[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:2002":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":15,"ima_formula":16,"elements":17,"sigelements":21,"key_elements":22,"impurities":11,"cim":23,"ima_status":24,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":27,"discovery_year":28,"strunz10ed1":29,"strunz10ed2":30,"strunz10ed3":31,"strunz10ed4":32,"dana8ed1":29,"dana8ed2":33,"dana8ed3":34,"dana8ed4":35,"csystem":36,"cclass":11,"spacegroup":11,"spacegroupset":37,"a":38,"b":37,"c":39,"alpha":37,"beta":37,"gamma":37,"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":42,"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":45,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":46,"commentluster":11,"diapheny":47,"streak":11,"colour":48,"commentcolor":11,"colors":49,"streak_colors":11,"luminescence":11,"uv":53,"cleavage":11,"cleavagetype":54,"fracturetype":55,"tenacity":56,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":37,"opticalalpha2":37,"opticalalphaerror":11,"opticalbeta":37,"opticalbeta2":37,"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":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":57,"opticalinternal":11,"opticaltropic":58,"opticalanisotropism":59,"opticalbireflectance":11,"opticalextinction":11,"opticalr":60,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":61,"otheroccurrence":11,"type_specimen_store":62,"description_short":63,"aboutname":64,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":65,"reviewed_at":11,"variety_of":11,"varieties":66,"group_members":67,"associates":68,"confused_with":76,"type_localities":77,"occurrence_total":82,"citations":83,"images":138,"structures":167,"synonyms":168,"language_names":171,"wikidata_qid":199,"texts":200},2002,"1:1:2002:8","3df280ec-ffd9-494d-a78f-9e020095959d","Idaite","Ida",0,"mineral",null,430,false,"Cu\u003Csub>5\u003C\u002Fsub>FeS\u003Csub>6\u003C\u002Fsub>","Very close to Cu\u003Csub>5.5\u003C\u002Fsub>FeS\u003Csub>6.5\u003C\u002Fsub> according to Sugaki et al. (1975).","Cu\u003Csub>3\u003C\u002Fsub>FeS\u003Csub>4\u003C\u002Fsub>",[18,19,20],"Cu","Fe","S",[18,19,20],[18],"3.1.29",[25,26],"APPROVED","GRANDFATHERED",1958,"1958","2","C","B","15a","9","14","1","Hexagonal","0","3.90","16.95",1,"Space group unknown.","Lamellar.",2.5,3.5,"4.2","Metallic,Sub-Metallic","Opaque","red-brown, bronzy-brown, or coppery-red, like untarnished bornite.",[50,51,52],"red","brown","orange","Not fluorescent in UV","None Observed","Irregular\u002FUneven,Sub-Conchoidal","brittle","Red-orange to yellow-grey.","Anisotropic","Strong, reddish orange to reddish brown","(13.9,17.7) 400,\r\n(14.8,18.5) 420,\r\n(15.7,19.3) 440,\r\n(16.9,21.0) 460,\r\n(18.4,23.2) 480,\r\n(20.5,25.5) 500,\r\n(23.2,27.8) 520,\r\n(26.1,29.4) 540,\r\n(28.9,30.6) 560,\r\n(30.6,31.4) 580,\r\n(31.9,31.6) 600,\r\n(32.8,31.9) 620,\r\n(33.5,32.2) 640,\r\n(34.1,32.8) 660,\r\n(34.7,33.2) 680,\r\n(35.2,33.7) 700","A decomposition product of bornite.","Not recorded.","Grandfathered but inadequately described and questionable mineral; name may refer to both impure nukundamite, which was originally called \"idaite\", or to a tetragonal phase close to Sn-poor mawsonite (Rice et al., 1979). Most data here are consistent w...","Named for the type locality, the Ida mine in Namibia.","2025-12-19 20:17:12",[],[],[69],{"id":70,"name":71,"entrytype":9,"csystem":72,"ima_formula":73,"mindat_formula":73,"hmin":43,"hmax":43,"dmeas":37,"dcalc":74,"primary_image_id":75},4354,"Yarrowite","Trigonal","Cu\u003Csub>9\u003C\u002Fsub>S\u003Csub>8\u003C\u002Fsub>","4.89",28479,[],[78],{"id":79,"txt":80,"latitude":11,"longitude":11,"country":81},19001,"Ida Mine, Arandis Constituency, Erongo Region, Namibia","Namibia",159,[84,87,90,94,98,102,105,109,113,117,121,126,130,134],{"id":85,"year":27,"html":86,"doi":11},523140,"Fleischer, M. (1958) New Mineral Names. \u003Ci>American Mineralogist\u003C\u002Fi>,  43 (11-12). 1219-1225 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM43\u002FAM43_1219.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":88,"year":27,"html":89,"doi":11},15959597,"Frenzel, G. (1958) Ein neues Mineral: Idait. Neues Jahrbuch für Mineralogie, Monatshefte, 142-142. Fleischer. M. (1958) New mineral names. American Mineralogist, 43, 1219-1225.",{"id":91,"year":92,"html":93,"doi":11},16112687,1959,"Frenzel, G. (1959) Ein neues Mineral: Idait, natürliches Cu5FeS6. Neues Jahrbuch für Mineralogie, Abhandlungen, 93, 87–114. (in German)",{"id":95,"year":96,"html":97,"doi":11},16112688,1961,"Takeuchi, T., Nambu, M. (1961). On idaite (Cu5FeS6) in Japan. The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists, 45(3), 93-100.",{"id":99,"year":100,"html":101,"doi":11},523896,1963,"Yund, Richard A. (1963) Crystal Data For Synthetic Cu5.5xFexS6.5x (IDAITE). \u003Ci>American Mineralogist\u003C\u002Fi>,  48 (5-6). 672-677 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM48\u002FAM48_672.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":103,"year":100,"html":104,"doi":11},523897,"Frenzel, Gerhard (1963) On crystal data for idaite. \u003Ci>American Mineralogist\u003C\u002Fi>,  48 (5-6) 672-677 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM48\u002FAM48_672.