[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:236":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":14,"elements":15,"sigelements":18,"key_elements":19,"impurities":11,"cim":20,"ima_status":21,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":23,"discovery_year":24,"strunz10ed1":25,"strunz10ed2":26,"strunz10ed3":27,"strunz10ed4":28,"dana8ed1":25,"dana8ed2":29,"dana8ed3":30,"dana8ed4":31,"csystem":32,"cclass":33,"spacegroup":34,"spacegroupset":35,"a":36,"b":37,"c":38,"alpha":35,"beta":35,"gamma":35,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":39,"csmetamict":13,"commentcrystal":11,"twinning":40,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":41,"tlform":42,"hmin":43,"hmax":43,"hardtype":11,"vhnmin":35,"vhnmax":35,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":35,"dmeas2":35,"dcalc":44,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":45,"lustretype":45,"commentluster":11,"diapheny":46,"streak":47,"colour":48,"commentcolor":11,"colors":49,"streak_colors":52,"luminescence":11,"uv":53,"cleavage":11,"cleavagetype":54,"fracturetype":55,"tenacity":56,"commentbreak":57,"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":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":11,"otheroccurrence":58,"type_specimen_store":59,"description_short":60,"aboutname":61,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":62,"reviewed_at":11,"variety_of":11,"varieties":63,"group_members":64,"associates":65,"confused_with":107,"type_localities":108,"occurrence_total":115,"citations":116,"images":166,"structures":184,"synonyms":191,"language_names":196,"wikidata_qid":221,"texts":222},236,"1:1:236:9","9e0e3e15-cb88-4a57-9ff4-672bcb08c2d9","Anilite","Ani",0,"mineral",null,489,false,"Cu\u003Csub>7\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>",[16,17],"Cu","S",[16,17],[16],"3.1.4",[22],"APPROVED",1969,"1969","2","B","A","10","4","7","5","Orthorhombic",8,71,"0","7.89","7.84","11.01",4,"Present; \"neighboring twins\".","Prismatic or platy crystals to 5mm. Anilite cannot be identified using a powdered sample. Grinding transforms anilite to digenite (Morimoto, et. al., 1969).","Prismatic or platy crystals to 5 mm",3,"5.68","Metallic","Opaque","Black","Bluish-Grey",[50,51],"gray","black",[51],"Not fluorescent in UV","None Observed","None observed","sectile","Brittle","Hydrothermal copper ores.","Sakurai Museum, Tokyo, Japan","All specimens studied by the authors of the original description contained some djurleite.\r\n\r\nNote: Many of the reported associations of digenite and djurleite, identified by powder diffraction, could be anilite and djurleite, as anilite transforms to ...","For the type locality, Ani Mine, Japan.","2025-11-26 18:42:28",[],[],[66,73,82,92,100],{"id":67,"name":68,"entrytype":9,"csystem":32,"ima_formula":69,"mindat_formula":69,"hmin":43,"hmax":43,"dmeas":70,"dcalc":71,"primary_image_id":72},727,"Bornite","Cu\u003Csub>5\u003C\u002Fsub>FeS\u003Csub>4\u003C\u002Fsub>","5.06","5.09",3648,{"id":74,"name":75,"entrytype":9,"csystem":76,"ima_formula":77,"mindat_formula":77,"hmin":78,"hmax":39,"dmeas":79,"dcalc":80,"primary_image_id":81},955,"Chalcopyrite","Tetragonal","CuFeS\u003Csub>2\u003C\u002Fsub>",3.5,"4.1","4.18",29425,{"id":83,"name":84,"entrytype":9,"csystem":85,"ima_formula":86,"mindat_formula":86,"hmin":87,"hmax":88,"dmeas":89,"dcalc":90,"primary_image_id":91},1144,"Covellite","Hexagonal","CuS",1.5,2,"4.6","4.602",29544,{"id":93,"name":94,"entrytype":9,"csystem":95,"ima_formula":96,"mindat_formula":96,"hmin":97,"hmax":43,"dmeas":35,"dcalc":98,"primary_image_id":99},1300,"Djurleite","Monoclinic","Cu\u003Csub>31\u003C\u002Fsub>S\u003Csub>16\u003C\u002Fsub>",2.5,"5.749",7291,{"id":101,"name":102,"entrytype":9,"csystem":103,"ima_formula":104,"mindat_formula":104,"hmin":97,"hmax":97,"dmeas":35,"dcalc":105,"primary_image_id":106},4354,"Yarrowite","Trigonal","Cu\u003Csub>9\u003C\u002Fsub>S\u003Csub>8\u003C\u002Fsub>","4.89",28479,[],[109],{"id":110,"txt":111,"latitude":112,"longitude":113,"country":114},2175,"Ani Mine, Ani-machi, Kitaakita City, Akita Prefecture, Japan",39.9818103,140.4165222,"Japan",116,[117,120,124,128,132,137,141,145,149,153,157,162],{"id":118,"year":23,"html":119,"doi":11},525239,"Morimoto, Nobuo, Koto, Kichiro, Shimazaki, Yoshihiko (1969) Anilite, Cu7S4, a new mineral. \u003Ci>American Mineralogist\u003C\u002Fi>,  54 (9-10) 1256-1268 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM54\u002FAM54_1256.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":121,"year":122,"html":123,"doi":11},525308,1970,"Morimoto, Nobuo, Koto, Kichiro (1970) Phase relations of the Cu-S system at low temperatures: stability of anilite. \u003Ci>American Mineralogist\u003C\u002Fi>,  55 (1-2) 106-117 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM55\u002FAM55_106.