"Diageneze je proces, kter\u00FD je definov\u00E1n jako souhrn pochod\u016F m\u011Bn\u00EDc\u00EDch miner\u00E1ln\u00ED slo\u017Een\u00ED, strukturu a texturu sedimentu v obdob\u00ED, po\u010D\u00EDnaj\u00EDc\u00EDm jeho ulo\u017Een\u00EDm a kon\u010D\u00EDc\u00EDm bu\u010F metamorf\u00F3zou uveden\u00E9ho sedimentu, nebo jeho zv\u011Btr\u00E1v\u00E1n\u00EDm v povrchov\u00FDch podm\u00EDnk\u00E1ch. Diageneze se v\u0161ak net\u00FDk\u00E1 jen p\u0159em\u011Bny sediment\u016F v pevnou substanci. Mezi diagenetick\u00E9 procesy je \u0159azena i p\u0159em\u011Bna organick\u00FDch l\u00E1tek na kerogeny a n\u00E1sledn\u011B v ropu a zemn\u00ED plyn."@cs . . "Die Diagenese (altgriechisch \u03B4\u03B9\u03B1 \u201Adurch\u2018 und \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2 \u201AEntstehung\u2018) ist der geologische Prozess der Verfestigung von Sedimenten und der weiteren Ver\u00E4nderung der dadurch entstandenen Sedimentgesteine unter verh\u00E4ltnism\u00E4\u00DFig niedrigen Dr\u00FCcken und Temperaturen bis zu ihrer Abtragung. Sie ist damit ein Teil des Kreislaufs der Gesteine."@de . . "Diag\u00E9nesis"@es . . "La diagen\u00E8se, ou diag\u00E9n\u00E8se, d\u00E9signe l'ensemble des processus physico-chimiques et biochimiques par lesquels les d\u00E9p\u00F4ts de s\u00E9diments meubles sont transform\u00E9s en roches s\u00E9dimentaires. Ces transformations ont g\u00E9n\u00E9ralement lieu \u00E0 faible profondeur, donc dans des conditions de pression et de temp\u00E9rature peu \u00E9lev\u00E9es et o\u00F9 les interactions eaux-roches jouent un r\u00F4le tout \u00E0 fait pr\u00E9pond\u00E9rant dans les processus d'induration. Ces transformations engagent des processus vari\u00E9s, notamment : compaction, d\u00E9shydratation, dissolution, cimentation, \u00E9pig\u00E9nisation, m\u00E9tasomatose. Les s\u00E9diments sont g\u00E9n\u00E9ralement d'origine d\u00E9tritique (d\u00E9bris d'anciennes roches), mais ils peuvent \u00E9galement comporter, en plus ou moins grandes quantit\u00E9s, des restes d'organismes et de fossiles (le plus souvent microscopiques) et des min\u00E9raux apparus par transformations chimiques. Selon le pourcentage de chacun de ces divers \u00E9l\u00E9ments, on distingue donc trois types de roches : roches d\u00E9tritiques, roches biochimiques et roches chimiques. Les s\u00E9diments sont g\u00E9n\u00E9ralement meubles et riches en eau. La diagen\u00E8se consiste en leur transformation chimique, biochimique et physique en roches s\u00E9dimentaires compactes. Cette transformation se fait en plusieurs \u00E9tapes, plus ou moins respect\u00E9es selon la nature du s\u00E9diment : En surface on assiste \u00E0 : \n* l'action des \u00EAtres vivants : les animaux fouisseurs favorisent le m\u00E9lange des s\u00E9diments fins, et les protozoaires et bact\u00E9ries interviennent dans la dolomitisation, la formation des phosphates, de la pyrite, du p\u00E9trole, des charbons ; les algues, les cyanophyc\u00E9es et certaines bact\u00E9ries encroutantes ou certaines mousses (bryophytes) favorisent la cristallisation de carbonates en solution sursatur\u00E9e pour former les travertins ; le r\u00F4le des \u00EAtres vivants est donc loin d'\u00EAtre n\u00E9gligeable dans la diagen\u00E8se ; \n* la p\u00E9dogen\u00E8se (naissance des sols), qui intervient dans la formation de roches meubles (argile \u00E0 silex, lat\u00E9rites) et de roches dures (gr\u00E8s, meuli\u00E8res) ; par exemple, la silice dissoute sous climat humide peut cimenter les sables en gr\u00E8s lors des saisons plus s\u00E8ches ; \n* la dissolution, qui concerne les s\u00E9diments \u00E9merg\u00E9s : les parties superficielles du s\u00E9diment sont dissoutes par action de l'eau et entra\u00EEn\u00E9es en profondeur (poup\u00E9es du l\u0153ss) ; \n* la d\u00E9shydratation : lorsqu'un s\u00E9diment aquatique est ass\u00E9ch\u00E9, il y a durcissement et modification de ses propri\u00E9t\u00E9s physiques ; \n* la cimentation pr\u00E9coce, \u00E0 la surface de la zone supratidale ou c\u00F4ti\u00E8re, dans le cas d'une plate-forme \u00AB bahamienne \u00BB, comme la vaste plate-forme carbonat\u00E9e ancienne du Lias moyen au Maroc (Haut Atlas, Moyen Atlas, rides sud rifaines etc.) soit env. 200 x 300 km. La plate-forme carbonat\u00E9e s'\u00E9tend en Alg\u00E9rie et en Tunisie jusqu'en Oman, le long de la marge sud-t\u00E9thysienne. Un bon exemple actuel de s\u00E9dimentation et de diagen\u00E8se est donn\u00E9 par les d\u00E9p\u00F4ts c\u00F4tiers (de mar\u00E9e et de temp\u00EAtes) platiers et \u00AB chotts \u00BB (s\u00E9dimentaton cyclique) du fond du golfe de Gab\u00E8s en Tunisie. \u00C0 faible profondeur ont lieu : \n* la cimentation : les \u00E9l\u00E9ments dissous par l'eau peuvent, en pr\u00E9cipitant, cimenter les particules de s\u00E9diment entre elles ; on parle aussi de lithification ; \n* le concr\u00E9tionnement : les concr\u00E9tions sont des accumulations de min\u00E9raux particuliers qui ont lieu au cours du d\u00E9p\u00F4t s\u00E9dimentaire, ou ult\u00E9rieurement ; selon leur forme, elles portent plusieurs noms : les sph\u00E9rolites, les nodules, les g\u00E9odes, les septarias ; \n* l'\u00E9pig\u00E9nisation et la m\u00E9tasomatose : l'\u00E9pig\u00E9nisation correspond \u00E0 la transformation d'un min\u00E9ral pr\u00E9existant en un autre de m\u00EAme composition ; il s'agit souvent d'un changement dans la structure du min\u00E9ral : par exemple, l'aragonite, contenue g\u00E9n\u00E9ralement dans des restes calcaires d'organismes, se transforme en calcite ; la m\u00E9tasomatose a lieu \u00E0 plus grande \u00E9chelle et correspond \u00E0 la substitution d'un min\u00E9ral par un autre sans changement de volume : par exemple, le carbonate calcique (CaCO3) est parfois remplac\u00E9 par du sulfate de fer (ammonites pyriteuses) ; \n* la compaction : sous l'effet de la pression des s\u00E9diments sus-jacents il y a d\u00E9part d'eau ; dans un premier temps, l'eau tend \u00E0 fuir en grande quantit\u00E9 sous l'effet de la charge support\u00E9e ; dans un second temps, ce sont les grains qui se r\u00E9arrangent de fa\u00E7on \u00E0 supporter cette charge, et il y a tassement."