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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Mineral silikat membentuk kelompok terbesar dan terpenting dari mineral pembentuk batuan, serta terdiri dari sekitar 90 persen kerak Bumi. Batuan ini dikelompokkan berdasarkan struktur kelompok silikatnya. Semua mineral silikat berisi silikon dan oksigen."@in .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"I silicati sono la classe di minerali caratterizzati dalla presenza del gruppo tetraedrico (SiO4)4-. Il nome silicati fu adottato per la prima volta dal chimico svedese J\u00F6ns Jacob Berzelius. Ossigeno e silicio sono gli elementi pi\u00F9 abbondanti della crosta terrestre (46,6% e 27,7% in peso, rispettivamente) e questo rende i silicati i minerali pi\u00F9 diffusi sulla Terra (pi\u00F9 del 90%). Questi si presentano all'interno di rocce magmatiche, metamorfiche e sedimentarie."@it .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Silikatoak mineral talderik zabalena da. Silizio atomoak eta berau inguratzen duten 4 oxigenoak sortzen duten silika anioa (tetraedro itxurakoa) elkartzen da beste elementuekin mineralak sortzeko. Tetraedroen lotura motaren arabera sailkatzen dira silikato ezberdinak."@eu .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"I silicati sono la classe di minerali caratterizzati dalla presenza del gruppo tetraedrico (SiO4)4-. Il nome silicati fu adottato per la prima volta dal chimico svedese J\u00F6ns Jacob Berzelius. Ossigeno e silicio sono gli elementi pi\u00F9 abbondanti della crosta terrestre (46,6% e 27,7% in peso, rispettivamente) e questo rende i silicati i minerali pi\u00F9 diffusi sulla Terra (pi\u00F9 del 90%). Questi si presentano all'interno di rocce magmatiche, metamorfiche e sedimentarie."@it .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"\u7845\u9178\u76D0\u77FF\u7269"@zh .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Gr\u00FApa mianra\u00ED a chomhdh\u00E9anann 95% de screamh an Domhain, a chuims\u00EDonn sileacan is ocsaigin i gcomhcheangal le ch\u00E9ile n\u00F3 le d\u00FAile eile. \u00D3 thaobh strucht\u00FAir de, t\u00E1 siad uile bunaithe ar SiO4, teitrih\u00E9adr\u00E1n, agus is strucht\u00FAir chasta phoilim\u00E9aracha de theitrih\u00E9adr\u00E1in an chuid is m\u00F3 d\u00EDobh. Ranga\u00EDtear iad de r\u00E9ir a gc\u00E9im polaim\u00E9iri\u00FAch\u00E1in, \u00F3 shileac\u00E1it\u00ED a chuims\u00EDonn gr\u00FApa\u00ED aonraithe SiO4 (olaiv\u00EDn\u00ED is gairn\u00E9id), go dt\u00ED f\u00E1inn\u00ED (beiril), slabhrashileac\u00E1it\u00ED (pirix\u00E9in\u00ED le slabhra singil is amfab\u00F3il le slabhra\u00ED d\u00FAbailte), leath\u00E1in (mioca\u00ED is cr\u00E9anna), agus creatlaigh thr\u00EDthoiseacha (grianchloch is iathchlocha)."@ga .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"Silikatoak mineral talderik zabalena da. Silizio atomoak eta berau inguratzen duten 4 oxigenoak sortzen duten silika anioa (tetraedro itxurakoa) elkartzen da beste elementuekin mineralak sortzeko. Tetraedroen lotura motaren arabera sailkatzen dira silikato ezberdinak. Lurrazalaren %95a osatzen du mineral talde honek; feldespatoek %60 baino gehiago dira, eta kuartzoak %10 baino zertxobait gehixeago. Silikatoak arroka igneoetan oso ugariak dira, baita nahiko ugariak ere arroka metamorfikoetan eta sedimentarioetan. Silikatoen kopuru txiki bat oso arrunta den bitartean, kopuru zabal bat topatzeko arraroa da. Kristal egituran oinarrizko banako bat ageri du: SiO4 tetraedroa. Silizio ioia tetraedroaren erdian kokatzen da eta oxigeno ioiak erpinetan. Tetraedroak elkarrekin elkartzen dira oxigenoen arteko lotura bidez; tetraedro horiek elkartzeko eraren arabera silikato mota desberdinak eratzen dira: tektosilikatoak, filosilikatoak, inosilikatoak, ziklosilikatoak, sorosilikatoak eta nesosilikatoak. Egitura horien zirrikituetan ioi metalikoak (Fe, Mg, Ca, K eta Na) kokatzen dira. Silikato baten egiturak erabat baldintzatzen du bere kimika osaera eta tasun fisikoak. Horrela, mika mineral ezaguna xafletan agertzen da izadian eta piroxenoak prisma eran, baina denak silikatoak dira. Silikato naturalen artean hauek dira nagusiak: talkoa, buztinak, feldespatoa, mika eta beriloa. Sintesi bidez lortzen den silikato ezagunena sodio silikatoa da (uretan urtzen den beira). Silikatoek hainbat erabilera dituzte: ur gogorrak tratatzeko, zementuak ekoizteko, paperak estaltzeko, azidotasunaren aurka, etab."@eu .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Silicate minerals are rock-forming minerals made up of silicate groups. They are the largest and most important class of minerals and make up approximately 90 percent of Earth's crust. In mineralogy, silica (silicon dioxide) SiO2 is usually considered a silicate mineral. Silica is found in nature as the mineral quartz, and its polymorphs."@en .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"Gr\u00FApa mianra\u00ED a chomhdh\u00E9anann 95% de screamh an Domhain, a chuims\u00EDonn sileacan is ocsaigin i gcomhcheangal le ch\u00E9ile n\u00F3 le d\u00FAile eile. \u00D3 thaobh strucht\u00FAir de, t\u00E1 siad uile bunaithe ar SiO4, teitrih\u00E9adr\u00E1n, agus is strucht\u00FAir chasta phoilim\u00E9aracha de theitrih\u00E9adr\u00E1in an chuid is m\u00F3 d\u00EDobh. Ranga\u00EDtear iad de r\u00E9ir a gc\u00E9im polaim\u00E9iri\u00FAch\u00E1in, \u00F3 shileac\u00E1it\u00ED a chuims\u00EDonn gr\u00FApa\u00ED aonraithe SiO4 (olaiv\u00EDn\u00ED is gairn\u00E9id), go dt\u00ED f\u00E1inn\u00ED (beiril), slabhrashileac\u00E1it\u00ED (pirix\u00E9in\u00ED le slabhra singil is amfab\u00F3il le slabhra\u00ED d\u00FAbailte), leath\u00E1in (mioca\u00ED is cr\u00E9anna), agus creatlaigh thr\u00EDthoiseacha (grianchloch is iathchlocha)."