"Seismisches Moment"@de . . . . . "Momentu sismikoa sismologian lurrikarak neurtzeko erabiltzen den kantitate bat da. Momentu sismiko eskalarra honako ekuazioarekin definitzen da: , non \n* lurrikaran mugitu diren arroken ebakidura modulua da (dina / cm2) \n* failaren haustura azalera da lurrikara gertatu denean (cm2-tan) \n* n eman den batez besteko desplazamendua da (cm-tan). Lurrikara baten momentu sismikoa faktore horiek kontuan hartzen estimatzen da, nahiz eta beti ez diren datu zuzenak lortzen. Gaur egungo lurrikaratan sismogramak erabilita egiten da lan hori, lurraren mugimendua bera aztertuz. Antzinako lurrikaren balorazioak egiteko failaren haustura eta mugimenduaren arabera egiten da. asmatutako momentu magnitude eskala printzipio honetan oinarritzen da eta lurrikara handien arteko alderaketa egiteko erabiltzen da."@eu . "Seismisch moment"@nl . . . . "Il momento sismico \u00E8 utilizzato dai sismologi per misurare la quantit\u00E0 di energia rilasciata da un terremoto. Si misura nel sistema internazionale in Nm ed \u00E8 definito dall'equazione dove: \n* \u00E8 il modulo di taglio delle rocce coinvolte, di solito 30 GPa \n* \u00E8 l'area di rottura lungo la faglia dove \u00E8 avvenuto il terremoto (in m\u00B2) \n* \u00E8 lo spostamento medio lungo la faglia (in m) Il momento sismico pu\u00F2 essere stimato in molti modi. Oggi si \u00E8 soliti stimarlo dai sismogrammi. Nelle epoche precedenti allo sviluppo di stazioni sismiche era possibile stimarlo dalla geologia del territorio, per mezzo di misure delle dimensioni di rottura di faglia e dello spostamento. Il momento sismico \u00E8 la base per la Scala magnitudo momento, introdotta da Hiroo Kanamori, spesso usata per confrontare la grandezza di terremoti diversi, soprattutto quelli di grandi dimensioni."@it . "\u03A3\u03B5\u03B9\u03C3\u03BC\u03B9\u03BA\u03AE \u03C1\u03BF\u03C0\u03AE"@el . . . . . "Seismic moment"@en . "Seismic moment is a quantity used by seismologists to measure the size of an earthquake. The scalar seismic moment is defined by the equation, where \n* is the shear modulus of the rocks involved in the earthquake (in pascals (Pa), i.e. newtons per square meter) \n* is the area of the rupture along the geologic fault where the earthquake occurred (in square meters), and \n* is the average slip (displacement offset between the two sides of the fault) on (in meters)."@en . "Il momento sismico \u00E8 utilizzato dai sismologi per misurare la quantit\u00E0 di energia rilasciata da un terremoto. Si misura nel sistema internazionale in Nm ed \u00E8 definito dall'equazione dove: \n* \u00E8 il modulo di taglio delle rocce coinvolte, di solito 30 GPa \n* \u00E8 l'area di rottura lungo la faglia dove \u00E8 avvenuto il terremoto (in m\u00B2) \n* \u00E8 lo spostamento medio lungo la faglia (in m) Il momento sismico \u00E8 la base per la Scala magnitudo momento, introdotta da Hiroo Kanamori, spesso usata per confrontare la grandezza di terremoti diversi, soprattutto quelli di grandi dimensioni."