. . . . . . . . "Orogenes"@sv . . . . . . "\u041E\u0440\u043E\u0433\u0435\u043D\u0435\u0437"@uk . . . . . "\u9020\u5C71\u904B\u52D5"@ja . . . . . . . . . . . . "Orogenia (antzinako grezierazko \u1F44\u03C1\u03BF\u03C2, \u00F3ros, \u201Cmendi\u201D + \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2, g\u00E9nesis, \u201Csorrera/jatorria\u201D) mendien sorrera aztertzen duen Geografiaren adarra da. Baita ere mendien sorrera edo osatzea bera adierazten du, litosfera munduko zati kontinentalaren eremu zabalago edo txikiagoren deformazio konpresiboak sortutakoa da. Engrosazio kortikal bat sortzen da, eta materialek hainbat deformazio tektoniko konpresibo jasaten dituzte, tolestura, failazioa eta mantu luzperiak barne."@eu . . "Orogeneze, voln\u011B p\u0159elo\u017Eena do \u010De\u0161tiny jako horotvorba \u010Di horotvo\u0159en\u00ED (z \u0159eck\u00E9ho oros \u201Ehora\u201C a genesis \u201Evznik\u201C), spr\u00E1vn\u011Bji a v u\u017E\u0161\u00EDm smyslu tektogeneze je pom\u011Brn\u011B rychl\u00FD geologick\u00FD proces, p\u0159i kter\u00E9m v\u011Bt\u0161inou vlivem proces\u016F deskov\u00E9 tektoniky vznikaj\u00ED p\u00E1semn\u00E1 poho\u0159\u00ED (naz\u00FDvan\u00E1 t\u00E9\u017E orogenn\u00ED p\u00E1sma). Zahrnuje v sob\u011B jednak tektonick\u00E9 procesy, vnitrodeskov\u00E9 zkr\u00E1cen\u00ED, zes\u00EDlen\u00ED k\u016Fry, jako\u017E i v\u00FDzdvih poho\u0159\u00ED. Orogeneze v\u017Edy souvis\u00ED s deskovou tektonikou. Jedn\u00E1 se o proces, kter\u00FD je dlouhodob\u00FD a kter\u00FD trv\u00E1 mili\u00F3ny a\u017E des\u00EDtky mili\u00F3n\u016F let. Horskou soustavu vzniklou orogenez\u00ED naz\u00FDv\u00E1me orog\u00E9n."@cs . "L\u2019orogen\u00E8se, ou orog\u00E9n\u00E8se, est le terme scientifique d\u00E9signant l'ensemble des m\u00E9canismes de formation des montagnes, divers syst\u00E8mes th\u00E9oriques (mod\u00E8les g\u00E9odynamiques) englobant ces processus de formation des reliefs, et des ensembles d'orog\u00E8nes (syst\u00E8mes montagneux sur une portion de la cro\u00FBte terrestre ayant subi d'importantes contraintes compressives). Ces ph\u00E9nom\u00E8nes se succ\u00E8dent \u00E0 travers les temps g\u00E9ologiques, entrecoup\u00E9s par des phases d'\u00E9rosion des reliefs et de s\u00E9dimentation dans des bassins s\u00E9dimentaires. Ces regroupements temporels et g\u00E9ographiques sont expliqu\u00E9s par les cycles de Wilson, bas\u00E9s sur la tectonique des plaques et la finitude de la surface de la Terre. \u00C0 la p\u00E9riph\u00E9rie des vieux cratons, se sont form\u00E9es des ceintures orog\u00E9niques lin\u00E9aires anciennes (les vieux massifs y formant un socle aras\u00E9 par une longue \u00E9rosion et recouvert en discordance par des roches volcaniques et s\u00E9dimentaires), et, encore plus \u00E0 la p\u00E9riph\u00E9rie, des ceintures plus jeunes, visibles sous forme de cha\u00EEnes montagneuses. Cette disposition concentrique traduit les cycles de Wilson."@fr . . "53879"^^ . . . . . . . "Orogeny is the primary mechanism by which mountains are formed on continents. An orogeny is an event that takes place at a convergent plate margin when plate motion compresses the margin. An orogenic belt or orogen develops as the compressed plate crumples and is uplifted to form one or more mountain ranges. This involves a series of geological processes collectively called orogenesis. These include both structural deformation of existing continental crust and the creation of new continental crust through volcanism. Magma rising in the orogen carries less dense material upwards while leaving more dense material behind, resulting in compositional differentiation of Earth's lithosphere (crust and uppermost mantle). A synorogenic process or event is one that occurs during an orogeny."@en . . "Orog\u00E9nese (portugu\u00EAs europeu) ou orog\u00EAnese (portugu\u00EAs brasileiro) (do grego: Oros, montanha; e genesis, forma\u00E7\u00E3o), ou ainda orogenia, \u00E9 o conjunto de processos que levam \u00E0 forma\u00E7\u00E3o ou rejuvenescimento de montanhas ou cadeias de montanhas produzido principalmente pelo diastrofismo (dobramentos, falhas ou a combina\u00E7\u00E3o dos dois), ou seja, pela deforma\u00E7\u00E3o compressiva da litosfera continental. A orogenia ocorre quando h\u00E1 colis\u00E3o de placas tect\u00F4nicas e traz como consequ\u00EAncia a forma\u00E7\u00E3o de dobramentos, cordilheiras ou fossas. Sua \u00E1rea de atua\u00E7\u00E3o \u00E9 marcada pela ocorr\u00EAncia frequente de sismos e pela presen\u00E7a abundante de vulc\u00F5es. Quando os dobramentos datam de uma era geol\u00F3gica recente, (Era Cenozoica) como os Andes, s\u00E3o considerados modernos, e quando datam de uma era geol\u00F3gica antiga, (pr\u00E9-Cambriano, por exemplo) como o Escudo das Guianas, s\u00E3o considerados escudos ou maci\u00E7os antigos. As fossas, por sua vez, s\u00E3o forma\u00E7\u00F5es recentes, datadas do Cenozoico, por exemplo a Fossa das Marianas. S\u00E3o formadas quando, na colis\u00E3o, uma placa desloca-se para baixo da outra, criando o que costuma-se chamar de Zona de Subduc\u00E7\u00E3o ou Zona de Benioff. Caracterizam-se por representarem as \u00E1reas mais profundas do planeta, por estarem em contacto direto com a astenosfera e por sua grande instabilidade tect\u00F3nica. J\u00E1 a trafrog\u00EAnese \u00E9 respons\u00E1vel pela forma\u00E7\u00E3o das dorsais,ou seja, grandes cadeias montanhosas submersas onde ocorrem os fen\u00F4menos relacionados \u00E0 diverg\u00EAncia de placas litosf\u00E9ricas e das falhas geol\u00F3gicas na crosta continental (que s\u00E3o consequ\u00EAncia da separa\u00E7\u00E3o das placas). As cadeias montanhosas submarinas s\u00E3o a consequ\u00EAncia do intumenscimento da crosta oce\u00E2nica (em estado avan\u00E7ado de separa\u00E7\u00E3o continental), ocasionado pela efus\u00E3o de materiais do manto terrestre (devido a causas como as correntes de convec\u00E7\u00E3o do manto), que pruduzem, em meios a falhamentos e efus\u00E3o de magmas, o relevo dessas por\u00E7\u00F5es de litosfera oce\u00E2nica."