. . . "Rgd"@en . "Ringwoodit ist die Hochdruck-Modifikation von Olivin und ein an der Erdoberfl\u00E4che selten vorkommendes Mineral aus der Mineralklasse der \u201ESilikate und Germanate\u201C. Es kristallisiert im kubischen Kristallsystem mit der idealisierten chemischen Zusammensetzung Mg2(SiO4), ist also ein Magnesium-Silikat. Strukturell geh\u00F6rt Ringwoodit zu den Inselsilikaten sowie zur Supergruppe der Spinelle mit der f\u00FCr Spinelle normierten Formelschreibweise SiMg2O4."@de . "La ringwoodita es un mineral de la clase de los nesosilicatos, y dentro de esta pertenece al llamado \u201Cgrupo del olivino\u201D. Descubierta en 1969 en el meteorito que aparece en la imagen derecha \u2014ca\u00EDdo cerca de Charters Towers, en Queensland (Australia),\u200B\u2014, se la nombr\u00F3 as\u00ED luego de los estudios de Ted Ringwoodd (1930-1993) sobre las transiciones polim\u00F3rficas en minerales mant\u00E9licos como olivino y piroxeno a presiones equivalentes a profundidades cercanas a 600 km. Un sin\u00F3nimo es su clave: IMA1968-036."@es . "Ringwoodita silikato motako minerala da eta ulv\u00F6spinel subtaldearen kidea da."@eu . . "La ringwoodite est un polymorphe de l'orthosilicate de magn\u00E9sium et de fer (Mg,Fe)2SiO4, stable \u00E0 hautes pression et temp\u00E9rature. D'abord obtenue au laboratoire par le p\u00E9trologue et g\u00E9ochimiste australien Ted Ringwood, elle a ensuite \u00E9t\u00E9 observ\u00E9e dans des m\u00E9t\u00E9orites, puis dans de rares \u00E9chantillons terrestres. Les donn\u00E9es acquises en p\u00E9trologie exp\u00E9rimentale et en sismologie indiquent que la ringwoodite est un composant majeur du manteau sup\u00E9rieur terrestre."@fr . . . . "Ringwoodyt"@pl . "none"@en . "Ringwoodit adalah salah satu jenis mineral olivin yang terbentuk oleh tekanan dan suhu yang tinggi di mantel Bumi, di kedalaman sekitar 525 hingga 660 kilometer. Olivin merupakan mineral magnesium besi silikat. Mineral ini pertamakali diidentifikasi di sebuah meteorit pada 1969. Ada kemungkinan bahwa ada Ringwoodit dalam kuantitas sangat besar di dalam mantel Bumi. Ringwoodit memiliki ion hidroksida dalam struktur mineralnya. Ini meyakinkan para ilmuwan bahwa mineral ini terbentuk di sekitar zona peralihan antara kerak Bumi dan mantel, sekitar 410 hingga 660 km dalamnya."@in . . . . "A ringwoodita ou ringwoodite \u00E9 um mineral da classe dos nesossilicatos, e dentro desta pertence ao chamado \u201Cgrupo da olivina\". Descoberto em 1969 num meteorito ca\u00EDdo pr\u00F3ximo de , em Queensland, Austr\u00E1lia, foi assim nomeado em honra a Alfred E. Ringwood, geoqu\u00EDmico australiano."