@fr . . . . . . "Na pr\u00F3isis fhisici\u00FAla is cheimiceacha tr\u00EDna n-athra\u00EDtear dr\u00EDodar neamhchomhdhl\u00FAite ina charraig sholadach. Cuims\u00EDonn s\u00ED balcadh is p\u00E1irtdh\u00ED-uisci\u00FA, ansin stroighni\u00FA is cothrom\u00FA ag teocht \u00EDseal go dt\u00ED staid n\u00EDos cobhsa\u00ED \u00F3 thaobh comhdh\u00E9anaimh is ceimice de. N\u00ED g\u00E1 go dtiocfaidh aon mheiteamorfacht san \u00E1ireamh."@ga . "Diagenesis (/\u02CCda\u026A.\u0259\u02C8d\u0292\u025Bn\u0259s\u026As/) is the process that describes physical and chemical changes in sediments first caused by water-rock interactions, microbial activity, and compaction after their deposition. Increased pressure and temperature only start to play a role as sediments become buried much deeper in the Earth's crust. In the early stages, the transformation of poorly consolidated sediments into sedimentary rock (lithification) is simply accompanied by a reduction in porosity and water expulsion (clay sediments), while their main mineralogical assemblages remain unaltered. As the rock is carried deeper by further deposition above, its organic content is progressively transformed into kerogens and bitumens. The process of diagenesis excludes surface alteration (weathering) and deep metamorphism. There is no sharp boundary between diagenesis and metamorphism, but the latter occurs at higher temperatures and pressures. Hydrothermal solutions, meteoric groundwater, rock porosity, permeability, dissolution/precipitation reactions, and time are all influential factors. After deposition, sediments are compacted as they are buried beneath successive layers of sediment and cemented by minerals that precipitate from solution. Grains of sediment, rock fragments and fossils can be replaced by other minerals (e.g., calcite, siderite, pyrite, marcasite...) during diagenesis. Porosity usually decreases during diagenesis, except in rare cases such as dissolution of minerals and dolomitization. The study of diagenesis in rocks is used to understand the geologic history they have undergone and the nature and type of fluids that have circulated through them. From a commercial standpoint, such studies aid in assessing the likelihood of finding various economically viable mineral and hydrocarbon deposits. The process of diagenesis is also important in the decomposition of bone tissue."@en . . . . . "\u7D9A\u6210\u4F5C\u7528\uFF08\u305E\u304F\u305B\u3044\u3055\u3088\u3046\u3001diagenesis\uFF09\u306F\u3001\u5806\u7A4D\u7269\u304C\u56FA\u307E\u3063\u3066\u5806\u7A4D\u5CA9\u306B\u306A\u308B\u4F5C\u7528\u3002\u7815\u5C51\u5CA9\u3067\u306F\u4E3B\u306B\u5727\u5BC6\u4F5C\u7528\u3068\u81A0\u7D50\u4F5C\u7528\u306E2\u3064\u304B\u3089\u306A\u308B\u304C\u3001\u70AD\u9178\u5869\u5CA9\u3067\u306F\u3053\u308C\u4EE5\u5916\u306E\u7D9A\u6210\u4F5C\u7528\u3082\u591A\u304F\u898B\u3089\u308C\u308B\u3002"@ja . . . . . . . . . . . . . . . "La diagen\u00E8se, ou diag\u00E9n\u00E8se, d\u00E9signe l'ensemble des processus physico-chimiques et biochimiques par lesquels les d\u00E9p\u00F4ts de s\u00E9diments meubles sont transform\u00E9s en roches s\u00E9dimentaires. Ces transformations ont g\u00E9n\u00E9ralement lieu \u00E0 faible profondeur, donc dans des conditions de pression et de temp\u00E9rature peu \u00E9lev\u00E9es et o\u00F9 les interactions eaux-roches jouent un r\u00F4le tout \u00E0 fait pr\u00E9pond\u00E9rant dans les processus d'induration. Ces transformations engagent des processus vari\u00E9s, notamment : compaction, d\u00E9shydratation, dissolution, cimentation, \u00E9pig\u00E9nisation, m\u00E9tasomatose. En surface on assiste \u00E0 :"@fr . . . . . . . "En geologia i oceanografia, s'anomena diag\u00E8nesi el conjunt de processos qu\u00EDmics, f\u00EDsics o biol\u00F2gics que afecten al sediment des que es diposita i fins a la formaci\u00F3 d'una roca sediment\u00E0ria (litificaci\u00F3), excloent l'alteraci\u00F3 en superf\u00EDcie (meteoritzaci\u00F3). Aquests canvis es produeixen a baixa temperatura i pressi\u00F3, i inclouen, entre d'altres, la compactaci\u00F3, la p\u00E8rdua d'aigua, la cimentaci\u00F3, l'escalfament geot\u00E8rmic i la reordenaci\u00F3 de les part\u00EDcules. El l\u00EDmit inferior de la diag\u00E8nesi \u00E9s imprec\u00EDs i progressiu, tot i que normalment s'estableix quan es presenta la recristal\u00B7litzaci\u00F3 i d'altres indicadors del metamorfisme."@ca . . . . . "Diagenes \u00E4r en term som beskriver de kemiska, fysikaliska eller biologiska f\u00F6r\u00E4ndringar som ett sediment eller en jordart genomg\u00E5r fr\u00E5n det avsatts tills det omvandlats till en bergart. Ordet diagenes f\u00F6reslogs 1868 av den tyske geologen Karl Wilhelm von G\u00FCmbel f\u00F6r att beskriva litifiering. Diagenesens tre viktigaste faser \u00E4r , och kristallisation. Under kompaktionen pressas sedimentet ihop, s\u00E5 att porvolymen minskar. Lera kan minska i volym s\u00E5 mycket som 40 % och l\u00F6st packad sand kan minska sin porositet fr\u00E5n 50 % till 27 %. Osorterade, leriga jordarter packas mer \u00E4n v\u00E4lsorterad sand. Cementering inneb\u00E4r att det sker kemiska utf\u00E4llningar mellan mineralkornen, vanligen av kiseldioxid, karbonater eller j\u00E4rnoxider, som binder ihop mineralkornen. Denna process minskar ocks\u00E5 sedimentets porositet. Diagenes sker vid l\u00E5ga temperaturer, och n\u00E4r dessa \u00F6verskrids kallas processen ist\u00E4llet metamorfos. Gr\u00E4nsen mellan diagenes och metamorfos g\u00E5r ungef\u00E4r vid 150 - 200\u00B0C."