@ga .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pezzottaite> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"Os minerais silicatados ou simplesmente silicatos constituem a maior e mais importante classe de minerais constituintes das rochas. Classificam-se de acordo com a estrutura do seu grupo ani\u00F4nico silicato, dependendo da raz\u00E3o entre seus \u00E1tomos de sil\u00EDcio e oxig\u00EAnio. Subclasses:"@pt .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Kyanite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://mk.dbpedia.org/resource/\u0421\u0438\u043B\u0438\u043A\u0430\u0442\u043D\u0438_\u043C\u0438\u043D\u0435\u0440\u0430\u043B\u0438> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Hafnon> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"Silicate mineral"@en .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Almandine> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"\uADDC\uC0B0\uC5FC \uAD11\uBB3C"@ko .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Metamorphism> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Hydroxyl> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://sco.dbpedia.org/resource/Silicate_meenerals> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Mineral> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Hornblende> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://zh.dbpedia.org/resource/\u7845\u9178\u76D0\u77FF\u7269> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Scolecite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Sillimanite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"K\u0159emi\u010Ditany"@cs .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/thumbnail>	<http://commons.wikimedia.org/wiki/Special:FilePath/Chrysocolla.jpg?width=300> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Axinite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"Mineral silikat membentuk kelompok terbesar dan terpenting dari mineral pembentuk batuan, serta terdiri dari sekitar 90 persen kerak Bumi. Batuan ini dikelompokkan berdasarkan struktur kelompok silikatnya. Semua mineral silikat berisi silikon dan oksigen."@in .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Moganite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Nosean> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Nesosilicate> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Sugilite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Wollastonite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Crystallization> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ar.dbpedia.org/resource/\u0645\u0639\u0627\u062F\u0646_\u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0627\u062A> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/KaolinUSGOV.jpg> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Kaolinite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Inorganic_compound> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pyroxene> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Lunar_Ferroan_Anorthosite_(60025).jpg> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pyroxferroite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Silicate> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Antigorite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pyrosilicate> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://vi.dbpedia.org/resource/Kho\u00E1ng_v\u1EADt_silicat> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Deep_ocean> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Arfvedsonite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://hr.dbpedia.org/resource/Silikati> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Stishovite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Milarite.png> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"La silikatmineraloj estas la plej granda kaj plej grava klaso de petrofaraj mineraloj. Oni klasifikas ilin la\u016D la strukturo de ilia silikat-jon-grupo. Subklasoj:"@eo .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Augite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"Minerals silicats"@ca .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"\u77FD\u9178\u9E7D\u7926\u7269\u662F\u6307\u542B\u77FD\u7684\u7926\u7269\uFF0C\u662F\u9020\u5CA9\u7926\u7269\u4E2D\u6700\u91CD\u8981\u7684\u4E00\u7A2E\uFF0C\u5730\u6BBC\u4E2D\u4E3B\u8981\u662F\u7531\u77FD\u9178\u9E7D\u7926\u7269\u7D44\u6210\uFF0C\u77FD\u9178\u9E7D\u7926\u7269\u6703\u4F9D\u5176\u5206\u5B50\u7D50\u69CB\u518D\u9032\u884C\u5206\u985E\uFF0C\u4E0D\u540C\u7684\u985E\u5225\u4E2D\uFF0C\u5176\u542B\u77FD\u548C\u6C27\u7684\u6BD4\u4F8B\u4E5F\u6709\u4E0D\u540C\u3002"@zh .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Beta-quartz-CM-2D-balls.png> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<https://global.dbpedia.org/id/jirK> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Fuchsite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Beryll.ring.combined.png> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"K\u0159emi\u010Ditany (silik\u00E1ty) jsou kysl\u00EDkat\u00E9 slou\u010Deniny k\u0159em\u00EDku. Jsou to l\u00E1tky vesm\u011Bs nerozpustn\u00E9 ve vod\u011B a\u017E na k\u0159emi\u010Ditany alkalick\u00FDch kov\u016F Na2SiO3 (vodn\u00ED sklo, kapaln\u00E9 sklo) a K2SiO3. K\u0159emi\u010Ditany v\u00E1penat\u00E9, hlinit\u00E9 a \u017Eelezit\u00E9 jsou rozpustn\u00E9 v kyselin\u00E1ch a jsou sou\u010D\u00E1st\u00ED p\u0159\u00EDrodn\u00EDch miner\u00E1ln\u00EDch surovin pro . V\u0161echny k\u0159emi\u010Ditany lze rozpustit v koncentrovan\u00FDch roztoc\u00EDch alkalick\u00FDch hydroxid\u016F nebo za vysok\u00FDch teplot v jejich tavenin\u00E1ch. K\u0159emi\u010Ditany jako miner\u00E1ly jsou nerosty nekovov\u00E9ho vzhledu a obvykle jsou sou\u010D\u00E1stmi hornin. Jsou to nejroz\u0161\u00ED\u0159en\u011Bj\u0161\u00ED l\u00E1tky v zemsk\u00E9 k\u016F\u0159e."