[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:7367":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":16,"ima_formula":17,"elements":18,"sigelements":26,"key_elements":27,"impurities":11,"cim":11,"ima_status":28,"ima_notes":11,"ima_history":11,"approval_year":30,"publication_year":31,"discovery_year":11,"strunz10ed1":32,"strunz10ed2":23,"strunz10ed3":33,"strunz10ed4":34,"dana8ed1":35,"dana8ed2":35,"dana8ed3":35,"dana8ed4":35,"csystem":36,"cclass":37,"spacegroup":38,"spacegroupset":35,"a":39,"b":35,"c":40,"alpha":35,"beta":35,"gamma":35,"aerror":41,"berror":11,"cerror":41,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":42,"csmetamict":14,"commentcrystal":43,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":11,"hmin":44,"hmax":44,"hardtype":11,"vhnmin":35,"vhnmax":35,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":45,"dmeas2":45,"dcalc":46,"dmeaserror":47,"dcalcerror":11,"commentdense":11,"lustre":48,"lustretype":48,"commentluster":11,"diapheny":49,"streak":50,"colour":51,"commentcolor":11,"colors":52,"streak_colors":55,"luminescence":11,"uv":56,"cleavage":57,"cleavagetype":58,"fracturetype":59,"tenacity":60,"commentbreak":11,"opticaltype":61,"opticalsign":62,"opticalalpha":35,"opticalalpha2":35,"opticalalphaerror":11,"opticalbeta":35,"opticalbeta2":35,"opticalbetaerror":11,"opticalgamma":35,"opticalgamma2":35,"opticalgammaerror":11,"opticalomega":63,"opticalomega2":35,"opticalomegaerror":42,"opticalepsilon":64,"opticalepsilon2":35,"opticalepsilonerror":42,"opticaln":35,"opticaln2":35,"opticalnerror":11,"optical2vcalc":35,"optical2vcalc2":35,"optical2vcalcerror":11,"optical2vmeasured":35,"optical2vmeasured2":35,"optical2vmeasurederror":11,"rimin":65,"rimax":66,"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":67,"otheroccurrence":11,"type_specimen_store":68,"description_short":69,"aboutname":70,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":71,"reviewed_at":11,"variety_of":11,"varieties":72,"group_members":73,"associates":146,"confused_with":161,"type_localities":165,"occurrence_total":177,"citations":178,"images":208,"structures":280,"synonyms":287,"language_names":290,"wikidata_qid":338,"texts":339},7367,"1:1:7367:3","a013fc19-306f-4f38-89cd-b8f2892be54e","Wiluite","Wil",0,"mineral",null,32107,882,false,"Ca\u003Csub>19\u003C\u002Fsub>MgAl\u003Csub>4\u003C\u002Fsub>(Al,Mg)\u003Csub>8\u003C\u002Fsub>(B,&#9723;)\u003Csub>4\u003C\u002Fsub>&#9723;[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>4\u003C\u002Fsub>[(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>]O(O,OH)\u003Csub>9\u003C\u002Fsub>","The formula is a partial simplification of the full structural formula. The large (VII-IX)-coordinated (X4)\u003Csub>2\u003C\u002Fsub>(X3)\u003Csub>8\u003C\u002Fsub>(X2)\u003Csub>8\u003C\u002Fsub>(X1) sites are here combined (e.g. Ca\u003Csub>19\u003C\u002Fsub>) and are typically filled with Ca, although other large cations such as the REE may be present. The square-pyramidal Y1 site can host a variety of M\u003Csup>2+\u003C\u002Fsup> and M\u003Csup>3+\u003C\u002Fsup> ions and is the basis for the distinction of several species. The VI-coordinated Y2 site typically is filled with Al, whereas the also VI-coordinated Y3 site may contain Al, Mg, and other cations of similar charge and size. The tetrahedral T1 site is typically vacant but may contain B (less commonly Al); the trigonal T2 site is also typically vacant but may also contain B. Some of the (SiO\u003Csub>4\u003C\u002Fsub>) may be replaced by (H\u003Csub>4\u003C\u002Fsub>O\u003Csub>4\u003C\u002Fsub>), akin to the Si\u003Csup>4+\u003C\u002Fsup> ↔︎ 4H\u003Csup>+\u003C\u002Fsup> hydrogarnet substitution. Among the oxygen that are not part of the silica tetrahedra, there are eight \"O11\" that typically occur as OH, two \"O10\" that are typically O & OH or OH & OH (the latter arrangement notably when Y1 is an M\u003Csup>2+\u003C\u002Fsup> cation). There may also be up to three \"O12\" that in most vesuvianite-group minerals are absent (and are not included here), but may be present particularly when T1 is occupied.