305B\u304D\u3001pyroxene\u3001\u30D1\u30A4\u30ED\u30AD\u30B7\u30F3\uFF09\u306F\u3001\u30B1\u30A4\u9178\u5869\u9271\u7269\u306E\u4E00\u7A2E\u3002\u591A\u304F\u306E\u706B\u6210\u5CA9\u3084\u5909\u6210\u5CA9\u306B\u542B\u307E\u308C\u308B\u4EE3\u8868\u7684\u306A\u9020\u5CA9\u9271\u7269\u3002 \u8272\u306F\u7121\u8272\u30FB\u7DD1\u8272\u30FB\u8910\u8272\u30FB\u9ED2\u8272\u306A\u3069\u3067\u3001\u30AC\u30E9\u30B9\u5149\u6CA2\u3092\u6301\u3064\u3002\u81EA\u5F62\u7D50\u6676\u306F\u77ED\u67F1\u72B6\u3002\u4E8C\u65B9\u5411\u306E\u5288\u958B\u304C\u9855\u8457\u3002\u89D2\u9583\u77F3\u306B\u3088\u304F\u4F3C\u308B\u304C\u3001\u5288\u958B\u306E\u4EA4\u308F\u308B\u89D2\u5EA6\uFF08\u7D0490\u00B0\uFF09\u306B\u3088\u308A\u533A\u5225\u3055\u308C\u308B\u3002 \u57FA\u672C\u7684\u306A\u5316\u5B66\u7D44\u6210\u306F XY(Si,Al)2O6 \uFF08\u305F\u3060\u3057\u3001X \u306FCa\u3001Na\u3001Fe2+\u3001Zn\u3001Mn\u3001Mg\u3001Li\u3001Y \u306FCr\u3001Al\u3001Fe3+\u3001Mg\u3001Mn\u3001Sc\u3001Ti\u3001V\u3001Fe2+\uFF09\u3067\u8868\u3055\u308C\u308B\u3002 \u7D50\u6676\u7CFB\u306B\u3088\u308A\u3001\u76F4\u65B9\uFF08\u659C\u65B9\uFF09\u8F1D\u77F3\uFF08\u3061\u3087\u304F\u307B\u3046\u304D\u305B\u304D\u3001orthopyroxene\u3001\u76F4\u65B9\u6676\u7CFB\uFF08\u659C\u65B9\u8F1D\u77F3\uFF09\uFF09\u304A\u3088\u3073\u5358\u659C\u8F1D\u77F3\uFF08\u305F\u3093\u3057\u3083\u304D\u305B\u304D\u3001clinopyroxene\u3001\u5358\u659C\u6676\u7CFB\uFF09\u306E2\u3064\u306B\u5206\u985E\u3055\u308C\u3001\u3055\u3089\u306B\u4E0A\u8A18\u306E\u5316\u5B66\u7D44\u6210\u306B\u3088\u308A\u7D30\u304B\u304F\u5206\u985E\u3055\u308C\u308B\u3002 \u82F1\u8A9E: pyroxene\u306F\u300119\u4E16\u7D00\u306B\u706B\u6210\u5CA9\u4E2D\u306B\u898B\u51FA\u3055\u308C\u305F\u5F53\u521D\u306B\u3001\u77F3\u82F1\u3068\u306F\u7570\u306A\u308B\u7570\u7269\u8CEA\u3068\u3057\u3066\u30AE\u30EA\u30B7\u30E3\u8A9E\u3067\u300Cpyro-\uFF08\u706B\u306E\u3001\u706B\u6210\u5CA9\u4E2D\u306E\uFF09\u300D\u300Cxenon\uFF08\u304A\u304B\u3057\u306A\u7570\u7269\uFF09\u3001\u30AD\u30BB\u30CE\u30F3\u306E\u8A9E\u6E90\u3068\u540C\u7FA9\u300D\u3068\u3088\u3093\u3060\u3053\u3068\u306B\u3088\u308B\u3002"@ja . "Piroxenoak burdin, magnesio eta kaltziozko silikato monoklinikoak dira. Inosilikatoen taldekoak dira. Distira bitreoa dute eta azido klorhidrikoan aldaezinak dira. Burdina duten ilunak izaten dira eta ez dutenak txuriskak, grisak edo berde argiak. Arroka igneo askoren osagaiak dira. Kimikoki anfibolen antza dute, baina euren esfoliazio planoa 90\u00BAkoa da eta tetraedro errenkada bakarra dute lotuta. Formula orokorra XY(Si,Al)2O6 da, non X eta Yk burdina, magnesioa eta kaltzioa izan ohi diren."