. "6.5"^^ . "\u0645\u0639\u062F\u0646 \u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 \u0623\u0648 \u0627\u0644\u0632\u0628\u0631\u062C\u062F \u0627\u0644\u0632\u064A\u062A\u0648\u0646\u064A (olivine) \u0647\u0648 \u0645\u0639\u062F\u0646 \u0645\u0631\u0643\u0628 \u0645\u0646 \u0633\u064A\u0644\u064A\u0643\u0627\u062A \u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645 \u0648\u0627\u0644\u062D\u062F\u064A\u062F\u060C \u0648\u062A\u0631\u0643\u064A\u0628\u0647 \u0627\u0644\u0643\u064A\u0645\u064A\u0627\u0626\u064A (Mg,Fe)2SiO4. \u0648\u0647\u0648 \u0623\u062D\u062F \u0627\u0644\u0645\u0639\u0627\u062F\u0646 \u0627\u0644\u0645\u0648\u062C\u0648\u062F\u0629 \u0641\u064A \u0627\u0644\u0642\u0634\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629\u060C \u0643\u0645\u0627 \u064A\u0648\u062C\u062F \u0641\u064A \u0643\u062B\u064A\u0631 \u0645\u0646 \u0627\u0644\u0646\u064A\u0627\u0632\u0643 \u0648\u0627\u0644\u0634\u0647\u0628 \u0627\u0644\u0633\u0627\u0642\u0637\u0629 \u0639\u0644\u0649 \u0627\u0644\u0623\u0631\u0636\u060C \u0648\u0641\u064A \u0627\u0644\u0642\u0645\u0631 \u0648\u0641\u064A \u0627\u0644\u0645\u0630\u0646\u0628 \u0648\u064A\u0644\u062F 2. \u062A\u0633\u0645\u0649 \u0627\u0644\u062D\u0627\u0644\u0629 \u0627\u0644\u0646\u0642\u064A\u0629 \u0645\u0646\u0647 \u0630\u0627\u062A \u0627\u0644\u0628\u0644\u0648\u0631\u0627\u062A \u0627\u0644\u0643\u0628\u064A\u0631\u0629 \u0632\u0628\u0631\u062C\u062F peridot . \u064A\u062D\u062A\u0648\u064A \u0627\u0644\u0645\u0639\u062F\u0646 \u0639\u0644\u0649 \u062E\u0644\u064A\u0637 \u0645\u0646 \u0627\u0644\u0633\u0627\u0626\u0644\u064A\u0646 \u0627\u0644\u062C\u0627\u0645\u062F\u064A\u0646 \u0641\u0648\u0631\u0633\u062A\u0631\u064A\u062A forsterite \u0648\u0641\u064A\u0627\u0644\u064A\u062A fayalite \u062D\u064A\u062B \u062A\u0632\u064A\u062F \u0646\u0633\u0628\u0629 \u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645 \u0641\u064A \u0627\u0644\u0641\u0648\u0631\u0633\u062A\u0631\u064A\u062A \u0648\u062A\u0632\u064A\u062F \u0646\u0633\u0628\u0629 \u0627\u0644\u062D\u062F\u064A\u062F \u0641\u064A \u0627\u0644\u0641\u064A\u0627\u0644\u064A\u062A. \u0648\u064A\u062D\u062F\u062F \u062A\u0631\u0643\u064A\u0628 \u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 \u0639\u0644\u0649 \u0623\u0633\u0627\u0633 \u0627\u0644\u0646\u0633\u0628\u0629 \u0627\u0644\u0645\u0648\u0644\u064A\u0629 \u0644\u0644\u0641\u0648\u0631\u0633\u062A\u0631\u064A\u062A (Fo) \u0648\u0627\u0644\u0641\u064A\u0627\u0644\u064A\u062A (Fa) \u0645\u062B\u0644 Fo70Fa30. \u0648\u064A\u062A\u0645\u064A\u0632 \u0627\u0644\u0641\u0648\u0631\u0633\u062A\u0631\u064A\u062A \u0628\u062F\u0631\u062C\u0629 \u0627\u0646\u0635\u0647\u0627\u0631 \u0639\u0627\u0644\u064A\u0629 \u062A\u0628\u0644\u063A 1900 \u062F\u0631\u062C\u0629 \u0645\u0626\u0648\u064A\u0629\u060C \u0628\u064A\u0646\u0645\u0627 \u064A\u0646\u0635\u0647\u0631 \u0627\u0644\u0641\u064A\u0627\u0644\u064A\u062A \u0639\u0646 \u062F\u0631\u062C\u0629 \u0645\u0646\u062E\u0641\u0636\u0629 \u0646\u0633\u0628\u064A\u0627\u060C \u0639\u0646\u062F \u0646\u062D\u0648 1200 \u062F\u0631\u062C\u0629 \u0645\u0626\u0648\u064A\u0629. \u0648\u062A\u0639\u062A\u0645\u062F \u062F\u0631\u062C\u0629 \u0627\u0646\u0635\u0647\u0627\u0631 \u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 \u0639\u0644\u0649 \u0646\u0633\u0628\u0629 \u0627\u0644\u0641\u0648\u0631\u0633\u062A\u0631\u064A\u062A \u0625\u0644\u0649 \u0627\u0644\u0641\u064A\u0627\u0644\u064A\u062A\u060C \u0643\u0645\u0627 \u062A\u0639\u062A\u0645\u062F \u0627\u0644\u062E\u0648\u0627\u0635 \u0627\u0644\u0623\u062E\u0631\u0649 \u0644\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 \u0639\u0644\u0649 \u062A\u0644\u0643 \u0627\u0644\u0646\u0633\u0628\u0629. \u064A\u062D\u062A\u0648\u064A \u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 \u0639\u0627\u062F\u0629 \u0639\u0644\u0649 \u0643\u0645\u064A\u0627\u062A \u0628\u0633\u064A\u0637\u0629 \u0645\u0646 \u0627\u0644\u0634\u0648\u0627\u0626\u0628\u060C \u0623\u0647\u0645\u0647\u0627 \u0627\u0644\u0646\u064A\u0643\u0644 \u0648\u0627\u0644\u0645\u0646\u062C\u0646\u064A\u0632. \u0648\u0647\u0648 \u064A\u0648\u062C\u062F \u0641\u064A \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0646\u0627\u0631\u064A\u0629 \u0648\u0641\u064A \u0628\u0639\u0636 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0645\u062A\u062D\u0648\u0644\u0629. \u064A\u062A\u0628\u0644\u0648\u0631 \u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 \u0627\u0644\u063A\u0646\u064A \u0628\u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645 \u0645\u0646 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0627\u0644\u063A\u0646\u064A\u0629 \u0628\u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645 \u0648\u0627\u0644\u0641\u0642\u064A\u0631\u0629 \u0628\u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0627\u060C \u0648\u062A\u0643\u0648\u0646 \u062A\u0644\u0643 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0639\u0627\u062F\u0629 \u0628\u0627\u0632\u0644\u062A. \u0623\u0645\u0627 \u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 \u0627\u0644\u063A\u0646\u064A \u0628\u0627\u0644\u062D\u062F\u064A\u062F \u0641\u0647\u0648 \u0642\u0644\u064A\u0644 \u0627\u0644\u0648\u062C\u0648\u062F\u060C \u0648\u064A\u0648\u062C\u062F \u0641\u064A \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0646\u0627\u0631\u064A\u0629 \u0648\u0628\u0643\u0645\u064A\u0627\u062A \u0642\u0644\u064A\u0644\u0629 \u0641\u064A \u0627\u0644\u062C\u0631\u0627\u0646\u064A\u062A \u0648\u0627\u0644\u0631\u064A\u0648\u0644\u064A\u062A \u0648\u0627\u0644\u0643\u0648\u0627\u0631\u062A\u0632. \u0648\u0628\u0627\u0644\u0639\u0643\u0633 \u0641\u0644\u0627 \u064A\u0648\u062C\u062F \u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 \u0627\u0644\u063A\u0646\u064A \u0628\u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645 \u0641\u064A \u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0627 \u0648\u064A\u0643\u0648\u0646 \u0641\u064A \u062D\u0627\u0644\u0629 \u0645\u0633\u062A\u0642\u0631\u0629\u060C \u0625\u0630 \u064A\u062A\u0641\u0627\u0639\u0644 \u0648\u064A\u0634\u0643\u0644 \u0645\u0627 \u064A\u0633\u0645\u0649 \u0627\u0648\u0631\u062B\u0648\u0628\u064A\u0631\u0648\u0643\u0633\u064A\u0646 Mg,Fe)2Si2O6)."@ar . . . . . . . . . "\u041E\u043B\u0456\u0432\u0456\u043D \u2014 \u043F\u043E\u0440\u043E\u0434\u043E\u0442\u0432\u0456\u0440\u043D\u0438\u0439 \u043C\u0456\u043D\u0435\u0440\u0430\u043B \u043A\u043B\u0430\u0441\u0443 \u0441\u0438\u043B\u0456\u043A\u0430\u0442\u0456\u0432. \u041E\u0440\u0442\u043E\u0441\u0438\u043B\u0456\u043A\u0430\u0442 \u043C\u0430\u0433\u043D\u0456\u044E \u0442\u0430 \u0437\u0430\u043B\u0456\u0437\u0430 \u043E\u0441\u0442\u0440\u0456\u0432\u043D\u043E\u0457 \u0431\u0443\u0434\u043E\u0432\u0438. \u0412\u043C\u0456\u0441\u0442 \u0437\u0430\u043B\u0456\u0437\u0430 \u0456 \u043C\u0430\u0433\u043D\u0456\u044E \u0437\u043C\u0456\u043D\u044E\u0454\u0442\u044C\u0441\u044F \u043C\u0456\u0436 \u043A\u0440\u0430\u0439\u043D\u0456\u043C\u0438 \u0447\u043B\u0435\u043D\u0430\u043C\u0438 \u0456\u0437\u043E\u043C\u043E\u0440\u0444\u043D\u043E\u0433\u043E \u0440\u044F\u0434\u0443 \u043E\u043B\u0456\u0432\u0456\u043D\u0443: \u0444\u043E\u0440\u0441\u0442\u0435\u0440\u0438\u0442\u043E\u043C Mg2[SiO4] \u0456 \u0444\u0430\u044F\u043B\u0456\u0442\u043E\u043C \u2014 Fe2[SiO4]. \u041E\u043B\u0456\u0432\u0456\u043D \u0441\u043A\u043B\u0430\u0434\u0430\u0454 \u043E\u0441\u043D\u043E\u0432\u043D\u0456 \u0456 \u0443\u043B\u044C\u0442\u0440\u0430\u043E\u0441\u043D\u043E\u0432\u043D\u0456 \u043C\u0430\u0433\u043C\u0430\u0442\u0438\u0447\u043D\u0456 \u043F\u043E\u0440\u043E\u0434\u0438 \u0456 \u0454 \u0434\u0443\u0436\u0435 \u043F\u043E\u0448\u0438\u0440\u0435\u043D\u0438\u043C \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u043E\u043C \u0432 \u043C\u0430\u043D\u0442\u0456\u0457 \u0417\u0435\u043C\u043B\u0456. \u0426\u0435 \u043E\u0434\u0438\u043D \u0437 \u043D\u0430\u0439\u043F\u043E\u0448\u0438\u0440\u0435\u043D\u0456\u0448\u0438\u0445 \u0432 \u0437\u0435\u043C\u043D\u0456\u0439 \u043A\u043E\u0440\u0456 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432."