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About: Rapakivi granite
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href="http://dbpedia.org">dbpedia.org</a></span> </div> </div> </div> <div class="row pt-2"> <div class="col-xs-9 col-sm-10"> <p class="lead">Rapakivi granite is a hornblende-biotite granite containing large round crystals of orthoclase each with a rim of oligoclase (a variety of plagioclase). The name has come to be used most frequently as a textural term where it implies plagioclase rims around orthoclase in plutonic rocks. Rapakivi is a Finnish compound of "rapa" (meaning "mud" or "sand") and "kivi" (meaning "rock"), because the different heat expansion coefficients of the component minerals make exposed rapakivi crumble easily into sand.</p> </div> <div class="col-xs-3 col-sm-2"> <a href="#" class="thumbnail"> <img src="http://commons.wikimedia.org/wiki/Special:FilePath/Rapakiwi-Geschiebe.jpg?width=300" alt="thumbnail" class="img-fluid" /> </a> </div> </div> </div> </section> <!-- page-header --> <!-- property-table --> <section> <div class="container-xl"> <div class="row"> <div class="table-responsive"> <table class="table table-hover table-sm table-light"> <thead> <tr> <th class="col-xs-3 ">Property</th> <th class="col-xs-9 px-3">Value</th> </tr> </thead> <tbody> <tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/ontology/abstract"><small>dbo:</small>abstract</a> </td><td class="col-10 text-break"><ul> <li style="display:none;"><span class="literal"><span property="dbo:abstract" lang="ar" >الجرانيت الراباكيفي أو النسيج الراباكيفي (بالإنجليزية: Rapakivi granite)، هي أنواع من الصخور الجرانيتية التي تحتوي على كمية وفيرة من بلورات كبيرة بيضاوية الشكل من الفلسبار القلوي من الأورثوكليز أو الميكروكلين، مغطى بالبلاجيوكليز الصودي. يحيط بهذه البلورات كَنانْ من الكوارتز، الفلسبار القلوي، البلاجيوكليز بيوتيت وهورنبلند. وقد يحتوي مركز البلورات البيضاوية الكبيرة على حبيبات من معادن الكنان مرتبة في شرائط متحدة المركز. وعادة ما يطلق الآن مصطلح جرانيت راباكيفي على أي صخر جرانيتي يحتوي على بلورات من الفلسبار القلوي المغطى. وُصف لأول مرة في 1891 من قِبل العالم الفنلندي جاكوب سيديرهولم. كما أنها تنتشر بكثرة في جنوب فنلندا. كان يُستخدم في بناء الكنائس الحجرية في أولاند، وهي من معادن البناء.</span><small> (ar)</small></span></li> <li style="display:none;"><span class="literal"><span property="dbo:abstract" lang="de" >Als Rapakiwi oder früher als Murkstein bezeichnet man Granite mit ungleichkörnigen und bis zu mehreren Zentimetern großen, runden Einsprenglingen (Ovoide) aus Feldspat und einer relativ feinkörnigen Grundmasse aus Quarz, verschiedenen Feldspäten und Mafischen Mineralen.</span><small> (de)</small></span></li> <li style="display:none;"><span class="literal"><span property="dbo:abstract" lang="eo" >Rapakivoj estas granitgrupo kun diversgrajnaj kaj ĝis plurajn centimetrojn grandaj, rondaj dise entenataj kristaloj (ovoidoj) el feldspato kaj relative fajngrajna matrico el kvarco, diversaj feldapatoj kaj (mineraloj el magnezio kaj fero).</span><small> (eo)</small></span></li> <li style="display:none;"><span class="literal"><span property="dbo:abstract" lang="eu" >Rapakivi granitoa inguratutako ortosazko kristal biribil handiak dituen granito mota bat da. Hauen kanpoaldean material ilunak kokatzen dira, eta hornblenda batez ere. Hutsuneak betetzen, azkenik, kuartzoa agertzen da. Orokorrean oligoklasaz inguratutako ortosa duen edozein granito izendatzeko erabiltzen da izena. Hau fineratik dator, Finlandian eta bereziki erruz aurkitu daitekelako, nahiz eta munduan nahiko urria den.</span><small> (eu)</small></span></li> <li style="display:none;"><span class="literal"><span property="dbo:abstract" lang="fr" >Le granite rapakivi est un type de granite particulièrement sensible à l'érosion. Il est riche en hornblende et biotite et contient de grands cristaux arrondis d'orthose rose enveloppés dans de l'oligoclase gris. Le mot rapakivi vient du finnois et désigne une roche décomposée ou s'effritant facilement.