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http://dbpedia.org/ontology/abstract الحَجَر الغِرْيَني أو حجر الغرين (بالإنجليزية: Siltstone)‏، هو صخر رسوبي حتاتي دقيق الحُبيبات يتكون أساساً من جسيمات غرينية الحجم ولونه بُني مائِل للحُمرة. وهو أدق من الحجر الرملي وأخشن من حجر الصلصال. ويوجد في رواسب المجاري المائية وقِيعان البُحيرات. , Schluffstein (auch Siltstein) ist ein klas … Schluffstein (auch Siltstein) ist ein klastisches Sedimentgestein, in dem Mineralkörner mit einer Korngröße von 0,002 bis 0,063 mm Äquivalentdurchmesser überwiegen. Seine durchschnittliche Korngröße liegt zwischen Tonstein und Feinsandstein. Schluffsteine sind meist siliziklastisch, und die Schluffpartikel bestehen in der Regel aus Quarz.fpartikel bestehen in der Regel aus Quarz. , 粉砂岩（英語：Siltstone）又稱aleurolite，是一種碎屑沉積岩，主要由粉砂組成。與頁岩不同在於缺乏片狀裂理。粉砂岩滲透率和孔隙率相對較低，但可形成天然氣緻密儲層岩石 。 開采需要水力壓裂。粉砂岩在古埃及用於因製造雕像和化妝品調色板。 在 Wadi Hammamat 開采的粉砂岩最有名。是一種堅硬、細粒的粉砂岩，抗剝落。 , La siltite, souvent désignée par son nom a … La siltite, souvent désignée par son nom anglais de siltstone et parfois nommée aleurolite, est une roche sédimentaire dont la granulométrie, entre 1/256 et 1/16 mm, est intermédiaire entre celle du grès, la plus grossière, et celle des lutites (ou pélites), plus fine (les mudstones et les schistes ont une granulométrie encore plus fine).s ont une granulométrie encore plus fine). , Batu lanau (atau batu debu, ditulis pula sebagai batulanau tanpa spasi dalam jargon geologi, bahasa Inggris: siltstone) adalah batuan sedimen yang mempunyai ukuran butir pada kisaran lanau, lebih halus dari batupasir dan lebih kasar dari . , Le siltiti sono rocce sedimentarie apparte … Le siltiti sono rocce sedimentarie appartenenti alla categoria delle rocce clastiche, in particolare delle cosiddette Peliti o Lutiti. Le siltiti sono il prodotto della cementazione diagenetica del silt, ovvero di un sedimento caratterizzato da una granulometria compresa tra 1/16 e 1/256 di mm. Esse sono costituite da una frazione detritica litica consistente spesso in frammenti di minerali tipo feldspati, miche e quarzo, derivanti dalla disgregazione di preesistenti rocce.dalla disgregazione di preesistenti rocce. , Prachovec je sedimentární hornina, zpevněn … Prachovec je sedimentární hornina, zpevněný ekvivalent prachu, přičemž částice velikosti prachu se na složení horniny podílejí minimálně dvěma třetinami. V opačném případě se takové horniny nazývají (2/3 až 1/3 prachových částic), nebo jílovce (méně než 1/3 prachových částic z celého objemu horniny). Vyskytují se ve všech sedimentárních oblastech (od vysokohorských jezer až po mořské příkopy), v různých klimatických podmínkách (od polárních oblastí po džungle) a ve všech geologických obdobích (od archaika až po současnost). Metamorfózou prachovců vznikají břidlice, s pokračujícím stupněm přeměny se tvoří fylity. Důležitým identifikačním znakem prachových hornin je jejich barva, která závisí hlavně na oxidačním stupni železa. Červená až fialová barva indikuje výskyt železitých (Fe3+) kationtů, zelené odstíny naopak železnaté (Fe2+) kationty. Všeobecně se výskyt železitých kationtů váže na kontinentální (terestrická) prostředí, železnaté kationty se vyskytují v mořských prostředích. Nejčastěji je textura prachovců vrstevnatá, ale vyskytují se i masívní textury (hlavně při sedimentaci z hustých proudů). V jemnozrnných sedimentech se často vyskytují konkrece (kalcitové, sideritové, pyritové, křemité a fosfátové), ty vznikají buď těsně po uložení, nebo později, při litifikaci. po uložení, nebo později, při litifikaci. , Aleurit (russisch алеврит alewrit; von alt … Aleurit (russisch алеврит alewrit; von altgriechisch ἄλευρον aleuron ‚Weizenmehl oder -schrot) ist ein grobschluffiges und/oder feinsandiges Lockersediment mit Korngrößen von 0,01 bis 0,1 mm, wobei in groben Aleurit (0,05 bis 0,1 mm) und feinen Aleurit (0,01 bis 0,05 mm) differenziert werden kann. Der Begriff wurde in den 1930er Jahren vom russisch-sowjetischen Petrographen Alexander Sawarizki geprägt und wird heute