@prefix dbo: . @prefix dbr: . dbr:List_of_flood_basalt_provinces dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Cenomanian-Turonian_boundary_event dbo:wikiPageWikiLink dbr:Large_igneous_province . dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Madagascar_flood_basalt dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Snowball_Earth dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Tristan_hotspot dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Caribbean_large_igneous_province dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:North_Atlantic_Igneous_Province dbo:wikiPageWikiLink dbr:Large_igneous_province . dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Matachewan_dike_swarm dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Chilcotin_Group dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Ontong_Java_Plateau dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Ungava_magmatic_event dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Wrangellia_Terrane dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Long_Range_dikes dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Anoxic_event dbo:wikiPageWikiLink dbr:Large_igneous_province . dbr:Siberian_Traps dbo:wikiPageWikiLink dbr:Large_igneous_province . @prefix rdf: . @prefix yago: . dbr:Large_igneous_province rdf:type yago:PhysicalEntity100001930 , yago:Relation100031921 , yago:VolcanicRock114933314 , yago:IgneousRock114931879 , yago:WikicatFloodBasalts , yago:Substance100019613 , yago:Matter100020827 , yago:Material114580897 . @prefix owl: . dbr:Large_igneous_province rdf:type owl:Thing , yago:Abstraction100002137 , yago:Part113809207 , yago:Rock114696793 , yago:Basalt114773022 , yago:WikicatIgneousRocks . @prefix rdfs: . dbr:Large_igneous_province rdfs:label "\u0422\u0440\u0430\u043F\u043E\u0432\u0430 \u0444\u043E\u0440\u043C\u0430\u0446\u0456\u044F"@uk , "Gran provincia \u00EDgnea"@es , "\uAC70\uB300 \uD654\uC131\uC554 \uC9C0\uB300"@ko , "Large igneous province"@en , "Magmatische Gro\u00DFprovinz"@de , "\u0625\u0642\u0644\u064A\u0645 \u0646\u0627\u0631\u064A \u0643\u0628\u064A\u0631"@ar , "Large igneous province"@nl , "\u5DE8\u5927\u706B\u6210\u5CA9\u5CA9\u77F3\u533A"@ja , "Grande provincia ignea"@it , "Grande prov\u00EDncia \u00EDgnea"@pt , "\u5927\u578B\u706B\u6210\u5CA9\u533A\u57DF"@zh , "Large Igneous Provinces"@pt , "Du\u017Ca prowincja magmatyczna"@pl , "Province magmatique"@fr ; rdfs:comment "Uma Grande prov\u00EDncia \u00EDgnea \u00E9 o resultado de ac\u00FAmulo de rochas \u00EDgneas em \u00E1reas extremamente grandes (acima de 100 mil quil\u00F4metros quadrados. As rochas resultantes incluem tanto rochas intrusivass como soleira quanto rochas rochas extrusivas, como fluxos delava e dep\u00F3sitos de piroclastos), surgidas quando o magma extravasa na superf\u00EDcie, em tempos geol\u00F3gicos relativamente curtos.No Brasil, o maior exemplo de uma grande prov\u00EDncia \u00EDgnea \u00E9 a Prov\u00EDncia magm\u00E1tica do Paran\u00E1-Etendeka, que uma prov\u00EDncia formadas principalmente por basaltos depositados sobre a crosta continental da Am\u00E9rica do Sul, na Bacia do Paran\u00E1, e que se estende at\u00E9 a Nam\u00EDbia, com mais de 1,2 milh\u00F5es de quil\u00F4metros quadrados. A Prov\u00EDncia magm\u00E1tica do Paran\u00E1-Etendeka est\u00E1 relacionado \u00E0 abertura do Oceano Atl\u00E2ntico Sul, durante a "@pt , "\uAC70\uB300 \uD654\uC131\uC554 \uC9C0\uB300(\u5DE8\u5927\u706B\u6210\u5DD6\u5730\u5E36, \uC601\uC5B4: Large Igneous Province)\uB294 \uB9E4\uC6B0 \uAC70\uB300\uD558\uAC8C \uC313\uC544\uC9C4 \uD654\uC131\uC554 \uC9C0\uB300\uB85C, \uC5EC\uAE30\uC5D4 \uC62C\uB77C\uC628 \uB9C8\uADF8\uB9C8\uAC00 \uD45C\uBA74\uC744 \uD6D1\uC73C\uBA74\uC11C \uB9CC\uB4E4\uC5B4\uC9C4 \uD3C9\uD589, \uC218\uD3C9\uD55C \uD310\uC0C1 \uAD00\uC785\uC554\uCCB4 \uD639\uC740 \uC81C\uBC29, \uADF8\uB9AC\uACE0 \uBD84\uCD9C\uBB3C (\uC6A9\uC554 \uD750\uB984, \uD654\uC0B0 \uC1C4\uC124\uBB3C \uD1F4\uC801\uBB3C)\uB4F1\uC744 \uD3EC\uD568\uD55C\uB2E4. \uB610\uD55C \uC774\uB7EC\uD55C \uAC70\uB300 \uD654\uC131\uC554 \uC9C0\uB300\uC758 \uD615\uC131\uC740 \uB9E8\uD2C0 \uD50C\uB8F8\uC774\uB098 \uD639\uC740 \uBC1C\uC0B0\uD558\uB294 \uD310 \uAD6C\uC870\uB860\uC758 \uC601\uD5A5\uC744 \uBC1B\uB294\uB2E4. \uAC70\uB300 \uD654\uC131\uC554 \uC9C0\uB300\uB294 \uC9C0\uB09C 5\uC5B5\uB144 \uB3D9\uC548 \uC5EC\uB7EC \uB300\uB7C9 \uBA78\uC885\uACFC \uB354\uBD88\uC5B4 \uAE30\uD6C4\uBCC0\uD654\uC5D0 \uAD00\uB828\uB418\uC5B4 \uC788\uC73C\uBA70, \uC774\uC5D0 \uB530\uB974\uB294 \uC5EC\uB7EC \uAD00\uACC4\uB4E4\uC5D0 \uB300\uD55C \uAC00\uC124\uB4E4\uC774 \uB098\uC640 \uC788\uB294 \uC0C1\uD0DC\uC774\uB2E4. \uAC70\uB300 \uD654\uC131\uC554 \uC9C0\uB300\uB294 \uD65C\uD654\uC0B0\uC774\uB098 \uD639\uC740 \uD654\uC0B0\uACFC\uB294 \uB2E4\uB974\uB2E4."@ko , "Une province magmatique, ou province ign\u00E9e (LIP, pour l'anglais large igneous province), est une vaste r\u00E9gion dont le substratum est constitu\u00E9e de roches magmatiques (appel\u00E9es aussi roches ign\u00E9es) issues de l'association dans l'espace et le temps de massifs intrusifs et de volcans associ\u00E9s, g\u00E9n\u00E9ralement cog\u00E9n\u00E9tiques et formant une s\u00E9rie, parfois non cog\u00E9n\u00E9tiques et formant une suite. La pr\u00E9sence de ces roches est la cons\u00E9quence de grandes intrusions (g\u00E9n\u00E9ralement de type batholites) et d'une expulsion colossale de flots de laves (souvent de type basalte) par des panaches mantelliques, qui recouvre d'une couche \u00E9paisse et plane de tr\u00E8s grands secteurs, jusqu'\u00E0 des parties enti\u00E8res d'un continent (panaches qui se mettent en place dans les oc\u00E9ans sous forme de plateau oc\u00E9anique ou sur les con"@fr , "Eine magmatische Gro\u00DFprovinz (englisch large igneous province, kurz LIP) ist ein Gebiet der Erdkruste, das sehr gro\u00DFe Mengen magmatischer Gesteine enth\u00E4lt (bis zur Gr\u00F6\u00DFenordnung 1 Million km3 auf Fl\u00E4chen von mehreren Millionen km2), die sowohl intrusiv als auch extrusiv sein k\u00F6nnen und sich in geologisch kurzen Zeitr\u00E4umen gebildet haben."