"Matriu (geologia)"@ca . . . . . . "\u0627\u0644\u0641\u0631\u0634\u0629 \u0623\u0648 \u0627\u0644\u0643\u062A\u0644\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0644\u0635\u062E\u0631 \u0647\u064A \u0643\u062A\u0644\u0629 \u062F\u0642\u064A\u0642\u0629 \u0627\u0644\u062D\u0628\u064A\u0628\u0627\u062A \u0645\u0646 \u0627\u0644\u0645\u0648\u0627\u062F \u062D\u064A\u062B \u064A\u062A\u0645 \u062A\u0636\u0645\u064A\u0646 \u0627\u0644\u062D\u0628\u064A\u0628\u0627\u062A \u0627\u0644\u0643\u0628\u064A\u0631\u0629 \u0623\u0648 \u0627\u0644\u0628\u0644\u0648\u0631\u0627\u062A \u0623\u0648 \u0627\u0644\u0641\u062A\u0627\u062A. \u062A\u062A\u0643\u0648\u0646 \u0641\u0631\u0634\u0629 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0645\u0646 \u0628\u0644\u0648\u0631\u0627\u062A \u062F\u0642\u064A\u0642\u0629 \u0627\u0644\u062D\u0628\u064A\u0628\u0627\u062A\u060C \u0648\u063A\u0627\u0644\u0628\u064B\u0627 \u0645\u0627 \u062A\u0643\u0648\u0646 \u0645\u062C\u0647\u0631\u064A\u0629\u060C \u062A\u0643\u0648\u0646 \u0641\u064A\u0647\u0627 \u0628\u0644\u0648\u0631\u0627\u062A \u0623\u0643\u0628\u0631 (\u0641\u064A\u0646\u0648\u0643\u0631\u0627\u062A) \u0645\u0636\u0645\u0646\u0629. \u0647\u0630\u0627 \u0627\u0644\u0646\u0633\u064A\u062C \u0627\u0644\u0628\u0648\u0631\u0641\u064A\u0631\u064A \u064A\u062F\u0644 \u0639\u0644\u0649 \u0627\u0644\u062A\u0628\u0631\u064A\u062F \u0645\u062A\u0639\u062F\u062F \u0627\u0644\u0645\u0631\u0627\u062D\u0644 \u0645\u0646 \u0627\u0644\u0635\u0647\u0627\u0631\u0629. \u0639\u0644\u0649 \u0633\u0628\u064A\u0644 \u0627\u0644\u0645\u062B\u0627\u0644\u060C \u064A\u062D\u062A\u0648\u064A \u0623\u0646\u062F\u064A\u0633\u0627\u064A\u062A \u0627\u0644\u0628\u0648\u0631\u0641\u064A\u0631\u064A \u0639\u0644\u0649 \u0641\u064A\u0646\u0648\u0643\u0633\u062A\u0631\u0627\u062A \u0643\u0628\u064A\u0631\u0629 \u0645\u0646 \u0628\u0644\u0627\u062C\u064A\u0648\u0643\u0644\u064A\u0632 \u0641\u064A \u0641\u0631\u0634\u0629 \u062F\u0642\u064A\u0642\u0629 \u0627\u0644\u062D\u0628\u064A\u0628\u0627\u062A. \u0623\u064A\u0636\u0627 \u064A\u0633\u062A\u062E\u0631\u062C \u0627\u0644\u0645\u0627\u0633 \u063A\u0627\u0644\u0628\u0627 \u0641\u064A \u062C\u0646\u0648\u0628 \u0623\u0641\u0631\u064A\u0642\u064A\u0627 \u0645\u0646 \u0641\u0631\u0634\u0629 \u0645\u0646 \u0634\u0628\u0647 \u0627\u0644\u0635\u062E\u0631 \u0627\u0644\u0635\u0644\u0635\u0627\u0644 \u0627\u0644\u0645\u064F\u062C\u064E\u0648\u0649 (\u0627\u0644\u0643\u0645\u0628\u0631\u0644\u064A\u062A) \u064A\u0633\u0645\u0649 \u00AB\u0627\u0644\u0623\u0631\u0636 \u0627\u0644\u0635\u0641\u0631\u0627\u0621\u00BB."@ar . "\u77F3\u57FA\uFF08\u305B\u3063\u304D\u3001\u82F1: matrix \u3082\u3057\u304F\u306F groundmass\uFF09\u3068\u306F\u3001\u5CA9\u77F3\u3067\u7D30\u7C92\u304C\u56FA\u307E\u3063\u3066\u5927\u304D\u306A\u7C92\u3092\u5F62\u6210\u3057\u305F\u3001\u6C34\u6676\u3084\u7815\u5C51\u5CA9\u3092\u542B\u3080\u3082\u306E\u3067\u3042\u308B\u3002 \u706B\u6210\u5CA9\u306E\u77F3\u57FA\uFF08\u305B\u3063\u304D)\u306F\u3055\u3089\u306B\u5FAE\u5C0F\u306A\u7C92\u3092\u542B\u307F\u3001\u77F3\u82F1\u306E\u6591\u6676\uFF08phenocryst\uFF09\u304C\u542B\u307E\u308C\u3066\u3044\u308B\u3002\u3053\u306E\u6591\u5CA9\u306E\u6A21\u69D8\u306F\u30DE\u30B0\u30DE\u304C\u591A\u6BB5\u968E\u306B\u51B7\u3048\u3066\u3044\u304F\u3053\u3068\u306E\u6307\u6A19\u3067\u3042\u308B\u3002\u4F8B\u3048\u3070\u3001\u6591\u5CA9\u306E\u4E2D\u306E\u5B89\u5C71\u5CA9\u306F\u7D30\u7C92\u306E\u77F3\u57FA\u306E\u4E2D\u306B\u659C\u9577\u77F3\u306E\u5927\u304D\u306A\u6591\u6676\u3092\u6301\u3064\u3002\u5357\u30A2\u30D5\u30EA\u30AB\u5171\u548C\u56FD\u3067\u3082\u98A8\u5316\u3057\u305F\u7C98\u571F\u3092\u9271\u5E8A\u306B\u3082\u3064\u30C0\u30A4\u30E4\u30E2\u30F3\u30C9\u304C\u63A1\u6398\u3055\u308C\u308B\u3002\u3053\u306E\u9271\u5C71\u306F\u30A4\u30A8\u30ED\u30FC\u30B0\u30E9\u30A6\u30F3\u30C9\u3068\u547C\u3070\u308C\u3066\u3044\u308B\u3002 \u5806\u7A4D\u5CA9\u306E\u77F3\u57FA\u3082\u7C98\u571F\u3084\u30B7\u30EB\u30C8\u306E\u3088\u3046\u306B\u7C92\u304C\u7D30\u304B\u304F\u3001\u3088\u308A\u5927\u304D\u306A\u7C92\u3084\u7834\u7247\u5CA9\u304C\u542B\u307E\u308C\u3066\u3044\u308B\u3002\u307E\u305F\u305D\u308C\u306F\u5CA9\u77F3\u306B\u5316\u77F3\u304C\u542B\u307E\u308C\u3066\u3044\u308B\u304B\u8ABF\u3079\u308B\u3053\u3068\u306B\u3082\u4F7F\u308F\u308C\u308B\u3002"@ja . . . . . "Matriz \u00E9 a designa\u00E7\u00E3o dada em petrologia e geologia ao material intersticial de granulometria mais fina que rodeia as part\u00EDculas mais grosseiras que constituem uma rocha. A matriz pode ser composta por microcristais, material vitroso, f\u00F3sseis, seixos rolados ou minerais, entre outros materiais geol\u00F3gicos, ganhando uma acep\u00E7\u00E3o diferente consoante o tipo concreto de rocha em que se insira."@pt . . "\uAE30\uC9C8(\u57FA\u8CEA, \uC601\uC5B4: Matrix, Groundmass)\uC740 \uB354 \uD070 \uC785\uC790\uB4E4(\uACB0\uC815\uC774\uB098 \uC1C4\uC124\uC131 \uC785\uC790) \uC0AC\uC774\uB97C \uCC44\uC6B4 \uBBF8\uC138\uD55C \uC785\uC790\uC758 \uB369\uC5B4\uB9AC\uB97C \uB9D0\uD55C\uB2E4. \uC11D\uAE30(\u77F3\u57FA)\uB77C\uACE0\uB3C4 \uD55C\uB2E4. \uD654\uC131\uC554\uC758 \uAE30\uC9C8\uC740 \uC138\uB9BD\uC9C8 \uB610\uB294 \uC885\uC885 \uBBF8\uB9BD\uC9C8 \uACB0\uC815\uC774\uBA70, \uADF8 \uC548\uC5D0 \uD070 \uACB0\uC815, \uC989 \uBC18\uC815(\u6591\u6676\uC601\uC5B4: phenocryst)\uC744 \uD488\uACE0 \uC788\uB2E4. \uC774\uB7EC\uD55C \uBC18\uC554 \uC870\uC9C1\uC740 \uB9C8\uADF8\uB9C8\uAC00 \uC5EC\uB7EC \uB2E8\uACC4\uB97C \uAC70\uCCD0 \uC2DD\uC5C8\uB2E4\uB294 \uAC83\uC744 \uB73B\uD55C\uB2E4. \uC608\uB97C \uB4E4\uBA74 \uC548\uC0B0\uBC18\uC554\uC5D0\uB294 \uD070 \uC0AC\uC7A5\uC11D \uBC18\uC815\uC774 \uC138\uB9BD\uC9C8\uC758 \uAE30\uC9C8 \uC18D\uC5D0 \uB4E4\uC5B4 \uC788\uB2E4. \uB610\uD55C \uB0A8\uC544\uD504\uB9AC\uCE74 \uACF5\uD654\uAD6D\uC758 \uB2E4\uC774\uC544\uBAAC\uB4DC\uB294 \uD0B4\uBC8C\uB77C\uC774\uD2B8 \uC18D\uC5D0\uC11C \uCC44\uAD74\uB41C\uB2E4. \uD1F4\uC801\uC554\uC758 \uAE30\uC9C8\uC740 \uC9C4\uD759\uC774\uB098 \uC2E4\uD2B8\uC640 \uAC19\uC740 \uC138\uB9BD\uD654\uB41C \uD1F4\uC801\uBB3C\uC774\uBA70, \uADF8 \uC18D\uC5D0 \uB354 \uD070 \uC785\uC790\uB098 \uD30C\uD3B8\uB4E4\uC774 \uBB3B\uD78C\uB2E4. \uB610\uD55C \uD654\uC11D\uC774 \uBB3B\uD788\uAE30\uB3C4 \uD55C\uB2E4."@ko . "Matrice (g\u00E9ologie)"@fr . "Matrize (geologia)"@eu . "\u77F3\u57FA"@ja . "Matriks atau massa dasar batuan adalah massa berbutir lebih halus dari material tempat di mana kristal atau klas yang lebih besar tertanam. Matriks batuan beku terdiri dari kristal berbutir halus (sering berukuran mikroskopis) di mana kristal yang lebih besar yang tertanam. Tekstur porfiritik ini merupakan indikasi dari pendinginan magma multi-tahap. Misalnya, andesit porfiri akan memiliki fenokris plagioklas besar dalam matriks halus. Juga di Afrika Selatan, berlian sering ditambang dari matriks batuan mirip-lempung yang lapuk (kimberlit) dan sering disebut \"tanah kuning\". Matriks batuan sedimen adalah material berbutir halus, seperti tanah lempung atau lanau, di mana butir atau klas yang lebih besar tertanam. Istilah matriks pada batuan sedimen juga digunakan untuk material halus tempat fosil tertanam."