@uk . "Olivin (sebagai batu mulia disebut juga atau krisolit), adalah mineral magnesium besi silikat dengan rumus (Mg,Fe)2SiO4. Banyak ditemukan di bawah permukaan bumi namun lapuk dengan cepat di permukaan bumi. Rasio magnesium dan besi bervariasi: forsterit (bila Mg dominan) ataupun fayalit (bila Fe dominan). Komposisi olivin umumnya dinyatakan sebagai persentase molar forsterit (Fo) dan fayalit (Fa) (contoh: Fo70Fa30). Forsterit memiliki titik lebur yang sangat tinggi dalam tekanan atmosfer, yaitu mencapai 1900 \u00B0C, tetapi fayalit memiliki titik lebur yang lebih rendah (kira-kira 1200 \u00B0C). Titik lebur bervariasi antara kedua pembentuknya, sebagaimana sifat-sifat lainnya. Olivin bisa menggabungkan unsur selain oksigen, silikon, magnesium, dan besi; hanya dalam jumlah sedikit. Umumnya mangan dan nikel merupakan unsur tambahan dengan konsentrasi tertinggi. Olivin menamai sebuah kelompok mineral dengan struktur terkait (kelompok olivin)yang meliputi teproit ((Mn2SiO4)), montiselit (CaMgSiO4) and kirschsteinit (CaFeSiO4)."@in . . . "\u6A44\u6984\u77F3"@zh . "Oliwiny \u2013 grupa minera\u0142\u00F3w zaliczana do krzemian\u00F3w. Maj\u0105 zazwyczaj barw\u0119 zielon\u0105 w odcieniach, ale te\u017C br\u0105zow\u0105, czarn\u0105 a wyj\u0105tkowo s\u0105 bia\u0142e lub bezbarwne. Og\u00F3lny wz\u00F3r chemiczny oliwin\u00F3w to (Mg, Fe)2 SiO4."@pl . . . . "colorless or white"@en . "\u0645\u0639\u062F\u0646 \u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 \u0623\u0648 \u0627\u0644\u0632\u0628\u0631\u062C\u062F \u0627\u0644\u0632\u064A\u062A\u0648\u0646\u064A (olivine) \u0647\u0648 \u0645\u0639\u062F\u0646 \u0645\u0631\u0643\u0628 \u0645\u0646 \u0633\u064A\u0644\u064A\u0643\u0627\u062A \u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645 \u0648\u0627\u0644\u062D\u062F\u064A\u062F\u060C \u0648\u062A\u0631\u0643\u064A\u0628\u0647 \u0627\u0644\u0643\u064A\u0645\u064A\u0627\u0626\u064A (Mg,Fe)2SiO4. \u0648\u0647\u0648 \u0623\u062D\u062F \u0627\u0644\u0645\u0639\u0627\u062F\u0646 \u0627\u0644\u0645\u0648\u062C\u0648\u062F\u0629 \u0641\u064A \u0627\u0644\u0642\u0634\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629\u060C \u0643\u0645\u0627 \u064A\u0648\u062C\u062F \u0641\u064A \u0643\u062B\u064A\u0631 \u0645\u0646 \u0627\u0644\u0646\u064A\u0627\u0632\u0643 \u0648\u0627\u0644\u0634\u0647\u0628 \u0627\u0644\u0633\u0627\u0642\u0637\u0629 \u0639\u0644\u0649 \u0627\u0644\u0623\u0631\u0636\u060C \u0648\u0641\u064A \u0627\u0644\u0642\u0645\u0631 \u0648\u0641\u064A \u0627\u0644\u0645\u0630\u0646\u0628 \u0648\u064A\u0644\u062F 2. \u062A\u0633\u0645\u0649 \u0627\u0644\u062D\u0627\u0644\u0629 \u0627\u0644\u0646\u0642\u064A\u0629 \u0645\u0646\u0647 \u0630\u0627\u062A \u0627\u0644\u0628\u0644\u0648\u0631\u0627\u062A \u0627\u0644\u0643\u0628\u064A\u0631\u0629 \u0632\u0628\u0631\u062C\u062F peridot . \u064A\u062D\u062A\u0648\u064A \u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 \u0639\u0627\u062F\u0629 \u0639\u0644\u0649 \u0643\u0645\u064A\u0627\u062A \u0628\u0633\u064A\u0637\u0629 \u0645\u0646 \u0627\u0644\u0634\u0648\u0627\u0626\u0628\u060C \u0623\u0647\u0645\u0647\u0627 \u0627\u0644\u0646\u064A\u0643\u0644 \u0648\u0627\u0644\u0645\u0646\u062C\u0646\u064A\u0632. \u0648\u0647\u0648 \u064A\u0648\u062C\u062F \u0641\u064A \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0646\u0627\u0631\u064A\u0629 \u0648\u0641\u064A \u0628\u0639\u0636 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0645\u062A\u062D\u0648\u0644\u0629. \u064A\u062A\u0628\u0644\u0648\u0631 \u0627\u0644\u0623\u0648\u0644\u064A\u0641\u064A\u0646 \u0627\u0644\u063A\u0646\u064A \u0628\u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645 \u0645\u0646 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0627\u0644\u063A\u0646\u064A\u0629 \u0628\u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645 \u0648\u0627\u0644\u0641\u0642\u064A\u0631\u0629 \u0628\u0627\u0644\u0633\u064A\u0644\u064A\u0643\u0627\u060C \u0648\u062A\u0643\u0648\u0646 \u062A\u0644\u0643 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0639\u0627\u062F\u0629 \u0628\u0627\u0632\u0644\u062A."@ar . "\u041E\u043B\u0438\u0432\u0438\u0301\u043D (\u0433\u0440\u0443\u043F\u043F\u0430 \u043E\u043B\u0438\u0432\u0438\u043D\u0430) \u2014 \u043F\u043E\u0440\u043E\u0434\u043E\u043E\u0431\u0440\u0430\u0437\u0443\u044E\u0449\u0438\u0439 \u043C\u0438\u043D\u0435\u0440\u0430\u043B, \u043C\u0430\u0433\u043D\u0435\u0437\u0438\u0430\u043B\u044C\u043D\u043E-\u0436\u0435\u043B\u0435\u0437\u0438\u0441\u0442\u044B\u0439 \u0441\u0438\u043B\u0438\u043A\u0430\u0442 \u0441 \u0444\u043E\u0440\u043C\u0443\u043B\u043E\u0439 (Mg,Fe)2[SiO4]. \u041E\u0431\u0440\u0430\u0437\u0443\u0435\u0442 \u0433\u0440\u0443\u043F\u043F\u0443 \u0438\u043B\u0438 \u0440\u044F\u0434 \u043E\u043B\u0438\u0432\u0438\u043D\u0430. \u0421\u043E\u0434\u0435\u0440\u0436\u0430\u043D\u0438\u0435 Fe \u0438 Mg \u0432\u0430\u0440\u044C\u0438\u0440\u0443\u0435\u0442 \u043C\u0435\u0436\u0434\u0443 \u0434\u0432\u0443\u043C\u044F \u043A\u043E\u043D\u0435\u0447\u043D\u044B\u043C\u0438 \u0447\u043B\u0435\u043D\u0430\u043C\u0438 \u043D\u0435\u043F\u0440\u0435\u0440\u044B\u0432\u043D\u043E\u0433\u043E \u0438\u0437\u043E\u043C\u043E\u0440\u0444\u043D\u043E\u0433\u043E \u0440\u044F\u0434\u0430 \u043E\u043B\u0438\u0432\u0438\u043D\u043E\u0432: \u0444\u043E\u0440\u0441\u0442\u0435\u0440\u0438\u0442\u043E\u043C (Fo) \u2014 Mg2[SiO4] \u0438 \u0444\u0430\u044F\u043B\u0438\u0442\u043E\u043C (Fa) \u2014 Fe2[SiO4]. \u041E\u043B\u0438\u0432\u0438\u043D \u0441\u043B\u0430\u0433\u0430\u0435\u0442 \u043E\u0441\u043D\u043E\u0432\u043D\u044B\u0435 \u0438 \u0443\u043B\u044C\u0442\u0440\u0430\u043E\u0441\u043D\u043E\u0432\u043D\u044B\u0435 \u043C\u0430\u0433\u043C\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u0438\u0435 \u043F\u043E\u0440\u043E\u0434\u044B \u0438 \u043E\u0447\u0435\u043D\u044C \u0448\u0438\u0440\u043E\u043A\u043E \u0440\u0430\u0441\u043F\u0440\u043E\u0441\u0442\u0440\u0430\u043D\u0451\u043D \u0432 \u043C\u0430\u043D\u0442\u0438\u0438. \u042D\u0442\u043E \u043E\u0434\u0438\u043D \u0438\u0437 \u0441\u0430\u043C\u044B\u0445 \u0440\u0430\u0441\u043F\u0440\u043E\u0441\u0442\u0440\u0430\u043D\u0451\u043D\u043D\u044B\u0445 \u043D\u0430 \u0417\u0435\u043C\u043B\u0435 \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u043E\u0432. \u0421\u0438\u043D\u043E\u043D\u0438\u043C \u2014 \u043F\u0435\u0440\u0438\u0434\u043E\u0442 (\u0441\u043B\u043E\u0432\u043E \u0444\u0440\u0430\u043D\u0446\u0443\u0437\u0441\u043A\u043E\u0433\u043E \u043F\u0440\u043E\u0438\u0441\u0445\u043E\u0436\u0434\u0435\u043D\u0438\u044F). \u041F\u0440\u043E\u0437\u0440\u0430\u0447\u043D\u0443\u044E \u0436\u0451\u043B\u0442\u043E-\u0437\u0435\u043B\u0451\u043D\u0443\u044E \u0434\u043E \u0437\u0435\u043B\u0451\u043D\u043E\u0439 \u0440\u0430\u0437\u043D\u043E\u0432\u0438\u0434\u043D\u043E\u0441\u0442\u044C \u043E\u043B\u0438\u0432\u0438\u043D\u0430, \u044F\u0432\u043B\u044F\u044E\u0449\u0443\u044E\u0441\u044F \u043F\u043E\u043B\u0443\u0434\u0440\u0430\u0433\u043E\u0446\u0435\u043D\u043D\u044B\u043C \u043A\u0430\u043C\u043D\u0435\u043C, \u043F\u0440\u0438\u043D\u044F\u0442\u043E \u043D\u0430\u0437\u044B\u0432\u0430\u0442\u044C \u0445\u0440\u0438\u0437\u043E\u043B\u0438\u0442\u043E\u043C."