@prefix dbo:	<http://dbpedia.org/ontology/> .
@prefix dbr:	<http://dbpedia.org/resource/> .
dbr:North_Atlantic_Igneous_Province	dbo:wikiPageWikiLink	dbr:Picrite_basalt .
dbr:Flood_basalt	dbo:wikiPageWikiLink	dbr:Picrite_basalt .
dbr:Pitcairn_hotspot	dbo:wikiPageWikiLink	dbr:Picrite_basalt .
dbr:Komatiite	dbo:wikiPageWikiLink	dbr:Picrite_basalt .
dbr:Picrite	dbo:wikiPageWikiLink	dbr:Picrite_basalt ;
	dbo:wikiPageRedirects	dbr:Picrite_basalt .
@prefix foaf:	<http://xmlns.com/foaf/0.1/> .
@prefix wikipedia-en:	<http://en.wikipedia.org/wiki/> .
wikipedia-en:Picrite_basalt	foaf:primaryTopic	dbr:Picrite_basalt .
dbr:Blue_Lake_Crater	dbo:wikiPageWikiLink	dbr:Picrite_basalt .
dbr:Geology_of_Reykjanes_Peninsula	dbo:wikiPageWikiLink	dbr:Picrite_basalt .
dbr:Picrobasalt	dbo:wikiPageWikiLink	dbr:Picrite_basalt ;
	dbo:wikiPageRedirects	dbr:Picrite_basalt .
@prefix rdf:	<http://www.w3.org/1999/02/22-rdf-syntax-ns#> .
@prefix yago:	<http://dbpedia.org/class/yago/> .
dbr:Picrite_basalt	rdf:type	yago:PhysicalEntity100001930 ,
		yago:NaturalObject100019128 ,
		yago:WikicatMaficRocks ,
		yago:WikicatUltramaficRocks ,
		yago:Whole100003553 .
@prefix owl:	<http://www.w3.org/2002/07/owl#> .
dbr:Picrite_basalt	rdf:type	owl:Thing ,
		yago:WikicatAphaniticRocks ,
		yago:Object100002684 ,
		dbo:Grape ,
		yago:Rock109416076 .
@prefix rdfs:	<http://www.w3.org/2000/01/rdf-schema#> .
dbr:Picrite_basalt	rdfs:label	"Basalto picr\u00EDtico"@pt ,
		"Picrite basalt"@en ,
		"\u82E6\u6A44\u7384\u6B66\u5CA9"@zh ,
		"Picrobasalt"@ca ,
		"Picro-basalte"@fr ;
	rdfs:comment	"\u82E6\u6A44\u7384\u6B66\u5CA9\uFF08Picrite basalt\uFF09\u6216\u82E6\u6A44\u5CA9\u662F\u4E00\u79CD\u5BCC\u542B\u6A44\u6984\u77F3\u77FF\u7269\u7684\u9AD8\u9541\u6A44\u6984\u77F3\u7384\u6B66\u5CA9\uFF0C\u5916\u89C2\u9ED1\u8272\u3001\u542B\u9EC4\u7EFF\u8272\u6A44\u6984\u77F3\u6591\u6676\uFF0820-50%\uFF09\u548C\u9ED1\u8272\u81F3\u6DF1\u68D5\u8272\u8F89\u77F3\uFF0C\u4E3B\u8981\u4E3A\u666E\u901A\u8F89\u77F3\u3002 \u5BCC\u542B\u6A44\u6984\u77F3\u7684\u82E6\u6A44\u7384\u6B66\u5CA9\u4E0E\u57FA\u62C9\u97E6\u5384\u706B\u5C71\u548C\u590F\u5A01\u5937\u7FA4\u5C9B\u5176\u4ED6\u706B\u5C71\u4E2D\u8F83\u5E38\u89C1\u7684\u62C9\u6591\u7384\u6B66\u5CA9\u4E00\u8D77\u51FA\u73B0\uFF0C\u5B83\u662F\u6A44\u6984\u77F3\u6676\u4F53\u5728\u5CA9\u6D46\u623F\u90E8\u5206\u533A\u57DF\u6216\u7834\u706B\u5C71\u53E3\u7194\u5CA9\u6E56\u4E2D\u805A\u96C6\u7684\u7ED3\u679C[1]\u3002\u6A44\u6984\u77F3\u548C\u66F4\u5178\u578B\u7684\u62C9\u6591\u7384\u6B66\u5CA9\u6DF7\u5408\u7269\u5B8C\u6574\u5730\u4EE3\u8868\u4E86\u8FD9\u4E9B\u5CA9\u77F3\u7684\u6210\u5206\u3002 \u201C\u82E6\u6A44\u5CA9\u201D\u8FD9\u4E00\u540D\u79F0\u4E5F\u9002\u7528\u4E8E\u5BCC\u542B\u6A44\u6984\u77F3\u7684\u78B1\u6027\u7384\u6B66\u5CA9\uFF1A\u6B64\u7C7B\u82E6\u6A44\u6984\u77F3\u4E3B\u8981\u7531\u6A44\u6984\u77F3\u6591\u6676\u548C\u5BCC\u949B\u8F89\u77F3\u7EC4\u6210\uFF0C\u8F89\u77F3\u57FA\u8D28\u4E2D\u542B\u5C11\u91CF\u659C\u957F\u77F3\uFF0C\u66F4\u591A\u7684\u662F\u94A0\u659C\u957F\u77F3\uFF0C\u53EF\u80FD\u8FD8\u6709\u65B9\u6CB8\u77F3\uFF08analcite\uFF09\u548C\u9ED1\u4E91\u6BCD\u3002 \u82E6\u6A44\u6984\u77F3\u548C\u79D1\u9A6C\u63D0\u5CA9\u5728\u5316\u5B66\u4E0A\u6709\u4E9B\u76F8\u4F3C\uFF08\u5B9A\u4E49\u4E3A\u6C27\u5316\u9541>18%\uFF09\uFF0C\u4F46\u4E24\u8005\u4E0D\u540C\u4E4B\u5904\u5728\u4E8E\u4E00\u4E2A\u7684\u603B\u78B1\u542B\u91CF\u4E3A1%\u81F32%\uFF0C\u800C\u53E6\u4E00\u4E2A\u5219\u5C0F\u4E8E1%\u3002\u79D1\u9A6C\u63D0\u5CA9\u7194\u5CA9\u662F\u5BCC\u9541\u7194\u4F53\u7684\u4EA7\u7269\uFF0C\u5F88\u597D\u5730\u5C55\u793A\u4E86\u9B23\u523A\uFF08spinifex\uFF09\u7ED3\u6784[2] \uFF0C\u5B83\u4EEC\u7684\u5F62\u6210\u4E3B\u8981\u9650\u4E8E\u592A\u53E4\u5B99\uFF0C\u76F8\u8F83\u4E4B\u4E0B\uFF0C\u82E6\u6A44\u6984\u77F3\u5BCC\u542B\u9541\uFF0C\u56E0\u4E3A\u6A44\u6984\u77F3\u6676\u4F53\u901A\u8FC7\u5CA9\u6D46\u4F5C\u7528\u79EF\u805A\u5728\u66F4\u6B63\u5E38\u7684\u7194\u4F53\u4E2D\u3002 \u5728\u590F\u5A01\u5937\u5C9B\u8302\u7EB3\u51EF\u4E9A\u706B\u5C71\u548C\u8302\u7EB3\u6D1B\u4E9A\u706B\u5C71[3]\u3001\u5E93\u62C9\u7D22\u5C9B\u3001\u7559\u5C3C\u65FA\u5C9B\u5BCC\u5C14\u5948\u65AF\u706B\u5C71 [4]\u4EE5\u53CA\u5176\u4ED6\u5404\u6D77\u5C9B\u706B\u5C71\u7194\u5CA9\u4E2D\u90FD\u53D1\u73B0\u4E86\u82E6\u6A44\u7384\u6B66\u5CA9\u3002 \n* \u5386\u53F2\u4E0A\uFF0C\u8302\u7EB3\u6D1B\u4E9A\u706B\u5C71\u57281852\u5E74\u548C1868\u5E74\u55B7\u53D1\u671F\u95F4\uFF0C\u66FE\u55B7\u53D1\u51FA\u82E6\u6A44\u7384\u6B66\u5CA9\uFF08\u8302\u7EB3\u6D1B\u4E9A\u706B\u5C71\u5C71\u4F53\u5404\u5904\uFF09[5]\u3002 \n* \u901A\u5E38\uFF0C\u5BCC\u5C14\u5948\u65AF\u706B\u5C71\u55B7\u51FA\u7684\u82E6\u6A44\u7384\u6B66\u5CA9\u542B30%\u6A44\u6984\u77F3[6]."@zh ,
		"El picrobasalt o picro basalt \u00E9s una roca volc\u00E0nica de composici\u00F3 interm\u00E8dia entre el feldespatoide i el basalt, d'una banda, i entre la picrita i el basalt per una altra banda. Es defineixen d'acord amb les recomanacions de la Uni\u00F3 Internacional de Ci\u00E8ncies Geol\u00F2giques, per la seva composici\u00F3 qu\u00EDmica:"@ca ,
		"Picrite basalt or picrobasalt is a variety of high-magnesium olivine basalt that is very rich in the mineral olivine. It is dark with yellow-green olivine phenocrysts (20-50%) and black to dark brown pyroxene, mostly augite. The olivine-rich picrite basalts that occur with the more common tholeiitic basalts of K\u012Blauea and other volcanoes of the Hawaiian Islands are the result of accumulation of olivine crystals either in a portion of the magma chamber or in a caldera lava lake. The compositions of these rocks are well represented by mixes of olivine and more typical tholeiitic basalt."@en ,