relativ selten und faktisch nur im östlichen Europa und in den asiatischen Nachfolgestaaten der Sowjetunion verwendet.achfolgestaaten der Sowjetunion verwendet. , Siltsteen of siltiet (Engels: siltstone) is een sedimentair gesteente met een korrelgrootte van 2 - 63 μm. , Siltstone, also known as aleurolite, is a … Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility. Although its permeability and porosity is relatively low, siltstone is sometimes a tight gas reservoir rock, an unconventional reservoir for natural gas that requires hydraulic fracturing for economic gas production. Siltstone was prized in ancient Egypt for manufacturing statuary and cosmetic palettes. The siltstone quarried at Wadi Hammamat was a hard, fine-grained siltstone that resisted flaking and was almost ideal for such uses.laking and was almost ideal for such uses. , Siltsten är en klastisk sedimentär bergart … Siltsten är en klastisk sedimentär bergart med en huvudsaklig kornstorlek som silt, det vill säga 0,002–0,063 mm, vilket är finkornigare än sandsten och grövre än lersten. Vanliga mineraler i siltsten är kvarts, fältspat, glimmer och olika lermineral, där de två tidigare är mer dominerande i grövre partikelstorlekar och lermineral i finare storlekar. Då det är en sedimentär bergart, kan man i siltsten även finna konkretioner och fossiler.sten även finna konkretioner och fossiler. , Алеври́т (рос. алеврит, англ. aleurite, silt; нім. Aleurit) — дрібнозерниста пухка осадова гірська порода. , La limolita es una roca sedimentaria que tiene un tamaño de grano en el rango del limo, más fino que la arenisca y más grueso que arcillas. , Siltito é uma rocha sedimentar clástica fo … Siltito é uma rocha sedimentar clástica formada pela deposição e litificação de sedimentos com grãos de tamanho silte, intermediário entre os tamanhos areia e argila. É composta principalmente por quartzo, feldspato, mica e argila. O Siltito apresenta em sua composição potássio, silício, magnésio e traços de outros 70 elementos. Os siltitos diferem significativamente dos arenitos, devido aos seus poros menores e maior propensão a conter uma fração significativa de argila. Embora muitas vezes confundidos com folhelhos, os siltitos não possuem as laminações e fissibilidade típicas dos folhelhos.ões e fissibilidade típicas dos folhelhos. , Алевролі́т (рос. алевролит, англ. aleuroli … Алевролі́т (рос. алевролит, англ. aleurolite, siltstone; нім. Aleurolith m, Sandschiefer m) — тверда гірська порода, зцементований алеврит. Більш ніж на 50% складається з частинок розміром 0,1-0,01 мм. Колір сірий, чорний, червоно-коричневий, зеленуватий. Структура масивна, шарувата, іноді лінзоподібна. Основні породотвірні матеріали — кварц, глинисті мінерали, цемент (карбонатний, карбонатно-глинистий і слюдистий). В Україні А. поширені в осадових товщах фанерозою. Сировина для виробництва керамзиту, цегли, цементу.для виробництва керамзиту, цегли, цементу. , Aleuryty (siltyty) to pylaste skały okruch … Aleuryty (siltyty) to pylaste skały okruchowe luźne bądź zwięzłe. * Aleuryty zbudowane są z nagromadzonych okruchów mineralnych, pochodzących ze zwietrzałych skał. * Według klasyfikacji opartej na wielkości ziaren są to osadowe skały drobnookruchowe o średnicy ziaren od 0,01 mm do 0,1 mm lub od 0,0063 do 0,063 mm. * Składają się głównie z ziarn frakcji aleurytowej (pyłowej), która reprezentowana jest przez pył, muł, mułowiec, less.owana jest przez pył, muł, mułowiec, less. , Aleŭrolito (de greke άλευρον — faruno kaj greke λίθος — ŝtono) estas la malmola sedimenta rokaĵo, kiu formiĝas el dum ŝtoniĝo. , La limolita, en anglès: siltstone és una roca sedimentària que té la mida del seu gra en el rang del llim, més fi que en la pedra sorrenca i més gruixut que en la pedra argilosa. , Алевролит (от греч. ἄλευρον — мука и λίθος — камень) — твёрдая осадочная горная порода. Образуется из алеврита в процессе литификации. , Алеври́т (англ. aleurite, silt; нем. Aleurit; от др.-греч. ἄλευρον «мука») — рыхлая мелкообломочная осадочная порода.
