[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:241":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":23,"key_elements":11,"impurities":24,"cim":25,"ima_status":26,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":11,"discovery_year":29,"strunz10ed1":30,"strunz10ed2":31,"strunz10ed3":32,"strunz10ed4":33,"dana8ed1":34,"dana8ed2":35,"dana8ed3":36,"dana8ed4":37,"csystem":38,"cclass":39,"spacegroup":40,"spacegroupset":41,"a":42,"b":43,"c":44,"alpha":45,"beta":46,"gamma":45,"aerror":47,"berror":48,"cerror":47,"alphaerror":11,"betaerror":49,"gammaerror":11,"va3":11,"z":50,"csmetamict":14,"commentcrystal":11,"twinning":51,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":52,"tlform":11,"hmin":53,"hmax":54,"hardtype":11,"vhnmin":45,"vhnmax":45,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":55,"dmeas2":55,"dcalc":56,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":57,"lustretype":58,"commentluster":11,"diapheny":59,"streak":11,"colour":60,"commentcolor":11,"colors":61,"streak_colors":11,"luminescence":11,"uv":11,"cleavage":64,"cleavagetype":65,"fracturetype":11,"tenacity":66,"commentbreak":11,"opticaltype":67,"opticalsign":68,"opticalalpha":69,"opticalalpha2":70,"opticalalphaerror":11,"opticalbeta":71,"opticalbeta2":45,"opticalbetaerror":11,"opticalgamma":72,"opticalgamma2":73,"opticalgammaerror":11,"opticalomega":45,"opticalomega2":45,"opticalomegaerror":11,"opticalepsilon":45,"opticalepsilon2":45,"opticalepsilonerror":11,"opticaln":45,"opticaln2":45,"opticalnerror":11,"optical2vcalc":74,"optical2vcalc2":75,"optical2vcalcerror":11,"optical2vmeasured":45,"optical2vmeasured2":76,"optical2vmeasurederror":11,"rimin":77,"rimax":78,"opticaldispersion":79,"opticalpleochroism":11,"opticalpleochorismdesc":80,"opticalbirefringence":11,"opticalcomments":81,"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":82,"otheroccurrence":83,"type_specimen_store":11,"description_short":84,"aboutname":85,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":86,"reviewed_at":11,"variety_of":11,"varieties":87,"group_members":88,"associates":143,"confused_with":176,"type_localities":183,"occurrence_total":190,"citations":191,"images":263,"structures":393,"synonyms":423,"language_names":426,"wikidata_qid":477,"texts":478},241,"1:1:241:1","75bac520-9e95-4ab1-9304-c534b75c5272","Annite","Ann",0,"mineral",null,677,2273,false,"KFe\u003Csup>2+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(AlSi\u003Csub>3\u003C\u002Fsub>O\u003Csub>10\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub>",[17,18,19,20,21,22],"Al","Fe","Si","O","K","H",[17,18,19,20,21,22],",Ti,Mn,Mg,Ca,Na,K,Cl,","16.18.4",[27,28],"APPROVED","GRANDFATHERED","1868","9","E","C","20","71","2","2b","3","Monoclinic",5,11,"C2\u002Fm ","5.3860","9.3241","10.2683","0","100.63",9,7,1,2,"Contact twins, composition surface {001}, twin axis [310].","Tabular crystals or cleavage fragments, both having pseudohexagonal outlines, up to 15 cm in size; foliated masses.",2.5,3,"3.3","3.36","Adamantine, Vitreous","Vitreous","Transparent,Translucent","Black, brown",[62,63],"black","brown","{001}","Perfect","flexible","Biaxial","-","1.625","1.631","1.69","1.691","1.697","12","36","25",1.625,1.697,"weak to distinct (r \u003C v)","brown (X), dark brown (Y=Z)","Orientation: Y=b; measured 2V according to the Handbook of Mineralogy is from 0 to 5 deg.","Granite","Mg-low igneous and metamorphic rocks; associated minerals at Rockport, MA, USA.","Mica Group. Biotite series, forms a series with Phlogopite and other micas. \r\nThe Fe analogue of phlogopite, shirozulite, and hendricksite. The Al analogue of tetraferriannite. The hydroxyl analogue of fluorannite. Also the K analogue of the rubidium-d...","Originally named in 1868 by James Dwight Dana for a ferrian mica, but redefined as a ferroan mica by Alexander N. Winchell in 1925. Both authors named a mineral after the same locality at Rockport, Cape Ann, Essex Co., Massachusetts, USA.","2026-04-10 