[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:2052":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":19,"key_elements":20,"impurities":21,"cim":22,"ima_status":23,"ima_notes":11,"ima_history":11,"approval_year":25,"publication_year":11,"discovery_year":26,"strunz10ed1":27,"strunz10ed2":28,"strunz10ed3":29,"strunz10ed4":30,"dana8ed1":27,"dana8ed2":31,"dana8ed3":32,"dana8ed4":33,"csystem":34,"cclass":35,"spacegroup":36,"spacegroupset":37,"a":38,"b":37,"c":37,"alpha":37,"beta":37,"gamma":37,"aerror":39,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":11,"csmetamict":13,"commentcrystal":40,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":41,"tlform":42,"hmin":43,"hmax":43,"hardtype":11,"vhnmin":44,"vhnmax":37,"vhnerror":11,"vhng":45,"vhns":11,"commenthard":11,"dmeas":37,"dmeas2":37,"dcalc":46,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":47,"commentluster":11,"diapheny":48,"streak":11,"colour":49,"commentcolor":11,"colors":50,"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":57,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":58,"opticalinternal":11,"opticaltropic":59,"opticalanisotropism":11,"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":69,"type_localities":77,"occurrence_total":84,"citations":85,"images":130,"structures":141,"synonyms":149,"language_names":155,"wikidata_qid":178,"texts":179},2052,"1:1:2052:3","e3e2f0ae-d75d-464e-8599-a77e87d1d758","Isocubanite","Icb",0,"mineral",null,257,false,"CuFe\u003Csub>2\u003C\u002Fsub>S\u003Csub>3\u003C\u002Fsub>",[16,17,18],"Cu","Fe","S",[16,17,18],[16],",Zn,","3.1.28",[24],"APPROVED",1988,"1988","2","C","B","55b","9","13","3","Isometric",32,224,"0","5.303",3,"Z uncertain = 3 or 4. Sawada et al. (1962) give a = 5.295 Å; Fleet (1970) gives a = 5.2949(3) Å.","Fine-grained aggregates to minutely cubo-octahedral.","Euhedral grains",3.5,"175",100,"4.075","Metallic,Sub-Metallic","Opaque","Bronze yellow brown",[51,52],"yellow","brown","Not fluorescent","None Observed","Irregular\u002FUneven","brittle","Non-pleochroic","pinkish brown","Isotropic","(20.9) 400, \r\n(22.7) 420, \r\n(24.6) 440, \r\n(26.9) 460, \r\n(29.2) 480, \r\n(31.4) 500, \r\n(33.2) 520, \r\n(34.8) 540,\r\n(36.2) 560, \r\n(37.4) 580, \r\n(38.2) 600, \r\n(39.1) 620, \r\n(39.7) 640, \r\n(40.3) 660, \r\n(40.9) 680,\r\n(41.3) 700","In oceanic black smokers","National School of Mines, Paris, France","Structurally related to the Sphalerite Group.\r\n\r\nCharacteristic of high-temperature (> 200°C) present-day submarine sulphide deposits. Unstable and therefore unusual in fossil ores.\r\nCan be formed from cubanite by heating the latter to between 200°C an...","Named as the isometric polymorph of cubanite.","2025-08-11 12:14:21",[],[],[],[70],{"id":71,"name":72,"entrytype":9,"csystem":73,"ima_formula":14,"mindat_formula":14,"hmin":43,"hmax":43,"dmeas":74,"dcalc":75,"primary_image_id":76},1168,"Cubanite","Orthorhombic","4.03","4.076",6546,[78],{"id":79,"txt":80,"latitude":81,"longitude":82,"country":83},2526,"EPR 21° N, Juan de Fuca Ridge complex, East Pacific Rise, Pacific Ocean",20.8333,-109.0833,"Pacific Ocean",235,[86,89,94,99,104,108,112,116,120,125],{"id":87,"year":11,"html":88,"doi":11},16113035,"American Mineralogist: 74: 503.",{"id":90,"year":91,"html":92,"doi":93},180262,1966,"YUND, R. A.; KULLERUD, G. (1966) Thermal Stability of Assemblages in the Cu-Fe-S System. \u003Ci>Journal of Petrology\u003C\u002Fi>,  7 (3). 454-488 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1093\u002Fpetrology\u002F7.3.454'>doi:10.1093\u002Fpetrology\u002F7.3.454\u003C\u002Fa>","10.1093\u002Fpetrology\u002F7.3.454",{"id":95,"year":96,"html":97,"doi":98},108073,1970,"Fleet, M. E. (1970) Refinement of the crystal structure of cubanite and polymorphism of CuFe2S3. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  132 (1) 276-287 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1970.132.1-6.276'>doi:10.1524\u002Fzkri.1970.132.1-6.276\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fzk\u002Fvol132\u002FZK132_276.pdf' class='refpdflink'>\u003C\u002Fa>","10.1524\u002Fzkri.1970.132.1-6.276",{"id":100,"year":101,"html":102,"doi":103},230766,1973,"Cabri, Louis J. (1973) New data on Phase Relations in the Cu-Fe-S System. \u003Ci>Economic Geology\u003C\u002Fi>,  68 (4) 443-454 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgsecongeo.68.4.443'>doi:10.2113\u002Fgsecongeo.68.4.443\u003C\u002Fa>","10.2113\u002Fgsecongeo.68.4.443",{"id":105,"year":106,"html":107,"doi":11},17111050,1976,"Dutrizac, J. E. (1976) Reactions in cubanite and chalcopyrite. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  14 (2) 172-181 \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM14_172.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":109,"year":25,"html":110,"doi":111},16485662,"René, Caye, Cervelle, Bernard, Cesbron, Fabien, Oudin, Elisabeth, Picot, Paul, Pillard, François (1988) Isocubanite, a New Definition of the Cubic Polymorph of Cubanite CuFe\u003Csub>2\u003C\u002Fsub>S\u003Csub>3\u003C\u002Fsub>. \u003Ci>Mineralogical Magazine\u003C\u002Fi>, 52 (367) 509-514 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1988.052.367.10'>doi:10.1180\u002Fminmag.1988.052.367.10\u003C\u002Fa>","10.1180\u002Fminmag.1988.052.367.10",{"id":113,"year":114,"html":115,"doi":11},16105214,1994,"Wintenberger, M., Andre, G., Garcin, C., Imbert, P., Jehanno, G., Fouquet, Y., Wafik, A. (1994): Intermediate valency, Verwey transition and magnetic structures of a new mineral, Cu\u003Csub>1-x\u003C\u002Fsub>Fe\u003Csub>3+x\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>, resulting from the ageing of isocubanite. J. Magnetism Magnetic Materials: 132: 31-45; in: Jambor, J.L., Roberts, A.C (1995): New mineral Names. American Mineralogist: 80: 186",{"id":117,"year":118,"html":119,"doi":11},16965045,2005,"(2005) Isocubanite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fisocubanite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":121,"year":122,"html":123,"doi":124},64808,2010,"Chandra, U., Parthasarathy, G., Sharma, P. (2010) Synthetic cubanite CuFe\u003Csub>2\u003C\u002Fsub>S\u003Csub>3\u003C\u002Fsub>: pressure-induced transformation to isocubanite. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  48 (5) 1137-1147 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002Fcanmin.48.5.1137'>doi:10.3749\u002Fcanmin.48.5.1137\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM48_1137.pdf' class='refpdflink'>\u003C\u002Fa>","10.3749\u002Fcanmin.48.5.1137",{"id":126,"year":127,"html":128,"doi":129},19864,2015,"Nenasheva, S. N., Kravchenko, T. A. (2015) Composition features of isocubanite and polymorphous modifications of CuFe\u003Csub>2\u003C\u002Fsub>S\u003Csub>3\u003C\u002Fsub> compound. \u003Ci>Geology of Ore Deposits\u003C\u002Fi>,  57 (7) 626-633 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1134\u002Fs1075701515070090'>doi:10.1134\u002Fs1075701515070090\u003C\u002Fa>","10.1134\u002Fs1075701515070090",[131],{"id":132,"source_url":133,"license_code":134,"credit_html":135,"title":136,"description":137,"author":138,"original_width":139,"original_height":140},5239,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=132295565","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=132295565\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Isocubanite.jpg","Bronze yellowish brown crystal aggregates of the very rare sulphide mineral isocubanite from a big depth in the Pacific Ocean (Guaymas Basin, Pacific Ocean, United States of America) in a completely analyzed specimen by SEM\u002FEDS, associated to golden chalcopyrite and pyrrothite. Ex Vandenbroucke Museum collection from Waregem, Belgium.","David Hospital",606,466,[142],{"id":143,"url":144,"label":145,"formula":146,"spacegroup":147,"year":148},6712,"\u002Fcif\u002F6712.cif","Szymanski 1974","Cu.333 Fe.667 S","F -4 3 m",1974,[150,151,152,153,154],"Cubanite II","Cubic cubanite","IMA1983-E","Isochalcopyrite","Isocubaniet",[156,160,167,171,174],{"lang":157,"names":158},"ca",[159],"isocubanita",{"lang":161,"names":162},"de",[163,164,165,166],"Chalkopyrrhotin","Cubanit II","Isochalkopyrit","Isocubanit",{"lang":168,"names":169},"es",[170],"Isocubanita",{"lang":172,"names":173},"eu",[170],{"lang":175,"names":176},"it",[177,7],"Isocalcopirite","Q425798",{"history":11,"applications":11}]