. . . . . "\u91CD\u529B\u7570\u5E38"@ja . . "Se define como anomal\u00EDa gravitatoria a la diferencia entre el valor de gravedad observado (gobs) en un determinado lugar de un planeta \u2014generalmente un punto en su superficie\u2014 y la gravedad te\u00F3rica (\u03B3), obtenida de un modelo que contempla las dimensiones, masa y rotaci\u00F3n del planeta: . Una anomal\u00EDa positiva de gravedad indica la presencia de un cuerpo con exceso de masa respecto a la masa del modelo de referencia. Mediante el modelado num\u00E9rico del campo gravitatorio es posible determinar la estructura interna de los planetas. La anomal\u00EDa gravitatoria es medida a trav\u00E9s de medidas in situ o bien mediante sat\u00E9lite. Suele presentarse en forma de mapas y es expresada habitualmente en unidades de miligal (1 mGal = 10\u20135 m/s2). Adem\u00E1s se le suelen aplicar ciertas correcciones como la de Airy y Bouguer que facilitan la interpretaci\u00F3n de los datos."@es . "\u0634\u0630\u0648\u0630 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629"@ar . "\u062A\u0628\u0627\u064A\u0646 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629"@ar . "\u91CD\u529B\u5F02\u5E38\uFF08\u82F1\u8A9E\uFF1AGravity anomaly\uFF09\u5728\u5927\u5730\u6D4B\u91CF\u5B66\u4E2D\u7528\u4E8E\u63CF\u8FF0\u771F\u5B9E\u91CD\u529B\u4E0E\u6B63\u5E38\u91CD\u529B\u4E4B\u95F4\u7684\u5DEE\u5F02\u3002\u5728\u5927\u5730\u6C34\u51C6\u9762\u4E0A\uFF0C\u67D0\u70B9\u5904\u7684\u771F\u5B9E\u91CD\u529B\u77E2\u91CF\u4E0E\u8BE5\u70B9\u6CBF\u6CD5\u7EBF\u5230\u53C2\u8003\u692D\u7403\u9762\u4E0A\u6295\u5F71\u5904\u7684\u6B63\u5E38\u91CD\u529B\u77E2\u91CF\u4E4B\u5DEE\uFF0C\u88AB\u79F0\u4E3A\u8BE5\u70B9\u5904\u7684\u91CD\u529B\u5F02\u5E38\u77E2\u91CF\uFF0C\u8BE5\u70B9\u5904\u7684\u91CD\u529B\u5F02\u5E38\u5219\u662F\u8FD9\u4E00\u91CD\u529B\u5F02\u5E38\u77E2\u91CF\u7684\u5927\u5C0F\u3002\u6709\u65F6\u4E5F\u79F0\u8FD9\u4E00\u91CD\u529B\u5F02\u5E38\u4E3A\u6DF7\u5408\u91CD\u529B\u5F02\u5E38\uFF0C\u800C\u5C06\u5927\u5730\u6C34\u51C6\u9762\u4E0A\u540C\u4E00\u70B9\u5904\u7684\u771F\u5B9E\u91CD\u529B\u77E2\u91CF\u4E0E\u6B63\u5E38\u91CD\u529B\u77E2\u91CF\u4E4B\u5DEE\uFF08\u5373\u91CD\u529B\u6270\u52A8\uFF09\u79F0\u4E3A\u7EAF\u91CD\u529B\u5F02\u5E38\u3002\u91CD\u529B\u5F02\u5E38\u77E2\u91CF\u7684\u65B9\u5411\u88AB\u79F0\u4E3A\u5782\u7EBF\u504F\u5DEE\u3002"@zh . . . . . . "Un'anomalia gravitazionale o anomalia gravimetrica, \u00E8 la differenza o discrepanza tra il valore misurato dell'accelerazione in caduta libera sulla superficie di un pianeta (l'accelerazione di gravit\u00E0), e il corrispondente valore teorico previsto da un modello del campo gravitazionale del pianeta."@it . . . . . . "\u062A\u0628\u0627\u064A\u0646 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0623\u0648 \u0634\u0630\u0648\u0630 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0647\u0648 \u0627\u0644\u0641\u0631\u0642 \u0628\u064A\u0646 \u0642\u064A\u0645\u0629 \u0627\u0644\u062A\u0633\u0627\u0631\u0639 \u0627\u0644\u0645\u0644\u0627\u062D\u0638 \u0644\u0644\u0633\u0642\u0648\u0637 \u0627\u0644\u062D\u0631 \u0623\u0648 (\u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636) \u0648\u0627\u0644\u0642\u064A\u0645\u0629 \u0627\u0644\u0645\u062A\u0648\u0642\u0639\u0629 \u0645\u0646 \u0646\u0645\u0648\u0630\u062C \u0627\u0644\u0646\u0637\u0627\u0642 \u0627\u0644\u062C\u0630\u0628\u064A \u0644\u0644\u0643\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629\u060C \u064A\u062A\u0645 \u062A\u0645\u062B\u064A\u0644 \u0647\u0630\u0627 \u0627\u0644\u0641\u0631\u0642 \u0639\u0644\u0649 \u0645\u0646\u062D\u0646\u0649 \u064A\u0633\u0645\u0649 \u0645\u0646\u062D\u0646\u0649 \u0649 \u062A\u0628\u0627\u064A\u0646 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0648\u0627\u0644\u0630\u064A \u064A\u0646\u062A\u062C \u0639\u0646 \u0637\u0631\u064A\u0642 \u0637\u0631\u062D \u0642\u064A\u0645\u0629 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0627\u0644\u0645\u062A\u0648\u0642\u0639\u0629 \u0644\u0645\u0646\u0637\u0642\u0629 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u0645\u0646 \u0642\u064A\u0645\u0629 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0627\u0644\u0645\u0644\u0627\u062D\u0638\u0629. \u062A\u0639\u062F \u0637\u0631\u064A\u0642\u0629 \u062A\u0628\u0627\u064A\u0646 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0645\u0646 \u0625\u062D\u062F\u0649 \u0637\u0631\u0642 \u0639\u0644\u0645 \u0641\u064A\u0632\u064A\u0627\u0621 \u0627\u0644\u0623\u0631\u0636 - \u0627\u0644\u062C\u064A\u0648\u0641\u064A\u0632\u064A\u0627\u0621 \u0627\u0644\u0627\u0633\u062A\u0643\u0634\u0627\u0641\u064A\u0629 \u0644\u063A\u0627\u064A\u0627\u062A \u0645\u0639\u0631\u0641\u0629 \u0645\u0643\u0648\u0646\u0627\u062A \u0628\u0627\u0637\u0646 \u0627\u0644\u0623\u0631\u0636. \u064A\u062C\u0628 \u0627\u0644\u0623\u062E\u0630 \u0628\u0639\u064A\u0646 \u0627\u0644\u0627\u0639\u062A\u0628\u0627\u0631 \u0627\u062E\u062A\u0644\u0627\u0641 \u0627\u0644\u062A\u0636\u0627\u0631\u064A\u0633 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u0648\u0627\u0644\u062A\u064A \u062A\u0624\u062B\u0631 \u0639\u0644\u0649 \u0625\u0646\u062A\u0627\u062C\u064A\u0629 \u0645\u0646\u062D\u0646\u0649 \u062A\u0628\u0627\u064A\u0646 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629."@ar . . . . . "\u91CD\u529B\u5F02\u5E38\uFF08\u82F1\u8A9E\uFF1AGravity anomaly\uFF09\u5728\u5927\u5730\u6D4B\u91CF\u5B66\u4E2D\u7528\u4E8E\u63CF\u8FF0\u771F\u5B9E\u91CD\u529B\u4E0E\u6B63\u5E38\u91CD\u529B\u4E4B\u95F4\u7684\u5DEE\u5F02\u3002\u5728\u5927\u5730\u6C34\u51C6\u9762\u4E0A\uFF0C\u67D0\u70B9\u5904\u7684\u771F\u5B9E\u91CD\u529B\u77E2\u91CF\u4E0E\u8BE5\u70B9\u6CBF\u6CD5\u7EBF\u5230\u53C2\u8003\u692D\u7403\u9762\u4E0A\u6295\u5F71\u5904\u7684\u6B63\u5E38\u91CD\u529B\u77E2\u91CF\u4E4B\u5DEE\uFF0C\u88AB\u79F0\u4E3A\u8BE5\u70B9\u5904\u7684\u91CD\u529B\u5F02\u5E38\u77E2\u91CF\uFF0C\u8BE5\u70B9\u5904\u7684\u91CD\u529B\u5F02\u5E38\u5219\u662F\u8FD9\u4E00\u91CD\u529B\u5F02\u5E38\u77E2\u91CF\u7684\u5927\u5C0F\u3002\u6709\u65F6\u4E5F\u79F0\u8FD9\u4E00\u91CD\u529B\u5F02\u5E38\u4E3A\u6DF7\u5408\u91CD\u529B\u5F02\u5E38\uFF0C\u800C\u5C06\u5927\u5730\u6C34\u51C6\u9762\u4E0A\u540C\u4E00\u70B9\u5904\u7684\u771F\u5B9E\u91CD\u529B\u77E2\u91CF\u4E0E\u6B63\u5E38\u91CD\u529B\u77E2\u91CF\u4E4B\u5DEE\uFF08\u5373\u91CD\u529B\u6270\u52A8\uFF09\u79F0\u4E3A\u7EAF\u91CD\u529B\u5F02\u5E38\u3002\u91CD\u529B\u5F02\u5E38\u77E2\u91CF\u7684\u65B9\u5411\u88AB\u79F0\u4E3A\u5782\u7EBF\u504F\u5DEE\u3002"@zh . . . . . . . . . "Gravity anomaly"@en . . . . . . "\uC911\uB825\uC774\uC0C1(\u91CD\u529B\u7570\u5E38, Gravity anomaly)\uC740 \uC2E4\uCE21(\u5BE6\u6E2C) \uC911\uB825\uCE58\uC640 \uC774\uB860(\u7406\u8AD6) \uC911\uB825\uCE58\uC640\uC758 \uCC28\uC774\uB97C \uAC00\uB9AC\uD0A8\uB2E4. \uC774\uB860 \uC911\uB825\uCE58\uB294 \uD45C\uC900\uC911\uB825\uC2DD(\u6A19\u6E96\u91CD\u529B\u5F0F)\uC5D0 \uC758\uD558\uC5EC \uACC4\uC0B0\uD560 \uC218 \uC788\uB2E4. \uC911\uB825\uC774\uC0C1\uC758 \uAC12\uC774 (+)\uB77C\uACE0 \uD568\uC740 \uADF8 \uADFC\uBC29\uC758 \uC9C0\uAC01\uC758 \uBC00\uB3C4\uAC00 \uD3C9\uADE0\uC0C1\uD0DC\uC5D0 \uBE44\uD574\uC11C \uD06C\uB2E4\uB294 \uB73B\uC774\uBA70, \uBC18\uB300\uB85C (-)\uB77C \uD568\uC740 \uC9C0\uAC01\uBC00\uB3C4\uAC00 \uC791\uB2E4\uB294 \uB73B\uC774\uB2E4. \uAC00\uB839 \uB192\uC740 \uC0B0\uC5D0\uC11C \uC911\uB825\uC744 \uCE21\uC815\uD558\uACE0, \uC801\uB2F9\uD55C \uBCF4\uC815(\u88DC\u6B63)\uC744 \uAC00\uD558\uC5EC \uC774\uB97C \uD574\uBA74\uC0C1\uC758 \uAC12\uC73C\uB85C \uACE0\uCE5C \uB2E4\uC74C\uC5D0 \uD574\uBA74\uC0C1\uC758 \uD45C\uC900\uC911\uB825\uC758 \uAC12\uACFC \uBE44\uAD50\uD558\uBA74 (-)\uC758 \uC911\uB825\uC774\uC0C1\uCE58\uB97C \uC5BB\uC744 \uC218 \uC788\uC73C\uBA70, \uC9C0\uAC01 \uD3C9\uD615\uC124\uC774 \uC131\uB9BD\uD568\uC744 \uC54C \uC218 \uC788\uB2E4."@ko . "Un'anomalia gravitazionale o anomalia gravimetrica, \u00E8 la differenza o discrepanza tra il valore misurato dell'accelerazione in caduta libera sulla superficie di un pianeta (l'accelerazione di gravit\u00E0), e il corrispondente valore teorico previsto da un modello del campo gravitazionale del pianeta."