[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:471432":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":6,"synid":6,"polytypeof":6,"groupid":6,"weighting":11,"nolocadd":12,"blacklisted":12,"mindat_formula":13,"mindat_formula_note":6,"ima_formula":6,"elements":14,"sigelements":19,"key_elements":20,"impurities":6,"cim":6,"ima_status":21,"ima_notes":6,"ima_history":6,"approval_year":6,"publication_year":6,"discovery_year":6,"strunz10ed1":23,"strunz10ed2":24,"strunz10ed3":24,"strunz10ed4":6,"dana8ed1":6,"dana8ed2":6,"dana8ed3":6,"dana8ed4":6,"csystem":25,"cclass":26,"spacegroup":27,"spacegroupset":28,"a":29,"b":30,"c":31,"alpha":6,"beta":32,"gamma":6,"aerror":33,"berror":34,"cerror":33,"alphaerror":6,"betaerror":35,"gammaerror":6,"va3":6,"z":36,"csmetamict":12,"commentcrystal":37,"twinning":6,"tranglide":6,"parting":6,"epitaxidescription":6,"morphology":6,"tlform":38,"hmin":39,"hmax":6,"hardtype":6,"vhnmin":6,"vhnmax":6,"vhnerror":6,"vhng":6,"vhns":6,"commenthard":6,"dmeas":6,"dmeas2":6,"dcalc":40,"dmeaserror":6,"dcalcerror":6,"commentdense":6,"lustre":6,"lustretype":41,"commentluster":6,"diapheny":42,"streak":43,"colour":44,"commentcolor":6,"colors":45,"streak_colors":46,"luminescence":6,"uv":47,"cleavage":6,"cleavagetype":48,"fracturetype":49,"tenacity":50,"commentbreak":6,"opticaltype":51,"opticalsign":52,"opticalalpha":53,"opticalalpha2":6,"opticalalphaerror":6,"opticalbeta":54,"opticalbeta2":6,"opticalbetaerror":6,"opticalgamma":55,"opticalgamma2":6,"opticalgammaerror":6,"opticalomega":6,"opticalomega2":6,"opticalomegaerror":6,"opticalepsilon":6,"opticalepsilon2":6,"opticalepsilonerror":6,"opticaln":6,"opticaln2":6,"opticalnerror":6,"optical2vcalc":6,"optical2vcalc2":6,"optical2vcalcerror":6,"optical2vmeasured":56,"optical2vmeasured2":6,"optical2vmeasurederror":6,"rimin":57,"rimax":58,"opticaldispersion":6,"opticalpleochroism":6,"opticalpleochorismdesc":6,"opticalbirefringence":6,"opticalcomments":6,"opticalcolour":6,"opticalinternal":6,"opticaltropic":6,"opticalanisotropism":6,"opticalbireflectance":6,"opticalextinction":6,"opticalr":6,"specdispm":6,"ir":6,"electrical":6,"magnetism":6,"thermalbehaviour":6,"other":59,"industrial":6,"occurrence":60,"otheroccurrence":6,"type_specimen_store":61,"description_short":62,"aboutname":63,"rock_parent":6,"rock_parent2":6,"rock_root":9,"rock_bgs_code":6,"meteoritical_code":6,"updttime":64,"reviewed_at":6,"variety_of":6,"varieties":65,"group_members":66,"associates":67,"confused_with":68,"type_localities":69,"occurrence_total":34,"citations":76,"images":82,"structures":83,"synonyms":84,"language_names":87,"wikidata_qid":97,"texts":98},471432,"1:1:471432:9",null,"Králíkite","Kke",0,"mineral",16,false,"BaCl\u003Csub>2\u003C\u002Fsub>·2H\u003Csub>2\u003C\u002Fsub>O",[15,16,17,18],"Ba","Cl","O","H",[15,16,17,18],[15,16],[22],"APPROVED","3","B","Monoclinic",5,14,"0","6.7225","10.906","7.1301","91.101",8,1,6,4,"Spac group P21\u002Fn","It forms thin tabular crystals, usually imperfectly bounded, up to 25 μm long and only 3–5 μm thick, growing parallel to the surface of halite straws, more rarely also in central channels. It occurs as thin to thick tabular crystals; max. 160 × 120 × 10 μm in size forming crystalline aggregates up to 350 μm in size.",2.5,"3.103","Vitreous","Transparent","white","colorless",[44,43],[43],"Fluorescence was not recognized either on synthetic or natural phase.","None Observed","Conchoidal","brittle","Biaxial","+","1.635","1.646","1.660","83.75",1.635,1.66,"Králíkite is soluble in water and alcohol","The mineral is of the evaporite origin. It is subrecently formed in the environment of hypersaline brines stored in the Miocene aquifer entering both active and abandoned bituminous coal mine works. Requires low sulfate in the brines.","Type material is deposited in the collections of the Department of Mineralogy and Petrology, National Museum, Cirkusová 1740, Prague 9, Czech Republic, catalogue number P1P 19\u002F2019, and the Department of Mineralogy and Petrography, Moravian Museum, Zelný trh 6, Brno, Czech Republic, catalogue number A11366","Known synthetic analogue","mineral is named in honour of Ing. Jiří Králík, CSc. (1933–1986) who graduated at Vysoká škola báňská in Ostrava (Czechoslovakia) and worked there under the supervision of prof. dr. Jaroslav Kokta, renowned Czechoslovak mineralogist. Ing. Králík spent most of his professional career at Department of Mineralogy, Petrography and Geochemistry at Vysoká škola báňská in Ostrava, but also held lectures at the Havana University in Cuba between 1964 and 1965. His research focused on clay minerals, mostly applied to the Upper Silesian Basin, and biomineralization.","2026-03-25 14:07:32",[],[],[],[],[70],{"id":71,"txt":72,"latitude":73,"longitude":74,"country":75},446119,"Mining Plant I, ČSA Mine, Orlová, Karviná District, Moravian-Silesian Region, Czech Republic",49.8430556,18.4963889,"Czech Republic",[77],{"id":78,"year":79,"html":80,"doi":81},19772652,2026,"Matýsek, Dalibor; Jirásek, Jakub; Majzlan, Juraj; Filip, Jan; Osovský, Michal; Göttlicher, Jörg (2026) Evaporite minerals from the coal mines of the Czech part of the Upper Silesian Basin, including a new mineral králíkite (BaCl2·2H2O). \u003Ci>International Journal of Coal Geology\u003C\u002Fi>,  319. 104990 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.coal.2026.104990'>doi:10.1016\u002Fj.coal.2026.104990\u003C\u002Fa>","10.1016\u002Fj.coal.2026.104990",[],[],[85,86],"IMA2019-070a","Králíkiet",[88,92],{"lang":89,"names":90},"ca",[91],"kralikita",{"lang":93,"names":94},"de",[95,96],"IMA 2019-070a","Králíkit","Q130644218",{"history":6,"applications":6}]