@pt . . . "\uC870\uC0B0 \uC6B4\uB3D9"@ko . . . . . "Orogenezo"@eo . . . . . "Orogenes (fr\u00E5n grekiskans oros \"berg\" och genesis \"ursprung\" eller \"skapelse\") \u00E4r den vetenskapliga termen f\u00F6r en avl\u00E5ng och n\u00E5gorlunda bred zon av deformation av bergarter och som ofta tar sig uttryck i att bergskedjor bildas. Vid aktiva orogeneser brukar vulkanisk aktivitet och jordb\u00E4vningar f\u00F6rekomma. Orogeneser sker vanligtvis n\u00E4r tv\u00E5 kontinentalplattor kolliderar med varandra och den ena skjuts upp p\u00E5 den andra. I icke vetenskapliga sammanhang anv\u00E4nds ofta begreppet bergskedjebildning, och ibland det mindre l\u00E4mpliga bergskedjeveckning."@sv . . . . . . "L'orog\u00E8nesi \u00E9s la formaci\u00F3 de muntanyes i serralades que es produeix per la deformaci\u00F3 compressiva dels sediments dipositats en una conca sediment\u00E0ria o geosinclinal. Aquests sediments s\u00F3n l'origen dels plegaments o falles, que formen el relleu de la Terra."@ca . . . . . "Die Gebirgsbildung oder Orogenese (zusammengesetzt aus den griechischen W\u00F6rtern \u1F44\u03C1\u03BF\u03C2 \u00F3ros \u201ABerg\u2018 und \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2 g\u00E9nesis \u201AEntstehen, Zeugung, Geburt\u2018) wird durch tektonische Vorg\u00E4nge verursacht, die durch die Kollision von Lithosph\u00E4renplatten erzeugt werden. Spezialf\u00E4lle der Orogenese betreffen die Bruchtektonik (Bildung von Bruchschollengebirgen und Bruchfaltengebirgen), die nur indirekt durch die Verschiebung von Kontinentalplatten verursacht wird."@de . . . . "Gebirgsbildung"@de . . . . . "L'orogenesi (dal greco antico \u1F44\u03C1\u03BF\u03C2, \u00ABrilievo, montagna\u00BB e \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2, \u00ABorigine, causa produttiva\u00BB) indica in geologia il processo di formazione di un rilievo montuoso. Nel linguaggio geologico, il termine si riferisce alla formazione degli orogeni, derivanti da masse rocciose che hanno subito una deformazione tettonica, per prevalenza di spinte laterali, arrivando ad impilarsi creando una catena montuosa."@it . . . . . . "Orogeni"@in . . . "Gebergtevorming alias orogenese is een gevolg van de platentektoniek, de bewegingen van platen langs elkaar (zijschuivingsbewegingen), over en onder elkaar (compressieve bewegingen) en uit elkaar (extensionele bewegingen). Bij al deze bewegingen kan een gebergte gevormd worden, hoewel dit doorgaans het gevolg is van compressieve bewegingen."@nl . . "Gebergtevorming"@nl . . . . . "38748"^^ . . . . "L\u2019orogen\u00E8se, ou orog\u00E9n\u00E8se, est le terme scientifique d\u00E9signant l'ensemble des m\u00E9canismes de formation des montagnes, divers syst\u00E8mes th\u00E9oriques (mod\u00E8les g\u00E9odynamiques) englobant ces processus de formation des reliefs, et des ensembles d'orog\u00E8nes (syst\u00E8mes montagneux sur une portion de la cro\u00FBte terrestre ayant subi d'importantes contraintes compressives). Ces ph\u00E9nom\u00E8nes se succ\u00E8dent \u00E0 travers les temps g\u00E9ologiques, entrecoup\u00E9s par des phases d'\u00E9rosion des reliefs et de s\u00E9dimentation dans des bassins s\u00E9dimentaires. Ces regroupements temporels et g\u00E9ographiques sont expliqu\u00E9s par les cycles de Wilson, bas\u00E9s sur la tectonique des plaques et la finitude de la surface de la Terre."@fr . . . . . "\u039F\u03C1\u03BF\u03B3\u03AD\u03BD\u03B5\u03C3\u03B7"@el . "Orog\u00E8nesi"@ca . . "Orog\u00E9nese"@pt . . "Orogeneze"@cs . . "\uC870\uC0B0 \uC6B4\uB3D9\uC740 \uC9C0\uAD6C \uD45C\uBA74\uC744 \uB36E\uC740 \uC57D 10\uC7A5\uC758 \uAC15\uD55C \uD310\uC774 \uC6B4\uB3D9\uC744 \uD558\uC5EC \uB2E4\uB978 \uD310\uC5D0 \uBD80\uB52A\uCE58\uAC70\uB098 \uB2E4\uB978 \uD310 \uBC11\uC73C\uB85C \uB4E4\uC5B4\uAC00\uB294 \uAC83\uC744 \uB9D0\uD55C\uB2E4. \uD310\uB07C\uB9AC \uC811\uCD09\uD558\uB294 \uC9C0\uB300\uC5D0\uC11C\uB294 \uC9C0\uC9C4\uC774\uB098 \uD654\uC0B0 \uD65C\uB3D9\uC774 \uBE48\uBC88\uD558\uAC8C \uC77C\uC5B4\uB09C\uB2E4. \uC870\uC0B0 \uC6B4\uB3D9\uC744 \uD1B5\uD574 \uC54C\uD504\uC2A4\uB098 \uD788\uB9D0\uB77C\uC57C \uAC19\uC740 \uB300\uC0B0\uB9E5\uB3C4 \uC0DD\uACA8\uB09C\uB2E4. \uC774\uC640 \uAC19\uC740 \uACAC\uD574\uB97C \uD310\uAD6C\uC870\uB860\uC774\uB77C \uD55C\uB2E4. \uC5EC\uAE30\uC11C\uB294 \uD310\uAD6C\uC870\uB860\uC5D0 \uC785\uAC01\uD558\uC5EC \uC870\uC0B0\uD65C\uB3D9\uC744 \uC0B4\uD3B4\uBCF4\uAE30\uB85C \uD55C\uB2E4."