[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:1615":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":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":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":39,"c":40,"alpha":41,"beta":42,"gamma":41,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":43,"csmetamict":13,"commentcrystal":11,"twinning":44,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":45,"tlform":46,"hmin":47,"hmax":47,"hardtype":11,"vhnmin":48,"vhnmax":41,"vhnerror":11,"vhng":49,"vhns":11,"commenthard":11,"dmeas":50,"dmeas2":51,"dcalc":52,"dmeaserror":11,"dcalcerror":11,"commentdense":53,"lustre":11,"lustretype":54,"commentluster":55,"diapheny":56,"streak":57,"colour":58,"commentcolor":11,"colors":59,"streak_colors":62,"luminescence":11,"uv":11,"cleavage":63,"cleavagetype":64,"fracturetype":65,"tenacity":66,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":41,"opticalalpha2":41,"opticalalphaerror":11,"opticalbeta":41,"opticalbeta2":41,"opticalbetaerror":11,"opticalgamma":41,"opticalgamma2":41,"opticalgammaerror":11,"opticalomega":41,"opticalomega2":41,"opticalomegaerror":11,"opticalepsilon":41,"opticalepsilon2":41,"opticalepsilonerror":11,"opticaln":41,"opticaln2":41,"opticalnerror":11,"optical2vcalc":41,"optical2vcalc2":41,"optical2vcalcerror":11,"optical2vmeasured":41,"optical2vmeasured2":41,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":67,"opticalinternal":11,"opticaltropic":68,"opticalanisotropism":69,"opticalbireflectance":11,"opticalextinction":11,"opticalr":70,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":71,"otheroccurrence":11,"type_specimen_store":72,"description_short":73,"aboutname":74,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":75,"reviewed_at":11,"variety_of":11,"varieties":76,"group_members":77,"associates":78,"confused_with":79,"type_localities":80,"occurrence_total":87,"citations":88,"images":116,"structures":127,"synonyms":135,"language_names":137,"wikidata_qid":154,"texts":155},1615,"1:1:1615:1","1cb96d6b-8100-43df-96f8-e9addc89d4d9","Froodite","Fro",0,"mineral",null,339,false,"&#945;-PdBi\u003Csub>2\u003C\u002Fsub>","PdBi\u003Csub>2\u003C\u002Fsub>",[17,18],"Bi","Pd",[17,18],[17,18],",Te,,","3.12.41",[24,25],"APPROVED","GRANDFATHERED","1958","2","A","C","45a","12","15","1","Monoclinic",5,11,"C2\u002Fm ","12.74","4.29","5.71","0","102.52",4,"Sometimes","Rounded grains","Flat cleavage fragments and rounded grains",2.5,"84",25,"12.05","12.6","11.42","Synthetic - 11.5","Metallic","Quite reflective giving a silvery white reflection; splendent on fresh cleavage, tarnishes quickly;","Opaque","Black","Grey",[60,61],"gray","black",[61],"Perfect on {100}\r\nless perfect on {001}","Perfect","Irregular\u002FUneven","brittle","Creamy white","Anisotropic","Light and dark grays","(50.7,52.9) 420,\r\n(51.9,54.3) 440,\r\n(53.1,55.5) 460,\r\n(54.3,56.4) 480,\r\n(55.2,57.2) 500,\r\n(55.7,57.8) 520,\r\n(56.1,58.4) 540,\r\n(56.5,59.0) 560,\r\n(56.9,59.6) 580,\r\n(57.4,60.2) 600,\r\n(57.7,60.7) 620,\r\n(58.0,61.1) 640,\r\n(58.5,61.4) 660,\r\n(58.8,62.0) 680,\r\n(59.3,63.0) 700","Sudbury intrusive","Harvard University. The cleavage fragment is not available for\r\nfurther study.","Chemically related to 'UM1961-03-Bi:Pd' and 'UM1968-01-Bi:Pd'.