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Kleisteen is een klastisch sedimentair ges … Kleisteen is een klastisch sedimentair gesteente dat voornamelijk uit geconsolideerde klei bestaat. Afzonderlijke kleideeltjes (klasten) zijn in kleisteen, net als bij ongeconsolideerde klei, kleiner dan 2 μm en bestaan uit kleimineralen als illiet, smectiet of montmorilloniet. Maximaal 25% van het totaalvolume kan echter uit andere mineralen of andere materie bestaan, zoals kwarts, veldspaat, carbonaten, glauconiet, chloriet, oxiden of organische verbindingen zoals bitumen. Kleisteen kan sterk uiteenlopende kleuren hebben, afhankelijk van de hoeveelheid organische verbindingen en de mineraalinhoud. Wanneer een voornamelijk uit klei bestaand sedimentair gesteente laagjes (laminatie) heeft waarlangs zich een duidelijke splijting vormt, spreekt men niet van een kleisteen maar van een schalie.et van een kleisteen maar van een schalie.
, La pedra argilosa, en anglès, claystone, é … La pedra argilosa, en anglès, claystone, és un terme geològic usat per descriure roques sedimentàries clàstiques que estan compostes principalment per partícules de la mida de l'argila (de menys d'1/256 mil·límetres de diàmetre). Les pedres argilenques no es refereixen a les roques laminades que fàcilment es divideixen en capes fines anomenades en aquest cas pissarres. Són diferents de les pedres de fang o fangolita (mudstones), les quals estan parcialment endurides però es disgreguen quan són molles; la pedra d'argila és un material completament endurit.rgila és un material completament endurit.
, Iłowiec – rodzaj niezłupkowaconej skały osadowej w postaci skonsolidowanego iłu.
* Barwa – szara
* Struktura (frakcja) – iłowa
* Tekstura – bezładna
* Składniki mineralne – kwarc, minerały ilaste, okruchy, spoiwo ilaste.
, Argilŝtono estas sedimento ( malpli ol 0,0 … Argilŝtono estas sedimento ( malpli ol 0,002 mm) kaj konsistas ĉefe el (ekzemple montmorilonito, kaj ). Kromaj mikspartoj estas kvarco, feldspato kaj karbonatoj. Argilŝtonoj enhavantaj multe da nomiĝas . Argilŝtonoj povas havi diversajn kolorojn, ekzemple hel- ĝis malhelgrize, nigra, ruĝa, kaj verda. Pri la koloro respondecas kvantojn da limonito, hematito, kaj kiel bitumeno kaj karbo. Sub premo kaj temperaturo ŝanĝita, ofte maldikfolie fendanta argilŝtono nomiĝas . La fendotavoloj de tiu ŝtonaĵo iras paralele al la tavoloj.e tiu ŝtonaĵo iras paralele al la tavoloj.
, Tonstein ist ein pelitisches Sedimentgeste … Tonstein ist ein pelitisches Sedimentgestein (Korngröße kleiner als 0,002 mm) und besteht überwiegend aus Tonmineralen (z. B. Montmorillonit, Illit und Smectit). Weitere Gemengteile sind Quarz, Feldspat und Carbonate. Stark bituminöse Tonsteine werden Ölschiefer genannt. An den Schichtflächen leicht spaltbare, aber nicht metamorphe Tonsteine werden Schieferton genannt. Tonsteine treten in vielen verschiedenen Farben auf, so etwa hell- bis dunkelgrau, schwarz, rot und grün. Für die Farbe bestimmend sind Beimengungen von Limonit, Hämatit, Chlorit und organischen Kohlenstoffverbindungen wie Bitumen oder Kohle. Unter Druck und Temperatur umgewandelter, meist dünnblättrig spaltender Tonstein wird als Tonschiefer bezeichnet. Die Spaltflächen dieses metamorphen Gesteins verlaufen mitunter nicht parallel zu den Schichtflächen.
* Vorkommen in Deutschland (Auswahl):
* Messel im Landkreis Darmstadt-Dieburg (Hessen)
* Holzmaden (Baden-Württemberg)
* Ohmden (Schwaben)
* Niederschöna (Sachsen)
* Verwendung:
* Tonsteine aus quellfähigen Tonmineralien (Montmorillonit) finden Verwendung in der Ziegel- und keramischen Industrie. in der Ziegel- und keramischen Industrie.
, Jílovec je název sedimentární horniny tvořené v převážné míře (více než dvě třetiny objemu) jílem – částicemi nejmenší velikosti (méně než 0,0020 mm). Více zrnité horniny se nazývají , případně prachovce. Jíly jsou všeobecně jednou z hlavních složek půd.
, Lersten är en vanlig sedimentär bergart. N … Lersten är en vanlig sedimentär bergart. Namnet lersten kommer av att den övervägande delen av partiklarna i lersten är lermineral. Dessa är finkorniga partiklar som är mindre än 0,004 mm i diameter. Färgen kan vara svart eller grå, kalkhaltig lersten är blek. Bleka lerstenar kan vara ljusa nyanser av grått, gult, brunt och rött. Partiklarna är oftast gjord av söndervittrade som fältspat och kvarts. Lermineralen är t.ex. kaolin, organiska material eller mycket små kalciumkarbonatkristaller. Finkorniga lerpartiklar kan transporteras långa avstånd med vind och vatten. Lerstenar kan vara fossilförande. Lersten kan bli till lerskiffer genom dynamometamorfos (en sorts metamorfos som sker under högt tryck).rts metamorfos som sker under högt tryck).