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":125,"year":122,"html":126,"doi":127},217056,"Koto, K., Morimoto, N. (1970) The crystal structure of anilite. \u003Ci>Acta Crystallographica Section B Structural Crystallography and Crystal Chemistry\u003C\u002Fi>,  26 (7) 915-924 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs0567740870003370'>doi:10.1107\u002Fs0567740870003370\u003C\u002Fa>","10.1107\u002Fs0567740870003370",{"id":129,"year":130,"html":131,"doi":11},16100681,1973,"Goble, R.J., Smith, D.G.W. (1973) Electron microprobe investigation of copper sulphides in the Precambrian Lewis Series of S.W. Alberta, Canada. The Canadian Mineralogist: 12: 95-103. https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM12_95.pdf",{"id":133,"year":134,"html":135,"doi":136},230210,1977,"Potter II, R. W. (1977) An electrochemical investigation of the system copper-sulfur. \u003Ci>Economic Geology\u003C\u002Fi>,  72 (8). 1524-1542 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgsecongeo.72.8.1524'>doi:10.2113\u002Fgsecongeo.72.8.1524\u003C\u002Fa>","10.2113\u002Fgsecongeo.72.8.1524",{"id":138,"year":139,"html":140,"doi":11},16208113,1979,"Kucha, H. (1979) Anilite, Cu7S4 from Lubin mine, Lower Silesia, Poland. Mineralogia Polonica, 10 (2), 89-93.",{"id":142,"year":143,"html":144,"doi":11},527442,1980,"Gronvold, Fredrik, Westrum, Edgar F. (1980) The anilite\u002Flow-digenite transition. \u003Ci>American Mineralogist\u003C\u002Fi>,  65 (5-6) 574-575 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM65\u002FAM65_574.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":146,"year":147,"html":148,"doi":11},16100683,1981,"Goble, R.J. (1981) The leaching of copper from anilite and the production of a metastable copper sulfide structure. The Canadian Mineralogist: 19: 583-591. https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM19_583.pdf",{"id":150,"year":151,"html":152,"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":154,"year":155,"html":156,"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":158,"year":159,"html":160,"doi":161},14277337,1998,"Schmidt, JA, Sagua, A.E, Lescano, G (1998) Electrochemical investigation of the equilibria (covellite + anilite) and (covellite + digenite) \u003Ci>The Journal of Chemical Thermodynamics\u003C\u002Fi>, 30 (3) 283-290 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1006\u002Fjcht.1997.0287'>doi:10.1006\u002Fjcht.1997.0287\u003C\u002Fa>","10.1006\u002Fjcht.1997.0287",{"id":163,"year":164,"html":165,"doi":11},16962898,2005,"(2005) Anilite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fanilite.pdf' class='refpdflink'>\u003C\u002Fa>",[167,177],{"id":168,"source_url":169,"license_code":170,"credit_html":171,"title":172,"description":173,"author":174,"original_width":175,"original_height":176},1446,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10149695","CC BY-SA 3.0","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10149695\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anilite-170088.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnilite\" class=\"extiw\" title=\"en:Anilite\">Anilite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Tilva Mika deposit, Bor Mine, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBor\" class=\"extiw\" title=\"en:Bor\">Bor\u003C\u002Fa>, Bor-Majdanpek District, Serbia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-3047.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 5.6 x 2.8 x 2.4 cm.\u003C\u002Fdd>\n\u003Cdd>Extremely rare, this is a copper sulfide seldom found in such richness. It is absolutely outstanding for the species. These are 3-dimensional crystals, partially embedded in the matrix, showing an iridescent color range and demonstrating clear crystal form. Size is to 7-8 mm. Ex. Gunnar Farber Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",800,547,{"id":178,"source_url":179,"license_code":170,"credit_html":180,"title":181,"description":173,"author":174,"original_width":182,"original_height":183},1447,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10149697","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10149697\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anilite-170089.jpg",400,333,[185],{"id":186,"url":187,"label":188,"formula":189,"spacegroup":190,"year":122},613,"\u002Fcif\u002F613.cif","Koto 1970","Cu7 S4","P n m a",[192,193,194,195],"Aniliet","Anilit","Anilitt","IMA1968-030",[197,201,205,209,213,217],{"lang":198,"names":199},"ca",[200],"anilita",{"lang":202,"names":203},"de",[193,204],"Anilith",{"lang":206,"names":207},"eu",[208],"Anilita",{"lang":210,"names":211},"it",[212],"anilite",{"lang":214,"names":215},"ja",[216],"阿仁鉱",{"lang":218,"names":219},"ta",[220],"அனிலைட்டு","Q3617482",{"history":11,"applications":11}]