@in . "1093082686"^^ . . "\u0641\u0631\u0634\u0629 (\u062C\u064A\u0648\u0644\u0648\u062C\u064A\u0627)"@ar . "\uAE30\uC9C8(\u57FA\u8CEA, \uC601\uC5B4: Matrix, Groundmass)\uC740 \uB354 \uD070 \uC785\uC790\uB4E4(\uACB0\uC815\uC774\uB098 \uC1C4\uC124\uC131 \uC785\uC790) \uC0AC\uC774\uB97C \uCC44\uC6B4 \uBBF8\uC138\uD55C \uC785\uC790\uC758 \uB369\uC5B4\uB9AC\uB97C \uB9D0\uD55C\uB2E4. \uC11D\uAE30(\u77F3\u57FA)\uB77C\uACE0\uB3C4 \uD55C\uB2E4. \uD654\uC131\uC554\uC758 \uAE30\uC9C8\uC740 \uC138\uB9BD\uC9C8 \uB610\uB294 \uC885\uC885 \uBBF8\uB9BD\uC9C8 \uACB0\uC815\uC774\uBA70, \uADF8 \uC548\uC5D0 \uD070 \uACB0\uC815, \uC989 \uBC18\uC815(\u6591\u6676\uC601\uC5B4: phenocryst)\uC744 \uD488\uACE0 \uC788\uB2E4. \uC774\uB7EC\uD55C \uBC18\uC554 \uC870\uC9C1\uC740 \uB9C8\uADF8\uB9C8\uAC00 \uC5EC\uB7EC \uB2E8\uACC4\uB97C \uAC70\uCCD0 \uC2DD\uC5C8\uB2E4\uB294 \uAC83\uC744 \uB73B\uD55C\uB2E4. \uC608\uB97C \uB4E4\uBA74 \uC548\uC0B0\uBC18\uC554\uC5D0\uB294 \uD070 \uC0AC\uC7A5\uC11D \uBC18\uC815\uC774 \uC138\uB9BD\uC9C8\uC758 \uAE30\uC9C8 \uC18D\uC5D0 \uB4E4\uC5B4 \uC788\uB2E4. \uB610\uD55C \uB0A8\uC544\uD504\uB9AC\uCE74 \uACF5\uD654\uAD6D\uC758 \uB2E4\uC774\uC544\uBAAC\uB4DC\uB294 \uD0B4\uBC8C\uB77C\uC774\uD2B8 \uC18D\uC5D0\uC11C \uCC44\uAD74\uB41C\uB2E4. \uD1F4\uC801\uC554\uC758 \uAE30\uC9C8\uC740 \uC9C4\uD759\uC774\uB098 \uC2E4\uD2B8\uC640 \uAC19\uC740 \uC138\uB9BD\uD654\uB41C \uD1F4\uC801\uBB3C\uC774\uBA70, \uADF8 \uC18D\uC5D0 \uB354 \uD070 \uC785\uC790\uB098 \uD30C\uD3B8\uB4E4\uC774 \uBB3B\uD78C\uB2E4. \uB610\uD55C \uD654\uC11D\uC774 \uBB3B\uD788\uAE30\uB3C4 \uD55C\uB2E4."@ko . . "La matrico, a\u016D grundomaso, de \"perfajraj\" rokoj konsistas el fajngrajnaj kristaloj, en kiu pligrandaj kristaloj estas enka\u015Ditaj. \u0108i tio indikas multstadian malvarmadon de la magmo. En Sudafriko, diamantoj ofte estas ekstraktataj el matrico de argila roko (kimberlito) nomita \"flava grundo\"."@eo . "\u0627\u0644\u0641\u0631\u0634\u0629 \u0623\u0648 \u0627\u0644\u0643\u062A\u0644\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0644\u0635\u062E\u0631 \u0647\u064A \u0643\u062A\u0644\u0629 \u062F\u0642\u064A\u0642\u0629 \u0627\u0644\u062D\u0628\u064A\u0628\u0627\u062A \u0645\u0646 \u0627\u0644\u0645\u0648\u0627\u062F \u062D\u064A\u062B \u064A\u062A\u0645 \u062A\u0636\u0645\u064A\u0646 \u0627\u0644\u062D\u0628\u064A\u0628\u0627\u062A \u0627\u0644\u0643\u0628\u064A\u0631\u0629 \u0623\u0648 \u0627\u0644\u0628\u0644\u0648\u0631\u0627\u062A \u0623\u0648 \u0627\u0644\u0641\u062A\u0627\u062A. \u062A\u062A\u0643\u0648\u0646 \u0641\u0631\u0634\u0629 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0645\u0646 \u0628\u0644\u0648\u0631\u0627\u062A \u062F\u0642\u064A\u0642\u0629 \u0627\u0644\u062D\u0628\u064A\u0628\u0627\u062A\u060C \u0648\u063A\u0627\u0644\u0628\u064B\u0627 \u0645\u0627 \u062A\u0643\u0648\u0646 \u0645\u062C\u0647\u0631\u064A\u0629\u060C \u062A\u0643\u0648\u0646 \u0641\u064A\u0647\u0627 \u0628\u0644\u0648\u0631\u0627\u062A \u0623\u0643\u0628\u0631 (\u0641\u064A\u0646\u0648\u0643\u0631\u0627\u062A) \u0645\u0636\u0645\u0646\u0629. \u0647\u0630\u0627 \u0627\u0644\u0646\u0633\u064A\u062C \u0627\u0644\u0628\u0648\u0631\u0641\u064A\u0631\u064A \u064A\u062F\u0644 \u0639\u0644\u0649 \u0627\u0644\u062A\u0628\u0631\u064A\u062F \u0645\u062A\u0639\u062F\u062F \u0627\u0644\u0645\u0631\u0627\u062D\u0644 \u0645\u0646 \u0627\u0644\u0635\u0647\u0627\u0631\u0629. \u0639\u0644\u0649 \u0633\u0628\u064A\u0644 \u0627\u0644\u0645\u062B\u0627\u0644\u060C \u064A\u062D\u062A\u0648\u064A \u0623\u0646\u062F\u064A\u0633\u0627\u064A\u062A \u0627\u0644\u0628\u0648\u0631\u0641\u064A\u0631\u064A \u0639\u0644\u0649 \u0641\u064A\u0646\u0648\u0643\u0633\u062A\u0631\u0627\u062A \u0643\u0628\u064A\u0631\u0629 \u0645\u0646 \u0628\u0644\u0627\u062C\u064A\u0648\u0643\u0644\u064A\u0632 \u0641\u064A \u0641\u0631\u0634\u0629 \u062F\u0642\u064A\u0642\u0629 \u0627\u0644\u062D\u0628\u064A\u0628\u0627\u062A. \u0623\u064A\u0636\u0627 \u064A\u0633\u062A\u062E\u0631\u062C \u0627\u0644\u0645\u0627\u0633 \u063A\u0627\u0644\u0628\u0627 \u0641\u064A \u062C\u0646\u0648\u0628 \u0623\u0641\u0631\u064A\u0642\u064A\u0627 \u0645\u0646 \u0641\u0631\u0634\u0629 \u0645\u0646 \u0634\u0628\u0647 \u0627\u0644\u0635\u062E\u0631 \u0627\u0644\u0635\u0644\u0635\u0627\u0644 \u0627\u0644\u0645\u064F\u062C\u064E\u0648\u0649 (\u0627\u0644\u0643\u0645\u0628\u0631\u0644\u064A\u062A) \u064A\u0633\u0645\u0649 \u00AB\u0627\u0644\u0623\u0631\u0636 \u0627\u0644\u0635\u0641\u0631\u0627\u0621\u00BB. \u0641\u0631\u0634\u0629 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0631\u0633\u0648\u0628\u064A\u0629 \u0647\u064A \u0645\u0627\u062F\u0629 \u0631\u0633\u0648\u0628\u064A\u0629 \u0630\u0627\u062A \u062D\u0628\u064A\u0628\u0627\u062A \u062F\u0642\u064A\u0642\u0629\u060C \u0645\u062B\u0644 \u0627\u0644\u0635\u0644\u0635\u0627\u0644 \u0623\u0648 \u0627\u0644\u0637\u0645\u064A\u060C \u062D\u064A\u062B \u064A\u062A\u0645 \u062A\u0636\u0645\u064A\u0646 \u0627\u0644\u0641\u062A\u0627\u062A \u0623\u0648 \u0627\u0644\u062D\u0628\u064A\u0628\u0627\u062A \u0627\u0644\u0643\u0628\u064A\u0631\u0629. \u0643\u0645\u0627 \u0623\u0646\u0647\u0627 \u062A\u0633\u062A\u062E\u062F\u0645 \u0644\u0648\u0635\u0641 \u0627\u0644\u0645\u0648\u0627\u062F \u0627\u0644\u0635\u062E\u0631\u064A\u0629 \u0627\u0644\u062A\u064A \u062A\u062A\u0636\u0645\u0646 \u0627\u0644\u0623\u062D\u0641\u0648\u0631\u064A\u0627\u062A."@ar . . . "The matrix or groundmass of a rock is the finer-grained mass of material in which larger grains, crystals, or clasts are embedded. The matrix of an igneous rock consists of finer-grained, often microscopic, crystals in which larger crystals, called phenocrysts, are embedded. This porphyritic texture is indicative of multi-stage cooling of magma. For example, porphyritic andesite will have large phenocrysts of plagioclase in a fine-grained matrix. Also in South Africa, diamonds are often mined from a matrix of weathered clay-like rock (kimberlite) called \"yellow ground\"."@en . "Als Matrix wird in der Petrographie allgemein die relativ feink\u00F6rnige Grundmasse eines Gesteins bezeichnet, von der deutlich grobk\u00F6rnigere Gesteinsbestandteile unterscheidbar sind. F\u00FCr den Begriff Matrix im petrographischen Sinn existieren verschiedene spezielle Definitionen, deren G\u00FCltigkeit u. a. davon abh\u00E4ngt, welche Art von Gestein betrachtet wird."@de . . . . . "Met matrix wordt in de geologie, en met name in de sedimentologie en petrologie, bedoeld: \"de fijnkorrelige of fijnkristallijne grondmassa van een gesteente die de ruimte tussen de korrels of kristallen opvult\"."@nl . "Als Matrix wird in der Petrographie allgemein die relativ feink\u00F6rnige Grundmasse eines Gesteins bezeichnet, von der deutlich grobk\u00F6rnigere Gesteinsbestandteile unterscheidbar sind. F\u00FCr den Begriff Matrix im petrographischen Sinn existieren verschiedene spezielle Definitionen, deren G\u00FCltigkeit u. a. davon abh\u00E4ngt, welche Art von Gestein betrachtet wird."@de . . "Matriz \u00E9 a designa\u00E7\u00E3o dada em petrologia e geologia ao material intersticial de granulometria mais fina que rodeia as part\u00EDculas mais grosseiras que constituem uma rocha. A matriz pode ser composta por microcristais, material vitroso, f\u00F3sseis, seixos rolados ou minerais, entre outros materiais geol\u00F3gicos, ganhando uma acep\u00E7\u00E3o diferente consoante o tipo concreto de rocha em que se insira."