[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:586":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":16,"elements":17,"sigelements":22,"key_elements":23,"impurities":24,"cim":11,"ima_status":25,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":28,"discovery_year":29,"strunz10ed1":30,"strunz10ed2":31,"strunz10ed3":32,"strunz10ed4":33,"dana8ed1":34,"dana8ed2":35,"dana8ed3":35,"dana8ed4":36,"csystem":37,"cclass":38,"spacegroup":39,"spacegroupset":40,"a":41,"b":40,"c":42,"alpha":40,"beta":40,"gamma":40,"aerror":43,"berror":11,"cerror":43,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":44,"csmetamict":14,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":11,"hmin":45,"hmax":46,"hardtype":47,"vhnmin":40,"vhnmax":40,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":48,"dmeas2":49,"dcalc":50,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":51,"commentluster":11,"diapheny":52,"streak":53,"colour":54,"commentcolor":55,"colors":56,"streak_colors":61,"luminescence":11,"uv":11,"cleavage":62,"cleavagetype":63,"fracturetype":64,"tenacity":65,"commentbreak":11,"opticaltype":66,"opticalsign":67,"opticalalpha":40,"opticalalpha2":40,"opticalalphaerror":11,"opticalbeta":40,"opticalbeta2":40,"opticalbetaerror":11,"opticalgamma":40,"opticalgamma2":40,"opticalgammaerror":11,"opticalomega":68,"opticalomega2":69,"opticalomegaerror":11,"opticalepsilon":70,"opticalepsilon2":68,"opticalepsilonerror":11,"opticaln":40,"opticaln2":40,"opticalnerror":11,"optical2vcalc":40,"optical2vcalc2":40,"optical2vcalcerror":11,"optical2vmeasured":40,"optical2vmeasured2":40,"optical2vmeasurederror":11,"rimin":71,"rimax":72,"opticaldispersion":11,"opticalpleochroism":73,"opticalpleochorismdesc":74,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":75,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":76,"otheroccurrence":77,"type_specimen_store":78,"description_short":79,"aboutname":80,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":81,"reviewed_at":11,"variety_of":11,"varieties":82,"group_members":83,"associates":115,"confused_with":116,"type_localities":117,"occurrence_total":124,"citations":125,"images":190,"structures":245,"synonyms":257,"language_names":258,"wikidata_qid":334,"texts":335},586,"1:1:586:1","dc7ef081-9922-4970-a823-52b85b777626","Bazzite","Bz",0,"mineral",null,40374,1594,false,"Be\u003Csub>3\u003C\u002Fsub>Sc\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>)","Be\u003Csub>3\u003C\u002Fsub>(Sc,Fe\u003Csup>3+\u003C\u002Fsup>,Mg)\u003Csub>2\u003C\u002Fsub>Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub> · Na\u003Csub>0.32\u003C\u002Fsub> · nH\u003Csub>2\u003C\u002Fsub>O",[18,19,20,21],"Be","Sc","Si","O",[18,19,20,21],[18,19],",Fe,Mn,Mg,Li,Na,K,Rb,Cs,",[26,27],"APPROVED","GRANDFATHERED",1915,"1915","9","C","J","05","61","1","2","Hexagonal",20,123,"0","9.521 ","9.165",5,2,6.5,7,3,"2.77","2.8","2.82","Vitreous","Transparent,Translucent","White","Deep blue or other shades of blue, blue-green.","The blue colour is caused by appreciable iron contents, and, more specifically, the ratio between \u003Cf>Fe#2#+ and Fe#3#+\u003C\u002Ff> (Taran et al., 2017).",[57,58,59,60],"blue","green","white","yellow",[59],"Poor on {0001}.","Poor\u002FIndistinct","Irregular\u002FUneven","brittle","Uniaxial","-","1.622","1.637","1.602",1.602,1.637,"Strong","O = pale greenish yellow\r\nE = intense sky-blue","Water type II molecules (H–H vector perpendicular to the c-axis) are only observed in samples from Kent (Kazakhstan); H\u003Csub>2\u003C\u002Fsub>O IId type is indicated by the bands at 1621 and 3663 cm\u003Csup>−1\u003C\u002Fsup>, while the ones at 1633 and 3643 are indicative for th","Granite","Found in miarolitic cavities in granites, granite pegmatites and in Alpine veins associated with pegmatitic minerals.","Municipal Museum of Natural History, Milan, Italy.