[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:2708":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":22,"key_elements":23,"impurities":11,"cim":24,"ima_status":25,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":27,"discovery_year":11,"strunz10ed1":28,"strunz10ed2":29,"strunz10ed3":30,"strunz10ed4":31,"dana8ed1":32,"dana8ed2":33,"dana8ed3":34,"dana8ed4":33,"csystem":35,"cclass":11,"spacegroup":11,"spacegroupset":36,"a":37,"b":38,"c":39,"alpha":36,"beta":36,"gamma":36,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":40,"csmetamict":13,"commentcrystal":41,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":42,"hmin":43,"hmax":43,"hardtype":11,"vhnmin":44,"vhnmax":45,"vhnerror":11,"vhng":46,"vhns":47,"commenthard":11,"dmeas":36,"dmeas2":36,"dcalc":48,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":49,"commentluster":11,"diapheny":50,"streak":11,"colour":51,"commentcolor":11,"colors":52,"streak_colors":11,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":36,"opticalalpha2":36,"opticalalphaerror":11,"opticalbeta":36,"opticalbeta2":36,"opticalbetaerror":11,"opticalgamma":36,"opticalgamma2":36,"opticalgammaerror":11,"opticalomega":36,"opticalomega2":36,"opticalomegaerror":11,"opticalepsilon":36,"opticalepsilon2":36,"opticalepsilonerror":11,"opticaln":36,"opticaln2":36,"opticalnerror":11,"optical2vcalc":36,"optical2vcalc2":36,"optical2vcalcerror":11,"optical2vmeasured":36,"optical2vmeasured2":36,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":55,"opticalcolour":56,"opticalinternal":57,"opticaltropic":58,"opticalanisotropism":59,"opticalbireflectance":60,"opticalextinction":11,"opticalr":61,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":62,"industrial":11,"occurrence":63,"otheroccurrence":11,"type_specimen_store":64,"description_short":11,"aboutname":65,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":66,"reviewed_at":11,"variety_of":11,"varieties":67,"group_members":68,"associates":69,"confused_with":70,"type_localities":71,"occurrence_total":76,"citations":77,"images":107,"structures":108,"synonyms":115,"language_names":118,"wikidata_qid":142,"texts":143},2708,"1:1:2708:9","4c50b39e-963e-43e5-80da-a0039baf66c7","Miharaite","Mih",0,"mineral",null,135,false,"Cu\u003Csub>4\u003C\u002Fsub>FePbBiS\u003Csub>6\u003C\u002Fsub>","PbCu\u003Csub>4\u003C\u002Fsub>FeBiS\u003Csub>6\u003C\u002Fsub>",[17,18,19,20,21],"Bi","Cu","Fe","Pb","S",[17,18,19,20,21],[17,18,20],"5.8.9",[26],"APPROVED",1980,"2","L","B","05","3","1","5","Orthorhombic","0","10.85","11.98","3.87",2,"Space group Pbnm, Pb2n, or pb2tm","minute (\u003C0.3 mm) grains in bornite",4,"190","230",25,15,"6.06","Metallic","Opaque","Pale gray to grayish-white in reflected light",[53,54],"gray","white","Reflectance data from Choi and Imai (1983).","Pale gray to grayish white.","None.","Anisotropic","Moderate anisotropism from grayish-blue to pinkish-brown.","faint","(29.2–30.8) 400,\r\n(29.7–30.8) 420,\r\n(30.6–31.4) 440,\r\n(31.2–32.0) 460,\r\n(31.3–32.0) 480,\r\n(32.1–32.8) 500,\r\n(32.2–32.9) 520,\r\n(32.2–33.0) 540,\r\n(32.1–33.0) 560,\r\n(32.2–33.5) 580,\r\n(32.2–33.9) 600,\r\n(32.3–34.3) 620,\r\n(32.4–34.9) 640,\r\n(32.4–35.1) 660,\r\n(32.8–35.7) 680,\r\n(32.8–35.8) 700","Miharaite may readily be distinguished from wittichenite: HNO3 (1:1) etches wittichenite slowly, gradually staining to a brown colour, but does not affect miharaite at all.\r\n\r\nMiharaite is slightly stained to bluish tinges by KOH (40%). No reaction to KCN (20%), HCl (1:1), FeCl3 (20%), HgCl2(5%) and H2O2.","Bornite rich skarn","Institute of Mineralogy Petrology, and Economic Geology, Faculty of Science, Tohoku University, Sendai, Japan, and Department of Mining and Mineral Engineering, Faculty of Engineering,Yamaguchi University, Ube, Japan.