11:49:11",[],[89,95,101,107,114,120,127,134,139],{"id":90,"name":91,"entrytype":9,"csystem":38,"ima_formula":92,"mindat_formula":93,"hmin":11,"hmax":11,"dmeas":45,"dcalc":45,"primary_image_id":94},6909,"Eastonite","KAlMg\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>Al\u003Csub>2\u003C\u002Fsub>)O\u003Csub>10\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>","KMg\u003Csub>2\u003C\u002Fsub>Al(Al\u003Csub>2\u003C\u002Fsub>Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>10\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub>",7581,{"id":96,"name":97,"entrytype":9,"csystem":38,"ima_formula":98,"mindat_formula":98,"hmin":54,"hmax":54,"dmeas":99,"dcalc":100,"primary_image_id":11},10333,"Fluorannite","KFe\u003Csup>2+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(Si\u003Csub>3\u003C\u002Fsub>Al)O\u003Csub>10\u003C\u002Fsub>F\u003Csub>2\u003C\u002Fsub>","3.16","3.23",{"id":102,"name":103,"entrytype":9,"csystem":38,"ima_formula":104,"mindat_formula":104,"hmin":50,"hmax":54,"dmeas":45,"dcalc":105,"primary_image_id":106},29139,"Fluorophlogopite","KMg\u003Csub>3\u003C\u002Fsub>(Si\u003Csub>3\u003C\u002Fsub>Al)O\u003Csub>10\u003C\u002Fsub>F\u003Csub>2\u003C\u002Fsub>","2.83",9220,{"id":108,"name":109,"entrytype":9,"csystem":38,"ima_formula":110,"mindat_formula":111,"hmin":54,"hmax":112,"dmeas":11,"dcalc":113,"primary_image_id":11},40156,"Fluorotetraferriphlogopite","KMg\u003Csub>3\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>Si\u003Csub>3\u003C\u002Fsub>O\u003Csub>10\u003C\u002Fsub>F\u003Csub>2\u003C\u002Fsub>","KMg\u003Csub>3\u003C\u002Fsub>(Fe\u003Csup>3+\u003C\u002Fsup>Si\u003Csub>3\u003C\u002Fsub>O\u003Csub>10\u003C\u002Fsub>)F\u003Csub>2\u003C\u002Fsub>",4,"2.966",{"id":115,"name":116,"entrytype":9,"csystem":38,"ima_formula":117,"mindat_formula":117,"hmin":54,"hmax":54,"dmeas":118,"dcalc":119,"primary_image_id":11},39713,"Oxyphlogopite","K(Mg,Ti,Fe)\u003Csub>3\u003C\u002Fsub>[(Si,Al)\u003Csub>4\u003C\u002Fsub>O\u003Csub>10\u003C\u002Fsub>](O,F)\u003Csub>2\u003C\u002Fsub>","3.06","3.086",{"id":121,"name":122,"entrytype":9,"csystem":38,"ima_formula":123,"mindat_formula":123,"hmin":50,"hmax":54,"dmeas":124,"dcalc":125,"primary_image_id":126},3193,"Phlogopite","KMg\u003Csub>3\u003C\u002Fsub>(AlSi\u003Csub>3\u003C\u002Fsub>O\u003Csub>10\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub>","2.78","2.79",19310,{"id":128,"name":129,"entrytype":9,"csystem":38,"ima_formula":130,"mindat_formula":131,"hmin":53,"hmax":54,"dmeas":132,"dcalc":133,"primary_image_id":11},3651,"Siderophyllite","KFe\u003Csup>2+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Al(Si\u003Csub>2\u003C\u002Fsub>Al\u003Csub>2\u003C\u002Fsub>)O\u003Csub>10\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>","KFe\u003Csup>2+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Al(Al\u003Csub>2\u003C\u002Fsub>Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>10\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub>","3.1","3.17",{"id":135,"name":136,"entrytype":9,"csystem":38,"ima_formula":137,"mindat_formula":137,"hmin":53,"hmax":54,"dmeas":45,"dcalc":45,"primary_image_id":138},7333,"Tetraferriannite","KFe\u003Csup>2+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(Si\u003Csub>3\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>)O\u003Csub>10\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>",23919,{"id":140,"name":141,"entrytype":9,"csystem":38,"ima_formula":142,"mindat_formula":142,"hmin":11,"hmax":11,"dmeas":45,"dcalc":45,"primary_image_id":11},3922,"Tetraferriphlogopite","KMg\u003Csub>3\u003C\u002Fsub>(Si\u003Csub>3\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>)O\u003Csub>10\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>",[144,152,160,167],{"id":145,"name":146,"entrytype":9,"csystem":147,"ima_formula":148,"mindat_formula":149,"hmin":54,"hmax":54,"dmeas":150,"dcalc":45,"primary_image_id":151},405,"Astrophyllite","Triclinic","K\u003Csub>2\u003C\u002Fsub>NaFe\u003Csup>2+\u003C\u002Fsup>\u003Csub>7\u003C\u002Fsub>Ti\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>4\u003C\u002Fsub>O\u003Csub>12\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>F","K\u003Csub>2\u003C\u002Fsub>NaFe\u003Csup>2+\u003C\u002Fsup>\u003Csub>7\u003C\u002Fsub>Ti\u003Csub>2\u003C\u002Fsub>[Si\u003Csub>4\u003C\u002Fsub>O\u003Csub>12\u003C\u002Fsub>]\u003Csub>2\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>F","3.2",2224,{"id":153,"name":154,"entrytype":9,"csystem":155,"ima_formula":156,"mindat_formula":156,"hmin":112,"hmax":112,"dmeas":157,"dcalc":158,"primary_image_id":159},1576,"Fluorite","Isometric","CaF\u003Csub>2\u003C\u002Fsub>","3.175","3.181",29727,{"id":161,"name":162,"entrytype":9,"csystem":38,"ima_formula":163,"mindat_formula":164,"hmin":39,"hmax":165,"dmeas":166,"dcalc":45,"primary_image_id":11},2050,"Ishikawaite","(U,Fe,Y)NbO\u003Csub>4\u003C\u002Fsub>","U\u003Csup>4+\u003C\u002Fsup>Fe\u003Csup>2+\u003C\u002Fsup>Nb\u003Csub>2\u003C\u002Fsub>O\u003Csub>8\u003C\u002Fsub>",6,"6.2",{"id":168,"name":169,"entrytype":9,"csystem":170,"ima_formula":171,"mindat_formula":171,"hmin":172,"hmax":172,"dmeas":173,"dcalc":174,"primary_image_id":175},4421,"Zircon","Tetragonal","Zr(SiO\u003Csub>4\u003C\u002Fsub>)",7.5,"4.6","4.714",31046,[177],{"id":178,"name":179,"entrytype":9,"csystem":38,"ima_formula":180,"mindat_formula":180,"hmin":53,"hmax":54,"dmeas":45,"dcalc":181,"primary_image_id":182},4309,"Wonesite","(Na,K,◻)(Mg,Fe,Al)\u003Csub>6\u003C\u002Fsub>(Si,Al)\u003Csub>8\u003C\u002Fsub>O\u003Csub>20\u003C\u002Fsub>(OH,F)\u003Csub>4\u003C\u002Fsub>","2.89",28204,[184],{"id":185,"txt":186,"latitude":187,"longitude":188,"country":189},3825,"Rockport, Essex