. "Cementacja (geologia)"@pl . . . . . . . . . "Cementacja \u2013 proces lityfikacji, polegaj\u0105cy najcz\u0119\u015Bciej na wype\u0142nianiu pierwotnych lub wt\u00F3rnych pustek mi\u0119dzyziarnowych w lu\u017Anych ska\u0142ach klastycznych spoiwem (w\u0119glanami, krzemionk\u0105, zwi\u0105zkami \u017Celaza, minera\u0142ami ilastymi lub innymi zwi\u0105zkami). Jedno z pierwszych stadi\u00F3w diagenezy."@pl . . "Cementatie"@nl . . "Cementacja \u2013 proces lityfikacji, polegaj\u0105cy najcz\u0119\u015Bciej na wype\u0142nianiu pierwotnych lub wt\u00F3rnych pustek mi\u0119dzyziarnowych w lu\u017Anych ska\u0142ach klastycznych spoiwem (w\u0119glanami, krzemionk\u0105, zwi\u0105zkami \u017Celaza, minera\u0142ami ilastymi lub innymi zwi\u0105zkami). Jedno z pierwszych stadi\u00F3w diagenezy."@pl . "Se denomina cementaci\u00F3n al proceso por el cual durante la diag\u00E9nesis precipitan las sales disueltas en el agua situada en los poros de los sedimentos;\u200B las part\u00EDculas constituyentes de estos (clastos, cantos...) quedan unidas entre s\u00ED. La cementaci\u00F3n, junto con la compactaci\u00F3n, producen la litificaci\u00F3n.\u200B El precipitado que se forma se denomina cemento,\u200B y su composici\u00F3n puede ser muy variada, si bien abundan la s\u00EDlice, el carbonato y los \u00F3xidos de hierro.\u200B"@es . . . "La c\u00E9mentation est la pr\u00E9cipitation de sels \u00E0 la surface d'une nappe phr\u00E9atique. \n* Portail de la g\u00E9ologie"@fr . . . . . . "C\u00E9mentation (g\u00E9ologie)"@fr . . . . "\u0426\u0435\u043C\u0435\u043D\u0442\u0443\u0432\u0430\u043D\u043D\u044F (\u0433\u0435\u043E\u043B\u043E\u0433\u0456\u044F) \u2014 \u043F\u0440\u043E\u0446\u0435\u0441 \u043B\u0456\u0442\u0438\u0444\u0456\u043A\u0430\u0446\u0456\u0457, \u0449\u043E \u043D\u0430\u0439\u0447\u0430\u0441\u0442\u0456\u0448\u0435 \u043F\u043E\u043B\u044F\u0433\u0430\u0454 \u0443 \u0437\u0430\u043F\u043E\u0432\u043D\u0435\u043D\u043D\u0456 \u043F\u0435\u0440\u0432\u0438\u043D\u043D\u0438\u0445 \u0430\u0431\u043E \u0432\u0442\u043E\u0440\u0438\u043D\u043D\u0438\u0445 \u043C\u0456\u0436\u0437\u0435\u0440\u043D\u043E\u0432\u0438\u0445 \u043F\u0443\u0441\u0442\u043E\u0442 \u0443 \u043F\u0443\u0445\u043A\u0438\u0445 \u0443\u043B\u0430\u043C\u043A\u043E\u0432\u0438\u0445 \u043F\u043E\u0440\u043E\u0434\u0430\u0445 \u0441\u043F\u043E\u043B\u0443\u0447\u043D\u043E\u044E \u0440\u0435\u0447\u043E\u0432\u0438\u043D\u043E\u044E (\u043A\u0430\u0440\u0431\u043E\u043D\u0430\u0442\u0438, \u043A\u0440\u0435\u043C\u043D\u0435\u0437\u0435\u043C, \u0441\u043F\u043E\u043B\u0443\u043A\u0438 \u0437\u0430\u043B\u0456\u0437\u0430, \u0433\u043B\u0438\u043D\u0438\u0441\u0442\u0456 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0438 \u0430\u0431\u043E \u0456\u043D\u0448\u0456 \u0441\u043F\u043E\u043B\u0443\u043A\u0438). \u041E\u0434\u0438\u043D \u0437 \u043F\u0435\u0440\u0448\u0438\u0445 \u0435\u0442\u0430\u043F\u0456\u0432 \u0434\u0456\u0430\u0433\u0435\u043D\u0435\u0437\u0443."