[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:3258":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":11,"ima_formula":15,"elements":16,"sigelements":19,"key_elements":20,"impurities":21,"cim":22,"ima_status":23,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":26,"discovery_year":27,"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":38,"alpha":38,"beta":38,"gamma":38,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":40,"csmetamict":14,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":11,"hmin":41,"hmax":42,"hardtype":11,"vhnmin":38,"vhnmax":38,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":38,"dmeas2":38,"dcalc":38,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":43,"lustretype":43,"commentluster":11,"diapheny":11,"streak":44,"colour":45,"commentcolor":11,"colors":46,"streak_colors":50,"luminescence":11,"uv":11,"cleavage":51,"cleavagetype":11,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":52,"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":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":53,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":11,"otheroccurrence":11,"type_specimen_store":11,"description_short":54,"aboutname":55,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":56,"reviewed_at":11,"variety_of":11,"varieties":57,"group_members":58,"associates":138,"confused_with":139,"type_localities":140,"occurrence_total":147,"citations":148,"images":203,"structures":280,"synonyms":287,"language_names":293,"wikidata_qid":331,"texts":332},3258,"1:1:3258:8","1065d28e-274c-469b-ad50-7ec4095b2e41","Polydymite","Pld",0,"mineral",null,52935,1012,false,"Ni\u003Csup>2+\u003C\u002Fsup>Ni\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>",[17,18],"Ni","S",[17,18],[17],",Fe,Co,","3.11.4",[24,25],"APPROVED","GRANDFATHERED",1876,"1876","2","D","A","05","10","1","7","Isometric",32,222,"0","9.405",8,4.5,5.5,"Metallic","Black gray","Violet gray, copper red, light gray, or steel gray",[47,48,49],"gray","red","black",[49,47],"Indistinct","Isotropic","(44.3) 400,\r\n(45.3) 440,\r\n(46.0) 480,\r\n(46.2) 520,\r\n(45.8) 560,\r\n(46.2) 600,\r\n(48.0) 640,\r\n(51.2) 680,\r\n(53.0) 700","Linnaeite Group, and the Thiospinel Group. Linnaeite-Polydymite Series.\r\n\r\nCompare siegenite, violarite.","From the Greek πολνς, many, and διδνμος, twin, because it was observed in twinned forms.","2026-03-25 16:08:38",[],[59,64,72,80,88,93,99,104,109,114,121,127,134],{"id":60,"name":61,"entrytype":9,"csystem":35,"ima_formula":62,"mindat_formula":62,"hmin":11,"hmax":11,"dmeas":38,"dcalc":38,"primary_image_id":63},27212,"Cadmoindite","CdIn\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>",4287,{"id":65,"name":66,"entrytype":9,"csystem":35,"ima_formula":67,"mindat_formula":68,"hmin":69,"hmax":42,"dmeas":38,"dcalc":70,"primary_image_id":71},1188,"Cuprorhodsite","FeRh\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","(Cu\u003Csup>1+\u003C\u002Fsup>\u003Csub>0.5\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>0.5\u003C\u002Fsub>)Rh\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>",5,"5.88",6647,{"id":73,"name":74,"entrytype":9,"csystem":35,"ima_formula":75,"mindat_formula":76,"hmin":41,"hmax":69,"dmeas":77,"dcalc":78,"primary_image_id":79},1230,"Daubréelite","FeCr\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","Fe\u003Csup>2+\u003C\u002Fsup>Cr\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","3.81","3.842",6869,{"id":81,"name":82,"entrytype":9,"csystem":35,"ima_formula":83,"mindat_formula":83,"hmin":84,"hmax":41,"dmeas":85,"dcalc":86,"primary_image_id":87},1747,"Greigite","Fe\u003Csup>2+\u003C\u002Fsup>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>",4,"4.049","4.079",10455,{"id":89,"name":90,"entrytype":9,"csystem":35,"ima_formula":91,"mindat_formula":91,"hmin":41,"hmax":42,"dmeas":11,"dcalc":92,"primary_image_id":11},55244,"Grimmite","NiCo\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","4.96",{"id":94,"name":95,"entrytype":9,"csystem":35,"ima_formula":96,"mindat_formula":96,"hmin":69,"hmax":69,"dmeas":38,"dcalc":97,"primary_image_id":98},2029,"Indite","FeIn\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","4.67",7557,{"id":100,"name":101,"entrytype":9,"csystem":35,"ima_formula":102,"mindat_formula":102,"hmin":11,"hmax":11,"dmeas":11,"dcalc":103,"primary_image_id":11},46804,"Joegoldsteinite","MnCr\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","3.71",{"id":105,"name":106,"entrytype":9,"csystem":35,"ima_formula":107,"mindat_formula":107,"hmin":69,"hmax":69,"dmeas":38,"dcalc":108,"primary_image_id":11},2138,"Kalininite","ZnCr\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","4.045",{"id":110,"name":111,"entrytype":9,"csystem":35,"ima_formula":112,"mindat_formula":112,"hmin":41,"hmax":42,"dmeas":38,"dcalc":38,"primary_image_id":113},2409,"Linnaeite","Co\u003Csup>2+\u003C\u002Fsup>Co\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>",64620,{"id":115,"name":116,"entrytype":9,"csystem":35,"ima_formula":117,"mindat_formula":117,"hmin":41,"hmax":42,"dmeas":118,"dcalc":119,"primary_image_id":120},3655,"Siegenite","CoNi\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","4.5","4.83",22298,{"id":122,"name":123,"entrytype":9,"csystem":35,"ima_formula":124,"mindat_formula":124,"hmin":42,"hmax":125,"dmeas":38,"dcalc":126,"primary_image_id":11},25693,"Tarkianite","(Cu,Fe)(Re,Mo)\u003Csub>4\u003C\u002Fsub>S\u003Csub>8\u003C\u002Fsub>",6,"7.30",{"id":128,"name":129,"entrytype":9,"csystem":35,"ima_formula":130,"mindat_formula":131,"hmin":41,"hmax":42,"dmeas":38,"dcalc":132,"primary_image_id":133},4187,"Violarite","FeNi\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","Fe\u003Csup>2+\u003C\u002Fsup>Ni\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","4.79",27499,{"id":135,"name":136,"entrytype":9,"csystem":35,"ima_formula":11,"mindat_formula":137,"hmin":125,"hmax":125,"dmeas":38,"dcalc":38,"primary_image_id":11},4339,"Xingzhongite","Pb\u003Csup>2+\u003C\u002Fsup>Ir\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>",[],[],[141],{"id":142,"txt":143,"latitude":144,"longitude":145,"country":146},15123,"Grüneau Mine (Grüne Au Mine; Grünau Mine), Schutzbach, Daaden-Herdorf, Altenkirchen, Rhineland-Palatinate, Germany",50.7535904,7.898376,"Germany",154,[149,152,156,160,164,168,173,178,182,186,190,194,199],{"id":150,"year":26,"html":151,"doi":11},16120497,"Laspeyres, H. (1876) Chemische Untersuchungen von Nickelerzen; 1. Polydymit, ein neues Nickelerz. Journal für Praktische Chemie: 122: 397-413.",{"id":153,"year":154,"html":155,"doi":11},16120498,1916,"Zambonini (1916): Riv. min.: 47.",{"id":157,"year":158,"html":159,"doi":11},1118651,1944,"Palache, Charles, Berman, Harry, Frondel, Clifford (1944) \u003Ci>The System of Mineralogy\u003C\u002Fi> (7th ed.) Vol. 1 - Elements, Sulfides, Sulfosalts, Oxides. John Wiley and Sons, New York.",{"id":161,"year":162,"html":163,"doi":11},16111565,1947,"Lundqvist, D. (1947) X-ray studies on the binary system Ni-S. Arkiv för Kemi, Mineralogi och Geologi: 24A(21): 1-12.",{"id":165,"year":166,"html":167,"doi":11},16120499,1953,"Gritsaenko, G.S., Sludskaya, N.N., Aidinyan, N.K. (1953) Synthesis of vaesite and polydymite: Zapiski Vsesoyus. Mineralog. Obshchestva: 82: 42-52.",{"id":169,"year":170,"html":171,"doi":172},180368,1962,"KULLERUD, G., YUND, R. A. (1962) The Ni-S System and Related Minerals. \u003Ci>Journal of Petrology\u003C\u002Fi>,  3 (1) 126-175 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1093\u002Fpetrology\u002F3.1.126'>doi:10.1093\u002Fpetrology\u002F3.1.126\u003C\u002Fa>","10.1093\u002Fpetrology\u002F3.1.126",{"id":174,"year":175,"html":176,"doi":177},3128,1980,"Riley, John F. (1980) Ferroan carrollites, cobaltian violarites, and other members of the linnaeite group: (Co,Ni,Fe,Cu)\u003Csub>3\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  43 (330). 733-739 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1980.043.330.06'>doi:10.1180\u002Fminmag.1980.043.330.06\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_43\u002F43-330-733.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1980.043.330.06",{"id":179,"year":180,"html":181,"doi":11},528163,1985,"Vaughan, David J., Craig, James R. (1985) The crystal chemistry of iron-nickel thiospinels. \u003Ci>American Mineralogist\u003C\u002Fi>,  70 (9-10) 1036-1043 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM70\u002FAM70_1036.