@it . . . . "Uma anomalia gravim\u00E9trica (tamb\u00E9m anomalia grav\u00EDtica) \u00E9 a diferen\u00E7a entre o valor real da acelera\u00E7\u00E3o da gravidade de um lugar e o valor calculado teoricamente. Essa diferen\u00E7a entre o valor da acelera\u00E7\u00E3o da gravidade observado (gobs) num determinado local de um planeta, geralmente um ponto na sua superf\u00EDcie, e a acelera\u00E7\u00E3o da gravidade te\u00F3rica (\u03B3), \u00E9 obtida com base num modelo que contempla as dimens\u00F5es, massa e rota\u00E7\u00E3o do planeta: . Uma anomalia positiva indica a presen\u00E7a de um corpo com excesso de massa relativamente ao modelo de refer\u00EAncia. Mediante o do campo gravitacional \u00E9 poss\u00EDvel determinar a estrutura interna dos planetas. Quando o valor real \u00E9 inferior ao valor te\u00F3rico, a anomalia \u00E9 dita negativa. A anomalia gravim\u00E9trica \u00E9 medida in situ, por meio de um aparelho chamado grav\u00EDmetro, ou por meio de sat\u00E9lite. Este valor varia com a latitude, a altitude e a natureza geol\u00F3gica do local em que a medi\u00E7\u00E3o \u00E9 efetuada, sendo tanto maior quanto mais densos forem os materiais. Costuma ser representada na forma de mapas e \u00E9 normalmente expressa em miligal(1 mGal = 10\u22125 m/s2). Adicionalmente aplicam-se certas corre\u00E7\u00F5es como a de Bouguer que facilitam a interpreta\u00E7\u00E3o dos dados."@pt . . . "De zwaartekrachtanomalie of gravitatieanomalie is het lokale verschil tussen de gemeten valversnelling en de theoretische normale waarde."@nl . . . . . . "\u0634\u0630\u0648\u0630 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0647\u0648 \u0627\u0644\u0641\u0631\u0642 \u0628\u064A\u0646 \u0642\u064A\u0645\u0629 \u0627\u0644\u062A\u0633\u0627\u0631\u0639 \u0627\u0644\u0645\u0644\u0627\u062D\u0638 \u0644\u0644\u0633\u0642\u0648\u0637 \u0627\u0644\u062D\u0631 \u0623\u0648 (\u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636) \u0648\u0627\u0644\u0642\u064A\u0645\u0629 \u0627\u0644\u0645\u062A\u0648\u0642\u0639\u0629 \u0645\u0646 \u0646\u0645\u0648\u0630\u062C \u0627\u0644\u0646\u0637\u0627\u0642 \u0627\u0644\u062C\u0630\u0628\u064A \u0644\u0644\u0643\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629\u060C \u064A\u062A\u0645 \u062A\u0645\u062B\u064A\u0644 \u0647\u0630\u0627 \u0627\u0644\u0641\u0631\u0642 \u0639\u0644\u0649 \u0645\u0646\u062D\u0646\u0649 \u064A\u0633\u0645\u0649 \u0645\u0646\u062D\u0646\u0649 \u0634\u0630\u0648\u0630 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\u0627\u0644\u0627\u0639\u062A\u0628\u0627\u0631 \u0627\u062E\u062A\u0644\u0627\u0641 \u0627\u0644\u062A\u0636\u0627\u0631\u064A\u0633 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u0648\u0627\u0644\u062A\u064A \u062A\u0624\u062B\u0631 \u0639\u0644\u0649 \u0625\u0646\u062A\u0627\u062C\u064A\u0629 \u0645\u0646\u062D\u0646\u0649 \u0634\u0630\u0648\u0630 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629. \u064A\u0646\u0628\u063A\u064A \u0639\u062F\u0645 \u0627\u0644\u062E\u0644\u0637 \u0628\u064A\u0646 \u0634\u0630\u0648\u0630 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 anomaly gravity \u0648\u0628\u064A\u0646 \u0627\u0644\u0634\u0630\u0648\u0630 \u0627\u0644\u062C\u0630\u0628\u064A anomaly gravitational."@ar . . . . "\u91CD\u529B\u7570\u5E38\uFF08\u3058\u3085\u3046\u308A\u3087\u304F\u3044\u3058\u3087\u3046\u3001gravity anomaly\uFF09\u3068\u306F\u3001\u91CD\u529B\u306E\u5B9F\u6E2C\u5024\uFF08\u3042\u308B\u3044\u306F\u89B3\u6E2C\u5024\uFF09\u3068\u3001\u7406\u8AD6\u30E2\u30C7\u30EB\u304B\u3089\u4E88\u6E2C\u3055\u308C\u308B\u5024\u3068\u306E\u5DEE\u306E\u3053\u3068\u3067\u3042\u308B\u3002\u6E2C\u5730\u5B66\u30FB\u5730\u7403\u7269\u7406\u5B66\u306E\u5206\u91CE\u3068\u3001\u5929\u6587\u5B66\u30FB\u5B87\u5B99\u7269\u7406\u5B66\u306E\u5206\u91CE\u306E\u53CC\u65B9\u3067\u3001\u4E0A\u8A18\u306E\u610F\u5473\u3067\u540C\u3058\u7528\u8A9E\u304C\u4F7F\u308F\u308C\u3066\u3044\u308B\u304C\u3001\u5BFE\u8C61\u304C\u7570\u306A\u308B\u305F\u3081\u6982\u5FF5\u3082\u7570\u306A\u308B\u3002"@ja . "De zwaartekrachtanomalie of gravitatieanomalie is het lokale verschil tussen de gemeten valversnelling en de theoretische normale waarde."