\r\n\r\nWith increased filling of the T2 site by B, various charge balance mechanisms involving either increased O for OH in the \"O11\" position and\u002For increased M\u003Csup>2+\u003C\u002Fsup> for M\u003Csup>3+\u003C\u002Fsup> substitution in the Y3 site are necessary (see idealized formula for full T2 occupancy by B). In lieu of an explicitly defined \"end-member\" wiluite, more generic representations of site fillings are retained here, pending newer data.","Ca\u003Csub>19\u003C\u002Fsub>(Al,Mg)\u003Csub>13\u003C\u002Fsub>(B,&#9723;,Al)\u003Csub>5\u003C\u002Fsub>(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>(O,OH)\u003Csub>10\u003C\u002Fsub>",[19,20,21,22,23,24,25],"Al","Ca","Mg","Si","B","O","H",[19,20,21,22,23,24],[23],[29],"APPROVED",1997,1998,"9","G","35","0","Tetragonal",27,186,"15.716","11.704",1,2,"Wiluite from Ariccia, Latium, Italy",6,"3.36","3.358",3,"Vitreous","Transparent,Translucent","Colourless","Dark green",[53,54],"green","colorless",[54],"none","Poor cleavage on {100}.","Poor\u002FIndistinct","Irregular\u002FUneven","brittle","Uniaxial","+","1.721","1.725",1.721,1.725,"metasomatized skarn","Canadian Museum of Nature, Ottawa, Ontario, Canada.","Vesuvianite Group.","Named after the discovery locality, Wilui River basin, Sakha Republic (Yakutia), Russia.","2025-08-11 12:14:28",[],[74,81,89,95,103,110,118,125,133,138],{"id":75,"name":76,"entrytype":9,"csystem":36,"ima_formula":77,"mindat_formula":78,"hmin":79,"hmax":79,"dmeas":80,"dcalc":11,"primary_image_id":11},47914,"Alumovesuvianite","Ca\u003Csub>19\u003C\u002Fsub>Al(Al\u003Csub>10\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>)Si\u003Csub>18\u003C\u002Fsub>O\u003Csub>69\u003C\u002Fsub>(OH)\u003Csub>9\u003C\u002Fsub>","Ca\u003Csub>19\u003C\u002Fsub>AlAl\u003Csub>4\u003C\u002Fsub>(Al\u003Csub>6\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>)(☐\u003Csub>4\u003C\u002Fsub>)☐[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>4\u003C\u002Fsub>[(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>]O(OH)\u003Csub>9\u003C\u002Fsub>",6.5,"3.31",{"id":82,"name":83,"entrytype":9,"csystem":36,"ima_formula":84,"mindat_formula":85,"hmin":79,"hmax":79,"dmeas":86,"dcalc":87,"primary_image_id":88},46798,"Cyprine","Ca\u003Csub>19\u003C\u002Fsub>Cu\u003Csup>2+\u003C\u002Fsup>(Al,Mg)\u003Csub>12\u003C\u002Fsub>Si\u003Csub>18\u003C\u002Fsub>O\u003Csub>69\u003C\u002Fsub>(OH)\u003Csub>9\u003C\u002Fsub>","Ca\u003Csub>19\u003C\u002Fsub>Cu\u003Csup>2+\u003C\u002Fsup>Al\u003Csub>4\u003C\u002Fsub>(Al\u003Csub>6\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>)(&#9723;\u003Csub>4\u003C\u002Fsub>)&#9723;[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>4\u003C\u002Fsub>[(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>](OH)(OH)\u003Csub>9\u003C\u002Fsub>","3.40","3.41",29574,{"id":90,"name":91,"entrytype":9,"csystem":36,"ima_formula":92,"mindat_formula":93,"hmin":44,"hmax":44,"dmeas":94,"dcalc":86,"primary_image_id":11},25683,"Fluorvesuvianite","Ca\u003Csub>19\u003C\u002Fsub>(Al,Mg)\u003Csub>13\u003C\u002Fsub>(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>O(F,OH)\u003Csub>9\u003C\u002Fsub>","Ca\u003Csub>19\