@de , "\u5DE8\u5927\u706B\u6210\u5CA9\u5CA9\u77F3\u533A\uFF08\u304D\u3087\u3060\u3044\u304B\u3044\u305B\u3044\u304C\u3093\u304C\u3093\u305B\u304D\u304F, \u82F1: Large igneous provinces, LIPs\uFF09\u3068\u306F\u3001\u5E83\u5927\u306A\u7BC4\u56F2\u306B\u6E21\u308A\u706B\u6210\u5CA9\u304C\u5206\u5E03\u3057\u3066\u3044\u308B\u5730\u57DF\u304A\u3088\u3073\u305D\u308C\u3092\u751F\u6210\u3057\u305F\u706B\u5C71\u6D3B\u52D5\u306E\u3053\u3068\u3002\u706B\u6210\u5CA9\u5206\u5E03\u7BC4\u56F2\u306F\u5927\u9678\u3068\u6BD4\u8F03\u3057\u3046\u308B\u307B\u3069\u306E\u5E83\u5927\u306A\u9762\u7A4D\u3068\u306A\u308A\u3001\u305D\u306E\u751F\u6210\u306B\u4F34\u3046\u706B\u5C71\u5674\u51FA\u7269\u306F\u5730\u7403\u306E\u6C17\u5019\u5909\u52D5\u306B\u5F71\u97FF\u3092\u4E0E\u3048\u305F\u3068\u8003\u3048\u3089\u308C\u3066\u3044\u308B\u3002 \u4E2D\u592E\u6D77\u5DBA\u3084\u5CF6\u5F27\u5730\u5E2F\u306E\u3088\u3046\u306B\u9577\u671F\u306B\u308F\u305F\u308A\u6D3B\u52D5\u3057\u305F\u306E\u3068\u306F\u7570\u306A\u308A\u3001\u6570\u767E\u4E07\u5E74\u7A0B\u5EA6\u306E\u6BD4\u8F03\u7684\u77ED\u671F\u306B\u5927\u898F\u6A21\u306A\u706B\u5C71\u6D3B\u52D5\u3092\u304A\u3053\u3057\u305F\u3082\u306E\u3067\u3042\u308B\u3002\u5CA9\u77F3\u306E\u4F53\u7A4D\u306F\u6570\u767E\u4E07\u7ACB\u65B9\u30AD\u30ED\u30E1\u30FC\u30C8\u30EB\u306B\u3082\u9054\u3059\u308B\u3002\u3053\u306E\u6D3B\u52D5\u306E\u7D50\u679C\u3001\u5927\u9678\u5730\u57DF\u306B\u304A\u3044\u3066\u306F\u6D2A\u6C34\u7384\u6B66\u5CA9\u306B\u3088\u308B\u53F0\u5730\u3001\u6D77\u5E95\u306B\u304A\u3044\u3066\u306F\u6D77\u53F0\u304C\u5F62\u6210\u3055\u308C\u3001\u305D\u306E\u307B\u304B\u5927\u898F\u6A21\u306A\u8CAB\u5165\u5CA9\u8108\u304C\u6B8B\u3055\u308C\u3066\u3044\u308B\u5730\u57DF\u3082\u3042\u308B\u3002 \u5CA9\u8CEA\u306F\u7384\u6B66\u5CA9\u304C\u4E3B\u3067\u3042\u308A\u3001\u6210\u56E0\u3068\u3057\u3066\u306F\u30DE\u30F3\u30C8\u30EB\u30FB\u30D7\u30EA\u30E5\u30FC\u30E0\u304C\u8003\u3048\u3089\u308C\u3066\u3044\u308B\u3002"@ja , "As ( ou Grandes Prov\u00EDncias \u00CDgneas, em portugu\u00EAs) s\u00E3o \u00E1reas com um grande ac\u00FAmulo de rochas \u00EDgneas, sejam elas intrusivas ou extrusivas. Comumente est\u00E3o associadas \u00E0s ou aos limites de placas tect\u00F4nicas. Frequentemente o surgimento de uma LIP est\u00E1 associada aos epis\u00F3dios de extin\u00E7\u00E3o em massa e mudan\u00E7as clim\u00E1ticas relevantes no planeta. As LIPs s\u00E3o diferentes de vulc\u00F5es ativos ou de sistemas vulc\u00E2nicos."@pt , "A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including intrusive (sills, dikes) and extrusive (lava flows, tephra deposits), arising when magma travels through the crust towards the surface. The formation of LIPs is variously attributed to mantle plumes or to processes associated with divergent plate tectonics. The formation of some of the LIPs in the past 500 million years coincide in time with mass extinctions and rapid climatic changes, which has led to numerous hypotheses about causal relationships. LIPs are fundamentally different from any other currently active volcanoes or volcanic systems."@en , "Du\u017Ca prowincja magmatyczna (ang. large igneous province \u2013 LIP), tak\u017Ce: wielka pokrywa lawowa \u2013 bardzo rozleg\u0142y obszar wyst\u0119powania wylewnych ska\u0142 magmowych, g\u0142\u00F3wnie bazaltu. Pokrywa taka mo\u017Ce rozci\u0105ga\u0107 si\u0119 na powierzchni kilku milion\u00F3w kilometr\u00F3w kwadratowych i mie\u0107 obj\u0119to\u015B\u0107 rz\u0119du milion\u00F3w kilometr\u00F3w sze\u015Bciennych, a odpowiadaj\u0105ce jej pogrubienie skorupy ziemskiej mo\u017Ce wynie\u015B\u0107 nawet 35 kilometr\u00F3w."@pl , "Le Grandi Province Ignee (in inglese normalmente abbreviate in LIP, acronimo di Large Igneous Province) sono accumuli estremamente grandi di rocce magmatiche di tipo intrusivo, effusivo, o misto, affioranti sulla crosta terrestre. Il termine \"Grande provincia ignea\" \u00E8 stato originariamente proposto da Coffin ed Eldholm (1992) per riferirsi ad una tipologia di province ignee mafiche che si estendono su aree maggiori di 100000 km\u00B2 (circa un terzo della superficie dell'Italia), sono state eruttate in intervalli di tempo molto brevi dell'ordine di pochi milioni di anni o meno, e che hanno origine da processi non associati alla 'normale' tettonica a placche e di espansione del fondale oceanico."