@nl . . . . "Eine Schwereanomalie, auch als Gravitationsanomalie bezeichnet, ist die lokale Abweichung der Schwerebeschleunigung vom theoretischen Normalwert auf einer Referenzfl\u00E4che, diese ist im Fall der Erde meist das Referenzellipsoid."@de . "Anomal\u00EDa gravitatoria"@es . . . . . . . "Eine Schwereanomalie, auch als Gravitationsanomalie bezeichnet, ist die lokale Abweichung der Schwerebeschleunigung vom theoretischen Normalwert auf einer Referenzfl\u00E4che, diese ist im Fall der Erde meist das Referenzellipsoid."@de . "L'anomalia gravitat\u00F2ria \u00E9s la difer\u00E8ncia existent entre l'acceleraci\u00F3 de la gravetat en un determinat indret d'un planeta (generalment un punt de la superf\u00EDcie) i la gravetat que es pot esperar basant-se en un determinat model de densitat planet\u00E0ria de refer\u00E8ncia. Una anomalia de gravetat positiva indica la pres\u00E8ncia d'un cos profund m\u00E9s dens del suposat en el model de refer\u00E8ncia. Mitjan\u00E7ant el del camp gravitatori \u00E9s possible determinar l'estructura interna dels planetes."@ca . . . "Anomalia si\u0142y ci\u0119\u017Cko\u015Bci \u2013 w geofizyce r\u00F3\u017Cnica mi\u0119dzy zmierzon\u0105 (i zredukowan\u0105 do poziomu elipsoidy) w danym punkcie si\u0142\u0105 ci\u0119\u017Cko\u015Bci a wzorcow\u0105 ( na danej szeroko\u015Bci geograficznej. Zwyczajowo mierzona jest w miligalach (mGal), rzadko stosuje si\u0119 milimetry na sekund\u0119 do kwadratu (mm/s2). W celu okre\u015Blenia anomalii, nale\u017Cy dla zmierzonej si\u0142y ci\u0119\u017Cko\u015Bci zastosowa\u0107 szereg poprawek:"@pl . . "Schwereanomalie"@de . 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"Anomali gravitasi"@in . . . "Anomali gravitasi adalah perbedaan antara gravitasi observasi dengan nilai yang diprediksi oleh model. Perbedaan medan gravitasi dapat disebabkan variasi rapat massa batuan dibawah permukaan, sehingga dalam observasi yang diselidiki adalah perbedaan medan gravitasi antar titik observasi. Pemodelan gravitasi dapat dilakukan dengan dua cara yaitu: dua dimensi, dengan pengamatan efek gravitasi pada satu arah, dan tiga dimensi, dengan pengamatan efek gravitasi pada bidang horizontal X-Y. Pemodelan gravitasi dilakukan dengan pendekatan bentuk-bentuk sederhana untuk mempermudah interpretasi data. Salah satu contoh bentuk yang dapat digunakan adalah silinder. Bentuk silinder memiliki kelebihan karena memiliki sudut tak berhingga, sehingga pendekatan lebih mudah dilakukan. Bentuk bentuk sederhana yang digunakan dapat lebih dari satu bentuk, sehingga dapat diinterpretasi dengan menampilkan kontur dan profilnya. Hasil pembacaan anomali gravitasi dapat dilakukan secara kualitatif dan kuantitatif. Analisis kulaitatif dapat dilakukan dengan membaca pola kontur anomali Bouguer. Sedangkan analisis kuantitatif dapat dilakukan dengan membuat penampang dua dimensi."@in . . . "Se define como anomal\u00EDa gravitatoria a la diferencia entre el valor de gravedad observado (gobs) en un determinado lugar de un planeta \u2014generalmente un punto en su superficie\u2014 y la gravedad te\u00F3rica (\u03B3), obtenida de un modelo que contempla las dimensiones, masa y rotaci\u00F3n del planeta: . Una anomal\u00EDa positiva de gravedad indica la presencia de un cuerpo con exceso de masa respecto a la masa del modelo de referencia. Mediante el modelado num\u00E9rico del campo gravitatorio es posible determinar la estructura interna de los planetas."