\r\n","Named in 1980 by Asahiko Sugaki, Hiromi Shima, and Arashi Kitakaze after the type locality, \u003Cl id='45343'>Mihara Mine, Okayama, Japan\u003C\u002Fl>.","2025-08-11 12:14:22",[],[],[],[],[72],{"id":73,"txt":74,"latitude":11,"longitude":11,"country":75},45343,"Honpi deposit, Mihara mine, Higashi-Mihara, Ibara City, Okayama Prefecture, Japan","Japan",18,[78,81,86,90,94,98,102],{"id":79,"year":27,"html":80,"doi":11},527472,"Sugaki, Asahiko, Shima, Hiromi, Kitakaze, Arashi (1980) Miharaite, Cu4FePbBiS6, a new mineral from the Mihara mine, Okayama, Japan. \u003Ci>American Mineralogist\u003C\u002Fi>,  65 (7-8) 784-788 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM65\u002FAM65_784.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":82,"year":83,"html":84,"doi":85},89058,1983,"CHOI, SEON GYU, IMAI, NAOYA (1983) Miharaite in bornite-rich copper ore from the Ulsan mine, Republic of Korea. \u003Ci>The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists\u003C\u002Fi>,  78 (9) 350-360 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2465\u002Fganko1941.78.350'>doi:10.2465\u002Fganko1941.78.350\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.jstage.jst.go.jp\u002Farticle\u002Fganko1941\u002F78\u002F9\u002F78_9_350\u002F_pdf' class='refpdflink'>\u003C\u002Fa>","10.2465\u002Fganko1941.78.350",{"id":87,"year":88,"html":89,"doi":11},16117183,1988,"Petrova, I.V., Pobedimskaya, E.A., Bryzgalov, I.A. (1988) Crystal structure of micharaite Cu4FePbBiS6. Doklady Akademii Nauk SSSR: 299: 123-127.",{"id":91,"year":92,"html":93,"doi":11},16117184,1990,"Kang Guan, Zhenkuan Luo, Manzhi Wang, and Chuantai Wang (1990) The first discovery of miharaite in China. Acta Mineralogica Sinica: 10(3): 227-231.",{"id":95,"year":96,"html":97,"doi":11},15959288,1994,"Pinto, A., Bowles, J. F. W., & Gaspar, O. C. (1994). The mineral chemistry and textures of wittichenite, miharaite, carrolite, mawsonite and In±Bi±Hg tennantite from Neves-Corvo, Portugal. IMA 94. In XVI General Meeting of IMA, Pisa, ItaÂlia, Abstracts.",{"id":99,"year":100,"html":101,"doi":11},16966031,2005,"(2005) Miharaite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fmiharaite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":103,"year":104,"html":105,"doi":106},90572,2014,"IZUMINO, Yuya, NAKASHIMA, Kazuo, NAGASHIMA, Mariko (2014) Cuprobismutite group minerals (cuprobismutite, hodrušhite, kupčíkite and padĕraite), other Bi–sulfosalts and Bi–tellurides from the Obari mine, Yamagata Prefecture, Japan. \u003Ci>Journal of Mineralogical and Petrological Sciences\u003C\u002Fi>,  109 (4) 177-190 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2465\u002Fjmps.140129'>doi:10.2465\u002Fjmps.140129\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.jstage.jst.go.jp\u002Farticle\u002Fjmps\u002F109\u002F4\u002F109_140129\u002F_pdf' class='refpdflink'>\u003C\u002Fa>","10.2465\u002Fjmps.140129",[],[109],{"id":110,"url":111,"label":112,"formula":113,"spacegroup":114,"year":88},9379,"\u002Fcif\u002F9379.cif","Petrova 1988","Pb Cu4 Fe Bi S6","P b 21 m",[116,117],"IMA1976-012","Miharaiet",[119,123,128,132,135,139],{"lang":120,"names":121},"ca",[122],"miharaïta",{"lang":124,"names":125},"de",[126,127],"IMA 1976-012","Miharait",{"lang":129,"names":130},"eu",[131],"Miharaita",{"lang":133,"names":134},"it",[7],{"lang":136,"names":137},"ja",[138],"三原鉱",{"lang":140,"names":141},"scn",[7],"Q3857315",{"history":11,"applications":11}]