@ko . . "\u0627\u0644\u0623\u0648\u0631\u0648\u062C\u064A\u0646\u064A\u0629 \u0623\u0648 \u062A\u064E\u0643\u064E\u0648\u064F\u0651\u0646\u064F \u0627\u0644\u062C\u0650\u0628\u064E\u0627\u0644\u0650 \u0623\u0648 \u0646\u064F\u0634\u064F\u0648\u0621\u064F \u0627\u0644\u062C\u0650\u0628\u064E\u0627\u0644\u0650\u060C \u0648\u062A\u0646\u0637\u0642 \u0623\u064A\u0636\u0627 \u0627\u0644\u062A\u062C\u0628\u0644\u060C \u0648\u0647\u064A \u062A\u0634\u064A\u0631 \u0625\u0644\u0649 \u0627\u0644\u0642\u0648\u0649 \u0648\u0627\u0644\u0623\u062D\u062F\u0627\u062B \u0627\u0644\u062A\u064A \u062A\u0624\u062F\u064A \u0625\u0644\u0649 \u062A\u0634\u0648\u0647 \u062A\u0631\u0643\u064A\u0628\u064A \u0643\u0628\u064A\u0631 \u0641\u064A \u0627\u0644\u063A\u0644\u0627\u0641 \u0627\u0644\u0635\u062E\u0631\u064A \u0644\u0644\u0623\u0631\u0636 (\u0627\u0644\u0642\u0634\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0648\u0627\u0644\u062F\u062B\u0627\u0631) \u0628\u0633\u0628\u0628 \u0627\u0644\u062A\u062D\u0627\u0645 \u0627\u0644\u0635\u0641\u0627\u0626\u062D \u0627\u0644\u062A\u0643\u062A\u0648\u0646\u064A\u0629. \u0648\u064A\u0646\u062A\u062C \u0639\u0646 \u0627\u0644\u062A\u062C\u0627\u0648\u0628 \u0645\u0639 \u0645\u062B\u0644 \u0647\u0630\u0627 \u0627\u0644\u0627\u0644\u062A\u062D\u0627\u0645 \u062A\u0643\u0648\u064A\u0646 \u0645\u0633\u0627\u0644\u0643 \u0637\u0648\u064A\u0644\u0629 \u0645\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0634\u062F\u064A\u062F\u0629 \u0627\u0644\u062A\u0634\u0648\u0647 \u0627\u0644\u0645\u0633\u0645\u0627\u0629 \u0627\u0644\u0623\u0648\u0631\u0648\u062C\u064A\u0646\u0627\u062A \u0623\u0648 \u0627\u0644\u0623\u062D\u0632\u0645\u0629 \u0627\u0644\u0623\u0648\u0631\u0648\u062C\u064A\u0646\u064A\u0629 \u0623\u0648 \u0627\u0644\u0623\u064E\u062D\u0652\u0632\u0650\u0645\u064E\u0629 \u0627\u0644\u0634\u064F\u0651\u0645\u064F\u0648\u062E\u0650\u064A\u064E\u0651\u0629. \u0648\u0647\u064A \u0627\u0644\u0622\u0644\u064A\u0629 \u0627\u0644\u0623\u0633\u0627\u0633\u064A\u0629 \u0627\u0644\u062A\u064A \u062A\u062A\u0643\u0648\u0646 \u0645\u0646 \u062E\u0644\u0627\u0644\u0647\u0627 \u0627\u0644\u062C\u0628\u0627\u0644 \u0639\u0644\u0649 \u0627\u0644\u0642\u0627\u0631\u0627\u062A. \u0648\u062A\u062A\u0643\u0648\u0646 \u0627\u0644\u0623\u0648\u0631\u0648\u062C\u064A\u0646\u0627\u062A \u0641\u064A \u0627\u0644\u0648\u0642\u062A \u0627\u0644\u0630\u064A \u062A\u062A\u062C\u0639\u062F \u0641\u064A\u0647 \u0627\u0644\u0635\u0641\u0627\u0626\u062D \u0627\u0644\u0642\u0627\u0631\u064A\u0629\u060C \u0648\u064A\u062A\u0645 \u062F\u0641\u0639\u0647\u0627 \u0644\u0623\u0639\u0644\u0649 \u0644\u062A\u0634\u0643\u064A\u0644 \u0633\u0644\u0627\u0633\u0644 \u062C\u0628\u0644\u064A\u0629\u060C \u0648\u062A\u062A\u0636\u0645\u0646 \u0645\u062C\u0645\u0648\u0639\u0629 \u0643\u0628\u064A\u0631\u0629 \u0645\u0646 \u0627\u0644\u0639\u0645\u0644\u064A\u0627\u062A \u0627\u0644\u062C\u064A\u0648\u0644\u0648\u062C\u064A\u0629 \u0627\u0644\u062A\u064A \u062A\u0633\u0645\u0649 \u0639\u0645\u0648\u0645\u064B\u0627 \u062A\u0643\u0648\u0651\u0646 \u0627\u0644\u062C\u0628\u0627\u0644."@ar . "Orogenia"@eu . . . . . . . . . "\u0397 \u03BF\u03C1\u03BF\u03B3\u03AD\u03BD\u03B5\u03C3\u03B7 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C4\u03BF \u03C6\u03B1\u03B9\u03BD\u03CC\u03BC\u03B5\u03BD\u03BF \u03C4\u03BF\u03C5 \u03C3\u03C7\u03B7\u03BC\u03B1\u03C4\u03B9\u03C3\u03BC\u03BF\u03CD \u03C4\u03C9\u03BD \u03B2\u03BF\u03C5\u03BD\u03CE\u03BD \u03BA\u03B1\u03B9 \u03BA\u03B1\u03C4' \u03B5\u03C0\u03AD\u03BA\u03C4\u03B1\u03C3\u03B7 \u03C4\u03C9\u03BD \u03BF\u03C1\u03BF\u03C3\u03B5\u03B9\u03C1\u03CE\u03BD. \u039C\u03B5 \u03C4\u03BF\u03BD \u03CC\u03C1\u03BF \u03B1\u03C5\u03C4\u03CC\u03BD \u03C3\u03C4\u03B7 \u03B3\u03B5\u03C9\u03BB\u03BF\u03B3\u03AF\u03B1 \u03B1\u03C0\u03BF\u03BA\u03B1\u03BB\u03B5\u03AF\u03C4\u03B1\u03B9 \u03BC\u03AF\u03B1 \u03C3\u03B5\u03B9\u03C1\u03AC \u03B3\u03B5\u03B3\u03BF\u03BD\u03CC\u03C4\u03C9\u03BD \u03BA\u03B1\u03B9 \u03B1\u03BD\u03B1\u03BA\u03B1\u03C4\u03B1\u03C4\u03AC\u03BE\u03B5\u03C9\u03BD \u03C4\u03BF\u03C5 \u03C6\u03BB\u03BF\u03B9\u03BF\u03CD \u03C4\u03B7\u03C2 \u0393\u03B7\u03C2, \u03BA\u03B1\u03C4\u03AC \u03C4\u03B7 \u03B4\u03B9\u03AC\u03C1\u03BA\u03B5\u03B9\u03B1 \u03C4\u03C9\u03BD \u03BF\u03C0\u03BF\u03AF\u03C9\u03BD, \u03B1\u03BD\u03C5\u03C8\u03CE\u03BD\u03BF\u03BD\u03C4\u03B1\u03B9 \u03BA\u03B1\u03B9 \u03C0\u03C4\u03C5\u03C7\u03CE\u03BD\u03BF\u03BD\u03C4\u03B1\u03B9 \u03C4\u03B5\u03C1\u03AC\u03C3\u03C4\u03B9\u03B5\u03C2 \u03BC\u03AC\u03B6\u03B5\u03C2 \u03C0\u03B5\u03C4\u03C1\u03C9\u03BC\u03AC\u03C4\u03C9\u03BD \u03C4\u03C9\u03BD \u03B3\u03B5\u03C9\u03C3\u03CD\u03B3\u03BA\u03BB\u03B9\u03BD\u03C9\u03BD \u03BA\u03B1\u03B9 \u03B2\u03B1\u03B8\u03BC\u03B9\u03B1\u03AF\u03B1 \u03C3\u03C7\u03B7\u03BC\u03B1\u03C4\u03AF\u03B6\u03BF\u03BD\u03C4\u03B1\u03B9 \u03B2\u03BF\u03C5\u03BD\u03AC. \u039F\u03B9 \u03B1\u03BD\u03B1\u03BA\u03B1\u03C4\u03B1\u03C4\u03AC\u03BE\u03B5\u03B9\u03C2 \u03B1\u03C5\u03C4\u03AD\u03C2, \u03B4\u03B9\u03B1\u03C1\u03BA\u03BF\u03CD\u03BD \u03C3\u03C5\u03BD\u03AE\u03B8\u03C9\u03C2 \u03BC\u03B5\u03C1\u03B9\u03BA\u03AD\u03C2 \u03B4\u03B5\u03BA\u03AC\u03B4\u03B5\u03C2 \u03B5\u03BA\u03B1\u03C4\u03BF\u03BC\u03BC\u03CD\u03C1\u03B9\u03B1 \u03C7\u03C1\u03CC\u03BD\u03B9\u03B1."@el . . . "Orogeni mengacu pada gaya dan peristiwa yang mengarah ke deformasi struktural besar litosfer Bumi (kerak dan mantel teratas) karena interaksi antara lempeng-lempeng tektonik. Sabuk orogenik terbentuk ketika lempeng benua menyusut dan didorong ke atas untuk membentuk jajaran pegunungan, dan melibatkan sejumlah besar proses geologi yang secara kolektif disebut orogenesis. Kata \"orogeni\" berasal dari bahasa Yunani yang (oros untuk \"gunung\" ditambah genesis untuk \"penciptaan\" atau \"asal\"), orogeni adalah mekanisme utama dibangunnya pegunungan di atas benua."