[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:4354":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":15,"elements":17,"sigelements":20,"key_elements":21,"impurities":22,"cim":23,"ima_status":24,"ima_notes":11,"ima_history":11,"approval_year":26,"publication_year":27,"discovery_year":11,"strunz10ed1":28,"strunz10ed2":29,"strunz10ed3":30,"strunz10ed4":31,"dana8ed1":28,"dana8ed2":32,"dana8ed3":33,"dana8ed4":34,"csystem":35,"cclass":36,"spacegroup":37,"spacegroupset":38,"a":39,"b":38,"c":40,"alpha":38,"beta":38,"gamma":38,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":41,"csmetamict":14,"commentcrystal":42,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":11,"hmin":43,"hmax":43,"hardtype":11,"vhnmin":44,"vhnmax":45,"vhnerror":11,"vhng":46,"vhns":11,"commenthard":11,"dmeas":38,"dmeas2":38,"dcalc":47,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":48,"lustretype":48,"commentluster":11,"diapheny":49,"streak":11,"colour":50,"commentcolor":11,"colors":51,"streak_colors":11,"luminescence":11,"uv":11,"cleavage":55,"cleavagetype":56,"fracturetype":11,"tenacity":57,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":38,"opticalalpha2":38,"opticalalphaerror":11,"opticalbeta":38,"opticalbeta2":38,"opticalbetaerror":11,"opticalgamma":38,"opticalgamma2":38,"opticalgammaerror":11,"opticalomega":38,"opticalomega2":38,"opticalomegaerror":11,"opticalepsilon":38,"opticalepsilon2":38,"opticalepsilonerror":11,"opticaln":38,"opticaln2":38,"opticalnerror":11,"optical2vcalc":38,"optical2vcalc2":38,"optical2vcalcerror":11,"optical2vmeasured":38,"optical2vmeasured2":38,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":58,"opticalpleochorismdesc":59,"opticalbirefringence":11,"opticalcomments":60,"opticalcolour":61,"opticalinternal":11,"opticaltropic":62,"opticalanisotropism":63,"opticalbireflectance":11,"opticalextinction":11,"opticalr":64,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":65,"otheroccurrence":11,"type_specimen_store":66,"description_short":67,"aboutname":68,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":69,"reviewed_at":11,"variety_of":11,"varieties":70,"group_members":71,"associates":100,"confused_with":151,"type_localities":152,"occurrence_total":159,"citations":160,"images":185,"structures":196,"synonyms":197,"language_names":200,"wikidata_qid":224,"texts":225},4354,"1:1:4354:6","e1c2b243-2d28-49b7-839d-b5172f846db4","Yarrowite","Yar",0,"mineral",null,33145,272,false,"Cu\u003Csub>9\u003C\u002Fsub>S\u003Csub>8\u003C\u002Fsub>","\"Extended\" formula is Cu\u003Csup>+\u003C\u002Fsup>\u003Csub>20\u003C\u002Fsub>Cu\u003Csup>2+\u003C\u002Fsup>\u003Csub>7\u003C\u002Fsub>(S\u003Csub>2\u003C\u002Fsub>)\u003Csub>7\u003C\u002Fsub>S\u003Csub>10\u003C\u002Fsub> (Goble, 1985).",[18,19],"Cu","S",[18,19],[18],",Fe,Ag,","3.1.12",[25],"APPROVED",1978,1980,"2","C","A","05d","7","3","1","Trigonal",13,97,"0","3.800","67.264",3,"Also P3m1 and P321",2.5,"93","98",15,"4.89","Metallic","Opaque","Bluish-grey, black",[52,53,54],"gray","black","blue","{0001}","None Observed","brittle","Visible","Blue to bluish white.","Distinguished from spionkopite because yarrowite is a darker shade of blue and is more strongly bireflectant and anisotropic.","Blue with a slight violet tint in oil.","Anisotropic","Strong, orange-red.","(19.2,32.9,7.22,19.2) 400,\r\n(18.6,32.3,7.06,18.6) 420,\r\n(17.9,31.4,6.49,17.6) 440,\r\n(16.9,30.5,5.63,16.3) 460,\r\n(16.3,30.0,5.14,15.7) 470,\r\n(15.6,29.5,4.66,14.95) 480,\r\n(14.2,28.2,3.71,13.7) 500,\r\n(12.4,27.0,2.79,12.5) 