@es . . . . . . . . . "The gravity anomaly at a location on the Earth's surface is the difference between the observed value of gravity and the value predicted by a theoretical model. If the Earth were an ideal oblate spheroid of uniform density, then the gravity measured at every point on its surface would be given precisely by a simple algebraic expression. However, the Earth has a rugged surface and non-uniform composition, which distorts its gravitational field. The theoretical value of gravity can be corrected for altitude and the effects of nearby terrain, but it usually still differs slightly from the measured value. This gravity anomaly can reveal the presence of subsurface structures of unusual density. For example, a mass of dense ore below the surface will give a positive anomaly due to the increased "@en . . . "Anomalia si\u0142y ci\u0119\u017Cko\u015Bci"@pl . . . "19330"^^ . . "\u0413\u0440\u0430\u0432\u0438\u0442\u0430\u0446\u0438\u043E\u0301\u043D\u043D\u0430\u044F \u0430\u043D\u043E\u043C\u0430\u0301\u043B\u0438\u044F \u2014 \u043D\u0435\u043E\u0431\u044B\u0447\u043D\u043E\u0435, \u043E\u0442\u043A\u043B\u043E\u043D\u044F\u044E\u0449\u0435\u0435\u0441\u044F \u043E\u0442 \u0440\u0435\u0433\u0443\u043B\u044F\u0440\u043D\u043E\u0433\u043E \u043F\u0440\u043E\u044F\u0432\u043B\u0435\u043D\u0438\u0435 \u0433\u0440\u0430\u0432\u0438\u0442\u0430\u0446\u0438\u043E\u043D\u043D\u043E\u0433\u043E \u043F\u043E\u043B\u044F \u043A\u0430\u043A\u043E\u0433\u043E-\u043B\u0438\u0431\u043E \u043E\u0431\u044A\u0435\u043A\u0442\u0430."@ru . . . . "1122285663"^^ . . . . . "\u91CD\u529B\u7570\u5E38\uFF08\u3058\u3085\u3046\u308A\u3087\u304F\u3044\u3058\u3087\u3046\u3001gravity anomaly\uFF09\u3068\u306F\u3001\u91CD\u529B\u306E\u5B9F\u6E2C\u5024\uFF08\u3042\u308B\u3044\u306F\u89B3\u6E2C\u5024\uFF09\u3068\u3001\u7406\u8AD6\u30E2\u30C7\u30EB\u304B\u3089\u4E88\u6E2C\u3055\u308C\u308B\u5024\u3068\u306E\u5DEE\u306E\u3053\u3068\u3067\u3042\u308B\u3002\u6E2C\u5730\u5B66\u30FB\u5730\u7403\u7269\u7406\u5B66\u306E\u5206\u91CE\u3068\u3001\u5929\u6587\u5B66\u30FB\u5B87\u5B99\u7269\u7406\u5B66\u306E\u5206\u91CE\u306E\u53CC\u65B9\u3067\u3001\u4E0A\u8A18\u306E\u610F\u5473\u3067\u540C\u3058\u7528\u8A9E\u304C\u4F7F\u308F\u308C\u3066\u3044\u308B\u304C\u3001\u5BFE\u8C61\u304C\u7570\u306A\u308B\u305F\u3081\u6982\u5FF5\u3082\u7570\u306A\u308B\u3002"@ja . . . "Anomalia gravitat\u00F2ria"@ca . . "937535"^^ . . . . "Anomalia gravim\u00E9trica"@pt . "Uma anomalia gravim\u00E9trica (tamb\u00E9m anomalia grav\u00EDtica) \u00E9 a diferen\u00E7a entre o valor real da acelera\u00E7\u00E3o da gravidade de um lugar e o valor calculado teoricamente. Essa diferen\u00E7a entre o valor da acelera\u00E7\u00E3o da gravidade observado (gobs) num determinado local de um planeta, geralmente um ponto na sua superf\u00EDcie, e a acelera\u00E7\u00E3o da gravidade te\u00F3rica (\u03B3), \u00E9 obtida com base num modelo que contempla as dimens\u00F5es, massa e rota\u00E7\u00E3o do planeta: . Uma anomalia positiva indica a presen\u00E7a de um corpo com excesso de massa relativamente ao modelo de refer\u00EAncia. Mediante o do campo gravitacional \u00E9 poss\u00EDvel determinar a estrutura interna dos planetas. Quando o valor real \u00E9 inferior ao valor te\u00F3rico, a anomalia \u00E9 dita negativa."@pt . . . . "Zwaartekrachtanomalie"@nl . "L'anomalia gravitat\u00F2ria \u00E9s la difer\u00E8ncia existent entre l'acceleraci\u00F3 de la gravetat en un determinat indret d'un planeta (generalment un punt de la superf\u00EDcie) i la gravetat que es pot esperar basant-se en un determinat model de densitat planet\u00E0ria de refer\u00E8ncia. Una anomalia de gravetat positiva indica la pres\u00E8ncia d'un cos profund m\u00E9s dens del suposat en el model de refer\u00E8ncia. Mitjan\u00E7ant el del camp gravitatori \u00E9s possible determinar l'estructura interna dels planetes. L'anomalia gravitat\u00F2ria \u00E9s mesurada per mitj\u00E0 de mesures in situ o per sat\u00E8l\u00B7lit. Sol presentar-se en forma de mapes i \u00E9s expressada habitualment en unitats de mil\u00B7ligal (1mGal = 1e-5 m/s\u00B2). A m\u00E9s, se li solen aplicar certes correccions, com la d'Airy i Bouguer, que faciliten la interpretaci\u00F3 de les dades."