[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:471414":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":6,"synid":6,"polytypeof":6,"groupid":6,"weighting":11,"nolocadd":12,"blacklisted":12,"mindat_formula":13,"mindat_formula_note":6,"ima_formula":6,"elements":14,"sigelements":19,"key_elements":20,"impurities":6,"cim":6,"ima_status":21,"ima_notes":6,"ima_history":6,"approval_year":23,"publication_year":24,"discovery_year":6,"strunz10ed1":25,"strunz10ed2":26,"strunz10ed3":27,"strunz10ed4":6,"dana8ed1":6,"dana8ed2":6,"dana8ed3":6,"dana8ed4":6,"csystem":28,"cclass":29,"spacegroup":30,"spacegroupset":31,"a":32,"b":33,"c":34,"alpha":6,"beta":6,"gamma":6,"aerror":35,"berror":36,"cerror":37,"alphaerror":6,"betaerror":6,"gammaerror":6,"va3":6,"z":38,"csmetamict":12,"commentcrystal":6,"twinning":6,"tranglide":6,"parting":39,"epitaxidescription":6,"morphology":6,"tlform":40,"hmin":41,"hmax":42,"hardtype":6,"vhnmin":43,"vhnmax":6,"vhnerror":6,"vhng":36,"vhns":6,"commenthard":6,"dmeas":6,"dmeas2":6,"dcalc":44,"dmeaserror":6,"dcalcerror":6,"commentdense":6,"lustre":6,"lustretype":45,"commentluster":6,"diapheny":46,"streak":47,"colour":48,"commentcolor":6,"colors":49,"streak_colors":51,"luminescence":6,"uv":52,"cleavage":6,"cleavagetype":53,"fracturetype":54,"tenacity":55,"commentbreak":6,"opticaltype":56,"opticalsign":6,"opticalalpha":6,"opticalalpha2":6,"opticalalphaerror":6,"opticalbeta":6,"opticalbeta2":6,"opticalbetaerror":6,"opticalgamma":6,"opticalgamma2":6,"opticalgammaerror":6,"opticalomega":6,"opticalomega2":6,"opticalomegaerror":6,"opticalepsilon":6,"opticalepsilon2":6,"opticalepsilonerror":6,"opticaln":6,"opticaln2":6,"opticalnerror":6,"optical2vcalc":6,"optical2vcalc2":6,"optical2vcalcerror":6,"optical2vmeasured":6,"optical2vmeasured2":6,"optical2vmeasurederror":6,"rimin":6,"rimax":6,"opticaldispersion":6,"opticalpleochroism":57,"opticalpleochorismdesc":6,"opticalbirefringence":6,"opticalcomments":58,"opticalcolour":59,"opticalinternal":39,"opticaltropic":60,"opticalanisotropism":61,"opticalbireflectance":39,"opticalextinction":6,"opticalr":62,"specdispm":6,"ir":6,"electrical":6,"magnetism":6,"thermalbehaviour":6,"other":6,"industrial":6,"occurrence":63,"otheroccurrence":6,"type_specimen_store":64,"description_short":65,"aboutname":66,"rock_parent":6,"rock_parent2":6,"rock_root":9,"rock_bgs_code":6,"meteoritical_code":6,"updttime":67,"reviewed_at":6,"variety_of":6,"varieties":68,"group_members":69,"associates":70,"confused_with":71,"type_localities":72,"occurrence_total":11,"citations":79,"images":87,"structures":88,"synonyms":89,"language_names":91,"wikidata_qid":101,"texts":102},471414,"1:1:471414:5",null,"Boevskite","Boe",0,"mineral",1,false,"Pb\u003Csub>4\u003C\u002Fsub>(TeO\u003Csub>3\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)(S\u003Csub>2\u003C\u002Fsub>O\u003Csub>3\u003C\u002Fsub>)",[15,16,17,18],"Pb","Te","O","S",[15,16,17,18],[15,16],[22],"APPROVED",2024,2025,"7","J","A","Orthorhombic",8,71,"Pnma ","9.7764","13.3622","10.7213",7,10,9,4,"none","euhedral grains up to 0.25 mm at the contact of galena and pyrite, as inclusions in galena up to 0.2 mm, and as thin veinlets up to 0.2 × 0.03 mm filling cracks in sphalerite.",2.5,3,"110","6.599","Adamantine","Transparent","white","colourless",[50,47],"colorless",[47],"It does not fluoresce under ultraviolet light.","None Observed","Irregular\u002FUneven","brittle","Biaxial","Non-pleochroic","The mean refractive index calculated using the Gladstone-Dale equation is 2.08.","grey","Anisotropic","weak in gray tones","(14.7 ,14.1) 470,\r\n(13.5, 13.1) 546,\r\n(13.5, 13.2) 589,\r\n(13.8, 13.2) 650","The presence of sulfides in the ores of the deposit along with fluorite led to the formation of sulfuric and hydrofluoric acids in the oxidation zone and the active development of supergene processes to a depth of 100 meters. \r\n\r\nThe new mineral was formed as a result of the supergene alteration of the co-existing galena and tellurides (empressite, hessite, ingodite, joséite-B) in the oxidation zone.","Type material is deposited in the collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 119071, Russia, registration number 6127\u002F1","Boevskite has a unique structure formed by Te–Pb–O layers coplanar to the ac plane with thiosulfate groups and SO4 tetrahedra located between them. This is the first mineral having both sulfate and thiosulfate groups as species-defining constituents","After the type locality","2025-10-07 18:05:36",[],[],[],[],[73],{"id":74,"txt":75,"latitude":76,"longitude":77,"country":78},19827,"Boevskoe Be deposit (Boevka; Severnoye), Kaslinsky District, Chelyabinsk Oblast, Russia",56.2455556,61.3738889,"Russia",[80,83],{"id":81,"year":6,"html":82,"doi":6},17658922,"Kasatkin, A. V., Zubkova, N. V., Škoda, R., Gurzhiy, V. V., Nestola, F., Biagioni, C., Agakhanov, A. A., Britvin, S. N., Plášil, J., and Kuznetsov, A. M.: Boevskite, IMA 2024-041, in: CNMNC Newsletter 81, Eur. J. Mineral., 36, https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-36-917-2024, 2024.",{"id":84,"year":24,"html":85,"doi":86},18949244,"Kasatkin, Anatoly V.; Zubkova, Natalia V.; Škoda, Radek; Gurzhiy, Vladislav V.; Nestola, Fabrizio; Biagioni, Cristian; Agakhanov, Atali A.; Britvin, Sergey N.; Plášil, Jakub; Kuznetsov, Aleksey M. (2025) Boevskite, Pb4(TeO3)2(SO4)(S2O3), the first mixed sulfate–thiosulfate mineral from the Boevskoe deposit, Southern Urals, Russia. \u003Ci>Mineralogical Magazine\u003C\u002Fi>, 1-22 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fmgm.2025.10143'>doi:10.1180\u002Fmgm.2025.10143\u003C\u002Fa>","10.1180\u002Fmgm.2025.10143",[],[],[90],"Boevskiet",[92,96],{"lang":93,"names":94},"ca",[95],"boevskita",{"lang":97,"names":98},"de",[99,100],"Boevskit","IMA 2024-041","Q131363916",{"history":6,"applications":6}]