@uk . "5920"^^ . . "Es denomina cimentaci\u00F3 al proc\u00E9s pel qual durant la diag\u00E8nesi precipiten les sals dissoltes en l'aigua situada en els porus dels sediments; les part\u00EDcules constituents d'aquests (clastos, cants...) queden unides entre si. La cimentaci\u00F3, juntament amb la compactaci\u00F3, produeixen la litificaci\u00F3. El precipitat que es forma es denomina ciment, i la seva composici\u00F3 pot ser molt variada, si b\u00E9 abunden el s\u00EDlice, el carbonat i els \u00F2xids de ferro."@ca . . . . . . . . . "\u0426\u0435\u043C\u0435\u043D\u0442\u0443\u0432\u0430\u043D\u043D\u044F (\u0433\u0435\u043E\u043B\u043E\u0433\u0456\u044F)"@uk . . "Zementation (Geologie)"@de . . . . "In der Geologie bezeichnet die Zementation einen bestimmten Prozess der Diagenese, also der Ver\u00E4nderung von sediment\u00E4ren Ablagerungen. Die Zementation ist ein chemisch-physikalischer Vorgang, bei dem Minerale (meist Quarz oder Calcit) \u00FCber w\u00E4ssrige L\u00F6sungen in die Porenr\u00E4ume des Lockersediments transportiert und dort als Zemente ausgef\u00E4llt werden. Die Porosit\u00E4t des Ausgangsmaterials wird dadurch verringert, w\u00E4hrend gleichzeitig die K\u00F6rner des Sediments miteinander verkittet werden."@de . . . "La cementazione \u00E8 uno dei meccanismi con cui si verifica la litificazione dei sedimenti e consistente nella precipitazione di sostanze, portate in soluzione, dalle acque circolanti, nei pori del sedimento. Il processo di litificazione, ossia della trasformazione di un sedimento incoerente in uno coerente (duro), pu\u00F2 verificarsi con azioni meccaniche (costipamento) e con azioni chimiche (la cementazione, per l'appunto). Le azioni meccaniche consistono nella riduzione degli spazi vuoti, ossia dei pori, occupati generalmente da acqua o aria, per mezzo della compressione meccanica con conseguente riduzione del volume. Le reazioni chimiche determinano un'ulteriore riduzione del volume in quanto le acque interstiziali, ossia le acque contenute nei pori, determinano la precipitazione delle sostanze contenute nei pori del sedimento."@it . "1087148184"^^ . "\u0426\u0435\u043C\u0435\u043D\u0442\u0443\u0432\u0430\u043D\u043D\u044F (\u0433\u0435\u043E\u043B\u043E\u0433\u0456\u044F) \u2014 \u043F\u0440\u043E\u0446\u0435\u0441 \u043B\u0456\u0442\u0438\u0444\u0456\u043A\u0430\u0446\u0456\u0457, \u0449\u043E \u043D\u0430\u0439\u0447\u0430\u0441\u0442\u0456\u0448\u0435 \u043F\u043E\u043B\u044F\u0433\u0430\u0454 \u0443 \u0437\u0430\u043F\u043E\u0432\u043D\u0435\u043D\u043D\u0456 \u043F\u0435\u0440\u0432\u0438\u043D\u043D\u0438\u0445 \u0430\u0431\u043E \u0432\u0442\u043E\u0440\u0438\u043D\u043D\u0438\u0445 \u043C\u0456\u0436\u0437\u0435\u0440\u043D\u043E\u0432\u0438\u0445 \u043F\u0443\u0441\u0442\u043E\u0442 \u0443 \u043F\u0443\u0445\u043A\u0438\u0445 \u0443\u043B\u0430\u043C\u043A\u043E\u0432\u0438\u0445 \u043F\u043E\u0440\u043E\u0434\u0430\u0445 \u0441\u043F\u043E\u043B\u0443\u0447\u043D\u043E\u044E \u0440\u0435\u0447\u043E\u0432\u0438\u043D\u043E\u044E (\u043A\u0430\u0440\u0431\u043E\u043D\u0430\u0442\u0438, \u043A\u0440\u0435\u043C\u043D\u0435\u0437\u0435\u043C, \u0441\u043F\u043E\u043B\u0443\u043A\u0438 \u0437\u0430\u043B\u0456\u0437\u0430, \u0433\u043B\u0438\u043D\u0438\u0441\u0442\u0456 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0438 \u0430\u0431\u043E \u0456\u043D\u0448\u0456 \u0441\u043F\u043E\u043B\u0443\u043A\u0438). \u041E\u0434\u0438\u043D \u0437 \u043F\u0435\u0440\u0448\u0438\u0445 \u0435\u0442\u0430\u043F\u0456\u0432 \u0434\u0456\u0430\u0433\u0435\u043D\u0435\u0437\u0443."