@sv . "Diagenes"@sv . . . . . "Diageneze je proces, kter\u00FD je definov\u00E1n jako souhrn pochod\u016F m\u011Bn\u00EDc\u00EDch miner\u00E1ln\u00ED slo\u017Een\u00ED, strukturu a texturu sedimentu v obdob\u00ED, po\u010D\u00EDnaj\u00EDc\u00EDm jeho ulo\u017Een\u00EDm a kon\u010D\u00EDc\u00EDm bu\u010F metamorf\u00F3zou uveden\u00E9ho sedimentu, nebo jeho zv\u011Btr\u00E1v\u00E1n\u00EDm v povrchov\u00FDch podm\u00EDnk\u00E1ch. Diageneze se v\u0161ak net\u00FDk\u00E1 jen p\u0159em\u011Bny sediment\u016F v pevnou substanci. Mezi diagenetick\u00E9 procesy je \u0159azena i p\u0159em\u011Bna organick\u00FDch l\u00E1tek na kerogeny a n\u00E1sledn\u011B v ropu a zemn\u00ED plyn."@cs . . . . . . "Diag\u00E8nesi"@ca . . . . "\u0646\u0634\u0623\u0629 \u0645\u0627\u0628\u0639\u062F\u064A\u0629"@ar . . . . "Diagenese"@nl . . . . . "\u0627\u0644\u0646\u0634\u0623\u0629 \u0627\u0644\u0645\u0627\u0628\u0639\u062F\u064A\u0629 \u0623\u0648 \u0627\u0644\u0646\u0634\u0623\u0629 \u0627\u0644\u0644\u0627\u062D\u0642\u0629 \u0641\u064A \u0639\u0644\u0645 \u0637\u0628\u064A\u0639\u0629 \u0627\u0644\u0623\u0631\u0636 \u0648\u0641\u064A \u0639\u0644\u0645 \u0627\u0644\u0628\u062D\u0627\u0631 \u0647\u064A \u0639\u0645\u0644\u064A\u0629 \u062A\u063A\u064A\u0631 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0631\u0633\u0648\u0628\u064A\u0629 \u0645\u0646 \u0646\u0648\u0639 \u0625\u0644\u0649 \u0646\u0648\u0639 \u0622\u062E\u0631 \u062A\u062D\u062A \u062A\u0623\u062B\u064A\u0631 \u0636\u063A\u0637 \u0628\u0633\u064A\u0637 \u0648\u0641\u0639\u0644 \u0627\u0644\u062D\u0631\u0627\u0631\u0629 \u0625\u0644\u0649 \u0623\u0646 \u062A\u062A\u0622\u0643\u0644 \u0628\u0641\u0639\u0644 \u0627\u0644\u062A\u0639\u0631\u064A\u0629 . \u0648\u0628\u0627\u0633\u062A\u0645\u0631\u0627\u0631 \u0639\u0645\u0644\u064A\u0629 \u062A\u0631\u0633\u064A\u0628 \u0627\u0644\u0631\u0648\u0627\u0633\u0628 \u064A\u062A\u0632\u0627\u064A\u062F \u0627\u0644\u0636\u063A\u0637 \u0627\u0644\u0648\u0627\u0642\u0639 \u0639\u0644\u0649 \u0627\u0644\u0631\u0648\u0627\u0633\u0628 \u0628\u0627\u0633\u062A\u0645\u0631\u0627\u0631. \u0641\u062A\u0646\u0643\u0628\u0633 \u0627\u0644\u0631\u0648\u0627\u0633\u0628 \u0648\u062A\u062A\u062E\u0644\u0635 \u0645\u0646 \u0627\u0644\u0645\u064A\u0627\u0647 \u0627\u0644\u062A\u064A \u062A\u062D\u0648\u064A\u0647\u0627 . \u0643\u0645\u0627 \u062A\u0631\u062A\u0641\u0639 \u062F\u0631\u062C\u0629 \u0627\u0644\u062D\u0631\u0627\u0631\u0629 \u0642\u0644\u064A\u0644\u0627 . \u0648\u0644\u0623\u0646 \u0627\u0644\u0631\u0648\u0627\u0633\u0628 \u0642\u062F \u062A\u062D\u062A\u0648\u064A \u0639\u0644\u0649 \u0645\u062D\u0627\u0644\u064A\u0644 \u0644\u0644\u0645\u0639\u0627\u062F\u0646 \u060C \u0648\u0645\u0646 \u0636\u0645\u0646\u0647\u0627 \u0639\u0644\u0649 \u0627\u0644\u0623\u062E\u0635 \u0627\u0644\u0643\u0631\u0628\u0648\u0646\u0627\u062A \u0648 \u0627\u0644\u062C\u064A\u0631 \u060C \u062A\u0628\u062F\u0623 \u0627\u0644\u0645\u0648\u0627\u062F \u0639\u0645\u0644\u064A\u0629 \u0646\u0641\u0627\u0630 \u0648 \u062A\u0628\u0644\u0648\u0631 (\u062A\u0643\u0648\u064A\u0646 \u0628\u0644\u0648\u0631\u0627\u062A) \u0648\u062A\u0635\u0628\u062D \u0627\u0644\u0645\u0627\u062F\u0629 \u0627\u0644\u0647\u0634\u0629 \u0645\u0627\u062F\u0629 \u0635\u0644\u0628\u0629 \u060C \u0648\u0645\u0646 \u0627\u0644\u0631\u0645\u0644 \u064A\u062A\u0643\u0648\u0651\u0646 \u0627\u0644\u062D\u062C\u0631 \u0627\u0644\u0631\u0645\u0644\u064A ."@ar . "Diagen\u00E8se"@fr . . . "\u6210\u5CA9\u4F5C\u7528"@zh . . "Carraig-ghini\u00FAint"@ga . "Diagenezo estas en Geologio la procezo per kio formi\u011Das la sedimentaj petroj. La diversaj tipoj de erozio transportas materialon kiu amasi\u011Das la\u016D tavoloj. Tiuj sedimentoj \u015Dtoni\u011Das por du \u0109efaj kialoj: unue la pezo de la supraj tavoloj sur la subaj tavoloj, kiu premas la sedimentojn, forigas la internan akvon kaj premas porojn, kaj due la precipiti\u011Do de cementigaj substancoj, \u0109efe karbonato de kalcio a\u016D siliko, ofte kune kun argilmineraloj."@eo . "Diageneza"@pl . . "Diagenesis"@en . . . "\u0414\u0456\u0430\u0433\u0435\u043D\u0435\u0301\u0437 (\u0440\u043E\u0441.\u0434\u0438\u0430\u0433\u0435\u043D\u0435\u0437, \u0430\u043D\u0433. diagenesis, \u043D\u0456\u043C. Diagenese, \u043F\u043E\u043B. Diageneza) \u2014 \u0441\u0443\u043A\u0443\u043F\u043D\u0456\u0441\u0442\u044C \u043F\u0440\u043E\u0446\u0435\u0441\u0456\u0432 \u043F\u0435\u0440\u0435\u0442\u0432\u043E\u0440\u0435\u043D\u043D\u044F \u043F\u0443\u0445\u043A\u0438\u0445 \u043E\u0441\u0430\u0434\u0456\u0432 \u043D\u0430 \u043E\u0441\u0430\u0434\u043E\u0432\u0456 \u0433\u0456\u0440\u0441\u044C\u043A\u0456 \u043F\u043E\u0440\u043E\u0434\u0438. \u0412\u0456\u0434\u0431\u0443\u0432\u0430\u0454\u0442\u044C\u0441\u044F \u0443 \u0432\u0435\u0440\u0445\u043D\u0456\u0445 \u0448\u0430\u0440\u0430\u0445 \u0437\u0435\u043C\u043D\u043E\u0457 \u043A\u043E\u0440\u0438 \u0456 \u043F\u043E\u043B\u044F\u0433\u0430\u0454 \u0432 \u043F\u0435\u0440\u0435\u043A\u0440\u0438\u0441\u0442\u0430\u043B\u0456\u0437\u0430\u0446\u0456\u0457 \u043E\u0441\u0430\u0434\u0456\u0432, \u0443\u0442\u0432\u043E\u0440\u0435\u043D\u043D\u0456 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432, \u043A\u043E\u043D\u043A\u0440\u0435\u0446\u0456\u0439, \u0433\u0456\u0434\u0440\u0430\u0442\u0430\u0446\u0456\u0457 \u0430\u0431\u043E \u0434\u0435\u0433\u0456\u0434\u0440\u0430\u0442\u0430\u0446\u0456\u0457 (\u0437\u043D\u0435\u0432\u043E\u0434\u043D\u0435\u043D\u043D\u0456), \u0446\u0435\u043C\u0435\u043D\u0442\u0430\u0446\u0456\u0457 \u043E\u0441\u0430\u0434\u0456\u0432 \u0442\u043E\u0449\u043E. \u0420\u043E\u0437\u0440\u0456\u0437\u043D\u044F\u044E\u0442\u044C \u0434\u0432\u0430 \u0435\u0442\u0430\u043F\u0438 \u0434\u0456\u0430\u0433\u0435\u043D\u0435\u0442\u0438\u0447\u043D\u043E\u0433\u043E \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u043E\u0443\u0442\u0432\u043E\u0440\u0435\u043D\u043D\u044F: \u043E\u043A\u0438\u0441\u043D\u044E\u0432\u0430\u043B\u044C\u043D\u0438\u0439 \u0456 \u0432\u0456\u0434\u043D\u043E\u0432\u043D\u0438\u0439."