[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:1425":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":11,"polytypeof":11,"groupid":12,"weighting":13,"nolocadd":14,"blacklisted":14,"mindat_formula":15,"mindat_formula_note":16,"ima_formula":17,"elements":18,"sigelements":28,"key_elements":29,"impurities":11,"cim":30,"ima_status":31,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":11,"discovery_year":11,"strunz10ed1":34,"strunz10ed2":35,"strunz10ed3":36,"strunz10ed4":37,"dana8ed1":38,"dana8ed2":39,"dana8ed3":38,"dana8ed4":40,"csystem":41,"cclass":42,"spacegroup":43,"spacegroupset":44,"a":45,"b":46,"c":47,"alpha":48,"beta":48,"gamma":48,"aerror":49,"berror":50,"cerror":51,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":52,"csmetamict":14,"commentcrystal":53,"twinning":54,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":55,"tlform":11,"hmin":56,"hmax":57,"hardtype":11,"vhnmin":58,"vhnmax":59,"vhnerror":11,"vhng":60,"vhns":11,"commenthard":11,"dmeas":61,"dmeas2":62,"dcalc":63,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":64,"commentluster":11,"diapheny":11,"streak":65,"colour":66,"commentcolor":67,"colors":68,"streak_colors":75,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":76,"tenacity":77,"commentbreak":11,"opticaltype":78,"opticalsign":11,"opticalalpha":48,"opticalalpha2":48,"opticalalphaerror":11,"opticalbeta":48,"opticalbeta2":48,"opticalbetaerror":11,"opticalgamma":48,"opticalgamma2":48,"opticalgammaerror":11,"opticalomega":48,"opticalomega2":48,"opticalomegaerror":11,"opticalepsilon":48,"opticalepsilon2":48,"opticalepsilonerror":11,"opticaln":79,"opticaln2":80,"opticalnerror":11,"optical2vcalc":48,"optical2vcalc2":48,"optical2vcalcerror":11,"optical2vmeasured":48,"optical2vmeasured2":48,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":78,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":11,"otheroccurrence":81,"type_specimen_store":11,"description_short":82,"aboutname":83,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":84,"reviewed_at":11,"variety_of":11,"varieties":85,"group_members":86,"associates":128,"confused_with":136,"type_localities":138,"occurrence_total":143,"citations":144,"images":179,"structures":289,"synonyms":302,"language_names":311,"wikidata_qid":441,"texts":442},1425,"1:1:1425:6","3ef27e33-959c-405a-9951-ed2d56ea9d9e","Euxenite-(Y)","Eux-Y",0,"mineral",null,47564,5782,false,"(Y,Ca,Ce,U,Th)(Nb,Ta,Ti)\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>","Usually the sum (Nb+Ta) is close to Ti, in other words (Nb+Ta)\u002FTi ~ 1.\r\nSynthetic end-member: YTiNbO\u003Csub>6\u003C\u002Fsub>","Y(Ti,Nb)\u003Csub>2\u003C\u002Fsub>(O,OH)\u003Csub>6\u003C\u002Fsub>",[19,20,21,22,23,24,25,26,27],"Ca","Ce","Nb","Ta","Th","Ti","O","U","Y",[21,25,27],[21,27],"18.4.5",[32,33],"APPROVED","GRANDFATHERED","4","D","G","05","8","3","2","Orthorhombic",8,63,"Pbcn ","5.5528","14.6432","5.1953","0",6,20,7,4,"Typically metamict; heating at high temperatures will restore crystallinity.","1. On {201}, common. The twins are flattened {010} and striated [001] 2. Possibly on {101}, rare. 3. Possibly on {013}.","Stout prismatic [001]. The faces are striated parallel to their intersection with {010} Often in parallel or subparallel and slightly radial aggregates of crystals. Massive.",5.5,6.5,"633","692",50,"5.3","5.9","5.16","Vitreous,Greasy,Sub-Metallic","Yellowish, grayish, reddish brown","Black, greenish or brownish tint at times","Brown to yellow brown in transmitted light.",[69,70,71,72,73,74],"black","brown","green","yellow","gray","red",[72,73,74,70],"Conchoidal,Sub-Conchoidal","brittle","Isotropic","2.06","2.24","Granitic pegmatites. Placer deposits.","Minerals of the Euxenite-(Y)-Polycrase-(Y) series are the most widespread niobates after columbite-(Fe) and pyrochlore.\r\nEuxenite-(Y) is typically metamict.