@in . . . . . . "Die Gebirgsbildung oder Orogenese (zusammengesetzt aus den griechischen W\u00F6rtern \u1F44\u03C1\u03BF\u03C2 \u00F3ros \u201ABerg\u2018 und \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2 g\u00E9nesis \u201AEntstehen, Zeugung, Geburt\u2018) wird durch tektonische Vorg\u00E4nge verursacht, die durch die Kollision von Lithosph\u00E4renplatten erzeugt werden. Spezialf\u00E4lle der Orogenese betreffen die Bruchtektonik (Bildung von Bruchschollengebirgen und Bruchfaltengebirgen), die nur indirekt durch die Verschiebung von Kontinentalplatten verursacht wird."@de . . . . . . . "\u0397 \u03BF\u03C1\u03BF\u03B3\u03AD\u03BD\u03B5\u03C3\u03B7 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C4\u03BF \u03C6\u03B1\u03B9\u03BD\u03CC\u03BC\u03B5\u03BD\u03BF \u03C4\u03BF\u03C5 \u03C3\u03C7\u03B7\u03BC\u03B1\u03C4\u03B9\u03C3\u03BC\u03BF\u03CD \u03C4\u03C9\u03BD \u03B2\u03BF\u03C5\u03BD\u03CE\u03BD \u03BA\u03B1\u03B9 \u03BA\u03B1\u03C4' \u03B5\u03C0\u03AD\u03BA\u03C4\u03B1\u03C3\u03B7 \u03C4\u03C9\u03BD \u03BF\u03C1\u03BF\u03C3\u03B5\u03B9\u03C1\u03CE\u03BD. \u039C\u03B5 \u03C4\u03BF\u03BD \u03CC\u03C1\u03BF \u03B1\u03C5\u03C4\u03CC\u03BD \u03C3\u03C4\u03B7 \u03B3\u03B5\u03C9\u03BB\u03BF\u03B3\u03AF\u03B1 \u03B1\u03C0\u03BF\u03BA\u03B1\u03BB\u03B5\u03AF\u03C4\u03B1\u03B9 \u03BC\u03AF\u03B1 \u03C3\u03B5\u03B9\u03C1\u03AC \u03B3\u03B5\u03B3\u03BF\u03BD\u03CC\u03C4\u03C9\u03BD \u03BA\u03B1\u03B9 \u03B1\u03BD\u03B1\u03BA\u03B1\u03C4\u03B1\u03C4\u03AC\u03BE\u03B5\u03C9\u03BD \u03C4\u03BF\u03C5 \u03C6\u03BB\u03BF\u03B9\u03BF\u03CD \u03C4\u03B7\u03C2 \u0393\u03B7\u03C2, \u03BA\u03B1\u03C4\u03AC \u03C4\u03B7 \u03B4\u03B9\u03AC\u03C1\u03BA\u03B5\u03B9\u03B1 \u03C4\u03C9\u03BD \u03BF\u03C0\u03BF\u03AF\u03C9\u03BD, \u03B1\u03BD\u03C5\u03C8\u03CE\u03BD\u03BF\u03BD\u03C4\u03B1\u03B9 \u03BA\u03B1\u03B9 \u03C0\u03C4\u03C5\u03C7\u03CE\u03BD\u03BF\u03BD\u03C4\u03B1\u03B9 \u03C4\u03B5\u03C1\u03AC\u03C3\u03C4\u03B9\u03B5\u03C2 \u03BC\u03AC\u03B6\u03B5\u03C2 \u03C0\u03B5\u03C4\u03C1\u03C9\u03BC\u03AC\u03C4\u03C9\u03BD \u03C4\u03C9\u03BD \u03B3\u03B5\u03C9\u03C3\u03CD\u03B3\u03BA\u03BB\u03B9\u03BD\u03C9\u03BD \u03BA\u03B1\u03B9 \u03B2\u03B1\u03B8\u03BC\u03B9\u03B1\u03AF\u03B1 \u03C3\u03C7\u03B7\u03BC\u03B1\u03C4\u03AF\u03B6\u03BF\u03BD\u03C4\u03B1\u03B9 \u03B2\u03BF\u03C5\u03BD\u03AC. \u039F\u03B9 \u03B1\u03BD\u03B1\u03BA\u03B1\u03C4\u03B1\u03C4\u03AC\u03BE\u03B5\u03B9\u03C2 \u03B1\u03C5\u03C4\u03AD\u03C2, \u03B4\u03B9\u03B1\u03C1\u03BA\u03BF\u03CD\u03BD \u03C3\u03C5\u03BD\u03AE\u03B8\u03C9\u03C2 \u03BC\u03B5\u03C1\u03B9\u03BA\u03AD\u03C2 \u03B4\u03B5\u03BA\u03AC\u03B4\u03B5\u03C2 \u03B5\u03BA\u03B1\u03C4\u03BF\u03BC\u03BC\u03CD\u03C1\u03B9\u03B1 \u03C7\u03C1\u03CC\u03BD\u03B9\u03B1."@el . . . . . "\u041E\u0440\u043E\u0433\u0435\u043D\u0435\u0301\u0437 (\u0440\u043E\u0441. \u043E\u0440\u043E\u0433\u0435\u043D\u0435\u0437, \u0430\u043D\u0433\u043B. orogenesis, \u043D\u0456\u043C. Orogenese f, Gebirgsbildung f) \u2014 \u0441\u0443\u043A\u0443\u043F\u043D\u0456\u0441\u0442\u044C \u0456\u043D\u0442\u0435\u043D\u0441\u0438\u0432\u043D\u0438\u0445 \u0432\u0438\u0441\u0445\u0456\u0434\u043D\u0438\u0445 \u0432\u0435\u0440\u0442\u0438\u043A\u0430\u043B\u044C\u043D\u0438\u0445 \u0442\u0435\u043A\u0442\u043E\u043D\u0456\u0447\u043D\u0438\u0445 \u0440\u0443\u0445\u0456\u0432 (\u0441\u043A\u043B\u0430\u0434\u0447\u0430\u0441\u0442\u043E\u0441\u0442\u0456 \u0442\u0430 \u0440\u043E\u0437\u0440\u0438\u0432\u0456\u0432), \u043F\u0440\u043E\u0446\u0435\u0441\u0456\u0432, \u0437 \u044F\u043A\u0438\u043C\u0438 \u043F\u043E\u0432'\u044F\u0437\u0430\u043D\u0435 \u0432\u0438\u043D\u0438\u043A\u043D\u0435\u043D\u043D\u044F \u0442\u0430 \u0440\u043E\u0437\u0432\u0438\u0442\u043E\u043A \u0433\u0456\u0440."@uk . . . "Se denomina orog\u00E9nesis u orogenia al proceso geol\u00F3gico por el cual una zona alargada de la corteza terrestre se acorta y engrosa por deformaci\u00F3n y fracturaci\u00F3n como consecuencia de esfuerzos tect\u00F3nicos laterales.\u200B Normalmente las orogenias son acompa\u00F1adas por la formaci\u00F3n de cabalgamientos y plegamientos.\u200B La palabra orog\u00E9nesis proviene del idioma griego (oros significa \"monta\u00F1a\" y g\u00E9nesis significa \"creaci\u00F3n\" u \"origen\"),\u200B y es el mecanismo principal mediante el cual las cordilleras se forman en los continentes. Los or\u00F3genos o cordilleras se crean cuando una placa tect\u00F3nica con corteza continental es \"arrugada\" y fracturada y los fragmentos se apilan, aumentando el grosor original de la corteza. Adem\u00E1s tambi\u00E9n suelen producirse procesos de magmatismo, que aportan nuevos materiales gran\u00EDticos que se incorporan a la corteza. Todo esto implica una gran cantidad de procesos geol\u00F3gicos que en conjunto se llaman orog\u00E9nesis.\u200B\u200B Com\u00FAnmente la orog\u00E9nesis produce estructuras alargadas y levemente arqueadas que se conocen como cinturones orog\u00E9nicos. Los cinturones orog\u00E9nicos consisten generalmente en franjas alargadas y paralelas de rocas de caracter\u00EDsticas similares en toda su longitud. Los cinturones orog\u00E9nicos est\u00E1n asociados a zonas de subducci\u00F3n, las cuales consumen corteza terrestre, y arcos volc\u00E1nicos.\u200B La altura topogr\u00E1fica de cordilleras orog\u00E9nicas est\u00E1 relacionada con el principio de isostasia,\u200B que es el equilibrio de la fuerza gravitacional sobre la cordillera (compuesta normalmente de material de corteza continental relativamente ligero) y las fuerzas involucradas en la flotabilidad de la cordillera que descansa sobre el denso manto.