@cs .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Rhodonite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Humite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://la.dbpedia.org/resource/Silicatum> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Clinohumite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pyrophyllite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://fa.dbpedia.org/resource/\u06A9\u0627\u0646\u06CC\u200C\u0647\u0627\u06CC_\u0633\u06CC\u0644\u06CC\u06A9\u0627\u062A> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://d-nb.info/gnd/4077444-2> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Nickel\u2013Strunz_classification> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://mn.dbpedia.org/resource/\u0421\u0438\u043B\u0438\u043A\u0430\u0442_\u044D\u0440\u0434\u044D\u0441> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pyrope> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Spessartine> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Oligoclase> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Orthosilicate_(ion)> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Clay_minerals> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Vermiculite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Muscovite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"Silikatmineraloj"@eo .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Bytownite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Apophyllite.sheet.png> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Carletonite.sheet.png> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Riebeckite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Pellyite-chain.png> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Hydrate> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Ilvaite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://af.dbpedia.org/resource/Silikaatminerale> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Os minerais silicatados ou simplesmente silicatos constituem a maior e mais importante classe de minerais constituintes das rochas. Classificam-se de acordo com a estrutura do seu grupo ani\u00F4nico silicato, dependendo da raz\u00E3o entre seus \u00E1tomos de sil\u00EDcio e oxig\u00EAnio. Subclasses:"@pt .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ga.dbpedia.org/resource/Mianra\u00ED_sileac\u00E1ite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Category:Silicate_minerals> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"\uADDC\uC0B0\uC5FC \uAD11\uBB3C(\u7845\u9178\u9E7D\u945B\u7269, silicate minerals)\uC740 \uC9C0\uAC01(\u5730\u6BBC, earth's crust)\uC758 \uC57D 90%\uB97C \uCC28\uC9C0\uD558\uB294 \uC870\uC554 \uAD11\uBB3C\uC774\uB2E4. \uAC01\uAE30 \uB2E4\uB978 \uBE44\uC728\uC758 \uADDC\uC18C\uC640 \uC0B0\uC18C\uB97C \uD568\uC720\uD558\uACE0 \uC788\uB294 \uADDC\uC0B0\uC5FC\uAD70\uC758 \uAD6C\uC870\uB97C \uAE30\uBC18\uC73C\uB85C \uBD84\uB958\uB41C\uB2E4. \uD06C\uAE30\uAC00 \uAC00\uC7A5 \uD06C\uACE0 \uAC00\uC7A5 \uC911\uC694\uD55C \uACC4\uC5F4\uC758 \uC870\uC554 \uAD11\uBB3C\uB85C \uC774\uB8E8\uC5B4\uC838 \uC788\uB2E4."@ko .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Silicate_minerals> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"Roches silicat\u00E9es"@fr .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Cordierite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Inosilicate> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://purl.org/dc/terms/subject>	<http://dbpedia.org/resource/Category:Silicate_minerals> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Plankton> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"Silicate (standardsprachlich Silikate) sind die Salze und Ester der Ortho-Kiesels\u00E4ure (Si(OH)4) und deren Kondensate. Die Ester werden unter Kiesels\u00E4ureester beschrieben, f\u00FCr die Kondensate siehe Kiesels\u00E4uren. Alle Salze sind durch SiO4\u2212Tetraeder aufgebaute Verbindungen, deren Tetraeder jedoch auf verschiedene Weise miteinander verkn\u00FCpft sein k\u00F6nnen. Unverkn\u00FCpfte Stellen der Tetraeder tragen zum Ladungsausgleich Metallkationen bei oder liegen eventuell als Hydroxidionen (OH\u2212) vor. Mit Ausnahme der Alkalisilicate sind Silicate unl\u00F6slich in Wasser oder anderen L\u00F6sungsmitteln. Nat\u00FCrliche Silicate (Silicatminerale) spielen eine gro\u00DFe Rolle in der Mineralogie, da sich sehr viele Minerale dieser Stoffgruppe zuordnen lassen. Die Erdkruste besteht mit einem Massenanteil von \u00FCber 90 % aus Silicaten und der Erdmantel fast vollst\u00E4ndig. Die h\u00E4ufigsten Silicate in der Erdkruste sind mit einem Volumenanteil von 50\u201360 % die Feldsp\u00E4te. Andere wichtige gesteinsbildende Minerale sind Glimmer, Tonminerale, Amphibole, Pyroxene, Granat und Olivin. Das h\u00E4ufige Mineral Quarz (SiO2) wird in deutschsprachiger Literatur zu den Oxiden gez\u00E4hlt, im anglo-amerikanischen Schrifttum jedoch zu den Silicaten."