@pt . . . . "Matrix (Geologie)"@de . "\u77F3\u57FA\uFF08\u305B\u3063\u304D\u3001\u82F1: matrix \u3082\u3057\u304F\u306F groundmass\uFF09\u3068\u306F\u3001\u5CA9\u77F3\u3067\u7D30\u7C92\u304C\u56FA\u307E\u3063\u3066\u5927\u304D\u306A\u7C92\u3092\u5F62\u6210\u3057\u305F\u3001\u6C34\u6676\u3084\u7815\u5C51\u5CA9\u3092\u542B\u3080\u3082\u306E\u3067\u3042\u308B\u3002 \u706B\u6210\u5CA9\u306E\u77F3\u57FA\uFF08\u305B\u3063\u304D)\u306F\u3055\u3089\u306B\u5FAE\u5C0F\u306A\u7C92\u3092\u542B\u307F\u3001\u77F3\u82F1\u306E\u6591\u6676\uFF08phenocryst\uFF09\u304C\u542B\u307E\u308C\u3066\u3044\u308B\u3002\u3053\u306E\u6591\u5CA9\u306E\u6A21\u69D8\u306F\u30DE\u30B0\u30DE\u304C\u591A\u6BB5\u968E\u306B\u51B7\u3048\u3066\u3044\u304F\u3053\u3068\u306E\u6307\u6A19\u3067\u3042\u308B\u3002\u4F8B\u3048\u3070\u3001\u6591\u5CA9\u306E\u4E2D\u306E\u5B89\u5C71\u5CA9\u306F\u7D30\u7C92\u306E\u77F3\u57FA\u306E\u4E2D\u306B\u659C\u9577\u77F3\u306E\u5927\u304D\u306A\u6591\u6676\u3092\u6301\u3064\u3002\u5357\u30A2\u30D5\u30EA\u30AB\u5171\u548C\u56FD\u3067\u3082\u98A8\u5316\u3057\u305F\u7C98\u571F\u3092\u9271\u5E8A\u306B\u3082\u3064\u30C0\u30A4\u30E4\u30E2\u30F3\u30C9\u304C\u63A1\u6398\u3055\u308C\u308B\u3002\u3053\u306E\u9271\u5C71\u306F\u30A4\u30A8\u30ED\u30FC\u30B0\u30E9\u30A6\u30F3\u30C9\u3068\u547C\u3070\u308C\u3066\u3044\u308B\u3002 \u5806\u7A4D\u5CA9\u306E\u77F3\u57FA\u3082\u7C98\u571F\u3084\u30B7\u30EB\u30C8\u306E\u3088\u3046\u306B\u7C92\u304C\u7D30\u304B\u304F\u3001\u3088\u308A\u5927\u304D\u306A\u7C92\u3084\u7834\u7247\u5CA9\u304C\u542B\u307E\u308C\u3066\u3044\u308B\u3002\u307E\u305F\u305D\u308C\u306F\u5CA9\u77F3\u306B\u5316\u77F3\u304C\u542B\u307E\u308C\u3066\u3044\u308B\u304B\u8ABF\u3079\u308B\u3053\u3068\u306B\u3082\u4F7F\u308F\u308C\u308B\u3002"@ja . . "Geologian, matrizea partikula oso finez osatutako sedimentuari deitzen zaio, basa tamainako partikulez osatuta dagoen sedimentuari hain zuzen. Sarritan, arroketan, trama edo partikula handiagoen artean kokatzen da."@eu . "En p\u00E9trologie, la matrice d'une roche composite est le mat\u00E9riau, constitu\u00E9 de petits grains, qui englobe des grains de plus grosse taille. \n* Dans les kimberlites par exemple, les diamants sont extraits d'une matrice de terre argileuse appel\u00E9e \u00AB roche jaune \u00BB. \n* Dans une roche s\u00E9dimentaire, la matrice correspond \u00E0 la fraction du s\u00E9diment aux grains les plus fins, souvent de nature argileuse. Il ne faut pas la confondre avec le ciment, un mat\u00E9riel (quartz ou calcite, notamment) pr\u00E9cipit\u00E9 et cristallis\u00E9 entre les grains apr\u00E8s leur s\u00E9dimentation (la matrice, elle, est syns\u00E9dimentaire). \n* Dans une chondrite (m\u00E9t\u00E9orite indiff\u00E9renci\u00E9e), la matrice est l'ensemble du mat\u00E9riau qui entoure les chondres et les inclusions (notamment les CAI)."@fr . . "Met matrix wordt in de geologie, en met name in de sedimentologie en petrologie, bedoeld: \"de fijnkorrelige of fijnkristallijne grondmassa van een gesteente die de ruimte tussen de korrels of kristallen opvult\"."@nl . . "Z\u00E1kladn\u00ED hmota (geologie) je n\u00E1zev, kter\u00FDm se ozna\u010Duje jemnozrnn\u00E1 a\u017E sklovit\u00E1 hmota mezi vyrostlicemi v porfyrick\u00FDch struktur\u00E1ch vyv\u0159el\u00FDch hornin. Je tvo\u0159ena miner\u00E1ly men\u0161\u00EDch rozm\u011Br\u016F. M\u016F\u017Ee b\u00FDt holokrystalick\u00E1, hemikrystalick\u00E1 nebo sklovit\u00E1. U metamorfit\u016F se pou\u017E\u00EDv\u00E1 tak\u00E9 term\u00EDn z\u00E1kladn\u00ED osnova nebo z\u00E1kladn\u00ED tk\u00E1\u0148. U sediment\u016F je to prim\u00E1rn\u00ED jemnozrnn\u00E1 slo\u017Eka (nap\u0159\u00EDklad j\u00EDl), kter\u00E1 uzav\u00EDr\u00E1 hrub\u0161\u00ED \u010D\u00E1stice. Jako synonymum pro z\u00E1kladn\u00ED hmotu se tak\u00E9 u\u017E\u00EDv\u00E1 slovo matrix."@cs . . . . . "Matrix (\u00E4ven grundmassa och mellanmassa) \u00E4r den fyllnadsmassa som omger mineralkorn, fossil och liknande i en bergart. N\u00E4r Carl von Linn\u00E9 i sina ungdomsskrifter studerade gruvor och bergarter, dokumenterade han \u00E4ven vilket matrix som omger dessa."