@it , "Een large igneous province (ook wel afgekort tot LIP) is in de geologie een vulkanische vlakte ontstaan door de stolling van zeer grote hoeveelheden magma (meestal basalt). Large igneous provinces werden oorspronkelijk gedefinieerd door Coffin en Eldholm (1992) als gebieden van het aardoppervlak waar zeer grote hoeveelheden magmatische gesteenten (meestal basalt) uitvloeiden over een zeer korte geologische tijd met tussenpozen van een paar miljoen jaar of minder. Deze LIP's zijn niet gekoppeld aan een normaal tektonisch magmatisme, namelijk ter hoogte van MOR's of eilandbogen (subductie). Het fenomeen LIP omvat basaltvloeden, oceaanvloeren, vulkanische riften en dike swarms (een \"zwerm\" van dikes onder een vulkanische vlakte, zie Mackenzie dikes). Wanneer LIP's ontstaan nemen zij al snel o"@nl , "\u0627\u0644\u0625\u0642\u0644\u064A\u0645 \u0627\u0644\u0646\u0627\u0631\u064A \u0627\u0644\u0643\u0628\u064A\u0631 \u0647\u0648 \u062A\u0631\u0627\u0643\u0645 \u0643\u0628\u064A\u0631 \u062C\u062F\u064B\u0627 \u0645\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0628\u0645\u0627 \u0641\u064A \u0630\u0644\u0643 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0633\u0627\u0626\u0644\u0629 (\u0627\u0644\u0627\u0633\u062A\u0631\u0633\u0627\u0628) \u0623\u0648 \u062A\u0634\u0643\u064A\u0644\u0627\u062A \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 (\u0627\u0644\u0635\u062E\u0631 \u0627\u0644\u0646\u0627\u0628\u0637)\u060C \u0639\u0646\u062F\u0645\u0627 \u062A\u064F\u0642\u0630\u0641 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0627\u0644\u0633\u0627\u062E\u0646\u0629 \u0645\u0646 \u062F\u0627\u062E\u0644 \u0627\u0644\u0623\u0631\u0636 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\u0627\u0644\u0641\u064A\u0636\u0627\u0646\u0627\u062A \u0648\u0627\u0644\u0623\u0642\u0627\u0644\u064A\u0645 \u0627\u0644\u062C\u0648\u0641\u064A\u0629 \u0627\u0644\u0643\u0628\u064A\u0631\u0629\u060C \u0648\u0642\u0639\u062A \u0623\u062D\u062F \u0639\u0634\u0631 \u062D\u0644\u0642\u0629 \u0628\u0627\u0631\u0632\u0629 \u0645\u0646 \u0628\u0627\u0632\u0644\u062A \u0627\u0644\u0641\u064A\u0636\u0627\u0646\u0627\u062A \u0641\u064A \u0627\u0644\u0640 250 \u0645\u0644\u064A\u0648\u0646 \u0633\u0646\u0629 \u0627\u0644\u0645\u0627\u0636\u064A\u0629 \u062E\u0627\u0644\u0642\u0629 \u0623\u0642\u0627\u0644\u064A\u0645 \u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0648\u0627\u0644\u062A\u064A \u062A\u062A\u0632\u0627\u0645\u0646 \u0645\u0639 \u0627\u0646\u0642\u0631\u0627\u0636\u0627\u062A \u062C\u0645\u0627\u0639\u064A\u0629 \u0641\u064A \u0639\u0635\u0648\u0631 \u0645\u0627 \u0642\u0628\u0644 \u0627\u0644\u062A\u0627\u0631\u064A\u062E\u060C \u0627\u0644\u062A\u0634\u0643\u064A\u0644 \u064A\u0639\u062A\u0645\u062F \u0639\u0644\u0649 \u0645\u062C\u0645\u0648\u0639\u0629 \u0645\u0646 \u0627\u0644\u0639\u0648\u0627\u0645\u0644 \u0645\u062B\u0644 \u0627\u0644\u062A\u0643\u0648\u064A\u0646 \u0627\u0644\u0642\u0627\u0631\u064A \u0648\u0627\u0644\u0639\u0631\u0636 \u0648\u0627\u0644\u062D\u062C\u0645 \u0648\u0627\u0644\u0645\u0639\u062F\u0644 \u0648\u0645\u062F\u0629 \u0627\u0644\u062B\u0648\u0631\u0627\u0646.\u060C \u0648\u0627\u0644\u0623\u0633\u0644\u0648\u0628\u060C \u0648\u0627\u0644\u0625\u0639\u062F\u0627\u062F (\u0627\u0644\u0642\u0627\u0631\u064A \u0645\u0642\u0627\u0628\u0644 \u0627\u0644\u0645\u062D\u064A\u0637\u0627\u062A)\u060C \u0648\u062D\u0627\u0644\u0629 \u0627\u0644\u0645\u0646\u0627\u062E \u0627\u0644\u0645\u0648\u062C\u0648\u062F\u0629 \u0645\u0646 \u0642\u0628\u0644 \u0648\u0645\u0642\u0627\u0648\u0645\u0629 \u0627\u0644\u0643\u0627\u0626\u0646\u0627\u062A \u0627\u0644\u062D\u064A\u0629 \u0644\u0644\u062A\u063A\u064A\u064A\u0631."@ar , "\u5927\u578B\u706B\u6210\u5CA9\u533A\uFF08\u82F1\u8BED\uFF1ALarge igneous province\uFF0CLIP\uFF09\uFF0C\u4E5F\u8BD1\u4F5C\u5927\u706B\u6210\u5CA9\u7701\uFF0C\u662F\u5728\u5730\u58F3\u4E2D\u89C4\u6A21\u5DE8\u5927\u7684\u706B\u6210\u5CA9\u7684\u5806\u79EF\uFF0C\u5305\u62EC\u4FB5\u5165\u6216\u30021992\u5E74\uFF0C\u7814\u7A76\u8005\u9996\u6B21\u7528\u6B64\u672F\u8BED\u63CF\u8FF0\u9762\u79EF\u5927\u4E8E100,000\u5E73\u65B9\u5343\u7C73\u7684\u706B\u6210\u5CA9\u5806\u79EF\uFF08\u7565\u5927\u4E8E\u8461\u8404\u7259\uFF09\u2014\u5728\u51E0\u767E\u4E07\u5E74\u751A\u81F3\u66F4\u77ED\u7684\u5730\u8D28\u65F6\u95F4\u95F4\u9694\u5185\uFF0C\u767C\u751F\u57FA\u6027\u706B\u6210\u5CA9\u55B7\u51FA\u6216\u6DF1\u5904\u4FB5\u5165\u3002\u57FA\u6027\u7684\u7384\u6B66\u5CA9\u6D77\u5E8A\u4E0E\u5176\u4ED6\u6B63\u5E38\u7684\u677F\u5757\u6784\u9020\u7684\u5730\u8D28\u7ED3\u679C\u4E0D\u5C5E\u4E8E\u5927\u578B\u706B\u6210\u5CA9\u533A\u57DF\u3002 \u73B0\u5728\uFF0C\u5927\u578B\u706B\u6210\u5CA9\u533A\u57DF\u7684\u5916\u5EF6\u4E0D\u4EC5\u5305\u62EC\u57FA\u6027\uFF0C\u4E5F\u5305\u62EC\u5404\u7C7B\u578B\u7684\u706B\u6210\u5CA9\u5927\u9762\u79EF\u7D2F\u79EF\u3002\u53EF\u7EC6\u5206\u4E3A\u201C\u5927\u578B\u706B\u5C71\u5CA9\u533A\u57DF\u201D\uFF08large volcanic provinces\uFF0CLVP\uFF09\u4E0E\u201C\u5927\u578B\u6DF1\u6210\u5CA9\u533A\u57DF\u201D\uFF08large plutonic provinces\uFF0CLPP\uFF09\u3002 \u5927\u578B\u706B\u6210\u5CA9\u533A\u57DF\u57FA\u672C\u4E0A\u662F\u5730\u5E54\u70ED\u67F1\u5347\u81F3\u5730\u58F3\u7684\u7ED3\u679C\u3002 \u67D0\u4E9B\u5927\u578B\u706B\u6210\u5CA9\u533A\u57DF\u73B0\u5728\u8FD8\u5F88\u5B8C\u6574\uFF0C\u5982\u5370\u5EA6\u7684\u5FB7\u5E72\u6697\u8272\u5CA9\uFF1B\u5176\u4ED6\u5927\u578B\u706B\u6210\u5CA9\u533A\u57DF\u88AB\u677F\u5757\u6784\u9020\u8FD0\u52A8\u6240\u80A2\u89E3\uFF0C\u5982\uFF08CAMP\uFF09\u5206\u5E03\u5728\u5DF4\u897F\u3001\u5317\u7F8E\u4E1C\u90E8\u3001\u897F\u5317\u975E\u3002"@zh , "Una gran provincia \u00EDgnea o GPI (en ingl\u00E9s, Large igneous province, o LIP) es una acumulaci\u00F3n extremadamente grande de rocas \u00EDgneas, que incluyen tanto rocas intrusivas (alf\u00E9izares, diques) como extrusivas (flujos de lava, yacimientos de tefra), que surgen cuando el magma viaja a trav\u00E9s de la corteza terrestre hacia la superficie. La formaci\u00F3n de una GPI se atribuye de diversas maneras a las plumas del manto o a los procesos asociados con la tect\u00F3nica de placas divergentes.