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>Al\u003Csub>4\u003C\u002Fsub>(Al\u003Csub>6\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>)(&#9723;\u003Csub>4\u003C\u002Fsub>)&#9723;[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>4\u003C\u002Fsub>[(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>]O(F,OH)\u003Csub>9\u003C\u002Fsub>","3.43",{"id":96,"name":97,"entrytype":9,"csystem":36,"ima_formula":98,"mindat_formula":99,"hmin":44,"hmax":100,"dmeas":101,"dcalc":102,"primary_image_id":11},52166,"Hongheite","Ca\u003Csub>19\u003C\u002Fsub>Fe\u003Csup>2+\u003C\u002Fsup>Al\u003Csub>4\u003C\u002Fsub>(Fe\u003Csup>3+\u003C\u002Fsup>,Mg,Al)\u003Csub>8\u003C\u002Fsub>(&#9723;,B)\u003Csub>4\u003C\u002Fsub>BSi\u003Csub>18\u003C\u002Fsub>O\u003Csub>69\u003C\u002Fsub>(O,OH)\u003Csub>9\u003C\u002Fsub>","Ca\u003Csub>19\u003C\u002Fsub>Fe\u003Csup>2+\u003C\u002Fsup>Al\u003Csub>4\u003C\u002Fsub>(Fe\u003Csup>3+\u003C\u002Fsup>,Mg)\u003Csub>8\u003C\u002Fsub>(&#9723;\u003Csub>4\u003C\u002Fsub>)B[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>4\u003C\u002Fsub>[(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>]O(OH,O)\u003Csub>9\u003C\u002Fsub>",7,"3.446","3.423",{"id":104,"name":105,"entrytype":9,"csystem":36,"ima_formula":106,"mindat_formula":107,"hmin":44,"hmax":44,"dmeas":108,"dcalc":109,"primary_image_id":11},47594,"Magnesiovesuvianite","Ca\u003Csub>19\u003C\u002Fsub>Mg(Al\u003Csub>11\u003C\u002Fsub>Mg)Si\u003Csub>18\u003C\u002Fsub>O\u003Csub>69\u003C\u002Fsub>(OH)\u003Csub>9\u003C\u002Fsub>","Ca\u003Csub>19\u003C\u002Fsub>MgAl\u003Csub>4\u003C\u002Fsub>(Al\u003Csub>6\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>)(&#9723;\u003Csub>4\u003C\u002Fsub>)&#9723;[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>4\u003C\u002Fsub>[(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>](OH)(OH)\u003Csub>9\u003C\u002Fsub>","3.30","3.35",{"id":111,"name":112,"entrytype":9,"csystem":36,"ima_formula":113,"mindat_formula":114,"hmin":115,"hmax":11,"dmeas":116,"dcalc":117,"primary_image_id":11},53139,"Manaevite-(Ce)","Ca\u003Csub>11\u003C\u002Fsub>(Ce,H\u003Csub>2\u003C\u002Fsub>O,Ca)\u003Csub>8\u003C\u002Fsub>Mg(Al,Fe)\u003Csub>4\u003C\u002Fsub>(Mg,Ti,Fe\u003Csup>3+\u003C\u002Fsup>)\u003Csub>8\u003C\u002Fsub>[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>4\u003C\u002Fsub>[(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>8\u003C\u002Fsub>(H\u003Csub>4\u003C\u002Fsub>O\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>](OH)\u003Csub>9\u003C\u002Fsub>","(Ca\u003Csub>13\u003C\u002Fsub>Ce\u003Csub>4\u003C\u002Fsub>[H\u003Csub>2\u003C\u002Fsub>O]\u003Csub>2\u003C\u002Fsub>)Mg(Al\u003Csub>3\u003C\u002Fsub>Mg)(Mg\u003Csub>3\u003C\u002Fsub>Ti\u003Csub>3\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>)(&#9723;\u003Csub>4\u003C\u002Fsub>)&#9723;[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>4\u003C\u002Fsub>[(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>8\u003C\u002Fsub>(H\u003Csub>4\u003C\u002Fsub>O\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>]O(OH)\u003Csub>9\u003C\u002Fsub>",4.5,"3.80","3.72",{"id":119,"name":120,"entrytype":9,"csystem":36,"ima_formula":121,"mindat_formula":122,"hmin":44,"hmax":100,"dmeas":35,"dcalc":123,"primary_image_id":124},11475,"Manganvesuvianite","Ca\u003Csub>19\u003C\u002Fsub>Mn\u003Csup>3+\u003C\u002Fsup>Al\u003Csub>10\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>O(OH)\u003Csub>9\u003C\u002Fsub>","Ca\u003Csub>19\u003C\u002Fsub>Mn\u003Csup>3+\u003C\u002Fsup>Al\u003Csub>4\u003C\u002Fsub>(Al\u003Csub>6\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>)(&#9723;\u003