@ru . . . . . . "Olibino minerala (baita ere krisolita deitua eta gema denean ) magnesio eta burdinadun nesosilikato bat da (Mg,Fe)2SiO4 formularekin. Lurreko mineralik ohikoena da eta Ilargian eta Marten ere aurkitu da, hala nola kometan. Magnesio eta burdinaren arteko erratioa aldakorra da eta forsterita (magnesioa bakarrik) eta fayalita (burdina bakarrik) artean ibiltzen da. Euren arteko erlazioa normalean Fo eta Fa arteko portzentajeetan ematen da, adibidez: Fo70Fa30. Forsteritaren urtzen puntura oso altua da, 1900\u00B0C, baina fayalitarena baxuagoa da, 1200 \u00B0C. Olibinoak bere mineral taldeari izena ere ematen dio, antzeko estruktura baitu. Mineralak tefroita (Mn2SiO4), monticellita (CaMgSiO4), eta kirschsteinita (CaFeSiO4) dira."@eu . . . . . . "31084"^^ . . . "Olivina"@it . . . "Olivine group"@en . . . . . . . . . . "Olivino (el la latina oliva: olivo post aldono de \u2019\u2019in\u2019\u2019, pli frue aperis la vorto kiel oliveno, pro timo de la in-fina\u0135o) estas komuna nomo de silikat-mineraloj, kiuj fakte havas la kemian konsiston (Mg,Fe)2SiO4; la natura olivino entenas anka\u016D ankora\u016D etan kvanton de nikelo, kiu anstata\u016Das Mg a\u016D Fe. La krampigo signifas, ke fero kaj magnezio povas aperi kune en ia ajn rilato, sed \u0109iufoje du metalatomoj je unu silikata unuo SiO4. La tielnomataj finmembroj de la olivino estas la pli densa ferori\u0109a Fayalit Fe2SiO4 kaj la magneziori\u0109a Forsterit Mg2SiO4, la t.n. intermembroj estas Hyalosiderit kaj Hortonolith. La klaraj kaj grandaj olivinkristaloj estas aprezitaj juvel\u015Dtonoj kaj estas nomataj kiel peridoto a\u016D Chrysolith (Krisolit). Olivino kristali\u011Das en ortoromba kristala sistemo, havas duron inter 6,5 kaj 7, kaj flavverdan koloron en pura stato, cetere flavbrunan \u011Dis nigran koloron kaj blankan skrapokoloron. La kristaloj estas plej ofte prismaj a\u016D tavolaj."@eo . . "El olivino es un grupo de minerales constituyentes de rocas, aunque el nombre se suele aplicar con especial referencia a la principal soluci\u00F3n s\u00F3lida del grupo, que es entre forsterita (Mg2SiO4) y fayalita (Fe2SiO4).\u200B\u200B Los olivinos son de los minerales m\u00E1s importantes en la clasificaci\u00F3n de rocas \u00EDgneas.\u200B El olivino rico en magnesio destaca por ser el componente principal del manto superior de la Tierra.\u200B En cuanto a su qu\u00EDmica y estructura los olivinos son nesosilicatos que cristalizan en el sistema cristalino ortorr\u00F3mbico.\u200B La f\u00F3rmula qu\u00EDmica de los olivinos es A2SiO4 donde A puede ser hierro, magnesio, manganeso o n\u00EDquel entre otros.\u200B Mientras m\u00E1s hierro contiene m\u00E1s denso es el olivino.\u200B El color del olivino varia desde verde amarillento,\u200B a caf\u00E9\u200B y verde oliva\u200B siendo este \u00FAltimo color la raz\u00F3n de su nombre, que viene del lat\u00EDn.\u200B Contenidos bajos de hierro (12-15 %) le dan al olivino colores verdes y claros,\u200B mientras que olivinos ricos en fayalita suelen ser de color caf\u00E9 a negro.\u200B El olivino es una fuente de magnesio en la miner\u00EDa, y se extrae de rocas ricas en olivino como la dunita.\u200B En la industria minera tambi\u00E9n se emplea olivino para purificar hierro produciendo escoria.\u200B Aparte de esto el olivino tambi\u00E9n es utilizado en la fabricaci\u00F3n de materiales resistentes a bajas temperaturas.\u200B"@es . . "\u30AB\u30F3\u30E9\u30F3\u77F3"@ja . "L'olivina \u00E8 un minerale appartenente ai nesosilicati. \u00C8 una miscela isomorfa di forsterite (estremo magnesifero) Mg2SiO4 e fayalite (estremo ferrifero) Fe2SiO4. Questi ultimi sono rari in natura. Poich\u00E9 \u00E8 un termine intermedio di una serie, non \u00E8 considerato una specie valida dall'IMA, ma va considerata come nome della serie. Le olivine possono contenere manganese in sostituzione di ferro e magnesio. La sostituzione totale tra Mn e il Fe nella fayalite genera la tefroite (Mn2SiO4) e i termini intermedi della serie sono chiamati knebelite (Mn,Fe)2SiO4 (non riconosciuto dall'IMA); piccole quantit\u00E0 di zinco possono sostituirsi a (Fe,Mn) formando roepperite (non riconosciuto dall'IMA) mentre se si sostituisce il calcio si forma glauchocroite (CaMnSiO4). Un'altra serie relativamente rara delle olivine \u00E8 quella tra monticellite (CaMgSiO4) e kirschteinite (CaFeSiO4). Campioni trasparenti di olivina vengono tagliati e lavorati con ottimi risultati."@it . "Olivine series"@en . . "Oliwiny"@pl . . . "45159"^^ . "Es coneix com a olivina un grup de minerals intermedis de la s\u00E8rie de soluci\u00F3 s\u00F2lida que es forma entre la forsterita (Mg\u2082SiO\u2084) i la faialita (Fe\u2082SiO\u2084). Es tracta d'uns nesosilicats de ferro i magnesi corrents de les roques eruptives b\u00E0siques. Es troba t\u00EDpicament a les roques plut\u00F2niques, com ara les peridotites, i a les roques volc\u00E0niques. El seu nom deriva del llat\u00ED oliva, que, com en catal\u00E0, significa oliva, en al\u00B7lusi\u00F3 al color del mineral."@ca . . . . "L\u2019olivine est un min\u00E9ral du groupe des silicates, sous-groupe des n\u00E9sosilicates. Elle cristallise dans le syst\u00E8me orthorhombique. L'olivine n'a pas le statut d'esp\u00E8ce reconnue par l'Association internationale de min\u00E9ralogie , car \u00AB olivine \u00BB est en fait le nom g\u00E9n\u00E9rique de tous les min\u00E9raux de la s\u00E9rie forst\u00E9rite-fayalite. La vari\u00E9t\u00E9 gemme de la forst\u00E9rite est utilis\u00E9e comme pierre fine en joaillerie sous le nom de p\u00E9ridot."@fr . . . . "Het mineraal olivijn is een nesosilicaat met als chemische formule (Mg,Fe)2SiO4, waarbij de eindleden tussen magnesium en ijzer worden gevormd door de mineralenreeks forsteriet (rijk aan Mg) en fayaliet (rijk aan Fe)."@nl . . "Es coneix com a olivina un grup de minerals intermedis de la s\u00E8rie de soluci\u00F3 s\u00F2lida que es forma entre la forsterita (Mg\u2082SiO\u2084) i la faialita (Fe\u2082SiO\u2084). Es tracta d'uns nesosilicats de ferro i magnesi corrents de les roques eruptives b\u00E0siques. Es troba t\u00EDpicament a les roques plut\u00F2niques, com ara les peridotites, i a les roques volc\u00E0niques. El seu nom deriva del llat\u00ED oliva, que, com en catal\u00E0, significa oliva, en al\u00B7lusi\u00F3 al color del mineral."