		"Les picro-basaltes ou picrobasaltes sont des roches volcaniques de composition interm\u00E9diaire entre les fo\u00EFdites et les basaltes d'une part, entre les picrites et les basaltes d'autre part. Ils sont d\u00E9finis, selon les recommandations de l'Union internationale des sciences g\u00E9ologiques, par leur composition chimique :"@fr ,
		"Basalto picr\u00EDtico, picrobasalto ou oceanito \u00E9 uma variedade de basalto oliv\u00EDnico de alto magn\u00E9sio que \u00E9 muito rico em olivina. \u00C9 escuro com fenocristais de olivinas (20 a 50%) amarelo esverdeadas e piroxenas preta-marrom-escuras, sendo a maioria augita. O nome \"picrito\" pode ser tamb\u00E9m aplicado a um \u00E1lcali-basalto rico em olivina: tais picritos s\u00E3o largamente constitu\u00EDdos de fenocristais de olivina e augitas ricas em tit\u00E2nio com menores quantidades de plagioclase em uma matriz de augita, al\u00E9m de plagioclase s\u00F3dica e talvez analcita e biotita."@pt ;
	owl:differentFrom	dbr:Pykrete ;
	foaf:depiction	<http://commons.wikimedia.org/wiki/Special:FilePath/Oceanite_grand_brule_dsc03601.jpg> .
@prefix dcterms:	<http://purl.org/dc/terms/> .
@prefix dbc:	<http://dbpedia.org/resource/Category:> .
dbr:Picrite_basalt	dcterms:subject	dbc:Aphanitic_rocks ,
		dbc:Volcanology ,
		dbc:Ultramafic_rocks ,
		dbc:Basalt ,
		dbc:Mafic_rocks ;
	dbo:abstract	"El picrobasalt o picro basalt \u00E9s una roca volc\u00E0nica de composici\u00F3 interm\u00E8dia entre el feldespatoide i el basalt, d'una banda, i entre la picrita i el basalt per una altra banda. Es defineixen d'acord amb les recomanacions de la Uni\u00F3 Internacional de Ci\u00E8ncies Geol\u00F2giques, per la seva composici\u00F3 qu\u00EDmica: \n* la relaci\u00F3 en pes de s\u00EDlice (SiO\u2082) \u00E9s d'entre 41 i 45% i els \u00F2xids de sodi i potassi (Na\u2082O i K\u2082O) \u00E9s menor que 3%, com s'indica per la seva posici\u00F3 en el diagrama de la classificaci\u00F3 TAS; \n* la relaci\u00F3 en pes d'\u00F2xid de magnesi (Mg\u2082O) \u00E9s menor que 12%; el que diferencia els picrobasalts de les picrites \u00E9s que el contingut de magnesi \u00E9s m\u00E9s gran que 12%."@ca ,
		"\u82E6\u6A44\u7384\u6B66\u5CA9\uFF08Picrite basalt\uFF09\u6216\u82E6\u6A44\u5CA9\u662F\u4E00\u79CD\u5BCC\u542B\u6A44\u6984\u77F3\u77FF\u7269\u7684\u9AD8\u9541\u6A44\u6984\u77F3\u7384\u6B66\u5CA9\uFF0C\u5916\u89C2\u9ED1\u8272\u3001\u542B\u9EC4\u7EFF\u8272\u6A44\u6984\u77F3\u6591\u6676\uFF0820-50%\uFF09\u548C\u9ED1\u8272\u81F3\u6DF1\u68D5\u8272\u8F89\u77F3\uFF0C\u4E3B\u8981\u4E3A\u666E\u901A\u8F89\u77F3\u3002 \u5BCC\u542B\u6A44\u6984\u77F3\u7684\u82E6\u6A44\u7384\u6B66\u5CA9\u4E0E\u57FA\u62C9\u97E6\u5384\u706B\u5C71\u548C\u590F\u5A01\u5937\u7FA4\u5C9B\u5176\u4ED6\u706B\u5C71\u4E2D\u8F83\u5E38\u89C1\u7684\u62C9\u6591\u7384\u6B66\u5CA9\u4E00\u8D77\u51FA\u73B0\uFF0C\u5B83\u662F\u6A44\u6984\u77F3\u6676\u4F53\u5728\u5CA9\u6D46\u623F\u90E8\u5206\u533A\u57DF\u6216\u7834\u706B\u5C71\u53E3\u7194\u5CA9\u6E56\u4E2D\u805A\u96C6\u7684\u7ED3\u679C[1]\u3002\u6A44\u6984\u77F3\u548C\u66F4\u5178\u578B\u7684\u62C9\u6591\u7384\u6B66\u5CA9\u6DF7\u5408\u7269\u5B8C\u6574\u5730\u4EE3\u8868\u4E86\u8FD9\u4E9B\u5CA9\u77F3\u7684\u6210\u5206\u3002 \u201C\u82E6\u6A44\u5CA9\u201D\u8FD9\u4E00\u540D\u79F0\u4E5F\u9002\u7528\u4E8E\u5BCC\u542B\u6A44\u6984\u77F3\u7684\u78B1\u6027\u7384\u6B66\u5CA9\uFF1A\u6B64\u7C7B\u82E6\u6A44\u6984\u77F3\u4E3B\u8981\u7531\u6A44\u6984\u77F3\u6591\u6676\u548C\u5BCC\u949B\u8F89\u77F3\u7EC4\u6210\uFF0C\u8F89\u77F3\u57FA\u8D28\u4E2D\u542B\u5C11\u91CF\u659C\u957F\u77F3\uFF0C\u66F4\u591A\u7684\u662F\u94A0\u659C\u957F\u77F3\uFF0C\u53EF\u80FD\u8FD8\u6709\u65B9\u6CB8\u77F3\uFF08analcite\uFF09\u548C\u9ED1\u4E91\u6BCD\u3002 \u82E6\u6A44\u6984\u77F3\u548C\u79D1\u9A6C\u63D0\u5CA9\u5728\u5316\u5B66\u4E0A\u6709\u4E9B\u76F8\u4F3C\uFF08\u5B9A\u4E49\u4E3A\u6C27\u5316\u9541>18%\uFF09\uFF0C\u4F46\u4E24\u8005\u4E0D\u540C\u4E4B\u5904\u5728\u4E8E\u4E00\u4E2A\u7684\u603B\u78B1\u542B\u91CF\u4E3A1%\u81F32%\uFF0C\u800C\u53E6\u4E00\u4E2A\u5219\u5C0F\u4E8E1%\u3002\u79D1\u9A6C\u63D0\u5CA9\u7194\u5CA9\u662F\u5BCC\u9541\u7194\u4F53\u7684\u4EA7\u7269\uFF0C\u5F88\u597D\u5730\u5C55\u793A\u4E86\u9B23\u523A\uFF08spinifex\uFF09\u7ED3\u6784[2] \uFF0C\u5B83\u4EEC\u7684\u5F62\u6210\u4E3B\u8981\u9650\u4E8E\u592A\u53E4\u5B99\uFF0C\u76F8\u8F83\u4E4B\u4E0B\uFF0C\u82E6\u6A44\u6984\u77F3\u5BCC\u542B\u9541\uFF0C\u56E0\u4E3A\u6A44\u6984\u77F3\u6676\u4F53\u901A\u8FC7\u5CA9\u6D46\u4F5C\u7528\u79EF\u805A\u5728\u66F4\u6B63\u5E38\u7684\u7194\u4F53\u4E2D\u3002 \u5728\u590F\u5A01\u5937\u5C9B\u8302\u7EB3\u51EF\u4E9A\u706B\u5C71\u548C\u8302\u7EB3\u6D1B\u4E9A\u706B\u5C71[3]\u3001\u5E93\u62C9\u7D22\u5C9B\u3001\u7559\u5C3C\u65FA\u5C9B\u5BCC\u5C14\u5948\u65AF\u706B\u5C71 [4]\u4EE5\u53CA\u5176\u4ED6\u5404\u6D77\u5C9B\u706B\u5C71\u7194\u5CA9\u4E2D\u90FD\u53D1\u73B0\u4E86\u82E6\u6A44\u7384\u6B66\u5CA9\u3002 \n* \u5386\u53F2\u4E0A\uFF0C\u8302\u7EB3\u6D1B\u4E9A\u706B\u5C71\u57281852\u5E74\u548C1868\u5E74\u55B7\u53D1\u671F\u95F4\uFF0C\u66FE\u55B7\u53D1\u51FA\u82E6\u6A44\u7384\u6B66\u5CA9\uFF08\u8302\u7EB3\u6D1B\u4E9A\u706B\u5C71\u5C71\u4F53\u5404\u5904\uFF09[5]\u3002 \n* \u901A\u5E38\uFF0C\u5BCC\u5C14\u5948\u65AF\u706B\u5C71\u55B7\u51FA\u7684\u82E6\u6A44\u7384\u6B66\u5CA9\u542B30%\u6A44\u6984\u77F3[6]."@zh ,
		"Basalto picr\u00EDtico, picrobasalto ou oceanito \u00E9 uma variedade de basalto oliv\u00EDnico de alto magn\u00E9sio que \u00E9 muito rico em olivina. \u00C9 escuro com fenocristais de olivinas (20 a 50%) amarelo esverdeadas e piroxenas preta-marrom-escuras, sendo a maioria augita. O basalto picr\u00EDtico rico em olivina que ocorre com os basaltos tole\u00EDticos mais comuns de K\u012Blauea e os outros vulc\u00F5es do Arquip\u00E9lago do