[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:4274":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":22,"key_elements":23,"impurities":11,"cim":24,"ima_status":25,"ima_notes":11,"ima_history":11,"approval_year":27,"publication_year":28,"discovery_year":29,"strunz10ed1":30,"strunz10ed2":31,"strunz10ed3":32,"strunz10ed4":33,"dana8ed1":34,"dana8ed2":35,"dana8ed3":36,"dana8ed4":35,"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":38,"betaerror":38,"gammaerror":38,"va3":11,"z":48,"csmetamict":13,"commentcrystal":11,"twinning":49,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":11,"hmin":48,"hmax":38,"hardtype":11,"vhnmin":39,"vhnmax":39,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":50,"dmeas2":50,"dcalc":51,"dmeaserror":47,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":52,"commentluster":11,"diapheny":53,"streak":54,"colour":55,"commentcolor":11,"colors":56,"streak_colors":59,"luminescence":11,"uv":60,"cleavage":61,"cleavagetype":62,"fracturetype":11,"tenacity":63,"commentbreak":11,"opticaltype":64,"opticalsign":65,"opticalalpha":66,"opticalalpha2":39,"opticalalphaerror":47,"opticalbeta":67,"opticalbeta2":39,"opticalbetaerror":38,"opticalgamma":68,"opticalgamma2":39,"opticalgammaerror":38,"opticalomega":39,"opticalomega2":39,"opticalomegaerror":11,"opticalepsilon":39,"opticalepsilon2":39,"opticalepsilonerror":11,"opticaln":39,"opticaln2":39,"opticalnerror":11,"optical2vcalc":69,"optical2vcalc2":39,"optical2vcalcerror":11,"optical2vmeasured":70,"optical2vmeasured2":39,"optical2vmeasurederror":71,"rimin":72,"rimax":73,"opticaldispersion":74,"opticalpleochroism":11,"opticalpleochorismdesc":75,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":76,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":77,"industrial":11,"occurrence":78,"otheroccurrence":11,"type_specimen_store":79,"description_short":80,"aboutname":81,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":82,"reviewed_at":11,"variety_of":11,"varieties":83,"group_members":84,"associates":85,"confused_with":86,"type_localities":87,"occurrence_total":46,"citations":94,"images":121,"structures":122,"synonyms":133,"language_names":136,"wikidata_qid":153,"texts":154},4274,"1:1:4274:7","61ba4ff8-d2ea-48f3-a37d-049477610444","Wheatleyite","Wty",0,"mineral",null,34,false,"Na\u003Csub>2\u003C\u002Fsub>Cu(C\u003Csub>2\u003C\u002Fsub>O\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>&middot;2H\u003Csub>2\u003C\u002Fsub>O","Na\u003Csub>2\u003C\u002Fsub>Cu(C\u003Csub>2\u003C\u002Fsub>O\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub> &middot; 2H\u003Csub>2\u003C\u002Fsub>O",[17,18,19,20,21],"Cu","Na","O","C","H",[17,18,19,20,21],[17],"31.1.3",[26],"APPROVED",1984,1986,"1984","10","A","B","30","50","1","8","Triclinic",2,"0","7.559","9.665","3.589","76.65","103.67","109.10",3,4,1,"Sometimes observed on the single-crystal diffraction photographs, but the twin law was not determined.","2.27","2.250","Vitreous","Translucent","Light blue","Bright blue",[57,58],"blue","colorless",[57],"None observed.","{100};  two additionally observed optically.","Perfect","very brittle","Biaxial","+","1.400","1.499","1.667","84","83",5,1.4,1.667,"none","X = colorless; Y = very pale blue; Z = intense dark blue.","Must be kept dry.","Water soluble.","Vein-type lead-zinc deposit.","Canadian Museum of Nature, Ottawa, Canada, 80196.