. . . . . . . . "Charnockita"@es . . . . . . . "Charnockite"@en . . . . "Charnockita es el nombre que se le da al granito (sensu stricto) con ortopiroxeno, usualmente hiperstena.\u200B\u200B Se ha postulado un origen metam\u00F3rfico en altas temperaturas y presiones para la charnockita en la facie de granulita, es decir ser\u00EDa un tipo de granulita.\u200B Tambi\u00E9n se ha postulado su formaci\u00F3n a partir de magma pobre en agua.\u200B Las charnockitas ocurren principalmente en terrenos prec\u00E1mbricos con grados altos de metamorfismo.\u200B La charnockita fue descrita originalmente en Tamil Nadu en el sur de la India y lleva el nombre del fundador de Calcuta Job Charnock cuya l\u00E1pida es de charnockita.\u200B\u200B Aparte de la India se ha hallado charnockita en Sri Lanka, Groenlandia, Suecia, Australia Occidental, R\u00EDo de Janeiro y \u00C1frica Occidental.\u200B\u200B"@es . "Charnockita es el nombre que se le da al granito (sensu stricto) con ortopiroxeno, usualmente hiperstena.\u200B\u200B Se ha postulado un origen metam\u00F3rfico en altas temperaturas y presiones para la charnockita en la facie de granulita, es decir ser\u00EDa un tipo de granulita.\u200B Tambi\u00E9n se ha postulado su formaci\u00F3n a partir de magma pobre en agua.\u200B Las charnockitas ocurren principalmente en terrenos prec\u00E1mbricos con grados altos de metamorfismo.\u200B"@es . "Czarnokity (charnockity) \u2013 ska\u0142y magmowe, kt\u00F3rych nazwa pochodzi od nagrobka (by\u0142 u\u017Cyty jako materia\u0142 do jego budowy) w Kalkucie. Wsp\u00F3\u0142wyst\u0119puj\u0105 najcz\u0119\u015Bciej z anortozytem lub norytem. Niezale\u017Cnie od genezy s\u0105 ska\u0142ami szarawymi, \u015Brednio lub gruboziarnistymi odznaczaj\u0105ce si\u0119 bez\u0142adn\u0105 b\u0105d\u017A tylko cz\u0119\u015Bciowo kierunkow\u0105 (gnejsow\u0105) tekstur\u0105."@pl . "Charnockite (/\u02C8t\u0283\u0251\u02D0rn\u0259ka\u026At/) is any orthopyroxene-bearing quartz-feldspar rock formed at high temperature and pressure, commonly found in granulite facies metamorphic regions, sensu stricto as an endmember of the charnockite series."@en . "Les charnockites s\u00F3n roques \u00EDgnies quarso-feldesp\u00E0tiques amb ortopirox\u00E8 (granits amb ortopirox\u00E8), formades a altes temperatures i pressions. Malgrat que les charnockites presenten signes de metamorfisme com ara deformaci\u00F3 i recristal\u00B7litzaci\u00F3, segons la IUGS s\u00F3n roques \u00EDgnies i tenen aparen\u00E7a de roca \u00EDgnia; malgrat aix\u00F2, en el m\u00F3n acad\u00E8mic hi ha cert debat sobre l'origen \u00EDgni o metam\u00F2rfic de la roca. Les charnockites poden ser definides com a granits d'hiperstena, del camp 3 del diagrama QAPF de Streckeisen; anteriorment, per\u00F2, s'associaven a altres membres de l'anomenada successi\u00F3 de la charnockita, qua incloia des de les charnockites sensu stricto, passant per membres intermedis com ara les norites o les peridotites d'hiperstena i fins a les piroxenites. L'origen del nom de la roca prov\u00E9 del tipus de pedra de la tomba de , fundador de Calcuta."