. . . . "Bl\u00E5skiffer \u00E4r en sorts skiffer med metamorft ursprung. som och kan ge bergarten en bl\u00E5 f\u00E4rg. Trots inneh\u00E5ll av glaukofan som \u00E4r lilabl\u00E5 \u00E4r \u00E4nd\u00E5 bl\u00E5skiffrarna ofta gr\u00E5. Bl\u00E5skiffer har liten kornstorlek p\u00E5 0,5 \u2013 2 mm och best\u00E5r huvudsakligen av glaukofan, klorit och epidot. Andra \u00E4mnen som kan ing\u00E5 \u00E4r , jadeit, glimmer och/eller kvarts. Bl\u00E5skiffer bildas oftast i milj\u00F6er med h\u00F6gt tryck och relativt l\u00E5ga temperaturer av ursprungsbergarter med basisk sammans\u00E4ttning. Bl\u00E5skiffer finns l\u00E4ngs i Toscana i Italien. Gr\u00F6nskiffer \u00E4r en bergart som liknar bl\u00E5skiffer."@sv . . . . . . . . . . "\u85CD\u7247\u5CA9"@zh . "Modr\u00E1 b\u0159idlice nebo glaukofanit nebo glaukofanov\u00E1 b\u0159idlice je p\u0159em\u011Bn\u011Bn\u00E1 hornina typick\u00E1 pro vysokotlakou a n\u00EDzkoteplotn\u00ED metamorf\u00F3zu, kter\u00E1 p\u0159edstavuje . Term\u00EDn glaukofanit zavedl roce 1888 chorvatsk\u00FD geolog . Term\u00EDn modr\u00E1 b\u0159idlice zavedl v roce 1962 americk\u00FD geolog United States Geological Survey Edgar Bailey."@cs . . . . . . "1238181"^^ . . . . "Els esquists blaus, tamb\u00E9 anomenats a vegades esquists de glauc\u00F2fan (no confondre amb les ) s\u00F3n roques metavolc\u00E0niques que es formen a partir del metamorfisme d'un basalt o de roques de composici\u00F3 similar a aquest a altes pressions i baixes temperatures, corresponents aproximadament a entre 15 i 20 km de profunditat i entre 200 i 500 \u00B0C. El color blau de la roca \u00E9s degut a la pres\u00E8ncia dels minerals predominants\u02D0 el glauc\u00F2fan i la lawsonita. Els esquists blaus troben t\u00EDpicament en cinturons orog\u00E8nics, sovint en contacte per falla amb o roques de la f\u00E0cies eclogita."@ca . . . "Els esquists blaus, tamb\u00E9 anomenats a vegades esquists de glauc\u00F2fan (no confondre amb les ) s\u00F3n roques metavolc\u00E0niques que es formen a partir del metamorfisme d'un basalt o de roques de composici\u00F3 similar a aquest a altes pressions i baixes temperatures, corresponents aproximadament a entre 15 i 20 km de profunditat i entre 200 i 500 \u00B0C. El color blau de la roca \u00E9s degut a la pres\u00E8ncia dels minerals predominants\u02D0 el glauc\u00F2fan i la lawsonita. Els esquists blaus troben t\u00EDpicament en cinturons orog\u00E8nics, sovint en contacte per falla amb o roques de la f\u00E0cies eclogita."