[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:2026":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":11,"impurities":23,"cim":24,"ima_status":25,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":11,"discovery_year":28,"strunz10ed1":29,"strunz10ed2":30,"strunz10ed3":31,"strunz10ed4":32,"dana8ed1":33,"dana8ed2":34,"dana8ed3":34,"dana8ed4":35,"csystem":36,"cclass":37,"spacegroup":38,"spacegroupset":39,"a":40,"b":39,"c":41,"alpha":39,"beta":39,"gamma":39,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":42,"csmetamict":14,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":43,"tlform":11,"hmin":44,"hmax":45,"hardtype":11,"vhnmin":39,"vhnmax":39,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":46,"dmeas2":46,"dcalc":47,"dmeaserror":11,"dcalcerror":11,"commentdense":48,"lustre":11,"lustretype":49,"commentluster":11,"diapheny":50,"streak":11,"colour":51,"commentcolor":11,"colors":52,"streak_colors":11,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":54,"opticalsign":55,"opticalalpha":39,"opticalalpha2":39,"opticalalphaerror":11,"opticalbeta":39,"opticalbeta2":39,"opticalbetaerror":11,"opticalgamma":39,"opticalgamma2":39,"opticalgammaerror":11,"opticalomega":56,"opticalomega2":39,"opticalomegaerror":11,"opticalepsilon":57,"opticalepsilon2":39,"opticalepsilonerror":11,"opticaln":39,"opticaln2":39,"opticalnerror":11,"optical2vcalc":39,"optical2vcalc2":39,"optical2vcalcerror":11,"optical2vmeasured":39,"optical2vmeasured2":39,"optical2vmeasurederror":11,"rimin":58,"rimax":59,"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":60,"occurrence":61,"otheroccurrence":62,"type_specimen_store":11,"description_short":63,"aboutname":64,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":65,"reviewed_at":11,"variety_of":11,"varieties":66,"group_members":67,"associates":95,"confused_with":119,"type_localities":121,"occurrence_total":128,"citations":129,"images":186,"structures":228,"synonyms":256,"language_names":258,"wikidata_qid":282,"texts":283},2026,"1:1:2026:4","75dc355d-71db-4a4c-a233-576059c4ac59","Indialite","Ind",0,"mineral",null,494681,226,false,"Mg\u003Csub>2\u003C\u002Fsub>Al\u003Csub>3\u003C\u002Fsub>(AlSi\u003Csub>5\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>)","Mg\u003Csub>2\u003C\u002Fsub>Al\u003Csub>3\u003C\u002Fsub>(AlSi\u003Csub>5\u003C\u002Fsub>)O\u003Csub>18\u003C\u002Fsub>",[18,19,20,21],"Al","Mg","Si","O",[18,19,20,21],",Fe,Mn,Na,","16.19.1",[26,27],"APPROVED","GRANDFATHERED","1954","9","C","J","05","61","1","3","Hexagonal",20,123,"0","9.8","9.345",2,"Small hexagonal grains and clusters of spiral-shaped grains, some exhibiting tentacles or multiple terminations.",7,7.5,"2.512","2.59","Measured values on artificial material.","Vitreous","Transparent","Colourless (thin section).",[53],"colorless","Uniaxial","-","1.539","1.534",1.534,1.539,"None.","Burning coal seam underlying sedimentary rocks","Polymetamorphosed pelitic rock (Japan); volcanic eruptive matter (Bellerberg volcano).","The Mg analogue of ferroindialite.\r\nThe hexagonal high-temperature dimorph of cordierite (orthorhombic-pseudohexagonal).\r\n\r\nNote: the formula has also been expressed as Al2SiMg2[Al2Si4]O18 (Pezzotta, 2005), and the mineral has been assigned to the bery...","Named by A. Miyashiro and T. Iiyama in 1954 after the country of India, where the type locality is located.","2025-08-11 12:14:21",[],[68,76,83,88],{"id":69,"name":70,"entrytype":9,"csystem":71,"ima_formula":72,"mindat_formula":72,"hmin":44,"hmax":45,"dmeas":73,"dcalc":74,"primary_image_id":75},1128,"Cordierite","Orthorhombic","Mg\u003Csub>2\u003C\u002Fsub>Al\u003Csub>4\u003C\u002Fsub>Si\u003Csub>5\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>","2.6","2.505",6260,{"id":77,"name":78,"entrytype":9,"csystem":36,"ima_formula":79,"mindat_formula":79,"hmin":44,"hmax":44,"dmeas":80,"dcalc":81,"primary_image_id":82},43879,"Ferroindialite","(Fe\u003Csup>2+\u003C\u002Fsup>,Mg)\u003Csub>2\u003C\u002Fsub>Al\u003Csub>4\u003C\u002Fsub>Si\u003Csub>5\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>","2.66","2.667",8795,{"id":84,"name":85,"entrytype":9,"csystem":71,"ima_formula":86,"mindat_formula":87,"hmin":11,"hmax":11,"dmeas":11,"dcalc":11,"primary_image_id":11},470681,"Sachanbińskiite","NaMn\u003Csub>4\u003C\u002Fsub>(Al\u003Csub>5\u003C\u002Fsub>Be)(AlSi\u003Csub>5\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub> · 