@ca . . . . "Charnockite sind Gesteine mit granit\u00E4hnlicher Zusammensetzung und magmatischem Gef\u00FCge. Der Name Charnockit leitet sich vom Namen des Gr\u00FCnders von Kalkutta, (1630\u20131692), ab, dessen Mausoleum aus einem Charnockit erbaut worden ist. Die wissenschaftliche Erstbeschreibung erfolgte 1893 (Journal of the Asiatic Society of Bengal) und 1900 (Memoirs of the Geological Society of India) durch den f\u00FCr Indien zust\u00E4ndigen Landesgeologen Thomas Henry Holland, der den Namen nach dem f\u00FCr die Grabst\u00E4tte verwendeten Gestein aus den Vorkommen am St. Thomas Mount pr\u00E4gte."@de . . . . . . . . . . . . "8763"^^ . "Les charnockites s\u00F3n roques \u00EDgnies quarso-feldesp\u00E0tiques amb ortopirox\u00E8 (granits amb ortopirox\u00E8), formades a altes temperatures i pressions. Malgrat que les charnockites presenten signes de metamorfisme com ara deformaci\u00F3 i recristal\u00B7litzaci\u00F3, segons la IUGS s\u00F3n roques \u00EDgnies i tenen aparen\u00E7a de roca \u00EDgnia; malgrat aix\u00F2, en el m\u00F3n acad\u00E8mic hi ha cert debat sobre l'origen \u00EDgni o metam\u00F2rfic de la roca."@ca . . . "Charnockite sind Gesteine mit granit\u00E4hnlicher Zusammensetzung und magmatischem Gef\u00FCge. Der Name Charnockit leitet sich vom Namen des Gr\u00FCnders von Kalkutta, (1630\u20131692), ab, dessen Mausoleum aus einem Charnockit erbaut worden ist. Die wissenschaftliche Erstbeschreibung erfolgte 1893 (Journal of the Asiatic Society of Bengal) und 1900 (Memoirs of the Geological Society of India) durch den f\u00FCr Indien zust\u00E4ndigen Landesgeologen Thomas Henry Holland, der den Namen nach dem f\u00FCr die Grabst\u00E4tte verwendeten Gestein aus den Vorkommen am St. Thomas Mount pr\u00E4gte."@de . . . . . "Charnockita"@ca . "Charnockiti (suite delle)"@it . . . "La suite delle charnockiti \u00E8 un gruppo di rocce in parte magmatiche intrusive e in parte ricristallizzate in facies metamorfica di alto grado, di varia composizione, caratterizzate dalla presenza dell'ortopirosseno (o di fayalite pi\u00F9 quarzo), da una grana grossa e dal carattere pertitico dei feldspati alcalini. Sono quasi sempre di colore scuro."@it . "Charnockite"@fr . "\u0427\u0430\u0440\u043D\u043E\u043A\u0456\u0442"@uk . . . . . . . . "Charnockit, \u00E4r en ljusf\u00E4rgad, medium till grovkornig magmatisk bergart som till st\u00F6rsta delen inneh\u00E5ller mineralen kvarts och mikroklin, med i minskande ordning delarna oligoklas, f\u00E4ltspat, hypersten, biotit och magnetit. Trots den mindre delen hypersten \u00E4r det detta mineral som karakt\u00E4riserar bergarten. Bergarter med charnockitisk sammans\u00E4ttning kan ocks\u00E5 bildas under metamorfos av kvarts-f\u00E4ltspatsrika bergarter i granulitomr\u00E5den. Typomr\u00E5det f\u00F6r bergarten \u00E4r i den indiska delstaten Tamil Nadu. Bergarten \u00E4r Hallands landskapssten."