"Fosforit \u00E4r en kolloidal form av apatit i tr\u00E5daktig till t\u00E4t, ofta jordartad form med vit-, gul-, brun- eller gr\u00E5aktig f\u00E4rg. Den f\u00F6rekommer dels i lagerformade massor av st\u00F6rre utstr\u00E4ckning, dels som st\u00F6rre eller mindre klumpar i lera eller sand, och ibland som tillf\u00E4lliga best\u00E5ndsdelar i andra bergarter. Fosforit \u00E4r den enda bergartsbildande fosfaten, f\u00F6rmodligen en g\u00E5ng bildad som rester efter djur."@sv . . . . . . "1117463086"^^ . . . . . . . . . . . . . . . . . . . . . . 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"Fosforito"@eo . "\uC778\uAD11\uC11D(\u71D0\u945B\u77F3, phosphate rock)\uC740 \uC778\uD68C\uC11D(Apatite)\uC744 \uD568\uC720\uD558\uB294 \uC554\uC11D\uC73C\uB85C \uC0DD\uD654\uD559 \uAE30\uC6D0\uC758 \uD1F4\uC801\uC554\uC774\uB2E4. \uB530\uB77C\uC11C \uC778\uAD11\uC11D\uC740 \uB2E4\uB978 \uAD11\uBB3C\uACFC \uAC19\uC774 \uD654\uD559\uC870\uC131\uC73C\uB85C \uD45C\uC2DC\uD560 \uC218 \uC5C6\uB2E4. \uC778\uD68C\uC11D\uC740 \uD654\uC131\uC554 \uAE30\uC6D0\uC73C\uB85C \uB9E5\uC0C1\uC73C\uB85C \uB098\uD0C0\uB098\uBA70, \uC778\uAD11\uC11D\uC740 \uC720\uAE30\uBB3C\uC774 \uD1F4\uC801\uB418\uC5B4 \uB098\uD0C0\uB098\uB294 2\uCC28 \uAD11\uC0C1\uC73C\uB85C \uC778(P2O5)\uC744 18%\u223C40% \uD568\uC720\uD55C\uB2E4. \uC778\uD68C\uC11D\uACFC \uC778\uAD11\uC11D\uC740 \uC778\uC758 \uD568\uB7C9\uC5D0 \uB530\uB77C \uAD11\uBB3C \uAC00\uCE58\uAC00 \uACB0\uC815\uB418\uBA70 \uC8FC\uB85C \uBE44\uB8CC\uC6D0\uB8CC\uB85C \uB9CE\uC774 \uC0AC\uC6A9\uB41C\uB2E4. \uC774 \uBC16\uC5D0 \uC778\uD68C\uC11D\uC740 \uC778\uC0B0\uC81C\uC870, \uC758\uC57D\uD488, \uBC18\uB3C4\uCCB4, \uC138\uB77C\uBBF9, \uC2E4\uD06C, \uC12C\uC720, \uBC29\uCDA9\uC81C, \uC124\uD0D5 \uC815\uB828, \uD3ED\uC57D \uB4F1\uC5D0\uB3C4 \uC0AC\uC6A9\uB418\uACE0 \uC788\uB2E4. \uC778\uC758 \uC21C\uB3C4\uAC00 \uB0AE\uC740 \uACBD\uC6B0\uC5D0\uB294 \uD488\uC704\uB97C \uB192\uC5EC\uC8FC\uB294 \uC120\uAD11 \uC791\uC5C5\uC744 \uAC70\uCCD0 \uC0AC\uC6A9\uD55C\uB2E4. \uC778\uC0B0\uC774\uB098 \uBE44\uB8CC\uC6A9\uC73C\uB85C \uC0AC\uC6A9\uD558\uB294 \uC778\uD68C\uC11D(\uC778\uAD11\uC11D \uD3EC\uD568)\uC740 \uC778\uC774 30%\uC774\uC0C1 \uD568\uC720\uB418\uC5B4\uC57C \uD55C\uB2E4. \uC778\uAD11\uC11D\uC758 \uD488\uC9C8\uAE30\uC900\uC5D0\uB294 \uC0C1\uC5C5\uC801\uC73C\uB85C BPL(Bone Phosphate of Lime)\uC774\uB77C\uB294 \uB2E8\uC704\uAC00 \uC0AC\uC6A9\uB41C\uB2E4."@ko . . "Phosphorit ist ein marines Sedimentgestein, das schichtgebunden mit anderen marinen Gesteinen, meistens mit Kalken auftritt."@de . . "La fosforita es una roca sedimentaria no detr\u00EDtica que contiene altas cantidades de minerales fosfatados. El contenido en fosfatos es por lo menos de entre un 15 y un 20 %, un incremento importante respecto a una roca sedimentaria t\u00EDpica que contiene menos de un 0,2 %.\u200B El fosfato est\u00E1 presente como fluorapatita, Ca5(PO4)3F, t\u00EDpico en masas criptocristalinas (tama\u00F1os de grano <1 \u03BCm).\u200B Tambi\u00E9n est\u00E1 presente en forma de hidroxiapatita, Ca5(PO4)3OH, que a menudo se disuelve por huesos de animales vertebrados. Tambi\u00E9n se encuentran disueltos en rocas \u00EDgneas y metam\u00F3rficas. A menudo se dan dep\u00F3sitos de fosforita en capas extensas, que en conjunto cubren decenas de miles de kil\u00F3metros cuadrados de la corteza terrestre.\u200B"@es . . . "\uC778\uAD11\uC11D"@ko . . . . "\u0424\u043E\u0441\u0444\u043E\u0440\u0438\u0442\u0438 \u2014 \u043E\u0441\u0430\u0434\u043E\u0432\u0430 \u0433\u0456\u0440\u0441\u044C\u043A\u0430 \u043F\u043E\u0440\u043E\u0434\u0430 \u043C\u043E\u0440\u0441\u044C\u043A\u043E\u0433\u043E \u043F\u043E\u0445\u043E\u0434\u0436\u0435\u043D\u043D\u044F, \u0441\u0444\u043E\u0440\u043C\u043E\u0432\u0430\u043D\u0430 \u0433\u043E\u043B\u043E\u0432\u043D\u0438\u043C \u0447\u0438\u043D\u043E\u043C \u0437 \u0444\u043E\u0441\u0444\u0430\u0442\u0443 \u043A\u0430\u043B\u044C\u0446\u0456\u044E (Ca3(PO4)2), \u0430 \u0442\u0430\u043A\u043E\u0436 \u043A\u0432\u0430\u0440\u0446\u0443, \u043A\u0430\u043B\u044C\u0446\u0438\u0442\u0443, \u0434\u043E\u043B\u043E\u043C\u0456\u0442\u0443, \u0445\u0430\u043B\u0446\u0435\u0434\u043E\u043D\u0443, \u0491\u043B\u0430\u0443\u043A\u043E\u043D\u0456\u0442\u0443, \u043A\u0430\u0440\u0431\u043E\u043D\u0430\u0442\u0456\u0432, \u0433\u0456\u0434\u0440\u0430\u0442\u0456\u0432, \u043E\u043A\u0441\u0438\u0434\u0456\u0432 \u0437\u0430\u043B\u0456\u0437\u0430 \u0456 \u0442.