@uk . . "Diagenese is binnen de geologie elke chemische, fysische of biologische verandering die een sediment ondergaat nadat het afgezet is. Verwering wordt niet onder diagenese gerekend. De processen die onder diagenese vallen vinden plaats bij relatief lage temperatuur en druk en zorgen ervoor dat de mineralogie en textuur van het gesteente verandert."@nl . "\u7D9A\u6210\u4F5C\u7528\uFF08\u305E\u304F\u305B\u3044\u3055\u3088\u3046\u3001diagenesis\uFF09\u306F\u3001\u5806\u7A4D\u7269\u304C\u56FA\u307E\u3063\u3066\u5806\u7A4D\u5CA9\u306B\u306A\u308B\u4F5C\u7528\u3002\u7815\u5C51\u5CA9\u3067\u306F\u4E3B\u306B\u5727\u5BC6\u4F5C\u7528\u3068\u81A0\u7D50\u4F5C\u7528\u306E2\u3064\u304B\u3089\u306A\u308B\u304C\u3001\u70AD\u9178\u5869\u5CA9\u3067\u306F\u3053\u308C\u4EE5\u5916\u306E\u7D9A\u6210\u4F5C\u7528\u3082\u591A\u304F\u898B\u3089\u308C\u308B\u3002"@ja . . . . . . . . "Diagenesis adalah perubahan dari sedimen atau batuan sedimen yang ada menjadi batuan sedimen yang berbeda selama dan setelah terbentuknya batuan (litifikasi), pada suhu dan tekanan kurang dari yang dibutuhkan untuk pembentukan batuan metamorf. Diagenesis tidak termasuk perubahan dari pelapukan. Diagenesis adalah segala perubahan kimia, fisika, atau perubahan biologi yang dialami oleh sedimen setelah deposisi awal, setelah proses litifiakasi. Proses ini tidak termasuk alterasi permukaan (pelapukan) dan metamorfisme. Perubahan ini terjadi pada suhu dan tekanan yang relatif rendah dan mengakibatkan perubahan mineralogi dan tekstur asli batuan. Tidak ada batas yang jelas antara diagenesis dan metamorfosis, tetapi metamorfosis terjadi pada suhu dan tekanan yang lebih tinggi daripada diagenesis. Larutan hidrotermal, air tanah meteorik, porositas, permeabilitas, kelarutan, dan waktu merupakan faktor-faktor yang berpengaruh. Setelah deposisi, sedimen-sedimen akan terkompaksi dan terkubur di bawah lapisan sedimen yang berurut dan disemen oleh mineral yang mengendap dari larutan (mineral presipitasi). Butir sedimen, fragmen batuan dan fosil dapat digantikan oleh mineral lain selama diagenesis. Porositas biasanya menurun selama diagenesis, kecuali dalam kasus-kasus langka seperti pelarutan mineral mineral dan dolomitisasi Studi tentang diagenesis dalam batuan digunakan untuk memahami sejarah geologi yang mereka alami serta sifat dan jenis cairan yang beredar melalui mereka. Dari sudut pandang komersial, studi tersebut membantu dalam menilai kemungkinan menemukan berbagai mineral ekonomis dan endapan hidrokarbon. Proses diagenesis juga penting dalam dekomposisi jaringan tulang."@in . "La diag\u00E9nesis (griego, \u03B4\u03B9\u03B1- d\u00EDa-, \u00ABa trav\u00E9s de\u00BB, y \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2 g\u00E9nesis, \u00ABorigen\u00BB)\u200B es el conjunto de procesos de formaci\u00F3n de una roca sedimentaria a partir de sedimentos, tales como compactaci\u00F3n, recristalizaci\u00F3n o cementaci\u00F3n. La diag\u00E9nesis se produce en el interior de los primeros 5 o 6 km de la corteza terrestre a temperaturas inferiores a 150-200 \u00B0C; m\u00E1s all\u00E1 se considera ya metamorfismo.\u200B La diag\u00E9nesis se denomina tambi\u00E9n diagenizaci\u00F3n o litificaci\u00F3n."@es . . . "Diagenesis adalah perubahan dari sedimen atau batuan sedimen yang ada menjadi batuan sedimen yang berbeda selama dan setelah terbentuknya batuan (litifikasi), pada suhu dan tekanan kurang dari yang dibutuhkan untuk pembentukan batuan metamorf. Diagenesis tidak termasuk perubahan dari pelapukan. Diagenesis adalah segala perubahan kimia, fisika, atau perubahan biologi yang dialami oleh sedimen setelah deposisi awal, setelah proses litifiakasi. Proses ini tidak termasuk alterasi permukaan (pelapukan) dan metamorfisme. Perubahan ini terjadi pada suhu dan tekanan yang relatif rendah dan mengakibatkan perubahan mineralogi dan tekstur asli batuan. Tidak ada batas yang jelas antara diagenesis dan metamorfosis, tetapi metamorfosis terjadi pada suhu dan tekanan yang lebih tinggi daripada diagenesis."@in . . . . . . "Diageneza (gr. \u03B4\u03B9\u03B1 \u201Eprzez, na wskro\u015B\u201C i \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2 \u201Epowstawanie\u201C) \u2013 proces tworzenia ska\u0142y zwi\u0119z\u0142ej ze ska\u0142 lu\u017Anych polegaj\u0105cy na \u0142\u0105czeniu (zlepianiu) spoiwem ziaren skalnych. Osad \u015Bwie\u017Co z\u0142o\u017Cony jest lu\u017Any, mi\u0119kki i zazwyczaj przesi\u0105kni\u0119ty wod\u0105. Pod wp\u0142ywem r\u00F3\u017Cnych czynnik\u00F3w ulega przeobra\u017Ceniom chemicznym i fizycznym, kt\u00F3re prowadz\u0105 do tego, \u017Ce staje si\u0119 on spoisty, twardy i prawie zupe\u0142nie pozbawiony wody. Procesy do tego prowadz\u0105ce przebiegaj\u0105 w warunkach ci\u015Bnienia i temperatury, nier\u00F3\u017Cni\u0105cych si\u0119 lub niewiele r\u00F3\u017Cni\u0105cych si\u0119 od tych warunk\u00F3w, w jakich osad zosta\u0142 z\u0142o\u017Cony. Procesy diagenetyczne rozpoczynaj\u0105 si\u0119 bardzo wcze\u015Bnie, najcz\u0119\u015Bciej ju\u017C w trakcie tworzenia si\u0119 osadu, a trwa\u0107 mog\u0105 bardzo d\u0142ugo, dzia\u0142aj\u0105c jeszcze wtedy, kiedy osad straci kontakt ze \u015Brodowiskiem (morzem, jeziorem, pustyni\u0105 itd.), w kt\u00F3rym zosta\u0142 utworzony. \n* Osad odpowiednio g\u0142\u0119boko pogr\u0105\u017Cony mo\u017Ce dosta\u0107 si\u0119 w stref\u0119 znacznie podwy\u017Cszonego ci\u015Bnienia i temperatury. \n* Je\u015Bli minera\u0142y ska\u0142otw\u00F3rcze ulegaj\u0105 przeobra\u017Ceniom, to proces tych przeobra\u017Ce\u0144 nazywamy metamorfizmem. \n* Wszystkie przeobra\u017Cenia fizyczne i chemiczne zachodz\u0105ce w osadzie, kt\u00F3re nie wytwarzaj\u0105 zmian metamorficznych nazywamy diagenez\u0105. (J. Walther, 1894) Rodzaje diagenez: \n* diageneza halmyrolityczna \u2013 pod wp\u0142ywem wody morskiej \n* diageneza epigenetyczna \u2013 przemiany, zw\u0142aszcza chemiczne, zachodz\u0105 jeszcze po stwardnieniu utworu W procesie diagenezy g\u0142\u00F3wn\u0105 rol\u0119 gra twardnienie koloid\u00F3w, kompakcja osad\u00F3w wywo\u0142ana ci\u0119\u017Carem gromadz\u0105cych si\u0119 osad\u00F3w, cementacja i procesy rekrystalizacyjne polegaj\u0105ce na rozpuszczeniu i str\u0105caniu si\u0119 zwi\u0105zk\u00F3w chemicznych. Diageneza odbywa si\u0119 na ma\u0142ej g\u0142\u0119boko\u015Bci (temperatura i ci\u015Bnienie zbli\u017Cone do warunk\u00F3w panuj\u0105cych na powierzchni Ziemi \u2013 w przeciwie\u0144stwie do metamorfizmu). G\u0142\u00F3wnym czynnikiem zmiany jest spoiwo, kt\u00F3re mo\u017Ce by\u0107 krzemionkowe, w\u0119glanowe lub \u017Celaziste."