2H\u003Csub>2\u003C\u002Fsub>O","NaMn\u003Csub>4\u003C\u002Fsub>(Al\u003Csub>5\u003C\u002Fsub>Be)(AlSi\u003Csub>5\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>·2H\u003Csub>2\u003C\u002Fsub>O",{"id":89,"name":90,"entrytype":9,"csystem":71,"ima_formula":91,"mindat_formula":91,"hmin":44,"hmax":45,"dmeas":92,"dcalc":93,"primary_image_id":94},3609,"Sekaninaite","Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Al\u003Csub>4\u003C\u002Fsub>Si\u003Csub>5\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>","2.76","2.78",78846,[96,105,106,113],{"id":97,"name":98,"entrytype":9,"csystem":71,"ima_formula":99,"mindat_formula":100,"hmin":101,"hmax":45,"dmeas":102,"dcalc":103,"primary_image_id":104},217,"Andalusite","Al\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>5\u003C\u002Fsub>","Al\u003Csub>2\u003C\u002Fsub>(SiO\u003Csub>4\u003C\u002Fsub>)O",6.5,"3.13","3.149",29089,{"id":69,"name":70,"entrytype":9,"csystem":71,"ima_formula":72,"mindat_formula":72,"hmin":44,"hmax":45,"dmeas":73,"dcalc":74,"primary_image_id":75},{"id":107,"name":108,"entrytype":9,"csystem":109,"ima_formula":110,"mindat_formula":110,"hmin":44,"hmax":44,"dmeas":111,"dcalc":80,"primary_image_id":112},3337,"Quartz","Trigonal","SiO\u003Csub>2\u003C\u002Fsub>","2.65",30579,{"id":114,"name":115,"entrytype":9,"csystem":71,"ima_formula":99,"mindat_formula":100,"hmin":101,"hmax":45,"dmeas":116,"dcalc":117,"primary_image_id":118},3662,"Sillimanite","3.23","3.24",30699,[120],{"id":69,"name":70,"entrytype":9,"csystem":71,"ima_formula":72,"mindat_formula":72,"hmin":44,"hmax":45,"dmeas":73,"dcalc":74,"primary_image_id":75},[122],{"id":123,"txt":124,"latitude":125,"longitude":126,"country":127},64212,"Bokaro coalfield, Ramgarh District, Jharkhand, India",23.7666667,85.5833333,"India",27,[130,134,138,142,146,151,155,160,165,169,173,178,182],{"id":131,"year":132,"html":133,"doi":11},522283,1952,"Venkatesh, V. (1952) Development and growth of cordierite in para-lavas. \u003Ci>American Mineralogist\u003C\u002Fi>,  37 (9-10) 831-848 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM37\u002FAM37_831.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":135,"year":136,"html":137,"doi":11},16112893,1954,"Miyashiro, A. and Iiyama, T. (1954) A preliminary note on a new mineral, indialite, polymorphic with cordierite. Proceedings of the Japan Academy: 30: 746-751.",{"id":139,"year":140,"html":141,"doi":11},15961547,1955,"Fleischer, M. (1955) New mineral names. American Mineralogist: 40: 787-788.",{"id":143,"year":140,"html":144,"doi":145},1155580,"Miyashiro, A., Iiyama, T., Miyashiro, T., Yamasaki, M. (1955) The polymorphism of cordierite and indialite. \u003Ci>American Journal of Science\u003C\u002Fi>,  253 (4) 185-208 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2475\u002Fajs.253.4.185'>doi:10.2475\u002Fajs.253.4.185\u003C\u002Fa>","10.2475\u002Fajs.253.4.185",{"id":147,"year":148,"html":149,"doi":150},1155780,1957,"Miyashiro, A. (1957) Cordierite-indialite relations. \u003Ci>American Journal of Science\u003C\u002Fi>,  255 (1) 43-62 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2475\u002Fajs.255.1.43'>doi:10.2475\u002Fajs.255.1.43\u003C\u002Fa>","10.2475\u002Fajs.255.1.43",{"id":152,"year":153,"html":154,"doi":11},16112896,1977,"Meagher, E.P. and Gibbs, G.V. (1977) The polymorphism of cordierite: II. The crystal structure of indialite. Canadian Mineralogist: 15: 43-49.",{"id":156,"year":157,"html":158,"doi":159},75322,1982,"Kitamura, Masao, Hiroi, Yoshikuni (1982) Indialite from Unazuki Pelitic Schist, Japan, and its transition texture to cordierite. \u003Ci>Contributions to Mineralogy and Petrology\u003C\u002Fi>,  80 (2) 110-116 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf00374888'>doi:10.1007\u002Fbf00374888\u003C\u002Fa>","10.1007\u002Fbf00374888",{"id":161,"year":162,"html":163,"doi":164},112012,1990,"Daniels, P. (1990) What is the true space group of high-cordierite? \u003Ci>Zeitschrift für Kristallographie\u003C\u002Fi>,  190 (3-4). 