@sv . . . . . . "Matriz (geolog\u00EDa)"@es . "La matrice \u00E8 materiale granulare di dimensione fangosa che tiene uniti tra loro i grani in una roccia sedimentaria. \u00C8 fango (termine generico per indicare sedimento sciolto delle dimensioni di silt e argilla) al sotto i 63 micron (limite massimo granulometrico del silt). Se si tratta di materiale carbonatico si parla di fino ai 63 micron e di in senso stretto sotto i 4 micron. Una importante distinzione va fatta con il cemento: si riserva infatti tale termine a materiale granulare che tiene insieme i grani di una roccia sedimentaria, che sia per\u00F2 di origine post-deposizionale; la matrice invece \u00E8 il risultato di un evento sin-deposizionale (cio\u00E8 contemporaneo alla deposizione dei grani). Per quanto riguarda la matrice carbonatica, essa pu\u00F2 avere origine organica o inorganica (chimico-fisica). Quella organica \u00E8 causata principalmente dall'azione delle alghe verdi che morendo vanno a formare il fango, quella inorganica \u00E8 dovuta a una liberazione di anidride carbonica (CO2) che favorisce precipitazione di carbonato di calcio (CaCO3) e dalla bioerosione. Ci sono cinque possibili modi di formazione: 1. \n* produzione di aghi aragonitici per diretta precipitazione da acque ad alta salinit\u00E0 soprasature in CaCO3; 2. \n* produzione di aghi aragonitici per disintegrazione post-mortem di alghe verdi calcificate; 3. \n* produzione di fine detrito scheletrico per frammentazione meccanica in ambienti agitati; 4. \n* produzione di fango scheletrico attraverso processi biologici; 5. \n* produzione di melme scheletriche per decantazione di minutissimi organismi planctonici."@it . "Matrice (geologia)"@it . . "Matriks (geologi)"@in . . "La matrico, a\u016D grundomaso, de \"perfajraj\" rokoj konsistas el fajngrajnaj kristaloj, en kiu pligrandaj kristaloj estas enka\u015Ditaj. \u0108i tio indikas multstadian malvarmadon de la magmo. En Sudafriko, diamantoj ofte estas ekstraktataj el matrico de argila roko (kimberlito) nomita \"flava grundo\"."@eo . . . "Matrico mineralogia"@eo . "La matrice \u00E8 materiale granulare di dimensione fangosa che tiene uniti tra loro i grani in una roccia sedimentaria. \u00C8 fango (termine generico per indicare sedimento sciolto delle dimensioni di silt e argilla) al sotto i 63 micron (limite massimo granulometrico del silt). Se si tratta di materiale carbonatico si parla di fino ai 63 micron e di in senso stretto sotto i 4 micron. Una importante distinzione va fatta con il cemento: si riserva infatti tale termine a materiale granulare che tiene insieme i grani di una roccia sedimentaria, che sia per\u00F2 di origine post-deposizionale; la matrice invece \u00E8 il risultato di un evento sin-deposizionale (cio\u00E8 contemporaneo alla deposizione dei grani)."@it . . . . . . "Matrix (geology)"@en . . . . . "\u57FA\u8D28 (\u5730\u8D28)"@zh . . "752377"^^ . . "The matrix or groundmass of a rock is the finer-grained mass of material in which larger grains, crystals, or clasts are embedded. The matrix of an igneous rock consists of finer-grained, often microscopic, crystals in which larger crystals, called phenocrysts, are embedded. This porphyritic texture is indicative of multi-stage cooling of magma. For example, porphyritic andesite will have large phenocrysts of plagioclase in a fine-grained matrix. Also in South Africa, diamonds are often mined from a matrix of weathered clay-like rock (kimberlite) called \"yellow ground\". The matrix of sedimentary rocks is finer-grained sedimentary material, such as clay or silt, in which larger grains or clasts are embedded. It is also used to describe the rock material in which a fossil is embedded."