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It occurs as crystals lining the walls of cavities in cavernous alkali basalt and growing into the rock near the caverns.","Fersman Mineralogical Museum of the Russian Academy of Sciences, Moscow, Russia: registration nos. 3884\u002F1 (cotype) and 3884\u002F2 (holotype).","It forms coarse dark brown to black vitreous prismatic (up to 1.5 mm) or platy (up to 4×4×0.2 mm) crystals in cavities of alkaline basalt.","Named in 2010 by N. V. Chukanov, A. A. Mukhanova, R. K. Rastsvetaeva, D.I. Belakovskiy, S. Möckel, O. V. Karimova, S. N. Britvin, and S. V. Krivovichev for its chemical relationship to phlogopite.","2026-03-29 17:14:42",[],[76,84,91,97,103,110,117,124,129],{"id":77,"name":78,"entrytype":9,"csystem":34,"ima_formula":79,"mindat_formula":79,"hmin":80,"hmax":45,"dmeas":81,"dcalc":82,"primary_image_id":83},241,"Annite","KFe\u003Csup>2+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>(AlSi\u003Csub>3\u003C\u002Fsub>O\u003Csub>10\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub>",2.5,"3.3","3.36",1491,{"id":85,"name":86,"entrytype":9,"csystem":34,"ima_formula":87,"mindat_formula":88,"hmin":11,"hmax":11,"dmeas":89,"dcalc":89,"primary_image_id":90},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>","0",7581,{"id":92,"name":93,"entrytype":9,"csystem":34,"ima_formula":94,"mindat_formula":94,"hmin":45,"hmax":45,"dmeas":95,"dcalc":96,"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":98,"name":99,"entrytype":9,"csystem":34,"ima_formula":100,"mindat_formula":100,"hmin":43,"hmax":45,"dmeas":89,"dcalc":101,"primary_image_id":102},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":104,"name":105,"entrytype":9,"csystem":34,"ima_formula":106,"mindat_formula":107,"hmin":45,"hmax":108,"dmeas":11,"dcalc":109,"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":111,"name":112,"entrytype":9,"csystem":34,"ima_formula":113,"mindat_formula":113,"hmin":43,"hmax":45,"dmeas":114,"dcalc":115,"primary_image_id":116},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":118,"name":119,"entrytype":9,"csystem":34,"ima_formula":120,"mindat_formula":121,"hmin":80,"hmax":45,"dmeas":122,"dcalc":123,"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":125,"name":126,"entrytype":9,"csystem":34,"ima_formula":127,"mindat_formula":127,"hmin":80,"hmax":45,"dmeas":89,"dcalc":89,"primary_image_id":128},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":130,"name":131,"entrytype":9,"csystem":34,"ima_formula":132,"mindat_formula":132,"hmin":11,"hmax":11,"dmeas":89,"dcalc":89,"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>",[],[],[136],{"id":137,"txt":138,"latitude":139,"longitude":140,"country":141},13787,"Rothenberg Quarry, Bell, Mendig, Mayen-Koblenz, Rhineland-Palatinate, Germany",50.4044444,7.2322222,"Germany",9,[144,148,153],{"id":145,"year":146,"html":147,"doi":11},16138035,2010,"Chukanov N.V., Mukhanova, A.A., Rastsvetaeva, R.K., Belakovskiy, D.I., Möckel, S., Karimova, O.V., Britvin, S.N. & Krivovichev, S.V. (2010): Oxyphlogopite, K(Mg,Ti,Fe)3[(Si,Al)4O10](O,F)2, a new mica-group mineral. Zapiski Rossiyskogo Mineralogicheskogo Obshchestva, 139(3), 31-40 (in Russian). English translation: (2011) Geology of Ore Deposits, 53, 583-590.",{"id":149,"year":150,"html":151,"doi":152},19609,2011,"Chukanov, N. V., Mukhanova, A. A., Rastsvetaeva, R. K., Belakovsky, D. I., Möckel, S., Karimova, O. V., Britvin, S. N., Krivovichev, S. V. (2011) Oxyphlogopite K(Mg,Ti,Fe)3[(Si,Al)4O10](O,F)2: A new mineral species of the mica group. \u003Ci>Geology of Ore Deposits\u003C\u002Fi>,  53 (7) 583-590 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1134\u002Fs1075701511070063'>doi:10.1134\u002Fs1075701511070063\u003C\u002Fa>","10.1134\u002Fs1075701511070063",{"id":154,"year":155,"html":156,"doi":11},16966470,2021,"(2021) Oxyphlogopite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002FOxyphlogopite.pdf' class='refpdflink'>\u003C\u002Fa>",[],[],[160,161,162,163],"IMA2009-069","Oxyphlogopiet","Titanbiotit  (of Freudenberg)","Wodanit",[165,169,174,178],{"lang":166,"names":167},"ca",[168],"oxiflogopita",{"lang":170,"names":171},"de",[172,173],"IMA 2009-069","Oxyphlogopit",{"lang":175,"names":176},"eu",[177],"Oxiflogopita",{"lang":179,"names":180},"it",[181],"oxyphlogopite","Q19861127",{"history":11,"applications":11}]