\r\nUniversity of Milan, Milan, Italy.\r\nThe Natural History Museum, London, England, 1925,534.\r\nNatural History Museum, Paris, France, 115.132.","The scandium analogue of Beryl.\r\n\r\nTypically found as small to tiny hexagonal crystals with a deep blue or blue-green color. Hard to distinguish from beryl.\r\nThe blue colour is caused by appreciable iron contents, and, more specifically, the intensity ...","Named in 1915 for Alessandro Eugenio Bazzi (1892-1929), discoverer of the mineral.","2025-08-11 12:14:18",[],[84,93,99,108],{"id":85,"name":86,"entrytype":9,"csystem":37,"ima_formula":87,"mindat_formula":88,"hmin":89,"hmax":90,"dmeas":91,"dcalc":40,"primary_image_id":92},819,"Beryl","Be\u003Csub>3\u003C\u002Fsub>Al\u003Csub>2\u003C\u002Fsub>Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>","Be\u003Csub>3\u003C\u002Fsub>Al\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>)",7.5,8,"2.63",3157,{"id":94,"name":95,"entrytype":9,"csystem":37,"ima_formula":96,"mindat_formula":96,"hmin":89,"hmax":89,"dmeas":97,"dcalc":98,"primary_image_id":11},53764,"Johnkoivulaite-(Cs)","Cs[Be\u003Csub>2\u003C\u002Fsub>B]Mg\u003Csub>2\u003C\u002Fsub>Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>","3.01","3.117",{"id":100,"name":101,"entrytype":9,"csystem":102,"ima_formula":103,"mindat_formula":104,"hmin":90,"hmax":90,"dmeas":105,"dcalc":106,"primary_image_id":107},25652,"Pezzottaite-(Cs)","Trigonal","CsLiBe\u003Csub>2\u003C\u002Fsub>Al\u003Csub>2\u003C\u002Fsub>Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>","Cs(Be\u003Csub>2\u003C\u002Fsub>Li)Al\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>)","2.97","3.06",19205,{"id":109,"name":110,"entrytype":9,"csystem":37,"ima_formula":111,"mindat_formula":112,"hmin":89,"hmax":89,"dmeas":113,"dcalc":114,"primary_image_id":11},7315,"Stoppaniite","Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Be\u003Csub>3\u003C\u002Fsub>Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub> · H\u003Csub>2\u003C\u002Fsub>O","Be\u003Csub>3\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>)·H\u003Csub>2\u003C\u002Fsub>O","2.79","2.811",[],[],[118],{"id":119,"txt":120,"latitude":121,"longitude":122,"country":123},2103,"Seula mine, Mount Camoscio, Oltrefiume, Baveno, Verbano-Cusio-Ossola Province, Piedmont, Italy",45.9166667,8.4836111,"Italy",50,[126,129,133,136,141,145,150,154,159,163,168,172,176,180,185],{"id":127,"year":28,"html":128,"doi":11},16102574,"Artini, E. (1915): Due minerali di Baveno contenenti terre rare: weibyeïte e bazzite. Atti della Reale Accademia dei Lincei, Rendiconti della Classe di Scienze Fisiche, Matematiche e Naturali 24, 313-319.",{"id":130,"year":131,"html":132,"doi":11},16102575,1955,"American Mineralogist (1955): 40: 370.",{"id":134,"year":131,"html":135,"doi":11},16102578,"Bergerhoff, G. (1955): Uber die Kristallstruktur des Bazzit und ihre Beziehungen",{"id":137,"year":138,"html":139,"doi":140},467335,1956,"Peyronel, G. (1956) The crystal structure of Baveno bazzite. \u003Ci>Acta Crystallographica\u003C\u002Fi>,  9 (2) 181-186 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs0365110x56000401'>doi:10.1107\u002Fs0365110x56000401\u003C\u002Fa>","10.1107\u002Fs0365110x56000401",{"id":142,"year":143,"html":144,"doi":11},524675,1967,"Fleischer, Michael (1967) New Mineral Names. \u003Ci>American Mineralogist\u003C\u002Fi>,  52 (3-4) 559-564 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM52\u002FAM52_559.