[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:26445":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":24,"key_elements":25,"impurities":11,"cim":11,"ima_status":26,"ima_notes":11,"ima_history":11,"approval_year":28,"publication_year":29,"discovery_year":30,"strunz10ed1":31,"strunz10ed2":32,"strunz10ed3":32,"strunz10ed4":33,"dana8ed1":34,"dana8ed2":34,"dana8ed3":34,"dana8ed4":34,"csystem":35,"cclass":36,"spacegroup":37,"spacegroupset":34,"a":38,"b":34,"c":39,"alpha":34,"beta":34,"gamma":34,"aerror":40,"berror":11,"cerror":40,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":40,"csmetamict":14,"commentcrystal":41,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":42,"tlform":43,"hmin":44,"hmax":44,"hardtype":11,"vhnmin":34,"vhnmax":34,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":34,"dmeas2":34,"dcalc":45,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":46,"commentluster":11,"diapheny":47,"streak":48,"colour":48,"commentcolor":11,"colors":49,"streak_colors":51,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":52,"fracturetype":53,"tenacity":54,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":34,"opticalalpha2":34,"opticalalphaerror":11,"opticalbeta":34,"opticalbeta2":34,"opticalbetaerror":11,"opticalgamma":34,"opticalgamma2":34,"opticalgammaerror":11,"opticalomega":34,"opticalomega2":34,"opticalomegaerror":11,"opticalepsilon":34,"opticalepsilon2":34,"opticalepsilonerror":11,"opticaln":34,"opticaln2":34,"opticalnerror":11,"optical2vcalc":34,"optical2vcalc2":34,"optical2vcalcerror":11,"optical2vmeasured":34,"optical2vmeasured2":34,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":55,"opticalpleochorismdesc":56,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":48,"opticalinternal":11,"opticaltropic":57,"opticalanisotropism":58,"opticalbireflectance":59,"opticalextinction":11,"opticalr":60,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":61,"otheroccurrence":11,"type_specimen_store":62,"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":186,"confused_with":187,"type_localities":188,"occurrence_total":195,"citations":196,"images":216,"structures":227,"synonyms":234,"language_names":237,"wikidata_qid":263,"texts":264},26445,"1:1:26445:5","44bc0bfa-6e65-4b27-b4c1-10dc4a4c3659","Gramaccioliite-(Y)","Gmc-Y",0,"mineral",null,29190,301,false,"(Pb,Sr)(Y,Mn)Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>(Ti,Fe\u003Csup>3+\u003C\u002Fsup>)\u003Csub>18\u003C\u002Fsub>O\u003Csub>38\u003C\u002Fsub>",[17,18,19,20,21,22,23],"Fe","Mn","Pb","Sr","Ti","O","Y",[17,19,21,22,23],[19,21,23],[27],"APPROVED",2001,2004,"1976","4","C","40","0","Trigonal",10,80,"10.411","20.97",3,"Cell refined from powder data; single-crystal data gave smaller parameters, a = 10.383, c = 20.882 Å (Orlandi et al., 1994). REE-rich material from Samos island has a = 9.1814(5) Å and α = 68.820(4)° (hexagonal setting: a = 10.377, c = 20.872 Å) (Theye et al., 2010).","Six-sided tabular crystals (rhombohedral-pseudohexagonal), often with a strongly corroded appearance.","Six-sided tabular crystals to 8 mm across.",6,"4.66","Greasy,Sub-Metallic","Opaque","Black",[50],"black",[50],"None Observed","Conchoidal","brittle","Non-pleochroic","\u003Cf>R^1 in oil. R^2 in air.