@sv . "John Flett"@en . . "Charnockit"@de . . . . . . . "Charnockite (/\u02C8t\u0283\u0251\u02D0rn\u0259ka\u026At/) is any orthopyroxene-bearing quartz-feldspar rock formed at high temperature and pressure, commonly found in granulite facies metamorphic regions, sensu stricto as an endmember of the charnockite series."@en . . . . . . . . . . "\u7D2B\u82CF\u82B1\u5C97\u5CA9\uFF08\u82F1\u8A9E\uFF1ACharnockite\uFF09\u662F\u6307\u5728\u9AD8\u6EAB\u548C\u9AD8\u58D3\u4E0B\u5F62\u6210\u7684\u4EFB\u4F55\u542B\u659C\u65B9\u8F1D\u77F3\u7684\u77F3\u82F1\u9577\u77F3\u5CA9\u77F3\uFF0C\u5E38\u898B\u65BC\u9EBB\u7C92\u5CA9\u76F8\u8B8A\u8CEA\u5340\u3002 \u7D2B\u82CF\u82B1\u5C97\u5CA9\u4E2D\u666E\u904D\u5B58\u5728\u6709\u7194\u4F53\u4EA4\u4EE3\u7ED3\u6784,\u4E3B\u8981\u7531\u6B8B\u6676\u76F8\u77FF\u7269\u548C\u7ED3\u6676\u76F8\u77FF\u7269\u7EC4\u6210.\u5BF9\u7D2B\u82CF\u82B1\u5C97\u5CA9\u53CA\u53D8\u8D28\u8868\u58F3\u4E2D\u6D41\u4F53\u5305\u88F9\u4F53\u4EA7\u72B6\u3001\u6210\u5206\u7684\u7814\u7A76\u53D1\u73B0\uFF0C\u5BCCCO2\u6D41\u4F53\u5305\u88F9\u4F53\u548C\u5BCCN2\u6D41\u4F53\u5305\u88F9\u4F53\u5747\u6765\u81EA\u5730\u5E54\u6DF1\u90E8\u3002\u7D2B\u82CF\u82B1\u5C97\u5CA9\u5E38\u5448\u7C97\u7C92\u5757\u72B6\u6216\u7247\u9EBB\u72B6\uFF0C\u82B1\u5C97\u7ED3\u6784\uFF0C\u6BD4\u91CD2.67\u5DE6\u53F3\uFF0C\u989C\u8272\u8F83\u6DF1\u3002\u77F3\u82F1\u5448\u70DF\u7070\u81F3\u6D45\u84DD\u8272\uFF0C\u53EF\u542B\u6781\u7EC6\u5C0F\u91D1\u7EA2\u77F3\u3001\u5BCC\u9506\u77FF\u7269\u6216\u6709\u4F17\u591A\u88C2\u9699\u548CCO2\u5305\u88F9\u4F53\uFF1B\u659C\u957F\u77F3\u4E3A\u66F4\u957F\u77F3\u6216\u4E2D\u957F\u77F3\uFF0C\u5E38\u89C1\u94A0\u957F\u77F3\u5F8B\u53CC\u6676\u548C\u53CD\u6761\u7EB9\u6784\u9020\uFF1B\u78B1\u6027\u957F\u77F3\u4E3A\u6B63\u957F\u77F3\u6216\u5FAE\u659C\u957F\u77F3\uFF0C\u5F80\u5F80\u5448\u73B0\u6761\u7EB9\u6784\u9020\uFF08\u6761\u7EB9\u76F8\u7684\u6210\u5206\u5E38\u4E3A\u66F4\u3001\u4E2D\u957F\u77F3\uFF09\uFF1B\u666E\u904D\u542B\u7D2B\u82CF\u8F89\u77F3\uFF0C\u591A\u8272\u6027\u663E\u8457\uFF0C\u77F3\u69B4\u5B50\u77F3\u662F\u7D2B\u82CF\u82B1\u5C97\u5CA9\u7684\u7279\u5F81\u77FF\u7269;\u6709\u65F6\u542B\u5C11\u91CF\u5355\u659C\u8F89\u77F3\u3001\u666E\u901A\u89D2\u95EA\u77F3\u548C\u9ED1\u4E91\u6BCD\u3002"@zh . "\u7D2B\u82CF\u82B1\u5C97\u5CA9\uFF08\u82F1\u8A9E\uFF1ACharnockite\uFF09\u662F\u6307\u5728\u9AD8\u6EAB\u548C\u9AD8\u58D3\u4E0B\u5F62\u6210\u7684\u4EFB\u4F55\u542B\u659C\u65B9\u8F1D\u77F3\u7684\u77F3\u82F1\u9577\u77F3\u5CA9\u77F3\uFF0C\u5E38\u898B\u65BC\u9EBB\u7C92\u5CA9\u76F8\u8B8A\u8CEA\u5340\u3002 \u7D2B\u82CF\u82B1\u5C97\u5CA9\u4E2D\u666E\u904D\u5B58\u5728\u6709\u7194\u4F53\u4EA4\u4EE3\u7ED3\u6784,\u4E3B\u8981\u7531\u6B8B\u6676\u76F8\u77FF\u7269\u548C\u7ED3\u6676\u76F8\u77FF\u7269\u7EC4\u6210.