\r\n\r\nCompare Nioboaeschynite-(Y) which has different space-group symmetry. Compare also Fergusoni...","From the Greek εΰζευος, friendly to strangers, hospitale, in allusion to the many rare elements that it contains.","2026-04-22 13:47:41",[],[87,94,102,109,116,121],{"id":88,"name":89,"entrytype":9,"csystem":41,"ima_formula":90,"mindat_formula":90,"hmin":52,"hmax":91,"dmeas":48,"dcalc":92,"primary_image_id":93},1539,"Fersmite","CaNb\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>",4.5,"4.78",8871,{"id":95,"name":96,"entrytype":9,"csystem":97,"ima_formula":98,"mindat_formula":98,"hmin":56,"hmax":56,"dmeas":99,"dcalc":100,"primary_image_id":101},2232,"Kobeite-(Y)","Isometric","(Y,U)(Ti,Nb)\u003Csub>2\u003C\u002Fsub>(O,OH)\u003Csub>6\u003C\u002Fsub> (?)","4.60","4.13",13456,{"id":103,"name":104,"entrytype":9,"csystem":11,"ima_formula":105,"mindat_formula":106,"hmin":107,"hmax":107,"dmeas":108,"dcalc":48,"primary_image_id":11},2435,"Loranskite-(Y)","(Y,Ce,Ca)(Zr,Ta)\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub> (?)","(Y,Ce,Ca)ZrTaO\u003Csub>6\u003C\u002Fsub> (?)",5,"4.6",{"id":110,"name":111,"entrytype":9,"csystem":41,"ima_formula":112,"mindat_formula":113,"hmin":56,"hmax":49,"dmeas":114,"dcalc":48,"primary_image_id":115},3883,"Tanteuxenite-(Y)","Y(TaTi)O\u003Csub>6\u003C\u002Fsub>","Y(Ta,Nb,Ti)\u003Csub>2\u003C\u002Fsub>(O,OH)\u003Csub>6\u003C\u002Fsub>","5.4",23599,{"id":117,"name":118,"entrytype":9,"csystem":41,"ima_formula":119,"mindat_formula":120,"hmin":107,"hmax":49,"dmeas":48,"dcalc":48,"primary_image_id":11},4109,"Uranopolycrase","UTi\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>","(U\u003Csup>4+\u003C\u002Fsup>,Y)(Ti,Nb)\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>",{"id":122,"name":123,"entrytype":9,"csystem":124,"ima_formula":11,"mindat_formula":125,"hmin":56,"hmax":49,"dmeas":126,"dcalc":48,"primary_image_id":127},4370,"Yttrocrasite-(Y)","Amorphous","(Y,Th,Ca,U)(Ti,Fe)\u003Csub>2\u003C\u002Fsub>(O,OH)\u003Csub>6\u003C\u002Fsub>","4.8",86877,[129],{"id":130,"name":131,"entrytype":9,"csystem":41,"ima_formula":132,"mindat_formula":132,"hmin":107,"hmax":49,"dmeas":133,"dcalc":134,"primary_image_id":135},39,"Aeschynite-(Y)","Y(TiNb)O\u003Csub>6\u003C\u002Fsub>","4.82","5.5",296,[137],{"id":110,"name":111,"entrytype":9,"csystem":41,"ima_formula":112,"mindat_formula":113,"hmin":56,"hmax":49,"dmeas":114,"dcalc":48,"primary_image_id":115},[139],{"id":140,"txt":141,"latitude":11,"longitude":11,"country":142},246082,"Undisclosed pegmatite, Jølster, Sunnfjord, Vestland, Norway","Norway",526,[145,150,154,158,162,166,170,175],{"id":146,"year":147,"html":148,"doi":149},4458703,1840,"Scheerer, Th. (1840) Ueber den Euxenit, eine neue Mineralspecies. \u003Ci>Annalen der Physik und Chemie\u003C\u002Fi>, 126. 149-153 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fandp.18401260510'>doi:10.1002\u002Fandp.18401260510\u003C\u002Fa>","10.1002\u002Fandp.18401260510",{"id":151,"year":152,"html":153,"doi":11},16108821,1847,"Scheerer (1847) Ann. Phys.: 72: 566.",{"id":155,"year":156,"html":157,"doi":11},16108822,1927,"Ellsworth (1927) American Mineralogist: 12: 212.",{"id":159,"year":160,"html":161,"doi":11},16108823,1928,"Simpson E S (1928) Tanteuxenite (Sp.nov.) Pilbara Goldfield, N.W. Div.. Journal of the Royal Society of Western Australia 14, 45-48.",{"id":163,"year":164,"html":165,"doi":11},1118651,1944,"Palache, Charles, Berman, Harry, Frondel, Clifford (1944) \u003Ci>The System of Mineralogy\u003C\u002Fi> (7th ed.) Vol. 1 - Elements, Sulfides, Sulfosalts, Oxides. John Wiley and Sons, New York.",{"id":167,"year":168,"html":169,"doi":11},16108825,1977,"Ewing R.C., Snetsinger K.G., Bunch T.E. (1977) Euxenite from Ampangabé, Madagascar. The Canadian Mineralogist 15, 92-96.",{"id":171,"year":172,"html":173,"doi":174},109661,1980,"Weitzel, H.; Schröcke, H. (1980) Kristallstrukturverfeinerungen von Euxenit, Y(Nb\u003Csub>0,5\u003C\u002Fsub>Ti\u003Csub>0,5\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>, und M-Fergusonit, YNbO\u003Csub>4\u003C\u002Fsub>. \u003Ci>Zeitschrift für Kristallographie\u003C\u002Fi>,  152 (1-2). p.69-82. \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1980.152.1-2.69'>doi:10.1524\u002Fzkri.1980.152.1-2.69\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fzk\u002Fvol152\u002FZK152_69.pdf?reftype=unknown' class='refpdflink'>\u003C\u002Fa>","10.1524\u002Fzkri.1980.152.1-2.69",{"id":176,"year":177,"html":178,"doi":11},16964178,2005,"(2005) Euxenite-(Y). \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Feuxenite-Y.pdf' class='refpdflink'>\u003C\u002Fa>",[180,190,199,206,214,219,227,232,242,249,258,268,275,280],{"id":181,"source_url":182,"license_code":183,"credit_html":184,"title":185,"description":186,"author":187,"original_width":188,"original_height":189},8207,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=3080280","CC BY-SA 3.0","Aangelo, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=3080280\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Euxenite - Vegusdal, Norvegia 01.jpg","Euxenite, crystals aggregation (11 cm) - Vegusdal, Norway","Aangelo",3264,2448,{"id":191,"source_url":192,"license_code":183,"credit_html":193,"title":194,"description":195,"author":196,"original_width":197,"original_height":198},8482,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10153138","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10153138\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Euxenite-(Y)-180877.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEuxenite\" class=\"extiw\" title=\"en:Euxenite\">Euxenite-(Y)\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Besakoa (Besekoa), Madagascar (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-190794.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 2.5 x 1.5 x 1 cm.\u003C\u002Fdd>\n\u003Cdd>An exceptionally well-crystallized specimen of the rare Yttrium Niobate, Euxenite. This tan-colored fan is composed of blades about .15 cm thick and 1.2 cm across. Ex. Dick Bideaux Collection (originally labelled \"fergusonite\").\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",348,500,{"id":200,"source_url":201,"license_code":202,"credit_html":203,"title":7,"description":11,"author":11,"original_width":204,"original_height":205},29694,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F168307","CC BY-SA 4.0","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F168307\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",944,1000,{"id":207,"source_url":208,"license_code":183,"credit_html":209,"title":210,"description":211,"author":196,"original_width":212,"original_height":213},8208,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10169798","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10169798\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Euxenite-(Y)-263711.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEuxenite\" class=\"extiw\" title=\"en:Euxenite\">Euxenite-(Y)\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Luella Pegmatite, Trout Creek Pass pegmatite District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBuena_Vista\" class=\"extiw\" title=\"en:Buena Vista\">Buena Vista\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FChaffee_County,_Colorado\" class=\"extiw\" title=\"en:Chaffee County, Colorado\">Chaffee County\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FColorado\" class=\"extiw\" title=\"en:Colorado\">Colorado\u003C\u002Fa>, USA (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-110810.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 5.8 x 4.8 x 3.3 cm.\u003C\u002Fdd>\n\u003Cdd>This locality is one of many rare-earth pegmatites along the front range of Colorado. Specimens of Euxenite from Colorado are not terribly common, and are often only found in old collections. Field collectors do not often find many specimens of Euxenite these days, and rich specimens such as this one are hard to find. This piece shows the typical greasy luster and black color for a Colorado Euxenite. A good reference specimen from the Richard A. Kosnar collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",483,432,{"id":215,"source_url":216,"license_code":202,"credit_html":217,"title":7,"description":11,"author":11,"original_width":205,"original_height":218},29695,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F168305","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F168305\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",976,{"id":220,"source_url":221,"license_code":183,"credit_html":222,"title":223,"description":224,"author":196,"original_width":225,"original_height":226},8209,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=30345740","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=30345740\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Euxenite-(Y)-568158.