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":183,"year":184,"html":185,"doi":11},16120502,1986,"Bochek, L., Vinogradova, R., Sandomirskaya, S. (1986) Composition and optical charachteristics of sulfides of polydymite-greigite isomorphic series. Izvestiya Akademii Nauk SSSR Seriya Geologicheskaya: (10): 141-145.",{"id":187,"year":188,"html":189,"doi":11},16120503,1994,"Vedanand, S., Reddy, B.J., Reddy, Y.P. (1994) Spectroscopic investigations on polydymite. Radiation effects and defects in solids: 128(3): 257-262.",{"id":191,"year":192,"html":193,"doi":11},16966779,2005,"(2005) Polydymite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fpolydymite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":195,"year":196,"html":197,"doi":198},129793,2019,"Bosi, Ferdinando, Biagioni, Cristian, Pasero, Marco (2019) Nomenclature and classification of the spinel supergroup. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  31 (1) 183-192 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1127\u002Fejm\u002F2019\u002F0031-2788'>doi:10.1127\u002Fejm\u002F2019\u002F0031-2788\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FEJM31_183.pdf' class='refpdflink'>\u003C\u002Fa>","10.1127\u002Fejm\u002F2019\u002F0031-2788",{"id":200,"year":201,"html":202,"doi":11},17110692,2023,"Hochleitner, Rupert, Weiß, Stefan (2023) Steckbrief Polydymit. \u003Ci>Lapis\u003C\u002Fi>,  48 (6) 9-11",[204,214,224,230,240,248,254,264,272],{"id":205,"source_url":206,"license_code":207,"credit_html":208,"title":209,"description":210,"author":211,"original_width":212,"original_height":213},19752,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=63839437","CC BY-SA 3.0","Christian Rewitzer, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=63839437\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Polydymite-614287.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FPolydymite\" class=\"extiw\" title=\"en:Polydymite\">Polydymite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Dimensions: 20 mm x 18 mm x 14 mm; Field of view: 2,4 mm; largest crystal: 1,7 mm\u003C\u002Fdd>\n\u003Cdd>Locality: Grüneau Mine, Schutzbach, Betzdorf, Siegerland, Rhineland-Palatinate, Germany\u003C\u002Fdd>\n\u003Cdd>Description: Collection and photograph Christian Rewitzer 5.2014\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Christian Rewitzer",978,945,{"id":215,"source_url":216,"license_code":217,"credit_html":218,"title":219,"description":220,"author":221,"original_width":222,"original_height":223},19754,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118194711","CC BY-SA 2.0","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118194711\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Polydymite (47700370712).jpg","\u003Cp>Betzdorf\nGermany\n\u003C\u002Fp>\n\u003Col>\u003Cli>548\u003C\u002Fli>\u003C\u002Fol>","Pacific Museum of Earth from Canada",4000,6000,{"id":225,"source_url":226,"license_code":217,"credit_html":227,"title":228,"description":229,"author":221,"original_width":222,"original_height":223},19755,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118194715","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118194715\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Polydymite (40786572883).jpg","\u003Cp>Schutzbach\nAltenkirchen, Sayn\nGermany\n\u003C\u002Fp>\n\u003Col>\u003Cli>547\u003C\u002Fli>\u003C\u002Fol>",{"id":231,"source_url":232,"license_code":233,"credit_html":234,"title":235,"description":236,"author":237,"original_width":238,"original_height":239},19758,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163482530","CC0 1.0","Darla Sondrol, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163482530\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Polydymite (GeoDIL number - 1202).jpg","Polydymite (Ni3S4) is (when fresh) a violet gray, copper red, light gray, or steel gray mineral that forms a series with linnaeite (Co3S4). The name comes from Greek for “many” and “twin” because this mineral often occurs as twinned crystals. This sample, 8 cm across is too fine grained to show twins.","Darla Sondrol",2446,1478,{"id":241,"source_url":242,"license_code":233,"credit_html":243,"title":244,"description":245,"author":237,"original_width":246,"original_height":247},19759,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163482543","Darla