\u5BF9\u7D2B\u82CF\u82B1\u5C97\u5CA9\u53CA\u53D8\u8D28\u8868\u58F3\u4E2D\u6D41\u4F53\u5305\u88F9\u4F53\u4EA7\u72B6\u3001\u6210\u5206\u7684\u7814\u7A76\u53D1\u73B0\uFF0C\u5BCCCO2\u6D41\u4F53\u5305\u88F9\u4F53\u548C\u5BCCN2\u6D41\u4F53\u5305\u88F9\u4F53\u5747\u6765\u81EA\u5730\u5E54\u6DF1\u90E8\u3002\u7D2B\u82CF\u82B1\u5C97\u5CA9\u5E38\u5448\u7C97\u7C92\u5757\u72B6\u6216\u7247\u9EBB\u72B6\uFF0C\u82B1\u5C97\u7ED3\u6784\uFF0C\u6BD4\u91CD2.67\u5DE6\u53F3\uFF0C\u989C\u8272\u8F83\u6DF1\u3002\u77F3\u82F1\u5448\u70DF\u7070\u81F3\u6D45\u84DD\u8272\uFF0C\u53EF\u542B\u6781\u7EC6\u5C0F\u91D1\u7EA2\u77F3\u3001\u5BCC\u9506\u77FF\u7269\u6216\u6709\u4F17\u591A\u88C2\u9699\u548CCO2\u5305\u88F9\u4F53\uFF1B\u659C\u957F\u77F3\u4E3A\u66F4\u957F\u77F3\u6216\u4E2D\u957F\u77F3\uFF0C\u5E38\u89C1\u94A0\u957F\u77F3\u5F8B\u53CC\u6676\u548C\u53CD\u6761\u7EB9\u6784\u9020\uFF1B\u78B1\u6027\u957F\u77F3\u4E3A\u6B63\u957F\u77F3\u6216\u5FAE\u659C\u957F\u77F3\uFF0C\u5F80\u5F80\u5448\u73B0\u6761\u7EB9\u6784\u9020\uFF08\u6761\u7EB9\u76F8\u7684\u6210\u5206\u5E38\u4E3A\u66F4\u3001\u4E2D\u957F\u77F3\uFF09\uFF1B\u666E\u904D\u542B\u7D2B\u82CF\u8F89\u77F3\uFF0C\u591A\u8272\u6027\u663E\u8457\uFF0C\u77F3\u69B4\u5B50\u77F3\u662F\u7D2B\u82CF\u82B1\u5C97\u5CA9\u7684\u7279\u5F81\u77FF\u7269;\u6709\u65F6\u542B\u5C11\u91CF\u5355\u659C\u8F89\u77F3\u3001\u666E\u901A\u89D2\u95EA\u77F3\u548C\u9ED1\u4E91\u6BCD\u3002"@zh . "\uCC28\uB178\uCE74\uC774\uD2B8(Charnockite, /\u02C8t\u0283\u0251\u02D0rn\u0259ka\u026At/)\uB294 \uC0AC\uBC29\uD718\uC11D\uC744 \uD3EC\uD568\uD558\uACE0 \uC788\uB294 \uC11D\uC601-\uC7A5\uC11D\uC9C8 \uC554\uC11D\uB4E4\uC744 \uAC00\uB9AC\uD0A4\uB294 \uC774\uB984\uC73C\uB85C \uC8FC\uB85C \uC11D\uC601\uACFC \uC7A5\uC11D\uC758 \uD37C\uC2F8\uC774\uD2B8\u00B7\uC548\uD2F0\uD37C\uC2F8\uC774\uD2B8, \uADF8\uB9AC\uACE0 \uACE0\uC628\uACE0\uC555\uC5D0\uC11C \uD615\uC131\uB41C \uC0AC\uBC29\uD718\uC11D(\uC8FC\uB85C \uD558\uC774\uD37C\uC52C)\uC73C\uB85C \uC870\uC131\uB418\uC5EC\uC788\uB2E4. \uD754\uD788 \uBC31\uB9BD\uC554\uC0C1 \uBCC0\uC131\uC0C1\uC5D0\uC11C \uBC1C\uACAC\uB418\uACE0 \uC788\uB2E4."@ko . . . . . . . . . . "John Smith"@en . . . "\u7D2B\u82CF\u82B1\u5C97\u5CA9"@zh . . . "\uCC28\uB178\uCE74\uC774\uD2B8(Charnockite, /\u02C8t\u0283\u0251\u02D0rn\u0259ka\u026At/)\uB294 \uC0AC\uBC29\uD718\uC11D\uC744 \uD3EC\uD568\uD558\uACE0 \uC788\uB294 \uC11D\uC601-\uC7A5\uC11D\uC9C8 \uC554\uC11D\uB4E4\uC744 \uAC00\uB9AC\uD0A4\uB294 \uC774\uB984\uC73C\uB85C \uC8FC\uB85C \uC11D\uC601\uACFC \uC7A5\uC11D\uC758 \uD37C\uC2F8\uC774\uD2B8\u00B7\uC548\uD2F0\uD37C\uC2F8\uC774\uD2B8, \uADF8\uB9AC\uACE0 \uACE0\uC628\uACE0\uC555\uC5D0\uC11C \uD615\uC131\uB41C \uC0AC\uBC29\uD718\uC11D(\uC8FC\uB85C \uD558\uC774\uD37C\uC52C)\uC73C\uB85C \uC870\uC131\uB418\uC5EC\uC788\uB2E4. \uD754\uD788 \uBC31\uB9BD\uC554\uC0C1 \uBCC0\uC131\uC0C1\uC5D0\uC11C \uBC1C\uACAC\uB418\uACE0 \uC788\uB2E4."