County, Massachusetts, USA",42.6555556,-70.6202778,"USA",382,[192,195,199,203,208,212,216,221,226,231,235,239,244,249,253,258],{"id":193,"year":11,"html":194,"doi":11},18462687,"D.R. Wones, R.G. Burns, B.M. Carrol (1971): Stability and properties of synthetic annite, Am. Geophys. Union Trans. 52, 369.",{"id":196,"year":197,"html":198,"doi":11},16100734,1867,"Cooke, J.P. Jr. (1867) On cryophyllite, a new mineral species of the mica family, with some associated minerals in the granite of Rockport, Massachusetts. American Journal of Science: II(43): 217-230. (as lepidomelane)",{"id":200,"year":201,"html":202,"doi":11},1118643,1868,"Dana, James D., Brush, George Jarvis (1868) \u003Ci>A System of Mineralogy\u003C\u002Fi> (5th ed.). p.882",{"id":204,"year":205,"html":206,"doi":207},144350,1957,"Yoder, Hatten S. (1957) Experimental Studies on Micas: A Synthesis. \u003Ci>Clays and Clay Minerals\u003C\u002Fi>,  6 (1) 42-60 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1346\u002Fccmn.1957.0060105'>doi:10.1346\u002Fccmn.1957.0060105\u003C\u002Fa>","10.1346\u002Fccmn.1957.0060105",{"id":209,"year":210,"html":211,"doi":11},526136,1973,"Hazen, Robert M., Burnham, and Charles W. (1973) The crystal structures of one-layer phlogopite and annite. \u003Ci>American Mineralogist\u003C\u002Fi>,  58 (9-10) 889-900 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM58\u002FAM58_889.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":213,"year":214,"html":215,"doi":11},16100738,1981,"Kwak, T.A.P. (1981) Sector–zoned annite85phlogopite15 micas from the Mt. Lindsay Sn—W—F(—Be) deposit, Tasmania, Australia. The Canadian Mineralogist: 19: 643-650.",{"id":217,"year":218,"html":219,"doi":220},1490,1989,"Tlili, A., Smith, D. C., Beny, J.-M., Boyer, H. (1989) A Raman microprobe study of natural micas. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  53 (370) 165-179 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1989.053.370.04'>doi:10.1180\u002Fminmag.1989.053.370.04\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_53\u002F53-370-165.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1989.053.370.04",{"id":222,"year":223,"html":224,"doi":225},152145,1993,"Redhammer, G.J.; Beran, A.; Dachs, E.; Amthauer, G. (1993) A Mössbauer and X-ray diffraction study of annites synthesized at different oxygen fugacities and crystal chemical implications. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  20 (6). 382-394 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf00203107'>doi:10.1007\u002Fbf00203107\u003C\u002Fa>","10.1007\u002Fbf00203107",{"id":227,"year":228,"html":229,"doi":230},152289,1995,"Redhammer, G.J.; Dachs, E.; Amthauer, G. (1995) Mössbauer spectroscopic and x-ray powder diffraction studies of synthetic micas on the join annite KFe3AlSi3O10(OH)2-phlogopite KMg3AlSi3O10(OH)2. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  22 (5). 282-294 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf00202768'>doi:10.1007\u002Fbf00202768\u003C\u002Fa>","10.1007\u002Fbf00202768",{"id":232,"year":233,"html":234,"doi":11},15949274,1998,"Rieder, M., Cavazzini, G., D’Yakonov, Y.S., Frank-Kamenetskii, V.A., Gottardt, G., Guggenheim, S., Koval, P.V., Muller, G., Neiva, A.M.R., Radoslovich, E.W., Robert, J.L., Sassi, F.P., Takeda, H., Weiss, Z., Wones, D.R. (1998) Nomenclature of the micas. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  36 (3) 905-912 \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fuploads\u002FCM36_905.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":236,"year":237,"html":238,"doi":11},16962902,2001,"(2001) Annite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fannite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":240,"year":241,"html":242,"doi":243},16689,2005,"Redhammer, G. J., Amthauer, G., Lottermoser, W., Bernroider, M., Tippelt, G., Roth, G. (2005) X-ray powder diffraction and 57Fe – Mössbauer spectroscopy of synthetic trioctahedral micas {K}[Me3]⟨TSi3⟩O10(OH)2, Me = Ni2+, Mg2+, Co2+, Fe2+; T = Al3+, Fe3+. \u003Ci>Mineralogy and Petrology\u003C\u002Fi>,  85 (1-2). 