[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:46073":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":15,"ima_formula":14,"elements":16,"sigelements":23,"key_elements":11,"impurities":11,"cim":11,"ima_status":24,"ima_notes":11,"ima_history":11,"approval_year":26,"publication_year":27,"discovery_year":11,"strunz10ed1":28,"strunz10ed2":29,"strunz10ed3":30,"strunz10ed4":31,"dana8ed1":32,"dana8ed2":32,"dana8ed3":32,"dana8ed4":32,"csystem":33,"cclass":34,"spacegroup":11,"spacegroupset":32,"a":35,"b":36,"c":37,"alpha":11,"beta":11,"gamma":11,"aerror":34,"berror":38,"cerror":39,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":40,"z":39,"csmetamict":13,"commentcrystal":41,"twinning":11,"tranglide":11,"parting":42,"epitaxidescription":11,"morphology":43,"tlform":44,"hmin":45,"hmax":46,"hardtype":11,"vhnmin":47,"vhnmax":11,"vhnerror":11,"vhng":48,"vhns":11,"commenthard":11,"dmeas":11,"dmeas2":11,"dcalc":49,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":50,"commentluster":11,"diapheny":51,"streak":52,"colour":53,"commentcolor":11,"colors":54,"streak_colors":57,"luminescence":11,"uv":58,"cleavage":11,"cleavagetype":59,"fracturetype":60,"tenacity":61,"commentbreak":11,"opticaltype":62,"opticalsign":63,"opticalalpha":11,"opticalalpha2":11,"opticalalphaerror":11,"opticalbeta":11,"opticalbeta2":11,"opticalbetaerror":11,"opticalgamma":11,"opticalgamma2":11,"opticalgammaerror":11,"opticalomega":64,"opticalomega2":11,"opticalomegaerror":65,"opticalepsilon":66,"opticalepsilon2":11,"opticalepsilonerror":65,"opticaln":11,"opticaln2":11,"opticalnerror":11,"optical2vcalc":11,"optical2vcalc2":11,"optical2vcalcerror":11,"optical2vmeasured":11,"optical2vmeasured2":11,"optical2vmeasurederror":11,"rimin":67,"rimax":68,"opticaldispersion":11,"opticalpleochroism":69,"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":70,"otheroccurrence":11,"type_specimen_store":71,"description_short":72,"aboutname":73,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":74,"reviewed_at":11,"variety_of":11,"varieties":75,"group_members":76,"associates":77,"confused_with":78,"type_localities":79,"occurrence_total":86,"citations":87,"images":105,"structures":106,"synonyms":107,"language_names":110,"wikidata_qid":128,"texts":129},46073,"1:1:46073:0","aaa45033-8f89-4168-a84c-02361a891e13","Flamite","Fmt",0,"mineral",null,32,false,"Ca\u003Csub>8-x\u003C\u002Fsub>(Na,K)\u003Csub>x\u003C\u002Fsub>(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>4-x\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>x\u003C\u002Fsub>","From structure analysis (Gfeller et al. 2015) ",[17,18,19,20,21,22],"Ca","Na","Si","O","P","K",[17,18,19,20,21],[25],"APPROVED",2013,2015,"9","A","H","45","0","Orthorhombic",6,"9.3845","21.7310","6.8346",14,4,1393.81,"Space group is Pnm2\u003Csub>1\u003C\u002Fsub>; previously though to be hexagonal, sp. gr. P6\u003Csub>3\u003C\u002Fsub>","None","Flamite occurs as 100-250 μm anhedral crystals with typical lamellar textures. ","Regular lamellar intergrowths with partially hydrated larnite; the particular lamellae differ in terms of Na, K, and P substitution",5,5.5,"706",50,"3.264","Vitreous","Transparent","white","Greyish to yellowish",[55,56,52],"gray","yellow",[52],"Non-fluorescent under ultraviolet light","None Observed","Irregular\u002FUneven","brittle","Uniaxial","+","1.643",2,"1.640",1.64,1.643,"Non-pleochroic","Ca- and Al-rich paralava (pyrometamorphic rocks)","Type material is deposited in the collections of the Central Siberian Geological Museum, V.S. Sobolev Institute of Geology and Mineralogy, 3 Ac. Koptyuga Avenue, Novosibirsk, 630090 Russia, catalogue number XIII-341\u002F1","A natural analogue of the P,Na,K-stabilised α-Ca2SiO4 modification which, if chemically pure, is only stable at high temperatures (1425-2150°C) and cannot be quenched. In the cement industry (clinker production) the α-Ca2SiO4 is stabilised by Ba, Sr, P...","The name is derived from ‘flame’ and refers to the origin of the mineral by ultrahigh-temperature combustion metamorphism triggered by fossil-fuel ignition.","2025-08-11 12:15:13",[],[],[],[],[80],{"id":81,"txt":82,"latitude":83,"longitude":84,"country":85},259776,"Southern Hatrurim Basin, Hatrurim Basin, Tamar Regional Council, Beersheba Subdistrict, Southern District, Israel",31.1738889,35.2919444,"Israel",12,[88,93,97,101],{"id":89,"year":90,"html":91,"doi":92},244518,2014,"Williams, P. A., Hatert, F., Pasero, M., Mills, S. J. (2014) New minerals and nomenclature modifications approved in 2014, CNMNC Newsletter No 20. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  78 (3) 549-558 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2014.078.3.05'>doi:10.1180\u002Fminmag.2014.078.3.05\u003C\u002Fa>","10.1180\u002Fminmag.2014.078.3.05",{"id":94,"year":27,"html":95,"doi":96},244654,"Sokol, E. V.; Seryotkin, Y. V.; Kokh, S. N.; Vapnik, Ye.; Nigmatulina, E. N.; Goryainov, S. V.; Belogub, E. V.; Sharygin, V. V. (2015) Flamite, (Ca,Na,K)\u003Csub>2\u003C\u002Fsub>(Si,P)O\u003Csub>4\u003C\u002Fsub>, a new mineral from ultrahigh-temperature combustion metamorphic rocks, Hatrurim Basin, Negev Desert, Israel. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  79 (3). 583-596 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2015.079.3.05'>doi:10.1180\u002Fminmag.2015.079.3.05\u003C\u002Fa>","10.1180\u002Fminmag.2015.079.3.05",{"id":98,"year":27,"html":99,"doi":100},129438,"Gfeller, Frank, Widmer, Remo, Krüger, Biljana, Galuskin, Evgeny V., Galuskina, Irina O., Armbruster, Thomas (2015) The crystal structure of flamite and its relation to Ca2 SiO4 polymorphs and nagelschmidtite. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  27 (6) 755-769 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1127\u002Fejm\u002F2015\u002F0027-2476'>doi:10.1127\u002Fejm\u002F2015\u002F0027-2476\u003C\u002Fa>","10.1127\u002Fejm\u002F2015\u002F0027-2476",{"id":102,"year":103,"html":104,"doi":11},16964349,2016,"(2016) Flamite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fflamite.pdf' class='refpdflink'>\u003C\u002Fa>",[],[],[108,109],"Flamiet","IMA2013-122",[111,115,120,124],{"lang":112,"names":113},"ca",[114],"flamita",{"lang":116,"names":117},"de",[118,119],"Flamit","IMA 2013-122",{"lang":121,"names":122},"eu",[123],"Flamita",{"lang":125,"names":126},"it",[127],"flamite","Q19833651",{"history":11,"applications":11}]