@pt . . "Ringwoodite"@it . "Microcrystalline aggregates"@en . . "Ringwoodite"@en . . "Ringwoodit"@in . . "Semitransparent"@en . . . . . . . "Ringwoodita"@pt . . "\u5C16\u6676\u6A44\u6B16\u77F3\uFF0C\u4EA6\u4F5C\u03B3\u76F8\u6A44\u6B16\u77F3\u6216\u5F9E\u82F1\u8A9E\u97F3\u8B6F\u4F5C\u6797\u4F0D\u5FB7\u77F3\uFF0C\u662F\u4E00\u7A2E\u65BC\u9AD8\u6EAB\u9AD8\u58D3\u74B0\u5883\u4E0B\uFF08\u7D04\u4ECB\u65BC525\u516C\u91CC\u81F3660\u516C\u91CC\u9593\u7684\u5730\u51FD\uFF09\u7522\u751F\u7684\u7926\u7269\uFF0C\u70BA\u6A44\u6B16\u77F3\uFF08\u4E00\u7A2E\u9435\u9382\u77FD\u9178\u9E7D\u7926\u7269\uFF09\u7684\u9AD4\u3002 \u5C16\u6676\u6A44\u6B16\u77F3\u80FD\u5C07\u6C34\u5408\u7269\u5305\u542B\u65BC\u5176\u7D50\u69CB\u4E2D\uFF0C\u7D50\u5408\u5176\u65BC\u5730\u7403\u5167\u90E8\u5730\u51FD\u51FA\u73FE\u7684\u8B49\u64DA\uFF0C\u8AAA\u660E\u5F88\u6709\u53EF\u80FD\u5728410\u81F3660\u516C\u91CC\u6DF1\u8655\u7684\u5730\u5E541%\u662F\u6C34\uFF0C\u5C31\u76F8\u5F53\u4E8E\u5730\u7403\u4E0A\u6240\u6709\u6D77\u6D0B\u6C34\u91CF\u603B\u548C\u76843\u500D\u3002 \u6B64\u7926\u7269\u9996\u6B21\u57281969\u5E74\u65BCTemham\u9695\u77F3\u4E2D\u88AB\u767C\u73FE\uFF0C\u4E14\u88AB\u8A8D\u70BA\u5F88\u6709\u53EF\u80FD\u5927\u91CF\u5730\u5B58\u5728\u65BC\u5730\u7403\u7684\u5730\u51FD\u4E2D\u3002\u4ECE\u5DF4\u897F\u8339\u4F0A\u7EB3\u5730\u533A\u5730\u9762\u4E0A\u7684\u5CA9\u6D46\u4E2D\u53D1\u73B0\u7684\u94BB\u77F3\u4E2D\u5B58\u572840\u5FAE\u7C73\u957F\u7684\u6676\u4F53\u5185\u542B\u7269\u3002\u5149\u8C31\u5206\u6790\u8868\u660E\u8FD9\u5C31\u662F\u5C16\u6676\u6A44\u6984\u77F3\uFF1B\u5728\u7EBF\u53D1\u8868\u4E8E\u300A\u81EA\u7136\u300B\u4E0A\u7684\u8FDB\u4E00\u6B65\u5206\u6790\u663E\u793A\uFF0C\u5C16\u6676\u6A44\u6984\u77F3\u542B\u6709\u6C22\u6C27\u952E\uFF0C\u8868\u660E\u6676\u683C\u4E2D\u81F3\u5C11\u542B\u67091.4%\u7684\u6C34\u3002 \u5C16\u6676\u6A44\u6B16\u77F3\u53C8\u540D\u6797\u4F0D\u5FB7\u77F3\uFF08Ringwoodite\uFF09\uFF0C\u4EE5\u8457\u540D\u7684\u6FB3\u6D32\u5730\u7403\u5167\u90E8\u5B78\u5BB6\uFF081930\uFF0D1993\uFF09\u547D\u540D\uFF0C\u4ED6\u4E3B\u8981\u7814\u7A76\u5730\u51FD\u7926\u7269\uFF08\u5982\u8F1D\u77F3\u8207\u6A44\u6B16\u77F3\uFF09\u65BC\u5730\u7403\u5167\u90E8\u8D85\u904E600\u516C\u91CC\u6DF1\u8655\u7684\u540C\u8CEA\u7570\u76F8\u9AD4\u7279\u6027\u3002 \u5728\u5730\u9762\u4EE5\u4E0B410km\u6DF1\u5904\uFF0814GPa\uFF09\u7684\u5730\u5E54\u8FC7\u6E21\u5E26\u4E0A\u754C\uFF0C\u6A44\u6B16\u77F3\uFF08\u03B1\u76F8\uFF09\u7684\u6676\u4F53\u7C92\u5EA6\u968F\u7740\u538B\u529B\u5347\u9AD8\u8F6C\u53D8\u4E3A\u66F4\u9AD8\u5BC6\u5EA6\u548C\u6CE2\u901F\u7684\uFF08\u4F3C\u5C16\u6676\u6A44\u6B16\u77F3\uFF09\uFF08\u03B2\u76F8\uFF09\uFF0C\u4F53\u79EF\u51CF\u5C118%\u3002\u5728\u8FC7\u6E21\u5E26520km\u6DF1\u5904\uFF0C\u74E6\u5179\u5229\u77F3\u53D8\u6210\u5C16\u6676\u6A44\u6984\u77F3\uFF08\u03B3\u76F8\uFF09\u4E0E\u77F3\u69B4\u77F3\uFF0C\u4F53\u79EF\u51CF\u5C1129%\u3002\u800C\u5728\u8D85\u904E660\u516C\u91CC\u6DF1\u8655\uFF0823.5GPa\uFF09\u7684\u5730\u51FD\uFF0C\u9AD8\u538B\u76F8\u7684\u5C16\u6676\u6A44\u6984\u77F3\u968F\u7740\u538B\u529B\u5347\u9AD8\u53D1\u751F\u4E86\u4E24\u79CD\u5BC6\u5EA6\u66F4\u5927\u7684\u540E\u5C16\u6676\u77F3\u76F8\u53D8\uFF1A\u5E03\u91CC\u5947\u66FC\u77F3\u4E0E\u3002"@zh . . . . . . . . "Ringwoodite"@en . "Ringwoodit \u00E4r en h\u00F6gtrycksfas av Mg2SiO4 som bildas vid h\u00F6ga temperaturer och tryck i jordens mantel p\u00E5 mellan 525 och 660 km djup. Det \u00E4r polymorft av olivinfasen , ett magnesiumj\u00E4rnsilikat. Ringwoodit kan inneh\u00E5lla hydroxidjoner i sin struktur. Ringwoodit har p\u00E5visats djupt ner i jordmanteln och ber\u00E4kningar tyder p\u00E5 att det kan finnas motsvarande en till tre g\u00E5nger v\u00E4rldshavens volym av vatten i mantelns \u00F6verg\u00E5ngszon vid 410 till 660 km djup. Ringwoodit identifierades f\u00F6rsta g\u00E5ngen i Tenhammeteoriten 1969, d\u00E5 man ocks\u00E5 drog slutsatsen att mineralet kan f\u00F6rekomma i stor m\u00E4ngd i jordens mantel. Mineralet namngavs efter den australiensiska geologen (1930-1993), som studerat polymorfa fas\u00F6verg\u00E5ngar i mantelmineralen olivin och pyroxen vid tryck motsvarande djup s\u00E5 stora som ca 600 km."@sv . . . "9"^^ . "Fdm"@en . . . "Ringwoodita"@es . . . . . "Ringwoodit ist die Hochdruck-Modifikation von Olivin und ein an der Erdoberfl\u00E4che selten vorkommendes Mineral aus der Mineralklasse der \u201ESilikate und Germanate\u201C. Es kristallisiert im kubischen Kristallsystem mit der idealisierten chemischen Zusammensetzung Mg2(SiO4), ist also ein Magnesium-Silikat. Strukturell geh\u00F6rt Ringwoodit zu den Inselsilikaten sowie zur Supergruppe der Spinelle mit der f\u00FCr Spinelle normierten Formelschreibweise SiMg2O4. Aufgrund von Mischkristallbildung zwischen den Mineralen der Olivingruppe wird die Formel f\u00FCr den Ringwoodit oft auch als Mischformel mit (Mg,Fe)2[SiO4] angegeben. In der Natur \u00FCberwiegen Mg-reiche Mischkristalle; \u03B3-Fe2(SiO4) wurde erst k\u00FCrzlich in nat\u00FCrlichen Proben nachgewiesen und wird daher seit 2013 als Ahrensit bezeichnet. Ringwoodit ist durchscheinend und konnte bisher nur in Form von abgerundeten K\u00F6rnern bis etwa 100 Mikrometer Gr\u00F6\u00DFe und massigen Mineral-Aggregaten gefunden werden. In reiner Form ist Ringwoodit farblos. Durch Fremdbeimengungen kann er aber auch eine violette, bl\u00E4uliche oder rauchgraue Farbe annehmen."@de . . . . "H-M symbol:"@en . "Ringwoodita silikato motako minerala da eta ulv\u00F6spinel subtaldearen kidea da."@eu . . . "\u5C16\u6676\u6A44\u6984\u77F3"@zh . . "Hexoctahedral"@en . . . . . . . . "\u0420\u0438\u043D\u0433\u0432\u0443\u0434\u0438\u0442"@ru . . . "Ringwoodit"@de . . . . . . . . . "Ringwoodite is a high-pressure phase of Mg2SiO4 (magnesium silicate) formed at high temperatures and pressures of the Earth's mantle between 525 and 660 km (326 and 410 mi) depth. It may also contain iron and hydrogen. It is polymorphous with the olivine phase forsterite (a magnesium iron silicate). Ringwoodite is notable for being able to contain hydroxide ions (oxygen and hydrogen atoms bound together) within its structure. In this case two hydroxide ions usually take the place of a magnesium ion and two oxide