\u200B La formaci\u00F3n de algunas de las GPI en los \u00FAltimos 500 millones de a\u00F1os coinciden en el tiempo con extinciones masivas y r\u00E1pidos cambios clim\u00E1ticos, lo que ha llevado a numerosas hip\u00F3tesis sobre las relaciones causales. Las GPI son fundamentalmente diferentes de cualquier otro volc\u00E1n o sistema volc\u00E1nico actualmente activ"@es , "\u0422\u0440\u0430\u043F\u043E\u0432\u0430 \u0444\u043E\u0440\u043C\u0430\u0446\u0456\u044F (\u0430\u043D\u0433\u043B. trapp formation; \u043D\u0456\u043C. Trappe-Formation f; \u0432\u0456\u0434 \u043D\u043E\u0440\u0432. trapp \u2014 \u0441\u0445\u043E\u0434\u0438) \u2014 \u043C\u0430\u0433\u043C\u0430\u0442\u0438\u0447\u043D\u0430 \u0444\u043E\u0440\u043C\u0430\u0446\u0456\u044F, \u0449\u043E \u0432\u0445\u043E\u0434\u0438\u0442\u044C \u0432 \u0431\u0456\u043B\u044C\u0448\u043E\u0441\u0442\u0456 \u0432\u0438\u043F\u0430\u0434\u043A\u0456\u0432 \u0434\u043E \u0441\u043A\u043B\u0430\u0434\u0443 \u0447\u043E\u0445\u043B\u0430 \u0434\u0440\u0435\u0432\u043D\u0456\u0445 \u0456 \u043C\u043E\u043B\u043E\u0434\u0438\u0445 \u043F\u043B\u0430\u0442\u0444\u043E\u0440\u043C \u0456 \u0445\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u043D\u0430 \u0434\u043B\u044F \u0440\u0435\u0436\u0438\u043C\u0443 \u043F\u043B\u0430\u0442\u0444\u043E\u0440\u043C\u043D\u043E\u0433\u043E \u0440\u043E\u0437\u0432\u0438\u0442\u043A\u0443 \u0441\u043A\u043B\u0430\u0434\u0447\u0430\u0441\u0442\u0438\u0445 \u0441\u0442\u0440\u0443\u043A\u0442\u0443\u0440."@uk ; rdfs:seeAlso . @prefix foaf: . dbr:Large_igneous_province foaf:depiction , , , , . @prefix dct: . @prefix dbc: . dbr:Large_igneous_province dct:subject dbc:Flood_basalts , dbc:Petrology , dbc:Orogeny , dbc:Climate_forcing , dbc:Supervolcanoes , dbc:Large_igneous_provinces , dbc:Geomorphology , dbc:Igneous_rocks , dbc:Geological_hazards , dbc:Volcanology ; dbo:abstract "As ( ou Grandes Prov\u00EDncias \u00CDgneas, em portugu\u00EAs) s\u00E3o \u00E1reas com um grande ac\u00FAmulo de rochas \u00EDgneas, sejam elas intrusivas ou extrusivas. Comumente est\u00E3o associadas \u00E0s ou aos limites de placas tect\u00F4nicas. Frequentemente o surgimento de uma LIP est\u00E1 associada aos epis\u00F3dios de extin\u00E7\u00E3o em massa e mudan\u00E7as clim\u00E1ticas relevantes no planeta. As LIPs s\u00E3o diferentes de vulc\u00F5es ativos ou de sistemas vulc\u00E2nicos."@pt , "Une province magmatique, ou province ign\u00E9e (LIP, pour l'anglais large igneous province), est une vaste r\u00E9gion dont le substratum est constitu\u00E9e de roches magmatiques (appel\u00E9es aussi roches ign\u00E9es) issues de l'association dans l'espace et le temps de massifs intrusifs et de volcans associ\u00E9s, g\u00E9n\u00E9ralement cog\u00E9n\u00E9tiques et formant une s\u00E9rie, parfois non cog\u00E9n\u00E9tiques et formant une suite. La pr\u00E9sence de ces roches est la cons\u00E9quence de grandes intrusions (g\u00E9n\u00E9ralement de type batholites) et d'une expulsion colossale de flots de laves (souvent de type basalte) par des panaches mantelliques, qui recouvre d'une couche \u00E9paisse et plane de tr\u00E8s grands secteurs, jusqu'\u00E0 des parties enti\u00E8res d'un continent (panaches qui se mettent en place dans les oc\u00E9ans sous forme de plateau oc\u00E9anique ou sur les continents sous forme de trapps). Le territoire de l'Islande par exemple est totalement inclus dans une province ign\u00E9e. Bien que non explosifs, les gaz et la poussi\u00E8re lib\u00E9r\u00E9s par une telle \u00E9ruption ont un impact climatique \u00E9quivalent aux \u00E9ruptions de niveau 8 (supervolcan). Ces inondations basaltiques, significativement assez importantes pour former ces vastes provinces ign\u00E9es, ont \u00E9t\u00E9 soup\u00E7onn\u00E9es d'\u00EAtre la ou du moins une des causes des extinctions de masse du pass\u00E9, dont les extinctions massives (extinction permienne) qui ont affect\u00E9 la majorit\u00E9 des esp\u00E8ces vivantes de l'\u00E9poque ainsi que la plus connue bien que plus petite, l'extinction du Cr\u00E9tac\u00E9 qui a vu dispara\u00EEtre la plupart des dinosaures."@fr , "Du\u017Ca prowincja magmatyczna (ang. large igneous province \u2013 LIP), tak\u017Ce: wielka pokrywa lawowa \u2013 bardzo rozleg\u0142y obszar wyst\u0119powania wylewnych ska\u0142 magmowych, g\u0142\u00F3wnie bazaltu. Pokrywa taka mo\u017Ce rozci\u0105ga\u0107 si\u0119 na powierzchni kilku milion\u00F3w kilometr\u00F3w kwadratowych i mie\u0107 obj\u0119to\u015B\u0107 rz\u0119du milion\u00F3w kilometr\u00F3w sze\u015Bciennych, a odpowiadaj\u0105ce jej pogrubienie skorupy ziemskiej mo\u017Ce wynie\u015B\u0107 nawet 35 kilometr\u00F3w. Formowanie wielkich pokryw lawowych by\u0142o, w geologicznej skali czasu, zjawiskiem gwa\u0142townym \u2013 w wi\u0119kszo\u015Bci przypadk\u00F3w najwi\u0119ksza obj\u0119to\u015Bciowo cz\u0119\u015B\u0107 pokrywy wylewa\u0142a si\u0119 kr\u00F3cej ni\u017C milion lat, cho\u0107 formowanie ca\u0142ych du\u017Cych prowincji magmatycznych trwa zwykle \u0142\u0105cznie do 100 milion\u00F3w lat. Szacuje si\u0119, \u017Ce mniej wi\u0119cej 10% masy i energii cieplnej wydobywa si\u0119 z wn\u0119trza Ziemi za po\u015Brednictwem DPM, przez co zjawiska te nale\u017Cy traktowa\u0107 jako istotne dla dynamiki wn\u0119trza ziemi. W przeciwie\u0144stwie do stabilnych proces\u00F3w wulkanicznych zachodz\u0105cych w grzbietach \u015Br\u00F3doceanicznych i strefach subdukcji powstawanie DPM jest procesem \u015Bci\u015Ble epizodycznym."