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rdfs:comment Aleŭrolito (de greke άλευρον — faruno kaj greke λίθος — ŝtono) estas la malmola sedimenta rokaĵo, kiu formiĝas el dum ŝtoniĝo. , Siltstone, also known as aleurolite, is a … Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility. Although its permeability and porosity is relatively low, siltstone is sometimes a tight gas reservoir rock, an unconventional reservoir for natural gas that requires hydraulic fracturing for economic gas production.ic fracturing for economic gas production. , Prachovec je sedimentární hornina, zpevněn … Prachovec je sedimentární hornina, zpevněný ekvivalent prachu, přičemž částice velikosti prachu se na složení horniny podílejí minimálně dvěma třetinami. V opačném případě se takové horniny nazývají (2/3 až 1/3 prachových částic), nebo jílovce (méně než 1/3 prachových částic z celého objemu horniny). Vyskytují se ve všech sedimentárních oblastech (od vysokohorských jezer až po mořské příkopy), v různých klimatických podmínkách (od polárních oblastí po džungle) a ve všech geologických obdobích (od archaika až po současnost). Metamorfózou prachovců vznikají břidlice, s pokračujícím stupněm přeměny se tvoří fylity.račujícím stupněm přeměny se tvoří fylity. , La siltite, souvent désignée par son nom a … La siltite, souvent désignée par son nom anglais de siltstone et parfois nommée aleurolite, est une roche sédimentaire dont la granulométrie, entre 1/256 et 1/16 mm, est intermédiaire entre celle du grès, la plus grossière, et celle des lutites (ou pélites), plus fine (les mudstones et les schistes ont une granulométrie encore plus fine).s ont une granulométrie encore plus fine). , Алеври́т (рос. алеврит, англ. aleurite, silt; нім. Aleurit) — дрібнозерниста пухка осадова гірська порода. , La limolita es una roca sedimentaria que tiene un tamaño de grano en el rango del limo, más fino que la arenisca y más grueso que arcillas. , Siltito é uma rocha sedimentar clástica fo … Siltito é uma rocha sedimentar clástica formada pela deposição e litificação de sedimentos com grãos de tamanho silte, intermediário entre os tamanhos areia e argila. É composta principalmente por quartzo, feldspato, mica e argila. O Siltito apresenta em sua composição potássio, silício, magnésio e traços de outros 70 elementos. Os siltitos diferem significativamente dos arenitos, devido aos seus poros menores e maior propensão a conter uma fração significativa de argila. Embora muitas vezes confundidos com folhelhos, os siltitos não possuem as laminações e fissibilidade típicas dos folhelhos.ões e fissibilidade típicas dos folhelhos. , Le siltiti sono rocce sedimentarie apparte … Le siltiti sono rocce sedimentarie appartenenti alla categoria delle rocce clastiche, in particolare delle cosiddette Peliti o Lutiti. Le siltiti sono il prodotto della cementazione diagenetica del silt, ovvero di un sedimento caratterizzato da una granulometria compresa tra 1/16 e 1/256 di mm. Esse sono costituite da una frazione detritica litica consistente spesso in frammenti di minerali tipo feldspati, miche e quarzo, derivanti dalla disgregazione di preesistenti rocce.dalla disgregazione di preesistenti rocce. , الحَجَر الغِرْيَني أو حجر الغرين (بالإنجليزية: Siltstone)‏، هو صخر رسوبي حتاتي دقيق الحُبيبات يتكون أساساً من جسيمات غرينية الحجم ولونه بُني مائِل للحُمرة. وهو أدق من الحجر الرملي وأخشن من حجر الصلصال. ويوجد في رواسب المجاري المائية وقِيعان البُحيرات. , Siltsteen of siltiet (Engels: siltstone) is een sedimentair gesteente met een korrelgrootte van 2 - 63 μm. , Schluffstein (auch Siltstein) ist ein klas … Schluffstein (auch Siltstein) ist ein klastisches Sedimentgestein, in dem Mineralkörner mit einer Korngröße von 0,002 bis 0,063 mm Äquivalentdurchmesser überwiegen. Seine durchschnittliche Korngröße liegt zwischen Tonstein und Feinsandstein. Schluffsteine sind meist siliziklastisch, und die Schluffpartikel bestehen in der Regel aus Quarz.fpartikel bestehen in der Regel aus Quarz. , Алеври́т (англ. aleurite, silt; нем. Aleurit; от др.