@ca . "\uC911\uB825\uC774\uC0C1"@ko . . "\u062A\u0628\u0627\u064A\u0646 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0623\u0648 \u0634\u0630\u0648\u0630 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0647\u0648 \u0627\u0644\u0641\u0631\u0642 \u0628\u064A\u0646 \u0642\u064A\u0645\u0629 \u0627\u0644\u062A\u0633\u0627\u0631\u0639 \u0627\u0644\u0645\u0644\u0627\u062D\u0638 \u0644\u0644\u0633\u0642\u0648\u0637 \u0627\u0644\u062D\u0631 \u0623\u0648 (\u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636) \u0648\u0627\u0644\u0642\u064A\u0645\u0629 \u0627\u0644\u0645\u062A\u0648\u0642\u0639\u0629 \u0645\u0646 \u0646\u0645\u0648\u0630\u062C \u0627\u0644\u0646\u0637\u0627\u0642 \u0627\u0644\u062C\u0630\u0628\u064A \u0644\u0644\u0643\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629\u060C \u064A\u062A\u0645 \u062A\u0645\u062B\u064A\u0644 \u0647\u0630\u0627 \u0627\u0644\u0641\u0631\u0642 \u0639\u0644\u0649 \u0645\u0646\u062D\u0646\u0649 \u064A\u0633\u0645\u0649 \u0645\u0646\u062D\u0646\u0649 \u0649 \u062A\u0628\u0627\u064A\u0646 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0648\u0627\u0644\u0630\u064A \u064A\u0646\u062A\u062C \u0639\u0646 \u0637\u0631\u064A\u0642 \u0637\u0631\u062D \u0642\u064A\u0645\u0629 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0627\u0644\u0645\u062A\u0648\u0642\u0639\u0629 \u0644\u0645\u0646\u0637\u0642\u0629 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u0645\u0646 \u0642\u064A\u0645\u0629 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0627\u0644\u0645\u0644\u0627\u062D\u0638\u0629. \u064A\u0635\u0641 \u0645\u0646\u062D\u0646\u0649 \u062A\u0628\u0627\u064A\u0646 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0627\u0644\u062A\u063A\u064A\u0631\u0627\u062A \u0627\u0644\u0645\u062D\u0644\u064A\u0629 \u0644\u0646\u0637\u0627\u0642 \u062C\u0630\u0628 \u0627\u0644\u0643\u0631\u0629 \u0627\u0644\u0627\u0631\u0636\u064A\u0629 \u0641\u064A \u0645\u0646\u0637\u0642\u0629 \u0645\u0639\u064A\u0646\u0629\u060C \u0639\u0646\u062F\u0645\u0627 \u064A\u0643\u0648\u0646 \u0644\u0644\u0645\u0646\u0637\u0642\u0629 \u062A\u0628\u0627\u064A\u0646 \u062C\u0627\u0630\u0628\u064A\u0629 \u0645\u0648\u062C\u0628 (\u0645\u0646\u062D\u0646\u0649 \u062A\u0628\u0627\u064A\u0646 \u062C\u0627\u0630\u0628\u064A\u0629 \u0645\u0642\u0639\u0631 \u0644\u0644\u0627\u0633\u0641\u0644) \u062A\u0643\u0648\u0646 \u0642\u064A\u0645\u0629 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0627\u0644\u0645\u0644\u0627\u062D\u0638\u0629 \u0623\u0643\u0628\u0631 \u0645\u0646 \u0642\u064A\u0645\u0629 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0627\u0644\u0645\u062A\u0648\u0642\u0639\u0629 \u0644\u0644\u0645\u0646\u0637\u0642\u0629 \u0645\u0645\u0627 \u064A\u062F\u0644 \u0639\u0644\u0649 \u0648\u062C\u0648\u062F \u0643\u062A\u0644 (\u062C\u0645\u0639 \u0643\u062A\u0644\u0629) \u062A\u062D\u062A \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u0644\u0647\u0627 \u0643\u062B\u0627\u0641\u0629 \u0623\u0643\u0628\u0631 \u0645\u0646 \u0643\u062B\u0627\u0641\u0629 \u0627\u0644\u0645\u0648\u0627\u062F \u0627\u0644\u0645\u062D\u064A\u0637\u0629 \u0644\u0623\u0646 \u0627\u0644\u062A\u0633\u0627\u0631\u0639 \u0627\u0644\u062C\u0630\u0628\u064A \u0627\u0644\u0645\u0644\u0627\u062D\u0638 \u064A\u0639\u062A\u0645\u062F \u0639\u0644\u0649 \u0627\u0644\u0643\u062B\u0627\u0641\u0629 \u0627\u0644\u062A\u064A \u062A\u062A\u0646\u0627\u0633\u0628 \u062A\u0646\u0627\u0633\u0628\u0627 \u0637\u0631\u062F\u064A\u0627 \u0645\u0639 \u0627\u0644\u0643\u062A\u0644\u0629 \u062D\u064A\u062B \u0627\u0646 \u0627\u0644\u0643\u062B\u0627\u0641\u0629 = \u0627\u0644\u0643\u062A\u0644\u0629 / \u0627\u0644\u062D\u062C\u0645 \u0648\u0628\u0646\u0627\u0621\u0627 \u0639\u0644\u0649 \u0642\u0627\u0646\u0648\u0646 \u0646\u064A\u0648\u062A\u0646 \u0627\u0644\u062B\u0627\u0646\u064A \u0627\u0644\u0630\u064A \u064A\u0645\u062B\u0644 \u0628\u0627\u0644\u0639\u0644\u0627\u0642\u0629 \u0627\u0644\u0631\u064A\u0627\u0636\u064A\u0629 (\u0627\u0644\u0642\u0648\u0629= \u0627\u0644\u0643\u062A\u0644\u0629 * \u0627\u0644\u062A\u0633\u0627\u0631\u0639) \u0648\u0639\u0644\u064A\u0647 (\u0642\u0648\u0629 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 = \u0627\u0644\u0643\u062A\u0644\u0629 * \u0627\u0644\u062A\u0633\u0627\u0631\u0639 \u0627\u0644\u062C\u0630\u0628\u064A)\u060C \u0639\u0646\u062F\u0645\u0627 \u064A\u0643\u0648\u0646 \u0644\u0644\u0645\u0646\u0637\u0642\u0629 \u062A\u0628\u0627\u064A\u0646 \u062C\u0627\u0630\u0628\u064A\u0629 \u0633\u0627\u0644\u0628 \u062A\u0643\u0648\u0646 \u0627\u0644\u0642\u064A\u0645\u0629 \u0627\u0644\u0645\u0644\u0627\u062D\u0638\u0629 \u0623\u0642\u0644 \u0645\u0646 \u0627\u0644\u0642\u064A\u0645\u0629 \u0627\u0644\u0645\u062A\u0648\u0642\u0639\u0629 \u0644\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0641\u064A \u062A\u0644\u0643 \u0627\u0644\u0645\u0646\u0637\u0642\u0629 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 (\u0645\u0646\u062D\u0646\u0649 \u062A\u0628\u0627\u064A\u0646 \u062C\u0627\u0630\u0628\u064A\u0629 \u0645\u0642\u0639\u0631 \u0644\u0644\u0623\u0639\u0644\u0649) \u0648\u0627\u0644\u0630\u064A \u064A\u062F\u0644 \u0639\u0644\u0649 \u0648\u062C\u0648\u062F \u0643\u062A\u0644 \u062A\u062D\u062A \u0623\u0631\u0636\u064A\u0629 \u0644\u0647\u0627 \u0643\u062B\u0627\u0641\u0629 \u0623\u0642\u0644 \u0645\u0646 \u0643\u062B\u0627\u0641\u0629 \u0627\u0644\u0645\u0648\u0627\u062F \u0627\u0644\u0645\u062D\u064A\u0637\u0629 \u0628\u0647\u0627. \u062A\u0639\u062F \u0637\u0631\u064A\u0642\u0629 \u062A\u0628\u0627\u064A\u0646 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629 \u0645\u0646 \u0625\u062D\u062F\u0649 \u0637\u0631\u0642 \u0639\u0644\u0645 \u0641\u064A\u0632\u064A\u0627\u0621 \u0627\u0644\u0623\u0631\u0636 - \u0627\u0644\u062C\u064A\u0648\u0641\u064A\u0632\u064A\u0627\u0621 \u0627\u0644\u0627\u0633\u062A\u0643\u0634\u0627\u0641\u064A\u0629 \u0644\u063A\u0627\u064A\u0627\u062A \u0645\u0639\u0631\u0641\u0629 \u0645\u0643\u0648\u0646\u0627\u062A \u0628\u0627\u0637\u0646 \u0627\u0644\u0623\u0631\u0636. \u064A\u062C\u0628 \u0627\u0644\u0623\u062E\u0630 \u0628\u0639\u064A\u0646 \u0627\u0644\u0627\u0639\u062A\u0628\u0627\u0631 \u0627\u062E\u062A\u0644\u0627\u0641 \u0627\u0644\u062A\u0636\u0627\u0631\u064A\u0633 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u0648\u0627\u0644\u062A\u064A \u062A\u0624\u062B\u0631 \u0639\u0644\u0649 \u0625\u0646\u062A\u0627\u062C\u064A\u0629 \u0645\u0646\u062D\u0646\u0649 \u062A\u0628\u0627\u064A\u0646 \u0627\u0644\u062C\u0627\u0630\u0628\u064A\u0629."@ar . . . . "\u0413\u0440\u0430\u0432\u0438\u0442\u0430\u0446\u0438\u043E\u043D\u043D\u0430\u044F \u0430\u043D\u043E\u043C\u0430\u043B\u0438\u044F"@ru . . . . . . . . "\u91CD\u529B\u5F02\u5E38"@zh . . . . . "Anomalia gravitazionale"@it . "The gravity anomaly at a location on the Earth's surface is the difference between the observed value of gravity and the value predicted by a theoretical model. If the Earth were an ideal oblate spheroid of uniform density, then the gravity measured at every point on its surface would be given precisely by a simple algebraic expression. However, the Earth has a rugged surface and non-uniform composition, which distorts its gravitational field. The theoretical value of gravity can be corrected for altitude and the effects of nearby terrain, but it usually still differs slightly from the measured value. This gravity anomaly can reveal the presence of subsurface structures of unusual density. For example, a mass of dense ore below the surface will give a positive anomaly due to the increased gravitational attraction of the ore. Different theoretical models will predict different values of gravity, and so a gravity anomaly is always specified with reference to a particular model. The Bouguer, free-air, and isostatic gravity anomalies are each based on different theoretical corrections to the value of gravity. A gravity survey is conducted by measuring the gravity anomaly at many locations in a region of interest, using a portable instrument called a gravimeter. Careful analysis of the gravity data allows geologists to make inferences about the subsurface geology."