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":106,"year":107,"html":108,"doi":11},526566,1975,"Constantinou, G. (1975) Idaite from the Skouriotissa massive sulfide orebody, Cyprus: Its composition and conditions of formation. \u003Ci>American Mineralogist\u003C\u002Fi>,  60 (11-12) 1013-1018 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM60\u002FAM60_1013.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":110,"year":107,"html":111,"doi":112},230531,"Sugaki, A., Shima, H., Kitakaze, A., Harada, H. (1975) Isothermal phase relations in the system Cu-Fe-S under hydrothermal conditions at 350°C and 300°C. \u003Ci>Economic Geology\u003C\u002Fi>,  70 (4) 806-823 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgsecongeo.70.4.806'>doi:10.2113\u002Fgsecongeo.70.4.806\u003C\u002Fa>","10.2113\u002Fgsecongeo.70.4.806",{"id":114,"year":115,"html":116,"doi":11},16112690,1976,"Wang, N. (1976) Idaite and the synthetic phases Cu4.33Ge0.67S5 and Cu9.67Sn2.33S13. Neues Jahrbuch für Mineralogie, Monatshefte, 6, 241-247.",{"id":118,"year":119,"html":120,"doi":11},16112692,1978,"Weigel, D.A. (1978). Idaite,\" Cu5.5FeS6.5\" and related phases: their physico-chemical features, occurrence and genesis in ore deposits. Doctoral dissertation, Auckland.",{"id":122,"year":123,"html":124,"doi":125},3012,1979,"Rice, C. M., Atkin, D., Bowles, J. F. W., Criddle, A. J. (1979) Nukundamite, a new mineral, and idaite. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  43 (326) 193-200 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1979.043.326.01'>doi:10.1180\u002Fminmag.1979.043.326.01\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_43\u002F43-326-193.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1979.043.326.01",{"id":127,"year":128,"html":129,"doi":11},16112695,1989,"Makundi, I.N. (1989). Moessbauer studies on Idaite (Cu5.5FeS6.5). Tanzania Journal of Science, 15(1), 73-85.",{"id":131,"year":132,"html":133,"doi":11},16112696,1994,"Weigel, Dennis A. (1994). The idaite-nukundamite-bornite-chalcopyrite metastable solid solution--Crystal chemistry, superlattice architecture and bonding; thermochemistry and phase equilibria; natural occurrences, geochemistry and metallogenesis. Geoscience Reports of Shizuoka University, 20, 75-90.",{"id":135,"year":136,"html":137,"doi":11},16964990,2005,"(2005) Idaite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fidaite.pdf' class='refpdflink'>\u003C\u002Fa>",[139,149,159],{"id":140,"source_url":141,"license_code":142,"credit_html":143,"title":144,"description":145,"author":146,"original_width":147,"original_height":148},12103,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130251429","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130251429\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Weissite & Idaite.jpg","Black metallic crystal aggregate of the rare copper telluride weissite associated to also rare minoritary idaite from Winston, Sierra County, New Mexico, United States of America. Ex Vandenbroucke Museum collection from Waregem, Belgium.","David Hospital",761,553,{"id":150,"source_url":151,"license_code":152,"credit_html":153,"title":154,"description":155,"author":156,"original_width":157,"original_height":158},12104,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163481289","CC0 1.0","Darla Sondrol, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163481289\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Chalcopyrite with idaite (GeoDIL number - 1056).jpg","This sample is mostly tarnished yellow chalcopyrite, CuFeS2, but contains minor amounts of browner idaite, Cu5FeS6, as inclusions. Chalcopyrite is a major copper ore mineral. The specimen is 9 cm across.","Darla Sondrol",2314,1914,{"id":160,"source_url":161,"license_code":152,"credit_html":162,"title":163,"description":164,"author":156,"original_width":165,"original_height":166},12105,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163481750","Darla Sondrol, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163481750\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Covellite, idaite and pyrite (GeoDIL number - 1106).jpg","This specimen, 11 cm across, contains primarily (metallic indigo color) covellite (copper sulfide, CuS), (dark coppery brown-black color) idaite (copper iron sulfide, Cu5FeS6), and (gold color) pyrite (iron sulfide, FeS2). Covellite may be bright metallic indigo when fresh, but it quickly tarnishes and darkens when exposed to air. Spectacular samples show irredescence between various shades of violet, blue, yellow and red. In this specimen the covellite is mixed with the dark colored idaite; the two minerals are hard to distinguish from each other. This is a sample of copper ore from the well known mining district at Butte, Montana.",2734,1758,[],[169,170],"Idaiet","Orange bornite",[172,176,180,184,187,191,195],{"lang":173,"names":174},"ca",[175],"idaïta",{"lang":177,"names":178},"de",[179],"Idait",{"lang":181,"names":182},"eu",[183],"Idaita",{"lang":185,"names":186},"it",[7],{"lang":188,"names":189},"nb",[190],"idaitt",{"lang":192,"names":193},"nn",[194],"Idaitt",{"lang":196,"names":197},"uk",[198],"Ідаїт","Q3791761",{"history":11,"applications":11}]