\u200B"@es . "Orog\u00E9nesis"@es . . . . . . . "Orogeny"@en . . . . . . . . . . . "Orogenezo, a\u016D montari\u011Do, estas rezulto de platotektonismo, movi\u011Do de platoj unu apud la alia, unu sur la alia kaj unu for de la alia. Dum tiuj \u0109i movi\u011Doj foje ekestas montaro, kvankam tio \u0109i estas plejofte nur la ka\u016Dzo de movi\u011Doj kiuj kunpremas."@eo . . . . "Orogeneza"@pl . . . "Orogenezo, a\u016D montari\u011Do, estas rezulto de platotektonismo, movi\u011Do de platoj unu apud la alia, unu sur la alia kaj unu for de la alia. Dum tiuj \u0109i movi\u011Doj foje ekestas montaro, kvankam tio \u0109i estas plejofte nur la ka\u016Dzo de movi\u011Doj kiuj kunpremas."@eo . . . . . . . . . . . "Orogeni mengacu pada gaya dan peristiwa yang mengarah ke deformasi struktural besar litosfer Bumi (kerak dan mantel teratas) karena interaksi antara lempeng-lempeng tektonik. Sabuk orogenik terbentuk ketika lempeng benua menyusut dan didorong ke atas untuk membentuk jajaran pegunungan, dan melibatkan sejumlah besar proses geologi yang secara kolektif disebut orogenesis. Kata \"orogeni\" berasal dari bahasa Yunani yang (oros untuk \"gunung\" ditambah genesis untuk \"penciptaan\" atau \"asal\"), orogeni adalah mekanisme utama dibangunnya pegunungan di atas benua."@in . . . . . . . . . . . "L'orog\u00E8nesi \u00E9s la formaci\u00F3 de muntanyes i serralades que es produeix per la deformaci\u00F3 compressiva dels sediments dipositats en una conca sediment\u00E0ria o geosinclinal. Aquests sediments s\u00F3n l'origen dels plegaments o falles, que formen el relleu de la Terra."@ca . . . . . "\u041E\u0440\u043E\u0433\u0435\u043D\u0435\u0301\u0437 (\u0440\u043E\u0441. \u043E\u0440\u043E\u0433\u0435\u043D\u0435\u0437, \u0430\u043D\u0433\u043B. orogenesis, \u043D\u0456\u043C. Orogenese f, Gebirgsbildung f) \u2014 \u0441\u0443\u043A\u0443\u043F\u043D\u0456\u0441\u0442\u044C \u0456\u043D\u0442\u0435\u043D\u0441\u0438\u0432\u043D\u0438\u0445 \u0432\u0438\u0441\u0445\u0456\u0434\u043D\u0438\u0445 \u0432\u0435\u0440\u0442\u0438\u043A\u0430\u043B\u044C\u043D\u0438\u0445 \u0442\u0435\u043A\u0442\u043E\u043D\u0456\u0447\u043D\u0438\u0445 \u0440\u0443\u0445\u0456\u0432 (\u0441\u043A\u043B\u0430\u0434\u0447\u0430\u0441\u0442\u043E\u0441\u0442\u0456 \u0442\u0430 \u0440\u043E\u0437\u0440\u0438\u0432\u0456\u0432), \u043F\u0440\u043E\u0446\u0435\u0441\u0456\u0432, \u0437 \u044F\u043A\u0438\u043C\u0438 \u043F\u043E\u0432'\u044F\u0437\u0430\u043D\u0435 \u0432\u0438\u043D\u0438\u043A\u043D\u0435\u043D\u043D\u044F \u0442\u0430 \u0440\u043E\u0437\u0432\u0438\u0442\u043E\u043A \u0433\u0456\u0440."@uk . "Orog\u00E9nese (portugu\u00EAs europeu) ou orog\u00EAnese (portugu\u00EAs brasileiro) (do grego: Oros, montanha; e genesis, forma\u00E7\u00E3o), ou ainda orogenia, \u00E9 o conjunto de processos que levam \u00E0 forma\u00E7\u00E3o ou rejuvenescimento de montanhas ou cadeias de montanhas produzido principalmente pelo diastrofismo (dobramentos, falhas ou a combina\u00E7\u00E3o dos dois), ou seja, pela deforma\u00E7\u00E3o compressiva da litosfera continental."@pt . . . . "Orogen\u00E8se"@fr . . . "\u9020\u5C71\u904B\u52D5\uFF08\u305E\u3046\u3056\u3093\u3046\u3093\u3069\u3046\u3001\u82F1: orogeny\uFF09\u3068\u306F\u3001\u5927\u5C71\u8108\u3084\u5F27\u72B6\u5217\u5CF6\u3092\u5F62\u6210\u3059\u308B\u3088\u3046\u306A\u5730\u6BBB\u5909\u52D5\u306E\u3053\u3068\u3002\u3053\u306E\u69D8\u306A\u9020\u5C71\u904B\u52D5\u304C\u8D77\u304D\u305F\u5730\u57DF\u3092\u9020\u5C71\u5E2F\u3068\u547C\u3076\u3002"@ja . "1124933726"^^ . . "Orogenes (fr\u00E5n grekiskans oros \"berg\" och genesis \"ursprung\" eller \"skapelse\") \u00E4r den vetenskapliga termen f\u00F6r en avl\u00E5ng och n\u00E5gorlunda bred zon av deformation av bergarter och som ofta tar sig uttryck i att bergskedjor bildas. Vid aktiva orogeneser brukar vulkanisk aktivitet och jordb\u00E4vningar f\u00F6rekomma. Orogeneser sker vanligtvis n\u00E4r tv\u00E5 kontinentalplattor kolliderar med varandra och den ena skjuts upp p\u00E5 den andra. I icke vetenskapliga sammanhang anv\u00E4nds ofta begreppet bergskedjebildning, och ibland det mindre l\u00E4mpliga bergskedjeveckning."@sv . . "\uC870\uC0B0 \uC6B4\uB3D9\uC740 \uC9C0\uAD6C \uD45C\uBA74\uC744 \uB36E\uC740 \uC57D 10\uC7A5\uC758 \uAC15\uD55C \uD310\uC774 \uC6B4\uB3D9\uC744 \uD558\uC5EC \uB2E4\uB978 \uD310\uC5D0 \uBD80\uB52A\uCE58\uAC70\uB098 \uB2E4\uB978 \uD310 \uBC11\uC73C\uB85C \uB4E4\uC5B4\uAC00\uB294 \uAC83\uC744 \uB9D0\uD55C\uB2E4. \uD310\uB07C\uB9AC \uC811\uCD09\uD558\uB294 \uC9C0\uB300\uC5D0\uC11C\uB294 \uC9C0\uC9C4\uC774\uB098 \uD654\uC0B0 \uD65C\uB3D9\uC774 \uBE48\uBC88\uD558\uAC8C \uC77C\uC5B4\uB09C\uB2E4. \uC870\uC0B0 \uC6B4\uB3D9\uC744 \uD1B5\uD574 \uC54C\uD504\uC2A4\uB098 \uD788\uB9D0\uB77C\uC57C \uAC19\uC740 \uB300\uC0B0\uB9E5\uB3C4 \uC0DD\uACA8\uB09C\uB2E4. \uC774\uC640 \uAC19\uC740 \uACAC\uD574\uB97C \uD310\uAD6C\uC870\uB860\uC774\uB77C \uD55C\uB2E4. \uC5EC\uAE30\uC11C\uB294 \uD310\uAD6C\uC870\uB860\uC5D0 \uC785\uAC01\uD558\uC5EC \uC870\uC0B0\uD65C\uB3D9\uC744 \uC0B4\uD3B4\uBCF4\uAE30\uB85C \uD55C\uB2E4."