@pl , "\u0627\u0644\u0625\u0642\u0644\u064A\u0645 \u0627\u0644\u0646\u0627\u0631\u064A \u0627\u0644\u0643\u0628\u064A\u0631 \u0647\u0648 \u062A\u0631\u0627\u0643\u0645 \u0643\u0628\u064A\u0631 \u062C\u062F\u064B\u0627 \u0645\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0628\u0645\u0627 \u0641\u064A \u0630\u0644\u0643 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0633\u0627\u0626\u0644\u0629 (\u0627\u0644\u0627\u0633\u062A\u0631\u0633\u0627\u0628) \u0623\u0648 \u062A\u0634\u0643\u064A\u0644\u0627\u062A \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 (\u0627\u0644\u0635\u062E\u0631 \u0627\u0644\u0646\u0627\u0628\u0637)\u060C \u0639\u0646\u062F\u0645\u0627 \u062A\u064F\u0642\u0630\u0641 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0627\u0644\u0633\u0627\u062E\u0646\u0629 \u0645\u0646 \u062F\u0627\u062E\u0644 \u0627\u0644\u0623\u0631\u0636 \u0648\u062A\u062A\u062F\u0641\u0642 \u062E\u0627\u0631\u062C\u0647\u0627\u060C \u0645\u0635\u062F\u0631 \u0627\u0644\u0639\u062F\u064A\u062F \u0645\u0646 \u0647\u0630\u0647 \u0627\u0644\u0623\u0642\u0627\u0644\u064A\u0645 \u0627\u0644\u0646\u0627\u0631\u064A\u0629 \u064A\u0639\u0648\u062F \u0625\u0644\u0649 \u0623\u0639\u0645\u062F\u0629 \u0627\u0644\u062F\u062B\u0627\u0631 \u0623\u0648 \u0625\u0644\u0649 \u0627\u0644\u0639\u0645\u0644\u064A\u0627\u062A \u0627\u0644\u0645\u0631\u062A\u0628\u0637\u0629 \u0628\u0627\u0644\u0635\u0641\u0627\u0626\u062D \u0627\u0644\u062A\u0643\u062A\u0648\u0646\u064A\u0629\u060C \u0623\u0646\u0648\u0627\u0639 \u0627\u0644\u0623\u0642\u0627\u0644\u064A\u0645 \u064A\u0645\u0643\u0646 \u0623\u0646 \u062A\u062A\u0636\u0645\u0646 \u0623\u0642\u0627\u0644\u064A\u0645 \u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0643\u0628\u0631\u0649\u060C \u062A\u062A\u0643\u0648\u0646 \u0645\u0646 \u062E\u0644\u0627\u0644 \u0628\u0627\u0632\u0644\u062A \u0627\u0644\u0641\u064A\u0636\u0627\u0646\u0627\u062A \u0648\u0627\u0644\u0623\u0642\u0627\u0644\u064A\u0645 \u0627\u0644\u062C\u0648\u0641\u064A\u0629 \u0627\u0644\u0643\u0628\u064A\u0631\u0629\u060C \u0648\u0642\u0639\u062A \u0623\u062D\u062F \u0639\u0634\u0631 \u062D\u0644\u0642\u0629 \u0628\u0627\u0631\u0632\u0629 \u0645\u0646 \u0628\u0627\u0632\u0644\u062A \u0627\u0644\u0641\u064A\u0636\u0627\u0646\u0627\u062A \u0641\u064A \u0627\u0644\u0640 250 \u0645\u0644\u064A\u0648\u0646 \u0633\u0646\u0629 \u0627\u0644\u0645\u0627\u0636\u064A\u0629 \u062E\u0627\u0644\u0642\u0629 \u0623\u0642\u0627\u0644\u064A\u0645 \u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0648\u0627\u0644\u062A\u064A \u062A\u062A\u0632\u0627\u0645\u0646 \u0645\u0639 \u0627\u0646\u0642\u0631\u0627\u0636\u0627\u062A \u062C\u0645\u0627\u0639\u064A\u0629 \u0641\u064A \u0639\u0635\u0648\u0631 \u0645\u0627 \u0642\u0628\u0644 \u0627\u0644\u062A\u0627\u0631\u064A\u062E\u060C \u0627\u0644\u062A\u0634\u0643\u064A\u0644 \u064A\u0639\u062A\u0645\u062F \u0639\u0644\u0649 \u0645\u062C\u0645\u0648\u0639\u0629 \u0645\u0646 \u0627\u0644\u0639\u0648\u0627\u0645\u0644 \u0645\u062B\u0644 \u0627\u0644\u062A\u0643\u0648\u064A\u0646 \u0627\u0644\u0642\u0627\u0631\u064A \u0648\u0627\u0644\u0639\u0631\u0636 \u0648\u0627\u0644\u062D\u062C\u0645 \u0648\u0627\u0644\u0645\u0639\u062F\u0644 \u0648\u0645\u062F\u0629 \u0627\u0644\u062B\u0648\u0631\u0627\u0646.\u060C \u0648\u0627\u0644\u0623\u0633\u0644\u0648\u0628\u060C \u0648\u0627\u0644\u0625\u0639\u062F\u0627\u062F (\u0627\u0644\u0642\u0627\u0631\u064A \u0645\u0642\u0627\u0628\u0644 \u0627\u0644\u0645\u062D\u064A\u0637\u0627\u062A)\u060C \u0648\u062D\u0627\u0644\u0629 \u0627\u0644\u0645\u0646\u0627\u062E \u0627\u0644\u0645\u0648\u062C\u0648\u062F\u0629 \u0645\u0646 \u0642\u0628\u0644 \u0648\u0645\u0642\u0627\u0648\u0645\u0629 \u0627\u0644\u0643\u0627\u0626\u0646\u0627\u062A \u0627\u0644\u062D\u064A\u0629 \u0644\u0644\u062A\u063A\u064A\u064A\u0631."@ar , "Uma Grande prov\u00EDncia \u00EDgnea \u00E9 o resultado de ac\u00FAmulo de rochas \u00EDgneas em \u00E1reas extremamente grandes (acima de 100 mil quil\u00F4metros quadrados. As rochas resultantes incluem tanto rochas intrusivass como soleira quanto rochas rochas extrusivas, como fluxos delava e dep\u00F3sitos de piroclastos), surgidas quando o magma extravasa na superf\u00EDcie, em tempos geol\u00F3gicos relativamente curtos.No Brasil, o maior exemplo de uma grande prov\u00EDncia \u00EDgnea \u00E9 a Prov\u00EDncia magm\u00E1tica do Paran\u00E1-Etendeka, que uma prov\u00EDncia formadas principalmente por basaltos depositados sobre a crosta continental da Am\u00E9rica do Sul, na Bacia do Paran\u00E1, e que se estende at\u00E9 a Nam\u00EDbia, com mais de 1,2 milh\u00F5es de quil\u00F4metros quadrados. A Prov\u00EDncia magm\u00E1tica do Paran\u00E1-Etendeka est\u00E1 relacionado \u00E0 abertura do Oceano Atl\u00E2ntico Sul, durante a Era Mesozoica, quando da fragmenta\u00E7\u00E3o do supercontinente Gondwana."