\u0456\u043D., \u0434\u0440\u0443\u0433\u043E\u0440\u044F\u0434\u043D\u0438\u0445 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432 \u2014 \u0433\u043B\u0438\u043D\u0438\u0441\u0442\u0438\u0445, \u0430\u043B\u044E\u043C\u043E\u0441\u0438\u043B\u0456\u043A\u0430\u0442\u0456\u0432, \u043F\u0456\u0440\u0438\u0442\u0443, \u0433\u0456\u0434\u0440\u043E\u043A\u0441\u0438\u0434\u0456\u0432 \u0437\u0430\u043B\u0456\u0437\u0430 \u0442\u0430 \u043E\u0440\u0433\u0430\u043D\u0456\u0447\u043D\u043E\u0457 \u0440\u0435\u0447\u043E\u0432\u0438\u043D\u0438, \u0437\u0446\u0435\u043C\u0435\u043D\u0442\u043E\u0432\u0430\u043D\u0438\u0445 \u0444\u043E\u0441\u0444\u0430\u0442\u043E\u043C \u043A\u0430\u043B\u044C\u0446\u0456\u044E \u0430\u0431\u043E \u0437\u0431\u0430\u0433\u0430\u0447\u0435\u043D\u0438\u0445 \u0441\u043A\u0443\u043F\u0447\u0435\u043D\u043D\u044F\u043C \u0436\u043E\u0432\u0435\u043D \u0447\u0438 \u043E\u043E\u043B\u0456\u0442\u0456\u0432."@uk . . . . . . . "\u0635\u062E\u0631 \u0627\u0644\u0641\u0648\u0633\u0641\u0648\u0631\u064A\u062A (\u0648\u0627\u0644\u0630\u064A \u064A\u0633\u0645\u0649 \u0623\u064A\u0636\u0627\u064B \u0635\u062E\u0631 \u0627\u0644\u0641\u0648\u0633\u0641\u0627\u062A) \u0647\u0648 \u0646\u0648\u0639 \u0645\u0646 \u0623\u0646\u0648\u0627\u0639 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0631\u0633\u0648\u0628\u064A\u0629 \u063A\u064A\u0631 \u0627\u0644\u0645\u062A\u0641\u062A\u062A\u0629 \u062A\u062D\u062A\u0648\u064A \u0639\u0644\u0649 \u0643\u0645\u064A\u0627\u062A \u0645\u0631\u062A\u0641\u0639\u0629 \u0645\u0646 \u0645\u0639\u0627\u062F\u0646 \u0627\u0644\u0641\u0648\u0633\u0641\u0627\u062A. \u064A\u062E\u062A\u0644\u0641 \u0645\u062D\u062A\u0648\u0649 \u0627\u0644\u0641\u0648\u0633\u0641\u0627\u062A \u0641\u064A \u0639\u064A\u0646\u0627\u062A \u0635\u062E\u0648\u0631 \u0627\u0644\u0641\u0648\u0633\u0641\u0648\u0631\u064A\u062A (\u0623\u0648 \u062F\u0631\u062C\u0629 \u0635\u062E\u0631 \u0627\u0644\u0641\u0648\u0633\u0641\u0627\u062A) \u0627\u062E\u062A\u0644\u0627\u0641\u0627\u064B \u0643\u0628\u064A\u0631\u0627\u064B\u060C \u064A\u062A\u0631\u0627\u0648\u062D \u0645\u0646 4\u066A\u060C \u0625\u0644\u0649 20\u066A \u0639\u0644\u0649 \u0647\u064A\u0626\u0629 \u062E\u0645\u0627\u0633\u064A \u0623\u0643\u0633\u064A\u062F \u0627\u0644\u0641\u0648\u0633\u0641\u0648\u0631 (P2O5)\u061B \u0648\u0644\u0643\u0646 \u064A\u0645\u0643\u0646 \u0625\u062B\u0631\u0627\u0621 \u0635\u062E\u0631 \u0627\u0644\u0641\u0648\u0633\u0641\u0627\u062A \u0627\u0644\u0645\u0633\u0648\u0642 \u0628\u0646\u0633\u0628\u0629 \u0644\u0627 \u062A\u0642\u0644 \u062D\u0648\u0627\u0644\u064A 30\u066A \u0645\u0646 P2O5\u060C \u0648\u0630\u0644\u0643 \u0623\u062B\u0646\u0627\u0621 \u0639\u0645\u0644\u064A\u0627\u062A \u0627\u0644\u0645\u0639\u0627\u0644\u062C\u0629. \u064A\u0639\u062F \u0647\u0630\u0627 \u0627\u0644\u0646\u0648\u0639 \u0645\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0623\u063A\u0646\u0649 \u0623\u0646\u0648\u0627\u0639 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0631\u0633\u0648\u0628\u064A\u0629 \u0628\u0627\u0644\u0641\u0648\u0633\u0641\u0648\u0631\u060C \u0625\u0630 \u0623\u0646 \u0645\u062A\u0648\u0633\u0637 \u0645\u062D\u062A\u0648\u0649 \u0627\u0644\u0641\u0648\u0633\u0641\u0648\u0631 \u0645\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0631\u0633\u0648\u0628\u064A\u0629 \u0627\u0644\u0623\u062E\u0631\u0649 \u0623\u0642\u0644 \u0645\u0646 0.2\u066A. \u062A\u0646\u062A\u0634\u0631 \u062A\u0648\u0636\u0639\u0627\u062A \u0648\u062A\u0631\u0633\u0628\u0627\u062A \u0627\u0644\u0641\u0648\u0633\u0641\u0648\u0631\u064A\u062A \u0641\u064A \u0627\u0644\u0642\u0634\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0641\u064A \u0645\u0646\u0627\u0637\u0642 \u0639\u062F\u0629 \u0645\u0646 \u0627\u0644\u0639\u0627\u0644\u0645."@ar . "Fosforyty \u2013 ska\u0142y osadowe o chemicznym lub organicznym pochodzeniu. \n* Chemizm: z\u0142o\u017Cone g\u0142\u00F3wnie z fosforan\u00F3w (zawieraj\u0105 od 12 do 40% P4O10), reprezentowanych przez apatyt (kolofan) i kwarc, kalcyt, glaukonit, kaolinit, montmorillonit, czasami te\u017C limonit i substancje organiczne. \n* charakterystyczn\u0105 cech\u0105 jest zazwyczaj rozleg\u0142e, poziome rozprzestrzenienie z\u0142o\u017Ca o niewielkiej masy i wielko\u015Bci. \n* Fosforyty tworz\u0105 wk\u0142adki, przewarstwienia lub szeroko rozprzestrzenione pok\u0142ady w\u015Br\u00F3d wapieni i margli."@pl . "Fosforyty \u2013 ska\u0142y osadowe o chemicznym lub organicznym pochodzeniu. \n* Chemizm: z\u0142o\u017Cone g\u0142\u00F3wnie z fosforan\u00F3w (zawieraj\u0105 od 12 do 40% P4O10), reprezentowanych przez apatyt (kolofan) i kwarc, kalcyt, glaukonit, kaolinit, montmorillonit, czasami te\u017C limonit i substancje organiczne. \n* charakterystyczn\u0105 cech\u0105 jest zazwyczaj rozleg\u0142e, poziome rozprzestrzenienie z\u0142o\u017Ca o niewielkiej masy i wielko\u015Bci. \n* Fosforyty tworz\u0105 wk\u0142adki, przewarstwienia lub szeroko rozprzestrzenione pok\u0142ady w\u015Br\u00F3d wapieni i margli."