@ko . "\u062A\u0643\u0648\u0646 \u0627\u0644\u062C\u0628\u0627\u0644"@ar . . . . . "\u9020\u5C71\u904B\u52D5\uFF08\u82F1\u8A9E\uFF1AOrogeny\uFF09\u6307\u5730\u6BBC\u7D50\u69CB\u56E0\u70BA\u677F\u584A\u904B\u52D5\u7522\u751F\u5287\u70C8\u8B8A\u5316\uFF0C\u5C6C\u5730\u6BBC\u8B8A\u52D5\u7684\u4E00\u7A2E\u3002\u8A72\u4F5C\u7528\u6703\u7522\u751F\u5CA9\u77F3\u9AD8\u5EA6\u8B8A\u5F62\u7684\u5E36\u72C0\u5340\u57DF\uFF0C\u7A31\u70BA\u9020\u5C71\u5E36\uFF08Orogens\u6216Orogenic belts\uFF09\u3002\u201COrogeny\u201D\u4E00\u8A5E\u4F86\u81EA\u53E4\u5E0C\u81D8\u8A9E\u8A5E\u6839\u1F44\u03C1\u03BF\u03C2\uFF08\u00F3ros\uFF0C\u5C71\uFF09\u548C\u03B3\u03B5\u03BD\u03B5\u03B9\u03B1\uFF08geneia\uFF0C\u8A95\u751F\uFF1B\u8D77\u6E90\uFF09\u3002\u9020\u5C71\u904B\u52D5\u662F\u9020\u6210\u5404\u5927\u9678\u5C71\u5730\u7684\u4E3B\u8981\u6A5F\u5236\uFF1B\u7576\u5927\u9678\u5730\u6BBC\u56E0\u70BA\u9020\u5C71\u904B\u52D5\u7522\u751F\u8936\u76BA\u548C\u539A\u5EA6\u589E\u52A0\u6642\u5C31\u5F62\u6210\u5C71\u8108\u3002\u6D89\u53CA\u5927\u7BC4\u570D\u7684\u5730\u8CEA\u4F5C\u7528\u7D71\u7A31\u9020\u904B\u52D5(\u9020\u904B\u52D5\uFF1F\u540D\u8A5E\u9700\u6CE8\u89E3)\u3002"@zh . . "\u9020\u5C71\u904B\u52D5\uFF08\u82F1\u8A9E\uFF1AOrogeny\uFF09\u6307\u5730\u6BBC\u7D50\u69CB\u56E0\u70BA\u677F\u584A\u904B\u52D5\u7522\u751F\u5287\u70C8\u8B8A\u5316\uFF0C\u5C6C\u5730\u6BBC\u8B8A\u52D5\u7684\u4E00\u7A2E\u3002\u8A72\u4F5C\u7528\u6703\u7522\u751F\u5CA9\u77F3\u9AD8\u5EA6\u8B8A\u5F62\u7684\u5E36\u72C0\u5340\u57DF\uFF0C\u7A31\u70BA\u9020\u5C71\u5E36\uFF08Orogens\u6216Orogenic belts\uFF09\u3002\u201COrogeny\u201D\u4E00\u8A5E\u4F86\u81EA\u53E4\u5E0C\u81D8\u8A9E\u8A5E\u6839\u1F44\u03C1\u03BF\u03C2\uFF08\u00F3ros\uFF0C\u5C71\uFF09\u548C\u03B3\u03B5\u03BD\u03B5\u03B9\u03B1\uFF08geneia\uFF0C\u8A95\u751F\uFF1B\u8D77\u6E90\uFF09\u3002\u9020\u5C71\u904B\u52D5\u662F\u9020\u6210\u5404\u5927\u9678\u5C71\u5730\u7684\u4E3B\u8981\u6A5F\u5236\uFF1B\u7576\u5927\u9678\u5730\u6BBC\u56E0\u70BA\u9020\u5C71\u904B\u52D5\u7522\u751F\u8936\u76BA\u548C\u539A\u5EA6\u589E\u52A0\u6642\u5C31\u5F62\u6210\u5C71\u8108\u3002\u6D89\u53CA\u5927\u7BC4\u570D\u7684\u5730\u8CEA\u4F5C\u7528\u7D71\u7A31\u9020\u904B\u52D5(\u9020\u904B\u52D5\uFF1F\u540D\u8A5E\u9700\u6CE8\u89E3)\u3002"@zh . . . "Orogenia (antzinako grezierazko \u1F44\u03C1\u03BF\u03C2, \u00F3ros, \u201Cmendi\u201D + \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2, g\u00E9nesis, \u201Csorrera/jatorria\u201D) mendien sorrera aztertzen duen Geografiaren adarra da. Baita ere mendien sorrera edo osatzea bera adierazten du, litosfera munduko zati kontinentalaren eremu zabalago edo txikiagoren deformazio konpresiboak sortutakoa da. Engrosazio kortikal bat sortzen da, eta materialek hainbat deformazio tektoniko konpresibo jasaten dituzte, tolestura, failazioa eta mantu luzperiak barne."@eu . . . . . . . . "\u9020\u5C71\u904B\u52D5\uFF08\u305E\u3046\u3056\u3093\u3046\u3093\u3069\u3046\u3001\u82F1: orogeny\uFF09\u3068\u306F\u3001\u5927\u5C71\u8108\u3084\u5F27\u72B6\u5217\u5CF6\u3092\u5F62\u6210\u3059\u308B\u3088\u3046\u306A\u5730\u6BBB\u5909\u52D5\u306E\u3053\u3068\u3002\u3053\u306E\u69D8\u306A\u9020\u5C71\u904B\u52D5\u304C\u8D77\u304D\u305F\u5730\u57DF\u3092\u9020\u5C71\u5E2F\u3068\u547C\u3076\u3002"@ja . . . . . . . "\u0627\u0644\u0623\u0648\u0631\u0648\u062C\u064A\u0646\u064A\u0629 \u0623\u0648 \u062A\u064E\u0643\u064E\u0648\u064F\u0651\u0646\u064F \u0627\u0644\u062C\u0650\u0628\u064E\u0627\u0644\u0650 \u0623\u0648 \u0646\u064F\u0634\u064F\u0648\u0621\u064F \u0627\u0644\u062C\u0650\u0628\u064E\u0627\u0644\u0650\u060C \u0648\u062A\u0646\u0637\u0642 \u0623\u064A\u0636\u0627 \u0627\u0644\u062A\u062C\u0628\u0644\u060C \u0648\u0647\u064A \u062A\u0634\u064A\u0631 \u0625\u0644\u0649 \u0627\u0644\u0642\u0648\u0649 \u0648\u0627\u0644\u0623\u062D\u062F\u0627\u062B \u0627\u0644\u062A\u064A \u062A\u0624\u062F\u064A \u0625\u0644\u0649 \u062A\u0634\u0648\u0647 \u062A\u0631\u0643\u064A\u0628\u064A \u0643\u0628\u064A\u0631 \u0641\u064A \u0627\u0644\u063A\u0644\u0627\u0641 \u0627\u0644\u0635\u062E\u0631\u064A \u0644\u0644\u0623\u0631\u0636 (\u0627\u0644\u0642\u0634\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0648\u0627\u0644\u062F\u062B\u0627\u0631) \u0628\u0633\u0628\u0628 \u0627\u0644\u062A\u062D\u0627\u0645 \u0627\u0644\u0635\u0641\u0627\u0626\u062D \u0627\u0644\u062A\u0643\u062A\u0648\u0646\u064A\u0629. \u0648\u064A\u0646\u062A\u062C \u0639\u0646 \u0627\u0644\u062A\u062C\u0627\u0648\u0628 \u0645\u0639 \u0645\u062B\u0644 \u0647\u0630\u0627 \u0627\u0644\u0627\u0644\u062A\u062D\u0627\u0645 \u062A\u0643\u0648\u064A\u0646 \u0645\u0633\u0627\u0644\u0643 \u0637\u0648\u064A\u0644\u0629 \u0645\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0634\u062F\u064A\u062F\u0629 \u0627\u0644\u062A\u0634\u0648\u0647 \u0627\u0644\u0645\u0633\u0645\u0627\u0629 \u0627\u0644\u0623\u0648\u0631\u0648\u062C\u064A\u0646\u0627\u062A \u0623\u0648 \u0627\u0644\u0623\u062D\u0632\u0645\u0629 \u0627\u0644\u0623\u0648\u0631\u0648\u062C\u064A\u0646\u064A\u0629 \u0623\u0648 \u0627\u0644\u0623\u064E\u062D\u0652\u0632\u0650\u0645\u064E\u0629 \u0627\u0644\u0634\u064F\u0651\u0645\u064F\u0648\u062E\u0650\u064A\u064E\u0651\u0629. \u0648\u0647\u064A \u0627\u0644\u0622\u0644\u064A\u0629 \u0627\u0644\u0623\u0633\u0627\u0633\u064A\u0629 \u0627\u0644\u062A\u064A \u062A\u062A\u0643\u0648\u0646 \u0645\u0646 \u062E\u0644\u0627\u0644\u0647\u0627 \u0627\u0644\u062C\u0628\u0627\u0644 \u0639\u0644\u0649 \u0627\u0644\u0642\u0627\u0631\u0627\u062A. \u0648\u062A\u062A\u0643\u0648\u0646 \u0627\u0644\u0623\u0648\u0631\u0648\u062C\u064A\u0646\u0627\u062A \u0641\u064A \u0627\u0644\u0648\u0642\u062A \u0627\u0644\u0630\u064A \u062A\u062A\u062C\u0639\u062F \u0641\u064A\u0647 \u0627\u0644\u0635\u0641\u0627\u0626\u062D \u0627\u0644\u0642\u0627\u0631\u064A\u0629\u060C \u0648\u064A\u062A\u0645 \u062F\u0641\u0639\u0647\u0627 \u0644\u0623\u0639\u0644\u0649 \u0644\u062A\u0634\u0643\u064A\u0644 \u0633\u0644\u0627\u0633\u0644 \u062C\u0628\u0644\u064A\u0629\u060C \u0648\u062A\u062A\u0636\u0645\u0646 \u0645\u062C\u0645\u0648\u0639\u0629 \u0643\u0628\u064A\u0631\u0629 \u0645\u0646 \u0627\u0644\u0639\u0645\u0644\u064A\u0627\u062A \u0627\u0644\u062C\u064A\u0648\u0644\u0648\u062C\u064A\u0629 \u0627\u0644\u062A\u064A \u062A\u0633\u0645\u0649 \u0639\u0645\u0648\u0645\u064B\u0627 \u062A\u0643\u0648\u0651\u0646 \u0627\u0644\u062C\u0628\u0627\u0644."