@de .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ast.dbpedia.org/resource/Silicatu> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ru.dbpedia.org/resource/\u0421\u0438\u043B\u0438\u043A\u0430\u0442\u044B_(\u043C\u0438\u043D\u0435\u0440\u0430\u043B\u044B)> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Silicon> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Reflist> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Cancrinite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Allanite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Mineralogy> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://lt.dbpedia.org/resource/Silikatai> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Actinolite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Andalusite> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Silikatmineral utg\u00F6r den st\u00F6rsta och viktigaste gruppen av bergartsbildande mineral. Silikatmineralen \u00E4r naturliga silikater som huvudsakligen best\u00E5r av SiO4-tetraedrar ensamma eller f\u00F6renade med varandra p\u00E5 olika s\u00E4tt (par, kedjor, band ringar, skikt eller 3D-n\u00E4tverk). N\u00E5gon metall beh\u00F6vs f\u00F6r laddningsutj\u00E4mning som ofta \u00E4r natrium, kalium, kalcium, j\u00E4rn eller magnesium. Aluminium kan ibland ing\u00E5 som centralatom i tetraedern i st\u00E4llet f\u00F6r kisel. Kvoten antal syreatomer per centralatom \u00E4r 2 f\u00F6r tektosilikater, 2,5 i fyllosilikat, 2,75 i inosilikat med dubbla kedjor (band), 3 i cyklosilikat och i inosilikat med enkelkedjor, 3,5 i sorosilikat samt 4 f\u00F6r nesosikikat."@sv .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"\u0421\u0438\u043B\u0438\u043A\u0430\u0442\u044B \u0438 \u0430\u043B\u044E\u043C\u043E\u0441\u0438\u043B\u0438\u043A\u0430\u0442\u044B \u043F\u0440\u0435\u0434\u0441\u0442\u0430\u0432\u043B\u044F\u044E\u0442 \u0441\u043E\u0431\u043E\u0439 \u043E\u0431\u0448\u0438\u0440\u043D\u0443\u044E \u0433\u0440\u0443\u043F\u043F\u0443 \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u043E\u0432. \u0414\u043B\u044F \u043D\u0438\u0445 \u0445\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u0435\u043D \u0441\u043B\u043E\u0436\u043D\u044B\u0439 \u0445\u0438\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u0439 \u0441\u043E\u0441\u0442\u0430\u0432 \u0438 \u0438\u0437\u043E\u043C\u043E\u0440\u0444\u043D\u044B\u0435 \u0437\u0430\u043C\u0435\u0449\u0435\u043D\u0438\u044F \u043E\u0434\u043D\u0438\u0445 \u044D\u043B\u0435\u043C\u0435\u043D\u0442\u043E\u0432 \u0438 \u043A\u043E\u043C\u043F\u043B\u0435\u043A\u0441\u043E\u0432 \u044D\u043B\u0435\u043C\u0435\u043D\u0442\u043E\u0432 \u0434\u0440\u0443\u0433\u0438\u043C\u0438. \u0413\u043B\u0430\u0432\u043D\u044B\u043C\u0438 \u0445\u0438\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u043C\u0438 \u044D\u043B\u0435\u043C\u0435\u043D\u0442\u0430\u043C\u0438, \u0432\u0445\u043E\u0434\u044F\u0449\u0438\u043C\u0438 \u0432 \u0441\u043E\u0441\u0442\u0430\u0432 \u0441\u0438\u043B\u0438\u043A\u0430\u0442\u043E\u0432, \u044F\u0432\u043B\u044F\u044E\u0442\u0441\u044F Si, O, Al, Fe2+, Fe3+, Mg, Mn, Ca, Na, K, \u0430 \u0442\u0430\u043A\u0436\u0435 Li, B, Be, Zr, Ti, F, H, \u0432 \u0432\u0438\u0434\u0435 (OH)\u2212 \u0438\u043B\u0438 H2O \u0438 \u0434\u0440\u0443\u0433\u0438\u0435. \u041E\u0431\u0449\u0435\u0435 \u043A\u043E\u043B\u0438\u0447\u0435\u0441\u0442\u0432\u043E \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u044C\u043D\u044B\u0445 \u0432\u0438\u0434\u043E\u0432 \u0441\u0438\u043B\u0438\u043A\u0430\u0442\u043E\u0432 \u043E\u043A\u043E\u043B\u043E 800. \u041F\u043E \u0440\u0430\u0441\u043F\u0440\u043E\u0441\u0442\u0440\u0430\u043D\u0451\u043D\u043D\u043E\u0441\u0442\u0438 \u043D\u0430 \u0438\u0445 \u0434\u043E\u043B\u044E \u043F\u0440\u0438\u0445\u043E\u0434\u0438\u0442\u0441\u044F \u0431\u043E\u043B\u0435\u0435 90 % \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u043E\u0432 \u043B\u0438\u0442\u043E\u0441\u0444\u0435\u0440\u044B. \u0421\u0438\u043B\u0438\u043A\u0430\u0442\u044B \u0438 \u0430\u043B\u044E\u043C\u043E\u0441\u0438\u043B\u0438\u043A\u0430\u0442\u044B \u044F\u0432\u043B\u044F\u044E\u0442\u0441\u044F \u043F\u043E\u0440\u043E\u0434\u043E\u043E\u0431\u0440\u0430\u0437\u0443\u044E\u0449\u0438\u043C\u0438 \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u0430\u043C\u0438. \u0418\u0437 \u043D\u0438\u0445 \u0441\u043B\u043E\u0436\u0435\u043D\u0430 \u043E\u0441\u043D\u043E\u0432\u043D\u0430\u044F \u043C\u0430\u0441\u0441\u0430 \u0433\u043E\u0440\u043D\u044B\u0445 \u043F\u043E\u0440\u043E\u0434: \u043F\u043E\u043B\u0435\u0432\u044B\u0435 \u0448\u043F\u0430\u0442\u044B, \u043A\u0432\u0430\u0440\u0446, \u0441\u043B\u044E\u0434\u044B, \u0440\u043E\u0433\u043E\u0432\u044B\u0435 \u043E\u0431\u043C\u0430\u043D\u043A\u0438, \u043F\u0438\u0440\u043E\u043A\u0441\u0435\u043D\u044B, \u043E\u043B\u0438\u0432\u0438\u043D \u0438 \u0434\u0440\u0443\u0433\u0438\u0435. \u0421\u0430\u043C\u044B\u043C\u0438 \u0440\u0430\u0441\u043F\u0440\u043E\u0441\u0442\u0440\u0430\u043D\u0451\u043D\u043D\u044B\u043C\u0438 \u044F\u0432\u043B\u044F\u044E\u0442\u0441\u044F \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u044B \u0433\u0440\u0443\u043F\u043F\u044B \u043F\u043E\u043B\u0435\u0432\u044B\u0445 \u0448\u043F\u0430\u0442\u043E\u0432 \u0438 \u0437\u0430\u0442\u0435\u043C \u043A\u0432\u0430\u0440\u0446, \u043D\u0430 \u0434\u043E\u043B\u044E \u043A\u043E\u0442\u043E\u0440\u043E\u0433\u043E \u043F\u0440\u0438\u0445\u043E\u0434\u0438\u0442\u0441\u044F \u043E\u043A\u043E\u043B\u043E 12 % \u043E\u0442 \u0432\u0441\u0435\u0445 \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u043E\u0432."