\u003C\u002Ff>","Anisotropic","Very weak","Low","(19.2,6.7) 470,\r\n(17.9,5.9) 546,\r\n(17.6,5.7) 589,\r\n(17.4,5.8) 650\r\n","Mineralized clefts in a biotite-rich granite gneiss.","Natural History Museum, University of Pisa, Italy, number 18299.","A member of the Crichtonite Group.\r\n\r\nThe yttrium analogue of senaite (providing the same Fe valencies) and the lead analogue of dessauite.","Honouring Carlo Maria Gramaccioli (1935-2013), mineral collector and Professor of Physical Chemistry, University of Milan, Italy.  The suffix\u002Fmodifier follows the Levinson rule for species with essential REE denoting, in this case, predominant yttrium.","2025-08-11 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(Ti,Fe\u003Csup>3+\u003C\u002Fsup>)\u003Csub>18\u003C\u002Fsub>O\u003Csub>38\u003C\u002Fsub>","4.62","4.77",{"id":161,"name":162,"entrytype":9,"csystem":35,"ima_formula":163,"mindat_formula":164,"hmin":11,"hmax":11,"dmeas":11,"dcalc":165,"primary_image_id":11},55116,"Mirnyite","SrZr\u003Csup>4+\u003C\u002Fsup>(Ti\u003Csup>4+\u003C\u002Fsup>\u003Csub>12\u003C\u002Fsub>Cr\u003Csup>3+\u003C\u002Fsup>\u003Csub>6\u003C\u002Fsub>)Mg\u003Csub>2\u003C\u002Fsub>O\u003Csub>38\u003C\u002Fsub>","SrZr\u003Csup>4+\u003C\u002Fsup>Mg\u003Csub>2\u003C\u002Fsub>(Cr\u003Csup>3+\u003C\u002Fsup>\u003Csub>6\u003C\u002Fsub>Ti\u003Csup>4+\u003C\u002Fsup>\u003Csub>12\u003C\u002Fsub>)O\u003Csub>38\u003C\u002Fsub>","4.3867",{"id":167,"name":168,"entrytype":9,"csystem":35,"ima_formula":169,"mindat_formula":170,"hmin":44,"hmax":116,"dmeas":11,"dcalc":171,"primary_image_id":11},42381,"Paseroite","Pb(Mn\u003Csup>2+\u003C\u002Fsup>,◻)(Fe\u003Csup>3+\u003C\u002Fsup>,◻)\u003Csub>2\u003C\u002Fsub>(V\u003Csup>5+\u003C\u002Fsup>,Ti\u003Csup>4+\u003C\u002Fsup>,◻)\u003Csub>18\u003C\u002Fsub>O\u003Csub>38\u003C\u002Fsub>","PbMn\u003Csup>2+\u003C\u002Fsup>(Mn\u003Csup>2+\u003C\u002Fsup>,Fe\u003Csup>3+\u003C\u002Fsup>)\u003Csub>2\u003C\u002Fsub>(V\u003Csup>5+\u003C\u002Fsup>,Ti,◻)\u003Csub>18\u003C\u002Fsub>O\u003Csub>38\u003C\u002Fsub> ","4.315",{"id":173,"name":174,"entrytype":9,"csystem":35,"ima_formula":175,"mindat_formula":176,"hmin":177,"hmax":177,"dmeas":178,"dcalc":178,"primary_image_id":11},55032,"Saranovskite","SrCaFe\u003Csup>2+\u003C\u002Fsup>\u003Csub> 2\u003C\u002Fsub>(Cr\u003Csub>4\u003C\u002Fsub>Ti\u003Csub>2\u003C\u002Fsub>)Ti\u003Csub>12\u003C\u002Fsub>O\u003Csub>38\u003C\u002Fsub>","SrCaFe\u003Csup>2+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>(Cr\u003Csub>4\u003C\u002Fsub>Ti\u003Csub>2\u003C\u002Fsub>)Ti\u003Csub>12\u003C\u002Fsub>O\u003Csub>38\u003C\u002Fsub>",8.5,"4.25",{"id":180,"name":181,"entrytype":9,"csystem":35,"ima_formula":182,"mindat_formula":182,"hmin":44,"hmax":116,"dmeas":183,"dcalc":184,"primary_image_id":185},3617,"Senaite","Pb(Mn,Y,U)(Fe,Zn)\u003Csub>2\u003C\u002Fsub>(Ti,Fe,Cr,V)\u003Csub>18\u003C\u002Fsub>(O,OH)\u003Csub>38\u003C\u002Fsub>","5.204","5.23",22064,[],[],[189],{"id":190,"txt":191,"latitude":192,"longitude":193,"country":194},50390,"Sambuco