@ca . . "Biaxial"@en . "Olivino (el la latina oliva: olivo post aldono de \u2019\u2019in\u2019\u2019, pli frue aperis la vorto kiel oliveno, pro timo de la in-fina\u0135o) estas komuna nomo de silikat-mineraloj, kiuj fakte havas la kemian konsiston (Mg,Fe)2SiO4; la natura olivino entenas anka\u016D ankora\u016D etan kvanton de nikelo, kiu anstata\u016Das Mg a\u016D Fe. La krampigo signifas, ke fero kaj magnezio povas aperi kune en ia ajn rilato, sed \u0109iufoje du metalatomoj je unu silikata unuo SiO4. La tielnomataj finmembroj de la olivino estas la pli densa ferori\u0109a Fayalit Fe2SiO4 kaj la magneziori\u0109a Forsterit Mg2SiO4, la t.n. intermembroj estas Hyalosiderit kaj Hortonolith. La klaraj kaj grandaj olivinkristaloj estas aprezitaj juvel\u015Dtonoj kaj estas nomataj kiel peridoto a\u016D Chrysolith (Krisolit). Olivino kristali\u011Das en ortoromba kristala sistemo, havas duro"@eo . . . . "Ol"@en . "Olivine"@en . . . . "\u041E\u043B\u0456\u0432\u0456\u043D \u2014 \u043F\u043E\u0440\u043E\u0434\u043E\u0442\u0432\u0456\u0440\u043D\u0438\u0439 \u043C\u0456\u043D\u0435\u0440\u0430\u043B \u043A\u043B\u0430\u0441\u0443 \u0441\u0438\u043B\u0456\u043A\u0430\u0442\u0456\u0432. \u041E\u0440\u0442\u043E\u0441\u0438\u043B\u0456\u043A\u0430\u0442 \u043C\u0430\u0433\u043D\u0456\u044E \u0442\u0430 \u0437\u0430\u043B\u0456\u0437\u0430 \u043E\u0441\u0442\u0440\u0456\u0432\u043D\u043E\u0457 \u0431\u0443\u0434\u043E\u0432\u0438. \u0412\u043C\u0456\u0441\u0442 \u0437\u0430\u043B\u0456\u0437\u0430 \u0456 \u043C\u0430\u0433\u043D\u0456\u044E \u0437\u043C\u0456\u043D\u044E\u0454\u0442\u044C\u0441\u044F \u043C\u0456\u0436 \u043A\u0440\u0430\u0439\u043D\u0456\u043C\u0438 \u0447\u043B\u0435\u043D\u0430\u043C\u0438 \u0456\u0437\u043E\u043C\u043E\u0440\u0444\u043D\u043E\u0433\u043E \u0440\u044F\u0434\u0443 \u043E\u043B\u0456\u0432\u0456\u043D\u0443: \u0444\u043E\u0440\u0441\u0442\u0435\u0440\u0438\u0442\u043E\u043C Mg2[SiO4] \u0456 \u0444\u0430\u044F\u043B\u0456\u0442\u043E\u043C \u2014 Fe2[SiO4]. \u041E\u043B\u0456\u0432\u0456\u043D \u0441\u043A\u043B\u0430\u0434\u0430\u0454 \u043E\u0441\u043D\u043E\u0432\u043D\u0456 \u0456 \u0443\u043B\u044C\u0442\u0440\u0430\u043E\u0441\u043D\u043E\u0432\u043D\u0456 \u043C\u0430\u0433\u043C\u0430\u0442\u0438\u0447\u043D\u0456 \u043F\u043E\u0440\u043E\u0434\u0438 \u0456 \u0454 \u0434\u0443\u0436\u0435 \u043F\u043E\u0448\u0438\u0440\u0435\u043D\u0438\u043C \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u043E\u043C \u0432 \u043C\u0430\u043D\u0442\u0456\u0457 \u0417\u0435\u043C\u043B\u0456. \u0426\u0435 \u043E\u0434\u0438\u043D \u0437 \u043D\u0430\u0439\u043F\u043E\u0448\u0438\u0440\u0435\u043D\u0456\u0448\u0438\u0445 \u0432 \u0437\u0435\u043C\u043D\u0456\u0439 \u043A\u043E\u0440\u0456 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432."@uk . . "Olivina \u00E9 um grupo de minerais da fam\u00EDlia dos nesossilicatos cujos membros s\u00E3o constitu\u00EDdos por silicatos de magn\u00E9sio e ferro, com f\u00F3rmula qu\u00EDmica (Mg,Fe)2SiO4, formando uma solu\u00E7\u00E3o s\u00F3lida em que a raz\u00E3o Fe/Mg varia entre dois extremos constitu\u00EDdos pela forsterite (Mg2SiO4) e a faialite (Fe2SiO4). Este mineral d\u00E1 ainda o nome a um grupo de minerais com estrutura semelhante (o grupo da olivina) que inclui os minerais monticellite e . Os minerais do grupo da olivina cristalizam no sistema ortorr\u00F4mbico, e s\u00E3o nesossilicatos."@pt . . . . "Olibino"@eu . . . "brittle"@en . . . "\u30AB\u30F3\u30E9\u30F3\u77F3\uFF08\u304B\u3093\u3089\u3093\u305B\u304D\u3001\u6A44\u6B16\u77F3\u3001olivine\u3001\u30AA\u30EA\u30D3\u30F3\uFF09\u306F\u3001\u9271\u7269\uFF08\u30B1\u30A4\u9178\u5869\u9271\u7269\uFF09\u306E\u30B0\u30EB\u30FC\u30D7\u540D\u3002 \u30DE\u30B0\u30CD\u30B7\u30A6\u30E0\u3084\u9244\u306E\u30CD\u30BD\u30B1\u30A4\u9178\u5869\u9271\u7269\u3067\u3042\u308B\u3002Mg2SiO4\uFF08\u82E6\u571F\u6A44\u6B16\u77F3\uFF09\u3068 Fe2SiO4\uFF08\u9244\u6A44\u6B16\u77F3\uFF09\u3068\u306E\u9593\u306E\u9023\u7D9A\u56FA\u6EB6\u4F53\u3092\u306A\u3059\u3002 \u591A\u304F\u306E\u30AB\u30F3\u30E9\u30F3\u77F3\u306F\u3001\u5730\u7403\u306E\u5927\u90E8\u5206\u3092\u5360\u3081\u3001\u5730\u4E0A\u306B\u706B\u6210\u5CA9\u3068\u3057\u3066\u51FA\u3066\u304D\u305F\u30AB\u30F3\u30E9\u30F3\u5CA9\uFF08peridotite\uFF09\u3082\u30DE\u30F3\u30C8\u30EB\u7531\u6765\u3067\u3042\u308B\u3002\u7D50\u6676\u5316\u3057\u305F\u3082\u306E\u306F\u5B9D\u77F3\u306E\u30DA\u30EA\u30C9\u30C3\u30C8\u3067\u3042\u308B\u3002"@ja . . "Oliwiny \u2013 grupa minera\u0142\u00F3w zaliczana do krzemian\u00F3w. Maj\u0105 zazwyczaj barw\u0119 zielon\u0105 w odcieniach, ale te\u017C br\u0105zow\u0105, czarn\u0105 a wyj\u0105tkowo s\u0105 bia\u0142e lub bezbarwne. Og\u00F3lny wz\u00F3r chemiczny oliwin\u00F3w to (Mg, Fe)2 SiO4."@pl . . . "Olivina"@pt . . . . . . . . . . "Poor"@en . "Olivine"@fr . . . . "9"^^ . . . . "L\u2019olivine est un min\u00E9ral du groupe des silicates, sous-groupe des n\u00E9sosilicates. Elle cristallise dans le syst\u00E8me orthorhombique. L'olivine n'a pas le statut d'esp\u00E8ce reconnue par l'Association internationale de min\u00E9ralogie , car \u00AB olivine \u00BB est en fait le nom g\u00E9n\u00E9rique de tous les min\u00E9raux de la s\u00E9rie forst\u00E9rite-fayalite. La vari\u00E9t\u00E9 gemme de la forst\u00E9rite est utilis\u00E9e comme pierre fine en joaillerie sous le nom de p\u00E9ridot."@fr . "Olibino minerala (baita ere krisolita deitua eta gema denean ) magnesio eta burdinadun nesosilikato bat da (Mg,Fe)2SiO4 formularekin. Lurreko mineralik ohikoena da eta Ilargian eta Marten ere aurkitu da, hala nola kometan. Magnesio eta burdinaren arteko erratioa aldakorra da eta forsterita (magnesioa bakarrik) eta fayalita (burdina bakarrik) artean ibiltzen da. Euren arteko erlazioa normalean Fo eta Fa arteko portzentajeetan ematen da, adibidez: Fo70Fa30. Forsteritaren urtzen puntura oso altua da, 1900\u00B0C, baina fayalitarena baxuagoa da, 1200 \u00B0C."@eu . . . . . . "Het mineraal olivijn is een nesosilicaat met als chemische formule (Mg,Fe)2SiO4, waarbij de eindleden tussen magnesium en ijzer worden gevormd door de mineralenreeks forsteriet (rijk aan Mg) en fayaliet (rijk aan Fe)."@nl . "Yellow to yellow-green"@en . "\uAC10\uB78C\uC11D(\uC601\uC5B4: olivine)\uC740 \uB9C8\uADF8\uB124\uC298-\uCCA0\uC9C8\uC758 \uADDC\uC0B0\uC5FC \uAD11\uBB3C\uB85C \uD654\uD559\uC2DD\uC740 (Mg2+,Fe2+)2SiO4\uC774\uBA70, \uB9C8\uADF8\uB124\uC298\uACFC \uCCA0\uC758 \uBE44\uAC00 \uB450 \uB0B4\uC131\uBD84\uC778 (\uB9C8\uADF8\uB124\uC298 \uB0B4\uC131\uBD84)\uC640 (\uCCA0 \uB0B4\uC131\uBD84) \uC0AC\uC774\uC5D0\uC11C \uBCC0\uD654\uD558\uB294 \uACE0\uC6A9\uCCB4\uC774\uB2E4. \uD06C\uB9AC\uC194\uB77C\uC774\uD2B8(chrysolite)\uB77C\uACE0 \uBD88\uB9AC\uAE30\uB3C4 \uD558\uBA70 \uBCF4\uC11D \uC218\uC900\uC758 \uD488\uC9C8\uC744 \uAC00\uC9C8 \uB54C\uB294 \uD398\uB9AC\uB3C4\uD2B8\uB77C\uACE0 \uD55C\uB2E4. \uC774\uB294 8\uC6D4\uC758 \uD0C4\uC0DD\uC11D\uC774\uAE30\uB3C4 \uD558\uB2E4. \uC9C0\uAD6C \uC0C1\uC5D0\uC11C \uAC00\uC7A5 \uD754\uD55C \uAD11\uBB3C \uC911\uC758 \uD558\uB098\uC774\uBA70 \uB2EC, \uD654\uC131, , \uAE30\uD0C0 \uB9CE\uC740 \uC6B4\uC11D \uB4F1\uC5D0\uC11C\uB3C4 \uADF8 \uC874\uC7AC\uAC00 \uD655\uC778\uB418\uC5C8\uB2E4. \uAC10\uB78C\uC11D\uC758 \uC131\uBD84\uC740 \uBCF4\uD1B5 \uCCA0\uACFC \uB9C8\uADF8\uB124\uC298\uC758 \uBAB0\uC218\uBE44\uB85C \uB098\uD0C0\uB0B8\uB2E4. \uD3EC\uC2A4\uD130\uB77C\uC774\uD2B8\uB294 1900 \u00B0C\uC5D0 \uC774\uB974\uB294 \uC720\uB2EC\uB9AC \uB192\uC740 \uB179\uB294\uC810\uC744 \uAC00\uC9C0\uACE0 \uC788\uC73C\uB098 \uD30C\uC584\uB77C\uC774\uD2B8\uC758 \uB179\uB294\uC810\uC740 1200 \u00B0C \uC815\uB3C4\uC774\uB2E4."@ko . . "Olivin (sebagai batu mulia disebut juga atau krisolit), adalah mineral magnesium besi silikat dengan rumus (Mg,Fe)2SiO4. Banyak ditemukan di bawah permukaan bumi namun lapuk dengan cepat di permukaan bumi. Olivin menamai sebuah kelompok mineral dengan struktur terkait (kelompok olivin)yang meliputi teproit ((Mn2SiO4)), montiselit (CaMgSiO4) and kirschsteinit (CaFeSiO4)."