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEuxenite\" class=\"extiw\" title=\"en:Euxenite\">Euxenite-(Y)\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Besakoa (Besekoa), Madagascar (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-190794.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 5 cm x 3.8 cm x 2.4 cm\u003C\u002Fdd>\n\u003Cdd>Euxenite-(Y) is an uncommon rare earth oxide containing numerous rare earth elements and is found in granite pegmatites. This is a sharp, well-formed, tan, floater, parallel-growth crystal with a chisel termination. This is a fine old-time piece. Accompanied by a N. Boubee label dating to before 1937.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",443,600,{"id":228,"source_url":229,"license_code":202,"credit_html":230,"title":7,"description":11,"author":11,"original_width":205,"original_height":231},29696,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F168304","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F168304\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",827,{"id":233,"source_url":234,"license_code":235,"credit_html":236,"title":237,"description":238,"author":239,"original_width":240,"original_height":241},8210,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=30346016","CC BY 3.0","Kelly Nash, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=30346016\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Euxenite-(Y)-491055.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEuxenite-(Y)\" class=\"extiw\" title=\"en:Euxenite-(Y)\">Euxenite-(Y)\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Cactus Jack pegmatite, Burnet County, Texas, USA\u003C\u002Fdd>\n\u003Cdd>\u003Ci>Original description:\u003C\u002Fi> Crystalline euxenite, 27 x 16 x 13 mm. Collected by Frank Roberts, 2007. Slightly radioactive (~40 microrems\u002Fhr., roughly 5 - 10 x background). Trade from Art Smith. K. Nash specimen & photo.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Kelly Nash",684,1024,{"id":243,"source_url":244,"license_code":183,"credit_html":245,"title":246,"description":247,"author":196,"original_width":248,"original_height":226},53973,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=66377551","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=66377551\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Polycrase-(Y)-619586.jpg","Polycrase-(Y) is a rare multiple-oxide containing Y, U, Ti or Nb and is mainly found in pegmatites. Specimens labeled as being from this obscure locality may be from a pegmatite district around the cities of Rio Pomba and Uba (MINDAT). Specimens of any species are rare from this district. This is a stout, terminated, euhedral, prismatic crystal with an orangish-brown oxidation rind. The minimal bruising reveals the high waxy lustre and moderate translucence of the chocolate-brown crystal with orange highlights. Very rarely available. Ex. Josef Vajdak Collection.\n\u003Cdl>\u003Cdd>Size: 5.2 x 2.7 x 2.0 cm.\u003C\u002Fdd>\n\u003Cdd>From: Rio Pomba, Minas Gerais, Brazil\u003C\u002Fdd>\u003C\u002Fdl>",418,{"id":250,"source_url":251,"license_code":202,"credit_html":252,"title":253,"description":254,"author":255,"original_width":256,"original_height":257},8212,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130375385","Raimond Spekking, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130375385\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Euxenite. Salesbury, Rhodesia-9221.