[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:55438":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":11,"ima_formula":15,"elements":16,"sigelements":19,"key_elements":20,"impurities":11,"cim":11,"ima_status":21,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":23,"discovery_year":11,"strunz10ed1":24,"strunz10ed2":25,"strunz10ed3":26,"strunz10ed4":11,"dana8ed1":11,"dana8ed2":11,"dana8ed3":11,"dana8ed4":11,"csystem":27,"cclass":28,"spacegroup":11,"spacegroupset":26,"a":29,"b":30,"c":31,"alpha":11,"beta":32,"gamma":11,"aerror":33,"berror":33,"cerror":33,"alphaerror":11,"betaerror":34,"gammaerror":11,"va3":11,"z":11,"csmetamict":14,"commentcrystal":35,"twinning":11,"tranglide":11,"parting":36,"epitaxidescription":11,"morphology":11,"tlform":37,"hmin":34,"hmax":38,"hardtype":11,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":11,"dmeas2":11,"dcalc":39,"dmeaserror":11,"dcalcerror":11,"commentdense":40,"lustre":11,"lustretype":41,"commentluster":11,"diapheny":42,"streak":43,"colour":44,"commentcolor":11,"colors":45,"streak_colors":49,"luminescence":11,"uv":50,"cleavage":11,"cleavagetype":51,"fracturetype":11,"tenacity":52,"commentbreak":11,"opticaltype":11,"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":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":53,"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":11,"industrial":11,"occurrence":54,"otheroccurrence":11,"type_specimen_store":55,"description_short":56,"aboutname":57,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":58,"reviewed_at":11,"variety_of":11,"varieties":59,"group_members":60,"associates":61,"confused_with":62,"type_localities":63,"occurrence_total":70,"citations":71,"images":89,"structures":100,"synonyms":107,"language_names":110,"wikidata_qid":123,"texts":124},55438,"1:1:55438:5","4f922dc0-9629-4a09-830d-dce1ffecbe28","Liguowuite","Lgw",0,"mineral",null,55904,11,false,"WO\u003Csub>3\u003C\u002Fsub>",[17,18],"O","W",[17,18],[18],[22],"APPROVED",2022,"4","E","0","Monoclinic",5,"7.3258","7.5477","7.7113","90.678",2,3,"the space group is P2\u003Csub>1\u003C\u002Fsub>\u002Fn","None observed","Prismatic crystals, 0.05 to 0.1 mm in diameter; triclinic pseudomorphism is known, due to the presence of \"nanoparticles with many cracks and nanovoids\".",4,"7.22","Calculated value based on the empirical formula.","Greasy","Transparent","White","Greenish yellow",[46,47,48],"yellow","green","white",[48],"Not fluorescent.","None Observed","brittle","An average refraction index of 2.24 is calculated based on the Gladstone–Dale relationship.","Neoproterozoic Sinian biotite-quartz monzonite.","Mineralogical collections of (1) the Geological Museum of China, Xisi, Yangrou Hutong No. 15, Beijing 100083, People’s Republic of China, catalogue number M16121 (holotype), and (2) the Crystal Structure Laboratory, China University of Geosciences, Beijing 100083, People’s Republic of China, catalogue number NY-5-3Z (cotype).","Known synthetic analogue. Perovskite-type structure.\r\n\r\nThe first example of A-site vacant single oxide, thus formulating a new perovskite subgroup.\r\n\r\nThe structure is based on corner-sharing, distorted and tilted WO6 octahedra, with the W atoms being...","Named in honor of after Li Guowu (李国武) (1964–), China University of Geosciences, Beijing, China, in recognition of his great contributions to new mineral research, including tewite and wumuite from the area of the type locality.","2026-03-17 14:16:41",[],[],[],[],[64],{"id":65,"txt":66,"latitude":67,"longitude":68,"country":69},263087,"Nanyang, Huaping County, Lijiang, Yunnan, China",26.7716667,101.4536111,"China",1,[72,77,80,84],{"id":73,"year":74,"html":75,"doi":76},16139477,2021,"Miyawaki, Ritsuro, Hatert, Frédéric, Pasero, Marco, Mills, Stuart J. (2021) IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) – Newsletter 61. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  33 (3) 299-304 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-33-299-2021'>doi:10.5194\u002Fejm-33-299-2021\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fejm.copernicus.org\u002Farticles\u002F33\u002F299\u002F2021\u002Fejm-33-299-2021.pdf' class='refpdflink'>\u003C\u002Fa>","10.5194\u002Fejm-33-299-2021",{"id":78,"year":23,"html":79,"doi":11},16965594,"(2022) Liguowuite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fhandbookofmineralogy.org\u002Fpdfs\u002FLiguowuite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":81,"year":23,"html":82,"doi":83},17068367,"Xue, Yuan, Sun, Ningyue, He, Hongping, Chen, Aiqing, Yang, Yiping (2022) Liguowuite, WO\u003Csub>3\u003C\u002Fsub>, a new member of the \u003Ci>A\u003C\u002Fi>-site vacant perovskite type minerals from the Panzhihua–Xichang region, China. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  34 (1) 95-108 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-34-95-2022'>doi:10.5194\u002Fejm-34-95-2022\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fejm.copernicus.org\u002Farticles\u002F34\u002F95\u002F2022\u002Fejm-34-95-2022.pdf' class='refpdflink'>\u003C\u002Fa>","10.5194\u002Fejm-34-95-2022",{"id":85,"year":86,"html":87,"doi":88},19172552,2025,"Bosi, Ferdinando; Hatert, Frédéric; Meisser, Nicolas; Pasero, Marco; Mills, Stuart (2025) IMA-CNMNC guidelines for assessing the natural geological origin of minerals. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  37 (6). 871-876 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-37-871-2025'>doi:10.5194\u002Fejm-37-871-2025\u003C\u002Fa>","10.5194\u002Fejm-37-871-2025",[90],{"id":91,"source_url":92,"license_code":93,"credit_html":94,"title":95,"description":96,"author":97,"original_width":98,"original_height":99},14497,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=124136457","CC BY-SA 4.0","Yuan Xue, Ningyue Sun, Hongping He, Aiqing Chen and Yiping Yang, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=124136457\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","BSE images of liguowuite (a).png","Photo of the liguowuite. (a) Yellow grains of liguowuite. The liguowuite grain is composed of nanoparticles with many cracks and nanovoids. \nThe image is published in an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (\u003Ca rel=\"nofollow\" class=\"external free\" href=\"https:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby\u002F4.0\u002F\">https:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby\u002F4.0\u002F\u003C\u002Fa>).","Yuan Xue, Ningyue Sun, Hongping He, Aiqing Chen and Yiping Yang",976,738,[101],{"id":102,"url":103,"label":104,"formula":105,"spacegroup":106,"year":23},7686,"\u002Fcif\u002F7686.cif","Xue 2022","W O3","P 1 21\u002Fn 1",[108,109],"IMA2020-097","Liguowuiet",[111,115,120],{"lang":112,"names":113},"ca",[114],"liguowuïta",{"lang":116,"names":117},"de",[118,119],"IMA 2020-097","Liguowuit",{"lang":121,"names":122},"it",[7],"Q107303628",{"history":11,"applications":11}]