@pl . . . . . "\u30EA\u30F3\u9271\u77F3\uFF08\u30EA\u30F3\u3053\u3046\u305B\u304D\u3001phosphate ore\u3001phosphorite\u3001phosphate rock\u3001rock phosphate\uFF09\u306F\u3001\u5DE5\u696D\u539F\u6599\u3068\u3057\u3066\u5229\u7528\u53EF\u80FD\u306A\u30EA\u30F3\u3092\u63A1\u53D6\u3067\u304D\u308B\u3001\u30EA\u30F3\u9178\u5869\u9271\u7269\u3092\u4E3B\u6210\u5206\u3068\u3057\u305F\u9271\u77F3\u3067\u3042\u308B\u3002"@ja . "\u30EA\u30F3\u9271\u77F3\uFF08\u30EA\u30F3\u3053\u3046\u305B\u304D\u3001phosphate ore\u3001phosphorite\u3001phosphate rock\u3001rock phosphate\uFF09\u306F\u3001\u5DE5\u696D\u539F\u6599\u3068\u3057\u3066\u5229\u7528\u53EF\u80FD\u306A\u30EA\u30F3\u3092\u63A1\u53D6\u3067\u304D\u308B\u3001\u30EA\u30F3\u9178\u5869\u9271\u7269\u3092\u4E3B\u6210\u5206\u3068\u3057\u305F\u9271\u77F3\u3067\u3042\u308B\u3002"@ja . "\u30EA\u30F3\u9271\u77F3"@ja . "\u039F \u03C6\u03C9\u03C3\u03C6\u03BF\u03C1\u03AF\u03C4\u03B7\u03C2 \u03AE \u03C0\u03AD\u03C4\u03C1\u03C9\u03BC\u03B1 \u03C6\u03C9\u03C3\u03C6\u03AC\u03C4\u03C9\u03BD \u03B5\u03AF\u03BD\u03B1\u03B9 \u03B9\u03B6\u03B7\u03BC\u03B1\u03C4\u03BF\u03B3\u03B5\u03BD\u03AD\u03C2 \u03C0\u03AD\u03C4\u03C1\u03C9\u03BC\u03B1 \u03C0\u03BF\u03C5 \u03C0\u03B5\u03C1\u03B9\u03AD\u03C7\u03B5\u03B9 \u03BC\u03B5\u03B3\u03AC\u03BB\u03BF \u03C0\u03BF\u03C3\u03BF\u03C3\u03C4\u03CC \u03BF\u03C1\u03C5\u03BA\u03C4\u03CE\u03BD \u03C6\u03C9\u03C3\u03C6\u03BF\u03C1\u03B9\u03BA\u03CE\u03BD \u03B1\u03BB\u03AC\u03C4\u03C9\u03BD (\u00AB\u03C6\u03C9\u03C3\u03C6\u03AC\u03C4\u03C9\u03BD\u00BB). \u0397 \u03C0\u03B5\u03C1\u03B9\u03B5\u03BA\u03C4\u03B9\u03BA\u03CC\u03C4\u03B7\u03C4\u03B1 \u03C4\u03BF\u03C5 \u03C6\u03C9\u03C3\u03C6\u03BF\u03C1\u03AF\u03C4\u03B7 \u03C3\u03B5 \u03C6\u03C9\u03C3\u03C6\u03BF\u03C1\u03B9\u03BA\u03AC \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C4\u03BF\u03C5\u03BB\u03AC\u03C7\u03B9\u03C3\u03C4\u03BF\u03BD 15 \u03C9\u03C2 20%. \u0391\u03BD\u03AC\u03BB\u03BF\u03B3\u03B1 \u03BC\u03B5 \u03C4\u03BF \u03B5\u03AF\u03B4\u03BF\u03C2 \u03C4\u03BF\u03C5 \u03BF\u03C1\u03C5\u03BA\u03C4\u03BF\u03CD, \u03C3\u03C5\u03BD\u03AE\u03B8\u03C9\u03C2 \u03BF \u03C6\u03C9\u03C3\u03C6\u03BF\u03C1\u03AF\u03C4\u03B7\u03C2 \u03C0\u03B5\u03C1\u03B9\u03AD\u03C7\u03B5\u03B9 \u03C4\u03BF \u03C3\u03C4\u03BF\u03B9\u03C7\u03B5\u03AF\u03BF \u03C6\u03C9\u03C3\u03C6\u03CC\u03C1\u03BF\u03C2 \u03C3\u03B5 \u03C0\u03B5\u03C1\u03B9\u03B5\u03BA\u03C4\u03B9\u03BA\u03CC\u03C4\u03B7\u03C4\u03B1 \u03B1\u03C0\u03CC 4 \u03BC\u03AD\u03C7\u03C1\u03B9 18,5% \u03BA\u03B1\u03C4\u03AC \u03B2\u03AC\u03C1\u03BF\u03C2, \u03BC\u03AF\u03B1 \u03C3\u03B7\u03BC\u03B1\u03BD\u03C4\u03B9\u03BA\u03AC \u03BC\u03B5\u03B3\u03B1\u03BB\u03CD\u03C4\u03B5\u03C1\u03B7 \u03C0\u03B5\u03C1\u03B9\u03B5\u03BA\u03C4\u03B9\u03BA\u03CC\u03C4\u03B7\u03C4\u03B1 \u03B1\u03C0\u03CC \u03C4\u03BF \u03BC\u03AD\u03C3\u03BF \u03B9\u03B6\u03B7\u03BC\u03B1\u03C4\u03BF\u03B3\u03B5\u03BD\u03AD\u03C2 \u03C0\u03AD\u03C4\u03C1\u03C9\u03BC\u03B1, \u03C4\u03BF\u03C5 \u03BF\u03C0\u03BF\u03AF\u03BF\u03C5 \u03B7 \u03C0\u03B5\u03C1\u03B9\u03B5\u03BA\u03C4\u03B9\u03BA\u03CC\u03C4\u03B7\u03C4\u03B1 \u03C3\u03B5 \u03C6\u03C9\u03C3\u03C6\u03CC\u03C1\u03BF \u03B5\u03AF\u03BD\u03B1\u03B9 \u03BC\u03B9\u03BA\u03C1\u03CC\u03C4\u03B5\u03C1\u03B7 \u03C4\u03BF\u03C5 0,2%."@el . . "\u03A6\u03C9\u03C3\u03C6\u03BF\u03C1\u03AF\u03C4\u03B7\u03C2"@el . "Fosforiet of fosfaatgesteente is een sedimentair gesteente dat voor minstens 20% uit fosfaten bestaat. Fosforiet heeft dezelfde interne structuur en textuur als fijnkorrelige kalksteen en is vaak het resultaat van diagenetische omzetting van kalksteen, waarbij carbonaat wordt vervangen door fosfaat. Voor deze diagenetische omzetting zijn grote hoeveelheden fosfaat in het grondwater nodig, zoals in de buurt van grote hoeveelheden guano. Het fosfaat is in de meeste gevallen een vorm van fluorapatiet, bijvoorbeeld met een carbonaat en hydroxylgroep (Ca10(PO4CO3)F2-3), en vormt massa's van zeer kleine kristallen (cryptokristallijne massa's, < 1 \u03BCm) die genoemd worden. Fosforiet komt meestal voor in Paleozo\u00EFsche of Cenozo\u00EFsche sedimenten, maar wordt ook in Proterozo\u00EFsche banded iron formations gevonden. Voorbeelden van omvangrijke fosforietformaties zijn de Phosphorites du Quercy in Frankrijk of de in de Verenigde Staten. Commercieel wordt fosforiet gewonnen in Frankrijk, Belgi\u00EB, de VS, Spanje, Marokko, Tunesi\u00EB en Algerije."