[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:3126":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":21,"key_elements":22,"impurities":11,"cim":23,"ima_status":24,"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":34,"dana8ed3":35,"dana8ed4":36,"csystem":37,"cclass":38,"spacegroup":38,"spacegroupset":39,"a":40,"b":41,"c":42,"alpha":43,"beta":44,"gamma":45,"aerror":46,"berror":47,"cerror":48,"alphaerror":49,"betaerror":49,"gammaerror":49,"va3":50,"z":38,"csmetamict":13,"commentcrystal":51,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":52,"tlform":53,"hmin":54,"hmax":55,"hardtype":11,"vhnmin":39,"vhnmax":39,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":56,"dmeas2":57,"dcalc":58,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":59,"commentluster":11,"diapheny":60,"streak":11,"colour":61,"commentcolor":11,"colors":62,"streak_colors":11,"luminescence":11,"uv":67,"cleavage":11,"cleavagetype":68,"fracturetype":69,"tenacity":11,"commentbreak":11,"opticaltype":70,"opticalsign":71,"opticalalpha":72,"opticalalpha2":39,"opticalalphaerror":11,"opticalbeta":39,"opticalbeta2":39,"opticalbetaerror":11,"opticalgamma":73,"opticalgamma2":39,"opticalgammaerror":11,"opticalomega":39,"opticalomega2":39,"opticalomegaerror":11,"opticalepsilon":39,"opticalepsilon2":39,"opticalepsilonerror":11,"opticaln":39,"opticaln2":39,"opticalnerror":11,"optical2vcalc":39,"optical2vcalc2":39,"optical2vcalcerror":11,"optical2vmeasured":74,"optical2vmeasured2":75,"optical2vmeasurederror":11,"rimin":76,"rimax":77,"opticaldispersion":78,"opticalpleochroism":79,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":80,"industrial":11,"occurrence":81,"otheroccurrence":11,"type_specimen_store":82,"description_short":83,"aboutname":84,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":85,"reviewed_at":11,"variety_of":11,"varieties":86,"group_members":87,"associates":88,"confused_with":96,"type_localities":97,"occurrence_total":104,"citations":105,"images":160,"structures":207,"synonyms":218,"language_names":222,"wikidata_qid":252,"texts":253},3126,"1:1:3126:0","2cc5e70d-2497-4b53-bd6d-d3a58322f255","Parsonsite","Pso",0,"mineral",null,2351,false,"Pb\u003Csub>2\u003C\u002Fsub>(UO\u003Csub>2\u003C\u002Fsub>)(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>","Water content appears to be variable.\r\nBoth 0-0.5H\u003Csub>2\u003C\u002Fsub>O and ~2H\u003Csub>2\u003C\u002Fsub>O per formula unit were measured.",[17,18,19,20],"Pb","O","P","U",[17,18,19,20],[17,20],"19.11.36",[25,26],"APPROVED","GRANDFATHERED",1923,"1923","8","E","A","10","40","2a","31","1","Triclinic",2,"0","6.842","10.383","6.670","101.26","98.17","86.38",4,6,40,7,459.8,"Non-standard setting; reduced cell: 6.670, 6.842, 10.383 Å, 86.38, 78.74, 81.83°. Cell parameters from Burns (2000)","Crystals lath-like, elongated [001] and flattened {010}, exhibiting {001}, {101}, and {100}. Radial-fibrous spherulites; commonly as crusts and powdery aggregates.","Minute tabular crystals.",2.5,3,"5.72","5.75","6.21","Sub-Adamantine,Greasy","Transparent,Translucent","Light citron-yellow, honey-brown, green-brown, pale rose (rare); pale yellow in transmitted light.",[63,64,65,66],"yellow","brown","green","pink","Not fluorescent.","None Observed","Conchoidal","Biaxial","-","1.85","1.86","11","26",1.85,1.86,"relatively strong","Non-pleochroic","Radioactive. Soluble in acids.\r\nIn a closed tube yields H2O and becomes yellowish.\r\nOn charcoal fuses to a black globule.","Oxidized zone of a hydrothermal uranium deposit.","National School of Mines, Paris, France  #123.89.","Hallimondite-Parsonsite Series.