@ca . . "\u0627\u0644\u0634\u064A\u0633\u062A \u0627\u0644\u0623\u0632\u0631\u0642 (\u0628\u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A\u0629: Blueschist)\u200F \u0623\u064A\u0636\u0627\u064B \u064A\u064F\u0637\u0644\u0642 \u0639\u0644\u064A\u0647 \u0627\u0644\u0634\u064A\u0633\u062A \u0627\u0644\u0643\u0644\u0648\u0641\u064A\u0646\u064A\u060C \u0647\u0648 \u0635\u062E\u0631 \u0628\u0631\u0643\u0627\u0646\u064A \u0645\u062A\u062D\u0648\u0644 \u064A\u062A\u0634\u0643\u0644 \u0645\u0646 \u062E\u0644\u0627\u0644 \u062A\u062D\u0648\u0644 \u0645\u0646 \u0627\u0644\u0628\u0627\u0632\u0644\u062A \u0648\u0627\u0644\u0635\u062E\u0648\u0631 \u0645\u0639 \u062A\u0643\u0648\u064A\u0646 \u0645\u0645\u0627\u062B\u0644 \u0641\u064A \u0627\u0644\u0636\u063A\u0648\u0637 \u0627\u0644\u0639\u0627\u0644\u064A\u0629 \u0648\u062F\u0631\u062C\u0627\u062A \u0627\u0644\u062D\u0631\u0627\u0631\u0629 \u0627\u0644\u0645\u0646\u062E\u0641\u0636\u0629 (200 ~ 500 \u062F\u0631\u062C\u0629 \u0645\u0626\u0648\u064A\u0629)\u060C \u0623\u064A \u0645\u0627 \u064A\u0639\u0627\u062F\u0644 \u062A\u0642\u0631\u064A\u0628\u0627\u064B \u0639\u0645\u0642 15 \u0625\u0644\u0649 30 \u0643\u064A\u0644\u0648\u0645\u062A\u0631\u0627\u064B. \u0627\u0644\u0644\u0648\u0646 \u0627\u0644\u0623\u0632\u0631\u0642 \u064A\u0623\u062A\u064A \u0645\u0646 \u0648\u062C\u0648\u062F \u0627\u0644\u063A\u0644\u0648\u0643\u0648\u0641\u0627\u0646 \u0627\u0644\u0645\u0639\u0627\u062F\u0646 \u0627\u0644\u063A\u0627\u0644\u0628\u0629 \u0648\u0627\u0644\u0644\u0648\u0633\u0648\u0646\u064A\u062A."@ar . "Blueschist"@en . "\u0421\u043B\u0430\u043D\u0446\u0456 \u0431\u043B\u0430\u043A\u0438\u0442\u043D\u0456 (\u0440\u043E\u0441. \u0441\u043B\u0430\u043D\u0446\u044B \u0433\u043E\u043B\u0443\u0431\u044B\u0435, \u0430\u043D\u0433\u043B. blue schistes, \u043D\u0456\u043C. blaue Schiefer m) \u2014 \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 \u0430\u0431\u043E \u043C\u0435\u0442\u0430\u043C\u043E\u0440\u0444\u0456\u0447\u043D\u0430 \u0444\u0430\u0446\u0456\u044F, \u044F\u043A\u0430 \u0445\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u0438\u0437\u0443\u0454\u0442\u044C\u0441\u044F \u0430\u0441\u043E\u0446\u0456\u0430\u0446\u0456\u0454\u044E \u043D\u0438\u0437\u044C\u043A\u043E\u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u043D\u0438\u0445 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432 \u0432\u0438\u0441\u043E\u043A\u043E\u0433\u043E \u0442\u0438\u0441\u043A\u0443. \u0412\u0432\u0430\u0436\u0430\u0454\u0442\u044C\u0441\u044F, \u0449\u043E \u0421\u043B\u0430\u043D\u0446\u0456 \u0431\u043B\u0430\u043A\u0438\u0442\u043D\u0456 \u0444\u043E\u0440\u043C\u0443\u044E\u0442\u044C\u0441\u044F, \u0433\u043E\u043B\u043E\u0432\u043D\u0438\u043C \u0447\u0438\u043D\u043E\u043C, \u0432 \u0445\u043E\u043B\u043E\u0434\u043D\u0438\u0445 \u043B\u0456\u0442\u043E\u0441\u0444\u0435\u0440\u043D\u0438\u0445 \u043F\u043B\u0438\u0442\u0430\u0445 \u0432 \u0437\u043E\u043D\u0430\u0445 \u0441\u0443\u0431\u0434\u0443\u043A\u0446\u0456\u0457."