@it . "Momentu sismiko"@eu . "Het seismisch moment is een eenheid die seismologen gebruiken om de grootte van een aardbeving mee aan te geven. Het seismisch moment (MO) wordt bepaald door de vergelijking M0 = \u03BCAu, waarbij: \n* \u03BC is de schuifmodulus van het gesteente, meestal ongeveer 30 GPa; \n* A is de oppervlakte van de breukvlak waarlangs het verzet plaatsvond; \n* u is de grootte van de gemiddelde verplaatsingsvector over dit oppervlakte. Het seismisch moment van een aardbeving wordt bepaald aan de hand van de beschikbare informatie waarmee de factoren ingeschat kunnen worden. Tegenwoordig wordt het seismisch moment meestal ingeschat vanuit informatie in seismogrammen.Het seismisch moment van historische aardbevingen wordt bepaald door schattingen van het oppervlak van het breukvlak en de verplaatsing die erlangs heeft plaatsgevonden. Het seismisch moment vormt de basis van de momentmagnitudeschaal van de Japanse seismoloog . Ze wordt vooral gebruikt om grote aardbevingen met elkaar te vergelijken."@nl . . . "\u0397 \u03C3\u03B5\u03B9\u03C3\u03BC\u03B9\u03BA\u03AE \u03C1\u03BF\u03C0\u03AE \u03B5\u03AF\u03BD\u03B1\u03B9 \u03BC\u03B9\u03B1 \u03C0\u03BF\u03C3\u03CC\u03C4\u03B7\u03C4\u03B1 \u03C0\u03BF\u03C5 \u03C7\u03C1\u03B7\u03C3\u03B9\u03BC\u03BF\u03C0\u03BF\u03B9\u03B5\u03AF\u03C4\u03B1\u03B9 \u03B1\u03C0\u03CC \u03C4\u03BF\u03C5\u03C2 \u03C3\u03B5\u03B9\u03C3\u03BC\u03BF\u03BB\u03CC\u03B3\u03BF\u03C5\u03C2 \u03B3\u03B9\u03B1 \u03C4\u03B7 \u03BC\u03AD\u03C4\u03C1\u03B7\u03C3\u03B7 \u03C4\u03BF\u03C5 \u03BC\u03B5\u03B3\u03AD\u03B8\u03BF\u03C5\u03C2 \u03B5\u03BD\u03CC\u03C2 \u03C3\u03B5\u03B9\u03C3\u03BC\u03BF\u03CD. \u0397 \u03C3\u03B5\u03B9\u03C3\u03BC\u03B9\u03BA\u03AE \u03C1\u03BF\u03C0\u03AE \u03B5\u03BD\u03CC\u03C2 \u03C3\u03B5\u03B9\u03C3\u03BC\u03BF\u03CD \u03B5\u03BA\u03C4\u03B9\u03BC\u03AC\u03C4\u03B1\u03B9 \u03C3\u03C5\u03BD\u03AE\u03B8\u03C9\u03C2 \u03BC\u03B5 \u03C4\u03B7 \u03C7\u03C1\u03AE\u03C3\u03B7 \u03C4\u03B7\u03C2 \u03CC\u03C0\u03BF\u03B9\u03B1\u03C2 \u03B4\u03B9\u03B1\u03B8\u03AD\u03C3\u03B9\u03BC\u03B7\u03C2 \u03C0\u03BB\u03B7\u03C1\u03BF\u03C6\u03BF\u03C1\u03AF\u03B1\u03C2 \u03C0\u03BF\u03C5 \u03BC\u03C0\u03BF\u03C1\u03B5\u03AF \u03BD\u03B1 \u03BF\u03C1\u03AF\u03C3\u03B5\u03B9 \u03C4\u03BF \u03BC\u03AD\u03B3\u03B5\u03B8\u03CC\u03C2 \u03BA\u03B1\u03B9 \u03C4\u03B1 \u03C3\u03C4\u03BF\u03B9\u03C7\u03B5\u03AF\u03B1 \u03C4\u03BF\u03C5. \u0393\u03B9\u03B1 \u03C3\u03CD\u03B3\u03C7\u03C1\u03BF\u03BD\u03BF\u03C2 \u03C3\u03B5\u03B9\u03C3\u03BC\u03BF\u03CD\u03C2, \u03B7 \u03C1\u03BF\u03C0\u03AE \u03C3\u03C5\u03BD\u03AE\u03B8\u03C9\u03C2 \u03BC\u03B5\u03C4\u03C1\u03B9\u03AD\u03C4\u03B1\u03B9 \u03BC\u03B5 \u03C3\u03B5\u03B9\u03C3\u03BC\u03CC\u03B3\u03C1\u03B1\u03BC\u03BC\u03B1. \u0393\u03B9\u03B1 \u03C3\u03B5\u03B9\u03C3\u03BC\u03BF\u03CD\u03C2 \u03C0\u03BF\u03C5 \u03AD\u03BB\u03B1\u03B2\u03B1\u03BD \u03C7\u03CE\u03C1\u03B1 \u03C3\u03B5 \u03BC\u03B9\u03B1 \u03C0\u03B1\u03BB\u03B1\u03B9\u03CC\u03C4\u03B5\u03C1\u03B7 \u03B5\u03C0\u03BF\u03C7\u03AE, \u03B7 \u03C1\u03BF\u03C0\u03AE \u03B5\u03BA\u03C4\u03B9\u03BC\u03AC\u03C4\u03B1\u03B9 \u03BC\u03B5 \u03B3\u03B5\u03C9\u03BB\u03BF\u03B3\u03B9\u03BA\u03AD\u03C2 \u03B5\u03BA\u03C4\u03B9\u03BC\u03AE\u03C3\u03B5\u03B9\u03C2."