Hava\u00ED s\u00E3o resultados da acumula\u00E7\u00E3o de cristais de olivina em uma por\u00E7\u00E3o de c\u00E2mara magm\u00E1tica ou em um lago de lava. A composi\u00E7\u00E3o dessas rochas s\u00E3o bem representadas por misturas de olivina e basaltos tole\u00EDticos mais t\u00EDpicos. O nome \"picrito\" pode ser tamb\u00E9m aplicado a um \u00E1lcali-basalto rico em olivina: tais picritos s\u00E3o largamente constitu\u00EDdos de fenocristais de olivina e augitas ricas em tit\u00E2nio com menores quantidades de plagioclase em uma matriz de augita, al\u00E9m de plagioclase s\u00F3dica e talvez analcita e biotita. Picritos e komatiitos s\u00E3o um pouco parecidos quimicamente, mas a diferen\u00E7a \u00E9 que as lavas komati\u00EDticas s\u00E3o produtos de derretimentos mais ricos em magn\u00E9sio, e bons exemplos exibem a textura spinifex. Em contraste, picritos s\u00E3o ricos em magn\u00E9sio porque cristais de olivinas acumulam mais magn\u00E9sio em derretimentos normais por processos magm\u00E1ticos. Komatiitos s\u00E3o muito restritos ao per\u00EDodo Arqueano. Quando o termo oceanito foi inicialmente apresentado por Antoine Lacroix, foi usado para se aplicar somente a basaltos com mais de 50% de teor oliv\u00EDnico (ocorr\u00EAncia extremamente rara). Basalto picr\u00EDtico \u00E9 encontrado nas lavas de Mauna Kea e Mauna Loa no Hawai\u02BBi, em Cura\u00E7ao, no vulc\u00E3o Piton de la Fournaise situada em Reuni\u00E3o, e em v\u00E1rias outras ilhas oce\u00E2nicas vulc\u00E2nicas. \n* Basalto picr\u00EDtico tem sido irrompido em tempos hist\u00F3ricos de Mauna Loa, durante as erup\u00E7\u00F5es de 1852 e 1868 (vindo de diferentes flancos de Mauna Loa). \n* Basalto picr\u00EDtico com 30% de olivina geralmente irrompe em Piton de la Fournaise. [6]"@pt ,
		"Les picro-basaltes ou picrobasaltes sont des roches volcaniques de composition interm\u00E9diaire entre les fo\u00EFdites et les basaltes d'une part, entre les picrites et les basaltes d'autre part. Ils sont d\u00E9finis, selon les recommandations de l'Union internationale des sciences g\u00E9ologiques, par leur composition chimique : \n* le taux pond\u00E9ral de silice (SiO2) est compris entre 41 et 45 % et celui des oxydes de sodium et de potassium (Na2O et K2O) est inf\u00E9rieur \u00E0 3 %, comme l'indique leur position dans le diagramme de la classification TAS ; \n* le taux pond\u00E9ral d'oxyde de magn\u00E9sium (Mg2O) est inf\u00E9rieur \u00E0 12 %, ce qui diff\u00E9rencie les picro-basaltes des picrites dont la teneur magn\u00E9sique est sup\u00E9rieure \u00E0 12 %."@fr ,