@ko . . . . "Charnockity"@pl . "Flett"@en . . . "Carnokit"@in . . . . . . "\uCC28\uB178\uCE74\uC774\uD2B8"@ko . . . "5"^^ . . . "Charnockite"@en . "Charnockit, \u00E4r en ljusf\u00E4rgad, medium till grovkornig magmatisk bergart som till st\u00F6rsta delen inneh\u00E5ller mineralen kvarts och mikroklin, med i minskande ordning delarna oligoklas, f\u00E4ltspat, hypersten, biotit och magnetit. Trots den mindre delen hypersten \u00E4r det detta mineral som karakt\u00E4riserar bergarten. Bergarter med charnockitisk sammans\u00E4ttning kan ocks\u00E5 bildas under metamorfos av kvarts-f\u00E4ltspatsrika bergarter i granulitomr\u00E5den. Typomr\u00E5det f\u00F6r bergarten \u00E4r i den indiska delstaten Tamil Nadu. Bergarten \u00E4r Hallands landskapssten. Under tidigare geologiska perioder, f\u00F6r 1 700 till 1 200 miljoner \u00E5r sedan, har den hall\u00E4ndska berggrunden varit utsatt f\u00F6r h\u00F6g temperatur och tryck p\u00E5 stora djup. Speciellt kraftig var denna process i trakten av vad som skulle bli Varberg; charnockiten kallas \u00E4ven \"varbergsgranit\". Den gnejs som berggrunden ursprungligen bestod av blev under dessa f\u00F6rh\u00E5llanden omvandlad till en homogen bergart med medel- till grovkornig struktur och ungef\u00E4r samma kemiska sammans\u00E4ttning som granit. Den inneh\u00E5ller dock pyroxenen hypersten samt f\u00E4ltspat med gr\u00F6naktig f\u00E4rg, vilket ger charnockiten dess gr\u00F6na f\u00E4rg. Just f\u00E4rgen har gjort charnockiten till en popul\u00E4r byggnadssten, s\u00E4rskilt under 1800-talet. Den vittrar dock l\u00E4tt och blir matt i f\u00E4rgen, men br\u00F6ts \u00E4nd\u00E5 fram till 1940-talet."@sv . . "Istilah Carnokit diterapkan untuk setiap Batuan Felspar-kuarsa orthopyroxen-bearing, yang terdiri terutama dari kuarsa, atau antipertit dan ortopiroksen (biasanya hipersten), yang terbentuk pada suhu dan tekanan yang tinggi, umumnya ditemukan di fasies metamorfik granulit, sebagai anggota terakhir kelompok carnokit."@in . "Istilah Carnokit diterapkan untuk setiap Batuan Felspar-kuarsa orthopyroxen-bearing, yang terdiri terutama dari kuarsa, atau antipertit dan ortopiroksen (biasanya hipersten), yang terbentuk pada suhu dan tekanan yang tinggi, umumnya ditemukan di fasies metamorfik granulit, sebagai anggota terakhir kelompok carnokit."@in . . . . "La suite delle charnockiti \u00E8 un gruppo di rocce in parte magmatiche intrusive e in parte ricristallizzate in facies metamorfica di alto grado, di varia composizione, caratterizzate dalla presenza dell'ortopirosseno (o di fayalite pi\u00F9 quarzo), da una grana grossa e dal carattere pertitico dei feldspati alcalini. Sono quasi sempre di colore scuro."@it . . . "1394538"^^ . . "\u0427\u0430\u0440\u043D\u043E\u043A\u0456\u0442 (\u0440\u043E\u0441. \u0447\u0430\u0440\u043D\u043E\u043A\u0438\u0442, \u0430\u043D\u0433\u043B. charnockite; \u043D\u0456\u043C. Charnockit m) \u2014 \u043C\u0430\u0433\u043C\u0430\u0442\u0438\u0447\u043D\u0430 \u0456 \u043C\u0435\u0442\u0430\u043C\u043E\u0440\u0444\u0456\u0447\u043D\u0430 \u0433\u0456\u0440\u0441\u044C\u043A\u0430 \u043F\u043E\u0440\u043E\u0434\u0430 \u0441\u0456\u043C\u0435\u0439\u0441\u0442\u0432\u0430 \u043D\u0438\u0437\u044C\u043A\u043E\u043B\u0443\u0436\u043D\u0438\u0445 \u0491\u0440\u0430\u043D\u0456\u0442\u0456\u0432."