@uk . . . "\u0627\u0644\u0634\u064A\u0633\u062A \u0627\u0644\u0623\u0632\u0631\u0642 (\u0628\u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A\u0629: Blueschist)\u200F \u0623\u064A\u0636\u0627\u064B \u064A\u064F\u0637\u0644\u0642 \u0639\u0644\u064A\u0647 \u0627\u0644\u0634\u064A\u0633\u062A \u0627\u0644\u0643\u0644\u0648\u0641\u064A\u0646\u064A\u060C \u0647\u0648 \u0635\u062E\u0631 \u0628\u0631\u0643\u0627\u0646\u064A \u0645\u062A\u062D\u0648\u0644 \u064A\u062A\u0634\u0643\u0644 \u0645\u0646 \u062E\u0644\u0627\u0644 \u062A\u062D\u0648\u0644 \u0645\u0646 \u0627\u0644\u0628\u0627\u0632\u0644\u062A \u0648\u0627\u0644\u0635\u062E\u0648\u0631 \u0645\u0639 \u062A\u0643\u0648\u064A\u0646 \u0645\u0645\u0627\u062B\u0644 \u0641\u064A \u0627\u0644\u0636\u063A\u0648\u0637 \u0627\u0644\u0639\u0627\u0644\u064A\u0629 \u0648\u062F\u0631\u062C\u0627\u062A \u0627\u0644\u062D\u0631\u0627\u0631\u0629 \u0627\u0644\u0645\u0646\u062E\u0641\u0636\u0629 (200 ~ 500 \u062F\u0631\u062C\u0629 \u0645\u0626\u0648\u064A\u0629)\u060C \u0623\u064A \u0645\u0627 \u064A\u0639\u0627\u062F\u0644 \u062A\u0642\u0631\u064A\u0628\u0627\u064B \u0639\u0645\u0642 15 \u0625\u0644\u0649 30 \u0643\u064A\u0644\u0648\u0645\u062A\u0631\u0627\u064B. \u0627\u0644\u0644\u0648\u0646 \u0627\u0644\u0623\u0632\u0631\u0642 \u064A\u0623\u062A\u064A \u0645\u0646 \u0648\u062C\u0648\u062F \u0627\u0644\u063A\u0644\u0648\u0643\u0648\u0641\u0627\u0646 \u0627\u0644\u0645\u0639\u0627\u062F\u0646 \u0627\u0644\u063A\u0627\u0644\u0628\u0629 \u0648\u0627\u0644\u0644\u0648\u0633\u0648\u0646\u064A\u062A."@ar . . . . . . . "Esquisto azul"@es . . . . . . "El esquisto azul es una roca metam\u00F3rfica. Su color caracter\u00EDstico, el azul, se debe a la presencia de anf\u00EDbol rico en sodio (anf\u00EDbol s\u00F3dico), o glaucofana. El esquisto azul es t\u00EDpico de zonas con un bajo como los son las zonas de subducci\u00F3n. Se forman en ambientes de alta presi\u00F3n y baja temperatura.[cita requerida]\u200B"@es . . . . . . "Blauschiefer"@de . . . "\u0421\u043B\u0430\u043D\u0446\u0456 \u0431\u043B\u0430\u043A\u0438\u0442\u043D\u0456"@uk . . . . . "Blueschist ( /\u02C8blu\u02D0\u0283\u026Ast/), also called glaucophane schist, is a metavolcanic rock that forms by the metamorphism of basalt and rocks with similar composition at high pressures and low temperatures (200\u2013500 \u00B0C (392\u2013932 \u00B0F)), approximately corresponding to a depth of 15\u201330 km (9.3\u201318.6 mi). The blue color of the rock comes from the presence of the predominant minerals glaucophane and lawsonite. Blueschists are schists typically found within orogenic belts as terranes of lithology in faulted contact with greenschist or rarely eclogite facies rocks."