@el . . "Seismic moment is a quantity used by seismologists to measure the size of an earthquake. The scalar seismic moment is defined by the equation, where \n* is the shear modulus of the rocks involved in the earthquake (in pascals (Pa), i.e. newtons per square meter) \n* is the area of the rupture along the geologic fault where the earthquake occurred (in square meters), and \n* is the average slip (displacement offset between the two sides of the fault) on (in meters). thus has dimensions of torque, measured in newton meters. The connection between seismic moment and a torque is natural in the body-force equivalent representation of seismic sources as a double-couple (a pair of force couples with opposite torques): the seismic moment is the torque of each of the two couples. Despite having the same dimensions as energy, seismic moment is not a measure of energy. The relations between seismic moment, potential energy drop and radiated energy are indirect and approximative. The seismic moment of an earthquake is typically estimated using whatever information is available to constrain its factors. For modern earthquakes, moment is usually estimated from ground motion recordings of earthquakes known as seismograms. For earthquakes that occurred in times before modern instruments were available, moment may be estimated from geologic estimates of the size of the fault rupture and the slip. Seismic moment is the basis of the moment magnitude scale introduced by Hiroo Kanamori, which is often used to compare the size of different earthquakes and is especially useful for comparing the sizes of large (great) earthquakes. The seismic moment is not restricted to earthquakes. For a more general seismic source described by a seismic moment tensor (a symmetric tensor, but not necessarily a double couple tensor), the seismic moment is"@en . . . "1117444880"^^ . "Momentu sismikoa sismologian lurrikarak neurtzeko erabiltzen den kantitate bat da. Momentu sismiko eskalarra honako ekuazioarekin definitzen da: , non \n* lurrikaran mugitu diren arroken ebakidura modulua da (dina / cm2) \n* failaren haustura azalera da lurrikara gertatu denean (cm2-tan) \n* n eman den batez besteko desplazamendua da (cm-tan). asmatutako momentu magnitude eskala printzipio honetan oinarritzen da eta lurrikara handien arteko alderaketa egiteko erabiltzen da."@eu . "\uC9C0\uC9C4 \uBAA8\uBA58\uD2B8"@ko . "Das seismische Moment ist \u2013 wie die seismische Energie oder die Magnitude \u2013 ein Ma\u00DF f\u00FCr die St\u00E4rke eines Erdbebens. Es berechnet sich aus , wobei \n* das Schermodul des Gesteins entlang der Bruchfl\u00E4che (normalerweise 30 Gigapascal) \n* die Bruchfl\u00E4che \n* die durchschnittliche Verschiebung entlang der Bruchfl\u00E4che A ist. F\u00FCr historische Erdbeben kann das seismische Moment aus geologischen Sch\u00E4tzungen der Bruchfl\u00E4che und der Verschiebung berechnet werden, f\u00FCr heutige Erdbeben werden innerhalb kurzer Zeit Sch\u00E4tzwerte aus den Seismogrammen berechnet. Das seismische Moment ist die Grundlage der Momenten-Magnituden-Skala, des heute in der Seismologie \u00FCblichen Ma\u00DFes f\u00FCr die St\u00E4rke eines Erdbebens."