@uk . . . . . . "Au sens strict, le terme charnockite est utilis\u00E9 pour d\u00E9signer un granite \u00E0 orthopyrox\u00E8ne, roche magmatique compos\u00E9e de quartz, feldspath alcalin (microcline ou orthose perthitique), feldspath plagioclase, et orthopyrox\u00E8ne (hypersth\u00E8ne). D\u2019autres min\u00E9raux comme la biotite ou le grenat peuvent \u00EAtre pr\u00E9sents. Au sens plus large, le terme charnockite est utilis\u00E9 pour d\u00E9signer toute roche quartzofeldspathique \u00E0 orthopyrox\u00E8ne, en particulier des roches d\u2019origine m\u00E9tamorphique. Cet usage est maintenant d\u00E9conseill\u00E9 par de nombreux auteurs, en particulier \u00E0 la suite de nombreuses confusions car il devient ainsi un synonyme de granulite. Les min\u00E9raux des charnockites contiennent souvent de nombreuses inclusions align\u00E9es parall\u00E8lement \u00E0 certains plans cristallographiques. Ces inclusions donnent des "@fr . . "\u0427\u0430\u0440\u043D\u043E\u043A\u0456\u0442 (\u0440\u043E\u0441. \u0447\u0430\u0440\u043D\u043E\u043A\u0438\u0442, \u0430\u043D\u0433\u043B. charnockite; \u043D\u0456\u043C. Charnockit m) \u2014 \u043C\u0430\u0433\u043C\u0430\u0442\u0438\u0447\u043D\u0430 \u0456 \u043C\u0435\u0442\u0430\u043C\u043E\u0440\u0444\u0456\u0447\u043D\u0430 \u0433\u0456\u0440\u0441\u044C\u043A\u0430 \u043F\u043E\u0440\u043E\u0434\u0430 \u0441\u0456\u043C\u0435\u0439\u0441\u0442\u0432\u0430 \u043D\u0438\u0437\u044C\u043A\u043E\u043B\u0443\u0436\u043D\u0438\u0445 \u0491\u0440\u0430\u043D\u0456\u0442\u0456\u0432."@uk . "947"^^ . "Au sens strict, le terme charnockite est utilis\u00E9 pour d\u00E9signer un granite \u00E0 orthopyrox\u00E8ne, roche magmatique compos\u00E9e de quartz, feldspath alcalin (microcline ou orthose perthitique), feldspath plagioclase, et orthopyrox\u00E8ne (hypersth\u00E8ne). D\u2019autres min\u00E9raux comme la biotite ou le grenat peuvent \u00EAtre pr\u00E9sents. Au sens plus large, le terme charnockite est utilis\u00E9 pour d\u00E9signer toute roche quartzofeldspathique \u00E0 orthopyrox\u00E8ne, en particulier des roches d\u2019origine m\u00E9tamorphique. Cet usage est maintenant d\u00E9conseill\u00E9 par de nombreux auteurs, en particulier \u00E0 la suite de nombreuses confusions car il devient ainsi un synonyme de granulite. Les min\u00E9raux des charnockites contiennent souvent de nombreuses inclusions align\u00E9es parall\u00E8lement \u00E0 certains plans cristallographiques. Ces inclusions donnent des aspects iridescents caract\u00E9ristiques aux charnockites."@fr . "Charnockit"@sv . . . "Czarnokity (charnockity) \u2013 ska\u0142y magmowe, kt\u00F3rych nazwa pochodzi od nagrobka (by\u0142 u\u017Cyty jako materia\u0142 do jego budowy) w Kalkucie. Wsp\u00F3\u0142wyst\u0119puj\u0105 najcz\u0119\u015Bciej z anortozytem lub norytem. Niezale\u017Cnie od genezy s\u0105 ska\u0142ami szarawymi, \u015Brednio lub gruboziarnistymi odznaczaj\u0105ce si\u0119 bez\u0142adn\u0105 b\u0105d\u017A tylko cz\u0119\u015Bciowo kierunkow\u0105 (gnejsow\u0105) tekstur\u0105."@pl . . . . . . . . . . "1068357931"^^ .