[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:2941":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":22,"key_elements":23,"impurities":11,"cim":24,"ima_status":25,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":27,"discovery_year":28,"strunz10ed1":29,"strunz10ed2":30,"strunz10ed3":31,"strunz10ed4":32,"dana8ed1":33,"dana8ed2":33,"dana8ed3":34,"dana8ed4":35,"csystem":36,"cclass":37,"spacegroup":11,"spacegroupset":38,"a":39,"b":40,"c":41,"alpha":38,"beta":38,"gamma":38,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":11,"csmetamict":13,"commentcrystal":42,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":43,"hmin":44,"hmax":45,"hardtype":11,"vhnmin":38,"vhnmax":38,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":46,"dmeas2":46,"dcalc":47,"dmeaserror":48,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":49,"commentluster":11,"diapheny":50,"streak":51,"colour":52,"commentcolor":11,"colors":53,"streak_colors":58,"luminescence":11,"uv":11,"cleavage":59,"cleavagetype":60,"fracturetype":61,"tenacity":62,"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":63,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":64,"opticalinternal":65,"opticaltropic":66,"opticalanisotropism":67,"opticalbireflectance":68,"opticalextinction":11,"opticalr":69,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":70,"otheroccurrence":11,"type_specimen_store":71,"description_short":72,"aboutname":73,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":74,"reviewed_at":11,"variety_of":11,"varieties":75,"group_members":76,"associates":77,"confused_with":78,"type_localities":79,"occurrence_total":86,"citations":87,"images":120,"structures":131,"synonyms":145,"language_names":148,"wikidata_qid":165,"texts":166},2941,"1:1:2941:0","2f1c85df-707c-4122-91a9-1fe9e0dff756","Nuffieldite","Nuf",0,"mineral",null,137,false,"Cu\u003Csub>1.4\u003C\u002Fsub>Pb\u003Csub>2.4\u003C\u002Fsub>Bi\u003Csub>2.4\u003C\u002Fsub>Sb\u003Csub>0.2\u003C\u002Fsub>S\u003Csub>7\u003C\u002Fsub>","According to several studies, Sb is an essential component for the stabilisation of nuffieldite.",[17,18,19,20,21],"Bi","Cu","Pb","Sb","S",[17,18,19,20,21],[17,18,19,20],"5.7.10",[26],"APPROVED",1968,"1968","2","J","B","25g","3","4","1","Orthorhombic",8,"0","14.61","21.38","4.03","Non-standard space-group setting Pbnm","Prismatic to acicular crystals, deeply striated parallel to [001]. The crystals frequently occur as bundles of parallel unterminated needles (to 3 mm) in the vugs.",3.5,4,"7.01","7.21",7,"Metallic","Opaque","Dark greenish gray to black.","Shiny lead-gray to steel-gray on fresh surface, tarnishes to pale iridescent grayish green to reddish brown.",[54,55,56,57],"gray","green","brown","black",[55,54,57],"Excellent parallel to [001] and indistinct perpendicular to [001].","Very Good","Irregular\u002FUneven,Conchoidal","very brittle","Non-pleochroic","light gray","none","Anisotropic","strong, but with no color effects","weak - noticeable only in contact with other grains.","(35.9,45.5) 400,\r\n(36.7,44.6) 420,\r\n(37.2,45.9) 440,\r\n(37.4,46.3) 460,\r\n(37.8,46.6) 480,\r\n(38.1,46.6) 500,\r\n(37.7,46.6) 520,\r\n(37.8,46.3) 540,\r\n(37.7,46.2) 560,\r\n(37.5,46.1) 580,\r\n(37.3,45.8) 600,\r\n(36.9,45.4) 620,\r\n(36.9,45.1) 640,\r\n(36.5,44.9) 660,\r\n(36.7,44.4) 680,\r\n(36.2,44.0) 700","In quartz veins in quartz diorite.","Canadian Geological Survey, Ottawa, Canada, 13448.