[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:3768":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":24,"key_elements":25,"impurities":26,"cim":27,"ima_status":28,"ima_notes":11,"ima_history":11,"approval_year":30,"publication_year":31,"discovery_year":32,"strunz10ed1":33,"strunz10ed2":34,"strunz10ed3":35,"strunz10ed4":36,"dana8ed1":37,"dana8ed2":38,"dana8ed3":37,"dana8ed4":39,"csystem":40,"cclass":41,"spacegroup":11,"spacegroupset":42,"a":43,"b":44,"c":45,"alpha":42,"beta":46,"gamma":42,"aerror":47,"berror":48,"cerror":49,"alphaerror":11,"betaerror":50,"gammaerror":11,"va3":11,"z":11,"csmetamict":14,"commentcrystal":51,"twinning":52,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":53,"tlform":54,"hmin":55,"hmax":55,"hardtype":56,"vhnmin":42,"vhnmax":42,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":42,"dmeas2":42,"dcalc":57,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":58,"commentluster":11,"diapheny":59,"streak":60,"colour":60,"commentcolor":11,"colors":61,"streak_colors":63,"luminescence":11,"uv":11,"cleavage":64,"cleavagetype":65,"fracturetype":66,"tenacity":67,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":42,"opticalalpha2":42,"opticalalphaerror":11,"opticalbeta":42,"opticalbeta2":42,"opticalbetaerror":11,"opticalgamma":42,"opticalgamma2":42,"opticalgammaerror":11,"opticalomega":42,"opticalomega2":42,"opticalomegaerror":11,"opticalepsilon":42,"opticalepsilon2":42,"opticalepsilonerror":11,"opticaln":42,"opticaln2":42,"opticalnerror":11,"optical2vcalc":42,"optical2vcalc2":42,"optical2vcalcerror":11,"optical2vmeasured":42,"optical2vmeasured2":42,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":68,"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":11,"occurrence":11,"otheroccurrence":11,"type_specimen_store":69,"description_short":70,"aboutname":71,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":72,"reviewed_at":11,"variety_of":11,"varieties":73,"group_members":74,"associates":79,"confused_with":80,"type_localities":81,"occurrence_total":41,"citations":88,"images":117,"structures":128,"synonyms":135,"language_names":138,"wikidata_qid":155,"texts":156},3768,"1:1:3768:2","734a5659-625b-43ff-96dc-f41d3624ee83","Sterryite","Srr",0,"mineral",null,470882,304,false,"Cu(Ag,Cu)\u003Csub>3\u003C\u002Fsub>Pb\u003Csub>19\u003C\u002Fsub>(Sb,As)\u003Csub>22\u003C\u002Fsub>(As\u003Csub>2\u003C\u002Fsub>)S\u003Csub>56\u003C\u002Fsub>","Cu(Ag,Cu)\u003Csub>3\u003C\u002Fsub>Pb\u003Csub>19\u003C\u002Fsub>(Sb,As)\u003Csub>22\u003C\u002Fsub>(As)\u003Csub>2\u003C\u002Fsub>S\u003Csub>56\u003C\u002Fsub>",[18,19,20,21,22,23],"Ag","As","Cu","Pb","Sb","S",[18,19,20,21,22,23],[18,19,20,21,22],"Ag,Cu,","5.7.31",[29],"APPROVED",1966,1967,"1966","2","L","B","30","3","5","1","Monoclinic",5,"0","8.1891","28.5294","42.98","94.896",10,13,2,8,"Space group P21\u002Fn. Originally assumed to be orthorhombic, Pbam, with 28.48, 42.62, 4.09 A.","Commonly twinned on (001).","Rod-like to acicular crystals.","Needlelike laths which cut veenite, as single anhedral grains. Loose fragments are plumose and characteristically occur as bundles of fibres.",3.5,3,"5.91","Metallic,Sub-Metallic","Opaque","Black",[62],"black",[62],"Parallel to c","Perfect","Irregular\u002FUneven","brittle","Strong","Canadian Geological Survey, Ottawa, Ontario, Canada, 12169\r\nRoyal Ontario Museum, Toronto, Ontario, Canada.\r\nNational Museum of Natural History, Washington, D.C., USA, 160258.","Black, metallic rod-like crystals, also massive.\r\n\r\nClosely related to parasterryite.