[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:3730":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":14,"elements":16,"sigelements":19,"key_elements":20,"impurities":21,"cim":22,"ima_status":23,"ima_notes":11,"ima_history":11,"approval_year":25,"publication_year":26,"discovery_year":11,"strunz10ed1":27,"strunz10ed2":28,"strunz10ed3":29,"strunz10ed4":30,"dana8ed1":27,"dana8ed2":31,"dana8ed3":32,"dana8ed4":32,"csystem":33,"cclass":34,"spacegroup":11,"spacegroupset":35,"a":36,"b":35,"c":37,"alpha":35,"beta":35,"gamma":35,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":38,"csmetamict":13,"commentcrystal":39,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":11,"hmin":40,"hmax":41,"hardtype":11,"vhnmin":42,"vhnmax":43,"vhnerror":11,"vhng":44,"vhns":11,"commenthard":11,"dmeas":11,"dmeas2":35,"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":51,"cleavage":11,"cleavagetype":11,"fracturetype":11,"tenacity":52,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":35,"opticalalpha2":35,"opticalalphaerror":11,"opticalbeta":35,"opticalbeta2":35,"opticalbetaerror":11,"opticalgamma":35,"opticalgamma2":35,"opticalgammaerror":11,"opticalomega":35,"opticalomega2":35,"opticalomegaerror":11,"opticalepsilon":35,"opticalepsilon2":35,"opticalepsilonerror":11,"opticaln":35,"opticaln2":35,"opticalnerror":11,"optical2vcalc":35,"optical2vcalc2":35,"optical2vcalcerror":11,"optical2vmeasured":35,"optical2vmeasured2":35,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":53,"opticalcolour":11,"opticalinternal":11,"opticaltropic":54,"opticalanisotropism":55,"opticalbireflectance":11,"opticalextinction":11,"opticalr":56,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":57,"otheroccurrence":11,"type_specimen_store":58,"description_short":59,"aboutname":60,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":61,"reviewed_at":11,"variety_of":11,"varieties":62,"group_members":63,"associates":64,"confused_with":74,"type_localities":75,"occurrence_total":82,"citations":83,"images":108,"structures":109,"synonyms":110,"language_names":113,"wikidata_qid":130,"texts":131},3730,"1:1:3730:9","d8d3fa54-a859-4c49-b87b-b8910a5a8299","Spionkopite","Spi",0,"mineral",null,205,false,"Cu\u003Csub>39\u003C\u002Fsub>S\u003Csub>28\u003C\u002Fsub>","\"Extended\" formula is Cu\u003Csup>+\u003C\u002Fsup>\u003Csub>15\u003C\u002Fsub>Cu\u003Csup>2+\u003C\u002Fsup>\u003Csub>4.5\u003C\u002Fsub>(S\u003Csub>2\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>S\u003Csub>10\u003C\u002Fsub> (Goble, 1985).\r\n",[17,18],"Cu","S",[17,18],[17],",Fe,Zn,","3.1.6",[24],"APPROVED",1978,1980,"2","C","A","05c","4","7","Hexagonal",19,"0","22.962","41.429",18,"Possible space group is \u003Ci>P\u003C\u002Fi>-3\u003Ci>m\u003C\u002Fi>1.",2.5,3,"63","93",15,"5.13","Metallic","Opaque","Blue",[50],"blue","Not fluorescent in UV","brittle","Distinguished from yarrowite because yarrowite is a darker shade of blue and is more strongly bireflectant and anisotropic.","Anisotropic","Orange","(26.1,33.4,13.1,19.9) 400,\r\n(25.8,32.9,12.5,19.3) 420,\r\n(25.1,32.3,11.7,18.6) 440,\r\n(24.2,31.45,10.6,17.4) 460,\r\n(23.6,31.0,10.0,16.8) 470,\r\n(23.0,30.5,9.46,16.2) 480,\r\n(21.8,29.5,8.32,15.1) 500,\r\n(20.5,28.5,7.38,14.1) 520,\r\n(19.0,27.4,6.39,13.0) 540,\r\n(18.6,27.1,6.10,12.3) 546,\r\n(17.6,26.4,5.49,12.1) 560,\r\n(16.3,25.4,4.64,11.3) 580,\r\n(15.6,24.9,4.27,10.9) 589,\r\n(14.9,24.45,3.86,10.6) 600,\r\n(13.6,23.8,3.21,10.1) 620,\r\n(12.4,23.8,2.63,10.2) 640,\r\n(11.8,24.05,2.37,10.3) 650,\r\n(11.2,24.3,2.12,10.6) 660,\r\n(10.0,24.55,1.75,10.7) 680,\r\n(9.06,24.3,1.55,10.5) 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\nHarvard University, Cambridge, Massachusetts, USA, 122290. National Museum of Natural History, Washington, D.C., USA, 149430, 149431.","See also the closely related yarrowite.\r\nA typical intergrowth of yarrowite and spionkopite is called Blaubleibender Covellite.\r\n\r\nCompare UM1976-15-S:CuSe.","Named after its discovery locality, the Spionkop Creek valley, Alberta, Canada.","2025-08-11 12:14:23",[],[],[65],{"id":66,"name":67,"entrytype":9,"csystem":68,"ima_formula":69,"mindat_formula":69,"hmin":70,"hmax":71,"dmeas":35,"dcalc":72,"primary_image_id":73},1666,"Geerite","Trigonal","Cu\u003Csub>8\u003C\u002Fsub>S\u003Csub>5\u003C\u002Fsub>",3.5,4,"5.61",9714,[],[76],{"id":77,"txt":78,"latitude":79,"longitude":80,"country":81},19046,"Spionkop Creek, Yarrow Creek-Spionkop Creek deposit, Pincher Creek, Alberta, Canada",49.234475,-114.0508861,"Canada",92,[84,87,91,95,99,104],{"id":85,"year":26,"html":86,"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":88,"year":89,"html":90,"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":92,"year":93,"html":94,"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":96,"year":97,"html":98,"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":100,"year":101,"html":102,"doi":103},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":105,"year":106,"html":107,"doi":11},16967403,2005,"(2005) Spionkopite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fspionkopite.pdf' class='refpdflink'>\u003C\u002Fa>",[],[],[111,112],"IMA1978-023","Spionkopiet",[114,118,123,127],{"lang":115,"names":116},"ca",[117],"spionkopita",{"lang":119,"names":120},"de",[121,122],"IMA 1978-023","Spionkopit",{"lang":124,"names":125},"eu",[126],"Spionkopita",{"lang":128,"names":129},"it",[7],"Q1111766",{"history":11,"applications":11}]