[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:51565":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":11,"polytypeof":11,"groupid":12,"weighting":13,"nolocadd":14,"blacklisted":14,"mindat_formula":15,"mindat_formula_note":16,"ima_formula":17,"elements":18,"sigelements":23,"key_elements":24,"impurities":11,"cim":11,"ima_status":25,"ima_notes":11,"ima_history":11,"approval_year":27,"publication_year":28,"discovery_year":11,"strunz10ed1":29,"strunz10ed2":30,"strunz10ed3":22,"strunz10ed4":11,"dana8ed1":31,"dana8ed2":31,"dana8ed3":31,"dana8ed4":31,"csystem":32,"cclass":33,"spacegroup":34,"spacegroupset":35,"a":36,"b":11,"c":11,"alpha":11,"beta":11,"gamma":11,"aerror":13,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":11,"csmetamict":14,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":37,"hmin":38,"hmax":38,"hardtype":39,"vhnmin":40,"vhnmax":41,"vhnerror":11,"vhng":42,"vhns":43,"commenthard":44,"dmeas":11,"dmeas2":11,"dcalc":45,"dmeaserror":11,"dcalcerror":11,"commentdense":46,"lustre":11,"lustretype":47,"commentluster":11,"diapheny":48,"streak":11,"colour":49,"commentcolor":11,"colors":50,"streak_colors":11,"luminescence":11,"uv":52,"cleavage":11,"cleavagetype":11,"fracturetype":53,"tenacity":54,"commentbreak":11,"opticaltype":55,"opticalsign":11,"opticalalpha":11,"opticalalpha2":11,"opticalalphaerror":11,"opticalbeta":11,"opticalbeta2":11,"opticalbetaerror":11,"opticalgamma":11,"opticalgamma2":11,"opticalgammaerror":11,"opticalomega":11,"opticalomega2":11,"opticalomegaerror":11,"opticalepsilon":11,"opticalepsilon2":11,"opticalepsilonerror":11,"opticaln":11,"opticaln2":11,"opticalnerror":11,"optical2vcalc":11,"optical2vcalc2":11,"optical2vcalcerror":11,"optical2vmeasured":11,"optical2vmeasured2":11,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":56,"opticalpleochorismdesc":57,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":58,"opticalinternal":59,"opticaltropic":55,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":60,"otheroccurrence":11,"type_specimen_store":61,"description_short":62,"aboutname":63,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":64,"reviewed_at":11,"variety_of":11,"varieties":65,"group_members":66,"associates":133,"confused_with":134,"type_localities":135,"occurrence_total":13,"citations":142,"images":160,"structures":161,"synonyms":162,"language_names":164,"wikidata_qid":178,"texts":179},51565,"1:1:51565:0","199826ab-bfd8-451b-8590-02ac9d3ea679","Cesiokenopyrochlore","Ckpcl",0,"mineral",null,3316,1,false,"◻Nb\u003Csub>2\u003C\u002Fsub>(O,OH)\u003Csub>6\u003C\u002Fsub>(Cs,◻)  "," ([]∼ 0.20); simplified formula of the holotype: □\u003Csub>2\u003C\u002Fsub>(Nb,W,Ta)\u003Csub>Σ2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>Cs","◻Nb\u003Csub>2\u003C\u002Fsub>(O,OH)\u003Csub>6\u003C\u002Fsub>Cs\u003Csub>1-x\u003C\u002Fsub>",[19,20,21,22],"Cs","Nb","O","H",[19,20,21],[19,20],[26],"APPROVED",2016,2021,"4","D","0","Isometric",32,222,"Fd-3m"," 10.444","Rough, equant crystals, up to 0.05 mm, intergrown with béhierite and rynersonite on a surface of crystal of béhierite.",5,3,"567","625",100,15,"~5","5.984","Could not be measured","Resinous","Translucent","Light brown",[51],"brown","non-fluorescent","Irregular\u002FUneven","brittle","Isotropic","Non-pleochroic","None observed","Light gray","Strong, light-brown","LCT granitic pegmatite ","Type material is deposited in the collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, Russia, catalogue numbers 4954\u002F1","Unique combination of elements: the only known mineral with both Cs and Nb as essential elements.\r\n\r\nFirst natural \"niobate\" to adopt the inverse pyrochlore structure.","For its chemical composition and relationship to pyrochlore. The Y site is predominantly occupied by Cs (= the prefix cesio-), the A site is dominated by vacancy (= the prefix keno), and the B site is dominated by Nb, hence the root name pyrochlore. 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J. (2017) New minerals and nomenclature modifications approved in 2017. CNMNC Newsletter No 36. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  81 (2) 403-409 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2017.081.022'>doi:10.1180\u002Fminmag.2017.081.022\u003C\u002Fa>","10.1180\u002Fminmag.2017.081.022",{"id":149,"year":28,"html":150,"doi":151},17061509,"Agakhanov, Atali A., Kasatkin, Anatoly V., Britvin, Sergey N., Siidra, Oleg I., Pautov, Leonid A., Pekov, Igor V., Karpenko, Vladimir Yu. (2021) Cesiokenopyrochlore, the First Natural Niobate with an Inverse Pyrochlore Structure. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  59 (1) 149-157 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002Fcanmin.2000056'>doi:10.3749\u002Fcanmin.2000056\u003C\u002Fa>","10.3749\u002Fcanmin.2000056",{"id":153,"year":154,"html":155,"doi":11},16963590,2022,"(2022) Cesiokenopyrochlore. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002FCesiokenopyrochlore.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":157,"year":158,"html":159,"doi":11},15897736,2023,"Larsen, Knut Edvard (2023) Minerals first described from Madagascar. \u003Ci>Norsk Mineralsymposium 2023\u003C\u002Fi>, 89-122",[],[],[163],"IMA2016-104",[165,169,174],{"lang":166,"names":167},"ca",[168],"cesiocenopiroclor",{"lang":170,"names":171},"de",[172,173],"Cesiokenopyrochlor","IMA 2016-104",{"lang":175,"names":176},"eu",[177],"Zesiokenopirokloro","Q29476016",{"history":11,"applications":11}]