@pl . "\u0394\u03B9\u03B1\u03B3\u03AD\u03BD\u03B5\u03C3\u03B7"@el . . "\u0397 \u03B4\u03B9\u03B1\u03B3\u03AD\u03BD\u03B5\u03C3\u03B7, \u03B5\u03AF\u03BD\u03B1\u03B9 \u03B7 \u03C6\u03AC\u03C3\u03B7 \u03BC\u03B5\u03C4\u03B1\u03C4\u03C1\u03BF\u03C0\u03AE\u03C2 \u03C4\u03C9\u03BD \u03B1\u03C3\u03CD\u03BD\u03B4\u03B5\u03C4\u03C9\u03BD \u03B9\u03B6\u03B7\u03BC\u03AC\u03C4\u03C9\u03BD \u03C3\u03B5 \u03C0\u03C1\u03B1\u03B3\u03BC\u03B1\u03C4\u03B9\u03BA\u03AC \u03C0\u03B5\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1. \u0391\u03C5\u03C4\u03CC \u03C0\u03B5\u03C4\u03C5\u03C7\u03B1\u03AF\u03BD\u03B5\u03C4\u03B1\u03B9 \u03BC\u03B5 \u03BC\u03AF\u03B1 \u03C3\u03B5\u03B9\u03C1\u03AC \u03C6\u03C5\u03C3\u03B9\u03BA\u03BF\u03C7\u03B7\u03BC\u03B9\u03BA\u03CE\u03BD \u03BA\u03B1\u03B9 \u03BC\u03B7\u03C7\u03B1\u03BD\u03B9\u03BA\u03CE\u03BD \u03C6\u03B1\u03B9\u03BD\u03BF\u03BC\u03AD\u03BD\u03C9\u03BD."@el . . . . . . . . "Diagenezo"@eo . "\u6210\u5CA9\u4F5C\u7528\u662F\u6307\u6C89\u79EF\u7269\u5728\u57CB\u85CF\u540E\uFF0C\u56FA\u7ED3\u4E3A\u575A\u786C\u5CA9\u77F3\uFF0C\u53D7\u5230\u53D8\u8D28\u3001\u98CE\u5316\u4F5C\u7528\u524D\u7684\u5404\u79CD\u7269\u7406\u3001\u5316\u5B66\u3001\u751F\u7269\u7684\u53D8\u5316\u3002\u5176\u4E2D\u6C89\u79EF\u7269\u53D8\u4E3A\u6C89\u79EF\u5CA9\u7684\u53D8\u5316\uFF0C\u662F\u72ED\u4E49\u7684\u6210\u5CA9\u4F5C\u7528\u3002\u5B83\u4E5F\u662F\u5CA9\u77F3\u5FAA\u74B0\u7684\u4E00\u500B\u904E\u7A0B\u3002 \u6C89\u79EF\u540E\uFF0C\u6C89\u79EF\u7269\u8FDE\u7EED\u57CB\u85CF\uFF0C\u88AB\u6EB6\u89E3\u7269\u4E2D\u7684\u77FF\u7269\u80F6\u7ED3\u3002\u6C89\u79EF\u7269\u7684\u9897\u7C92\uFF0C\u5CA9\u77F3\u788E\u7247\u3001\u5316\u77F3\u53EF\u5728\u6210\u5CA9\u65F6\u88AB\u5176\u5B83\u77FF\u7269\u4EA4\u4EE3\u3002\u5728\u6210\u5CA9\u65F6\u5B54\u9699\u5EA6\u5E38\u4F1A\u51CF\u5C0F\uFF0C\u9664\u77FF\u7269\u6EB6\u89E3\u3001\u767D\u4E91\u77F3\u5316\u4F5C\u7528\u3002\u7814\u7A76\u5CA9\u77F3\u7684\u6210\u5CA9\u4F5C\u7528\u5E38\u7528\u4E8E\u4E86\u89E3\u5B83\u4EEC\u7684\u6784\u9020\u53F2\uFF0C\u53CA\u901A\u8FC7\u5B83\u4EEC\u7684\u6D41\u4F53\u7684\u6027\u8D28\u548C\u7C7B\u578B\u3002\u4ECE\u5546\u4E1A\u89D2\u5EA6\uFF0C\u8FD9\u4E9B\u7814\u7A76\u53EF\u5E2E\u52A9\u8BC4\u4F30\u53D1\u73B0\u5404\u79CD\u7ECF\u6D4E\u4E0A\u53EF\u884C\u7684\u77FF\u85CF\u7684\u53EF\u80FD\u6027\u4EE5\u53CA\u77F3\u6CB9\u8D44\u6E90\u3002\u6210\u5CA9\u4F5C\u7528\u8FC7\u7A0B\u540C\u6837\u5728\u9AA8\u5934\u7684\u5206\u89E3\u4E2D\u6709\u91CD\u8981\u4F5C\u7528\u3002"@zh . . "\u0414\u0456\u0430\u0433\u0435\u043D\u0435\u0301\u0437 (\u0440\u043E\u0441.\u0434\u0438\u0430\u0433\u0435\u043D\u0435\u0437, \u0430\u043D\u0433. diagenesis, \u043D\u0456\u043C. Diagenese, \u043F\u043E\u043B. Diageneza) \u2014 \u0441\u0443\u043A\u0443\u043F\u043D\u0456\u0441\u0442\u044C \u043F\u0440\u043E\u0446\u0435\u0441\u0456\u0432 \u043F\u0435\u0440\u0435\u0442\u0432\u043E\u0440\u0435\u043D\u043D\u044F \u043F\u0443\u0445\u043A\u0438\u0445 \u043E\u0441\u0430\u0434\u0456\u0432 \u043D\u0430 \u043E\u0441\u0430\u0434\u043E\u0432\u0456 \u0433\u0456\u0440\u0441\u044C\u043A\u0456 \u043F\u043E\u0440\u043E\u0434\u0438. \u0412\u0456\u0434\u0431\u0443\u0432\u0430\u0454\u0442\u044C\u0441\u044F \u0443 \u0432\u0435\u0440\u0445\u043D\u0456\u0445 \u0448\u0430\u0440\u0430\u0445 \u0437\u0435\u043C\u043D\u043E\u0457 \u043A\u043E\u0440\u0438 \u0456 \u043F\u043E\u043B\u044F\u0433\u0430\u0454 \u0432 \u043F\u0435\u0440\u0435\u043A\u0440\u0438\u0441\u0442\u0430\u043B\u0456\u0437\u0430\u0446\u0456\u0457 \u043E\u0441\u0430\u0434\u0456\u0432, \u0443\u0442\u0432\u043E\u0440\u0435\u043D\u043D\u0456 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432, \u043A\u043E\u043D\u043A\u0440\u0435\u0446\u0456\u0439, \u0433\u0456\u0434\u0440\u0430\u0442\u0430\u0446\u0456\u0457 \u0430\u0431\u043E \u0434\u0435\u0433\u0456\u0434\u0440\u0430\u0442\u0430\u0446\u0456\u0457 (\u0437\u043D\u0435\u0432\u043E\u0434\u043D\u0435\u043D\u043D\u0456), \u0446\u0435\u043C\u0435\u043D\u0442\u0430\u0446\u0456\u0457 \u043E\u0441\u0430\u0434\u0456\u0432 \u0442\u043E\u0449\u043E. \u0420\u043E\u0437\u0440\u0456\u0437\u043D\u044F\u044E\u0442\u044C \u0434\u0432\u0430 \u0435\u0442\u0430\u043F\u0438 \u0434\u0456\u0430\u0433\u0435\u043D\u0435\u0442\u0438\u0447\u043D\u043E\u0433\u043E \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u043E\u0443\u0442\u0432\u043E\u0440\u0435\u043D\u043D\u044F: \u043E\u043A\u0438\u0441\u043D\u044E\u0432\u0430\u043B\u044C\u043D\u0438\u0439 \u0456 \u0432\u0456\u0434\u043D\u043E\u0432\u043D\u0438\u0439."@uk . . . . . "Diagenese"@de . "\u0414\u0456\u0430\u0433\u0435\u043D\u0435\u0437"@uk . . "\u0397 \u03B4\u03B9\u03B1\u03B3\u03AD\u03BD\u03B5\u03C3\u03B7, \u03B5\u03AF\u03BD\u03B1\u03B9 \u03B7 \u03C6\u03AC\u03C3\u03B7 \u03BC\u03B5\u03C4\u03B1\u03C4\u03C1\u03BF\u03C0\u03AE\u03C2 \u03C4\u03C9\u03BD \u03B1\u03C3\u03CD\u03BD\u03B4\u03B5\u03C4\u03C9\u03BD \u03B9\u03B6\u03B7\u03BC\u03AC\u03C4\u03C9\u03BD \u03C3\u03B5 \u03C0\u03C1\u03B1\u03B3\u03BC\u03B1\u03C4\u03B9\u03BA\u03AC \u03C0\u03B5\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1. \u0391\u03C5\u03C4\u03CC \u03C0\u03B5\u03C4\u03C5\u03C7\u03B1\u03AF\u03BD\u03B5\u03C4\u03B1\u03B9 \u03BC\u03B5 \u03BC\u03AF\u03B1 \u03C3\u03B5\u03B9\u03C1\u03AC \u03C6\u03C5\u03C3\u03B9\u03BA\u03BF\u03C7\u03B7\u03BC\u03B9\u03BA\u03CE\u03BD \u03BA\u03B1\u03B9 \u03BC\u03B7\u03C7\u03B1\u03BD\u03B9\u03BA\u03CE\u03BD \u03C6\u03B1\u03B9\u03BD\u03BF\u03BC\u03AD\u03BD\u03C9\u03BD."