Csub>4\u003C\u002Fsub>)&#9723;[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>4\u003C\u002Fsub>[(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>]O(OH)\u003Csub>9\u003C\u002Fsub>","3.404",15383,{"id":126,"name":127,"entrytype":9,"csystem":36,"ima_formula":128,"mindat_formula":129,"hmin":44,"hmax":44,"dmeas":130,"dcalc":131,"primary_image_id":132},53137,"Milanriederite","(Ca,REE)\u003Csub>19\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>Al\u003Csub>4\u003C\u002Fsub>(Mg,Al,Fe\u003Csup>3+\u003C\u002Fsup>)\u003Csub>8\u003C\u002Fsub>Si\u003Csub>18\u003C\u002Fsub>O\u003Csub>68\u003C\u002Fsub>(OH,O)\u003Csub>10\u003C\u002Fsub>","(Ca\u003Csub>18\u003C\u002Fsub>[REE])Fe\u003Csup>3+\u003C\u002Fsup>Al\u003Csub>4\u003C\u002Fsub>(Mg\u003Csub>4\u003C\u002Fsub>Al\u003Csub>4\u003C\u002Fsub>)(&#9723;\u003Csub>4\u003C\u002Fsub>)&#9723;[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>4\u003C\u002Fsub>[(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>](OH)(OH)\u003Csub>9\u003C\u002Fsub>","3.53","3.547",16258,{"id":134,"name":135,"entrytype":9,"csystem":36,"ima_formula":11,"mindat_formula":136,"hmin":11,"hmax":11,"dmeas":11,"dcalc":11,"primary_image_id":137},471108,"Modraite","Ca\u003Csub>19\u003C\u002Fsub>Fe\u003Csup>2+\u003C\u002Fsup>Al\u003Csub>4\u003C\u002Fsub>(Al\u003Csub>6\u003C\u002Fsub>Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>)(&#9723;\u003Csub>4\u003C\u002Fsub>)&#9723;[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>4\u003C\u002Fsub>[(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>](OH)(OH)\u003Csub>9\u003C\u002Fsub>",16420,{"id":139,"name":140,"entrytype":9,"csystem":36,"ima_formula":141,"mindat_formula":142,"hmin":79,"hmax":79,"dmeas":143,"dcalc":144,"primary_image_id":145},4223,"Vesuvianite","(Ca,Na)\u003Csub>19\u003C\u002Fsub>(Al,Mg,Fe)\u003Csub>13\u003C\u002Fsub>(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>(OH,F,O)\u003Csub>10\u003C\u002Fsub>","Ca\u003Csub>19\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>Al\u003Csub>4\u003C\u002Fsub>(Al\u003Csub>6\u003C\u002Fsub>Mg\u003Csub>2\u003C\u002Fsub>)(&#9723;\u003Csub>4\u003C\u002Fsub>)&#9723;[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>4\u003C\u002Fsub>[(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>10\u003C\u002Fsub>]O(OH)\u003Csub>9\u003C\u002Fsub>","3.32","3.42",6769,[147,154],{"id":148,"name":149,"entrytype":9,"csystem":150,"ima_formula":151,"mindat_formula":151,"hmin":79,"hmax":100,"dmeas":152,"dcalc":152,"primary_image_id":153},1755,"Grossular","Isometric","Ca\u003Csub>3\u003C\u002Fsub>Al\u003Csub>2\u003C\u002Fsub>(SiO\u003Csub>4\u003C\u002Fsub>)\u003Csub>3\u003C\u002Fsub>","3.594",29814,{"id":155,"name":156,"entrytype":9,"csystem":150,"ima_formula":157,"mindat_formula":157,"hmin":44,"hmax":79,"dmeas":158,"dcalc":159,"primary_image_id":160},3314,"Pyrite","FeS\u003Csub>2\u003C\u002Fsub>","4.8","5.01",20239,[162,163,164],{"id":90,"name":91,"entrytype":9,"csystem":36,"ima_formula":92,"mindat_formula":93,"hmin":44,"hmax":44,"dmeas":94,"dcalc":86,"primary_image_id":11},{"id":119,"name":120,"entrytype":9,"csystem":36,"ima_formula":121,"mindat_formula":122,"hmin":44,"hmax":100,"dmeas":35,"dcalc":123,"primary_image_id":124},{"id":139,"name":140,"entrytype":9,"csystem":36,"ima_formula":141,"mindat_formula":142,"hmin":79,"hmax":79,"dmeas":143,"dcalc":144,"primary_image_id":145},[166,172],{"id":167,"txt":168,"latitude":169,"longitude":170,"country":171},2758,"Akhtaragda River mouth, Vilyui River Basin, Mirninsky District, Sakha, Russia",63.1060975,112.2025103,"Russia",{"id":173,"txt":174,"latitude":175,"longitude":176,"country":171},2759,"Vilyui River Basin, Mirninsky District, Sakha, Russia",63.022664,112.246597,9,[179,183,187,191,194,199,204],{"id":180,"year":181,"html":182,"doi":11},16772249,1797,"Klaproth, M. H. (1797) XXXI. 2. Untersuchung des Vesuvians, Vesuvian aus Sibirien. In \u003Ci>Beiträge zur chemischen Kenntniss der Mineralkörper\u003C\u002Fi> Vol. 2. Rottmann. p.33-38. \u003Ca target='_blank' href='https:\u002F\u002Fwww.e-rara.ch\u002Fdownload\u002Fpdf\u002F12724631.