@eu . . "\uD718\uC11D(\u8F1D\u77F3, pyroxene)\uC740 \uC870\uC554\uAD11\uBB3C\uC758 \uD558\uB098\uB85C \uD654\uC131\uC554\uACFC \uBCC0\uC131\uC554\uC5D0\uC11C \uD3ED\uB113\uAC8C \uB098\uD0C0\uB09C\uB2E4. \uD718\uC11D\uC740 \uADDC\uC0B0\uC5FC \uC0AC\uBA74\uCCB4\uC758 \uB2E8\uC77C\uC0AC\uC2AC \uAD6C\uC870\uB85C \uC774\uB8E8\uC5B4\uC838 \uC788\uACE0, \uB2E8\uC0AC\uC815\uACC4 \uB610\uB294 \uC0AC\uBC29\uC815\uACC4\uC774\uB2E4. \uD718\uC11D\uC758 \uD654\uD559\uC2DD\uC740 \uC77C\uBC18\uC801\uC73C\uB85C XY(Si,Al)2O6\uB85C \uB098\uD0C0\uB0BC \uC218 \uC788\uB2E4. \uC5EC\uAE30\uC5D0\uC11C X\uB294 \uCE7C\uC298, \uC18C\uB4D0, 2\uAC00 \uCCA0, \uB9C8\uADF8\uB124\uC298\uC774 \uB418\uB294 \uACBD\uC6B0\uAC00 \uB9CE\uC73C\uB098 \uB4DC\uBB3C\uAC8C \uC544\uC5F0, \uB9DD\uAC04, \uB9AC\uD2AC\uC774 \uCE58\uD658\uB418\uAE30\uB3C4 \uD55C\uB2E4. Y\uB294 \uC774\uBCF4\uB2E4 \uC774\uC628\uC758 \uD06C\uAE30\uAC00 \uC791\uC740 \uD06C\uB85C\uBBB4\uC774\uB098 \uC54C\uB8E8\uBBF8\uB284, 3\uAC00 \uCCA0, \uB9C8\uADF8\uB124\uC298, \uB9DD\uAC04, \uC2A4\uCE78\uB4D0, \uD2F0\uD0C0\uB284, \uBC14\uB098\uB4D0 \uB4F1\uC758 \uC774\uC628\uC774 \uB4E4\uC5B4\uAC08 \uC218 \uC788\uB2E4. \uC54C\uB8E8\uBBF8\uB284\uC740 \uADDC\uC18C\uB97C \uCE58\uD658\uD558\uB294 \uC77C\uC774 \uB9CE\uC73C\uB098 \uD718\uC11D\uC5D0\uC11C\uB294 \uC774\uB7F0 \uACBD\uC6B0\uAC00 \uC0C1\uB2F9\uD788 \uC81C\uD55C\uC801\uC774\uB2E4. \uC9C0\uAD6C\uC758 \uC0C1\uBD80 \uB9E8\uD2C0\uC740 \uC8FC\uB85C \uAC10\uB78C\uC11D\uACFC \uD718\uC11D\uC73C\uB85C \uB418\uC5B4\uC788\uB2E4."@ko . . . . . . . "Los piroxenos son un importante grupo de silicatos que forman parte de muchas rocas \u00EDgneas y metam\u00F3rficas.\u200B Su nombre proviene de las palabras \"piro\" y \"xeno\" del griego antiguo que significan \"fuego\" y \"extra\u00F1o\".\u200B Este nombre se lo dio Ren\u00E9 Just Ha\u00FCy debido a que este consideraba su ocurrencia en lavas como algo ajeno.\u200B"@es . . . . . . "\u8F1D\u77F3\uFF08\u304D\u305B\u304D\u3001pyroxene\u3001\u30D1\u30A4\u30ED\u30AD\u30B7\u30F3\uFF09\u306F\u3001\u30B1\u30A4\u9178\u5869\u9271\u7269\u306E\u4E00\u7A2E\u3002\u591A\u304F\u306E\u706B\u6210\u5CA9\u3084\u5909\u6210\u5CA9\u306B\u542B\u307E\u308C\u308B\u4EE3\u8868\u7684\u306A\u9020\u5CA9\u9271\u7269\u3002 \u8272\u306F\u7121\u8272\u30FB\u7DD1\u8272\u30FB\u8910\u8272\u30FB\u9ED2\u8272\u306A\u3069\u3067\u3001\u30AC\u30E9\u30B9\u5149\u6CA2\u3092\u6301\u3064\u3002\u81EA\u5F62\u7D50\u6676\u306F\u77ED\u67F1\u72B6\u3002\u4E8C\u65B9\u5411\u306E\u5288\u958B\u304C\u9855\u8457\u3002\u89D2\u9583\u77F3\u306B\u3088\u304F\u4F3C\u308B\u304C\u3001\u5288\u958B\u306E\u4EA4\u308F\u308B\u89D2\u5EA6\uFF08\u7D0490\u00B0\uFF09\u306B\u3088\u308A\u533A\u5225\u3055\u308C\u308B\u3002 \u57FA\u672C\u7684\u306A\u5316\u5B66\u7D44\u6210\u306F XY(Si,Al)2O6 \uFF08\u305F\u3060\u3057\u3001X \u306FCa\u3001Na\u3001Fe2+\u3001Zn\u3001Mn\u3001Mg\u3001Li\u3001Y \u306FCr\u3001Al\u3001Fe3+\u3001Mg\u3001Mn\u3001Sc\u3001Ti\u3001V\u3001Fe2+\uFF09\u3067\u8868\u3055\u308C\u308B\u3002 \u7D50\u6676\u7CFB\u306B\u3088\u308A\u3001\u76F4\u65B9\uFF08\u659C\u65B9\uFF09\u8F1D\u77F3\uFF08\u3061\u3087\u304F\u307B\u3046\u304D\u305B\u304D\u3001orthopyroxene\u3001\u76F4\u65B9\u6676\u7CFB\uFF08\u659C\u65B9\u8F1D\u77F3\uFF09\uFF09\u304A\u3088\u3073\u5358\u659C\u8F1D\u77F3\uFF08\u305F\u3093\u3057\u3083\u304D\u305B\u304D\u3001clinopyroxene\u3001\u5358\u659C\u6676\u7CFB\uFF09\u306E2\u3064\u306B\u5206\u985E\u3055\u308C\u3001\u3055\u3089\u306B\u4E0A\u8A18\u306E\u5316\u5B66\u7D44\u6210\u306B\u3088\u308A\u7D30\u304B\u304F\u5206\u985E\u3055\u308C\u308B\u3002 \u82F1\u8A9E: pyroxene\u306F\u300119\u4E16\u7D00\u306B\u706B\u6210\u5CA9\u4E2D\u306B\u898B\u51FA\u3055\u308C\u305F\u5F53\u521D\u306B\u3001\u77F3\u82F1\u3068\u306F\u7570\u306A\u308B\u7570\u7269\u8CEA\u3068\u3057\u3066\u30AE\u30EA\u30B7\u30E3\u8A9E\u3067\u300Cpyro-\uFF08\u706B\u306E\u3001\u706B\u6210\u5CA9\u4E2D\u306E\uFF09\u300D\u300Cxenon\uFF08\u304A\u304B\u3057\u306A\u7570\u7269\uFF09\u3001\u30AD\u30BB\u30CE\u30F3\u306E\u8A9E\u6E90\u3068\u540C\u7FA9\u300D\u3068\u3088\u3093\u3060\u3053\u3068\u306B\u3088\u308B\u3002"@ja . "Na pyrox trig.svg"@en . . . . . . "Pyroxen \u00E4r en samlingsbeteckning f\u00F6r ett antal silikatmineral, som \u00E4r vanligt f\u00F6rekommande i magmatiska och metamorfa bergarter och f\u00F6rekommer till exempel i basalt, diabas och gabbro. Pyroxenerna ing\u00E5r i den st\u00F6rre gruppen eller . Pyroxenerna \u00E4r viktiga bergartsbildande mineral. Den negativa jonen \u00E4r SiO3, som bildar o\u00E4ndliga kedjor i kristallens l\u00E4ngdriktning, vilket ger upphov till den karakt\u00E4ristiska spaltningen i parallellogramform d\u00E4r vinklarna \u00E4r omkring 87\u00B0 och 93\u00B0. Dessa spaltvinklar skiljer dem fr\u00E5n de n\u00E4rbesl\u00E4ktade amfibolerna, vars spaltvinklar \u00E4r cirka 124\u00B0 och 56\u00B0. I flera av pyroxenmineralen avs\u00F6ndras dessutom ofta parallella plattor vinkelr\u00E4tt mot kristallens l\u00E4ngdriktning. I pyroxengruppen ing\u00E5r: \n* Diopsid