@el . . "In geologia la diagenesi \u00E8 un qualsiasi cambiamento chimico-fisico subito da un sedimento dopo la sua deposizione iniziale, durante e dopo la sua trasformazione in roccia coerente, ad esclusione dell'alterazione superficiale (erosione), I cambiamenti diagenetici avvengono a temperature (fino a circa 200 \u00B0C) e pressioni (2-3 bar) relativamente basse e possono avere come conseguenza variazioni della mineralogia e/o della struttura originale della roccia. La diagenesi rientra a pieno titolo nei processi sedimentari, per quanto potrebbe essere considerata il grado pi\u00F9 basso del metamorfismo, nel quale sfocerebbe se la combinazione di pressione e temperatura fosse pi\u00F9 elevata. I processi diagenetici precoci avvengono al momento della sedimentazione fino a un modesto seppellimento; in questa fase pu\u00F2 essere molto intensa l'azione dei batteri. I processi diagenetici cosiddetti tardivi hanno luogo invece dopo un seppellimento pi\u00F9 profondo dovuto ad esempio a subsidenza. La durata complessiva di questi processi pu\u00F2 essere anche di milioni di anni. Si riconoscono diversi fasi nel corso della diagenesi: \n* compattazione, che \u00E8 dovuta al peso dei sedimenti sovrastanti (pressione litostatica); essa provoca la fuoriuscita delle acque interstiziali e quindi l'avvicinamento dei singoli clasti; di conseguenza la porosit\u00E0 e la permeabilit\u00E0 tendono a diminuire durante la diagenesi. \n* ricristallizzazione, che coinvolge alcuni minerali instabili presenti nel sedimento; questo processo produce una cementazione dei clasti coinvolti ed \u00E8 causato proprio dalla pressione tra clasto e clasto. \n* dissoluzione e sostituzione, che interessano alcuni minerali che possono disciogliersi e/o essere rimpiazzati da altri; questo \u00E8 un processo importante nella trasformazione di alcune rocce come la trasformazione della calcite in dolomite (dolomitizzazione). \n* precipitazione di nuovi minerali dalle acque percolanti tra gli interstizi del sedimento; se la precipitazione \u00E8 elevata, arrivando a riempire gran parte dello spazio dei pori entro la roccia, si ottiene la cementazione del sedimento stesso che da incoerente diviene infine coerente. Lo studio della diagenesi nelle rocce \u00E8 usato per capire la storia tettonica a cui sono state sottoposte e la natura e il tipo di fluidi che le hanno attraversate; da un punto di vista economico, permette di valutare la probabilit\u00E0 di trovare minerali sfruttabili e idrocarburi."@it . . . "Diagenese is binnen de geologie elke chemische, fysische of biologische verandering die een sediment ondergaat nadat het afgezet is. Verwering wordt niet onder diagenese gerekend. De processen die onder diagenese vallen vinden plaats bij relatief lage temperatuur en druk en zorgen ervoor dat de mineralogie en textuur van het gesteente verandert. In feite kan diagenese worden gezien als de laagste graad van metamorfose. Bij hogere drukken en temperaturen komt het gesteente in het regime van de zeoliet-facies, de laagste metamorfe facies. Diagenese wordt soms onderverdeeld in , alle processen aan het oppervlak en op geringe diepte, en , de diepere processen."@nl . . . . . . "Na pr\u00F3isis fhisici\u00FAla is cheimiceacha tr\u00EDna n-athra\u00EDtear dr\u00EDodar neamhchomhdhl\u00FAite ina charraig sholadach. Cuims\u00EDonn s\u00ED balcadh is p\u00E1irtdh\u00ED-uisci\u00FA, ansin stroighni\u00FA is cothrom\u00FA ag teocht \u00EDseal go dt\u00ED staid n\u00EDos cobhsa\u00ED \u00F3 thaobh comhdh\u00E9anaimh is ceimice de. N\u00ED g\u00E1 go dtiocfaidh aon mheiteamorfacht san \u00E1ireamh."@ga . . . "Diagenesi"@eu . . "La diag\u00E9nesis (griego, \u03B4\u03B9\u03B1- d\u00EDa-, \u00ABa trav\u00E9s de\u00BB, y \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2 g\u00E9nesis, \u00ABorigen\u00BB)\u200B es el conjunto de procesos de formaci\u00F3n de una roca sedimentaria a partir de sedimentos, tales como compactaci\u00F3n, recristalizaci\u00F3n o cementaci\u00F3n. La diag\u00E9nesis se produce en el interior de los primeros 5 o 6 km de la corteza terrestre a temperaturas inferiores a 150-200 \u00B0C; m\u00E1s all\u00E1 se considera ya metamorfismo.\u200B La mayor\u00EDa de las veces la consolidaci\u00F3n de los sedimentos se debe a la infiltraci\u00F3n de las aguas que contienen sustancias disueltas. La diag\u00E9nesis convierte as\u00ED las gravas en conglomerados, las arenas en areniscas, las arcillas en lutitas, los lodos calc\u00E1reos en calizas o dolom\u00EDas, las cenizas volc\u00E1nicas en cineritas, etc. Las reacciones y otros fen\u00F3menos de oxidorreducci\u00F3n, deshidrataci\u00F3n, recristalizaci\u00F3n, cementaci\u00F3n, litificaci\u00F3n, mineralizaci\u00F3n y sustituci\u00F3n de un mineral preexistente por otro constituyen en su conjunto la autog\u00E9nesis y los minerales resultantes de \u00E9sta son calificados de autog\u00E9nicos. El principio u origen de las rocas sedimentarias es la diag\u00E9nesis producto de presi\u00F3n y temperatura bajas. La diag\u00E9nesis se denomina tambi\u00E9n diagenizaci\u00F3n o litificaci\u00F3n."