89-115 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00710-005-0096-2'>doi:10.1007\u002Fs00710-005-0096-2\u003C\u002Fa>","10.1007\u002Fs00710-005-0096-2",{"id":245,"year":246,"html":247,"doi":248},676430,2009,"Ogorodova, L. P., Kiseleva, I. A., Mel’chakova, L. V., Shuriga, T. N. (2009) Formation enthalpy of natural annite and biotite. \u003Ci>Geochemistry International\u003C\u002Fi>,  47 (1) 105-108 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1134\u002Fs001670290901008x'>doi:10.1134\u002Fs001670290901008x\u003C\u002Fa>","10.1134\u002Fs001670290901008x",{"id":250,"year":251,"html":252,"doi":11},16100989,2016,"Anthony, John W., Bideaux, Richard A., Bladh, Kenneth W., Nichols, Monte C. - \u003Ci>Eds.\u003C\u002Fi> (2016) Handbook of Mineralogy. \u003Ca target='_blank' rel='nofollow' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002F'>https:\u002F\u002Fwww.handbookofmineralogy.org\u002F\u003C\u002Fa>",{"id":254,"year":255,"html":256,"doi":257},16100741,2022,"Aspiotis, Stylianos, Schlüter, Jochen, Redhammer, Günther J., Mihailova, Boriana (2022) Non-destructive determination of the biotite crystal chemistry using Raman spectroscopy: how far we can go? \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  34 (6). 573-590 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-34-573-2022'>doi:10.5194\u002Fejm-34-573-2022\u003C\u002Fa>","10.5194\u002Fejm-34-573-2022",{"id":259,"year":260,"html":261,"doi":262},17565503,2024,"Dubacq, Benoît, Forshaw, Jacob B. (2024) The composition of metapelitic biotite, white mica, and chlorite: a review with implications for solid-solution models. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  36 (4). 657-685 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-36-657-2024'>doi:10.5194\u002Fejm-36-657-2024\u003C\u002Fa>","10.5194\u002Fejm-36-657-2024",[264,274,284,293,301,309,317,326,331,339,347,357,365,371,377,387],{"id":265,"source_url":266,"license_code":267,"credit_html":268,"title":269,"description":270,"author":271,"original_width":272,"original_height":273},1491,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10456207","CC BY-SA 3.0","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10456207\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Annite-pas-130ab.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnnite\" class=\"extiw\" title=\"en:Annite\">Annite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRockport\" class=\"extiw\" title=\"en:Rockport\">Rockport\u003C\u002Fa>, Essex County, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMassachusetts\" class=\"extiw\" title=\"en:Massachusetts\">Massachusetts\u003C\u002Fa>, USA (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-3825.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: small cabinet, 6.8 x 5.4 x 4.6 cm\n\u003Cdl>\u003Cdt>Annite\u003C\u002Fdt>\u003C\u002Fdl>\u003C\u002Fdd>\n\u003Cdd>According to MINDAT this is an extremely rare member of the Mica Group in the Biotite-Phlogopite Series. Regardless, its the most oddly crystallized mica I have seen. It looks more like a dark phosphate than a mica. From the TYPE LOCALITY where it was first noted in 1868!\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",340,400,{"id":275,"source_url":276,"license_code":277,"credit_html":278,"title":279,"description":280,"author":281,"original_width":282,"original_height":283},1495,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150434617","Public domain","Modris Baum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150434617\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Annite-283530.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnnite\" class=\"extiw\" title=\"en:Annite\">Annite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Field of view: 2.3 mm × 2.7 mm\u003C\u002Fdd>\n\u003Cdd>Locality: Poudrette quarry (De-Mix quarry; Demix quarry; Uni-Mix quarry; Carrière Mont Saint-Hilaire; MSH), Mont Saint-Hilaire, La Vallée-du-Richelieu RCM, Montérégie, Québec, Canada\u003C\u002Fdd>\n\u003Cdd>Description: This is actually a penkvilksite specimen. But these annite xls have rather interesting stepped terminations. This is from marble xenolith. The purple stuff is disseminated fluorite. Other associated minerals are calcite (in several habits including tabular hex) and (perhaps) tabular labuntsovite. Note August 2021: Originally posted as \"biotite\" because the specimen is from a marble xenolith, and one would expect phlogopite\" or fluorophlogopite rather than annite in this environment. Lacking analytical data I chose the generic \"biotite\". However, per the discussion of MSH micas in Horváth et al (2019), and the environment specific rarity tables therein, very dark micas, such as this - even from marble xenoliths - are almost certainly annite. (That said, annite is considered to be very are in this environment - not that \"phlogopite\" is very common.)