\r\nThe phosphate analogue of Hallimondite.","In honor of Arthur Leonard Parsons (1873-1957), Professor and Head of Mineralogy and Petrography, University of Toronto (1936-1943), Assistant Director (1920-1939) and Director (1939-1957) of the Royal Ontario Museum.","2026-04-18 15:59:20",[],[],[89],{"id":90,"name":91,"entrytype":9,"csystem":92,"ima_formula":93,"mindat_formula":94,"hmin":54,"hmax":54,"dmeas":39,"dcalc":39,"primary_image_id":95},3182,"Phosphuranylite","Orthorhombic","KCa(H\u003Csub>3\u003C\u002Fsub>O)\u003Csub>3\u003C\u002Fsub>(UO\u003Csub>2\u003C\u002Fsub>)\u003Csub>7\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>O\u003Csub>4\u003C\u002Fsub> · 8H\u003Csub>2\u003C\u002Fsub>O","KCa(H\u003Csub>3\u003C\u002Fsub>O)\u003Csub>3\u003C\u002Fsub>(UO\u003Csub>2\u003C\u002Fsub>)\u003Csub>7\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>O\u003Csub>4\u003C\u002Fsub>·8H\u003Csub>2\u003C\u002Fsub>O",19370,[],[98],{"id":99,"txt":100,"latitude":101,"longitude":102,"country":103},4328,"Shinkolobwe Mine, Shinkolobwe, Kambove Territory, Haut-Katanga, DR Congo",-11.0486111,26.5508333,"DR Congo",64,[106,109,112,117,121,126,130,134,139,144,147,151,156],{"id":107,"year":27,"html":108,"doi":11},16119554,"Wherry, E.T. (1923) New minerals: new species. American Mineralogist: 8: 150-151.",{"id":110,"year":27,"html":111,"doi":11},16161383,"Schoep, A. (1923) Sur la parsonsite, nouveau minéral radioactif. Comptes rendus hebdomadaires des séances de l'Académie des Sciences, Paris: 176: 171-173 (in French). https:\u002F\u002Fgallica.bnf.fr\u002Fark:\u002F12148\u002Fbpt6k31295\u002Ff171.item",{"id":113,"year":114,"html":115,"doi":116},400364,1926,"Billiet, Valère (1926) Détermination des indices de réfraction de la becquerélite, de la curite, de la kasolite, de la fourmariérite, de la parsonsite, de la dumontite, et de l'ianthinite. \u003Ci>Bulletin de la Société française de Minéralogie\u003C\u002Fi>,  49 (3). 136-140 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3406\u002Fbulmi.1926.4309'>doi:10.3406\u002Fbulmi.1926.4309\u003C\u002Fa>","10.3406\u002Fbulmi.1926.4309",{"id":118,"year":119,"html":120,"doi":11},521978,1950,"Frondel, Clifford (1950) Studies of uranium minerals (I) : Parsonite and randite. \u003Ci>American Mineralogist\u003C\u002Fi>,  35 (3-4) 245-250 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM35\u002FAM35_245.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":122,"year":123,"html":124,"doi":125},595495,1958,"Frondel, Clifford (1958) Systematic mineralogy of uranium and thorium. \u003Ci>Bulletin\u003C\u002Fi> 1064. US Geological Survey \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3133\u002Fb1064'>doi:10.3133\u002Fb1064\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fpubs.usgs.gov\u002Fbul\u002F1064\u002Freport.pdf' class='refpdflink'>\u003C\u002Fa>","10.3133\u002Fb1064",{"id":127,"year":128,"html":129,"doi":11},16119556,1959,"Mazzi, F., Garavelli, C.L., Rinaldi, F. (1959): Richerche strutturali sulla parsonite (sic). Rendiconti della Società Mineralogica Italiana 25, 364-365 (in Italian).",{"id":131,"year":132,"html":133,"doi":11},16119557,1981,"Deliens, M., Piret, P., Comblain, G. (1981) Les minéraux secondaires d’uranium du Zaïre. Published by Musée Royal de l’Afrique Central, Tavuren, Belgium, 64-65 (in French).",{"id":135,"year":136,"html":137,"doi":138},394227,2000,"Burns, Peter C. (2000) A new uranyl phosphate chain in the structure of parsonsite. \u003Ci>American Mineralogist\u003C\u002Fi>,  85 (5) 801-805 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2000-5-621'>doi:10.2138\u002Fam-2000-5-621\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol85\u002FAM85_801.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam-2000-5-621",{"id":140,"year":141,"html":142,"doi":143},395151,2005,"Locock, Andrew J., Burns, Peter C., Flynn, Theodore M. (2005) The role of water in the structures of synthetic hallimondite, Pb\u003Csub>2\u003C\u002Fsub>[(UO\u003Csub>2\u003C\u002Fsub>)(AsO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>](H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>n\u003C\u002Fsub> and synthetic parsonsite, Pb\u003Csub>2\u003C\u002Fsub>[(UO\u003Csub>2\u003C\u002Fsub>)(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>](H\u003Csub>2\u003C\u002Fsub>O)\u003Csub>n\u003C\u002Fsub>, 0 ≤n≤ 0.5. \u003Ci>American Mineralogist\u003C\u002Fi>,  90 (1) 240-246 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2005.1705'>doi:10.2138\u002Fam.2005.1705\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol90\u002FAM90_240.