@nl . . "La fosforita es una roca sedimentaria no detr\u00EDtica que contiene altas cantidades de minerales fosfatados. El contenido en fosfatos es por lo menos de entre un 15 y un 20 %, un incremento importante respecto a una roca sedimentaria t\u00EDpica que contiene menos de un 0,2 %.\u200B El fosfato est\u00E1 presente como fluorapatita, Ca5(PO4)3F, t\u00EDpico en masas criptocristalinas (tama\u00F1os de grano <1 \u03BCm).\u200B Tambi\u00E9n est\u00E1 presente en forma de hidroxiapatita, Ca5(PO4)3OH, que a menudo se disuelve por huesos de animales vertebrados. Tambi\u00E9n se encuentran disueltos en rocas \u00EDgneas y metam\u00F3rficas. A menudo se dan dep\u00F3sitos de fosforita en capas extensas, que en conjunto cubren decenas de miles de kil\u00F3metros cuadrados de la corteza terrestre.\u200B Calizas y esquistos frecuentemente presenta fosfatos.\u200B Las rocas sedimentarias ricas en fosfatos pueden ser marrones o negras, y van desde l\u00E1minas de un cent\u00EDmetro de grosor a camas de varios metros de espesor. En esta \u00FAltima posibilidad, no suele haber exclusivamente rocas fosfatadas, sino que van acompa\u00F1adas de lutitas, s\u00EDlex , piedra caliza, dolom\u00EDas y a veces areniscas.\u200B Estas capas contienen las mismas texturas y estructuras que las calizas de grano fino y pueden representar reemplazos diagen\u00E9ticos de los minerales carbonatados por fosfatos.\u200B Tambi\u00E9n pueden estar compuestos de , ooides, f\u00F3siles y clastos. Hay algunas fosforitas que son muy peque\u00F1as y no tienen texturas granulares distintivas.\u200B Existen fosforitas del Proterozoico, pero son m\u00E1s comunes del Paleozoico y de sedimentos del Cenozoico. Algunos yacimientos alcanzan un espesor de 420 metros y una superficie de 350 000 km\u00B2.\u200B Hay minas para su uso comercial en Francia, B\u00E9lgica, Espa\u00F1a, Marruecos, T\u00FAnez y Argelia.\u200B"@es . . "Phosphorite"@fr . "Fosforit \u00E4r en kolloidal form av apatit i tr\u00E5daktig till t\u00E4t, ofta jordartad form med vit-, gul-, brun- eller gr\u00E5aktig f\u00E4rg. Den f\u00F6rekommer dels i lagerformade massor av st\u00F6rre utstr\u00E4ckning, dels som st\u00F6rre eller mindre klumpar i lera eller sand, och ibland som tillf\u00E4lliga best\u00E5ndsdelar i andra bergarter. Fosforit \u00E4r den enda bergartsbildande fosfaten, f\u00F6rmodligen en g\u00E5ng bildad som rester efter djur. Den st\u00F6rsta ansamlingen av fosforit finns p\u00E5 havsbotten dit fosforf\u00F6reningar kommer med nederb\u00F6rd, damm, glaci\u00E4r avsm\u00E4ltning (glacial runoff), hydrotermisk vulkanisk aktivitet och deposition av organiskt material. Fosforeningarna omvandlas av mikro- och makroorganismer, s\u00E5som kiselalger, fytoplankton och zooplankton, till l\u00F6sta fosfater. Vissa fiskar tar upp fosfat i t\u00E4nder och skelett som begravs i sedimentet p\u00E5 havets botten n\u00E4r fiskarna d\u00F6r."@sv . . . . . . . . . . . "Fosforiet of fosfaatgesteente is een sedimentair gesteente dat voor minstens 20% uit fosfaten bestaat. Fosforiet heeft dezelfde interne structuur en textuur als fijnkorrelige kalksteen en is vaak het resultaat van diagenetische omzetting van kalksteen, waarbij carbonaat wordt vervangen door fosfaat. Voor deze diagenetische omzetting zijn grote hoeveelheden fosfaat in het grondwater nodig, zoals in de buurt van grote hoeveelheden guano."@nl . . . . . . "Fosforit je usazen\u00E1 hornina biogenn\u00EDho p\u016Fvodu s obsahem P4O10 od 5 % do 35 %. Je to sm\u011Bs fosfore\u010Dnan\u016F p\u0159\u00EDrodn\u00EDho p\u016Fvodu, ve kter\u00E9m je jedna z hlavn\u00EDch slo\u017Eek miner\u00E1ln\u00ED skupina apatitu. Pou\u017E\u00EDv\u00E1 se po \u00FAprav\u011B jako hnojivo - zdroj fosforu pro v\u00FD\u017Eivu rostlin. N\u00E1zev fosforit se p\u016Fvodn\u011B pou\u017E\u00EDval jako ozna\u010Den\u00ED apatitu."@cs . . "Is \u00E9ard is fosfair\u00EDt, carraig fosf\u00E1ite n\u00F3 fosf\u00E1it charraige ann n\u00E1 carraig dhr\u00EDodair neamh-dhr\u00E1imh, ina mb\u00EDonn m\u00E9ideanna arda de mhianra\u00ED fosf\u00E1it. Athra\u00EDonn m\u00E9id na fosf\u00E1ite san fhosfair\u00EDt (n\u00F3 gr\u00E1d na carraige fosf\u00E1ite) go m\u00F3r, \u00F3 4% go dt\u00ED 20% peantocsa\u00EDd fhosfair (P2O5).Cuirtear an charraig fosf\u00E1ite saibhrithe (n\u00F3 \"beinif\u00EDthe\") go 28% ar a laghad ar an margadh, go minic n\u00EDos m\u00F3 n\u00E1 30% P2O5. Tarla\u00EDonn s\u00E9 seo tr\u00ED n\u00EDoch\u00E1in, scagadh, d\u00ED-aoladh, scaradh maighn\u00E9adach n\u00F3 sn\u00E1mhacht. S\u00E9 sin, i gcompar\u00E1id le n\u00EDos l\u00FA n\u00E1 0.2% an me\u00E1n-mh\u00E9id fosfair sna carraigeacha collaf\u00E1in dr\u00EDodair. T\u00E1 an fhosf\u00E1it i l\u00E1thair mar Ca5(PO4)3F, de ghn\u00E1th i maiseanna cripticriostalta (gr\u00E1nmh\u00E9ideanna <1 \u03BCm) d\u00E1 ngairtear deasc\u00E1in d'apait\u00EDte dr\u00EDodair de bhunadh neamhchinnte. T\u00E1 s\u00ED i l\u00E1thair freisin mar Ca5(PO4)3OH n\u00F3 Ca10("@ga . . . . . . . . "Fosforite \u00E9 uma rocha sedimentar cujo teor de minerais fosfatados a torna economicamente interessante. Geralmente trata-se de uma rocha estratificada de origem marinha, composta de carbonatada e , na forma de l\u00E2minas, n\u00F3dulos, o\u00F3litos e fragmentos de ossos e conchas."