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":184,"year":185,"html":186,"doi":11},16127619,1994,"Groat, L.A., Hawthorne, F.C., Ercit, T.S. (1994) The incorporation of boron into the vesuvianite structure. The Canadian Mineralogist: 32: 505-523.",{"id":188,"year":189,"html":190,"doi":11},15418311,1996,"Grew, Edward S.; Anovitz, Lawrence M. - \u003Ci>Eds.\u003C\u002Fi> (1996) Boron - Mineralogy, Petrology and Geochemistry. \u003Ci>Reviews in Mineralogy\u003C\u002Fi> Vol. 33. Mineralogical Society of America p.862",{"id":192,"year":31,"html":193,"doi":11},16880877,"Groat, L. A., Hawthorne, F. C., Erit, T. S., Grice, J. D. (1998) Wiluite, Ca\u003Csub>19\u003C\u002Fsub>(Al,Mg,Fe,Ti)\u003Csub>13\u003C\u002Fsub>(B,Al,◻)\u003Csub>5\u003C\u002Fsub>Si\u003Csub>18\u003C\u002Fsub>O\u003Csub>68\u003C\u002Fsub>(O,OH)\u003Csub>10\u003C\u002Fsub>, a new mineral species isostructural with vesuvianite, from the Sakha Republic, Russian Federation. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  36 (5). 1301-1304 \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM36_1301.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":195,"year":196,"html":197,"doi":198},64183,2005,"Bellatreccia, F., Camara, F., Ottolini, L., Della Ventura, G., Cibin, G., Mottana, A. (2005) Wiluite from Ariccia, Latium, Italy: Occurrence and crystal structure. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  43 (5). 1457-1468 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgscanmin.43.5.1457'>doi:10.2113\u002Fgscanmin.43.5.1457\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fcm\u002Fvol43\u002FCM43_1457.pdf' class='refpdflink'>\u003C\u002Fa>","10.2113\u002Fgscanmin.43.5.1457",{"id":200,"year":201,"html":202,"doi":203},154188,2017,"Panikorovskii, Taras L., Mazur, Anton S., Bazai, Ayya V., Shilovskikh, Vladimir V., Galuskin, Evgeny V., Chukanov, Nikita V., Rusakov, Vyacheslav S., Zhukov, Yurii M., Avdontseva, Evgenia Yu., Aksenov, Sergey M., Krivovichev, Sergey V. (2017) X-ray diffraction and spectroscopic study of wiluite: implications for the vesuvianite-group nomenclature. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  44 (8) 577-593 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00269-017-0885-2'>doi:10.1007\u002Fs00269-017-0885-2\u003C\u002Fa>","10.1007\u002Fs00269-017-0885-2",{"id":205,"year":206,"html":207,"doi":11},16968139,2021,"(2021) Wiluite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002FWiluite.pdf' class='refpdflink'>\u003C\u002Fa>",[209,216,226,235,243,251,258,264,271],{"id":210,"source_url":211,"license_code":212,"credit_html":213,"title":7,"description":11,"author":11,"original_width":214,"original_height":215},30977,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F112724","CC BY 4.0","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F112724\" rel=\"noopener\">Department of Geology, TalTech\u003C\u002Fa> via Europeana",1000,666,{"id":217,"source_url":218,"license_code":219,"credit_html":220,"title":221,"description":222,"author":223,"original_width":224,"original_height":225},27477,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8389277","CC BY-SA 3.0","Ra&#039;ike (see also: de:Benutzer:Ra&#039;ike), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8389277\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Wiluit - Wiljui (Fluss), Sacha (Jakutien), Russland.