</span><small> (fr)</small></span></li> <li><span class="literal"><span property="dbo:abstract" lang="en" >Rapakivi granite is a hornblende-biotite granite containing large round crystals of orthoclase each with a rim of oligoclase (a variety of plagioclase). The name has come to be used most frequently as a textural term where it implies plagioclase rims around orthoclase in plutonic rocks. Rapakivi is a Finnish compound of "rapa" (meaning "mud" or "sand") and "kivi" (meaning "rock"), because the different heat expansion coefficients of the component minerals make exposed rapakivi crumble easily into sand. Rapakivi was first described by Finnish petrologist Jakob Sederholm in 1891. Since then, southern Finland's rapakivi granite intrusions have been the type locality of this variety of granite.</span><small> (en)</small></span></li> <li style="display:none;"><span class="literal"><span property="dbo:abstract" lang="nl" >Rapakivi is een texturele variëteit van graniet. Het gesteente wordt gekenmerkt door de zeer grote (1 – 5 cm) fenocrysten van orthoklaas (kaliveldspaat) soms met een ring van oligoklaas (plagioklaas). De grondmassa bestaat uit kwarts, veldspaten en mafische mineralen. De veel fijner kristallijne grondmassa wordt gekenmerkt door kristallen van kwarts en veldspaat die door elkaar heen geweven zijn.</span><small> (nl)</small></span></li> <li style="display:none;"><span class="literal"><span property="dbo:abstract" lang="pl" >Granit rapakiwi (fin. rapakivi – zgniły kamień) – regionalna nazwa dla granitoidów pochodzących z Finlandii. Skała magmowa głębinowa, barwy czerwono-brunatnej, o teksturze nierównoziarnistej, jawnokrystalicznej niekiedy zbliżonej do porfirowej. Składa się z dużych czerwonych lub różowoczerwonych kryształów skaleni potasowych, otoczonych zielonkawą obwódką oligoklazu oraz poprzerastanych wrostkami kwarcu, hornblendy i biotytu. Łatwo podlega procesom wietrzenia. Został opisany w 1891 roku przez fińskiego petrologa Jakoba J. Sederholma. Granit rapakiwi występuje w największych ilościach w południowo-zachodniej Finlandii, można go też znaleźć w Szwecji, północno-zachodniej Rosji oraz na Wyspach Alandzkich. W Polsce występuje w postaci silnie zwietrzałych głazów narzutowych przywleczonych przez lodowce w okresie plejstocenu. Wykorzystywano go w średniowieczu na Wyspach Alandzkich do budowy kościołów.</span><small> (pl)</small></span></li> <li style="display:none;"><span class="literal"><span property="dbo:abstract" lang="ru" >Рапакиви (фин. rapakivi — «гнилой или крошащийся камень») — горная порода кислого состава, разновидность гранита. Он состоит из олигоклаза (около 20 %), ортоклаза (около 40 %), идиоморфного кварца (около 30 %), и содержит малые примеси второстепенных акцессорных минералов (около 2 %): ортита, амфибола, диопсида, сфена, апатита, магнетита и др. На срезе отчётливо различается крупная зернистость этого гранита. По своей прочности и долговечности сильно уступает в сравнении с образцами мелкозернистого гранита. Может быть окрашен в различные оттенки буровато-розового, иногда это красноватый, зеленоватый. Гранит рапакиви широко распространён в Швеции и Финляндии, встречается в Карелии и Ленинградской области (выборгиты — в районе г. Выборга, питерлит — в окрестностях деревень Виролахти, Питерлакс, Вилькиля), на Украине (район с. Городище Черкасской области). Овоиды в выборгите окрашены в красные и розовые тона и часто окружены зеленовато-серыми оторочками минерала плагиоклаза. Монолиты выборгитов вырубались для Казанского собора в имении баронов Николаи, в каменоломне Саанлахти, в западной части Монрепо на острове Твердыш, в черте нынешнего Выборга. Из многотонных глыб артель Суханова вытесала 56 колонн для Казанского собора. Цоколь Биржи выполнен из двух сортов выборгита – розового и серого. Из серого выборгита вытесаны базы Ростральных колонн и вырезаны маскароны в стенах спуска к Неве на Стрелке Васильевского острова. На монолите из этого гранита установлен «Медный всадник». В питерлите овоиды без плагиоклазовых оторочек (или вообще нет овоидов). Самый большой в мире монолит гранита весом в 600 тонн был вырублен по способу Суханова в Питерлакской каменоломне для изготовления Александровской колонны на Дворцовой площади.