@en . "En p\u00E9trologie, la matrice d'une roche composite est le mat\u00E9riau, constitu\u00E9 de petits grains, qui englobe des grains de plus grosse taille. \n* Dans les kimberlites par exemple, les diamants sont extraits d'une matrice de terre argileuse appel\u00E9e \u00AB roche jaune \u00BB. \n* Dans une roche s\u00E9dimentaire, la matrice correspond \u00E0 la fraction du s\u00E9diment aux grains les plus fins, souvent de nature argileuse. Il ne faut pas la confondre avec le ciment, un mat\u00E9riel (quartz ou calcite, notamment) pr\u00E9cipit\u00E9 et cristallis\u00E9 entre les grains apr\u00E8s leur s\u00E9dimentation (la matrice, elle, est syns\u00E9dimentaire). \n* Dans une chondrite (m\u00E9t\u00E9orite indiff\u00E9renci\u00E9e), la matrice est l'ensemble du mat\u00E9riau qui entoure les chondres et les inclusions (notamment les CAI)."@fr . "Geologian, matrizea partikula oso finez osatutako sedimentuari deitzen zaio, basa tamainako partikulez osatuta dagoen sedimentuari hain zuzen. Sarritan, arroketan, trama edo partikula handiagoen artean kokatzen da."@eu . . "4557"^^ . . . "Z\u00E1kladn\u00ED hmota (geologie) je n\u00E1zev, kter\u00FDm se ozna\u010Duje jemnozrnn\u00E1 a\u017E sklovit\u00E1 hmota mezi vyrostlicemi v porfyrick\u00FDch struktur\u00E1ch vyv\u0159el\u00FDch hornin. Je tvo\u0159ena miner\u00E1ly men\u0161\u00EDch rozm\u011Br\u016F. M\u016F\u017Ee b\u00FDt holokrystalick\u00E1, hemikrystalick\u00E1 nebo sklovit\u00E1. U metamorfit\u016F se pou\u017E\u00EDv\u00E1 tak\u00E9 term\u00EDn z\u00E1kladn\u00ED osnova nebo z\u00E1kladn\u00ED tk\u00E1\u0148. U sediment\u016F je to prim\u00E1rn\u00ED jemnozrnn\u00E1 slo\u017Eka (nap\u0159\u00EDklad j\u00EDl), kter\u00E1 uzav\u00EDr\u00E1 hrub\u0161\u00ED \u010D\u00E1stice. Jako synonymum pro z\u00E1kladn\u00ED hmotu se tak\u00E9 u\u017E\u00EDv\u00E1 slovo matrix."@cs . "Matrix (geologi)"@sv . . "En la geolog\u00EDa la matriz es el material de grano fino de una roca en el que se incluyen otros mayores, que constituyen el esqueleto o f\u00E1brica. La matriz puede estar compuesta de part\u00EDculas de arcilla o fragmentos de minerales, rocas o f\u00F3siles.\u200B Se distingue del cemento en que este \u00FAltimo est\u00E1 formado por cristales de minerales que han crecido o recrecido in situ, rellenando los huecos de la roca, en ocasiones obliterando la textura original."@es . . . "\u57FA\u8D28\uFF08\u82F1\u8BED\uFF1Amatrix\u6216groundmass\uFF09\u662F\u6DF7\u6742\u5728\u8F83\u5927\u5CA9\u77F3\u9897\u7C92\uFF08\u79F0\u4E3A\u201C\u6591\u6676\u201D\uFF09\u548C\u6676\u4F53\u4E2D\u7684\u7EC6\u5C0F\u9897\u7C92\u3002\u4E5F\u79F0\u77F3\u57FA\u3002 \u5982\u679C\u77F3\u57FA\u4E3A\u8089\u773C\u53EF\u8FA8\u7684\u663E\u6676\u8D28\uFF0C\u5219\u79F0\u4E3A\u4F3C\u6591\u72B6\u7ED3\u6784\u3002\u6591\u72B6\u7ED3\u6784\u7684\u5F62\u6210\uFF0C\u662F\u7531\u4E8E\u5CA9\u6D46\u5728\u5730\u7403\u6DF1\u5904\u6709\u4E00\u90E8\u5206\u5148\u7ED3\u6676\u800C\u5F62\u6210\u6591\u6676\uFF0C\u4EE5\u540E\u5CA9\u6D46\u7EE7\u7EED\u4E0A\u5347\uFF0C\u7531\u4E8E\u51B7\u5374\u5F88\u5FEB\uFF0C\u5CA9\u6D46\u6765\u4E0D\u53CA\u7ED3\u6676\u6216\u7ED3\u6676\u5F97\u5F88\u5C0F\uFF0C\u4ECE\u800C\u5F62\u6210\u77F3\u57FA\u3002\u6591\u72B6\u7ED3\u6784\u591A\u4EA7\u751F\u5728\u6D45\u6210\u4FB5\u5165\u5CA9\u4E2D\u3002"@zh . "En la geolog\u00EDa la matriz es el material de grano fino de una roca en el que se incluyen otros mayores, que constituyen el esqueleto o f\u00E1brica. La matriz puede estar compuesta de part\u00EDculas de arcilla o fragmentos de minerales, rocas o f\u00F3siles.\u200B Se distingue del cemento en que este \u00FAltimo est\u00E1 formado por cristales de minerales que han crecido o recrecido in situ, rellenando los huecos de la roca, en ocasiones obliterando la textura original."