@in . . . . . . "\uAC10\uB78C\uC11D"@ko . "L'olivina \u00E8 un minerale appartenente ai nesosilicati. \u00C8 una miscela isomorfa di forsterite (estremo magnesifero) Mg2SiO4 e fayalite (estremo ferrifero) Fe2SiO4. Questi ultimi sono rari in natura. Poich\u00E9 \u00E8 un termine intermedio di una serie, non \u00E8 considerato una specie valida dall'IMA, ma va considerata come nome della serie. Campioni trasparenti di olivina vengono tagliati e lavorati con ottimi risultati."@it . . "Massive to granular"@en . . . . . . . . . "Mianra sileac\u00E1ite a mb\u00EDonn comhdh\u00E9anaimh \u00E9ags\u00FAla aige, ina measc Fe2SiO4 is Mg2SiO4. Gloini\u00FAil crua, ar ghlaise na hol\u00F3ige de ghn\u00E1th. Suntasach i gcarraigeacha at\u00E1 gann i silice. Comhph\u00E1irt phr\u00EDomh\u00FAil de screamh an Domhain. Tugtar peiriadat ar a chriostal de chine\u00E1l seoide."@ga . . . . "n\u03B1 = 1.630\u20131.650"@en . . . "\u6A44\u6984\u77F3\uFF08\u82F1\u6587\uFF1AOlivine\uFF09\u662F\u4E00\u79CD\u9541\u4E0E\u94C1\u7684\u7845\u9178\u76D0\uFF0C\u5176\u5316\u5B66\u5F0F\u4E3A(Mg,Fe)2SiO4\u3002\u5B83\u662F\u5730\u7403\u5730\u8868\u4E0B\u6700\u5E38\u89C1\u7684\u77FF\u7269\u4E4B\u4E00\uFF0C\u4F46\u662F\u5728\u5730\u8868\u8868\u9762\u4E0A\u5F88\u5FEB\u4F1A\u98CE\u5316\u3002\u5B83\u8FD8\u51FA\u73B0\u5728\u90E8\u5206\u9668\u77F3\u3001\u6708\u7403\u3001\u706B\u661F\u53CA\u4E00\u4E9B\u5F57\u661F\u4E0A\uFF08\u5982\u7EF4\u5C14\u7279\u4E8C\u53F7\u5F57\u661F\u4E0A\u5F57\u9AEE\u90E8\u5206\u7684\u5C18\u57C3\uFF0C\u4EE5\u53CA\u5766\u666E\u5C14\u4E00\u53F7\u5F57\u661F\u7684\u5F57\u6838\uFF09\u3002 \u6A44\u6984\u77F3\uFF08Olivine\uFF09\u56E0\u989C\u8272\u5982\u6A44\u6984\uFF08Olive\uFF09\u800C\u5F97\u540D\uFF0C\u5B9D\u77F3\u7EA7\u7684\u6A44\u6984\u77F3\u53C8\u79F0\u7FE0\u7EFF\u6A44\u6984\u77F3\u6216\uFF0C\u8FD9\u4E00\u540D\u79F0\u76F4\u63A5\u6E90\u4E8E\u6CD5\u6587p\u00E9ridot\u3002\u6A44\u6984\u77F3\u662F\uFF08Mg2SiO4\uFF09\u2014\uFF08Fe2SiO4\uFF09\u7CFB\u5217\u4E2D\u6700\u5E38\u89C1\u7684\u4E00\u4E2A\u6210\u5458\uFF0C\u4E5F\u662F\u8FD9\u4E24\u79CD\u5F62\u6210\u7684\u56FA\u6EB6\u4F53\u3002\u6A44\u6984\u77F3\u7684\u6210\u5206\u7ECF\u5E38\u7531\u9541\u6A44\u6984\u77F3\uFF08Fo\uFF09\u548C\u94C1\u6A44\u6984\u77F3\uFF08Fa\uFF09\u8FD9\u4E24\u79CD\u7AEF\u5143\u7EC4\u5206\u7684\u8868\u793A\uFF0C\u4F8B\u5982Fo70 Fa30\u8868\u793A\u9541\u6A44\u6984\u77F3\u7AEF\u5143\u7EC4\u5206\u536070%\u7684\u6A44\u6984\u77F3\u3002\u5728\u5E38\u538B\u4E0B\uFF0C\u9541\u6A44\u6984\u77F3\u6709\u975E\u5E38\u9AD8\u7684\u7194\u70B9\uFF08\u63A5\u8FD11900\u00B0C\uFF09\uFF0C\u4F46\u94C1\u6A44\u6984\u77F3\u7684\u7194\u70B9\u5C31\u4F4E\u4E86\u5F88\u591A\uFF0C\u53EA\u6709\u7EA61200\u00B0C\u3002\u7194\u70B9\u4EE5\u53CA\u5176\u4ED6\u7269\u7406\u91CF\u968F\u6A44\u6984\u77F3\u7684\u6210\u5206\u5728\u9541\u6A44\u6984\u77F3\u4E0E\u94C1\u6A44\u6984\u77F3\u8FD9\u4E24\u79CD\u7AEF\u5143\u7EC4\u5206\u4E4B\u95F4\u8FDE\u7EED\u53D8\u5316\u3002\u9664\u4E86\u6C27\u3001\u7845\u3001\u9541\u548C\u94C1\u8FD9\u56DB\u79CD\u5143\u7D20\u4E4B\u5916\uFF0C\u6A44\u6984\u77F3\u53EA\u542B\u6709\u5F88\u5C11\u91CF\u7684\u5176\u4ED6\u5143\u7D20\uFF0C\u5E38\u89C1\u5982\u9530\u548C\u954D\u3002 \u4E0E\u6A44\u6984\u77F3\u7ED3\u6784\u76F8\u4F3C\u7684\u77FF\u7269\u7EC4\u6210\u4E86\u6A44\u6984\u77F3\u7C7B\u77FF\u7269\u3002\u6B64\u7C7B\u77FF\u7269\u5305\u62EC\uFF08Mn2SiO4\uFF09\u3001\uFF08CaMgSiO4\uFF09\u4EE5\u53CA \uFF08CaFeSiO4\uFF09\u3002"@zh . "Olivino"@eo . . . . . . . "\u30AB\u30F3\u30E9\u30F3\u77F3\uFF08\u304B\u3093\u3089\u3093\u305B\u304D\u3001\u6A44\u6B16\u77F3\u3001olivine\u3001\u30AA\u30EA\u30D3\u30F3\uFF09\u306F\u3001\u9271\u7269\uFF08\u30B1\u30A4\u9178\u5869\u9271\u7269\uFF09\u306E\u30B0\u30EB\u30FC\u30D7\u540D\u3002 \u30DE\u30B0\u30CD\u30B7\u30A6\u30E0\u3084\u9244\u306E\u30CD\u30BD\u30B1\u30A4\u9178\u5869\u9271\u7269\u3067\u3042\u308B\u3002Mg2SiO4\uFF08\u82E6\u571F\u6A44\u6B16\u77F3\uFF09\u3068 Fe2SiO4\uFF08\u9244\u6A44\u6B16\u77F3\uFF09\u3068\u306E\u9593\u306E\u9023\u7D9A\u56FA\u6EB6\u4F53\u3092\u306A\u3059\u3002 \u591A\u304F\u306E\u30AB\u30F3\u30E9\u30F3\u77F3\u306F\u3001\u5730\u7403\u306E\u5927\u90E8\u5206\u3092\u5360\u3081\u3001\u5730\u4E0A\u306B\u706B\u6210\u5CA9\u3068\u3057\u3066\u51FA\u3066\u304D\u305F\u30AB\u30F3\u30E9\u30F3\u5CA9\uFF08peridotite\uFF09\u3082\u30DE\u30F3\u30C8\u30EB\u7531\u6765\u3067\u3042\u308B\u3002\u7D50\u6676\u5316\u3057\u305F\u3082\u306E\u306F\u5B9D\u77F3\u306E\u30DA\u30EA\u30C9\u30C3\u30C8\u3067\u3042\u308B\u3002"@ja . . "Olivino"@es . "\u041E\u043B\u0438\u0432\u0438\u0301\u043D (\u0433\u0440\u0443\u043F\u043F\u0430 \u043E\u043B\u0438\u0432\u0438\u043D\u0430) \u2014 \u043F\u043E\u0440\u043E\u0434\u043E\u043E\u0431\u0440\u0430\u0437\u0443\u044E\u0449\u0438\u0439 \u043C\u0438\u043D\u0435\u0440\u0430\u043B, \u043C\u0430\u0433\u043D\u0435\u0437\u0438\u0430\u043B\u044C\u043D\u043E-\u0436\u0435\u043B\u0435\u0437\u0438\u0441\u0442\u044B\u0439 \u0441\u0438\u043B\u0438\u043A\u0430\u0442 \u0441 \u0444\u043E\u0440\u043C\u0443\u043B\u043E\u0439 (Mg,Fe)2[SiO4]. \u041E\u0431\u0440\u0430\u0437\u0443\u0435\u0442 \u0433\u0440\u0443\u043F\u043F\u0443 \u0438\u043B\u0438 \u0440\u044F\u0434 \u043E\u043B\u0438\u0432\u0438\u043D\u0430. \u0421\u043E\u0434\u0435\u0440\u0436\u0430\u043D\u0438\u0435 Fe \u0438 Mg \u0432\u0430\u0440\u044C\u0438\u0440\u0443\u0435\u0442 \u043C\u0435\u0436\u0434\u0443 \u0434\u0432\u0443\u043C\u044F \u043A\u043E\u043D\u0435\u0447\u043D\u044B\u043C\u0438 \u0447\u043B\u0435\u043D\u0430\u043C\u0438 \u043D\u0435\u043F\u0440\u0435\u0440\u044B\u0432\u043D\u043E\u0433\u043E \u0438\u0437\u043E\u043C\u043E\u0440\u0444\u043D\u043E\u0433\u043E \u0440\u044F\u0434\u0430 \u043E\u043B\u0438\u0432\u0438\u043D\u043E\u0432: \u0444\u043E\u0440\u0441\u0442\u0435\u0440\u0438\u0442\u043E\u043C (Fo) \u2014 Mg2[SiO4] \u0438 \u0444\u0430\u044F\u043B\u0438\u0442\u043E\u043C (Fa) \u2014 Fe2[SiO4]. \u041E\u043B\u0438\u0432\u0438\u043D \u0441\u043B\u0430\u0433\u0430\u0435\u0442 \u043E\u0441\u043D\u043E\u0432\u043D\u044B\u0435 \u0438 \u0443\u043B\u044C\u0442\u0440\u0430\u043E\u0441\u043D\u043E\u0432\u043D\u044B\u0435 \u043C\u0430\u0433\u043C\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u0438\u0435 \u043F\u043E\u0440\u043E\u0434\u044B \u0438 \u043E\u0447\u0435\u043D\u044C \u0448\u0438\u0440\u043E\u043A\u043E \u0440\u0430\u0441\u043F\u0440\u043E\u0441\u0442\u0440\u0430\u043D\u0451\u043D \u0432 \u043C\u0430\u043D\u0442\u0438\u0438. \u042D\u0442\u043E \u043E\u0434\u0438\u043D \u0438\u0437 \u0441\u0430\u043C\u044B\u0445 \u0440\u0430\u0441\u043F\u0440\u043E\u0441\u0442\u0440\u0430\u043D\u0451\u043D\u043D\u044B\u0445 \u043D\u0430 \u0417\u0435\u043C\u043B\u0435 \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u043E\u0432."@ru . "Oliv\u00EDn (peridot) (Werner, 1789), chemick\u00FD vzorec (Mg,Fe)2[SiO4] je koso\u010Dtvere\u010Dn\u00FD miner\u00E1l s prom\u011Bnliv\u00FDm pod\u00EDlem ho\u0159\u010D\u00EDku a \u017Eeleza v z\u00E1vislosti na podm\u00EDnk\u00E1ch p\u0159i jeho vzniku. Pr\u00E1v\u011B \u017Eelezo zp\u016Fsobuje zelen\u00E9 zabarven\u00ED kamene. Perfekcionist\u00E9 tvrd\u00ED, \u017Ee dokonal\u00FD oliv\u00EDn by m\u011Bl obsahovat m\u00E9n\u011B ne\u017E 15 % \u017Eeleza a \u017Ee nesm\u00ED v jeho m\u0159\u00ED\u017Ece chyb\u011Bt stopov\u00E9 prvky niklu a chromu. Krajn\u00ED \u010Dleny izomorfn\u00ED \u0159ady jsou forsterit \u2013 Mg2[SiO4] a \u2013 Fe2[SiO4]."@cs . . . . . . . . . . "The mineral olivine (/\u02C8\u0252l.