[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:3598":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":11,"cim":21,"ima_status":22,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":24,"discovery_year":25,"strunz10ed1":26,"strunz10ed2":27,"strunz10ed3":28,"strunz10ed4":29,"dana8ed1":26,"dana8ed2":26,"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":39,"berror":39,"cerror":39,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":40,"csmetamict":13,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":41,"tlform":42,"hmin":11,"hmax":11,"hardtype":11,"vhnmin":35,"vhnmax":35,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":35,"dmeas2":35,"dcalc":43,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":44,"commentluster":11,"diapheny":45,"streak":46,"colour":47,"commentcolor":11,"colors":48,"streak_colors":52,"luminescence":11,"uv":53,"cleavage":54,"cleavagetype":55,"fracturetype":11,"tenacity":11,"commentbreak":11,"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":56,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":57,"opticalinternal":58,"opticaltropic":59,"opticalanisotropism":60,"opticalbireflectance":61,"opticalextinction":11,"opticalr":62,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":63,"otheroccurrence":11,"type_specimen_store":64,"description_short":65,"aboutname":66,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":67,"reviewed_at":11,"variety_of":11,"varieties":68,"group_members":69,"associates":70,"confused_with":71,"type_localities":87,"occurrence_total":33,"citations":94,"images":123,"structures":134,"synonyms":142,"language_names":145,"wikidata_qid":165,"texts":166},3598,"1:1:3598:5","bf6c84cc-b69a-4da5-a9a5-285c5c82d062","Scrutinyite","Sny",0,"mineral",null,127,false,"α-PbO\u003Csub>2\u003C\u002Fsub>","PbO\u003Csub>2\u003C\u002Fsub>",[17,18],"Pb","O",[17,18],[17],"7.11.24",[23],"APPROVED",1988,"1988","4","D","B","20","6","2","Orthorhombic",8,63,"0","4.971","5.956","5.438",2,4,"Tabular crystals up to 30 micron.","Euhedral crystals 25-30 microns across and 1-2 microns thick.","9.867","Sub-Metallic","Translucent,Opaque","Dark brown","Dark reddish brown, clove-brown, red on thin edges",[49,50,51],"red","brown","black",[50],"Not fluorescent.","{100}, perfect; {010}, imperfect (forms by analogy to columbite).","Perfect","Not Visible","Grey-white","Reddish brown","Anisotropic","Weak with a bluish color","Very weak, grey-white to bluish grey-white","(17.9,18.8) 546,\r\n(17.0,17.9) 589","Oxidation product of hydrothermal mineralization.","National Museum of Natural History, Washington, D.C., USA, 165479.","A secondary lead oxide difficult to distinguish from plattnerite.\r\nAn oxidation product in lead piping and oil paintings.","Named from the word \"scrutiny,\" referring to the care required to making the initial identification of the mineral.","2025-12-09 17:09:46",[],[],[],[72,79],{"id":73,"name":74,"entrytype":9,"csystem":32,"ima_formula":75,"mindat_formula":75,"hmin":76,"hmax":77,"dmeas":11,"dcalc":78,"primary_image_id":11},470602,"Nioboixiolite-([])","(Nb\u003Csub>0.8\u003C\u002Fsub>◻\u003Csub>0.2\u003C\u002Fsub>)\u003Csup>4+\u003C\u002Fsup>O\u003Csub>2\u003C\u002Fsub>",6,6.5,"6.05",{"id":80,"name":81,"entrytype":9,"csystem":82,"ima_formula":15,"mindat_formula":15,"hmin":83,"hmax":83,"dmeas":84,"dcalc":85,"primary_image_id":86},3237,"Plattnerite","Tetragonal",5.5,"9.564","9.563",19583,[88],{"id":89,"txt":90,"latitude":91,"longitude":92,"country":93},26242,"Sunshine No. 1 Adit, Blanchard Mine, Bingham, Hansonburg District, Socorro County, New Mexico, USA",33.8116667,-106.375,"USA",[95,99,102,106,110,114,118],{"id":96,"year":97,"html":98,"doi":11},16123125,1952,"Zaslavskii, A.I., Tolkachev, S.S. (1952) The structure of the α-modification of lead dioxide. Zhurnal Fizicheskoi Khimii, 26, 743-752.",{"id":100,"year":24,"html":101,"doi":11},16123126,"Taggart, J.E., Foord, E.E., Rosenzweig, A., Hanson, T. (1988) Scrutinyite, natural occurrences of αPbO2 from Bingham, New Mexico, U.S.A., and Mapimi, Mexico. The Canadian Mineralogist, 26, 905-910. https:\u002F\u002Fwww.rruff.net\u002Fodr\u002Fview\u002Fdownloadfile\u002F66798",{"id":103,"year":104,"html":105,"doi":11},528889,1990,"Jambor, John L., Vanko, David A. (1990) New Mineral Names. \u003Ci>American Mineralogist\u003C\u002Fi>,  75 (5-6) 706-713 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM75\u002FAM75_706.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":107,"year":108,"html":109,"doi":11},16123128,1994,"Nekrasov, I.Y. (1994) Scrutinyite, α-PbO2, its second find in the world. Transactions of the Russian Academy of Sciences, Earth Science Sections, 324(4), 150-153.",{"id":111,"year":112,"html":113,"doi":11},16967230,2005,"(2005) Scrutinyite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fscrutinyite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":115,"year":116,"html":117,"doi":11},16123129,2014,"Kushnir, C. S. (2014). Influence of water chemistry parameters on the dissolution rate of the Lead (II) carbonate hydrocerussite. The University of Western Ontario (Canada).",{"id":119,"year":120,"html":121,"doi":122},15718297,2023,"Chukanov, Nikita V., Pasero, Marco, Aksenov, Sergey M., Britvin, Sergey N., Zubkova, Natalia V., Yike, Li, Witzke, Thomas (2023) Columbite supergroup of minerals: nomenclature and classification. \u003Ci>Mineralogical Magazine\u003C\u002Fi>, 87 (1) 18-33 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fmgm.2022.105'>doi:10.1180\u002Fmgm.2022.105\u003C\u002Fa>","10.1180\u002Fmgm.2022.105",[124],{"id":125,"source_url":126,"license_code":127,"credit_html":128,"title":129,"description":130,"author":131,"original_width":132,"original_height":133},21940,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=148553107","CC BY 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=148553107\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Scrutinyite.jpg","Brown patches of scrutinyite from the famous Blanchard claims in New Mexico (Sunshine #1 Adit, Blanchard Mine, Bingham, Socorro County, New Mexico, United States of America). Ex Vandenbroucke Museum collection from Waregem, Belgium.","David Hospital",601,452,[135],{"id":136,"url":137,"label":138,"formula":139,"spacegroup":140,"year":141},12557,"\u002Fcif\u002F12557.cif","Wyckoff 1963","Pb O2","P b c n",1963,[143,144],"IMA1984-061","Scrutinyiet",[146,150,155,159,162],{"lang":147,"names":148},"ca",[149],"scrutinyita",{"lang":151,"names":152},"de",[153,154],"IMA 1984-061","Scrutinyit",{"lang":156,"names":157},"eu",[158],"Scrutinyita",{"lang":160,"names":161},"it",[7],{"lang":163,"names":164},"ja",[7],"Q3953137",{"history":11,"applications":11}]