@uk . . . . "Cementation involves ions carried in groundwater chemically precipitating to form new crystalline material between sedimentary grains. The new pore-filling minerals forms \"bridges\" between original sediment grains, thereby binding them together. In this way, sand becomes sandstone, and gravel becomes conglomerate or breccia. Cementation occurs as part of the diagenesis or lithification of sediments. Cementation occurs primarily below the water table regardless of sedimentary grain sizes present. Large volumes of pore water must pass through sediment pores for new mineral cements to crystallize and so millions of years are generally required to complete the cementation process. Common mineral cements include calcite, quartz, and silica phases like cristobalite, iron oxides, and clay minerals; other mineral cements also occur. Cementation is continuous in the groundwater zone, so much so that the term \"zone of cementation\" is sometimes used interchangeably. Cementation occurs in fissures or other openings of existing rocks and is a dynamic process more or less in equilibrium with a dissolution or dissolving process. Cement found on the sea floor is commonly aragonite and can take different textural forms. These textural forms include pendant cement, meniscus cement, isopachous cement, needle cement, botryoidal cement, blocky cement, syntaxial rim cement, and coarse mosaic cement. The environment in which each of the cements is found depends on the pore space available. Cements that are found in phreatic zones include: isopachous, blocky, and syntaxial rim cements. As for calcite cementation, which occurs in meteoric realms (freshwater sources), the cement is produced by the dissolution of less stable aragonite and high-Mg calcite. (Boggs, 2011) Classifying rocks while using the Folk classification depends on the matrix, which is either sparry (prominently composed of cement) or micritic (prominently composed of mud)."@en . "La c\u00E9mentation est la pr\u00E9cipitation de sels \u00E0 la surface d'une nappe phr\u00E9atique. \n* Portail de la g\u00E9ologie"@fr . "Cementatie is een proces waardoor de pori\u00EBn in een sediment dichtgegroeid raken door de neerslag van bepaalde mineralen. Zoals bij elke neerslagreactie vormen deze mineralen (bekende voorbeelden zijn calciet, aragoniet en kwarts) kristallen, meestal te klein om met het blote oog te zien. Het gevolg is dat dat de losse deeltjes (klasten) waaruit het sediment bestaat aan elkaar gekit raken en het sediment consolideert."@nl . . . . "Cementatie is een proces waardoor de pori\u00EBn in een sediment dichtgegroeid raken door de neerslag van bepaalde mineralen. Zoals bij elke neerslagreactie vormen deze mineralen (bekende voorbeelden zijn calciet, aragoniet en kwarts) kristallen, meestal te klein om met het blote oog te zien. Het gevolg is dat dat de losse deeltjes (klasten) waaruit het sediment bestaat aan elkaar gekit raken en het sediment consolideert."