@pt , "\uAC70\uB300 \uD654\uC131\uC554 \uC9C0\uB300(\u5DE8\u5927\u706B\u6210\u5DD6\u5730\u5E36, \uC601\uC5B4: Large Igneous Province)\uB294 \uB9E4\uC6B0 \uAC70\uB300\uD558\uAC8C \uC313\uC544\uC9C4 \uD654\uC131\uC554 \uC9C0\uB300\uB85C, \uC5EC\uAE30\uC5D4 \uC62C\uB77C\uC628 \uB9C8\uADF8\uB9C8\uAC00 \uD45C\uBA74\uC744 \uD6D1\uC73C\uBA74\uC11C \uB9CC\uB4E4\uC5B4\uC9C4 \uD3C9\uD589, \uC218\uD3C9\uD55C \uD310\uC0C1 \uAD00\uC785\uC554\uCCB4 \uD639\uC740 \uC81C\uBC29, \uADF8\uB9AC\uACE0 \uBD84\uCD9C\uBB3C (\uC6A9\uC554 \uD750\uB984, \uD654\uC0B0 \uC1C4\uC124\uBB3C \uD1F4\uC801\uBB3C)\uB4F1\uC744 \uD3EC\uD568\uD55C\uB2E4. \uB610\uD55C \uC774\uB7EC\uD55C \uAC70\uB300 \uD654\uC131\uC554 \uC9C0\uB300\uC758 \uD615\uC131\uC740 \uB9E8\uD2C0 \uD50C\uB8F8\uC774\uB098 \uD639\uC740 \uBC1C\uC0B0\uD558\uB294 \uD310 \uAD6C\uC870\uB860\uC758 \uC601\uD5A5\uC744 \uBC1B\uB294\uB2E4. \uAC70\uB300 \uD654\uC131\uC554 \uC9C0\uB300\uB294 \uC9C0\uB09C 5\uC5B5\uB144 \uB3D9\uC548 \uC5EC\uB7EC \uB300\uB7C9 \uBA78\uC885\uACFC \uB354\uBD88\uC5B4 \uAE30\uD6C4\uBCC0\uD654\uC5D0 \uAD00\uB828\uB418\uC5B4 \uC788\uC73C\uBA70, \uC774\uC5D0 \uB530\uB974\uB294 \uC5EC\uB7EC \uAD00\uACC4\uB4E4\uC5D0 \uB300\uD55C \uAC00\uC124\uB4E4\uC774 \uB098\uC640 \uC788\uB294 \uC0C1\uD0DC\uC774\uB2E4. \uAC70\uB300 \uD654\uC131\uC554 \uC9C0\uB300\uB294 \uD65C\uD654\uC0B0\uC774\uB098 \uD639\uC740 \uD654\uC0B0\uACFC\uB294 \uB2E4\uB974\uB2E4."@ko , "\u0422\u0440\u0430\u043F\u043E\u0432\u0430 \u0444\u043E\u0440\u043C\u0430\u0446\u0456\u044F (\u0430\u043D\u0433\u043B. trapp formation; \u043D\u0456\u043C. Trappe-Formation f; \u0432\u0456\u0434 \u043D\u043E\u0440\u0432. trapp \u2014 \u0441\u0445\u043E\u0434\u0438) \u2014 \u043C\u0430\u0433\u043C\u0430\u0442\u0438\u0447\u043D\u0430 \u0444\u043E\u0440\u043C\u0430\u0446\u0456\u044F, \u0449\u043E \u0432\u0445\u043E\u0434\u0438\u0442\u044C \u0432 \u0431\u0456\u043B\u044C\u0448\u043E\u0441\u0442\u0456 \u0432\u0438\u043F\u0430\u0434\u043A\u0456\u0432 \u0434\u043E \u0441\u043A\u043B\u0430\u0434\u0443 \u0447\u043E\u0445\u043B\u0430 \u0434\u0440\u0435\u0432\u043D\u0456\u0445 \u0456 \u043C\u043E\u043B\u043E\u0434\u0438\u0445 \u043F\u043B\u0430\u0442\u0444\u043E\u0440\u043C \u0456 \u0445\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u043D\u0430 \u0434\u043B\u044F \u0440\u0435\u0436\u0438\u043C\u0443 \u043F\u043B\u0430\u0442\u0444\u043E\u0440\u043C\u043D\u043E\u0433\u043E \u0440\u043E\u0437\u0432\u0438\u0442\u043A\u0443 \u0441\u043A\u043B\u0430\u0434\u0447\u0430\u0441\u0442\u0438\u0445 \u0441\u0442\u0440\u0443\u043A\u0442\u0443\u0440. \u041C\u0430\u0433\u043C\u0430\u0442\u0438\u0447\u043D\u0430 \u0434\u0456\u044F\u043B\u044C\u043D\u0456\u0441\u0442\u044C, \u044F\u043A\u0430 \u043F\u0440\u0438\u0437\u0432\u043E\u0434\u0438\u0442\u044C \u0434\u043E \u0443\u0442\u0432\u043E\u0440\u0435\u043D\u043D\u044F \u0442\u0440\u0430\u043F\u043E\u0432\u0438\u0445 \u0444\u043E\u0440\u043C\u0430\u0446\u0456\u0439, \u043C\u0430\u0454 \u043D\u0430\u0434\u0437\u0432\u0438\u0447\u0430\u0439\u043D\u043E \u0432\u0435\u043B\u0438\u043A\u0456 \u043C\u0430\u0441\u0448\u0442\u0430\u0431\u0438, \u0437\u0430\u0432\u0434\u044F\u043A\u0438 \u0447\u043E\u043C\u0443 \u043E\u0431\u0441\u044F\u0433 \u0432\u0438\u043B\u0438\u0432\u043D\u043E\u0457 \u043C\u0430\u0433\u043C\u0438 \u0442\u0430 \u0456\u043D\u0442\u0440\u0443\u0437\u0456\u0439 \u043C\u0430\u0433\u043C\u0430\u0442\u0438\u0447\u043D\u043E\u0433\u043E \u043C\u0430\u0442\u0435\u0440\u0456\u0430\u043B\u0443 \u0443 \u0432\u0435\u0440\u0445\u043D\u0456 \u0448\u0430\u0440\u0438 \u043B\u0456\u0442\u043E\u0441\u0444\u0435\u0440\u0438 \u0434\u043E\u0441\u044F\u0433\u0430\u0454 1 \u043C\u043B\u043D \u043A\u043C\u00B3. \u0414\u043B\u044F \u0442\u0440\u0430\u043F\u043E\u0432\u0438\u0445 \u0444\u043E\u0440\u043C\u0430\u0446\u0456\u0439 \u0445\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u043D\u0435 \u0433\u043E\u0440\u0438\u0437\u043E\u043D\u0442\u0430\u043B\u044C\u043D\u0435 \u0437\u0430\u043B\u044F\u0433\u0430\u043D\u043D\u044F \u0433\u0456\u0440\u0441\u044C\u043A\u0438\u0445 \u043F\u043E\u0440\u0456\u0434 \u0443 \u0432\u0438\u0433\u043B\u044F\u0434\u0456 \u043F\u043E\u043A\u0440\u0438\u0432\u0456\u0432 \u0435\u0444\u0443\u0437\u0438\u0432\u0456\u0432 \u0442\u0430 \u0456\u043D\u0442\u0440\u0443\u0437\u0438\u0432\u043D\u0438\u0445 (\u0441\u0443\u0431\u0432\u0443\u043B\u043A\u0430\u043D\u0456\u0447\u043D\u0438\u0445) \u043F\u043E\u043A\u043B\u0430\u0434\u0456\u0432, \u0449\u043E \u0430\u0441\u043E\u0446\u0456\u044E\u044E\u0442\u044C\u0441\u044F \u0437 \u043A\u043E\u043D\u0442\u0438\u043D\u0435\u043D\u0442\u0430\u043B\u044C\u043D\u0438\u043C\u0438 \u0456 \u043B\u0430\u0433\u0443\u043D\u043D\u0438\u043C\u0438 \u043E\u0441\u0430\u0434\u0430\u043C\u0438, \u0456\u043D\u043E\u0434\u0456 \u0437 \u0442\u0443\u0444\u0430\u043C\u0438."@uk , "Una gran provincia \u00EDgnea o GPI (en ingl\u00E9s, Large igneous province, o LIP) es una acumulaci\u00F3n extremadamente grande de rocas \u00EDgneas, que incluyen tanto rocas intrusivas (alf\u00E9izares, diques) como extrusivas (flujos de lava, yacimientos de tefra), que surgen cuando el magma viaja a trav\u00E9s de la corteza terrestre hacia la superficie. La formaci\u00F3n de una GPI se atribuye de diversas maneras a las plumas del manto o a los procesos asociados con la tect\u00F3nica de placas divergentes.\u200B La formaci\u00F3n de algunas de las GPI en los \u00FAltimos 500 millones de a\u00F1os coinciden en el tiempo con extinciones masivas y r\u00E1pidos cambios clim\u00E1ticos, lo que ha llevado a numerosas hip\u00F3tesis sobre las relaciones causales. Las GPI son fundamentalmente diferentes de cualquier otro volc\u00E1n o sistema volc\u00E1nico actualmente activo."