\u026A\u02CCvi\u02D0n/) is a magnesium iron silicate with the chemical formula (Mg,Fe)2SiO4. It is a type of nesosilicate or orthosilicate. The primary component of the Earth's upper mantle, it is a common mineral in Earth's subsurface, but weathers quickly on the surface. For this reason, olivine has been proposed as a good candidate for accelerated weathering to sequester carbon dioxide from the Earth's oceans and atmosphere, as part of climate change mitigation. Olivine also has many other historical uses, such as the gemstone peridot (or chrysolite), as well as industrial applications like metalworking processes. The ratio of magnesium to iron varies between the two endmembers of the solid solution series: forsterite (Mg-endmember: Mg2SiO4) and fayalite (Fe-endmember: Fe2SiO4). Compositions of olivine are commonly expressed as molar percentages of forsterite (Fo) and fayalite (Fa) (e.g., Fo70Fa30). Forsterite's melting temperature is unusually high at atmospheric pressure, almost 1,900 \u00B0C (3,450 \u00B0F), while fayalite's is much lower \u2013 about 1,200 \u00B0C (2,190 \u00B0F). Melting temperature varies smoothly between the two endmembers, as do other properties. Olivine incorporates only minor amounts of elements other than oxygen (O), silicon (Si), magnesium (Mg) and iron (Fe). Manganese (Mn) and nickel (Ni) commonly are the additional elements present in highest concentrations. Olivine gives its name to the group of minerals with a related structure (the olivine group) \u2013 which includes tephroite (Mn2SiO4), monticellite (CaMgSiO4), larnite (Ca2SiO4) and kirschsteinite (CaFeSiO4) (commonly also spelled kirschteinite). Olivine's crystal structure incorporates aspects of the orthorhombic P Bravais lattice, which arise from each silica (SiO4) unit being joined by metal divalent cations with each oxygen in SiO4 bound to three metal ions. It has a spinel-like structure similar to magnetite but uses one quadrivalent and two divalent cations M22+ M4+O4 instead of two trivalent and one divalent cations."@en . "n\u03B3 = 1.670\u20131.690"@en . "432000.0"^^ . "Olivin"@in . . . . "n\u03B2 = 1.650\u20131.670"@en . . . . . . . . "Transparent to translucent"@en . "Olivijn"@nl . . . . "\u0632\u0628\u0631\u062C\u062F \u0632\u064A\u062A\u0648\u0646\u064A"@ar . . "Oliv\u00EDn"@cs . . . . "Vitreous"@en . . . . . . . . . "Olivina \u00E9 um grupo de minerais da fam\u00EDlia dos nesossilicatos cujos membros s\u00E3o constitu\u00EDdos por silicatos de magn\u00E9sio e ferro, com f\u00F3rmula qu\u00EDmica (Mg,Fe)2SiO4, formando uma solu\u00E7\u00E3o s\u00F3lida em que a raz\u00E3o Fe/Mg varia entre dois extremos constitu\u00EDdos pela forsterite (Mg2SiO4) e a faialite (Fe2SiO4). Este mineral d\u00E1 ainda o nome a um grupo de minerais com estrutura semelhante (o grupo da olivina) que inclui os minerais monticellite e . Os minerais do grupo da olivina cristalizam no sistema ortorr\u00F4mbico, e s\u00E3o nesossilicatos. \u00C9 um dos minerais mais comuns na Terra, tendo tamb\u00E9m sido encontrada em rochas lunares, em meteoritos e inclusive em rochas de Marte."@pt . . "Olivin \u00E4r ett m\u00F6rkt, gr\u00F6nf\u00E4rgat mineral som oftast f\u00F6rknippas med basiska bergarter. Det \u00E4r ett av v\u00E4rldens vanligaste mineral."@sv . . . . . . "Olivina"@ca . . . . . . . . . "Pbnm"@en . . . . . . . . . . "Olivin \u00E4r ett m\u00F6rkt, gr\u00F6nf\u00E4rgat mineral som oftast f\u00F6rknippas med basiska bergarter. Det \u00E4r ett av v\u00E4rldens vanligaste mineral."@sv . "\u03B4 = 0.040"@en . . . . "\u6A44\u6984\u77F3\uFF08\u82F1\u6587\uFF1AOlivine\uFF09\u662F\u4E00\u79CD\u9541\u4E0E\u94C1\u7684\u7845\u9178\u76D0\uFF0C\u5176\u5316\u5B66\u5F0F\u4E3A(Mg,Fe)2SiO4\u3002\u5B83\u662F\u5730\u7403\u5730\u8868\u4E0B\u6700\u5E38\u89C1\u7684\u77FF\u7269\u4E4B\u4E00\uFF0C\u4F46\u662F\u5728\u5730\u8868\u8868\u9762\u4E0A\u5F88\u5FEB\u4F1A\u98CE\u5316\u3002\u5B83\u8FD8\u51FA\u73B0\u5728\u90E8\u5206\u9668\u77F3\u3001\u6708\u7403\u3001\u706B\u661F\u53CA\u4E00\u4E9B\u5F57\u661F\u4E0A\uFF08\u5982\u7EF4\u5C14\u7279\u4E8C\u53F7\u5F57\u661F\u4E0A\u5F57\u9AEE\u90E8\u5206\u7684\u5C18\u57C3\uFF0C\u4EE5\u53CA\u5766\u666E\u5C14\u4E00\u53F7\u5F57\u661F\u7684\u5F57\u6838\uFF09\u3002 \u6A44\u6984\u77F3\uFF08Olivine\uFF09\u56E0\u989C\u8272\u5982\u6A44\u6984\uFF08Olive\uFF09\u800C\u5F97\u540D\uFF0C\u5B9D\u77F3\u7EA7\u7684\u6A44\u6984\u77F3\u53C8\u79F0\u7FE0\u7EFF\u6A44\u6984\u77F3\u6216\uFF0C\u8FD9\u4E00\u540D\u79F0\u76F4\u63A5\u6E90\u4E8E\u6CD5\u6587p\u00E9ridot\u3002\u6A44\u6984\u77F3\u662F\uFF08Mg2SiO4\uFF09\u2014\uFF08Fe2SiO4\uFF09\u7CFB\u5217\u4E2D\u6700\u5E38\u89C1\u7684\u4E00\u4E2A\u6210\u5458\uFF0C\u4E5F\u662F\u8FD9\u4E24\u79CD\u5F62\u6210\u7684\u56FA\u6EB6\u4F53\u3002\u6A44\u6984\u77F3\u7684\u6210\u5206\u7ECF\u5E38\u7531\u9541\u6A44\u6984\u77F3\uFF08Fo\uFF09\u548C\u94C1\u6A44\u6984\u77F3\uFF08Fa\uFF09\u8FD9\u4E24\u79CD\u7AEF\u5143\u7EC4\u5206\u7684\u8868\u793A\uFF0C\u4F8B\u5982Fo70 Fa30\u8868\u793A\u9541\u6A44\u6984\u77F3\u7AEF\u5143\u7EC4\u5206\u536070%\u7684\u6A44\u6984\u77F3\u3002\u5728\u5E38\u538B\u4E0B\uFF0C\u9541\u6A44\u6984\u77F3\u6709\u975E\u5E38\u9AD8\u7684\u7194\u70B9\uFF08\u63A5\u8FD11900\u00B0C\uFF09\uFF0C\u4F46\u94C1\u6A44\u6984\u77F3\u7684\u7194\u70B9\u5C31\u4F4E\u4E86\u5F88\u591A\uFF0C\u53EA\u6709\u7EA61200\u00B0C\u3002\u7194\u70B9\u4EE5\u53CA\u5176\u4ED6\u7269\u7406\u91CF\u968F\u6A44\u6984\u77F3\u7684\u6210\u5206\u5728\u9541\u6A44\u6984\u77F3\u4E0E\u94C1\u6A44\u6984\u77F3\u8FD9\u4E24\u79CD\u7AEF\u5143\u7EC4\u5206\u4E4B\u95F4\u8FDE\u7EED\u53D8\u5316\u3002\u9664\u4E86\u6C27\u3001\u7845\u3001\u9541\u548C\u94C1\u8FD9\u56DB\u79CD\u5143\u7D20\u4E4B\u5916\uFF0C\u6A44\u6984\u77F3\u53EA\u542B\u6709\u5F88\u5C11\u91CF\u7684\u5176\u4ED6\u5143\u7D20\uFF0C\u5E38\u89C1\u5982\u9530\u548C\u954D\u3002 \u4E0E\u6A44\u6984\u77F3\u7ED3\u6784\u76F8\u4F3C\u7684\u77FF\u7269\u7EC4\u6210\u4E86\u6A44\u6984\u77F3\u7C7B\u77FF\u7269\u3002\u6B64\u7C7B\u77FF\u7269\u5305\u62EC\uFF08Mn2SiO4\uFF09\u3001\uFF08CaMgSiO4\uFF09\u4EE5\u53CA \uFF08CaFeSiO4\uFF09\u3002"@zh . . . "1118363866"^^ . . . . "Mianra sileac\u00E1ite a mb\u00EDonn comhdh\u00E9anaimh \u00E9ags\u00FAla aige, ina measc Fe2SiO4 is Mg2SiO4. Gloini\u00FAil crua, ar ghlaise na hol\u00F3ige de ghn\u00E1th. Suntasach i gcarraigeacha at\u00E1 gann i silice. Comhph\u00E1irt phr\u00EDomh\u00FAil de screamh an Domhain. Tugtar peiriadat ar a chriostal de chine\u00E1l seoide."@ga . . . . . . . . "Olivine"@en . . "Olivine"@en . . "The mineral olivine (/\u02C8\u0252l.\u026A\u02CCvi\u02D0n/) is a magnesium iron silicate with the chemical formula (Mg,Fe)2SiO4. It is a type of nesosilicate or orthosilicate. The primary component of the Earth's upper mantle, it is a common mineral in Earth's subsurface, but weathers quickly on the surface. For this reason, olivine has been proposed as a good candidate for accelerated weathering to sequester carbon dioxide from the Earth's oceans and atmosphere, as part of climate change mitigation. Olivine also has many other historical uses, such as the gemstone peridot (or chrysolite), as well as industrial applications like metalworking processes."