@pt . . "\uC778\uAD11\uC11D(\u71D0\u945B\u77F3, phosphate rock)\uC740 \uC778\uD68C\uC11D(Apatite)\uC744 \uD568\uC720\uD558\uB294 \uC554\uC11D\uC73C\uB85C \uC0DD\uD654\uD559 \uAE30\uC6D0\uC758 \uD1F4\uC801\uC554\uC774\uB2E4. \uB530\uB77C\uC11C \uC778\uAD11\uC11D\uC740 \uB2E4\uB978 \uAD11\uBB3C\uACFC \uAC19\uC774 \uD654\uD559\uC870\uC131\uC73C\uB85C \uD45C\uC2DC\uD560 \uC218 \uC5C6\uB2E4. \uC778\uD68C\uC11D\uC740 \uD654\uC131\uC554 \uAE30\uC6D0\uC73C\uB85C \uB9E5\uC0C1\uC73C\uB85C \uB098\uD0C0\uB098\uBA70, \uC778\uAD11\uC11D\uC740 \uC720\uAE30\uBB3C\uC774 \uD1F4\uC801\uB418\uC5B4 \uB098\uD0C0\uB098\uB294 2\uCC28 \uAD11\uC0C1\uC73C\uB85C \uC778(P2O5)\uC744 18%\u223C40% \uD568\uC720\uD55C\uB2E4. \uC778\uD68C\uC11D\uACFC \uC778\uAD11\uC11D\uC740 \uC778\uC758 \uD568\uB7C9\uC5D0 \uB530\uB77C \uAD11\uBB3C \uAC00\uCE58\uAC00 \uACB0\uC815\uB418\uBA70 \uC8FC\uB85C \uBE44\uB8CC\uC6D0\uB8CC\uB85C \uB9CE\uC774 \uC0AC\uC6A9\uB41C\uB2E4. \uC774 \uBC16\uC5D0 \uC778\uD68C\uC11D\uC740 \uC778\uC0B0\uC81C\uC870, \uC758\uC57D\uD488, \uBC18\uB3C4\uCCB4, \uC138\uB77C\uBBF9, \uC2E4\uD06C, \uC12C\uC720, \uBC29\uCDA9\uC81C, \uC124\uD0D5 \uC815\uB828, \uD3ED\uC57D \uB4F1\uC5D0\uB3C4 \uC0AC\uC6A9\uB418\uACE0 \uC788\uB2E4. \uC778\uC758 \uC21C\uB3C4\uAC00 \uB0AE\uC740 \uACBD\uC6B0\uC5D0\uB294 \uD488\uC704\uB97C \uB192\uC5EC\uC8FC\uB294 \uC120\uAD11 \uC791\uC5C5\uC744 \uAC70\uCCD0 \uC0AC\uC6A9\uD55C\uB2E4. \uC778\uC0B0\uC774\uB098 \uBE44\uB8CC\uC6A9\uC73C\uB85C \uC0AC\uC6A9\uD558\uB294 \uC778\uD68C\uC11D(\uC778\uAD11\uC11D \uD3EC\uD568)\uC740 \uC778\uC774 30%\uC774\uC0C1 \uD568\uC720\uB418\uC5B4\uC57C \uD55C\uB2E4. \uC778\uAD11\uC11D\uC758 \uD488\uC9C8\uAE30\uC900\uC5D0\uB294 \uC0C1\uC5C5\uC801\uC73C\uB85C BPL(Bone Phosphate of Lime)\uC774\uB77C\uB294 \uB2E8\uC704\uAC00 \uC0AC\uC6A9\uB41C\uB2E4."@ko . "\u0424\u043E\u0441\u0444\u043E\u0440\u0438\u0301\u0442 (\u0444\u043E\u0441\u0444\u043E\u0440\u0438\u0442\u044B) \u2014 \u043E\u0441\u0430\u0434\u043E\u0447\u043D\u0430\u044F \u0433\u043E\u0440\u043D\u0430\u044F \u043F\u043E\u0440\u043E\u0434\u0430, \u0430\u0433\u0440\u043E\u043D\u043E\u043C\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u0440\u0443\u0434\u0430, \u0441\u043E\u0441\u0442\u043E\u044F\u0449\u0430\u044F \u043F\u0440\u0435\u0438\u043C\u0443\u0449\u0435\u0441\u0442\u0432\u0435\u043D\u043D\u043E \u0438\u0437 \u0444\u043E\u0441\u0444\u0430\u0442\u043D\u044B\u0445 \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u043E\u0432 \u0433\u0440\u0443\u043F\u043F\u044B \u0430\u043F\u0430\u0442\u0438\u0442\u0430, \u043D\u0430\u0445\u043E\u0434\u044F\u0449\u0438\u0445\u0441\u044F \u0432 \u0441\u043A\u0440\u044B\u0442\u043E- \u0438\u043B\u0438 \u043C\u0438\u043A\u0440\u043E\u043A\u0440\u0438\u0441\u0442\u0430\u043B\u043B\u0438\u0447\u0435\u0441\u043A\u043E\u0439 \u0444\u043E\u0440\u043C\u0435."@ru . . . . . . . . . . . . . "Fosfair\u00EDt"@ga . . . . . "20774"^^ . . . . . "Fosforyty"@pl . "Fosforite"@pt . . . . "Fosforiet"@nl . . . . "Fosforita"@es . "\u0424\u043E\u0441\u0444\u043E\u0440\u0438\u0442\u0438 \u2014 \u043E\u0441\u0430\u0434\u043E\u0432\u0430 \u0433\u0456\u0440\u0441\u044C\u043A\u0430 \u043F\u043E\u0440\u043E\u0434\u0430 \u043C\u043E\u0440\u0441\u044C\u043A\u043E\u0433\u043E \u043F\u043E\u0445\u043E\u0434\u0436\u0435\u043D\u043D\u044F, \u0441\u0444\u043E\u0440\u043C\u043E\u0432\u0430\u043D\u0430 \u0433\u043E\u043B\u043E\u0432\u043D\u0438\u043C \u0447\u0438\u043D\u043E\u043C \u0437 \u0444\u043E\u0441\u0444\u0430\u0442\u0443 \u043A\u0430\u043B\u044C\u0446\u0456\u044E (Ca3(PO4)2), \u0430 \u0442\u0430\u043A\u043E\u0436 \u043A\u0432\u0430\u0440\u0446\u0443, \u043A\u0430\u043B\u044C\u0446\u0438\u0442\u0443, \u0434\u043E\u043B\u043E\u043C\u0456\u0442\u0443, \u0445\u0430\u043B\u0446\u0435\u0434\u043E\u043D\u0443, \u0491\u043B\u0430\u0443\u043A\u043E\u043D\u0456\u0442\u0443, \u043A\u0430\u0440\u0431\u043E\u043D\u0430\u0442\u0456\u0432, \u0433\u0456\u0434\u0440\u0430\u0442\u0456\u0432, \u043E\u043A\u0441\u0438\u0434\u0456\u0432 \u0437\u0430\u043B\u0456\u0437\u0430 \u0456 \u0442.