271-276 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1990.190.3-4.271'>doi:10.1524\u002Fzkri.1990.190.3-4.271\u003C\u002Fa>","10.1524\u002Fzkri.1990.190.3-4.271",{"id":166,"year":167,"html":168,"doi":11},529268,1992,"Daniels, Peter (1992) Structural effects of the incorporation of large radius alkalis in high cordierite. \u003Ci>American Mineralogist\u003C\u002Fi>,  77 (3-4) 407-411 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM77\u002FAM77_407.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":170,"year":171,"html":172,"doi":11},16965017,2001,"(2001) Indialite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Findialite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":174,"year":175,"html":176,"doi":177},394897,2004,"Balassone, Giuseppina, Franco, Enrico, Mattia, Carlo Andrea, Puliti, Raffaella (2004) Indialite in xenolithic rocks from Somma-Vesuvius volcano (Southern Italy): Crystal chemistry and petrogenetic features. \u003Ci>American Mineralogist\u003C\u002Fi>,  89 (1) 1-6 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2004-0101'>doi:10.2138\u002Fam-2004-0101\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol89\u002FAM89_1.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam-2004-0101",{"id":179,"year":180,"html":181,"doi":11},16112901,2005,"Pezzotta, F. (2005) Rivista Mineralogica Italiana: 2, 98.",{"id":183,"year":184,"html":185,"doi":11},15945707,2006,"Rakovan, J., Kitamura, M., Tamada, O. (2006) Sakura Ish: Mica pseudomorphs of complex cordierite-indialite intergrowths from Kameoka, Kyoto Prefecture, Japan. Rocks & Minerals, 81, 284-292.",[187,197,206,214,221],{"id":188,"source_url":189,"license_code":190,"credit_html":191,"title":192,"description":193,"author":194,"original_width":195,"original_height":196},60721,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=74327920","CC BY 2.0","James St. John (jsj1771) (https:\u002F\u002Fwww.flickr.com\u002Fpeople\u002Fjsjgeology\u002F), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=74327920\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hornfels from Mikata on Honshu in Japan.jpg","Hornfels with pinite (= muscovite mica replacing intergrown cordierite-indialite; “cherry blossom stones”), Tamba Group, Mesozoic (Triassic to lowermost Cretaceous), ~98 m.y. contact metamorphic date. \n\u003Cp>Locality: at or near Mikata, Mikata District, Fukui Prefecture, Honshu Island, southern Japan. \n\u003C\u002Fp>\n(Limper Geology Museum specimen, Miami University, Oxford, Ohio, USA)","James St. John (jsj1771) (https:\u002F\u002Fwww.flickr.com\u002Fpeople\u002Fjsjgeology\u002F)",2908,1723,{"id":198,"source_url":199,"license_code":190,"credit_html":200,"title":201,"description":202,"author":203,"original_width":204,"original_height":205},19484,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97560060","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97560060\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cherry blossom stones (pinite) (muscovite mica replacing intergrown cordierite-indialite) (mid-Cretaceous, 98 Ma; Kameoka, Honshu Island, Japan) 2.jpg","“Cherry blossom stones” - pinite (= muscovite mica replacing intergrown cordierite-indialite) from Kameoka, west of Kyoto, Kyoto Prefecture, southwestern Honshu Island, southern Japan.  (Limper Geology Museum specimens, Miami University, Oxford, Ohio, USA)\n\u003Chr>\n\u003Cp>One of the most famous & visually intriguing geologic materials collected in Japan is the cherry blossom stone.  These interesting structures have a complex geologic history.\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>What are they now?\nCherry blossom stones are relatively small, subhexagonal-shaped masses of fine-grained muscovite mica that show a flower-like pattern in transverse cross-section.\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>What did they used to be?\nThe muscovite mica is not the original material making up these structures.  