[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:26781":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":8,"polytypeof":8,"groupid":8,"weighting":12,"nolocadd":13,"blacklisted":13,"mindat_formula":14,"mindat_formula_note":8,"ima_formula":8,"elements":15,"sigelements":19,"key_elements":20,"impurities":8,"cim":8,"ima_status":8,"ima_notes":8,"ima_history":8,"approval_year":8,"publication_year":8,"discovery_year":8,"strunz10ed1":21,"strunz10ed2":21,"strunz10ed3":21,"strunz10ed4":8,"dana8ed1":21,"dana8ed2":21,"dana8ed3":21,"dana8ed4":21,"csystem":8,"cclass":8,"spacegroup":8,"spacegroupset":21,"a":8,"b":8,"c":8,"alpha":8,"beta":8,"gamma":8,"aerror":8,"berror":8,"cerror":8,"alphaerror":8,"betaerror":8,"gammaerror":8,"va3":8,"z":8,"csmetamict":13,"commentcrystal":8,"twinning":8,"tranglide":8,"parting":8,"epitaxidescription":8,"morphology":8,"tlform":8,"hmin":8,"hmax":8,"hardtype":8,"vhnmin":21,"vhnmax":21,"vhnerror":8,"vhng":8,"vhns":8,"commenthard":8,"dmeas":21,"dmeas2":21,"dcalc":21,"dmeaserror":8,"dcalcerror":8,"commentdense":8,"lustre":8,"lustretype":8,"commentluster":8,"diapheny":8,"streak":8,"colour":8,"commentcolor":8,"colors":8,"streak_colors":8,"luminescence":8,"uv":22,"cleavage":8,"cleavagetype":8,"fracturetype":8,"tenacity":8,"commentbreak":8,"opticaltype":8,"opticalsign":8,"opticalalpha":8,"opticalalpha2":8,"opticalalphaerror":8,"opticalbeta":8,"opticalbeta2":8,"opticalbetaerror":8,"opticalgamma":8,"opticalgamma2":8,"opticalgammaerror":8,"opticalomega":8,"opticalomega2":21,"opticalomegaerror":8,"opticalepsilon":8,"opticalepsilon2":21,"opticalepsilonerror":8,"opticaln":8,"opticaln2":8,"opticalnerror":8,"optical2vcalc":8,"optical2vcalc2":8,"optical2vcalcerror":8,"optical2vmeasured":8,"optical2vmeasured2":8,"optical2vmeasurederror":8,"rimin":8,"rimax":8,"opticaldispersion":8,"opticalpleochroism":8,"opticalpleochorismdesc":8,"opticalbirefringence":8,"opticalcomments":8,"opticalcolour":8,"opticalinternal":8,"opticaltropic":8,"opticalanisotropism":8,"opticalbireflectance":8,"opticalextinction":8,"opticalr":8,"specdispm":8,"ir":8,"electrical":8,"magnetism":8,"thermalbehaviour":8,"other":8,"industrial":8,"occurrence":8,"otheroccurrence":8,"type_specimen_store":8,"description_short":8,"aboutname":23,"rock_parent":8,"rock_parent2":8,"rock_root":24,"rock_bgs_code":8,"meteoritical_code":8,"updttime":25,"reviewed_at":8,"variety_of":26,"varieties":34,"group_members":35,"associates":36,"confused_with":37,"type_localities":38,"occurrence_total":39,"citations":40,"images":49,"structures":50,"synonyms":51,"language_names":52,"wikidata_qid":8,"texts":53},26781,"1:1:26781:4","e32fe4de-923c-4a14-8a5a-83a9a77d23e9","Beta-Willemite",null,2,"variety",4292,71,false,"Zn\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub>",[16,17,18],"Si","Zn","O",[16,17,18],[17],"0","Golden-yellow (LW & SW UV).","Named by Arthur Schleede and Arno Gruhl in 1923 for a supposed second structural (metastable) state of willemite, a claim that was many years in verification. Taylor (1962) suggested that the mineral beta-willemite has essentially the same structure as willemite, but does show some structural abnormalities which still have not been well-defined. Beta-willemite does show anomalous yellow, rather than green, fluorescence in ultraviolet light and the implication is that the difference in the ultraviolet luminescence is related to subtle, but consistent, structural differences.",0,"2025-08-11 12:14:51",{"id":11,"name":27,"entrytype":24,"csystem":28,"ima_formula":14,"mindat_formula":14,"hmin":29,"hmax":29,"dmeas":30,"dcalc":31,"strunz10ed1":32,"primary_image_id":33},"Willemite","Trigonal",5.5,"3.89","4.224","9",30976,[],[],[],[],[],1,[41,45],{"id":42,"year":43,"html":44,"doi":8},16134052,1923,"\u003Cstrong>Arthur Schleede and Arno Gruhl \u003C\u002Fstrong>(1923)\u003Cem> Über röntgenographische Beobachtungen an Luminescenzfähigen Zinksilikat,\u003C\u002Fem> \u003Cstrong>Deutsche Bunsen-Gesellschaft für Angewandte Physikalische Chemie; journal later incorporated as Zeitschrift für Elektrochemie und angewandte physikalische Chemie,\u003C\u002Fstrong> v. 29, p. 41-412.",{"id":46,"year":47,"html":48,"doi":8},523745,1962,"Taylor, H. F. W. (1962) The dehydration of hemimorphite. \u003Ci>American Mineralogist\u003C\u002Fi>,  47 (7-8) 932-944 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM47\u002FAM47_932.pdf' class='refpdflink'>\u003C\u002Fa>",[],[],[],[],{"history":8,"applications":8}]