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FWiluite\" class=\"extiw\" title=\"en:Wiluite\">Wiluite\u003C\u002Fa> - Locality: Wiljui (River), Sakha (Yakutia), Russia","Ra'ike (see also: de:Benutzer:Ra'ike)",2600,2000,{"id":227,"source_url":228,"license_code":219,"credit_html":229,"title":230,"description":231,"author":232,"original_width":233,"original_height":234},27478,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10148568","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10148568\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Wiluite-165271.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FWiluite\" class=\"extiw\" title=\"en:Wiluite\">Wiluite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Vilyui River Basin (Vilui River Basin; Wilui River Basin), Saha Republic (Sakha Republic; Yakutia), Eastern-Siberian Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2759.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 3.7 x 2.4 x 2.0 cm.\u003C\u002Fdd>\n\u003Cdd>A LARGE, 3.7 cm, doubly terminated, sharp crystal of the ULTRA RARE vesuvianite group species, wiluite, from the Type Locality. This lustrous, dark olive-green, FLOATER crystal is pristine. These crystals originally sold cheaply as vesuvianite, until they were determined to be a new species. This is a SUPER piece. Ex. George Elling Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",400,293,{"id":236,"source_url":237,"license_code":219,"credit_html":238,"title":239,"description":240,"author":232,"original_width":241,"original_height":242},27479,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10164434","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10164434\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Wiluite-235309.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FWiluite\" class=\"extiw\" title=\"en:Wiluite\">Wiluite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Akhtaragda River mouth (Achtaragda River mouth), Vilyui River Basin (Vilui River Basin; Wilui River Basin), Saha Republic (Sakha Republic; Yakutia), Eastern-Siberian Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2758.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 8.4 x 6.4 x 6.0 cm.\u003C\u002Fdd>\n\u003Cdd>This rare titanium-bearing member of the Vesuvianite group is only found in a few worldwide localities, and the most desirable specimens are those from the type locality in Russia. This specimen features a pair predominant, good quality, sharp, euhedral dark blackish-green color prismatic tetragonal crystal measuring 1.5 cm aesthetically sitting on serpentine matrix. Ex. Richard Kosnar Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",500,432,{"id":244,"source_url":245,"license_code":219,"credit_html":246,"title":247,"description":248,"author":232,"original_width":249,"original_height":250},27480,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10169502","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10169502\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Wiluite-261805.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FWiluite\" class=\"extiw\" title=\"en:Wiluite\">Wiluite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Vilyui River Basin (Vilui River Basin; Wilui River Basin), Saha Republic (Sakha Republic; Yakutia), Eastern-Siberian Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2759.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 2.5 x 1.7 x 1.5 cm.