ions. Combined with evidence of its occurrence deep in the Earth's mantle, this suggests that there is from one to three times the world ocean's equivalent of water in the mantle transition zone from 410 to 660 km deep. This mineral was first identified in the Tenham meteorite in 1969, and is inferred to be present in large quantities in the Earth's mantle. Ringwoodite was named after the Australian earth scientist Ted Ringwood (1930\u20131993), who studied polymorphic phase transitions in the common mantle minerals olivine and pyroxene at pressures equivalent to depths as great as about 600 km. Olivine, wadsleyite, and ringwoodite are polymorphs found in the upper mantle of the earth. At depths greater than about 660 kilometres (410 mi), other minerals, including some with the perovskite structure, are stable. The properties of these minerals determine many of the properties of the mantle."@en . . . . "La ringwoodita \u00E9s un mineral de la classe dels silicats del grup de l'olivina. Va ser descoberta l'any 1967 a partir del meteorit Tenham, que va impactar a , Queensland, Austr\u00E0lia i va rebre el seu nom en honor del geoqu\u00EDmic australi\u00E0 (1930-1993), el qual va estudiar les transicions de fase polim\u00F2rfiques dels minerals d'olivina i piroxens comuns en el mantell terrestre a pressions equivalent a profunditats d'uns 600 km."@ca . "Ringwoodite is a high-pressure phase of Mg2SiO4 (magnesium silicate) formed at high temperatures and pressures of the Earth's mantle between 525 and 660 km (326 and 410 mi) depth. It may also contain iron and hydrogen. It is polymorphous with the olivine phase forsterite (a magnesium iron silicate). Ringwoodite is notable for being able to contain hydroxide ions (oxygen and hydrogen atoms bound together) within its structure. In this case two hydroxide ions usually take the place of a magnesium ion and two oxide ions."@en . . . . . "Ringwoodita"@ca . . "8949285"^^ . . "Ringwoodit \u00E4r en h\u00F6gtrycksfas av Mg2SiO4 som bildas vid h\u00F6ga temperaturer och tryck i jordens mantel p\u00E5 mellan 525 och 660 km djup. Det \u00E4r polymorft av olivinfasen , ett magnesiumj\u00E4rnsilikat. Ringwoodit kan inneh\u00E5lla hydroxidjoner i sin struktur. Ringwoodit har p\u00E5visats djupt ner i jordmanteln och ber\u00E4kningar tyder p\u00E5 att det kan finnas motsvarande en till tre g\u00E5nger v\u00E4rldshavens volym av vatten i mantelns \u00F6verg\u00E5ngszon vid 410 till 660 km djup."@sv . . "Ringwoodit adalah salah satu jenis mineral olivin yang terbentuk oleh tekanan dan suhu yang tinggi di mantel Bumi, di kedalaman sekitar 525 hingga 660 kilometer. Olivin merupakan mineral magnesium besi silikat. Mineral ini pertamakali diidentifikasi di sebuah meteorit pada 1969. Ada kemungkinan bahwa ada Ringwoodit dalam kuantitas sangat besar di dalam mantel Bumi. Ringwoodit memiliki ion hidroksida dalam struktur mineralnya. Ini meyakinkan para ilmuwan bahwa mineral ini terbentuk di sekitar zona peralihan antara kerak Bumi dan mantel, sekitar 410 hingga 660 km dalamnya."