@de . . . "\u5730\u9707\u77E9"@zh . . "3727"^^ . . . "\u5730\u9707\u30E2\u30FC\u30E1\u30F3\u30C8"@ja . . . "Le moment sismique est une mesure de la force d'un s\u00E9isme. Depuis les ann\u00E9es 1960, les sismologues pr\u00E9f\u00E8rent cette mesure \u00E0 la magnitude sismique car le moment sismique est directement li\u00E9 aux param\u00E8tres de la source sismique. Ce concept est introduit par Vvedenskaya en 1956 et repris ensuite par Keiiti Aki. Puisqu'un tremblement de terre observ\u00E9 \u00E0 grande distance (l\u00E0 o\u00F9 le s\u00E9isme peut \u00EAtre assimil\u00E9 \u00E0 un point dans l'espace) a une \u00E9mission d'\u00E9nergie comparable \u00E0 celui d'un double couple de forces, sa grandeur peut \u00EAtre d\u00E9finie par un moment, souvent not\u00E9 . Ce moment est reli\u00E9 \u00E0 la source par la relation : o\u00F9 est le module de rigidit\u00E9 du milieu, est la surface rompue durant le s\u00E9isme et est le d\u00E9placement moyen ayant eu lieu sur la faille. L'unit\u00E9 de mesure est donc le newton m\u00E8tre (N m) dans le Syst\u00E8me international. Souvent, principalement dans les pays anglophones, cette mesure est donn\u00E9e en dyne centim\u00E8tre (dyn cm) (1 N m = 107 dyn cm).En 1977, Hiroo Kanamori \u00E9tablit la relation empirique entre magnitude (sans dimension, la lettre W correspondant au travail d'une force, Work en anglais) et moment sismique (exprim\u00E9 en N m) : Lorsque la magnitude du s\u00E9isme est d\u00E9duite du moment, on parle de magnitude de moment."@fr . . . . "\u5730\u9707\u30E2\u30FC\u30E1\u30F3\u30C8\uFF08\u3058\u3057\u3093\u30E2\u30FC\u30E1\u30F3\u30C8\uFF09\u3068\u306F\u3001\u5730\u9707\u306E\u5927\u304D\u3055\u3092\u793A\u3059\u6307\u6A19\u306E\u3072\u3068\u3064\u3067\u3001\u65AD\u5C64\u904B\u52D5\u306E\u529B\u306E\u30E2\u30FC\u30E1\u30F3\u30C8\uFF08\u30A8\u30CD\u30EB\u30AE\u30FC\uFF09\u306E\u5927\u304D\u3055\u3092\u8868\u3059\u3002 \u65AD\u5C64\u9762\u306E\u525B\u6027\u7387\u3092\uFF08Pa\uFF09\u3001\u65AD\u5C64\u9762\u7A4D\u306E\u5408\u8A08\u3092\uFF08m2\uFF09\u3001\u65AD\u5C64\u5168\u4F53\u3067\u306E\u5909\u4F4D\uFF08\u3059\u3079\u308A\uFF09\u91CF\u306E\u5E73\u5747\u3092\uFF08m\uFF09\u3068\u3057\u305F\u3068\u304D\u3001\u5730\u9707\u30E2\u30FC\u30E1\u30F3\u30C8\u306F\u3001 \u3068\u8868\u3055\u308C\u308B\u3002\u5358\u4F4D\u306F\u30CB\u30E5\u30FC\u30C8\u30F3\u30E1\u30FC\u30C8\u30EB\uFF08N\u30FBm\uFF09\u3067\u3042\u308B\u3002"@ja . "Momento s\u00EDsmico \u00E9 uma quantidade usada pelos sism\u00F3logos para medir a magnitude de um terremoto. O momento s\u00EDsmico escalar \u00E9 definido pela equa\u00E7\u00E3o , onde \n* \u00E9 o m\u00F3dulo de cisalhamento das rochas envolvidas no terremoto, geralmente 30 gigapascals \n* \u00E9 a \u00E1rea de ruptura ao longo da falha geol\u00F3gica onde ocorre o terremoto e \n* \u00E9 o deslocamento m\u00E9dio em . Para os terremotos modernos, o momento s\u00EDsmico \u00E9 usualmente estimado a partir dos registros de movimento da superf\u00EDcie, conhecidos como sismogramas. Para terremotos que ocorreram no passado, quando n\u00E3o havia o instrumental necess\u00E1rio, utilizam-se estimativas geol\u00F3gicas do tamanho da ruptura da falha e do seu deslocamento. O momento s\u00EDsmico \u00E9 a base da escala de magnitude de momento, introduzida por Hiroo Kanamori, a qual \u00E9 atualmente usada para comparar a magnitude de diferentes terremotos - especialmente para comparar os grandes terremotos."