Mudrock (original) (raw)
Skała ilasta - skała osadowa zawierająca ponad 50% frakcji pelitowej o ziarnach poniżej 0,01 mm, pochodzenia sedymetacyjnego lub wietrzeniowego, złożona głównie z glinokrzemianów stanowiących produkt wietrzenia chemicznego skał magmowych. Skała zbudowana głównie z illitu, kaolinitu, montmorillonitu lub innych minerałów ilastych, występować mogą również drobne ziarna kwarcu, łyszczyków, węglanów, związków żelaza.
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dbo:abstract | Les mudrocks (littéralement des roches de boues) sont une classe de roches sédimentaires siliciclastiques à grains fins. Les mudrocks sont assimilables aux lutites.En effet, une partie de la terminologie géologique anglaise, réputée plus précise que la terminologie employée en français, utilisant les termes « shale », « slate »,« mudstone », « claystone », « mudrock » et « clayrock », est abondamment utilisée en français depuis des années 1970, (quelques fois plus tôt, dans les cercles des géologues du Québec notamment, et dans l'industrie pétrolière), lorsque la terminologie française utilise des expressions réputées imprécises comme schiste argileux, pour décrire les roches d'aspect terne « chargées quelquefois de paillettes de mica, colorées en brun, en jaune, ou en vert, ou bien en noir; dans ce dernier cas leur coloration est due à des matières charbonneuses ». Les termes « mudstone » et « mudrock » font référence à l'expression « mud » qui à le même sens que boue en français, mais désigne ici les plus fines particules véhiculées par le vent puis les rivières et qui vont sédimenter, jusque très loin dans les océans (et compactées vont former les mudrocks). Approximativement 60% des roches sédimentaires exposées à la surface de la Terre sont aujourd'hui des mudrocks. (fr) Mudrocks are a class of fine-grained siliciclastic sedimentary rocks. The varying types of mudrocks include siltstone, claystone, mudstone, slate, and shale. Most of the particles of which the stone is composed are less than 1⁄16 mm (0.0625 mm; 0.00246 in) and are too small to study readily in the field. At first sight, the rock types appear quite similar; however, there are important differences in composition and nomenclature. There has been a great deal of disagreement involving the classification of mudrocks. A few important hurdles to their classification include the following: 1. * Mudrocks are the least understood and among the most understudied sedimentary rocks to date. 2. * Studying mudrock constituents is difficult due to their diminutive size and susceptibility to weathering on outcrops. 3. * And most importantly, scientists accept more than one classification scheme. Mudrocks make up 50% of the sedimentary rocks in the geologic record and are easily the most widespread deposits on Earth. Fine sediment is the most abundant product of erosion, and these sediments contribute to the overall omnipresence of mudrocks. With increased pressure over time, the platey clay minerals may become aligned, with the appearance of parallel layering (fissility). This finely bedded material that splits readily into thin layers is called shale, as distinct from mudstone. The lack of fissility or layering in mudstone may be due either to the original texture or to the disruption of layering by burrowing organisms in the sediment prior to lithification. From the beginning of civilization, when pottery and mudbricks were made by hand, to now, mudrocks have been important. The first book on mudrocks, Geologie des Argils by Millot, was not published until 1964; however, scientists, engineers, and oil producers have understood the significance of mudrocks since the discovery of the Burgess Shale and the relatedness of mudrocks and oil. Literature on this omnipresent rock-type has been increasing in recent years, and technology continues to allow for better analysis. (en) Skała ilasta - skała osadowa zawierająca ponad 50% frakcji pelitowej o ziarnach poniżej 0,01 mm, pochodzenia sedymetacyjnego lub wietrzeniowego, złożona głównie z glinokrzemianów stanowiących produkt wietrzenia chemicznego skał magmowych. Skała zbudowana głównie z illitu, kaolinitu, montmorillonitu lub innych minerałów ilastych, występować mogą również drobne ziarna kwarcu, łyszczyków, węglanów, związków żelaza. (pl) Гли́нисті поро́ди — група порід, що складені головним чином глинистими мінералами (каолініт, гідрослюди, монтморилоніт, палигорськіт та інші), розмір часток яких не перевищує 0,01 мм у діаметрі, та тонкими уламками інших мінералів. (uk) |
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gold:hypernym | dbr:Rocks |
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rdfs:comment | Skała ilasta - skała osadowa zawierająca ponad 50% frakcji pelitowej o ziarnach poniżej 0,01 mm, pochodzenia sedymetacyjnego lub wietrzeniowego, złożona głównie z glinokrzemianów stanowiących produkt wietrzenia chemicznego skał magmowych. Skała zbudowana głównie z illitu, kaolinitu, montmorillonitu lub innych minerałów ilastych, występować mogą również drobne ziarna kwarcu, łyszczyków, węglanów, związków żelaza. (pl) Гли́нисті поро́ди — група порід, що складені головним чином глинистими мінералами (каолініт, гідрослюди, монтморилоніт, палигорськіт та інші), розмір часток яких не перевищує 0,01 мм у діаметрі, та тонкими уламками інших мінералів. (uk) Mudrocks are a class of fine-grained siliciclastic sedimentary rocks. The varying types of mudrocks include siltstone, claystone, mudstone, slate, and shale. Most of the particles of which the stone is composed are less than 1⁄16 mm (0.0625 mm; 0.00246 in) and are too small to study readily in the field. At first sight, the rock types appear quite similar; however, there are important differences in composition and nomenclature. There has been a great deal of disagreement involving the classification of mudrocks. A few important hurdles to their classification include the following: (en) Les mudrocks (littéralement des roches de boues) sont une classe de roches sédimentaires siliciclastiques à grains fins. Les mudrocks sont assimilables aux lutites.En effet, une partie de la terminologie géologique anglaise, réputée plus précise que la terminologie employée en français, utilisant les termes « shale », « slate »,« mudstone », « claystone », « mudrock » et « clayrock », est abondamment utilisée en français depuis des années 1970, (quelques fois plus tôt, dans les cercles des géologues du Québec notamment, et dans l'industrie pétrolière), lorsque la terminologie française utilise des expressions réputées imprécises comme schiste argileux, pour décrire les roches d'aspect terne « chargées quelquefois de paillettes de mica, colorées en brun, en jaune, ou en vert, ou bien en noi (fr) |
rdfs:label | Mudrock (en) Mudrock (fr) Skała ilasta (pl) Глинисті породи (uk) |
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prov:wasDerivedFrom | wikipedia-en:Mudrock?oldid=1105875878&ns=0 |
foaf:depiction | wiki-commons:Special:FilePath/Mississippi_delta_from_space.jpg wiki-commons:Special:FilePath/GLMsed.jpg wiki-commons:Special:FilePath/Claystone2.jpg wiki-commons:Special:FilePath/Fossil_Ridge.jpg wiki-commons:Special:FilePath/MarcellusShaleCloseUp.jpg wiki-commons:Special:FilePath/Pyrite-117549.jpg wiki-commons:Special:FilePath/Red_mudrock.jpg wiki-commons:Special:FilePath/Siltstone1.jpg wiki-commons:Special:FilePath/Slate_roof_in_Andorra.jpg |
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