[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:47800":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":14,"elements":15,"sigelements":19,"key_elements":20,"impurities":11,"cim":11,"ima_status":21,"ima_notes":11,"ima_history":11,"approval_year":23,"publication_year":24,"discovery_year":11,"strunz10ed1":25,"strunz10ed2":26,"strunz10ed3":27,"strunz10ed4":28,"dana8ed1":29,"dana8ed2":29,"dana8ed3":29,"dana8ed4":29,"csystem":30,"cclass":31,"spacegroup":32,"spacegroupset":29,"a":33,"b":11,"c":34,"alpha":11,"beta":11,"gamma":11,"aerror":35,"berror":11,"cerror":35,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":11,"csmetamict":13,"commentcrystal":36,"twinning":11,"tranglide":11,"parting":37,"epitaxidescription":11,"morphology":11,"tlform":38,"hmin":39,"hmax":40,"hardtype":11,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":41,"dmeas":11,"dmeas2":11,"dcalc":42,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":11,"commentluster":11,"diapheny":11,"streak":11,"colour":43,"commentcolor":11,"colors":44,"streak_colors":11,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":46,"fracturetype":11,"tenacity":11,"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":11,"opticalcolour":47,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":48,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":49,"industrial":11,"occurrence":50,"otheroccurrence":11,"type_specimen_store":51,"description_short":52,"aboutname":53,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":54,"reviewed_at":11,"variety_of":11,"varieties":55,"group_members":56,"associates":57,"confused_with":58,"type_localities":72,"occurrence_total":79,"citations":80,"images":98,"structures":99,"synonyms":106,"language_names":109,"wikidata_qid":123,"texts":124},47800,"1:1:47800:3","acdf2d2b-6c1f-460a-8913-2f258dff6801","Wangdaodeite","Wdd",0,"mineral",null,13,false,"FeTiO\u003Csub>3\u003C\u002Fsub>",[16,17,18],"Fe","Ti","O",[16,17,18],[17],[22],"APPROVED",2016,2020,"4","C","B","95","0","Trigonal",11,85,"5.13","13.78",1,"LiNbO3-type FeTiO3 can be conserved at ambient pressure and has found attention in solid state physics because of its multiferroic behavior","None observed","Irregular particles (2–20 microns in size)",5,5.5,"Estimated by similar relief to associated ilmenite of polished section","4.72","Gray (in reflected polarized light)",[45],"gray","None Observed","Gray","(21.0, 18.7) 470,\r\n(19.9, 17.9) 546,\r\n(20.1, 18.0) 589,\r\n(20.4, 18.3) 650","the Raman peak at 738–740 cm−1 is indicative for this phase","In shock veins of the Suizhou L6 meteorite.","In the mineralogical collections of  1) the Geological Museum, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, China, catalogue number 15010, 2)the Mineral Museum of the University of Arizona, USA, catalogue number 21312, and the RRUFF.","A high-pressure high-temperature polymorph with a LiNbO3-type structure. The P–T conditions for the formation of wangdaodeite are estimated to be 20–24 GPa and >1200°C.","Named in honor of Daode Wang (王道德), Department of Meteoritics and Cosmochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences (CAS), for the systematic study of Chinese meteorites in general and Antarctic meteorites in particular.","2025-12-05 17:09:08",[],[],[],[59,68],{"id":60,"name":61,"entrytype":9,"csystem":30,"ima_formula":62,"mindat_formula":63,"hmin":39,"hmax":64,"dmeas":65,"dcalc":66,"primary_image_id":67},2013,"Ilmenite","Fe\u003Csup>2+\u003C\u002Fsup>Ti\u003Csup>4+\u003C\u002Fsup>O\u003Csub>3\u003C\u002Fsub>","Fe\u003Csup>2+\u003C\u002Fsup>TiO\u003Csub>3\u003C\u002Fsub>",6,"4.68","4.789",29925,{"id":69,"name":70,"entrytype":9,"csystem":71,"ima_formula":14,"mindat_formula":14,"hmin":11,"hmax":11,"dmeas":11,"dcalc":11,"primary_image_id":11},53253,"Liuite","Orthorhombic",[73],{"id":74,"txt":75,"latitude":76,"longitude":77,"country":78},5562,"Suizhou meteorite (Suizhou L6 chondrite), Xihe, Zengdu District, Suizhou, Hubei, China",31.6166667,113.4666667,"China",3,[81,85,90,94],{"id":82,"year":23,"html":83,"doi":84},244799,"Hålenius, U., Hatert, F., Pasero, M., Mills, S. J. (2016) New minerals and nomenclature modifications approved in 2016, CNMNC Newsletter no 31. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  80 (4) 691-697 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2016.080.083'>doi:10.1180\u002Fminmag.2016.080.083\u003C\u002Fa>","10.1180\u002Fminmag.2016.080.083",{"id":86,"year":87,"html":88,"doi":89},335203,2019,"Xie, Xiande; Gu, Xiangping; Yang, Hexiong; Chen, Ming; Li, Kai (2019) Wangdaodeite, the LiNbO\u003Csub>3\u003C\u002Fsub>‐structured high‐pressure polymorph of ilmenite, a new mineral from the Suizhou L6 chondrite. \u003Ci>Meteoritics & Planetary Science\u003C\u002Fi>,  55 (1). 184-192 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1111\u002Fmaps.13426'>doi:10.1111\u002Fmaps.13426\u003C\u002Fa>","10.1111\u002Fmaps.13426",{"id":91,"year":24,"html":92,"doi":93},13422739,"Tschauner, Oliver, Ma, Chi, Newville, Matthew G., Lanzirotti, Antonio (2020) Structure Analysis of Natural Wangdaodeite—LiNbO3-Type FeTiO3. \u003Ci>Minerals\u003C\u002Fi>, 10 (12) 1072 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3390\u002Fmin10121072'>doi:10.3390\u002Fmin10121072\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.mdpi.com\u002F2075-163X\u002F10\u002F12\u002F1072\u002Fpdf?version=1606720256' class='refpdflink'>\u003C\u002Fa>","10.3390\u002Fmin10121072",{"id":95,"year":96,"html":97,"doi":11},16968064,2021,"(2021) Wangdaodeite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002FWangdaodeite.pdf' class='refpdflink'>\u003C\u002Fa>",[],[100],{"id":101,"url":102,"label":103,"formula":104,"spacegroup":105,"year":24},14389,"\u002Fcif\u002F14389.cif","Tschauner 2020","(Fe.92 Mn.08) Ti O3","R -3",[107,108],"IMA2016-007","Wangdaodeiet",[110,114,119],{"lang":111,"names":112},"ca",[113],"wangdaodeïta",{"lang":115,"names":116},"de",[117,118],"IMA 2016-007","Wangdaodeit",{"lang":120,"names":121},"eu",[122],"Wangdaodeita","Q26202498",{"history":11,"applications":11}]