\u0456\u043D., \u0434\u0440\u0443\u0433\u043E\u0440\u044F\u0434\u043D\u0438\u0445 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432 \u2014 \u0433\u043B\u0438\u043D\u0438\u0441\u0442\u0438\u0445, \u0430\u043B\u044E\u043C\u043E\u0441\u0438\u043B\u0456\u043A\u0430\u0442\u0456\u0432, \u043F\u0456\u0440\u0438\u0442\u0443, \u0433\u0456\u0434\u0440\u043E\u043A\u0441\u0438\u0434\u0456\u0432 \u0437\u0430\u043B\u0456\u0437\u0430 \u0442\u0430 \u043E\u0440\u0433\u0430\u043D\u0456\u0447\u043D\u043E\u0457 \u0440\u0435\u0447\u043E\u0432\u0438\u043D\u0438, \u0437\u0446\u0435\u043C\u0435\u043D\u0442\u043E\u0432\u0430\u043D\u0438\u0445 \u0444\u043E\u0441\u0444\u0430\u0442\u043E\u043C \u043A\u0430\u043B\u044C\u0446\u0456\u044E \u0430\u0431\u043E \u0437\u0431\u0430\u0433\u0430\u0447\u0435\u043D\u0438\u0445 \u0441\u043A\u0443\u043F\u0447\u0435\u043D\u043D\u044F\u043C \u0436\u043E\u0432\u0435\u043D \u0447\u0438 \u043E\u043E\u043B\u0456\u0442\u0456\u0432."@uk . "\u039F \u03C6\u03C9\u03C3\u03C6\u03BF\u03C1\u03AF\u03C4\u03B7\u03C2 \u03AE \u03C0\u03AD\u03C4\u03C1\u03C9\u03BC\u03B1 \u03C6\u03C9\u03C3\u03C6\u03AC\u03C4\u03C9\u03BD \u03B5\u03AF\u03BD\u03B1\u03B9 \u03B9\u03B6\u03B7\u03BC\u03B1\u03C4\u03BF\u03B3\u03B5\u03BD\u03AD\u03C2 \u03C0\u03AD\u03C4\u03C1\u03C9\u03BC\u03B1 \u03C0\u03BF\u03C5 \u03C0\u03B5\u03C1\u03B9\u03AD\u03C7\u03B5\u03B9 \u03BC\u03B5\u03B3\u03AC\u03BB\u03BF \u03C0\u03BF\u03C3\u03BF\u03C3\u03C4\u03CC \u03BF\u03C1\u03C5\u03BA\u03C4\u03CE\u03BD \u03C6\u03C9\u03C3\u03C6\u03BF\u03C1\u03B9\u03BA\u03CE\u03BD \u03B1\u03BB\u03AC\u03C4\u03C9\u03BD (\u00AB\u03C6\u03C9\u03C3\u03C6\u03AC\u03C4\u03C9\u03BD\u00BB). \u0397 \u03C0\u03B5\u03C1\u03B9\u03B5\u03BA\u03C4\u03B9\u03BA\u03CC\u03C4\u03B7\u03C4\u03B1 \u03C4\u03BF\u03C5 \u03C6\u03C9\u03C3\u03C6\u03BF\u03C1\u03AF\u03C4\u03B7 \u03C3\u03B5 \u03C6\u03C9\u03C3\u03C6\u03BF\u03C1\u03B9\u03BA\u03AC \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C4\u03BF\u03C5\u03BB\u03AC\u03C7\u03B9\u03C3\u03C4\u03BF\u03BD 15 \u03C9\u03C2 20%. \u0391\u03BD\u03AC\u03BB\u03BF\u03B3\u03B1 \u03BC\u03B5 \u03C4\u03BF \u03B5\u03AF\u03B4\u03BF\u03C2 \u03C4\u03BF\u03C5 \u03BF\u03C1\u03C5\u03BA\u03C4\u03BF\u03CD, \u03C3\u03C5\u03BD\u03AE\u03B8\u03C9\u03C2 \u03BF \u03C6\u03C9\u03C3\u03C6\u03BF\u03C1\u03AF\u03C4\u03B7\u03C2 \u03C0\u03B5\u03C1\u03B9\u03AD\u03C7\u03B5\u03B9 \u03C4\u03BF \u03C3\u03C4\u03BF\u03B9\u03C7\u03B5\u03AF\u03BF \u03C6\u03C9\u03C3\u03C6\u03CC\u03C1\u03BF\u03C2 \u03C3\u03B5 \u03C0\u03B5\u03C1\u03B9\u03B5\u03BA\u03C4\u03B9\u03BA\u03CC\u03C4\u03B7\u03C4\u03B1 \u03B1\u03C0\u03CC 4 \u03BC\u03AD\u03C7\u03C1\u03B9 18,5% \u03BA\u03B1\u03C4\u03AC \u03B2\u03AC\u03C1\u03BF\u03C2, \u03BC\u03AF\u03B1 \u03C3\u03B7\u03BC\u03B1\u03BD\u03C4\u03B9\u03BA\u03AC \u03BC\u03B5\u03B3\u03B1\u03BB\u03CD\u03C4\u03B5\u03C1\u03B7 \u03C0\u03B5\u03C1\u03B9\u03B5\u03BA\u03C4\u03B9\u03BA\u03CC\u03C4\u03B7\u03C4\u03B1 \u03B1\u03C0\u03CC \u03C4\u03BF \u03BC\u03AD\u03C3\u03BF \u03B9\u03B6\u03B7\u03BC\u03B1\u03C4\u03BF\u03B3\u03B5\u03BD\u03AD\u03C2 \u03C0\u03AD\u03C4\u03C1\u03C9\u03BC\u03B1, \u03C4\u03BF\u03C5 \u03BF\u03C0\u03BF\u03AF\u03BF\u03C5 \u03B7 \u03C0\u03B5\u03C1\u03B9\u03B5\u03BA\u03C4\u03B9\u03BA\u03CC\u03C4\u03B7\u03C4\u03B1 \u03C3\u03B5 \u03C6\u03C9\u03C3\u03C6\u03CC\u03C1\u03BF \u03B5\u03AF\u03BD\u03B1\u03B9 \u03BC\u03B9\u03BA\u03C1\u03CC\u03C4\u03B5\u03C1\u03B7 \u03C4\u03BF\u03C5 0,2%."@el . . "\u0424\u043E\u0441\u0444\u043E\u0440\u0438\u0442\u0438"@uk . "\u0641\u0648\u0633\u0641\u0648\u0631\u064A\u062A"@ar . . . . . . . . . . . . . . "Fosforite \u00E9 uma rocha sedimentar cujo teor de minerais fosfatados a torna economicamente interessante. Geralmente trata-se de uma rocha estratificada de origem marinha, composta de carbonatada e , na forma de l\u00E2minas, n\u00F3dulos, o\u00F3litos e fragmentos de ossos e conchas."@pt . . . "Phosphorite"@en . . . "Is \u00E9ard is fosfair\u00EDt, carraig fosf\u00E1ite n\u00F3 fosf\u00E1it charraige ann n\u00E1 carraig dhr\u00EDodair neamh-dhr\u00E1imh, ina mb\u00EDonn m\u00E9ideanna arda de mhianra\u00ED fosf\u00E1it. Athra\u00EDonn m\u00E9id na fosf\u00E1ite san fhosfair\u00EDt (n\u00F3 gr\u00E1d na carraige fosf\u00E1ite) go m\u00F3r, \u00F3 4% go dt\u00ED 20% peantocsa\u00EDd fhosfair (P2O5).Cuirtear an charraig fosf\u00E1ite saibhrithe (n\u00F3 \"beinif\u00EDthe\") go 28% ar a laghad ar an margadh, go minic n\u00EDos m\u00F3 n\u00E1 30% P2O5. Tarla\u00EDonn s\u00E9 seo tr\u00ED n\u00EDoch\u00E1in, scagadh, d\u00ED-aoladh, scaradh maighn\u00E9adach n\u00F3 sn\u00E1mhacht. S\u00E9 sin, i gcompar\u00E1id le n\u00EDos l\u00FA n\u00E1 0.2% an me\u00E1n-mh\u00E9id fosfair sna carraigeacha collaf\u00E1in dr\u00EDodair. T\u00E1 an fhosf\u00E1it i l\u00E1thair mar Ca5(PO4)3F, de ghn\u00E1th i maiseanna cripticriostalta (gr\u00E1nmh\u00E9ideanna <1 \u03BCm) d\u00E1 ngairtear deasc\u00E1in d'apait\u00EDte dr\u00EDodair de bhunadh neamhchinnte. T\u00E1 s\u00ED i l\u00E1thair freisin mar Ca5(PO4)3OH n\u00F3 Ca10(PO4)6(OH)2, a bh\u00EDonn d\u00EDscaoilte go minic \u00F3 chn\u00E1mha agus fiacla veirteabracha, c\u00E9 gur f\u00E9idir le fluar-apait\u00EDt a thionscnamh \u00F3 .Is minic a bh\u00EDonn deasc\u00E1n fosfair\u00EDte i sraitheanna fairsing, a chl\u00FAda\u00EDonn i ndiaidh a ch\u00E9ile na m\u00EDlte cilim\u00E9adar cearnach de screamh an Domhain."