@in . . . . . "La ringwoodita es un mineral de la clase de los nesosilicatos, y dentro de esta pertenece al llamado \u201Cgrupo del olivino\u201D. Descubierta en 1969 en el meteorito que aparece en la imagen derecha \u2014ca\u00EDdo cerca de Charters Towers, en Queensland (Australia),\u200B\u2014, se la nombr\u00F3 as\u00ED luego de los estudios de Ted Ringwoodd (1930-1993) sobre las transiciones polim\u00F3rficas en minerales mant\u00E9licos como olivino y piroxeno a presiones equivalentes a profundidades cercanas a 600 km. Un sin\u00F3nimo es su clave: IMA1968-036."@es . "Ringwoodyt \u2013 jest form\u0105 oliwinu. Sk\u0142ad chemiczny minera\u0142u mo\u017Ce by\u0107 r\u00F3\u017Cny, od czystego Mg2SiO4, do Fe2SiO4. Minera\u0142 zawiera 2,5% wagowych wody, a najbardziej uwodnione oko\u0142o 3% wagowych. Uzyskany w warunkach laboratoryjnych minera\u0142 nie zawieraj\u0105cy \u017Celaza jest bezbarwny. Przy zawarto\u015Bci jednego procenta molowego Fe2SiO4 barwa minera\u0142u jest intensywnie niebieska. Ringwoodyt zidentyfikowano po raz pierwszy w 1969 roku w meteorycie Tenham.Zaproponowana przez odkrywc\u00F3w nazwa upami\u0119tnia Australijczyka profesora z Australian National University, kt\u00F3ry bada\u0142 polimorficzne przej\u015Bcia fazowe minera\u0142\u00F3w p\u0142aszcza ziemskiego. Nazwa zosta\u0142a zaaprobowana przez Commission on New Minerals and Mineral Names. Z bada\u0144 i modeli wynika, \u017Ce ringwoodyty wyst\u0119puj\u0105 w strefie przej\u015Bciowej na g\u0142\u0119boko\u015Bciach 410-660 (525-660) kilometr\u00F3w. Ringwoodyt ziemskiego pochodzenia odkryto w 2008 roku na terenie Ju\u00EDny w stanie Mato Grosso w drobnym diamencie, znalezionym w \u017Cwirze p\u0142ytkiej rzeki. Diament zosta\u0142 wyniesiony na powierzchni\u0119 Ziemi przez ska\u0142\u0119 wulkaniczn\u0105 zwan\u0105 kimberlitem. W badanym elemencie zawarto\u015B\u0107 wody wynosi\u0142a oko\u0142o 1% wagowo. Jednak przy powszechnym wyst\u0119powaniu tego minera\u0142u w p\u0142aszczu Ziemi oznacza\u0142oby to, \u017Ce w strefie przej\u015Bciowej zgromadzone jest wi\u0119cej wody ni\u017C we wszystkich oceanach na powierzchni planety. Wyniki bada\u0144 wskazuj\u0105 na istnienie rozleg\u0142ej strefy w p\u0142aszczu ziemskim bogatej w wod\u0119."@pl . . . . "Ringwoodite"@en . "3.9"^^ . . "\u0420\u0438\u043D\u0433\u0432\u0443\u0434\u0438\u0442 (\u0441\u043E\u043A\u0440\u0430\u0449\u0451\u043D\u043D\u043E Rv) \u2014 \u043F\u043B\u043E\u0442\u043D\u044B\u0439 \u0443\u043B\u044C\u0442\u0440\u0430\u0432\u044B\u0441\u043E\u043A\u043E\u0431\u0430\u0440\u043D\u044B\u0439 \u043C\u0438\u043D\u0435\u0440\u0430\u043B \u0433\u0440\u0443\u043F\u043F\u044B \u043E\u043B\u0438\u0432\u0438\u043D\u0430. \u041A\u0443\u0431\u0438\u0447\u0435\u0441\u043A\u0438\u0439 \u0442\u0440\u0438\u043C\u043E\u0440\u0444 \u0444\u043E\u0440\u0441\u0442\u0435\u0440\u0438\u0442\u0430 \u0438 . \u0412\u0441\u0442\u0440\u0435\u0447\u0430\u0435\u0442\u0441\u044F \u0432 \u043C\u0435\u0442\u0435\u043E\u0440\u0438\u0442\u0430\u0445 (\u0445\u043E\u043D\u0434\u0440\u0438\u0442\u0430\u0445). \u0420\u0430\u0437\u043D\u043E\u0432\u0438\u0434\u043D\u043E\u0441\u0442\u044C \u0437\u0435\u043B\u0451\u043D\u043E\u0433\u043E \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u0430 \u043F\u0435\u0440\u0438\u0434\u043E\u0442\u0430."@ru . "La ringwoodite \u00E8 un minerale scoperto nel 1969 nel e si presume essere presente in quantit\u00E0 abbondante nel mantello terrestre. La ringwoodite \u00E8 un polimorfo di alta pressione dell'olivina che \u00E8 stabile alle temperature e pressioni presenti nel mantello terrestre a profondit\u00E0 comprese fra i 525 e i 660 km. L'olivina, la wadsleyite e la ringwoodite sono dei polimorfi trovati nel mantello superiore terrestre. A profondit\u00E0 superiori ai 660 km sono stabili altri minerali tra cui quelli con la struttura della perovskite. Le propriet\u00E0 di questi minerali determinano molte delle propriet\u00E0 del mantello."@it . "\u0420\u0438\u043D\u0433\u0432\u0443\u0434\u0438\u0442"@uk . . . . "Deep blue, also red, violet, or colourless"@en . . "Ringwoodit"@sv . . . . . "Ringwoodita"@eu . . . "Crystal of Fo90 composition blue ringwoodite synthesized at 20 GPa and 1200 \u00B0C."@en . "\u0420\u0438\u043D\u0433\u0432\u0443\u0434\u0438\u0442 (\u0441\u043E\u043A\u0440\u0430\u0449\u0451\u043D\u043D\u043E Rv) \u2014 \u043F\u043B\u043E\u0442\u043D\u044B\u0439 \u0443\u043B\u044C\u0442\u0440\u0430\u0432\u044B\u0441\u043E\u043A\u043E\u0431\u0430\u0440\u043D\u044B\u0439 \u043C\u0438\u043D\u0435\u0440\u0430\u043B \u0433\u0440\u0443\u043F\u043F\u044B \u043E\u043B\u0438\u0432\u0438\u043D\u0430. \u041A\u0443\u0431\u0438\u0447\u0435\u0441\u043A\u0438\u0439 \u0442\u0440\u0438\u043C\u043E\u0440\u0444 \u0444\u043E\u0440\u0441\u0442\u0435\u0440\u0438\u0442\u0430 \u0438 . \u0412\u0441\u0442\u0440\u0435\u0447\u0430\u0435\u0442\u0441\u044F \u0432 \u043C\u0435\u0442\u0435\u043E\u0440\u0438\u0442\u0430\u0445 (\u0445\u043E\u043D\u0434\u0440\u0438\u0442\u0430\u0445). \u0420\u0430\u0437\u043D\u043E\u0432\u0438\u0434\u043D\u043E\u0441\u0442\u044C \u0437\u0435\u043B\u0451\u043D\u043E\u0433\u043E \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u0430 \u043F\u0435\u0440\u0438\u0434\u043E\u0442\u0430."@ru . "\u5C16\u6676\u6A44\u6B16\u77F3\uFF0C\u4EA6\u4F5C\u03B3\u76F8\u6A44\u6B16\u77F3\u6216\u5F9E\u82F1\u8A9E\u97F3\u8B6F\u4F5C\u6797\u4F0D\u5FB7\u77F3\uFF0C\u662F\u4E00\u7A2E\u65BC\u9AD8\u6EAB\u9AD8\u58D3\u74B0\u5883\u4E0B\uFF08\u7D04\u4ECB\u65BC525\u516C\u91CC\u81F3660\u516C\u91CC\u9593\u7684\u5730\u51FD\uFF09\u7522\u751F\u7684\u7926\u7269\uFF0C\u70BA\u6A44\u6B16\u77F3\uFF08\u4E00\u7A2E\u9435\u9382\u77FD\u9178\u9E7D\u7926\u7269\uFF09\u7684\u9AD4\u3002 \u5C16\u6676\u6A44\u6B16\u77F3\u80FD\u5C07\u6C34\u5408\u7269\u5305\u542B\u65BC\u5176\u7D50\u69CB\u4E2D\uFF0C\u7D50\u5408\u5176\u65BC\u5730\u7403\u5167\u90E8\u5730\u51FD\u51FA\u73FE\u7684\u8B49\u64DA\uFF0C\u8AAA\u660E\u5F88\u6709\u53EF\u80FD\u5728410\u81F3660\u516C\u91CC\u6DF1\u8655\u7684\u5730\u5E541%\u662F\u6C34\uFF0C\u5C31\u76F8\u5F53\u4E8E\u5730\u7403\u4E0A\u6240\u6709\u6D77\u6D0B\u6C34\u91CF\u603B\u548C\u76843\u500D\u3002 \u6B64\u7926\u7269\u9996\u6B21\u57281969\u5E74\u65BCTemham\u9695\u77F3\u4E2D\u88AB\u767C\u73FE\uFF0C\u4E14\u88AB\u8A8D\u70BA\u5F88\u6709\u53EF\u80FD\u5927\u91CF\u5730\u5B58\u5728\u65BC\u5730\u7403\u7684\u5730\u51FD\u4E2D\u3002\u4ECE\u5DF4\u897F\u8339\u4F0A\u7EB3\u5730\u533A\u5730\u9762\u4E0A\u7684\u5CA9\u6D46\u4E2D\u53D1\u73B0\u7684\u94BB\u77F3\u4E2D\u5B58\u572840\u5FAE\u7C73\u957F\u7684\u6676\u4F53\u5185\u542B\u7269\u3002\u5149\u8C31\u5206\u6790\u8868\u660E\u8FD9\u5C31\u662F\u5C16\u6676\u6A44\u6984\u77F3\uFF1B\u5728\u7EBF\u53D1\u8868\u4E8E\u300A\u81EA\u7136\u300B\u4E0A\u7684\u8FDB\u4E00\u6B65\u5206\u6790\u663E\u793A\uFF0C\u5C16\u6676\u6A44\u6984\u77F3\u542B\u6709\u6C22\u6C27\u952E\uFF0C\u8868\u660E\u6676\u683C\u4E2D\u81F3\u5C11\u542B\u67091.4%\u7684\u6C34\u3002 \u5C16\u6676\u6A44\u6B16\u77F3\u53C8\u540D\u6797\u4F0D\u5FB7\u77F3\uFF08Ringwoodite\uFF09\uFF0C\u4EE5\u8457\u540D\u7684\u6FB3\u6D32\u5730\u7403\u5167\u90E8\u5B78\u5BB6\uFF081930\uFF0D1993\uFF09\u547D\u540D\uFF0C\u4ED6\u4E3B\u8981\u7814\u7A76\u5730\u51FD\u7926\u7269\uFF08\u5982\u8F1D\u77F3\u8207\u6A44\u6B16\u77F3\uFF09\u65BC\u5730\u7403\u5167\u90E8\u8D85\u904E600\u516C\u91CC\u6DF1\u8655\u7684\u540C\u8CEA\u7570\u76F8\u9AD4\u7279\u6027\u3002 \u5728\u5730\u9762\u4EE5\u4E0B410km\u6DF1\u5904\uFF0814GPa\uFF09\u7684\u5730\u5E54\u8FC7\u6E21\u5E26\u4E0A\u754C\uFF0C\u6A44\u6B16\u77F3\uFF08\u03B1\u76F8\uFF09\u7684\u6676\u4F53\u7C92\u5EA6\u968F\u7740\u538B\u529B\u5347\u9AD8\u8F6C\u53D8\u4E3A\u66F4\u9AD8\u5BC6\u5EA6\u548C\u6CE2\u901F\u7684\uFF08\u4F3C\u5C16\u6676\u6A44\u6B16\u77F3\uFF09\uFF08\u03B2\u76F8\uFF09\uFF0C\u4F53\u79EF\u51CF\u5C118%\u3002\u5728\u8FC7\u6E21\u5E26520km\u6DF1\u5904\uFF0C\u74E6\u5179\u5229\u77F3\u53D8\u6210\u5C16\u6676\u6A44\u6984\u77F3\uFF08\u03B3\u76F8\uFF09\u4E0E\u77F3\u69B4\u77F3\uFF0C\u4F53\u79EF\u51CF\u5C1129%\u3002\u800C\u5728\u8D85\u904E660\u516C\u91CC\u6DF1\u8655\uFF0823.5GPa\uFF09\u7684\u5730\u51FD\uFF0C\u9AD8\u538B\u76F8\u7684\u5C16\u6676\u6A44\u6984\u77F3\u968F\u7740\u538B\u529B\u5347\u9AD8\u53D1\u751F\u4E86\u4E24\u79CD\u5BC6\u5EA6\u66F4\u5927\u7684\u540E\u5C16\u6676\u77F3\u76F8\u53D8\uFF1A\u5E03\u91CC\u5947\u66FC\u77F3\u4E0E\u3002"@zh . . . . . . . . "La ringwoodite est un polymorphe de l'orthosilicate de magn\u00E9sium et de fer (Mg,Fe)2SiO4, stable \u00E0 hautes pression et temp\u00E9rature. D'abord obtenue au laboratoire par le p\u00E9trologue et g\u00E9ochimiste australien Ted Ringwood, elle a ensuite \u00E9t\u00E9 observ\u00E9e dans des m\u00E9t\u00E9orites, puis dans de rares \u00E9chantillons terrestres. Les donn\u00E9es acquises en p\u00E9trologie exp\u00E9rimentale et en sismologie indiquent que la ringwoodite est un composant majeur du manteau sup\u00E9rieur terrestre."