Sondrol, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163482543\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Polydymite (GeoDIL number - 1204).jpg","Polydymite, Ni3S4 (nickel sulfide), is a violet gray, copper red, light gray, or steel gray mineral that forms a series with linnaeite (its coblat equivalent). This sample is 7 cm across.",3040,2016,{"id":249,"source_url":250,"license_code":217,"credit_html":251,"title":252,"description":253,"author":221,"original_width":223,"original_height":222},19753,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118187770","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118187770\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Gaspeite with Millerite and Polydymite (48522446716).jpg","Transvaal, South Africa",{"id":255,"source_url":256,"license_code":257,"credit_html":258,"title":259,"description":260,"author":261,"original_width":262,"original_height":263},19756,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=162676031","CC BY-SA 4.0","Lodewicus de Honsvels, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=162676031\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Millerit-Linneit-Polydymit.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMillerite\" class=\"extiw\" title=\"en:Millerite\">Millerite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLinnaeite\" class=\"extiw\" title=\"en:Linnaeite\">Linnaeite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FPolydymite\" class=\"extiw\" title=\"en:Polydymite\">Polydymite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Weight: 368.3 g\u003C\u002Fdd>\n\u003Cdd>Locality: Grüne Au Mine, Schutzbach, North Rhine-Westphalia, Germany\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Lodewicus de Honsvels",6004,4003,{"id":265,"source_url":266,"license_code":257,"credit_html":267,"title":268,"description":269,"author":261,"original_width":270,"original_height":271},74864,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=162993365","Lodewicus de Honsvels, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=162993365\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Polydymit-Chalkopyrit-Siderit.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FPolydymite\" class=\"extiw\" title=\"en:Polydymite\">Polydymite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FChalcopyrite\" class=\"extiw\" title=\"en:Chalcopyrite\">Chalcopyrite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSiderite\" class=\"extiw\" title=\"en:Siderite\">Siderite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Weight: 125.2 g\u003C\u002Fdd>\n\u003Cdd>Locality: Grüne Au Mine, Schutzbach, North Rhine-Westphalia, Germany\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",5032,3944,{"id":273,"source_url":274,"license_code":233,"credit_html":275,"title":276,"description":277,"author":237,"original_width":278,"original_height":279},19757,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163481799","Darla Sondrol, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163481799\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Nickeline with polydymite (GeoDIL number - 1111).jpg","The copper colored mineral in this photo is nickeline, a nickel arsenide mineral having formula NiAs. The nickeline is mixed with some gray colored polydymite, Ni3S4, which is not easily seen unless the photo is enlarged. Also present are veins mostly made of green malachite, a copper carbonate hydroxide. The sample is about 9 cm across. It comes from a nickel mine in Nevada.",2158,1842,[281],{"id":282,"url":283,"label":284,"formula":285,"spacegroup":286,"year":162},11401,"\u002Fcif\u002F11401.cif","Lundqvist 1947","Ni3 S4","F d 3 m",[288,289,290,291,292],"Grünauite","Polydymiet","Polydymita","Sainit","Saynit",[294,298,302,307,311,314,318,323,327],{"lang":295,"names":296},"az",[297],"Polidimit",{"lang":299,"names":300},"ca",[301],"polidimita",{"lang":303,"names":304},"de",[305,306],"Polydymit","Trinickeltetrasulfid",{"lang":308,"names":309},"eu",[310],"Polidimita",{"lang":312,"names":313},"fr",[7],{"lang":315,"names":316},"he",[317],"פולידיימיט",{"lang":319,"names":320},"it",[321,322],"polidimite","polydymite",{"lang":324,"names":325},"uk",[326],"Полідиміт",{"lang":328,"names":329},"zh",[330],"輝鎳礦","Q7226301",{"history":11,"applications":11}]