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam.2005.1705",{"id":145,"year":141,"html":146,"doi":11},16966586,"(2005) Parsonsite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fparsonsite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":148,"year":141,"html":149,"doi":150},64215,"Burns, Peter C. (2005) U\u003Csup>6+\u003C\u002Fsup> minerals and inorganic compounds: insights into an expanded structural hierarchy of crystal structures. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  43 (6) 1839-1894 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgscanmin.43.6.1839'>doi:10.2113\u002Fgscanmin.43.6.1839\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fcm\u002Fvol43\u002FCM43_1839.pdf' class='refpdflink'>\u003C\u002Fa>","10.2113\u002Fgscanmin.43.6.1839",{"id":152,"year":153,"html":154,"doi":155},2425933,2006,"Frost, Ray L., Čejka, Jiří, Weier, Matt, Martens, Wayde N. (2006) A Raman spectroscopic study of the uranyl phosphate mineral parsonsite. \u003Ci>Journal of Raman Spectroscopy\u003C\u002Fi>, 37 (9). 879-891 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fjrs.1517'>doi:10.1002\u002Fjrs.1517\u003C\u002Fa>","10.1002\u002Fjrs.1517",{"id":157,"year":158,"html":159,"doi":11},16693622,2009,"Plášil, J., Čejka, J., Sejkora, J., Škácha, P. (2009) The question of water content in parsonsite: a model case - occurrence at the Červené žíly vein system, Jáchymov (St. Joachimsthal), Czech Republic. \u003Ci>Journal of GEOsciences\u003C\u002Fi>,  54 (4) 385-394 \u003Ca target='_blank' href='http:\u002F\u002Fwww.jgeosci.org\u002Fcontent\u002Fjgeosci.056_2009_4_plasil1.pdf' class='refpdflink'>\u003C\u002Fa>",[161,171,181,191,198],{"id":162,"source_url":163,"license_code":164,"credit_html":165,"title":166,"description":167,"author":168,"original_width":169,"original_height":170},18836,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118193026","CC BY-SA 2.0","Pacific Museum of Earth from Canada, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=118193026\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Parsonsite (49055734126).jpg","\u003Cp>La Faye, Grury\n\u003C\u002Fp>\nMorvan, France","Pacific Museum of Earth from Canada",4000,6000,{"id":172,"source_url":173,"license_code":174,"credit_html":175,"title":176,"description":177,"author":178,"original_width":179,"original_height":180},18837,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130437418","CC BY 4.0","Henk Smeets – tomeikminerals.com, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130437418\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Parsonsite Grury RGrant-9.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FParsonsite\" class=\"extiw\" title=\"en:Parsonsite\">Parsonsite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Field of view: 5 mm\u003C\u002Fdd>\n\u003Cdd>Locality: La Faye Mine, Grury, Charolles, Saône-et-Loire, Bourgogne-Franche-Comté, France (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"https:\u002F\u002Fwww.mindat.org\u002Floc-1737.html\">locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Henk Smeets – tomeikminerals.com",1920,1280,{"id":182,"source_url":183,"license_code":184,"credit_html":185,"title":186,"description":187,"author":188,"original_width":189,"original_height":190},7136,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10446947","CC BY-SA 3.0","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10446947\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Curite-Dewindtite-Parsonsite-d06-53b.