CaMg[Si2O6] \n* Hedenbergit CaFe[Si2O6] \n* Augit Ca(Mg,Fe,Al)[(Si,Al)2O6] \n* Aegirin NaFe3+[Si2O6] \n* Spodumen LiAl[Si2O6] \n* Enstatit Mg2[Si2O6] \n* Hypersten (Mg,Fe)2[Si2O6] \n* Wollastonit Ca[SiO3] \n* Rodonit Mn[SiO3]"@sv . . . "Pyrox names.svg"@en . . "Pyroxen"@sv . "Pyroxene"@en . . "Els piroxens s\u00F3n un important grup de minerals de silicat trobats en moltes roques \u00EDgnies i metam\u00F2rfiques. Comparteixen una estructura comuna que consisteix en cadenes simples de tetraedres de s\u00EDlice i es cristal\u00B7litzen en els sistemes monocl\u00EDnics i ortor\u00F2mbic. Els piroxens tenen la f\u00F3rmula general XY (Si,Al)\u2082O\u2086 (on X representa calci, sodi, ferro (II) i magnesi, i m\u00E9s rarament, zinc, mangan\u00E8s i liti, i Y representa els ions de mida m\u00E9s petita, com el crom, alumini, ferro (III), magnesi, mangan\u00E8s, escandi, titani, vanadi i fins ferro (II)). Encara que l'alumini es substitueix extensament per silici en silicats com els feldespats i els amf\u00EDbols, la substituci\u00F3 es produeix nom\u00E9s en una mesura limitada en la majoria dels piroxens."@ca . "Pyroxeen"@nl . "Piroksen"@in . "Als Pyroxengruppe bezeichnet man eine Gruppe von Mineralen aus der Abteilung der Kettensilikate. Ihre Kristallstruktur zeichnet sich durch Einfachketten aus eckenverkn\u00FCpften SiO4-Tetraedern aus und ihre Zusammensetzung gen\u00FCgt der folgenden verallgemeinerten Summenformel: M1 M2 T2O6. In dieser Strukturformel repr\u00E4sentieren M1, M2 und T unterschiedliche Positionen in der Pyroxenstruktur. Sie werden vorwiegend durch folgende Kationen belegt: \n* M1: Mg2+, Fe2+, Mn2+, Al3+, Fe3+, Ti4+, Ti3+, V3+, Sc3+, Cr3+, Zr4+, Zn2+, \n* M2: Mg2+, Fe2+, Mn2+, Ca2+, Na+, Li+ \n* T: Si4+, Al3+, Fe3+ Fett hervorgehoben sind die dominierenden Kationen auf den einzelnen Positionen. Die Zusammensetzungen der Pyroxene sind sehr variabel und sie treten weltweit in sehr vielen verschiedenen Paragenesen und geologischen Milieus auf. Sie sind wichtiger Bestandteil sowohl magmatischer wie auch metamorpher Gesteine unterschiedlichster Zusammensetzung und Bildungsbedingungen. Pyroxene haben eine H\u00E4rte zwischen 5 und 6,5 sowie eine bleichgr\u00FCne bis br\u00E4unlichgr\u00FCne oder bronzene Farbe. Strichfarbe ist ein gr\u00FCnliches Wei\u00DF. Eine sehr \u00E4hnliche Mineralgruppe sind die Amphibole; Pyroxen unterscheidet sich von diesen jedoch in der Spaltbarkeit; die Spaltwinkel bei Pyroxenen liegen bei 90 Grad, w\u00E4hrend sie bei Amphibol 120 Grad betragen. Pyroxene bilden kurze S\u00E4ulen, Amphibole dagegen meist lange. Idiomorphe Pyroxene haben zwei Kopffl\u00E4chen, Amphibole hingegen drei."