[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:40150":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":18,"key_elements":11,"impurities":11,"cim":11,"ima_status":19,"ima_notes":11,"ima_history":11,"approval_year":21,"publication_year":22,"discovery_year":11,"strunz10ed1":23,"strunz10ed2":24,"strunz10ed3":24,"strunz10ed4":25,"dana8ed1":23,"dana8ed2":23,"dana8ed3":26,"dana8ed4":27,"csystem":28,"cclass":29,"spacegroup":30,"spacegroupset":31,"a":32,"b":11,"c":33,"alpha":11,"beta":11,"gamma":11,"aerror":34,"berror":11,"cerror":35,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":11,"csmetamict":13,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":36,"tlform":37,"hmin":38,"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":11,"lustre":11,"lustretype":40,"commentluster":11,"diapheny":41,"streak":42,"colour":43,"commentcolor":11,"colors":44,"streak_colors":47,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":48,"fracturetype":49,"tenacity":50,"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":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":51,"otheroccurrence":11,"type_specimen_store":52,"description_short":53,"aboutname":54,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":55,"reviewed_at":11,"variety_of":11,"varieties":56,"group_members":57,"associates":58,"confused_with":59,"type_localities":60,"occurrence_total":67,"citations":68,"images":105,"structures":116,"synonyms":137,"language_names":141,"wikidata_qid":174,"texts":175},40150,"1:1:40150:6","374640c0-fbb0-4bb1-817c-0be1316438d7","Linzhiite","Lzh",0,"mineral",null,36,false,"FeSi\u003Csub>2\u003C\u002Fsub>",[16,17],"Fe","Si",[16,17],[20],"APPROVED",2010,2012,"1","B","20","33","3","Tetragonal",27,181,"P4\u002Fmmm ","2.725","5.202",3,10,"Irregular grains ranging from 0.04 to 0.5 mm in diameter.","As irregular grains ranging from 0.04 to 0.5 mm in diameter and intergrowths with zangboite and native silicon.",6.5,"4.972","Metallic","Opaque","Greyish-black","Steel grey",[45,46],"gray","black",[45,46],"None Observed","Conchoidal","brittle","In a podiform chromitite from the Luobusha ophiolite, Tibet.","Geological Museum of China (specimen no. M11799).\r\nInstitute of Geology, Chinese Academy of Geological Sciences, Beijing, P.R. China, catalog no. 97-6.","Originally reported  as \"ferdisilicite\" from Poltava series, Zachativsk station, Donets (Donetsk) region, Donets'k Oblast' (Donetsk Oblast'), Ukraine.\r\n\r\nOne of many natural Fe-Si phases; beside the approved species (listed below) you may want to compa...","First described, without CNMMN approval as \"Ferdisilicite\" (FeSi2), the first described member of the Fe–Si alloy mineral series by Gevork’yan (1969).  Redefined as a new mineral, revalidated with the new name linzhiite with a CNMNC approval (IMA 2010-011). Linzhiite is named for the Linzhi Prefecture, which is situated close to the type locality.","2026-03-08 17:00:36",[],[],[],[],[61],{"id":62,"txt":63,"latitude":64,"longitude":65,"country":66},5457,"Luobusha ophiolite (\"Luobusa ophiolite\"), Qusum Co. (Qusong Co.), Shannan Prefecture (Lhokha Prefecture; Lhoka Prefecture), Tibet, China",29.1827778,92.2966667,"China",8,[69,74,78,81,85,89,93,97,101],{"id":70,"year":71,"html":72,"doi":73},16490733,1960,"Aronsson, Bertil, Templeton, David H., Rundqvist, S., Varde, E., Westin, Gertrud (1960) A Note on the Compositions and Crystal Structures of MnB2, Mn3Si, Mn5Si3, and FeSi2. \u003Ci>Acta Chemica Scandinavica\u003C\u002Fi>, 14. 1414-1418 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3891\u002Facta.chem.scand.14-1414'>doi:10.3891\u002Facta.chem.scand.14-1414\u003C\u002Fa>","10.3891\u002Facta.chem.scand.14-1414",{"id":75,"year":76,"html":77,"doi":11},525294,1969,"Fleischer, Michael (1969) New Mineral Names. \u003Ci>American Mineralogist\u003C\u002Fi>,  54 (11-12) 1737-1742 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM54\u002FAM54_1737.