[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:53410":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":20,"key_elements":21,"impurities":11,"cim":11,"ima_status":22,"ima_notes":11,"ima_history":11,"approval_year":24,"publication_year":25,"discovery_year":11,"strunz10ed1":26,"strunz10ed2":27,"strunz10ed3":27,"strunz10ed4":28,"dana8ed1":11,"dana8ed2":11,"dana8ed3":11,"dana8ed4":11,"csystem":29,"cclass":30,"spacegroup":31,"spacegroupset":32,"a":33,"b":34,"c":35,"alpha":11,"beta":36,"gamma":11,"aerror":37,"berror":38,"cerror":39,"alphaerror":11,"betaerror":39,"gammaerror":11,"va3":40,"z":13,"csmetamict":14,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":41,"hmin":30,"hmax":42,"hardtype":11,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":11,"dmeas2":11,"dcalc":43,"dmeaserror":11,"dcalcerror":39,"commentdense":11,"lustre":11,"lustretype":11,"commentluster":11,"diapheny":11,"streak":11,"colour":11,"commentcolor":11,"colors":11,"streak_colors":11,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"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":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":44,"industrial":11,"occurrence":45,"otheroccurrence":11,"type_specimen_store":46,"description_short":47,"aboutname":48,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":49,"reviewed_at":11,"variety_of":11,"varieties":50,"group_members":51,"associates":67,"confused_with":68,"type_localities":71,"occurrence_total":13,"citations":78,"images":91,"structures":92,"synonyms":93,"language_names":96,"wikidata_qid":110,"texts":111},53410,"1:1:53410:5","53f13f04-8ac4-440d-b05d-133dc0ebe927","Nixonite","Nix",0,"mineral",null,494675,2,false,"Na\u003Csub>2\u003C\u002Fsub>Ti\u003Csub>6\u003C\u002Fsub>O\u003Csub>13\u003C\u002Fsub>",[17,18,19],"Na","Ti","O",[17,18,19],[18],[23],"APPROVED",2018,2019,"4","C","25","Monoclinic",5,11,"C2\u002Fm ","15.363","3.7782","9.127","99.3",3,7,1,522.72,"Microcrystalline aggregates, 15 to 40 microns in length.",6,"3.51","The five main Raman peaks of nixonite, in order of decreasing intensity, are at 863, 280, 664, 135, and 113 cm–1.","Heavily metasomatized pyroxenite xenolith.","Mineralogical collections of the Royal Ontario Museum, 100 Queen’s Park, Toronto, Ontario M5S 2C6, Canada, catalogue number M59224","The Na analogue of jeppeite. Chemically related to freudenbergite and loparite-(Ce).","In honour of Peter H. Nixon (1935–2025), who was Professor of Mantle Geology at Leeds University, UK, and is now retired. He authored two very influential books on mantle petrology and, in addition to a lifetime of work on kimberlites and their mantle- and deep crustal-derived xenoliths, he also named knorringite and described the second occurrence of yimengite. Peter Nixon was a visionary who brought the scientific community’s attention to the growing evidence of orogenically-emplaced mantle rocks from the diamond stability field, co-authoring numerous key publications that provided the first strong evidence for this process.","2025-11-29 18:36:51",[],[52,59],{"id":53,"name":54,"entrytype":9,"csystem":29,"ima_formula":11,"mindat_formula":55,"hmin":30,"hmax":56,"dmeas":11,"dcalc":57,"primary_image_id":58},494657,"Hopmannite","Ba\u003Csub>2\u003C\u002Fsub>(Ti\u003Csub>5\u003C\u002Fsub>Fe)O\u003Csub>13\u003C\u002Fsub>",5.5,"4.15",9416,{"id":60,"name":61,"entrytype":9,"csystem":29,"ima_formula":62,"mindat_formula":63,"hmin":30,"hmax":42,"dmeas":64,"dcalc":65,"primary_image_id":66},2089,"Jeppeite","(K,Ba)\u003Csub>2\u003C\u002Fsub>(Ti,Fe\u003Csup>3+\u003C\u002Fsup>)\u003Csub>6\u003C\u002Fsub>O\u003Csub>13\u003C\u002Fsub>","K\u003Csub>2\u003C\u002Fsub>Ti\u003Csub>6\u003C\u002Fsub>O\u003Csub>13\u003C\u002Fsub>","3.94","3.972",12588,[],[69,70],{"id":53,"name":54,"entrytype":9,"csystem":29,"ima_formula":11,"mindat_formula":55,"hmin":30,"hmax":56,"dmeas":11,"dcalc":57,"primary_image_id":58},{"id":60,"name":61,"entrytype":9,"csystem":29,"ima_formula":62,"mindat_formula":63,"hmin":30,"hmax":42,"dmeas":64,"dcalc":65,"primary_image_id":66},[72],{"id":73,"txt":74,"latitude":75,"longitude":76,"country":77},309765,"Darby kimberlite field, Kitikmeot Region, Nunavut, Canada",67.3991667,-93.3538889,"Canada",[79,83,87],{"id":80,"year":25,"html":81,"doi":82},245135,"Miyawaki, Ritsuro, Hatert, Frédéric, Pasero, Marco, Mills, Stuart J. (2019) New minerals and nomenclature modifications approved in 2019. CNMNC Newsletter No 48. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  83 (2) 315-317 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fmgm.2019.23'>doi:10.1180\u002Fmgm.2019.23\u003C\u002Fa>","10.1180\u002Fmgm.2019.23",{"id":84,"year":25,"html":85,"doi":86},398864,"Anzolini, Chiara, Wang, Fei, Harris, Garrett A., Locock, Andrew J., Zhang, Dongzhou, Nestola, Fabrizio, Peruzzo, Luca, Jacobsen, Steven D., Pearson, D.Graham (2019) Nixonite, Na2Ti6O13, a new mineral from a metasomatized mantle garnet pyroxenite from the western Rae Craton, Darby kimberlite field, Canada. \u003Ci>American Mineralogist\u003C\u002Fi>,  104 (9) 1336-1344 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2019-7023'>doi:10.2138\u002Fam-2019-7023\u003C\u002Fa>","10.2138\u002Fam-2019-7023",{"id":88,"year":89,"html":90,"doi":11},16966320,2020,"(2020) Nixonite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fnixonite.pdf' class='refpdflink'>\u003C\u002Fa>",[],[],[94,95],"IMA2018-133","Nixoniet",[97,101,106],{"lang":98,"names":99},"ca",[100],"nixonita",{"lang":102,"names":103},"de",[104,105],"IMA 2018-133","Nixonit",{"lang":107,"names":108},"eu",[109],"Nixonita","Q66477033",{"history":11,"applications":11}]