\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Modris Baum",2353,2789,{"id":285,"source_url":286,"license_code":277,"credit_html":287,"title":288,"description":289,"author":290,"original_width":291,"original_height":292},1492,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=11648396","Sncervantes, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=11648396\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Annite sample.jpg","Annite sample.","Sncervantes",1712,2560,{"id":294,"source_url":295,"license_code":277,"credit_html":296,"title":297,"description":298,"author":281,"original_width":299,"original_height":300},1493,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150426077","Modris Baum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150426077\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Annite-184502.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnnite\" class=\"extiw\" title=\"en:Annite\">Annite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Field of view: ca. 4.8 × 3.4 cm – long crystal in center is ~ 2.5 cm\u003C\u002Fdd>\n\u003Cdd>Locality: Poudrette quarry (De-Mix quarry; Demix quarry; Uni-Mix quarry; Carrière Mont Saint-Hilaire; MSH), Mont Saint-Hilaire, La Vallée-du-Richelieu RCM, Montérégie, Québec, Canada\u003C\u002Fdd>\n\u003Cdd>Description: Found late 1990s. Not analyzed. Just an example of macro anite from MSH. Concentrations of large annite are not rare here. Update August 2021: Originally posted as \"biotite\", but per Horváth et al (2019), this is almost certainly annite. The only other \"black\" mica, siderophyllite, is very rare at MSH, and is not found in the cores of a pegmatites.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",3388,2428,{"id":302,"source_url":303,"license_code":267,"credit_html":304,"title":305,"description":306,"author":271,"original_width":307,"original_height":308},33112,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159377","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159377\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Annite-202026.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnnite\" class=\"extiw\" title=\"en:Annite\">Annite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRockport\" class=\"extiw\" title=\"en:Rockport\">Rockport\u003C\u002Fa>, Essex County, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMassachusetts\" class=\"extiw\" title=\"en:Massachusetts\">Massachusetts\u003C\u002Fa>, USA (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-3825.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 6.8 x 5.4 x 4.6 cm.\u003C\u002Fdd>\n\u003Cdd>According to MINDAT this is a very rare member of the Mica Group in the Biotite-Phlogopite Series. Regardless, it’s the most oddly crystallized mica I have seen. It looks more like a dark phosphate than a mica. From the TYPE LOCALITY where it was first noted in 1868. Ex. Academy of Natural Sciences Philadelphia Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",674,800,{"id":310,"source_url":311,"license_code":277,"credit_html":312,"title":313,"description":314,"author":281,"original_width":315,"original_height":316},1494,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150434297","Modris Baum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150434297\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Annite-184503.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnnite\" class=\"extiw\" title=\"en:Annite\">Annite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCalcite\" class=\"extiw\" title=\"en:Calcite\">Calcite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FPectolite\" class=\"extiw\" title=\"en:Pectolite\">Pectolite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGrossular\" class=\"extiw\" title=\"en:Grossular\">Grossular\u003C\u002Fa> (Var: \u003Ci>Hibschite\u003C\u002Fi>), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FPyrrhotite\" class=\"extiw\" title=\"en:Pyrrhotite\">Pyrrhotite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Field of view: ca. 2.6 cm × 3.5 cm – The black annite cystal is about 2.5 cm tall\u003C\u002Fdd>\n\u003Cdd>Locality: Poudrette quarry (De-Mix quarry; Demix quarry; Uni-Mix quarry; Carrière Mont Saint-Hilaire; MSH), Mont