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":146,"year":147,"html":148,"doi":149},15845,1990,"Juve, G., Bergstøl, S. (1990) Caesian Bazzite in Granite pegmatite in Tørdal, Telemark, Norway. \u003Ci>Mineralogy and Petrology\u003C\u002Fi>,  43 (2) 131-136 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf01164306'>doi:10.1007\u002Fbf01164306\u003C\u002Fa>","10.1007\u002Fbf01164306",{"id":151,"year":147,"html":152,"doi":153},151899,"Hagemann, H.; Lucken, A.; Bill, H.; Gysler-Sanz, J.; Stalder, H.A. (1990) Polarized Raman spectra of beryl and bazzite. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  17 (5). 395-401 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf00212207'>doi:10.1007\u002Fbf00212207\u003C\u002Fa>","10.1007\u002Fbf00212207",{"id":155,"year":156,"html":157,"doi":158},16065,1995,"Armbruster, Th., Libowitzky, E., Auernhammer, M., Bauerhansl, P., Hoffmann, Ch., Irran, E., Kurka, A., Rosenstingl, H., Diamond, L. (1995) Crystal chemistry and optics of bazzite from Furkabasistunnel (Switzerland) \u003Ci>Mineralogy and Petrology\u003C\u002Fi>,  52 (1) 113-126 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf01163130'>doi:10.1007\u002Fbf01163130\u003C\u002Fa>","10.1007\u002Fbf01163130",{"id":160,"year":161,"html":162,"doi":11},1118654,1997,"Gaines, Richard V.; Skinner, H. Catherine W.; Foord, Eugene E.; Mason, Brian; Rosenzweig, Abraham; King, Vandall T. (1997) \u003Ci>Dana's New Mineralogy\u003C\u002Fi> (8th ed.). Wiley-Interscience. 1872 pp.",{"id":164,"year":165,"html":166,"doi":167},63420,2000,"Gramaccioli, C. M., Diella, V., Demartin, F., Orlandi, P., Campostrini, I. (2000) Cesian bazzite and thortveitite from Cuasso al Monte, Varese, Italy: A comparison with the material from Baveno, and inferred origin. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  38 (6) 1409-1418 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgscanmin.38.6.1409'>doi:10.2113\u002Fgscanmin.38.6.1409\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fcm\u002Fvol38\u002FCM38_1409.pdf' class='refpdflink'>\u003C\u002Fa>","10.2113\u002Fgscanmin.38.6.1409",{"id":169,"year":165,"html":170,"doi":171},63421,"Demartin, F., Gramaccioli, C. M., Pilati, T. (2000) Structure refinement of bazzite from pegmatitic and miarolitic occurrences. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  38 (6) 1419-1424 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgscanmin.38.6.1419'>doi:10.2113\u002Fgscanmin.38.6.1419\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fcm\u002Fvol38\u002FCM38_1419.pdf' class='refpdflink'>\u003C\u002Fa>","10.2113\u002Fgscanmin.38.6.1419",{"id":173,"year":174,"html":175,"doi":11},16963153,2001,"(2001) Bazzite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fbazzite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":177,"year":178,"html":179,"doi":11},16102585,2012,"www.handbookofmineralogy.com (n.d.) \u003Ca target='_blank' rel='nofollow' href='http:\u002F\u002Fwww.handbookofmineralogy.com\u002Fpdfs\u002Fbazzite.pdf'>http:\u002F\u002Fwww.handbookofmineralogy.com\u002Fpdfs\u002Fbazzite.pdf\u003C\u002Fa>\u003Ca target='_blank' href='http:\u002F\u002Fwww.handbookofmineralogy.com\u002Fpdfs\u002Fbazzite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":181,"year":182,"html":183,"doi":184},154178,2017,"Taran, Michail N., Dyar, M. Darby, Khomenko, Vladimir M., Boesenberg, Joseph S. (2017) Optical absorption, Mössbauer, and FTIR spectroscopic studies of two blue bazzites. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  44 (7) 497-507 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00269-017-0877-2'>doi:10.1007\u002Fs00269-017-0877-2\u003C\u002Fa>","10.1007\u002Fs00269-017-0877-2",{"id":186,"year":187,"html":188,"doi":189},18444541,2024,"Piilonen, Paula C.; Rowe, Ralph; Poirier, Glenn; Friis, Henrik; Robak, Chris; Bainbridge, Michael (2024) The First (and Second) Known Occurrences of Bazzite in Canada – The Quadeville Rose Quartz Quarry, Ontario, and the Bugaboo Castles Aquamarine Deposit, British Columbia – Description and Crystal Structure. \u003Ci>The Canadian Journal of Mineralogy and Petrology\u003C\u002Fi>,  62 (3). 457-478 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002F2300035'>doi:10.3749\u002F2300035\u003C\u002Fa>","10.3749\u002F2300035",[191,201,208,216,226,235],{"id":192,"source_url":193,"license_code":194,"credit_html":195,"title":196,"description":197,"author":198,"original_width":199,"original_height":200},2915,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10164305","CC BY-SA 3.0","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10164305\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Bazzite-234890.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBazzite\" class=\"extiw\" title=\"en:Bazzite\">Bazzite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Gjaidtroghöhe Mt., Große Fleiß valley, Goldberg group, Hohe Tauern Mts, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCarinthia\" class=\"extiw\" title=\"en:Carinthia\">Carinthia\u003C\u002Fa>, Austria (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-41778.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 8.7 x 4.9 x 3.6 cm.\u003C\u002Fdd>\n\u003Cdd>Bazzite is the rare scandium analogue of beryl found in few localities worldwide in miarolitic cavities in granites, granite pegmatites and in Alpine veins associated with pegmatitic minerals. A 2.0 cm, deep blue, gemmy and lustrous bazzite crystal is set in a 3.5 cm, quartz-lined vug in granitic gneiss matrix. This is a large and very uncommon crystal for this rare species and hails from mineralized clefts on Gjaidtroghohe Mountain in the Hohe Tauren Mountains of Austria. Ex. Mullane Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",750,466,{"id":202,"source_url":203,"license_code":194,"credit_html":204,"title":205,"description":197,"author":198,"original_width":206,"original_height":207},2916,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10164307","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10164307\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Bazzite-234891.jpg",600,572,{"id":209,"source_url":210,"license_code":194,"credit_html":211,"title":212,"description":213,"author":214,"original_width":215,"original_height":206},2917,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=16219136","Leon Hupperichs, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=16219136\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Bazzite-401670.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBazzite\" class=\"extiw\" title=\"en:Bazzite\">Bazzite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: A4 Highway tunnel, Thiemendorf, Görlitz, Oberlausitz, Saxony, Germany (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-22273.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Field of view 3 mm. Specimen and photo Leon Hupperichs.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Leon Hupperichs",695,{"id":217,"source_url":218,"license_code":219,"credit_html":220,"title":221,"description":222,"author":223,"original_width":224,"original_height":225},2918,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=16219425","Public domain","Sergio Varvello, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=16219425\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Bazzite-184999.