-греч. ἄλευρον «мука») — рыхлая мелкообломочная осадочная порода. , La limolita, en anglès: siltstone és una roca sedimentària que té la mida del seu gra en el rang del llim, més fi que en la pedra sorrenca i més gruixut que en la pedra argilosa. , Batu lanau (atau batu debu, ditulis pula sebagai batulanau tanpa spasi dalam jargon geologi, bahasa Inggris: siltstone) adalah batuan sedimen yang mempunyai ukuran butir pada kisaran lanau, lebih halus dari batupasir dan lebih kasar dari . , Алевролит (от греч. ἄλευρον — мука и λίθος — камень) — твёрдая осадочная горная порода. Образуется из алеврита в процессе литификации. , Aleuryty (siltyty) to pylaste skały okruch … Aleuryty (siltyty) to pylaste skały okruchowe luźne bądź zwięzłe. * Aleuryty zbudowane są z nagromadzonych okruchów mineralnych, pochodzących ze zwietrzałych skał. * Według klasyfikacji opartej na wielkości ziaren są to osadowe skały drobnookruchowe o średnicy ziaren od 0,01 mm do 0,1 mm lub od 0,0063 do 0,063 mm. * Składają się głównie z ziarn frakcji aleurytowej (pyłowej), która reprezentowana jest przez pył, muł, mułowiec, less.owana jest przez pył, muł, mułowiec, less. , 粉砂岩（英語：Siltstone）又稱aleurolite，是一種碎屑沉積岩，主要由粉砂組成。與頁岩不同在於缺乏片狀裂理。粉砂岩滲透率和孔隙率相對較低，但可形成天然氣緻密儲層岩石 。 開采需要水力壓裂。粉砂岩在古埃及用於因製造雕像和化妝品調色板。 在 Wadi Hammamat 開采的粉砂岩最有名。是一種堅硬、細粒的粉砂岩，抗剝落。 , Aleurit (russisch алеврит alewrit; von alt … Aleurit (russisch алеврит alewrit; von altgriechisch ἄλευρον aleuron ‚Weizenmehl oder -schrot) ist ein grobschluffiges und/oder feinsandiges Lockersediment mit Korngrößen von 0,01 bis 0,1 mm, wobei in groben Aleurit (0,05 bis 0,1 mm) und feinen Aleurit (0,01 bis 0,05 mm) differenziert werden kann. Der Begriff wurde in den 1930er Jahren vom russisch-sowjetischen Petrographen Alexander Sawarizki geprägt und wird heute relativ selten und faktisch nur im östlichen Europa und in den asiatischen Nachfolgestaaten der Sowjetunion verwendet.achfolgestaaten der Sowjetunion verwendet. , Алевролі́т (рос. алевролит, англ. aleuroli … Алевролі́т (рос. алевролит, англ. aleurolite, siltstone; нім. Aleurolith m, Sandschiefer m) — тверда гірська порода, зцементований алеврит. Більш ніж на 50% складається з частинок розміром 0,1-0,01 мм. Колір сірий, чорний, червоно-коричневий, зеленуватий. Структура масивна, шарувата, іноді лінзоподібна. Основні породотвірні матеріали — кварц, глинисті мінерали, цемент (карбонатний, карбонатно-глинистий і слюдистий). В Україні А. поширені в осадових товщах фанерозою. Сировина для виробництва керамзиту, цегли, цементу.для виробництва керамзиту, цегли, цементу. , Siltsten är en klastisk sedimentär bergart … Siltsten är en klastisk sedimentär bergart med en huvudsaklig kornstorlek som silt, det vill säga 0,002–0,063 mm, vilket är finkornigare än sandsten och grövre än lersten. Vanliga mineraler i siltsten är kvarts, fältspat, glimmer och olika lermineral, där de två tidigare är mer dominerande i grövre partikelstorlekar och lermineral i finare storlekar. Då det är en sedimentär bergart, kan man i siltsten även finna konkretioner och fossiler.sten även finna konkretioner och fossiler.
rdfs:label Aleuryty , Schluffstein , Limolita , Siltsteen , Siltite , Aleurit , Aleŭrolito , Алеврит , Siltstone , Batu lanau , Алевролит , 粉砂岩 , Siltito , Алевроліт , Siltsten , حجر غريني , Prachovec
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http://dbpedia.org/resource/Siltstone + owl:sameAs
 

 

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