[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:2906":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":11,"polytypeof":11,"groupid":11,"weighting":12,"nolocadd":13,"blacklisted":13,"mindat_formula":14,"mindat_formula_note":11,"ima_formula":15,"elements":16,"sigelements":23,"key_elements":24,"impurities":11,"cim":25,"ima_status":26,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":28,"discovery_year":11,"strunz10ed1":29,"strunz10ed2":30,"strunz10ed3":31,"strunz10ed4":32,"dana8ed1":33,"dana8ed2":34,"dana8ed3":29,"dana8ed4":35,"csystem":36,"cclass":11,"spacegroup":11,"spacegroupset":37,"a":38,"b":39,"c":40,"alpha":37,"beta":37,"gamma":37,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":11,"csmetamict":13,"commentcrystal":41,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":42,"hmin":43,"hmax":44,"hardtype":11,"vhnmin":37,"vhnmax":37,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":37,"dmeas2":37,"dcalc":37,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":11,"commentluster":11,"diapheny":11,"streak":11,"colour":45,"commentcolor":11,"colors":46,"streak_colors":11,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":49,"opticalsign":11,"opticalalpha":50,"opticalalpha2":51,"opticalalphaerror":11,"opticalbeta":52,"opticalbeta2":53,"opticalbetaerror":11,"opticalgamma":37,"opticalgamma2":37,"opticalgammaerror":11,"opticalomega":37,"opticalomega2":37,"opticalomegaerror":11,"opticalepsilon":37,"opticalepsilon2":37,"opticalepsilonerror":11,"opticaln":37,"opticaln2":37,"opticalnerror":11,"optical2vcalc":37,"optical2vcalc2":37,"optical2vcalcerror":11,"optical2vmeasured":37,"optical2vmeasured2":37,"optical2vmeasurederror":11,"rimin":54,"rimax":55,"opticaldispersion":56,"opticalpleochroism":57,"opticalpleochorismdesc":58,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":59,"otheroccurrence":11,"type_specimen_store":60,"description_short":61,"aboutname":62,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":63,"reviewed_at":11,"variety_of":11,"varieties":64,"group_members":65,"associates":66,"confused_with":67,"type_localities":68,"occurrence_total":75,"citations":76,"images":140,"structures":161,"synonyms":162,"language_names":164,"wikidata_qid":184,"texts":185},2906,"1:1:2906:9","cc7abfac-402e-491a-bb62-529ed374ba6b","Ningyoite","Nin",0,"mineral",null,107,false,"(U,Ca,Ce)\u003Csub>2\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>&middot;1-2H\u003Csub>2\u003C\u002Fsub>O","(U,Ca,Ce)\u003Csub>2\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub> &middot; 1-2H\u003Csub>2\u003C\u002Fsub>O",[17,18,19,20,21,22],"Ca","Ce","O","P","H","U",[19,20,21,22],[22],"19.11.13",[27],"APPROVED",1959,"8","C","J","85","40","4","1","Orthorhombic","0","6.78","12.1","6.38","May be hexagonal or trigonal (see Scharmová & Scharm (1994) and references cited therein).","Unoxidized zone, usually as a thin coating\r\non pyrite and apatite or filling cavities in the conglomerate.",3,4,"Brownish green to brown",[47,48],"brown","green","Biaxial","1.69","1.70","1.64","1.71",1.64,1.71,"not discernible","Weak","Paler in X direction","Black uranium ores in conglomerate","The Natural History Museum, London, England, 1960,92.\r\nNational Museum of Natural History, Washington, D.C., USA, 113822, 115885.","A potential Fe-Th-REE analogue is known as 'UM1979-10-PO:FeHREETh'. Also comparable to 'UM1980-04-PO:CaHREETh'.","Named in 1959 by Tadashi Muto, Robert Meyrowitz, Alfred M. Pommer, and Toru Murano for the Ningyo Pass, Japan, where the country's largest uranium deposit and type locality mine are located.","2026-03-31 12:03:05",[],[],[],[],[69],{"id":70,"txt":71,"latitude":72,"longitude":73,"country":74},13944,"Ningyo-toge mine, Tottori Prefecture, Japan",35.3083333,133.9227778,"Japan",25,[77,80,84,89,94,99,103,106,110,114,118,122,126,131,135],{"id":78,"year":28,"html":79,"doi":11},523216,"Muto, T., Meyrowitz, R., Pommer, A. M., Murano, T. (1959) Ningyoite, a new uranous phosphate from Japan. \u003Ci>American Mineralogist\u003C\u002Fi>,  44 (5-6) 633-650 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM44\u002FAM44_633.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":81,"year":82,"html":83,"doi":11},523399,1960,"Fleischer, M.; Chao, E.C.T. (1960) New mineral names. \u003Ci>American Mineralogist\u003C\u002Fi>,  45 (5-6). 753-756 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM45\u002FAM45_753.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":85,"year":86,"html":87,"doi":88},81353,1962,"MUTO, TADASHI (1962) The precipitation environment of ningyoite. \u003Ci>Mineralogical Journal\u003C\u002Fi>,  3 (5). 306-337 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2465\u002Fminerj1953.3.306'>doi:10.2465\u002Fminerj1953.3.306\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.jstage.jst.go.jp\u002Farticle\u002Fminerj1953\u002F3\u002F5-6\u002F3_5-6_306\u002F_pdf?reftype=.pdf' class='refpdflink'>\u003C\u002Fa>","10.2465\u002Fminerj1953.3.306",{"id":90,"year":91,"html":92,"doi":93},81373,1965,"MUTO, TADASHI (1965) Thermochemical stability of ningyoite. \u003Ci>Mineralogical Journal\u003C\u002Fi>,  4 (4). 