Saint-Hilaire, La Vallée-du-Richelieu RCM, Montérégie, Québec, Canada\u003C\u002Fdd>\n\u003Cdd>Description: Found August 1997. Update August 2021: Originally posted as \"biotite\", but according to Horváth et al (2019), it i safe to assume that almost all black mica at MSH is annite. There are rare exceptions, in particular siderophyllite, but that has not been reported from the marble xenolith environment which this specimen is from. That said, it should be noted that annite is a rare mineral in this environemnt. Phlogopite is much more common, but it does not get quite this dark. In any case, this is a rather strange xl - almost square in cross section. But see \u003Ca rel=\"nofollow\" class=\"external free\" href=\"http:\u002F\u002Fwww.mindat.org\u002Fphoto-34791.html\">http:\u002F\u002Fwww.mindat.org\u002Fphoto-34791.html\u003C\u002Fa> for an example of four sided annite from the Eifel. The associated hibschite is also very strange - it is nearly black. The largest of these, showing the characteristic stepped growth and rounded octahedral form can be seen just to the right of the biotite xl. The fact that the hibschite is so dark does suggest that the mica crystal might be coated rather than inherently dark. But as can be seen from the plates that have \"parted\", the interior of the crystal is just as dark. Other associated minerals are greenish yellow calcite (mostly in the lower half of the photo), partly fibrous pectolite (mostly at the top), and a bit of brassy pyrrhotite (on the left). Update May 2023: Thanks to my new LED MW UV source, I have recently discovered that the cavity lining consists, in part, of a mixture of calcite and wollastonite with abundant cuspidine. See \u003Ca rel=\"nofollow\" class=\"external free\" href=\"https:\u002F\u002Fwww.mindat.org\u002Fphoto-1298359.html\">https:\u002F\u002Fwww.mindat.org\u002Fphoto-1298359.html\u003C\u002Fa>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",2415,3228,{"id":318,"source_url":319,"license_code":277,"credit_html":320,"title":321,"description":322,"author":323,"original_width":324,"original_height":325},1496,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150436556","Jerry Cone, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150436556\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Annite-984121.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnnite\" class=\"extiw\" title=\"en:Annite\">Annite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Field of view: 1.8 mm\u003C\u002Fdd>\n\u003Cdd>Locality: Poudrette quarry (De-Mix quarry; Demix quarry; Uni-Mix quarry; Carrière Mont Saint-Hilaire; MSH), Mont Saint-Hilaire, La Vallée-du-Richelieu RCM, Montérégie, Québec, Canada\u003C\u002Fdd>\n\u003Cdd>The analyst had trouble locking in on this shiny black specimen because of lots of charging. He interprets this spectrum as a poor annite pattern (the lower end is suppressed). It was collected on 8\u002F14\u002F1993.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Jerry Cone",5128,3572,{"id":327,"source_url":328,"license_code":277,"credit_html":329,"title":330,"description":289,"author":290,"original_width":291,"original_height":292},33114,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=11648389","Sncervantes, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=11648389\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","IMAG0426.jpg",{"id":332,"source_url":333,"license_code":277,"credit_html":334,"title":335,"description":336,"author":337,"original_width":338,"original_height":338},33111,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1955898","Dave Dyet http:\u002F\u002Fwww.shutterstone.com http:\u002F\u002Fwww.dyet.com, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1955898\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Annite w-almandine Basic potassium iron aluminum silicate and fluoride Kawai Mine Ena shi Gifu Prefecture Japan 2083.jpg","These mineral images are free to use how you wish.","Dave Dyet http:\u002F\u002Fwww.shutterstone.com http:\u002F\u002Fwww.dyet.com",640,{"id":340,"source_url":341,"license_code":277,"credit_html":342,"title":343,"description":344,"author":281,"original_width":345,"original_height":346},1498,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150437190","Modris Baum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150437190\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Annite-1161454.