@pt . . "Momento s\u00EDsmico"@pt . . . "\uC9C0\uC9C4 \uBAA8\uBA58\uD2B8(Seismic moment)\uB294 \uC9C0\uC9C4\uD559\uC5D0\uC11C \uC9C0\uC9C4\uC758 \uD06C\uAE30\uB97C \uCE21\uC815\uD558\uB294 \uB370 \uC4F0\uC774\uB294 \uC9C0\uD45C\uC774\uB2E4. \uC2A4\uCE7C\uB77C \uC9C0\uC9C4 \uBAA8\uBA58\uD2B8 \uC740 \uB2E4\uC74C\uACFC \uAC19\uC774 \uC815\uC758\uB41C\uB2E4. \uC5EC\uAE30\uC11C, \n* \uC740 \uC9C0\uC9C4\uC774 \uC77C\uC5B4\uB09C \uC9C0\uC5ED \uC554\uC11D\uC758 \uC804\uB2E8 \uD0C4\uC131 \uACC4\uC218(Pa \uB610\uB294 N/m2) \n* \uB294 \uC9C0\uC9C4\uC774 \uBC1C\uC0DD\uD55C \uC9C0\uC5ED\uC5D0\uC11C \uB2E8\uCE35\uC774 \uD30C\uAD34\uB41C \uC601\uC5ED \uD06C\uAE30(m2) \n* \uB294 \uC601\uC5ED\uC5D0\uC11C \uD3C9\uADE0 \uBBF8\uB044\uB7EC\uC9D0 \uD06C\uAE30(in m) \uC740 \uB274\uD134 \uBBF8\uD130 \uB2E8\uC704\uC758 \uB3CC\uB9BC\uD798\uC73C\uB85C\uB3C4 \uB098\uD0C0\uB0BC \uC218 \uC788\uB2E4. \uC9C0\uC9C4 \uBAA8\uBA58\uD2B8\uC640 \uD1A0\uD06C \uC0AC\uC774 \uAD00\uACC4\uB294 \uC9C0\uC9C4\uC758 \uADFC\uC6D0\uC5D0\uC11C \uB098\uC624\uB294 \uCCB4\uC801\uB825\uACFC \uC774\uC911 \uACB0\uD569 \uAD00\uACC4(\uC11C\uB85C \uBC18\uB300\uB418\uB294 \uD1A0\uD06C\uAC00 \uC11C\uB85C \uD569\uCCD0\uC838 \uC791\uC6A9\uD558\uB294 \uACB0\uD569\uD798)\uB85C \uC5F0\uAD00\uB418\uBA70, \uC9C0\uC9C4 \uBAA8\uBA58\uD2B8\uB294 \uB450 \uADFC\uC6D0\uC5D0\uC11C \uB098\uC624\uB294 \uD1A0\uD06C\uC758 \uACB0\uD569\uC774\uB77C\uACE0 \uB9D0\uD560 \uC218 \uC788\uB2E4. \uC9C0\uC9C4 \uBAA8\uBA58\uD2B8\uB294 \uAD6D\uC81C\uB2E8\uC704\uACC4(SI \uB2E8\uC704\uACC4)\uC5D0\uC11C \uB274\uD134 \uBBF8\uD130(N m \uB610\uB294 N\u00B7m)\uB85C \uD45C\uAE30\uD558\uBA70 \uAD6C\uD615 CGS \uB2E8\uC704\uACC4\uC5D0\uC11C\uB294 \uB2E4\uC778 \uC13C\uCE58\uBBF8\uD130(dyn-cm)\uB85C \uD45C\uAE30\uD55C\uB2E4. \uC9C0\uC9C4 \uBAA8\uBA58\uD2B8\uB294 \uAC00\uC7A5 \uAC04\uB2E8\uD558\uAC8C\uB294 \uBBF8\uB044\uB7EC\uC9C4 \uC591\uACFC \uD30C\uC5F4\uB41C \uD639\uC740 \uBBF8\uB044\uB7EC\uC9C4 \uB2E8\uCE35 \uBA74\uC801, \uC800\uD56D \uB610\uB294 \uB9C8\uCC30 \uACC4\uC218 \uC14B\uB9CC \uAC00\uC9C0\uACE0 \uACC4\uC0B0\uD560 \uC218 \uC788\uB2E4. \uC774\uB7F0 \uBBF8\uC9C0\uC218\uB4E4\uC740 \uACFC\uAC70 \uC9C0\uC9C4 \uADDC\uBAA8\uB098 \uBBF8\uB798\uC5D0 \uC62C \uAC83\uC73C\uB85C \uC608\uC0C1\uB418\uB294 \uC9C0\uC9C4\uC758 \uADDC\uBAA8\uB97C \uAE30\uC874\uC758 \uB2E8\uCE35 \uC5F0\uAD6C\uB97C \uD1B5\uD574 \uCD94\uC815\uD560 \uC218 \uC788\uB2E4\uB294 \uC7A5\uC810\uC774 \uC788\uB2E4."@ko . . . . "Het seismisch moment is een eenheid die seismologen gebruiken om de grootte van een aardbeving mee aan te geven. Het seismisch moment (MO) wordt bepaald door de vergelijking M0 = \u03BCAu, waarbij: \n* \u03BC is de schuifmodulus van het gesteente, meestal ongeveer 30 GPa; \n* A is de oppervlakte van de breukvlak waarlangs het verzet plaatsvond; \n* u is de grootte van de gemiddelde verplaatsingsvector over dit oppervlakte. Het seismisch moment vormt de basis van de momentmagnitudeschaal van de Japanse seismoloog . Ze wordt vooral gebruikt om grote aardbevingen met elkaar te vergelijken."