520,\r\n(10.7,25.6,2.02,11.4) 540,\r\n(10.2,25.3,1.83,11.1) 546,\r\n(9.08,24.3,1.42,10.4) 560,\r\n(7.51,23.1,1.05,9.38) 580,\r\n(6.89,22.8,1.00,9.09) 589,\r\n(6.15,22.2,1.00,8.82) 600,\r\n(5.02,22.2,1.28,8.99) 620,\r\n(4.33,23.0,2.21,9.65) 640,\r\n(4.2,23.3,2.93,9.96) 650,\r\n(4.38,23.6,3.91,10.1) 660,\r\n(5.96,23.4,7.11,9.92) 680,\r\n(9.44,22.95,11.6,9.57) 700","Selective replacement of small (~0.5 mm diameter) spheroidal quartz aggregates, feldspar grains, fractured quartz grains and carbonate cement within sandstones and quartzites of a redbed formation, a marginal continental, shallow water sequence.","Canadian Geological Survey, Ottawa, Canada.\r\nQueen’s University, Kingston, Ontario, Canada.\r\nNational Museum of Natural History, Washington, D.C., USA, 149430, 149431.\r\nHarvard University, Cambridge, Massachusetts, USA, 122290.","Chalcocite-Yarrowite Series.\r\n\r\nStoichiometrically similar to the covellite (CuS).\r\nSee also the closely related spionkopite. Often forms mixtures with anilite, covellite, digenite, djurleite, and\u002For spionkopite.\r\nA typical intergrowth of yarrowite and...","Named in 1980 by R. J. Goble after its discovery locality, Yarrow Creek valley, Alberta, Canada.","2025-08-11 12:14:25",[],[72,80,88,94],{"id":73,"name":74,"entrytype":9,"csystem":75,"ima_formula":76,"mindat_formula":76,"hmin":43,"hmax":41,"dmeas":77,"dcalc":78,"primary_image_id":79},962,"Chalcocite","Monoclinic","Cu\u003Csub>2\u003C\u002Fsub>S","5.5","5.8",5161,{"id":81,"name":82,"entrytype":9,"csystem":35,"ima_formula":83,"mindat_formula":84,"hmin":43,"hmax":41,"dmeas":85,"dcalc":86,"primary_image_id":87},1291,"Digenite","Cu\u003Csub>1.8\u003C\u002Fsub>S","Cu\u003Csub>9\u003C\u002Fsub>S\u003Csub>5\u003C\u002Fsub>","5.546","5.706",7221,{"id":89,"name":90,"entrytype":9,"csystem":75,"ima_formula":91,"mindat_formula":91,"hmin":43,"hmax":41,"dmeas":38,"dcalc":92,"primary_image_id":93},1300,"Djurleite","Cu\u003Csub>31\u003C\u002Fsub>S\u003Csub>16\u003C\u002Fsub>","5.749",7291,{"id":95,"name":96,"entrytype":9,"csystem":97,"ima_formula":84,"mindat_formula":98,"hmin":43,"hmax":41,"dmeas":38,"dcalc":38,"primary_image_id":99},3468,"Roxbyite","Triclinic","Cu\u003Csub>58\u003C\u002Fsub>S\u003Csub>32\u003C\u002Fsub>",21236,[101,108,115,125,135,136,137,144],{"id":102,"name":103,"entrytype":9,"csystem":104,"ima_formula":105,"mindat_formula":105,"hmin":41,"hmax":41,"dmeas":38,"dcalc":106,"primary_image_id":107},236,"Anilite","Orthorhombic","Cu\u003Csub>7\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","5.68",1446,{"id":109,"name":110,"entrytype":9,"csystem":104,"ima_formula":111,"mindat_formula":111,"hmin":41,"hmax":41,"dmeas":112,"dcalc":113,"primary_image_id":114},727,"Bornite","Cu\u003Csub>5\u003C\u002Fsub>FeS\u003Csub>4\u003C\u002Fsub>","5.06","5.09",3648,{"id":116,"name":117,"entrytype":9,"csystem":118,"ima_formula":119,"mindat_formula":119,"hmin":120,"hmax":121,"dmeas":122,"dcalc":123,"primary_image_id":124},955,"Chalcopyrite","Tetragonal","CuFeS\u003Csub>2\u003C\u002Fsub>",3.5,4,"4.1","4.18",29425,{"id":126,"name":127,"entrytype":9,"csystem":128,"ima_formula":129,"mindat_formula":129,"hmin":130,"hmax":131,"dmeas":132,"dcalc":133,"primary_image_id":134},1144,"Covellite","Hexagonal","CuS",1.5,2,"4.6","4.602",29544,{"id":81,"name":82,"entrytype":9,"csystem":35,"ima_formula":83,"mindat_formula":84,"hmin":43,"hmax":41,"dmeas":85,"dcalc":86,"primary_image_id":87},{"id":89,"name":90,"entrytype":9,"csystem":75,"ima_formula":91,"mindat_formula":91,"hmin":43,"hmax":41,"dmeas":38,"dcalc":92,"primary_image_id":93},{"id":138,"name":139,"entrytype":9,"csystem":128,"ima_formula":140,"mindat_formula":141,"hmin":43,"hmax":120,"dmeas":38,"dcalc":142,"primary_image_id":143},2002,"Idaite","Cu\u003Csub>3\u003C\u002Fsub>FeS\u003Csub>4\u003C\u002Fsub>","Cu\u003Csub>5\u003C\u002Fsub>FeS\u003Csub>6\u003C\u002Fsub>","4.2",12103,{"id":145,"name":146,"entrytype":9,"csystem":104,"ima_formula":147,"mindat_formula":147,"hmin":131,"hmax":41,"dmeas":148,"dcalc":149,"primary_image_id":150},4300,"Wittichenite","Cu\u003Csub>3\u003C\u002Fsub>BiS\u003Csub>3\u003C\u002Fsub>","6.3","6.23",28148,[],[153],{"id":154,"txt":155,"latitude":156,"longitude":157,"country":158},4371,"Yarrow Creek, Yarrow Creek-Spionkop Creek deposit, Pincher Creek, Alberta, Canada",49.2666667,-113.8666667,"Canada",89,[161,164,168,172,176,181],{"id":162,"year":27,"html":163,"doi":11},15959628,"Goble, R.J. (1980) Copper sulfides from Alberta: Yarrowite Cu9S8 and Spionkopite Cu39S28. The Canadian Mineralogist, 18, 511-518. https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM18_511.pdf",{"id":165,"year":166,"html":167,"doi":11},527706,1981,"Fleischer, Michael, Cabri, Louis J. (1981) New Mineral Names. \u003Ci>American Mineralogist\u003C\u002Fi>,  66 (11-12) 1274-1280 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM66\u002FAM66_1274.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":169,"year":170,"html":171,"doi":11},16100684,1985,"Goble, R.J. (1985) The relationship between crystal structure, bonding and cell dimensions in the copper sulfides. The Canadian Mineralogist: 23: 61-76. https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM23_61.pdf",{"id":173,"year":174,"html":175,"doi":11},16100685,1986,"Whiteside, L.S., Goble, R.J. (1986) Structural and compositional changes in copper sulfides during leaching and dissolution. The Canadian Mineralogist: 24: 247-258. https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM24_247.pdf",{"id":177,"year":178,"html":179,"doi":180},1126563,1993,"Criddle, A. J., Stanley, C. J. (1993) Data file. In \u003Ci>Quantitative Data File for Ore Minerals\u003C\u002Fi>. Springer Netherlands. p.1-635. \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002F978-94-011-1486-8_1'>doi:10.1007\u002F978-94-011-1486-8_1\u003C\u002Fa>","10.1007\u002F978-94-011-1486-8_1",{"id":182,"year":183,"html":184,"doi":11},16968205,2005,"(2005) Yarrowite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fyarrowite.pdf' class='refpdflink'>\u003C\u002Fa>",[186],{"id":187,"source_url":188,"license_code":189,"credit_html":190,"title":191,"description":192,"author":193,"original_width":194,"original_height":195},28479,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=106138814","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=106138814\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Yarrowite.jpg","Black microcrystals of the very rare copper sulphide yarrowite from New Mexico (High Rolls District, Otero County, New Mexico, United States of America). Ex Vandenbroucke Museum collection from Waregem, Belgium.","David Hospital",603,600,[],[198,199],"IMA1978-022","Yarrowiet",[201,205,210,214,217,220],{"lang":202,"names":203},"ca",[204],"yarrowita",{"lang":206,"names":207},"de",[208,209],"IMA 1978-022","Yarrowit",{"lang":211,"names":212},"es",[213],"Yarrowita",{"lang":215,"names":216},"eu",[213],{"lang":218,"names":219},"it",[7],{"lang":221,"names":222},"ru",[223],"Ярровит","Q1796630",{"history":11,"applications":11}]