</span><small> (ru)</small></span></li> <li style="display:none;"><span class="literal"><span property="dbo:abstract" lang="uk" >Рапаківі (рос. рапакиви, англ. rapakiwi, нім. Rapakiwi m) — двополевошпатові граніти підвищеної лужності з характерною центричною структурою, зумовленою наявністю великих овоїдів калієвого польового шпату, звичайно оточених облямівками олігоклазу. Така структура обумовлює відносно швидке руйнування породи. Різновид Р., в якому овоїди не покриті олігоклазовою оболонкою, наз. , якщо облямовані овоїди переважають, порода наз. . Колір сірий і рожевий. Темнокольорові мінерали представлені біотитом і роговою обманкою високої залізистості; акцесорні — титаномагнетит, олівін, флюорит, апатит, циркон. Густина бл. 2,65, пористість 0,3 %, опір стисненню 100—200 МПа. Р. — типові субплатформні посторогенні утворення, що виникли в тісній асоціації з комагматичними ефузивами і базальтоїдним магматизмом. Найбільші масиви знаходяться на Російській і Півн.-Американській платформах. Назва — від фін. «rapa» — гнилий і «kivi» — камінь (за властивістю швидко руйнуватися).</span><small> (uk)</small></span></li> <li style="display:none;"><span class="literal"><span property="dbo:abstract" lang="sv" >Rapakivi eller rapakivigranit [ra'pakivi-] är en granit bildad av hornblände-biotit under , vanligen röd och bestående av stora rundade kristaller av ortoklas täckta med oligoklas. Rapakivi är i allmänhet förhållandevis grovkornig och har ofta porfyrisk textur, i samband med vilken de rundade och flera centimeter stora kalifältspatströkornen i den kan vara omgivna av ett yttre smalt oligoklas- eller plagioklasbälte. De övriga mineral vilka den består av är kvarts och amfibol. Ordet är sammansatt av orden på finska ”rapa” (ordagrant "lera", "smuts") och kivi ("sten", "stenblock") och betyder i överförd bemärkelse ungefär "vittrad sten" eller "förvittrad granit", eftersom de olika värmeexpansionskoefficienterna av mineralerna som rapakivigranit består av gör den smulig. En del varieteter vittrar lätt till grus. Rapakivi är en ganska ovanlig typ av granit och den yngsta kända prekambriska graniten. I Finland finns den i form av viborgit och pyterlahtigranit i Viborgbatoliten i sydöstra Finland, samt bland annat i Letala i sydvästra Finland och i Ålandsbatoliten på Åland. Finlands största förekomst av rapakivi är Viborgs rapakivimassiv, i vilket Repovesiområdet söder om sundet ingår. I Sverige förekommer den i smärre områden i norra Sverige vid Nordingrå, Ragunda socken, Strömsbro och på Rödön öster om Alnön, samt – under namnet götemargranit – i södra Sverige vid Kråkemåla i närheten av sjön Götemaren samt under namnet jungfrugranit på Blå Jungfrun. Rapakivi är ett material som ofta använts i Ålands medeltida stenkyrkor och i byggnadsprojekt och monument i Sankt Petersburg i Ryssland, till exempel pelare i Isakskatedralen samt . Bergarten är en viktig bas för Finlands stenindustri, med början av export till anläggandet av Rysslands nya huvudstad Sankt Petersburg från slutet av 1700-talet.</span><small> (sv)</small></span></li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/ontology/thumbnail"><small>dbo:</small>thumbnail</a> </td><td class="col-10 text-break"><ul> <li><span class="literal"><a class="uri" rel="dbo:thumbnail" resource="http://commons.wikimedia.org/wiki/Special:FilePath/Rapakiwi-Geschiebe.jpg?width=300" href="http://commons.wikimedia.org/wiki/Special:FilePath/Rapakiwi-Geschiebe.jpg?width=300"><small>wiki-commons</small>:Special:FilePath/Rapakiwi-Geschiebe.jpg?width=300</a></span></li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/ontology/wikiPageID"><small>dbo:</small>wikiPageID</a> </td><td class="col-10 