@en . . . . . . "3.2"^^ . "\u041E\u043B\u0456\u0432\u0456\u043D"@uk . . . "\u039C\u03B5 \u03C4\u03BF\u03BD \u03CC\u03C1\u03BF \u03BF\u03BB\u03B9\u03B2\u03AF\u03BD\u03B7\u03C2 (\u03B1\u03B3\u03B3\u03BB. olivine) \u03B5\u03BD\u03BD\u03BF\u03B5\u03AF\u03C4\u03B1\u03B9 \u03B9\u03C3\u03CC\u03BC\u03BF\u03C1\u03C6\u03B7 \u03C0\u03B1\u03C1\u03AC\u03BC\u03B9\u03BE\u03B7 \u03C0\u03BF\u03C5 \u03C0\u03C1\u03BF\u03BA\u03CD\u03C0\u03C4\u03B5\u03B9 \u03B1\u03C0\u03CC \u03C4\u03B1 \u03BF\u03C1\u03C5\u03BA\u03C4\u03AC \u03C6\u03BF\u03C1\u03C3\u03C4\u03B5\u03C1\u03AF\u03C4\u03B7 (Mg2SiO4) \u03BA\u03B1\u03B9 \u03A6\u03B1\u03CB\u03B1\u03BB\u03AF\u03C4\u03B7 (Fe+22SiO4) \u03BA\u03B1\u03B9, \u03B5\u03C0\u03B9\u03C3\u03AE\u03BC\u03C9\u03C2, \u03B4\u03B5\u03BD \u03B1\u03C0\u03BF\u03C4\u03B5\u03BB\u03B5\u03AF, \u03C9\u03C2 \u03C0\u03B1\u03C1\u03AC\u03BC\u03B9\u03BE\u03B7, \u03B1\u03C5\u03C4\u03BF\u03C4\u03B5\u03BB\u03AD\u03C2 \u03BF\u03C1\u03C5\u03BA\u03C4\u03CC. \u039F \u03BF\u03BB\u03B9\u03B2\u03AF\u03BD\u03B7\u03C2 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03B2\u03B9\u03BF\u03BC\u03B7\u03C7\u03B1\u03BD\u03B9\u03BA\u03CC \u03BF\u03C1\u03C5\u03BA\u03C4\u03CC \u03C0\u03BF\u03C5 \u03C7\u03C1\u03B7\u03C3\u03B9\u03BC\u03BF\u03C0\u03BF\u03B9\u03B5\u03AF\u03C4\u03B1\u03B9 \u03C3\u03B1\u03BD \u03C0\u03C5\u03C1\u03AF\u03BC\u03B1\u03C7\u03BF \u03C5\u03BB\u03B9\u03BA\u03CC. \u03A4\u03BF \u03CC\u03BD\u03BF\u03BC\u03AC \u03C4\u03BF\u03C5 \u03C0\u03C1\u03BF\u03AD\u03C1\u03C7\u03B5\u03C4\u03B1\u03B9 \u03B1\u03C0\u03CC \u03C4\u03BF \u03B5\u03BB\u03B1\u03B9\u03BF\u03C0\u03C1\u03AC\u03C3\u03B9\u03BD\u03BF (olive-green) \u03C7\u03C1\u03CE\u03BC\u03B1 \u03C4\u03BF\u03C5. \u0391\u03C0\u03BF\u03C4\u03B5\u03BB\u03B5\u03AF \u03BA\u03C5\u03C1\u03AF\u03B1\u03C1\u03C7\u03BF \u03C3\u03C5\u03C3\u03C4\u03B1\u03C4\u03B9\u03BA\u03CC \u03C4\u03C9\u03BD \u03B2\u03B1\u03C3\u03B9\u03BA\u03CE\u03BD (\u03B2\u03B1\u03C3\u03AC\u03BB\u03C4\u03B7\u03C2, \u03B3\u03AC\u03B2\u03B2\u03C1\u03BF\u03C2, ) \u03BA\u03B1\u03B9 \u03C4\u03C9\u03BD \u03C5\u03C0\u03B5\u03C1\u03B2\u03B1\u03C3\u03B9\u03BA\u03CE\u03BD \u03C0\u03C5\u03C1\u03B9\u03B3\u03B5\u03BD\u03CE\u03BD \u03C0\u03B5\u03C4\u03C1\u03C9\u03BC\u03AC\u03C4\u03C9\u03BD . \u03A3\u03C5\u03BD\u03B4\u03AD\u03B5\u03C4\u03B1\u03B9 \u03BC\u03B5 \u03BF\u03C1\u03C5\u03BA\u03C4\u03AC \u03C4\u03B7\u03C2 \u03BF\u03BC\u03AC\u03B4\u03B1\u03C2 \u03C4\u03BF\u03C5 , , \u03C4\u03AC\u03BB\u03BA\u03B7 \u03BA\u03B1\u03B9, \u03B9\u03B4\u03B9\u03B1\u03AF\u03C4\u03B5\u03C1\u03B1, \u03C3\u03B5\u03C1\u03C0\u03B5\u03BD\u03C4\u03AF\u03BD\u03B7, \u03C0\u03C1\u03BF\u03C2 \u03C4\u03BF\u03BD \u03BF\u03C0\u03BF\u03AF\u03BF \u03BA\u03B1\u03B9 \u03B5\u03BE\u03B1\u03BB\u03BB\u03BF\u03B9\u03CE\u03BD\u03B5\u03C4\u03B1\u03B9. \u0391\u03C0\u03B1\u03BD\u03C4\u03AC, \u03B5\u03C0\u03AF\u03C3\u03B7\u03C2, \u03BA\u03B1\u03B9 \u03C3\u03B5 \u03BC\u03B5\u03C4\u03B1\u03BC\u03BF\u03C1\u03C6\u03C9\u03BC\u03AD\u03BD\u03B1 \u03C0\u03B5\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1, \u03BA\u03C5\u03C1\u03AF\u03C9\u03C2 \u03C0\u03C1\u03AC\u03C3\u03B9\u03BD\u03BF \u03BC\u03AC\u03C1\u03BC\u03B1\u03C1\u03BF (\u03BF\u03BB\u03B9\u03B2\u03B9\u03BD\u03B9\u03BA\u03AC \u03BC\u03AC\u03C1\u03BC\u03B1\u03C1\u03B1). \u0394\u03B5\u03BD \u03B5\u03AF\u03BD\u03B1\u03B9 \u03B4\u03C5\u03BD\u03B1\u03C4\u03CC \u03BD\u03B1 \u03C3\u03C5\u03BD\u03C5\u03C0\u03AC\u03C1\u03BE\u03B5\u03B9 \u03BC\u03B5 \u03C0\u03B5\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1 \u03C0\u03BF\u03C5 \u03C0\u03B5\u03C1\u03B9\u03AD\u03C7\u03BF\u03C5\u03BD \u03C7\u03B1\u03BB\u03B1\u03B6\u03AF\u03B1 (\u03B4\u03B9\u03BF\u03BE\u03B5\u03AF\u03B4\u03B9\u03BF \u03C4\u03BF\u03C5 \u03C0\u03C5\u03C1\u03B9\u03C4\u03AF\u03BF\u03C5, SiO2), \u03B5\u03C0\u03B5\u03B9\u03B4\u03AE \u03B8\u03B1 \u03B1\u03BD\u03C4\u03B9\u03B4\u03C1\u03BF\u03CD\u03C3\u03B5 \u03BC\u03B5 \u03B1\u03C5\u03C4\u03CC \u03C0\u03C1\u03BF\u03C2 (MgSiO3):"@el . . "El olivino es un grupo de minerales constituyentes de rocas, aunque el nombre se suele aplicar con especial referencia a la principal soluci\u00F3n s\u00F3lida del grupo, que es entre forsterita (Mg2SiO4) y fayalita (Fe2SiO4).\u200B\u200B Los olivinos son de los minerales m\u00E1s importantes en la clasificaci\u00F3n de rocas \u00EDgneas.\u200B El olivino rico en magnesio destaca por ser el componente principal del manto superior de la Tierra.\u200B"@es . "Olivin"@sv . . "\u039C\u03B5 \u03C4\u03BF\u03BD \u03CC\u03C1\u03BF \u03BF\u03BB\u03B9\u03B2\u03AF\u03BD\u03B7\u03C2 (\u03B1\u03B3\u03B3\u03BB. olivine) \u03B5\u03BD\u03BD\u03BF\u03B5\u03AF\u03C4\u03B1\u03B9 \u03B9\u03C3\u03CC\u03BC\u03BF\u03C1\u03C6\u03B7 \u03C0\u03B1\u03C1\u03AC\u03BC\u03B9\u03BE\u03B7 \u03C0\u03BF\u03C5 \u03C0\u03C1\u03BF\u03BA\u03CD\u03C0\u03C4\u03B5\u03B9 \u03B1\u03C0\u03CC \u03C4\u03B1 \u03BF\u03C1\u03C5\u03BA\u03C4\u03AC \u03C6\u03BF\u03C1\u03C3\u03C4\u03B5\u03C1\u03AF\u03C4\u03B7 (Mg2SiO4) \u03BA\u03B1\u03B9 \u03A6\u03B1\u03CB\u03B1\u03BB\u03AF\u03C4\u03B7 (Fe+22SiO4) \u03BA\u03B1\u03B9, \u03B5\u03C0\u03B9\u03C3\u03AE\u03BC\u03C9\u03C2, \u03B4\u03B5\u03BD \u03B1\u03C0\u03BF\u03C4\u03B5\u03BB\u03B5\u03AF, \u03C9\u03C2 \u03C0\u03B1\u03C1\u03AC\u03BC\u03B9\u03BE\u03B7, \u03B1\u03C5\u03C4\u03BF\u03C4\u03B5\u03BB\u03AD\u03C2 \u03BF\u03C1\u03C5\u03BA\u03C4\u03CC. \u039F \u03BF\u03BB\u03B9\u03B2\u03AF\u03BD\u03B7\u03C2 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03B2\u03B9\u03BF\u03BC\u03B7\u03C7\u03B1\u03BD\u03B9\u03BA\u03CC \u03BF\u03C1\u03C5\u03BA\u03C4\u03CC \u03C0\u03BF\u03C5 \u03C7\u03C1\u03B7\u03C3\u03B9\u03BC\u03BF\u03C0\u03BF\u03B9\u03B5\u03AF\u03C4\u03B1\u03B9 \u03C3\u03B1\u03BD \u03C0\u03C5\u03C1\u03AF\u03BC\u03B1\u03C7\u03BF \u03C5\u03BB\u03B9\u03BA\u03CC. \u03A4\u03BF \u03CC\u03BD\u03BF\u03BC\u03AC \u03C4\u03BF\u03C5 \u03C0\u03C1\u03BF\u03AD\u03C1\u03C7\u03B5\u03C4\u03B1\u03B9 \u03B1\u03C0\u03CC \u03C4\u03BF \u03B5\u03BB\u03B1\u03B9\u03BF\u03C0\u03C1\u03AC\u03C3\u03B9\u03BD\u03BF (olive-green) \u03C7\u03C1\u03CE\u03BC\u03B1 \u03C4\u03BF\u03C5. \u0391\u03C0\u03BF\u03C4\u03B5\u03BB\u03B5\u03AF \u03BA\u03C5\u03C1\u03AF\u03B1\u03C1\u03C7\u03BF \u03C3\u03C5\u03C3\u03C4\u03B1\u03C4\u03B9\u03BA\u03CC \u03C4\u03C9\u03BD \u03B2\u03B1\u03C3\u03B9\u03BA\u03CE\u03BD (\u03B2\u03B1\u03C3\u03AC\u03BB\u03C4\u03B7\u03C2, \u03B3\u03AC\u03B2\u03B2\u03C1\u03BF\u03C2, ) \u03BA\u03B1\u03B9 \u03C4\u03C9\u03BD \u03C5\u03C0\u03B5\u03C1\u03B2\u03B1\u03C3\u03B9\u03BA\u03CE\u03BD \u03C0\u03C5\u03C1\u03B9\u03B3\u03B5\u03BD\u03CE\u03BD \u03C0\u03B5\u03C4\u03C1\u03C9\u03BC\u03AC\u03C4\u03C9\u03BD . \u03A3\u03C5\u03BD\u03B4\u03AD\u03B5\u03C4\u03B1\u03B9 \u03BC\u03B5 \u03BF\u03C1\u03C5\u03BA\u03C4\u03AC \u03C4\u03B7\u03C2 \u03BF\u03BC\u03AC\u03B4\u03B1\u03C2 \u03C4\u03BF\u03C5 , , \u03C4\u03AC\u03BB\u03BA\u03B7 \u03BA\u03B1\u03B9, \u03B9\u03B4\u03B9\u03B1\u03AF\u03C4\u03B5\u03C1\u03B1, \u03C3\u03B5\u03C1\u03C0\u03B5\u03BD\u03C4\u03AF\u03BD\u03B7, \u03C0\u03C1\u03BF\u03C2 \u03C4\u03BF\u03BD \u03BF\u03C0\u03BF\u03AF\u03BF \u03BA\u03B1\u03B9 \u03B5\u03BE\u03B1\u03BB\u03BB\u03BF\u03B9\u03CE\u03BD\u03B5\u03C4\u03B1\u03B9. \u0391\u03C0\u03B1\u03BD\u03C4\u03AC, \u03B5\u03C0\u03AF\u03C3\u03B7\u03C2, \u03BA\u03B1\u03B9 \u03C3\u03B5 \u03BC\u03B5\u03C4\u03B1\u03BC\u03BF\u03C1\u03C6\u03C9\u03BC\u03AD\u03BD\u03B1 \u03C0\u03B5\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1, \u03BA\u03C5\u03C1\u03AF\u03C9\u03C2 \u03C0\u03C1\u03AC\u03C3\u03B9\u03BD\u03BF \u03BC\u03AC\u03C1\u03BC\u03B1\u03C1\u03BF (\u03BF\u03BB\u03B9\u03B2\u03B9\u03BD\u03B9\u03BA\u03AC \u03BC\u03AC\u03C1\u03BC\u03B1\u03C1\u03B1). \u0394\u03B5\u03BD \u03B5\u03AF\u03BD\u03B1\u03B9 \u03B4\u03C5\u03BD\u03B1\u03C4\u03CC \u03BD\u03B1 \u03C3\u03C5\u03BD\u03C5\u03C0\u03AC\u03C1\u03BE\u03B5\u03B9 \u03BC\u03B5 \u03C0\u03B5\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1 \u03C0\u03BF\u03C5 \u03C0\u03B5\u03C1\u03B9\u03AD\u03C7\u03BF\u03C5\u03BD \u03C7\u03B1\u03BB\u03B1\u03B6\u03AF\u03B1 (\u03B4\u03B9\u03BF\u03BE\u03B5\u03AF\u03B4\u03B9\u03BF \u03C4\u03BF\u03C5 \u03C0\u03C5\u03C1\u03B9\u03C4\u03AF\u03BF\u03C5, SiO2), \u03B5\u03C0\u03B5\u03B9\u03B4\u03AE \u03B8\u03B1 \u03B1\u03BD\u03C4\u03B9\u03B4\u03C1\u03BF\u03CD\u03C3\u03B5 \u03BC\u03B5 \u03B1\u03C5\u03C4\u03CC \u03C0\u03C1\u03BF\u03C2 (MgSiO3): Mg2SiO4 + SiO2 \u2192 2MgSiO3 \u039B\u03CC\u03B3\u03C9 \u03C4\u03B7\u03C2 \u03C5\u03C8\u03B7\u03BB\u03AE\u03C2 \u03C4\u03BF\u03C5 \u03B1\u03BD\u03B8\u03B5\u03BA\u03C4\u03B9\u03BA\u03CC\u03C4\u03B7\u03C4\u03B1\u03C2 \u03C3\u03C4\u03B7\u03BD \u03B8\u03B5\u03C1\u03BC\u03CC\u03C4\u03B7\u03C4\u03B1 \u03C7\u03C1\u03B7\u03C3\u03B9\u03BC\u03BF\u03C0\u03BF\u03B9\u03B5\u03AF\u03C4\u03B1\u03B9 \u03C3\u03C4\u03B7\u03BD \u03BA\u03B1\u03C4\u03B1\u03C3\u03BA\u03B5\u03C5\u03AE \u03B2\u03B1\u03C3\u03B9\u03BA\u03CE\u03BD \u03C0\u03C5\u03C1\u03AF\u03BC\u03B1\u03C7\u03C9\u03BD \u03C5\u03BB\u03B9\u03BA\u03CE\u03BD \u03BC\u03AD\u03C4\u03C1\u03B9\u03B1\u03C2 \u03C0\u03C1\u03BF\u03C2 \u03C5\u03C8\u03B7\u03BB\u03AE\u03C2 \u03B1\u03BD\u03C4\u03BF\u03C7\u03AE\u03C2, \u03C0\u03B1\u03C1\u03CC\u03BB\u03BF \u03C0\u03BF\u03C5 \u03B4\u03B5\u03BD \u03AD\u03C7\u03B5\u03B9 \u03C4\u03B7\u03BD \u03C0\u03C5\u03C1\u03B9\u03BC\u03B1\u03C7\u03B9\u03BA\u03CC\u03C4\u03B7\u03C4\u03B1 \u03C4\u03B7\u03C2 \u03BC\u03B1\u03B3\u03BD\u03B7\u03C3\u03AF\u03B1\u03C2. \u0395\u03AF\u03BD\u03B1\u03B9 \u03B5\u03C5\u03C1\u03CD\u03C4\u03B1\u03C4\u03B1 \u03B4\u03B9\u03B1\u03B4\u03B5\u03B4\u03BF\u03BC\u03AD\u03BD\u03BF\u03C2, \u03BA\u03B1\u03B8\u03CE\u03C2 \u03B1\u03C0\u03BF\u03C4\u03B5\u03BB\u03B5\u03AF \u03C3\u03C5\u03C3\u03C4\u03B1\u03C4\u03B9\u03BA\u03CC \u03C3\u03C5\u03C7\u03BD\u03AC \u03B5\u03BC\u03C6\u03B1\u03BD\u03B9\u03B6\u03CC\u03BC\u03B5\u03BD\u03C9\u03BD \u03C0\u03B5\u03C4\u03C1\u03C9\u03BC\u03AC\u03C4\u03C9\u03BD. \u0388\u03C7\u03B5\u03B9 \u03B1\u03BD\u03B9\u03C7\u03BD\u03B5\u03C5\u03B8\u03B5\u03AF \u03B4\u03B5 \u03BA\u03B1\u03B9 \u03C3\u03C4\u03B7 \u03A3\u03B5\u03BB\u03AE\u03BD\u03B7, \u03C3\u03C4\u03BF\u03BD \u0386\u03C1\u03B7 \u03BA\u03B1\u03B9 \u03B3\u03B5\u03BD\u03B9\u03BA\u03AC \u03C3\u03B5 \u03C0\u03BB\u03B1\u03BD\u03AE\u03C4\u03B5\u03C2 \u03BA\u03B1\u03B9 \u03BC\u03B5\u03C4\u03B5\u03C9\u03C1\u03AF\u03C4\u03B5\u03C2. \u0391\u03BD\u03B1\u03C6\u03AD\u03C1\u03B5\u03C4\u03B1\u03B9 \u03B4\u03B5 \u03C9\u03C2 \u03AD\u03BD\u03B1 \u03C3\u03B7\u03BC\u03B1\u03BD\u03C4\u03B9\u03BA\u03CC \u03C3\u03C5\u03C3\u03C4\u03B1\u03C4\u03B9\u03BA\u03CC \u03C0\u03BB\u03B1\u03BD\u03B7\u03C4\u03CE\u03BD \u03C4\u03CD\u03C0\u03BF\u03C5 \u03B3\u03B7\u03C2. \u03A3\u03C5\u03BD\u03CE\u03BD\u03C5\u03BC\u03CC \u03C4\u03BF\u03C5 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C4\u03BF \u03BF\u03C1\u03C5\u03BA\u03C4\u03CC \u03C7\u03C1\u03C5\u03C3\u03BF\u03C0\u03AC\u03BB\u03B9\u03BF\u03C2 (chrysopal). \u039C\u03B9\u03B1 \u03B4\u03B9\u03B1\u03C6\u03B1\u03BD\u03AE\u03C2 \u03C0\u03C1\u03AC\u03C3\u03B9\u03BD\u03B7 \u03C0\u03BF\u03B9\u03BA\u03B9\u03BB\u03AF\u03B1 \u03C4\u03BF\u03C5 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C4\u03BF \u03C0\u03B5\u03C1\u03AF\u03B4\u03BF\u03C4\u03BF (\u03B1\u03B3\u03B3\u03BB. peridote), \u03C4\u03BF \u03BF\u03C0\u03BF\u03AF\u03BF \u03C7\u03C1\u03B7\u03C3\u03B9\u03BC\u03BF\u03C0\u03BF\u03B9\u03B5\u03AF\u03C4\u03B1\u03B9 \u03C9\u03C2 \u03B7\u03BC\u03B9\u03C0\u03BF\u03BB\u03CD\u03C4\u03B9\u03BC\u03BF\u03C2 \u03BB\u03AF\u03B8\u03BF\u03C2. \u0397 \u03BA\u03B1\u03BB\u03AE \u03C0\u03BF\u03B9\u03CC\u03C4\u03B7\u03C4\u03B1 \u03C0\u03B5\u03C1\u03B9\u03B4\u03CC\u03C4\u03BF\u03C5 \u03C0\u03B5\u03C1\u03B9\u03AD\u03C7\u03B5\u03B9 \u03BB\u03B9\u03B3\u03CC\u03C4\u03B5\u03C1\u03BF \u03B1\u03C0\u03CC 15% \u03C3\u03AF\u03B4\u03B7\u03C1\u03BF, \u03B5\u03BD\u03CE \u03BC\u03C0\u03BF\u03C1\u03B5\u03AF \u03BD\u03B1 \u03C0\u03B5\u03C1\u03B9\u03AD\u03C7\u03B5\u03B9 \u03BA\u03B1\u03B9 \u03AF\u03C7\u03BD\u03B7 \u03C7\u03C1\u03C9\u03BC\u03AF\u03BF\u03C5 \u03AE \u03BD\u03B9\u03BA\u03B5\u03BB\u03AF\u03BF\u03C5, \u03C0\u03BF\u03C5 \u03C3\u03C5\u03BC\u03B2\u03AC\u03BB\u03BB\u03BF\u03C5\u03BD \u03C3\u03C4\u03BF\u03BD \u03C7\u03C1\u03C9\u03BC\u03B1\u03C4\u03B9\u03C3\u03BC\u03CC \u03C4\u03BF\u03C5. \u03A4\u03BF \u03C0\u03B5\u03C1\u03AF\u03B4\u03BF\u03C4\u03BF \u03B2\u03C1\u03AD\u03B8\u03B7\u03BA\u03B5 \u03B3\u03B9\u03B1 \u03C0\u03C1\u03CE\u03C4\u03B7 \u03C6\u03BF\u03C1\u03AC \u03C3\u03C4\u03BF \u03BD\u03B7\u03C3\u03AF \u0396\u03B1\u03BC\u03C0\u03B1\u03C1\u03B3\u03BA\u03AC\u03BD\u03C4 (Zabargad) \u03C4\u03B7\u03C2 \u0395\u03C1\u03C5\u03B8\u03C1\u03AC\u03C2 \u03B8\u03AC\u03BB\u03B1\u03C3\u03C3\u03B1\u03C2, \u03BA\u03BF\u03BD\u03C4\u03AC \u03C3\u03C4\u03B7\u03BD \u0391\u03AF\u03B3\u03C5\u03C0\u03C4\u03BF. \u0388\u03C7\u03B5\u03B9, \u03B5\u03C0\u03AF\u03C3\u03B7\u03C2, \u03B1\u03BD\u03B5\u03C5\u03C1\u03B5\u03B8\u03B5\u03AF \u03C3\u03C4\u03BF\u03C5\u03C2 \u03C3\u03B9\u03B4\u03B7\u03C1\u03BF\u03BD\u03B9\u03BA\u03B5\u03BB\u03B9\u03BF\u03CD\u03C7\u03BF\u03C5\u03C2 \u03BC\u03B5\u03C4\u03B5\u03C9\u03C1\u03AF\u03C4\u03B5\u03C2 (\u03C0\u03B1\u03BB\u03BB\u03B1\u03C3\u03AF\u03C4\u03B5\u03C2, pallasites)."@el . . . . "\u039F\u03BB\u03B9\u03B2\u03AF\u03BD\u03B7\u03C2"@el . . . "Oliv\u00EDn (peridot) (Werner, 1789), chemick\u00FD vzorec (Mg,Fe)2[SiO4] je koso\u010Dtvere\u010Dn\u00FD miner\u00E1l s prom\u011Bnliv\u00FDm pod\u00EDlem ho\u0159\u010D\u00EDku a \u017Eeleza v z\u00E1vislosti na podm\u00EDnk\u00E1ch p\u0159i jeho vzniku. Pr\u00E1v\u011B \u017Eelezo zp\u016Fsobuje zelen\u00E9 zabarven\u00ED kamene. Perfekcionist\u00E9 tvrd\u00ED, \u017Ee dokonal\u00FD oliv\u00EDn by m\u011Bl obsahovat m\u00E9n\u011B ne\u017E 15 % \u017Eeleza a \u017Ee nesm\u00ED v jeho m\u0159\u00ED\u017Ece chyb\u011Bt stopov\u00E9 prvky niklu a chromu. Krajn\u00ED \u010Dleny izomorfn\u00ED \u0159ady jsou forsterit \u2013 Mg2[SiO4] a \u2013 Fe2[SiO4]. Nazv\u00E1n byl podle olivov\u011B zelen\u00E9ho zbarven\u00ED, kter\u00E9 spojovalo slova oliva a zelen\u00FD (v angli\u010Dtin\u011B slovo green), ale jeho n\u00E1zev byl n\u011Bkolikr\u00E1t zam\u011B\u0148ov\u00E1n. Sta\u0159\u00ED \u0158\u00EDman\u00E9 pou\u017E\u00EDvali n\u00E1zev Topazos dle ostrova, kde byl t\u011B\u017Een a francouz\u0161t\u00ED klenotn\u00EDci pozd\u011Bji pak pou\u017E\u00EDvali n\u00E1zev peridot. Ozna\u010Den\u00ED peridot se odvozuje z arabsk\u00E9ho slova faridat, kter\u00E9 znamen\u00E1 diamant. Oliv\u00EDnu se p\u0159ezd\u00EDv\u00E1 \"smaragd k\u0159i\u017E\u00E1k\u016F\"."@cs . . . . . . "\u041E\u043B\u0438\u0432\u0438\u043D"@ru . . . . . "\uAC10\uB78C\uC11D(\uC601\uC5B4: olivine)\uC740 \uB9C8\uADF8\uB124\uC298-\uCCA0\uC9C8\uC758 \uADDC\uC0B0\uC5FC \uAD11\uBB3C\uB85C \uD654\uD559\uC2DD\uC740 (Mg2+,Fe2+)2SiO4\uC774\uBA70, \uB9C8\uADF8\uB124\uC298\uACFC \uCCA0\uC758 \uBE44\uAC00 \uB450 \uB0B4\uC131\uBD84\uC778 (\uB9C8\uADF8\uB124\uC298 \uB0B4\uC131\uBD84)\uC640 (\uCCA0 \uB0B4\uC131\uBD84) \uC0AC\uC774\uC5D0\uC11C \uBCC0\uD654\uD558\uB294 \uACE0\uC6A9\uCCB4\uC774\uB2E4. \uD06C\uB9AC\uC194\uB77C\uC774\uD2B8(chrysolite)\uB77C\uACE0 \uBD88\uB9AC\uAE30\uB3C4 \uD558\uBA70 \uBCF4\uC11D \uC218\uC900\uC758 \uD488\uC9C8\uC744 \uAC00\uC9C8 \uB54C\uB294 \uD398\uB9AC\uB3C4\uD2B8\uB77C\uACE0 \uD55C\uB2E4. \uC774\uB294 8\uC6D4\uC758 \uD0C4\uC0DD\uC11D\uC774\uAE30\uB3C4 \uD558\uB2E4. \uC9C0\uAD6C \uC0C1\uC5D0\uC11C \uAC00\uC7A5 \uD754\uD55C \uAD11\uBB3C \uC911\uC758 \uD558\uB098\uC774\uBA70 \uB2EC, \uD654\uC131, , \uAE30\uD0C0 \uB9CE\uC740 \uC6B4\uC11D \uB4F1\uC5D0\uC11C\uB3C4 \uADF8 \uC874\uC7AC\uAC00 \uD655\uC778\uB418\uC5C8\uB2E4. \uAC10\uB78C\uC11D\uC758 \uC131\uBD84\uC740 \uBCF4\uD1B5 \uCCA0\uACFC \uB9C8\uADF8\uB124\uC298\uC758 \uBAB0\uC218\uBE44\uB85C \uB098\uD0C0\uB0B8\uB2E4. \uD3EC\uC2A4\uD130\uB77C\uC774\uD2B8\uB294 1900 \u00B0C\uC5D0 \uC774\uB974\uB294 \uC720\uB2EC\uB9AC \uB192\uC740 \uB179\uB294\uC810\uC744 \uAC00\uC9C0\uACE0 \uC788\uC73C\uB098 \uD30C\uC584\uB77C\uC774\uD2B8\uC758 \uB179\uB294\uC810\uC740 1200 \u00B0C \uC815\uB3C4\uC774\uB2E4."@ko . . . . . . . . . . . . . "Olaiv\u00EDn"@ga . . .