\r\nRoyal Ontario Museum, Toronto, Canada.","Compare argentonuffieldite.","Named in 1968 by Paul William Errol Kingston in honor of Professor Edward Wilfrid Nuffield [April 13, 1914 Gretna, Manitoba, Canada - June 10, 2006 Vancouver, British Columbia, Canada] mineralogist of the University of Toronto, Ontario, Canada.","2025-08-11 12:14:22",[],[],[],[],[80],{"id":81,"txt":82,"latitude":83,"longitude":84,"country":85},8878,"British Columbia Molybdenum Ltd. Mine, Patsy Creek, Kitsault, Alice Arm, Skeena Mining Division, British Columbia, Canada",55.4223406,-129.420621,"Canada",31,[88,91,94,99,103,107,111,115],{"id":89,"year":11,"html":90,"doi":11},15975754,"Moëlo, Y., Meerschaut, A., Makovicky, E. (1997): Refinement of the crystal structure of nuffieldite, Pb2Cu1.4(Pb0.4Bi0.4Sb0.2)Bi2S7: Structural relationship and genesis of complex lead sulfosalt structures. Canadian Mineralogist 35, 1497-1508. https:\u002F\u002Frruff.geo.arizona.edu\u002Fdoclib\u002Fcm\u002Fvol35\u002FCM35_1497.pdf",{"id":92,"year":27,"html":93,"doi":11},15947475,"KINGSTON, P.W. (1968): Studies of mineral sulphosalts. XXI. Nuffieldite, a new species. Canadian Mineralogist 9, 439-452.",{"id":95,"year":96,"html":97,"doi":98},108622,1973,"Kohatsu, Iwao; Wuensch, B. J. (1973) The crystal structure of nuffieldite, Pb2Cu(Pb,Bi)Bi2S7. \u003Ci>Zeitschrift für Kristallographie\u003C\u002Fi>,  138 (1). 343-365 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1973.138.1-4.343'>doi:10.1524\u002Fzkri.1973.138.1-4.343\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fzk\u002Fvol138\u002FZK138_343.pdf' class='refpdflink'>\u003C\u002Fa>","10.1524\u002Fzkri.1973.138.1-4.343",{"id":100,"year":101,"html":102,"doi":11},16118773,1990,"Maurel, C., Moëlo, Y. (1990) Synthèse de la nuffieldite dans le système Bi-Pb-Sb-Cu-S. The Canadian Mineralogist 28, 745-749.",{"id":104,"year":105,"html":106,"doi":11},16080282,1994,"Mozgova, N. N., Nenasheva, S. N., Borodaev, Y. S., & Yudovskaya, M. A. (1994). Nuffieldite from the Maleevskoe massive sulfide deposit, Russia. The Canadian Mineralogist, 32(2), 359-364.",{"id":108,"year":109,"html":110,"doi":11},16966348,2005,"(2005) Nuffieldite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fnuffieldite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":112,"year":113,"html":114,"doi":11},15997349,2006,"Pršek J., Makovicky M., Chovan M., Smirnov A. (2006): A note on chemical composition of nuffieldite solid-solution from sulphide mineralizations (Western Carpathians, Slovakia) Mineralogia Polonica 37 (1), 51-60.",{"id":116,"year":117,"html":118,"doi":119},16650780,2021,"Števko, Martin, Sejkora, Jiří, Dojčanský, Ľudovít (2021) New data on sulphosalts from hydrothermal siderite-type veins in the Spišsko-gemerské rudohorie Mts. (eastern Slovakia): 1. Nuffieldite and aikinite from Slovinky-Došťavná vein. \u003Ci>Bulletin Mineralogie Petrologie\u003C\u002Fi>,  29 (1) Bulletin Mineralogie Petrologie. 108-114 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.46861\u002Fbmp.29.108'>doi:10.46861\u002Fbmp.29.108\u003C\u002Fa>","10.46861\u002Fbmp.29.108",[121],{"id":122,"source_url":123,"license_code":124,"credit_html":125,"title":126,"description":127,"author":128,"original_width":129,"original_height":130},17939,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=94257433","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=94257433\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Nuffieldite.jpg","Black metallic crystals of the very rare Cu-Pb-Bi sulphosalt mineral nuffieldite from USA (Granite Gap, Hidalgo County, New Mexico, United States of America), associated to a green mineral that it is probably malachite.","David Hospital",1121,1120,[132,139],{"id":133,"url":134,"label":135,"formula":136,"spacegroup":137,"year":138},10083,"\u002Fcif\u002F10083.cif","Moelo 1997","Pb2.37 Bi2.39 Sb.24 Cu1.37 S7","P b n m",1997,{"id":140,"url":141,"label":142,"formula":143,"spacegroup":144,"year":96},10084,"\u002Fcif\u002F10084.cif","Kohatsu 1973","Pb2.5 Bi2.5 Cu S7","P b m n",[146,147],"IMA1967-003","Nuffieldiet",[149,153,158,162],{"lang":150,"names":151},"ca",[152],"nuffieldita",{"lang":154,"names":155},"de",[156,157],"IMA 1967-003","Nuffieldit",{"lang":159,"names":160},"eu",[161],"Nuffieldita",{"lang":163,"names":164},"it",[7],"Q3879294",{"history":11,"applications":11}]