Before the growth of muscovite mica, these were complex intergrowths of six cordierite crystals and one indialite crystal.  So, cherry blossom stones represent muscovite mica replacing cordierite-indialite (muscovite pseudomorphs after cordierite-indialite).  Such complex pseudomorphs have been referred to as pinite.\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>What is the host rock?\nCherry blossom stones are hosted in a matrix of hornfels, a fine-grained, contact metamorphic rock.  Hornfels form by intense alteration (heating & chemical alteration) of shales by nearby lava or magma.\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>How did they form?\nThe hornfels host rocks were originally fine-grained siliciclastic sedimentary rocks (shales) of the Tamba Group (Triassic-Jurassic-lowermost Cretaceous).  In the mid-Cretaceous (early Cenomanian Stage, ~98 m.y.), underground igneous activity resulted in granites and granodiorite intrusions altering the shales into hornfels by contact metamorphism.  These hornfels had decent-sized masses of intergrown cordierite-indialite.\n\u003C\u002Fp>\u003Cp>Indialite is a magnesium aluminosilicate mineral (Mg2Al4Si5O18).  Cordierite is an iron magnesium aluminosilicate mineral ((Fe,Mg)2Al4Si5O18).  The subhexagonal-shaped masses of cordierite-indialite in the hornfels consist of seven individual crystals.  At the center of each mass is a dumbbell-shaped indialite crystal - very narrow at the center, and relatively wide at the ends (look at the varying sizes of the center hexagon in the cherry blossom stones shown above).  Surrounding the indialite crystal are six prism-shaped cordierite crystals.  They are widest at the center of each cherry blossom stone and narrowest at the ends.\n\u003C\u002Fp>\u003Cp>A second metamorphic event altered the cordierite-indialite masses.  Hydrothermal metamorphism resulted in fine-grained muscovite mica replacing the original minerals.\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Much info. from:\n\u003C\u002Fp>\nRakovan et al. (2006) - Sakura Ishi (cherry blossom stones): mica pseudomorphs of complex cordierite-indialite intergrowths from Kameoka, Kyoto Prefecture, Japan.  in  Minerals from Japan.  Rocks & Minerals Reprint 2006: 31-39.","James St. John",1330,1216,{"id":207,"source_url":208,"license_code":190,"credit_html":209,"title":210,"description":211,"author":203,"original_width":212,"original_height":213},19485,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97560061","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97560061\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cherry blossom stone (pinite) (muscovite mica replacing intergrown cordierite-indialite) (mid-Cretaceous, 98 Ma; Kameoka, Honshu Island, Japan) 1.jpg","“Cherry blossom stone” (9 mm across) - pinite (= muscovite mica replacing intergrown cordierite-indialite) from Kameoka, west of Kyoto, Kyoto Prefecture, southwestern Honshu Island, southern Japan.  The small, central, hexagonal structure represents where indialite used to be.  The “petals” of the cherry blossom flower (= the 6 wedge-shaped masses surrounding the center hexagon) represent where cordierite used to be.\n\u003Chr>\n\u003Cp>One of the most famous & visually intriguing geologic materials collected in Japan is the cherry blossom stone.  These interesting structures have a complex geologic history.\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>What are they now?\nCherry blossom stones are relatively small, subhexagonal-shaped masses of fine-grained muscovite mica that show a flower-like pattern in transverse cross-section.\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>What did they used to be?\nThe muscovite mica is not the original material making up these structures.  Before the growth of muscovite mica, these were complex intergrowths of six cordierite crystals and one indialite crystal.  So, cherry blossom stones represent muscovite mica replacing cordierite-indialite (muscovite pseudomorphs after cordierite-indialite).  Such complex pseudomorphs have been referred to as pinite.\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>What is the host rock?