@ru .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"Los silicatos son el grupo de minerales de mayor abundancia, pues constituyen el 95 % de la corteza terrestre, adem\u00E1s del grupo de m\u00E1s importancia geol\u00F3gica por ser petrog\u00E9nicos, es decir, los minerales que forman las rocas. Todos los silicatos est\u00E1n compuestos por silicio y ox\u00EDgeno. Estos elementos pueden estar acompa\u00F1ados de otros entre los que destacan aluminio, hierro, magnesio o calcio. Los silicatos forman parte de la mayor\u00EDa de las rocas, arenas y arcillas. Tambi\u00E9n se puede obtener vidrio a partir de muchos silicatos Qu\u00EDmicamente son sales del \u00E1cido sil\u00EDcico. Los silicatos, as\u00ED como los aluminosilicatos \u2014en los que un \u00E1tomo de silicio es sustituido por uno de aluminio\u2014, son la base de numerosos minerales que tienen al tetraedro de silicio-ox\u00EDgeno (un \u00E1tomo de silicio coordinado tetra\u00E9dricamente a cuatro \u00E1tomos de ox\u00EDgeno) como su estructura b\u00E1sica: feldespatos, micas, arcillas. En situaciones de muy altas presiones, el silicio estar\u00E1 coordinado seis veces, o en coordinaci\u00F3n octa\u00E9drica, como en la estructura de perovskita o en el cuarzo polimorfo stishovita (SiO2). (En el \u00FAltimo caso, el mineral ya no tiene una estructura de silicato, sino de rutilo (TiO2) y su grupo asociado, que son \u00F3xidos simples.) Los silicatos forman materiales basados en la repetici\u00F3n de la unidad tetra\u00E9drica [SiO4]4\u2212. El ani\u00F3n [SiO4]4\u2212 tiene cuatro cargas negativas que generalmente son compensadas por la presencia de iones de metales alcalinos o alcalinot\u00E9rreos, as\u00ED como de otros metales como el aluminio. Es com\u00FAn que el Si4+ sea sustituido por Al3+ debido a la similitud en radio i\u00F3nico y en carga; en otros casos, los tetraedros de [AlO4]5\u2212 forman las mismas estructuras que lo hac\u00EDan los tetraedros no sustituidos, pero los requisitos del equilibrio de cargas son diferentes.\u200B Los \u00E1tomos de ox\u00EDgeno pueden compartirse entre dos de estas unidades [SiO4]4\u2212, es decir, se comparte uno de los v\u00E9rtices del tetraedro. Por ejemplo, el disilicato tiene como f\u00F3rmula [Si2O5]6\u2212 y, en general, los silicatos tienen como f\u00F3rmula [SiO3]2\u2212n. En el caso de que todos los \u00E1tomos de ox\u00EDgeno est\u00E9n compartidos, y por tanto la carga est\u00E9 neutralizada, se tiene un cristal, una red tridimensional denominada s\u00EDlice o di\u00F3xido de silicio, SiO2."@es .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"\uADDC\uC0B0\uC5FC \uAD11\uBB3C(\u7845\u9178\u9E7D\u945B\u7269, silicate minerals)\uC740 \uC9C0\uAC01(\u5730\u6BBC, earth's crust)\uC758 \uC57D 90%\uB97C \uCC28\uC9C0\uD558\uB294 \uC870\uC554 \uAD11\uBB3C\uC774\uB2E4. \uAC01\uAE30 \uB2E4\uB978 \uBE44\uC728\uC758 \uADDC\uC18C\uC640 \uC0B0\uC18C\uB97C \uD568\uC720\uD558\uACE0 \uC788\uB294 \uADDC\uC0B0\uC5FC\uAD70\uC758 \uAD6C\uC870\uB97C \uAE30\uBC18\uC73C\uB85C \uBD84\uB958\uB41C\uB2E4. \uD06C\uAE30\uAC00 \uAC00\uC7A5 \uD06C\uACE0 \uAC00\uC7A5 \uC911\uC694\uD55C \uACC4\uC5F4\uC758 \uC870\uC554 \uAD11\uBB3C\uB85C \uC774\uB8E8\uC5B4\uC838 \uC788\uB2E4."@ko .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"\u0421\u0438\u043B\u0438\u043A\u0430\u0442\u044B (\u043C\u0438\u043D\u0435\u0440\u0430\u043B\u044B)"@ru .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"Silikatmineral utg\u00F6r den st\u00F6rsta och viktigaste gruppen av bergartsbildande mineral. Silikatmineralen \u00E4r naturliga silikater som huvudsakligen best\u00E5r av SiO4-tetraedrar ensamma eller f\u00F6renade med varandra p\u00E5 olika s\u00E4tt (par, kedjor, band ringar, skikt eller 3D-n\u00E4tverk). N\u00E5gon metall beh\u00F6vs f\u00F6r laddningsutj\u00E4mning som ofta \u00E4r natrium, kalium, kalcium, j\u00E4rn eller magnesium. Aluminium kan ibland ing\u00E5 som centralatom i tetraedern i st\u00E4llet f\u00F6r kisel. Kvoten antal syreatomer per centralatom \u00E4r 2 f\u00F6r tektosilikater, 2,5 i fyllosilikat, 2,75 i inosilikat med dubbla kedjor (band), 3 i cyklosilikat och i inosilikat med enkelkedjor, 3,5 i sorosilikat samt 4 f\u00F6r nesosikikat. De omkring 500 silikatmineralen klassificeras efter strukturen p\u00E5 deras silikatanjongrupp."@sv .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"\u041F\u0440\u0438\u0440\u043E\u0434\u043D\u0456 \u0441\u0438\u043B\u0456\u043A\u0430\u0442\u0438 \u2014 \u0441\u043F\u043E\u043B\u0443\u043A\u0438 \u0434\u0456\u043E\u043A\u0441\u0438\u0434\u0443 \u043A\u0440\u0435\u043C\u043D\u0456\u044E \u0437 \u043E\u043A\u0441\u0438\u0434\u0430\u043C\u0438 \u0456\u043D\u0448\u0438\u0445 \u0445\u0456\u043C\u0456\u0447\u043D\u0438\u0445 \u0435\u043B\u0435\u043C\u0435\u043D\u0442\u0456\u0432, \u043A\u043B\u0430\u0441 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432, \u0441\u043E\u043B\u0435\u0439 \u043A\u0440\u0435\u043C\u043D\u0456\u0454\u0432\u043E\u0457, \u0456\u0437\u043E- \u0456 \u0433\u0435\u0442\u0435\u0440\u043E\u043F\u043E\u043B\u0456\u043A\u0440\u0435\u043C\u043D\u0456\u0454\u0432\u0438\u0445 \u043A\u0438\u0441\u043B\u043E\u0442."@uk .