@nl . "631443"^^ . . "Le moment sismique est une mesure de la force d'un s\u00E9isme. Depuis les ann\u00E9es 1960, les sismologues pr\u00E9f\u00E8rent cette mesure \u00E0 la magnitude sismique car le moment sismique est directement li\u00E9 aux param\u00E8tres de la source sismique. Ce concept est introduit par Vvedenskaya en 1956 et repris ensuite par Keiiti Aki. Puisqu'un tremblement de terre observ\u00E9 \u00E0 grande distance (l\u00E0 o\u00F9 le s\u00E9isme peut \u00EAtre assimil\u00E9 \u00E0 un point dans l'espace) a une \u00E9mission d'\u00E9nergie comparable \u00E0 celui d'un double couple de forces, sa grandeur peut \u00EAtre d\u00E9finie par un moment, souvent not\u00E9 ."@fr . "\u0397 \u03C3\u03B5\u03B9\u03C3\u03BC\u03B9\u03BA\u03AE \u03C1\u03BF\u03C0\u03AE \u03B5\u03AF\u03BD\u03B1\u03B9 \u03BC\u03B9\u03B1 \u03C0\u03BF\u03C3\u03CC\u03C4\u03B7\u03C4\u03B1 \u03C0\u03BF\u03C5 \u03C7\u03C1\u03B7\u03C3\u03B9\u03BC\u03BF\u03C0\u03BF\u03B9\u03B5\u03AF\u03C4\u03B1\u03B9 \u03B1\u03C0\u03CC \u03C4\u03BF\u03C5\u03C2 \u03C3\u03B5\u03B9\u03C3\u03BC\u03BF\u03BB\u03CC\u03B3\u03BF\u03C5\u03C2 \u03B3\u03B9\u03B1 \u03C4\u03B7 \u03BC\u03AD\u03C4\u03C1\u03B7\u03C3\u03B7 \u03C4\u03BF\u03C5 \u03BC\u03B5\u03B3\u03AD\u03B8\u03BF\u03C5\u03C2 \u03B5\u03BD\u03CC\u03C2 \u03C3\u03B5\u03B9\u03C3\u03BC\u03BF\u03CD. \u0397 \u03C3\u03B5\u03B9\u03C3\u03BC\u03B9\u03BA\u03AE \u03C1\u03BF\u03C0\u03AE \u03B5\u03BD\u03CC\u03C2 \u03C3\u03B5\u03B9\u03C3\u03BC\u03BF\u03CD \u03B5\u03BA\u03C4\u03B9\u03BC\u03AC\u03C4\u03B1\u03B9 \u03C3\u03C5\u03BD\u03AE\u03B8\u03C9\u03C2 \u03BC\u03B5 \u03C4\u03B7 \u03C7\u03C1\u03AE\u03C3\u03B7 \u03C4\u03B7\u03C2 \u03CC\u03C0\u03BF\u03B9\u03B1\u03C2 \u03B4\u03B9\u03B1\u03B8\u03AD\u03C3\u03B9\u03BC\u03B7\u03C2 \u03C0\u03BB\u03B7\u03C1\u03BF\u03C6\u03BF\u03C1\u03AF\u03B1\u03C2 \u03C0\u03BF\u03C5 \u03BC\u03C0\u03BF\u03C1\u03B5\u03AF \u03BD\u03B1 \u03BF\u03C1\u03AF\u03C3\u03B5\u03B9 \u03C4\u03BF \u03BC\u03AD\u03B3\u03B5\u03B8\u03CC\u03C2 \u03BA\u03B1\u03B9 \u03C4\u03B1 \u03C3\u03C4\u03BF\u03B9\u03C7\u03B5\u03AF\u03B1 \u03C4\u03BF\u03C5. \u0393\u03B9\u03B1 \u03C3\u03CD\u03B3\u03C7\u03C1\u03BF\u03BD\u03BF\u03C2 \u03C3\u03B5\u03B9\u03C3\u03BC\u03BF\u03CD\u03C2, \u03B7 \u03C1\u03BF\u03C0\u03AE \u03C3\u03C5\u03BD\u03AE\u03B8\u03C9\u03C2 \u03BC\u03B5\u03C4\u03C1\u03B9\u03AD\u03C4\u03B1\u03B9 \u03BC\u03B5 \u03C3\u03B5\u03B9\u03C3\u03BC\u03CC\u03B3\u03C1\u03B1\u03BC\u03BC\u03B1. \u0393\u03B9\u03B1 \u03C3\u03B5\u03B9\u03C3\u03BC\u03BF\u03CD\u03C2 \u03C0\u03BF\u03C5 \u03AD\u03BB\u03B1\u03B2\u03B1\u03BD \u03C7\u03CE\u03C1\u03B1 \u03C3\u03B5 \u03BC\u03B9\u03B1 \u03C0\u03B1\u03BB\u03B1\u03B9\u03CC\u03C4\u03B5\u03C1\u03B7 \u03B5\u03C0\u03BF\u03C7\u03AE, \u03B7 \u03C1\u03BF\u03C0\u03AE \u03B5\u03BA\u03C4\u03B9\u03BC\u03AC\u03C4\u03B1\u03B9 \u03BC\u03B5 \u03B3\u03B5\u03C9\u03BB\u03BF\u03B3\u03B9\u03BA\u03AD\u03C2 \u03B5\u03BA\u03C4\u03B9\u03BC\u03AE\u03C3\u03B5\u03B9\u03C2."