\r\nNational Museum of Natural History, Washington, D.C., USA, 162531.","The second Na-Cu oxalate mineral after antipinite (that also contains K). Compare other Cu-bearing oxalate minerals - middlebackite, moolooite, and fiemmeite.","Named after its discovery locality, the Wheatley Mines, Phoenixville, Pennsylvania, USA.","2025-08-11 12:14:25",[],[],[],[],[88],{"id":89,"txt":90,"latitude":91,"longitude":92,"country":93},4075,"Wheatley Mines, Schuylkill Township, Chester County, Pennsylvania, USA",40.1055556,-75.5166667,"USA",[95,100,104,107,112,116],{"id":96,"year":97,"html":98,"doi":99},1399154,1980,"Gleizes, A., Maury, F., Galy, J. (1980) Crystal structure and magnetism of sodium bis(oxalato)cuprate(II)dihydrate, Na2Cu(C2O4)2.2H2O. A deductive proposal for the structure of copper oxalate, CuC2O4.xH2O (O \u003C= x \u003C= 1). \u003Ci>Inorganic Chemistry\u003C\u002Fi>,  19 (7). 2074-2078 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1021\u002Fic50209a048'>doi:10.1021\u002Fic50209a048\u003C\u002Fa>","10.1021\u002Fic50209a048",{"id":101,"year":97,"html":102,"doi":103},201197,"Chananont, P., Nixon, P. E., Waters, J. M., Waters, T. N. (1980) The structure of disodium catena-bis(μ-oxalato)-cuprate(II) dihydrate. \u003Ci>Acta Crystallographica Section B Structural Crystallography and Crystal Chemistry\u003C\u002Fi>,  36 (9) 2145-2147 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs0567740880008163'>doi:10.1107\u002Fs0567740880008163\u003C\u002Fa>","10.1107\u002Fs0567740880008163",{"id":105,"year":28,"html":106,"doi":11},15964487,"Rouse, R.C., Peacor, D.R., Dunn, P.J., Simmons, W.B., Newbury, D. (1986) Wheatleyite, Na2Cu(C2O4)2·2H2O, a natural sodium copper salt of oxalic acid. American Mineralogist: 71: 1240-1242.",{"id":108,"year":109,"html":110,"doi":111},13252977,1989,"Polou, R., Triche, C., Barbier, B., Pitet, G. (1989) Sodium Copper Oxalate Dihydrate: Na\u003Csub>2\u003C\u002Fsub>Cu(C\u003Csub>2\u003C\u002Fsub>O\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>.2H\u003Csub>2\u003C\u002Fsub>O Synthesis, Characterization, Morphology and Optical Properties. \u003Ci>Powder Diffraction\u003C\u002Fi>,  4 (1). 14-18 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1017\u002Fs0885715600016237'>doi:10.1017\u002Fs0885715600016237\u003C\u002Fa>","10.1017\u002Fs0885715600016237",{"id":113,"year":114,"html":115,"doi":11},16968104,2005,"(2005) Wheatleyite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fwheatleyite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":117,"year":118,"html":119,"doi":120},64823,2010,"Echigo, T., Kimata, M. (2010) Crystal Chemistry and Genesis of Organic Minerals: a Review of Oxalate and Polycyclic Aromatic Hydrocarbon Minerals. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  48 (6) 1329-1357 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002Fcanmin.48.5.1329'>doi:10.3749\u002Fcanmin.48.5.1329\u003C\u002Fa>","10.3749\u002Fcanmin.48.5.1329",[],[123,129],{"id":124,"url":125,"label":126,"formula":127,"spacegroup":128,"year":97},14478,"\u002Fcif\u002F14478.cif","Chananont 1980","Na2 Cu C4 O10 H4","P -1",{"id":130,"url":131,"label":132,"formula":127,"spacegroup":128,"year":97},14479,"\u002Fcif\u002F14479.cif","Gleizes 1980",[134,135],"IMA1984-040","Wheatleyiet",[137,141,146,150],{"lang":138,"names":139},"ca",[140],"wheatleyita",{"lang":142,"names":143},"de",[144,145],"IMA 1984-040","Wheatleyit",{"lang":147,"names":148},"eu",[149],"Wheatleyita",{"lang":151,"names":152},"it",[7],"Q2566612",{"history":11,"applications":11}]