\nCherry blossom stones are hosted in a matrix of hornfels, a fine-grained, contact metamorphic rock.  Hornfels form by intense alteration (heating & chemical alteration) of shales by nearby lava or magma.\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>How did they form?\nThe hornfels host rocks were originally fine-grained siliciclastic sedimentary rocks (shales) of the Tamba Group (Triassic-Jurassic-lowermost Cretaceous).  In the mid-Cretaceous (early Cenomanian Stage, ~98 m.y.), underground igneous activity resulted in granites and granodiorite intrusions altering the shales into hornfels by contact metamorphism.  These hornfels had decent-sized masses of intergrown cordierite-indialite.\n\u003C\u002Fp>\u003Cp>Indialite is a magnesium aluminosilicate mineral (Mg2Al4Si5O18).  Cordierite is an iron magnesium aluminosilicate mineral ((Fe,Mg)2Al4Si5O18).  The subhexagonal-shaped masses of cordierite-indialite in the hornfels consist of seven individual crystals.  At the center of each mass is a dumbbell-shaped indialite crystal - very narrow at the center, and relatively wide at the ends (look at the varying sizes of the center hexagon in the cherry blossom stones in this photo album).  Surrounding the indialite crystal are six prism-shaped cordierite crystals.  They are widest at the center of each cherry blossom stone and narrowest at the ends.\n\u003C\u002Fp>\u003Cp>A second metamorphic event altered the cordierite-indialite masses.  Hydrothermal metamorphism resulted in fine-grained muscovite mica replacing the original minerals.\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Much info. from:\n\u003C\u002Fp>\nRakovan et al. (2006) - Sakura Ishi (cherry blossom stones): mica pseudomorphs of complex cordierite-indialite intergrowths from Kameoka, Kyoto Prefecture, Japan.  in  Minerals from Japan.  Rocks & Minerals Reprint 2006: 31-39.",666,642,{"id":215,"source_url":216,"license_code":190,"credit_html":217,"title":218,"description":202,"author":203,"original_width":219,"original_height":220},19486,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97560064","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97560064\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cherry blossom stones (pinite) (muscovite mica replacing intergrown cordierite-indialite) (mid-Cretaceous, 98 Ma; Kameoka, Honshu Island, Japan) 4.jpg",1132,1237,{"id":222,"source_url":223,"license_code":190,"credit_html":224,"title":225,"description":202,"author":203,"original_width":226,"original_height":227},19487,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97560065","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97560065\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cherry blossom stones (pinite) (muscovite mica replacing intergrown cordierite-indialite) (mid-Cretaceous, 98 Ma; Kameoka, Honshu Island, Japan) 3.jpg",1060,1048,[229,235,241,246,251],{"id":230,"url":231,"label":232,"formula":233,"spacegroup":234,"year":175},6549,"\u002Fcif\u002F6549.cif","Balassone 2004","(Al4.251 Si4.749) (Mg1.94 Fe.06) O18 K.336 Ca.084","P 6\u002Fm c c",{"id":236,"url":237,"label":238,"formula":239,"spacegroup":234,"year":240},6550,"\u002Fcif\u002F6550.cif","Schwartz 1994 · Mg2 (Al4 Si5) O18","Mg2 (Al4 Si5) O18",1994,{"id":242,"url":243,"label":244,"formula":245,"spacegroup":234,"year":240},6551,"\u002Fcif\u002F6551.cif","Schwartz 1994 · Mg2 (Al4 Si5) O18 Bi.168","Mg2 (Al4 Si5) O18 Bi.168",{"id":247,"url":248,"label":249,"formula":250,"spacegroup":234,"year":167},6552,"\u002Fcif\u002F6552.cif","Daniels 1992","Mg2 (Al4.281 Si4.719) O18 Cs.281",{"id":252,"url":253,"label":254,"formula":255,"spacegroup":234,"year":153},6553,"\u002Fcif\u002F6553.cif","Meagher 1977","(Si5.04 Al3.96) (Mg1.36 Fe.64) O18",[257],"Indialiet",[259,263,267,271,274,278],{"lang":260,"names":261},"ca",[262],"indialita",{"lang":264,"names":265},"de",[266],"Indialith",{"lang":268,"names":269},"eu",[270],"Indialita",{"lang":272,"names":273},"it",[7],{"lang":275,"names":276},"pl",[277],"Indialit",{"lang":279,"names":280},"sr",[281],"индијалит","Q3797918",{"history":11,"applications":11}]