@en . . . . . . . . . . . . . . . "7611"^^ . "1104138849"^^ . "Lo scisto blu \u00E8 una roccia metamorfica contenente un tipo di anfibolo blu, chiamato glaucofane, che si sviluppa quando il protolito (basalto o peridotite) viene sottoposto a grandi sforzi differenziali, pur mantenendo una temperatura relativamente bassa. Il suo modello di genesi \u00E8 particolare in quanto solitamente l'aumento della Pressione litostatica \u00E8 associato ad un aumento anche della temperatura; ci\u00F2 \u00E8 quasi sempre vero, salvo nei prismi di accrescimento lungo i margini convergenti, dove la litosfera oceanica in subduzione non trasferisce il calore normalmente associato al sedimento sepolto fino a 20 km di profondit\u00E0 (il gradiente geotermico aumenta progressivamente con l'aumentare della profondit\u00E0), tuttavia sottopone la roccia ad altissime pressioni che generano foliazione metamorfica, associata ad orientamento preferenziale dei granuli minerali."@it . "El esquisto azul es una roca metam\u00F3rfica. Su color caracter\u00EDstico, el azul, se debe a la presencia de anf\u00EDbol rico en sodio (anf\u00EDbol s\u00F3dico), o glaucofana. El esquisto azul es t\u00EDpico de zonas con un bajo como los son las zonas de subducci\u00F3n. Se forman en ambientes de alta presi\u00F3n y baja temperatura.[cita requerida]\u200B"@es . . . . . "\u0634\u064A\u0633\u062A \u0623\u0632\u0631\u0642"@ar . . "\u85CD\u7247\u5CA9\uFF08\u82F1\u8A9E\uFF1Ablueschist\uFF09\u4E5F\u7A31\u70BA\u85CD\u9583\u77F3\u7247\u5CA9\uFF0C\u662F\u4E00\u7A2E\u5728\u9AD8\u58D3\u548C\u4F4E\u6EAB\uFF08200\uFF0D500 \u00B0C\uFF08392\uFF0D932 \u00B0F\uFF09\uFF09\u4E0B\u8B8A\u8CEA\u5F62\u6210\u7684\u8B8A\u8CEA\u5CA9\u3002\u5927\u7D04\u5C0D\u61C9\u65BC 15-30 \u516C\u91CC\uFF089.3-18.6 \u82F1\u91CC\uFF09\u7684\u6DF1\u5EA6\u3002\u5CA9\u77F3\u7684\u85CD\u8272\u4F86\u81EA\u4E3B\u8981\u7926\u7269\u84DD\u95EA\u77F3\u548C\u786C\u67F1\u77F3\u3002\u85CD\u7247\u5CA9\u901A\u5E38\u5728\u9020\u5C71\u5E36\u4E2D\u767C\u73FE\uFF0C\u9694\u65B7\u5C64\u5076\u5C14\u8207\u7DA0\u7247\u5CA9\u6216\u8207\u69B4\u8F1D\u5CA9\u63A5\u89F8\u3002 \u85CD\u7247\u5CA9\u76F8\u4E2D\u7684\u5CA9\u77F3\u7926\u7269\u6210\u5206\u56E0\u539F\u5CA9\u800C\u6709\u6240\u4E0D\u540C\u3002 \u7384\u6B66\u5CA9\uFF1A\u85CD\u9583\u77F3 + \u786C\u67F1\u77F3\u548C/\u6216\u7DA0\u7C3E\u77F3 + \u9209\u9577\u77F3 + \u9226\u77F3 +/- \u77F3\u69B4\u77F3 +/- \u77F3\u82F1\u786C\u7389 + \u77F3\u82F1 \u8D85\u9382\u9435\u8CEA\u5CA9\u77F3\uFF1A\u86C7\u7D0B\u5CA9/ +/- \u6ED1\u77F3 +/- \u9EDD\u7C3E\u77F3 \u6CE5\u8CEA\u5CA9\uFF1AFe-Mg-carpholite +/- \u7DA0\u6CE5\u77F3 +/- \u85CD\u6676\u77F3 +/- \u9209\u9577\u77F3 +/- \u77F3\u82F1 +/- \u6ED1\u77F3 +/- \u77F3\u69B4\u77F3 \u82B1\u5D17\u5CA9\uFF1A\u85CD\u6676\u77F3 +/- \u767D\u96F2\u77F3 +/- \u7DA0\u6CE5\u77F3 +/- \u9209\u9577\u77F3 +/- \u77F3\u82F1 +/- \u767D\u96F2\u6BCD \u77F3\u7070\u77F3\u548C\u5927\u7406\u77F3\uFF1A\u65B9\u89E3\u77F3\u5728\u9AD8\u58D3\u4E0B\u8F49\u8B8A\u70BA\u6587\u77F3\uFF0C\u4F46\u901A\u5E38\u5728\u6316\u6398\u6642\u6062\u5FA9\u70BA\u65B9\u89E3\u77F3\u3002"@zh . . "Blueschist ( /\u02C8blu\u02D0\u0283\u026Ast/), also called glaucophane schist, is a metavolcanic rock that forms by the metamorphism of basalt and rocks with similar composition at high pressures and low temperatures (200\u2013500 \u00B0C (392\u2013932 \u00B0F)), approximately corresponding to a depth of 15\u201330 km (9.3\u201318.6 mi). The blue color of the rock comes from the presence of the predominant minerals glaucophane and lawsonite. Blueschists are schists typically found within orogenic belts as terranes of lithology in faulted contact with greenschist or rarely eclogite facies rocks."@en . . . "Modr\u00E1 b\u0159idlice"@cs . . . . . "Bl\u00E5skiffer"@sv . . . . . . "Bl\u00E5skiffer \u00E4r en sorts skiffer med metamorft ursprung. som och kan ge bergarten en bl\u00E5 f\u00E4rg. Trots inneh\u00E5ll av glaukofan som \u00E4r lilabl\u00E5 \u00E4r \u00E4nd\u00E5 bl\u00E5skiffrarna ofta gr\u00E5. Bl\u00E5skiffer har liten kornstorlek p\u00E5 0,5 \u2013 2 mm och best\u00E5r huvudsakligen av glaukofan, klorit och epidot. Andra \u00E4mnen som kan ing\u00E5 \u00E4r , jadeit, glimmer och/eller kvarts. Bl\u00E5skiffer bildas oftast i milj\u00F6er med h\u00F6gt tryck och relativt l\u00E5ga temperaturer av ursprungsbergarter med basisk sammans\u00E4ttning. Bl\u00E5skiffer finns l\u00E4ngs i Toscana i Italien. Gr\u00F6nskiffer \u00E4r en bergart som liknar bl\u00E5skiffer."@sv . . . "Scisto blu"@it . . . . . . . . . . . . . "Le schiste bleu (ou glaucophanite, ou schiste \u00E0 glaucophane) est une roche m\u00E9tamorphique caract\u00E9ris\u00E9e par la pr\u00E9sence de glaucophane (couleur bleue) et de mica blancs. Elle pr\u00E9sente des tons bleu\u00E2tres ou l\u00E9g\u00E8rement violets. Son composant principal est le glaucophane, mais elle peut aussi pr\u00E9senter une grande vari\u00E9t\u00E9 de min\u00E9raux accessoires (calcite, grenat, quartz\u2026).Les schistes bleus sont des marqueurs de la subduction de la plaque oc\u00E9anique sous la plaque continentale."@fr . . . . . "\u85CD\u7247\u5CA9\uFF08\u82F1\u8A9E\uFF1Ablueschist\uFF09\u4E5F\u7A31\u70BA\u85CD\u9583\u77F3\u7247\u5CA9\uFF0C\u662F\u4E00\u7A2E\u5728\u9AD8\u58D3\u548C\u4F4E\u6EAB\uFF08200\uFF0D500 \u00B0C\uFF08392\uFF0D932 \u00B0F\uFF09\uFF09\u4E0B\u8B8A\u8CEA\u5F62\u6210\u7684\u8B8A\u8CEA\u5CA9\u3002\u5927\u7D04\u5C0D\u61C9\u65BC 15-30 \u516C\u91CC\uFF089.3-18.6 \u82F1\u91CC\uFF09\u7684\u6DF1\u5EA6\u3002\u5CA9\u77F3\u7684\u85CD\u8272\u4F86\u81EA\u4E3B\u8981\u7926\u7269\u84DD\u95EA\u77F3\u548C\u786C\u67F1\u77F3\u3002\u85CD\u7247\u5CA9\u901A\u5E38\u5728\u9020\u5C71\u5E36\u4E2D\u767C\u73FE\uFF0C\u9694\u65B7\u5C64\u5076\u5C14\u8207\u7DA0\u7247\u5CA9\u6216\u8207\u69B4\u8F1D\u5CA9\u63A5\u89F8\u3002 \u85CD\u7247\u5CA9\u76F8\u4E2D\u7684\u5CA9\u77F3\u7926\u7269\u6210\u5206\u56E0\u539F\u5CA9\u800C\u6709\u6240\u4E0D\u540C\u3002 \u7384\u6B66\u5CA9\uFF1A\u85CD\u9583\u77F3 + \u786C\u67F1\u77F3\u548C/\u6216\u7DA0\u7C3E\u77F3 + \u9209\u9577\u77F3 + \u9226\u77F3 +/- \u77F3\u69B4\u77F3 +/- \u77F3\u82F1\u786C\u7389 + \u77F3\u82F1 \u8D85\u9382\u9435\u8CEA\u5CA9\u77F3\uFF1A\u86C7\u7D0B\u5CA9/ +/- \u6ED1\u77F3 +/- \u9EDD\u7C3E\u77F3 \u6CE5\u8CEA\u5CA9\uFF1AFe-Mg-carpholite +/- \u7DA0\u6CE5\u77F3 +/- \u85CD\u6676\u77F3 +/- \u9209\u9577\u77F3 +/- \u77F3\u82F1 +/- \u6ED1\u77F3 +/- \u77F3\u69B4\u77F3 \u82B1\u5D17\u5CA9\uFF1A\u85CD\u6676\u77F3 +/- \u767D\u96F2\u77F3 +/- \u7DA0\u6CE5\u77F3 +/- \u9209\u9577\u77F3 +/- \u77F3\u82F1 +/- \u767D\u96F2\u6BCD \u77F3\u7070\u77F3\u548C\u5927\u7406\u77F3\uFF1A\u65B9\u89E3\u77F3\u5728\u9AD8\u58D3\u4E0B\u8F49\u8B8A\u70BA\u6587\u77F3\uFF0C\u4F46\u901A\u5E38\u5728\u6316\u6398\u6642\u6062\u5FA9\u70BA\u65B9\u89E3\u77F3\u3002"@zh . . . . "Modr\u00E1 b\u0159idlice nebo glaukofanit nebo glaukofanov\u00E1 b\u0159idlice je p\u0159em\u011Bn\u011Bn\u00E1 hornina typick\u00E1 pro vysokotlakou a n\u00EDzkoteplotn\u00ED metamorf\u00F3zu, kter\u00E1 p\u0159edstavuje . Term\u00EDn glaukofanit zavedl roce 1888 chorvatsk\u00FD geolog . Term\u00EDn modr\u00E1 b\u0159idlice zavedl v roce 1962 americk\u00FD geolog United States Geological Survey Edgar Bailey."@cs . . . "Blauschiefer oder Glaukophanschiefer sind oft bl\u00E4ulich gef\u00E4rbte Gesteine, die eine Metamorphose bei relativ niedrigen Temperaturen und hohen Dr\u00FCcken erlitten haben (kleiner 400 \u00B0C GPa\u22121). Solche Gesteine finden sich aufgrund des immer k\u00FChler werdenden Erdmantels und der dar\u00FCber liegenden Erdkruste haupts\u00E4chlich in aktiven oder ehemaligen Subduktionszonen von maximal neoproterozoischem Alter (0,8 Mrd. Jahre BP) oder j\u00FCnger. Die bl\u00E4uliche Farbe wird durch das Mineral Glaukophan, einen Amphibol, hervorgerufen, der aber nicht immer vorhanden ist, sodass Blauschiefer nicht zwingend bl\u00E4ulich gef\u00E4rbt sind. Die Blauschiefer sind kennzeichnend f\u00FCr Gesteine, die eine Metamorphose erfahren haben, sodass nach ihnen die sogenannte Blauschiefer-Fazies (siehe auch metamorphe Fazies) benannt ist."@de . . . . . . . "Lo scisto blu \u00E8 una roccia metamorfica contenente un tipo di anfibolo blu, chiamato glaucofane, che si sviluppa quando il protolito (basalto o peridotite) viene sottoposto a grandi sforzi differenziali, pur mantenendo una temperatura relativamente bassa."