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Fractionation> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Datolite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://lb.dbpedia.org/resource/Silikat> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://eu.dbpedia.org/resource/Silikato_(mineral)> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://nl.dbpedia.org/resource/Silicaten> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Diopside> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Cummingtonite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Tanzanite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Tremolite-chain.png> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Els minerals silicats formen la classe m\u00E9s gran i m\u00E9s important dels minerals que formen roques, i constitueixen aproximadament el 90% de l'escor\u00E7a terrestre. Es classifiquen basant-se en l'estructura del seu grup silicat. Tots el minerals silicats contenen silici i oxigen. Segons la seva composici\u00F3 trobem nesosilicats, sorosilicats, ciclosilicats, inosilicats, fil\u00B7losilicats i tectosilicats."@ca .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Cyclosilicate_exhibit,_Museum_of_Geology,_South_Dakota.jpg> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Willemite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Quartz_oisan.jpg> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Labradorite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Grunerite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"Silicate minerals are rock-forming minerals made up of silicate groups. They are the largest and most important class of minerals and make up approximately 90 percent of Earth's crust. In mineralogy, silica (silicon dioxide) SiO2 is usually considered a silicate mineral. Silica is found in nature as the mineral quartz, and its polymorphs. On Earth, a wide variety of silicate minerals occur in an even wider range of combinations as a result of the processes that have been forming and re-working the crust for billions of years. These processes include partial melting, crystallization, fractionation, metamorphism, weathering, and diagenesis. Living organisms also contribute to this geologic cycle. For example, a type of plankton known as diatoms construct their exoskeletons (\"frustules\") from silica extracted from seawater. The frustules of dead diatoms are a major constituent of deep ocean sediment, and of diatomaceous earth."@en .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Beta-quartz-CM-2D-balls.png> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Amphibole> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Fayalite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Lazurite> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"Mineral silikat"@in .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Transl> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Clinozoisite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://sw.dbpedia.org/resource/Madini_silikati> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Bazzite_-_Fibbia_Ticino_Switzerland.jpg> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Aluminosilicate> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Aluminum> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Melilite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Hedenbergite> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Sekaninaite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://als.dbpedia.org/resource/Silikat> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"Silicato"@it .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Mordenite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pectolite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Crust_(geology)> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Diatomaceous_Earth_BrightField.jpg> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Meionite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Chrysotile> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"La silikatmineraloj estas la plej granda kaj plej grava klaso de petrofaraj mineraloj. Oni klasifikas ilin la\u016D la strukturo de ilia silikat-jon-grupo. Subklasoj:"@eo .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://fi.dbpedia.org/resource/Silikaattimineraali> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Phlogopite> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Silicate (standardsprachlich Silikate) sind die Salze und Ester der Ortho-Kiesels\u00E4ure (Si(OH)4) und deren Kondensate. Die Ester werden unter Kiesels\u00E4ureester beschrieben, f\u00FCr die Kondensate siehe Kiesels\u00E4uren. Alle Salze sind durch SiO4\u2212Tetraeder aufgebaute Verbindungen, deren Tetraeder jedoch auf verschiedene Weise miteinander verkn\u00FCpft sein k\u00F6nnen. Unverkn\u00FCpfte Stellen der Tetraeder tragen zum Ladungsausgleich Metallkationen bei oder liegen eventuell als Hydroxidionen (OH\u2212) vor. Mit Ausnahme der Alkalisilicate sind Silicate unl\u00F6slich in Wasser oder anderen L\u00F6sungsmitteln."@de .