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Jílovec je název sedimentární horniny tvořené v převážné míře (více než dvě třetiny objemu) jílem – částicemi nejmenší velikosti (méně než 0,0020 mm). Více zrnité horniny se nazývají , případně prachovce. Jíly jsou všeobecně jednou z hlavních složek půd.
, Tonstein ist ein pelitisches Sedimentgeste … Tonstein ist ein pelitisches Sedimentgestein (Korngröße kleiner als 0,002 mm) und besteht überwiegend aus Tonmineralen (z. B. Montmorillonit, Illit und Smectit). Weitere Gemengteile sind Quarz, Feldspat und Carbonate. Stark bituminöse Tonsteine werden Ölschiefer genannt. An den Schichtflächen leicht spaltbare, aber nicht metamorphe Tonsteine werden Schieferton genannt. Unter Druck und Temperatur umgewandelter, meist dünnblättrig spaltender Tonstein wird als Tonschiefer bezeichnet. Die Spaltflächen dieses metamorphen Gesteins verlaufen mitunter nicht parallel zu den Schichtflächen.nter nicht parallel zu den Schichtflächen.
, La pedra argilosa, en anglès, claystone, é … La pedra argilosa, en anglès, claystone, és un terme geològic usat per descriure roques sedimentàries clàstiques que estan compostes principalment per partícules de la mida de l'argila (de menys d'1/256 mil·límetres de diàmetre). Les pedres argilenques no es refereixen a les roques laminades que fàcilment es divideixen en capes fines anomenades en aquest cas pissarres. Són diferents de les pedres de fang o fangolita (mudstones), les quals estan parcialment endurides però es disgreguen quan són molles; la pedra d'argila és un material completament endurit.rgila és un material completament endurit.
, Argilŝtono estas sedimento ( malpli ol 0,0 … Argilŝtono estas sedimento ( malpli ol 0,002 mm) kaj konsistas ĉefe el (ekzemple montmorilonito, kaj ). Kromaj mikspartoj estas kvarco, feldspato kaj karbonatoj. Argilŝtonoj enhavantaj multe da nomiĝas . Argilŝtonoj povas havi diversajn kolorojn, ekzemple hel- ĝis malhelgrize, nigra, ruĝa, kaj verda. Pri la koloro respondecas kvantojn da limonito, hematito, kaj kiel bitumeno kaj karbo. Sub premo kaj temperaturo ŝanĝita, ofte maldikfolie fendanta argilŝtono nomiĝas . La fendotavoloj de tiu ŝtonaĵo iras paralele al la tavoloj.e tiu ŝtonaĵo iras paralele al la tavoloj.
, Iłowiec – rodzaj niezłupkowaconej skały osadowej w postaci skonsolidowanego iłu.
* Barwa – szara
* Struktura (frakcja) – iłowa
* Tekstura – bezładna
* Składniki mineralne – kwarc, minerały ilaste, okruchy, spoiwo ilaste.
, Kleisteen is een klastisch sedimentair ges … Kleisteen is een klastisch sedimentair gesteente dat voornamelijk uit geconsolideerde klei bestaat. Afzonderlijke kleideeltjes (klasten) zijn in kleisteen, net als bij ongeconsolideerde klei, kleiner dan 2 μm en bestaan uit kleimineralen als illiet, smectiet of montmorilloniet. Maximaal 25% van het totaalvolume kan echter uit andere mineralen of andere materie bestaan, zoals kwarts, veldspaat, carbonaten, glauconiet, chloriet, oxiden of organische verbindingen zoals bitumen. Kleisteen kan sterk uiteenlopende kleuren hebben, afhankelijk van de hoeveelheid organische verbindingen en de mineraalinhoud.anische verbindingen en de mineraalinhoud.
, Lersten är en vanlig sedimentär bergart. N … Lersten är en vanlig sedimentär bergart. Namnet lersten kommer av att den övervägande delen av partiklarna i lersten är lermineral. Dessa är finkorniga partiklar som är mindre än 0,004 mm i diameter. Färgen kan vara svart eller grå, kalkhaltig lersten är blek. Bleka lerstenar kan vara ljusa nyanser av grått, gult, brunt och rött. Partiklarna är oftast gjord av söndervittrade som fältspat och kvarts. Lermineralen är t.ex. kaolin, organiska material eller mycket små kalciumkarbonatkristaller. Finkorniga lerpartiklar kan transporteras långa avstånd med vind och vatten. Lerstenar kan vara fossilförande. Lersten kan bli till lerskiffer genom dynamometamorfos (en sorts metamorfos som sker under högt tryck).rts metamorfos som sker under högt tryck).
|
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Pedra argilosa
, Argilŝtono
, Iłowiec (skała osadowa)
, Tonstein
, Lersten (bergart)
, Jílovec
, Kleisteen
, Claystone
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|
http://dbpedia.org/resource/Claystone +
|
owl:sameAs |