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FEuxenite\" class=\"extiw\" title=\"en:Euxenite\">Euxenite\u003C\u002Fa> (Weight: 16.67 g) – Place of discovery: Harare, Zimbabwe (formerly \u003Ci>Salisbury, Rhodesia\u003C\u002Fi>","Raimond Spekking",5105,3829,{"id":259,"source_url":260,"license_code":261,"credit_html":262,"title":263,"description":264,"author":265,"original_width":266,"original_height":267},53978,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118185074","CC BY-SA 2.0","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118185074\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Euxenite (47975540271).jpg","\u003Cp>Renfrew County\n\u003C\u002Fp>\nOntario, Canada","Pacific Museum of Earth from Canada",4000,6000,{"id":269,"source_url":270,"license_code":202,"credit_html":271,"title":272,"description":254,"author":255,"original_width":273,"original_height":274},8213,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130375392","Raimond Spekking, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130375392\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Euxenite. Salesbury, Rhodesia-9222.jpg",6715,4477,{"id":276,"source_url":277,"license_code":202,"credit_html":278,"title":279,"description":254,"author":255,"original_width":273,"original_height":274},8214,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130375398","Raimond Spekking, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130375398\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Euxenite. Salesbury, Rhodesia-9223.jpg",{"id":281,"source_url":282,"license_code":202,"credit_html":283,"title":284,"description":285,"author":286,"original_width":287,"original_height":288},8211,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=65897960","Ismoon (talk) 21:09, 27 January 2018 (UTC), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=65897960\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rare-earth mineral. Euxenite. Madagascar. Musée des Confluences.jpg","Rare-earth mineral. Euxenite. Madagascar. Musée des Confluences. Lyon.","Ismoon (talk) 21:09, 27 January 2018 (UTC)",1086,724,[290,297],{"id":291,"url":292,"label":293,"formula":294,"spacegroup":295,"year":296},4324,"\u002Fcif\u002F4324.cif","Johnsen 1999","Y.48 Dy.02 Ti.54 Nb.46 O3","P b c n",1999,{"id":298,"url":299,"label":300,"formula":301,"spacegroup":295,"year":172},4325,"\u002Fcif\u002F4325.cif","Weitzel 1980","Y (Nb Ti) O6",[303,304,305,306,307,308,309,310],"Euxeniet-(Y)","Euxenite","Euxenite-Polycrase","Euxenite-Polycrase Group","Euxenite-Polycrase Series","Guimaraesite (of Gagarin & Cuomo)","Lyndochite","Polycrase-(Y)",[312,316,320,325,330,334,339,342,346,350,355,358,363,368,372,376,380,384,388,392,395,399,403,406,409,413,417,421,425,430,433,438],{"lang":313,"names":314},"ar",[315],"يوكسينيت",{"lang":317,"names":318},"be-tarask",[319],"эўксэніт",{"lang":321,"names":322},"ca",[323,324],"Euxenita-","euxenita-(Y)",{"lang":326,"names":327},"de",[328,329],"Euxenit-","Euxenit-(Y)",{"lang":331,"names":332},"el",[333],"Ευξενίτης",{"lang":335,"names":336},"es",[337,338],"Euxenita","Euxenita-(Y)",{"lang":340,"names":341},"eu",[323,338],{"lang":343,"names":344},"fa",[345],"اگزنیت",{"lang":347,"names":348},"fi",[349],"Eukseniitti",{"lang":351,"names":352},"fr",[353,354],"Euxénite-","Euxénite-(Y)",{"lang":356,"names":357},"gl",[337],{"lang":359,"names":360},"it",[304,361,362],"Euxenite-","euxenite-(Y)",{"lang":364,"names":365},"ja",[366,367],"ユークセナイト","ユークセン石",{"lang":369,"names":370},"kk",[371],"Эвксенит",{"lang":373,"names":374},"ko",[375],"육세나이트",{"lang":377,"names":378},"lt",[379],"Euksenitas",{"lang":381,"names":382},"mk",[383],"Евксенит",{"lang":385,"names":386},"nb",[387],"euxenitt",{"lang":389,"names":390},"nl",[391],"euxeniet",{"lang":393,"names":394},"nn",[387],{"lang":396,"names":397},"no",[398],"Euxenitt",{"lang":400,"names":401},"pl",[402],"Euksenit",{"lang":404,"names":405},"pt",[337,338,304],{"lang":407,"names":408},"ru",[371],{"lang":410,"names":411},"sl",[412],"evksenit-(Y)",{"lang":414,"names":415},"sv",[416],"Euxenit",{"lang":418,"names":419},"ta",[420],"யூக்சனைட்டு",{"lang":422,"names":423},"tr",[424],"Öksenit",{"lang":426,"names":427},"uk",[428,429],"Евксеніт","Евксеніт-",{"lang":431,"names":432},"vi",[416],{"lang":434,"names":435},"zh",[436,437],"黑稀金矿","黑稀金礦",{"lang":439,"names":440},"zh-hans",[436],"Q1146596",{"history":11,"applications":11}]