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Glauconite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Lawsonite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Pezzottaite-256889.jpg> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Montmorillonite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Apophyllite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Tremolite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Biotite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://eo.dbpedia.org/resource/Silikatmineraloj> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/ns/prov#wasDerivedFrom>	<http://en.wikipedia.org/wiki/Silicate_mineral?oldid=1124362710&ns=0> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Talc> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://de.dbpedia.org/resource/Silicate> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Coesite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Milarite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Zircon> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://sk.dbpedia.org/resource/Kremi\u010Ditan> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Seawater> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Andradite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://bs.dbpedia.org/resource/Silikatni_minerali> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://tr.dbpedia.org/resource/Silikat> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"\u77FD\u9178\u9E7D\u7926\u7269\u662F\u6307\u542B\u77FD\u7684\u7926\u7269\uFF0C\u662F\u9020\u5CA9\u7926\u7269\u4E2D\u6700\u91CD\u8981\u7684\u4E00\u7A2E\uFF0C\u5730\u6BBC\u4E2D\u4E3B\u8981\u662F\u7531\u77FD\u9178\u9E7D\u7926\u7269\u7D44\u6210\uFF0C\u77FD\u9178\u9E7D\u7926\u7269\u6703\u4F9D\u5176\u5206\u5B50\u7D50\u69CB\u518D\u9032\u884C\u5206\u985E\uFF0C\u4E0D\u540C\u7684\u985E\u5225\u4E2D\uFF0C\u5176\u542B\u77FD\u548C\u6C27\u7684\u6BD4\u4F8B\u4E5F\u6709\u4E0D\u540C\u3002"@zh .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Spodumene> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Zeolite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Earth> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ro.dbpedia.org/resource/Silicat_(mineral)> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Chabazite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Tetrahedral_molecular_geometry> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"Silicate"@de .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://et.dbpedia.org/resource/Silikaatsed_mineraalid> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Enstatite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Portal> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Norbergite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://gl.dbpedia.org/resource/Silicato> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://www.wikidata.org/entity/Q178977> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Tetrahedra> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Garnet> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Earth\u0027s_crust> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Analcime> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Silicate-double-tetrahedra-3D-balls.png> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://sh.dbpedia.org/resource/Silikati> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"Els minerals silicats formen la classe m\u00E9s gran i m\u00E9s important dels minerals que formen roques, i constitueixen aproximadament el 90% de l'escor\u00E7a terrestre. Es classifiquen basant-se en l'estructura del seu grup silicat. Tots el minerals silicats contenen silici i oxigen. Segons la seva composici\u00F3 trobem nesosilicats, sorosilicats, ciclosilicats, inosilicats, fil\u00B7losilicats i tectosilicats."@ca .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Silicate-tetrahedron-3D-balls.png> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Calamine_(mineral)> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pigeonite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://hi.dbpedia.org/resource/\u0938\u093F\u0932\u093F\u0915\u0947\u091F_\u0916\u0928\u093F\u091C> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Olivine> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Grossular> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"K\u0159emi\u010Ditany (silik\u00E1ty) jsou kysl\u00EDkat\u00E9 slou\u010Deniny k\u0159em\u00EDku. Jsou to l\u00E1tky vesm\u011Bs nerozpustn\u00E9 ve vod\u011B a\u017E na k\u0159emi\u010Ditany alkalick\u00FDch kov\u016F Na2SiO3 (vodn\u00ED sklo, kapaln\u00E9 sklo) a K2SiO3. K\u0159emi\u010Ditany v\u00E1penat\u00E9, hlinit\u00E9 a \u017Eelezit\u00E9 jsou rozpustn\u00E9 v kyselin\u00E1ch a jsou sou\u010D\u00E1st\u00ED p\u0159\u00EDrodn\u00EDch miner\u00E1ln\u00EDch surovin pro . V\u0161echny k\u0159emi\u010Ditany lze rozpustit v koncentrovan\u00FDch roztoc\u00EDch alkalick\u00FDch hydroxid\u016F nebo za vysok\u00FDch teplot v jejich tavenin\u00E1ch. K\u0159emi\u010Ditany jako miner\u00E1ly jsou nerosty nekovov\u00E9ho vzhledu a obvykle jsou sou\u010D\u00E1stmi hornin. Jsou to nejroz\u0161\u00ED\u0159en\u011Bj\u0161\u00ED l\u00E1tky v zemsk\u00E9 k\u016F\u0159e."@cs .