@ga . . . . "Phosphorite, phosphate rock or rock phosphate is a non-detrital sedimentary rock that contains high amounts of phosphate minerals. The phosphate content of phosphorite (or grade of phosphate rock) varies greatly, from 4% to 20% phosphorus pentoxide (P2O5). Marketed phosphate rock is enriched (\"beneficiated\") to at least 28%, often more than 30% P2O5. This occurs through washing, screening, de-liming, magnetic separation or flotation. By comparison, the average phosphorus content of sedimentary rocks is less than 0.2%. The phosphate is present as fluorapatite Ca5(PO4)3F typically in cryptocrystalline masses (grain sizes < 1 \u03BCm) referred to as collophane-sedimentary apatite deposits of uncertain origin. It is also present as hydroxyapatite Ca5(PO4)3OH or Ca10(PO4)6(OH)2, which is often disso"@en . . . "La fosforite \u00E8 una roccia sedimentaria non clastica, ma di origine chimica, che presenta alte concentrazioni in minerali del fosforo. Il contenuto di fosfato della fosforite \u00E8 almeno del 15-20%, percentuale che la distingue dalla media delle rocce sedimentarie che hanno un contenuto di fosfato inferiore allo 0,2% Il fosfato \u00E8 presente come fluorapatite Ca5(PO4)3F, tipicamente in masse criptocristalline (cristalli inferiori ad 1 \u00B5m) variet\u00E0 definite localmente collofane o staffelite. Un altro minerale rilevante \u00E8 l'idrossiapatite Ca5(PO4)3OH, spesso di origine organogena mentre la fluorapatite \u00E8 di origine idrotermale. Un'altra fonte di fosforo pu\u00F2 essere la lisciviazione di rocce ignee e metamorfiche. Le fosforiti costituiscono strati estesi complessivamente decine di migliaia di chilometr"@it . "Phosphorit"@de . . . . "\u0424\u043E\u0441\u0444\u043E\u0440\u0438\u0442"@ru . . "La phosphorite est \u00E0 la fois un min\u00E9ral, une esp\u00E8ce chimique de formule 3 Ca3(PO4)2, Ca(OH,F,Cl)2, ainsi qu'une roche phosphat\u00E9e d'origine d\u00E9tritique dont il est le principal constituant."@fr . . "Fosforit je usazen\u00E1 hornina biogenn\u00EDho p\u016Fvodu s obsahem P4O10 od 5 % do 35 %. Je to sm\u011Bs fosfore\u010Dnan\u016F p\u0159\u00EDrodn\u00EDho p\u016Fvodu, ve kter\u00E9m je jedna z hlavn\u00EDch slo\u017Eek miner\u00E1ln\u00ED skupina apatitu. Pou\u017E\u00EDv\u00E1 se po \u00FAprav\u011B jako hnojivo - zdroj fosforu pro v\u00FD\u017Eivu rostlin. N\u00E1zev fosforit se p\u016Fvodn\u011B pou\u017E\u00EDval jako ozna\u010Den\u00ED apatitu."@cs . . . . . . "1227081"^^ . . . . . . . . . . . . . . "Phosphorit ist ein marines Sedimentgestein, das schichtgebunden mit anderen marinen Gesteinen, meistens mit Kalken auftritt."@de . . . "Phosphorite, phosphate rock or rock phosphate is a non-detrital sedimentary rock that contains high amounts of phosphate minerals. The phosphate content of phosphorite (or grade of phosphate rock) varies greatly, from 4% to 20% phosphorus pentoxide (P2O5). Marketed phosphate rock is enriched (\"beneficiated\") to at least 28%, often more than 30% P2O5. This occurs through washing, screening, de-liming, magnetic separation or flotation. By comparison, the average phosphorus content of sedimentary rocks is less than 0.2%. The phosphate is present as fluorapatite Ca5(PO4)3F typically in cryptocrystalline masses (grain sizes < 1 \u03BCm) referred to as collophane-sedimentary apatite deposits of uncertain origin. It is also present as hydroxyapatite Ca5(PO4)3OH or Ca10(PO4)6(OH)2, which is often dissolved from vertebrate bones and teeth, whereas fluorapatite can originate from hydrothermal veins. Other sources also include chemically dissolved phosphate minerals from igneous and metamorphic rocks. Phosphorite deposits often occur in extensive layers, which cumulatively cover tens of thousands of square kilometres of the Earth's crust. Limestones and mudstones are common phosphate-bearing rocks. Phosphate-rich sedimentary rocks can occur in dark brown to black beds, ranging from centimeter-sized laminae to beds that are several meters thick. Although these thick beds can exist, they are rarely only composed of phosphatic sedimentary rocks. Phosphatic sedimentary rocks are commonly accompanied by or interbedded with shales, cherts, limestone, dolomites and sometimes sandstone. These layers contain the same