@es . . . . . . "\uAE30\uC9C8 (\uC9C0\uC9C8\uD559)"@ko . . . . . . . "\u57FA\u8D28\uFF08\u82F1\u8BED\uFF1Amatrix\u6216groundmass\uFF09\u662F\u6DF7\u6742\u5728\u8F83\u5927\u5CA9\u77F3\u9897\u7C92\uFF08\u79F0\u4E3A\u201C\u6591\u6676\u201D\uFF09\u548C\u6676\u4F53\u4E2D\u7684\u7EC6\u5C0F\u9897\u7C92\u3002\u4E5F\u79F0\u77F3\u57FA\u3002 \u5982\u679C\u77F3\u57FA\u4E3A\u8089\u773C\u53EF\u8FA8\u7684\u663E\u6676\u8D28\uFF0C\u5219\u79F0\u4E3A\u4F3C\u6591\u72B6\u7ED3\u6784\u3002\u6591\u72B6\u7ED3\u6784\u7684\u5F62\u6210\uFF0C\u662F\u7531\u4E8E\u5CA9\u6D46\u5728\u5730\u7403\u6DF1\u5904\u6709\u4E00\u90E8\u5206\u5148\u7ED3\u6676\u800C\u5F62\u6210\u6591\u6676\uFF0C\u4EE5\u540E\u5CA9\u6D46\u7EE7\u7EED\u4E0A\u5347\uFF0C\u7531\u4E8E\u51B7\u5374\u5F88\u5FEB\uFF0C\u5CA9\u6D46\u6765\u4E0D\u53CA\u7ED3\u6676\u6216\u7ED3\u6676\u5F97\u5F88\u5C0F\uFF0C\u4ECE\u800C\u5F62\u6210\u77F3\u57FA\u3002\u6591\u72B6\u7ED3\u6784\u591A\u4EA7\u751F\u5728\u6D45\u6210\u4FB5\u5165\u5CA9\u4E2D\u3002"@zh . . . "La matriu d'una roca \u00E9s la massa de material de gra m\u00E9s fi en la qual els grans m\u00E9s grossos, cristalls o clasts estan integrats. La matriu d'una roca \u00EDgnia consta de cristalls de gra fi sovint microsc\u00F2pics en la qual els cristalls m\u00E9s grossos (fenocristalls) estan integrats. Aquesta textura p\u00F2rfiritica indica un refredament en molts estadis del magma. Per exemple l'andesita porfir\u00EDtica tindr\u00E0 grans fenocristalls de plagioclasa en una matriu de gra fi. Tamb\u00E9 a \u00C0frica del Sud els diamants sovint s'extreuen d'una matriu meteoritzada d la roca similar a l'argila anomenada kimberlita altrament dita \"yellow ground\". La matriu de les roques sediment\u00E0ries \u00E9s un material de gra m\u00E9s fi, com l'argila o el llim, en la qual s'integren grans m\u00E9s grossos o clasts. Tamb\u00E9 es fa servir el nom de matriu per descriure la roca on s'integren els f\u00F2ssils."@ca . . "Matrix (geologie)"@nl . "Z\u00E1kladn\u00ED hmota (geologie)"@cs . . . "Matriz (geologia)"@pt . . "Matrix (\u00E4ven grundmassa och mellanmassa) \u00E4r den fyllnadsmassa som omger mineralkorn, fossil och liknande i en bergart. N\u00E4r Carl von Linn\u00E9 i sina ungdomsskrifter studerade gruvor och bergarter, dokumenterade han \u00E4ven vilket matrix som omger dessa."@sv . . "La matriu d'una roca \u00E9s la massa de material de gra m\u00E9s fi en la qual els grans m\u00E9s grossos, cristalls o clasts estan integrats. La matriu d'una roca \u00EDgnia consta de cristalls de gra fi sovint microsc\u00F2pics en la qual els cristalls m\u00E9s grossos (fenocristalls) estan integrats. Aquesta textura p\u00F2rfiritica indica un refredament en molts estadis del magma. Per exemple l'andesita porfir\u00EDtica tindr\u00E0 grans fenocristalls de plagioclasa en una matriu de gra fi. Tamb\u00E9 a \u00C0frica del Sud els diamants sovint s'extreuen d'una matriu meteoritzada d la roca similar a l'argila anomenada kimberlita altrament dita \"yellow ground\"."@ca . "Matriks atau massa dasar batuan adalah massa berbutir lebih halus dari material tempat di mana kristal atau klas yang lebih besar tertanam. Matriks batuan beku terdiri dari kristal berbutir halus (sering berukuran mikroskopis) di mana kristal yang lebih besar yang tertanam. Tekstur porfiritik ini merupakan indikasi dari pendinginan magma multi-tahap. Misalnya, andesit porfiri akan memiliki fenokris plagioklas besar dalam matriks halus. Juga di Afrika Selatan, berlian sering ditambang dari matriks batuan mirip-lempung yang lapuk (kimberlit) dan sering disebut \"tanah kuning\". Matriks batuan sedimen adalah material berbutir halus, seperti tanah lempung atau lanau, di mana butir atau klas yang lebih besar tertanam. Istilah matriks pada batuan sedimen juga digunakan untuk material halus temp"@in . .