@ar . . . . "Orogeneza (gr. \u1F44\u03C1\u03BF\u03C2\u2009 \u2013 \u201Eg\u00F3ra\u201D i \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2\u2009 \u2013 \u201Etworzenie, pocz\u0105tek\u201D) \u2013 ruchy orogeniczne, g\u00F3rotw\u00F3rczo\u015B\u0107, ruchy g\u00F3rotw\u00F3rcze, fa\u0142dowanie. 1. Powstanie g\u00F3r wskutek ruch\u00F3w tektonicznych. 2. Intensywne, kr\u00F3tkotrwa\u0142e i nieodwracalne ruchy skorupy ziemskiej obejmuj\u0105ce do\u015B\u0107 ograniczone obszary. Zwykle orogenezie towarzyszy plutonizm. Jest to definicja klasyczna. 3. Epoka g\u00F3rotw\u00F3rcza."@pl . . . . "Orogeneza (gr. \u1F44\u03C1\u03BF\u03C2\u2009 \u2013 \u201Eg\u00F3ra\u201D i \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2\u2009 \u2013 \u201Etworzenie, pocz\u0105tek\u201D) \u2013 ruchy orogeniczne, g\u00F3rotw\u00F3rczo\u015B\u0107, ruchy g\u00F3rotw\u00F3rcze, fa\u0142dowanie. 1. Powstanie g\u00F3r wskutek ruch\u00F3w tektonicznych. 2. Intensywne, kr\u00F3tkotrwa\u0142e i nieodwracalne ruchy skorupy ziemskiej obejmuj\u0105ce do\u015B\u0107 ograniczone obszary. Zwykle orogenezie towarzyszy plutonizm. Jest to definicja klasyczna. 3. Epoka g\u00F3rotw\u00F3rcza. Wsp\u00F3\u0142cze\u015Bnie uwa\u017Ca si\u0119, \u017Ce powstawanie g\u00F3r zachodzi na granicach p\u0142yt tektonicznych, gdy w strefie kontaktu napr\u0119\u017Cenia prowadz\u0105 do wyniesienia jednych blok\u00F3w skalnych ponad inne (jako fa\u0142dy lub uskoki), lub gdy zachodz\u0105 intensywne \u2013 powstaj\u0105ce wtedy g\u00F3ry maj\u0105 charakter wulkaniczny. Przez lata przyjmowano, \u017Ce prekursorem \u0142a\u0144cucha g\u00F3rskiego jest geosynklina, czyli zag\u0142\u0119bienie terenu gromadz\u0105ce osady, kt\u00F3re zostaj\u0105 nast\u0119pnie \u015Bci\u015Bni\u0119te i wypi\u0119trzone. Dzi\u015B odchodzi si\u0119 od tego prostego obrazu w kierunku z\u0142o\u017Conej klasyfikacji mo\u017Cliwych warunk\u00F3w orogenez, w\u015Br\u00F3d kt\u00F3rych tylko niekt\u00F3re pasuj\u0105 do za\u0142o\u017Ce\u0144 dawnej teorii geosynkliny. Niekt\u00F3re istotne aspekty zwi\u0105zane ze wsp\u00F3\u0142czesnymi wynikami geologii poruszone s\u0105 r\u00F3wnie\u017C w artyku\u0142ach: geosynklina, terran."@pl . . . . . . . "Orogeneze, voln\u011B p\u0159elo\u017Eena do \u010De\u0161tiny jako horotvorba \u010Di horotvo\u0159en\u00ED (z \u0159eck\u00E9ho oros \u201Ehora\u201C a genesis \u201Evznik\u201C), spr\u00E1vn\u011Bji a v u\u017E\u0161\u00EDm smyslu tektogeneze je pom\u011Brn\u011B rychl\u00FD geologick\u00FD proces, p\u0159i kter\u00E9m v\u011Bt\u0161inou vlivem proces\u016F deskov\u00E9 tektoniky vznikaj\u00ED p\u00E1semn\u00E1 poho\u0159\u00ED (naz\u00FDvan\u00E1 t\u00E9\u017E orogenn\u00ED p\u00E1sma). Zahrnuje v sob\u011B jednak tektonick\u00E9 procesy, vnitrodeskov\u00E9 zkr\u00E1cen\u00ED, zes\u00EDlen\u00ED k\u016Fry, jako\u017E i v\u00FDzdvih poho\u0159\u00ED. Orogeneze v\u017Edy souvis\u00ED s deskovou tektonikou. Jedn\u00E1 se o proces, kter\u00FD je dlouhodob\u00FD a kter\u00FD trv\u00E1 mili\u00F3ny a\u017E des\u00EDtky mili\u00F3n\u016F let. Horskou soustavu vzniklou orogenez\u00ED naz\u00FDv\u00E1me orog\u00E9n. N\u011Bkdy je orogeneze zam\u011B\u0148ov\u00E1na s term\u00EDnem vr\u00E1sn\u011Bn\u00ED, co\u017E v\u0161ak je jen jeden z proces\u016F, kter\u00E9 orogenezi doprov\u00E1zej\u00ED. Term\u00EDn orogeneze by m\u011Bl b\u00FDt spjat hlavn\u011B se st\u00E1diem vzniku pozitivn\u00EDho georeli\u00E9fu, tedy se z\u00E1v\u011Bre\u010Dn\u00FDm st\u00E1diem vzniku poho\u0159\u00ED, zat\u00EDmco tektogeneze by m\u011Bla zahrnovat \u0161ir\u0161\u00ED r\u00E1mec d\u011Bj\u016F, kter\u00E9 j\u00ED p\u0159edch\u00E1zely. V sou\u010Dasnosti v\u0161ak p\u0159evl\u00E1d\u00E1 pou\u017Eit\u00ED term\u00EDnu orogeneze pro cel\u00FD proces vzniku poho\u0159\u00ED. Orogeneze se v\u011Bt\u0161inou d\u011Bl\u00ED na \u0159adu d\u00EDl\u010D\u00EDch maxim neboli f\u00E1z\u00ED. V pr\u016Fb\u011Bhu orogeneze doch\u00E1z\u00ED ke vzniku charakteristick\u00FDch geologick\u00FDch \u00FAtvar\u016F v podob\u011B fly\u0161e a molasy. Orogeneze je spojena s pohybem tektonick\u00FDch desek a s jejich vz\u00E1jemn\u00FDmi kolizemi. P\u0159i orogenezi doch\u00E1z\u00ED k tomu, \u017Ee se dv\u011B litosf\u00E9rick\u00E9 desky sraz\u00ED a jedna se za\u010Dne podsouvat pod druhou . B\u011Bhem procesu doch\u00E1z\u00ED vlivem ohromn\u00FDch tlak\u016F a teplot ke vr\u00E1sn\u011Bn\u00ED a , kter\u00E9 m\u00E1 za n\u00E1sledek vyzdvihov\u00E1n\u00ED oblast\u00ED, kter\u00E9 se st\u00E1vaj\u00ED poho\u0159\u00EDmi. V historii rozezn\u00E1v\u00E1me 4 z\u00E1kladn\u00ED orogenetick\u00E9 jednotky: \n* kadomsk\u00E9 (assynthsk\u00E9) vr\u00E1sn\u011Bn\u00ED \n* kaledonsk\u00E9 vr\u00E1sn\u011Bn\u00ED \n* hercynsk\u00E9 (varisk\u00E9) vr\u00E1sn\u011Bn\u00ED \n* alpinsk\u00E9 vr\u00E1sn\u011Bn\u00ED (n\u011Bkdy zvan\u00E9 alpsko-him\u00E1lajsk\u00E9)Kolize dvou kontinent\u00E1ln\u00EDch desek a vznik p\u00E1semn\u00E9ho poho\u0159\u00ED Jde o ozna\u010Den\u00ED cel\u00FDch geologick\u00FDch epoch, ve kter\u00FDch doch\u00E1zelo na r\u016Fzn\u00FDch m\u00EDstech planety k jednotliv\u00FDm horotvorn\u00FDm pohyb\u016Fm. V u\u017E\u0161\u00EDm smyslu se uveden\u00E9 n\u00E1zvy vztahuj\u00ED na konkr\u00E9tn\u00ED orogenezi v r\u00E1mci dan\u00E9 epochy. Nap\u0159\u00EDklad hercynsk\u00E9 vr\u00E1sn\u011Bn\u00ED v u\u017E\u0161\u00EDm smyslu ozna\u010Duje vznik hercynsk\u00FDch poho\u0159\u00ED p\u0159i sr\u00E1\u017Ece Eurameriky a Gondwany, ale v \u0161ir\u0161\u00EDm smyslu jsou hercynsk\u00E9ho st\u00E1\u0159\u00ED i mnoh\u00E1 dal\u0161\u00ED horstva (hercynidy) vznikl\u00E1 jin\u00FDmi sr\u00E1\u017Ekami ve stejn\u00E9 epo\u0161e, t\u0159eba Ural nebo \u0164an-\u0161an. P\u0159\u00EDkladem dal\u0161\u00ED orogeneze je nap\u0159\u00EDklad Grenvillsk\u00E9 vr\u00E1sn\u011Bn\u00ED. Orogenn\u00ED p\u00E1sma jsou obvykle dlouh\u00E1 p\u00E1sma v\u00FDrazn\u011B deformovan\u00FDch hornin, kter\u00E9 jsou b\u011B\u017En\u011B zvr\u00E1sn\u011Bn\u00E9 a rozt\u0159\u00ED\u0161t\u011Bn\u00E9 zlomy. Tyto zlomy rozd\u011Bluj\u00ED horniny na soustavu mal\u00FDch desek (nezam\u011B\u0148ovat s tektonick\u00FDmi deskami). Desky jsou naskl\u00E1d\u00E1ny v r\u00E1mci p\u00E1sma jedna vedle druh\u00E9. V\u00FD\u0161ka vytvo\u0159en\u00FDch \u0161t\u00EDt\u016F koresponduje s hloubkou pono\u0159en\u00ED jejich z\u00E1kladny. \u010C\u00EDm je dan\u00E9 poho\u0159\u00ED v\u00FD\u0161e, t\u00EDm v\u00EDce kles\u00E1 i masa hornin, nach\u00E1zej\u00EDc\u00ED se pod nimi (nap\u0159. poho\u0159\u00ED Him\u00E1laj je pono\u0159eno a\u017E do hloubky 130 kilometr\u016F). Proces tvorby orogenn\u00EDho p\u00E1sma trv\u00E1 i miliony let. Nast\u00E1v\u00E1 bu\u010F p\u0159i sr\u00E1\u017Ece dvou kontinent\u00E1ln\u00EDch desek, p\u0159i\u010Dem\u017E horniny jsou kolizn\u011B deformov\u00E1ny a \u010Dasto podrobeny metamorf\u00F3ze nebo se vyskytuje na styku kontinent\u00E1ln\u00ED a oce\u00E1nsk\u00E9 desky, kdy v\u0161ak nedoch\u00E1z\u00ED ke kolizi (Andy). Term\u00EDn orogeneze zavedl Cleveland Abbe mlad\u0161\u00ED v roce 1889. Pojem orog\u00E9n byl zaveden d\u0159\u00EDve."@cs . . . . . . . . . . . . . . . "L'orogenesi (dal greco antico \u1F44\u03C1\u03BF\u03C2, \u00ABrilievo, montagna\u00BB e \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2, \u00ABorigine, causa produttiva\u00BB) indica in geologia il processo di formazione di un rilievo montuoso. Nel linguaggio geologico, il termine si riferisce alla formazione degli orogeni, derivanti da masse rocciose che hanno subito una deformazione tettonica, per prevalenza di spinte laterali, arrivando ad impilarsi creando una catena montuosa."@it . . . . . . . "\u9020\u5C71\u904B\u52D5"@zh . . . "Orogenesi"@it . . "Se denomina orog\u00E9nesis u orogenia al proceso geol\u00F3gico por el cual una zona alargada de la corteza terrestre se acorta y engrosa por deformaci\u00F3n y fracturaci\u00F3n como consecuencia de esfuerzos tect\u00F3nicos laterales.\u200B Normalmente las orogenias son acompa\u00F1adas por la formaci\u00F3n de cabalgamientos y plegamientos.\u200B La palabra orog\u00E9nesis proviene del idioma griego (oros significa \"monta\u00F1a\" y g\u00E9nesis significa \"creaci\u00F3n\" u \"origen\"),\u200B y es el mecanismo principal mediante el cual las cordilleras se forman en los continentes. Los or\u00F3genos o cordilleras se crean cuando una placa tect\u00F3nica con corteza continental es \"arrugada\" y fracturada y los fragmentos se apilan, aumentando el grosor original de la corteza. Adem\u00E1s tambi\u00E9n suelen producirse procesos de magmatismo, que aportan nuevos materiales gran\u00EDti"@es . . . . . "Gebergtevorming alias orogenese is een gevolg van de platentektoniek, de bewegingen van platen langs elkaar (zijschuivingsbewegingen), over en onder elkaar (compressieve bewegingen) en uit elkaar (extensionele bewegingen). Bij al deze bewegingen kan een gebergte gevormd worden, hoewel dit doorgaans het gevolg is van compressieve bewegingen."@nl . . "Orogeny is the primary mechanism by which mountains are formed on continents. An orogeny is an event that takes place at a convergent plate margin when plate motion compresses the margin. An orogenic belt or orogen develops as the compressed plate crumples and is uplifted to form one or more mountain ranges. This involves a series of geological processes collectively called orogenesis. These include both structural deformation of existing continental crust and the creation of new continental crust through volcanism. Magma rising in the orogen carries less dense material upwards while leaving more dense material behind, resulting in compositional differentiation of Earth's lithosphere (crust and uppermost mantle). A synorogenic process or event is one that occurs during an orogeny. The word \"orogeny\" (/\u0252\u02C8r\u0252d\u0292\u0259ni/) comes from Ancient Greek (\u1F44\u03C1\u03BF\u03C2, \u00F3ros, lit.\u2009''mountain'' + \u03B3\u03AD\u03BD\u03B5\u03C3\u03B9\u03C2, g\u00E9nesis, lit.\u2009''creation, origin''). Although it was used before him, the term was employed by the American geologist G. K. Gilbert in 1890 to describe the process of mountain-building as distinguished from epeirogeny."@en . . .