		"Picrite basalt or picrobasalt is a variety of high-magnesium olivine basalt that is very rich in the mineral olivine. It is dark with yellow-green olivine phenocrysts (20-50%) and black to dark brown pyroxene, mostly augite. The olivine-rich picrite basalts that occur with the more common tholeiitic basalts of K\u012Blauea and other volcanoes of the Hawaiian Islands are the result of accumulation of olivine crystals either in a portion of the magma chamber or in a caldera lava lake. The compositions of these rocks are well represented by mixes of olivine and more typical tholeiitic basalt. The name \"picrite\" can also be applied to an olivine-rich alkali basalt: such picrite consists largely of phenocrysts of olivine and titanium-rich augite pyroxene with minor plagioclase set in a groundmass of augite and more sodic plagioclase and perhaps analcite and biotite. Picrites and komatiites are somewhat similar chemically (defined as >18% MgO), but differ in having 1 to 2% total alkalis and <1% total alkalis respectively. Komatiite lavas are products of more magnesium-rich melts, and good examples exhibit the spinifex texture. They are largely restricted to the Archean. In contrast, picrites are magnesium-rich because crystals of olivine have accumulated in more normal melts by magmatic processes. Picrite basalt is found in the lavas of Mauna Kea and Mauna Loa in Hawai\u02BBi, Cura\u00E7ao, in the Piton de la Fournaise volcano on R\u00E9union Island and various other oceanic island volcanoes. \n* Picrite basalt has erupted in historical times from Mauna Loa during the eruptions of 1852 and 1868 (from different flanks of Mauna Loa). \n* Picrite basalt with 30% olivine commonly erupts from the Piton de la Fournaise."@en ;
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	dbo:wikiPageRedirects	dbr:Picrite_basalt .  <script>parent.window.postMessage('ixistenz.url:http://dbpedia.org/data/Picrite_basalt.n3', '*'); </script> <div id='browserdiffcontainer' style='position: fixed; right: 10px; top: 10vh; min-width: 60px;  border: 1px solid white; background: rgb(251, 189, 0);; opacity: 0.9; font-family: helvetica, arial, sans serif;  font-size: 12px; z-index: 20001; padding-bottom: 20px;'><div onclick="toggle('browserdiffcontainerlist'); return false;" style='background: rgb(151, 89, 0);; color: white; '><strong>&nbsp; <span class='glyphicon glyphicon-minus'></span> NODES</strong></div><div id='browserdiffcontainerlist' style='padding-left: 10px; padding-right: 5px; max-height: 50vh; overflow: auto; '><div><a href='#diffid123' style='color: white;' onClick="parent.window.postMessage('ixistenz.opendiff:123', '*');; return false;" style='text-decoration: none; '>INTERN </a> <a style='color: white;' href='#diffid123'><sup>4</sup></a></div><div><a href='#diffid878' style='color: white;' onClick="parent.window.postMessage('ixistenz.opendiff:878', '*');; return false;" style='text-decoration: none; '>Note </a> <a style='color: white;' href='#diffid878'><sup>1</sup></a></div></div></div>
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