@es , "Eine magmatische Gro\u00DFprovinz (englisch large igneous province, kurz LIP) ist ein Gebiet der Erdkruste, das sehr gro\u00DFe Mengen magmatischer Gesteine enth\u00E4lt (bis zur Gr\u00F6\u00DFenordnung 1 Million km3 auf Fl\u00E4chen von mehreren Millionen km2), die sowohl intrusiv als auch extrusiv sein k\u00F6nnen und sich in geologisch kurzen Zeitr\u00E4umen gebildet haben. Die meisten der magmatischen Gro\u00DFprovinzen bestehen aus Basalt, einige aber enthalten gro\u00DFe Mengen an Rhyolith, so etwa der Columbia-Plateaubasalt in den westlichen Vereinigten Staaten. Dieser Rhyolith besitzt typischerweise einen nur geringen Wassergehalt und deutlich h\u00F6here Eruptionstemperaturen (850 \u00B0C bis 1000 \u00B0C) im Vergleich zu dem an Inselb\u00F6gen entstehenden Rhyolithen. Einige der magmatischen Gro\u00DFprovinzen sind heute noch mehr oder weniger intakt, wie etwa der Dekkan-Trapp, andere hingegen sind durch plattentektonische Bewegungen in Teile zerfallen, wie etwa die (Central Atlantic Magmatic Province, kurz CAMP), die heute in Brasilien, den \u00F6stlichen Vereinigten Staaten, Kanada und Nordwest-Afrika zu finden sind."@de , "\u5927\u578B\u706B\u6210\u5CA9\u533A\uFF08\u82F1\u8BED\uFF1ALarge igneous province\uFF0CLIP\uFF09\uFF0C\u4E5F\u8BD1\u4F5C\u5927\u706B\u6210\u5CA9\u7701\uFF0C\u662F\u5728\u5730\u58F3\u4E2D\u89C4\u6A21\u5DE8\u5927\u7684\u706B\u6210\u5CA9\u7684\u5806\u79EF\uFF0C\u5305\u62EC\u4FB5\u5165\u6216\u30021992\u5E74\uFF0C\u7814\u7A76\u8005\u9996\u6B21\u7528\u6B64\u672F\u8BED\u63CF\u8FF0\u9762\u79EF\u5927\u4E8E100,000\u5E73\u65B9\u5343\u7C73\u7684\u706B\u6210\u5CA9\u5806\u79EF\uFF08\u7565\u5927\u4E8E\u8461\u8404\u7259\uFF09\u2014\u5728\u51E0\u767E\u4E07\u5E74\u751A\u81F3\u66F4\u77ED\u7684\u5730\u8D28\u65F6\u95F4\u95F4\u9694\u5185\uFF0C\u767C\u751F\u57FA\u6027\u706B\u6210\u5CA9\u55B7\u51FA\u6216\u6DF1\u5904\u4FB5\u5165\u3002\u57FA\u6027\u7684\u7384\u6B66\u5CA9\u6D77\u5E8A\u4E0E\u5176\u4ED6\u6B63\u5E38\u7684\u677F\u5757\u6784\u9020\u7684\u5730\u8D28\u7ED3\u679C\u4E0D\u5C5E\u4E8E\u5927\u578B\u706B\u6210\u5CA9\u533A\u57DF\u3002 \u73B0\u5728\uFF0C\u5927\u578B\u706B\u6210\u5CA9\u533A\u57DF\u7684\u5916\u5EF6\u4E0D\u4EC5\u5305\u62EC\u57FA\u6027\uFF0C\u4E5F\u5305\u62EC\u5404\u7C7B\u578B\u7684\u706B\u6210\u5CA9\u5927\u9762\u79EF\u7D2F\u79EF\u3002\u53EF\u7EC6\u5206\u4E3A\u201C\u5927\u578B\u706B\u5C71\u5CA9\u533A\u57DF\u201D\uFF08large volcanic provinces\uFF0CLVP\uFF09\u4E0E\u201C\u5927\u578B\u6DF1\u6210\u5CA9\u533A\u57DF\u201D\uFF08large plutonic provinces\uFF0CLPP\uFF09\u3002 \u5927\u578B\u706B\u6210\u5CA9\u533A\u57DF\u57FA\u672C\u4E0A\u662F\u5730\u5E54\u70ED\u67F1\u5347\u81F3\u5730\u58F3\u7684\u7ED3\u679C\u3002 \u67D0\u4E9B\u5927\u578B\u706B\u6210\u5CA9\u533A\u57DF\u73B0\u5728\u8FD8\u5F88\u5B8C\u6574\uFF0C\u5982\u5370\u5EA6\u7684\u5FB7\u5E72\u6697\u8272\u5CA9\uFF1B\u5176\u4ED6\u5927\u578B\u706B\u6210\u5CA9\u533A\u57DF\u88AB\u677F\u5757\u6784\u9020\u8FD0\u52A8\u6240\u80A2\u89E3\uFF0C\u5982\uFF08CAMP\uFF09\u5206\u5E03\u5728\u5DF4\u897F\u3001\u5317\u7F8E\u4E1C\u90E8\u3001\u897F\u5317\u975E\u3002"@zh , "\u5DE8\u5927\u706B\u6210\u5CA9\u5CA9\u77F3\u533A\uFF08\u304D\u3087\u3060\u3044\u304B\u3044\u305B\u3044\u304C\u3093\u304C\u3093\u305B\u304D\u304F, \u82F1: Large igneous provinces, LIPs\uFF09\u3068\u306F\u3001\u5E83\u5927\u306A\u7BC4\u56F2\u306B\u6E21\u308A\u706B\u6210\u5CA9\u304C\u5206\u5E03\u3057\u3066\u3044\u308B\u5730\u57DF\u304A\u3088\u3073\u305D\u308C\u3092\u751F\u6210\u3057\u305F\u706B\u5C71\u6D3B\u52D5\u306E\u3053\u3068\u3002\u706B\u6210\u5CA9\u5206\u5E03\u7BC4\u56F2\u306F\u5927\u9678\u3068\u6BD4\u8F03\u3057\u3046\u308B\u307B\u3069\u306E\u5E83\u5927\u306A\u9762\u7A4D\u3068\u306A\u308A\u3001\u305D\u306E\u751F\u6210\u306B\u4F34\u3046\u706B\u5C71\u5674\u51FA\u7269\u306F\u5730\u7403\u306E\u6C17\u5019\u5909\u52D5\u306B\u5F71\u97FF\u3092\u4E0E\u3048\u305F\u3068\u8003\u3048\u3089\u308C\u3066\u3044\u308B\u3002 \u4E2D\u592E\u6D77\u5DBA\u3084\u5CF6\u5F27\u5730\u5E2F\u306E\u3088\u3046\u306B\u9577\u671F\u306B\u308F\u305F\u308A\u6D3B\u52D5\u3057\u305F\u306E\u3068\u306F\u7570\u306A\u308A\u3001\u6570\u767E\u4E07\u5E74\u7A0B\u5EA6\u306E\u6BD4\u8F03\u7684\u77ED\u671F\u306B\u5927\u898F\u6A21\u306A\u706B\u5C71\u6D3B\u52D5\u3092\u304A\u3053\u3057\u305F\u3082\u306E\u3067\u3042\u308B\u3002\u5CA9\u77F3\u306E\u4F53\u7A4D\u306F\u6570\u767E\u4E07\u7ACB\u65B9\u30AD\u30ED\u30E1\u30FC\u30C8\u30EB\u306B\u3082\u9054\u3059\u308B\u3002\u3053\u306E\u6D3B\u52D5\u306E\u7D50\u679C\u3001\u5927\u9678\u5730\u57DF\u306B\u304A\u3044\u3066\u306F\u6D2A\u6C34\u7384\u6B66\u5CA9\u306B\u3088\u308B\u53F0\u5730\u3001\u6D77\u5E95\u306B\u304A\u3044\u3066\u306F\u6D77\u53F0\u304C\u5F62\u6210\u3055\u308C\u3001\u305D\u306E\u307B\u304B\u5927\u898F\u6A21\u306A\u8CAB\u5165\u5CA9\u8108\u304C\u6B8B\u3055\u308C\u3066\u3044\u308B\u5730\u57DF\u3082\u3042\u308B\u3002 \u5CA9\u8CEA\u306F\u7384\u6B66\u5CA9\u304C\u4E3B\u3067\u3042\u308A\u3001\u6210\u56E0\u3068\u3057\u3066\u306F\u30DE\u30F3\u30C8\u30EB\u30FB\u30D7\u30EA\u30E5\u30FC\u30E0\u304C\u8003\u3048\u3089\u308C\u3066\u3044\u308B\u3002"@ja , "A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including intrusive (sills, dikes) and extrusive (lava flows, tephra deposits), arising when magma travels through the crust towards the surface. The formation of LIPs is variously attributed to mantle plumes or to processes associated with divergent plate tectonics. The formation of some of the LIPs in the past 500 million years coincide in time with mass extinctions and rapid climatic changes, which has led to numerous hypotheses about causal relationships. LIPs are fundamentally different from any other currently active volcanoes or volcanic systems."