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnnite\" class=\"extiw\" title=\"en:Annite\">Annite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Field of view: 6.8 mm – largest crystal 3.6 mm\u003C\u002Fdd>\n\u003Cdd>Locality: Poudrette quarry (De-Mix quarry; Demix quarry; Uni-Mix quarry; Carrière Mont Saint-Hilaire; MSH), Mont Saint-Hilaire, La Vallée-du-Richelieu RCM, Montérégie, Québec, Canada\u003C\u002Fdd>\n\u003Cdd>Description: These crystals are embedded in a calcareous matrix which separates cleanly from the annite crystals, leaving very sharp casts. One such cast can be seen on the upper right, but in this “flat” photo it looks like a coated annite crystal. If you can fuse the stereo images (child photo), you will see that it is actually a cast. Only the black part at the “top” is part of an annite crystal. Most of the annite crystals on this specimen occur as an inter-grown “rind” of apparently free-growing crystals surrounding a calcareous “blob” of no apparent symmetry. Some of the annite crystals (such as the ones in this photo) were embedded in the blob.\u003Cbr>Based on the descriptions given by Horváth et al (2019, p. 262-3, 299 & 346), this material was suspected to similar to the “biotite xenolith” (1976) which produced låvenite, petarasite, and nordstrandite, but none of those minerals has been found on specimens from this find. (Some further analysis is anticipated.) Associated minerals in this find include “astrophyllite supergroup”, some of it exhibiting an odd “centipede-like” habit \u003Ca rel=\"nofollow\" class=\"external autonumber\" href=\"https:\u002F\u002Fwww.mindat.org\u002Fphoto-177899.html\">[1]\u003C\u002Fa>, small natrolite and “ancylite” crystals, and very sparse aegirine and pyrite, some of the latter as thin films on the casts. Also present are yellow\u002Forange, mostly anhedral, but gemmy, grains, some of which appear to be altering, variously to a grainy white, tan, or yellowish substances.\u003Cbr>Possibly this might be petarasite, but the habit is ambiguous. “Eudialyte group” might be another possibility. The only euhedral crystal of this yellow material that I found is shown in \u003Ca rel=\"nofollow\" class=\"external autonumber\" href=\"https:\u002F\u002Fwww.mindat.org\u002Fphoto-1161489.html\">[2]\u003C\u002Fa>, which see for further discussion. The annite from this find has not been analyzed, but according to Horváth et al (2019), “nearly all biotite reported from Mont Saint-Hilaire ... is annite”, so “annite” is a very likely ID.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",4947,2946,{"id":348,"source_url":349,"license_code":350,"credit_html":351,"title":352,"description":353,"author":354,"original_width":355,"original_height":356},33117,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=85250185","CC BY 3.0","Douglas Watts, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=85250185\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cancrinite, Nepheline, Sodalite, Annite-463949.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCancrinite\" class=\"extiw\" title=\"en:Cancrinite\">Cancrinite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FNepheline\" class=\"extiw\" title=\"en:Nepheline\">Nepheline\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSodalite\" class=\"extiw\" title=\"en:Sodalite\">Sodalite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnnite\" class=\"extiw\" title=\"en:Annite\">Annite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Dennis Hill locality (Litchfield sodalite locality), Litchfield, Kennebec County, Maine, USA\u003C\u002Fdd>\n\u003Cdd>Description: 1.5 cm polished section of Litchfieldite, showing yellow cancrinite, greenish nepheline, black annite, blue sodalite and white albite from Dennis Hill, Litchfield, Maine along Rt. 126.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Douglas Watts",1070,767,{"id":358,"source_url":359,"license_code":277,"credit_html":360,"title":361,"description":362,"author":281,"original_width":363,"original_height":364},33119,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150435927","Modris Baum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150435927\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Annite stereo-1361691.