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Lizardite> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"\u0421\u0438\u043B\u0438\u043A\u0430\u0442\u044B \u0438 \u0430\u043B\u044E\u043C\u043E\u0441\u0438\u043B\u0438\u043A\u0430\u0442\u044B \u043F\u0440\u0435\u0434\u0441\u0442\u0430\u0432\u043B\u044F\u044E\u0442 \u0441\u043E\u0431\u043E\u0439 \u043E\u0431\u0448\u0438\u0440\u043D\u0443\u044E \u0433\u0440\u0443\u043F\u043F\u0443 \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u043E\u0432. \u0414\u043B\u044F \u043D\u0438\u0445 \u0445\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u0435\u043D \u0441\u043B\u043E\u0436\u043D\u044B\u0439 \u0445\u0438\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u0439 \u0441\u043E\u0441\u0442\u0430\u0432 \u0438 \u0438\u0437\u043E\u043C\u043E\u0440\u0444\u043D\u044B\u0435 \u0437\u0430\u043C\u0435\u0449\u0435\u043D\u0438\u044F \u043E\u0434\u043D\u0438\u0445 \u044D\u043B\u0435\u043C\u0435\u043D\u0442\u043E\u0432 \u0438 \u043A\u043E\u043C\u043F\u043B\u0435\u043A\u0441\u043E\u0432 \u044D\u043B\u0435\u043C\u0435\u043D\u0442\u043E\u0432 \u0434\u0440\u0443\u0433\u0438\u043C\u0438. \u0413\u043B\u0430\u0432\u043D\u044B\u043C\u0438 \u0445\u0438\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u043C\u0438 \u044D\u043B\u0435\u043C\u0435\u043D\u0442\u0430\u043C\u0438, \u0432\u0445\u043E\u0434\u044F\u0449\u0438\u043C\u0438 \u0432 \u0441\u043E\u0441\u0442\u0430\u0432 \u0441\u0438\u043B\u0438\u043A\u0430\u0442\u043E\u0432, \u044F\u0432\u043B\u044F\u044E\u0442\u0441\u044F Si, O, Al, Fe2+, Fe3+, Mg, Mn, Ca, Na, K, \u0430 \u0442\u0430\u043A\u0436\u0435 Li, B, Be, Zr, Ti, F, H, \u0432 \u0432\u0438\u0434\u0435 (OH)\u2212 \u0438\u043B\u0438 H2O \u0438 \u0434\u0440\u0443\u0433\u0438\u0435."@ru .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"Silicato (mineral)"@es .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://sv.dbpedia.org/resource/Silikatmineral> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ko.dbpedia.org/resource/\uADDC\uC0B0\uC5FC_\uAD11\uBB3C> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Chrysocolla.jpg> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Dollaseite-(Ce)> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"Mianra\u00ED sileac\u00E1ite"@ga .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Melting> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Heulandite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Sanidine> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Microcline> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Asbestos> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Pezzottaite-256889.jpg> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://sr.dbpedia.org/resource/Silikatni_minerali> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Orthoclase> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Clay> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Los silicatos son el grupo de minerales de mayor abundancia, pues constituyen el 95 % de la corteza terrestre, adem\u00E1s del grupo de m\u00E1s importancia geol\u00F3gica por ser petrog\u00E9nicos, es decir, los minerales que forman las rocas. Todos los silicatos est\u00E1n compuestos por silicio y ox\u00EDgeno. Estos elementos pueden estar acompa\u00F1ados de otros entre los que destacan aluminio, hierro, magnesio o calcio. Los silicatos forman parte de la mayor\u00EDa de las rocas, arenas y arcillas. Tambi\u00E9n se puede obtener vidrio a partir de muchos silicatos"@es .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Zeolite-ZSM-5-vdW.png> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://az.dbpedia.org/resource/Silikatlar> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2002/07/owl#sameAs>	<http://bg.dbpedia.org/resource/\u0421\u0438\u043B\u0438\u043A\u0430\u0442\u0438> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Vesuvianite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Nepheline> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Chlorite_group> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Papagoite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Polymorphism_(materials_science)> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Dumortierite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Chloritoid> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/abstract>	"\u0645\u0639\u0627\u062F\u0646 \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0627\u062A \u0647\u064A \u0645\u062C\u0645\u0648\u0639\u0629 \u0645\u0646 \u0627\u0644\u0645\u0639\u0627\u062F\u0646 \u062A\u0634\u0643\u0644 \u0623\u0643\u0628\u0631 \u0648\u0623\u0647\u0645 \u0641\u0626\u0629 \u0645\u0646 \u0627\u0644\u0645\u0639\u0627\u062F\u0646 \u0627\u0644\u062A\u064A \u0639\u0644\u0649 \u0647\u064A\u0626\u0629 \u0635\u062E\u0648\u0631\u060C \u0648\u062A\u0634\u0643\u0644 \u062D\u0648\u0627\u0644\u064A 96\u066A\u061C \u0645\u0646 \u0645\u0643\u0648\u0646\u0627\u062A \u0627\u0644\u0642\u0634\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629. \u0648\u062A\u0635\u0646\u0641 \u0639\u0644\u0649 \u0623\u0633\u0627\u0633 \u0628\u0646\u0627\u0621 \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0627\u062A \u0641\u064A \u0645\u0631\u0643\u0628\u0627\u062A\u0647\u0645. \u0645\u0639\u0627\u062F\u0646 \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0627\u062A \u062A\u062D\u062A\u0648\u064A \u062C\u0645\u064A\u0639\u0647\u0627 \u0639\u0644\u0649 \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0648\u0646 \u0648\u0627\u0644\u0623\u0648\u0643\u0633\u062C\u064A\u0646."@ar .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Hydrogrossular> .
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<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Pyroxen-chain.png> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Zoisite> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Beryl> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Tourmaline> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://xmlns.com/foaf/0.1/isPrimaryTopicOf>	<http://en.wikipedia.org/wiki/Silicate_mineral> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Water> .
<http://dbpedia.org/resource/Silicate_mineral>	<http://www.w3.org/2000/01/rdf-schema#label>	"Silicaten"@nl .