@el . "\u5730\u9707\u77E9 \u662F\u5730\u9707\u5B78\u5BB6\u7528\u4F86\u8868\u793A\u5730\u9707\u6240\u91CB\u653E\u51FA\u4E4B\u80FD\u91CF\u7684\u6578\u91CF\uFF0C\u5B9A\u7FA9\u70BA: \uFF0C \u5176\u4E2D: \u70BA\u65B7\u5C64\u7269\u8CEA\u4E4B\u525B\u6027\u4FC2\u6578 (rigidity \u6216 shear modulus)\uFF0C\u4E00\u822C\u70BA 30x109 \u5E15\u65AF\u5361\u3002 \u70BA\u65B7\u5C64\u4E4B\u5E73\u5747\u6ED1\u52D5\u91CF (\u4F4D\u79FB)\u3002 \u70BA\u65B7\u5C64\u9762\u7A4D\u3002 \u5730\u9707\u77E9\u901A\u5E38\u6839\u64DA\u53EF\u7372\u53D6\u4E4B\u8CC7\u6599\u800C\u4F30\u7B97\u3002\u73FE\u4EE3\u5730\u9707\u53EF\u4F7F\u7528\u5730\u9707\u5100\u7684\u5730\u9707\u8A18\u9304\uFF0C\u53E4\u4EE3\u5730\u9707\u5247\u4F9D\u9760\u5730\u8CEA\u5B78\u7814\u7A76\u4F86\u63A8\u6E2C\u65B7\u5C64\u4E4B\u9762\u7A4D\u548C\u6ED1\u52D5\u91CF\u3002 \u5730\u9707\u77E9\u898F\u6A21\u662F\u5F9E\u5730\u9707\u77E9\u6F14\u7B97\u800C\u4F86\u7684\u5730\u9707\u898F\u6A21\u6A19\u5EA6\uFF0C\u73FE\u5728\u5E38\u7528\u4F86\u6BD4\u8F03\u5927\u578B\u5730\u9707\u7684\u5F37\u5EA6\u3002"@zh . "\u5730\u9707\u77E9 \u662F\u5730\u9707\u5B78\u5BB6\u7528\u4F86\u8868\u793A\u5730\u9707\u6240\u91CB\u653E\u51FA\u4E4B\u80FD\u91CF\u7684\u6578\u91CF\uFF0C\u5B9A\u7FA9\u70BA: \uFF0C \u5176\u4E2D: \u70BA\u65B7\u5C64\u7269\u8CEA\u4E4B\u525B\u6027\u4FC2\u6578 (rigidity \u6216 shear modulus)\uFF0C\u4E00\u822C\u70BA 30x109 \u5E15\u65AF\u5361\u3002 \u70BA\u65B7\u5C64\u4E4B\u5E73\u5747\u6ED1\u52D5\u91CF (\u4F4D\u79FB)\u3002 \u70BA\u65B7\u5C64\u9762\u7A4D\u3002 \u5730\u9707\u77E9\u901A\u5E38\u6839\u64DA\u53EF\u7372\u53D6\u4E4B\u8CC7\u6599\u800C\u4F30\u7B97\u3002\u73FE\u4EE3\u5730\u9707\u53EF\u4F7F\u7528\u5730\u9707\u5100\u7684\u5730\u9707\u8A18\u9304\uFF0C\u53E4\u4EE3\u5730\u9707\u5247\u4F9D\u9760\u5730\u8CEA\u5B78\u7814\u7A76\u4F86\u63A8\u6E2C\u65B7\u5C64\u4E4B\u9762\u7A4D\u548C\u6ED1\u52D5\u91CF\u3002 \u5730\u9707\u77E9\u898F\u6A21\u662F\u5F9E\u5730\u9707\u77E9\u6F14\u7B97\u800C\u4F86\u7684\u5730\u9707\u898F\u6A21\u6A19\u5EA6\uFF0C\u73FE\u5728\u5E38\u7528\u4F86\u6BD4\u8F03\u5927\u578B\u5730\u9707\u7684\u5F37\u5EA6\u3002"@zh . . "\uC9C0\uC9C4 \uBAA8\uBA58\uD2B8(Seismic moment)\uB294 \uC9C0\uC9C4\uD559\uC5D0\uC11C \uC9C0\uC9C4\uC758 \uD06C\uAE30\uB97C \uCE21\uC815\uD558\uB294 \uB370 \uC4F0\uC774\uB294 \uC9C0\uD45C\uC774\uB2E4. \uC2A4\uCE7C\uB77C \uC9C0\uC9C4 \uBAA8\uBA58\uD2B8 \uC740 \uB2E4\uC74C\uACFC \uAC19\uC774 \uC815\uC758\uB41C\uB2E4. \uC5EC\uAE30\uC11C, \n* \uC740 \uC9C0\uC9C4\uC774 \uC77C\uC5B4\uB09C \uC9C0\uC5ED \uC554\uC11D\uC758 \uC804\uB2E8 \uD0C4\uC131 \uACC4\uC218(Pa \uB610\uB294 N/m2) \n* \uB294 \uC9C0\uC9C4\uC774 \uBC1C\uC0DD\uD55C \uC9C0\uC5ED\uC5D0\uC11C \uB2E8\uCE35\uC774 \uD30C\uAD34\uB41C \uC601\uC5ED \uD06C\uAE30(m2) \n* \uB294 \uC601\uC5ED\uC5D0\uC11C \uD3C9\uADE0 \uBBF8\uB044\uB7EC\uC9D0 \uD06C\uAE30(in m) \uC740 \uB274\uD134 \uBBF8\uD130 \uB2E8\uC704\uC758 \uB3CC\uB9BC\uD798\uC73C\uB85C\uB3C4 \uB098\uD0C0\uB0BC \uC218 \uC788\uB2E4. \uC9C0\uC9C4 \uBAA8\uBA58\uD2B8\uC640 \uD1A0\uD06C \uC0AC\uC774 \uAD00\uACC4\uB294 \uC9C0\uC9C4\uC758 \uADFC\uC6D0\uC5D0\uC11C \uB098\uC624\uB294 \uCCB4\uC801\uB825\uACFC \uC774\uC911 \uACB0\uD569 \uAD00\uACC4(\uC11C\uB85C \uBC18\uB300\uB418\uB294 \uD1A0\uD06C\uAC00 \uC11C\uB85C \uD569\uCCD0\uC838 \uC791\uC6A9\uD558\uB294 \uACB0\uD569\uD798)\uB85C \uC5F0\uAD00\uB418\uBA70, \uC9C0\uC9C4 \uBAA8\uBA58\uD2B8\uB294 \uB450 \uADFC\uC6D0\uC5D0\uC11C \uB098\uC624\uB294 \uD1A0\uD06C\uC758 \uACB0\uD569\uC774\uB77C\uACE0 \uB9D0\uD560 \uC218 \uC788\uB2E4. \uC9C0\uC9C4 \uBAA8\uBA58\uD2B8\uB294 \uAD6D\uC81C\uB2E8\uC704\uACC4(SI \uB2E8\uC704\uACC4)\uC5D0\uC11C \uB274\uD134 \uBBF8\uD130(N m \uB610\uB294 N\u00B7m)\uB85C \uD45C\uAE30\uD558\uBA70 \uAD6C\uD615 CGS \uB2E8\uC704\uACC4\uC5D0\uC11C\uB294 \uB2E4\uC778 \uC13C\uCE58\uBBF8\uD130(dyn-cm)\uB85C \uD45C\uAE30\uD55C\uB2E4. \uC9C0\uC9C4 \uBAA8\uBA58\uD2B8\uB294 \uAC00\uC7A5 \uAC04\uB2E8\uD558\uAC8C\uB294 \uBBF8\uB044\uB7EC\uC9C4 \uC591\uACFC \uD30C\uC5F4\uB41C \uD639\uC740 \uBBF8\uB044\uB7EC\uC9C4 \uB2E8\uCE35 \uBA74\uC801, \uC800\uD56D \uB610\uB294 \uB9C8\uCC30 \uACC4\uC218 \uC14B\uB9CC \uAC00\uC9C0\uACE0 \uACC4\uC0B0\uD560 \uC218 \uC788\uB2E4. \uC774\uB7F0 \uBBF8\uC9C0\uC218\uB4E4\uC740 \uACFC\uAC70 \uC9C0\uC9C4 \uADDC\uBAA8\uB098 \uBBF8\uB798\uC5D0 \uC62C \uAC83\uC73C\uB85C \uC608\uC0C1\uB418\uB294 \uC9C0\uC9C4\uC758 \uADDC\uBAA8\uB97C \uAE30\uC874\uC758 \uB2E8\uCE35 \uC5F0\uAD6C\uB97C \uD1B5\uD574 \uCD94\uC815\uD560 \uC218 \uC788\uB2E4\uB294 \uC7A5\uC810\uC774 \uC788\uB2E4."@ko . "Das seismische Moment ist \u2013 wie die seismische Energie oder die Magnitude \u2013 ein Ma\u00DF f\u00FCr die St\u00E4rke eines Erdbebens. Es berechnet sich aus , wobei \n* das Schermodul des Gesteins entlang der Bruchfl\u00E4che (normalerweise 30 Gigapascal) \n* die Bruchfl\u00E4che \n* die durchschnittliche Verschiebung entlang der Bruchfl\u00E4che A ist. F\u00FCr historische Erdbeben kann das seismische Moment aus geologischen Sch\u00E4tzungen der Bruchfl\u00E4che und der Verschiebung berechnet werden, f\u00FCr heutige Erdbeben werden innerhalb kurzer Zeit Sch\u00E4tzwerte aus den Seismogrammen berechnet."@de . . "Momento sismico"@it . . "Momento s\u00EDsmico \u00E9 uma quantidade usada pelos sism\u00F3logos para medir a magnitude de um terremoto. O momento s\u00EDsmico escalar \u00E9 definido pela equa\u00E7\u00E3o , onde \n* \u00E9 o m\u00F3dulo de cisalhamento das rochas envolvidas no terremoto, geralmente 30 gigapascals \n* \u00E9 a \u00E1rea de ruptura ao longo da falha geol\u00F3gica onde ocorre o terremoto e \n* \u00E9 o deslocamento m\u00E9dio em . O momento s\u00EDsmico \u00E9 a base da escala de magnitude de momento, introduzida por Hiroo Kanamori, a qual \u00E9 atualmente usada para comparar a magnitude de diferentes terremotos - especialmente para comparar os grandes terremotos."@pt . . . . . . "Moment sismique"@fr . "\u5730\u9707\u30E2\u30FC\u30E1\u30F3\u30C8\uFF08\u3058\u3057\u3093\u30E2\u30FC\u30E1\u30F3\u30C8\uFF09\u3068\u306F\u3001\u5730\u9707\u306E\u5927\u304D\u3055\u3092\u793A\u3059\u6307\u6A19\u306E\u3072\u3068\u3064\u3067\u3001\u65AD\u5C64\u904B\u52D5\u306E\u529B\u306E\u30E2\u30FC\u30E1\u30F3\u30C8\uFF08\u30A8\u30CD\u30EB\u30AE\u30FC\uFF09\u306E\u5927\u304D\u3055\u3092\u8868\u3059\u3002 \u65AD\u5C64\u9762\u306E\u525B\u6027\u7387\u3092\uFF08Pa\uFF09\u3001\u65AD\u5C64\u9762\u7A4D\u306E\u5408\u8A08\u3092\uFF08m2\uFF09\u3001\u65AD\u5C64\u5168\u4F53\u3067\u306E\u5909\u4F4D\uFF08\u3059\u3079\u308A\uFF09\u91CF\u306E\u5E73\u5747\u3092\uFF08m\uFF09\u3068\u3057\u305F\u3068\u304D\u3001\u5730\u9707\u30E2\u30FC\u30E1\u30F3\u30C8\u306F\u3001 \u3068\u8868\u3055\u308C\u308B\u3002\u5358\u4F4D\u306F\u30CB\u30E5\u30FC\u30C8\u30F3\u30E1\u30FC\u30C8\u30EB\uFF08N\u30FBm\uFF09\u3067\u3042\u308B\u3002"@ja . .