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnnite\" class=\"extiw\" title=\"en:Annite\">Annite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMicrocline\" class=\"extiw\" title=\"en:Microcline\">Microcline\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FQuartz\" class=\"extiw\" title=\"en:Quartz\">Quartz\u003C\u002Fa> (Var: \u003Ci>Smoky Quartz\u003C\u002Fi>)\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Dimensions: 6 cm × 5 cm × 5.5 cm\u003C\u002Fdd>\n\u003Cdd>Locality: Poudrette quarry (De-Mix quarry; Demix quarry; Uni-Mix quarry; Carrière Mont Saint-Hilaire; MSH), Mont Saint-Hilaire, La Vallée-du-Richelieu RCM, Montérégie, Québec, Canada\u003C\u002Fdd>\n\u003Cdd>Description: Found 7\u002F17\u002F99. This is a stereo pair – but the images don’t need to be viewed in 3D. Annite is a very common mineral in the pegmatites at MSH. This is not an exceptionally large crystal. But the crystals are almost always embedded in matrix and impossible to extract undamaged. In this case the matrix consists mostly of very fluorescent “feldspar” (probably microcline – red under SW and magenta under MW, the latter being somewhat unusual) and massive smoky quartz. Some of the quartz has rims of fluorescent sodalite. There are also minor amounts of franconite, zircon, and an altered – nearly black – rhombohedral carbonate in a small cavity on the back.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",7506,3304,{"id":366,"source_url":367,"license_code":277,"credit_html":368,"title":369,"description":362,"author":281,"original_width":370,"original_height":364},33120,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150436019","Modris Baum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150436019\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Annite stereo-1361691 (single left).jpg",3755,{"id":372,"source_url":373,"license_code":277,"credit_html":374,"title":375,"description":362,"author":281,"original_width":376,"original_height":364},33121,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150436191","Modris Baum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=150436191\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Annite stereo-1361691 (single right).jpg",3746,{"id":378,"source_url":379,"license_code":380,"credit_html":381,"title":382,"description":383,"author":384,"original_width":385,"original_height":386},63429,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=180411641","CC BY-SA 4.0","Марися Лебідь, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=180411641\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Кіаніт в Мінералогічному музеї імені Євгена Лазаренка.jpg","Minerals in Yevhen Lazarenko Mineralogical Museum","Марися Лебідь",4080,3060,{"id":388,"source_url":389,"license_code":380,"credit_html":390,"title":391,"description":392,"author":384,"original_width":385,"original_height":386},63430,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=180416026","Марися Лебідь, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=180416026\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Кіаніт у Мінералогічному музеї.jpg","Minerals in the Mineralogical Museum of Lviv",[394,401,406,412,417],{"id":395,"url":396,"label":397,"formula":398,"spacegroup":399,"year":400},623,"\u002Fcif\u002F623.cif","Laurora 2007 · (K.93 Na.07) Mg1.02 Fe1.41 Ti.46 (Al1.28 Si2.72) O12","(K.93 Na.07) Mg1.02 Fe1.41 Ti.46 (Al1.28 Si2.72) O12","C 1 2\u002Fm 1",2007,{"id":402,"url":403,"label":404,"formula":405,"spacegroup":399,"year":400},624,"\u002Fcif\u002F624.cif","Laurora 2007 · K.92 Na.07 Mg1.11 Fe1.35 Ti.18 Al1.34 Si2.72 O12","K.92 Na.07 Mg1.11 Fe1.35 Ti.18 Al1.34 Si2.72 O12",{"id":407,"url":408,"label":409,"formula":410,"spacegroup":399,"year":411},626,"\u002Fcif\u002F626.cif","Redhammer 2002 · Si2.84 Al Fe2.68 Mg.06 Mn.18 Ti.09 (K.93 Na.07) O11.86 F.14 H1.84","Si2.84 Al Fe2.68 Mg.06 Mn.18 Ti.09 (K.93 Na.07) O11.86 F.14 H1.84",2002,{"id":413,"url":414,"label":415,"formula":416,"spacegroup":399,"year":411},627,"\u002Fcif\u002F627.cif","Redhammer 2002 · Al1.71 Si2.56 Mg.12 Fe2.37 Mn.03 Ti.03 K O11.96 F.04 H1.9","Al1.71 Si2.56 Mg.12 Fe2.37 Mn.03 Ti.03 K O11.96 F.04 H1.9",{"id":418,"url":419,"label":420,"formula":421,"spacegroup":399,"year":422},628,"\u002Fcif\u002F628.cif","Brigatti 2000","(K.96 Na.04) Fe1.5 Mg.76 Ti.22 Al1.62 Si2.72 O11.96 F.04 H1.8",2000,[424,425],"Anniet","Annitt",[427,431,435,439,443,446,449,453,458,462,467,473],{"lang":428,"names":429},"ar",[430],"عنيت",{"lang":432,"names":433},"ca",[434],"annita",{"lang":436,"names":437},"de",[438],"Annit",{"lang":440,"names":441},"eu",[442],"Annita",{"lang":444,"names":445},"fr",[7],{"lang":447,"names":448},"it",[7],{"lang":450,"names":451},"ja",[452],"鉄雲母",{"lang":454,"names":455},"ko",[456,457],"애나이트","철운모",{"lang":459,"names":460},"sr",[461],"анит",{"lang":463,"names":464},"uk",[465,466],"Аніт","Анніт",{"lang":468,"names":469},"zh",[470,471,472],"羟铁云母","鐵雲母","铁云母",{"lang":474,"names":475},"zh-tw",[476,471],"羥鐵雲母","Q3618110",{"history":11,"applications":11}]