\r\n\r\nThe phase transition in structure of the PdBi2 compound has been studied using high-temperature in-situ methods (differential thermal analysis and high-temperature single-crystal X-ray d...","For the type locality.","2025-10-08 06:23:05",[],[],[],[],[81],{"id":82,"txt":83,"latitude":84,"longitude":85,"country":86},11253,"Frood Mine, McKim Township, Greater Sudbury, Ontario, Canada",46.53394,-80.99854,"Canada",77,[89,93,97,102,107,111],{"id":90,"year":91,"html":92,"doi":11},19426819,1958,"Hawley, James Edwin; Berry, Leonard Gascoigne (1958) Michenerite and froodite, palladium bismuthide minerals [Ontario]. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  6 (2). 200-209 \u003Ca target='_blank' href='https:\u002F\u002Fwww.rruff.net\u002Fdoclib\u002Fcm\u002Fvol6\u002FCM6_200.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":94,"year":95,"html":96,"doi":11},16117142,1973,"Cabri, L.J., Harris, D.C., and Gait, R.I. (1973) Michenerite (PdBiTe) redefined and froodite (PdBi2) confirmed from the Sudbury area. The Canadian Mineralogist: 11: 903-912.",{"id":98,"year":99,"html":100,"doi":101},127435,1996,"Evstigneeva, Tatiana, Tarkian, Mahmud (1996) Synthesis of platinum-group minerals under hydrothermal conditions. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  8 (3) 549-564 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1127\u002Fejm\u002F8\u002F3\u002F0549'>doi:10.1127\u002Fejm\u002F8\u002F3\u002F0549\u003C\u002Fa>","10.1127\u002Fejm\u002F8\u002F3\u002F0549",{"id":103,"year":104,"html":105,"doi":106},16299,1998,"Vavřín, I., Frýda, J. (1998) Michenerite PdBiTe and froodite PdBi2 from the Cu-Ni mineralization in the Ransko massif, Czech Republic. \u003Ci>Mineralogy and Petrology\u003C\u002Fi>,  63 (1) 141-146 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf01162772'>doi:10.1007\u002Fbf01162772\u003C\u002Fa>","10.1007\u002Fbf01162772",{"id":108,"year":109,"html":110,"doi":11},16964464,2005,"(2005) Froodite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Ffroodite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":112,"year":113,"html":114,"doi":115},18794825,2025,"Karimova, O. V.; Eremin, N. N.; Mezhueva, A. A.; Uporova, N. S.; Zolotarev, A. A.; Chareev, D. A. (2025) Structural Transformations and Froodite (α-PdBi2)–Urvantsevite (β-PdBi2) Phase Transition at High Temperatures. \u003Ci>Moscow University Geology Bulletin\u003C\u002Fi>,  80 (2). 199-205 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3103\u002Fs0145875225700310'>doi:10.3103\u002Fs0145875225700310\u003C\u002Fa>","10.3103\u002Fs0145875225700310",[117],{"id":118,"source_url":119,"license_code":120,"credit_html":121,"title":122,"description":123,"author":124,"original_width":125,"original_height":126},9455,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130259674","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130259674\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Urvantsevite & Froodite.jpg","Metallic inclusions of the two extremely rare palladium-bismuth minerals urvantsevite &amp; froodite from the famous Talnakh deposit (Mayak Mine, Talnakh, Noril'sk, Putoran Plateau, Taimyr Peninsula, Krasnoyarsk Krai, Russian Federation) in a completely analyzed specimen by SEM\u002FEdS. Ex Vandenbroucke Museum collection from Waregem, Belgium.","David Hospital",765,542,[128],{"id":129,"url":130,"label":131,"formula":132,"spacegroup":133,"year":134},5268,"\u002Fcif\u002F5268.cif","Zhuravlev 1957","Bi2 Pd","C 1 2\u002Fm 1",1957,[136],"Froodiet",[138,142,146,150],{"lang":139,"names":140},"ca",[141],"froodita",{"lang":143,"names":144},"de",[145],"Froodit",{"lang":147,"names":148},"eu",[149],"Froodita",{"lang":151,"names":152},"it",[153],"froodite","Q1470345",{"history":11,"applications":11}]