@fr . . "Ringwoodyt \u2013 jest form\u0105 oliwinu. Sk\u0142ad chemiczny minera\u0142u mo\u017Ce by\u0107 r\u00F3\u017Cny, od czystego Mg2SiO4, do Fe2SiO4. Minera\u0142 zawiera 2,5% wagowych wody, a najbardziej uwodnione oko\u0142o 3% wagowych. Uzyskany w warunkach laboratoryjnych minera\u0142 nie zawieraj\u0105cy \u017Celaza jest bezbarwny. Przy zawarto\u015Bci jednego procenta molowego Fe2SiO4 barwa minera\u0142u jest intensywnie niebieska. Z bada\u0144 i modeli wynika, \u017Ce ringwoodyty wyst\u0119puj\u0105 w strefie przej\u015Bciowej na g\u0142\u0119boko\u015Bciach 410-660 (525-660) kilometr\u00F3w."@pl . "La ringwoodite \u00E8 un minerale scoperto nel 1969 nel e si presume essere presente in quantit\u00E0 abbondante nel mantello terrestre. La ringwoodite \u00E8 un polimorfo di alta pressione dell'olivina che \u00E8 stabile alle temperature e pressioni presenti nel mantello terrestre a profondit\u00E0 comprese fra i 525 e i 660 km. La ringwoodite \u00E8 nota perch\u00E9 la sua struttura \u00E8 in grado di trattenere acqua all'interno, non allo stato liquido ma sotto forma di ioni idrossido (atomi di ossigeno ed idrogeno legati insieme). Questa sua caratteristica, unita alle prove della sua presenza nel mantello terrestre, fa supporre che nella zona di transizione del mantello (fra i 400 e i 670 km di profondit\u00E0) ci possa essere una quantit\u00E0 d'acqua corrispondente ad un oceano, secondo altri la quantit\u00E0 stimata \u00E8 circa il triplo di quella di tutti gli oceani in superficie. L'olivina, la wadsleyite e la ringwoodite sono dei polimorfi trovati nel mantello superiore terrestre. A profondit\u00E0 superiori ai 660 km sono stabili altri minerali tra cui quelli con la struttura della perovskite. Le propriet\u00E0 di questi minerali determinano molte delle propriet\u00E0 del mantello."@it . . . . . "A ringwoodita ou ringwoodite \u00E9 um mineral da classe dos nesossilicatos, e dentro desta pertence ao chamado \u201Cgrupo da olivina\". Descoberto em 1969 num meteorito ca\u00EDdo pr\u00F3ximo de , em Queensland, Austr\u00E1lia, foi assim nomeado em honra a Alfred E. Ringwood, geoqu\u00EDmico australiano."@pt . . . . "19724"^^ . "a = 8.113 \u00C5; Z = 8"@en . . . "1116497723"^^ . . . . . . . . . . "Magnesium silicate"@en . . . . . "n = 1.8"@en . . "Ringwoodite"@fr . "La ringwoodita \u00E9s un mineral de la classe dels silicats del grup de l'olivina. Va ser descoberta l'any 1967 a partir del meteorit Tenham, que va impactar a , Queensland, Austr\u00E0lia i va rebre el seu nom en honor del geoqu\u00EDmic australi\u00E0 (1930-1993), el qual va estudiar les transicions de fase polim\u00F2rfiques dels minerals d'olivina i piroxens comuns en el mantell terrestre a pressions equivalent a profunditats d'uns 600 km."@ca . "none"@en .