@en , "Le Grandi Province Ignee (in inglese normalmente abbreviate in LIP, acronimo di Large Igneous Province) sono accumuli estremamente grandi di rocce magmatiche di tipo intrusivo, effusivo, o misto, affioranti sulla crosta terrestre. Il termine \"Grande provincia ignea\" \u00E8 stato originariamente proposto da Coffin ed Eldholm (1992) per riferirsi ad una tipologia di province ignee mafiche che si estendono su aree maggiori di 100000 km\u00B2 (circa un terzo della superficie dell'Italia), sono state eruttate in intervalli di tempo molto brevi dell'ordine di pochi milioni di anni o meno, e che hanno origine da processi non associati alla 'normale' tettonica a placche e di espansione del fondale oceanico. Si ritiene che i pennacchi del mantello possano essere la fonte di molte o tutte le LIP che non sono associate a una 'tettonica a zolle normale'."@it , "Een large igneous province (ook wel afgekort tot LIP) is in de geologie een vulkanische vlakte ontstaan door de stolling van zeer grote hoeveelheden magma (meestal basalt). Large igneous provinces werden oorspronkelijk gedefinieerd door Coffin en Eldholm (1992) als gebieden van het aardoppervlak waar zeer grote hoeveelheden magmatische gesteenten (meestal basalt) uitvloeiden over een zeer korte geologische tijd met tussenpozen van een paar miljoen jaar of minder. Deze LIP's zijn niet gekoppeld aan een normaal tektonisch magmatisme, namelijk ter hoogte van MOR's of eilandbogen (subductie). Het fenomeen LIP omvat basaltvloeden, oceaanvloeren, vulkanische riften en dike swarms (een \"zwerm\" van dikes onder een vulkanische vlakte, zie Mackenzie dikes). Wanneer LIP's ontstaan nemen zij al snel oppervlaktes van enkele miljoen km\u00B2 in beslag en volumes kunnen zo gemakkelijk 1 miljoen km\u00B3 bedragen."@nl ; dbo:wikiPageWikiLink dbr:Mackenzie_Large_Igneous_Province , dbr:Mistassini_dike_swarm , dbr:High_Arctic_Large_Igneous_Province , dbr:Karoo-Ferrar , dbr:Basalt , dbr:Azores_Plateau , dbr:Ultramafic , dbr:Mackenzie_hotspot , dbr:Astrid_Ridge , dbr:Iceland_Plateau , dbr:Mackenzie_dike_swarm , dbr:Oceanic_anoxic_event , , dbr:Pluton , , , dbc:Geological_hazards , dbr:Passive_margin , dbr:Iron_oxide_copper_gold_ore_deposits , , , dbc:Igneous_rocks , dbr:Ninety_East_Ridge , dbr:Ethiopia-Yemen_Continental_Flood_Basalts , dbr:Agulhas_Plateau , dbr:Andesitic , dbr:New_Zealand , dbc:Volcanology , dbr:Gawler_Ranges , dbr:Hikurangi_Plateau , dbr:Triassic-Jurassic_extinction_event , dbr:Permian-Triassic_extinction_event , dbr:Plate_tectonics , dbr:Coppermine_River_Group , dbr:Mafic , dbr:Franz_Josef_Land , dbr:Ontong-Java_Plateau , dbr:Volcanic_and_igneous_plumbing_systems , dbr:Dongargarh , dbr:Richard_Stothers , , dbr:Norway , dbr:Greenland , dbr:Antarctica , dbr:Paleozoic , dbr:Yemen , dbc:Large_igneous_provinces , dbr:Long_Range_dikes , dbr:Siberian_Traps , dbr:Thulean_Plateau , dbr:Wrangellia_Terrane , dbr:Namibia , dbr:Winagami_sill_complex , dbc:Geomorphology , dbr:Emeishan_Traps , dbr:Yellowstone_hotspot , dbr:Platinum_group , dbr:Marion_Island , dbr:Kerguelen_hotspot , dbr:List_of_flood_basalt_provinces , dbr:Matachewan_dike_swarm , dbr:North_Atlantic_Igneous_Province , dbr:Caribbean_large_igneous_province , dbr:Ontong_Java_Plateau , , dbr:Ore , dbr:Tristan_hotspot , , dbr:Bushveld_Igneous_Complex , dbr:Sverdrup_Basin_Magmatic_Province , dbr:Dike_swarm , , dbr:Caribbean-Colombian_oceanic_plateau , dbr:Felsic , dbr:Ellesmere_Island_Volcanics , dbr:Mid-ocean_ridge , dbr:Strand_Fiord_Formation , dbr:Brazilian_Highlands , dbr:Jameson_Land , dbr:Alpha_Ridge , dbr:Faeroe_Islands , dbr:Gawler_Range_Volcanics , dbr:Pitcairn_hotspot , dbc:Orogeny , dbc:Petrology , dbr:India , dbr:Pilbara_craton , dbc:Climate_forcing , dbr:Geological_time , dbr:Mass_extinctions , dbr:Gabbro , dbr:South_Australia , , dbr:Abrupt_climate_change , dbr:Lava , , dbr:Helium-4 , dbr:Mozambique_Ridge , dbr:Hawaii_hotspot , dbr:Helium-3 , dbr:Mantle_plume , dbr:Pacific_Plate , , , , dbr:Central_Atlantic_Magmatic_Province , dbr:Equatorial_Atlantic_Magmatic_Province , dbr:Intraplate , dbr:Northeast_Georgia_Rise , dbr:Hiltaba_Suite , dbr:Rhyolite , dbr:Igneous_rock , dbc:Supervolcanoes , dbr:Michael_Rampino , dbr:Rajmahal , dbr:Subduction_zone , dbr:Canadian_Shield , dbr:Amerasian_Basin , dbr:Mass_extinction , dbr:Extinction_event , dbr:Peridotite , dbr:Lithosphere , dbr:Siberian_traps , dbr:Kimberlite , dbr:Geologic_province , dbr:Volcanic_passive_margin , dbr:Maud_Rise , dbr:Manihiki_Plateau , dbr:Warakurna_large_igneous_province , dbr:Supervolcano , dbr:Pliensbachian-Toarcian_extinction , , dbr:Tephra , dbr:Madagascar , dbr:Ethiopia , , dbr:Kerguelen_Plateau , , dbr:Columbia_River_Basalt_Group , dbr:Copper , dbr:Midcontinent_Rift_System , dbr:Mesoproterozoic , dbr:Svalbard , dbr:Proterozoic , dbr:Flood_basalt , dbr:Orogeny , dbr:Rajmahal_Traps , dbr:Louisville_hotspot , dbr:Central_Atlantic_magmatic_province , dbr:Brazil , , dbr:Deccan_Traps , dbr:Oceanic_plateau , dbr:Iceland_hotspot , dbr:Scotland , dbr:Nickel , dbc:Flood_basalts , dbr:Tomography , . @prefix dbp: . @prefix dbt: . dbr:Large_igneous_province dbp:wikiPageUsesTemplate dbt:Circa , dbt:Portal , dbt:Citation_needed , dbt:Cvt , dbt:Cite_web , dbt:See_also , dbt:Clarify , dbt:Val , dbt:Reflist , dbt:Use_dmy_dates , dbt:Cite_conference , dbt:Large_igneous_provinces , dbt:Convert , dbt:Cite_book , dbt:Short_description , dbt:Cite_journal ; 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