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":79,"year":76,"html":80,"doi":11},16060024,"Gevork’yan, V.Kh. (1969) The occurrence of natural ferrosilicon in the northern Azov region. Doklady Akademii Nauk SSSR: 185: 416-418.",{"id":82,"year":83,"html":84,"doi":11},16138274,1985,"Wei, J., Zheng, Z., Chen, S. (1985) A study on ferdisilicite and its geological implications. Acta Mineralogica Sinica: 2: 184-186.",{"id":86,"year":87,"html":88,"doi":11},16138275,1991,"Hu, X. (1991) A preliminary study on ferrosilicium from the Proterozoic, southwestern Zhejiang Province. Acta Mineralogica Sinica: 11(3): 285-289 (in Chinese with English abstract).",{"id":90,"year":21,"html":91,"doi":92},16013729,"Williams, P. A., Hatert, F., Pasero, M., Mills, S. J. (2010) New minerals and nomenclature modifications approved in 2010. CNMNC Newsletter No 3. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  74 (3) 577-579 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fs0026461x00054979'>doi:10.1180\u002Fs0026461x00054979\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Forbi.uliege.be\u002Fbitstream\u002F2268\u002F77811\u002F1\u002FCNMNC%20NEWSLETTER%203.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fs0026461x00054979",{"id":94,"year":22,"html":95,"doi":96},129180,"Li, Guowu, Bai, Wenji, Shi, Nicheng, Fang, Qinsong, Xiong, Ming, Yang, Jingsui, Ma, Zhesheng, Rong, He (2012) Linzhiite, FeSi2, a redefined and revalidated new mineral species from Luobusha, Tibet, China. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  24 (6) 1047-1052 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1127\u002F0935-1221\u002F2012\u002F0024-2237'>doi:10.1127\u002F0935-1221\u002F2012\u002F0024-2237\u003C\u002Fa>","10.1127\u002F0935-1221\u002F2012\u002F0024-2237",{"id":98,"year":99,"html":100,"doi":11},16965611,2014,"(2014) Linzhiite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Flinzhiite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":102,"year":99,"html":103,"doi":104},397587,"Camara, F.; Gatta, G. D.; Uvarova, Y.; Gagne, O. C.; Belakovskiy, D. I. (2014) New Mineral Names. \u003Ci>American Mineralogist\u003C\u002Fi>,  99 (7). 1511-1518 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2014.646'>doi:10.2138\u002Fam.2014.646\u003C\u002Fa>","10.2138\u002Fam.2014.646",[106],{"id":107,"source_url":108,"license_code":109,"credit_html":110,"title":111,"description":112,"author":113,"original_width":114,"original_height":115},14576,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=79585173","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=79585173\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Linzhiite.jpg","Silvery metallic nugget of the extremely rare silicon-iron intermetallic linzhiite (FeSi2). An analyzed specimen from Zachativsk Station, Donetsk Oblast', Ukraine. Linzhiite is a mineral from Group I .Elements, and is very rarely seen in the mineral market, much less in analyzed specimens. It is a very sought after mineral species from Group I collectors.","David Hospital",709,667,[117,123,128,132],{"id":118,"url":119,"label":120,"formula":121,"spacegroup":122,"year":22},7773,"\u002Fcif\u002F7773.cif","Li 2012","Fe Si2","P 4\u002Fm m m",{"id":124,"url":125,"label":126,"formula":121,"spacegroup":122,"year":127},7774,"\u002Fcif\u002F7774.cif","Li 2007",2007,{"id":129,"url":130,"label":131,"formula":121,"spacegroup":122,"year":71},7775,"\u002Fcif\u002F7775.cif","Aronsson 1960",{"id":133,"url":134,"label":135,"formula":121,"spacegroup":122,"year":136},7776,"\u002Fcif\u002F7776.cif","Phragmen 1923",1923,[138,139,140],"Ferdisilicite","IMA2010-011","Linzhiiet",[142,146,151,155,158,162,167,171],{"lang":143,"names":144},"ca",[145],"linzhiïta",{"lang":147,"names":148},"de",[149,150],"IMA 2010-011","Linzhiit",{"lang":152,"names":153},"eu",[154],"Linzhiita",{"lang":156,"names":157},"it",[138,7],{"lang":159,"names":160},"ta",[139,161],"இலின்சைட்டு",{"lang":163,"names":164},"uk",[165,166],"Лінжиїт","Ліньчжиїт",{"lang":168,"names":169},"zh",[170],"林芝矿",{"lang":172,"names":173},"zh-cn",[170],"Q3833146",{"history":11,"applications":11}]