@es . . . . . . . . . . . "Diageneze"@cs . "\u0414\u0438\u0430\u0433\u0435\u043D\u0435\u0437 (\u0432 \u043F\u0435\u0440. \u0441 \u0433\u0440\u0435\u0447. \u2014 \u00AB\u043F\u0435\u0440\u0435\u0440\u043E\u0436\u0434\u0435\u043D\u0438\u0435, \u043F\u0440\u0435\u043E\u0431\u0440\u0430\u0437\u043E\u0432\u0430\u043D\u0438\u0435\u00BB) \u2014 \u0441\u043E\u0432\u043E\u043A\u0443\u043F\u043D\u043E\u0441\u0442\u044C \u0444\u0438\u0437\u0438\u043A\u043E-\u0445\u0438\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u0445 \u043F\u0440\u043E\u0446\u0435\u0441\u0441\u043E\u0432 \u043F\u0440\u0435\u043E\u0431\u0440\u0430\u0437\u043E\u0432\u0430\u043D\u0438\u044F \u0440\u044B\u0445\u043B\u044B\u0445 \u043E\u0441\u0430\u0434\u043A\u043E\u0432 \u0432 \u043E\u0441\u0430\u0434\u043E\u0447\u043D\u044B\u0435 \u0433\u043E\u0440\u043D\u044B\u0435 \u043F\u043E\u0440\u043E\u0434\u044B. \u0421\u0442\u0430\u0434\u0438\u044F \u041B\u0438\u0442\u043E\u0433\u0435\u043D\u0435\u0437\u0430."@ru . . . "\u7D9A\u6210\u4F5C\u7528"@ja . . "\u6210\u5CA9\u4F5C\u7528\u662F\u6307\u6C89\u79EF\u7269\u5728\u57CB\u85CF\u540E\uFF0C\u56FA\u7ED3\u4E3A\u575A\u786C\u5CA9\u77F3\uFF0C\u53D7\u5230\u53D8\u8D28\u3001\u98CE\u5316\u4F5C\u7528\u524D\u7684\u5404\u79CD\u7269\u7406\u3001\u5316\u5B66\u3001\u751F\u7269\u7684\u53D8\u5316\u3002\u5176\u4E2D\u6C89\u79EF\u7269\u53D8\u4E3A\u6C89\u79EF\u5CA9\u7684\u53D8\u5316\uFF0C\u662F\u72ED\u4E49\u7684\u6210\u5CA9\u4F5C\u7528\u3002\u5B83\u4E5F\u662F\u5CA9\u77F3\u5FAA\u74B0\u7684\u4E00\u500B\u904E\u7A0B\u3002 \u6C89\u79EF\u540E\uFF0C\u6C89\u79EF\u7269\u8FDE\u7EED\u57CB\u85CF\uFF0C\u88AB\u6EB6\u89E3\u7269\u4E2D\u7684\u77FF\u7269\u80F6\u7ED3\u3002\u6C89\u79EF\u7269\u7684\u9897\u7C92\uFF0C\u5CA9\u77F3\u788E\u7247\u3001\u5316\u77F3\u53EF\u5728\u6210\u5CA9\u65F6\u88AB\u5176\u5B83\u77FF\u7269\u4EA4\u4EE3\u3002\u5728\u6210\u5CA9\u65F6\u5B54\u9699\u5EA6\u5E38\u4F1A\u51CF\u5C0F\uFF0C\u9664\u77FF\u7269\u6EB6\u89E3\u3001\u767D\u4E91\u77F3\u5316\u4F5C\u7528\u3002\u7814\u7A76\u5CA9\u77F3\u7684\u6210\u5CA9\u4F5C\u7528\u5E38\u7528\u4E8E\u4E86\u89E3\u5B83\u4EEC\u7684\u6784\u9020\u53F2\uFF0C\u53CA\u901A\u8FC7\u5B83\u4EEC\u7684\u6D41\u4F53\u7684\u6027\u8D28\u548C\u7C7B\u578B\u3002\u4ECE\u5546\u4E1A\u89D2\u5EA6\uFF0C\u8FD9\u4E9B\u7814\u7A76\u53EF\u5E2E\u52A9\u8BC4\u4F30\u53D1\u73B0\u5404\u79CD\u7ECF\u6D4E\u4E0A\u53EF\u884C\u7684\u77FF\u85CF\u7684\u53EF\u80FD\u6027\u4EE5\u53CA\u77F3\u6CB9\u8D44\u6E90\u3002\u6210\u5CA9\u4F5C\u7528\u8FC7\u7A0B\u540C\u6837\u5728\u9AA8\u5934\u7684\u5206\u89E3\u4E2D\u6709\u91CD\u8981\u4F5C\u7528\u3002"@zh . . . 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"\u0414\u0438\u0430\u0433\u0435\u043D\u0435\u0437"@ru . . . "\u0414\u0438\u0430\u0433\u0435\u043D\u0435\u0437 (\u0432 \u043F\u0435\u0440. \u0441 \u0433\u0440\u0435\u0447. \u2014 \u00AB\u043F\u0435\u0440\u0435\u0440\u043E\u0436\u0434\u0435\u043D\u0438\u0435, \u043F\u0440\u0435\u043E\u0431\u0440\u0430\u0437\u043E\u0432\u0430\u043D\u0438\u0435\u00BB) \u2014 \u0441\u043E\u0432\u043E\u043A\u0443\u043F\u043D\u043E\u0441\u0442\u044C \u0444\u0438\u0437\u0438\u043A\u043E-\u0445\u0438\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u0445 \u043F\u0440\u043E\u0446\u0435\u0441\u0441\u043E\u0432 \u043F\u0440\u0435\u043E\u0431\u0440\u0430\u0437\u043E\u0432\u0430\u043D\u0438\u044F \u0440\u044B\u0445\u043B\u044B\u0445 \u043E\u0441\u0430\u0434\u043A\u043E\u0432 \u0432 \u043E\u0441\u0430\u0434\u043E\u0447\u043D\u044B\u0435 \u0433\u043E\u0440\u043D\u044B\u0435 \u043F\u043E\u0440\u043E\u0434\u044B. \u0421\u0442\u0430\u0434\u0438\u044F \u041B\u0438\u0442\u043E\u0433\u0435\u043D\u0435\u0437\u0430."@ru . . "Diagenes \u00E4r en term som beskriver de kemiska, fysikaliska eller biologiska f\u00F6r\u00E4ndringar som ett sediment eller en jordart genomg\u00E5r fr\u00E5n det avsatts tills det omvandlats till en bergart. Ordet diagenes f\u00F6reslogs 1868 av den tyske geologen Karl Wilhelm von G\u00FCmbel f\u00F6r att beskriva litifiering. Diagenes sker vid l\u00E5ga temperaturer, och n\u00E4r dessa \u00F6verskrids kallas processen ist\u00E4llet metamorfos. Gr\u00E4nsen mellan diagenes och metamorfos g\u00E5r ungef\u00E4r vid 150 - 200\u00B0C."@sv . "13368"^^ . "Diagenesia sedimentuak mekanismo fisiko-kimiko edo biokimikoen bitartez arroka sedimentario bilakatzen direneko prozesua da. Ziklo sedimentarioren azken etapa da, materialak elkartzen direnean alterazio kimiko eta fisiko bat jasaten dute bere zanpatzea eragiten duena.Gehienetan sakonera txikian, hain altuak ez diren tenperatura eta presio-mailetan eta konpaktazioz, deshidratazioz, disoluzioz, zimentazioz, eta gertatzen dira."@eu . . . "Diageneza (gr. \u03B4\u03B9\u03B1 \u201Eprzez, na wskro\u015B\u201C i \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2 \u201Epowstawanie\u201C) \u2013 proces tworzenia ska\u0142y zwi\u0119z\u0142ej ze ska\u0142 lu\u017Anych polegaj\u0105cy na \u0142\u0105czeniu (zlepianiu) spoiwem ziaren skalnych. Osad \u015Bwie\u017Co z\u0142o\u017Cony jest lu\u017Any, mi\u0119kki i zazwyczaj przesi\u0105kni\u0119ty wod\u0105. Pod wp\u0142ywem r\u00F3\u017Cnych czynnik\u00F3w ulega przeobra\u017Ceniom chemicznym i fizycznym, kt\u00F3re prowadz\u0105 do tego, \u017Ce staje si\u0119 on spoisty, twardy i prawie zupe\u0142nie pozbawiony wody. Procesy do tego prowadz\u0105ce przebiegaj\u0105 w warunkach ci\u015Bnienia i temperatury, nier\u00F3\u017Cni\u0105cych si\u0119 lub niewiele r\u00F3\u017Cni\u0105cych si\u0119 od tych warunk\u00F3w, w jakich osad zosta\u0142 z\u0142o\u017Cony. Rodzaje diagenez:"@pl . . . . . . "Diagenesis"@in . "Diagenesis (/\u02CCda\u026A.\u0259\u02C8d\u0292\u025Bn\u0259s\u026As/) is the process that describes physical and chemical changes in sediments first caused by water-rock interactions, microbial activity, and compaction after their deposition. Increased pressure and temperature only start to play a role as sediments become buried much deeper in the Earth's crust. In the early stages, the transformation of poorly consolidated sediments into sedimentary rock (lithification) is simply accompanied by a reduction in porosity and water expulsion (clay sediments), while their main mineralogical assemblages remain unaltered. As the rock is carried deeper by further deposition above, its organic content is progressively transformed into kerogens and bitumens. The process of diagenesis excludes surface alteration (weathering) and deep me"@en . . "Diagenezo estas en Geologio la procezo per kio formi\u011Das la sedimentaj petroj. La diversaj tipoj de erozio transportas materialon kiu amasi\u011Das la\u016D tavoloj. Tiuj sedimentoj \u015Dtoni\u011Das por du \u0109efaj kialoj: unue la pezo de la supraj tavoloj sur la subaj tavoloj, kiu premas la sedimentojn, forigas la internan akvon kaj premas porojn, kaj due la precipiti\u011Do de cementigaj substancoj, \u0109efe karbonato de kalcio a\u016D siliko, ofte kune kun argilmineraloj."