\r\nThe Ag analogue of ciriottiite.","Named in honour of Thomas Sterry Hunt (5 September 1826, Norwich, Connecticut, USA - 12 February 1892, New York City, New York, USA), chemist and a pioneer of Canadian mineralogy. Hunt was the first chemist and later mineralogist on the staff of the Geological Survey of Canada, and the co-author of Geology of Canada (1863).","2026-02-27 22:04:31",[],[75],{"id":76,"name":77,"entrytype":9,"csystem":40,"ima_formula":11,"mindat_formula":78,"hmin":11,"hmax":11,"dmeas":11,"dcalc":11,"primary_image_id":11},470883,"Hayyanite","Cu\u003Csub>5\u003C\u002Fsub>Ag\u003Csub>11\u003C\u002Fsub>Pb\u003Csub>76\u003C\u002Fsub>Sb\u003Csub>71\u003C\u002Fsub>As\u003Csub>17\u003C\u002Fsub>(As\u003Csup>2+\u003C\u002Fsup>)\u003Csub>8\u003C\u002Fsub>S\u003Csub>224\u003C\u002Fsub>",[],[],[82],{"id":83,"txt":84,"latitude":85,"longitude":86,"country":87},550,"Taylor Pit, Madoc, Centre Hastings Municipality, Hastings County, Ontario, Canada",44.5022222,-77.4663889,"Canada",[89,92,95,99,103,107,112],{"id":90,"year":31,"html":91,"doi":11},16856039,"Jambor, John Leslie (1967) New lead sulfantimonides from Madoc, Ontario. Part 1. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  9 (1) 7-24 \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM9_7.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":93,"year":31,"html":94,"doi":11},16856040,"Jambor, John Leslie (1967) New lead sulfantimonides from Madoc, Ontario. Part 2 - mineral descriptions. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  9 (2) 191-213 \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM9_191.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":96,"year":97,"html":98,"doi":11},16856043,1968,"Jambor, John Leslie (1968) New lead sulfantimonides from Madoc, Ontario. Part 3--Syntheses, paragenesis, origin. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  9 (4). 505-521 \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM9_505.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":100,"year":101,"html":102,"doi":11},12907587,1982,"Jambor, John L.; Laflamme, J. H. G.; Walker, D. A. (1982) A Re-examination of the Madoc Sulfosalts, in \u003Ci>Ontario\u003C\u002Fi>. \u003Ci>The Mineralogical Record\u003C\u002Fi>,  13 (2). 93-100",{"id":104,"year":105,"html":106,"doi":11},16967446,2005,"(2005) Sterryite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fsterryite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":108,"year":109,"html":110,"doi":111},64883,2011,"Moëlo, Y., Orlandi, P., Guillot-Deudon, C., Biagioni, C., Paar, W., Evain, M. (2011) LEAD-ANTIMONY SULFOSALTS FROM TUSCANY (ITALY). XI. THE NEW MINERAL SPECIES PARASTERRYITE, Ag4Pb20(Sb14.5As9.5) 24S58, AND ASSOCIATED STERRYITE, Cu(Ag,Cu)3Pb19(Sb,As)22(As-As)S56, FROM THE POLLONE MINE, TUSCANY, ITALY. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  49 (2). 623-638 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002Fcanmin.49.2.623'>doi:10.3749\u002Fcanmin.49.2.623\u003C\u002Fa>","10.3749\u002Fcanmin.49.2.623",{"id":113,"year":114,"html":115,"doi":116},187349,2012,"Moëlo, Yves, Guillot-Deudon, Catherine, Evain, Michel, Orlandi, Paolo, Biagioni, Cristian (2012) Comparative modular analysis of two complex sulfosalt structures: sterryite, Cu(Ag,Cu)3Pb19(Sb,As)22(As–As)S56, and parasterryite, Ag4Pb20(Sb,As)24S58. \u003Ci>Acta Crystallographica Section B Structural Science\u003C\u002Fi>,  68 (5) 480-492 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs0108768112034027'>doi:10.1107\u002Fs0108768112034027\u003C\u002Fa>","10.1107\u002Fs0108768112034027",[118],{"id":119,"source_url":120,"license_code":121,"credit_html":122,"title":123,"description":124,"author":125,"original_width":126,"original_height":127},22828,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=65867256","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=65867256\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Sterryite.jpg","Sterryite, a silver lead sulphosalt, is a very rare mineral present only in two localities worldwide, being this one in Apuan Alps the best by far. From: Pollone Mine, Valdicastello Carducci, Lucca, Tuscany, Italy.","David Hospital",930,666,[129],{"id":130,"url":131,"label":132,"formula":133,"spacegroup":134,"year":114},13126,"\u002Fcif\u002F13126.cif","Moelo 2012","Pb19.13 Bi.1 Sb16.47 As7.06 Tl.24 Ag1.86 Cu1.73 Hg.24 S56","P 1 21\u002Fn 1",[136,137],"IMA1966-020","Sterryiet",[139,143,148,152],{"lang":140,"names":141},"ca",[142],"sterryita",{"lang":144,"names":145},"de",[146,147],"IMA 1966-020","Sterryit",{"lang":149,"names":150},"eu",[151],"Sterryita",{"lang":153,"names":154},"it",[7],"Q3973296",{"history":11,"applications":11}]