text-break"><ul> <li><span class="literal"><span property="dbo:wikiPageID" datatype="xsd:integer" 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href="http://dbpedia.org/class/yago/Rock114696793"><small>yago</small>:Rock114696793</a></span></li> <li><span class="literal"><a class="uri" rel="rdf:type" resource="http://dbpedia.org/class/yago/Substance100019613" href="http://dbpedia.org/class/yago/Substance100019613"><small>yago</small>:Substance100019613</a></span></li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://www.w3.org/2000/01/rdf-schema#comment"><small>rdfs:</small>comment</a> </td><td class="col-10 text-break"><ul> <li style="display:none;"><span class="literal"><span property="rdfs:comment" lang="de" >Als Rapakiwi oder früher als Murkstein bezeichnet man Granite mit ungleichkörnigen und bis zu mehreren Zentimetern großen, runden Einsprenglingen (Ovoide) aus Feldspat und einer relativ feinkörnigen Grundmasse aus Quarz, verschiedenen Feldspäten und Mafischen Mineralen.</span><small> (de)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:comment" lang="eo" >Rapakivoj estas granitgrupo kun diversgrajnaj kaj ĝis plurajn centimetrojn grandaj, rondaj dise entenataj kristaloj (ovoidoj) el feldspato kaj relative fajngrajna matrico el kvarco, diversaj feldapatoj kaj (mineraloj el magnezio kaj fero).</span><small> (eo)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:comment" lang="eu" >Rapakivi granitoa inguratutako ortosazko kristal biribil handiak dituen granito mota bat da. Hauen kanpoaldean material ilunak kokatzen dira, eta hornblenda batez ere. Hutsuneak betetzen, azkenik, kuartzoa agertzen da. Orokorrean oligoklasaz inguratutako ortosa duen edozein granito izendatzeko erabiltzen da izena. Hau fineratik dator, Finlandian eta bereziki erruz aurkitu daitekelako, nahiz eta munduan nahiko urria den.</span><small> (eu)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:comment" lang="fr" >Le granite rapakivi est un type de granite particulièrement sensible à l'érosion. Il est riche en hornblende et biotite et contient de grands cristaux arrondis d'orthose rose enveloppés dans de l'oligoclase gris. Le mot rapakivi vient du finnois et désigne une roche décomposée ou s'effritant facilement.</span><small> (fr)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:comment" lang="nl" >Rapakivi is een texturele variëteit van graniet. Het gesteente wordt gekenmerkt door de zeer grote (1 – 5 cm) fenocrysten van orthoklaas (kaliveldspaat) soms met een ring van oligoklaas (plagioklaas). De grondmassa bestaat uit kwarts, veldspaten en mafische mineralen. De veel fijner kristallijne grondmassa wordt gekenmerkt door kristallen van kwarts en veldspaat die door elkaar heen geweven zijn.</span><small> (nl)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:comment" lang="ar" >الجرانيت الراباكيفي أو النسيج الراباكيفي (بالإنجليزية: Rapakivi granite)، هي أنواع من الصخور الجرانيتية التي تحتوي على كمية وفيرة من بلورات كبيرة بيضاوية الشكل من الفلسبار القلوي من الأورثوكليز أو الميكروكلين، مغطى بالبلاجيوكليز الصودي. يحيط بهذه البلورات كَنانْ من الكوارتز، الفلسبار القلوي، البلاجيوكليز بيوتيت وهورنبلند. وقد يحتوي مركز البلورات البيضاوية الكبيرة على حبيبات من معادن الكنان مرتبة في شرائط متحدة المركز. وعادة ما يطلق الآن مصطلح جرانيت راباكيفي على أي صخر جرانيتي يحتوي على بلورات من الفلسبار القلوي المغطى.</span><small> (ar)</small></span></li> <li><span class="literal"><span property="rdfs:comment" lang="en" >Rapakivi granite is a hornblende-biotite granite containing large round crystals of orthoclase each with a rim of oligoclase (a variety of plagioclase). The name has come to be used most frequently as a textural term where it implies plagioclase rims around orthoclase in plutonic rocks. Rapakivi is a Finnish compound of "rapa" (meaning "mud" or "sand") and "kivi" (meaning "rock"), because the different heat expansion coefficients of the component minerals make exposed rapakivi crumble easily into sand.