gramaccioliite site (Sambuco “historical” site), Sambuco, Cuneo Province, Piedmont, Italy",44.3115738,7.1066415,"Italy",19,[197,201,204,208,212],{"id":198,"year":199,"html":200,"doi":11},16133853,1981,"Piccoli, G.C. (1981): Davidite di Pianche di Vinadio (CN). Prima segnalazione. Rivista Mineralogica Italiana, 1981, 19-22.",{"id":202,"year":29,"html":203,"doi":11},16133855,"Orlandi, P. & Piccoli, G.C. (2004): Gramaccioliite-(Y) un nuovo minerale alpino del gruppo della crichtonite. Rivista Mineralogica Italiana, 1\u002F2004, 16-17.",{"id":205,"year":29,"html":206,"doi":207},128320,"Orlandi, Paolo, Pasero, Marco, Rotiroti, Nicola, Olmi, Filippo, Demartin, Francesco, Moëlo, Yves (2004) Gramaccioliite-(Y), a new mineral of the crichtonite group from Stura Valley, Piedmont, Italy. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  16 (1) 171-175 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1127\u002F0935-1221\u002F2004\u002F0016-0171'>doi:10.1127\u002F0935-1221\u002F2004\u002F0016-0171\u003C\u002Fa>","10.1127\u002F0935-1221\u002F2004\u002F0016-0171",{"id":209,"year":210,"html":211,"doi":11},16025851,2010,"Theye, T., Hatert, F., Ockenga, E., Bertoldi, C., Lathe, C. (2010): Gramaccioliite-(Y): paragenesis chemistry, and structure in a new occurrence, Samos Island, Greece. European Journal of Mineralogy, 22, 443-452.",{"id":213,"year":214,"html":215,"doi":11},16964639,2015,"(2015) Gramaccioliite-(Y). \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fgramaccioliite-Y.pdf' class='refpdflink'>\u003C\u002Fa>",[217],{"id":218,"source_url":219,"license_code":220,"credit_html":221,"title":222,"description":223,"author":224,"original_width":225,"original_height":226},10335,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=69674172","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=69674172\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Gramaccioliite-(Y).jpg","Sharp grammacioliite-(Y) crystals from the type and most famous locality for the mineral: Sambuco Gramaccioliite Site, Valle Stura, Cunoe, Piedmont, Italy","David Hospital",722,667,[228],{"id":229,"url":230,"label":231,"formula":232,"spacegroup":233,"year":29},5685,"\u002Fcif\u002F5685.cif","Orlandi 2004","Pb.6 Sr.3 (Y.48 Mn.34 Ce.12 U.06) Fe8 Ti12 O38","R -3",[235,236],"Gramaccioliiet-(Y)","IMA2001-034",[238,243,248,253,258],{"lang":239,"names":240},"ca",[241,242],"Gramaccioliïta-","gramaccioliïta-(Y)",{"lang":244,"names":245},"de",[246,247],"Gramaccioliit-(Y)","IMA 2001-034",{"lang":249,"names":250},"es",[251,252],"Gramaccioliíta-","Gramaccioliíta-(Y)",{"lang":254,"names":255},"eu",[256,257],"Gramaccioliita-","Gramaccioliita-(Y)",{"lang":259,"names":260},"it",[261,262],"Gramaccioliite-","gramaccioliite-(Y)","Q3774232",{"history":11,"applications":11}]