@nl . . . . "Cementaci\u00F3n (geolog\u00EDa)"@es . "Cementation (geology)"@en . . "Es denomina cimentaci\u00F3 al proc\u00E9s pel qual durant la diag\u00E8nesi precipiten les sals dissoltes en l'aigua situada en els porus dels sediments; les part\u00EDcules constituents d'aquests (clastos, cants...) queden unides entre si. La cimentaci\u00F3, juntament amb la compactaci\u00F3, produeixen la litificaci\u00F3. El precipitat que es forma es denomina ciment, i la seva composici\u00F3 pot ser molt variada, si b\u00E9 abunden el s\u00EDlice, el carbonat i els \u00F2xids de ferro."@ca . . . . . . . . "Cementation involves ions carried in groundwater chemically precipitating to form new crystalline material between sedimentary grains. The new pore-filling minerals forms \"bridges\" between original sediment grains, thereby binding them together. In this way, sand becomes sandstone, and gravel becomes conglomerate or breccia. Cementation occurs as part of the diagenesis or lithification of sediments. Cementation occurs primarily below the water table regardless of sedimentary grain sizes present. Large volumes of pore water must pass through sediment pores for new mineral cements to crystallize and so millions of years are generally required to complete the cementation process. Common mineral cements include calcite, quartz, and silica phases like cristobalite, iron oxides, and clay mineral"@en . . "Se denomina cementaci\u00F3n al proceso por el cual durante la diag\u00E9nesis precipitan las sales disueltas en el agua situada en los poros de los sedimentos;\u200B las part\u00EDculas constituyentes de estos (clastos, cantos...) quedan unidas entre s\u00ED. La cementaci\u00F3n, junto con la compactaci\u00F3n, producen la litificaci\u00F3n.\u200B El precipitado que se forma se denomina cemento,\u200B y su composici\u00F3n puede ser muy variada, si bien abundan la s\u00EDlice, el carbonato y los \u00F3xidos de hierro.\u200B"@es . . . "Cementazione (geologia)"@it . "In der Geologie bezeichnet die Zementation einen bestimmten Prozess der Diagenese, also der Ver\u00E4nderung von sediment\u00E4ren Ablagerungen. Die Zementation ist ein chemisch-physikalischer Vorgang, bei dem Minerale (meist Quarz oder Calcit) \u00FCber w\u00E4ssrige L\u00F6sungen in die Porenr\u00E4ume des Lockersediments transportiert und dort als Zemente ausgef\u00E4llt werden. Die Porosit\u00E4t des Ausgangsmaterials wird dadurch verringert, w\u00E4hrend gleichzeitig die K\u00F6rner des Sediments miteinander verkittet werden. Zusammen mit der Kompaktion, einem rein physikalischen Prozess der Diagenese, der eine druckbedingte Zunahme der Dichte durch auflastendes Material bewirkt, f\u00FChrt die Zementation zur Umwandlung einer lockeren unverfestigten Sedimentmasse zu einem festen Gestein. Dieser Vorgang wird auch Lithifizierung (griechisch Versteinerung) genannt."@de . "Cimentaci\u00F3 (geologia)"@ca . "La cementazione \u00E8 uno dei meccanismi con cui si verifica la litificazione dei sedimenti e consistente nella precipitazione di sostanze, portate in soluzione, dalle acque circolanti, nei pori del sedimento. Il processo di litificazione, ossia della trasformazione di un sedimento incoerente in uno coerente (duro), pu\u00F2 verificarsi con azioni meccaniche (costipamento) e con azioni chimiche (la cementazione, per l'appunto)."@it . . . . . . "16969883"^^ . .