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCurite\" class=\"extiw\" title=\"en:Curite\">Curite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDewindtite\" class=\"extiw\" title=\"en:Dewindtite\">Dewindtite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FParsonsite\" class=\"extiw\" title=\"en:Parsonsite\">Parsonsite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTorbernite\" class=\"extiw\" title=\"en:Torbernite\">Torbernite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Shinkolobwe Mine (Kasolo Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FShinkolobwe\" class=\"extiw\" title=\"en:Shinkolobwe\">Shinkolobwe\u003C\u002Fa>, Central area, Katanga Copper Crescent, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FKatanga\" class=\"extiw\" title=\"en:Katanga\">Katanga (Shaba)\u003C\u002Fa>, Democratic Republic of Congo (Zaïre) (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-4328.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: miniature, 5.2 x 2.8 x 1.5 cm\n\u003Cdl>\u003Cdt>Dewindtite on Torbernite, with Curite and Parsonsite\u003C\u002Fdt>\u003C\u002Fdl>\u003C\u002Fdd>\n\u003Cdd>This is a very rich specimen of dewindtite, dating to 1925 before it was even officially named, and the early era of exploration of this region by many great Belgian mineralogists. The label is noted WWI-era collector Robert Gage's, in his own hand. I showed this to Bill Pinch, to confirm its legitimacy , and he told me it is indeed one of the better example sof the species he has seen. A rare (if hot) treasure!\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",400,352,{"id":192,"source_url":193,"license_code":184,"credit_html":194,"title":195,"description":187,"author":188,"original_width":196,"original_height":197},6719,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10446949","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10446949\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Curite-Dewindtite-Parsonsite-d06-53a.jpg",800,474,{"id":199,"source_url":200,"license_code":184,"credit_html":201,"title":202,"description":203,"author":204,"original_width":205,"original_height":206},18834,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14866116","Leon Hupperichs, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14866116\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Parsonsite-Torbernite-90912.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FParsonsite\" class=\"extiw\" title=\"en:Parsonsite\">Parsonsite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTorbernite\" class=\"extiw\" title=\"en:Torbernite\">Torbernite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Pinhal do Souto mine, Tragos, Chãs de Tavares, Mangualde, Viseu District, Portugal\u003C\u002Fdd>\n\u003Cdd>Yellow-brown xls of Parsonsite together with Torbernite xls. Field of view 4 mm.  Depth of field is achieved with CombineZM. Specimen and photo Leon Hupperichs.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Leon Hupperichs",729,536,[208,214],{"id":209,"url":210,"label":211,"formula":212,"spacegroup":213,"year":141},10502,"\u002Fcif\u002F10502.cif","Locock 2005","U Pb2 P2 O10","P -1",{"id":215,"url":216,"label":217,"formula":212,"spacegroup":213,"year":136},10503,"\u002Fcif\u002F10503.cif","Burns 2000",[219,220,221],"Parsonsiet","UM2000-\u002F\u002F-PO:AlPbU","Unnamed (Pb-U-Al Phosphate)",[223,227,231,235,238,241,244,248],{"lang":224,"names":225},"ca",[226],"parsonsita",{"lang":228,"names":229},"de",[230],"Parsonsit",{"lang":232,"names":233},"es",[234],"Parsonsita",{"lang":236,"names":237},"eu",[234],{"lang":239,"names":240},"it",[7],{"lang":242,"names":243},"pl",[230],{"lang":245,"names":246},"ta",[247],"பார்சன்சைட்டு",{"lang":249,"names":250},"uk",[251],"парсонсит","Q1067103",{"history":11,"applications":11}]