</span><small> (en)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:comment" lang="pl" >Granit rapakiwi (fin. rapakivi – zgniły kamień) – regionalna nazwa dla granitoidów pochodzących z Finlandii. Skała magmowa głębinowa, barwy czerwono-brunatnej, o teksturze nierównoziarnistej, jawnokrystalicznej niekiedy zbliżonej do porfirowej. Składa się z dużych czerwonych lub różowoczerwonych kryształów skaleni potasowych, otoczonych zielonkawą obwódką oligoklazu oraz poprzerastanych wrostkami kwarcu, hornblendy i biotytu. Łatwo podlega procesom wietrzenia. Został opisany w 1891 roku przez fińskiego petrologa Jakoba J. Sederholma.</span><small> (pl)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:comment" lang="ru" >Рапакиви (фин. rapakivi — «гнилой или крошащийся камень») — горная порода кислого состава, разновидность гранита. Он состоит из олигоклаза (около 20 %), ортоклаза (около 40 %), идиоморфного кварца (около 30 %), и содержит малые примеси второстепенных акцессорных минералов (около 2 %): ортита, амфибола, диопсида, сфена, апатита, магнетита и др. На срезе отчётливо различается крупная зернистость этого гранита. По своей прочности и долговечности сильно уступает в сравнении с образцами мелкозернистого гранита.</span><small> (ru)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:comment" lang="sv" >Rapakivi eller rapakivigranit [ra'pakivi-] är en granit bildad av hornblände-biotit under , vanligen röd och bestående av stora rundade kristaller av ortoklas täckta med oligoklas. Rapakivi är i allmänhet förhållandevis grovkornig och har ofta porfyrisk textur, i samband med vilken de rundade och flera centimeter stora kalifältspatströkornen i den kan vara omgivna av ett yttre smalt oligoklas- eller plagioklasbälte. De övriga mineral vilka den består av är kvarts och amfibol.</span><small> (sv)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:comment" lang="uk" >Рапаківі (рос. рапакиви, англ. rapakiwi, нім. Rapakiwi m) — двополевошпатові граніти підвищеної лужності з характерною центричною структурою, зумовленою наявністю великих овоїдів калієвого польового шпату, звичайно оточених облямівками олігоклазу. Така структура обумовлює відносно швидке руйнування породи. Найбільші масиви знаходяться на Російській і Півн.-Американській платформах. Назва — від фін. «rapa» — гнилий і «kivi» — камінь (за властивістю швидко руйнуватися).</span><small> (uk)</small></span></li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://www.w3.org/2000/01/rdf-schema#label"><small>rdfs:</small>label</a> </td><td class="col-10 text-break"><ul> <li style="display:none;"><span class="literal"><span property="rdfs:label" lang="ar" >جرانيت راباكيفي</span><small> (ar)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:label" lang="de" >Rapakiwi</span><small> (de)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:label" lang="eo" >Rapakivo</span><small> (eo)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:label" lang="eu" >Rapakivi granito</span><small> (eu)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:label" lang="fr" >Granite rapakivi</span><small> (fr)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:label" lang="nl" >Rapakivi</span><small> (nl)</small></span></li> <li><span class="literal"><span property="rdfs:label" lang="en" >Rapakivi granite</span><small> (en)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:label" lang="pl" >Granit rapakiwi</span><small> (pl)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:label" lang="ru" >Рапакиви</span><small> (ru)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:label" lang="sv" >Rapakivi</span><small> (sv)</small></span></li> <li style="display:none;"><span class="literal"><span property="rdfs:label" lang="uk" >Рапаківі</span><small> (uk)</small></span></li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://www.w3.org/2002/07/owl#sameAs"><small>owl:</small>sameAs</a> </td><td class="col-10 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