@en . "\u0413\u0440\u0430\u0432\u0438\u0442\u0430\u0446\u0438\u043E\u0301\u043D\u043D\u0430\u044F \u0430\u043D\u043E\u043C\u0430\u0301\u043B\u0438\u044F \u2014 \u043D\u0435\u043E\u0431\u044B\u0447\u043D\u043E\u0435, \u043E\u0442\u043A\u043B\u043E\u043D\u044F\u044E\u0449\u0435\u0435\u0441\u044F \u043E\u0442 \u0440\u0435\u0433\u0443\u043B\u044F\u0440\u043D\u043E\u0433\u043E \u043F\u0440\u043E\u044F\u0432\u043B\u0435\u043D\u0438\u0435 \u0433\u0440\u0430\u0432\u0438\u0442\u0430\u0446\u0438\u043E\u043D\u043D\u043E\u0433\u043E \u043F\u043E\u043B\u044F \u043A\u0430\u043A\u043E\u0433\u043E-\u043B\u0438\u0431\u043E \u043E\u0431\u044A\u0435\u043A\u0442\u0430."@ru . . . . "Anomali gravitasi adalah perbedaan antara gravitasi observasi dengan nilai yang diprediksi oleh model. Perbedaan medan gravitasi dapat disebabkan variasi rapat massa batuan dibawah permukaan, sehingga dalam observasi yang diselidiki adalah perbedaan medan gravitasi antar titik observasi. Pemodelan gravitasi dapat dilakukan dengan dua cara yaitu: dua dimensi, dengan pengamatan efek gravitasi pada satu arah, dan tiga dimensi, dengan pengamatan efek gravitasi pada bidang horizontal X-Y."@in . . . . . "Anomalia si\u0142y ci\u0119\u017Cko\u015Bci \u2013 w geofizyce r\u00F3\u017Cnica mi\u0119dzy zmierzon\u0105 (i zredukowan\u0105 do poziomu elipsoidy) w danym punkcie si\u0142\u0105 ci\u0119\u017Cko\u015Bci a wzorcow\u0105 ( na danej szeroko\u015Bci geograficznej. Zwyczajowo mierzona jest w miligalach (mGal), rzadko stosuje si\u0119 milimetry na sekund\u0119 do kwadratu (mm/s2). W celu okre\u015Blenia anomalii, nale\u017Cy dla zmierzonej si\u0142y ci\u0119\u017Cko\u015Bci zastosowa\u0107 szereg poprawek: \n* poprawka wolnopowietrzna (Faye'a) \u2013 sprowadza punkt pomiarowy do poziomu elipsoidy \n* (tzw. redukcja Bouguera) \u2013 uwzgl\u0119dnia masy le\u017C\u0105ce mi\u0119dzy punktem pomiaru a powierzchni\u0105 odniesienia \n* \u2013 uwzgl\u0119dnia wp\u0142yw ukszta\u0142towania otaczaj\u0105cego terenu \n* \u2013 uwzgl\u0119dnia wp\u0142yw oddzia\u0142ywania S\u0142o\u0144ca i Ksi\u0119\u017Cyca. Na podstawie anomalii si\u0142y ci\u0119\u017Cko\u015Bci mo\u017Cna okre\u015Bli\u0107 po\u0142o\u017Cenie i kszta\u0142t niekt\u00F3rych struktur geologicznych. Obiekty o g\u0119sto\u015Bci wy\u017Cszej, ni\u017C otoczenie (np. rudy) oddzia\u0142uj\u0105 dodatnio na si\u0142\u0119 ci\u0119\u017Cko\u015Bci, natomiast te o g\u0119sto\u015Bci mniejszej (kawerny, wysady solne) \u2013 ujemnie. Nale\u017Cy przy tym zaznaczy\u0107, \u017Ce nad \u0142a\u0144cuchami g\u00F3rskimi anomalie s\u0105 ujemne, a nad morzami dodatnie \u2013 spowodowane jest to zjawiskiem izostazji. W centralnych Alpach typowa warto\u015B\u0107 anomalii wynosi \u2013150 mGal (\u20131,5 mm/s2). Anomalie spowodowane du\u017Cymi i g\u0142\u0119boko zalegaj\u0105cymi strukturami nosz\u0105 nazw\u0119 anomalii regionalnych i rzadko stanowi\u0105 obiekt bada\u0144 \u2013 geofizyka stosowana wykorzystuje anomalie lokalne (nale\u017Cy je oddzieli\u0107 od anomalii regionalnych na drodze )."@pl . . "\uC911\uB825\uC774\uC0C1(\u91CD\u529B\u7570\u5E38, Gravity anomaly)\uC740 \uC2E4\uCE21(\u5BE6\u6E2C) \uC911\uB825\uCE58\uC640 \uC774\uB860(\u7406\u8AD6) \uC911\uB825\uCE58\uC640\uC758 \uCC28\uC774\uB97C \uAC00\uB9AC\uD0A8\uB2E4. \uC774\uB860 \uC911\uB825\uCE58\uB294 \uD45C\uC900\uC911\uB825\uC2DD(\u6A19\u6E96\u91CD\u529B\u5F0F)\uC5D0 \uC758\uD558\uC5EC \uACC4\uC0B0\uD560 \uC218 \uC788\uB2E4. \uC911\uB825\uC774\uC0C1\uC758 \uAC12\uC774 (+)\uB77C\uACE0 \uD568\uC740 \uADF8 \uADFC\uBC29\uC758 \uC9C0\uAC01\uC758 \uBC00\uB3C4\uAC00 \uD3C9\uADE0\uC0C1\uD0DC\uC5D0 \uBE44\uD574\uC11C \uD06C\uB2E4\uB294 \uB73B\uC774\uBA70, \uBC18\uB300\uB85C (-)\uB77C \uD568\uC740 \uC9C0\uAC01\uBC00\uB3C4\uAC00 \uC791\uB2E4\uB294 \uB73B\uC774\uB2E4. \uAC00\uB839 \uB192\uC740 \uC0B0\uC5D0\uC11C \uC911\uB825\uC744 \uCE21\uC815\uD558\uACE0, \uC801\uB2F9\uD55C \uBCF4\uC815(\u88DC\u6B63)\uC744 \uAC00\uD558\uC5EC \uC774\uB97C \uD574\uBA74\uC0C1\uC758 \uAC12\uC73C\uB85C \uACE0\uCE5C \uB2E4\uC74C\uC5D0 \uD574\uBA74\uC0C1\uC758 \uD45C\uC900\uC911\uB825\uC758 \uAC12\uACFC \uBE44\uAD50\uD558\uBA74 (-)\uC758 \uC911\uB825\uC774\uC0C1\uCE58\uB97C \uC5BB\uC744 \uC218 \uC788\uC73C\uBA70, \uC9C0\uAC01 \uD3C9\uD615\uC124\uC774 \uC131\uB9BD\uD568\uC744 \uC54C \uC218 \uC788\uB2E4."@ko . . . . .