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBazzite\" class=\"extiw\" title=\"en:Bazzite\">Bazzite\u003C\u002Fa> \n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Seula Mine (ex Montecatini quarry), Mount Camoscio, Oltrefiume, Baveno, Verbano-Cusio-Ossola Province, Piedmont, Italy\u003C\u002Fdd>\n\u003Cdd>\u003Ci>Original description:\u003C\u002Fi> bazzite - a 2 mm crystal on albite and orthoclase, self collected november 2007, sergio varvello photo and collection\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Sergio Varvello",1024,768,{"id":227,"source_url":228,"license_code":194,"credit_html":229,"title":230,"description":231,"author":232,"original_width":233,"original_height":234},2919,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=16242774","Joachim Esche, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=16242774\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Bazzite - Fibbia Ticino Switzerland.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBazzite\" class=\"extiw\" title=\"en:Bazzite\">Bazzite\u003C\u002Fa> (image width: 2.6 mm mm)\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Fibbia Mountain, Fontana, Central St Gotthard Massif, Leventina, Ticino (Tessin), Switzerland\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Joachim Esche",1327,965,{"id":236,"source_url":237,"license_code":238,"credit_html":239,"title":240,"description":241,"author":242,"original_width":243,"original_height":244},35227,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163485504","CC0 1.0","Shannon Heinle, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163485504\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Bazzite (GeoDIL number - 1868).jpg","Bazzite is the scandium rich variety of beryl, with the scandium replacing some of the aluminum. Usually it is classified as an individual mineral species and not as a variety of beryl. The chemical formula is Be3(Sc,Al)2Si6O18. Bazzite is named after the Italian engineer, A. E. Bazzi. This sample is approximately 11 cm.","Shannon Heinle",2128,1872,[246,252],{"id":247,"url":248,"label":249,"formula":250,"spacegroup":251,"year":165},1338,"\u002Fcif\u002F1338.cif","Demartin 2000 · (Sc1.52 Fe.48) Si6 Cs.1 O18.9 Na.44 Be3 H1.8","(Sc1.52 Fe.48) Si6 Cs.1 O18.9 Na.44 Be3 H1.8","P 6\u002Fm c c",{"id":253,"url":254,"label":255,"formula":256,"spacegroup":251,"year":165},1339,"\u002Fcif\u002F1339.cif","Demartin 2000 · (Sc1.36 Fe.52 Al.12) Si6 Cs.14 O18.86 Na.36 (Be2.91 Li.09) H1.72","(Sc1.36 Fe.52 Al.12) Si6 Cs.14 O18.86 Na.36 (Be2.91 Li.09) H1.72",[],[259,263,267,271,275,278,282,287,290,295,299,303,307,311,314,318,322,326,330],{"lang":260,"names":261},"ar",[262],"بازيت",{"lang":264,"names":265},"ca",[266],"bazzita",{"lang":268,"names":269},"de",[270],"Bazzit",{"lang":272,"names":273},"es",[274],"Bazzita",{"lang":276,"names":277},"eu",[274],{"lang":279,"names":280},"fa",[281],"بازیت",{"lang":283,"names":284},"fr",[285,286],"bazzite","beryl bleu",{"lang":288,"names":289},"it",[7],{"lang":291,"names":292},"ja",[293,294],"バッジ石","バッツィ石",{"lang":296,"names":297},"mk",[298],"Базит",{"lang":300,"names":301},"mn",[302],"Баццит",{"lang":304,"names":305},"nb",[306],"bazzitt",{"lang":308,"names":309},"nl",[310],"bazziet",{"lang":312,"names":313},"nn",[306],{"lang":315,"names":316},"pl",[317],"Bazzyt",{"lang":319,"names":320},"sr",[321],"базит",{"lang":323,"names":324},"sr-ec",[325],"bazit",{"lang":327,"names":328},"uk",[329],"Бацит",{"lang":331,"names":332},"zh",[333],"钪绿柱石","Q412938",{"history":11,"applications":11}]