@it . . "Le schiste bleu (ou glaucophanite, ou schiste \u00E0 glaucophane) est une roche m\u00E9tamorphique caract\u00E9ris\u00E9e par la pr\u00E9sence de glaucophane (couleur bleue) et de mica blancs. Elle pr\u00E9sente des tons bleu\u00E2tres ou l\u00E9g\u00E8rement violets. Son composant principal est le glaucophane, mais elle peut aussi pr\u00E9senter une grande vari\u00E9t\u00E9 de min\u00E9raux accessoires (calcite, grenat, quartz\u2026).Les schistes bleus sont des marqueurs de la subduction de la plaque oc\u00E9anique sous la plaque continentale."@fr . . . . . . . . . . "\u0421\u043B\u0430\u043D\u0446\u0456 \u0431\u043B\u0430\u043A\u0438\u0442\u043D\u0456 (\u0440\u043E\u0441. \u0441\u043B\u0430\u043D\u0446\u044B \u0433\u043E\u043B\u0443\u0431\u044B\u0435, \u0430\u043D\u0433\u043B. blue schistes, \u043D\u0456\u043C. blaue Schiefer m) \u2014 \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 \u0430\u0431\u043E \u043C\u0435\u0442\u0430\u043C\u043E\u0440\u0444\u0456\u0447\u043D\u0430 \u0444\u0430\u0446\u0456\u044F, \u044F\u043A\u0430 \u0445\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u0438\u0437\u0443\u0454\u0442\u044C\u0441\u044F \u0430\u0441\u043E\u0446\u0456\u0430\u0446\u0456\u0454\u044E \u043D\u0438\u0437\u044C\u043A\u043E\u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u043D\u0438\u0445 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432 \u0432\u0438\u0441\u043E\u043A\u043E\u0433\u043E \u0442\u0438\u0441\u043A\u0443. \u0412\u0432\u0430\u0436\u0430\u0454\u0442\u044C\u0441\u044F, \u0449\u043E \u0421\u043B\u0430\u043D\u0446\u0456 \u0431\u043B\u0430\u043A\u0438\u0442\u043D\u0456 \u0444\u043E\u0440\u043C\u0443\u044E\u0442\u044C\u0441\u044F, \u0433\u043E\u043B\u043E\u0432\u043D\u0438\u043C \u0447\u0438\u043D\u043E\u043C, \u0432 \u0445\u043E\u043B\u043E\u0434\u043D\u0438\u0445 \u043B\u0456\u0442\u043E\u0441\u0444\u0435\u0440\u043D\u0438\u0445 \u043F\u043B\u0438\u0442\u0430\u0445 \u0432 \u0437\u043E\u043D\u0430\u0445 \u0441\u0443\u0431\u0434\u0443\u043A\u0446\u0456\u0457."@uk . . "Esquist blau"@ca . "Blauschiefer oder Glaukophanschiefer sind oft bl\u00E4ulich gef\u00E4rbte Gesteine, die eine Metamorphose bei relativ niedrigen Temperaturen und hohen Dr\u00FCcken erlitten haben (kleiner 400 \u00B0C GPa\u22121). Solche Gesteine finden sich aufgrund des immer k\u00FChler werdenden Erdmantels und der dar\u00FCber liegenden Erdkruste haupts\u00E4chlich in aktiven oder ehemaligen Subduktionszonen von maximal neoproterozoischem Alter (0,8 Mrd. Jahre BP) oder j\u00FCnger. Die bl\u00E4uliche Farbe wird durch das Mineral Glaukophan, einen Amphibol, hervorgerufen, der aber nicht immer vorhanden ist, sodass Blauschiefer nicht zwingend bl\u00E4ulich gef\u00E4rbt sind. Die Blauschiefer sind kennzeichnend f\u00FCr Gesteine, die eine Metamorphose erfahren haben, sodass nach ihnen die sogenannte Blauschiefer-Fazies (siehe auch metamorphe Fazies) benannt ist."@de . . . . . "Schiste bleu"@fr .