textures and structures as fine-grained limestones and may represent diagenetic replacements of carbonate minerals by phosphates. They also can be composed of peloids, ooids, fossils, and clasts that are made up of apatite. There are some phosphorites that are very small and have no distinctive granular textures. This means that their textures are similar to that of collophane, or fine micrite-like texture. Phosphatic grains may be accompanied by organic matter, clay minerals, silt-sized detrital grains, and pyrite. Peloidal or pelletal phosphorites occur normally; whereas oolitic phosphorites are not common. Phosphorites are known from Proterozoic banded iron formations in Australia, but are more common from Paleozoic and Cenozoic sediments. The Permian Phosphoria Formation of the western United States represents some 15 million years of sedimentation. It reaches a thickness of 420 metres and covers an area of 350,000 km2. Commercially mined phosphorites occur in France, Belgium, Spain, Morocco, Tunisia and Algeria. In the United States phosphorites have been mined in Florida, Tennessee, Wyoming, Utah, Idaho and Kansas."@en . "Fosforito estas densa, plej ofte terece loza , kiu ekestis el fosforri\u0109a kalko kaj povas trovi\u011Di petroformanta je grandaj tavoloj. La \u0109efa konsista\u0135oparto estas la mineralo (Ca5[(F,OH,CO3)/(PO4)3], kiu plejparte estas bestodevena. \u011Ci povas origini el la malkomponado de fosforenhavaj bestaj resta\u0135oj. La \u015Dtona\u0135on fosforito oni uzas kiel krudmaterialon por produkti fosforon, precipe sterka\u0135on, kaj en la kemia industrio."@eo . . . . . . "Fosforit"@sv . . . . . . "Fosforito estas densa, plej ofte terece loza , kiu ekestis el fosforri\u0109a kalko kaj povas trovi\u011Di petroformanta je grandaj tavoloj. La \u0109efa konsista\u0135oparto estas la mineralo (Ca5[(F,OH,CO3)/(PO4)3], kiu plejparte estas bestodevena. \u011Ci povas origini el la malkomponado de fosforenhavaj bestaj resta\u0135oj. La \u015Dtona\u0135on fosforito oni uzas kiel krudmaterialon por produkti fosforon, precipe sterka\u0135on, kaj en la kemia industrio. Konataj trovejoj de fosforito, parte en konkrementoj, trovi\u011Das sur Nauro (preska\u016D el\u0109erpita), en Maroko, Florido, Tunizio, Estonio kaj Al\u011Derio. Fosforittubera horizonto ekzistas \u0109e Lepsiko, fosforitoj estis elminigitaj en la minejo Zollhaus sur la teritorio de la komunumo Katzenelnbogen en Germanio."@eo . . . . "Fosforite"@it . "La fosforite \u00E8 una roccia sedimentaria non clastica, ma di origine chimica, che presenta alte concentrazioni in minerali del fosforo. Il contenuto di fosfato della fosforite \u00E8 almeno del 15-20%, percentuale che la distingue dalla media delle rocce sedimentarie che hanno un contenuto di fosfato inferiore allo 0,2% Il fosfato \u00E8 presente come fluorapatite Ca5(PO4)3F, tipicamente in masse criptocristalline (cristalli inferiori ad 1 \u00B5m) variet\u00E0 definite localmente collofane o staffelite. Un altro minerale rilevante \u00E8 l'idrossiapatite Ca5(PO4)3OH, spesso di origine organogena mentre la fluorapatite \u00E8 di origine idrotermale. Un'altra fonte di fosforo pu\u00F2 essere la lisciviazione di rocce ignee e metamorfiche. Le fosforiti costituiscono strati estesi complessivamente decine di migliaia di chilometri quadrati nella crosta terrestre. Le fosforiti si associano comunemente ai calcari ed alle argille. Le fosforiti sono presenti in strati laminati dal marrone scuro al nero aventi spessori di strato da centimetrici a metrici. Gli strati di rocce fosfatiche sono comunemente intercalati con altre rocce sedimentarie come selci, calcari, dolomie e, a volte, arenarie. Gli strati presentano le stesse strutture dei calcari fini e spesso rappresentano una sostituzione diagenetica dei minerali carbonatici con i fosfati. Le fosforiti sono note a partire da particolari rocce formatesi nel Proterozoico le cosiddette Banded iron beds (letteralmente orizzonti ferriferi a bande) australiane, ma sono pi\u00F9 comuni nei sedimenti del paleozoico e cenozoico. Una formazione rilevante \u00E8 la Phosphoria Formation del permiano nord americano che copre, con uno spessore massimo di 420m, 350.000 km2 ed un intervallo deposizionale di 15 milioni di anni.Le fosforiti sono sfruttate minerariamente negli Stati Uniti, Francia, Belgio, Spagna, Marocco, Tunisia, Algeria.."@it . . "La phosphorite est \u00E0 la fois un min\u00E9ral, une esp\u00E8ce chimique de formule 3 Ca3(PO4)2, Ca(OH,F,Cl)2, ainsi qu'une roche phosphat\u00E9e d'origine d\u00E9tritique dont il est le principal constituant."@fr . . 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"Fosforit"@cs . . . . .