@eo . . "1096365176"^^ . . . . . . "Diag\u00E9nese (portugu\u00EAs europeu) ou diag\u00EAnese (portugu\u00EAs brasileiro), em geologia e oceanografia refere-se a qualquer mudan\u00E7a e altera\u00E7\u00E3o do sedimento ap\u00F3s sua deposi\u00E7\u00E3o inicial, durante e ap\u00F3s a sua litifica\u00E7\u00E3o, excluindo altera\u00E7\u00E3o superficial (desgaste) e metamorfismo. Estas mudan\u00E7as acontecem em temperatura e press\u00E3o relativamente baixas e resultam em altera\u00E7\u00F5es mineral\u00F3gicas que originam rochas. N\u00E3o h\u00E1 nenhuma fronteira n\u00EDtida entre diag\u00E9nese e metamorfismo, mas o \u00FAltimo ocorre em temperaturas e press\u00E3o mais elevadas. Ap\u00F3s a deposi\u00E7\u00E3o, os sedimentos s\u00E3o compactados e s\u00E3o enterrados sob camadas sucessivas de sedimentos e cimentados por minerais que se precipitam da solu\u00E7\u00E3o. Gr\u00E3os de sedimentos, rochas e f\u00F3sseis podem ser substitu\u00EDdos por outros minerais durante a diag\u00E9nese. A porosidade geralmente diminui durante a diag\u00E9nese, exceto em casos raros, como a dissolu\u00E7\u00E3o de minerais e dolomitiza\u00E7\u00E3o. O estudo da diag\u00E9nese em rochas \u00E9 usado para entender a hist\u00F3ria tect\u00F4nica a que foram submetidos e os tipos de fluidos que circularam atrav\u00E9s deles. Do ponto de vista comercial, tais estudos ajudam a avaliar a probabilidade de encontrar mineral economicamente vi\u00E1vel e v\u00E1rios dep\u00F3sitos de hidrocarbonetos. O processo de diag\u00E9nese tamb\u00E9m \u00E9 importante na determina\u00E7\u00E3o da decomposi\u00E7\u00E3o de tecido \u00F3sseo."@pt . . . "Diag\u00E9nese (portugu\u00EAs europeu) ou diag\u00EAnese (portugu\u00EAs brasileiro), em geologia e oceanografia refere-se a qualquer mudan\u00E7a e altera\u00E7\u00E3o do sedimento ap\u00F3s sua deposi\u00E7\u00E3o inicial, durante e ap\u00F3s a sua litifica\u00E7\u00E3o, excluindo altera\u00E7\u00E3o superficial (desgaste) e metamorfismo. Estas mudan\u00E7as acontecem em temperatura e press\u00E3o relativamente baixas e resultam em altera\u00E7\u00F5es mineral\u00F3gicas que originam rochas. N\u00E3o h\u00E1 nenhuma fronteira n\u00EDtida entre diag\u00E9nese e metamorfismo, mas o \u00FAltimo ocorre em temperaturas e press\u00E3o mais elevadas."@pt . . . "En geologia i oceanografia, s'anomena diag\u00E8nesi el conjunt de processos qu\u00EDmics, f\u00EDsics o biol\u00F2gics que afecten al sediment des que es diposita i fins a la formaci\u00F3 d'una roca sediment\u00E0ria (litificaci\u00F3), excloent l'alteraci\u00F3 en superf\u00EDcie (meteoritzaci\u00F3). Aquests canvis es produeixen a baixa temperatura i pressi\u00F3, i inclouen, entre d'altres, la compactaci\u00F3, la p\u00E8rdua d'aigua, la cimentaci\u00F3, l'escalfament geot\u00E8rmic i la reordenaci\u00F3 de les part\u00EDcules. El l\u00EDmit inferior de la diag\u00E8nesi \u00E9s imprec\u00EDs i progressiu, tot i que normalment s'estableix quan es presenta la recristal\u00B7litzaci\u00F3 i d'altres indicadors del metamorfisme. L'evoluci\u00F3 diagen\u00E8tica es divideix en tres fases: sindiag\u00E8nesi, anadiag\u00E8nesi i epidiag\u00E8nesi. La majoria de les vegades la consolidaci\u00F3 dels sediments es deu a la infiltraci\u00F3 d'aig\u00FCes que contenen mat\u00E8ries dissoltes. La diag\u00E8nesi converteix aix\u00ED la sorra en gres, als fangs calcaris en calc\u00E0ria, a les cendres volc\u00E0niques en cinerita, etc. Les reaccions i altres fen\u00F2mens d'oxidorreducci\u00F3, deshidrataci\u00F3, , cimentaci\u00F3, mineralitzaci\u00F3 i substituci\u00F3 d'un mineral preexistent per un altre constitueixen en conjunt l'autog\u00E8nesis i els minerals resultants d'aquesta s\u00F3n qualificats com a autog\u00E8nics."@ca . . . . . . . . . . "Diagenesi"@it . . . "Die Diagenese (altgriechisch \u03B4\u03B9\u03B1 \u201Adurch\u2018 und \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2 \u201AEntstehung\u2018) ist der geologische Prozess der Verfestigung von Sedimenten und der weiteren Ver\u00E4nderung der dadurch entstandenen Sedimentgesteine unter verh\u00E4ltnism\u00E4\u00DFig niedrigen Dr\u00FCcken und Temperaturen bis zu ihrer Abtragung. Sie ist damit ein Teil des Kreislaufs der Gesteine."@de . "Diag\u00E9nese"@pt . "174236"^^ . . . . "In geologia la diagenesi \u00E8 un qualsiasi cambiamento chimico-fisico subito da un sedimento dopo la sua deposizione iniziale, durante e dopo la sua trasformazione in roccia coerente, ad esclusione dell'alterazione superficiale (erosione), I cambiamenti diagenetici avvengono a temperature (fino a circa 200 \u00B0C) e pressioni (2-3 bar) relativamente basse e possono avere come conseguenza variazioni della mineralogia e/o della struttura originale della roccia. Si riconoscono diversi fasi nel corso della diagenesi:"@it . "Diagenesia sedimentuak mekanismo fisiko-kimiko edo biokimikoen bitartez arroka sedimentario bilakatzen direneko prozesua da. Ziklo sedimentarioren azken etapa da, materialak elkartzen direnean alterazio kimiko eta fisiko bat jasaten dute bere zanpatzea eragiten duena.Gehienetan sakonera txikian, hain altuak ez diren tenperatura eta presio-mailetan eta konpaktazioz, deshidratazioz, disoluzioz, zimentazioz, eta gertatzen dira."@eu . . . .