245-274 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2465\u002Fminerj1953.4.245'>doi:10.2465\u002Fminerj1953.4.245\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.jstage.jst.go.jp\u002Farticle\u002Fminerj1953\u002F4\u002F4\u002F4_4_245\u002F_pdf?reftype=.pdf' class='refpdflink'>\u003C\u002Fa>","10.2465\u002Fminerj1953.4.245",{"id":95,"year":96,"html":97,"doi":98},231148,1970,"Kajitani, Kei (1970) A geochemical study on the genesis of ningyoite the special calcium uranous phosphate mineral. \u003Ci>Economic Geology\u003C\u002Fi>,  65 (4) 470-480 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgsecongeo.65.4.470'>doi:10.2113\u002Fgsecongeo.65.4.470\u003C\u002Fa>","10.2113\u002Fgsecongeo.65.4.470",{"id":100,"year":101,"html":102,"doi":11},16118520,1978,"Belova L.N., Gorshkov A.I., Ivanova O.A. (1978) First discovery of ningyoite in the U.S.S.R.. Doklady Akademii Nauk SSSR: 238(1): 215-216.",{"id":104,"year":101,"html":105,"doi":11},16118521,"Belova, L.N., Gorshkov, A.I., Ivanova, O.A. (1978) New data on ningyoite: iron-containing ningyoite. Doklady Akademii Nauk SSSR: 243(4): 1022-1023.",{"id":107,"year":108,"html":109,"doi":11},16118522,1981,"Boyle, D.R., Littlejohn, A.L., Roberts, A.C., Watson, D.M. (1981) Ningyoite in uranium deposits of South-central British Columbia: first North American occurrence. The Canadian Mineralogist: 19: 325-331. https:\u002F\u002Frruff.info\u002Fdoclib\u002Fcm\u002Fvol19\u002FCM19_325.pdf",{"id":111,"year":112,"html":113,"doi":11},16118523,1985,"Belova, L.N., Gorshkov, A.I., Ivanova, O.A., Dikov, Y.P., Sivtsov, A.V. (1985) Recent experimental data on ningyoite. Izvestiya Akademii Nauk SSSR, Seriya Geologicheskaya, 101-109.",{"id":115,"year":116,"html":117,"doi":11},16118524,1986,"Dymkov, Y.M., Bojtsov, V.E., Preobrazhenskij, A.N., Ivanova, O.A. (1986) Ningyoite from hydrothermal veins of Gorny Slavkov (Czechoslovakia). Mineralogicheskii Zhurnal: 34-43.",{"id":119,"year":120,"html":121,"doi":11},16694249,1994,"Scharmová, M., Scharm, B. (1994) Rhabdophane group minerals in the uranium ore district of northern Bohemia (Czech Republic) \u003Ci>Journal of the Czech Geological Society\u003C\u002Fi>,  39 (4) 267-280 \u003Ca target='_blank' href='http:\u002F\u002Fwww.jgeosci.org\u002Fcontent\u002FScharmova_and_Scharm_1994.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":123,"year":124,"html":125,"doi":11},16966297,2005,"(2005) Ningyoite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fningyoite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":127,"year":128,"html":129,"doi":130},19237,2007,"Doinikova, O. A. (2007) Uranium deposits with a new phosphate type of blacks. \u003Ci>Geology of Ore Deposits\u003C\u002Fi>,  49 (1) 80-86 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1134\u002Fs1075701507010047'>doi:10.1134\u002Fs1075701507010047\u003C\u002Fa>","10.1134\u002Fs1075701507010047",{"id":132,"year":133,"html":134,"doi":11},16118527,2008,"Utsunomiya, S., Deditius, A.P., Pointeau, V., Ewing, R. C. (2008) Coffinite and ningyoite from the natural, nuclear reactor at Bangombé, Gabon. Geology in China: 42(5).",{"id":136,"year":137,"html":138,"doi":139},7735791,2019,"René, Miloš, Dolníček, Zdeněk, Sejkora, Jiří, Škácha, Pavel, Šrein, Vladimír (2019) Uraninite, Coffinite and Ningyoite from Vein-Type Uranium Deposits of the Bohemian Massif (Central European Variscan Belt). \u003Ci>Minerals\u003C\u002Fi>,  9 (2). 123 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3390\u002Fmin9020123'>doi:10.3390\u002Fmin9020123\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.mdpi.com\u002F2075-163X\u002F9\u002F2\u002F123\u002Fpdf?version=1551171490' class='refpdflink'>\u003C\u002Fa>","10.3390\u002Fmin9020123",[141,151],{"id":142,"source_url":143,"license_code":144,"credit_html":145,"title":146,"description":147,"author":148,"original_width":149,"original_height":150},17709,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68387332","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=68387332\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Ningyoite.jpg","A specimen of the very rare mineral ningyoite from the type locality (Ningyo-toge Mine, Tottori Prefecture, Honshu Island, Japan). Ningyoite occurs as almost black crystal aggregates in a small pieces of matrix.","David Hospital",973,667,{"id":152,"source_url":153,"license_code":154,"credit_html":155,"title":156,"description":157,"author":158,"original_width":159,"original_height":160},17710,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118187591","CC BY-SA 2.0","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118187591\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Ningyoite (48522605102).jpg","\u003Cp>Ningyo - Toge\n\u003C\u002Fp>\nTottori Prefecture, Japan","Pacific Museum of Earth from Canada",6000,4000,[],[163],"Ningyoiet",[165,169,173,177,180],{"lang":166,"names":167},"ca",[168],"ningyoïta",{"lang":170,"names":171},"de",[172],"Ningyoit",{"lang":174,"names":175},"eu",[176],"Ningyoita",{"lang":178,"names":179},"it",[7],{"lang":181,"names":182},"ja",[183],"人形石","Q3877116",{"history":11,"applications":11}]