@de . . "Pirokseny \u2013 grupa bardzo rozpowszechnionych minera\u0142\u00F3w ska\u0142otw\u00F3rczych o strukturze wewn\u0119trznej odpowiadaj\u0105cej krzemianom \u0142a\u0144cuchowym i og\u00F3lnym wzorze: AB[Si2O6]gdzie:A to najcz\u0119\u015Bciej wap\u0144, s\u00F3d, lit;B to najcz\u0119\u015Bciej magnez, \u017Celazo, glin. Pirokseny stanowi\u0105 cz\u0119sty sk\u0142adnik ska\u0142 magmowych i metamorficznych, a najwi\u0119ksz\u0105 rol\u0119 ska\u0142otw\u00F3rcz\u0105 odgrywa augit. Spotykane s\u0105 w ska\u0142ach na ca\u0142ym \u015Bwiecie.Nazw\u0119 wprowadzi\u0142 Ren\u00E9-Just Ha\u00FCy od s\u0142\u00F3w greckich pyr = ogie\u0144 i xenos = obcy. Uwa\u017Ca\u0142 bowiem, \u017Ce pirokseny nie tworz\u0105 si\u0119 w chwili erupcji, lecz p\u00F3\u017Aniej."@pl . "Els piroxens s\u00F3n un important grup de minerals de silicat trobats en moltes roques \u00EDgnies i metam\u00F2rfiques. Comparteixen una estructura comuna que consisteix en cadenes simples de tetraedres de s\u00EDlice i es cristal\u00B7litzen en els sistemes monocl\u00EDnics i ortor\u00F2mbic. Els piroxens tenen la f\u00F3rmula general XY (Si,Al)\u2082O\u2086 (on X representa calci, sodi, ferro (II) i magnesi, i m\u00E9s rarament, zinc, mangan\u00E8s i liti, i Y representa els ions de mida m\u00E9s petita, com el crom, alumini, ferro (III), magnesi, mangan\u00E8s, escandi, titani, vanadi i fins ferro (II)). Encara que l'alumini es substitueix extensament per silici en silicats com els feldespats i els amf\u00EDbols, la substituci\u00F3 es produeix nom\u00E9s en una mesura limitada en la majoria dels piroxens."@ca . "500"^^ . "Piroxenoak burdin, magnesio eta kaltziozko silikato monoklinikoak dira. Inosilikatoen taldekoak dira. Distira bitreoa dute eta azido klorhidrikoan aldaezinak dira. Burdina duten ilunak izaten dira eta ez dutenak txuriskak, grisak edo berde argiak. Arroka igneo askoren osagaiak dira. Kimikoki anfibolen antza dute, baina euren esfoliazio planoa 90\u00BAkoa da eta tetraedro errenkada bakarra dute lotuta. Formula orokorra XY(Si,Al)2O6 da, non X eta Yk burdina, magnesioa eta kaltzioa izan ohi diren. Pirixeno erronbikoek sistema ortorronbikoan kristalizatzen dute eta ez dute aluminiorik. Euren artean brontzita, enstatita eta daude. Beste piroxenoak, edo , sistema monoklinikoak kristaltzen dute eta aluminioa izan dezakete. Hauen adibideak augita, diopsidoa eta espodumenoa dira."@eu .