\u003C\u002Fdd>\n\u003Cdd>A doubly terminated, sharp crystal of the very rare species wiluite, from the Type Locality. This lustrous, dark olive-green, floater crystal is pristine. One termination has a pyramidal termination and the other end is a modified pinacoid. Very interesting. These crystals originally sold as vesuvianite, until they were determined to be a new species. Ex. Carlton Davis Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",547,600,{"id":252,"source_url":253,"license_code":219,"credit_html":254,"title":255,"description":256,"author":232,"original_width":233,"original_height":257},27481,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10442656","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10442656\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Wiluite-rh3-48b.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FWiluite\" class=\"extiw\" title=\"en:Wiluite\">Wiluite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Wilui River, Yakutxk, Siberia, Russia\u003C\u002Fdd>\n\u003Cdd>Size: small cabinet, 6.9 x 4.0 x 2.7 cm\n\u003Cdl>\u003Cdt>Wiluite\u003C\u002Fdt>\u003C\u002Fdl>\u003C\u002Fdd>\n\u003Cdd>If the name of this species is unfamiliar to you, it is a rare member of the vesuvianite family of minerals. This matrix specimen displays a clearly tetragonal habit. It is a doubly terminated, lustrous, black wiluite crystal, measuring 2.5 cm in length. Sharp. Ex. Richard Hauck Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",367,{"id":259,"source_url":260,"license_code":219,"credit_html":261,"title":262,"description":256,"author":232,"original_width":233,"original_height":263},27482,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10442660","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10442660\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Wiluite-rh3-48c.jpg",338,{"id":265,"source_url":266,"license_code":219,"credit_html":267,"title":268,"description":256,"author":232,"original_width":269,"original_height":270},27483,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10442661","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10442661\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Wiluite-rh3-48a.jpg",800,489,{"id":272,"source_url":273,"license_code":212,"credit_html":274,"title":275,"description":276,"author":277,"original_width":278,"original_height":279},27484,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146588330","Slashme, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146588330\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Wiluit.jpg","Wiluite, Akhtaragda River mouth, Vilyui River Basin, Sakha, Siberia","Slashme",4343,3007,[281],{"id":282,"url":283,"label":284,"formula":285,"spacegroup":286,"year":196},14513,"\u002Fcif\u002F14513.cif","Bellatreccia 2005","Ca18.659 Mg3.9 Sr.02 La.05 Ce.04 Nd.01 Fe1.91 Ti.27 Mn.11 Al6.98 B2.86 Be.02 H.79 Si18 O78.83 F1.21","P 4\u002Fn n c",[288,289],"IMA1997-026","Viluite (of von Leonhard)",[291,295,300,304,307,310,314,318,323,326,330,334],{"lang":292,"names":293},"ca",[294],"wiluïta",{"lang":296,"names":297},"de",[298,299],"IMA 1997-026","Wiluit",{"lang":301,"names":302},"es",[303],"Wiluita",{"lang":305,"names":306},"eu",[303],{"lang":308,"names":309},"fr",[7],{"lang":311,"names":312},"it",[313],"wiluite",{"lang":315,"names":316},"ja",[317],"ウィルアイト",{"lang":319,"names":320},"nl",[321,322],"Viluet","wiluiet",{"lang":324,"names":325},"pl",[299],{"lang":327,"names":328},"ru",[329],"вилуит",{"lang":331,"names":332},"uk",[333],"Вілюїт",{"lang":335,"names":336},"zh",[337],"硼符山石","Q409428",{"history":11,"applications":11}]